var bibbase_data = {"data":"<img src=\"//bibbase.org/img/ajax-loader.gif\" id=\"spinner\"\n  style=\"display: none;\" alt=\"Loading..\" />\n\n<div id=\"bibbase\">\n\n  <script type=\"text/javascript\">\n    var bibbase = {\n      params: {\"bib\":\"https://api.zotero.org/users/1338965/collections/6NAF4EJR/items?key=PkJJchvSOOs0UBX6cmKBYOul&format=bibtex&limit=100\",\"jsonp\":\"1\",\"host\":\"bibbase.org\"},\n      data: [{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Mountain aquatic <i>Isoëtes</i> populations reflect millennial-scale environmental changes in the Bohemian Forest Ecosystem, Central Europe\",\"volume\":\"31\",\"issn\":\"0959-6836\",\"doi\":\"10.1177/0959683620988060\",\"abstract\":\"In this study we aim to investigate millennial-scale dynamics of Isoëtes, a type of macrophyte well adapted to oligotrophic and clear-water lakes. Despite its wide distribution during the Early Holocene, nowadays Isoëtes is considered as vulnerable or critically endangered in many Central European countries. Using a multi-proxy palaeoecological reconstruction involving Isoëtes micro- and megaspores, pollen, plant macrofossils, macro-charcoal, diatoms and chironomids from four lakes (Prášilské jezero, Plešné jezero, Černé jezero, Rachelsee) located in the Bohemian Forest Ecosystem mountain region in Central Europe, we reconstruct Isoëtes dynamics and discuss how local environmental factors impacted its distribution and abundance during the Holocene. Our results show regionally concurrent patterns of Isoëtes colonisation across all lakes beginning 10,300–9300 cal yr BP, and substantially declining around 6400 cal yr BP. Results from Prášilské jezero imply that Isoëtes decline and collapse in this lake reflect gradual dystrophication that led to the browning of lake water. This is evidenced by a shift in diatom assemblages towards more acidophilous taxa dominated by Asterionella ralfsii and by a decrease in total chironomid abundance and taxa sensitive to low oxygen levels. Dystrophication of Prášilské jezero was linked with the immigration of the late-successional tree taxa (Picea abies and later Fagus sylvatica and Abies alba), peatland expansion, and decreasing fire activity. Multi-site comparison of pollen records suggest that these vegetation-related environmental changes were common for the whole region. Our study demonstrates the sensitivity of Isoëtes to millennial-scale natural environmental changes within the surrounding lake catchment.\",\"language\":\"English\",\"number\":\"5\",\"urldate\":\"2021-05-17\",\"journal\":\"The Holocene\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Moravcová\"],\"firstnames\":[\"Alice\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tichá\"],\"firstnames\":[\"Anna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Carter\"],\"firstnames\":[\"Vachel\",\"A\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Vondrák\"],\"firstnames\":[\"Daniel\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Čtvrtlíková\"],\"firstnames\":[\"Martina\"],\"suffixes\":[]},{\"propositions\":[\"van\"],\"lastnames\":[\"Leeuwen\"],\"firstnames\":[\"Jacqueline\",\"FN\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Heurich\"],\"firstnames\":[\"Marco\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tinner\"],\"firstnames\":[\"Willy\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"month\":\"May\",\"year\":\"2021\",\"note\":\"[IF2020=2.769]\",\"keywords\":\"disturbance, fire regime, lake dystrophy, podzolisation, quillwort decline, thermal stratification, vegetation change\",\"pages\":\"746–759\",\"bibtex\":\"@article{moravcova_mountain_2021,\\n\\ttitle = {Mountain aquatic \\\\textit{{Isoëtes}} populations reflect millennial-scale environmental changes in the {Bohemian} {Forest} {Ecosystem}, {Central} {Europe}},\\n\\tvolume = {31},\\n\\tissn = {0959-6836},\\n\\tdoi = {10.1177/0959683620988060},\\n\\tabstract = {In this study we aim to investigate millennial-scale dynamics of Isoëtes, a type of macrophyte well adapted to oligotrophic and clear-water lakes. Despite its wide distribution during the Early Holocene, nowadays Isoëtes is considered as vulnerable or critically endangered in many Central European countries. Using a multi-proxy palaeoecological reconstruction involving Isoëtes micro- and megaspores, pollen, plant macrofossils, macro-charcoal, diatoms and chironomids from four lakes (Prášilské jezero, Plešné jezero, Černé jezero, Rachelsee) located in the Bohemian Forest Ecosystem mountain region in Central Europe, we reconstruct Isoëtes dynamics and discuss how local environmental factors impacted its distribution and abundance during the Holocene. Our results show regionally concurrent patterns of Isoëtes colonisation across all lakes beginning 10,300–9300 cal yr BP, and substantially declining around 6400 cal yr BP. Results from Prášilské jezero imply that Isoëtes decline and collapse in this lake reflect gradual dystrophication that led to the browning of lake water. This is evidenced by a shift in diatom assemblages towards more acidophilous taxa dominated by Asterionella ralfsii and by a decrease in total chironomid abundance and taxa sensitive to low oxygen levels. Dystrophication of Prášilské jezero was linked with the immigration of the late-successional tree taxa (Picea abies and later Fagus sylvatica and Abies alba), peatland expansion, and decreasing fire activity. Multi-site comparison of pollen records suggest that these vegetation-related environmental changes were common for the whole region. Our study demonstrates the sensitivity of Isoëtes to millennial-scale natural environmental changes within the surrounding lake catchment.},\\n\\tlanguage = {English},\\n\\tnumber = {5},\\n\\turldate = {2021-05-17},\\n\\tjournal = {The Holocene},\\n\\tauthor = {Moravcová, Alice and Tichá, Anna and Carter, Vachel A and Vondrák, Daniel and Čtvrtlíková, Martina and van Leeuwen, Jacqueline FN and Heurich, Marco and Tinner, Willy and Kuneš, Petr},\\n\\tmonth = may,\\n\\tyear = {2021},\\n\\tnote = {[IF2020=2.769]},\\n\\tkeywords = {disturbance, fire regime, lake dystrophy, podzolisation, quillwort decline, thermal stratification, vegetation change},\\n\\tpages = {746--759},\\n}\\n\\n\",\"author_short\":[\"Moravcová, A.\",\"Tichá, A.\",\"Carter, V. A\",\"Vondrák, D.\",\"Čtvrtlíková, M.\",\"van Leeuwen, J. F.\",\"Heurich, M.\",\"Tinner, W.\",\"Kuneš, P.\"],\"key\":\"moravcova_mountain_2021\",\"id\":\"moravcova_mountain_2021\",\"bibbaseid\":\"moravcov-tich-carter-vondrk-tvrtlkov-vanleeuwen-heurich-tinner-etal-mountainaquaticiisotesipopulationsreflectmillennialscaleenvironmentalchangesinthebohemianforestecosystemcentraleurope-2021\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"disturbance\",\"fire regime\",\"lake dystrophy\",\"podzolisation\",\"quillwort decline\",\"thermal stratification\",\"vegetation change\"],\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"A new Middle Pleistocene interglacial record from Denmark: Chronostratigraphic correlation, palaeovegetation and fire dynamics\",\"volume\":\"42\",\"copyright\":\"© 2013 The Authors. Boreas © 2013 The Boreas Collegium\",\"issn\":\"1502-3885\",\"shorttitle\":\"A new Middle Pleistocene interglacial record from Denmark\",\"doi\":\"10.1111/bor.12002\",\"abstract\":\"Previously only three terrestrial interglacial periods were known from southern Scandinavia, all of which could be relatively easily correlated within the central European stratigraphical framework. Here, we present a new interglacial–interstadial pollen, plant macrofossil and charcoal record from Trelde Klint, Denmark, and analyse its biostratigraphy, correlation with other European records, vegetation development, fire dynamics and absolute dating. Except for a slight truncation of the early part of the record, the pollen stratigraphy exhibits a full interglacial succession, including temperate trees (Quercus, Ulmus and Tilia) during its mesocratic stage. Macrofossil analysis allowed identification to species level for Quercus robur, Picea abies and two mosses. Conifers (Pinus and Picea) dominate the pollen record of the interglacial sequence, and the occurrence of Larix pollen in the top part of the interglacial record as well as in the interstadial sediments is especially indicative of this interglacial. The overall diversity of tree genera is rather low. These biostratigraphical features suggest that Trelde Klint is unique among Danish records, but it is similar to records from northern Germany. Numerical analyses (REVEALS and DCA) indicate that forests during the temperate stage were dense and that vegetation openness increased only towards the end of the interglacial, accompanied by increased fire occurrence. A short interstadial sequence with a dominance of Pinus and Betula and the presence of Larix is present above the interglacial deposit. We argue that lack of attention to differences in fire regimes may hamper understanding of between-site correlations of interglacial pollen records. OSL dating, using a novel feldspar technique, yields an average age of 350±20 ka for the sandy sediments above the interglacial layers at Trelde Klint, suggesting that the whole interglacial–interstadial succession belongs to Marine Isotope Stage 11.\",\"language\":\"English\",\"number\":\"3\",\"urldate\":\"2013-06-23\",\"journal\":\"Boreas\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kjærsgaard\",\"Sørensen\"],\"firstnames\":[\"Malene\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Buylaert\"],\"firstnames\":[\"Jan-Pieter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Murray\"],\"firstnames\":[\"Andrew\",\"S.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Houmark-Nielsen\"],\"firstnames\":[\"Michael\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Odgaard\"],\"firstnames\":[\"Bent\",\"Vad\"],\"suffixes\":[]}],\"year\":\"2013\",\"note\":\"[IF2012=2.457]\",\"keywords\":\"Denmark, OSL dating, Plant macroremains, REVEALS, charcoal, interglacial, pollen analysis\",\"pages\":\"596–612\",\"bibtex\":\"@article{kunes_new_2013,\\n\\ttitle = {A new {Middle} {Pleistocene} interglacial record from {Denmark}: {Chronostratigraphic} correlation, palaeovegetation and fire dynamics},\\n\\tvolume = {42},\\n\\tcopyright = {© 2013 The Authors. Boreas © 2013 The Boreas Collegium},\\n\\tissn = {1502-3885},\\n\\tshorttitle = {A new {Middle} {Pleistocene} interglacial record from {Denmark}},\\n\\tdoi = {10.1111/bor.12002},\\n\\tabstract = {Previously only three terrestrial interglacial periods were known from southern Scandinavia, all of which could be relatively easily correlated within the central European stratigraphical framework. Here, we present a new interglacial–interstadial pollen, plant macrofossil and charcoal record from Trelde Klint, Denmark, and analyse its biostratigraphy, correlation with other European records, vegetation development, fire dynamics and absolute dating. Except for a slight truncation of the early part of the record, the pollen stratigraphy exhibits a full interglacial succession, including temperate trees (Quercus, Ulmus and Tilia) during its mesocratic stage. Macrofossil analysis allowed identification to species level for Quercus robur, Picea abies and two mosses. Conifers (Pinus and Picea) dominate the pollen record of the interglacial sequence, and the occurrence of Larix pollen in the top part of the interglacial record as well as in the interstadial sediments is especially indicative of this interglacial. The overall diversity of tree genera is rather low. These biostratigraphical features suggest that Trelde Klint is unique among Danish records, but it is similar to records from northern Germany. Numerical analyses (REVEALS and DCA) indicate that forests during the temperate stage were dense and that vegetation openness increased only towards the end of the interglacial, accompanied by increased fire occurrence. A short interstadial sequence with a dominance of Pinus and Betula and the presence of Larix is present above the interglacial deposit. We argue that lack of attention to differences in fire regimes may hamper understanding of between-site correlations of interglacial pollen records. OSL dating, using a novel feldspar technique, yields an average age of 350±20 ka for the sandy sediments above the interglacial layers at Trelde Klint, suggesting that the whole interglacial–interstadial succession belongs to Marine Isotope Stage 11.},\\n\\tlanguage = {English},\\n\\tnumber = {3},\\n\\turldate = {2013-06-23},\\n\\tjournal = {Boreas},\\n\\tauthor = {Kuneš, Petr and Kjærsgaard Sørensen, Malene and Buylaert, Jan-Pieter and Murray, Andrew S. and Houmark-Nielsen, Michael and Odgaard, Bent Vad},\\n\\tyear = {2013},\\n\\tnote = {[IF2012=2.457]},\\n\\tkeywords = {Denmark, OSL dating, Plant macroremains, REVEALS, charcoal, interglacial, pollen analysis},\\n\\tpages = {596--612},\\n}\\n\\n\",\"author_short\":[\"Kuneš, P.\",\"Kjærsgaard Sørensen, M.\",\"Buylaert, J.\",\"Murray, A. S.\",\"Houmark-Nielsen, M.\",\"Odgaard, B. V.\"],\"key\":\"kunes_new_2013\",\"id\":\"kunes_new_2013\",\"bibbaseid\":\"kune-kjrsgaardsrensen-buylaert-murray-houmarknielsen-odgaard-anewmiddlepleistoceneinterglacialrecordfromdenmarkchronostratigraphiccorrelationpalaeovegetationandfiredynamics-2013\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Denmark\",\"OSL dating\",\"Plant macroremains\",\"REVEALS\",\"charcoal\",\"interglacial\",\"pollen analysis\"],\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Insight into the environment of a pre-Roman Iron Age hillfort at Vladař, Czech Republic, using a multi-proxy approach\",\"volume\":\"15\",\"copyright\":\"All rights reserved\",\"issn\":\"0939-6314, 1617-6278\",\"doi\":\"10.1007/s00334-006-0064-8\",\"language\":\"English\",\"number\":\"4\",\"urldate\":\"2012-01-05\",\"journal\":\"Vegetation History and Archaeobotany\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Pokorný\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Boenke\"],\"firstnames\":[\"Nicole\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chytráček\"],\"firstnames\":[\"Miloslav\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Nováková\"],\"firstnames\":[\"Kateřina\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Sádlo\"],\"firstnames\":[\"Jiří\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Veselý\"],\"firstnames\":[\"Josef\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jankovská\"],\"firstnames\":[\"Vlasta\"],\"suffixes\":[]}],\"month\":\"July\",\"year\":\"2006\",\"note\":\"[IF2005=0.739]\",\"keywords\":\"Czech Republic, Plant macroremains, archeology, cladocera, human impact, pollen analysis\",\"pages\":\"419–433\",\"bibtex\":\"@article{pokorny_insight_2006,\\n\\ttitle = {Insight into the environment of a pre-{Roman} {Iron} {Age} hillfort at {Vladař}, {Czech} {Republic}, using a multi-proxy approach},\\n\\tvolume = {15},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {0939-6314, 1617-6278},\\n\\tdoi = {10.1007/s00334-006-0064-8},\\n\\tlanguage = {English},\\n\\tnumber = {4},\\n\\turldate = {2012-01-05},\\n\\tjournal = {Vegetation History and Archaeobotany},\\n\\tauthor = {Pokorný, Petr and Boenke, Nicole and Chytráček, Miloslav and Nováková, Kateřina and Sádlo, Jiří and Veselý, Josef and Kuneš, Petr and Jankovská, Vlasta},\\n\\tmonth = jul,\\n\\tyear = {2006},\\n\\tnote = {[IF2005=0.739]},\\n\\tkeywords = {Czech Republic, Plant macroremains, archeology, cladocera, human impact, pollen analysis},\\n\\tpages = {419--433},\\n}\\n\\n\",\"author_short\":[\"Pokorný, P.\",\"Boenke, N.\",\"Chytráček, M.\",\"Nováková, K.\",\"Sádlo, J.\",\"Veselý, J.\",\"Kuneš, P.\",\"Jankovská, V.\"],\"key\":\"pokorny_insight_2006\",\"id\":\"pokorny_insight_2006\",\"bibbaseid\":\"pokorn-boenke-chytrek-novkov-sdlo-vesel-kune-jankovsk-insightintotheenvironmentofapreromanironagehillfortatvladaczechrepublicusingamultiproxyapproach-2006\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Czech Republic\",\"Plant macroremains\",\"archeology\",\"cladocera\",\"human impact\",\"pollen analysis\"],\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Conservation targets from the perspective of a palaeoecological reconstruction: the case study of Dářko peat bog in the Czech Republic\",\"volume\":\"92\",\"doi\":\"10.23855/preslia.2020.087\",\"language\":\"English\",\"number\":\"2\",\"journal\":\"Preslia\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Roleček\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svitavská\",\"Svobodová\"],\"firstnames\":[\"Helena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jamrichová\"],\"firstnames\":[\"Eva\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Dudová\"],\"firstnames\":[\"Lydie\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hájková\"],\"firstnames\":[\"Petra\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kletetschka\"],\"firstnames\":[\"Günther\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Abraham\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]}],\"year\":\"2020\",\"note\":\"[IF2019=4.357]\",\"keywords\":\"conservation\",\"pages\":\"87–114\",\"bibtex\":\"@article{rolecek_conservation_2020,\\n\\ttitle = {Conservation targets from the perspective of a palaeoecological reconstruction: the case study of {Dářko} peat bog in the {Czech} {Republic}},\\n\\tvolume = {92},\\n\\tdoi = {10.23855/preslia.2020.087},\\n\\tlanguage = {English},\\n\\tnumber = {2},\\n\\tjournal = {Preslia},\\n\\tauthor = {Roleček, Jan and Svitavská Svobodová, Helena and Jamrichová, Eva and Dudová, Lydie and Hájková, Petra and Kletetschka, Günther and Kuneš, Petr and Abraham, Vojtěch},\\n\\tyear = {2020},\\n\\tnote = {[IF2019=4.357]},\\n\\tkeywords = {conservation},\\n\\tpages = {87--114},\\n}\\n\\n\",\"author_short\":[\"Roleček, J.\",\"Svitavská Svobodová, H.\",\"Jamrichová, E.\",\"Dudová, L.\",\"Hájková, P.\",\"Kletetschka, G.\",\"Kuneš, P.\",\"Abraham, V.\"],\"key\":\"rolecek_conservation_2020\",\"id\":\"rolecek_conservation_2020\",\"bibbaseid\":\"roleek-svitavsksvobodov-jamrichov-dudov-hjkov-kletetschka-kune-abraham-conservationtargetsfromtheperspectiveofapalaeoecologicalreconstructionthecasestudyofdkopeatbogintheczechrepublic-2020\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"conservation\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":2,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Millennial scale perspective on biodiversity conservation of the forest-steppe ecotone in Europe\",\"volume\":\"30\",\"issn\":\"2411605X, 24119180\",\"doi\":\"10.22498/pages.30.1.24\",\"number\":\"1\",\"urldate\":\"2022-04-05\",\"journal\":\"Past Global Changes Magazine\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Giesecke\"],\"firstnames\":[\"Thomas\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Shumilovskikh\"],\"firstnames\":[\"Lyudmila\"],\"suffixes\":[]}],\"month\":\"April\",\"year\":\"2022\",\"keywords\":\"conservation\",\"pages\":\"24–25\",\"bibtex\":\"@article{giesecke_millennial_2022,\\n\\ttitle = {Millennial scale perspective on biodiversity conservation of the forest-steppe ecotone in {Europe}},\\n\\tvolume = {30},\\n\\tissn = {2411605X, 24119180},\\n\\tdoi = {10.22498/pages.30.1.24},\\n\\tnumber = {1},\\n\\turldate = {2022-04-05},\\n\\tjournal = {Past Global Changes Magazine},\\n\\tauthor = {Giesecke, Thomas and Kuneš, Petr and Shumilovskikh, Lyudmila},\\n\\tmonth = apr,\\n\\tyear = {2022},\\n\\tkeywords = {conservation},\\n\\tpages = {24--25},\\n}\\n\\n\",\"author_short\":[\"Giesecke, T.\",\"Kuneš, P.\",\"Shumilovskikh, L.\"],\"key\":\"giesecke_millennial_2022\",\"id\":\"giesecke_millennial_2022\",\"bibbaseid\":\"giesecke-kune-shumilovskikh-millennialscaleperspectiveonbiodiversityconservationoftheforeststeppeecotoneineurope-2022\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"conservation\"],\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Population and forest dynamics during the Central European Eneolithic (4500–2000 BC)\",\"volume\":\"10\",\"copyright\":\"All rights reserved\",\"issn\":\"1866-9557, 1866-9565\",\"doi\":\"10.1007/s12520-016-0446-5\",\"abstract\":\"The population boom-and-bust during the European Neolithic (7000–2000 BC) has been the subject of lively discussion for the past decade. Most of the research on this topic was carried out with help of summed radiocarbon probability distributions. We aim to reconstruct population dynamics within the catchment of a medium sized lake on the basis of information on the presence of all known past human activities. We calculated a human activity model based on Monte Carlo simulations. The model showed the lowest level of human activity between 4000 and 3000 BC. For a better understanding of long-term socio-environmental dynamics, we also used the results of a pollen-based quantitative vegetation model, as well as a local macrophysical climate model. The beginning of the decline of archaeologically visible human activities corresponds with climatic changes and an increase in secondary forest taxa probably indicating more extensive land use. In addition, social and technological innovations are important, such as the introduction of the ard, wheel, animal traction and metallurgy, as well as changes in social hierarchy characterizing the same period.\",\"language\":\"English\",\"number\":\"5\",\"urldate\":\"2016-12-14\",\"journal\":\"Archaeological and Anthropological Sciences\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kolář\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Szabó\"],\"firstnames\":[\"Péter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hajnalová\"],\"firstnames\":[\"Mária\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svobodová\"],\"firstnames\":[\"Helena\",\"Svitavská\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Macek\"],\"firstnames\":[\"Martin\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tkáč\"],\"firstnames\":[\"Peter\"],\"suffixes\":[]}],\"month\":\"August\",\"year\":\"2018\",\"note\":\"[IF2017=2.414]\",\"keywords\":\"Czech Republic, MCM model, Neolithic, Population density, REVEALS, climate, conservation, cultural landscape, reconstruction\",\"pages\":\"1153–1164\",\"bibtex\":\"@article{kolar_population_2018,\\n\\ttitle = {Population and forest dynamics during the {Central} {European} {Eneolithic} (4500–2000 {BC})},\\n\\tvolume = {10},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {1866-9557, 1866-9565},\\n\\tdoi = {10.1007/s12520-016-0446-5},\\n\\tabstract = {The population boom-and-bust during the European Neolithic (7000–2000 BC) has been the subject of lively discussion for the past decade. Most of the research on this topic was carried out with help of summed radiocarbon probability distributions. We aim to reconstruct population dynamics within the catchment of a medium sized lake on the basis of information on the presence of all known past human activities. We calculated a human activity model based on Monte Carlo simulations. The model showed the lowest level of human activity between 4000 and 3000 BC. For a better understanding of long-term socio-environmental dynamics, we also used the results of a pollen-based quantitative vegetation model, as well as a local macrophysical climate model. The beginning of the decline of archaeologically visible human activities corresponds with climatic changes and an increase in secondary forest taxa probably indicating more extensive land use. In addition, social and technological innovations are important, such as the introduction of the ard, wheel, animal traction and metallurgy, as well as changes in social hierarchy characterizing the same period.},\\n\\tlanguage = {English},\\n\\tnumber = {5},\\n\\turldate = {2016-12-14},\\n\\tjournal = {Archaeological and Anthropological Sciences},\\n\\tauthor = {Kolář, Jan and Kuneš, Petr and Szabó, Péter and Hajnalová, Mária and Svobodová, Helena Svitavská and Macek, Martin and Tkáč, Peter},\\n\\tmonth = aug,\\n\\tyear = {2018},\\n\\tnote = {[IF2017=2.414]},\\n\\tkeywords = {Czech Republic, MCM model, Neolithic, Population density, REVEALS, climate, conservation, cultural landscape, reconstruction},\\n\\tpages = {1153--1164},\\n}\\n\\n\",\"author_short\":[\"Kolář, J.\",\"Kuneš, P.\",\"Szabó, P.\",\"Hajnalová, M.\",\"Svobodová, H. S.\",\"Macek, M.\",\"Tkáč, P.\"],\"key\":\"kolar_population_2018\",\"id\":\"kolar_population_2018\",\"bibbaseid\":\"kol-kune-szab-hajnalov-svobodov-macek-tk-populationandforestdynamicsduringthecentraleuropeaneneolithic45002000bc-2018\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Czech Republic\",\"MCM model\",\"Neolithic\",\"Population density\",\"REVEALS\",\"climate\",\"conservation\",\"cultural landscape\",\"reconstruction\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Using historical ecology to reassess the conservation status of coniferous forests in Central Europe\",\"volume\":\"31\",\"copyright\":\"All rights reserved\",\"issn\":\"1523-1739\",\"doi\":\"10.1111/cobi.12763\",\"abstract\":\"Forests cover approximately one-third of Central Europe. Oak (Quercus) and European beech (Fagus sylvatica) are considered the natural dominants at low and middle elevations, respectively. Many coniferous forests (especially of Picea abies) occur primarily at midelevations, but these are thought to have resulted from forestry plantations planted over the past 200 years. Nature conservation and forestry policy seek to promote broadleaved trees over conifers. However, there are discrepancies between conservation guidelines (included in Natura 2000) and historical and palaeoecological data with regard to the distribution of conifers. Our aim was to bring new evidence to the debate on the conservation of conifers versus broadleaved trees at midelevations in Central Europe. We created a vegetation and land-cover model based on pollen data for a highland area of 11,300 km2 in the Czech Republic and assessed tree species composition in the forests before the onset of modern forestry based on 18th-century archival sources. Conifers dominated the study region throughout the entire Holocene (approximately 40–60% of the area). Broadleaved trees were present in a much smaller area than envisaged by current ideas of natural vegetation. Rather than casting doubt on the principles of Central European nature conservation in general, our results highlight the necessity of detailed regional investigations and the importance of historical data in challenging established notions on the natural distribution of tree species.\",\"language\":\"English\",\"number\":\"1\",\"urldate\":\"2017-01-26\",\"journal\":\"Conservation Biology\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Szabó\"],\"firstnames\":[\"Péter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svobodová‐Svitavská\"],\"firstnames\":[\"Helena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Švarcová\"],\"firstnames\":[\"Markéta\",\"Gabriela\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Křížová\"],\"firstnames\":[\"Lucie\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Suchánková\"],\"firstnames\":[\"Silvie\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Müllerová\"],\"firstnames\":[\"Jana\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hédl\"],\"firstnames\":[\"Radim\"],\"suffixes\":[]}],\"month\":\"February\",\"year\":\"2017\",\"note\":\"[IF2016=4.842]\",\"keywords\":\"Czech Republic, Historical ecology, Holocene, LRA, REVEALS, conservation, interdisciplinarity, potential natural vegetation, reconstruction\",\"pages\":\"150–160\",\"bibtex\":\"@article{szabo_using_2017,\\n\\ttitle = {Using historical ecology to reassess the conservation status of coniferous forests in {Central} {Europe}},\\n\\tvolume = {31},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {1523-1739},\\n\\tdoi = {10.1111/cobi.12763},\\n\\tabstract = {Forests cover approximately one-third of Central Europe. Oak (Quercus) and European beech (Fagus sylvatica) are considered the natural dominants at low and middle elevations, respectively. Many coniferous forests (especially of Picea abies) occur primarily at midelevations, but these are thought to have resulted from forestry plantations planted over the past 200 years. Nature conservation and forestry policy seek to promote broadleaved trees over conifers. However, there are discrepancies between conservation guidelines (included in Natura 2000) and historical and palaeoecological data with regard to the distribution of conifers. Our aim was to bring new evidence to the debate on the conservation of conifers versus broadleaved trees at midelevations in Central Europe. We created a vegetation and land-cover model based on pollen data for a highland area of 11,300 km2 in the Czech Republic and assessed tree species composition in the forests before the onset of modern forestry based on 18th-century archival sources. Conifers dominated the study region throughout the entire Holocene (approximately 40–60\\\\% of the area). Broadleaved trees were present in a much smaller area than envisaged by current ideas of natural vegetation. Rather than casting doubt on the principles of Central European nature conservation in general, our results highlight the necessity of detailed regional investigations and the importance of historical data in challenging established notions on the natural distribution of tree species.},\\n\\tlanguage = {English},\\n\\tnumber = {1},\\n\\turldate = {2017-01-26},\\n\\tjournal = {Conservation Biology},\\n\\tauthor = {Szabó, Péter and Kuneš, Petr and Svobodová‐Svitavská, Helena and Švarcová, Markéta Gabriela and Křížová, Lucie and Suchánková, Silvie and Müllerová, Jana and Hédl, Radim},\\n\\tmonth = feb,\\n\\tyear = {2017},\\n\\tnote = {[IF2016=4.842]},\\n\\tkeywords = {Czech Republic, Historical ecology, Holocene, LRA, REVEALS, conservation, interdisciplinarity, potential natural vegetation, reconstruction},\\n\\tpages = {150--160},\\n}\\n\\n\",\"author_short\":[\"Szabó, P.\",\"Kuneš, P.\",\"Svobodová‐Svitavská, H.\",\"Švarcová, M. G.\",\"Křížová, L.\",\"Suchánková, S.\",\"Müllerová, J.\",\"Hédl, R.\"],\"key\":\"szabo_using_2017\",\"id\":\"szabo_using_2017\",\"bibbaseid\":\"szab-kune-svobodovsvitavsk-varcov-kov-suchnkov-mllerov-hdl-usinghistoricalecologytoreassesstheconservationstatusofconiferousforestsincentraleurope-2017\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Czech Republic\",\"Historical ecology\",\"Holocene\",\"LRA\",\"REVEALS\",\"conservation\",\"interdisciplinarity\",\"potential natural vegetation\",\"reconstruction\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":3,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"A pollen-based quantitative reconstruction of the Holocene vegetation updates a perspective on the natural vegetation in the Czech Republic and Slovakia\",\"volume\":\"88\",\"copyright\":\"All rights reserved\",\"url\":\"http://www.preslia.cz/P164Abraham.pdf\",\"language\":\"English\",\"number\":\"4\",\"journal\":\"Preslia\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Abraham\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Petr\"],\"firstnames\":[\"Libor\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svitavská-Svobodová\"],\"firstnames\":[\"Helena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kozáková\"],\"firstnames\":[\"Radka\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jamrichová\"],\"firstnames\":[\"Eva\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Švarcová\"],\"firstnames\":[\"Markéta\",\"Gabriela\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pokorný\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"year\":\"2016\",\"note\":\"[IF2015=2.711]\",\"keywords\":\"Czech Republic, Database, Holocene, LRA, REVEALS, Slovakia, conservation, pollen data, potential natural vegetation, reconstruction\",\"pages\":\"409–434\",\"bibtex\":\"@article{abraham_pollen-based_2016,\\n\\ttitle = {A pollen-based quantitative reconstruction of the {Holocene} vegetation updates a perspective on the natural vegetation in the {Czech} {Republic} and {Slovakia}},\\n\\tvolume = {88},\\n\\tcopyright = {All rights reserved},\\n\\turl = {http://www.preslia.cz/P164Abraham.pdf},\\n\\tlanguage = {English},\\n\\tnumber = {4},\\n\\tjournal = {Preslia},\\n\\tauthor = {Abraham, Vojtěch and Kuneš, Petr and Petr, Libor and Svitavská-Svobodová, Helena and Kozáková, Radka and Jamrichová, Eva and Švarcová, Markéta Gabriela and Pokorný, Petr},\\n\\tyear = {2016},\\n\\tnote = {[IF2015=2.711]},\\n\\tkeywords = {Czech Republic, Database, Holocene, LRA, REVEALS, Slovakia, conservation, pollen data, potential natural vegetation, reconstruction},\\n\\tpages = {409--434},\\n}\\n\\n\",\"author_short\":[\"Abraham, V.\",\"Kuneš, P.\",\"Petr, L.\",\"Svitavská-Svobodová, H.\",\"Kozáková, R.\",\"Jamrichová, E.\",\"Švarcová, M. G.\",\"Pokorný, P.\"],\"key\":\"abraham_pollen-based_2016\",\"id\":\"abraham_pollen-based_2016\",\"bibbaseid\":\"abraham-kune-petr-svitavsksvobodov-kozkov-jamrichov-varcov-pokorn-apollenbasedquantitativereconstructionoftheholocenevegetationupdatesaperspectiveonthenaturalvegetationintheczechrepublicandslovakia-2016\",\"role\":\"author\",\"urls\":{\"Paper\":\"http://www.preslia.cz/P164Abraham.pdf\"},\"keyword\":[\"Czech Republic\",\"Database\",\"Holocene\",\"LRA\",\"REVEALS\",\"Slovakia\",\"conservation\",\"pollen data\",\"potential natural vegetation\",\"reconstruction\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"The origin of grasslands in the temperate forest zone of east-central Europe: long-term legacy of climate and human impact\",\"volume\":\"116\",\"copyright\":\"All rights reserved\",\"issn\":\"0277-3791\",\"shorttitle\":\"The origin of grasslands in the temperate forest zone of east-central Europe\",\"doi\":\"10.1016/j.quascirev.2015.03.014\",\"abstract\":\"The post-glacial fate of central European grasslands has stimulated palaeoecological debates for a century. Some argued for the continuous survival of open land, while others claimed that closed forest had developed during the Middle Holocene. The reasons behind stability or changes in the proportion of open land are also unclear. We aim to reconstruct regional vegetation openness and test the effects of climate and human impact on vegetation change throughout the Holocene. We present a newly dated pollen record from north-western fringes of the Pannonian Plain, east-central Europe, and reconstruct Holocene regional vegetation development by the REVEALS model for 27 pollen-equivalent taxa. Estimated vegetation is correlated in the same area with a human activity model based on all available archaeological information and a macrophysical climate model. The palaeovegetation record indicates the continuous presence of open land throughout the Holocene. Grasslands and open woodlands were probably maintained by local arid climatic conditions during the early Holocene delaying the spread of deciduous (oak) forests. Significantly detectable human-made landscape transformation started only after 2000 BC. Our analyses suggest that Neolithic people spread into a landscape that was already open. Humans probably contributed to the spread of oak, and influenced the dynamics of hazel and hornbeam.\",\"language\":\"English\",\"urldate\":\"2015-04-09\",\"journal\":\"Quaternary Science Reviews\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svobodová-Svitavská\"],\"firstnames\":[\"Helena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kolář\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hajnalová\"],\"firstnames\":[\"Mária\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Abraham\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Macek\"],\"firstnames\":[\"Martin\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tkáč\"],\"firstnames\":[\"Peter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Szabó\"],\"firstnames\":[\"Péter\"],\"suffixes\":[]}],\"month\":\"May\",\"year\":\"2015\",\"note\":\"[IF2014=4.572]\",\"keywords\":\"Carpathian Basin, Czech Republic, Holocene, LRA, MCM model, REVEALS, conservation, pollen analysis, quantitative vegetation reconstruction\",\"pages\":\"15–27\",\"bibtex\":\"@article{kunes_origin_2015,\\n\\ttitle = {The origin of grasslands in the temperate forest zone of east-central {Europe}: long-term legacy of climate and human impact},\\n\\tvolume = {116},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {0277-3791},\\n\\tshorttitle = {The origin of grasslands in the temperate forest zone of east-central {Europe}},\\n\\tdoi = {10.1016/j.quascirev.2015.03.014},\\n\\tabstract = {The post-glacial fate of central European grasslands has stimulated palaeoecological debates for a century. Some argued for the continuous survival of open land, while others claimed that closed forest had developed during the Middle Holocene. The reasons behind stability or changes in the proportion of open land are also unclear. We aim to reconstruct regional vegetation openness and test the effects of climate and human impact on vegetation change throughout the Holocene. We present a newly dated pollen record from north-western fringes of the Pannonian Plain, east-central Europe, and reconstruct Holocene regional vegetation development by the REVEALS model for 27 pollen-equivalent taxa. Estimated vegetation is correlated in the same area with a human activity model based on all available archaeological information and a macrophysical climate model. The palaeovegetation record indicates the continuous presence of open land throughout the Holocene. Grasslands and open woodlands were probably maintained by local arid climatic conditions during the early Holocene delaying the spread of deciduous (oak) forests. Significantly detectable human-made landscape transformation started only after 2000 BC. Our analyses suggest that Neolithic people spread into a landscape that was already open. Humans probably contributed to the spread of oak, and influenced the dynamics of hazel and hornbeam.},\\n\\tlanguage = {English},\\n\\turldate = {2015-04-09},\\n\\tjournal = {Quaternary Science Reviews},\\n\\tauthor = {Kuneš, Petr and Svobodová-Svitavská, Helena and Kolář, Jan and Hajnalová, Mária and Abraham, Vojtěch and Macek, Martin and Tkáč, Peter and Szabó, Péter},\\n\\tmonth = may,\\n\\tyear = {2015},\\n\\tnote = {[IF2014=4.572]},\\n\\tkeywords = {Carpathian Basin, Czech Republic, Holocene, LRA, MCM model, REVEALS, conservation, pollen analysis, quantitative vegetation reconstruction},\\n\\tpages = {15--27},\\n}\\n\\n\",\"author_short\":[\"Kuneš, P.\",\"Svobodová-Svitavská, H.\",\"Kolář, J.\",\"Hajnalová, M.\",\"Abraham, V.\",\"Macek, M.\",\"Tkáč, P.\",\"Szabó, P.\"],\"key\":\"kunes_origin_2015\",\"id\":\"kunes_origin_2015\",\"bibbaseid\":\"kune-svobodovsvitavsk-kol-hajnalov-abraham-macek-tk-szab-theoriginofgrasslandsinthetemperateforestzoneofeastcentraleuropelongtermlegacyofclimateandhumanimpact-2015\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Carpathian Basin\",\"Czech Republic\",\"Holocene\",\"LRA\",\"MCM model\",\"REVEALS\",\"conservation\",\"pollen analysis\",\"quantitative vegetation reconstruction\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":2,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Early occurrence of temperate oak-dominated forest in the northern part of the Little Hungarian Plain, SW Slovakia\",\"volume\":\"24\",\"copyright\":\"All rights reserved\",\"issn\":\"0959-6836, 1477-0911\",\"doi\":\"10.1177/0959683614551225\",\"abstract\":\"Using a multi-proxy analysis of a postglacial sedimentary sequence from a lowland wetland, we address the possible drivers of change in the wetland habitats and surrounding landscapes of southwestern Slovakia. A 5 m-deep core in the Parížske močiare marshes was investigated for pollen, plant macro-remains, molluscs, organic content and magnetic susceptibility. The palaeoecological record extends from the Pleistocene–Holocene transition (≥11,200 cal. BP) to the 5th millennium cal. BP and was correlated with a macrophysical climate model (MCM) and archaeological data. Our results show the transformation of an open parkland landscape with patches of coniferous forest to a temperate deciduous forest at the onset of the Holocene. The record is remarkable for an early occurrence of Quercus pollen and macro-remains around 11,200 cal. BP and its early expansion (10,390 cal. BP) in the vegetation. Such an early spread of Quercus has not previously been recorded in the region, where Corylus is usually the first to expand among temperate trees. This unusual development of forest communities was most probably triggered by a short-lived increase in precipitation and decrease in temperature, as reconstructed by the MCM model. Higher moisture availability and low temperature inhibited Corylus and favoured the spread of Quercus. Later, the climate became drier and warmer, which, together with fires, supported the expansion of Corylus. Since 7300 cal. BP, human activities became most likely the dominant influence on the landscape. Deforestation contributed to soil erosion, which halted the accumulation of organic material after 5520 cal. BP, followed by the accumulation of clay sediments.\",\"language\":\"English\",\"number\":\"12\",\"urldate\":\"2014-12-10\",\"journal\":\"The Holocene\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Jamrichová\"],\"firstnames\":[\"Eva\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Potůčková\"],\"firstnames\":[\"Anna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Horsák\"],\"firstnames\":[\"Michal\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hajnalová\"],\"firstnames\":[\"Mária\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Barta\"],\"firstnames\":[\"Peter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tóth\"],\"firstnames\":[\"Peter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"month\":\"December\",\"year\":\"2014\",\"note\":\"[IF2013=3.794]\",\"keywords\":\"Lowland vegetation, MCM model, Palaeoecology, Plant macroremains, Slovakia, climate, conservation, cultural landscape, human impact, multi-proxy, pollen analysis\",\"pages\":\"1810–1824\",\"bibtex\":\"@article{jamrichova_early_2014,\\n\\ttitle = {Early occurrence of temperate oak-dominated forest in the northern part of the {Little} {Hungarian} {Plain}, {SW} {Slovakia}},\\n\\tvolume = {24},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {0959-6836, 1477-0911},\\n\\tdoi = {10.1177/0959683614551225},\\n\\tabstract = {Using a multi-proxy analysis of a postglacial sedimentary sequence from a lowland wetland, we address the possible drivers of change in the wetland habitats and surrounding landscapes of southwestern Slovakia. A 5 m-deep core in the Parížske močiare marshes was investigated for pollen, plant macro-remains, molluscs, organic content and magnetic susceptibility. The palaeoecological record extends from the Pleistocene–Holocene transition (≥11,200 cal. BP) to the 5th millennium cal. BP and was correlated with a macrophysical climate model (MCM) and archaeological data. Our results show the transformation of an open parkland landscape with patches of coniferous forest to a temperate deciduous forest at the onset of the Holocene. The record is remarkable for an early occurrence of Quercus pollen and macro-remains around 11,200 cal. BP and its early expansion (10,390 cal. BP) in the vegetation. Such an early spread of Quercus has not previously been recorded in the region, where Corylus is usually the first to expand among temperate trees. This unusual development of forest communities was most probably triggered by a short-lived increase in precipitation and decrease in temperature, as reconstructed by the MCM model. Higher moisture availability and low temperature inhibited Corylus and favoured the spread of Quercus. Later, the climate became drier and warmer, which, together with fires, supported the expansion of Corylus. Since 7300 cal. BP, human activities became most likely the dominant influence on the landscape. Deforestation contributed to soil erosion, which halted the accumulation of organic material after 5520 cal. BP, followed by the accumulation of clay sediments.},\\n\\tlanguage = {English},\\n\\tnumber = {12},\\n\\turldate = {2014-12-10},\\n\\tjournal = {The Holocene},\\n\\tauthor = {Jamrichová, Eva and Potůčková, Anna and Horsák, Michal and Hajnalová, Mária and Barta, Peter and Tóth, Peter and Kuneš, Petr},\\n\\tmonth = dec,\\n\\tyear = {2014},\\n\\tnote = {[IF2013=3.794]},\\n\\tkeywords = {Lowland vegetation, MCM model, Palaeoecology, Plant macroremains, Slovakia, climate, conservation, cultural landscape, human impact, multi-proxy, pollen analysis},\\n\\tpages = {1810--1824},\\n}\\n\\n\",\"author_short\":[\"Jamrichová, E.\",\"Potůčková, A.\",\"Horsák, M.\",\"Hajnalová, M.\",\"Barta, P.\",\"Tóth, P.\",\"Kuneš, P.\"],\"key\":\"jamrichova_early_2014\",\"id\":\"jamrichova_early_2014\",\"bibbaseid\":\"jamrichov-potkov-horsk-hajnalov-barta-tth-kune-earlyoccurrenceoftemperateoakdominatedforestinthenorthernpartofthelittlehungarianplainswslovakia-2014\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Lowland vegetation\",\"MCM model\",\"Palaeoecology\",\"Plant macroremains\",\"Slovakia\",\"climate\",\"conservation\",\"cultural landscape\",\"human impact\",\"multi-proxy\",\"pollen analysis\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Continuity and change in the vegetation of a Central European oakwood\",\"volume\":\"23\",\"copyright\":\"All rights reserved\",\"issn\":\"0959-6836, 1477-0911\",\"doi\":\"10.1177/0959683612450200\",\"abstract\":\"The issue of continuity in deciduous oakwood vegetation has been in the forefront of woodland ecological studies for many decades. The two basic questions that emerge from existing research are whether or not oakwoods can be characterized by long-term stability and what may be the driving forces of the observed stability or change. To answer these questions in a well-defined case study, we examined the history of a large subcontinental oakwood (Dúbrava) in the southeastern Czech Republic with interdisciplinary methods using palaeoecological and archival sources. Palaeoecology allowed us to reconstruct the vegetation composition and fire disturbances in Dúbrava in the past 2000 years, while written sources provided information about tree composition and management from the 14th century onwards. The pollen profiles show that the present oakwood was established in the mid-14th century with an abrupt change from shrubby, hazel-dominated vegetation to oak forest. This change was most probably caused by a ban on oak felling in ad 1350. From the 14th to the late 18th centuries Dúbrava had multiple uses, of which wood-pasture and hay-cutting kept the forest considerably open. The second remarkable change was dated to the late 18th century, when multiple-use management was abandoned and Dúbrava was divided into pasture-only and coppice-only parts. The last major shift occurred in the mid-19th century, when modern forestry and Scotch pine plantation became dominant. We conclude that Dúbrava Wood did not show stability in the long run and that its species composition has dramatically changed during the last two millennia. The most important driving force in the shaping and maintenance of the unique vegetation of Dúbrava was human management.\",\"language\":\"English\",\"number\":\"1\",\"urldate\":\"2012-12-20\",\"journal\":\"The Holocene\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Jamrichová\"],\"firstnames\":[\"Eva\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Szabó\"],\"firstnames\":[\"Péter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hédl\"],\"firstnames\":[\"Radim\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bobek\"],\"firstnames\":[\"Přemysl\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pelánková\"],\"firstnames\":[\"Barbora\"],\"suffixes\":[]}],\"month\":\"January\",\"year\":\"2013\",\"note\":\"[IF2012=3.218]\",\"keywords\":\"Historical ecology, conservation, ecosystem stability, management history, pollen analysis, temperate oakwood\",\"pages\":\"46–56\",\"bibtex\":\"@article{jamrichova_continuity_2013,\\n\\ttitle = {Continuity and change in the vegetation of a {Central} {European} oakwood},\\n\\tvolume = {23},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {0959-6836, 1477-0911},\\n\\tdoi = {10.1177/0959683612450200},\\n\\tabstract = {The issue of continuity in deciduous oakwood vegetation has been in the forefront of woodland ecological studies for many decades. The two basic questions that emerge from existing research are whether or not oakwoods can be characterized by long-term stability and what may be the driving forces of the observed stability or change. To answer these questions in a well-defined case study, we examined the history of a large subcontinental oakwood (Dúbrava) in the southeastern Czech Republic with interdisciplinary methods using palaeoecological and archival sources. Palaeoecology allowed us to reconstruct the vegetation composition and fire disturbances in Dúbrava in the past 2000 years, while written sources provided information about tree composition and management from the 14th century onwards. The pollen profiles show that the present oakwood was established in the mid-14th century with an abrupt change from shrubby, hazel-dominated vegetation to oak forest. This change was most probably caused by a ban on oak felling in ad 1350. From the 14th to the late 18th centuries Dúbrava had multiple uses, of which wood-pasture and hay-cutting kept the forest considerably open. The second remarkable change was dated to the late 18th century, when multiple-use management was abandoned and Dúbrava was divided into pasture-only and coppice-only parts. The last major shift occurred in the mid-19th century, when modern forestry and Scotch pine plantation became dominant. We conclude that Dúbrava Wood did not show stability in the long run and that its species composition has dramatically changed during the last two millennia. The most important driving force in the shaping and maintenance of the unique vegetation of Dúbrava was human management.},\\n\\tlanguage = {English},\\n\\tnumber = {1},\\n\\turldate = {2012-12-20},\\n\\tjournal = {The Holocene},\\n\\tauthor = {Jamrichová, Eva and Szabó, Péter and Hédl, Radim and Kuneš, Petr and Bobek, Přemysl and Pelánková, Barbora},\\n\\tmonth = jan,\\n\\tyear = {2013},\\n\\tnote = {[IF2012=3.218]},\\n\\tkeywords = {Historical ecology, conservation, ecosystem stability, management history, pollen analysis, temperate oakwood},\\n\\tpages = {46--56},\\n}\\n\\n\",\"author_short\":[\"Jamrichová, E.\",\"Szabó, P.\",\"Hédl, R.\",\"Kuneš, P.\",\"Bobek, P.\",\"Pelánková, B.\"],\"key\":\"jamrichova_continuity_2013\",\"id\":\"jamrichova_continuity_2013\",\"bibbaseid\":\"jamrichov-szab-hdl-kune-bobek-pelnkov-continuityandchangeinthevegetationofacentraleuropeanoakwood-2013\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Historical ecology\",\"conservation\",\"ecosystem stability\",\"management history\",\"pollen analysis\",\"temperate oakwood\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Dosavadní výsledky paleoekologických výzkumů v Ašském výběžku – podklady pro ochranu přírody\",\"volume\":\"30\",\"issn\":\"1803-6066\",\"language\":\"Czech\",\"journal\":\"Sborník muzea Karlovarského kraje\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bobek\"],\"firstnames\":[\"Přemysl\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svobodová-Svitavská\"],\"firstnames\":[\"Helena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Švarcová\"],\"firstnames\":[\"Markéta\",\"G\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Šulc\"],\"firstnames\":[\"Václav\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Šturma\"],\"firstnames\":[\"Jan\",\"Albert\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Smrtová\"],\"firstnames\":[\"Erika\"],\"suffixes\":[]}],\"year\":\"2022\",\"pages\":\"131–150\",\"bibtex\":\"@article{kunes_dosavadni_2022,\\n\\ttitle = {Dosavadní výsledky paleoekologických výzkumů v {Ašském} výběžku – podklady pro ochranu přírody},\\n\\tvolume = {30},\\n\\tissn = {1803-6066},\\n\\tlanguage = {Czech},\\n\\tjournal = {Sborník muzea Karlovarského kraje},\\n\\tauthor = {Kuneš, Petr and Bobek, Přemysl and Svobodová-Svitavská, Helena and Švarcová, Markéta G and Šulc, Václav and Šturma, Jan Albert and Smrtová, Erika},\\n\\tyear = {2022},\\n\\tpages = {131--150},\\n}\\n\\n\",\"author_short\":[\"Kuneš, P.\",\"Bobek, P.\",\"Svobodová-Svitavská, H.\",\"Švarcová, M. G\",\"Šulc, V.\",\"Šturma, J. A.\",\"Smrtová, E.\"],\"key\":\"kunes_dosavadni_2022\",\"id\":\"kunes_dosavadni_2022\",\"bibbaseid\":\"kune-bobek-svobodovsvitavsk-varcov-ulc-turma-smrtov-dosavadnvsledkypaleoekologickchvzkumvaskmvbkupodkladyproochranuprody-2022\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"European pollen-based REVEALS land-cover reconstructions for the Holocene: methodology, mapping and potentials\",\"volume\":\"14\",\"issn\":\"1866-3508\",\"shorttitle\":\"European pollen-based REVEALS land-cover reconstructions for the Holocene\",\"doi\":\"10.5194/essd-14-1581-2022\",\"abstract\":\"\\\\textlessp\\\\textgreater\\\\textlessstrong class=\\\"journal-contentHeaderColor\\\"\\\\textgreaterAbstract.\\\\textless/strong\\\\textgreater Quantitative reconstructions of past land cover are necessary to determine the processes involved in climate–human–land-cover interactions. We present the first temporally continuous and most spatially extensive pollen-based land-cover reconstruction for Europe over the Holocene (last 11 700 cal yr BP). We describe how vegetation cover has been quantified from pollen records at a 1\\\\textlessspan class=\\\"inline-formula\\\"\\\\textgreater$^{\\\\textrm{∘}}$\\\\textless/span\\\\textgreater \\\\textlessspan class=\\\"inline-formula\\\"\\\\textgreater×\\\\textless/span\\\\textgreater 1\\\\textlessspan class=\\\"inline-formula\\\"\\\\textgreater$^{\\\\textrm{∘}}$\\\\textless/span\\\\textgreater spatial scale using the “Regional Estimates of VEgetation Abundance from Large Sites” (REVEALS) model. REVEALS calculates estimates of past regional vegetation cover in proportions or percentages. REVEALS has been applied to 1128 pollen records across Europe and part of the eastern Mediterranean–Black Sea–Caspian corridor (30–75\\\\textlessspan class=\\\"inline-formula\\\"\\\\textgreater$^{\\\\textrm{∘}}$\\\\textless/span\\\\textgreater N, 25\\\\textlessspan class=\\\"inline-formula\\\"\\\\textgreater$^{\\\\textrm{∘}}$\\\\textless/span\\\\textgreater W–50\\\\textlessspan class=\\\"inline-formula\\\"\\\\textgreater$^{\\\\textrm{∘}}$\\\\textless/span\\\\textgreater E) to reconstruct the percentage cover of 31 plant taxa assigned to 12 plant functional types (PFTs) and 3 land-cover types (LCTs). A new synthesis of relative pollen productivities (RPPs) for European plant taxa was performed for this reconstruction. It includes multiple RPP values (\\\\textlessspan class=\\\"inline-formula\\\"\\\\textgreater≥2\\\\textless/span\\\\textgreater values) for 39 taxa and single values for 15 taxa (total of 54 taxa). To illustrate this, we present distribution maps for five taxa (<i>Calluna vulgaris</i>, Cerealia type (t)., <i>Picea abies</i>, deciduous <i>Quercus</i> t. and evergreen <i>Quercus</i> t.) and three land-cover types (open land, OL; evergreen trees, ETs; and summer-green trees, STs) for eight selected time windows. The reliability of the REVEALS reconstructions and issues related to the interpretation of the results in terms of landscape openness and human-induced vegetation change are discussed. This is followed by a review of the current use of this reconstruction and its future potential utility and development. REVEALS data quality are primarily determined by pollen count data (pollen count and sample, pollen identification, and chronology) and site type and number (lake or bog, large or small, one site vs. multiple sites) used for REVEALS analysis (for each grid cell). A large number of sites with high-quality pollen count data will produce more reliable land-cover estimates with lower standard errors compared to a low number of sites with lower-quality pollen count data. The REVEALS data presented here can be downloaded from \\\\textlessa href=\\\"https://doi.org/10.1594/PANGAEA.937075\\\"\\\\textgreaterhttps://doi.org/10.1594/PANGAEA.937075\\\\textless/a\\\\textgreater (Fyfe et al., 2022).\\\\textless/p\\\\textgreater\",\"language\":\"English\",\"number\":\"4\",\"urldate\":\"2022-04-19\",\"journal\":\"Earth System Science Data\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Githumbi\"],\"firstnames\":[\"Esther\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Fyfe\"],\"firstnames\":[\"Ralph\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Gaillard\"],\"firstnames\":[\"Marie-Jose\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Trondman\"],\"firstnames\":[\"Anna-Kari\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Mazier\"],\"firstnames\":[\"Florence\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Nielsen\"],\"firstnames\":[\"Anne-Birgitte\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Poska\"],\"firstnames\":[\"Anneli\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Sugita\"],\"firstnames\":[\"Shinya\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Woodbridge\"],\"firstnames\":[\"Jessie\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Azuara\"],\"firstnames\":[\"Julien\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Feurdean\"],\"firstnames\":[\"Angelica\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Grindean\"],\"firstnames\":[\"Roxana\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Lebreton\"],\"firstnames\":[\"Vincent\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Marquer\"],\"firstnames\":[\"Laurent\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Nebout-Combourieu\"],\"firstnames\":[\"Nathalie\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Stančikaitė\"],\"firstnames\":[\"Miglė\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tanţău\"],\"firstnames\":[\"Ioan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tonkov\"],\"firstnames\":[\"Spassimir\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Shumilovskikh\"],\"firstnames\":[\"Lyudmila\"],\"suffixes\":[]},{\"firstnames\":[\"LandClimII\"],\"propositions\":[\"data\",\"contributors\"],\"lastnames\":[],\"suffixes\":[]}],\"month\":\"April\",\"year\":\"2022\",\"note\":\"[IF2021=11.815; AIS2021=4.141]\",\"keywords\":\"reconstruction\",\"pages\":\"1581–1619\",\"bibtex\":\"@article{githumbi_european_2022,\\n\\ttitle = {European pollen-based {REVEALS} land-cover reconstructions for the {Holocene}: methodology, mapping and potentials},\\n\\tvolume = {14},\\n\\tissn = {1866-3508},\\n\\tshorttitle = {European pollen-based {REVEALS} land-cover reconstructions for the {Holocene}},\\n\\tdoi = {10.5194/essd-14-1581-2022},\\n\\tabstract = {{\\\\textless}p{\\\\textgreater}{\\\\textless}strong class=\\\"journal-contentHeaderColor\\\"{\\\\textgreater}Abstract.{\\\\textless}/strong{\\\\textgreater} Quantitative reconstructions of past land cover are necessary to determine the processes involved in climate–human–land-cover interactions. We present the first temporally continuous and most spatially extensive pollen-based land-cover reconstruction for Europe over the Holocene (last 11 700 cal yr BP). We describe how vegetation cover has been quantified from pollen records at a 1{\\\\textless}span class=\\\"inline-formula\\\"{\\\\textgreater}$^{\\\\textrm{∘}}${\\\\textless}/span{\\\\textgreater} {\\\\textless}span class=\\\"inline-formula\\\"{\\\\textgreater}×{\\\\textless}/span{\\\\textgreater} 1{\\\\textless}span class=\\\"inline-formula\\\"{\\\\textgreater}$^{\\\\textrm{∘}}${\\\\textless}/span{\\\\textgreater} spatial scale using the “Regional Estimates of VEgetation Abundance from Large Sites” (REVEALS) model. REVEALS calculates estimates of past regional vegetation cover in proportions or percentages. REVEALS has been applied to 1128 pollen records across Europe and part of the eastern Mediterranean–Black Sea–Caspian corridor (30–75{\\\\textless}span class=\\\"inline-formula\\\"{\\\\textgreater}$^{\\\\textrm{∘}}${\\\\textless}/span{\\\\textgreater} N, 25{\\\\textless}span class=\\\"inline-formula\\\"{\\\\textgreater}$^{\\\\textrm{∘}}${\\\\textless}/span{\\\\textgreater} W–50{\\\\textless}span class=\\\"inline-formula\\\"{\\\\textgreater}$^{\\\\textrm{∘}}${\\\\textless}/span{\\\\textgreater} E) to reconstruct the percentage cover of 31 plant taxa assigned to 12 plant functional types (PFTs) and 3 land-cover types (LCTs). A new synthesis of relative pollen productivities (RPPs) for European plant taxa was performed for this reconstruction. It includes multiple RPP values ({\\\\textless}span class=\\\"inline-formula\\\"{\\\\textgreater}≥2{\\\\textless}/span{\\\\textgreater} values) for 39 taxa and single values for 15 taxa (total of 54 taxa). To illustrate this, we present distribution maps for five taxa (\\\\textit{Calluna vulgaris}, Cerealia type (t)., \\\\textit{Picea abies}, deciduous \\\\textit{Quercus} t. and evergreen \\\\textit{Quercus} t.) and three land-cover types (open land, OL; evergreen trees, ETs; and summer-green trees, STs) for eight selected time windows. The reliability of the REVEALS reconstructions and issues related to the interpretation of the results in terms of landscape openness and human-induced vegetation change are discussed. This is followed by a review of the current use of this reconstruction and its future potential utility and development. REVEALS data quality are primarily determined by pollen count data (pollen count and sample, pollen identification, and chronology) and site type and number (lake or bog, large or small, one site vs. multiple sites) used for REVEALS analysis (for each grid cell). A large number of sites with high-quality pollen count data will produce more reliable land-cover estimates with lower standard errors compared to a low number of sites with lower-quality pollen count data. The REVEALS data presented here can be downloaded from {\\\\textless}a href=\\\"https://doi.org/10.1594/PANGAEA.937075\\\"{\\\\textgreater}https://doi.org/10.1594/PANGAEA.937075{\\\\textless}/a{\\\\textgreater} (Fyfe et al., 2022).{\\\\textless}/p{\\\\textgreater}},\\n\\tlanguage = {English},\\n\\tnumber = {4},\\n\\turldate = {2022-04-19},\\n\\tjournal = {Earth System Science Data},\\n\\tauthor = {Githumbi, Esther and Fyfe, Ralph and Gaillard, Marie-Jose and Trondman, Anna-Kari and Mazier, Florence and Nielsen, Anne-Birgitte and Poska, Anneli and Sugita, Shinya and Woodbridge, Jessie and Azuara, Julien and Feurdean, Angelica and Grindean, Roxana and Lebreton, Vincent and Marquer, Laurent and Nebout-Combourieu, Nathalie and Stančikaitė, Miglė and Tanţău, Ioan and Tonkov, Spassimir and Shumilovskikh, Lyudmila and LandClimII data contributors},\\n\\tmonth = apr,\\n\\tyear = {2022},\\n\\tnote = {[IF2021=11.815; AIS2021=4.141]},\\n\\tkeywords = {reconstruction},\\n\\tpages = {1581--1619},\\n}\\n\\n\",\"author_short\":[\"Githumbi, E.\",\"Fyfe, R.\",\"Gaillard, M.\",\"Trondman, A.\",\"Mazier, F.\",\"Nielsen, A.\",\"Poska, A.\",\"Sugita, S.\",\"Woodbridge, J.\",\"Azuara, J.\",\"Feurdean, A.\",\"Grindean, R.\",\"Lebreton, V.\",\"Marquer, L.\",\"Nebout-Combourieu, N.\",\"Stančikaitė, M.\",\"Tanţău, I.\",\"Tonkov, S.\",\"Shumilovskikh, L.\",\"data contributors , L.\"],\"key\":\"githumbi_european_2022\",\"id\":\"githumbi_european_2022\",\"bibbaseid\":\"githumbi-fyfe-gaillard-trondman-mazier-nielsen-poska-sugita-etal-europeanpollenbasedrevealslandcoverreconstructionsfortheholocenemethodologymappingandpotentials-2022\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"reconstruction\"],\"metadata\":{\"authorlinks\":{}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Sub-fossil bark beetles as indicators of past disturbance events in temperate Picea abies mountain forests\",\"volume\":\"275\",\"issn\":\"0277-3791\",\"doi\":\"10.1016/j.quascirev.2021.107289\",\"abstract\":\"Temperate mountain forests have experienced an increase in frequency and severity of natural disturbances (e.g., droughts, fires, windstorms and insect outbreaks) in recent decades due to climate and environmental change. Outbreaks of bark beetles have caused significant dieback of conifer forests in Central Europe and it is essential to model and predict the potential severity of future bark beetle outbreaks. However, to predict future bark beetle activity, historical baseline information is required to contextualize the magnitude of current and potential future outbreaks. A fossil beetle record from a forest hollow in the Tatra Mountains, Slovakia; one of the best-preserved national parks in Central Europe, was produced to identify insect outbreaks during the last millennia. Sub-fossil bark beetle remains were compared with parallel pollen and charcoal to assess whether peaks in conifer bark beetle remains correspond with indications of disturbance documented in historical or sedimentary fossil records. Three peaks in bark beetle remains were detected (1) post-2004, (2) AD 1140–1440, and (3) AD 930–1030. The abundance of species Pityogenes chalcographus and Pityophthorus pityographus in the two top samples can be linked directly to large bark beetle outbreaks in the High Tatra Mountains after 2004. P. chalcographus and P. pityographus are also the abundant species in the second peak (AD 1140–1440) while the third peak (AD 930–1030) consists of the species Polygraphus poligraphus. The most prominent conifer bark beetle in Central Europe, Ips typographus, was found to be present in most of the samples but always at very low numbers. It is plausible that P. chalcographus and P. pityographus fossils might be useful proxies for past conifer bark beetle outbreaks in Central Europe, as they occur together with fossils of I. typographus but appear to be well-preserved. A significant correlation was found between primary bark beetles and macroscopic charcoal densities in the sediment, highlighting the complex interactions between disturbance agents, bark beetles and fire, in this long-term regime of natural disturbances. Our 1400-year disturbance record shows how bark beetle outbreaks have been an important component of the regional natural disturbance regime for over a millennium and have intensified with increasing anthropogenic activity. Bark beetle outbreaks are likely one of the drivers promoting the future ecological stability of the temperate conifer ecosystem over decades to centuries.\",\"language\":\"English\",\"urldate\":\"2021-11-29\",\"journal\":\"Quaternary Science Reviews\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Schafstall\"],\"firstnames\":[\"Nick\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuosmanen\"],\"firstnames\":[\"Niina\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svobodová\"],\"firstnames\":[\"Helena\",\"Svitavská\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svitok\"],\"firstnames\":[\"Marek\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chiverrell\"],\"firstnames\":[\"Richard\",\"C.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Halsall\"],\"firstnames\":[\"Karen\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Fleischer\"],\"firstnames\":[\"Peter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Knížek\"],\"firstnames\":[\"Miloš\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Clear\"],\"firstnames\":[\"Jennifer\",\"L.\"],\"suffixes\":[]}],\"month\":\"January\",\"year\":\"2022\",\"note\":\"[IF2021=4.456;AIS2021=1.586]\",\"keywords\":\"Bark beetle outbreaks, Central Europe, Disturbance history, Ecosystem services, Fire, Fossil proxies, High Tatra mountains, disturbance\",\"pages\":\"107289\",\"bibtex\":\"@article{schafstall_sub-fossil_2022,\\n\\ttitle = {Sub-fossil bark beetles as indicators of past disturbance events in temperate {Picea} abies mountain forests},\\n\\tvolume = {275},\\n\\tissn = {0277-3791},\\n\\tdoi = {10.1016/j.quascirev.2021.107289},\\n\\tabstract = {Temperate mountain forests have experienced an increase in frequency and severity of natural disturbances (e.g., droughts, fires, windstorms and insect outbreaks) in recent decades due to climate and environmental change. Outbreaks of bark beetles have caused significant dieback of conifer forests in Central Europe and it is essential to model and predict the potential severity of future bark beetle outbreaks. However, to predict future bark beetle activity, historical baseline information is required to contextualize the magnitude of current and potential future outbreaks. A fossil beetle record from a forest hollow in the Tatra Mountains, Slovakia; one of the best-preserved national parks in Central Europe, was produced to identify insect outbreaks during the last millennia. Sub-fossil bark beetle remains were compared with parallel pollen and charcoal to assess whether peaks in conifer bark beetle remains correspond with indications of disturbance documented in historical or sedimentary fossil records. Three peaks in bark beetle remains were detected (1) post-2004, (2) AD 1140–1440, and (3) AD 930–1030. The abundance of species Pityogenes chalcographus and Pityophthorus pityographus in the two top samples can be linked directly to large bark beetle outbreaks in the High Tatra Mountains after 2004. P. chalcographus and P. pityographus are also the abundant species in the second peak (AD 1140–1440) while the third peak (AD 930–1030) consists of the species Polygraphus poligraphus. The most prominent conifer bark beetle in Central Europe, Ips typographus, was found to be present in most of the samples but always at very low numbers. It is plausible that P. chalcographus and P. pityographus fossils might be useful proxies for past conifer bark beetle outbreaks in Central Europe, as they occur together with fossils of I. typographus but appear to be well-preserved. A significant correlation was found between primary bark beetles and macroscopic charcoal densities in the sediment, highlighting the complex interactions between disturbance agents, bark beetles and fire, in this long-term regime of natural disturbances. Our 1400-year disturbance record shows how bark beetle outbreaks have been an important component of the regional natural disturbance regime for over a millennium and have intensified with increasing anthropogenic activity. Bark beetle outbreaks are likely one of the drivers promoting the future ecological stability of the temperate conifer ecosystem over decades to centuries.},\\n\\tlanguage = {English},\\n\\turldate = {2021-11-29},\\n\\tjournal = {Quaternary Science Reviews},\\n\\tauthor = {Schafstall, Nick and Kuosmanen, Niina and Kuneš, Petr and Svobodová, Helena Svitavská and Svitok, Marek and Chiverrell, Richard C. and Halsall, Karen and Fleischer, Peter and Knížek, Miloš and Clear, Jennifer L.},\\n\\tmonth = jan,\\n\\tyear = {2022},\\n\\tnote = {[IF2021=4.456;AIS2021=1.586]},\\n\\tkeywords = {Bark beetle outbreaks, Central Europe, Disturbance history, Ecosystem services, Fire, Fossil proxies, High Tatra mountains, disturbance},\\n\\tpages = {107289},\\n}\\n\\n\",\"author_short\":[\"Schafstall, N.\",\"Kuosmanen, N.\",\"Kuneš, P.\",\"Svobodová, H. S.\",\"Svitok, M.\",\"Chiverrell, R. C.\",\"Halsall, K.\",\"Fleischer, P.\",\"Knížek, M.\",\"Clear, J. L.\"],\"key\":\"schafstall_sub-fossil_2022\",\"id\":\"schafstall_sub-fossil_2022\",\"bibbaseid\":\"schafstall-kuosmanen-kune-svobodov-svitok-chiverrell-halsall-fleischer-etal-subfossilbarkbeetlesasindicatorsofpastdisturbanceeventsintemperatepiceaabiesmountainforests-2022\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Bark beetle outbreaks\",\"Central Europe\",\"Disturbance history\",\"Ecosystem services\",\"Fire\",\"Fossil proxies\",\"High Tatra mountains\",\"disturbance\"],\"metadata\":{\"authorlinks\":{}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Disruption of cultural burning promotes shrub encroachment and unprecedented wildfires\",\"volume\":\"20\",\"issn\":\"1540-9309\",\"doi\":\"10.1002/fee.2395\",\"abstract\":\"Recent catastrophic fires in Australia and North America have raised broad-scale questions about how the cessation of Indigenous burning practices has impacted fuel accumulation and structure. For sustainable coexistence with fire, a better understanding of the ancient nexus between humans and flammable landscapes is needed. We used novel palaeoecological modeling and charcoal compilations to reassess evidence for changes in land cover and fire activity, focusing on southeast Australia before and after British colonization. Here, we provide what we believe is the first quantitative evidence that the region’s forests and woodlands contained fewer shrubs and more grass before colonization. Changes in vegetation, fuel structures, and connectivity followed different trajectories in different vegetation types. The pattern is best explained by the disruption of Indigenous vegetation management caused by European settlement. Combined with climate-change impacts on fire weather and drought, the widespread absence of Indigenous fire management practices likely preconditioned fire-prone regions for wildfires of unprecedented extent.\",\"language\":\"English\",\"number\":\"5\",\"urldate\":\"2022-06-22\",\"journal\":\"Frontiers in Ecology and the Environment\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Mariani\"],\"firstnames\":[\"Michela\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Connor\"],\"firstnames\":[\"Simon\",\"E\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Theuerkauf\"],\"firstnames\":[\"Martin\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Herbert\"],\"firstnames\":[\"Annika\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bowman\"],\"firstnames\":[\"David\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Fletcher\"],\"firstnames\":[\"Michael-Shawn\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Head\"],\"firstnames\":[\"Lesley\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kershaw\"],\"firstnames\":[\"A\",\"Peter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Haberle\"],\"firstnames\":[\"Simon\",\"G\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Stevenson\"],\"firstnames\":[\"Janelle\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Adeleye\"],\"firstnames\":[\"Matthew\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Cadd\"],\"firstnames\":[\"Haidee\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hopf\"],\"firstnames\":[\"Feli\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Briles\"],\"firstnames\":[\"Christy\"],\"suffixes\":[]}],\"year\":\"2022\",\"note\":\"[IF2021=13.789;AIS2021=4.071]\",\"keywords\":\"disturbance, reconstruction\",\"pages\":\"292–300\",\"bibtex\":\"@article{mariani_disruption_2022,\\n\\ttitle = {Disruption of cultural burning promotes shrub encroachment and unprecedented wildfires},\\n\\tvolume = {20},\\n\\tissn = {1540-9309},\\n\\tdoi = {10.1002/fee.2395},\\n\\tabstract = {Recent catastrophic fires in Australia and North America have raised broad-scale questions about how the cessation of Indigenous burning practices has impacted fuel accumulation and structure. For sustainable coexistence with fire, a better understanding of the ancient nexus between humans and flammable landscapes is needed. We used novel palaeoecological modeling and charcoal compilations to reassess evidence for changes in land cover and fire activity, focusing on southeast Australia before and after British colonization. Here, we provide what we believe is the first quantitative evidence that the region’s forests and woodlands contained fewer shrubs and more grass before colonization. Changes in vegetation, fuel structures, and connectivity followed different trajectories in different vegetation types. The pattern is best explained by the disruption of Indigenous vegetation management caused by European settlement. Combined with climate-change impacts on fire weather and drought, the widespread absence of Indigenous fire management practices likely preconditioned fire-prone regions for wildfires of unprecedented extent.},\\n\\tlanguage = {English},\\n\\tnumber = {5},\\n\\turldate = {2022-06-22},\\n\\tjournal = {Frontiers in Ecology and the Environment},\\n\\tauthor = {Mariani, Michela and Connor, Simon E and Theuerkauf, Martin and Herbert, Annika and Kuneš, Petr and Bowman, David and Fletcher, Michael-Shawn and Head, Lesley and Kershaw, A Peter and Haberle, Simon G and Stevenson, Janelle and Adeleye, Matthew and Cadd, Haidee and Hopf, Feli and Briles, Christy},\\n\\tyear = {2022},\\n\\tnote = {[IF2021=13.789;AIS2021=4.071]},\\n\\tkeywords = {disturbance, reconstruction},\\n\\tpages = {292--300},\\n}\\n\\n\",\"author_short\":[\"Mariani, M.\",\"Connor, S. E\",\"Theuerkauf, M.\",\"Herbert, A.\",\"Kuneš, P.\",\"Bowman, D.\",\"Fletcher, M.\",\"Head, L.\",\"Kershaw, A P.\",\"Haberle, S. G\",\"Stevenson, J.\",\"Adeleye, M.\",\"Cadd, H.\",\"Hopf, F.\",\"Briles, C.\"],\"key\":\"mariani_disruption_2022\",\"id\":\"mariani_disruption_2022\",\"bibbaseid\":\"mariani-connor-theuerkauf-herbert-kune-bowman-fletcher-head-etal-disruptionofculturalburningpromotesshrubencroachmentandunprecedentedwildfires-2022\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"disturbance\",\"reconstruction\"],\"metadata\":{\"authorlinks\":{}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Settlement activity in later prehistory: invisible in the archaeological record but documented by pollen and sedimentary evidence\",\"volume\":\"11\",\"issn\":\"1866-9565\",\"shorttitle\":\"Settlement activity in later prehistory\",\"url\":\"https://doi.org/10.1007/s12520-018-0614-x\",\"doi\":\"10.1007/s12520-018-0614-x\",\"abstract\":\"The paper deals with landscape and settlement development between ca. 300 BC and AD 600 in a defined area of the northern Czech Republic. Despite favourable natural conditions, human occupation of the area did not begin until the end of the first millennium BC. Natural soil and vegetation development therefore lasted longer than in the traditionally settled lowland areas. Initial settlement activity from the La Tène period caused substantial erosion of deforested luvisols and retisols, well-documented by an accumulation of eroded soil horizons in a local wetland. The erosion process continued for more than 500 years following the end of the La Tène settlement, despite the fact that archaeological research revealed no reliable evidence of occupation prior to the twelfth century AD. Pollen and sedimentary records from the wetland, however, clearly indicate the existence of settlement activity during the “archaeologically invisible” Roman and Migration periods. This case is not unique and underlines the importance of environmental analysis for the detection of settlement history, particularly during periods of poor archaeological visibility or in places that are difficult to research using standard archaeological methods. The change in conditions after the first deforestation and subsequent late prehistoric settlement triggered the degradation of the deforested luvisols and retisols and led to the diversification of the soil cover, which now also includes regosols, gleysols, and truncated luvisols and retisols.\",\"language\":\"en\",\"number\":\"5\",\"urldate\":\"2020-03-05\",\"journal\":\"Archaeological and Anthropological Sciences\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Dreslerová\"],\"firstnames\":[\"Dagmar\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kozáková\"],\"firstnames\":[\"Radka\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chuman\"],\"firstnames\":[\"Tomáš\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Strouhalová\"],\"firstnames\":[\"Barbora\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Abraham\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Poništiak\"],\"firstnames\":[\"Štefan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Šefrna\"],\"firstnames\":[\"Luděk\"],\"suffixes\":[]}],\"month\":\"May\",\"year\":\"2019\",\"pages\":\"1683–1700\",\"bibtex\":\"@article{dreslerova_settlement_2019,\\n\\ttitle = {Settlement activity in later prehistory: invisible in the archaeological record but documented by pollen and sedimentary evidence},\\n\\tvolume = {11},\\n\\tissn = {1866-9565},\\n\\tshorttitle = {Settlement activity in later prehistory},\\n\\turl = {https://doi.org/10.1007/s12520-018-0614-x},\\n\\tdoi = {10.1007/s12520-018-0614-x},\\n\\tabstract = {The paper deals with landscape and settlement development between ca. 300 BC and AD 600 in a defined area of the northern Czech Republic. Despite favourable natural conditions, human occupation of the area did not begin until the end of the first millennium BC. Natural soil and vegetation development therefore lasted longer than in the traditionally settled lowland areas. Initial settlement activity from the La Tène period caused substantial erosion of deforested luvisols and retisols, well-documented by an accumulation of eroded soil horizons in a local wetland. The erosion process continued for more than 500 years following the end of the La Tène settlement, despite the fact that archaeological research revealed no reliable evidence of occupation prior to the twelfth century AD. Pollen and sedimentary records from the wetland, however, clearly indicate the existence of settlement activity during the “archaeologically invisible” Roman and Migration periods. This case is not unique and underlines the importance of environmental analysis for the detection of settlement history, particularly during periods of poor archaeological visibility or in places that are difficult to research using standard archaeological methods. The change in conditions after the first deforestation and subsequent late prehistoric settlement triggered the degradation of the deforested luvisols and retisols and led to the diversification of the soil cover, which now also includes regosols, gleysols, and truncated luvisols and retisols.},\\n\\tlanguage = {en},\\n\\tnumber = {5},\\n\\turldate = {2020-03-05},\\n\\tjournal = {Archaeological and Anthropological Sciences},\\n\\tauthor = {Dreslerová, Dagmar and Kozáková, Radka and Chuman, Tomáš and Strouhalová, Barbora and Abraham, Vojtěch and Poništiak, Štefan and Šefrna, Luděk},\\n\\tmonth = may,\\n\\tyear = {2019},\\n\\tpages = {1683--1700},\\n}\\n\\n\",\"author_short\":[\"Dreslerová, D.\",\"Kozáková, R.\",\"Chuman, T.\",\"Strouhalová, B.\",\"Abraham, V.\",\"Poništiak, Š.\",\"Šefrna, L.\"],\"key\":\"dreslerova_settlement_2019\",\"id\":\"dreslerova_settlement_2019\",\"bibbaseid\":\"dreslerov-kozkov-chuman-strouhalov-abraham-ponitiak-efrna-settlementactivityinlaterprehistoryinvisibleinthearchaeologicalrecordbutdocumentedbypollenandsedimentaryevidence-2019\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://doi.org/10.1007/s12520-018-0614-x\"},\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Comparative biology of four Rhodanthidium species (Hymenoptera, Megachilidae) that nest in snail shells\",\"volume\":\"85\",\"issn\":\"1314-2607\",\"doi\":\"10.3897/jhr.85.66544\",\"abstract\":\"Some species of two tribes (Anthidiini and Osmiini) of the bee family Megachilidae utilize empty gastropod shells as nesting cavities. While snail-nesting Osmiini have been more frequently studied and the nesting biology of several species is well-known, much less is known about the habits of snail-nesting Anthidiini. We collected nests of four species of the genus Rhodanthidium (R. septemdentatum, R. sticticum, R. siculum and R. infuscatum) in the Czech Republic, Slovakia, Catalonia (Spain) and Sicily (Italy). We dissected these nests in the laboratory and documented their structure, pollen sources and nest associates. The four species usually choose large snail shells. All four species close their nests with a plug made of resin, sand and fragments of snail shells. However, nests of the four species can be distinguished based on the presence (R. septemdentatum, R. sticticum) or absence (R. siculum, R. infuscatum) of mineral and plant debris in the vestibular space, and the presence (R. septemdentatum, R. infuscatum) or absence (R. sticticum, R. siculum) of a resin partition between the vestibular space and the brood cell. Rhodanthidium septemdentatum, R. sticticum and R. siculum usually build a single brood cell per nest, but all R. infuscatum nests studied contained two or more cells. For three of the species (R. siculum, R. septemdentatum and R. sticticum) we confirmed overwintering in the adult stage. Contrary to R. siculum, R. septemdentatum and R. sticticum do not hide their nest shells and usually use shells under the stones or hidden in crevices within stone walls. Nest associates were very infrequent. We only found two R. sticticum nests parasitized by the chrysidid wasp Chrysura refulgens and seven nests infested with pollen mites Chaetodactylus cf. anthidii. Our pollen analyses confirm that Rhodanthidium are polylectic but show a preference for Fabaceae by R. sticticum.\",\"language\":\"English\",\"urldate\":\"2021-09-01\",\"journal\":\"Journal of Hymenoptera Research\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Hostinská\"],\"firstnames\":[\"Lucie\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hadrava\"],\"firstnames\":[\"Jiří\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bosch\"],\"firstnames\":[\"Jordi\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Scaramozzino\"],\"firstnames\":[\"Pier\",\"Luigi\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bogusch\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"month\":\"August\",\"year\":\"2021\",\"note\":\"[IF2020=1.733]\",\"pages\":\"11–28\",\"bibtex\":\"@article{hostinska_comparative_2021,\\n\\ttitle = {Comparative biology of four {Rhodanthidium} species ({Hymenoptera}, {Megachilidae}) that nest in snail shells},\\n\\tvolume = {85},\\n\\tissn = {1314-2607},\\n\\tdoi = {10.3897/jhr.85.66544},\\n\\tabstract = {Some species of two tribes (Anthidiini and Osmiini) of the bee family Megachilidae utilize empty gastropod shells as nesting cavities. While snail-nesting Osmiini have been more frequently studied and the nesting biology of several species is well-known, much less is known about the habits of snail-nesting Anthidiini. We collected nests of four species of the genus Rhodanthidium (R. septemdentatum, R. sticticum, R. siculum and R. infuscatum) in the Czech Republic, Slovakia, Catalonia (Spain) and Sicily (Italy). We dissected these nests in the laboratory and documented their structure, pollen sources and nest associates. The four species usually choose large snail shells. All four species close their nests with a plug made of resin, sand and fragments of snail shells. However, nests of the four species can be distinguished based on the presence (R. septemdentatum, R. sticticum) or absence (R. siculum, R. infuscatum) of mineral and plant debris in the vestibular space, and the presence (R. septemdentatum, R. infuscatum) or absence (R. sticticum, R. siculum) of a resin partition between the vestibular space and the brood cell. Rhodanthidium septemdentatum, R. sticticum and R. siculum usually build a single brood cell per nest, but all R. infuscatum nests studied contained two or more cells. For three of the species (R. siculum, R. septemdentatum and R. sticticum) we confirmed overwintering in the adult stage. Contrary to R. siculum, R. septemdentatum and R. sticticum do not hide their nest shells and usually use shells under the stones or hidden in crevices within stone walls. Nest associates were very infrequent. We only found two R. sticticum nests parasitized by the chrysidid wasp Chrysura refulgens and seven nests infested with pollen mites Chaetodactylus cf. anthidii. Our pollen analyses confirm that Rhodanthidium are polylectic but show a preference for Fabaceae by R. sticticum.},\\n\\tlanguage = {English},\\n\\turldate = {2021-09-01},\\n\\tjournal = {Journal of Hymenoptera Research},\\n\\tauthor = {Hostinská, Lucie and Kuneš, Petr and Hadrava, Jiří and Bosch, Jordi and Scaramozzino, Pier Luigi and Bogusch, Petr},\\n\\tmonth = aug,\\n\\tyear = {2021},\\n\\tnote = {[IF2020=1.733]},\\n\\tpages = {11--28},\\n}\\n\\n\",\"author_short\":[\"Hostinská, L.\",\"Kuneš, P.\",\"Hadrava, J.\",\"Bosch, J.\",\"Scaramozzino, P. L.\",\"Bogusch, P.\"],\"key\":\"hostinska_comparative_2021\",\"id\":\"hostinska_comparative_2021\",\"bibbaseid\":\"hostinsk-kune-hadrava-bosch-scaramozzino-bogusch-comparativebiologyoffourrhodanthidiumspecieshymenopteramegachilidaethatnestinsnailshells-2021\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Global acceleration in rates of vegetation change over the past 18,000 years\",\"volume\":\"372\",\"issn\":\"0036-8075, 1095-9203\",\"url\":\"https://science.sciencemag.org/content/372/6544/860\",\"doi\":\"10.1126/science.abg1685\",\"abstract\":\"The pace of Holocene vegetation change Although much is known about the rapid environmental changes that have occurred since the Industrial Revolution, the patterns of change over the preceding millennia have been only patchily understood. Using a global set of \\\\textgreater1100 fossil pollen records, Mottl et al. explored the rates of vegetation change over the past 18,000 years (see the Perspective by Overpeck and Breshears). The authors show that the rates of change accelerated markedly during the Late Holocene (∼4.6 to 2.9 thousand years ago), even more rapidly than the climate-driven vegetation changes associated with the end of the last glacial period. In addition, the Late Holocene acceleration began for terrestrial communities as a whole, suggesting that the acceleration in turnover over the past two centuries is the tip of a deeper trend. Science, abg1685, this issue p. 860; see also abi9902, p. 786 Global vegetation over the past 18,000 years has been transformed first by the climate changes that accompanied the last deglaciation and again by increasing human pressures; however, the magnitude and patterns of rates of vegetation change are poorly understood globally. Using a compilation of 1181 fossil pollen sequences and newly developed statistical methods, we detect a worldwide acceleration in the rates of vegetation compositional change beginning between 4.6 and 2.9 thousand years ago that is globally unprecedented over the past 18,000 years in both magnitude and extent. Late Holocene rates of change equal or exceed the deglacial rates for all continents, which suggests that the scale of human effects on terrestrial ecosystems exceeds even the climate-driven transformations of the last deglaciation. The acceleration of biodiversity change demonstrated in ecological datasets from the past century began millennia ago. A compilation of fossil pollen sequences shows that the acceleration of biodiversity change began millennia ago. A compilation of fossil pollen sequences shows that the acceleration of biodiversity change began millennia ago.\",\"language\":\"English\",\"number\":\"6544\",\"urldate\":\"2021-05-20\",\"journal\":\"Science\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Mottl\"],\"firstnames\":[\"Ondřej\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Flantua\"],\"firstnames\":[\"Suzette\",\"G.\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bhatta\"],\"firstnames\":[\"Kuber\",\"P.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Felde\"],\"firstnames\":[\"Vivian\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Giesecke\"],\"firstnames\":[\"Thomas\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Goring\"],\"firstnames\":[\"Simon\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Grimm\"],\"firstnames\":[\"Eric\",\"C.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Haberle\"],\"firstnames\":[\"Simon\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hooghiemstra\"],\"firstnames\":[\"Henry\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Ivory\"],\"firstnames\":[\"Sarah\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Wolters\"],\"firstnames\":[\"Steffen\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Seddon\"],\"firstnames\":[\"Alistair\",\"W.\",\"R.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Williams\"],\"firstnames\":[\"John\",\"W.\"],\"suffixes\":[]}],\"month\":\"May\",\"year\":\"2021\",\"note\":\"[IF2020=47.728]\",\"keywords\":\"Database, reconstruction\",\"pages\":\"860–864\",\"bibtex\":\"@article{mottl_global_2021,\\n\\ttitle = {Global acceleration in rates of vegetation change over the past 18,000 years},\\n\\tvolume = {372},\\n\\tissn = {0036-8075, 1095-9203},\\n\\turl = {https://science.sciencemag.org/content/372/6544/860},\\n\\tdoi = {10.1126/science.abg1685},\\n\\tabstract = {The pace of Holocene vegetation change\\nAlthough much is known about the rapid environmental changes that have occurred since the Industrial Revolution, the patterns of change over the preceding millennia have been only patchily understood. Using a global set of {\\\\textgreater}1100 fossil pollen records, Mottl et al. explored the rates of vegetation change over the past 18,000 years (see the Perspective by Overpeck and Breshears). The authors show that the rates of change accelerated markedly during the Late Holocene (∼4.6 to 2.9 thousand years ago), even more rapidly than the climate-driven vegetation changes associated with the end of the last glacial period. In addition, the Late Holocene acceleration began for terrestrial communities as a whole, suggesting that the acceleration in turnover over the past two centuries is the tip of a deeper trend.\\nScience, abg1685, this issue p. 860; see also abi9902, p. 786\\nGlobal vegetation over the past 18,000 years has been transformed first by the climate changes that accompanied the last deglaciation and again by increasing human pressures; however, the magnitude and patterns of rates of vegetation change are poorly understood globally. Using a compilation of 1181 fossil pollen sequences and newly developed statistical methods, we detect a worldwide acceleration in the rates of vegetation compositional change beginning between 4.6 and 2.9 thousand years ago that is globally unprecedented over the past 18,000 years in both magnitude and extent. Late Holocene rates of change equal or exceed the deglacial rates for all continents, which suggests that the scale of human effects on terrestrial ecosystems exceeds even the climate-driven transformations of the last deglaciation. The acceleration of biodiversity change demonstrated in ecological datasets from the past century began millennia ago.\\nA compilation of fossil pollen sequences shows that the acceleration of biodiversity change began millennia ago.\\nA compilation of fossil pollen sequences shows that the acceleration of biodiversity change began millennia ago.},\\n\\tlanguage = {English},\\n\\tnumber = {6544},\\n\\turldate = {2021-05-20},\\n\\tjournal = {Science},\\n\\tauthor = {Mottl, Ondřej and Flantua, Suzette G. A. and Bhatta, Kuber P. and Felde, Vivian A. and Giesecke, Thomas and Goring, Simon and Grimm, Eric C. and Haberle, Simon and Hooghiemstra, Henry and Ivory, Sarah and Kuneš, Petr and Wolters, Steffen and Seddon, Alistair W. R. and Williams, John W.},\\n\\tmonth = may,\\n\\tyear = {2021},\\n\\tnote = {[IF2020=47.728]},\\n\\tkeywords = {Database, reconstruction},\\n\\tpages = {860--864},\\n}\\n\\n\",\"author_short\":[\"Mottl, O.\",\"Flantua, S. G. A.\",\"Bhatta, K. P.\",\"Felde, V. A.\",\"Giesecke, T.\",\"Goring, S.\",\"Grimm, E. C.\",\"Haberle, S.\",\"Hooghiemstra, H.\",\"Ivory, S.\",\"Kuneš, P.\",\"Wolters, S.\",\"Seddon, A. W. R.\",\"Williams, J. W.\"],\"key\":\"mottl_global_2021\",\"id\":\"mottl_global_2021\",\"bibbaseid\":\"mottl-flantua-bhatta-felde-giesecke-goring-grimm-haberle-etal-globalaccelerationinratesofvegetationchangeoverthepast18000years-2021\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://science.sciencemag.org/content/372/6544/860\"},\"keyword\":[\"Database\",\"reconstruction\"],\"metadata\":{\"authorlinks\":{}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"incollection\",\"type\":\"incollection\",\"address\":\"Praha\",\"title\":\"Post-glacial vegetation development in sandstone areas of the Czech Republic\",\"copyright\":\"All rights reserved\",\"isbn\":\"978-80-200-1577-8\",\"language\":\"English\",\"booktitle\":\"Sandstone Landscapes\",\"publisher\":\"Academia\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pokorný\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jankovská\"],\"firstnames\":[\"Vlasta\"],\"suffixes\":[]}],\"editor\":[{\"propositions\":[],\"lastnames\":[\"Härtel\"],\"firstnames\":[\"Handrij\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Cílek\"],\"firstnames\":[\"Václav\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Herben\"],\"firstnames\":[\"Tomáš\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jackson\"],\"firstnames\":[\"Andrew\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Williams\"],\"firstnames\":[\"Rendel\"],\"suffixes\":[]}],\"year\":\"2007\",\"keywords\":\"Czech Republic, Holocene, Late Glacial, human impact, pollen analysis, sandstone, vegetation history\",\"pages\":\"244–257\",\"bibtex\":\"@incollection{kunes_post-glacial_2007,\\n\\taddress = {Praha},\\n\\ttitle = {Post-glacial vegetation development in sandstone areas of the {Czech} {Republic}},\\n\\tcopyright = {All rights reserved},\\n\\tisbn = {978-80-200-1577-8},\\n\\tlanguage = {English},\\n\\tbooktitle = {Sandstone {Landscapes}},\\n\\tpublisher = {Academia},\\n\\tauthor = {Kuneš, Petr and Pokorný, Petr and Jankovská, Vlasta},\\n\\teditor = {Härtel, Handrij and Cílek, Václav and Herben, Tomáš and Jackson, Andrew and Williams, Rendel},\\n\\tyear = {2007},\\n\\tkeywords = {Czech Republic, Holocene, Late Glacial, human impact, pollen analysis, sandstone, vegetation history},\\n\\tpages = {244--257},\\n}\\n\\n\",\"author_short\":[\"Kuneš, P.\",\"Pokorný, P.\",\"Jankovská, V.\"],\"editor_short\":[\"Härtel, H.\",\"Cílek, V.\",\"Herben, T.\",\"Jackson, A.\",\"Williams, R.\"],\"key\":\"kunes_post-glacial_2007\",\"id\":\"kunes_post-glacial_2007\",\"bibbaseid\":\"kune-pokorn-jankovsk-postglacialvegetationdevelopmentinsandstoneareasoftheczechrepublic-2007\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Czech Republic\",\"Holocene\",\"Late Glacial\",\"human impact\",\"pollen analysis\",\"sandstone\",\"vegetation history\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Present-day vegetation helps quantifying past land cover in selected regions of the Czech Republic\",\"volume\":\"9\",\"copyright\":\"All rights reserved\",\"doi\":\"10.1371/journal.pone.0100117\",\"abstract\":\"The REVEALS model is a tool for recalculating pollen data into vegetation abundances on a regional scale. We explored the general effect of selected parameters by performing simulations and ascertained the best model setting for the Czech Republic using the shallowest samples from 120 fossil sites and data on actual regional vegetation (60 km radius). Vegetation proportions of 17 taxa were obtained by combining the CORINE Land Cover map with forest inventories, agricultural statistics and habitat mapping data. Our simulation shows that changing the site radius for all taxa substantially affects REVEALS estimates of taxa with heavy or light pollen grains. Decreasing the site radius has a similar effect as increasing the wind speed parameter. However, adjusting the site radius to 1 m for local taxa only (even taxa with light pollen) yields lower, more correct estimates despite their high pollen signal. Increasing the background radius does not affect the estimates significantly. Our comparison of estimates with actual vegetation in seven regions shows that the most accurate relative pollen productivity estimates (PPEs) come from Central Europe and Southern Sweden. The initial simulation and pollen data yielded unrealistic estimates for Abies under the default setting of the wind speed parameter (3 m/s). We therefore propose the setting of 4 m/s, which corresponds to the spring average in most regions of the Czech Republic studied. Ad hoc adjustment of PPEs with this setting improves the match 3–4-fold. We consider these values (apart from four exceptions) to be appropriate, because they are within the ranges of standard errors, so they are related to original PPEs. Setting a 1 m radius for local taxa (Alnus, Salix, Poaceae) significantly improves the match between estimates and actual vegetation. However, further adjustments to PPEs exceed the ranges of original values, so their relevance is uncertain.\",\"language\":\"English\",\"number\":\"6\",\"urldate\":\"2014-06-18\",\"journal\":\"PLoS ONE\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Abraham\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Oušková\"],\"firstnames\":[\"Veronika\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"month\":\"June\",\"year\":\"2014\",\"note\":\"[IF2013=3.534]\",\"keywords\":\"Czech Republic, LRA, Pollen dispersal, Pollen production estimate (PPE), REVEALS, reconstruction, vegetation\",\"pages\":\"e100117\",\"bibtex\":\"@article{abraham_present-day_2014,\\n\\ttitle = {Present-day vegetation helps quantifying past land cover in selected regions of the {Czech} {Republic}},\\n\\tvolume = {9},\\n\\tcopyright = {All rights reserved},\\n\\tdoi = {10.1371/journal.pone.0100117},\\n\\tabstract = {The REVEALS model is a tool for recalculating pollen data into vegetation abundances on a regional scale. We explored the general effect of selected parameters by performing simulations and ascertained the best model setting for the Czech Republic using the shallowest samples from 120 fossil sites and data on actual regional vegetation (60 km radius). Vegetation proportions of 17 taxa were obtained by combining the CORINE Land Cover map with forest inventories, agricultural statistics and habitat mapping data. Our simulation shows that changing the site radius for all taxa substantially affects REVEALS estimates of taxa with heavy or light pollen grains. Decreasing the site radius has a similar effect as increasing the wind speed parameter. However, adjusting the site radius to 1 m for local taxa only (even taxa with light pollen) yields lower, more correct estimates despite their high pollen signal. Increasing the background radius does not affect the estimates significantly. Our comparison of estimates with actual vegetation in seven regions shows that the most accurate relative pollen productivity estimates (PPEs) come from Central Europe and Southern Sweden. The initial simulation and pollen data yielded unrealistic estimates for Abies under the default setting of the wind speed parameter (3 m/s). We therefore propose the setting of 4 m/s, which corresponds to the spring average in most regions of the Czech Republic studied. Ad hoc adjustment of PPEs with this setting improves the match 3–4-fold. We consider these values (apart from four exceptions) to be appropriate, because they are within the ranges of standard errors, so they are related to original PPEs. Setting a 1 m radius for local taxa (Alnus, Salix, Poaceae) significantly improves the match between estimates and actual vegetation. However, further adjustments to PPEs exceed the ranges of original values, so their relevance is uncertain.},\\n\\tlanguage = {English},\\n\\tnumber = {6},\\n\\turldate = {2014-06-18},\\n\\tjournal = {PLoS ONE},\\n\\tauthor = {Abraham, Vojtěch and Oušková, Veronika and Kuneš, Petr},\\n\\tmonth = jun,\\n\\tyear = {2014},\\n\\tnote = {[IF2013=3.534]},\\n\\tkeywords = {Czech Republic, LRA, Pollen dispersal, Pollen production estimate (PPE), REVEALS, reconstruction, vegetation},\\n\\tpages = {e100117},\\n}\\n\\n\",\"author_short\":[\"Abraham, V.\",\"Oušková, V.\",\"Kuneš, P.\"],\"key\":\"abraham_present-day_2014\",\"id\":\"abraham_present-day_2014\",\"bibbaseid\":\"abraham-oukov-kune-presentdayvegetationhelpsquantifyingpastlandcoverinselectedregionsoftheczechrepublic-2014\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Czech Republic\",\"LRA\",\"Pollen dispersal\",\"Pollen production estimate (PPE)\",\"REVEALS\",\"reconstruction\",\"vegetation\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Regional climate model simulations for Europe at 6 and 0.2 k BP: sensitivity to changes in anthropogenic deforestation\",\"volume\":\"10\",\"copyright\":\"All rights reserved\",\"issn\":\"1814-9332\",\"shorttitle\":\"Regional climate model simulations for Europe at 6 and 0.2 k BP\",\"doi\":\"10.5194/cp-10-661-2014\",\"language\":\"English\",\"number\":\"2\",\"urldate\":\"2014-03-28\",\"journal\":\"Climate of the Past\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Strandberg\"],\"firstnames\":[\"G.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kjellström\"],\"firstnames\":[\"E.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Poska\"],\"firstnames\":[\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Wagner\"],\"firstnames\":[\"S.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Gaillard\"],\"firstnames\":[\"M.-J.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Trondman\"],\"firstnames\":[\"A.-K.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Mauri\"],\"firstnames\":[\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Davis\"],\"firstnames\":[\"B.\",\"A.\",\"S.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kaplan\"],\"firstnames\":[\"J.\",\"O.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Birks\"],\"firstnames\":[\"H.\",\"J.\",\"B.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bjune\"],\"firstnames\":[\"A.\",\"E.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Fyfe\"],\"firstnames\":[\"R.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Giesecke\"],\"firstnames\":[\"T.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kalnina\"],\"firstnames\":[\"L.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kangur\"],\"firstnames\":[\"M.\"],\"suffixes\":[]},{\"propositions\":[\"van\",\"der\"],\"lastnames\":[\"Knaap\"],\"firstnames\":[\"W.\",\"O.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kokfelt\"],\"firstnames\":[\"U.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"P.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Latałova\"],\"firstnames\":[\"M.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Marquer\"],\"firstnames\":[\"L.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Mazier\"],\"firstnames\":[\"F.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Nielsen\"],\"firstnames\":[\"A.\",\"B.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Smith\"],\"firstnames\":[\"B.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Seppä\"],\"firstnames\":[\"H.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Sugita\"],\"firstnames\":[\"S.\"],\"suffixes\":[]}],\"month\":\"March\",\"year\":\"2014\",\"note\":\"[IF2013=3.482]\",\"keywords\":\"Europe, REVEALS, climate model, human impact, reconstruction\",\"pages\":\"661–680\",\"bibtex\":\"@article{strandberg_regional_2014,\\n\\ttitle = {Regional climate model simulations for {Europe} at 6 and 0.2 k {BP}: sensitivity to changes in anthropogenic deforestation},\\n\\tvolume = {10},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {1814-9332},\\n\\tshorttitle = {Regional climate model simulations for {Europe} at 6 and 0.2 k {BP}},\\n\\tdoi = {10.5194/cp-10-661-2014},\\n\\tlanguage = {English},\\n\\tnumber = {2},\\n\\turldate = {2014-03-28},\\n\\tjournal = {Climate of the Past},\\n\\tauthor = {Strandberg, G. and Kjellström, E. and Poska, A. and Wagner, S. and Gaillard, M.-J. and Trondman, A.-K. and Mauri, A. and Davis, B. A. S. and Kaplan, J. O. and Birks, H. J. B. and Bjune, A. E. and Fyfe, R. and Giesecke, T. and Kalnina, L. and Kangur, M. and van der Knaap, W. O. and Kokfelt, U. and Kuneš, P. and Latałova, M. and Marquer, L. and Mazier, F. and Nielsen, A. B. and Smith, B. and Seppä, H. and Sugita, S.},\\n\\tmonth = mar,\\n\\tyear = {2014},\\n\\tnote = {[IF2013=3.482]},\\n\\tkeywords = {Europe, REVEALS, climate model, human impact, reconstruction},\\n\\tpages = {661--680},\\n}\\n\\n\",\"author_short\":[\"Strandberg, G.\",\"Kjellström, E.\",\"Poska, A.\",\"Wagner, S.\",\"Gaillard, M.\",\"Trondman, A.\",\"Mauri, A.\",\"Davis, B. A. S.\",\"Kaplan, J. O.\",\"Birks, H. J. B.\",\"Bjune, A. E.\",\"Fyfe, R.\",\"Giesecke, T.\",\"Kalnina, L.\",\"Kangur, M.\",\"van der Knaap, W. O.\",\"Kokfelt, U.\",\"Kuneš, P.\",\"Latałova, M.\",\"Marquer, L.\",\"Mazier, F.\",\"Nielsen, A. B.\",\"Smith, B.\",\"Seppä, H.\",\"Sugita, S.\"],\"key\":\"strandberg_regional_2014\",\"id\":\"strandberg_regional_2014\",\"bibbaseid\":\"strandberg-kjellstrm-poska-wagner-gaillard-trondman-mauri-davis-etal-regionalclimatemodelsimulationsforeuropeat6and02kbpsensitivitytochangesinanthropogenicdeforestation-2014\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Europe\",\"REVEALS\",\"climate model\",\"human impact\",\"reconstruction\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Testing quantitative pollen dispersal models in animal-pollinated vegetation mosaics: An example from temperate Tasmania, Australia\",\"volume\":\"154\",\"copyright\":\"All rights reserved\",\"issn\":\"0277-3791\",\"shorttitle\":\"Testing quantitative pollen dispersal models in animal-pollinated vegetation mosaics\",\"url\":\"http://www.sciencedirect.com/science/article/pii/S0277379116304851\",\"doi\":\"10.1016/j.quascirev.2016.10.020\",\"abstract\":\"Reconstructing past vegetation abundance and land-cover changes through time has important implications in land management and climate modelling. To date palaeovegetation reconstructions in Australia have been limited to qualitative or semi-quantitative inferences from pollen data. Testing pollen dispersal models constitutes a crucial step in developing quantitative past vegetation and land cover reconstructions. Thus far, the application of quantitative pollen dispersal models has been restricted to regions dominated by wind-pollinated plants (e.g. Europe) and their performance in a landscape dominated by animal-pollinated plant taxa is still unexplored. Here we test, for the first time in Australia, two well-known pollen dispersal models to assess their performance in the wind- and animal-pollinated vegetation mosaics of western Tasmania. We focus on a mix of wind- (6 taxa) and animal- (7 taxa) pollinated species that comprise the most common pollen types and key representatives of the dominant vegetation formations. Pollen Productivity Estimates and Relevant Source Area of Pollen obtained using Lagrangian Stochastic turbulent simulations appear to be more realistic when compared to the results from the widely used Gaussian Plume Model.\",\"urldate\":\"2016-11-18\",\"journal\":\"Quaternary Science Reviews\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Mariani\"],\"firstnames\":[\"M.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Connor\"],\"firstnames\":[\"S.\",\"E.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Theuerkauf\"],\"firstnames\":[\"M.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"P.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Fletcher\"],\"firstnames\":[\"M.\",\"-S.\"],\"suffixes\":[]}],\"month\":\"December\",\"year\":\"2016\",\"note\":\"[IF2015=4.521]\",\"keywords\":\"Australia, Pollen dispersal, Pollen production estimate (PPE), Tasmania, reconstruction\",\"pages\":\"214–225\",\"bibtex\":\"@article{mariani_testing_2016,\\n\\ttitle = {Testing quantitative pollen dispersal models in animal-pollinated vegetation mosaics: {An} example from temperate {Tasmania}, {Australia}},\\n\\tvolume = {154},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {0277-3791},\\n\\tshorttitle = {Testing quantitative pollen dispersal models in animal-pollinated vegetation mosaics},\\n\\turl = {http://www.sciencedirect.com/science/article/pii/S0277379116304851},\\n\\tdoi = {10.1016/j.quascirev.2016.10.020},\\n\\tabstract = {Reconstructing past vegetation abundance and land-cover changes through time has important implications in land management and climate modelling. To date palaeovegetation reconstructions in Australia have been limited to qualitative or semi-quantitative inferences from pollen data. Testing pollen dispersal models constitutes a crucial step in developing quantitative past vegetation and land cover reconstructions. Thus far, the application of quantitative pollen dispersal models has been restricted to regions dominated by wind-pollinated plants (e.g. Europe) and their performance in a landscape dominated by animal-pollinated plant taxa is still unexplored. Here we test, for the first time in Australia, two well-known pollen dispersal models to assess their performance in the wind- and animal-pollinated vegetation mosaics of western Tasmania. We focus on a mix of wind- (6 taxa) and animal- (7 taxa) pollinated species that comprise the most common pollen types and key representatives of the dominant vegetation formations. Pollen Productivity Estimates and Relevant Source Area of Pollen obtained using Lagrangian Stochastic turbulent simulations appear to be more realistic when compared to the results from the widely used Gaussian Plume Model.},\\n\\turldate = {2016-11-18},\\n\\tjournal = {Quaternary Science Reviews},\\n\\tauthor = {Mariani, M. and Connor, S. E. and Theuerkauf, M. and Kuneš, P. and Fletcher, M. -S.},\\n\\tmonth = dec,\\n\\tyear = {2016},\\n\\tnote = {[IF2015=4.521]},\\n\\tkeywords = {Australia, Pollen dispersal, Pollen production estimate (PPE), Tasmania, reconstruction},\\n\\tpages = {214--225},\\n}\\n\\n\",\"author_short\":[\"Mariani, M.\",\"Connor, S. E.\",\"Theuerkauf, M.\",\"Kuneš, P.\",\"Fletcher, M. -.\"],\"key\":\"mariani_testing_2016\",\"id\":\"mariani_testing_2016\",\"bibbaseid\":\"mariani-connor-theuerkauf-kune-fletcher-testingquantitativepollendispersalmodelsinanimalpollinatedvegetationmosaicsanexamplefromtemperatetasmaniaaustralia-2016\",\"role\":\"author\",\"urls\":{\"Paper\":\"http://www.sciencedirect.com/science/article/pii/S0277379116304851\"},\"keyword\":[\"Australia\",\"Pollen dispersal\",\"Pollen production estimate (PPE)\",\"Tasmania\",\"reconstruction\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"incollection\",\"type\":\"incollection\",\"address\":\"Cham\",\"edition\":\"1\",\"series\":\"Plant and Vegetation\",\"title\":\"History of Czech vegetation since the Late Pleistocene\",\"copyright\":\"All rights reserved\",\"isbn\":\"978-3-319-63180-6\",\"url\":\"https://link.springer.com/chapter/10.1007/978-3-319-63181-3_6\",\"abstract\":\"A long-term perspective is a crucial dimension for understanding the present-day composition and structure of the Czech flora and vegetation. We outline processes that were important for the development of the present-day diversity of flora and vegetation including extinctions of taxa and ecological mechanisms operating within glacial-interglacial cycles. Further, we present the history of vegetation during the key stages in the glacial and postglacial periods. First, we outline the pattern in the vegetation during the last glacial, including a discussion of the existence of refugia for trees. We further describe the changes in vegetation during the Late Glacial, which were mostly the results of abrupt climatic events. We also present a new synthesis of the Holocene regional development in vegetation based on a Landscape Reconstruction Algorithm, which results in different regional vegetation trajectories and three main phases in the development of vegetation. Finally, we give some examples of the histories of local vegetation at several sites mainly based on plant macrofossils.\",\"language\":\"English\",\"number\":\"14\",\"booktitle\":\"Flora and Vegetation of the Czech Republic\",\"publisher\":\"Springer\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Abraham\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]}],\"editor\":[{\"propositions\":[],\"lastnames\":[\"Chytrý\"],\"firstnames\":[\"Milan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Danihelka\"],\"firstnames\":[\"Jiří\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kaplan\"],\"firstnames\":[\"Zdeněk\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pyšek\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"year\":\"2017\",\"keywords\":\"Czech Republic, Holocene, Late Glacial, Plant macroremains, glacial, interglacial, pollen analysis, reconstruction, vegetation history\",\"pages\":\"193–227\",\"bibtex\":\"@incollection{kunes_history_2017,\\n\\taddress = {Cham},\\n\\tedition = {1},\\n\\tseries = {Plant and {Vegetation}},\\n\\ttitle = {History of {Czech} vegetation since the {Late} {Pleistocene}},\\n\\tcopyright = {All rights reserved},\\n\\tisbn = {978-3-319-63180-6},\\n\\turl = {https://link.springer.com/chapter/10.1007/978-3-319-63181-3_6},\\n\\tabstract = {A long-term perspective is a crucial dimension for understanding the present-day composition and structure of the Czech flora and vegetation. We outline processes that were important for the development of the present-day diversity of flora and vegetation including extinctions of taxa and ecological mechanisms operating within glacial-interglacial cycles. Further, we present the history of vegetation during the key stages in the glacial and postglacial periods. First, we outline the pattern in the vegetation during the last glacial, including a discussion of the existence of refugia for trees. We further describe the changes in vegetation during the Late Glacial, which were mostly the results of abrupt climatic events. We also present a new synthesis of the Holocene regional development in vegetation based on a Landscape Reconstruction Algorithm, which results in different regional vegetation trajectories and three main phases in the development of vegetation. Finally, we give some examples of the histories of local vegetation at several sites mainly based on plant macrofossils.},\\n\\tlanguage = {English},\\n\\tnumber = {14},\\n\\tbooktitle = {Flora and {Vegetation} of the {Czech} {Republic}},\\n\\tpublisher = {Springer},\\n\\tauthor = {Kuneš, Petr and Abraham, Vojtěch},\\n\\teditor = {Chytrý, Milan and Danihelka, Jiří and Kaplan, Zdeněk and Pyšek, Petr},\\n\\tyear = {2017},\\n\\tkeywords = {Czech Republic, Holocene, Late Glacial, Plant macroremains, glacial, interglacial, pollen analysis, reconstruction, vegetation history},\\n\\tpages = {193--227},\\n}\\n\\n\",\"author_short\":[\"Kuneš, P.\",\"Abraham, V.\"],\"editor_short\":[\"Chytrý, M.\",\"Danihelka, J.\",\"Kaplan, Z.\",\"Pyšek, P.\"],\"key\":\"kunes_history_2017\",\"id\":\"kunes_history_2017\",\"bibbaseid\":\"kune-abraham-historyofczechvegetationsincethelatepleistocene-2017\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://link.springer.com/chapter/10.1007/978-3-319-63181-3_6\"},\"keyword\":[\"Czech Republic\",\"Holocene\",\"Late Glacial\",\"Plant macroremains\",\"glacial\",\"interglacial\",\"pollen analysis\",\"reconstruction\",\"vegetation history\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"How old is the Tasmanian cultural landscape? A test of landscape openness using quantitative land-cover reconstructions\",\"volume\":\"44\",\"copyright\":\"All rights reserved\",\"issn\":\"1365–2699\",\"shorttitle\":\"How old is the Tasmanian cultural landscape?\",\"doi\":\"10.1111/jbi.13040\",\"abstract\":\"Aim: To test competing hypotheses about the timing and extent of Holocene landscape opening using pollen-based quantitative land-cover estimates. Location: Dove Lake, Tasmanian Wilderness World Heritage Area, Australia. Methods: Fossil pollen data were incorporated into pollen dispersal models and corrected for differences in pollen productivity among key plant taxa. Mechanistic models (REVEALS—Regional Estimates of VEgetation Abundance from Large Sites) employing different models for pollen dispersal (Gaussian plume and Lagrangian stochastic models) were evaluated and applied in the Southern Hemisphere for the first time. Results: Validation of the REVEALS model with vegetation cover data suggests an overall better performance of the Lagrangian stochastic model. Regional land-cover estimates for forest and non-forest plant taxa show persistent landscape openness throughout the Holocene (average landscape openness ~50%). Gymnoschoenus sphaerocephalus, an indicator of moorland vegetation, shows higher values during the early Holocene (11.7–9 ka) and declines slightly through the mid-Holocene (9–4.5 ka) during a phase of partial landscape afforestation. Rain forest cover reduced (from ~40% to ~20%) during the period between 4.2–3.5 ka. Main conclusions: Pollen percentages severely under-represent landscape openness in western Tasmania and this bias has fostered an over-estimation of Holocene forest cover from pollen data. Treeless vegetation dominated Holocene landscapes of the Dove Lake area, allowing us to reject models of landscape evolution that invoke late-Holocene replacement of a rain forest-dominated landscape by moorland. Instead, we confirm a model of Late Pleistocene inheritance of open vegetation. Rapid forest decline occurred after c. 4 ka, likely in response to regional moisture decline.\",\"language\":\"English\",\"number\":\"10\",\"journal\":\"Journal of Biogeography\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Mariani\"],\"firstnames\":[\"Michela\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Connor\"],\"firstnames\":[\"Simon\",\"E.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Fletcher\"],\"firstnames\":[\"Michael-S.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Theuerkauf\"],\"firstnames\":[\"Martin\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jacobsen\"],\"firstnames\":[\"Geraldine\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Saunders\"],\"firstnames\":[\"Krystyna\",\"M.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Zawadzki\"],\"firstnames\":[\"Atun\"],\"suffixes\":[]}],\"year\":\"2017\",\"note\":\"[IF2016=4.248]\",\"keywords\":\"Australia, Holocene, REVEALS, Tasmania, cultural landscape, dispersal models, fire, landcover reconstruction, moorland, rain forest, reconstruction\",\"pages\":\"2410–2420\",\"bibtex\":\"@article{mariani_how_2017,\\n\\ttitle = {How old is the {Tasmanian} cultural landscape? {A} test of landscape openness using quantitative land-cover reconstructions},\\n\\tvolume = {44},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {1365–2699},\\n\\tshorttitle = {How old is the {Tasmanian} cultural landscape?},\\n\\tdoi = {10.1111/jbi.13040},\\n\\tabstract = {Aim: To test competing hypotheses about the timing and extent of Holocene landscape opening using pollen-based quantitative land-cover estimates.\\nLocation: Dove Lake, Tasmanian Wilderness World Heritage Area, Australia.\\nMethods: Fossil pollen data were incorporated into pollen dispersal models and corrected for differences in pollen productivity among key plant taxa. Mechanistic models (REVEALS—Regional Estimates of VEgetation Abundance from Large Sites) employing different models for pollen dispersal (Gaussian plume and Lagrangian stochastic models) were evaluated and applied in the Southern Hemisphere for the first time.\\nResults: Validation of the REVEALS model with vegetation cover data suggests an overall better performance of the Lagrangian stochastic model. Regional land-cover estimates for forest and non-forest plant taxa show persistent landscape openness throughout the Holocene (average landscape openness {\\\\textasciitilde}50\\\\%). Gymnoschoenus sphaerocephalus, an indicator of moorland vegetation, shows higher values during the early Holocene (11.7–9 ka) and declines slightly through the mid-Holocene (9–4.5 ka) during a phase of partial landscape afforestation. Rain forest cover reduced (from {\\\\textasciitilde}40\\\\% to {\\\\textasciitilde}20\\\\%) during the period between 4.2–3.5 ka.\\nMain conclusions: Pollen percentages severely under-represent landscape openness in western Tasmania and this bias has fostered an over-estimation of Holocene forest cover from pollen data. Treeless vegetation dominated Holocene landscapes of the Dove Lake area, allowing us to reject models of landscape evolution that invoke late-Holocene replacement of a rain forest-dominated landscape by moorland. Instead, we confirm a model of Late Pleistocene inheritance of open vegetation. Rapid forest decline occurred after c. 4 ka, likely in response to regional moisture decline.},\\n\\tlanguage = {English},\\n\\tnumber = {10},\\n\\tjournal = {Journal of Biogeography},\\n\\tauthor = {Mariani, Michela and Connor, Simon E. and Fletcher, Michael-S. and Theuerkauf, Martin and Kuneš, Petr and Jacobsen, Geraldine and Saunders, Krystyna M. and Zawadzki, Atun},\\n\\tyear = {2017},\\n\\tnote = {[IF2016=4.248]},\\n\\tkeywords = {Australia, Holocene, REVEALS, Tasmania, cultural landscape, dispersal models, fire, landcover reconstruction, moorland, rain forest, reconstruction},\\n\\tpages = {2410--2420},\\n}\\n\\n\",\"author_short\":[\"Mariani, M.\",\"Connor, S. E.\",\"Fletcher, M.\",\"Theuerkauf, M.\",\"Kuneš, P.\",\"Jacobsen, G.\",\"Saunders, K. M.\",\"Zawadzki, A.\"],\"key\":\"mariani_how_2017\",\"id\":\"mariani_how_2017\",\"bibbaseid\":\"mariani-connor-fletcher-theuerkauf-kune-jacobsen-saunders-zawadzki-howoldisthetasmanianculturallandscapeatestoflandscapeopennessusingquantitativelandcoverreconstructions-2017\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Australia\",\"Holocene\",\"REVEALS\",\"Tasmania\",\"cultural landscape\",\"dispersal models\",\"fire\",\"landcover reconstruction\",\"moorland\",\"rain forest\",\"reconstruction\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Quantitative palynology informing conservation ecology in the Bohemian/Bavarian Forests of Central Europe\",\"volume\":\"8\",\"issn\":\"1664-462X\",\"doi\":\"10.3389/fpls.2017.02268\",\"abstract\":\"In 1927, the first pollen diagram was published from the Bohemian/Bavarian Forest region of Central Europe, providing one of the first qualitative views of the long-term vegetation development in the region. Since then significant methodological advances in quantitative approaches such as pollen influx and pollen-based vegetation models (e.g., Landscape Reconstruction Algorithm, LRA) have contributed to enhance our understanding of temporal and spatial ecology. These types of quantitative reconstructions are fundamental for conservation and restoration ecology because they provide long-term perspectives on ecosystem functioning. In the Bohemian/Bavarian Forests, forest managers have a goal to restore the original forest composition at mid-elevation forests, yet they rely on natural potential vegetation maps that do not take into account long-term vegetation dynamics. Here we reconstruct the Holocene history of forest composition and discuss the implications the LRA has for regional forest management and conservation. Two newly analysed pollen records from Prášilské jezero and Rachelsee were compared to 10 regional peat bogs/mires and two other regional lakes to reconstruct total land-cover abundance at both the regional- and local-scales. The results demonstrate that spruce has been the dominate canopy cover across the region for the past 9000 years at both high- (\\\\textgreater900 m) and mid-elevations (\\\\textgreater700-900 m) elevations. At the regional-scale, inferred from lake records, spruce has comprised an average of ~50% of the total forest canopy; whereas at the more local-scale at mid-elevations, spruce formed ~59%. Beech established ~6000 cal yr BP while fir established ~5500 cal yr BP, and reached a maximum land-cover abundance of 24% and 13% roughly 1000 years ago at mid-elevations. Over the past 500 years spruce has comprised ~47% land-cover, while beech and fir comprised ~8% and \\\\textless5% at mid-elevations. This approach argues for the ‘natural’ development of spruce and fir locally in zones where the paleoecology indicates the persistence of these species for millennia. Contrasting local and regional reconstructions of forest canopy cover points to a patchwork mosaic with local variability in the dominant taxa. Incorporation of paleoecological data in dialogues about biodiversity and ecosystem management is an approach that has wider utility.\",\"language\":\"English\",\"number\":\"Article 2268\",\"urldate\":\"2017-12-28\",\"journal\":\"Frontiers in Plant Science\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Carter\"],\"firstnames\":[\"Vachel\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chiverrell\"],\"firstnames\":[\"Richard\",\"C.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Clear\"],\"firstnames\":[\"Jennifer\",\"L.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuosmanen\"],\"firstnames\":[\"Niina\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Moravcová\"],\"firstnames\":[\"Alice\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svoboda\"],\"firstnames\":[\"Miroslav\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svobodová-Svitavská\"],\"firstnames\":[\"Helena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Leeuwen\"],\"firstnames\":[\"Van\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Van\",\"Leeuwen\"],\"firstnames\":[\"Jacqueline\"],\"suffixes\":[]},{\"propositions\":[\"van\",\"der\"],\"lastnames\":[\"Knaap\"],\"firstnames\":[\"Willem\",\"O.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"year\":\"2018\",\"note\":\"[IF2017=3.678]\",\"keywords\":\"Abies alba, Fagus sylvatica, Holocene, Picea abies, Pollen, Reveals, disturbance, landcover, palynology, reconstruction\",\"pages\":\"1–14\",\"bibtex\":\"@article{carter_quantitative_2018,\\n\\ttitle = {Quantitative palynology informing conservation ecology in the {Bohemian}/{Bavarian} {Forests} of {Central} {Europe}},\\n\\tvolume = {8},\\n\\tissn = {1664-462X},\\n\\tdoi = {10.3389/fpls.2017.02268},\\n\\tabstract = {In 1927, the first pollen diagram was published from the Bohemian/Bavarian Forest region of Central Europe, providing one of the first qualitative views of the long-term vegetation development in the region. Since then significant methodological advances in quantitative approaches such as pollen influx and pollen-based vegetation models (e.g., Landscape Reconstruction Algorithm, LRA) have contributed to enhance our understanding of temporal and spatial ecology. These types of quantitative reconstructions are fundamental for conservation and restoration ecology because they provide long-term perspectives on ecosystem functioning. In the Bohemian/Bavarian Forests, forest managers have a goal to restore the original forest composition at mid-elevation forests, yet they rely on natural potential vegetation maps that do not take into account long-term vegetation dynamics. Here we reconstruct the Holocene history of forest composition and discuss the implications the LRA has for regional forest management and conservation. Two newly analysed pollen records from Prášilské jezero and Rachelsee were compared to 10 regional peat bogs/mires and two other regional lakes to reconstruct total land-cover abundance at both the regional- and local-scales. The results demonstrate that spruce has been the dominate canopy cover across the region for the past 9000 years at both high- ({\\\\textgreater}900 m) and mid-elevations ({\\\\textgreater}700-900 m) elevations. At the regional-scale, inferred from lake records, spruce has comprised an average of {\\\\textasciitilde}50\\\\% of the total forest canopy; whereas at the more local-scale at mid-elevations, spruce formed {\\\\textasciitilde}59\\\\%. Beech established {\\\\textasciitilde}6000 cal yr BP while fir established {\\\\textasciitilde}5500 cal yr BP, and reached a maximum land-cover abundance of 24\\\\% and 13\\\\% roughly 1000 years ago at mid-elevations. Over the past 500 years spruce has comprised {\\\\textasciitilde}47\\\\% land-cover, while beech and fir comprised {\\\\textasciitilde}8\\\\% and {\\\\textless}5\\\\% at mid-elevations. This approach argues for the ‘natural’ development of spruce and fir locally in zones where the paleoecology indicates the persistence of these species for millennia. Contrasting local and regional reconstructions of forest canopy cover points to a patchwork mosaic with local variability in the dominant taxa. Incorporation of paleoecological data in dialogues about biodiversity and ecosystem management is an approach that has wider utility.},\\n\\tlanguage = {English},\\n\\tnumber = {Article 2268},\\n\\turldate = {2017-12-28},\\n\\tjournal = {Frontiers in Plant Science},\\n\\tauthor = {Carter, Vachel A. and Chiverrell, Richard C. and Clear, Jennifer L. and Kuosmanen, Niina and Moravcová, Alice and Svoboda, Miroslav and Svobodová-Svitavská, Helena and Leeuwen, Van and Van Leeuwen, Jacqueline and van der Knaap, Willem O. and Kuneš, Petr},\\n\\tyear = {2018},\\n\\tnote = {[IF2017=3.678]},\\n\\tkeywords = {Abies alba, Fagus sylvatica, Holocene, Picea abies, Pollen, Reveals, disturbance, landcover, palynology, reconstruction},\\n\\tpages = {1--14},\\n}\\n\\n\",\"author_short\":[\"Carter, V. A.\",\"Chiverrell, R. C.\",\"Clear, J. L.\",\"Kuosmanen, N.\",\"Moravcová, A.\",\"Svoboda, M.\",\"Svobodová-Svitavská, H.\",\"Leeuwen, V.\",\"Van Leeuwen, J.\",\"van der Knaap, W. O.\",\"Kuneš, P.\"],\"key\":\"carter_quantitative_2018\",\"id\":\"carter_quantitative_2018\",\"bibbaseid\":\"carter-chiverrell-clear-kuosmanen-moravcov-svoboda-svobodovsvitavsk-leeuwen-etal-quantitativepalynologyinformingconservationecologyinthebohemianbavarianforestsofcentraleurope-2018\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Abies alba\",\"Fagus sylvatica\",\"Holocene\",\"Picea abies\",\"Pollen\",\"Reveals\",\"disturbance\",\"landcover\",\"palynology\",\"reconstruction\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":2,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Relative pollen productivity estimates for vegetation reconstruction in central-eastern Europe inferred at local and regional scales\",\"volume\":\"29\",\"issn\":\"0959-6836\",\"doi\":\"10.1177/0959683619862026\",\"abstract\":\"Understanding pollen-vegetation relationships is crucial for accurate land-cover and climate reconstructions, yet important parameters for quantifying past vegetation abundance are mostly unknown for large parts of Europe harbouring temperate thermophilous ecosystems. We collected pollen and vegetation data in central-eastern Europe, a region covered by patchy cultural landscapes of high biodiversity to estimate relative pollen productivity (RPP) for important pollen-equivalent taxa. Our study area was situated in the south-western part of the White Carpathians (Czechia–Slovakia borderland), where we collected 40 modern moss pollen samples scattered over 250 km2 and mapped vegetation within 100 m around each pollen site. Additional vegetation data were compiled from Forest management plans, Natura 2000 habitat mapping and floristic inventories over the entire area. We calculated RPP (referenced to Poaceae) by testing two approaches: the extended R-value (ERV) model by estimating relevant source area of pollen and the REVEALS-based productivity using regional scale vegetation estimates. Two models were applied to depict pollen dispersal: Lagrangian stochastic and the Gaussian plume (Prentice) models. We estimated RPP for 16 taxa using the ERV model and an additional nine taxa using REVEALS. Both approaches found Plantago lanceolata-type to be a high pollen producer, Quercus medium-to-high, Asteraceae subf. Cichorioideae, Anthemis-type, Ranunculus acris-type and Rubiaceae low-to-medium and Brassicaceae and Senecio-type as low pollen producers. Results for other, mainly tree taxa, significantly differed in both approaches mainly due to largely uneven representation in both local and regional vegetation. In comparison with other studies, our data demonstrate a high variability in the estimated RPPs which could be influenced by climatic conditions or potentially vegetation structure. We suggest that the accuracy of RPP estimates could be enhanced by comparing modern pollen data with large-scale vegetation data in the future.\",\"language\":\"English\",\"number\":\"11\",\"urldate\":\"2019-09-18\",\"journal\":\"The Holocene\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Abraham\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Werchan\"],\"firstnames\":[\"Barbora\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Plesková\"],\"firstnames\":[\"Zuzana\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Fajmon\"],\"firstnames\":[\"Karel\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jamrichová\"],\"firstnames\":[\"Eva\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Roleček\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]}],\"month\":\"November\",\"year\":\"2019\",\"note\":\"[IF2018=2.547]\",\"keywords\":\"Czech Republic, ERV model, Gaussian plume model, LRA, Lagrangian stochastic model, REVEALS, modern pollen spectra, reconstruction, vegetation cover\",\"pages\":\"1708–1719\",\"bibtex\":\"@article{kunes_relative_2019,\\n\\ttitle = {Relative pollen productivity estimates for vegetation reconstruction in central-eastern {Europe} inferred at local and regional scales},\\n\\tvolume = {29},\\n\\tissn = {0959-6836},\\n\\tdoi = {10.1177/0959683619862026},\\n\\tabstract = {Understanding pollen-vegetation relationships is crucial for accurate land-cover and climate reconstructions, yet important parameters for quantifying past vegetation abundance are mostly unknown for large parts of Europe harbouring temperate thermophilous ecosystems. We collected pollen and vegetation data in central-eastern Europe, a region covered by patchy cultural landscapes of high biodiversity to estimate relative pollen productivity (RPP) for important pollen-equivalent taxa. Our study area was situated in the south-western part of the White Carpathians (Czechia–Slovakia borderland), where we collected 40 modern moss pollen samples scattered over 250 km2 and mapped vegetation within 100 m around each pollen site. Additional vegetation data were compiled from Forest management plans, Natura 2000 habitat mapping and floristic inventories over the entire area. We calculated RPP (referenced to Poaceae) by testing two approaches: the extended R-value (ERV) model by estimating relevant source area of pollen and the REVEALS-based productivity using regional scale vegetation estimates. Two models were applied to depict pollen dispersal: Lagrangian stochastic and the Gaussian plume (Prentice) models. We estimated RPP for 16 taxa using the ERV model and an additional nine taxa using REVEALS. Both approaches found Plantago lanceolata-type to be a high pollen producer, Quercus medium-to-high, Asteraceae subf. Cichorioideae, Anthemis-type, Ranunculus acris-type and Rubiaceae low-to-medium and Brassicaceae and Senecio-type as low pollen producers. Results for other, mainly tree taxa, significantly differed in both approaches mainly due to largely uneven representation in both local and regional vegetation. In comparison with other studies, our data demonstrate a high variability in the estimated RPPs which could be influenced by climatic conditions or potentially vegetation structure. We suggest that the accuracy of RPP estimates could be enhanced by comparing modern pollen data with large-scale vegetation data in the future.},\\n\\tlanguage = {English},\\n\\tnumber = {11},\\n\\turldate = {2019-09-18},\\n\\tjournal = {The Holocene},\\n\\tauthor = {Kuneš, Petr and Abraham, Vojtěch and Werchan, Barbora and Plesková, Zuzana and Fajmon, Karel and Jamrichová, Eva and Roleček, Jan},\\n\\tmonth = nov,\\n\\tyear = {2019},\\n\\tnote = {[IF2018=2.547]},\\n\\tkeywords = {Czech Republic, ERV model, Gaussian plume model, LRA, Lagrangian stochastic model, REVEALS, modern pollen spectra, reconstruction, vegetation cover},\\n\\tpages = {1708--1719},\\n}\\n\\n\",\"author_short\":[\"Kuneš, P.\",\"Abraham, V.\",\"Werchan, B.\",\"Plesková, Z.\",\"Fajmon, K.\",\"Jamrichová, E.\",\"Roleček, J.\"],\"key\":\"kunes_relative_2019\",\"id\":\"kunes_relative_2019\",\"bibbaseid\":\"kune-abraham-werchan-pleskov-fajmon-jamrichov-roleek-relativepollenproductivityestimatesforvegetationreconstructionincentraleasterneuropeinferredatlocalandregionalscales-2019\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Czech Republic\",\"ERV model\",\"Gaussian plume model\",\"LRA\",\"Lagrangian stochastic model\",\"REVEALS\",\"modern pollen spectra\",\"reconstruction\",\"vegetation cover\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":2,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Changes in species composition and diversity of a montane beetle community over the last millennium in the High Tatras, Slovakia: Implications for forest conservation and management\",\"volume\":\"555\",\"issn\":\"0031-0182\",\"shorttitle\":\"Changes in species composition and diversity of a montane beetle community over the last millennium in the High Tatras, Slovakia\",\"doi\":\"10.1016/j.palaeo.2020.109834\",\"abstract\":\"Montane biomes are niche environments high in biodiversity with a variety of habitats. Often isolated, these non-continuous remnant ecosystems inhabit narrow ecological zones putting them under threat from changing climatic conditions and anthropogenic pressure. Twelve sediment cores were retrieved from a peat bog in Tatra National Park, Slovakia, and correlated to each other by wiggle-matching geochemical signals derived from micro-XRF scanning, to make a reconstruction of past conditions. A fossil beetle (Coleoptera) record, covering the last 1000 years at 50- to 100-year resolution, gives a new insight into changing flora and fauna in this region. Our findings reveal a diverse beetle community with varied ecological groups inhabiting a range of forest, meadow and synanthropic habitats. Changes in the beetle community were related to changes in the landscape, driven by anthropogenic activities. The first clear evidence for human activity in the area occurs c. 1250 CE and coincides with the arrival of beetle species living on the dung of domesticated animals (e.g. Aphodius spp.). From 1500 CE, human (re)settlement, and activities such as pasturing and charcoal burning, appear to have had a pronounced effect on the beetle community. Local beetle diversity declined steadily towards the present day, likely due to an infilling of the forest hollow leading to a decrease in moisture level. We conclude that beetle communities are directly affected by anthropogenic intensity and land-use change. When aiming to preserve or restore natural forest conditions, recording their past changes in diversity can help guide conservation and restoration. In doing so, it is important to look back beyond the time of significant human impact, and for this, information contained in paleoecological records is irreplaceable.\",\"language\":\"English\",\"urldate\":\"2020-06-20\",\"journal\":\"Palaeogeography, Palaeoclimatology, Palaeoecology\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Schafstall\"],\"firstnames\":[\"Nick\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Whitehouse\"],\"firstnames\":[\"Nicki\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuosmanen\"],\"firstnames\":[\"Niina\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svobodová-Svitavská\"],\"firstnames\":[\"Helena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Saulnier\"],\"firstnames\":[\"Mélanie\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chiverrell\"],\"firstnames\":[\"Richard\",\"C.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Fleischer\"],\"firstnames\":[\"Peter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Clear\"],\"firstnames\":[\"Jennifer\",\"L.\"],\"suffixes\":[]}],\"month\":\"October\",\"year\":\"2020\",\"note\":\"[IF2019=2.833]\",\"keywords\":\"Biodiversity, Central Europe, Climate change, Coleoptera, Human impact, Nature conservation, disturbance\",\"pages\":\"109834\",\"bibtex\":\"@article{schafstall_changes_2020,\\n\\ttitle = {Changes in species composition and diversity of a montane beetle community over the last millennium in the {High} {Tatras}, {Slovakia}: {Implications} for forest conservation and management},\\n\\tvolume = {555},\\n\\tissn = {0031-0182},\\n\\tshorttitle = {Changes in species composition and diversity of a montane beetle community over the last millennium in the {High} {Tatras}, {Slovakia}},\\n\\tdoi = {10.1016/j.palaeo.2020.109834},\\n\\tabstract = {Montane biomes are niche environments high in biodiversity with a variety of habitats. Often isolated, these non-continuous remnant ecosystems inhabit narrow ecological zones putting them under threat from changing climatic conditions and anthropogenic pressure. Twelve sediment cores were retrieved from a peat bog in Tatra National Park, Slovakia, and correlated to each other by wiggle-matching geochemical signals derived from micro-XRF scanning, to make a reconstruction of past conditions. A fossil beetle (Coleoptera) record, covering the last 1000 years at 50- to 100-year resolution, gives a new insight into changing flora and fauna in this region. Our findings reveal a diverse beetle community with varied ecological groups inhabiting a range of forest, meadow and synanthropic habitats. Changes in the beetle community were related to changes in the landscape, driven by anthropogenic activities. The first clear evidence for human activity in the area occurs c. 1250 CE and coincides with the arrival of beetle species living on the dung of domesticated animals (e.g. Aphodius spp.). From 1500 CE, human (re)settlement, and activities such as pasturing and charcoal burning, appear to have had a pronounced effect on the beetle community. Local beetle diversity declined steadily towards the present day, likely due to an infilling of the forest hollow leading to a decrease in moisture level. We conclude that beetle communities are directly affected by anthropogenic intensity and land-use change. When aiming to preserve or restore natural forest conditions, recording their past changes in diversity can help guide conservation and restoration. In doing so, it is important to look back beyond the time of significant human impact, and for this, information contained in paleoecological records is irreplaceable.},\\n\\tlanguage = {English},\\n\\turldate = {2020-06-20},\\n\\tjournal = {Palaeogeography, Palaeoclimatology, Palaeoecology},\\n\\tauthor = {Schafstall, Nick and Whitehouse, Nicki and Kuosmanen, Niina and Svobodová-Svitavská, Helena and Saulnier, Mélanie and Chiverrell, Richard C. and Fleischer, Peter and Kuneš, Petr and Clear, Jennifer L.},\\n\\tmonth = oct,\\n\\tyear = {2020},\\n\\tnote = {[IF2019=2.833]},\\n\\tkeywords = {Biodiversity, Central Europe, Climate change, Coleoptera, Human impact, Nature conservation, disturbance},\\n\\tpages = {109834},\\n}\\n\\n\",\"author_short\":[\"Schafstall, N.\",\"Whitehouse, N.\",\"Kuosmanen, N.\",\"Svobodová-Svitavská, H.\",\"Saulnier, M.\",\"Chiverrell, R. C.\",\"Fleischer, P.\",\"Kuneš, P.\",\"Clear, J. L.\"],\"key\":\"schafstall_changes_2020\",\"id\":\"schafstall_changes_2020\",\"bibbaseid\":\"schafstall-whitehouse-kuosmanen-svobodovsvitavsk-saulnier-chiverrell-fleischer-kune-etal-changesinspeciescompositionanddiversityofamontanebeetlecommunityoverthelastmillenniuminthehightatrasslovakiaimplicationsforforestconservationandmanagement-2020\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Biodiversity\",\"Central Europe\",\"Climate change\",\"Coleoptera\",\"Human impact\",\"Nature conservation\",\"disturbance\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":2,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Integration of dendrochronological and palaeoecological disturbance reconstructions in temperate mountain forests\",\"volume\":\"475\",\"issn\":\"0378-1127\",\"doi\":\"10.1016/j.foreco.2020.118413\",\"abstract\":\"Disentangling the long-term changes in forest disturbance dynamics provides a basis for predicting the forest responses to changing environmental conditions. The combination of multidisciplinary records can offer more robust reconstructions of past forest disturbance dynamics. Here we link disturbance histories of the central European mountain spruce forest obtained from dendrochronological and palaeoecological records (fossil pollen, sedimentary charcoal, bark beetle remains and geochemistry) using a small glacial lake and the surrounding forest in the Šumava National Park (Czech Republic). Dendrochronological reconstructions of disturbance were created for 300-year-long records from 6 study plots with a minimum of 35 trees analyzed for the abrupt growth increases (releases) and rapid early growth rates, both indicative of disturbance events. High-resolution analysis of lake sediments were used to reconstruct 800-year long changes in forest composition and landscape openness (fossil pollen), past fire events (micro- and macroscopic charcoal), bark beetle occurrence (fossil bark beetle remains), and erosion episodes (geochemical signals in the sediment) potentially resulting from disturbance events. Tree-ring data indicate that disturbances occurred regularly through the last three centuries and identify a most intensive period of disturbances between 1780 and 1830 CE. Geochemical erosion markers (e.g. K, Zr, % inorganic) show greater flux of catchment sediment and soils in the periods 1250–1400 and 1450–1500 CE, before a substantial shift to a more erosive regime 1600–1850 and 1900 CE onwards. Pollen records demonstrate relatively small changes in forest composition during the last 800 years until the beginning of the 20th century, when there was decrease in Picea. Fossil bark beetle remains indicate continuous presence of bark beetles from 1620s to 1800s, and charcoal records suggest that more frequent fires occurred during the 18th century. Each of the dendrochronological, palaeoecological and sedimentological records provide a unique perspective on forest disturbance dynamics, and combined offer a more robust and complete record of disturbance history. We demonstrate that sedimentary proxies originating from the lake catchment mirror the forest disturbance dynamics recorded in the tree-rings. The multidisciplinary records likely record forest disturbances at different spatial and temporal scales revealing different disturbance characteristics. Integrating these multidisciplinary datasets demonstrates a promising way to obtain more complete understanding of long-term disturbance dynamics. However, integrating datasets with variable spatial and temporal influence remains challenging. Our results indicated that multiple disturbance factors, such as windstorms, bark beetle outbeaks and fires, may occur simultaneously creating a complex disturbance regime in mountain forests, which should be considered in forest management and conservation strategies.\",\"language\":\"English\",\"urldate\":\"2020-08-02\",\"journal\":\"Forest Ecology and Management\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kuosmanen\"],\"firstnames\":[\"Niina\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Čada\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Halsall\"],\"firstnames\":[\"Karen\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chiverrell\"],\"firstnames\":[\"Richard\",\"C.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Schafstall\"],\"firstnames\":[\"Nick\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Boyle\"],\"firstnames\":[\"John\",\"F.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Knížek\"],\"firstnames\":[\"Miloš\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Appleby\"],\"firstnames\":[\"Peter\",\"G.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svoboda\"],\"firstnames\":[\"Miroslav\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Clear\"],\"firstnames\":[\"Jennifer\",\"L.\"],\"suffixes\":[]}],\"month\":\"November\",\"year\":\"2020\",\"note\":\"[IF2019=3.17]\",\"keywords\":\"Bark beetles, Fire, Forest dynamics, Geochemistry, Pollen, Tree-rings, disturbance\",\"pages\":\"118413\",\"bibtex\":\"@article{kuosmanen_integration_2020,\\n\\ttitle = {Integration of dendrochronological and palaeoecological disturbance reconstructions in temperate mountain forests},\\n\\tvolume = {475},\\n\\tissn = {0378-1127},\\n\\tdoi = {10.1016/j.foreco.2020.118413},\\n\\tabstract = {Disentangling the long-term changes in forest disturbance dynamics provides a basis for predicting the forest responses to changing environmental conditions. The combination of multidisciplinary records can offer more robust reconstructions of past forest disturbance dynamics. Here we link disturbance histories of the central European mountain spruce forest obtained from dendrochronological and palaeoecological records (fossil pollen, sedimentary charcoal, bark beetle remains and geochemistry) using a small glacial lake and the surrounding forest in the Šumava National Park (Czech Republic). Dendrochronological reconstructions of disturbance were created for 300-year-long records from 6 study plots with a minimum of 35 trees analyzed for the abrupt growth increases (releases) and rapid early growth rates, both indicative of disturbance events. High-resolution analysis of lake sediments were used to reconstruct 800-year long changes in forest composition and landscape openness (fossil pollen), past fire events (micro- and macroscopic charcoal), bark beetle occurrence (fossil bark beetle remains), and erosion episodes (geochemical signals in the sediment) potentially resulting from disturbance events. Tree-ring data indicate that disturbances occurred regularly through the last three centuries and identify a most intensive period of disturbances between 1780 and 1830 CE. Geochemical erosion markers (e.g. K, Zr, \\\\% inorganic) show greater flux of catchment sediment and soils in the periods 1250–1400 and 1450–1500 CE, before a substantial shift to a more erosive regime 1600–1850 and 1900 CE onwards. Pollen records demonstrate relatively small changes in forest composition during the last 800 years until the beginning of the 20th century, when there was decrease in Picea. Fossil bark beetle remains indicate continuous presence of bark beetles from 1620s to 1800s, and charcoal records suggest that more frequent fires occurred during the 18th century. Each of the dendrochronological, palaeoecological and sedimentological records provide a unique perspective on forest disturbance dynamics, and combined offer a more robust and complete record of disturbance history. We demonstrate that sedimentary proxies originating from the lake catchment mirror the forest disturbance dynamics recorded in the tree-rings. The multidisciplinary records likely record forest disturbances at different spatial and temporal scales revealing different disturbance characteristics. Integrating these multidisciplinary datasets demonstrates a promising way to obtain more complete understanding of long-term disturbance dynamics. However, integrating datasets with variable spatial and temporal influence remains challenging. Our results indicated that multiple disturbance factors, such as windstorms, bark beetle outbeaks and fires, may occur simultaneously creating a complex disturbance regime in mountain forests, which should be considered in forest management and conservation strategies.},\\n\\tlanguage = {English},\\n\\turldate = {2020-08-02},\\n\\tjournal = {Forest Ecology and Management},\\n\\tauthor = {Kuosmanen, Niina and Čada, Vojtěch and Halsall, Karen and Chiverrell, Richard C. and Schafstall, Nick and Kuneš, Petr and Boyle, John F. and Knížek, Miloš and Appleby, Peter G. and Svoboda, Miroslav and Clear, Jennifer L.},\\n\\tmonth = nov,\\n\\tyear = {2020},\\n\\tnote = {[IF2019=3.17]},\\n\\tkeywords = {Bark beetles, Fire, Forest dynamics, Geochemistry, Pollen, Tree-rings, disturbance},\\n\\tpages = {118413},\\n}\\n\\n\",\"author_short\":[\"Kuosmanen, N.\",\"Čada, V.\",\"Halsall, K.\",\"Chiverrell, R. C.\",\"Schafstall, N.\",\"Kuneš, P.\",\"Boyle, J. F.\",\"Knížek, M.\",\"Appleby, P. G.\",\"Svoboda, M.\",\"Clear, J. L.\"],\"key\":\"kuosmanen_integration_2020\",\"id\":\"kuosmanen_integration_2020\",\"bibbaseid\":\"kuosmanen-ada-halsall-chiverrell-schafstall-kune-boyle-knek-etal-integrationofdendrochronologicalandpalaeoecologicaldisturbancereconstructionsintemperatemountainforests-2020\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Bark beetles\",\"Fire\",\"Forest dynamics\",\"Geochemistry\",\"Pollen\",\"Tree-rings\",\"disturbance\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":2,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Pollen-based climate reconstruction techniques for late Quaternary studies\",\"volume\":\"210\",\"issn\":\"0012-8252\",\"url\":\"http://www.sciencedirect.com/science/article/pii/S001282522030430X\",\"doi\":\"10.1016/j.earscirev.2020.103384\",\"abstract\":\"Fossil pollen records are well-established indicators of past vegetation changes. The prevalence of pollen across environmental settings including lakes, wetlands, and marine sediments, has made palynology one of the most ubiquitous and valuable tools for studying past environmental and climatic change globally for decades. A complementary research focus has been the development of statistical techniques to derive quantitative estimates of climatic conditions from pollen assemblages. This paper reviews the most commonly used statistical techniques and their rationale and seeks to provide a resource to facilitate their inclusion in more palaeoclimatic research. To this end, we first address the fundamental aspects of fossil pollen data that should be considered when undertaking pollen-based climate reconstructions. We then introduce the range of techniques currently available, the history of their development, and the situations in which they can be best employed. We review the literature on how to define robust calibration datasets, produce high-quality reconstructions, and evaluate climate reconstructions, and suggest methods and products that could be developed to facilitate accessibility and global usability. To continue to foster the development and inclusion of pollen climate reconstruction methods, we promote the development of reporting standards. When established, such standards should 1) enable broader application of climate reconstruction techniques, especially in regions where such methods are currently underused, and 2) enable the evaluation and reproduction of individual reconstructions, structuring them for the evolving open-science era, and optimising the use of fossil pollen data as a vital means for the study of past environmental and climatic variability. We also strongly encourage developers and users of palaeoclimate reconstruction methodologies to make associated programming code publicly available, which will further help disseminate these techniques to interested communities.\",\"language\":\"English\",\"urldate\":\"2020-12-09\",\"journal\":\"Earth-Science Reviews\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Chevalier\"],\"firstnames\":[\"Manuel\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Davis\"],\"firstnames\":[\"Basil\",\"A.\",\"S.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Heiri\"],\"firstnames\":[\"Oliver\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Seppä\"],\"firstnames\":[\"Heikki\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chase\"],\"firstnames\":[\"Brian\",\"M.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Gajewski\"],\"firstnames\":[\"Konrad\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Lacourse\"],\"firstnames\":[\"Terri\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Telford\"],\"firstnames\":[\"Richard\",\"J.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Finsinger\"],\"firstnames\":[\"Walter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Guiot\"],\"firstnames\":[\"Joël\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kühl\"],\"firstnames\":[\"Norbert\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Maezumi\"],\"firstnames\":[\"S.\",\"Yoshi\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tipton\"],\"firstnames\":[\"John\",\"R.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Carter\"],\"firstnames\":[\"Vachel\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Brussel\"],\"firstnames\":[\"Thomas\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Phelps\"],\"firstnames\":[\"Leanne\",\"N.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Dawson\"],\"firstnames\":[\"Andria\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Zanon\"],\"firstnames\":[\"Marco\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Vallé\"],\"firstnames\":[\"Francesca\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Nolan\"],\"firstnames\":[\"Connor\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Mauri\"],\"firstnames\":[\"Achille\"],\"suffixes\":[]},{\"propositions\":[\"de\"],\"lastnames\":[\"Vernal\"],\"firstnames\":[\"Anne\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Izumi\"],\"firstnames\":[\"Kenji\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Holmström\"],\"firstnames\":[\"Lasse\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Marsicek\"],\"firstnames\":[\"Jeremiah\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Goring\"],\"firstnames\":[\"Simon\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Sommer\"],\"firstnames\":[\"Philipp\",\"S.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chaput\"],\"firstnames\":[\"Michelle\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kupriyanov\"],\"firstnames\":[\"Dmitry\"],\"suffixes\":[]}],\"month\":\"November\",\"year\":\"2020\",\"keywords\":\"Analogues, Climate, Community-based standards, Palaeoclimate, Pollen, Probability density functions, Quantitative reconstructions, Transfer functions\",\"pages\":\"103384\",\"bibtex\":\"@article{chevalier_pollen-based_2020,\\n\\ttitle = {Pollen-based climate reconstruction techniques for late {Quaternary} studies},\\n\\tvolume = {210},\\n\\tissn = {0012-8252},\\n\\turl = {http://www.sciencedirect.com/science/article/pii/S001282522030430X},\\n\\tdoi = {10.1016/j.earscirev.2020.103384},\\n\\tabstract = {Fossil pollen records are well-established indicators of past vegetation changes. The prevalence of pollen across environmental settings including lakes, wetlands, and marine sediments, has made palynology one of the most ubiquitous and valuable tools for studying past environmental and climatic change globally for decades. A complementary research focus has been the development of statistical techniques to derive quantitative estimates of climatic conditions from pollen assemblages. This paper reviews the most commonly used statistical techniques and their rationale and seeks to provide a resource to facilitate their inclusion in more palaeoclimatic research. To this end, we first address the fundamental aspects of fossil pollen data that should be considered when undertaking pollen-based climate reconstructions. We then introduce the range of techniques currently available, the history of their development, and the situations in which they can be best employed. We review the literature on how to define robust calibration datasets, produce high-quality reconstructions, and evaluate climate reconstructions, and suggest methods and products that could be developed to facilitate accessibility and global usability. To continue to foster the development and inclusion of pollen climate reconstruction methods, we promote the development of reporting standards. When established, such standards should 1) enable broader application of climate reconstruction techniques, especially in regions where such methods are currently underused, and 2) enable the evaluation and reproduction of individual reconstructions, structuring them for the evolving open-science era, and optimising the use of fossil pollen data as a vital means for the study of past environmental and climatic variability. We also strongly encourage developers and users of palaeoclimate reconstruction methodologies to make associated programming code publicly available, which will further help disseminate these techniques to interested communities.},\\n\\tlanguage = {English},\\n\\turldate = {2020-12-09},\\n\\tjournal = {Earth-Science Reviews},\\n\\tauthor = {Chevalier, Manuel and Davis, Basil A. S. and Heiri, Oliver and Seppä, Heikki and Chase, Brian M. and Gajewski, Konrad and Lacourse, Terri and Telford, Richard J. and Finsinger, Walter and Guiot, Joël and Kühl, Norbert and Maezumi, S. Yoshi and Tipton, John R. and Carter, Vachel A. and Brussel, Thomas and Phelps, Leanne N. and Dawson, Andria and Zanon, Marco and Vallé, Francesca and Nolan, Connor and Mauri, Achille and de Vernal, Anne and Izumi, Kenji and Holmström, Lasse and Marsicek, Jeremiah and Goring, Simon and Sommer, Philipp S. and Chaput, Michelle and Kupriyanov, Dmitry},\\n\\tmonth = nov,\\n\\tyear = {2020},\\n\\tkeywords = {Analogues, Climate, Community-based standards, Palaeoclimate, Pollen, Probability density functions, Quantitative reconstructions, Transfer functions},\\n\\tpages = {103384},\\n}\\n\\n\",\"author_short\":[\"Chevalier, M.\",\"Davis, B. A. S.\",\"Heiri, O.\",\"Seppä, H.\",\"Chase, B. M.\",\"Gajewski, K.\",\"Lacourse, T.\",\"Telford, R. J.\",\"Finsinger, W.\",\"Guiot, J.\",\"Kühl, N.\",\"Maezumi, S. Y.\",\"Tipton, J. R.\",\"Carter, V. A.\",\"Brussel, T.\",\"Phelps, L. N.\",\"Dawson, A.\",\"Zanon, M.\",\"Vallé, F.\",\"Nolan, C.\",\"Mauri, A.\",\"de Vernal, A.\",\"Izumi, K.\",\"Holmström, L.\",\"Marsicek, J.\",\"Goring, S.\",\"Sommer, P. S.\",\"Chaput, M.\",\"Kupriyanov, D.\"],\"key\":\"chevalier_pollen-based_2020\",\"id\":\"chevalier_pollen-based_2020\",\"bibbaseid\":\"chevalier-davis-heiri-sepp-chase-gajewski-lacourse-telford-etal-pollenbasedclimatereconstructiontechniquesforlatequaternarystudies-2020\",\"role\":\"author\",\"urls\":{\"Paper\":\"http://www.sciencedirect.com/science/article/pii/S001282522030430X\"},\"keyword\":[\"Analogues\",\"Climate\",\"Community-based standards\",\"Palaeoclimate\",\"Pollen\",\"Probability density functions\",\"Quantitative reconstructions\",\"Transfer functions\"],\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Recent fire regime in the southern boreal forests of western Siberia is unprecedented in the last five millennia\",\"volume\":\"244\",\"issn\":\"0277-3791\",\"doi\":\"10.1016/j.quascirev.2020.106495\",\"abstract\":\"Wildfires in Siberia are documented to have increased in frequency and severity over recent decades. However, in the absence of long-term records, it is unclear how far and why this trend deviates from centennial to millennial scale variability. Here we reconstruct past patterns of fire frequency and fire type, and explore how the fire-related traits of boreal species and plant functional types (PFTs) determine ecosystem responses to changing fire regimes. We use charcoal-based reconstructions of the fire regime in combination with a pollen-based assessment of vegetation composition in two boreal forest peat profiles from Plotnikovo Mire in western Siberia that span the last 2400 and 5000 years. We found moderate levels of biomass burning between 5000 and 4000 cal yr BP. Biomass burning and fire severity i.e., more biomass burning per fire episode, increased over the last 1500 cal yr BP associated with the dominance of fire invaders (Betula). Conversely, between 4000 and 1500 cal yr BP lower biomass burning, with perhaps fire types affecting mostly litter and understorey vegetation, coincided with the dominance of fire resisters (e.g., Pinus sylvestris, P. sibirica, Larix) intermixed with a considerable number of fire avoiders (e.g., Abies sibirica and Picea obovata). This long-term perspective shows that the current fire regime commenced 1500 years ago and deviates from the trends observed over the last 5000 years. This deviation is linked to a combination of climate conditions conducive to fire, the amount and composition of woody fuels, and land use changes. Although pines reacted more sensitively to increased fire severity, the fire avoider Picea obovata appears to be much more vulnerable to both frequent, severe fires than Abies sibirica. We anticipate that climatically driven changes in fire weather, with frequent warm and dry spells, and anthropogenic land use intensification will heighten fire severity and their impact, driving vegetation composition towards Betula species to the detriment of Picea obovata. This study also shows that charcoal morphotypes can provide useful information on fuel and fire type, and that, although all macro-charcoal size classes reliably indicate local-scale fires, the larger fraction (\\\\textgreater300–500 μm) allows the identification of on-site fire episodes. We recommend multi-site palaeo-fire reconstructions in boreal peatlands to adequately reflect the influence of localised peat moisture content, and vegetation composition and structure variability on the small-scale heterogeneity of fire type and spread. This will ensure that trends in fire regime dynamics are representative and not limited to the local scale. We also propose future directions in fire research that can be tested using fossil records of fire, climate and vegetation ideally in an interdisciplinary approach.\",\"language\":\"English\",\"urldate\":\"2020-10-02\",\"journal\":\"Quaternary Science Reviews\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Feurdean\"],\"firstnames\":[\"Angelica\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Florescu\"],\"firstnames\":[\"Gabriela\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tanţău\"],\"firstnames\":[\"Ioan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Vannière\"],\"firstnames\":[\"Boris\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Diaconu\"],\"firstnames\":[\"Andrei-Cosmin\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pfeiffer\"],\"firstnames\":[\"Mirjam\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Warren\"],\"firstnames\":[\"Dan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hutchinson\"],\"firstnames\":[\"Simon\",\"M.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Gorina\"],\"firstnames\":[\"Natalia\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Gałka\"],\"firstnames\":[\"Mariusz\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kirpotin\"],\"firstnames\":[\"Sergey\"],\"suffixes\":[]}],\"month\":\"September\",\"year\":\"2020\",\"keywords\":\"Biomass burning, Charcoal morphologies, Climate change, Drought, Fire frequency, Fire severity, Great Vasyugan Mire, Peat archives, Pollen, Russia, Satellite images\",\"pages\":\"106495\",\"bibtex\":\"@article{feurdean_recent_2020,\\n\\ttitle = {Recent fire regime in the southern boreal forests of western {Siberia} is unprecedented in the last five millennia},\\n\\tvolume = {244},\\n\\tissn = {0277-3791},\\n\\tdoi = {10.1016/j.quascirev.2020.106495},\\n\\tabstract = {Wildfires in Siberia are documented to have increased in frequency and severity over recent decades. However, in the absence of long-term records, it is unclear how far and why this trend deviates from centennial to millennial scale variability. Here we reconstruct past patterns of fire frequency and fire type, and explore how the fire-related traits of boreal species and plant functional types (PFTs) determine ecosystem responses to changing fire regimes. We use charcoal-based reconstructions of the fire regime in combination with a pollen-based assessment of vegetation composition in two boreal forest peat profiles from Plotnikovo Mire in western Siberia that span the last 2400 and 5000 years. We found moderate levels of biomass burning between 5000 and 4000 cal yr BP. Biomass burning and fire severity i.e., more biomass burning per fire episode, increased over the last 1500 cal yr BP associated with the dominance of fire invaders (Betula). Conversely, between 4000 and 1500 cal yr BP lower biomass burning, with perhaps fire types affecting mostly litter and understorey vegetation, coincided with the dominance of fire resisters (e.g., Pinus sylvestris, P. sibirica, Larix) intermixed with a considerable number of fire avoiders (e.g., Abies sibirica and Picea obovata). This long-term perspective shows that the current fire regime commenced 1500 years ago and deviates from the trends observed over the last 5000 years. This deviation is linked to a combination of climate conditions conducive to fire, the amount and composition of woody fuels, and land use changes. Although pines reacted more sensitively to increased fire severity, the fire avoider Picea obovata appears to be much more vulnerable to both frequent, severe fires than Abies sibirica. We anticipate that climatically driven changes in fire weather, with frequent warm and dry spells, and anthropogenic land use intensification will heighten fire severity and their impact, driving vegetation composition towards Betula species to the detriment of Picea obovata. This study also shows that charcoal morphotypes can provide useful information on fuel and fire type, and that, although all macro-charcoal size classes reliably indicate local-scale fires, the larger fraction ({\\\\textgreater}300–500 μm) allows the identification of on-site fire episodes. We recommend multi-site palaeo-fire reconstructions in boreal peatlands to adequately reflect the influence of localised peat moisture content, and vegetation composition and structure variability on the small-scale heterogeneity of fire type and spread. This will ensure that trends in fire regime dynamics are representative and not limited to the local scale. We also propose future directions in fire research that can be tested using fossil records of fire, climate and vegetation ideally in an interdisciplinary approach.},\\n\\tlanguage = {English},\\n\\turldate = {2020-10-02},\\n\\tjournal = {Quaternary Science Reviews},\\n\\tauthor = {Feurdean, Angelica and Florescu, Gabriela and Tanţău, Ioan and Vannière, Boris and Diaconu, Andrei-Cosmin and Pfeiffer, Mirjam and Warren, Dan and Hutchinson, Simon M. and Gorina, Natalia and Gałka, Mariusz and Kirpotin, Sergey},\\n\\tmonth = sep,\\n\\tyear = {2020},\\n\\tkeywords = {Biomass burning, Charcoal morphologies, Climate change, Drought, Fire frequency, Fire severity, Great Vasyugan Mire, Peat archives, Pollen, Russia, Satellite images},\\n\\tpages = {106495},\\n}\\n\\n\",\"author_short\":[\"Feurdean, A.\",\"Florescu, G.\",\"Tanţău, I.\",\"Vannière, B.\",\"Diaconu, A.\",\"Pfeiffer, M.\",\"Warren, D.\",\"Hutchinson, S. M.\",\"Gorina, N.\",\"Gałka, M.\",\"Kirpotin, S.\"],\"key\":\"feurdean_recent_2020\",\"id\":\"feurdean_recent_2020\",\"bibbaseid\":\"feurdean-florescu-tanu-vannire-diaconu-pfeiffer-warren-hutchinson-etal-recentfireregimeinthesouthernborealforestsofwesternsiberiaisunprecedentedinthelastfivemillennia-2020\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Biomass burning\",\"Charcoal morphologies\",\"Climate change\",\"Drought\",\"Fire frequency\",\"Fire severity\",\"Great Vasyugan Mire\",\"Peat archives\",\"Pollen\",\"Russia\",\"Satellite images\"],\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Compositional turnover and variation in Eemian pollen sequences in Europe\",\"volume\":\"29\",\"issn\":\"1617-6278\",\"doi\":\"10.1007/s00334-019-00726-5\",\"abstract\":\"The Eemian interglacial represents a natural experiment on how past vegetation with negligible human impact responded to amplified temperature changes compared to the Holocene. Here, we assemble 47 carefully selected Eemian pollen sequences from Europe to explore geographical patterns of (1) total compositional turnover and total variation for each sequence and (2) stratigraphical turnover between samples within each sequence using detrended canonical correspondence analysis, multivariate regression trees, and principal curves. Our synthesis shows that turnover and variation are highest in central Europe (47–55°N), low in southern Europe (south of 45°N), and lowest in the north (above 60°N). These results provide a basis for developing hypotheses about causes of vegetation change during the Eemian and their possible drivers.\",\"language\":\"English\",\"number\":\"1\",\"urldate\":\"2020-01-07\",\"journal\":\"Vegetation History and Archaeobotany\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Felde\"],\"firstnames\":[\"Vivian\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Flantua\"],\"firstnames\":[\"Suzette\",\"G.\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jenks\"],\"firstnames\":[\"Cathy\",\"R.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Benito\"],\"firstnames\":[\"Blas\",\"M.\"],\"suffixes\":[]},{\"propositions\":[\"de\"],\"lastnames\":[\"Beaulieu\"],\"firstnames\":[\"Jacques-Louis\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Magri\"],\"firstnames\":[\"Donatella\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Nalepka\"],\"firstnames\":[\"Dorota\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Risebrobakken\"],\"firstnames\":[\"Bjørg\"],\"suffixes\":[]},{\"propositions\":[\"ter\"],\"lastnames\":[\"Braak\"],\"firstnames\":[\"Cajo\",\"J.\",\"F.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Allen\"],\"firstnames\":[\"Judy\",\"R.\",\"M.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Granoszewski\"],\"firstnames\":[\"Wojciech\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Helmens\"],\"firstnames\":[\"Karin\",\"F.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Huntley\"],\"firstnames\":[\"Brian\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kondratienė\"],\"firstnames\":[\"Ona\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kalniņa\"],\"firstnames\":[\"Laimdota\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kupryjanowicz\"],\"firstnames\":[\"Mirosława\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Malkiewicz\"],\"firstnames\":[\"Małgorzata\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Milner\"],\"firstnames\":[\"Alice\",\"M.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Nita\"],\"firstnames\":[\"Małgorzata\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Noryśkiewicz\"],\"firstnames\":[\"Bożena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pidek\"],\"firstnames\":[\"Irena\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Reille\"],\"firstnames\":[\"Maurice\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Salonen\"],\"firstnames\":[\"J.\",\"Sakari\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Šeirienė\"],\"firstnames\":[\"Vaida\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Winter\"],\"firstnames\":[\"Hanna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tzedakis\"],\"firstnames\":[\"Polychronis\",\"C.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Birks\"],\"firstnames\":[\"H.\",\"John\",\"B.\"],\"suffixes\":[]}],\"month\":\"January\",\"year\":\"2020\",\"note\":\"[IF2019=2.364]\",\"keywords\":\"Detrended canonical correspondence analysis, Extrinsic and intrinsic processes, Inertia, Last interglacial dataset, Multivariate regression trees, Neutral processes, Principal curves, database, interglacial\",\"pages\":\"101–109\",\"bibtex\":\"@article{felde_compositional_2020,\\n\\ttitle = {Compositional turnover and variation in {Eemian} pollen sequences in {Europe}},\\n\\tvolume = {29},\\n\\tissn = {1617-6278},\\n\\tdoi = {10.1007/s00334-019-00726-5},\\n\\tabstract = {The Eemian interglacial represents a natural experiment on how past vegetation with negligible human impact responded to amplified temperature changes compared to the Holocene. Here, we assemble 47 carefully selected Eemian pollen sequences from Europe to explore geographical patterns of (1) total compositional turnover and total variation for each sequence and (2) stratigraphical turnover between samples within each sequence using detrended canonical correspondence analysis, multivariate regression trees, and principal curves. Our synthesis shows that turnover and variation are highest in central Europe (47–55°N), low in southern Europe (south of 45°N), and lowest in the north (above 60°N). These results provide a basis for developing hypotheses about causes of vegetation change during the Eemian and their possible drivers.},\\n\\tlanguage = {English},\\n\\tnumber = {1},\\n\\turldate = {2020-01-07},\\n\\tjournal = {Vegetation History and Archaeobotany},\\n\\tauthor = {Felde, Vivian A. and Flantua, Suzette G. A. and Jenks, Cathy R. and Benito, Blas M. and de Beaulieu, Jacques-Louis and Kuneš, Petr and Magri, Donatella and Nalepka, Dorota and Risebrobakken, Bjørg and ter Braak, Cajo J. F. and Allen, Judy R. M. and Granoszewski, Wojciech and Helmens, Karin F. and Huntley, Brian and Kondratienė, Ona and Kalniņa, Laimdota and Kupryjanowicz, Mirosława and Malkiewicz, Małgorzata and Milner, Alice M. and Nita, Małgorzata and Noryśkiewicz, Bożena and Pidek, Irena A. and Reille, Maurice and Salonen, J. Sakari and Šeirienė, Vaida and Winter, Hanna and Tzedakis, Polychronis C. and Birks, H. John B.},\\n\\tmonth = jan,\\n\\tyear = {2020},\\n\\tnote = {[IF2019=2.364]},\\n\\tkeywords = {Detrended canonical correspondence analysis, Extrinsic and intrinsic processes, Inertia, Last interglacial dataset, Multivariate regression trees, Neutral processes, Principal curves, database, interglacial},\\n\\tpages = {101--109},\\n}\\n\\n\",\"author_short\":[\"Felde, V. A.\",\"Flantua, S. G. A.\",\"Jenks, C. R.\",\"Benito, B. M.\",\"de Beaulieu, J.\",\"Kuneš, P.\",\"Magri, D.\",\"Nalepka, D.\",\"Risebrobakken, B.\",\"ter Braak, C. J. F.\",\"Allen, J. R. M.\",\"Granoszewski, W.\",\"Helmens, K. F.\",\"Huntley, B.\",\"Kondratienė, O.\",\"Kalniņa, L.\",\"Kupryjanowicz, M.\",\"Malkiewicz, M.\",\"Milner, A. M.\",\"Nita, M.\",\"Noryśkiewicz, B.\",\"Pidek, I. A.\",\"Reille, M.\",\"Salonen, J. S.\",\"Šeirienė, V.\",\"Winter, H.\",\"Tzedakis, P. C.\",\"Birks, H. J. B.\"],\"key\":\"felde_compositional_2020\",\"id\":\"felde_compositional_2020\",\"bibbaseid\":\"felde-flantua-jenks-benito-debeaulieu-kune-magri-nalepka-etal-compositionalturnoverandvariationineemianpollensequencesineurope-2020\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Detrended canonical correspondence analysis\",\"Extrinsic and intrinsic processes\",\"Inertia\",\"Last interglacial dataset\",\"Multivariate regression trees\",\"Neutral processes\",\"Principal curves\",\"database\",\"interglacial\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Fire hazard modulation by long-term dynamics in land cover and dominant forest type in eastern and central Europe\",\"volume\":\"17\",\"issn\":\"1726-4170\",\"url\":\"https://www.biogeosciences.net/17/1213/2020/\",\"doi\":\"10.5194/bg-17-1213-2020\",\"abstract\":\"\\\\textlessp\\\\textgreater\\\\textlessstrong\\\\textgreaterAbstract.\\\\textless/strong\\\\textgreater Wildfire occurrence is influenced by climate, vegetation and human activities. A key challenge for understanding the risk of fires is quantifying the mediating effect of vegetation on fire regimes. Here, we explore the relative importance of Holocene land cover, land use, dominant functional forest type, and climate dynamics on biomass burning in temperate and boreo-nemoral regions of central and eastern Europe over the past 12&thinsp;kyr. We used an extensive data set of Holocene pollen and sedimentary charcoal records, in combination with climate simulations and statistical modelling. Biomass burning was highest during the early Holocene and lowest during the mid-Holocene in all three ecoregions (Atlantic, continental and boreo-nemoral) but was more spatially variable over the past 3–4&thinsp;kyr. Although climate explained a significant variance in biomass burning during the early Holocene, tree cover was consistently the highest predictor of past biomass burning over the past 8&thinsp;kyr. In temperate forests, biomass burning was high at \\\\textlessspan class=\\\"inline-formula\\\"\\\\textgreater∼45\\\\textless/span\\\\textgreater&thinsp;% tree cover and decreased to a minimum at between 60&thinsp;% and 70&thinsp;% tree cover. In needleleaf-dominated forests, biomass burning was highest at \\\\textlessspan class=\\\"inline-formula\\\"\\\\textgreater∼\\\\textless/span\\\\textgreater&thinsp;60&thinsp;%–65&thinsp;% tree cover and steeply declined at \\\\textlessspan class=\\\"inline-formula\\\"\\\\textgreater&gt;65\\\\textless/span\\\\textgreater&thinsp;% tree cover. Biomass burning also increased when arable lands and grasslands reached \\\\textlessspan class=\\\"inline-formula\\\"\\\\textgreater∼\\\\textless/span\\\\textgreater&thinsp;15&thinsp;%–20&thinsp;%, although this relationship was variable depending on land use practice via ignition sources, fuel type and quantities. Higher tree cover reduced the amount of solar radiation reaching the forest floor and could provide moister, more wind-protected microclimates underneath canopies, thereby decreasing fuel flammability. Tree cover at which biomass burning increased appears to be driven by warmer and drier summer conditions during the early Holocene and by increasing human influence on land cover during the late Holocene. We suggest that long-term fire hazard may be effectively reduced through land cover management, given that land cover has controlled fire regimes under the dynamic climates of the Holocene.\\\\textless/p\\\\textgreater\",\"language\":\"English\",\"number\":\"5\",\"urldate\":\"2020-03-05\",\"journal\":\"Biogeosciences\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Feurdean\"],\"firstnames\":[\"Angelica\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Vannière\"],\"firstnames\":[\"Boris\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Finsinger\"],\"firstnames\":[\"Walter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Warren\"],\"firstnames\":[\"Dan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Connor\"],\"firstnames\":[\"Simon\",\"C.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Forrest\"],\"firstnames\":[\"Matthew\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Liakka\"],\"firstnames\":[\"Johan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Panait\"],\"firstnames\":[\"Andrei\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Werner\"],\"firstnames\":[\"Christian\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Andrič\"],\"firstnames\":[\"Maja\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bobek\"],\"firstnames\":[\"Premysl\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Carter\"],\"firstnames\":[\"Vachel\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Davis\"],\"firstnames\":[\"Basil\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Diaconu\"],\"firstnames\":[\"Andrei-Cosmin\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Dietze\"],\"firstnames\":[\"Elisabeth\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Feeser\"],\"firstnames\":[\"Ingo\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Florescu\"],\"firstnames\":[\"Gabriela\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Gałka\"],\"firstnames\":[\"Mariusz\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Giesecke\"],\"firstnames\":[\"Thomas\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jahns\"],\"firstnames\":[\"Susanne\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jamrichová\"],\"firstnames\":[\"Eva\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kajukało\"],\"firstnames\":[\"Katarzyna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kaplan\"],\"firstnames\":[\"Jed\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Karpińska-Kołaczek\"],\"firstnames\":[\"Monika\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kołaczek\"],\"firstnames\":[\"Piotr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kupriyanov\"],\"firstnames\":[\"Dimitry\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Lamentowicz\"],\"firstnames\":[\"Mariusz\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Lemmen\"],\"firstnames\":[\"Carsten\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Magyari\"],\"firstnames\":[\"Enikö\",\"K.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Marcisz\"],\"firstnames\":[\"Katarzyna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Marinova\"],\"firstnames\":[\"Elena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Niamir\"],\"firstnames\":[\"Aidin\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Novenko\"],\"firstnames\":[\"Elena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Obremska\"],\"firstnames\":[\"Milena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pędziszewska\"],\"firstnames\":[\"Anna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pfeiffer\"],\"firstnames\":[\"Mirjam\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Poska\"],\"firstnames\":[\"Anneli\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Rösch\"],\"firstnames\":[\"Manfred\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Słowiński\"],\"firstnames\":[\"Michal\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Stančikaitė\"],\"firstnames\":[\"Miglė\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Szal\"],\"firstnames\":[\"Marta\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Święta-Musznicka\"],\"firstnames\":[\"Joanna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tanţău\"],\"firstnames\":[\"Ioan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Theuerkauf\"],\"firstnames\":[\"Martin\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tonkov\"],\"firstnames\":[\"Spassimir\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Valkó\"],\"firstnames\":[\"Orsolya\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Vassiljev\"],\"firstnames\":[\"Jüri\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Veski\"],\"firstnames\":[\"Siim\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Vincze\"],\"firstnames\":[\"Ildiko\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Wacnik\"],\"firstnames\":[\"Agnieszka\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Wiethold\"],\"firstnames\":[\"Julian\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hickler\"],\"firstnames\":[\"Thomas\"],\"suffixes\":[]}],\"month\":\"March\",\"year\":\"2020\",\"note\":\"[IF2019=3.48]\",\"keywords\":\"disturbance\",\"pages\":\"1213–1230\",\"bibtex\":\"@article{feurdean_fire_2020,\\n\\ttitle = {Fire hazard modulation by long-term dynamics in land cover and dominant forest type in eastern and central {Europe}},\\n\\tvolume = {17},\\n\\tissn = {1726-4170},\\n\\turl = {https://www.biogeosciences.net/17/1213/2020/},\\n\\tdoi = {10.5194/bg-17-1213-2020},\\n\\tabstract = {{\\\\textless}p{\\\\textgreater}{\\\\textless}strong{\\\\textgreater}Abstract.{\\\\textless}/strong{\\\\textgreater} Wildfire occurrence is influenced by climate, vegetation and human activities. A key challenge for understanding the risk of fires is quantifying the mediating effect of vegetation on fire regimes. Here, we explore the relative importance of Holocene land cover, land use, dominant functional forest type, and climate dynamics on biomass burning in temperate and boreo-nemoral regions of central and eastern Europe over the past 12\\\\&thinsp;kyr. We used an extensive data set of Holocene pollen and sedimentary charcoal records, in combination with climate simulations and statistical modelling. Biomass burning was highest during the early Holocene and lowest during the mid-Holocene in all three ecoregions (Atlantic, continental and boreo-nemoral) but was more spatially variable over the past 3–4\\\\&thinsp;kyr. Although climate explained a significant variance in biomass burning during the early Holocene, tree cover was consistently the highest predictor of past biomass burning over the past 8\\\\&thinsp;kyr. In temperate forests, biomass burning was high at {\\\\textless}span class=\\\"inline-formula\\\"{\\\\textgreater}∼45{\\\\textless}/span{\\\\textgreater}\\\\&thinsp;\\\\% tree cover and decreased to a minimum at between 60\\\\&thinsp;\\\\% and 70\\\\&thinsp;\\\\% tree cover. In needleleaf-dominated forests, biomass burning was highest at {\\\\textless}span class=\\\"inline-formula\\\"{\\\\textgreater}∼{\\\\textless}/span{\\\\textgreater}\\\\&thinsp;60\\\\&thinsp;\\\\%–65\\\\&thinsp;\\\\% tree cover and steeply declined at {\\\\textless}span class=\\\"inline-formula\\\"{\\\\textgreater}\\\\&gt;65{\\\\textless}/span{\\\\textgreater}\\\\&thinsp;\\\\% tree cover. Biomass burning also increased when arable lands and grasslands reached {\\\\textless}span class=\\\"inline-formula\\\"{\\\\textgreater}∼{\\\\textless}/span{\\\\textgreater}\\\\&thinsp;15\\\\&thinsp;\\\\%–20\\\\&thinsp;\\\\%, although this relationship was variable depending on land use practice via ignition sources, fuel type and quantities. Higher tree cover reduced the amount of solar radiation reaching the forest floor and could provide moister, more wind-protected microclimates underneath canopies, thereby decreasing fuel flammability. Tree cover at which biomass burning increased appears to be driven by warmer and drier summer conditions during the early Holocene and by increasing human influence on land cover during the late Holocene. We suggest that long-term fire hazard may be effectively reduced through land cover management, given that land cover has controlled fire regimes under the dynamic climates of the Holocene.{\\\\textless}/p{\\\\textgreater}},\\n\\tlanguage = {English},\\n\\tnumber = {5},\\n\\turldate = {2020-03-05},\\n\\tjournal = {Biogeosciences},\\n\\tauthor = {Feurdean, Angelica and Vannière, Boris and Finsinger, Walter and Warren, Dan and Connor, Simon C. and Forrest, Matthew and Liakka, Johan and Panait, Andrei and Werner, Christian and Andrič, Maja and Bobek, Premysl and Carter, Vachel A. and Davis, Basil and Diaconu, Andrei-Cosmin and Dietze, Elisabeth and Feeser, Ingo and Florescu, Gabriela and Gałka, Mariusz and Giesecke, Thomas and Jahns, Susanne and Jamrichová, Eva and Kajukało, Katarzyna and Kaplan, Jed and Karpińska-Kołaczek, Monika and Kołaczek, Piotr and Kuneš, Petr and Kupriyanov, Dimitry and Lamentowicz, Mariusz and Lemmen, Carsten and Magyari, Enikö K. and Marcisz, Katarzyna and Marinova, Elena and Niamir, Aidin and Novenko, Elena and Obremska, Milena and Pędziszewska, Anna and Pfeiffer, Mirjam and Poska, Anneli and Rösch, Manfred and Słowiński, Michal and Stančikaitė, Miglė and Szal, Marta and Święta-Musznicka, Joanna and Tanţău, Ioan and Theuerkauf, Martin and Tonkov, Spassimir and Valkó, Orsolya and Vassiljev, Jüri and Veski, Siim and Vincze, Ildiko and Wacnik, Agnieszka and Wiethold, Julian and Hickler, Thomas},\\n\\tmonth = mar,\\n\\tyear = {2020},\\n\\tnote = {[IF2019=3.48]},\\n\\tkeywords = {disturbance},\\n\\tpages = {1213--1230},\\n}\\n\\n\",\"author_short\":[\"Feurdean, A.\",\"Vannière, B.\",\"Finsinger, W.\",\"Warren, D.\",\"Connor, S. C.\",\"Forrest, M.\",\"Liakka, J.\",\"Panait, A.\",\"Werner, C.\",\"Andrič, M.\",\"Bobek, P.\",\"Carter, V. A.\",\"Davis, B.\",\"Diaconu, A.\",\"Dietze, E.\",\"Feeser, I.\",\"Florescu, G.\",\"Gałka, M.\",\"Giesecke, T.\",\"Jahns, S.\",\"Jamrichová, E.\",\"Kajukało, K.\",\"Kaplan, J.\",\"Karpińska-Kołaczek, M.\",\"Kołaczek, P.\",\"Kuneš, P.\",\"Kupriyanov, D.\",\"Lamentowicz, M.\",\"Lemmen, C.\",\"Magyari, E. K.\",\"Marcisz, K.\",\"Marinova, E.\",\"Niamir, A.\",\"Novenko, E.\",\"Obremska, M.\",\"Pędziszewska, A.\",\"Pfeiffer, M.\",\"Poska, A.\",\"Rösch, M.\",\"Słowiński, M.\",\"Stančikaitė, M.\",\"Szal, M.\",\"Święta-Musznicka, J.\",\"Tanţău, I.\",\"Theuerkauf, M.\",\"Tonkov, S.\",\"Valkó, O.\",\"Vassiljev, J.\",\"Veski, S.\",\"Vincze, I.\",\"Wacnik, A.\",\"Wiethold, J.\",\"Hickler, T.\"],\"key\":\"feurdean_fire_2020\",\"id\":\"feurdean_fire_2020\",\"bibbaseid\":\"feurdean-vannire-finsinger-warren-connor-forrest-liakka-panait-etal-firehazardmodulationbylongtermdynamicsinlandcoveranddominantforesttypeineasternandcentraleurope-2020\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://www.biogeosciences.net/17/1213/2020/\"},\"keyword\":[\"disturbance\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Inter- and intraspecific variation in grass phytolith shape and size: a geometric morphometrics perspective\",\"shorttitle\":\"Inter- and intraspecific variation in grass phytolith shape and size\",\"doi\":\"10.1093/aob/mcaa102\",\"abstract\":\"AbstractBackground and Aims. The relative contributions of inter- and intraspecific variation to phytolith shape and size have only been investigated in a limi\",\"language\":\"English\",\"urldate\":\"2020-06-19\",\"journal\":\"Annals of Botany\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Hošková\"],\"firstnames\":[\"Kristýna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pokorná\"],\"firstnames\":[\"Adéla\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Neustupa\"],\"firstnames\":[\"Jiří\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pokorný\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"year\":\"2020\",\"bibtex\":\"@article{hoskova_inter-_2020,\\n\\ttitle = {Inter- and intraspecific variation in grass phytolith shape and size: a geometric morphometrics perspective},\\n\\tshorttitle = {Inter- and intraspecific variation in grass phytolith shape and size},\\n\\tdoi = {10.1093/aob/mcaa102},\\n\\tabstract = {AbstractBackground and Aims.  The relative contributions of inter- and intraspecific variation to phytolith shape and size have only been investigated in a limi},\\n\\tlanguage = {English},\\n\\turldate = {2020-06-19},\\n\\tjournal = {Annals of Botany},\\n\\tauthor = {Hošková, Kristýna and Pokorná, Adéla and Neustupa, Jiří and Pokorný, Petr},\\n\\tyear = {2020},\\n}\\n\\n\",\"author_short\":[\"Hošková, K.\",\"Pokorná, A.\",\"Neustupa, J.\",\"Pokorný, P.\"],\"key\":\"hoskova_inter-_2020\",\"id\":\"hoskova_inter-_2020\",\"bibbaseid\":\"hokov-pokorn-neustupa-pokorn-interandintraspecificvariationingrassphytolithshapeandsizeageometricmorphometricsperspective-2020\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Human-induced changes in fire regime and subsequent alteration of the sandstone landscape of Northern Bohemia (Czech Republic)\",\"volume\":\"28\",\"issn\":\"0959-6836\",\"doi\":\"10.1177/0959683617729443\",\"abstract\":\"Multiproxy palaeoecological evidence from a sandstone region in northern Czech Republic was collected to explore the impact of fire disturbances on the decline of the broadleaved forests during the Late Bronze Age (3250–3050 cal. BP). It has been hypothesized that human-accelerated soil leaching affected the nutrient availability in the sandstone area, thus promoting the expansion of oligotrophic-adapted plant communities in the late-Holocene. Little is known about the mechanisms which induced such large-scale vegetation transformation. We sought to determine which driving forces were involved using independent proxy records – soil and sedimentary charcoal, pollen and fungal spores. Local fire history was derived from the variation in charcoal accumulation rates (CHAR) preserved in Eustach peatbog. The fire frequency (FF) estimation over the past ~7500 years revealed distinct phases of increased burning between 3100 and 2120 cal. BP (3.0 fires 1000 yr−1) and 1400–600 cal. BP (4.3 fires 1000 yr−1). Rapid compositional changes in the pollen assemblage were documented during the Late Bronze Age period, suggesting vegetation responded to increased fire disturbances. The human influence on the fire regime is implied by the short-term increase in cereal pollen concurrent with a major fire event, indicating possible use of slash-and-burn cultivation by Late Bronze societies. This type of human subsistence strategy practised in the sandstone landscape further evolved to pastoralism as suggested by continuous presence of coprophilous fungi Sporormiella and Sordaria, which occurred since the Hallstatt/La Tène period (2750–1950 cal. BP). Our study documents, for the first time, the intentional, human-caused biomass burning from densely forested areas of Northern Bohemian sandstone region. Our results imply that increased rate of fire disturbances contributed to the Late Bronze Age transformation of broadleaved forests to oligotrophic forest communities of late-Holocene.\",\"language\":\"English\",\"number\":\"3\",\"urldate\":\"2018-03-31\",\"journal\":\"The Holocene\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Bobek\"],\"firstnames\":[\"Přemysl\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svitavská\",\"Svobodová\"],\"firstnames\":[\"Helena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Werchan\"],\"firstnames\":[\"Barbora\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Švarcová\"],\"firstnames\":[\"Markéta\",\"Gabriela\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"month\":\"March\",\"year\":\"2018\",\"note\":\"[IF2017=2.419]\",\"keywords\":\"disturbance\",\"pages\":\"427–443\",\"bibtex\":\"@article{bobek_human-induced_2018,\\n\\ttitle = {Human-induced changes in fire regime and subsequent alteration of the sandstone landscape of {Northern} {Bohemia} ({Czech} {Republic})},\\n\\tvolume = {28},\\n\\tissn = {0959-6836},\\n\\tdoi = {10.1177/0959683617729443},\\n\\tabstract = {Multiproxy palaeoecological evidence from a sandstone region in northern Czech Republic was collected to explore the impact of fire disturbances on the decline of the broadleaved forests during the Late Bronze Age (3250–3050 cal. BP). It has been hypothesized that human-accelerated soil leaching affected the nutrient availability in the sandstone area, thus promoting the expansion of oligotrophic-adapted plant communities in the late-Holocene. Little is known about the mechanisms which induced such large-scale vegetation transformation. We sought to determine which driving forces were involved using independent proxy records – soil and sedimentary charcoal, pollen and fungal spores. Local fire history was derived from the variation in charcoal accumulation rates (CHAR) preserved in Eustach peatbog. The fire frequency (FF) estimation over the past {\\\\textasciitilde}7500 years revealed distinct phases of increased burning between 3100 and 2120 cal. BP (3.0 fires 1000 yr−1) and 1400–600 cal. BP (4.3 fires 1000 yr−1). Rapid compositional changes in the pollen assemblage were documented during the Late Bronze Age period, suggesting vegetation responded to increased fire disturbances. The human influence on the fire regime is implied by the short-term increase in cereal pollen concurrent with a major fire event, indicating possible use of slash-and-burn cultivation by Late Bronze societies. This type of human subsistence strategy practised in the sandstone landscape further evolved to pastoralism as suggested by continuous presence of coprophilous fungi Sporormiella and Sordaria, which occurred since the Hallstatt/La Tène period (2750–1950 cal. BP). Our study documents, for the first time, the intentional, human-caused biomass burning from densely forested areas of Northern Bohemian sandstone region. Our results imply that increased rate of fire disturbances contributed to the Late Bronze Age transformation of broadleaved forests to oligotrophic forest communities of late-Holocene.},\\n\\tlanguage = {English},\\n\\tnumber = {3},\\n\\turldate = {2018-03-31},\\n\\tjournal = {The Holocene},\\n\\tauthor = {Bobek, Přemysl and Svitavská Svobodová, Helena and Werchan, Barbora and Švarcová, Markéta Gabriela and Kuneš, Petr},\\n\\tmonth = mar,\\n\\tyear = {2018},\\n\\tnote = {[IF2017=2.419]},\\n\\tkeywords = {disturbance},\\n\\tpages = {427--443},\\n}\\n\\n\",\"author_short\":[\"Bobek, P.\",\"Svitavská Svobodová, H.\",\"Werchan, B.\",\"Švarcová, M. G.\",\"Kuneš, P.\"],\"key\":\"bobek_human-induced_2018\",\"id\":\"bobek_human-induced_2018\",\"bibbaseid\":\"bobek-svitavsksvobodov-werchan-varcov-kune-humaninducedchangesinfireregimeandsubsequentalterationofthesandstonelandscapeofnorthernbohemiaczechrepublic-2018\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"disturbance\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Holocene-scale fire dynamics of central European temperate spruce-beech forests\",\"volume\":\"191\",\"issn\":\"0277-3791\",\"doi\":\"10.1016/j.quascirev.2018.05.001\",\"abstract\":\"This study investigated the long-term role and drivers of fire in the central European temperate spruce-beech forests from Prášilské jezero, Czech Republic. The results illustrate the complex relationship between broad-scale climate, vegetation composition, and local human activities on fire throughout the Holocene. Biomass burning was the highest (average 3 fires/1000 years) and most severe during the early Holocene when fire resistant taxa (Pinus, Corylus and Betula) dominated. Using a Generalized Additive Model to assess the response of dominant canopy taxa to changes in biomass burning and fire severity, response curves demonstrate a positive relationship (p &lt; 0.01) between fire resistant taxa and increases in biomass burning. Norway spruce (Picea abies) established ∼10,000 cal yr BP and expanded during peak biomass burning. Response curves show a slight negative relationship with Picea and increasing biomass burning, and a positive relationship with increasing fire severity. This suggests that central European spruce forests may not be significantly impacted by fire. Regional biomass burning dramatically decreased with the expansion of fire sensitive taxa (e.g. Fagus sylvatica) ∼6500 cal yr BP, yet no dramatic reduction in local fire frequency occurred. This suggests either human activities or rare fire-promoting climatic events were important in shaping local fire regimes. Fire activity peaked (6 fires/1000 years) ∼2500 cal yr BP and paralleled increases in anthropogenic pollen indicators. Fagus response curves illustrates a negative (p &lt; 0.01) relationship with increasing biomass burning and fire severity suggesting that natural Fagus forests may be increasingly vulnerable to projected increases in wildfire occurrence.\",\"language\":\"English\",\"urldate\":\"2018-05-26\",\"journal\":\"Quaternary Science Reviews\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Carter\"],\"firstnames\":[\"Vachel\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Moravcová\"],\"firstnames\":[\"Alice\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chiverrell\"],\"firstnames\":[\"Richard\",\"C.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Clear\"],\"firstnames\":[\"Jennifer\",\"L.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Finsinger\"],\"firstnames\":[\"Walter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Dreslerová\"],\"firstnames\":[\"Dagmar\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Halsall\"],\"firstnames\":[\"Karen\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"month\":\"July\",\"year\":\"2018\",\"note\":\"[IF2017=4.334]\",\"keywords\":\"Climate, Fire, Holocene, Macrofossils, Paleoecology, Pollen, Sedimentary charcoal, disturbance\",\"pages\":\"15–30\",\"bibtex\":\"@article{carter_holocene-scale_2018,\\n\\ttitle = {Holocene-scale fire dynamics of central {European} temperate spruce-beech forests},\\n\\tvolume = {191},\\n\\tissn = {0277-3791},\\n\\tdoi = {10.1016/j.quascirev.2018.05.001},\\n\\tabstract = {This study investigated the long-term role and drivers of fire in the central European temperate spruce-beech forests from Prášilské jezero, Czech Republic. The results illustrate the complex relationship between broad-scale climate, vegetation composition, and local human activities on fire throughout the Holocene. Biomass burning was the highest (average 3 fires/1000 years) and most severe during the early Holocene when fire resistant taxa (Pinus, Corylus and Betula) dominated. Using a Generalized Additive Model to assess the response of dominant canopy taxa to changes in biomass burning and fire severity, response curves demonstrate a positive relationship (p \\\\&lt; 0.01) between fire resistant taxa and increases in biomass burning. Norway spruce (Picea abies) established ∼10,000 cal yr BP and expanded during peak biomass burning. Response curves show a slight negative relationship with Picea and increasing biomass burning, and a positive relationship with increasing fire severity. This suggests that central European spruce forests may not be significantly impacted by fire. Regional biomass burning dramatically decreased with the expansion of fire sensitive taxa (e.g. Fagus sylvatica) ∼6500 cal yr BP, yet no dramatic reduction in local fire frequency occurred. This suggests either human activities or rare fire-promoting climatic events were important in shaping local fire regimes. Fire activity peaked (6 fires/1000 years) ∼2500 cal yr BP and paralleled increases in anthropogenic pollen indicators. Fagus response curves illustrates a negative (p \\\\&lt; 0.01) relationship with increasing biomass burning and fire severity suggesting that natural Fagus forests may be increasingly vulnerable to projected increases in wildfire occurrence.},\\n\\tlanguage = {English},\\n\\turldate = {2018-05-26},\\n\\tjournal = {Quaternary Science Reviews},\\n\\tauthor = {Carter, Vachel A. and Moravcová, Alice and Chiverrell, Richard C. and Clear, Jennifer L. and Finsinger, Walter and Dreslerová, Dagmar and Halsall, Karen and Kuneš, Petr},\\n\\tmonth = jul,\\n\\tyear = {2018},\\n\\tnote = {[IF2017=4.334]},\\n\\tkeywords = {Climate, Fire, Holocene, Macrofossils, Paleoecology, Pollen, Sedimentary charcoal, disturbance},\\n\\tpages = {15--30},\\n}\\n\\n\",\"author_short\":[\"Carter, V. A.\",\"Moravcová, A.\",\"Chiverrell, R. C.\",\"Clear, J. L.\",\"Finsinger, W.\",\"Dreslerová, D.\",\"Halsall, K.\",\"Kuneš, P.\"],\"key\":\"carter_holocene-scale_2018\",\"id\":\"carter_holocene-scale_2018\",\"bibbaseid\":\"carter-moravcov-chiverrell-clear-finsinger-dreslerov-halsall-kune-holocenescalefiredynamicsofcentraleuropeantemperatesprucebeechforests-2018\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Climate\",\"Fire\",\"Holocene\",\"Macrofossils\",\"Paleoecology\",\"Pollen\",\"Sedimentary charcoal\",\"disturbance\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":2,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Divergent fire history trajectories in Central European temperate forests revealed a pronounced influence of broadleaved trees on fire dynamics\",\"volume\":\"222\",\"issn\":\"0277-3791\",\"doi\":\"10.1016/j.quascirev.2019.105865\",\"abstract\":\"Fire occurrence is driven by a complex interplay between vegetation, climatic, landform and human factors making it challenging to separate the individual effect of each variable. Here we present a reconstruction of the Holocene biomass burning history of two regions located in the Central European temperate zone that differ in the timing of the Middle Holocene expansion of broadleaf-dominated forest communities. This allowed us to investigate the effect of biotic changes on past fire activity. Multiple-site charcoal accumulation records were used to estimate regional-scale trends in biomass burning and to compare them with major trajectories of vegetation development. Extensive 14C-dated soil charcoal records collected within both regions were amalgamated using a cumulative probability function to identify a stand-scale proxy of past fire occurrence. Our results suggest that rising vegetation productivity driven by rapid Early Holocene climate amelioration enhanced biomass burning. The increased fire activity during this period was driven by both a drier- and warmer-than-present climate and easily flammable fuels produced by conifer-dominated vegetation. We identified an inhibiting effect of the concomitant Fagus sylvatica expansion on levels of biomass burning that occurred asynchronously between our mountain and mid-elevation sandstone regions 6500 cal yr BP and 4900 cal yr BP, respectively. The amount of compositional change in plant communities was more related to the transformation of major vegetation types than to fluctuations in fire activity levels. The divergent timing of the fire decline in response to the Fagus sylvatica expansion implies biotic control over biomass burning that is independent of a direct climatic influence.\",\"language\":\"English\",\"urldate\":\"2019-09-16\",\"journal\":\"Quaternary Science Reviews\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Bobek\"],\"firstnames\":[\"Přemysl\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svobodová-Svitavská\"],\"firstnames\":[\"Helena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pokorný\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Šamonil\"],\"firstnames\":[\"Pavel\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kozáková\"],\"firstnames\":[\"Radka\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Abraham\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Klinerová\"],\"firstnames\":[\"Tereza\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Švarcová\"],\"firstnames\":[\"Markéta\",\"Gabriela\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jamrichová\"],\"firstnames\":[\"Eva\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Krauseová\"],\"firstnames\":[\"Eva\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Wild\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]}],\"month\":\"October\",\"year\":\"2019\",\"note\":\"[IF2018=4.641]\",\"keywords\":\"Fire history, Holocene, Human impact, Sedimentary charcoal, Species turnover, Vegetation dynamics, disturbance\",\"pages\":\"105865\",\"bibtex\":\"@article{bobek_divergent_2019,\\n\\ttitle = {Divergent fire history trajectories in {Central} {European} temperate forests revealed a pronounced influence of broadleaved trees on fire dynamics},\\n\\tvolume = {222},\\n\\tissn = {0277-3791},\\n\\tdoi = {10.1016/j.quascirev.2019.105865},\\n\\tabstract = {Fire occurrence is driven by a complex interplay between vegetation, climatic, landform and human factors making it challenging to separate the individual effect of each variable. Here we present a reconstruction of the Holocene biomass burning history of two regions located in the Central European temperate zone that differ in the timing of the Middle Holocene expansion of broadleaf-dominated forest communities. This allowed us to investigate the effect of biotic changes on past fire activity. Multiple-site charcoal accumulation records were used to estimate regional-scale trends in biomass burning and to compare them with major trajectories of vegetation development. Extensive 14C-dated soil charcoal records collected within both regions were amalgamated using a cumulative probability function to identify a stand-scale proxy of past fire occurrence. Our results suggest that rising vegetation productivity driven by rapid Early Holocene climate amelioration enhanced biomass burning. The increased fire activity during this period was driven by both a drier- and warmer-than-present climate and easily flammable fuels produced by conifer-dominated vegetation. We identified an inhibiting effect of the concomitant Fagus sylvatica expansion on levels of biomass burning that occurred asynchronously between our mountain and mid-elevation sandstone regions 6500 cal yr BP and 4900 cal yr BP, respectively. The amount of compositional change in plant communities was more related to the transformation of major vegetation types than to fluctuations in fire activity levels. The divergent timing of the fire decline in response to the Fagus sylvatica expansion implies biotic control over biomass burning that is independent of a direct climatic influence.},\\n\\tlanguage = {English},\\n\\turldate = {2019-09-16},\\n\\tjournal = {Quaternary Science Reviews},\\n\\tauthor = {Bobek, Přemysl and Svobodová-Svitavská, Helena and Pokorný, Petr and Šamonil, Pavel and Kuneš, Petr and Kozáková, Radka and Abraham, Vojtěch and Klinerová, Tereza and Švarcová, Markéta Gabriela and Jamrichová, Eva and Krauseová, Eva and Wild, Jan},\\n\\tmonth = oct,\\n\\tyear = {2019},\\n\\tnote = {[IF2018=4.641]},\\n\\tkeywords = {Fire history, Holocene, Human impact, Sedimentary charcoal, Species turnover, Vegetation dynamics, disturbance},\\n\\tpages = {105865},\\n}\\n\\n\",\"author_short\":[\"Bobek, P.\",\"Svobodová-Svitavská, H.\",\"Pokorný, P.\",\"Šamonil, P.\",\"Kuneš, P.\",\"Kozáková, R.\",\"Abraham, V.\",\"Klinerová, T.\",\"Švarcová, M. G.\",\"Jamrichová, E.\",\"Krauseová, E.\",\"Wild, J.\"],\"key\":\"bobek_divergent_2019\",\"id\":\"bobek_divergent_2019\",\"bibbaseid\":\"bobek-svobodovsvitavsk-pokorn-amonil-kune-kozkov-abraham-klinerov-etal-divergentfirehistorytrajectoriesincentraleuropeantemperateforestsrevealedapronouncedinfluenceofbroadleavedtreesonfiredynamics-2019\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Fire history\",\"Holocene\",\"Human impact\",\"Sedimentary charcoal\",\"Species turnover\",\"Vegetation dynamics\",\"disturbance\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Disruption in an alluvial landscape: Settlement and environment dynamics on the alluvium of the river Dyje at the Pohansko archaeological site (Czech Republic)\",\"volume\":\"511\",\"issn\":\"1040-6182\",\"shorttitle\":\"Disruption in an alluvial landscape\",\"url\":\"http://www.sciencedirect.com/science/article/pii/S1040618217309503\",\"doi\":\"10.1016/j.quaint.2018.04.013\",\"abstract\":\"Floodplain alluvia can provide a combination of natural and anthropogenic evidence of environmental changes, allowing to directly examine their evolution in relation to settlement dynamics. Such evidence is recorded, for example, at the archaeological site Pohansko by the town of Břeclav, a former centre of the Great Moravian Empire. The aim of our research was to explore what conditions on the floodplain could have caused the abandonment of this environment. Special attention was paid to the climax of the floodplain's occupation during the times of the Great Moravian Empire (AD 836–906) and to the decline of its occupation in the following centuries. The environmental record at the Pohansko site starts in the 7th century BC. From the Iron Age onwards (Hallstatt and La Tène periods) there is evidence of non-agricultural human activities. Since the 3rd and 2nd centuries BC to at least the second half of the 10th century AD, there is no record of any floodplain aggradation or flooding at the site. Later, both the archaeological and palaeoecological records on the floodplain probably got exposed and redeposited. The result is a mechanically disturbed layer that is synchronous with soil horizons and subsequent Early Mediaeval cultural layers covering sandy elevations. For an unknown reason, the site was deserted for many centuries after the end of the 10th century AD. During the High Mediaeval period and the early Modern Era, especially since the 15th century AD, overbank deposits covered the floodplain. Intensified human impact in the river catchment and climate change during the Little Ice Age were the main triggers of this change. The results correlate with the written historical sources pertaining to this area, which speak about an increasing frequency of flooding in the Czech lands since the 14th century, and especially in the second half of the 16th century. As a result, these sites became unsuitable for settlement and abandoned.\",\"language\":\"en\",\"urldate\":\"2020-03-05\",\"journal\":\"Quaternary International\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Petřík\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Petr\"],\"firstnames\":[\"Libor\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Adameková\"],\"firstnames\":[\"Katarína\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Prišťáková\"],\"firstnames\":[\"Michaela\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Potůčková\"],\"firstnames\":[\"Anna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Lenďáková\"],\"firstnames\":[\"Zuzana\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Frączek\"],\"firstnames\":[\"Marcin\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Dresler\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Macháček\"],\"firstnames\":[\"Jiří\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kalicki\"],\"firstnames\":[\"Tomasz\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Lisá\"],\"firstnames\":[\"Lenka\"],\"suffixes\":[]}],\"month\":\"March\",\"year\":\"2019\",\"keywords\":\"Aggradation, Early Middle Ages, Floodplain, Floodplain occupation, Great Moravian Empire, Human impact, Iron Age, Late Holocene\",\"pages\":\"124–139\",\"bibtex\":\"@article{petrik_disruption_2019,\\n\\ttitle = {Disruption in an alluvial landscape: {Settlement} and environment dynamics on the alluvium of the river {Dyje} at the {Pohansko} archaeological site ({Czech} {Republic})},\\n\\tvolume = {511},\\n\\tissn = {1040-6182},\\n\\tshorttitle = {Disruption in an alluvial landscape},\\n\\turl = {http://www.sciencedirect.com/science/article/pii/S1040618217309503},\\n\\tdoi = {10.1016/j.quaint.2018.04.013},\\n\\tabstract = {Floodplain alluvia can provide a combination of natural and anthropogenic evidence of environmental changes, allowing to directly examine their evolution in relation to settlement dynamics. Such evidence is recorded, for example, at the archaeological site Pohansko by the town of Břeclav, a former centre of the Great Moravian Empire. The aim of our research was to explore what conditions on the floodplain could have caused the abandonment of this environment. Special attention was paid to the climax of the floodplain's occupation during the times of the Great Moravian Empire (AD 836–906) and to the decline of its occupation in the following centuries. The environmental record at the Pohansko site starts in the 7th century BC. From the Iron Age onwards (Hallstatt and La Tène periods) there is evidence of non-agricultural human activities. Since the 3rd and 2nd centuries BC to at least the second half of the 10th century AD, there is no record of any floodplain aggradation or flooding at the site. Later, both the archaeological and palaeoecological records on the floodplain probably got exposed and redeposited. The result is a mechanically disturbed layer that is synchronous with soil horizons and subsequent Early Mediaeval cultural layers covering sandy elevations. For an unknown reason, the site was deserted for many centuries after the end of the 10th century AD. During the High Mediaeval period and the early Modern Era, especially since the 15th century AD, overbank deposits covered the floodplain. Intensified human impact in the river catchment and climate change during the Little Ice Age were the main triggers of this change. The results correlate with the written historical sources pertaining to this area, which speak about an increasing frequency of flooding in the Czech lands since the 14th century, and especially in the second half of the 16th century. As a result, these sites became unsuitable for settlement and abandoned.},\\n\\tlanguage = {en},\\n\\turldate = {2020-03-05},\\n\\tjournal = {Quaternary International},\\n\\tauthor = {Petřík, Jan and Petr, Libor and Adameková, Katarína and Prišťáková, Michaela and Potůčková, Anna and Lenďáková, Zuzana and Frączek, Marcin and Dresler, Petr and Macháček, Jiří and Kalicki, Tomasz and Lisá, Lenka},\\n\\tmonth = mar,\\n\\tyear = {2019},\\n\\tkeywords = {Aggradation, Early Middle Ages, Floodplain, Floodplain occupation, Great Moravian Empire, Human impact, Iron Age, Late Holocene},\\n\\tpages = {124--139},\\n}\\n\\n\",\"author_short\":[\"Petřík, J.\",\"Petr, L.\",\"Adameková, K.\",\"Prišťáková, M.\",\"Potůčková, A.\",\"Lenďáková, Z.\",\"Frączek, M.\",\"Dresler, P.\",\"Macháček, J.\",\"Kalicki, T.\",\"Lisá, L.\"],\"key\":\"petrik_disruption_2019\",\"id\":\"petrik_disruption_2019\",\"bibbaseid\":\"petk-petr-adamekov-prikov-potkov-lenkov-frczek-dresler-etal-disruptioninanalluviallandscapesettlementandenvironmentdynamicsonthealluviumoftheriverdyjeatthepohanskoarchaeologicalsiteczechrepublic-2019\",\"role\":\"author\",\"urls\":{\"Paper\":\"http://www.sciencedirect.com/science/article/pii/S1040618217309503\"},\"keyword\":[\"Aggradation\",\"Early Middle Ages\",\"Floodplain\",\"Floodplain occupation\",\"Great Moravian Empire\",\"Human impact\",\"Iron Age\",\"Late Holocene\"],\"metadata\":{\"authorlinks\":{}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Soil charcoal elucidates the role of humans in the development of landscape of extreme biodiversity\",\"volume\":\"30\",\"copyright\":\"© 2019 John Wiley & Sons, Ltd.\",\"issn\":\"1099-145X\",\"url\":\"https://onlinelibrary.wiley.com/doi/abs/10.1002/ldr.3350\",\"doi\":\"10.1002/ldr.3350\",\"abstract\":\"The south-western White Carpathians (Czech Republic, Slovakia) are one of the few places in low-elevation Central Europe where a diverse landscape, including extremely species rich meadows, scattered oak trees, and mixed oak woodlands, has escaped modern transformation. We studied C14-dated and taxonomically identified macroscopic soil charcoal record to elucidate the genesis of this landscape. Thirteen soil profiles were sampled in grasslands along a gradient of elevation and history of human settlement. We identified clear pattern in the taxonomic composition of woody soil charcoal and anthracomass along this gradient, which we ascribe to different pathways of landscape development. Charcoal assemblages of chernozem-like soils in the promontories of the mountain range have a low anthracomass and are dominated by heliophilous and semishade species (Quercus, Pinus), with the oldest charcoals dated to pre-Neolithic times. Soils of the middle elevations have a high anthracomass and often show pronounced differences in charcoal composition at different soil depths; the oldest charcoal samples date back between the Neolithic and Early Middle Ages, and heliophilous species increase towards the topsoil. The soil of the summit area shows a medium anthracomass and charcoal assemblage dominated by shade-tolerant trees; the charcoal dates from the Middle Ages. Our results suggest continuity of an open to semiopen landscape in lower elevations of the White Carpathians, whereas middle and higher elevations experienced a forested period. Humans and fire played an important role in landscape development, as indicated by both soil charcoal and available palaeoecological and archaeological evidence. Local meadows with extremely high biodiversity thus appear to be a continuation of an ancient forest-steppe-like ecosystem.\",\"language\":\"en\",\"number\":\"13\",\"urldate\":\"2020-03-05\",\"journal\":\"Land Degradation & Development\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Novák\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Roleček\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Dresler\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hájek\"],\"firstnames\":[\"Michal\"],\"suffixes\":[]}],\"year\":\"2019\",\"note\":\"_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/ldr.3350\",\"keywords\":\"Holocene, biodiversity, forest-steppe, human settlement, soil charcoal\",\"pages\":\"1607–1619\",\"bibtex\":\"@article{novak_soil_2019,\\n\\ttitle = {Soil charcoal elucidates the role of humans in the development of landscape of extreme biodiversity},\\n\\tvolume = {30},\\n\\tcopyright = {© 2019 John Wiley \\\\& Sons, Ltd.},\\n\\tissn = {1099-145X},\\n\\turl = {https://onlinelibrary.wiley.com/doi/abs/10.1002/ldr.3350},\\n\\tdoi = {10.1002/ldr.3350},\\n\\tabstract = {The south-western White Carpathians (Czech Republic, Slovakia) are one of the few places in low-elevation Central Europe where a diverse landscape, including extremely species rich meadows, scattered oak trees, and mixed oak woodlands, has escaped modern transformation. We studied C14-dated and taxonomically identified macroscopic soil charcoal record to elucidate the genesis of this landscape. Thirteen soil profiles were sampled in grasslands along a gradient of elevation and history of human settlement. We identified clear pattern in the taxonomic composition of woody soil charcoal and anthracomass along this gradient, which we ascribe to different pathways of landscape development. Charcoal assemblages of chernozem-like soils in the promontories of the mountain range have a low anthracomass and are dominated by heliophilous and semishade species (Quercus, Pinus), with the oldest charcoals dated to pre-Neolithic times. Soils of the middle elevations have a high anthracomass and often show pronounced differences in charcoal composition at different soil depths; the oldest charcoal samples date back between the Neolithic and Early Middle Ages, and heliophilous species increase towards the topsoil. The soil of the summit area shows a medium anthracomass and charcoal assemblage dominated by shade-tolerant trees; the charcoal dates from the Middle Ages. Our results suggest continuity of an open to semiopen landscape in lower elevations of the White Carpathians, whereas middle and higher elevations experienced a forested period. Humans and fire played an important role in landscape development, as indicated by both soil charcoal and available palaeoecological and archaeological evidence. Local meadows with extremely high biodiversity thus appear to be a continuation of an ancient forest-steppe-like ecosystem.},\\n\\tlanguage = {en},\\n\\tnumber = {13},\\n\\turldate = {2020-03-05},\\n\\tjournal = {Land Degradation \\\\& Development},\\n\\tauthor = {Novák, Jan and Roleček, Jan and Dresler, Petr and Hájek, Michal},\\n\\tyear = {2019},\\n\\tnote = {\\\\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/ldr.3350},\\n\\tkeywords = {Holocene, biodiversity, forest-steppe, human settlement, soil charcoal},\\n\\tpages = {1607--1619},\\n}\\n\\n\",\"author_short\":[\"Novák, J.\",\"Roleček, J.\",\"Dresler, P.\",\"Hájek, M.\"],\"key\":\"novak_soil_2019\",\"id\":\"novak_soil_2019\",\"bibbaseid\":\"novk-roleek-dresler-hjek-soilcharcoalelucidatestheroleofhumansinthedevelopmentoflandscapeofextremebiodiversity-2019\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://onlinelibrary.wiley.com/doi/abs/10.1002/ldr.3350\"},\"keyword\":[\"Holocene\",\"biodiversity\",\"forest-steppe\",\"human settlement\",\"soil charcoal\"],\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Holocene forest transformations in sandstone landscapes of the Czech Republic: Stand-scale comparison of charcoal and pollen records:\",\"shorttitle\":\"Holocene forest transformations in sandstone landscapes of the Czech Republic\",\"url\":\"https://journals.sagepub.com/doi/10.1177/0959683619854510\",\"doi\":\"10.1177/0959683619854510\",\"abstract\":\"Stand-scale palaeoecology in sandstone landscapes provides insight into contrasting Holocene forest succession trajectories. Sharp geomorphological gradients in...\",\"language\":\"en\",\"urldate\":\"2020-03-05\",\"journal\":\"The Holocene\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Novák\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Abraham\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Šída\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pokorný\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"month\":\"June\",\"year\":\"2019\",\"note\":\"Publisher: SAGE PublicationsSage UK: London, England\",\"bibtex\":\"@article{novak_holocene_2019,\\n\\ttitle = {Holocene forest transformations in sandstone landscapes of the {Czech} {Republic}: {Stand}-scale comparison of charcoal and pollen records:},\\n\\tshorttitle = {Holocene forest transformations in sandstone landscapes of the {Czech} {Republic}},\\n\\turl = {https://journals.sagepub.com/doi/10.1177/0959683619854510},\\n\\tdoi = {10.1177/0959683619854510},\\n\\tabstract = {Stand-scale palaeoecology in sandstone landscapes provides insight into contrasting Holocene forest succession trajectories. Sharp geomorphological gradients in...},\\n\\tlanguage = {en},\\n\\turldate = {2020-03-05},\\n\\tjournal = {The Holocene},\\n\\tauthor = {Novák, Jan and Abraham, Vojtěch and Šída, Petr and Pokorný, Petr},\\n\\tmonth = jun,\\n\\tyear = {2019},\\n\\tnote = {Publisher: SAGE PublicationsSage UK: London, England},\\n}\\n\\n\",\"author_short\":[\"Novák, J.\",\"Abraham, V.\",\"Šída, P.\",\"Pokorný, P.\"],\"key\":\"novak_holocene_2019\",\"id\":\"novak_holocene_2019\",\"bibbaseid\":\"novk-abraham-da-pokorn-holoceneforesttransformationsinsandstonelandscapesoftheczechrepublicstandscalecomparisonofcharcoalandpollenrecords-2019\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://journals.sagepub.com/doi/10.1177/0959683619854510\"},\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Buried Late Weichselian thermokarst landscape discovered in the Czech Republic, central Europe\",\"volume\":\"48\",\"copyright\":\"© 2019 Collegium Boreas. Published by John Wiley & Sons Ltd\",\"issn\":\"1502-3885\",\"doi\":\"10.1111/bor.12404\",\"abstract\":\"Pronounced climatic warming associated with the Late Weichselian Pleniglacial-to-Lateglacial transition caused considerable environmental changes throughout the former periglacial zones (in Europe 53°–46°N). During permafrost degradation and subsequent ground subsidence (i.e. thermokarst processes), the landscape changed rapidly. In this study we investigated a flat mid-altitude area in south Bohemia, Czech Republic, lying close to the southern limit of the Weichselian permafrost. We discovered palaeo-lake basins with sedimentary infillings up to 11 m in depth. According to radiocarbon and palynostratigraphical dating, these basins were formed at the onset of the Late Pleniglacial-to-Lateglacial transition, whereas the smaller depressions were formed later. We suggest that the basins resulted from thermal and fluvio-thermal erosion of the former permafrost and represent remnants of discontinuous gullies and possibly collapsed frost mounds (pingo/lithalsa scars). The formation of this a fossil thermokarst landscape was climatically driven and multiple phased, with the major phase during the climatic warming and wetting at the onset of GI-1e (Bølling) and the minor phase during GI-1c (Allerød). This study enhances knowledge of the palaeogeography of the former European periglacial zone by showing that Late Pleistocene thermokarst activity could have had a significant impact on the evolution of the landscape of at least some regions of central Europe along the southern limit of the continuous permafrost zone. The research also points to a similar history for the physical transformation of the landscape of the former European periglacial zone and current thermokarst landscapes and could be a valuable source of information with respect to the future transformation of the Arctic under conditions of ongoing global warming.\",\"language\":\"English\",\"number\":\"4\",\"urldate\":\"2020-03-05\",\"journal\":\"Boreas\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Hošek\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Prach\"],\"firstnames\":[\"Jindřich\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Křížek\"],\"firstnames\":[\"Marek\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Šída\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Moska\"],\"firstnames\":[\"Piotr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pokorný\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"year\":\"2019\",\"pages\":\"988–1005\",\"bibtex\":\"@article{hosek_buried_2019,\\n\\ttitle = {Buried {Late} {Weichselian} thermokarst landscape discovered in the {Czech} {Republic}, central {Europe}},\\n\\tvolume = {48},\\n\\tcopyright = {© 2019 Collegium Boreas. Published by John Wiley \\\\& Sons Ltd},\\n\\tissn = {1502-3885},\\n\\tdoi = {10.1111/bor.12404},\\n\\tabstract = {Pronounced climatic warming associated with the Late Weichselian Pleniglacial-to-Lateglacial transition caused considerable environmental changes throughout the former periglacial zones (in Europe 53°–46°N). During permafrost degradation and subsequent ground subsidence (i.e. thermokarst processes), the landscape changed rapidly. In this study we investigated a flat mid-altitude area in south Bohemia, Czech Republic, lying close to the southern limit of the Weichselian permafrost. We discovered palaeo-lake basins with sedimentary infillings up to 11 m in depth. According to radiocarbon and palynostratigraphical dating, these basins were formed at the onset of the Late Pleniglacial-to-Lateglacial transition, whereas the smaller depressions were formed later. We suggest that the basins resulted from thermal and fluvio-thermal erosion of the former permafrost and represent remnants of discontinuous gullies and possibly collapsed frost mounds (pingo/lithalsa scars). The formation of this a fossil thermokarst landscape was climatically driven and multiple phased, with the major phase during the climatic warming and wetting at the onset of GI-1e (Bølling) and the minor phase during GI-1c (Allerød). This study enhances knowledge of the palaeogeography of the former European periglacial zone by showing that Late Pleistocene thermokarst activity could have had a significant impact on the evolution of the landscape of at least some regions of central Europe along the southern limit of the continuous permafrost zone. The research also points to a similar history for the physical transformation of the landscape of the former European periglacial zone and current thermokarst landscapes and could be a valuable source of information with respect to the future transformation of the Arctic under conditions of ongoing global warming.},\\n\\tlanguage = {English},\\n\\tnumber = {4},\\n\\turldate = {2020-03-05},\\n\\tjournal = {Boreas},\\n\\tauthor = {Hošek, Jan and Prach, Jindřich and Křížek, Marek and Šída, Petr and Moska, Piotr and Pokorný, Petr},\\n\\tyear = {2019},\\n\\tpages = {988--1005},\\n}\\n\\n\",\"author_short\":[\"Hošek, J.\",\"Prach, J.\",\"Křížek, M.\",\"Šída, P.\",\"Moska, P.\",\"Pokorný, P.\"],\"key\":\"hosek_buried_2019\",\"id\":\"hosek_buried_2019\",\"bibbaseid\":\"hoek-prach-kek-da-moska-pokorn-buriedlateweichselianthermokarstlandscapediscoveredintheczechrepubliccentraleurope-2019\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Crops along the trade routes? Archaeobotany of the Bronze Age in the region of South Bohemia (Czech Republic) in context with longer distance trade and exchange networks\",\"volume\":\"11\",\"issn\":\"1866-9565\",\"shorttitle\":\"Crops along the trade routes?\",\"doi\":\"10.1007/s12520-019-00893-6\",\"abstract\":\"The number of species of crop plants in Central Europe increased constantly during the Bronze Age. The structure of the composition of cultivated plants was probably connected to the cultural contacts of human populations. During the Bronze Age (2300/2000–800 BC), the region of South Bohemia (Czech Republic) increasingly became the focus of long-distance trade and exchange networks with regions to the east and many other regions (the Eastern Alps, the Alpine Foreland, the central lowlands of the Czech Republic, Hungary and Western Slovakia). The aim of the paper is to examine archaeobotanical assemblages of charred plant remains to see if these changes within Bronze Age societies, and their spheres of interaction, are also recorded within their agricultural practices. In particular, the importance of specific individual crop species can be reflected in the study region in comparison with other individual regions of Central Europe. Humans in the region of South Bohemia had more connections with the Eastern Alps and the Alpine Foreland region during the Early and Middle Bronze Ages. Regarding the structure of crop species, the composition of sub/dominant crops in South Bohemia and the Eastern Alps and the Alpine Foreland had many similarities. The cultural trajectory of the human populations of the South Bohemian region changed substantially in the Late and Final Bronze Ages: intensive contacts are documented, primarily with the region of Central Bohemia. This is reflected in the composition of the sub/dominant crops in South Bohemia, which shows many similarities to the other regions of the Czech Republic. Changes in migration and exchange networks—in particular those that involved more formalised trade—are associated with a large number of innovations and specific goods and led to much wider levels of cultural and social integration within Bronze Age Europe than had been previously seen.\",\"language\":\"English\",\"number\":\"10\",\"urldate\":\"2020-03-05\",\"journal\":\"Archaeological and Anthropological Sciences\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Šálková\"],\"firstnames\":[\"Tereza\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chvojka\"],\"firstnames\":[\"Ondřej\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hlásek\"],\"firstnames\":[\"Daniel\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jiřík\"],\"firstnames\":[\"Jaroslav\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"John\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Novák\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kovačiková\"],\"firstnames\":[\"Lenka\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Beneš\"],\"firstnames\":[\"Jaromír\"],\"suffixes\":[]}],\"month\":\"October\",\"year\":\"2019\",\"pages\":\"5569–5590\",\"bibtex\":\"@article{salkova_crops_2019,\\n\\ttitle = {Crops along the trade routes? {Archaeobotany} of the {Bronze} {Age} in the region of {South} {Bohemia} ({Czech} {Republic}) in context with longer distance trade and exchange networks},\\n\\tvolume = {11},\\n\\tissn = {1866-9565},\\n\\tshorttitle = {Crops along the trade routes?},\\n\\tdoi = {10.1007/s12520-019-00893-6},\\n\\tabstract = {The number of species of crop plants in Central Europe increased constantly during the Bronze Age. The structure of the composition of cultivated plants was probably connected to the cultural contacts of human populations. During the Bronze Age (2300/2000–800 BC), the region of South Bohemia (Czech Republic) increasingly became the focus of long-distance trade and exchange networks with regions to the east and many other regions (the Eastern Alps, the Alpine Foreland, the central lowlands of the Czech Republic, Hungary and Western Slovakia). The aim of the paper is to examine archaeobotanical assemblages of charred plant remains to see if these changes within Bronze Age societies, and their spheres of interaction, are also recorded within their agricultural practices. In particular, the importance of specific individual crop species can be reflected in the study region in comparison with other individual regions of Central Europe. Humans in the region of South Bohemia had more connections with the Eastern Alps and the Alpine Foreland region during the Early and Middle Bronze Ages. Regarding the structure of crop species, the composition of sub/dominant crops in South Bohemia and the Eastern Alps and the Alpine Foreland had many similarities. The cultural trajectory of the human populations of the South Bohemian region changed substantially in the Late and Final Bronze Ages: intensive contacts are documented, primarily with the region of Central Bohemia. This is reflected in the composition of the sub/dominant crops in South Bohemia, which shows many similarities to the other regions of the Czech Republic. Changes in migration and exchange networks—in particular those that involved more formalised trade—are associated with a large number of innovations and specific goods and led to much wider levels of cultural and social integration within Bronze Age Europe than had been previously seen.},\\n\\tlanguage = {English},\\n\\tnumber = {10},\\n\\turldate = {2020-03-05},\\n\\tjournal = {Archaeological and Anthropological Sciences},\\n\\tauthor = {Šálková, Tereza and Chvojka, Ondřej and Hlásek, Daniel and Jiřík, Jaroslav and John, Jan and Novák, Jan and Kovačiková, Lenka and Beneš, Jaromír},\\n\\tmonth = oct,\\n\\tyear = {2019},\\n\\tpages = {5569--5590},\\n}\\n\\n\",\"author_short\":[\"Šálková, T.\",\"Chvojka, O.\",\"Hlásek, D.\",\"Jiřík, J.\",\"John, J.\",\"Novák, J.\",\"Kovačiková, L.\",\"Beneš, J.\"],\"key\":\"salkova_crops_2019\",\"id\":\"salkova_crops_2019\",\"bibbaseid\":\"lkov-chvojka-hlsek-jik-john-novk-kovaikov-bene-cropsalongthetraderoutesarchaeobotanyofthebronzeageintheregionofsouthbohemiaczechrepublicincontextwithlongerdistancetradeandexchangenetworks-2019\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Nutrient availability affected shallow-lake ecosystem response along the Late-Glacial/Holocene transition\",\"volume\":\"846\",\"issn\":\"1573-5117\",\"doi\":\"10.1007/s10750-019-04054-7\",\"abstract\":\"Shallow lowland lakes undergo long-lasting natural eutrophication processes, which can be studied through the development of communities of aquatic organisms. However, records showing millennial-scale trophic status variability in these water bodies are rare. Two radiocarbon-dated sedimentary profiles from former (now destroyed by brown coal mining) Lake Komořany (Central Europe, Czech Republic) served for a multi-proxy study of biological remains (diatoms, chironomids, pollen) supplemented by X-ray fluorescence (XRF) and loss-on-ignition (LOI). The age–depth model and palynostratigraphy confirm a continuous Late-Glacial to Early-Holocene record. The results suggest consistent in-lake conditions with high nutrient availability since the lake origin in the Late-Glacial period. A distinct shift at the Late-Glacial/Holocene boundary evidenced by an enhancement in diatom valve concentration and a lithological interface was foregone by a qualitative change in diatom and chironomid assemblages along with rise in LOI. It suggests that a major transformation occurred before the onset of the Holocene. As this qualitative change was characterized by a decrease in relative abundance of nutrient-demanding species, we propose an indirect climatic control by means of nutrient availability as the main driver of the aquatic species composition.\",\"language\":\"English\",\"number\":\"1\",\"urldate\":\"2020-03-05\",\"journal\":\"Hydrobiologia\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Tichá\"],\"firstnames\":[\"Anna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bešta\"],\"firstnames\":[\"Tomáš\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Vondrák\"],\"firstnames\":[\"Daniel\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Houfková\"],\"firstnames\":[\"Petra\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jankovská\"],\"firstnames\":[\"Vlasta\"],\"suffixes\":[]}],\"month\":\"December\",\"year\":\"2019\",\"pages\":\"87–108\",\"bibtex\":\"@article{ticha_nutrient_2019,\\n\\ttitle = {Nutrient availability affected shallow-lake ecosystem response along the {Late}-{Glacial}/{Holocene} transition},\\n\\tvolume = {846},\\n\\tissn = {1573-5117},\\n\\tdoi = {10.1007/s10750-019-04054-7},\\n\\tabstract = {Shallow lowland lakes undergo long-lasting natural eutrophication processes, which can be studied through the development of communities of aquatic organisms. However, records showing millennial-scale trophic status variability in these water bodies are rare. Two radiocarbon-dated sedimentary profiles from former (now destroyed by brown coal mining) Lake Komořany (Central Europe, Czech Republic) served for a multi-proxy study of biological remains (diatoms, chironomids, pollen) supplemented by X-ray fluorescence (XRF) and loss-on-ignition (LOI). The age–depth model and palynostratigraphy confirm a continuous Late-Glacial to Early-Holocene record. The results suggest consistent in-lake conditions with high nutrient availability since the lake origin in the Late-Glacial period. A distinct shift at the Late-Glacial/Holocene boundary evidenced by an enhancement in diatom valve concentration and a lithological interface was foregone by a qualitative change in diatom and chironomid assemblages along with rise in LOI. It suggests that a major transformation occurred before the onset of the Holocene. As this qualitative change was characterized by a decrease in relative abundance of nutrient-demanding species, we propose an indirect climatic control by means of nutrient availability as the main driver of the aquatic species composition.},\\n\\tlanguage = {English},\\n\\tnumber = {1},\\n\\turldate = {2020-03-05},\\n\\tjournal = {Hydrobiologia},\\n\\tauthor = {Tichá, Anna and Bešta, Tomáš and Vondrák, Daniel and Houfková, Petra and Jankovská, Vlasta},\\n\\tmonth = dec,\\n\\tyear = {2019},\\n\\tpages = {87--108},\\n}\\n\\n\",\"author_short\":[\"Tichá, A.\",\"Bešta, T.\",\"Vondrák, D.\",\"Houfková, P.\",\"Jankovská, V.\"],\"key\":\"ticha_nutrient_2019\",\"id\":\"ticha_nutrient_2019\",\"bibbaseid\":\"tich-beta-vondrk-houfkov-jankovsk-nutrientavailabilityaffectedshallowlakeecosystemresponsealongthelateglacialholocenetransition-2019\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"The dynamics of a non-forested stand in the Krušné Mts.: the effect of a short-lived medieval village on the local environment\",\"volume\":\"28\",\"issn\":\"1617-6278\",\"shorttitle\":\"The dynamics of a non-forested stand in the Krušné Mts.\",\"url\":\"https://doi.org/10.1007/s00334-019-00718-5\",\"doi\":\"10.1007/s00334-019-00718-5\",\"abstract\":\"Medieval vegetation–human–climate interactions were studied from a sediment profile situated in the centre of a short-lived medieval village located above 800 m a.s.l. on the ridge of the Krušné Mts., NW Bohemia, Central Europe. Analyses of pollen, seeds/fruits, micro- and macro-charcoals, diatoms and concentrations of microelements in connection with written sources revealed a significant human-induced deforestation in the second half of the 14th century. This deforestation occurred sooner than supposed and the area did not revert after ad 1347 as elsewhere in Europe. Arable fields probably enabled basic self-sustaining cultivation of winter cereals even at such elevations in the climatically favourable years of the Medieval Warm Period. The village presumably collapsed due to a combination of weather fluctuations at the onset of the Little Ice Age, simultaneous socioeconomic stagnation in the Czech Lands and exploitation of the surrounding forest. The dynamics of wet stand vegetation and Calthion palustris montane wet meadows were driven by fluctuating human and grazing impacts. Annual and biennial herbaceous species that peaked after village abandonment were rapidly replaced by Filipendula ulmaria and Salix stands. The secondary forest developed towards Picea stands. Only later, mesic montane meadows of medium tall grasses combined with Meum athamanticum and mountain dry pastures developed on nutrient poor patches.\",\"language\":\"en\",\"number\":\"6\",\"urldate\":\"2020-03-05\",\"journal\":\"Vegetation History and Archaeobotany\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Houfková\"],\"firstnames\":[\"Petra\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Horák\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pokorná\"],\"firstnames\":[\"Adéla\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bešta\"],\"firstnames\":[\"Tomáš\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pravcová\"],\"firstnames\":[\"Ivana\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Novák\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Klír\"],\"firstnames\":[\"Tomáš\"],\"suffixes\":[]}],\"month\":\"November\",\"year\":\"2019\",\"pages\":\"607–621\",\"bibtex\":\"@article{houfkova_dynamics_2019,\\n\\ttitle = {The dynamics of a non-forested stand in the {Krušné} {Mts}.: the effect of a short-lived medieval village on the local environment},\\n\\tvolume = {28},\\n\\tissn = {1617-6278},\\n\\tshorttitle = {The dynamics of a non-forested stand in the {Krušné} {Mts}.},\\n\\turl = {https://doi.org/10.1007/s00334-019-00718-5},\\n\\tdoi = {10.1007/s00334-019-00718-5},\\n\\tabstract = {Medieval vegetation–human–climate interactions were studied from a sediment profile situated in the centre of a short-lived medieval village located above 800 m a.s.l. on the ridge of the Krušné Mts., NW Bohemia, Central Europe. Analyses of pollen, seeds/fruits, micro- and macro-charcoals, diatoms and concentrations of microelements in connection with written sources revealed a significant human-induced deforestation in the second half of the 14th century. This deforestation occurred sooner than supposed and the area did not revert after ad 1347 as elsewhere in Europe. Arable fields probably enabled basic self-sustaining cultivation of winter cereals even at such elevations in the climatically favourable years of the Medieval Warm Period. The village presumably collapsed due to a combination of weather fluctuations at the onset of the Little Ice Age, simultaneous socioeconomic stagnation in the Czech Lands and exploitation of the surrounding forest. The dynamics of wet stand vegetation and Calthion palustris montane wet meadows were driven by fluctuating human and grazing impacts. Annual and biennial herbaceous species that peaked after village abandonment were rapidly replaced by Filipendula ulmaria and Salix stands. The secondary forest developed towards Picea stands. Only later, mesic montane meadows of medium tall grasses combined with Meum athamanticum and mountain dry pastures developed on nutrient poor patches.},\\n\\tlanguage = {en},\\n\\tnumber = {6},\\n\\turldate = {2020-03-05},\\n\\tjournal = {Vegetation History and Archaeobotany},\\n\\tauthor = {Houfková, Petra and Horák, Jan and Pokorná, Adéla and Bešta, Tomáš and Pravcová, Ivana and Novák, Jan and Klír, Tomáš},\\n\\tmonth = nov,\\n\\tyear = {2019},\\n\\tpages = {607--621},\\n}\\n\\n\",\"author_short\":[\"Houfková, P.\",\"Horák, J.\",\"Pokorná, A.\",\"Bešta, T.\",\"Pravcová, I.\",\"Novák, J.\",\"Klír, T.\"],\"key\":\"houfkova_dynamics_2019\",\"id\":\"houfkova_dynamics_2019\",\"bibbaseid\":\"houfkov-hork-pokorn-beta-pravcov-novk-klr-thedynamicsofanonforestedstandinthekrunmtstheeffectofashortlivedmedievalvillageonthelocalenvironment-2019\",\"role\":\"author\",\"urls\":{\"Paper\":\"https://doi.org/10.1007/s00334-019-00718-5\"},\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Lowland pine forests in the northwestern Pannonian Basin: between natural vegetation and modern plantations\",\"volume\":\"19\",\"issn\":\"1436-378X\",\"shorttitle\":\"Lowland pine forests in the northwestern Pannonian Basin\",\"doi\":\"10.1007/s10113-019-01555-y\",\"abstract\":\"Lowland Scots pine (Pinus sylvestris L.) forests cover extensive areas in Central Europe. Most of them are considered to be the results of relatively recent plantation-oriented forest management. We investigated the long-term history of lowland pine forests in the Záhorská Lowland region of aeolian sands in the northern margin of the Pannonian Basin. Pine monocultures were planted there already in the mid-seventeenth century and currently prevail in the land cover of the region. Our aim was to challenge the commonly accepted idea that the present pine-dominated forests lack connections to pre-plantation pine forests of the Early Holocene. Using multi-proxy data, we compared palaeoeocological data with archaeobotanical data, anthracological finds and evidence on past human settlement. Palaeoecological results suggested a distinct compositional linkage of recent pine-dominated forests with their Early Holocene predecessors. Moreover, no significant change was detected in tree dominants in at least the past two millennia. Contrary to palaeoecology, archeaeobotany suggested that broadleaved trees (mostly oak) dominated during the past 4000 years. However, this result is probably strongly biased by human preferences for wood for specific purposes. On the other hand, pine in palaeoecological data is doubtless overrepresented because of its abundant pollen production. We conclude that pine forests with a significant admixture of oak continuously covered the sandy substrates of the Záhorská Lowland throughout the Holocene. The present pine forests can therefore be considered fairly close to the original vegetation of the study region.\",\"language\":\"English\",\"number\":\"8\",\"urldate\":\"2020-03-05\",\"journal\":\"Regional Environmental Change\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Jamrichová\"],\"firstnames\":[\"Eva\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bobek\"],\"firstnames\":[\"Přemysl\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Šolcová\"],\"firstnames\":[\"Anna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tkáč\"],\"firstnames\":[\"Peter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hédl\"],\"firstnames\":[\"Radim\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Valachovič\"],\"firstnames\":[\"Milan\"],\"suffixes\":[]}],\"month\":\"December\",\"year\":\"2019\",\"pages\":\"2395–2409\",\"bibtex\":\"@article{jamrichova_lowland_2019,\\n\\ttitle = {Lowland pine forests in the northwestern {Pannonian} {Basin}: between natural vegetation and modern plantations},\\n\\tvolume = {19},\\n\\tissn = {1436-378X},\\n\\tshorttitle = {Lowland pine forests in the northwestern {Pannonian} {Basin}},\\n\\tdoi = {10.1007/s10113-019-01555-y},\\n\\tabstract = {Lowland Scots pine (Pinus sylvestris L.) forests cover extensive areas in Central Europe. Most of them are considered to be the results of relatively recent plantation-oriented forest management. We investigated the long-term history of lowland pine forests in the Záhorská Lowland region of aeolian sands in the northern margin of the Pannonian Basin. Pine monocultures were planted there already in the mid-seventeenth century and currently prevail in the land cover of the region. Our aim was to challenge the commonly accepted idea that the present pine-dominated forests lack connections to pre-plantation pine forests of the Early Holocene. Using multi-proxy data, we compared palaeoeocological data with archaeobotanical data, anthracological finds and evidence on past human settlement. Palaeoecological results suggested a distinct compositional linkage of recent pine-dominated forests with their Early Holocene predecessors. Moreover, no significant change was detected in tree dominants in at least the past two millennia. Contrary to palaeoecology, archeaeobotany suggested that broadleaved trees (mostly oak) dominated during the past 4000 years. However, this result is probably strongly biased by human preferences for wood for specific purposes. On the other hand, pine in palaeoecological data is doubtless overrepresented because of its abundant pollen production. We conclude that pine forests with a significant admixture of oak continuously covered the sandy substrates of the Záhorská Lowland throughout the Holocene. The present pine forests can therefore be considered fairly close to the original vegetation of the study region.},\\n\\tlanguage = {English},\\n\\tnumber = {8},\\n\\turldate = {2020-03-05},\\n\\tjournal = {Regional Environmental Change},\\n\\tauthor = {Jamrichová, Eva and Bobek, Přemysl and Šolcová, Anna and Tkáč, Peter and Hédl, Radim and Valachovič, Milan},\\n\\tmonth = dec,\\n\\tyear = {2019},\\n\\tpages = {2395--2409},\\n}\\n\\n\",\"author_short\":[\"Jamrichová, E.\",\"Bobek, P.\",\"Šolcová, A.\",\"Tkáč, P.\",\"Hédl, R.\",\"Valachovič, M.\"],\"key\":\"jamrichova_lowland_2019\",\"id\":\"jamrichova_lowland_2019\",\"bibbaseid\":\"jamrichov-bobek-olcov-tk-hdl-valachovi-lowlandpineforestsinthenorthwesternpannonianbasinbetweennaturalvegetationandmodernplantations-2019\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Changing disturbance-diversity relationships in temperate ecosystems over the past 12000 years\",\"volume\":\"107\",\"copyright\":\"© 2019 The Authors. Journal of Ecology © 2019 British Ecological Society\",\"issn\":\"1365-2745\",\"doi\":\"10.1111/1365-2745.13136\",\"abstract\":\"Disturbances such as fires and grazing have major impacts on biodiversity. While it has been suggested that species richness is highest with intermediate levels of disturbance, currently there is no consensus due to an absence of data covering large temporal and spatial scales. We developed a new method to examine disturbance-diversity relationships (DDR) using sedimentary pollen data linked with species’ disturbance ecology. We reconstructed disturbance and diversity dynamics in the region of the European temperate zone over the last 12,000 years and calculated DDR for 900-year sequential temporal windows. Disturbance frequency was highest in the early and late Holocene, while remaining low in the mid-Holocene. Diversity increased continuously from the start of the Holocene. Our results demonstrate that over the past 12,000 years DDR changed from hump-shaped into monotonic increasing pattern. While both highly disturbed and undisturbed sites were strongly impoverished in the early Holocene, as species migrated, biodiversity levels have subsequently affected disturbance regimes with highly disturbed sites now being the highest in species richness. Synthesis. Land-use changes in the last 4,000 years created an increasingly patchy landscape, allowing invasive species adapted to high-frequency disturbance to migrate across the landscape. The link between high diversity and disturbed areas is relatively recent and may anticipate even greater disturbance frequencies in future. Our findings also support a hypothesis that species migration, and the structure of the species pool critically determines the response of biota to external factors such as disturbance.\",\"language\":\"English\",\"number\":\"4\",\"urldate\":\"2019-06-28\",\"journal\":\"Journal of Ecology\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Abraham\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Herben\"],\"firstnames\":[\"Tomáš\"],\"suffixes\":[]}],\"year\":\"2019\",\"note\":\"[IF2018=5.687]\",\"keywords\":\"Central Europe, Holocene, disturbance, disturbance frequency, pollen, richness, vegetation\",\"pages\":\"1678–1688\",\"bibtex\":\"@article{kunes_changing_2019,\\n\\ttitle = {Changing disturbance-diversity relationships in temperate ecosystems over the past 12000 years},\\n\\tvolume = {107},\\n\\tcopyright = {© 2019 The Authors. Journal of Ecology © 2019 British Ecological Society},\\n\\tissn = {1365-2745},\\n\\tdoi = {10.1111/1365-2745.13136},\\n\\tabstract = {Disturbances such as fires and grazing have major impacts on biodiversity. While it has been suggested that species richness is highest with intermediate levels of disturbance, currently there is no consensus due to an absence of data covering large temporal and spatial scales. We developed a new method to examine disturbance-diversity relationships (DDR) using sedimentary pollen data linked with species’ disturbance ecology. We reconstructed disturbance and diversity dynamics in the region of the European temperate zone over the last 12,000 years and calculated DDR for 900-year sequential temporal windows. Disturbance frequency was highest in the early and late Holocene, while remaining low in the mid-Holocene. Diversity increased continuously from the start of the Holocene. Our results demonstrate that over the past 12,000 years DDR changed from hump-shaped into monotonic increasing pattern. While both highly disturbed and undisturbed sites were strongly impoverished in the early Holocene, as species migrated, biodiversity levels have subsequently affected disturbance regimes with highly disturbed sites now being the highest in species richness. Synthesis. Land-use changes in the last 4,000 years created an increasingly patchy landscape, allowing invasive species adapted to high-frequency disturbance to migrate across the landscape. The link between high diversity and disturbed areas is relatively recent and may anticipate even greater disturbance frequencies in future. Our findings also support a hypothesis that species migration, and the structure of the species pool critically determines the response of biota to external factors such as disturbance.},\\n\\tlanguage = {English},\\n\\tnumber = {4},\\n\\turldate = {2019-06-28},\\n\\tjournal = {Journal of Ecology},\\n\\tauthor = {Kuneš, Petr and Abraham, Vojtěch and Herben, Tomáš},\\n\\tyear = {2019},\\n\\tnote = {[IF2018=5.687]},\\n\\tkeywords = {Central Europe, Holocene, disturbance, disturbance frequency, pollen, richness, vegetation},\\n\\tpages = {1678--1688},\\n}\\n\\n\",\"author_short\":[\"Kuneš, P.\",\"Abraham, V.\",\"Herben, T.\"],\"key\":\"kunes_changing_2019\",\"id\":\"kunes_changing_2019\",\"bibbaseid\":\"kune-abraham-herben-changingdisturbancediversityrelationshipsintemperateecosystemsoverthepast12000years-2019\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Central Europe\",\"Holocene\",\"disturbance\",\"disturbance frequency\",\"pollen\",\"richness\",\"vegetation\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":4,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Holocene rapid climate changes and ice-rafting debris events reflected in high-resolution European charcoal records\",\"volume\":\"222\",\"issn\":\"0277-3791\",\"doi\":\"10.1016/j.quascirev.2019.105877\",\"abstract\":\"In contrast to marked climate change across glacial-interglacial cycles, the Holocene epoch represents a relatively warm, stable interval. However, on finer temporal scales, it too has experienced both gradual and rapid changes in climate. In the North Atlantic region, many rapid climate changes (RCCs) coincide with ice-rafted debris (IRD) or Bond events, which are associated with cooling and suggested to occur with periodicities of 1370 ± 500 years. Given that climate is a dominant control of fire activity, regulating both vegetation productivity and fuel moisture, this study investigated the linkage between Holocene fire, IRD episodes and associated RCCs in seven high-resolution charcoal records distributed across Europe. Results show low-frequency fire periodicities of 500–600 years, 900–1400 and 2400 years that occurred simultaneously across northern and mid-latitude Europe, suggesting that regional fire disturbance responded to large-scale climate drivers. The 900–1400 year periodicity is most common among sites and of similar frequency to IRD episodes, potentially reflecting a connection between mechanisms regulating IRD flux in the North Atlantic and wildfire activity in Europe. Although the data indicate some spatial variability in fire induced by local drivers (such as vegetation and human impact) during RCC events associated with IRD peaks, broad-scale patterns are discernible. Specifically, Northern Europe burned more during the 10.2, 9.4, 8.2, 5.9 and 4.2 kiloannum before present (ka) RCC events when climate was drier, and less during the 2.9 and 1.4 ka events when climate was moister. In contrast, in mid-latitude Europe, a higher incidence of fire is documented at 8.2 and 1.4 ka when climate was drier and a lower incidence of fire is associated with moister conditions at 10.2, 9.4 and 2.9 ka. Spatial heterogeneity is evident in mid-latitude Europe during the 5.9, 4.2 and 0.4 ka events. These spatially explicit sub-continental scale differences in fire activity may be related to differences in moisture availability resulting from shifts in associated atmospheric circulation patterns.\",\"language\":\"English\",\"urldate\":\"2019-09-08\",\"journal\":\"Quaternary Science Reviews\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Florescu\"],\"firstnames\":[\"Gabriela\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Brown\"],\"firstnames\":[\"Kendrick\",\"J.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Carter\"],\"firstnames\":[\"Vachel\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Veski\"],\"firstnames\":[\"Siim\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Feurdean\"],\"firstnames\":[\"Angelica\"],\"suffixes\":[]}],\"month\":\"October\",\"year\":\"2019\",\"note\":\"[IF2018=4.641]\",\"keywords\":\"Europe, Fire cycles, Holocene, Ice rafted debris events, Macroscopic charcoal, Rapid climate change, disturbance\",\"pages\":\"105877\",\"bibtex\":\"@article{florescu_holocene_2019,\\n\\ttitle = {Holocene rapid climate changes and ice-rafting debris events reflected in high-resolution {European} charcoal records},\\n\\tvolume = {222},\\n\\tissn = {0277-3791},\\n\\tdoi = {10.1016/j.quascirev.2019.105877},\\n\\tabstract = {In contrast to marked climate change across glacial-interglacial cycles, the Holocene epoch represents a relatively warm, stable interval. However, on finer temporal scales, it too has experienced both gradual and rapid changes in climate. In the North Atlantic region, many rapid climate changes (RCCs) coincide with ice-rafted debris (IRD) or Bond events, which are associated with cooling and suggested to occur with periodicities of 1370 ± 500 years. Given that climate is a dominant control of fire activity, regulating both vegetation productivity and fuel moisture, this study investigated the linkage between Holocene fire, IRD episodes and associated RCCs in seven high-resolution charcoal records distributed across Europe. Results show low-frequency fire periodicities of 500–600 years, 900–1400 and 2400 years that occurred simultaneously across northern and mid-latitude Europe, suggesting that regional fire disturbance responded to large-scale climate drivers. The 900–1400 year periodicity is most common among sites and of similar frequency to IRD episodes, potentially reflecting a connection between mechanisms regulating IRD flux in the North Atlantic and wildfire activity in Europe. Although the data indicate some spatial variability in fire induced by local drivers (such as vegetation and human impact) during RCC events associated with IRD peaks, broad-scale patterns are discernible. Specifically, Northern Europe burned more during the 10.2, 9.4, 8.2, 5.9 and 4.2 kiloannum before present (ka) RCC events when climate was drier, and less during the 2.9 and 1.4 ka events when climate was moister. In contrast, in mid-latitude Europe, a higher incidence of fire is documented at 8.2 and 1.4 ka when climate was drier and a lower incidence of fire is associated with moister conditions at 10.2, 9.4 and 2.9 ka. Spatial heterogeneity is evident in mid-latitude Europe during the 5.9, 4.2 and 0.4 ka events. These spatially explicit sub-continental scale differences in fire activity may be related to differences in moisture availability resulting from shifts in associated atmospheric circulation patterns.},\\n\\tlanguage = {English},\\n\\turldate = {2019-09-08},\\n\\tjournal = {Quaternary Science Reviews},\\n\\tauthor = {Florescu, Gabriela and Brown, Kendrick J. and Carter, Vachel A. and Kuneš, Petr and Veski, Siim and Feurdean, Angelica},\\n\\tmonth = oct,\\n\\tyear = {2019},\\n\\tnote = {[IF2018=4.641]},\\n\\tkeywords = {Europe, Fire cycles, Holocene, Ice rafted debris events, Macroscopic charcoal, Rapid climate change, disturbance},\\n\\tpages = {105877},\\n}\\n\\n\",\"author_short\":[\"Florescu, G.\",\"Brown, K. J.\",\"Carter, V. A.\",\"Kuneš, P.\",\"Veski, S.\",\"Feurdean, A.\"],\"key\":\"florescu_holocene_2019\",\"id\":\"florescu_holocene_2019\",\"bibbaseid\":\"florescu-brown-carter-kune-veski-feurdean-holocenerapidclimatechangesandiceraftingdebriseventsreflectedinhighresolutioneuropeancharcoalrecords-2019\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Europe\",\"Fire cycles\",\"Holocene\",\"Ice rafted debris events\",\"Macroscopic charcoal\",\"Rapid climate change\",\"disturbance\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Early and middle Holocene ecosystem changes at the Western Carpathian/Pannonian border driven by climate and Neolithic impact\",\"volume\":\"47\",\"copyright\":\"© 2018 Collegium Boreas. Published by John Wiley & Sons Ltd\",\"issn\":\"1502-3885\",\"doi\":\"10.1111/bor.12309\",\"abstract\":\"Travertine deposits are unique archives for multidisciplinary studies of past climate changes, associated vegetation development and the evolution of human societies. Despite their high potential in palaeoecological and palaeoclimate reconstructions, investigations of travertines are rather scarce in central Europe and particularly in Slovakia. Therefore, this study focused on a travertine deposit situated on the border between the Pannonian Basin and the Western Carpathians in a small valley in Santovka village (SW Slovakia), which is unique due to the presence of archaeological artefacts with known radiocarbon ages in the palaeoecological profile. Using a multidisciplinary approach combining macrofossil, pollen, mollusc, lithological and geochemical analyses, this study investigated climate–human–vegetation interactions. The Holocene onset was marked by the early arrival of oak trees; however, forest-steppe with a high representation of pine predominated until 9880 cal. a BP, followed by an expansion of temperate trees. The local ecosystem changed around 8600 cal. a BP when the valley was probably dammed by a travertine accumulation, probably resulting in the existence of a small travertine lake. This was associated with wetter climatic conditions, which were also documented in other sites in the Western Carpathians at that time. Surrounding temperate forest possibly retained a certain degree of openness, or local steppe habitat may have persisted on adjacent loess terraces until the neolithization of the area. Archaeological evidence represented by a ceramic shard dated to 7339 cal. a BP suggests the first appearance of humans at the site, yet pollen analysis records a significant change in vegetation first at 6650 cal. a BP. The local ecosystem records an abrupt change linked with human settlement earlier, at c. 7000 cal. a BP. Deforestation activities of the Neolithics resulted in the formation of an open calcareous fen occupied by numerous light-demanding mollusc species. The present study provides new important data about the spread of temperate trees at the onset of the Holocene, about further vegetation changes caused by activities of the first Neolithic farmers and about climate changes in the region of southwestern Slovakia.\",\"language\":\"English\",\"number\":\"3\",\"urldate\":\"2019-01-22\",\"journal\":\"Boreas\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Šolcová\"],\"firstnames\":[\"Anna\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Petr\"],\"firstnames\":[\"Libor\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Hájková\"],\"firstnames\":[\"Petra\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Petřík\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Tóth\"],\"firstnames\":[\"Peter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Rohovec\"],\"firstnames\":[\"Jan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"BáTORA\"],\"firstnames\":[\"Jozef\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Horsák\"],\"firstnames\":[\"Michal\"],\"suffixes\":[]}],\"year\":\"2018\",\"pages\":\"897–909\",\"bibtex\":\"@article{solcova_early_2018,\\n\\ttitle = {Early and middle {Holocene} ecosystem changes at the {Western} {Carpathian}/{Pannonian} border driven by climate and {Neolithic} impact},\\n\\tvolume = {47},\\n\\tcopyright = {© 2018 Collegium Boreas. Published by John Wiley \\\\& Sons Ltd},\\n\\tissn = {1502-3885},\\n\\tdoi = {10.1111/bor.12309},\\n\\tabstract = {Travertine deposits are unique archives for multidisciplinary studies of past climate changes, associated vegetation development and the evolution of human societies. Despite their high potential in palaeoecological and palaeoclimate reconstructions, investigations of travertines are rather scarce in central Europe and particularly in Slovakia. Therefore, this study focused on a travertine deposit situated on the border between the Pannonian Basin and the Western Carpathians in a small valley in Santovka village (SW Slovakia), which is unique due to the presence of archaeological artefacts with known radiocarbon ages in the palaeoecological profile. Using a multidisciplinary approach combining macrofossil, pollen, mollusc, lithological and geochemical analyses, this study investigated climate–human–vegetation interactions. The Holocene onset was marked by the early arrival of oak trees; however, forest-steppe with a high representation of pine predominated until 9880 cal. a BP, followed by an expansion of temperate trees. The local ecosystem changed around 8600 cal. a BP when the valley was probably dammed by a travertine accumulation, probably resulting in the existence of a small travertine lake. This was associated with wetter climatic conditions, which were also documented in other sites in the Western Carpathians at that time. Surrounding temperate forest possibly retained a certain degree of openness, or local steppe habitat may have persisted on adjacent loess terraces until the neolithization of the area. Archaeological evidence represented by a ceramic shard dated to 7339 cal. a BP suggests the first appearance of humans at the site, yet pollen analysis records a significant change in vegetation first at 6650 cal. a BP. The local ecosystem records an abrupt change linked with human settlement earlier, at c. 7000 cal. a BP. Deforestation activities of the Neolithics resulted in the formation of an open calcareous fen occupied by numerous light-demanding mollusc species. The present study provides new important data about the spread of temperate trees at the onset of the Holocene, about further vegetation changes caused by activities of the first Neolithic farmers and about climate changes in the region of southwestern Slovakia.},\\n\\tlanguage = {English},\\n\\tnumber = {3},\\n\\turldate = {2019-01-22},\\n\\tjournal = {Boreas},\\n\\tauthor = {Šolcová, Anna and Petr, Libor and Hájková, Petra and Petřík, Jan and Tóth, Peter and Rohovec, Jan and BáTORA, Jozef and Horsák, Michal},\\n\\tyear = {2018},\\n\\tpages = {897--909},\\n}\\n\\n\",\"author_short\":[\"Šolcová, A.\",\"Petr, L.\",\"Hájková, P.\",\"Petřík, J.\",\"Tóth, P.\",\"Rohovec, J.\",\"BáTORA, J.\",\"Horsák, M.\"],\"key\":\"solcova_early_2018\",\"id\":\"solcova_early_2018\",\"bibbaseid\":\"olcov-petr-hjkov-petk-tth-rohovec-btora-horsk-earlyandmiddleholoceneecosystemchangesatthewesterncarpathianpannonianborderdrivenbyclimateandneolithicimpact-2018\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"series\":\"The Fire-Human-Climate-Vegetation Nexus\",\"title\":\"A 1,500-year synthesis of wildfire activity stratified by elevation from the U.S. Rocky Mountains\",\"volume\":\"488\",\"issn\":\"1040-6182\",\"doi\":\"10.1016/j.quaint.2017.06.051\",\"abstract\":\"A key task in fire-climate research in the western United States is to characterize potential future fire-climate linkages across different elevational gradients. Using thirty-seven sedimentary charcoal records, here we present a 1500-year synthesis of wildfire activity across different elevational gradients to characterize fire-climate linkages. From our results, we have identified three periods of elevated fire occurrence centered on the 20th century, 900 cal yr BP, and 1350 cal yr BP. During the 20th century, fire activity has occurred primarily in the northern Rocky Mountains, with mid-elevations experiencing the greatest increase in wildfire activity. While wildfires occurred primarily in the SRM region ∼900 cal yr BP, the greatest increase in high-elevations occurred in the NRM at this time. Finally, synchronous wildfires occurred in both northern and southern Rocky Mountain mid-elevations ∼1350 cal yr BP, suggesting a potential analog for future wildfire conditions in response to warmer temperatures and more protracted droughts. We conclude that wildfire activity increased in most elevations during periods of protracted summer drought, warmer-than-average temperatures, and based on modern climate analogs, reduced atmospheric humidity.\",\"urldate\":\"2019-01-22\",\"journal\":\"Quaternary International\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Carter\"],\"firstnames\":[\"Vachel\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Power\"],\"firstnames\":[\"Mitchell\",\"J.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Lundeen\"],\"firstnames\":[\"Zachary\",\"J.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Morris\"],\"firstnames\":[\"Jesse\",\"L.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Petersen\"],\"firstnames\":[\"Kenneth\",\"L.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Brunelle\"],\"firstnames\":[\"Andrea\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Anderson\"],\"firstnames\":[\"R.\",\"Scott\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Shinker\"],\"firstnames\":[\"Jacqueline\",\"J.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Turney\"],\"firstnames\":[\"Lovina\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Koll\"],\"firstnames\":[\"Rebecca\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bartlein\"],\"firstnames\":[\"Patrick\",\"J.\"],\"suffixes\":[]}],\"month\":\"September\",\"year\":\"2018\",\"keywords\":\"Charcoal, Climate, Fire, Paleofire, Rocky Mountains\",\"pages\":\"107–119\",\"bibtex\":\"@article{carter_1500-year_2018,\\n\\tseries = {The {Fire}-{Human}-{Climate}-{Vegetation} {Nexus}},\\n\\ttitle = {A 1,500-year synthesis of wildfire activity stratified by elevation from the {U}.{S}. {Rocky} {Mountains}},\\n\\tvolume = {488},\\n\\tissn = {1040-6182},\\n\\tdoi = {10.1016/j.quaint.2017.06.051},\\n\\tabstract = {A key task in fire-climate research in the western United States is to characterize potential future fire-climate linkages across different elevational gradients. Using thirty-seven sedimentary charcoal records, here we present a 1500-year synthesis of wildfire activity across different elevational gradients to characterize fire-climate linkages. From our results, we have identified three periods of elevated fire occurrence centered on the 20th century, 900 cal yr BP, and 1350 cal yr BP. During the 20th century, fire activity has occurred primarily in the northern Rocky Mountains, with mid-elevations experiencing the greatest increase in wildfire activity. While wildfires occurred primarily in the SRM region ∼900 cal yr BP, the greatest increase in high-elevations occurred in the NRM at this time. Finally, synchronous wildfires occurred in both northern and southern Rocky Mountain mid-elevations ∼1350 cal yr BP, suggesting a potential analog for future wildfire conditions in response to warmer temperatures and more protracted droughts. We conclude that wildfire activity increased in most elevations during periods of protracted summer drought, warmer-than-average temperatures, and based on modern climate analogs, reduced atmospheric humidity.},\\n\\turldate = {2019-01-22},\\n\\tjournal = {Quaternary International},\\n\\tauthor = {Carter, Vachel A. and Power, Mitchell J. and Lundeen, Zachary J. and Morris, Jesse L. and Petersen, Kenneth L. and Brunelle, Andrea and Anderson, R. Scott and Shinker, Jacqueline J. and Turney, Lovina and Koll, Rebecca and Bartlein, Patrick J.},\\n\\tmonth = sep,\\n\\tyear = {2018},\\n\\tkeywords = {Charcoal, Climate, Fire, Paleofire, Rocky Mountains},\\n\\tpages = {107--119},\\n}\\n\\n\",\"author_short\":[\"Carter, V. A.\",\"Power, M. J.\",\"Lundeen, Z. J.\",\"Morris, J. L.\",\"Petersen, K. L.\",\"Brunelle, A.\",\"Anderson, R. S.\",\"Shinker, J. J.\",\"Turney, L.\",\"Koll, R.\",\"Bartlein, P. J.\"],\"key\":\"carter_1500-year_2018\",\"id\":\"carter_1500-year_2018\",\"bibbaseid\":\"carter-power-lundeen-morris-petersen-brunelle-anderson-shinker-etal-a1500yearsynthesisofwildfireactivitystratifiedbyelevationfromtheusrockymountains-2018\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Charcoal\",\"Climate\",\"Fire\",\"Paleofire\",\"Rocky Mountains\"],\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Drought and vegetation change in the central Rocky Mountains and western Great Plains: potential climatic mechanisms associated with megadrought conditions at 4200&thinsp;cal&thinsp;yr&thinsp;BP\",\"volume\":\"14\",\"issn\":\"1814-9324\",\"shorttitle\":\"Drought and vegetation change in the central Rocky Mountains and western Great Plains\",\"doi\":\"10.5194/cp-14-1195-2018\",\"abstract\":\"\\\\textlessp\\\\textgreater\\\\textlessstrong\\\\textgreaterAbstract.\\\\textless/strong\\\\textgreater Droughts are a naturally re-occurring phenomena that result in economic and societal losses. Yet, the most historic droughts that occurred in the 1930s and 1950s in the Great Plains and western United States were both shorter in duration and less severe than megadroughts that have plagued the region in the past. Roughly 4200 years ago, a ∼ 150-year long megadrought occurred in the central Rocky Mountains, as indicated by sedimentary pollen evidence documenting a brief and unique change in vegetation composition from Long Lake, southeastern Wyoming. Neighbouring the central Rocky Mountains, several dune fields reactivated in the western Great Plains around this time period illustrating a severe regional drought. While sedimentary pollen provides evidence of past drought, paleoecological evidence does not provide context for the climate mechanisms that may have caused the drought. Thus, a modern climate analogue technique was applied to the sedimentary pollen and regional dune reactivation evidence identified from the region to provide a conceptual framework for exploring possible mechanisms responsible for the observed ecological changes. The modern climate analogues of 2002/2012 illustrate that warm and dry conditions persisted through the growing season and were associated with anomalously higher-than-normal geopotential heights centred over the Great Plains. In the spring, higher-than-normal heights suppressed moisture transport via the low-level jet from the Gulf of Mexico creating a more southwesterly component of flow. In the summer, higher-than-normal heights persisted over the northern Great Plains resulting in a wind shift with an easterly component of flow, drawing in dry continental air into the study region. In both cases, lower-than-normal moisture in the atmosphere (via 850\\\\textlessspan class=\\\"thinspace\\\"\\\\textgreater\\\\textless/span\\\\textgreatermbar specific humidity) inhibited uplift and potential precipitation. Thus, if the present scenario existed during the 4.2\\\\textlessspan class=\\\"thinspace\\\"\\\\textgreater\\\\textless/span\\\\textgreaterka drought, the associated climatic responses are consistent with local and regional proxy data suggesting regional drought conditions in the central Rocky Mountains and western Great Plains.\\\\textless/p\\\\textgreater\",\"language\":\"English\",\"number\":\"8\",\"urldate\":\"2019-01-22\",\"journal\":\"Climate of the Past\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Carter\"],\"firstnames\":[\"Vachel\",\"A.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Shinker\"],\"firstnames\":[\"Jacqueline\",\"J.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Preece\"],\"firstnames\":[\"Jonathon\"],\"suffixes\":[]}],\"month\":\"August\",\"year\":\"2018\",\"pages\":\"1195–1212\",\"bibtex\":\"@article{carter_drought_2018,\\n\\ttitle = {Drought and vegetation change in the central {Rocky} {Mountains} and western {Great} {Plains}: potential climatic mechanisms associated with megadrought conditions at 4200\\\\&thinsp;cal\\\\&thinsp;yr\\\\&thinsp;{BP}},\\n\\tvolume = {14},\\n\\tissn = {1814-9324},\\n\\tshorttitle = {Drought and vegetation change in the central {Rocky} {Mountains} and western {Great} {Plains}},\\n\\tdoi = {10.5194/cp-14-1195-2018},\\n\\tabstract = {{\\\\textless}p{\\\\textgreater}{\\\\textless}strong{\\\\textgreater}Abstract.{\\\\textless}/strong{\\\\textgreater} Droughts are a naturally re-occurring phenomena that result in economic and societal losses. Yet, the most historic droughts that occurred in the 1930s and 1950s in the Great Plains and western United States were both shorter in duration and less severe than megadroughts that have plagued the region in the past. Roughly 4200 years ago, a ∼ 150-year long megadrought occurred in the central Rocky Mountains, as indicated by sedimentary pollen evidence documenting a brief and unique change in vegetation composition from Long Lake, southeastern Wyoming. Neighbouring the central Rocky Mountains, several dune fields reactivated in the western Great Plains around this time period illustrating a severe regional drought. While sedimentary pollen provides evidence of past drought, paleoecological evidence does not provide context for the climate mechanisms that may have caused the drought. Thus, a modern climate analogue technique was applied to the sedimentary pollen and regional dune reactivation evidence identified from the region to provide a conceptual framework for exploring possible mechanisms responsible for the observed ecological changes. The modern climate analogues of 2002/2012 illustrate that warm and dry conditions persisted through the growing season and were associated with anomalously higher-than-normal geopotential heights centred over the Great Plains. In the spring, higher-than-normal heights suppressed moisture transport via the low-level jet from the Gulf of Mexico creating a more southwesterly component of flow. In the summer, higher-than-normal heights persisted over the northern Great Plains resulting in a wind shift with an easterly component of flow, drawing in dry continental air into the study region. In both cases, lower-than-normal moisture in the atmosphere (via 850{\\\\textless}span class=\\\"thinspace\\\"{\\\\textgreater}{\\\\textless}/span{\\\\textgreater}mbar specific humidity) inhibited uplift and potential precipitation. Thus, if the present scenario existed during the 4.2{\\\\textless}span class=\\\"thinspace\\\"{\\\\textgreater}{\\\\textless}/span{\\\\textgreater}ka drought, the associated climatic responses are consistent with local and regional proxy data suggesting regional drought conditions in the central Rocky Mountains and western Great Plains.{\\\\textless}/p{\\\\textgreater}},\\n\\tlanguage = {English},\\n\\tnumber = {8},\\n\\turldate = {2019-01-22},\\n\\tjournal = {Climate of the Past},\\n\\tauthor = {Carter, Vachel A. and Shinker, Jacqueline J. and Preece, Jonathon},\\n\\tmonth = aug,\\n\\tyear = {2018},\\n\\tpages = {1195--1212},\\n}\\n\\n\",\"author_short\":[\"Carter, V. A.\",\"Shinker, J. J.\",\"Preece, J.\"],\"key\":\"carter_drought_2018\",\"id\":\"carter_drought_2018\",\"bibbaseid\":\"carter-shinker-preece-droughtandvegetationchangeinthecentralrockymountainsandwesterngreatplainspotentialclimaticmechanismsassociatedwithmegadroughtconditionsat4200thinspcalthinspyrthinspbp-2018\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{}},\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"New Radiocarbon Data for the North Bohemian Mesolithic\",\"volume\":\"2\",\"copyright\":\"All rights reserved\",\"url\":\"http://www.iansa.eu/papers/IANSA-2011-02-sida.pdf\",\"language\":\"English\",\"number\":\"2\",\"journal\":\"Interdisciplinaria Archaeologica\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Šída\"],\"firstnames\":[\"P.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Prostředník\"],\"firstnames\":[\"J.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"P.\"],\"suffixes\":[]}],\"year\":\"2011\",\"keywords\":\"Czech Republic, Mesolithic, archeology, pre-Neolithic, radiocarbon AMS dating\",\"pages\":\"151–157\",\"bibtex\":\"@article{sida_new_2011,\\n\\ttitle = {New {Radiocarbon} {Data} for the {North} {Bohemian} {Mesolithic}},\\n\\tvolume = {2},\\n\\tcopyright = {All rights reserved},\\n\\turl = {http://www.iansa.eu/papers/IANSA-2011-02-sida.pdf},\\n\\tlanguage = {English},\\n\\tnumber = {2},\\n\\tjournal = {Interdisciplinaria Archaeologica},\\n\\tauthor = {Šída, P. and Prostředník, J. and Kuneš, P.},\\n\\tyear = {2011},\\n\\tkeywords = {Czech Republic, Mesolithic, archeology, pre-Neolithic, radiocarbon AMS dating},\\n\\tpages = {151--157},\\n}\\n\\n\",\"author_short\":[\"Šída, P.\",\"Prostředník, J.\",\"Kuneš, P.\"],\"key\":\"sida_new_2011\",\"id\":\"sida_new_2011\",\"bibbaseid\":\"da-prostednk-kune-newradiocarbondataforthenorthbohemianmesolithic-2011\",\"role\":\"author\",\"urls\":{\"Paper\":\"http://www.iansa.eu/papers/IANSA-2011-02-sida.pdf\"},\"keyword\":[\"Czech Republic\",\"Mesolithic\",\"archeology\",\"pre-Neolithic\",\"radiocarbon AMS dating\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Palaeoenvironmental research of the Schwarzenberg Lake, southern Bohemia, and exploratory excavations of this key Mesolithic archaeological area\",\"volume\":\"101\",\"copyright\":\"All rights reserved\",\"language\":\"English\",\"journal\":\"Památky archeologické\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Pokorný\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Šída\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chvojka\"],\"firstnames\":[\"Ondřej\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Žáčková\"],\"firstnames\":[\"Pavla\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Světlík\"],\"firstnames\":[\"Ivo\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Veselý\"],\"firstnames\":[\"Josef\"],\"suffixes\":[]}],\"year\":\"2010\",\"keywords\":\"Czech Republic, Mesolithic, Plant macroremains, archeology, pollen analysis, pre-Neolithic\",\"pages\":\"5–38\",\"bibtex\":\"@article{pokorny_palaeoenvironmental_2010,\\n\\ttitle = {Palaeoenvironmental research of the {Schwarzenberg} {Lake}, southern {Bohemia}, and exploratory excavations of this key {Mesolithic} archaeological area},\\n\\tvolume = {101},\\n\\tcopyright = {All rights reserved},\\n\\tlanguage = {English},\\n\\tjournal = {Památky archeologické},\\n\\tauthor = {Pokorný, Petr and Šída, Petr and Chvojka, Ondřej and Žáčková, Pavla and Kuneš, Petr and Světlík, Ivo and Veselý, Josef},\\n\\tyear = {2010},\\n\\tkeywords = {Czech Republic, Mesolithic, Plant macroremains, archeology, pollen analysis, pre-Neolithic},\\n\\tpages = {5--38},\\n}\\n\\n\",\"author_short\":[\"Pokorný, P.\",\"Šída, P.\",\"Chvojka, O.\",\"Žáčková, P.\",\"Kuneš, P.\",\"Světlík, I.\",\"Veselý, J.\"],\"key\":\"pokorny_palaeoenvironmental_2010\",\"id\":\"pokorny_palaeoenvironmental_2010\",\"bibbaseid\":\"pokorn-da-chvojka-kov-kune-svtlk-vesel-palaeoenvironmentalresearchoftheschwarzenberglakesouthernbohemiaandexploratoryexcavationsofthiskeymesolithicarchaeologicalarea-2010\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Czech Republic\",\"Mesolithic\",\"Plant macroremains\",\"archeology\",\"pollen analysis\",\"pre-Neolithic\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Dřevěné artefakty raně holocenního stáří z litorálu zaniklého jezera Švarcenberk [Early Holocene wooden artifacts from the Lake Švarcenberk]\",\"volume\":\"48\",\"copyright\":\"All rights reserved\",\"language\":\"Czech\",\"journal\":\"Přehled výzkumů\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Šída\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pokorný\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"year\":\"2007\",\"note\":\"In Czech\",\"keywords\":\"Holocene, Mesolithic, archeology, pre-Neolithic\",\"pages\":\"55–64\",\"bibtex\":\"@article{sida_drevene_2007,\\n\\ttitle = {Dřevěné artefakty raně holocenního stáří z litorálu zaniklého jezera Švarcenberk [{Early} {Holocene} wooden artifacts from the {Lake} Švarcenberk]},\\n\\tvolume = {48},\\n\\tcopyright = {All rights reserved},\\n\\tlanguage = {Czech},\\n\\tjournal = {Přehled výzkumů},\\n\\tauthor = {Šída, Petr and Pokorný, Petr and Kuneš, Petr},\\n\\tyear = {2007},\\n\\tnote = {In Czech},\\n\\tkeywords = {Holocene, Mesolithic, archeology, pre-Neolithic},\\n\\tpages = {55--64},\\n}\\n\\n\",\"author_short\":[\"Šída, P.\",\"Pokorný, P.\",\"Kuneš, P.\"],\"key\":\"sida_drevene_2007\",\"id\":\"sida_drevene_2007\",\"bibbaseid\":\"da-pokorn-kune-devnartefaktyranholocennhostzlitorluzaniklhojezeravarcenberkearlyholocenewoodenartifactsfromthelakevarcenberk-2007\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Holocene\",\"Mesolithic\",\"archeology\",\"pre-Neolithic\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Interpretation of the last-glacial vegetation of eastern-central Europe using modern analogues from southern Siberia\",\"volume\":\"35\",\"copyright\":\"All rights reserved\",\"issn\":\"1365-2699\",\"doi\":\"10.1111/j.1365-2699.2008.01974.x\",\"language\":\"English\",\"number\":\"12\",\"journal\":\"Journal of Biogeography\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pelánková\"],\"firstnames\":[\"Barbora\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chytrý\"],\"firstnames\":[\"Milan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jankovská\"],\"firstnames\":[\"Vlasta\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pokorný\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Petr\"],\"firstnames\":[\"Libor\"],\"suffixes\":[]}],\"year\":\"2008\",\"note\":\"[IF2007=3.539]\",\"keywords\":\"Central Europe, Late Glacial, Pollen, Siberia, Surface sample, glacial, modern analogue, pre-Neolithic, steppe\",\"pages\":\"2223–2236\",\"bibtex\":\"@article{kunes_interpretation_2008,\\n\\ttitle = {Interpretation of the last-glacial vegetation of eastern-central {Europe} using modern analogues from southern {Siberia}},\\n\\tvolume = {35},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {1365-2699},\\n\\tdoi = {10.1111/j.1365-2699.2008.01974.x},\\n\\tlanguage = {English},\\n\\tnumber = {12},\\n\\tjournal = {Journal of Biogeography},\\n\\tauthor = {Kuneš, Petr and Pelánková, Barbora and Chytrý, Milan and Jankovská, Vlasta and Pokorný, Petr and Petr, Libor},\\n\\tyear = {2008},\\n\\tnote = {[IF2007=3.539]},\\n\\tkeywords = {Central Europe, Late Glacial, Pollen, Siberia, Surface sample, glacial, modern analogue, pre-Neolithic, steppe},\\n\\tpages = {2223--2236},\\n}\\n\\n\",\"author_short\":[\"Kuneš, P.\",\"Pelánková, B.\",\"Chytrý, M.\",\"Jankovská, V.\",\"Pokorný, P.\",\"Petr, L.\"],\"key\":\"kunes_interpretation_2008\",\"id\":\"kunes_interpretation_2008\",\"bibbaseid\":\"kune-pelnkov-chytr-jankovsk-pokorn-petr-interpretationofthelastglacialvegetationofeasterncentraleuropeusingmodernanaloguesfromsouthernsiberia-2008\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Central Europe\",\"Late Glacial\",\"Pollen\",\"Siberia\",\"Surface sample\",\"glacial\",\"modern analogue\",\"pre-Neolithic\",\"steppe\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":2,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Detection of the impact of early Holocene hunter-gatherers on vegetation in the Czech Republic, using multivariate analysis of pollen data\",\"volume\":\"17\",\"copyright\":\"All rights reserved\",\"issn\":\"0939-6314, 1617-6278\",\"doi\":\"10.1007/s00334-007-0119-5\",\"abstract\":\"Pollen data from the Czech Republic was used to detect the early Holocene impact of hunter-gatherers on vegetation based on a selection of 19 early Holocene pollen profiles, complemented with archaeological information regarding the intensity of local and regional Mesolithic human habitation. Archaeological evidence was assigned to simple categories reflecting the intensity of habitation and distance from pollen sites. Multivariate methods (PCA and RDA) were used to determine relationships between sites and possible anthropogenic pollen indicators and to test how these indicators relate to the archaeological evidence. In several profiles the pollen signal was influenced by local Mesolithic settlement. Specific pollen types (e.g. Calluna vulgaris, Plantago lanceolata, Solanum and Pteridium aquilinum) were found to be significantly correlated with human activity. The role of settlement proximity to the investigation site, the statistical significance of pollen indicators of human activity, as well as the early occurrence of Corylus avellana and its possible anthropogenic dispersal, are discussed.\",\"language\":\"English\",\"number\":\"3\",\"journal\":\"Vegetation History and Archaeobotany\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Pokorný\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Šída\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]}],\"month\":\"May\",\"year\":\"2008\",\"note\":\"[IF2007=1.076]\",\"keywords\":\"Database, Mesolithic, Multivariate analysis, Pollen, archeology, climate change, human impact, pre-Neolithic\",\"pages\":\"269–287\",\"bibtex\":\"@article{kunes_detection_2008,\\n\\ttitle = {Detection of the impact of early {Holocene} hunter-gatherers on vegetation in the {Czech} {Republic}, using multivariate analysis of pollen data},\\n\\tvolume = {17},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {0939-6314, 1617-6278},\\n\\tdoi = {10.1007/s00334-007-0119-5},\\n\\tabstract = {Pollen data from the Czech Republic was used to detect the early Holocene impact of hunter-gatherers on vegetation based on a selection of 19 early Holocene pollen profiles, complemented with archaeological information regarding the intensity of local and regional Mesolithic human habitation. Archaeological evidence was assigned to simple categories reflecting the intensity of habitation and distance from pollen sites. Multivariate methods (PCA and RDA) were used to determine relationships between sites and possible anthropogenic pollen indicators and to test how these indicators relate to the archaeological evidence. In several profiles the pollen signal was influenced by local Mesolithic settlement. Specific pollen types (e.g. Calluna vulgaris, Plantago lanceolata, Solanum and Pteridium aquilinum) were found to be significantly correlated with human activity. The role of settlement proximity to the investigation site, the statistical significance of pollen indicators of human activity, as well as the early occurrence of Corylus avellana and its possible anthropogenic dispersal, are discussed.},\\n\\tlanguage = {English},\\n\\tnumber = {3},\\n\\tjournal = {Vegetation History and Archaeobotany},\\n\\tauthor = {Kuneš, Petr and Pokorný, Petr and Šída, Petr},\\n\\tmonth = may,\\n\\tyear = {2008},\\n\\tnote = {[IF2007=1.076]},\\n\\tkeywords = {Database, Mesolithic, Multivariate analysis, Pollen, archeology, climate change, human impact, pre-Neolithic},\\n\\tpages = {269--287},\\n}\\n\\n\",\"author_short\":[\"Kuneš, P.\",\"Pokorný, P.\",\"Šída, P.\"],\"key\":\"kunes_detection_2008\",\"id\":\"kunes_detection_2008\",\"bibbaseid\":\"kune-pokorn-da-detectionoftheimpactofearlyholocenehuntergatherersonvegetationintheczechrepublicusingmultivariateanalysisofpollendata-2008\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Database\",\"Mesolithic\",\"Multivariate analysis\",\"Pollen\",\"archeology\",\"climate change\",\"human impact\",\"pre-Neolithic\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"The relationship of modern pollen spectra to vegetation and climate along a steppe-forest-tundra transition in southern Siberia, explored by decision trees\",\"volume\":\"18\",\"copyright\":\"All rights reserved\",\"doi\":\"10.1177/0959683608096600\",\"language\":\"English\",\"number\":\"8\",\"journal\":\"The Holocene\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Pelánková\"],\"firstnames\":[\"Barbora\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Jankovská\"],\"firstnames\":[\"Vlasta\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Chytrý\"],\"firstnames\":[\"Milan\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Ermakov\"],\"firstnames\":[\"Nikolai\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Svobodová-Svitavská\"],\"firstnames\":[\"Helena\"],\"suffixes\":[]}],\"year\":\"2008\",\"note\":\"[IF2007=2.343]\",\"keywords\":\"Pollen, Siberia, Surface sample, modern analogue, pre-Neolithic\",\"pages\":\"1259–1271\",\"bibtex\":\"@article{pelankova_relationship_2008,\\n\\ttitle = {The relationship of modern pollen spectra to vegetation and climate along a steppe-forest-tundra transition in southern {Siberia}, explored by decision trees},\\n\\tvolume = {18},\\n\\tcopyright = {All rights reserved},\\n\\tdoi = {10.1177/0959683608096600},\\n\\tlanguage = {English},\\n\\tnumber = {8},\\n\\tjournal = {The Holocene},\\n\\tauthor = {Pelánková, Barbora and Kuneš, Petr and Jankovská, Vlasta and Chytrý, Milan and Ermakov, Nikolai and Svobodová-Svitavská, Helena},\\n\\tyear = {2008},\\n\\tnote = {[IF2007=2.343]},\\n\\tkeywords = {Pollen, Siberia, Surface sample, modern analogue, pre-Neolithic},\\n\\tpages = {1259--1271},\\n}\\n\\n\",\"author_short\":[\"Pelánková, B.\",\"Kuneš, P.\",\"Jankovská, V.\",\"Chytrý, M.\",\"Ermakov, N.\",\"Svobodová-Svitavská, H.\"],\"key\":\"pelankova_relationship_2008\",\"id\":\"pelankova_relationship_2008\",\"bibbaseid\":\"pelnkov-kune-jankovsk-chytr-ermakov-svobodovsvitavsk-therelationshipofmodernpollenspectratovegetationandclimatealongasteppeforesttundratransitioninsouthernsiberiaexploredbydecisiontrees-2008\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Pollen\",\"Siberia\",\"Surface sample\",\"modern analogue\",\"pre-Neolithic\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":1,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Towards mapping the late Quaternary vegetation change of Europe\",\"volume\":\"23\",\"copyright\":\"All rights reserved\",\"issn\":\"0939-6314, 1617-6278\",\"doi\":\"10.1007/s00334-012-0390-y\",\"abstract\":\"The number of well-dated pollen diagrams in Europe has increased considerably over the last 30 years and many of them have been submitted to the European Pollen Database (EPD). This allows for the construction of increasingly precise maps of Holocene vegetation change across the continent. Chronological information in the EPD has been expressed in uncalibrated radiocarbon years, and most chronologies to date are based on this time scale. Here we present new chronologies for most of the datasets stored in the EPD based on calibrated radiocarbon years. Age information associated with pollen diagrams is often derived from the pollen stratigraphy itself or from other sedimentological information. We reviewed these chronological tie points and assigned uncertainties to them. The steps taken to generate the new chronologies are described and the rationale for a new classification system for age uncertainties is introduced. The resulting chronologies are fit for most continental-scale questions. They may not provide the best age model for particular sites, but may be viewed as general purpose chronologies. Taxonomic particularities of the data stored in the EPD are explained. An example is given of how the database can be queried to select samples with appropriate age control as well as the suitable taxonomic level to answer a specific research question.\",\"language\":\"English\",\"number\":\"1\",\"urldate\":\"2014-01-08\",\"journal\":\"Vegetation History and Archaeobotany\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Giesecke\"],\"firstnames\":[\"Thomas\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Davis\"],\"firstnames\":[\"Basil\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Brewer\"],\"firstnames\":[\"Simon\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Finsinger\"],\"firstnames\":[\"Walter\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Wolters\"],\"firstnames\":[\"Steffen\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Blaauw\"],\"firstnames\":[\"Maarten\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Beaulieu\"],\"firstnames\":[\"Jacques-Louis\",\"de\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Binney\"],\"firstnames\":[\"Heather\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Fyfe\"],\"firstnames\":[\"Ralph\",\"M.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Gaillard\"],\"firstnames\":[\"Marie-José\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Gil-Romera\"],\"firstnames\":[\"Graciela\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Knaap\"],\"firstnames\":[\"W.\",\"O.\",\"van\",\"der\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kühl\"],\"firstnames\":[\"Norbert\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Leeuwen\"],\"firstnames\":[\"Jacqueline\",\"F.\",\"N.\",\"van\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Leydet\"],\"firstnames\":[\"Michelle\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Lotter\"],\"firstnames\":[\"André\",\"F.\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Ortu\"],\"firstnames\":[\"Elena\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Semmler\"],\"firstnames\":[\"Malte\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Bradshaw\"],\"firstnames\":[\"Richard\",\"H.\",\"W.\"],\"suffixes\":[]}],\"month\":\"January\",\"year\":\"2014\",\"note\":\"[IF2013=2.061]\",\"keywords\":\"Age-depth relationships, Chronology, Database, European pollen database, climate, pollen data\",\"pages\":\"75–86\",\"bibtex\":\"@article{giesecke_towards_2014,\\n\\ttitle = {Towards mapping the late {Quaternary} vegetation change of {Europe}},\\n\\tvolume = {23},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {0939-6314, 1617-6278},\\n\\tdoi = {10.1007/s00334-012-0390-y},\\n\\tabstract = {The number of well-dated pollen diagrams in Europe has increased considerably over the last 30 years and many of them have been submitted to the European Pollen Database (EPD). This allows for the construction of increasingly precise maps of Holocene vegetation change across the continent. Chronological information in the EPD has been expressed in uncalibrated radiocarbon years, and most chronologies to date are based on this time scale. Here we present new chronologies for most of the datasets stored in the EPD based on calibrated radiocarbon years. Age information associated with pollen diagrams is often derived from the pollen stratigraphy itself or from other sedimentological information. We reviewed these chronological tie points and assigned uncertainties to them. The steps taken to generate the new chronologies are described and the rationale for a new classification system for age uncertainties is introduced. The resulting chronologies are fit for most continental-scale questions. They may not provide the best age model for particular sites, but may be viewed as general purpose chronologies. Taxonomic particularities of the data stored in the EPD are explained. An example is given of how the database can be queried to select samples with appropriate age control as well as the suitable taxonomic level to answer a specific research question.},\\n\\tlanguage = {English},\\n\\tnumber = {1},\\n\\turldate = {2014-01-08},\\n\\tjournal = {Vegetation History and Archaeobotany},\\n\\tauthor = {Giesecke, Thomas and Davis, Basil and Brewer, Simon and Finsinger, Walter and Wolters, Steffen and Blaauw, Maarten and Beaulieu, Jacques-Louis de and Binney, Heather and Fyfe, Ralph M. and Gaillard, Marie-José and Gil-Romera, Graciela and Knaap, W. O. van der and Kuneš, Petr and Kühl, Norbert and Leeuwen, Jacqueline F. N. van and Leydet, Michelle and Lotter, André F. and Ortu, Elena and Semmler, Malte and Bradshaw, Richard H. W.},\\n\\tmonth = jan,\\n\\tyear = {2014},\\n\\tnote = {[IF2013=2.061]},\\n\\tkeywords = {Age-depth relationships, Chronology, Database, European pollen database, climate, pollen data},\\n\\tpages = {75--86},\\n}\\n\\n\",\"author_short\":[\"Giesecke, T.\",\"Davis, B.\",\"Brewer, S.\",\"Finsinger, W.\",\"Wolters, S.\",\"Blaauw, M.\",\"Beaulieu, J. d.\",\"Binney, H.\",\"Fyfe, R. M.\",\"Gaillard, M.\",\"Gil-Romera, G.\",\"Knaap, W. O. v. d.\",\"Kuneš, P.\",\"Kühl, N.\",\"Leeuwen, J. F. N. v.\",\"Leydet, M.\",\"Lotter, A. F.\",\"Ortu, E.\",\"Semmler, M.\",\"Bradshaw, R. H. W.\"],\"key\":\"giesecke_towards_2014\",\"id\":\"giesecke_towards_2014\",\"bibbaseid\":\"giesecke-davis-brewer-finsinger-wolters-blaauw-beaulieu-binney-etal-towardsmappingthelatequaternaryvegetationchangeofeurope-2014\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Age-depth relationships\",\"Chronology\",\"Database\",\"European pollen database\",\"climate\",\"pollen data\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"1. Fláje-Kiefern (Krušné Hory Mountains): Late Glacial and Holocene vegetation development\",\"volume\":\"46\",\"copyright\":\"All rights reserved\",\"issn\":\"0017-3134\",\"url\":\"http://www.informaworld.com/10.1080/00173130701526341\",\"doi\":\"10.1080/00173130701526341\",\"language\":\"English\",\"number\":\"3\",\"journal\":\"Grana\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Jankovská\"],\"firstnames\":[\"Vlasta\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[\"van\",\"der\"],\"lastnames\":[\"Knaap\"],\"firstnames\":[\"Willem\",\"O.\"],\"suffixes\":[]}],\"month\":\"November\",\"year\":\"2007\",\"note\":\"[IF2006=0.689]\",\"keywords\":\"Czech Republic, Database, Holocene, pollen analysis, vegetation history\",\"pages\":\"214–216\",\"bibtex\":\"@article{jankovska_1._2007,\\n\\ttitle = {1. {Fláje}-{Kiefern} ({Krušné} {Hory} {Mountains}): {Late} {Glacial} and {Holocene} vegetation development},\\n\\tvolume = {46},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {0017-3134},\\n\\turl = {http://www.informaworld.com/10.1080/00173130701526341},\\n\\tdoi = {10.1080/00173130701526341},\\n\\tlanguage = {English},\\n\\tnumber = {3},\\n\\tjournal = {Grana},\\n\\tauthor = {Jankovská, Vlasta and Kuneš, Petr and van der Knaap, Willem O.},\\n\\tmonth = nov,\\n\\tyear = {2007},\\n\\tnote = {[IF2006=0.689]},\\n\\tkeywords = {Czech Republic, Database, Holocene, pollen analysis, vegetation history},\\n\\tpages = {214--216},\\n}\\n\\n\",\"author_short\":[\"Jankovská, V.\",\"Kuneš, P.\",\"van der Knaap, W. O.\"],\"key\":\"jankovska_1._2007\",\"id\":\"jankovska_1._2007\",\"bibbaseid\":\"jankovsk-kune-vanderknaap-1fljekiefernkrunhorymountainslateglacialandholocenevegetationdevelopment-2007\",\"role\":\"author\",\"urls\":{\"Paper\":\"http://www.informaworld.com/10.1080/00173130701526341\"},\"keyword\":[\"Czech Republic\",\"Database\",\"Holocene\",\"pollen analysis\",\"vegetation history\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"},{\"bibtype\":\"article\",\"type\":\"article\",\"title\":\"Czech Quaternary Palynological Database – PALYCZ: review and basic statistics of the data\",\"volume\":\"81\",\"copyright\":\"All rights reserved\",\"issn\":\"0032-7786\",\"language\":\"English\",\"number\":\"3\",\"journal\":\"Preslia\",\"author\":[{\"propositions\":[],\"lastnames\":[\"Kuneš\"],\"firstnames\":[\"Petr\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Abraham\"],\"firstnames\":[\"Vojtěch\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kovářík\"],\"firstnames\":[\"Oleg\"],\"suffixes\":[]},{\"propositions\":[],\"lastnames\":[\"Kopecký\"],\"firstnames\":[\"Martin\"],\"suffixes\":[]},{\"firstnames\":[],\"propositions\":[],\"lastnames\":[\"PALYCZcontributors\"],\"suffixes\":[]}],\"year\":\"2009\",\"note\":\"[IF2008=2.396]\",\"keywords\":\"Czech Republic, Database, Holocene, Late Glacial, Pollen, Slovakia, numerical methods\",\"pages\":\"209–238\",\"bibtex\":\"@article{kunes_czech_2009,\\n\\ttitle = {Czech {Quaternary} {Palynological} {Database} – {PALYCZ}: review and basic statistics of the data},\\n\\tvolume = {81},\\n\\tcopyright = {All rights reserved},\\n\\tissn = {0032-7786},\\n\\tlanguage = {English},\\n\\tnumber = {3},\\n\\tjournal = {Preslia},\\n\\tauthor = {Kuneš, Petr and Abraham, Vojtěch and Kovářík, Oleg and Kopecký, Martin and PALYCZcontributors},\\n\\tyear = {2009},\\n\\tnote = {[IF2008=2.396]},\\n\\tkeywords = {Czech Republic, Database, Holocene, Late Glacial, Pollen, Slovakia, numerical methods},\\n\\tpages = {209--238},\\n}\\n\",\"author_short\":[\"Kuneš, P.\",\"Abraham, V.\",\"Kovářík, O.\",\"Kopecký, M.\",\"PALYCZcontributors\"],\"key\":\"kunes_czech_2009\",\"id\":\"kunes_czech_2009\",\"bibbaseid\":\"kune-abraham-kovk-kopeck-palyczcontributors-czechquaternarypalynologicaldatabasepalyczreviewandbasicstatisticsofthedata-2009\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Czech Republic\",\"Database\",\"Holocene\",\"Late Glacial\",\"Pollen\",\"Slovakia\",\"numerical methods\"],\"metadata\":{\"authorlinks\":{\"kuneš, p\":\"https://petr.kunes.net/disturbance-dynamics/\"}},\"downloads\":0,\"html\":\"\"}],\n      metadata: {\"authorlinks\":{}},\n      ownerID: undefined\n    };\n  </script>\n\n  <script type=\"text/javascript\">\n  var site$;\n  if (typeof $ != 'undefined') {\n    console.log('existing jquery: storing and then restoring');\n    site$ = $;\n    $ = null;\n  }\n  </script>\n\n  <script src=\"https://ajax.googleapis.com/ajax/libs/jquery/2.2.4/jquery.min.js\">\n  </script>\n  <script type=\"text/javascript\">\n  if (site$) {\n    console.log('existing jquery: avoiding conflict and restoring');\n    bb$ = $.noConflict(true);\n    $ = site$;\n  } else {\n    bb$ = $;\n  }\n  </script>\n\n  <script src=\"//bibbase.org/js/bibbase.min.js\"\n          type=\"text/javascript\">\n  </script>\n\n  <script type=\"text/javascript\"\n          src=\"https://cdnjs.cloudflare.com/ajax/libs/mathjax/2.7.1/MathJax.js?config=TeX-AMS-MML_HTMLorMML\">\n  </script>\n  <script type=\"text/x-mathjax-config\">\n    MathJax.Hub.Config({tex2jax: {inlineMath: [['$','$'], ['\\\\(','\\\\)']]},\n                        skipTags: [\"body\"],\n                        processClass: \"bibbase_paper\"});\n  </script>\n\n  <style>\n  @media print {\n    .dontprint {\n        display: none !important;\n    }\n\n  .bibbase_group {\n    background-color: #E0E0E0;\n    font-style: italic;\n    font-size: larger;\n    text-shadow: 0px 0px 3px #FFFFFF;\n    border-radius: 4px 4px 4px 4px;\n    -moz-border-radius: 4px 4px 4px 4px;\n    -webkit-border-radius: 4px;\n    padding: 5px 40px 5px;\n    margin-top: 10px;\n    margin-bottom: 5px;\n    cursor: pointer;\n  }\n\n  .bibbase_paper {\n    margin-bottom: 5px;\n  }\n\n  }\n  </style>\n\n  \n  <div style=\"float: right; 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	title = {Mountain aquatic \textit{{Isoëtes}} populations reflect millennial-scale environmental changes in the {Bohemian} {Forest} {Ecosystem}, {Central} {Europe}},
	volume = {31},
	issn = {0959-6836},
	doi = {10.1177/0959683620988060},
	abstract = {In this study we aim to investigate millennial-scale dynamics of Isoëtes, a type of macrophyte well adapted to oligotrophic and clear-water lakes. Despite its wide distribution during the Early Holocene, nowadays Isoëtes is considered as vulnerable or critically endangered in many Central European countries. Using a multi-proxy palaeoecological reconstruction involving Isoëtes micro- and megaspores, pollen, plant macrofossils, macro-charcoal, diatoms and chironomids from four lakes (Prášilské jezero, Plešné jezero, Černé jezero, Rachelsee) located in the Bohemian Forest Ecosystem mountain region in Central Europe, we reconstruct Isoëtes dynamics and discuss how local environmental factors impacted its distribution and abundance during the Holocene. Our results show regionally concurrent patterns of Isoëtes colonisation across all lakes beginning 10,300–9300 cal yr BP, and substantially declining around 6400 cal yr BP. Results from Prášilské jezero imply that Isoëtes decline and collapse in this lake reflect gradual dystrophication that led to the browning of lake water. This is evidenced by a shift in diatom assemblages towards more acidophilous taxa dominated by Asterionella ralfsii and by a decrease in total chironomid abundance and taxa sensitive to low oxygen levels. Dystrophication of Prášilské jezero was linked with the immigration of the late-successional tree taxa (Picea abies and later Fagus sylvatica and Abies alba), peatland expansion, and decreasing fire activity. Multi-site comparison of pollen records suggest that these vegetation-related environmental changes were common for the whole region. Our study demonstrates the sensitivity of Isoëtes to millennial-scale natural environmental changes within the surrounding lake catchment.},
	language = {English},
	number = {5},
	urldate = {2021-05-17},
	journal = {The Holocene},
	author = {Moravcová, Alice and Tichá, Anna and Carter, Vachel A and Vondrák, Daniel and Čtvrtlíková, Martina and van Leeuwen, Jacqueline FN and Heurich, Marco and Tinner, Willy and Kuneš, Petr},
	month = may,
	year = {2021},
	note = {[IF2020=2.769]},
	keywords = {disturbance, fire regime, lake dystrophy, podzolisation, quillwort decline, thermal stratification, vegetation change},
	pages = {746--759},
}



@article{kunes_new_2013,
	title = {A new {Middle} {Pleistocene} interglacial record from {Denmark}: {Chronostratigraphic} correlation, palaeovegetation and fire dynamics},
	volume = {42},
	copyright = {© 2013 The Authors. Boreas © 2013 The Boreas Collegium},
	issn = {1502-3885},
	shorttitle = {A new {Middle} {Pleistocene} interglacial record from {Denmark}},
	doi = {10.1111/bor.12002},
	abstract = {Previously only three terrestrial interglacial periods were known from southern Scandinavia, all of which could be relatively easily correlated within the central European stratigraphical framework. Here, we present a new interglacial–interstadial pollen, plant macrofossil and charcoal record from Trelde Klint, Denmark, and analyse its biostratigraphy, correlation with other European records, vegetation development, fire dynamics and absolute dating. Except for a slight truncation of the early part of the record, the pollen stratigraphy exhibits a full interglacial succession, including temperate trees (Quercus, Ulmus and Tilia) during its mesocratic stage. Macrofossil analysis allowed identification to species level for Quercus robur, Picea abies and two mosses. Conifers (Pinus and Picea) dominate the pollen record of the interglacial sequence, and the occurrence of Larix pollen in the top part of the interglacial record as well as in the interstadial sediments is especially indicative of this interglacial. The overall diversity of tree genera is rather low. These biostratigraphical features suggest that Trelde Klint is unique among Danish records, but it is similar to records from northern Germany. Numerical analyses (REVEALS and DCA) indicate that forests during the temperate stage were dense and that vegetation openness increased only towards the end of the interglacial, accompanied by increased fire occurrence. A short interstadial sequence with a dominance of Pinus and Betula and the presence of Larix is present above the interglacial deposit. We argue that lack of attention to differences in fire regimes may hamper understanding of between-site correlations of interglacial pollen records. OSL dating, using a novel feldspar technique, yields an average age of 350±20 ka for the sandy sediments above the interglacial layers at Trelde Klint, suggesting that the whole interglacial–interstadial succession belongs to Marine Isotope Stage 11.},
	language = {English},
	number = {3},
	urldate = {2013-06-23},
	journal = {Boreas},
	author = {Kuneš, Petr and Kjærsgaard Sørensen, Malene and Buylaert, Jan-Pieter and Murray, Andrew S. and Houmark-Nielsen, Michael and Odgaard, Bent Vad},
	year = {2013},
	note = {[IF2012=2.457]},
	keywords = {Denmark, OSL dating, Plant macroremains, REVEALS, charcoal, interglacial, pollen analysis},
	pages = {596--612},
}



@article{pokorny_insight_2006,
	title = {Insight into the environment of a pre-{Roman} {Iron} {Age} hillfort at {Vladař}, {Czech} {Republic}, using a multi-proxy approach},
	volume = {15},
	copyright = {All rights reserved},
	issn = {0939-6314, 1617-6278},
	doi = {10.1007/s00334-006-0064-8},
	language = {English},
	number = {4},
	urldate = {2012-01-05},
	journal = {Vegetation History and Archaeobotany},
	author = {Pokorný, Petr and Boenke, Nicole and Chytráček, Miloslav and Nováková, Kateřina and Sádlo, Jiří and Veselý, Josef and Kuneš, Petr and Jankovská, Vlasta},
	month = jul,
	year = {2006},
	note = {[IF2005=0.739]},
	keywords = {Czech Republic, Plant macroremains, archeology, cladocera, human impact, pollen analysis},
	pages = {419--433},
}



@article{rolecek_conservation_2020,
	title = {Conservation targets from the perspective of a palaeoecological reconstruction: the case study of {Dářko} peat bog in the {Czech} {Republic}},
	volume = {92},
	doi = {10.23855/preslia.2020.087},
	language = {English},
	number = {2},
	journal = {Preslia},
	author = {Roleček, Jan and Svitavská Svobodová, Helena and Jamrichová, Eva and Dudová, Lydie and Hájková, Petra and Kletetschka, Günther and Kuneš, Petr and Abraham, Vojtěch},
	year = {2020},
	note = {[IF2019=4.357]},
	keywords = {conservation},
	pages = {87--114},
}



@article{giesecke_millennial_2022,
	title = {Millennial scale perspective on biodiversity conservation of the forest-steppe ecotone in {Europe}},
	volume = {30},
	issn = {2411605X, 24119180},
	doi = {10.22498/pages.30.1.24},
	number = {1},
	urldate = {2022-04-05},
	journal = {Past Global Changes Magazine},
	author = {Giesecke, Thomas and Kuneš, Petr and Shumilovskikh, Lyudmila},
	month = apr,
	year = {2022},
	keywords = {conservation},
	pages = {24--25},
}



@article{kolar_population_2018,
	title = {Population and forest dynamics during the {Central} {European} {Eneolithic} (4500–2000 {BC})},
	volume = {10},
	copyright = {All rights reserved},
	issn = {1866-9557, 1866-9565},
	doi = {10.1007/s12520-016-0446-5},
	abstract = {The population boom-and-bust during the European Neolithic (7000–2000 BC) has been the subject of lively discussion for the past decade. Most of the research on this topic was carried out with help of summed radiocarbon probability distributions. We aim to reconstruct population dynamics within the catchment of a medium sized lake on the basis of information on the presence of all known past human activities. We calculated a human activity model based on Monte Carlo simulations. The model showed the lowest level of human activity between 4000 and 3000 BC. For a better understanding of long-term socio-environmental dynamics, we also used the results of a pollen-based quantitative vegetation model, as well as a local macrophysical climate model. The beginning of the decline of archaeologically visible human activities corresponds with climatic changes and an increase in secondary forest taxa probably indicating more extensive land use. In addition, social and technological innovations are important, such as the introduction of the ard, wheel, animal traction and metallurgy, as well as changes in social hierarchy characterizing the same period.},
	language = {English},
	number = {5},
	urldate = {2016-12-14},
	journal = {Archaeological and Anthropological Sciences},
	author = {Kolář, Jan and Kuneš, Petr and Szabó, Péter and Hajnalová, Mária and Svobodová, Helena Svitavská and Macek, Martin and Tkáč, Peter},
	month = aug,
	year = {2018},
	note = {[IF2017=2.414]},
	keywords = {Czech Republic, MCM model, Neolithic, Population density, REVEALS, climate, conservation, cultural landscape, reconstruction},
	pages = {1153--1164},
}



@article{szabo_using_2017,
	title = {Using historical ecology to reassess the conservation status of coniferous forests in {Central} {Europe}},
	volume = {31},
	copyright = {All rights reserved},
	issn = {1523-1739},
	doi = {10.1111/cobi.12763},
	abstract = {Forests cover approximately one-third of Central Europe. Oak (Quercus) and European beech (Fagus sylvatica) are considered the natural dominants at low and middle elevations, respectively. Many coniferous forests (especially of Picea abies) occur primarily at midelevations, but these are thought to have resulted from forestry plantations planted over the past 200 years. Nature conservation and forestry policy seek to promote broadleaved trees over conifers. However, there are discrepancies between conservation guidelines (included in Natura 2000) and historical and palaeoecological data with regard to the distribution of conifers. Our aim was to bring new evidence to the debate on the conservation of conifers versus broadleaved trees at midelevations in Central Europe. We created a vegetation and land-cover model based on pollen data for a highland area of 11,300 km2 in the Czech Republic and assessed tree species composition in the forests before the onset of modern forestry based on 18th-century archival sources. Conifers dominated the study region throughout the entire Holocene (approximately 40–60\% of the area). Broadleaved trees were present in a much smaller area than envisaged by current ideas of natural vegetation. Rather than casting doubt on the principles of Central European nature conservation in general, our results highlight the necessity of detailed regional investigations and the importance of historical data in challenging established notions on the natural distribution of tree species.},
	language = {English},
	number = {1},
	urldate = {2017-01-26},
	journal = {Conservation Biology},
	author = {Szabó, Péter and Kuneš, Petr and Svobodová‐Svitavská, Helena and Švarcová, Markéta Gabriela and Křížová, Lucie and Suchánková, Silvie and Müllerová, Jana and Hédl, Radim},
	month = feb,
	year = {2017},
	note = {[IF2016=4.842]},
	keywords = {Czech Republic, Historical ecology, Holocene, LRA, REVEALS, conservation, interdisciplinarity, potential natural vegetation, reconstruction},
	pages = {150--160},
}



@article{abraham_pollen-based_2016,
	title = {A pollen-based quantitative reconstruction of the {Holocene} vegetation updates a perspective on the natural vegetation in the {Czech} {Republic} and {Slovakia}},
	volume = {88},
	copyright = {All rights reserved},
	url = {http://www.preslia.cz/P164Abraham.pdf},
	language = {English},
	number = {4},
	journal = {Preslia},
	author = {Abraham, Vojtěch and Kuneš, Petr and Petr, Libor and Svitavská-Svobodová, Helena and Kozáková, Radka and Jamrichová, Eva and Švarcová, Markéta Gabriela and Pokorný, Petr},
	year = {2016},
	note = {[IF2015=2.711]},
	keywords = {Czech Republic, Database, Holocene, LRA, REVEALS, Slovakia, conservation, pollen data, potential natural vegetation, reconstruction},
	pages = {409--434},
}



@article{kunes_origin_2015,
	title = {The origin of grasslands in the temperate forest zone of east-central {Europe}: long-term legacy of climate and human impact},
	volume = {116},
	copyright = {All rights reserved},
	issn = {0277-3791},
	shorttitle = {The origin of grasslands in the temperate forest zone of east-central {Europe}},
	doi = {10.1016/j.quascirev.2015.03.014},
	abstract = {The post-glacial fate of central European grasslands has stimulated palaeoecological debates for a century. Some argued for the continuous survival of open land, while others claimed that closed forest had developed during the Middle Holocene. The reasons behind stability or changes in the proportion of open land are also unclear. We aim to reconstruct regional vegetation openness and test the effects of climate and human impact on vegetation change throughout the Holocene. We present a newly dated pollen record from north-western fringes of the Pannonian Plain, east-central Europe, and reconstruct Holocene regional vegetation development by the REVEALS model for 27 pollen-equivalent taxa. Estimated vegetation is correlated in the same area with a human activity model based on all available archaeological information and a macrophysical climate model. The palaeovegetation record indicates the continuous presence of open land throughout the Holocene. Grasslands and open woodlands were probably maintained by local arid climatic conditions during the early Holocene delaying the spread of deciduous (oak) forests. Significantly detectable human-made landscape transformation started only after 2000 BC. Our analyses suggest that Neolithic people spread into a landscape that was already open. Humans probably contributed to the spread of oak, and influenced the dynamics of hazel and hornbeam.},
	language = {English},
	urldate = {2015-04-09},
	journal = {Quaternary Science Reviews},
	author = {Kuneš, Petr and Svobodová-Svitavská, Helena and Kolář, Jan and Hajnalová, Mária and Abraham, Vojtěch and Macek, Martin and Tkáč, Peter and Szabó, Péter},
	month = may,
	year = {2015},
	note = {[IF2014=4.572]},
	keywords = {Carpathian Basin, Czech Republic, Holocene, LRA, MCM model, REVEALS, conservation, pollen analysis, quantitative vegetation reconstruction},
	pages = {15--27},
}



@article{jamrichova_early_2014,
	title = {Early occurrence of temperate oak-dominated forest in the northern part of the {Little} {Hungarian} {Plain}, {SW} {Slovakia}},
	volume = {24},
	copyright = {All rights reserved},
	issn = {0959-6836, 1477-0911},
	doi = {10.1177/0959683614551225},
	abstract = {Using a multi-proxy analysis of a postglacial sedimentary sequence from a lowland wetland, we address the possible drivers of change in the wetland habitats and surrounding landscapes of southwestern Slovakia. A 5 m-deep core in the Parížske močiare marshes was investigated for pollen, plant macro-remains, molluscs, organic content and magnetic susceptibility. The palaeoecological record extends from the Pleistocene–Holocene transition (≥11,200 cal. BP) to the 5th millennium cal. BP and was correlated with a macrophysical climate model (MCM) and archaeological data. Our results show the transformation of an open parkland landscape with patches of coniferous forest to a temperate deciduous forest at the onset of the Holocene. The record is remarkable for an early occurrence of Quercus pollen and macro-remains around 11,200 cal. BP and its early expansion (10,390 cal. BP) in the vegetation. Such an early spread of Quercus has not previously been recorded in the region, where Corylus is usually the first to expand among temperate trees. This unusual development of forest communities was most probably triggered by a short-lived increase in precipitation and decrease in temperature, as reconstructed by the MCM model. Higher moisture availability and low temperature inhibited Corylus and favoured the spread of Quercus. Later, the climate became drier and warmer, which, together with fires, supported the expansion of Corylus. Since 7300 cal. BP, human activities became most likely the dominant influence on the landscape. Deforestation contributed to soil erosion, which halted the accumulation of organic material after 5520 cal. BP, followed by the accumulation of clay sediments.},
	language = {English},
	number = {12},
	urldate = {2014-12-10},
	journal = {The Holocene},
	author = {Jamrichová, Eva and Potůčková, Anna and Horsák, Michal and Hajnalová, Mária and Barta, Peter and Tóth, Peter and Kuneš, Petr},
	month = dec,
	year = {2014},
	note = {[IF2013=3.794]},
	keywords = {Lowland vegetation, MCM model, Palaeoecology, Plant macroremains, Slovakia, climate, conservation, cultural landscape, human impact, multi-proxy, pollen analysis},
	pages = {1810--1824},
}



@article{jamrichova_continuity_2013,
	title = {Continuity and change in the vegetation of a {Central} {European} oakwood},
	volume = {23},
	copyright = {All rights reserved},
	issn = {0959-6836, 1477-0911},
	doi = {10.1177/0959683612450200},
	abstract = {The issue of continuity in deciduous oakwood vegetation has been in the forefront of woodland ecological studies for many decades. The two basic questions that emerge from existing research are whether or not oakwoods can be characterized by long-term stability and what may be the driving forces of the observed stability or change. To answer these questions in a well-defined case study, we examined the history of a large subcontinental oakwood (Dúbrava) in the southeastern Czech Republic with interdisciplinary methods using palaeoecological and archival sources. Palaeoecology allowed us to reconstruct the vegetation composition and fire disturbances in Dúbrava in the past 2000 years, while written sources provided information about tree composition and management from the 14th century onwards. The pollen profiles show that the present oakwood was established in the mid-14th century with an abrupt change from shrubby, hazel-dominated vegetation to oak forest. This change was most probably caused by a ban on oak felling in ad 1350. From the 14th to the late 18th centuries Dúbrava had multiple uses, of which wood-pasture and hay-cutting kept the forest considerably open. The second remarkable change was dated to the late 18th century, when multiple-use management was abandoned and Dúbrava was divided into pasture-only and coppice-only parts. The last major shift occurred in the mid-19th century, when modern forestry and Scotch pine plantation became dominant. We conclude that Dúbrava Wood did not show stability in the long run and that its species composition has dramatically changed during the last two millennia. The most important driving force in the shaping and maintenance of the unique vegetation of Dúbrava was human management.},
	language = {English},
	number = {1},
	urldate = {2012-12-20},
	journal = {The Holocene},
	author = {Jamrichová, Eva and Szabó, Péter and Hédl, Radim and Kuneš, Petr and Bobek, Přemysl and Pelánková, Barbora},
	month = jan,
	year = {2013},
	note = {[IF2012=3.218]},
	keywords = {Historical ecology, conservation, ecosystem stability, management history, pollen analysis, temperate oakwood},
	pages = {46--56},
}



@article{kunes_dosavadni_2022,
	title = {Dosavadní výsledky paleoekologických výzkumů v {Ašském} výběžku – podklady pro ochranu přírody},
	volume = {30},
	issn = {1803-6066},
	language = {Czech},
	journal = {Sborník muzea Karlovarského kraje},
	author = {Kuneš, Petr and Bobek, Přemysl and Svobodová-Svitavská, Helena and Švarcová, Markéta G and Šulc, Václav and Šturma, Jan Albert and Smrtová, Erika},
	year = {2022},
	pages = {131--150},
}



@article{githumbi_european_2022,
	title = {European pollen-based {REVEALS} land-cover reconstructions for the {Holocene}: methodology, mapping and potentials},
	volume = {14},
	issn = {1866-3508},
	shorttitle = {European pollen-based {REVEALS} land-cover reconstructions for the {Holocene}},
	doi = {10.5194/essd-14-1581-2022},
	abstract = {{\textless}p{\textgreater}{\textless}strong class="journal-contentHeaderColor"{\textgreater}Abstract.{\textless}/strong{\textgreater} Quantitative reconstructions of past land cover are necessary to determine the processes involved in climate–human–land-cover interactions. We present the first temporally continuous and most spatially extensive pollen-based land-cover reconstruction for Europe over the Holocene (last 11 700 cal yr BP). We describe how vegetation cover has been quantified from pollen records at a 1{\textless}span class="inline-formula"{\textgreater}$^{\textrm{∘}}${\textless}/span{\textgreater} {\textless}span class="inline-formula"{\textgreater}×{\textless}/span{\textgreater} 1{\textless}span class="inline-formula"{\textgreater}$^{\textrm{∘}}${\textless}/span{\textgreater} spatial scale using the “Regional Estimates of VEgetation Abundance from Large Sites” (REVEALS) model. REVEALS calculates estimates of past regional vegetation cover in proportions or percentages. REVEALS has been applied to 1128 pollen records across Europe and part of the eastern Mediterranean–Black Sea–Caspian corridor (30–75{\textless}span class="inline-formula"{\textgreater}$^{\textrm{∘}}${\textless}/span{\textgreater} N, 25{\textless}span class="inline-formula"{\textgreater}$^{\textrm{∘}}${\textless}/span{\textgreater} W–50{\textless}span class="inline-formula"{\textgreater}$^{\textrm{∘}}${\textless}/span{\textgreater} E) to reconstruct the percentage cover of 31 plant taxa assigned to 12 plant functional types (PFTs) and 3 land-cover types (LCTs). A new synthesis of relative pollen productivities (RPPs) for European plant taxa was performed for this reconstruction. It includes multiple RPP values ({\textless}span class="inline-formula"{\textgreater}≥2{\textless}/span{\textgreater} values) for 39 taxa and single values for 15 taxa (total of 54 taxa). To illustrate this, we present distribution maps for five taxa (\textit{Calluna vulgaris}, Cerealia type (t)., \textit{Picea abies}, deciduous \textit{Quercus} t. and evergreen \textit{Quercus} t.) and three land-cover types (open land, OL; evergreen trees, ETs; and summer-green trees, STs) for eight selected time windows. The reliability of the REVEALS reconstructions and issues related to the interpretation of the results in terms of landscape openness and human-induced vegetation change are discussed. This is followed by a review of the current use of this reconstruction and its future potential utility and development. REVEALS data quality are primarily determined by pollen count data (pollen count and sample, pollen identification, and chronology) and site type and number (lake or bog, large or small, one site vs. multiple sites) used for REVEALS analysis (for each grid cell). A large number of sites with high-quality pollen count data will produce more reliable land-cover estimates with lower standard errors compared to a low number of sites with lower-quality pollen count data. The REVEALS data presented here can be downloaded from {\textless}a href="https://doi.org/10.1594/PANGAEA.937075"{\textgreater}https://doi.org/10.1594/PANGAEA.937075{\textless}/a{\textgreater} (Fyfe et al., 2022).{\textless}/p{\textgreater}},
	language = {English},
	number = {4},
	urldate = {2022-04-19},
	journal = {Earth System Science Data},
	author = {Githumbi, Esther and Fyfe, Ralph and Gaillard, Marie-Jose and Trondman, Anna-Kari and Mazier, Florence and Nielsen, Anne-Birgitte and Poska, Anneli and Sugita, Shinya and Woodbridge, Jessie and Azuara, Julien and Feurdean, Angelica and Grindean, Roxana and Lebreton, Vincent and Marquer, Laurent and Nebout-Combourieu, Nathalie and Stančikaitė, Miglė and Tanţău, Ioan and Tonkov, Spassimir and Shumilovskikh, Lyudmila and LandClimII data contributors},
	month = apr,
	year = {2022},
	note = {[IF2021=11.815; AIS2021=4.141]},
	keywords = {reconstruction},
	pages = {1581--1619},
}



@article{schafstall_sub-fossil_2022,
	title = {Sub-fossil bark beetles as indicators of past disturbance events in temperate {Picea} abies mountain forests},
	volume = {275},
	issn = {0277-3791},
	doi = {10.1016/j.quascirev.2021.107289},
	abstract = {Temperate mountain forests have experienced an increase in frequency and severity of natural disturbances (e.g., droughts, fires, windstorms and insect outbreaks) in recent decades due to climate and environmental change. Outbreaks of bark beetles have caused significant dieback of conifer forests in Central Europe and it is essential to model and predict the potential severity of future bark beetle outbreaks. However, to predict future bark beetle activity, historical baseline information is required to contextualize the magnitude of current and potential future outbreaks. A fossil beetle record from a forest hollow in the Tatra Mountains, Slovakia; one of the best-preserved national parks in Central Europe, was produced to identify insect outbreaks during the last millennia. Sub-fossil bark beetle remains were compared with parallel pollen and charcoal to assess whether peaks in conifer bark beetle remains correspond with indications of disturbance documented in historical or sedimentary fossil records. Three peaks in bark beetle remains were detected (1) post-2004, (2) AD 1140–1440, and (3) AD 930–1030. The abundance of species Pityogenes chalcographus and Pityophthorus pityographus in the two top samples can be linked directly to large bark beetle outbreaks in the High Tatra Mountains after 2004. P. chalcographus and P. pityographus are also the abundant species in the second peak (AD 1140–1440) while the third peak (AD 930–1030) consists of the species Polygraphus poligraphus. The most prominent conifer bark beetle in Central Europe, Ips typographus, was found to be present in most of the samples but always at very low numbers. It is plausible that P. chalcographus and P. pityographus fossils might be useful proxies for past conifer bark beetle outbreaks in Central Europe, as they occur together with fossils of I. typographus but appear to be well-preserved. A significant correlation was found between primary bark beetles and macroscopic charcoal densities in the sediment, highlighting the complex interactions between disturbance agents, bark beetles and fire, in this long-term regime of natural disturbances. Our 1400-year disturbance record shows how bark beetle outbreaks have been an important component of the regional natural disturbance regime for over a millennium and have intensified with increasing anthropogenic activity. Bark beetle outbreaks are likely one of the drivers promoting the future ecological stability of the temperate conifer ecosystem over decades to centuries.},
	language = {English},
	urldate = {2021-11-29},
	journal = {Quaternary Science Reviews},
	author = {Schafstall, Nick and Kuosmanen, Niina and Kuneš, Petr and Svobodová, Helena Svitavská and Svitok, Marek and Chiverrell, Richard C. and Halsall, Karen and Fleischer, Peter and Knížek, Miloš and Clear, Jennifer L.},
	month = jan,
	year = {2022},
	note = {[IF2021=4.456;AIS2021=1.586]},
	keywords = {Bark beetle outbreaks, Central Europe, Disturbance history, Ecosystem services, Fire, Fossil proxies, High Tatra mountains, disturbance},
	pages = {107289},
}



@article{mariani_disruption_2022,
	title = {Disruption of cultural burning promotes shrub encroachment and unprecedented wildfires},
	volume = {20},
	issn = {1540-9309},
	doi = {10.1002/fee.2395},
	abstract = {Recent catastrophic fires in Australia and North America have raised broad-scale questions about how the cessation of Indigenous burning practices has impacted fuel accumulation and structure. For sustainable coexistence with fire, a better understanding of the ancient nexus between humans and flammable landscapes is needed. We used novel palaeoecological modeling and charcoal compilations to reassess evidence for changes in land cover and fire activity, focusing on southeast Australia before and after British colonization. Here, we provide what we believe is the first quantitative evidence that the region’s forests and woodlands contained fewer shrubs and more grass before colonization. Changes in vegetation, fuel structures, and connectivity followed different trajectories in different vegetation types. The pattern is best explained by the disruption of Indigenous vegetation management caused by European settlement. Combined with climate-change impacts on fire weather and drought, the widespread absence of Indigenous fire management practices likely preconditioned fire-prone regions for wildfires of unprecedented extent.},
	language = {English},
	number = {5},
	urldate = {2022-06-22},
	journal = {Frontiers in Ecology and the Environment},
	author = {Mariani, Michela and Connor, Simon E and Theuerkauf, Martin and Herbert, Annika and Kuneš, Petr and Bowman, David and Fletcher, Michael-Shawn and Head, Lesley and Kershaw, A Peter and Haberle, Simon G and Stevenson, Janelle and Adeleye, Matthew and Cadd, Haidee and Hopf, Feli and Briles, Christy},
	year = {2022},
	note = {[IF2021=13.789;AIS2021=4.071]},
	keywords = {disturbance, reconstruction},
	pages = {292--300},
}



@article{dreslerova_settlement_2019,
	title = {Settlement activity in later prehistory: invisible in the archaeological record but documented by pollen and sedimentary evidence},
	volume = {11},
	issn = {1866-9565},
	shorttitle = {Settlement activity in later prehistory},
	url = {https://doi.org/10.1007/s12520-018-0614-x},
	doi = {10.1007/s12520-018-0614-x},
	abstract = {The paper deals with landscape and settlement development between ca. 300 BC and AD 600 in a defined area of the northern Czech Republic. Despite favourable natural conditions, human occupation of the area did not begin until the end of the first millennium BC. Natural soil and vegetation development therefore lasted longer than in the traditionally settled lowland areas. Initial settlement activity from the La Tène period caused substantial erosion of deforested luvisols and retisols, well-documented by an accumulation of eroded soil horizons in a local wetland. The erosion process continued for more than 500 years following the end of the La Tène settlement, despite the fact that archaeological research revealed no reliable evidence of occupation prior to the twelfth century AD. Pollen and sedimentary records from the wetland, however, clearly indicate the existence of settlement activity during the “archaeologically invisible” Roman and Migration periods. This case is not unique and underlines the importance of environmental analysis for the detection of settlement history, particularly during periods of poor archaeological visibility or in places that are difficult to research using standard archaeological methods. The change in conditions after the first deforestation and subsequent late prehistoric settlement triggered the degradation of the deforested luvisols and retisols and led to the diversification of the soil cover, which now also includes regosols, gleysols, and truncated luvisols and retisols.},
	language = {en},
	number = {5},
	urldate = {2020-03-05},
	journal = {Archaeological and Anthropological Sciences},
	author = {Dreslerová, Dagmar and Kozáková, Radka and Chuman, Tomáš and Strouhalová, Barbora and Abraham, Vojtěch and Poništiak, Štefan and Šefrna, Luděk},
	month = may,
	year = {2019},
	pages = {1683--1700},
}



@article{hostinska_comparative_2021,
	title = {Comparative biology of four {Rhodanthidium} species ({Hymenoptera}, {Megachilidae}) that nest in snail shells},
	volume = {85},
	issn = {1314-2607},
	doi = {10.3897/jhr.85.66544},
	abstract = {Some species of two tribes (Anthidiini and Osmiini) of the bee family Megachilidae utilize empty gastropod shells as nesting cavities. While snail-nesting Osmiini have been more frequently studied and the nesting biology of several species is well-known, much less is known about the habits of snail-nesting Anthidiini. We collected nests of four species of the genus Rhodanthidium (R. septemdentatum, R. sticticum, R. siculum and R. infuscatum) in the Czech Republic, Slovakia, Catalonia (Spain) and Sicily (Italy). We dissected these nests in the laboratory and documented their structure, pollen sources and nest associates. The four species usually choose large snail shells. All four species close their nests with a plug made of resin, sand and fragments of snail shells. However, nests of the four species can be distinguished based on the presence (R. septemdentatum, R. sticticum) or absence (R. siculum, R. infuscatum) of mineral and plant debris in the vestibular space, and the presence (R. septemdentatum, R. infuscatum) or absence (R. sticticum, R. siculum) of a resin partition between the vestibular space and the brood cell. Rhodanthidium septemdentatum, R. sticticum and R. siculum usually build a single brood cell per nest, but all R. infuscatum nests studied contained two or more cells. For three of the species (R. siculum, R. septemdentatum and R. sticticum) we confirmed overwintering in the adult stage. Contrary to R. siculum, R. septemdentatum and R. sticticum do not hide their nest shells and usually use shells under the stones or hidden in crevices within stone walls. Nest associates were very infrequent. We only found two R. sticticum nests parasitized by the chrysidid wasp Chrysura refulgens and seven nests infested with pollen mites Chaetodactylus cf. anthidii. Our pollen analyses confirm that Rhodanthidium are polylectic but show a preference for Fabaceae by R. sticticum.},
	language = {English},
	urldate = {2021-09-01},
	journal = {Journal of Hymenoptera Research},
	author = {Hostinská, Lucie and Kuneš, Petr and Hadrava, Jiří and Bosch, Jordi and Scaramozzino, Pier Luigi and Bogusch, Petr},
	month = aug,
	year = {2021},
	note = {[IF2020=1.733]},
	pages = {11--28},
}



@article{mottl_global_2021,
	title = {Global acceleration in rates of vegetation change over the past 18,000 years},
	volume = {372},
	issn = {0036-8075, 1095-9203},
	url = {https://science.sciencemag.org/content/372/6544/860},
	doi = {10.1126/science.abg1685},
	abstract = {The pace of Holocene vegetation change
Although much is known about the rapid environmental changes that have occurred since the Industrial Revolution, the patterns of change over the preceding millennia have been only patchily understood. Using a global set of {\textgreater}1100 fossil pollen records, Mottl et al. explored the rates of vegetation change over the past 18,000 years (see the Perspective by Overpeck and Breshears). The authors show that the rates of change accelerated markedly during the Late Holocene (∼4.6 to 2.9 thousand years ago), even more rapidly than the climate-driven vegetation changes associated with the end of the last glacial period. In addition, the Late Holocene acceleration began for terrestrial communities as a whole, suggesting that the acceleration in turnover over the past two centuries is the tip of a deeper trend.
Science, abg1685, this issue p. 860; see also abi9902, p. 786
Global vegetation over the past 18,000 years has been transformed first by the climate changes that accompanied the last deglaciation and again by increasing human pressures; however, the magnitude and patterns of rates of vegetation change are poorly understood globally. Using a compilation of 1181 fossil pollen sequences and newly developed statistical methods, we detect a worldwide acceleration in the rates of vegetation compositional change beginning between 4.6 and 2.9 thousand years ago that is globally unprecedented over the past 18,000 years in both magnitude and extent. Late Holocene rates of change equal or exceed the deglacial rates for all continents, which suggests that the scale of human effects on terrestrial ecosystems exceeds even the climate-driven transformations of the last deglaciation. The acceleration of biodiversity change demonstrated in ecological datasets from the past century began millennia ago.
A compilation of fossil pollen sequences shows that the acceleration of biodiversity change began millennia ago.
A compilation of fossil pollen sequences shows that the acceleration of biodiversity change began millennia ago.},
	language = {English},
	number = {6544},
	urldate = {2021-05-20},
	journal = {Science},
	author = {Mottl, Ondřej and Flantua, Suzette G. A. and Bhatta, Kuber P. and Felde, Vivian A. and Giesecke, Thomas and Goring, Simon and Grimm, Eric C. and Haberle, Simon and Hooghiemstra, Henry and Ivory, Sarah and Kuneš, Petr and Wolters, Steffen and Seddon, Alistair W. R. and Williams, John W.},
	month = may,
	year = {2021},
	note = {[IF2020=47.728]},
	keywords = {Database, reconstruction},
	pages = {860--864},
}



@incollection{kunes_post-glacial_2007,
	address = {Praha},
	title = {Post-glacial vegetation development in sandstone areas of the {Czech} {Republic}},
	copyright = {All rights reserved},
	isbn = {978-80-200-1577-8},
	language = {English},
	booktitle = {Sandstone {Landscapes}},
	publisher = {Academia},
	author = {Kuneš, Petr and Pokorný, Petr and Jankovská, Vlasta},
	editor = {Härtel, Handrij and Cílek, Václav and Herben, Tomáš and Jackson, Andrew and Williams, Rendel},
	year = {2007},
	keywords = {Czech Republic, Holocene, Late Glacial, human impact, pollen analysis, sandstone, vegetation history},
	pages = {244--257},
}



@article{abraham_present-day_2014,
	title = {Present-day vegetation helps quantifying past land cover in selected regions of the {Czech} {Republic}},
	volume = {9},
	copyright = {All rights reserved},
	doi = {10.1371/journal.pone.0100117},
	abstract = {The REVEALS model is a tool for recalculating pollen data into vegetation abundances on a regional scale. We explored the general effect of selected parameters by performing simulations and ascertained the best model setting for the Czech Republic using the shallowest samples from 120 fossil sites and data on actual regional vegetation (60 km radius). Vegetation proportions of 17 taxa were obtained by combining the CORINE Land Cover map with forest inventories, agricultural statistics and habitat mapping data. Our simulation shows that changing the site radius for all taxa substantially affects REVEALS estimates of taxa with heavy or light pollen grains. Decreasing the site radius has a similar effect as increasing the wind speed parameter. However, adjusting the site radius to 1 m for local taxa only (even taxa with light pollen) yields lower, more correct estimates despite their high pollen signal. Increasing the background radius does not affect the estimates significantly. Our comparison of estimates with actual vegetation in seven regions shows that the most accurate relative pollen productivity estimates (PPEs) come from Central Europe and Southern Sweden. The initial simulation and pollen data yielded unrealistic estimates for Abies under the default setting of the wind speed parameter (3 m/s). We therefore propose the setting of 4 m/s, which corresponds to the spring average in most regions of the Czech Republic studied. Ad hoc adjustment of PPEs with this setting improves the match 3–4-fold. We consider these values (apart from four exceptions) to be appropriate, because they are within the ranges of standard errors, so they are related to original PPEs. Setting a 1 m radius for local taxa (Alnus, Salix, Poaceae) significantly improves the match between estimates and actual vegetation. However, further adjustments to PPEs exceed the ranges of original values, so their relevance is uncertain.},
	language = {English},
	number = {6},
	urldate = {2014-06-18},
	journal = {PLoS ONE},
	author = {Abraham, Vojtěch and Oušková, Veronika and Kuneš, Petr},
	month = jun,
	year = {2014},
	note = {[IF2013=3.534]},
	keywords = {Czech Republic, LRA, Pollen dispersal, Pollen production estimate (PPE), REVEALS, reconstruction, vegetation},
	pages = {e100117},
}



@article{strandberg_regional_2014,
	title = {Regional climate model simulations for {Europe} at 6 and 0.2 k {BP}: sensitivity to changes in anthropogenic deforestation},
	volume = {10},
	copyright = {All rights reserved},
	issn = {1814-9332},
	shorttitle = {Regional climate model simulations for {Europe} at 6 and 0.2 k {BP}},
	doi = {10.5194/cp-10-661-2014},
	language = {English},
	number = {2},
	urldate = {2014-03-28},
	journal = {Climate of the Past},
	author = {Strandberg, G. and Kjellström, E. and Poska, A. and Wagner, S. and Gaillard, M.-J. and Trondman, A.-K. and Mauri, A. and Davis, B. A. S. and Kaplan, J. O. and Birks, H. J. B. and Bjune, A. E. and Fyfe, R. and Giesecke, T. and Kalnina, L. and Kangur, M. and van der Knaap, W. O. and Kokfelt, U. and Kuneš, P. and Latałova, M. and Marquer, L. and Mazier, F. and Nielsen, A. B. and Smith, B. and Seppä, H. and Sugita, S.},
	month = mar,
	year = {2014},
	note = {[IF2013=3.482]},
	keywords = {Europe, REVEALS, climate model, human impact, reconstruction},
	pages = {661--680},
}



@article{mariani_testing_2016,
	title = {Testing quantitative pollen dispersal models in animal-pollinated vegetation mosaics: {An} example from temperate {Tasmania}, {Australia}},
	volume = {154},
	copyright = {All rights reserved},
	issn = {0277-3791},
	shorttitle = {Testing quantitative pollen dispersal models in animal-pollinated vegetation mosaics},
	url = {http://www.sciencedirect.com/science/article/pii/S0277379116304851},
	doi = {10.1016/j.quascirev.2016.10.020},
	abstract = {Reconstructing past vegetation abundance and land-cover changes through time has important implications in land management and climate modelling. To date palaeovegetation reconstructions in Australia have been limited to qualitative or semi-quantitative inferences from pollen data. Testing pollen dispersal models constitutes a crucial step in developing quantitative past vegetation and land cover reconstructions. Thus far, the application of quantitative pollen dispersal models has been restricted to regions dominated by wind-pollinated plants (e.g. Europe) and their performance in a landscape dominated by animal-pollinated plant taxa is still unexplored. Here we test, for the first time in Australia, two well-known pollen dispersal models to assess their performance in the wind- and animal-pollinated vegetation mosaics of western Tasmania. We focus on a mix of wind- (6 taxa) and animal- (7 taxa) pollinated species that comprise the most common pollen types and key representatives of the dominant vegetation formations. Pollen Productivity Estimates and Relevant Source Area of Pollen obtained using Lagrangian Stochastic turbulent simulations appear to be more realistic when compared to the results from the widely used Gaussian Plume Model.},
	urldate = {2016-11-18},
	journal = {Quaternary Science Reviews},
	author = {Mariani, M. and Connor, S. E. and Theuerkauf, M. and Kuneš, P. and Fletcher, M. -S.},
	month = dec,
	year = {2016},
	note = {[IF2015=4.521]},
	keywords = {Australia, Pollen dispersal, Pollen production estimate (PPE), Tasmania, reconstruction},
	pages = {214--225},
}



@incollection{kunes_history_2017,
	address = {Cham},
	edition = {1},
	series = {Plant and {Vegetation}},
	title = {History of {Czech} vegetation since the {Late} {Pleistocene}},
	copyright = {All rights reserved},
	isbn = {978-3-319-63180-6},
	url = {https://link.springer.com/chapter/10.1007/978-3-319-63181-3_6},
	abstract = {A long-term perspective is a crucial dimension for understanding the present-day composition and structure of the Czech flora and vegetation. We outline processes that were important for the development of the present-day diversity of flora and vegetation including extinctions of taxa and ecological mechanisms operating within glacial-interglacial cycles. Further, we present the history of vegetation during the key stages in the glacial and postglacial periods. First, we outline the pattern in the vegetation during the last glacial, including a discussion of the existence of refugia for trees. We further describe the changes in vegetation during the Late Glacial, which were mostly the results of abrupt climatic events. We also present a new synthesis of the Holocene regional development in vegetation based on a Landscape Reconstruction Algorithm, which results in different regional vegetation trajectories and three main phases in the development of vegetation. Finally, we give some examples of the histories of local vegetation at several sites mainly based on plant macrofossils.},
	language = {English},
	number = {14},
	booktitle = {Flora and {Vegetation} of the {Czech} {Republic}},
	publisher = {Springer},
	author = {Kuneš, Petr and Abraham, Vojtěch},
	editor = {Chytrý, Milan and Danihelka, Jiří and Kaplan, Zdeněk and Pyšek, Petr},
	year = {2017},
	keywords = {Czech Republic, Holocene, Late Glacial, Plant macroremains, glacial, interglacial, pollen analysis, reconstruction, vegetation history},
	pages = {193--227},
}



@article{mariani_how_2017,
	title = {How old is the {Tasmanian} cultural landscape? {A} test of landscape openness using quantitative land-cover reconstructions},
	volume = {44},
	copyright = {All rights reserved},
	issn = {1365–2699},
	shorttitle = {How old is the {Tasmanian} cultural landscape?},
	doi = {10.1111/jbi.13040},
	abstract = {Aim: To test competing hypotheses about the timing and extent of Holocene landscape opening using pollen-based quantitative land-cover estimates.
Location: Dove Lake, Tasmanian Wilderness World Heritage Area, Australia.
Methods: Fossil pollen data were incorporated into pollen dispersal models and corrected for differences in pollen productivity among key plant taxa. Mechanistic models (REVEALS—Regional Estimates of VEgetation Abundance from Large Sites) employing different models for pollen dispersal (Gaussian plume and Lagrangian stochastic models) were evaluated and applied in the Southern Hemisphere for the first time.
Results: Validation of the REVEALS model with vegetation cover data suggests an overall better performance of the Lagrangian stochastic model. Regional land-cover estimates for forest and non-forest plant taxa show persistent landscape openness throughout the Holocene (average landscape openness {\textasciitilde}50\%). Gymnoschoenus sphaerocephalus, an indicator of moorland vegetation, shows higher values during the early Holocene (11.7–9 ka) and declines slightly through the mid-Holocene (9–4.5 ka) during a phase of partial landscape afforestation. Rain forest cover reduced (from {\textasciitilde}40\% to {\textasciitilde}20\%) during the period between 4.2–3.5 ka.
Main conclusions: Pollen percentages severely under-represent landscape openness in western Tasmania and this bias has fostered an over-estimation of Holocene forest cover from pollen data. Treeless vegetation dominated Holocene landscapes of the Dove Lake area, allowing us to reject models of landscape evolution that invoke late-Holocene replacement of a rain forest-dominated landscape by moorland. Instead, we confirm a model of Late Pleistocene inheritance of open vegetation. Rapid forest decline occurred after c. 4 ka, likely in response to regional moisture decline.},
	language = {English},
	number = {10},
	journal = {Journal of Biogeography},
	author = {Mariani, Michela and Connor, Simon E. and Fletcher, Michael-S. and Theuerkauf, Martin and Kuneš, Petr and Jacobsen, Geraldine and Saunders, Krystyna M. and Zawadzki, Atun},
	year = {2017},
	note = {[IF2016=4.248]},
	keywords = {Australia, Holocene, REVEALS, Tasmania, cultural landscape, dispersal models, fire, landcover reconstruction, moorland, rain forest, reconstruction},
	pages = {2410--2420},
}



@article{carter_quantitative_2018,
	title = {Quantitative palynology informing conservation ecology in the {Bohemian}/{Bavarian} {Forests} of {Central} {Europe}},
	volume = {8},
	issn = {1664-462X},
	doi = {10.3389/fpls.2017.02268},
	abstract = {In 1927, the first pollen diagram was published from the Bohemian/Bavarian Forest region of Central Europe, providing one of the first qualitative views of the long-term vegetation development in the region. Since then significant methodological advances in quantitative approaches such as pollen influx and pollen-based vegetation models (e.g., Landscape Reconstruction Algorithm, LRA) have contributed to enhance our understanding of temporal and spatial ecology. These types of quantitative reconstructions are fundamental for conservation and restoration ecology because they provide long-term perspectives on ecosystem functioning. In the Bohemian/Bavarian Forests, forest managers have a goal to restore the original forest composition at mid-elevation forests, yet they rely on natural potential vegetation maps that do not take into account long-term vegetation dynamics. Here we reconstruct the Holocene history of forest composition and discuss the implications the LRA has for regional forest management and conservation. Two newly analysed pollen records from Prášilské jezero and Rachelsee were compared to 10 regional peat bogs/mires and two other regional lakes to reconstruct total land-cover abundance at both the regional- and local-scales. The results demonstrate that spruce has been the dominate canopy cover across the region for the past 9000 years at both high- ({\textgreater}900 m) and mid-elevations ({\textgreater}700-900 m) elevations. At the regional-scale, inferred from lake records, spruce has comprised an average of {\textasciitilde}50\% of the total forest canopy; whereas at the more local-scale at mid-elevations, spruce formed {\textasciitilde}59\%. Beech established {\textasciitilde}6000 cal yr BP while fir established {\textasciitilde}5500 cal yr BP, and reached a maximum land-cover abundance of 24\% and 13\% roughly 1000 years ago at mid-elevations. Over the past 500 years spruce has comprised {\textasciitilde}47\% land-cover, while beech and fir comprised {\textasciitilde}8\% and {\textless}5\% at mid-elevations. This approach argues for the ‘natural’ development of spruce and fir locally in zones where the paleoecology indicates the persistence of these species for millennia. Contrasting local and regional reconstructions of forest canopy cover points to a patchwork mosaic with local variability in the dominant taxa. Incorporation of paleoecological data in dialogues about biodiversity and ecosystem management is an approach that has wider utility.},
	language = {English},
	number = {Article 2268},
	urldate = {2017-12-28},
	journal = {Frontiers in Plant Science},
	author = {Carter, Vachel A. and Chiverrell, Richard C. and Clear, Jennifer L. and Kuosmanen, Niina and Moravcová, Alice and Svoboda, Miroslav and Svobodová-Svitavská, Helena and Leeuwen, Van and Van Leeuwen, Jacqueline and van der Knaap, Willem O. and Kuneš, Petr},
	year = {2018},
	note = {[IF2017=3.678]},
	keywords = {Abies alba, Fagus sylvatica, Holocene, Picea abies, Pollen, Reveals, disturbance, landcover, palynology, reconstruction},
	pages = {1--14},
}



@article{kunes_relative_2019,
	title = {Relative pollen productivity estimates for vegetation reconstruction in central-eastern {Europe} inferred at local and regional scales},
	volume = {29},
	issn = {0959-6836},
	doi = {10.1177/0959683619862026},
	abstract = {Understanding pollen-vegetation relationships is crucial for accurate land-cover and climate reconstructions, yet important parameters for quantifying past vegetation abundance are mostly unknown for large parts of Europe harbouring temperate thermophilous ecosystems. We collected pollen and vegetation data in central-eastern Europe, a region covered by patchy cultural landscapes of high biodiversity to estimate relative pollen productivity (RPP) for important pollen-equivalent taxa. Our study area was situated in the south-western part of the White Carpathians (Czechia–Slovakia borderland), where we collected 40 modern moss pollen samples scattered over 250 km2 and mapped vegetation within 100 m around each pollen site. Additional vegetation data were compiled from Forest management plans, Natura 2000 habitat mapping and floristic inventories over the entire area. We calculated RPP (referenced to Poaceae) by testing two approaches: the extended R-value (ERV) model by estimating relevant source area of pollen and the REVEALS-based productivity using regional scale vegetation estimates. Two models were applied to depict pollen dispersal: Lagrangian stochastic and the Gaussian plume (Prentice) models. We estimated RPP for 16 taxa using the ERV model and an additional nine taxa using REVEALS. Both approaches found Plantago lanceolata-type to be a high pollen producer, Quercus medium-to-high, Asteraceae subf. Cichorioideae, Anthemis-type, Ranunculus acris-type and Rubiaceae low-to-medium and Brassicaceae and Senecio-type as low pollen producers. Results for other, mainly tree taxa, significantly differed in both approaches mainly due to largely uneven representation in both local and regional vegetation. In comparison with other studies, our data demonstrate a high variability in the estimated RPPs which could be influenced by climatic conditions or potentially vegetation structure. We suggest that the accuracy of RPP estimates could be enhanced by comparing modern pollen data with large-scale vegetation data in the future.},
	language = {English},
	number = {11},
	urldate = {2019-09-18},
	journal = {The Holocene},
	author = {Kuneš, Petr and Abraham, Vojtěch and Werchan, Barbora and Plesková, Zuzana and Fajmon, Karel and Jamrichová, Eva and Roleček, Jan},
	month = nov,
	year = {2019},
	note = {[IF2018=2.547]},
	keywords = {Czech Republic, ERV model, Gaussian plume model, LRA, Lagrangian stochastic model, REVEALS, modern pollen spectra, reconstruction, vegetation cover},
	pages = {1708--1719},
}



@article{schafstall_changes_2020,
	title = {Changes in species composition and diversity of a montane beetle community over the last millennium in the {High} {Tatras}, {Slovakia}: {Implications} for forest conservation and management},
	volume = {555},
	issn = {0031-0182},
	shorttitle = {Changes in species composition and diversity of a montane beetle community over the last millennium in the {High} {Tatras}, {Slovakia}},
	doi = {10.1016/j.palaeo.2020.109834},
	abstract = {Montane biomes are niche environments high in biodiversity with a variety of habitats. Often isolated, these non-continuous remnant ecosystems inhabit narrow ecological zones putting them under threat from changing climatic conditions and anthropogenic pressure. Twelve sediment cores were retrieved from a peat bog in Tatra National Park, Slovakia, and correlated to each other by wiggle-matching geochemical signals derived from micro-XRF scanning, to make a reconstruction of past conditions. A fossil beetle (Coleoptera) record, covering the last 1000 years at 50- to 100-year resolution, gives a new insight into changing flora and fauna in this region. Our findings reveal a diverse beetle community with varied ecological groups inhabiting a range of forest, meadow and synanthropic habitats. Changes in the beetle community were related to changes in the landscape, driven by anthropogenic activities. The first clear evidence for human activity in the area occurs c. 1250 CE and coincides with the arrival of beetle species living on the dung of domesticated animals (e.g. Aphodius spp.). From 1500 CE, human (re)settlement, and activities such as pasturing and charcoal burning, appear to have had a pronounced effect on the beetle community. Local beetle diversity declined steadily towards the present day, likely due to an infilling of the forest hollow leading to a decrease in moisture level. We conclude that beetle communities are directly affected by anthropogenic intensity and land-use change. When aiming to preserve or restore natural forest conditions, recording their past changes in diversity can help guide conservation and restoration. In doing so, it is important to look back beyond the time of significant human impact, and for this, information contained in paleoecological records is irreplaceable.},
	language = {English},
	urldate = {2020-06-20},
	journal = {Palaeogeography, Palaeoclimatology, Palaeoecology},
	author = {Schafstall, Nick and Whitehouse, Nicki and Kuosmanen, Niina and Svobodová-Svitavská, Helena and Saulnier, Mélanie and Chiverrell, Richard C. and Fleischer, Peter and Kuneš, Petr and Clear, Jennifer L.},
	month = oct,
	year = {2020},
	note = {[IF2019=2.833]},
	keywords = {Biodiversity, Central Europe, Climate change, Coleoptera, Human impact, Nature conservation, disturbance},
	pages = {109834},
}



@article{kuosmanen_integration_2020,
	title = {Integration of dendrochronological and palaeoecological disturbance reconstructions in temperate mountain forests},
	volume = {475},
	issn = {0378-1127},
	doi = {10.1016/j.foreco.2020.118413},
	abstract = {Disentangling the long-term changes in forest disturbance dynamics provides a basis for predicting the forest responses to changing environmental conditions. The combination of multidisciplinary records can offer more robust reconstructions of past forest disturbance dynamics. Here we link disturbance histories of the central European mountain spruce forest obtained from dendrochronological and palaeoecological records (fossil pollen, sedimentary charcoal, bark beetle remains and geochemistry) using a small glacial lake and the surrounding forest in the Šumava National Park (Czech Republic). Dendrochronological reconstructions of disturbance were created for 300-year-long records from 6 study plots with a minimum of 35 trees analyzed for the abrupt growth increases (releases) and rapid early growth rates, both indicative of disturbance events. High-resolution analysis of lake sediments were used to reconstruct 800-year long changes in forest composition and landscape openness (fossil pollen), past fire events (micro- and macroscopic charcoal), bark beetle occurrence (fossil bark beetle remains), and erosion episodes (geochemical signals in the sediment) potentially resulting from disturbance events. Tree-ring data indicate that disturbances occurred regularly through the last three centuries and identify a most intensive period of disturbances between 1780 and 1830 CE. Geochemical erosion markers (e.g. K, Zr, \% inorganic) show greater flux of catchment sediment and soils in the periods 1250–1400 and 1450–1500 CE, before a substantial shift to a more erosive regime 1600–1850 and 1900 CE onwards. Pollen records demonstrate relatively small changes in forest composition during the last 800 years until the beginning of the 20th century, when there was decrease in Picea. Fossil bark beetle remains indicate continuous presence of bark beetles from 1620s to 1800s, and charcoal records suggest that more frequent fires occurred during the 18th century. Each of the dendrochronological, palaeoecological and sedimentological records provide a unique perspective on forest disturbance dynamics, and combined offer a more robust and complete record of disturbance history. We demonstrate that sedimentary proxies originating from the lake catchment mirror the forest disturbance dynamics recorded in the tree-rings. The multidisciplinary records likely record forest disturbances at different spatial and temporal scales revealing different disturbance characteristics. Integrating these multidisciplinary datasets demonstrates a promising way to obtain more complete understanding of long-term disturbance dynamics. However, integrating datasets with variable spatial and temporal influence remains challenging. Our results indicated that multiple disturbance factors, such as windstorms, bark beetle outbeaks and fires, may occur simultaneously creating a complex disturbance regime in mountain forests, which should be considered in forest management and conservation strategies.},
	language = {English},
	urldate = {2020-08-02},
	journal = {Forest Ecology and Management},
	author = {Kuosmanen, Niina and Čada, Vojtěch and Halsall, Karen and Chiverrell, Richard C. and Schafstall, Nick and Kuneš, Petr and Boyle, John F. and Knížek, Miloš and Appleby, Peter G. and Svoboda, Miroslav and Clear, Jennifer L.},
	month = nov,
	year = {2020},
	note = {[IF2019=3.17]},
	keywords = {Bark beetles, Fire, Forest dynamics, Geochemistry, Pollen, Tree-rings, disturbance},
	pages = {118413},
}



@article{chevalier_pollen-based_2020,
	title = {Pollen-based climate reconstruction techniques for late {Quaternary} studies},
	volume = {210},
	issn = {0012-8252},
	url = {http://www.sciencedirect.com/science/article/pii/S001282522030430X},
	doi = {10.1016/j.earscirev.2020.103384},
	abstract = {Fossil pollen records are well-established indicators of past vegetation changes. The prevalence of pollen across environmental settings including lakes, wetlands, and marine sediments, has made palynology one of the most ubiquitous and valuable tools for studying past environmental and climatic change globally for decades. A complementary research focus has been the development of statistical techniques to derive quantitative estimates of climatic conditions from pollen assemblages. This paper reviews the most commonly used statistical techniques and their rationale and seeks to provide a resource to facilitate their inclusion in more palaeoclimatic research. To this end, we first address the fundamental aspects of fossil pollen data that should be considered when undertaking pollen-based climate reconstructions. We then introduce the range of techniques currently available, the history of their development, and the situations in which they can be best employed. We review the literature on how to define robust calibration datasets, produce high-quality reconstructions, and evaluate climate reconstructions, and suggest methods and products that could be developed to facilitate accessibility and global usability. To continue to foster the development and inclusion of pollen climate reconstruction methods, we promote the development of reporting standards. When established, such standards should 1) enable broader application of climate reconstruction techniques, especially in regions where such methods are currently underused, and 2) enable the evaluation and reproduction of individual reconstructions, structuring them for the evolving open-science era, and optimising the use of fossil pollen data as a vital means for the study of past environmental and climatic variability. We also strongly encourage developers and users of palaeoclimate reconstruction methodologies to make associated programming code publicly available, which will further help disseminate these techniques to interested communities.},
	language = {English},
	urldate = {2020-12-09},
	journal = {Earth-Science Reviews},
	author = {Chevalier, Manuel and Davis, Basil A. S. and Heiri, Oliver and Seppä, Heikki and Chase, Brian M. and Gajewski, Konrad and Lacourse, Terri and Telford, Richard J. and Finsinger, Walter and Guiot, Joël and Kühl, Norbert and Maezumi, S. Yoshi and Tipton, John R. and Carter, Vachel A. and Brussel, Thomas and Phelps, Leanne N. and Dawson, Andria and Zanon, Marco and Vallé, Francesca and Nolan, Connor and Mauri, Achille and de Vernal, Anne and Izumi, Kenji and Holmström, Lasse and Marsicek, Jeremiah and Goring, Simon and Sommer, Philipp S. and Chaput, Michelle and Kupriyanov, Dmitry},
	month = nov,
	year = {2020},
	keywords = {Analogues, Climate, Community-based standards, Palaeoclimate, Pollen, Probability density functions, Quantitative reconstructions, Transfer functions},
	pages = {103384},
}



@article{feurdean_recent_2020,
	title = {Recent fire regime in the southern boreal forests of western {Siberia} is unprecedented in the last five millennia},
	volume = {244},
	issn = {0277-3791},
	doi = {10.1016/j.quascirev.2020.106495},
	abstract = {Wildfires in Siberia are documented to have increased in frequency and severity over recent decades. However, in the absence of long-term records, it is unclear how far and why this trend deviates from centennial to millennial scale variability. Here we reconstruct past patterns of fire frequency and fire type, and explore how the fire-related traits of boreal species and plant functional types (PFTs) determine ecosystem responses to changing fire regimes. We use charcoal-based reconstructions of the fire regime in combination with a pollen-based assessment of vegetation composition in two boreal forest peat profiles from Plotnikovo Mire in western Siberia that span the last 2400 and 5000 years. We found moderate levels of biomass burning between 5000 and 4000 cal yr BP. Biomass burning and fire severity i.e., more biomass burning per fire episode, increased over the last 1500 cal yr BP associated with the dominance of fire invaders (Betula). Conversely, between 4000 and 1500 cal yr BP lower biomass burning, with perhaps fire types affecting mostly litter and understorey vegetation, coincided with the dominance of fire resisters (e.g., Pinus sylvestris, P. sibirica, Larix) intermixed with a considerable number of fire avoiders (e.g., Abies sibirica and Picea obovata). This long-term perspective shows that the current fire regime commenced 1500 years ago and deviates from the trends observed over the last 5000 years. This deviation is linked to a combination of climate conditions conducive to fire, the amount and composition of woody fuels, and land use changes. Although pines reacted more sensitively to increased fire severity, the fire avoider Picea obovata appears to be much more vulnerable to both frequent, severe fires than Abies sibirica. We anticipate that climatically driven changes in fire weather, with frequent warm and dry spells, and anthropogenic land use intensification will heighten fire severity and their impact, driving vegetation composition towards Betula species to the detriment of Picea obovata. This study also shows that charcoal morphotypes can provide useful information on fuel and fire type, and that, although all macro-charcoal size classes reliably indicate local-scale fires, the larger fraction ({\textgreater}300–500 μm) allows the identification of on-site fire episodes. We recommend multi-site palaeo-fire reconstructions in boreal peatlands to adequately reflect the influence of localised peat moisture content, and vegetation composition and structure variability on the small-scale heterogeneity of fire type and spread. This will ensure that trends in fire regime dynamics are representative and not limited to the local scale. We also propose future directions in fire research that can be tested using fossil records of fire, climate and vegetation ideally in an interdisciplinary approach.},
	language = {English},
	urldate = {2020-10-02},
	journal = {Quaternary Science Reviews},
	author = {Feurdean, Angelica and Florescu, Gabriela and Tanţău, Ioan and Vannière, Boris and Diaconu, Andrei-Cosmin and Pfeiffer, Mirjam and Warren, Dan and Hutchinson, Simon M. and Gorina, Natalia and Gałka, Mariusz and Kirpotin, Sergey},
	month = sep,
	year = {2020},
	keywords = {Biomass burning, Charcoal morphologies, Climate change, Drought, Fire frequency, Fire severity, Great Vasyugan Mire, Peat archives, Pollen, Russia, Satellite images},
	pages = {106495},
}



@article{felde_compositional_2020,
	title = {Compositional turnover and variation in {Eemian} pollen sequences in {Europe}},
	volume = {29},
	issn = {1617-6278},
	doi = {10.1007/s00334-019-00726-5},
	abstract = {The Eemian interglacial represents a natural experiment on how past vegetation with negligible human impact responded to amplified temperature changes compared to the Holocene. Here, we assemble 47 carefully selected Eemian pollen sequences from Europe to explore geographical patterns of (1) total compositional turnover and total variation for each sequence and (2) stratigraphical turnover between samples within each sequence using detrended canonical correspondence analysis, multivariate regression trees, and principal curves. Our synthesis shows that turnover and variation are highest in central Europe (47–55°N), low in southern Europe (south of 45°N), and lowest in the north (above 60°N). These results provide a basis for developing hypotheses about causes of vegetation change during the Eemian and their possible drivers.},
	language = {English},
	number = {1},
	urldate = {2020-01-07},
	journal = {Vegetation History and Archaeobotany},
	author = {Felde, Vivian A. and Flantua, Suzette G. A. and Jenks, Cathy R. and Benito, Blas M. and de Beaulieu, Jacques-Louis and Kuneš, Petr and Magri, Donatella and Nalepka, Dorota and Risebrobakken, Bjørg and ter Braak, Cajo J. F. and Allen, Judy R. M. and Granoszewski, Wojciech and Helmens, Karin F. and Huntley, Brian and Kondratienė, Ona and Kalniņa, Laimdota and Kupryjanowicz, Mirosława and Malkiewicz, Małgorzata and Milner, Alice M. and Nita, Małgorzata and Noryśkiewicz, Bożena and Pidek, Irena A. and Reille, Maurice and Salonen, J. Sakari and Šeirienė, Vaida and Winter, Hanna and Tzedakis, Polychronis C. and Birks, H. John B.},
	month = jan,
	year = {2020},
	note = {[IF2019=2.364]},
	keywords = {Detrended canonical correspondence analysis, Extrinsic and intrinsic processes, Inertia, Last interglacial dataset, Multivariate regression trees, Neutral processes, Principal curves, database, interglacial},
	pages = {101--109},
}



@article{feurdean_fire_2020,
	title = {Fire hazard modulation by long-term dynamics in land cover and dominant forest type in eastern and central {Europe}},
	volume = {17},
	issn = {1726-4170},
	url = {https://www.biogeosciences.net/17/1213/2020/},
	doi = {10.5194/bg-17-1213-2020},
	abstract = {{\textless}p{\textgreater}{\textless}strong{\textgreater}Abstract.{\textless}/strong{\textgreater} Wildfire occurrence is influenced by climate, vegetation and human activities. A key challenge for understanding the risk of fires is quantifying the mediating effect of vegetation on fire regimes. Here, we explore the relative importance of Holocene land cover, land use, dominant functional forest type, and climate dynamics on biomass burning in temperate and boreo-nemoral regions of central and eastern Europe over the past 12\&thinsp;kyr. We used an extensive data set of Holocene pollen and sedimentary charcoal records, in combination with climate simulations and statistical modelling. Biomass burning was highest during the early Holocene and lowest during the mid-Holocene in all three ecoregions (Atlantic, continental and boreo-nemoral) but was more spatially variable over the past 3–4\&thinsp;kyr. Although climate explained a significant variance in biomass burning during the early Holocene, tree cover was consistently the highest predictor of past biomass burning over the past 8\&thinsp;kyr. In temperate forests, biomass burning was high at {\textless}span class="inline-formula"{\textgreater}∼45{\textless}/span{\textgreater}\&thinsp;\% tree cover and decreased to a minimum at between 60\&thinsp;\% and 70\&thinsp;\% tree cover. In needleleaf-dominated forests, biomass burning was highest at {\textless}span class="inline-formula"{\textgreater}∼{\textless}/span{\textgreater}\&thinsp;60\&thinsp;\%–65\&thinsp;\% tree cover and steeply declined at {\textless}span class="inline-formula"{\textgreater}\&gt;65{\textless}/span{\textgreater}\&thinsp;\% tree cover. Biomass burning also increased when arable lands and grasslands reached {\textless}span class="inline-formula"{\textgreater}∼{\textless}/span{\textgreater}\&thinsp;15\&thinsp;\%–20\&thinsp;\%, although this relationship was variable depending on land use practice via ignition sources, fuel type and quantities. Higher tree cover reduced the amount of solar radiation reaching the forest floor and could provide moister, more wind-protected microclimates underneath canopies, thereby decreasing fuel flammability. Tree cover at which biomass burning increased appears to be driven by warmer and drier summer conditions during the early Holocene and by increasing human influence on land cover during the late Holocene. We suggest that long-term fire hazard may be effectively reduced through land cover management, given that land cover has controlled fire regimes under the dynamic climates of the Holocene.{\textless}/p{\textgreater}},
	language = {English},
	number = {5},
	urldate = {2020-03-05},
	journal = {Biogeosciences},
	author = {Feurdean, Angelica and Vannière, Boris and Finsinger, Walter and Warren, Dan and Connor, Simon C. and Forrest, Matthew and Liakka, Johan and Panait, Andrei and Werner, Christian and Andrič, Maja and Bobek, Premysl and Carter, Vachel A. and Davis, Basil and Diaconu, Andrei-Cosmin and Dietze, Elisabeth and Feeser, Ingo and Florescu, Gabriela and Gałka, Mariusz and Giesecke, Thomas and Jahns, Susanne and Jamrichová, Eva and Kajukało, Katarzyna and Kaplan, Jed and Karpińska-Kołaczek, Monika and Kołaczek, Piotr and Kuneš, Petr and Kupriyanov, Dimitry and Lamentowicz, Mariusz and Lemmen, Carsten and Magyari, Enikö K. and Marcisz, Katarzyna and Marinova, Elena and Niamir, Aidin and Novenko, Elena and Obremska, Milena and Pędziszewska, Anna and Pfeiffer, Mirjam and Poska, Anneli and Rösch, Manfred and Słowiński, Michal and Stančikaitė, Miglė and Szal, Marta and Święta-Musznicka, Joanna and Tanţău, Ioan and Theuerkauf, Martin and Tonkov, Spassimir and Valkó, Orsolya and Vassiljev, Jüri and Veski, Siim and Vincze, Ildiko and Wacnik, Agnieszka and Wiethold, Julian and Hickler, Thomas},
	month = mar,
	year = {2020},
	note = {[IF2019=3.48]},
	keywords = {disturbance},
	pages = {1213--1230},
}



@article{hoskova_inter-_2020,
	title = {Inter- and intraspecific variation in grass phytolith shape and size: a geometric morphometrics perspective},
	shorttitle = {Inter- and intraspecific variation in grass phytolith shape and size},
	doi = {10.1093/aob/mcaa102},
	abstract = {AbstractBackground and Aims.  The relative contributions of inter- and intraspecific variation to phytolith shape and size have only been investigated in a limi},
	language = {English},
	urldate = {2020-06-19},
	journal = {Annals of Botany},
	author = {Hošková, Kristýna and Pokorná, Adéla and Neustupa, Jiří and Pokorný, Petr},
	year = {2020},
}



@article{bobek_human-induced_2018,
	title = {Human-induced changes in fire regime and subsequent alteration of the sandstone landscape of {Northern} {Bohemia} ({Czech} {Republic})},
	volume = {28},
	issn = {0959-6836},
	doi = {10.1177/0959683617729443},
	abstract = {Multiproxy palaeoecological evidence from a sandstone region in northern Czech Republic was collected to explore the impact of fire disturbances on the decline of the broadleaved forests during the Late Bronze Age (3250–3050 cal. BP). It has been hypothesized that human-accelerated soil leaching affected the nutrient availability in the sandstone area, thus promoting the expansion of oligotrophic-adapted plant communities in the late-Holocene. Little is known about the mechanisms which induced such large-scale vegetation transformation. We sought to determine which driving forces were involved using independent proxy records – soil and sedimentary charcoal, pollen and fungal spores. Local fire history was derived from the variation in charcoal accumulation rates (CHAR) preserved in Eustach peatbog. The fire frequency (FF) estimation over the past {\textasciitilde}7500 years revealed distinct phases of increased burning between 3100 and 2120 cal. BP (3.0 fires 1000 yr−1) and 1400–600 cal. BP (4.3 fires 1000 yr−1). Rapid compositional changes in the pollen assemblage were documented during the Late Bronze Age period, suggesting vegetation responded to increased fire disturbances. The human influence on the fire regime is implied by the short-term increase in cereal pollen concurrent with a major fire event, indicating possible use of slash-and-burn cultivation by Late Bronze societies. This type of human subsistence strategy practised in the sandstone landscape further evolved to pastoralism as suggested by continuous presence of coprophilous fungi Sporormiella and Sordaria, which occurred since the Hallstatt/La Tène period (2750–1950 cal. BP). Our study documents, for the first time, the intentional, human-caused biomass burning from densely forested areas of Northern Bohemian sandstone region. Our results imply that increased rate of fire disturbances contributed to the Late Bronze Age transformation of broadleaved forests to oligotrophic forest communities of late-Holocene.},
	language = {English},
	number = {3},
	urldate = {2018-03-31},
	journal = {The Holocene},
	author = {Bobek, Přemysl and Svitavská Svobodová, Helena and Werchan, Barbora and Švarcová, Markéta Gabriela and Kuneš, Petr},
	month = mar,
	year = {2018},
	note = {[IF2017=2.419]},
	keywords = {disturbance},
	pages = {427--443},
}



@article{carter_holocene-scale_2018,
	title = {Holocene-scale fire dynamics of central {European} temperate spruce-beech forests},
	volume = {191},
	issn = {0277-3791},
	doi = {10.1016/j.quascirev.2018.05.001},
	abstract = {This study investigated the long-term role and drivers of fire in the central European temperate spruce-beech forests from Prášilské jezero, Czech Republic. The results illustrate the complex relationship between broad-scale climate, vegetation composition, and local human activities on fire throughout the Holocene. Biomass burning was the highest (average 3 fires/1000 years) and most severe during the early Holocene when fire resistant taxa (Pinus, Corylus and Betula) dominated. Using a Generalized Additive Model to assess the response of dominant canopy taxa to changes in biomass burning and fire severity, response curves demonstrate a positive relationship (p \&lt; 0.01) between fire resistant taxa and increases in biomass burning. Norway spruce (Picea abies) established ∼10,000 cal yr BP and expanded during peak biomass burning. Response curves show a slight negative relationship with Picea and increasing biomass burning, and a positive relationship with increasing fire severity. This suggests that central European spruce forests may not be significantly impacted by fire. Regional biomass burning dramatically decreased with the expansion of fire sensitive taxa (e.g. Fagus sylvatica) ∼6500 cal yr BP, yet no dramatic reduction in local fire frequency occurred. This suggests either human activities or rare fire-promoting climatic events were important in shaping local fire regimes. Fire activity peaked (6 fires/1000 years) ∼2500 cal yr BP and paralleled increases in anthropogenic pollen indicators. Fagus response curves illustrates a negative (p \&lt; 0.01) relationship with increasing biomass burning and fire severity suggesting that natural Fagus forests may be increasingly vulnerable to projected increases in wildfire occurrence.},
	language = {English},
	urldate = {2018-05-26},
	journal = {Quaternary Science Reviews},
	author = {Carter, Vachel A. and Moravcová, Alice and Chiverrell, Richard C. and Clear, Jennifer L. and Finsinger, Walter and Dreslerová, Dagmar and Halsall, Karen and Kuneš, Petr},
	month = jul,
	year = {2018},
	note = {[IF2017=4.334]},
	keywords = {Climate, Fire, Holocene, Macrofossils, Paleoecology, Pollen, Sedimentary charcoal, disturbance},
	pages = {15--30},
}



@article{bobek_divergent_2019,
	title = {Divergent fire history trajectories in {Central} {European} temperate forests revealed a pronounced influence of broadleaved trees on fire dynamics},
	volume = {222},
	issn = {0277-3791},
	doi = {10.1016/j.quascirev.2019.105865},
	abstract = {Fire occurrence is driven by a complex interplay between vegetation, climatic, landform and human factors making it challenging to separate the individual effect of each variable. Here we present a reconstruction of the Holocene biomass burning history of two regions located in the Central European temperate zone that differ in the timing of the Middle Holocene expansion of broadleaf-dominated forest communities. This allowed us to investigate the effect of biotic changes on past fire activity. Multiple-site charcoal accumulation records were used to estimate regional-scale trends in biomass burning and to compare them with major trajectories of vegetation development. Extensive 14C-dated soil charcoal records collected within both regions were amalgamated using a cumulative probability function to identify a stand-scale proxy of past fire occurrence. Our results suggest that rising vegetation productivity driven by rapid Early Holocene climate amelioration enhanced biomass burning. The increased fire activity during this period was driven by both a drier- and warmer-than-present climate and easily flammable fuels produced by conifer-dominated vegetation. We identified an inhibiting effect of the concomitant Fagus sylvatica expansion on levels of biomass burning that occurred asynchronously between our mountain and mid-elevation sandstone regions 6500 cal yr BP and 4900 cal yr BP, respectively. The amount of compositional change in plant communities was more related to the transformation of major vegetation types than to fluctuations in fire activity levels. The divergent timing of the fire decline in response to the Fagus sylvatica expansion implies biotic control over biomass burning that is independent of a direct climatic influence.},
	language = {English},
	urldate = {2019-09-16},
	journal = {Quaternary Science Reviews},
	author = {Bobek, Přemysl and Svobodová-Svitavská, Helena and Pokorný, Petr and Šamonil, Pavel and Kuneš, Petr and Kozáková, Radka and Abraham, Vojtěch and Klinerová, Tereza and Švarcová, Markéta Gabriela and Jamrichová, Eva and Krauseová, Eva and Wild, Jan},
	month = oct,
	year = {2019},
	note = {[IF2018=4.641]},
	keywords = {Fire history, Holocene, Human impact, Sedimentary charcoal, Species turnover, Vegetation dynamics, disturbance},
	pages = {105865},
}



@article{petrik_disruption_2019,
	title = {Disruption in an alluvial landscape: {Settlement} and environment dynamics on the alluvium of the river {Dyje} at the {Pohansko} archaeological site ({Czech} {Republic})},
	volume = {511},
	issn = {1040-6182},
	shorttitle = {Disruption in an alluvial landscape},
	url = {http://www.sciencedirect.com/science/article/pii/S1040618217309503},
	doi = {10.1016/j.quaint.2018.04.013},
	abstract = {Floodplain alluvia can provide a combination of natural and anthropogenic evidence of environmental changes, allowing to directly examine their evolution in relation to settlement dynamics. Such evidence is recorded, for example, at the archaeological site Pohansko by the town of Břeclav, a former centre of the Great Moravian Empire. The aim of our research was to explore what conditions on the floodplain could have caused the abandonment of this environment. Special attention was paid to the climax of the floodplain's occupation during the times of the Great Moravian Empire (AD 836–906) and to the decline of its occupation in the following centuries. The environmental record at the Pohansko site starts in the 7th century BC. From the Iron Age onwards (Hallstatt and La Tène periods) there is evidence of non-agricultural human activities. Since the 3rd and 2nd centuries BC to at least the second half of the 10th century AD, there is no record of any floodplain aggradation or flooding at the site. Later, both the archaeological and palaeoecological records on the floodplain probably got exposed and redeposited. The result is a mechanically disturbed layer that is synchronous with soil horizons and subsequent Early Mediaeval cultural layers covering sandy elevations. For an unknown reason, the site was deserted for many centuries after the end of the 10th century AD. During the High Mediaeval period and the early Modern Era, especially since the 15th century AD, overbank deposits covered the floodplain. Intensified human impact in the river catchment and climate change during the Little Ice Age were the main triggers of this change. The results correlate with the written historical sources pertaining to this area, which speak about an increasing frequency of flooding in the Czech lands since the 14th century, and especially in the second half of the 16th century. As a result, these sites became unsuitable for settlement and abandoned.},
	language = {en},
	urldate = {2020-03-05},
	journal = {Quaternary International},
	author = {Petřík, Jan and Petr, Libor and Adameková, Katarína and Prišťáková, Michaela and Potůčková, Anna and Lenďáková, Zuzana and Frączek, Marcin and Dresler, Petr and Macháček, Jiří and Kalicki, Tomasz and Lisá, Lenka},
	month = mar,
	year = {2019},
	keywords = {Aggradation, Early Middle Ages, Floodplain, Floodplain occupation, Great Moravian Empire, Human impact, Iron Age, Late Holocene},
	pages = {124--139},
}



@article{novak_soil_2019,
	title = {Soil charcoal elucidates the role of humans in the development of landscape of extreme biodiversity},
	volume = {30},
	copyright = {© 2019 John Wiley \& Sons, Ltd.},
	issn = {1099-145X},
	url = {https://onlinelibrary.wiley.com/doi/abs/10.1002/ldr.3350},
	doi = {10.1002/ldr.3350},
	abstract = {The south-western White Carpathians (Czech Republic, Slovakia) are one of the few places in low-elevation Central Europe where a diverse landscape, including extremely species rich meadows, scattered oak trees, and mixed oak woodlands, has escaped modern transformation. We studied C14-dated and taxonomically identified macroscopic soil charcoal record to elucidate the genesis of this landscape. Thirteen soil profiles were sampled in grasslands along a gradient of elevation and history of human settlement. We identified clear pattern in the taxonomic composition of woody soil charcoal and anthracomass along this gradient, which we ascribe to different pathways of landscape development. Charcoal assemblages of chernozem-like soils in the promontories of the mountain range have a low anthracomass and are dominated by heliophilous and semishade species (Quercus, Pinus), with the oldest charcoals dated to pre-Neolithic times. Soils of the middle elevations have a high anthracomass and often show pronounced differences in charcoal composition at different soil depths; the oldest charcoal samples date back between the Neolithic and Early Middle Ages, and heliophilous species increase towards the topsoil. The soil of the summit area shows a medium anthracomass and charcoal assemblage dominated by shade-tolerant trees; the charcoal dates from the Middle Ages. Our results suggest continuity of an open to semiopen landscape in lower elevations of the White Carpathians, whereas middle and higher elevations experienced a forested period. Humans and fire played an important role in landscape development, as indicated by both soil charcoal and available palaeoecological and archaeological evidence. Local meadows with extremely high biodiversity thus appear to be a continuation of an ancient forest-steppe-like ecosystem.},
	language = {en},
	number = {13},
	urldate = {2020-03-05},
	journal = {Land Degradation \& Development},
	author = {Novák, Jan and Roleček, Jan and Dresler, Petr and Hájek, Michal},
	year = {2019},
	note = {\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/ldr.3350},
	keywords = {Holocene, biodiversity, forest-steppe, human settlement, soil charcoal},
	pages = {1607--1619},
}



@article{novak_holocene_2019,
	title = {Holocene forest transformations in sandstone landscapes of the {Czech} {Republic}: {Stand}-scale comparison of charcoal and pollen records:},
	shorttitle = {Holocene forest transformations in sandstone landscapes of the {Czech} {Republic}},
	url = {https://journals.sagepub.com/doi/10.1177/0959683619854510},
	doi = {10.1177/0959683619854510},
	abstract = {Stand-scale palaeoecology in sandstone landscapes provides insight into contrasting Holocene forest succession trajectories. Sharp geomorphological gradients in...},
	language = {en},
	urldate = {2020-03-05},
	journal = {The Holocene},
	author = {Novák, Jan and Abraham, Vojtěch and Šída, Petr and Pokorný, Petr},
	month = jun,
	year = {2019},
	note = {Publisher: SAGE PublicationsSage UK: London, England},
}



@article{hosek_buried_2019,
	title = {Buried {Late} {Weichselian} thermokarst landscape discovered in the {Czech} {Republic}, central {Europe}},
	volume = {48},
	copyright = {© 2019 Collegium Boreas. Published by John Wiley \& Sons Ltd},
	issn = {1502-3885},
	doi = {10.1111/bor.12404},
	abstract = {Pronounced climatic warming associated with the Late Weichselian Pleniglacial-to-Lateglacial transition caused considerable environmental changes throughout the former periglacial zones (in Europe 53°–46°N). During permafrost degradation and subsequent ground subsidence (i.e. thermokarst processes), the landscape changed rapidly. In this study we investigated a flat mid-altitude area in south Bohemia, Czech Republic, lying close to the southern limit of the Weichselian permafrost. We discovered palaeo-lake basins with sedimentary infillings up to 11 m in depth. According to radiocarbon and palynostratigraphical dating, these basins were formed at the onset of the Late Pleniglacial-to-Lateglacial transition, whereas the smaller depressions were formed later. We suggest that the basins resulted from thermal and fluvio-thermal erosion of the former permafrost and represent remnants of discontinuous gullies and possibly collapsed frost mounds (pingo/lithalsa scars). The formation of this a fossil thermokarst landscape was climatically driven and multiple phased, with the major phase during the climatic warming and wetting at the onset of GI-1e (Bølling) and the minor phase during GI-1c (Allerød). This study enhances knowledge of the palaeogeography of the former European periglacial zone by showing that Late Pleistocene thermokarst activity could have had a significant impact on the evolution of the landscape of at least some regions of central Europe along the southern limit of the continuous permafrost zone. The research also points to a similar history for the physical transformation of the landscape of the former European periglacial zone and current thermokarst landscapes and could be a valuable source of information with respect to the future transformation of the Arctic under conditions of ongoing global warming.},
	language = {English},
	number = {4},
	urldate = {2020-03-05},
	journal = {Boreas},
	author = {Hošek, Jan and Prach, Jindřich and Křížek, Marek and Šída, Petr and Moska, Piotr and Pokorný, Petr},
	year = {2019},
	pages = {988--1005},
}



@article{salkova_crops_2019,
	title = {Crops along the trade routes? {Archaeobotany} of the {Bronze} {Age} in the region of {South} {Bohemia} ({Czech} {Republic}) in context with longer distance trade and exchange networks},
	volume = {11},
	issn = {1866-9565},
	shorttitle = {Crops along the trade routes?},
	doi = {10.1007/s12520-019-00893-6},
	abstract = {The number of species of crop plants in Central Europe increased constantly during the Bronze Age. The structure of the composition of cultivated plants was probably connected to the cultural contacts of human populations. During the Bronze Age (2300/2000–800 BC), the region of South Bohemia (Czech Republic) increasingly became the focus of long-distance trade and exchange networks with regions to the east and many other regions (the Eastern Alps, the Alpine Foreland, the central lowlands of the Czech Republic, Hungary and Western Slovakia). The aim of the paper is to examine archaeobotanical assemblages of charred plant remains to see if these changes within Bronze Age societies, and their spheres of interaction, are also recorded within their agricultural practices. In particular, the importance of specific individual crop species can be reflected in the study region in comparison with other individual regions of Central Europe. Humans in the region of South Bohemia had more connections with the Eastern Alps and the Alpine Foreland region during the Early and Middle Bronze Ages. Regarding the structure of crop species, the composition of sub/dominant crops in South Bohemia and the Eastern Alps and the Alpine Foreland had many similarities. The cultural trajectory of the human populations of the South Bohemian region changed substantially in the Late and Final Bronze Ages: intensive contacts are documented, primarily with the region of Central Bohemia. This is reflected in the composition of the sub/dominant crops in South Bohemia, which shows many similarities to the other regions of the Czech Republic. Changes in migration and exchange networks—in particular those that involved more formalised trade—are associated with a large number of innovations and specific goods and led to much wider levels of cultural and social integration within Bronze Age Europe than had been previously seen.},
	language = {English},
	number = {10},
	urldate = {2020-03-05},
	journal = {Archaeological and Anthropological Sciences},
	author = {Šálková, Tereza and Chvojka, Ondřej and Hlásek, Daniel and Jiřík, Jaroslav and John, Jan and Novák, Jan and Kovačiková, Lenka and Beneš, Jaromír},
	month = oct,
	year = {2019},
	pages = {5569--5590},
}



@article{ticha_nutrient_2019,
	title = {Nutrient availability affected shallow-lake ecosystem response along the {Late}-{Glacial}/{Holocene} transition},
	volume = {846},
	issn = {1573-5117},
	doi = {10.1007/s10750-019-04054-7},
	abstract = {Shallow lowland lakes undergo long-lasting natural eutrophication processes, which can be studied through the development of communities of aquatic organisms. However, records showing millennial-scale trophic status variability in these water bodies are rare. Two radiocarbon-dated sedimentary profiles from former (now destroyed by brown coal mining) Lake Komořany (Central Europe, Czech Republic) served for a multi-proxy study of biological remains (diatoms, chironomids, pollen) supplemented by X-ray fluorescence (XRF) and loss-on-ignition (LOI). The age–depth model and palynostratigraphy confirm a continuous Late-Glacial to Early-Holocene record. The results suggest consistent in-lake conditions with high nutrient availability since the lake origin in the Late-Glacial period. A distinct shift at the Late-Glacial/Holocene boundary evidenced by an enhancement in diatom valve concentration and a lithological interface was foregone by a qualitative change in diatom and chironomid assemblages along with rise in LOI. It suggests that a major transformation occurred before the onset of the Holocene. As this qualitative change was characterized by a decrease in relative abundance of nutrient-demanding species, we propose an indirect climatic control by means of nutrient availability as the main driver of the aquatic species composition.},
	language = {English},
	number = {1},
	urldate = {2020-03-05},
	journal = {Hydrobiologia},
	author = {Tichá, Anna and Bešta, Tomáš and Vondrák, Daniel and Houfková, Petra and Jankovská, Vlasta},
	month = dec,
	year = {2019},
	pages = {87--108},
}



@article{houfkova_dynamics_2019,
	title = {The dynamics of a non-forested stand in the {Krušné} {Mts}.: the effect of a short-lived medieval village on the local environment},
	volume = {28},
	issn = {1617-6278},
	shorttitle = {The dynamics of a non-forested stand in the {Krušné} {Mts}.},
	url = {https://doi.org/10.1007/s00334-019-00718-5},
	doi = {10.1007/s00334-019-00718-5},
	abstract = {Medieval vegetation–human–climate interactions were studied from a sediment profile situated in the centre of a short-lived medieval village located above 800 m a.s.l. on the ridge of the Krušné Mts., NW Bohemia, Central Europe. Analyses of pollen, seeds/fruits, micro- and macro-charcoals, diatoms and concentrations of microelements in connection with written sources revealed a significant human-induced deforestation in the second half of the 14th century. This deforestation occurred sooner than supposed and the area did not revert after ad 1347 as elsewhere in Europe. Arable fields probably enabled basic self-sustaining cultivation of winter cereals even at such elevations in the climatically favourable years of the Medieval Warm Period. The village presumably collapsed due to a combination of weather fluctuations at the onset of the Little Ice Age, simultaneous socioeconomic stagnation in the Czech Lands and exploitation of the surrounding forest. The dynamics of wet stand vegetation and Calthion palustris montane wet meadows were driven by fluctuating human and grazing impacts. Annual and biennial herbaceous species that peaked after village abandonment were rapidly replaced by Filipendula ulmaria and Salix stands. The secondary forest developed towards Picea stands. Only later, mesic montane meadows of medium tall grasses combined with Meum athamanticum and mountain dry pastures developed on nutrient poor patches.},
	language = {en},
	number = {6},
	urldate = {2020-03-05},
	journal = {Vegetation History and Archaeobotany},
	author = {Houfková, Petra and Horák, Jan and Pokorná, Adéla and Bešta, Tomáš and Pravcová, Ivana and Novák, Jan and Klír, Tomáš},
	month = nov,
	year = {2019},
	pages = {607--621},
}



@article{jamrichova_lowland_2019,
	title = {Lowland pine forests in the northwestern {Pannonian} {Basin}: between natural vegetation and modern plantations},
	volume = {19},
	issn = {1436-378X},
	shorttitle = {Lowland pine forests in the northwestern {Pannonian} {Basin}},
	doi = {10.1007/s10113-019-01555-y},
	abstract = {Lowland Scots pine (Pinus sylvestris L.) forests cover extensive areas in Central Europe. Most of them are considered to be the results of relatively recent plantation-oriented forest management. We investigated the long-term history of lowland pine forests in the Záhorská Lowland region of aeolian sands in the northern margin of the Pannonian Basin. Pine monocultures were planted there already in the mid-seventeenth century and currently prevail in the land cover of the region. Our aim was to challenge the commonly accepted idea that the present pine-dominated forests lack connections to pre-plantation pine forests of the Early Holocene. Using multi-proxy data, we compared palaeoeocological data with archaeobotanical data, anthracological finds and evidence on past human settlement. Palaeoecological results suggested a distinct compositional linkage of recent pine-dominated forests with their Early Holocene predecessors. Moreover, no significant change was detected in tree dominants in at least the past two millennia. Contrary to palaeoecology, archeaeobotany suggested that broadleaved trees (mostly oak) dominated during the past 4000 years. However, this result is probably strongly biased by human preferences for wood for specific purposes. On the other hand, pine in palaeoecological data is doubtless overrepresented because of its abundant pollen production. We conclude that pine forests with a significant admixture of oak continuously covered the sandy substrates of the Záhorská Lowland throughout the Holocene. The present pine forests can therefore be considered fairly close to the original vegetation of the study region.},
	language = {English},
	number = {8},
	urldate = {2020-03-05},
	journal = {Regional Environmental Change},
	author = {Jamrichová, Eva and Bobek, Přemysl and Šolcová, Anna and Tkáč, Peter and Hédl, Radim and Valachovič, Milan},
	month = dec,
	year = {2019},
	pages = {2395--2409},
}



@article{kunes_changing_2019,
	title = {Changing disturbance-diversity relationships in temperate ecosystems over the past 12000 years},
	volume = {107},
	copyright = {© 2019 The Authors. Journal of Ecology © 2019 British Ecological Society},
	issn = {1365-2745},
	doi = {10.1111/1365-2745.13136},
	abstract = {Disturbances such as fires and grazing have major impacts on biodiversity. While it has been suggested that species richness is highest with intermediate levels of disturbance, currently there is no consensus due to an absence of data covering large temporal and spatial scales. We developed a new method to examine disturbance-diversity relationships (DDR) using sedimentary pollen data linked with species’ disturbance ecology. We reconstructed disturbance and diversity dynamics in the region of the European temperate zone over the last 12,000 years and calculated DDR for 900-year sequential temporal windows. Disturbance frequency was highest in the early and late Holocene, while remaining low in the mid-Holocene. Diversity increased continuously from the start of the Holocene. Our results demonstrate that over the past 12,000 years DDR changed from hump-shaped into monotonic increasing pattern. While both highly disturbed and undisturbed sites were strongly impoverished in the early Holocene, as species migrated, biodiversity levels have subsequently affected disturbance regimes with highly disturbed sites now being the highest in species richness. Synthesis. Land-use changes in the last 4,000 years created an increasingly patchy landscape, allowing invasive species adapted to high-frequency disturbance to migrate across the landscape. The link between high diversity and disturbed areas is relatively recent and may anticipate even greater disturbance frequencies in future. Our findings also support a hypothesis that species migration, and the structure of the species pool critically determines the response of biota to external factors such as disturbance.},
	language = {English},
	number = {4},
	urldate = {2019-06-28},
	journal = {Journal of Ecology},
	author = {Kuneš, Petr and Abraham, Vojtěch and Herben, Tomáš},
	year = {2019},
	note = {[IF2018=5.687]},
	keywords = {Central Europe, Holocene, disturbance, disturbance frequency, pollen, richness, vegetation},
	pages = {1678--1688},
}



@article{florescu_holocene_2019,
	title = {Holocene rapid climate changes and ice-rafting debris events reflected in high-resolution {European} charcoal records},
	volume = {222},
	issn = {0277-3791},
	doi = {10.1016/j.quascirev.2019.105877},
	abstract = {In contrast to marked climate change across glacial-interglacial cycles, the Holocene epoch represents a relatively warm, stable interval. However, on finer temporal scales, it too has experienced both gradual and rapid changes in climate. In the North Atlantic region, many rapid climate changes (RCCs) coincide with ice-rafted debris (IRD) or Bond events, which are associated with cooling and suggested to occur with periodicities of 1370 ± 500 years. Given that climate is a dominant control of fire activity, regulating both vegetation productivity and fuel moisture, this study investigated the linkage between Holocene fire, IRD episodes and associated RCCs in seven high-resolution charcoal records distributed across Europe. Results show low-frequency fire periodicities of 500–600 years, 900–1400 and 2400 years that occurred simultaneously across northern and mid-latitude Europe, suggesting that regional fire disturbance responded to large-scale climate drivers. The 900–1400 year periodicity is most common among sites and of similar frequency to IRD episodes, potentially reflecting a connection between mechanisms regulating IRD flux in the North Atlantic and wildfire activity in Europe. Although the data indicate some spatial variability in fire induced by local drivers (such as vegetation and human impact) during RCC events associated with IRD peaks, broad-scale patterns are discernible. Specifically, Northern Europe burned more during the 10.2, 9.4, 8.2, 5.9 and 4.2 kiloannum before present (ka) RCC events when climate was drier, and less during the 2.9 and 1.4 ka events when climate was moister. In contrast, in mid-latitude Europe, a higher incidence of fire is documented at 8.2 and 1.4 ka when climate was drier and a lower incidence of fire is associated with moister conditions at 10.2, 9.4 and 2.9 ka. Spatial heterogeneity is evident in mid-latitude Europe during the 5.9, 4.2 and 0.4 ka events. These spatially explicit sub-continental scale differences in fire activity may be related to differences in moisture availability resulting from shifts in associated atmospheric circulation patterns.},
	language = {English},
	urldate = {2019-09-08},
	journal = {Quaternary Science Reviews},
	author = {Florescu, Gabriela and Brown, Kendrick J. and Carter, Vachel A. and Kuneš, Petr and Veski, Siim and Feurdean, Angelica},
	month = oct,
	year = {2019},
	note = {[IF2018=4.641]},
	keywords = {Europe, Fire cycles, Holocene, Ice rafted debris events, Macroscopic charcoal, Rapid climate change, disturbance},
	pages = {105877},
}



@article{solcova_early_2018,
	title = {Early and middle {Holocene} ecosystem changes at the {Western} {Carpathian}/{Pannonian} border driven by climate and {Neolithic} impact},
	volume = {47},
	copyright = {© 2018 Collegium Boreas. Published by John Wiley \& Sons Ltd},
	issn = {1502-3885},
	doi = {10.1111/bor.12309},
	abstract = {Travertine deposits are unique archives for multidisciplinary studies of past climate changes, associated vegetation development and the evolution of human societies. Despite their high potential in palaeoecological and palaeoclimate reconstructions, investigations of travertines are rather scarce in central Europe and particularly in Slovakia. Therefore, this study focused on a travertine deposit situated on the border between the Pannonian Basin and the Western Carpathians in a small valley in Santovka village (SW Slovakia), which is unique due to the presence of archaeological artefacts with known radiocarbon ages in the palaeoecological profile. Using a multidisciplinary approach combining macrofossil, pollen, mollusc, lithological and geochemical analyses, this study investigated climate–human–vegetation interactions. The Holocene onset was marked by the early arrival of oak trees; however, forest-steppe with a high representation of pine predominated until 9880 cal. a BP, followed by an expansion of temperate trees. The local ecosystem changed around 8600 cal. a BP when the valley was probably dammed by a travertine accumulation, probably resulting in the existence of a small travertine lake. This was associated with wetter climatic conditions, which were also documented in other sites in the Western Carpathians at that time. Surrounding temperate forest possibly retained a certain degree of openness, or local steppe habitat may have persisted on adjacent loess terraces until the neolithization of the area. Archaeological evidence represented by a ceramic shard dated to 7339 cal. a BP suggests the first appearance of humans at the site, yet pollen analysis records a significant change in vegetation first at 6650 cal. a BP. The local ecosystem records an abrupt change linked with human settlement earlier, at c. 7000 cal. a BP. Deforestation activities of the Neolithics resulted in the formation of an open calcareous fen occupied by numerous light-demanding mollusc species. The present study provides new important data about the spread of temperate trees at the onset of the Holocene, about further vegetation changes caused by activities of the first Neolithic farmers and about climate changes in the region of southwestern Slovakia.},
	language = {English},
	number = {3},
	urldate = {2019-01-22},
	journal = {Boreas},
	author = {Šolcová, Anna and Petr, Libor and Hájková, Petra and Petřík, Jan and Tóth, Peter and Rohovec, Jan and BáTORA, Jozef and Horsák, Michal},
	year = {2018},
	pages = {897--909},
}



@article{carter_1500-year_2018,
	series = {The {Fire}-{Human}-{Climate}-{Vegetation} {Nexus}},
	title = {A 1,500-year synthesis of wildfire activity stratified by elevation from the {U}.{S}. {Rocky} {Mountains}},
	volume = {488},
	issn = {1040-6182},
	doi = {10.1016/j.quaint.2017.06.051},
	abstract = {A key task in fire-climate research in the western United States is to characterize potential future fire-climate linkages across different elevational gradients. Using thirty-seven sedimentary charcoal records, here we present a 1500-year synthesis of wildfire activity across different elevational gradients to characterize fire-climate linkages. From our results, we have identified three periods of elevated fire occurrence centered on the 20th century, 900 cal yr BP, and 1350 cal yr BP. During the 20th century, fire activity has occurred primarily in the northern Rocky Mountains, with mid-elevations experiencing the greatest increase in wildfire activity. While wildfires occurred primarily in the SRM region ∼900 cal yr BP, the greatest increase in high-elevations occurred in the NRM at this time. Finally, synchronous wildfires occurred in both northern and southern Rocky Mountain mid-elevations ∼1350 cal yr BP, suggesting a potential analog for future wildfire conditions in response to warmer temperatures and more protracted droughts. We conclude that wildfire activity increased in most elevations during periods of protracted summer drought, warmer-than-average temperatures, and based on modern climate analogs, reduced atmospheric humidity.},
	urldate = {2019-01-22},
	journal = {Quaternary International},
	author = {Carter, Vachel A. and Power, Mitchell J. and Lundeen, Zachary J. and Morris, Jesse L. and Petersen, Kenneth L. and Brunelle, Andrea and Anderson, R. Scott and Shinker, Jacqueline J. and Turney, Lovina and Koll, Rebecca and Bartlein, Patrick J.},
	month = sep,
	year = {2018},
	keywords = {Charcoal, Climate, Fire, Paleofire, Rocky Mountains},
	pages = {107--119},
}



@article{carter_drought_2018,
	title = {Drought and vegetation change in the central {Rocky} {Mountains} and western {Great} {Plains}: potential climatic mechanisms associated with megadrought conditions at 4200\&thinsp;cal\&thinsp;yr\&thinsp;{BP}},
	volume = {14},
	issn = {1814-9324},
	shorttitle = {Drought and vegetation change in the central {Rocky} {Mountains} and western {Great} {Plains}},
	doi = {10.5194/cp-14-1195-2018},
	abstract = {{\textless}p{\textgreater}{\textless}strong{\textgreater}Abstract.{\textless}/strong{\textgreater} Droughts are a naturally re-occurring phenomena that result in economic and societal losses. Yet, the most historic droughts that occurred in the 1930s and 1950s in the Great Plains and western United States were both shorter in duration and less severe than megadroughts that have plagued the region in the past. Roughly 4200 years ago, a ∼ 150-year long megadrought occurred in the central Rocky Mountains, as indicated by sedimentary pollen evidence documenting a brief and unique change in vegetation composition from Long Lake, southeastern Wyoming. Neighbouring the central Rocky Mountains, several dune fields reactivated in the western Great Plains around this time period illustrating a severe regional drought. While sedimentary pollen provides evidence of past drought, paleoecological evidence does not provide context for the climate mechanisms that may have caused the drought. Thus, a modern climate analogue technique was applied to the sedimentary pollen and regional dune reactivation evidence identified from the region to provide a conceptual framework for exploring possible mechanisms responsible for the observed ecological changes. The modern climate analogues of 2002/2012 illustrate that warm and dry conditions persisted through the growing season and were associated with anomalously higher-than-normal geopotential heights centred over the Great Plains. In the spring, higher-than-normal heights suppressed moisture transport via the low-level jet from the Gulf of Mexico creating a more southwesterly component of flow. In the summer, higher-than-normal heights persisted over the northern Great Plains resulting in a wind shift with an easterly component of flow, drawing in dry continental air into the study region. In both cases, lower-than-normal moisture in the atmosphere (via 850{\textless}span class="thinspace"{\textgreater}{\textless}/span{\textgreater}mbar specific humidity) inhibited uplift and potential precipitation. Thus, if the present scenario existed during the 4.2{\textless}span class="thinspace"{\textgreater}{\textless}/span{\textgreater}ka drought, the associated climatic responses are consistent with local and regional proxy data suggesting regional drought conditions in the central Rocky Mountains and western Great Plains.{\textless}/p{\textgreater}},
	language = {English},
	number = {8},
	urldate = {2019-01-22},
	journal = {Climate of the Past},
	author = {Carter, Vachel A. and Shinker, Jacqueline J. and Preece, Jonathon},
	month = aug,
	year = {2018},
	pages = {1195--1212},
}



@article{sida_new_2011,
	title = {New {Radiocarbon} {Data} for the {North} {Bohemian} {Mesolithic}},
	volume = {2},
	copyright = {All rights reserved},
	url = {http://www.iansa.eu/papers/IANSA-2011-02-sida.pdf},
	language = {English},
	number = {2},
	journal = {Interdisciplinaria Archaeologica},
	author = {Šída, P. and Prostředník, J. and Kuneš, P.},
	year = {2011},
	keywords = {Czech Republic, Mesolithic, archeology, pre-Neolithic, radiocarbon AMS dating},
	pages = {151--157},
}



@article{pokorny_palaeoenvironmental_2010,
	title = {Palaeoenvironmental research of the {Schwarzenberg} {Lake}, southern {Bohemia}, and exploratory excavations of this key {Mesolithic} archaeological area},
	volume = {101},
	copyright = {All rights reserved},
	language = {English},
	journal = {Památky archeologické},
	author = {Pokorný, Petr and Šída, Petr and Chvojka, Ondřej and Žáčková, Pavla and Kuneš, Petr and Světlík, Ivo and Veselý, Josef},
	year = {2010},
	keywords = {Czech Republic, Mesolithic, Plant macroremains, archeology, pollen analysis, pre-Neolithic},
	pages = {5--38},
}



@article{sida_drevene_2007,
	title = {Dřevěné artefakty raně holocenního stáří z litorálu zaniklého jezera Švarcenberk [{Early} {Holocene} wooden artifacts from the {Lake} Švarcenberk]},
	volume = {48},
	copyright = {All rights reserved},
	language = {Czech},
	journal = {Přehled výzkumů},
	author = {Šída, Petr and Pokorný, Petr and Kuneš, Petr},
	year = {2007},
	note = {In Czech},
	keywords = {Holocene, Mesolithic, archeology, pre-Neolithic},
	pages = {55--64},
}



@article{kunes_interpretation_2008,
	title = {Interpretation of the last-glacial vegetation of eastern-central {Europe} using modern analogues from southern {Siberia}},
	volume = {35},
	copyright = {All rights reserved},
	issn = {1365-2699},
	doi = {10.1111/j.1365-2699.2008.01974.x},
	language = {English},
	number = {12},
	journal = {Journal of Biogeography},
	author = {Kuneš, Petr and Pelánková, Barbora and Chytrý, Milan and Jankovská, Vlasta and Pokorný, Petr and Petr, Libor},
	year = {2008},
	note = {[IF2007=3.539]},
	keywords = {Central Europe, Late Glacial, Pollen, Siberia, Surface sample, glacial, modern analogue, pre-Neolithic, steppe},
	pages = {2223--2236},
}



@article{kunes_detection_2008,
	title = {Detection of the impact of early {Holocene} hunter-gatherers on vegetation in the {Czech} {Republic}, using multivariate analysis of pollen data},
	volume = {17},
	copyright = {All rights reserved},
	issn = {0939-6314, 1617-6278},
	doi = {10.1007/s00334-007-0119-5},
	abstract = {Pollen data from the Czech Republic was used to detect the early Holocene impact of hunter-gatherers on vegetation based on a selection of 19 early Holocene pollen profiles, complemented with archaeological information regarding the intensity of local and regional Mesolithic human habitation. Archaeological evidence was assigned to simple categories reflecting the intensity of habitation and distance from pollen sites. Multivariate methods (PCA and RDA) were used to determine relationships between sites and possible anthropogenic pollen indicators and to test how these indicators relate to the archaeological evidence. In several profiles the pollen signal was influenced by local Mesolithic settlement. Specific pollen types (e.g. Calluna vulgaris, Plantago lanceolata, Solanum and Pteridium aquilinum) were found to be significantly correlated with human activity. The role of settlement proximity to the investigation site, the statistical significance of pollen indicators of human activity, as well as the early occurrence of Corylus avellana and its possible anthropogenic dispersal, are discussed.},
	language = {English},
	number = {3},
	journal = {Vegetation History and Archaeobotany},
	author = {Kuneš, Petr and Pokorný, Petr and Šída, Petr},
	month = may,
	year = {2008},
	note = {[IF2007=1.076]},
	keywords = {Database, Mesolithic, Multivariate analysis, Pollen, archeology, climate change, human impact, pre-Neolithic},
	pages = {269--287},
}



@article{pelankova_relationship_2008,
	title = {The relationship of modern pollen spectra to vegetation and climate along a steppe-forest-tundra transition in southern {Siberia}, explored by decision trees},
	volume = {18},
	copyright = {All rights reserved},
	doi = {10.1177/0959683608096600},
	language = {English},
	number = {8},
	journal = {The Holocene},
	author = {Pelánková, Barbora and Kuneš, Petr and Jankovská, Vlasta and Chytrý, Milan and Ermakov, Nikolai and Svobodová-Svitavská, Helena},
	year = {2008},
	note = {[IF2007=2.343]},
	keywords = {Pollen, Siberia, Surface sample, modern analogue, pre-Neolithic},
	pages = {1259--1271},
}



@article{giesecke_towards_2014,
	title = {Towards mapping the late {Quaternary} vegetation change of {Europe}},
	volume = {23},
	copyright = {All rights reserved},
	issn = {0939-6314, 1617-6278},
	doi = {10.1007/s00334-012-0390-y},
	abstract = {The number of well-dated pollen diagrams in Europe has increased considerably over the last 30 years and many of them have been submitted to the European Pollen Database (EPD). This allows for the construction of increasingly precise maps of Holocene vegetation change across the continent. Chronological information in the EPD has been expressed in uncalibrated radiocarbon years, and most chronologies to date are based on this time scale. Here we present new chronologies for most of the datasets stored in the EPD based on calibrated radiocarbon years. Age information associated with pollen diagrams is often derived from the pollen stratigraphy itself or from other sedimentological information. We reviewed these chronological tie points and assigned uncertainties to them. The steps taken to generate the new chronologies are described and the rationale for a new classification system for age uncertainties is introduced. The resulting chronologies are fit for most continental-scale questions. They may not provide the best age model for particular sites, but may be viewed as general purpose chronologies. Taxonomic particularities of the data stored in the EPD are explained. An example is given of how the database can be queried to select samples with appropriate age control as well as the suitable taxonomic level to answer a specific research question.},
	language = {English},
	number = {1},
	urldate = {2014-01-08},
	journal = {Vegetation History and Archaeobotany},
	author = {Giesecke, Thomas and Davis, Basil and Brewer, Simon and Finsinger, Walter and Wolters, Steffen and Blaauw, Maarten and Beaulieu, Jacques-Louis de and Binney, Heather and Fyfe, Ralph M. and Gaillard, Marie-José and Gil-Romera, Graciela and Knaap, W. O. van der and Kuneš, Petr and Kühl, Norbert and Leeuwen, Jacqueline F. N. van and Leydet, Michelle and Lotter, André F. and Ortu, Elena and Semmler, Malte and Bradshaw, Richard H. W.},
	month = jan,
	year = {2014},
	note = {[IF2013=2.061]},
	keywords = {Age-depth relationships, Chronology, Database, European pollen database, climate, pollen data},
	pages = {75--86},
}



@article{jankovska_1._2007,
	title = {1. {Fláje}-{Kiefern} ({Krušné} {Hory} {Mountains}): {Late} {Glacial} and {Holocene} vegetation development},
	volume = {46},
	copyright = {All rights reserved},
	issn = {0017-3134},
	url = {http://www.informaworld.com/10.1080/00173130701526341},
	doi = {10.1080/00173130701526341},
	language = {English},
	number = {3},
	journal = {Grana},
	author = {Jankovská, Vlasta and Kuneš, Petr and van der Knaap, Willem O.},
	month = nov,
	year = {2007},
	note = {[IF2006=0.689]},
	keywords = {Czech Republic, Database, Holocene, pollen analysis, vegetation history},
	pages = {214--216},
}



@article{kunes_czech_2009,
	title = {Czech {Quaternary} {Palynological} {Database} – {PALYCZ}: review and basic statistics of the data},
	volume = {81},
	copyright = {All rights reserved},
	issn = {0032-7786},
	language = {English},
	number = {3},
	journal = {Preslia},
	author = {Kuneš, Petr and Abraham, Vojtěch and Kovářík, Oleg and Kopecký, Martin and PALYCZcontributors},
	year = {2009},
	note = {[IF2008=2.396]},
	keywords = {Czech Republic, Database, Holocene, Late Glacial, Pollen, Slovakia, numerical methods},
	pages = {209--238},
}
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April 2022.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.22498/pages.30.1.24\"\n     onclick=\"log_download('giesecke-kune-shumilovskikh-millennialscaleperspectiveonbiodiversityconservationoftheforeststeppeecotoneineurope-2022', 'http://doi.org/10.22498/pages.30.1.24', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/giesecke-kune-shumilovskikh-millennialscaleperspectiveonbiodiversityconservationoftheforeststeppeecotoneineurope-2022\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('giesecke-kune-shumilovskikh-millennialscaleperspectiveonbiodiversityconservationoftheforeststeppeecotoneineurope-2022')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{giesecke_millennial_2022,\n\ttitle = {Millennial scale perspective on biodiversity conservation of the forest-steppe ecotone in {Europe}},\n\tvolume = {30},\n\tissn = {2411605X, 24119180},\n\tdoi = {10.22498/pages.30.1.24},\n\tnumber = {1},\n\turldate = {2022-04-05},\n\tjournal = {Past Global Changes Magazine},\n\tauthor = {Giesecke, Thomas and Kuneš, Petr and Shumilovskikh, Lyudmila},\n\tmonth = apr,\n\tyear = {2022},\n\tkeywords = {conservation},\n\tpages = {24--25},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"kune-bobek-svobodovsvitavsk-varcov-ulc-turma-smrtov-dosavadnvsledkypaleoekologickchvzkumvaskmvbkupodkladyproochranuprody-2022\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Dosavadní výsledky paleoekologických výzkumů v Ašském výběžku – podklady pro ochranu přírody.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Kuneš, P.; Bobek, P.; Svobodová-Svitavská, H.; Švarcová, M. G; Šulc, V.; Šturma, J. A.;  and Smrtová, E.\n</span>\n\n  \n\n</span>\n\n  <i>Sborník muzea Karlovarského kraje</i>, 30: 131–150.  2022.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kune-bobek-svobodovsvitavsk-varcov-ulc-turma-smrtov-dosavadnvsledkypaleoekologickchvzkumvaskmvbkupodkladyproochranuprody-2022\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kune-bobek-svobodovsvitavsk-varcov-ulc-turma-smrtov-dosavadnvsledkypaleoekologickchvzkumvaskmvbkupodkladyproochranuprody-2022')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{kunes_dosavadni_2022,\n\ttitle = {Dosavadní výsledky paleoekologických výzkumů v {Ašském} výběžku – podklady pro ochranu přírody},\n\tvolume = {30},\n\tissn = {1803-6066},\n\tlanguage = {Czech},\n\tjournal = {Sborník muzea Karlovarského kraje},\n\tauthor = {Kuneš, Petr and Bobek, Přemysl and Svobodová-Svitavská, Helena and Švarcová, Markéta G and Šulc, Václav and Šturma, Jan Albert and Smrtová, Erika},\n\tyear = {2022},\n\tpages = {131--150},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"githumbi-fyfe-gaillard-trondman-mazier-nielsen-poska-sugita-etal-europeanpollenbasedrevealslandcoverreconstructionsfortheholocenemethodologymappingandpotentials-2022\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  European pollen-based REVEALS land-cover reconstructions for the Holocene: methodology, mapping and potentials.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Githumbi, E.; Fyfe, R.; Gaillard, M.; Trondman, A.; Mazier, F.; Nielsen, A.; Poska, A.; Sugita, S.; Woodbridge, J.; Azuara, J.; Feurdean, A.; Grindean, R.; Lebreton, V.; Marquer, L.; Nebout-Combourieu, N.; Stančikaitė, M.; Tanţău, I.; Tonkov, S.; Shumilovskikh, L.;  and data contributors , L.\n</span>\n\n  \n\n</span>\n\n  <i>Earth System Science Data</i>, 14(4): 1581–1619. April 2022.\n  <span class=\"note\">[IF2021=11.815; AIS2021=4.141]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.5194/essd-14-1581-2022\"\n     onclick=\"log_download('githumbi-fyfe-gaillard-trondman-mazier-nielsen-poska-sugita-etal-europeanpollenbasedrevealslandcoverreconstructionsfortheholocenemethodologymappingandpotentials-2022', 'http://doi.org/10.5194/essd-14-1581-2022', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/githumbi-fyfe-gaillard-trondman-mazier-nielsen-poska-sugita-etal-europeanpollenbasedrevealslandcoverreconstructionsfortheholocenemethodologymappingandpotentials-2022\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('githumbi-fyfe-gaillard-trondman-mazier-nielsen-poska-sugita-etal-europeanpollenbasedrevealslandcoverreconstructionsfortheholocenemethodologymappingandpotentials-2022')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{githumbi_european_2022,\n\ttitle = {European pollen-based {REVEALS} land-cover reconstructions for the {Holocene}: methodology, mapping and potentials},\n\tvolume = {14},\n\tissn = {1866-3508},\n\tshorttitle = {European pollen-based {REVEALS} land-cover reconstructions for the {Holocene}},\n\tdoi = {10.5194/essd-14-1581-2022},\n\tabstract = {{\\textless}p{\\textgreater}{\\textless}strong class=&quot;journal-contentHeaderColor&quot;{\\textgreater}Abstract.{\\textless}/strong{\\textgreater} Quantitative reconstructions of past land cover are necessary to determine the processes involved in climate–human–land-cover interactions. We present the first temporally continuous and most spatially extensive pollen-based land-cover reconstruction for Europe over the Holocene (last 11 700 cal yr BP). We describe how vegetation cover has been quantified from pollen records at a 1{\\textless}span class=&quot;inline-formula&quot;{\\textgreater}$^{\\textrm{∘}}${\\textless}/span{\\textgreater} {\\textless}span class=&quot;inline-formula&quot;{\\textgreater}×{\\textless}/span{\\textgreater} 1{\\textless}span class=&quot;inline-formula&quot;{\\textgreater}$^{\\textrm{∘}}${\\textless}/span{\\textgreater} spatial scale using the “Regional Estimates of VEgetation Abundance from Large Sites” (REVEALS) model. REVEALS calculates estimates of past regional vegetation cover in proportions or percentages. REVEALS has been applied to 1128 pollen records across Europe and part of the eastern Mediterranean–Black Sea–Caspian corridor (30–75{\\textless}span class=&quot;inline-formula&quot;{\\textgreater}$^{\\textrm{∘}}${\\textless}/span{\\textgreater} N, 25{\\textless}span class=&quot;inline-formula&quot;{\\textgreater}$^{\\textrm{∘}}${\\textless}/span{\\textgreater} W–50{\\textless}span class=&quot;inline-formula&quot;{\\textgreater}$^{\\textrm{∘}}${\\textless}/span{\\textgreater} E) to reconstruct the percentage cover of 31 plant taxa assigned to 12 plant functional types (PFTs) and 3 land-cover types (LCTs). A new synthesis of relative pollen productivities (RPPs) for European plant taxa was performed for this reconstruction. It includes multiple RPP values ({\\textless}span class=&quot;inline-formula&quot;{\\textgreater}≥2{\\textless}/span{\\textgreater} values) for 39 taxa and single values for 15 taxa (total of 54 taxa). To illustrate this, we present distribution maps for five taxa (\\textit{Calluna vulgaris}, Cerealia type (t)., \\textit{Picea abies}, deciduous \\textit{Quercus} t. and evergreen \\textit{Quercus} t.) and three land-cover types (open land, OL; evergreen trees, ETs; and summer-green trees, STs) for eight selected time windows. The reliability of the REVEALS reconstructions and issues related to the interpretation of the results in terms of landscape openness and human-induced vegetation change are discussed. This is followed by a review of the current use of this reconstruction and its future potential utility and development. REVEALS data quality are primarily determined by pollen count data (pollen count and sample, pollen identification, and chronology) and site type and number (lake or bog, large or small, one site vs. multiple sites) used for REVEALS analysis (for each grid cell). A large number of sites with high-quality pollen count data will produce more reliable land-cover estimates with lower standard errors compared to a low number of sites with lower-quality pollen count data. The REVEALS data presented here can be downloaded from {\\textless}a href=&quot;https://doi.org/10.1594/PANGAEA.937075&quot;{\\textgreater}https://doi.org/10.1594/PANGAEA.937075{\\textless}/a{\\textgreater} (Fyfe et al., 2022).{\\textless}/p{\\textgreater}},\n\tlanguage = {English},\n\tnumber = {4},\n\turldate = {2022-04-19},\n\tjournal = {Earth System Science Data},\n\tauthor = {Githumbi, Esther and Fyfe, Ralph and Gaillard, Marie-Jose and Trondman, Anna-Kari and Mazier, Florence and Nielsen, Anne-Birgitte and Poska, Anneli and Sugita, Shinya and Woodbridge, Jessie and Azuara, Julien and Feurdean, Angelica and Grindean, Roxana and Lebreton, Vincent and Marquer, Laurent and Nebout-Combourieu, Nathalie and Stančikaitė, Miglė and Tanţău, Ioan and Tonkov, Spassimir and Shumilovskikh, Lyudmila and LandClimII data contributors},\n\tmonth = apr,\n\tyear = {2022},\n\tnote = {[IF2021=11.815; AIS2021=4.141]},\n\tkeywords = {reconstruction},\n\tpages = {1581--1619},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  \\textlessp\\textgreater\\textlessstrong class=\"journal-contentHeaderColor\"\\textgreaterAbstract.\\textless/strong\\textgreater Quantitative reconstructions of past land cover are necessary to determine the processes involved in climate–human–land-cover interactions. We present the first temporally continuous and most spatially extensive pollen-based land-cover reconstruction for Europe over the Holocene (last 11 700 cal yr BP). We describe how vegetation cover has been quantified from pollen records at a 1\\textlessspan class=\"inline-formula\"\\textgreater$^{\\textrm{∘}}$\\textless/span\\textgreater \\textlessspan class=\"inline-formula\"\\textgreater×\\textless/span\\textgreater 1\\textlessspan class=\"inline-formula\"\\textgreater$^{\\textrm{∘}}$\\textless/span\\textgreater spatial scale using the “Regional Estimates of VEgetation Abundance from Large Sites” (REVEALS) model. REVEALS calculates estimates of past regional vegetation cover in proportions or percentages. REVEALS has been applied to 1128 pollen records across Europe and part of the eastern Mediterranean–Black Sea–Caspian corridor (30–75\\textlessspan class=\"inline-formula\"\\textgreater$^{\\textrm{∘}}$\\textless/span\\textgreater N, 25\\textlessspan class=\"inline-formula\"\\textgreater$^{\\textrm{∘}}$\\textless/span\\textgreater W–50\\textlessspan class=\"inline-formula\"\\textgreater$^{\\textrm{∘}}$\\textless/span\\textgreater E) to reconstruct the percentage cover of 31 plant taxa assigned to 12 plant functional types (PFTs) and 3 land-cover types (LCTs). A new synthesis of relative pollen productivities (RPPs) for European plant taxa was performed for this reconstruction. It includes multiple RPP values (\\textlessspan class=\"inline-formula\"\\textgreater≥2\\textless/span\\textgreater values) for 39 taxa and single values for 15 taxa (total of 54 taxa). To illustrate this, we present distribution maps for five taxa (<i>Calluna vulgaris</i>, Cerealia type (t)., <i>Picea abies</i>, deciduous <i>Quercus</i> t. and evergreen <i>Quercus</i> t.) and three land-cover types (open land, OL; evergreen trees, ETs; and summer-green trees, STs) for eight selected time windows. The reliability of the REVEALS reconstructions and issues related to the interpretation of the results in terms of landscape openness and human-induced vegetation change are discussed. This is followed by a review of the current use of this reconstruction and its future potential utility and development. REVEALS data quality are primarily determined by pollen count data (pollen count and sample, pollen identification, and chronology) and site type and number (lake or bog, large or small, one site vs. multiple sites) used for REVEALS analysis (for each grid cell). A large number of sites with high-quality pollen count data will produce more reliable land-cover estimates with lower standard errors compared to a low number of sites with lower-quality pollen count data. The REVEALS data presented here can be downloaded from \\textlessa href=\"https://doi.org/10.1594/PANGAEA.937075\"\\textgreaterhttps://doi.org/10.1594/PANGAEA.937075\\textless/a\\textgreater (Fyfe et al., 2022).\\textless/p\\textgreater\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"schafstall-kuosmanen-kune-svobodov-svitok-chiverrell-halsall-fleischer-etal-subfossilbarkbeetlesasindicatorsofpastdisturbanceeventsintemperatepiceaabiesmountainforests-2022\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Sub-fossil bark beetles as indicators of past disturbance events in temperate Picea abies mountain forests.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Schafstall, N.; Kuosmanen, N.; Kuneš, P.; Svobodová, H. S.; Svitok, M.; Chiverrell, R. C.; Halsall, K.; Fleischer, P.; Knížek, M.;  and Clear, J. L.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Science Reviews</i>, 275: 107289. January 2022.\n  <span class=\"note\">[IF2021=4.456;AIS2021=1.586]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quascirev.2021.107289\"\n     onclick=\"log_download('schafstall-kuosmanen-kune-svobodov-svitok-chiverrell-halsall-fleischer-etal-subfossilbarkbeetlesasindicatorsofpastdisturbanceeventsintemperatepiceaabiesmountainforests-2022', 'http://doi.org/10.1016/j.quascirev.2021.107289', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/schafstall-kuosmanen-kune-svobodov-svitok-chiverrell-halsall-fleischer-etal-subfossilbarkbeetlesasindicatorsofpastdisturbanceeventsintemperatepiceaabiesmountainforests-2022\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('schafstall-kuosmanen-kune-svobodov-svitok-chiverrell-halsall-fleischer-etal-subfossilbarkbeetlesasindicatorsofpastdisturbanceeventsintemperatepiceaabiesmountainforests-2022')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{schafstall_sub-fossil_2022,\n\ttitle = {Sub-fossil bark beetles as indicators of past disturbance events in temperate {Picea} abies mountain forests},\n\tvolume = {275},\n\tissn = {0277-3791},\n\tdoi = {10.1016/j.quascirev.2021.107289},\n\tabstract = {Temperate mountain forests have experienced an increase in frequency and severity of natural disturbances (e.g., droughts, fires, windstorms and insect outbreaks) in recent decades due to climate and environmental change. Outbreaks of bark beetles have caused significant dieback of conifer forests in Central Europe and it is essential to model and predict the potential severity of future bark beetle outbreaks. However, to predict future bark beetle activity, historical baseline information is required to contextualize the magnitude of current and potential future outbreaks. A fossil beetle record from a forest hollow in the Tatra Mountains, Slovakia; one of the best-preserved national parks in Central Europe, was produced to identify insect outbreaks during the last millennia. Sub-fossil bark beetle remains were compared with parallel pollen and charcoal to assess whether peaks in conifer bark beetle remains correspond with indications of disturbance documented in historical or sedimentary fossil records. Three peaks in bark beetle remains were detected (1) post-2004, (2) AD 1140–1440, and (3) AD 930–1030. The abundance of species Pityogenes chalcographus and Pityophthorus pityographus in the two top samples can be linked directly to large bark beetle outbreaks in the High Tatra Mountains after 2004. P. chalcographus and P. pityographus are also the abundant species in the second peak (AD 1140–1440) while the third peak (AD 930–1030) consists of the species Polygraphus poligraphus. The most prominent conifer bark beetle in Central Europe, Ips typographus, was found to be present in most of the samples but always at very low numbers. It is plausible that P. chalcographus and P. pityographus fossils might be useful proxies for past conifer bark beetle outbreaks in Central Europe, as they occur together with fossils of I. typographus but appear to be well-preserved. A significant correlation was found between primary bark beetles and macroscopic charcoal densities in the sediment, highlighting the complex interactions between disturbance agents, bark beetles and fire, in this long-term regime of natural disturbances. Our 1400-year disturbance record shows how bark beetle outbreaks have been an important component of the regional natural disturbance regime for over a millennium and have intensified with increasing anthropogenic activity. Bark beetle outbreaks are likely one of the drivers promoting the future ecological stability of the temperate conifer ecosystem over decades to centuries.},\n\tlanguage = {English},\n\turldate = {2021-11-29},\n\tjournal = {Quaternary Science Reviews},\n\tauthor = {Schafstall, Nick and Kuosmanen, Niina and Kuneš, Petr and Svobodová, Helena Svitavská and Svitok, Marek and Chiverrell, Richard C. and Halsall, Karen and Fleischer, Peter and Knížek, Miloš and Clear, Jennifer L.},\n\tmonth = jan,\n\tyear = {2022},\n\tnote = {[IF2021=4.456;AIS2021=1.586]},\n\tkeywords = {Bark beetle outbreaks, Central Europe, Disturbance history, Ecosystem services, Fire, Fossil proxies, High Tatra mountains, disturbance},\n\tpages = {107289},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Temperate mountain forests have experienced an increase in frequency and severity of natural disturbances (e.g., droughts, fires, windstorms and insect outbreaks) in recent decades due to climate and environmental change. Outbreaks of bark beetles have caused significant dieback of conifer forests in Central Europe and it is essential to model and predict the potential severity of future bark beetle outbreaks. However, to predict future bark beetle activity, historical baseline information is required to contextualize the magnitude of current and potential future outbreaks. A fossil beetle record from a forest hollow in the Tatra Mountains, Slovakia; one of the best-preserved national parks in Central Europe, was produced to identify insect outbreaks during the last millennia. Sub-fossil bark beetle remains were compared with parallel pollen and charcoal to assess whether peaks in conifer bark beetle remains correspond with indications of disturbance documented in historical or sedimentary fossil records. Three peaks in bark beetle remains were detected (1) post-2004, (2) AD 1140–1440, and (3) AD 930–1030. The abundance of species Pityogenes chalcographus and Pityophthorus pityographus in the two top samples can be linked directly to large bark beetle outbreaks in the High Tatra Mountains after 2004. P. chalcographus and P. pityographus are also the abundant species in the second peak (AD 1140–1440) while the third peak (AD 930–1030) consists of the species Polygraphus poligraphus. The most prominent conifer bark beetle in Central Europe, Ips typographus, was found to be present in most of the samples but always at very low numbers. It is plausible that P. chalcographus and P. pityographus fossils might be useful proxies for past conifer bark beetle outbreaks in Central Europe, as they occur together with fossils of I. typographus but appear to be well-preserved. A significant correlation was found between primary bark beetles and macroscopic charcoal densities in the sediment, highlighting the complex interactions between disturbance agents, bark beetles and fire, in this long-term regime of natural disturbances. Our 1400-year disturbance record shows how bark beetle outbreaks have been an important component of the regional natural disturbance regime for over a millennium and have intensified with increasing anthropogenic activity. Bark beetle outbreaks are likely one of the drivers promoting the future ecological stability of the temperate conifer ecosystem over decades to centuries.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"mariani-connor-theuerkauf-herbert-kune-bowman-fletcher-head-etal-disruptionofculturalburningpromotesshrubencroachmentandunprecedentedwildfires-2022\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Disruption of cultural burning promotes shrub encroachment and unprecedented wildfires.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Mariani, M.; Connor, S. E; Theuerkauf, M.; Herbert, A.; Kuneš, P.; Bowman, D.; Fletcher, M.; Head, L.; Kershaw, A P.; Haberle, S. G; Stevenson, J.; Adeleye, M.; Cadd, H.; Hopf, F.;  and Briles, C.\n</span>\n\n  \n\n</span>\n\n  <i>Frontiers in Ecology and the Environment</i>, 20(5): 292–300.  2022.\n  <span class=\"note\">[IF2021=13.789;AIS2021=4.071]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1002/fee.2395\"\n     onclick=\"log_download('mariani-connor-theuerkauf-herbert-kune-bowman-fletcher-head-etal-disruptionofculturalburningpromotesshrubencroachmentandunprecedentedwildfires-2022', 'http://doi.org/10.1002/fee.2395', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/mariani-connor-theuerkauf-herbert-kune-bowman-fletcher-head-etal-disruptionofculturalburningpromotesshrubencroachmentandunprecedentedwildfires-2022\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('mariani-connor-theuerkauf-herbert-kune-bowman-fletcher-head-etal-disruptionofculturalburningpromotesshrubencroachmentandunprecedentedwildfires-2022')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{mariani_disruption_2022,\n\ttitle = {Disruption of cultural burning promotes shrub encroachment and unprecedented wildfires},\n\tvolume = {20},\n\tissn = {1540-9309},\n\tdoi = {10.1002/fee.2395},\n\tabstract = {Recent catastrophic fires in Australia and North America have raised broad-scale questions about how the cessation of Indigenous burning practices has impacted fuel accumulation and structure. For sustainable coexistence with fire, a better understanding of the ancient nexus between humans and flammable landscapes is needed. We used novel palaeoecological modeling and charcoal compilations to reassess evidence for changes in land cover and fire activity, focusing on southeast Australia before and after British colonization. Here, we provide what we believe is the first quantitative evidence that the region’s forests and woodlands contained fewer shrubs and more grass before colonization. Changes in vegetation, fuel structures, and connectivity followed different trajectories in different vegetation types. The pattern is best explained by the disruption of Indigenous vegetation management caused by European settlement. Combined with climate-change impacts on fire weather and drought, the widespread absence of Indigenous fire management practices likely preconditioned fire-prone regions for wildfires of unprecedented extent.},\n\tlanguage = {English},\n\tnumber = {5},\n\turldate = {2022-06-22},\n\tjournal = {Frontiers in Ecology and the Environment},\n\tauthor = {Mariani, Michela and Connor, Simon E and Theuerkauf, Martin and Herbert, Annika and Kuneš, Petr and Bowman, David and Fletcher, Michael-Shawn and Head, Lesley and Kershaw, A Peter and Haberle, Simon G and Stevenson, Janelle and Adeleye, Matthew and Cadd, Haidee and Hopf, Feli and Briles, Christy},\n\tyear = {2022},\n\tnote = {[IF2021=13.789;AIS2021=4.071]},\n\tkeywords = {disturbance, reconstruction},\n\tpages = {292--300},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Recent catastrophic fires in Australia and North America have raised broad-scale questions about how the cessation of Indigenous burning practices has impacted fuel accumulation and structure. For sustainable coexistence with fire, a better understanding of the ancient nexus between humans and flammable landscapes is needed. We used novel palaeoecological modeling and charcoal compilations to reassess evidence for changes in land cover and fire activity, focusing on southeast Australia before and after British colonization. Here, we provide what we believe is the first quantitative evidence that the region’s forests and woodlands contained fewer shrubs and more grass before colonization. Changes in vegetation, fuel structures, and connectivity followed different trajectories in different vegetation types. The pattern is best explained by the disruption of Indigenous vegetation management caused by European settlement. Combined with climate-change impacts on fire weather and drought, the widespread absence of Indigenous fire management practices likely preconditioned fire-prone regions for wildfires of unprecedented extent.\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2021\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2021')\"\n      onkeypress=\"toggleGroup('group_2021')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2021</span>\n      <span class=\"bibbase_group_count\">\n        \n        (3)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"moravcov-tich-carter-vondrk-tvrtlkov-vanleeuwen-heurich-tinner-etal-mountainaquaticiisotesipopulationsreflectmillennialscaleenvironmentalchangesinthebohemianforestecosystemcentraleurope-2021\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Mountain aquatic <i>Isoëtes</i> populations reflect millennial-scale environmental changes in the Bohemian Forest Ecosystem, Central Europe.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Moravcová, A.; Tichá, A.; Carter, V. A; Vondrák, D.; Čtvrtlíková, M.; van Leeuwen, J. F.; Heurich, M.; Tinner, W.;  and Kuneš, P.\n</span>\n\n  \n\n</span>\n\n  <i>The Holocene</i>, 31(5): 746–759. May 2021.\n  <span class=\"note\">[IF2020=2.769]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1177/0959683620988060\"\n     onclick=\"log_download('moravcov-tich-carter-vondrk-tvrtlkov-vanleeuwen-heurich-tinner-etal-mountainaquaticiisotesipopulationsreflectmillennialscaleenvironmentalchangesinthebohemianforestecosystemcentraleurope-2021', 'http://doi.org/10.1177/0959683620988060', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/moravcov-tich-carter-vondrk-tvrtlkov-vanleeuwen-heurich-tinner-etal-mountainaquaticiisotesipopulationsreflectmillennialscaleenvironmentalchangesinthebohemianforestecosystemcentraleurope-2021\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('moravcov-tich-carter-vondrk-tvrtlkov-vanleeuwen-heurich-tinner-etal-mountainaquaticiisotesipopulationsreflectmillennialscaleenvironmentalchangesinthebohemianforestecosystemcentraleurope-2021')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{moravcova_mountain_2021,\n\ttitle = {Mountain aquatic \\textit{{Isoëtes}} populations reflect millennial-scale environmental changes in the {Bohemian} {Forest} {Ecosystem}, {Central} {Europe}},\n\tvolume = {31},\n\tissn = {0959-6836},\n\tdoi = {10.1177/0959683620988060},\n\tabstract = {In this study we aim to investigate millennial-scale dynamics of Isoëtes, a type of macrophyte well adapted to oligotrophic and clear-water lakes. Despite its wide distribution during the Early Holocene, nowadays Isoëtes is considered as vulnerable or critically endangered in many Central European countries. Using a multi-proxy palaeoecological reconstruction involving Isoëtes micro- and megaspores, pollen, plant macrofossils, macro-charcoal, diatoms and chironomids from four lakes (Prášilské jezero, Plešné jezero, Černé jezero, Rachelsee) located in the Bohemian Forest Ecosystem mountain region in Central Europe, we reconstruct Isoëtes dynamics and discuss how local environmental factors impacted its distribution and abundance during the Holocene. Our results show regionally concurrent patterns of Isoëtes colonisation across all lakes beginning 10,300–9300 cal yr BP, and substantially declining around 6400 cal yr BP. Results from Prášilské jezero imply that Isoëtes decline and collapse in this lake reflect gradual dystrophication that led to the browning of lake water. This is evidenced by a shift in diatom assemblages towards more acidophilous taxa dominated by Asterionella ralfsii and by a decrease in total chironomid abundance and taxa sensitive to low oxygen levels. Dystrophication of Prášilské jezero was linked with the immigration of the late-successional tree taxa (Picea abies and later Fagus sylvatica and Abies alba), peatland expansion, and decreasing fire activity. Multi-site comparison of pollen records suggest that these vegetation-related environmental changes were common for the whole region. Our study demonstrates the sensitivity of Isoëtes to millennial-scale natural environmental changes within the surrounding lake catchment.},\n\tlanguage = {English},\n\tnumber = {5},\n\turldate = {2021-05-17},\n\tjournal = {The Holocene},\n\tauthor = {Moravcová, Alice and Tichá, Anna and Carter, Vachel A and Vondrák, Daniel and Čtvrtlíková, Martina and van Leeuwen, Jacqueline FN and Heurich, Marco and Tinner, Willy and Kuneš, Petr},\n\tmonth = may,\n\tyear = {2021},\n\tnote = {[IF2020=2.769]},\n\tkeywords = {disturbance, fire regime, lake dystrophy, podzolisation, quillwort decline, thermal stratification, vegetation change},\n\tpages = {746--759},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  In this study we aim to investigate millennial-scale dynamics of Isoëtes, a type of macrophyte well adapted to oligotrophic and clear-water lakes. Despite its wide distribution during the Early Holocene, nowadays Isoëtes is considered as vulnerable or critically endangered in many Central European countries. Using a multi-proxy palaeoecological reconstruction involving Isoëtes micro- and megaspores, pollen, plant macrofossils, macro-charcoal, diatoms and chironomids from four lakes (Prášilské jezero, Plešné jezero, Černé jezero, Rachelsee) located in the Bohemian Forest Ecosystem mountain region in Central Europe, we reconstruct Isoëtes dynamics and discuss how local environmental factors impacted its distribution and abundance during the Holocene. Our results show regionally concurrent patterns of Isoëtes colonisation across all lakes beginning 10,300–9300 cal yr BP, and substantially declining around 6400 cal yr BP. Results from Prášilské jezero imply that Isoëtes decline and collapse in this lake reflect gradual dystrophication that led to the browning of lake water. This is evidenced by a shift in diatom assemblages towards more acidophilous taxa dominated by Asterionella ralfsii and by a decrease in total chironomid abundance and taxa sensitive to low oxygen levels. Dystrophication of Prášilské jezero was linked with the immigration of the late-successional tree taxa (Picea abies and later Fagus sylvatica and Abies alba), peatland expansion, and decreasing fire activity. Multi-site comparison of pollen records suggest that these vegetation-related environmental changes were common for the whole region. Our study demonstrates the sensitivity of Isoëtes to millennial-scale natural environmental changes within the surrounding lake catchment.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"hostinsk-kune-hadrava-bosch-scaramozzino-bogusch-comparativebiologyoffourrhodanthidiumspecieshymenopteramegachilidaethatnestinsnailshells-2021\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Comparative biology of four Rhodanthidium species (Hymenoptera, Megachilidae) that nest in snail shells.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Hostinská, L.; Kuneš, P.; Hadrava, J.; Bosch, J.; Scaramozzino, P. L.;  and Bogusch, P.\n</span>\n\n  \n\n</span>\n\n  <i>Journal of Hymenoptera Research</i>, 85: 11–28. August 2021.\n  <span class=\"note\">[IF2020=1.733]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.3897/jhr.85.66544\"\n     onclick=\"log_download('hostinsk-kune-hadrava-bosch-scaramozzino-bogusch-comparativebiologyoffourrhodanthidiumspecieshymenopteramegachilidaethatnestinsnailshells-2021', 'http://doi.org/10.3897/jhr.85.66544', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/hostinsk-kune-hadrava-bosch-scaramozzino-bogusch-comparativebiologyoffourrhodanthidiumspecieshymenopteramegachilidaethatnestinsnailshells-2021\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('hostinsk-kune-hadrava-bosch-scaramozzino-bogusch-comparativebiologyoffourrhodanthidiumspecieshymenopteramegachilidaethatnestinsnailshells-2021')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{hostinska_comparative_2021,\n\ttitle = {Comparative biology of four {Rhodanthidium} species ({Hymenoptera}, {Megachilidae}) that nest in snail shells},\n\tvolume = {85},\n\tissn = {1314-2607},\n\tdoi = {10.3897/jhr.85.66544},\n\tabstract = {Some species of two tribes (Anthidiini and Osmiini) of the bee family Megachilidae utilize empty gastropod shells as nesting cavities. While snail-nesting Osmiini have been more frequently studied and the nesting biology of several species is well-known, much less is known about the habits of snail-nesting Anthidiini. We collected nests of four species of the genus Rhodanthidium (R. septemdentatum, R. sticticum, R. siculum and R. infuscatum) in the Czech Republic, Slovakia, Catalonia (Spain) and Sicily (Italy). We dissected these nests in the laboratory and documented their structure, pollen sources and nest associates. The four species usually choose large snail shells. All four species close their nests with a plug made of resin, sand and fragments of snail shells. However, nests of the four species can be distinguished based on the presence (R. septemdentatum, R. sticticum) or absence (R. siculum, R. infuscatum) of mineral and plant debris in the vestibular space, and the presence (R. septemdentatum, R. infuscatum) or absence (R. sticticum, R. siculum) of a resin partition between the vestibular space and the brood cell. Rhodanthidium septemdentatum, R. sticticum and R. siculum usually build a single brood cell per nest, but all R. infuscatum nests studied contained two or more cells. For three of the species (R. siculum, R. septemdentatum and R. sticticum) we confirmed overwintering in the adult stage. Contrary to R. siculum, R. septemdentatum and R. sticticum do not hide their nest shells and usually use shells under the stones or hidden in crevices within stone walls. Nest associates were very infrequent. We only found two R. sticticum nests parasitized by the chrysidid wasp Chrysura refulgens and seven nests infested with pollen mites Chaetodactylus cf. anthidii. Our pollen analyses confirm that Rhodanthidium are polylectic but show a preference for Fabaceae by R. sticticum.},\n\tlanguage = {English},\n\turldate = {2021-09-01},\n\tjournal = {Journal of Hymenoptera Research},\n\tauthor = {Hostinská, Lucie and Kuneš, Petr and Hadrava, Jiří and Bosch, Jordi and Scaramozzino, Pier Luigi and Bogusch, Petr},\n\tmonth = aug,\n\tyear = {2021},\n\tnote = {[IF2020=1.733]},\n\tpages = {11--28},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Some species of two tribes (Anthidiini and Osmiini) of the bee family Megachilidae utilize empty gastropod shells as nesting cavities. While snail-nesting Osmiini have been more frequently studied and the nesting biology of several species is well-known, much less is known about the habits of snail-nesting Anthidiini. We collected nests of four species of the genus Rhodanthidium (R. septemdentatum, R. sticticum, R. siculum and R. infuscatum) in the Czech Republic, Slovakia, Catalonia (Spain) and Sicily (Italy). We dissected these nests in the laboratory and documented their structure, pollen sources and nest associates. The four species usually choose large snail shells. All four species close their nests with a plug made of resin, sand and fragments of snail shells. However, nests of the four species can be distinguished based on the presence (R. septemdentatum, R. sticticum) or absence (R. siculum, R. infuscatum) of mineral and plant debris in the vestibular space, and the presence (R. septemdentatum, R. infuscatum) or absence (R. sticticum, R. siculum) of a resin partition between the vestibular space and the brood cell. Rhodanthidium septemdentatum, R. sticticum and R. siculum usually build a single brood cell per nest, but all R. infuscatum nests studied contained two or more cells. For three of the species (R. siculum, R. septemdentatum and R. sticticum) we confirmed overwintering in the adult stage. Contrary to R. siculum, R. septemdentatum and R. sticticum do not hide their nest shells and usually use shells under the stones or hidden in crevices within stone walls. Nest associates were very infrequent. We only found two R. sticticum nests parasitized by the chrysidid wasp Chrysura refulgens and seven nests infested with pollen mites Chaetodactylus cf. anthidii. Our pollen analyses confirm that Rhodanthidium are polylectic but show a preference for Fabaceae by R. sticticum.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"mottl-flantua-bhatta-felde-giesecke-goring-grimm-haberle-etal-globalaccelerationinratesofvegetationchangeoverthepast18000years-2021\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://science.sciencemag.org/content/372/6544/860\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'mottl-flantua-bhatta-felde-giesecke-goring-grimm-haberle-etal-globalaccelerationinratesofvegetationchangeoverthepast18000years-2021', 'https://science.sciencemag.org/content/372/6544/860', event);\">\n    Global acceleration in rates of vegetation change over the past 18,000 years.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Mottl, O.; Flantua, S. G. A.; Bhatta, K. P.; Felde, V. A.; Giesecke, T.; Goring, S.; Grimm, E. C.; Haberle, S.; Hooghiemstra, H.; Ivory, S.; Kuneš, P.; Wolters, S.; Seddon, A. W. R.;  and Williams, J. W.\n</span>\n\n  \n\n</span>\n\n  <i>Science</i>, 372(6544): 860–864. May 2021.\n  <span class=\"note\">[IF2020=47.728]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://science.sciencemag.org/content/372/6544/860\"\n     onclick=\"log_download('mottl-flantua-bhatta-felde-giesecke-goring-grimm-haberle-etal-globalaccelerationinratesofvegetationchangeoverthepast18000years-2021', 'https://science.sciencemag.org/content/372/6544/860', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Global acceleration in rates of vegetation change over the past 18,000 years [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1126/science.abg1685\"\n     onclick=\"log_download('mottl-flantua-bhatta-felde-giesecke-goring-grimm-haberle-etal-globalaccelerationinratesofvegetationchangeoverthepast18000years-2021', 'http://doi.org/10.1126/science.abg1685', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/mottl-flantua-bhatta-felde-giesecke-goring-grimm-haberle-etal-globalaccelerationinratesofvegetationchangeoverthepast18000years-2021\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('mottl-flantua-bhatta-felde-giesecke-goring-grimm-haberle-etal-globalaccelerationinratesofvegetationchangeoverthepast18000years-2021')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{mottl_global_2021,\n\ttitle = {Global acceleration in rates of vegetation change over the past 18,000 years},\n\tvolume = {372},\n\tissn = {0036-8075, 1095-9203},\n\turl = {https://science.sciencemag.org/content/372/6544/860},\n\tdoi = {10.1126/science.abg1685},\n\tabstract = {The pace of Holocene vegetation change\nAlthough much is known about the rapid environmental changes that have occurred since the Industrial Revolution, the patterns of change over the preceding millennia have been only patchily understood. Using a global set of {\\textgreater}1100 fossil pollen records, Mottl et al. explored the rates of vegetation change over the past 18,000 years (see the Perspective by Overpeck and Breshears). The authors show that the rates of change accelerated markedly during the Late Holocene (∼4.6 to 2.9 thousand years ago), even more rapidly than the climate-driven vegetation changes associated with the end of the last glacial period. In addition, the Late Holocene acceleration began for terrestrial communities as a whole, suggesting that the acceleration in turnover over the past two centuries is the tip of a deeper trend.\nScience, abg1685, this issue p. 860; see also abi9902, p. 786\nGlobal vegetation over the past 18,000 years has been transformed first by the climate changes that accompanied the last deglaciation and again by increasing human pressures; however, the magnitude and patterns of rates of vegetation change are poorly understood globally. Using a compilation of 1181 fossil pollen sequences and newly developed statistical methods, we detect a worldwide acceleration in the rates of vegetation compositional change beginning between 4.6 and 2.9 thousand years ago that is globally unprecedented over the past 18,000 years in both magnitude and extent. Late Holocene rates of change equal or exceed the deglacial rates for all continents, which suggests that the scale of human effects on terrestrial ecosystems exceeds even the climate-driven transformations of the last deglaciation. The acceleration of biodiversity change demonstrated in ecological datasets from the past century began millennia ago.\nA compilation of fossil pollen sequences shows that the acceleration of biodiversity change began millennia ago.\nA compilation of fossil pollen sequences shows that the acceleration of biodiversity change began millennia ago.},\n\tlanguage = {English},\n\tnumber = {6544},\n\turldate = {2021-05-20},\n\tjournal = {Science},\n\tauthor = {Mottl, Ondřej and Flantua, Suzette G. A. and Bhatta, Kuber P. and Felde, Vivian A. and Giesecke, Thomas and Goring, Simon and Grimm, Eric C. and Haberle, Simon and Hooghiemstra, Henry and Ivory, Sarah and Kuneš, Petr and Wolters, Steffen and Seddon, Alistair W. R. and Williams, John W.},\n\tmonth = may,\n\tyear = {2021},\n\tnote = {[IF2020=47.728]},\n\tkeywords = {Database, reconstruction},\n\tpages = {860--864},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The pace of Holocene vegetation change Although much is known about the rapid environmental changes that have occurred since the Industrial Revolution, the patterns of change over the preceding millennia have been only patchily understood. Using a global set of \\textgreater1100 fossil pollen records, Mottl et al. explored the rates of vegetation change over the past 18,000 years (see the Perspective by Overpeck and Breshears). The authors show that the rates of change accelerated markedly during the Late Holocene (∼4.6 to 2.9 thousand years ago), even more rapidly than the climate-driven vegetation changes associated with the end of the last glacial period. In addition, the Late Holocene acceleration began for terrestrial communities as a whole, suggesting that the acceleration in turnover over the past two centuries is the tip of a deeper trend. Science, abg1685, this issue p. 860; see also abi9902, p. 786 Global vegetation over the past 18,000 years has been transformed first by the climate changes that accompanied the last deglaciation and again by increasing human pressures; however, the magnitude and patterns of rates of vegetation change are poorly understood globally. Using a compilation of 1181 fossil pollen sequences and newly developed statistical methods, we detect a worldwide acceleration in the rates of vegetation compositional change beginning between 4.6 and 2.9 thousand years ago that is globally unprecedented over the past 18,000 years in both magnitude and extent. Late Holocene rates of change equal or exceed the deglacial rates for all continents, which suggests that the scale of human effects on terrestrial ecosystems exceeds even the climate-driven transformations of the last deglaciation. The acceleration of biodiversity change demonstrated in ecological datasets from the past century began millennia ago. A compilation of fossil pollen sequences shows that the acceleration of biodiversity change began millennia ago. A compilation of fossil pollen sequences shows that the acceleration of biodiversity change began millennia ago.\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2020\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2020')\"\n      onkeypress=\"toggleGroup('group_2020')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2020</span>\n      <span class=\"bibbase_group_count\">\n        \n        (8)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"roleek-svitavsksvobodov-jamrichov-dudov-hjkov-kletetschka-kune-abraham-conservationtargetsfromtheperspectiveofapalaeoecologicalreconstructionthecasestudyofdkopeatbogintheczechrepublic-2020\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Conservation targets from the perspective of a palaeoecological reconstruction: the case study of Dářko peat bog in the Czech Republic.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Roleček, J.; Svitavská Svobodová, H.; Jamrichová, E.; Dudová, L.; Hájková, P.; Kletetschka, G.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>;  and Abraham, V.\n</span>\n\n  \n\n</span>\n\n  <i>Preslia</i>, 92(2): 87–114.  2020.\n  <span class=\"note\">[IF2019=4.357]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.23855/preslia.2020.087\"\n     onclick=\"log_download('roleek-svitavsksvobodov-jamrichov-dudov-hjkov-kletetschka-kune-abraham-conservationtargetsfromtheperspectiveofapalaeoecologicalreconstructionthecasestudyofdkopeatbogintheczechrepublic-2020', 'http://doi.org/10.23855/preslia.2020.087', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/roleek-svitavsksvobodov-jamrichov-dudov-hjkov-kletetschka-kune-abraham-conservationtargetsfromtheperspectiveofapalaeoecologicalreconstructionthecasestudyofdkopeatbogintheczechrepublic-2020\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>2 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('roleek-svitavsksvobodov-jamrichov-dudov-hjkov-kletetschka-kune-abraham-conservationtargetsfromtheperspectiveofapalaeoecologicalreconstructionthecasestudyofdkopeatbogintheczechrepublic-2020')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{rolecek_conservation_2020,\n\ttitle = {Conservation targets from the perspective of a palaeoecological reconstruction: the case study of {Dářko} peat bog in the {Czech} {Republic}},\n\tvolume = {92},\n\tdoi = {10.23855/preslia.2020.087},\n\tlanguage = {English},\n\tnumber = {2},\n\tjournal = {Preslia},\n\tauthor = {Roleček, Jan and Svitavská Svobodová, Helena and Jamrichová, Eva and Dudová, Lydie and Hájková, Petra and Kletetschka, Günther and Kuneš, Petr and Abraham, Vojtěch},\n\tyear = {2020},\n\tnote = {[IF2019=4.357]},\n\tkeywords = {conservation},\n\tpages = {87--114},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"schafstall-whitehouse-kuosmanen-svobodovsvitavsk-saulnier-chiverrell-fleischer-kune-etal-changesinspeciescompositionanddiversityofamontanebeetlecommunityoverthelastmillenniuminthehightatrasslovakiaimplicationsforforestconservationandmanagement-2020\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Changes in species composition and diversity of a montane beetle community over the last millennium in the High Tatras, Slovakia: Implications for forest conservation and management.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Schafstall, N.; Whitehouse, N.; Kuosmanen, N.; Svobodová-Svitavská, H.; Saulnier, M.; Chiverrell, R. C.; Fleischer, P.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>;  and Clear, J. L.\n</span>\n\n  \n\n</span>\n\n  <i>Palaeogeography, Palaeoclimatology, Palaeoecology</i>, 555: 109834. October 2020.\n  <span class=\"note\">[IF2019=2.833]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.palaeo.2020.109834\"\n     onclick=\"log_download('schafstall-whitehouse-kuosmanen-svobodovsvitavsk-saulnier-chiverrell-fleischer-kune-etal-changesinspeciescompositionanddiversityofamontanebeetlecommunityoverthelastmillenniuminthehightatrasslovakiaimplicationsforforestconservationandmanagement-2020', 'http://doi.org/10.1016/j.palaeo.2020.109834', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/schafstall-whitehouse-kuosmanen-svobodovsvitavsk-saulnier-chiverrell-fleischer-kune-etal-changesinspeciescompositionanddiversityofamontanebeetlecommunityoverthelastmillenniuminthehightatrasslovakiaimplicationsforforestconservationandmanagement-2020\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>2 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('schafstall-whitehouse-kuosmanen-svobodovsvitavsk-saulnier-chiverrell-fleischer-kune-etal-changesinspeciescompositionanddiversityofamontanebeetlecommunityoverthelastmillenniuminthehightatrasslovakiaimplicationsforforestconservationandmanagement-2020')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{schafstall_changes_2020,\n\ttitle = {Changes in species composition and diversity of a montane beetle community over the last millennium in the {High} {Tatras}, {Slovakia}: {Implications} for forest conservation and management},\n\tvolume = {555},\n\tissn = {0031-0182},\n\tshorttitle = {Changes in species composition and diversity of a montane beetle community over the last millennium in the {High} {Tatras}, {Slovakia}},\n\tdoi = {10.1016/j.palaeo.2020.109834},\n\tabstract = {Montane biomes are niche environments high in biodiversity with a variety of habitats. Often isolated, these non-continuous remnant ecosystems inhabit narrow ecological zones putting them under threat from changing climatic conditions and anthropogenic pressure. Twelve sediment cores were retrieved from a peat bog in Tatra National Park, Slovakia, and correlated to each other by wiggle-matching geochemical signals derived from micro-XRF scanning, to make a reconstruction of past conditions. A fossil beetle (Coleoptera) record, covering the last 1000 years at 50- to 100-year resolution, gives a new insight into changing flora and fauna in this region. Our findings reveal a diverse beetle community with varied ecological groups inhabiting a range of forest, meadow and synanthropic habitats. Changes in the beetle community were related to changes in the landscape, driven by anthropogenic activities. The first clear evidence for human activity in the area occurs c. 1250 CE and coincides with the arrival of beetle species living on the dung of domesticated animals (e.g. Aphodius spp.). From 1500 CE, human (re)settlement, and activities such as pasturing and charcoal burning, appear to have had a pronounced effect on the beetle community. Local beetle diversity declined steadily towards the present day, likely due to an infilling of the forest hollow leading to a decrease in moisture level. We conclude that beetle communities are directly affected by anthropogenic intensity and land-use change. When aiming to preserve or restore natural forest conditions, recording their past changes in diversity can help guide conservation and restoration. In doing so, it is important to look back beyond the time of significant human impact, and for this, information contained in paleoecological records is irreplaceable.},\n\tlanguage = {English},\n\turldate = {2020-06-20},\n\tjournal = {Palaeogeography, Palaeoclimatology, Palaeoecology},\n\tauthor = {Schafstall, Nick and Whitehouse, Nicki and Kuosmanen, Niina and Svobodová-Svitavská, Helena and Saulnier, Mélanie and Chiverrell, Richard C. and Fleischer, Peter and Kuneš, Petr and Clear, Jennifer L.},\n\tmonth = oct,\n\tyear = {2020},\n\tnote = {[IF2019=2.833]},\n\tkeywords = {Biodiversity, Central Europe, Climate change, Coleoptera, Human impact, Nature conservation, disturbance},\n\tpages = {109834},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Montane biomes are niche environments high in biodiversity with a variety of habitats. Often isolated, these non-continuous remnant ecosystems inhabit narrow ecological zones putting them under threat from changing climatic conditions and anthropogenic pressure. Twelve sediment cores were retrieved from a peat bog in Tatra National Park, Slovakia, and correlated to each other by wiggle-matching geochemical signals derived from micro-XRF scanning, to make a reconstruction of past conditions. A fossil beetle (Coleoptera) record, covering the last 1000 years at 50- to 100-year resolution, gives a new insight into changing flora and fauna in this region. Our findings reveal a diverse beetle community with varied ecological groups inhabiting a range of forest, meadow and synanthropic habitats. Changes in the beetle community were related to changes in the landscape, driven by anthropogenic activities. The first clear evidence for human activity in the area occurs c. 1250 CE and coincides with the arrival of beetle species living on the dung of domesticated animals (e.g. Aphodius spp.). From 1500 CE, human (re)settlement, and activities such as pasturing and charcoal burning, appear to have had a pronounced effect on the beetle community. Local beetle diversity declined steadily towards the present day, likely due to an infilling of the forest hollow leading to a decrease in moisture level. We conclude that beetle communities are directly affected by anthropogenic intensity and land-use change. When aiming to preserve or restore natural forest conditions, recording their past changes in diversity can help guide conservation and restoration. In doing so, it is important to look back beyond the time of significant human impact, and for this, information contained in paleoecological records is irreplaceable.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"kuosmanen-ada-halsall-chiverrell-schafstall-kune-boyle-knek-etal-integrationofdendrochronologicalandpalaeoecologicaldisturbancereconstructionsintemperatemountainforests-2020\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Integration of dendrochronological and palaeoecological disturbance reconstructions in temperate mountain forests.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Kuosmanen, N.; Čada, V.; Halsall, K.; Chiverrell, R. C.; Schafstall, N.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Boyle, J. F.; Knížek, M.; Appleby, P. G.; Svoboda, M.;  and Clear, J. L.\n</span>\n\n  \n\n</span>\n\n  <i>Forest Ecology and Management</i>, 475: 118413. November 2020.\n  <span class=\"note\">[IF2019=3.17]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.foreco.2020.118413\"\n     onclick=\"log_download('kuosmanen-ada-halsall-chiverrell-schafstall-kune-boyle-knek-etal-integrationofdendrochronologicalandpalaeoecologicaldisturbancereconstructionsintemperatemountainforests-2020', 'http://doi.org/10.1016/j.foreco.2020.118413', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kuosmanen-ada-halsall-chiverrell-schafstall-kune-boyle-knek-etal-integrationofdendrochronologicalandpalaeoecologicaldisturbancereconstructionsintemperatemountainforests-2020\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>2 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kuosmanen-ada-halsall-chiverrell-schafstall-kune-boyle-knek-etal-integrationofdendrochronologicalandpalaeoecologicaldisturbancereconstructionsintemperatemountainforests-2020')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{kuosmanen_integration_2020,\n\ttitle = {Integration of dendrochronological and palaeoecological disturbance reconstructions in temperate mountain forests},\n\tvolume = {475},\n\tissn = {0378-1127},\n\tdoi = {10.1016/j.foreco.2020.118413},\n\tabstract = {Disentangling the long-term changes in forest disturbance dynamics provides a basis for predicting the forest responses to changing environmental conditions. The combination of multidisciplinary records can offer more robust reconstructions of past forest disturbance dynamics. Here we link disturbance histories of the central European mountain spruce forest obtained from dendrochronological and palaeoecological records (fossil pollen, sedimentary charcoal, bark beetle remains and geochemistry) using a small glacial lake and the surrounding forest in the Šumava National Park (Czech Republic). Dendrochronological reconstructions of disturbance were created for 300-year-long records from 6 study plots with a minimum of 35 trees analyzed for the abrupt growth increases (releases) and rapid early growth rates, both indicative of disturbance events. High-resolution analysis of lake sediments were used to reconstruct 800-year long changes in forest composition and landscape openness (fossil pollen), past fire events (micro- and macroscopic charcoal), bark beetle occurrence (fossil bark beetle remains), and erosion episodes (geochemical signals in the sediment) potentially resulting from disturbance events. Tree-ring data indicate that disturbances occurred regularly through the last three centuries and identify a most intensive period of disturbances between 1780 and 1830 CE. Geochemical erosion markers (e.g. K, Zr, \\% inorganic) show greater flux of catchment sediment and soils in the periods 1250–1400 and 1450–1500 CE, before a substantial shift to a more erosive regime 1600–1850 and 1900 CE onwards. Pollen records demonstrate relatively small changes in forest composition during the last 800 years until the beginning of the 20th century, when there was decrease in Picea. Fossil bark beetle remains indicate continuous presence of bark beetles from 1620s to 1800s, and charcoal records suggest that more frequent fires occurred during the 18th century. Each of the dendrochronological, palaeoecological and sedimentological records provide a unique perspective on forest disturbance dynamics, and combined offer a more robust and complete record of disturbance history. We demonstrate that sedimentary proxies originating from the lake catchment mirror the forest disturbance dynamics recorded in the tree-rings. The multidisciplinary records likely record forest disturbances at different spatial and temporal scales revealing different disturbance characteristics. Integrating these multidisciplinary datasets demonstrates a promising way to obtain more complete understanding of long-term disturbance dynamics. However, integrating datasets with variable spatial and temporal influence remains challenging. Our results indicated that multiple disturbance factors, such as windstorms, bark beetle outbeaks and fires, may occur simultaneously creating a complex disturbance regime in mountain forests, which should be considered in forest management and conservation strategies.},\n\tlanguage = {English},\n\turldate = {2020-08-02},\n\tjournal = {Forest Ecology and Management},\n\tauthor = {Kuosmanen, Niina and Čada, Vojtěch and Halsall, Karen and Chiverrell, Richard C. and Schafstall, Nick and Kuneš, Petr and Boyle, John F. and Knížek, Miloš and Appleby, Peter G. and Svoboda, Miroslav and Clear, Jennifer L.},\n\tmonth = nov,\n\tyear = {2020},\n\tnote = {[IF2019=3.17]},\n\tkeywords = {Bark beetles, Fire, Forest dynamics, Geochemistry, Pollen, Tree-rings, disturbance},\n\tpages = {118413},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Disentangling the long-term changes in forest disturbance dynamics provides a basis for predicting the forest responses to changing environmental conditions. The combination of multidisciplinary records can offer more robust reconstructions of past forest disturbance dynamics. Here we link disturbance histories of the central European mountain spruce forest obtained from dendrochronological and palaeoecological records (fossil pollen, sedimentary charcoal, bark beetle remains and geochemistry) using a small glacial lake and the surrounding forest in the Šumava National Park (Czech Republic). Dendrochronological reconstructions of disturbance were created for 300-year-long records from 6 study plots with a minimum of 35 trees analyzed for the abrupt growth increases (releases) and rapid early growth rates, both indicative of disturbance events. High-resolution analysis of lake sediments were used to reconstruct 800-year long changes in forest composition and landscape openness (fossil pollen), past fire events (micro- and macroscopic charcoal), bark beetle occurrence (fossil bark beetle remains), and erosion episodes (geochemical signals in the sediment) potentially resulting from disturbance events. Tree-ring data indicate that disturbances occurred regularly through the last three centuries and identify a most intensive period of disturbances between 1780 and 1830 CE. Geochemical erosion markers (e.g. K, Zr, % inorganic) show greater flux of catchment sediment and soils in the periods 1250–1400 and 1450–1500 CE, before a substantial shift to a more erosive regime 1600–1850 and 1900 CE onwards. Pollen records demonstrate relatively small changes in forest composition during the last 800 years until the beginning of the 20th century, when there was decrease in Picea. Fossil bark beetle remains indicate continuous presence of bark beetles from 1620s to 1800s, and charcoal records suggest that more frequent fires occurred during the 18th century. Each of the dendrochronological, palaeoecological and sedimentological records provide a unique perspective on forest disturbance dynamics, and combined offer a more robust and complete record of disturbance history. We demonstrate that sedimentary proxies originating from the lake catchment mirror the forest disturbance dynamics recorded in the tree-rings. The multidisciplinary records likely record forest disturbances at different spatial and temporal scales revealing different disturbance characteristics. Integrating these multidisciplinary datasets demonstrates a promising way to obtain more complete understanding of long-term disturbance dynamics. However, integrating datasets with variable spatial and temporal influence remains challenging. Our results indicated that multiple disturbance factors, such as windstorms, bark beetle outbeaks and fires, may occur simultaneously creating a complex disturbance regime in mountain forests, which should be considered in forest management and conservation strategies.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"chevalier-davis-heiri-sepp-chase-gajewski-lacourse-telford-etal-pollenbasedclimatereconstructiontechniquesforlatequaternarystudies-2020\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.sciencedirect.com/science/article/pii/S001282522030430X\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'chevalier-davis-heiri-sepp-chase-gajewski-lacourse-telford-etal-pollenbasedclimatereconstructiontechniquesforlatequaternarystudies-2020', 'http://www.sciencedirect.com/science/article/pii/S001282522030430X', event);\">\n    Pollen-based climate reconstruction techniques for late Quaternary studies.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Chevalier, M.; Davis, B. A. S.; Heiri, O.; Seppä, H.; Chase, B. M.; Gajewski, K.; Lacourse, T.; Telford, R. J.; Finsinger, W.; Guiot, J.; Kühl, N.; Maezumi, S. Y.; Tipton, J. R.; Carter, V. A.; Brussel, T.; Phelps, L. N.; Dawson, A.; Zanon, M.; Vallé, F.; Nolan, C.; Mauri, A.; de Vernal, A.; Izumi, K.; Holmström, L.; Marsicek, J.; Goring, S.; Sommer, P. S.; Chaput, M.;  and Kupriyanov, D.\n</span>\n\n  \n\n</span>\n\n  <i>Earth-Science Reviews</i>, 210: 103384. November 2020.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"http://www.sciencedirect.com/science/article/pii/S001282522030430X\"\n     onclick=\"log_download('chevalier-davis-heiri-sepp-chase-gajewski-lacourse-telford-etal-pollenbasedclimatereconstructiontechniquesforlatequaternarystudies-2020', 'http://www.sciencedirect.com/science/article/pii/S001282522030430X', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Pollen-based climate reconstruction techniques for late Quaternary studies [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.earscirev.2020.103384\"\n     onclick=\"log_download('chevalier-davis-heiri-sepp-chase-gajewski-lacourse-telford-etal-pollenbasedclimatereconstructiontechniquesforlatequaternarystudies-2020', 'http://doi.org/10.1016/j.earscirev.2020.103384', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/chevalier-davis-heiri-sepp-chase-gajewski-lacourse-telford-etal-pollenbasedclimatereconstructiontechniquesforlatequaternarystudies-2020\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('chevalier-davis-heiri-sepp-chase-gajewski-lacourse-telford-etal-pollenbasedclimatereconstructiontechniquesforlatequaternarystudies-2020')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{chevalier_pollen-based_2020,\n\ttitle = {Pollen-based climate reconstruction techniques for late {Quaternary} studies},\n\tvolume = {210},\n\tissn = {0012-8252},\n\turl = {http://www.sciencedirect.com/science/article/pii/S001282522030430X},\n\tdoi = {10.1016/j.earscirev.2020.103384},\n\tabstract = {Fossil pollen records are well-established indicators of past vegetation changes. The prevalence of pollen across environmental settings including lakes, wetlands, and marine sediments, has made palynology one of the most ubiquitous and valuable tools for studying past environmental and climatic change globally for decades. A complementary research focus has been the development of statistical techniques to derive quantitative estimates of climatic conditions from pollen assemblages. This paper reviews the most commonly used statistical techniques and their rationale and seeks to provide a resource to facilitate their inclusion in more palaeoclimatic research. To this end, we first address the fundamental aspects of fossil pollen data that should be considered when undertaking pollen-based climate reconstructions. We then introduce the range of techniques currently available, the history of their development, and the situations in which they can be best employed. We review the literature on how to define robust calibration datasets, produce high-quality reconstructions, and evaluate climate reconstructions, and suggest methods and products that could be developed to facilitate accessibility and global usability. To continue to foster the development and inclusion of pollen climate reconstruction methods, we promote the development of reporting standards. When established, such standards should 1) enable broader application of climate reconstruction techniques, especially in regions where such methods are currently underused, and 2) enable the evaluation and reproduction of individual reconstructions, structuring them for the evolving open-science era, and optimising the use of fossil pollen data as a vital means for the study of past environmental and climatic variability. We also strongly encourage developers and users of palaeoclimate reconstruction methodologies to make associated programming code publicly available, which will further help disseminate these techniques to interested communities.},\n\tlanguage = {English},\n\turldate = {2020-12-09},\n\tjournal = {Earth-Science Reviews},\n\tauthor = {Chevalier, Manuel and Davis, Basil A. S. and Heiri, Oliver and Seppä, Heikki and Chase, Brian M. and Gajewski, Konrad and Lacourse, Terri and Telford, Richard J. and Finsinger, Walter and Guiot, Joël and Kühl, Norbert and Maezumi, S. Yoshi and Tipton, John R. and Carter, Vachel A. and Brussel, Thomas and Phelps, Leanne N. and Dawson, Andria and Zanon, Marco and Vallé, Francesca and Nolan, Connor and Mauri, Achille and de Vernal, Anne and Izumi, Kenji and Holmström, Lasse and Marsicek, Jeremiah and Goring, Simon and Sommer, Philipp S. and Chaput, Michelle and Kupriyanov, Dmitry},\n\tmonth = nov,\n\tyear = {2020},\n\tkeywords = {Analogues, Climate, Community-based standards, Palaeoclimate, Pollen, Probability density functions, Quantitative reconstructions, Transfer functions},\n\tpages = {103384},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Fossil pollen records are well-established indicators of past vegetation changes. The prevalence of pollen across environmental settings including lakes, wetlands, and marine sediments, has made palynology one of the most ubiquitous and valuable tools for studying past environmental and climatic change globally for decades. A complementary research focus has been the development of statistical techniques to derive quantitative estimates of climatic conditions from pollen assemblages. This paper reviews the most commonly used statistical techniques and their rationale and seeks to provide a resource to facilitate their inclusion in more palaeoclimatic research. To this end, we first address the fundamental aspects of fossil pollen data that should be considered when undertaking pollen-based climate reconstructions. We then introduce the range of techniques currently available, the history of their development, and the situations in which they can be best employed. We review the literature on how to define robust calibration datasets, produce high-quality reconstructions, and evaluate climate reconstructions, and suggest methods and products that could be developed to facilitate accessibility and global usability. To continue to foster the development and inclusion of pollen climate reconstruction methods, we promote the development of reporting standards. When established, such standards should 1) enable broader application of climate reconstruction techniques, especially in regions where such methods are currently underused, and 2) enable the evaluation and reproduction of individual reconstructions, structuring them for the evolving open-science era, and optimising the use of fossil pollen data as a vital means for the study of past environmental and climatic variability. We also strongly encourage developers and users of palaeoclimate reconstruction methodologies to make associated programming code publicly available, which will further help disseminate these techniques to interested communities.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"feurdean-florescu-tanu-vannire-diaconu-pfeiffer-warren-hutchinson-etal-recentfireregimeinthesouthernborealforestsofwesternsiberiaisunprecedentedinthelastfivemillennia-2020\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Recent fire regime in the southern boreal forests of western Siberia is unprecedented in the last five millennia.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Feurdean, A.; Florescu, G.; Tanţău, I.; Vannière, B.; Diaconu, A.; Pfeiffer, M.; Warren, D.; Hutchinson, S. M.; Gorina, N.; Gałka, M.;  and Kirpotin, S.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Science Reviews</i>, 244: 106495. September 2020.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quascirev.2020.106495\"\n     onclick=\"log_download('feurdean-florescu-tanu-vannire-diaconu-pfeiffer-warren-hutchinson-etal-recentfireregimeinthesouthernborealforestsofwesternsiberiaisunprecedentedinthelastfivemillennia-2020', 'http://doi.org/10.1016/j.quascirev.2020.106495', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/feurdean-florescu-tanu-vannire-diaconu-pfeiffer-warren-hutchinson-etal-recentfireregimeinthesouthernborealforestsofwesternsiberiaisunprecedentedinthelastfivemillennia-2020\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('feurdean-florescu-tanu-vannire-diaconu-pfeiffer-warren-hutchinson-etal-recentfireregimeinthesouthernborealforestsofwesternsiberiaisunprecedentedinthelastfivemillennia-2020')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{feurdean_recent_2020,\n\ttitle = {Recent fire regime in the southern boreal forests of western {Siberia} is unprecedented in the last five millennia},\n\tvolume = {244},\n\tissn = {0277-3791},\n\tdoi = {10.1016/j.quascirev.2020.106495},\n\tabstract = {Wildfires in Siberia are documented to have increased in frequency and severity over recent decades. However, in the absence of long-term records, it is unclear how far and why this trend deviates from centennial to millennial scale variability. Here we reconstruct past patterns of fire frequency and fire type, and explore how the fire-related traits of boreal species and plant functional types (PFTs) determine ecosystem responses to changing fire regimes. We use charcoal-based reconstructions of the fire regime in combination with a pollen-based assessment of vegetation composition in two boreal forest peat profiles from Plotnikovo Mire in western Siberia that span the last 2400 and 5000 years. We found moderate levels of biomass burning between 5000 and 4000 cal yr BP. Biomass burning and fire severity i.e., more biomass burning per fire episode, increased over the last 1500 cal yr BP associated with the dominance of fire invaders (Betula). Conversely, between 4000 and 1500 cal yr BP lower biomass burning, with perhaps fire types affecting mostly litter and understorey vegetation, coincided with the dominance of fire resisters (e.g., Pinus sylvestris, P. sibirica, Larix) intermixed with a considerable number of fire avoiders (e.g., Abies sibirica and Picea obovata). This long-term perspective shows that the current fire regime commenced 1500 years ago and deviates from the trends observed over the last 5000 years. This deviation is linked to a combination of climate conditions conducive to fire, the amount and composition of woody fuels, and land use changes. Although pines reacted more sensitively to increased fire severity, the fire avoider Picea obovata appears to be much more vulnerable to both frequent, severe fires than Abies sibirica. We anticipate that climatically driven changes in fire weather, with frequent warm and dry spells, and anthropogenic land use intensification will heighten fire severity and their impact, driving vegetation composition towards Betula species to the detriment of Picea obovata. This study also shows that charcoal morphotypes can provide useful information on fuel and fire type, and that, although all macro-charcoal size classes reliably indicate local-scale fires, the larger fraction ({\\textgreater}300–500 μm) allows the identification of on-site fire episodes. We recommend multi-site palaeo-fire reconstructions in boreal peatlands to adequately reflect the influence of localised peat moisture content, and vegetation composition and structure variability on the small-scale heterogeneity of fire type and spread. This will ensure that trends in fire regime dynamics are representative and not limited to the local scale. We also propose future directions in fire research that can be tested using fossil records of fire, climate and vegetation ideally in an interdisciplinary approach.},\n\tlanguage = {English},\n\turldate = {2020-10-02},\n\tjournal = {Quaternary Science Reviews},\n\tauthor = {Feurdean, Angelica and Florescu, Gabriela and Tanţău, Ioan and Vannière, Boris and Diaconu, Andrei-Cosmin and Pfeiffer, Mirjam and Warren, Dan and Hutchinson, Simon M. and Gorina, Natalia and Gałka, Mariusz and Kirpotin, Sergey},\n\tmonth = sep,\n\tyear = {2020},\n\tkeywords = {Biomass burning, Charcoal morphologies, Climate change, Drought, Fire frequency, Fire severity, Great Vasyugan Mire, Peat archives, Pollen, Russia, Satellite images},\n\tpages = {106495},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Wildfires in Siberia are documented to have increased in frequency and severity over recent decades. However, in the absence of long-term records, it is unclear how far and why this trend deviates from centennial to millennial scale variability. Here we reconstruct past patterns of fire frequency and fire type, and explore how the fire-related traits of boreal species and plant functional types (PFTs) determine ecosystem responses to changing fire regimes. We use charcoal-based reconstructions of the fire regime in combination with a pollen-based assessment of vegetation composition in two boreal forest peat profiles from Plotnikovo Mire in western Siberia that span the last 2400 and 5000 years. We found moderate levels of biomass burning between 5000 and 4000 cal yr BP. Biomass burning and fire severity i.e., more biomass burning per fire episode, increased over the last 1500 cal yr BP associated with the dominance of fire invaders (Betula). Conversely, between 4000 and 1500 cal yr BP lower biomass burning, with perhaps fire types affecting mostly litter and understorey vegetation, coincided with the dominance of fire resisters (e.g., Pinus sylvestris, P. sibirica, Larix) intermixed with a considerable number of fire avoiders (e.g., Abies sibirica and Picea obovata). This long-term perspective shows that the current fire regime commenced 1500 years ago and deviates from the trends observed over the last 5000 years. This deviation is linked to a combination of climate conditions conducive to fire, the amount and composition of woody fuels, and land use changes. Although pines reacted more sensitively to increased fire severity, the fire avoider Picea obovata appears to be much more vulnerable to both frequent, severe fires than Abies sibirica. We anticipate that climatically driven changes in fire weather, with frequent warm and dry spells, and anthropogenic land use intensification will heighten fire severity and their impact, driving vegetation composition towards Betula species to the detriment of Picea obovata. This study also shows that charcoal morphotypes can provide useful information on fuel and fire type, and that, although all macro-charcoal size classes reliably indicate local-scale fires, the larger fraction (\\textgreater300–500 μm) allows the identification of on-site fire episodes. We recommend multi-site palaeo-fire reconstructions in boreal peatlands to adequately reflect the influence of localised peat moisture content, and vegetation composition and structure variability on the small-scale heterogeneity of fire type and spread. This will ensure that trends in fire regime dynamics are representative and not limited to the local scale. We also propose future directions in fire research that can be tested using fossil records of fire, climate and vegetation ideally in an interdisciplinary approach.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"felde-flantua-jenks-benito-debeaulieu-kune-magri-nalepka-etal-compositionalturnoverandvariationineemianpollensequencesineurope-2020\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Compositional turnover and variation in Eemian pollen sequences in Europe.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Felde, V. A.; Flantua, S. G. A.; Jenks, C. R.; Benito, B. M.; de Beaulieu, J.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Magri, D.; Nalepka, D.; Risebrobakken, B.; ter Braak, C. J. F.; Allen, J. R. M.; Granoszewski, W.; Helmens, K. F.; Huntley, B.; Kondratienė, O.; Kalniņa, L.; Kupryjanowicz, M.; Malkiewicz, M.; Milner, A. M.; Nita, M.; Noryśkiewicz, B.; Pidek, I. A.; Reille, M.; Salonen, J. S.; Šeirienė, V.; Winter, H.; Tzedakis, P. C.;  and Birks, H. J. B.\n</span>\n\n  \n\n</span>\n\n  <i>Vegetation History and Archaeobotany</i>, 29(1): 101–109. January 2020.\n  <span class=\"note\">[IF2019=2.364]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s00334-019-00726-5\"\n     onclick=\"log_download('felde-flantua-jenks-benito-debeaulieu-kune-magri-nalepka-etal-compositionalturnoverandvariationineemianpollensequencesineurope-2020', 'http://doi.org/10.1007/s00334-019-00726-5', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/felde-flantua-jenks-benito-debeaulieu-kune-magri-nalepka-etal-compositionalturnoverandvariationineemianpollensequencesineurope-2020\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('felde-flantua-jenks-benito-debeaulieu-kune-magri-nalepka-etal-compositionalturnoverandvariationineemianpollensequencesineurope-2020')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{felde_compositional_2020,\n\ttitle = {Compositional turnover and variation in {Eemian} pollen sequences in {Europe}},\n\tvolume = {29},\n\tissn = {1617-6278},\n\tdoi = {10.1007/s00334-019-00726-5},\n\tabstract = {The Eemian interglacial represents a natural experiment on how past vegetation with negligible human impact responded to amplified temperature changes compared to the Holocene. Here, we assemble 47 carefully selected Eemian pollen sequences from Europe to explore geographical patterns of (1) total compositional turnover and total variation for each sequence and (2) stratigraphical turnover between samples within each sequence using detrended canonical correspondence analysis, multivariate regression trees, and principal curves. Our synthesis shows that turnover and variation are highest in central Europe (47–55°N), low in southern Europe (south of 45°N), and lowest in the north (above 60°N). These results provide a basis for developing hypotheses about causes of vegetation change during the Eemian and their possible drivers.},\n\tlanguage = {English},\n\tnumber = {1},\n\turldate = {2020-01-07},\n\tjournal = {Vegetation History and Archaeobotany},\n\tauthor = {Felde, Vivian A. and Flantua, Suzette G. A. and Jenks, Cathy R. and Benito, Blas M. and de Beaulieu, Jacques-Louis and Kuneš, Petr and Magri, Donatella and Nalepka, Dorota and Risebrobakken, Bjørg and ter Braak, Cajo J. F. and Allen, Judy R. M. and Granoszewski, Wojciech and Helmens, Karin F. and Huntley, Brian and Kondratienė, Ona and Kalniņa, Laimdota and Kupryjanowicz, Mirosława and Malkiewicz, Małgorzata and Milner, Alice M. and Nita, Małgorzata and Noryśkiewicz, Bożena and Pidek, Irena A. and Reille, Maurice and Salonen, J. Sakari and Šeirienė, Vaida and Winter, Hanna and Tzedakis, Polychronis C. and Birks, H. John B.},\n\tmonth = jan,\n\tyear = {2020},\n\tnote = {[IF2019=2.364]},\n\tkeywords = {Detrended canonical correspondence analysis, Extrinsic and intrinsic processes, Inertia, Last interglacial dataset, Multivariate regression trees, Neutral processes, Principal curves, database, interglacial},\n\tpages = {101--109},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The Eemian interglacial represents a natural experiment on how past vegetation with negligible human impact responded to amplified temperature changes compared to the Holocene. Here, we assemble 47 carefully selected Eemian pollen sequences from Europe to explore geographical patterns of (1) total compositional turnover and total variation for each sequence and (2) stratigraphical turnover between samples within each sequence using detrended canonical correspondence analysis, multivariate regression trees, and principal curves. Our synthesis shows that turnover and variation are highest in central Europe (47–55°N), low in southern Europe (south of 45°N), and lowest in the north (above 60°N). These results provide a basis for developing hypotheses about causes of vegetation change during the Eemian and their possible drivers.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"feurdean-vannire-finsinger-warren-connor-forrest-liakka-panait-etal-firehazardmodulationbylongtermdynamicsinlandcoveranddominantforesttypeineasternandcentraleurope-2020\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://www.biogeosciences.net/17/1213/2020/\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'feurdean-vannire-finsinger-warren-connor-forrest-liakka-panait-etal-firehazardmodulationbylongtermdynamicsinlandcoveranddominantforesttypeineasternandcentraleurope-2020', 'https://www.biogeosciences.net/17/1213/2020/', event);\">\n    Fire hazard modulation by long-term dynamics in land cover and dominant forest type in eastern and central Europe.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Feurdean, A.; Vannière, B.; Finsinger, W.; Warren, D.; Connor, S. C.; Forrest, M.; Liakka, J.; Panait, A.; Werner, C.; Andrič, M.; Bobek, P.; Carter, V. A.; Davis, B.; Diaconu, A.; Dietze, E.; Feeser, I.; Florescu, G.; Gałka, M.; Giesecke, T.; Jahns, S.; Jamrichová, E.; Kajukało, K.; Kaplan, J.; Karpińska-Kołaczek, M.; Kołaczek, P.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Kupriyanov, D.; Lamentowicz, M.; Lemmen, C.; Magyari, E. K.; Marcisz, K.; Marinova, E.; Niamir, A.; Novenko, E.; Obremska, M.; Pędziszewska, A.; Pfeiffer, M.; Poska, A.; Rösch, M.; Słowiński, M.; Stančikaitė, M.; Szal, M.; Święta-Musznicka, J.; Tanţău, I.; Theuerkauf, M.; Tonkov, S.; Valkó, O.; Vassiljev, J.; Veski, S.; Vincze, I.; Wacnik, A.; Wiethold, J.;  and Hickler, T.\n</span>\n\n  \n\n</span>\n\n  <i>Biogeosciences</i>, 17(5): 1213–1230. March 2020.\n  <span class=\"note\">[IF2019=3.48]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://www.biogeosciences.net/17/1213/2020/\"\n     onclick=\"log_download('feurdean-vannire-finsinger-warren-connor-forrest-liakka-panait-etal-firehazardmodulationbylongtermdynamicsinlandcoveranddominantforesttypeineasternandcentraleurope-2020', 'https://www.biogeosciences.net/17/1213/2020/', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Fire hazard modulation by long-term dynamics in land cover and dominant forest type in eastern and central Europe [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.5194/bg-17-1213-2020\"\n     onclick=\"log_download('feurdean-vannire-finsinger-warren-connor-forrest-liakka-panait-etal-firehazardmodulationbylongtermdynamicsinlandcoveranddominantforesttypeineasternandcentraleurope-2020', 'http://doi.org/10.5194/bg-17-1213-2020', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/feurdean-vannire-finsinger-warren-connor-forrest-liakka-panait-etal-firehazardmodulationbylongtermdynamicsinlandcoveranddominantforesttypeineasternandcentraleurope-2020\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('feurdean-vannire-finsinger-warren-connor-forrest-liakka-panait-etal-firehazardmodulationbylongtermdynamicsinlandcoveranddominantforesttypeineasternandcentraleurope-2020')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{feurdean_fire_2020,\n\ttitle = {Fire hazard modulation by long-term dynamics in land cover and dominant forest type in eastern and central {Europe}},\n\tvolume = {17},\n\tissn = {1726-4170},\n\turl = {https://www.biogeosciences.net/17/1213/2020/},\n\tdoi = {10.5194/bg-17-1213-2020},\n\tabstract = {{\\textless}p{\\textgreater}{\\textless}strong{\\textgreater}Abstract.{\\textless}/strong{\\textgreater} Wildfire occurrence is influenced by climate, vegetation and human activities. A key challenge for understanding the risk of fires is quantifying the mediating effect of vegetation on fire regimes. Here, we explore the relative importance of Holocene land cover, land use, dominant functional forest type, and climate dynamics on biomass burning in temperate and boreo-nemoral regions of central and eastern Europe over the past 12\\&amp;thinsp;kyr. We used an extensive data set of Holocene pollen and sedimentary charcoal records, in combination with climate simulations and statistical modelling. Biomass burning was highest during the early Holocene and lowest during the mid-Holocene in all three ecoregions (Atlantic, continental and boreo-nemoral) but was more spatially variable over the past 3–4\\&amp;thinsp;kyr. Although climate explained a significant variance in biomass burning during the early Holocene, tree cover was consistently the highest predictor of past biomass burning over the past 8\\&amp;thinsp;kyr. In temperate forests, biomass burning was high at {\\textless}span class=&quot;inline-formula&quot;{\\textgreater}∼45{\\textless}/span{\\textgreater}\\&amp;thinsp;\\% tree cover and decreased to a minimum at between 60\\&amp;thinsp;\\% and 70\\&amp;thinsp;\\% tree cover. In needleleaf-dominated forests, biomass burning was highest at {\\textless}span class=&quot;inline-formula&quot;{\\textgreater}∼{\\textless}/span{\\textgreater}\\&amp;thinsp;60\\&amp;thinsp;\\%–65\\&amp;thinsp;\\% tree cover and steeply declined at {\\textless}span class=&quot;inline-formula&quot;{\\textgreater}\\&amp;gt;65{\\textless}/span{\\textgreater}\\&amp;thinsp;\\% tree cover. Biomass burning also increased when arable lands and grasslands reached {\\textless}span class=&quot;inline-formula&quot;{\\textgreater}∼{\\textless}/span{\\textgreater}\\&amp;thinsp;15\\&amp;thinsp;\\%–20\\&amp;thinsp;\\%, although this relationship was variable depending on land use practice via ignition sources, fuel type and quantities. Higher tree cover reduced the amount of solar radiation reaching the forest floor and could provide moister, more wind-protected microclimates underneath canopies, thereby decreasing fuel flammability. Tree cover at which biomass burning increased appears to be driven by warmer and drier summer conditions during the early Holocene and by increasing human influence on land cover during the late Holocene. We suggest that long-term fire hazard may be effectively reduced through land cover management, given that land cover has controlled fire regimes under the dynamic climates of the Holocene.{\\textless}/p{\\textgreater}},\n\tlanguage = {English},\n\tnumber = {5},\n\turldate = {2020-03-05},\n\tjournal = {Biogeosciences},\n\tauthor = {Feurdean, Angelica and Vannière, Boris and Finsinger, Walter and Warren, Dan and Connor, Simon C. and Forrest, Matthew and Liakka, Johan and Panait, Andrei and Werner, Christian and Andrič, Maja and Bobek, Premysl and Carter, Vachel A. and Davis, Basil and Diaconu, Andrei-Cosmin and Dietze, Elisabeth and Feeser, Ingo and Florescu, Gabriela and Gałka, Mariusz and Giesecke, Thomas and Jahns, Susanne and Jamrichová, Eva and Kajukało, Katarzyna and Kaplan, Jed and Karpińska-Kołaczek, Monika and Kołaczek, Piotr and Kuneš, Petr and Kupriyanov, Dimitry and Lamentowicz, Mariusz and Lemmen, Carsten and Magyari, Enikö K. and Marcisz, Katarzyna and Marinova, Elena and Niamir, Aidin and Novenko, Elena and Obremska, Milena and Pędziszewska, Anna and Pfeiffer, Mirjam and Poska, Anneli and Rösch, Manfred and Słowiński, Michal and Stančikaitė, Miglė and Szal, Marta and Święta-Musznicka, Joanna and Tanţău, Ioan and Theuerkauf, Martin and Tonkov, Spassimir and Valkó, Orsolya and Vassiljev, Jüri and Veski, Siim and Vincze, Ildiko and Wacnik, Agnieszka and Wiethold, Julian and Hickler, Thomas},\n\tmonth = mar,\n\tyear = {2020},\n\tnote = {[IF2019=3.48]},\n\tkeywords = {disturbance},\n\tpages = {1213--1230},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  \\textlessp\\textgreater\\textlessstrong\\textgreaterAbstract.\\textless/strong\\textgreater Wildfire occurrence is influenced by climate, vegetation and human activities. A key challenge for understanding the risk of fires is quantifying the mediating effect of vegetation on fire regimes. Here, we explore the relative importance of Holocene land cover, land use, dominant functional forest type, and climate dynamics on biomass burning in temperate and boreo-nemoral regions of central and eastern Europe over the past 12&thinsp;kyr. We used an extensive data set of Holocene pollen and sedimentary charcoal records, in combination with climate simulations and statistical modelling. Biomass burning was highest during the early Holocene and lowest during the mid-Holocene in all three ecoregions (Atlantic, continental and boreo-nemoral) but was more spatially variable over the past 3–4&thinsp;kyr. Although climate explained a significant variance in biomass burning during the early Holocene, tree cover was consistently the highest predictor of past biomass burning over the past 8&thinsp;kyr. In temperate forests, biomass burning was high at \\textlessspan class=\"inline-formula\"\\textgreater∼45\\textless/span\\textgreater&thinsp;% tree cover and decreased to a minimum at between 60&thinsp;% and 70&thinsp;% tree cover. In needleleaf-dominated forests, biomass burning was highest at \\textlessspan class=\"inline-formula\"\\textgreater∼\\textless/span\\textgreater&thinsp;60&thinsp;%–65&thinsp;% tree cover and steeply declined at \\textlessspan class=\"inline-formula\"\\textgreater&gt;65\\textless/span\\textgreater&thinsp;% tree cover. Biomass burning also increased when arable lands and grasslands reached \\textlessspan class=\"inline-formula\"\\textgreater∼\\textless/span\\textgreater&thinsp;15&thinsp;%–20&thinsp;%, although this relationship was variable depending on land use practice via ignition sources, fuel type and quantities. Higher tree cover reduced the amount of solar radiation reaching the forest floor and could provide moister, more wind-protected microclimates underneath canopies, thereby decreasing fuel flammability. Tree cover at which biomass burning increased appears to be driven by warmer and drier summer conditions during the early Holocene and by increasing human influence on land cover during the late Holocene. We suggest that long-term fire hazard may be effectively reduced through land cover management, given that land cover has controlled fire regimes under the dynamic climates of the Holocene.\\textless/p\\textgreater\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"hokov-pokorn-neustupa-pokorn-interandintraspecificvariationingrassphytolithshapeandsizeageometricmorphometricsperspective-2020\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Inter- and intraspecific variation in grass phytolith shape and size: a geometric morphometrics perspective.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Hošková, K.; Pokorná, A.; Neustupa, J.;  and Pokorný, P.\n</span>\n\n  \n\n</span>\n\n  <i>Annals of Botany</i>.  2020.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1093/aob/mcaa102\"\n     onclick=\"log_download('hokov-pokorn-neustupa-pokorn-interandintraspecificvariationingrassphytolithshapeandsizeageometricmorphometricsperspective-2020', 'http://doi.org/10.1093/aob/mcaa102', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/hokov-pokorn-neustupa-pokorn-interandintraspecificvariationingrassphytolithshapeandsizeageometricmorphometricsperspective-2020\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('hokov-pokorn-neustupa-pokorn-interandintraspecificvariationingrassphytolithshapeandsizeageometricmorphometricsperspective-2020')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{hoskova_inter-_2020,\n\ttitle = {Inter- and intraspecific variation in grass phytolith shape and size: a geometric morphometrics perspective},\n\tshorttitle = {Inter- and intraspecific variation in grass phytolith shape and size},\n\tdoi = {10.1093/aob/mcaa102},\n\tabstract = {AbstractBackground and Aims.  The relative contributions of inter- and intraspecific variation to phytolith shape and size have only been investigated in a limi},\n\tlanguage = {English},\n\turldate = {2020-06-19},\n\tjournal = {Annals of Botany},\n\tauthor = {Hošková, Kristýna and Pokorná, Adéla and Neustupa, Jiří and Pokorný, Petr},\n\tyear = {2020},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  AbstractBackground and Aims. The relative contributions of inter- and intraspecific variation to phytolith shape and size have only been investigated in a limi\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2019\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2019')\"\n      onkeypress=\"toggleGroup('group_2019')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2019</span>\n      <span class=\"bibbase_group_count\">\n        \n        (13)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"dreslerov-kozkov-chuman-strouhalov-abraham-ponitiak-efrna-settlementactivityinlaterprehistoryinvisibleinthearchaeologicalrecordbutdocumentedbypollenandsedimentaryevidence-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.1007/s12520-018-0614-x\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'dreslerov-kozkov-chuman-strouhalov-abraham-ponitiak-efrna-settlementactivityinlaterprehistoryinvisibleinthearchaeologicalrecordbutdocumentedbypollenandsedimentaryevidence-2019', 'https://doi.org/10.1007/s12520-018-0614-x', event);\">\n    Settlement activity in later prehistory: invisible in the archaeological record but documented by pollen and sedimentary evidence.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Dreslerová, D.; Kozáková, R.; Chuman, T.; Strouhalová, B.; Abraham, V.; Poništiak, Š.;  and Šefrna, L.\n</span>\n\n  \n\n</span>\n\n  <i>Archaeological and Anthropological Sciences</i>, 11(5): 1683–1700. May 2019.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://doi.org/10.1007/s12520-018-0614-x\"\n     onclick=\"log_download('dreslerov-kozkov-chuman-strouhalov-abraham-ponitiak-efrna-settlementactivityinlaterprehistoryinvisibleinthearchaeologicalrecordbutdocumentedbypollenandsedimentaryevidence-2019', 'https://doi.org/10.1007/s12520-018-0614-x', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Settlement activity in later prehistory: invisible in the archaeological record but documented by pollen and sedimentary evidence [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s12520-018-0614-x\"\n     onclick=\"log_download('dreslerov-kozkov-chuman-strouhalov-abraham-ponitiak-efrna-settlementactivityinlaterprehistoryinvisibleinthearchaeologicalrecordbutdocumentedbypollenandsedimentaryevidence-2019', 'http://doi.org/10.1007/s12520-018-0614-x', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/dreslerov-kozkov-chuman-strouhalov-abraham-ponitiak-efrna-settlementactivityinlaterprehistoryinvisibleinthearchaeologicalrecordbutdocumentedbypollenandsedimentaryevidence-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('dreslerov-kozkov-chuman-strouhalov-abraham-ponitiak-efrna-settlementactivityinlaterprehistoryinvisibleinthearchaeologicalrecordbutdocumentedbypollenandsedimentaryevidence-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{dreslerova_settlement_2019,\n\ttitle = {Settlement activity in later prehistory: invisible in the archaeological record but documented by pollen and sedimentary evidence},\n\tvolume = {11},\n\tissn = {1866-9565},\n\tshorttitle = {Settlement activity in later prehistory},\n\turl = {https://doi.org/10.1007/s12520-018-0614-x},\n\tdoi = {10.1007/s12520-018-0614-x},\n\tabstract = {The paper deals with landscape and settlement development between ca. 300 BC and AD 600 in a defined area of the northern Czech Republic. Despite favourable natural conditions, human occupation of the area did not begin until the end of the first millennium BC. Natural soil and vegetation development therefore lasted longer than in the traditionally settled lowland areas. Initial settlement activity from the La Tène period caused substantial erosion of deforested luvisols and retisols, well-documented by an accumulation of eroded soil horizons in a local wetland. The erosion process continued for more than 500 years following the end of the La Tène settlement, despite the fact that archaeological research revealed no reliable evidence of occupation prior to the twelfth century AD. Pollen and sedimentary records from the wetland, however, clearly indicate the existence of settlement activity during the “archaeologically invisible” Roman and Migration periods. This case is not unique and underlines the importance of environmental analysis for the detection of settlement history, particularly during periods of poor archaeological visibility or in places that are difficult to research using standard archaeological methods. The change in conditions after the first deforestation and subsequent late prehistoric settlement triggered the degradation of the deforested luvisols and retisols and led to the diversification of the soil cover, which now also includes regosols, gleysols, and truncated luvisols and retisols.},\n\tlanguage = {en},\n\tnumber = {5},\n\turldate = {2020-03-05},\n\tjournal = {Archaeological and Anthropological Sciences},\n\tauthor = {Dreslerová, Dagmar and Kozáková, Radka and Chuman, Tomáš and Strouhalová, Barbora and Abraham, Vojtěch and Poništiak, Štefan and Šefrna, Luděk},\n\tmonth = may,\n\tyear = {2019},\n\tpages = {1683--1700},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The paper deals with landscape and settlement development between ca. 300 BC and AD 600 in a defined area of the northern Czech Republic. Despite favourable natural conditions, human occupation of the area did not begin until the end of the first millennium BC. Natural soil and vegetation development therefore lasted longer than in the traditionally settled lowland areas. Initial settlement activity from the La Tène period caused substantial erosion of deforested luvisols and retisols, well-documented by an accumulation of eroded soil horizons in a local wetland. The erosion process continued for more than 500 years following the end of the La Tène settlement, despite the fact that archaeological research revealed no reliable evidence of occupation prior to the twelfth century AD. Pollen and sedimentary records from the wetland, however, clearly indicate the existence of settlement activity during the “archaeologically invisible” Roman and Migration periods. This case is not unique and underlines the importance of environmental analysis for the detection of settlement history, particularly during periods of poor archaeological visibility or in places that are difficult to research using standard archaeological methods. The change in conditions after the first deforestation and subsequent late prehistoric settlement triggered the degradation of the deforested luvisols and retisols and led to the diversification of the soil cover, which now also includes regosols, gleysols, and truncated luvisols and retisols.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"kune-abraham-werchan-pleskov-fajmon-jamrichov-roleek-relativepollenproductivityestimatesforvegetationreconstructionincentraleasterneuropeinferredatlocalandregionalscales-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Relative pollen productivity estimates for vegetation reconstruction in central-eastern Europe inferred at local and regional scales.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Abraham, V.; Werchan, B.; Plesková, Z.; Fajmon, K.; Jamrichová, E.;  and Roleček, J.\n</span>\n\n  \n\n</span>\n\n  <i>The Holocene</i>, 29(11): 1708–1719. November 2019.\n  <span class=\"note\">[IF2018=2.547]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1177/0959683619862026\"\n     onclick=\"log_download('kune-abraham-werchan-pleskov-fajmon-jamrichov-roleek-relativepollenproductivityestimatesforvegetationreconstructionincentraleasterneuropeinferredatlocalandregionalscales-2019', 'http://doi.org/10.1177/0959683619862026', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kune-abraham-werchan-pleskov-fajmon-jamrichov-roleek-relativepollenproductivityestimatesforvegetationreconstructionincentraleasterneuropeinferredatlocalandregionalscales-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>2 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kune-abraham-werchan-pleskov-fajmon-jamrichov-roleek-relativepollenproductivityestimatesforvegetationreconstructionincentraleasterneuropeinferredatlocalandregionalscales-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{kunes_relative_2019,\n\ttitle = {Relative pollen productivity estimates for vegetation reconstruction in central-eastern {Europe} inferred at local and regional scales},\n\tvolume = {29},\n\tissn = {0959-6836},\n\tdoi = {10.1177/0959683619862026},\n\tabstract = {Understanding pollen-vegetation relationships is crucial for accurate land-cover and climate reconstructions, yet important parameters for quantifying past vegetation abundance are mostly unknown for large parts of Europe harbouring temperate thermophilous ecosystems. We collected pollen and vegetation data in central-eastern Europe, a region covered by patchy cultural landscapes of high biodiversity to estimate relative pollen productivity (RPP) for important pollen-equivalent taxa. Our study area was situated in the south-western part of the White Carpathians (Czechia–Slovakia borderland), where we collected 40 modern moss pollen samples scattered over 250 km2 and mapped vegetation within 100 m around each pollen site. Additional vegetation data were compiled from Forest management plans, Natura 2000 habitat mapping and floristic inventories over the entire area. We calculated RPP (referenced to Poaceae) by testing two approaches: the extended R-value (ERV) model by estimating relevant source area of pollen and the REVEALS-based productivity using regional scale vegetation estimates. Two models were applied to depict pollen dispersal: Lagrangian stochastic and the Gaussian plume (Prentice) models. We estimated RPP for 16 taxa using the ERV model and an additional nine taxa using REVEALS. Both approaches found Plantago lanceolata-type to be a high pollen producer, Quercus medium-to-high, Asteraceae subf. Cichorioideae, Anthemis-type, Ranunculus acris-type and Rubiaceae low-to-medium and Brassicaceae and Senecio-type as low pollen producers. Results for other, mainly tree taxa, significantly differed in both approaches mainly due to largely uneven representation in both local and regional vegetation. In comparison with other studies, our data demonstrate a high variability in the estimated RPPs which could be influenced by climatic conditions or potentially vegetation structure. We suggest that the accuracy of RPP estimates could be enhanced by comparing modern pollen data with large-scale vegetation data in the future.},\n\tlanguage = {English},\n\tnumber = {11},\n\turldate = {2019-09-18},\n\tjournal = {The Holocene},\n\tauthor = {Kuneš, Petr and Abraham, Vojtěch and Werchan, Barbora and Plesková, Zuzana and Fajmon, Karel and Jamrichová, Eva and Roleček, Jan},\n\tmonth = nov,\n\tyear = {2019},\n\tnote = {[IF2018=2.547]},\n\tkeywords = {Czech Republic, ERV model, Gaussian plume model, LRA, Lagrangian stochastic model, REVEALS, modern pollen spectra, reconstruction, vegetation cover},\n\tpages = {1708--1719},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Understanding pollen-vegetation relationships is crucial for accurate land-cover and climate reconstructions, yet important parameters for quantifying past vegetation abundance are mostly unknown for large parts of Europe harbouring temperate thermophilous ecosystems. We collected pollen and vegetation data in central-eastern Europe, a region covered by patchy cultural landscapes of high biodiversity to estimate relative pollen productivity (RPP) for important pollen-equivalent taxa. Our study area was situated in the south-western part of the White Carpathians (Czechia–Slovakia borderland), where we collected 40 modern moss pollen samples scattered over 250 km2 and mapped vegetation within 100 m around each pollen site. Additional vegetation data were compiled from Forest management plans, Natura 2000 habitat mapping and floristic inventories over the entire area. We calculated RPP (referenced to Poaceae) by testing two approaches: the extended R-value (ERV) model by estimating relevant source area of pollen and the REVEALS-based productivity using regional scale vegetation estimates. Two models were applied to depict pollen dispersal: Lagrangian stochastic and the Gaussian plume (Prentice) models. We estimated RPP for 16 taxa using the ERV model and an additional nine taxa using REVEALS. Both approaches found Plantago lanceolata-type to be a high pollen producer, Quercus medium-to-high, Asteraceae subf. Cichorioideae, Anthemis-type, Ranunculus acris-type and Rubiaceae low-to-medium and Brassicaceae and Senecio-type as low pollen producers. Results for other, mainly tree taxa, significantly differed in both approaches mainly due to largely uneven representation in both local and regional vegetation. In comparison with other studies, our data demonstrate a high variability in the estimated RPPs which could be influenced by climatic conditions or potentially vegetation structure. We suggest that the accuracy of RPP estimates could be enhanced by comparing modern pollen data with large-scale vegetation data in the future.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"bobek-svobodovsvitavsk-pokorn-amonil-kune-kozkov-abraham-klinerov-etal-divergentfirehistorytrajectoriesincentraleuropeantemperateforestsrevealedapronouncedinfluenceofbroadleavedtreesonfiredynamics-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Divergent fire history trajectories in Central European temperate forests revealed a pronounced influence of broadleaved trees on fire dynamics.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Bobek, P.; Svobodová-Svitavská, H.; Pokorný, P.; Šamonil, P.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Kozáková, R.; Abraham, V.; Klinerová, T.; Švarcová, M. G.; Jamrichová, E.; Krauseová, E.;  and Wild, J.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Science Reviews</i>, 222: 105865. October 2019.\n  <span class=\"note\">[IF2018=4.641]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quascirev.2019.105865\"\n     onclick=\"log_download('bobek-svobodovsvitavsk-pokorn-amonil-kune-kozkov-abraham-klinerov-etal-divergentfirehistorytrajectoriesincentraleuropeantemperateforestsrevealedapronouncedinfluenceofbroadleavedtreesonfiredynamics-2019', 'http://doi.org/10.1016/j.quascirev.2019.105865', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/bobek-svobodovsvitavsk-pokorn-amonil-kune-kozkov-abraham-klinerov-etal-divergentfirehistorytrajectoriesincentraleuropeantemperateforestsrevealedapronouncedinfluenceofbroadleavedtreesonfiredynamics-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('bobek-svobodovsvitavsk-pokorn-amonil-kune-kozkov-abraham-klinerov-etal-divergentfirehistorytrajectoriesincentraleuropeantemperateforestsrevealedapronouncedinfluenceofbroadleavedtreesonfiredynamics-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{bobek_divergent_2019,\n\ttitle = {Divergent fire history trajectories in {Central} {European} temperate forests revealed a pronounced influence of broadleaved trees on fire dynamics},\n\tvolume = {222},\n\tissn = {0277-3791},\n\tdoi = {10.1016/j.quascirev.2019.105865},\n\tabstract = {Fire occurrence is driven by a complex interplay between vegetation, climatic, landform and human factors making it challenging to separate the individual effect of each variable. Here we present a reconstruction of the Holocene biomass burning history of two regions located in the Central European temperate zone that differ in the timing of the Middle Holocene expansion of broadleaf-dominated forest communities. This allowed us to investigate the effect of biotic changes on past fire activity. Multiple-site charcoal accumulation records were used to estimate regional-scale trends in biomass burning and to compare them with major trajectories of vegetation development. Extensive 14C-dated soil charcoal records collected within both regions were amalgamated using a cumulative probability function to identify a stand-scale proxy of past fire occurrence. Our results suggest that rising vegetation productivity driven by rapid Early Holocene climate amelioration enhanced biomass burning. The increased fire activity during this period was driven by both a drier- and warmer-than-present climate and easily flammable fuels produced by conifer-dominated vegetation. We identified an inhibiting effect of the concomitant Fagus sylvatica expansion on levels of biomass burning that occurred asynchronously between our mountain and mid-elevation sandstone regions 6500 cal yr BP and 4900 cal yr BP, respectively. The amount of compositional change in plant communities was more related to the transformation of major vegetation types than to fluctuations in fire activity levels. The divergent timing of the fire decline in response to the Fagus sylvatica expansion implies biotic control over biomass burning that is independent of a direct climatic influence.},\n\tlanguage = {English},\n\turldate = {2019-09-16},\n\tjournal = {Quaternary Science Reviews},\n\tauthor = {Bobek, Přemysl and Svobodová-Svitavská, Helena and Pokorný, Petr and Šamonil, Pavel and Kuneš, Petr and Kozáková, Radka and Abraham, Vojtěch and Klinerová, Tereza and Švarcová, Markéta Gabriela and Jamrichová, Eva and Krauseová, Eva and Wild, Jan},\n\tmonth = oct,\n\tyear = {2019},\n\tnote = {[IF2018=4.641]},\n\tkeywords = {Fire history, Holocene, Human impact, Sedimentary charcoal, Species turnover, Vegetation dynamics, disturbance},\n\tpages = {105865},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Fire occurrence is driven by a complex interplay between vegetation, climatic, landform and human factors making it challenging to separate the individual effect of each variable. Here we present a reconstruction of the Holocene biomass burning history of two regions located in the Central European temperate zone that differ in the timing of the Middle Holocene expansion of broadleaf-dominated forest communities. This allowed us to investigate the effect of biotic changes on past fire activity. Multiple-site charcoal accumulation records were used to estimate regional-scale trends in biomass burning and to compare them with major trajectories of vegetation development. Extensive 14C-dated soil charcoal records collected within both regions were amalgamated using a cumulative probability function to identify a stand-scale proxy of past fire occurrence. Our results suggest that rising vegetation productivity driven by rapid Early Holocene climate amelioration enhanced biomass burning. The increased fire activity during this period was driven by both a drier- and warmer-than-present climate and easily flammable fuels produced by conifer-dominated vegetation. We identified an inhibiting effect of the concomitant Fagus sylvatica expansion on levels of biomass burning that occurred asynchronously between our mountain and mid-elevation sandstone regions 6500 cal yr BP and 4900 cal yr BP, respectively. The amount of compositional change in plant communities was more related to the transformation of major vegetation types than to fluctuations in fire activity levels. The divergent timing of the fire decline in response to the Fagus sylvatica expansion implies biotic control over biomass burning that is independent of a direct climatic influence.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"petk-petr-adamekov-prikov-potkov-lenkov-frczek-dresler-etal-disruptioninanalluviallandscapesettlementandenvironmentdynamicsonthealluviumoftheriverdyjeatthepohanskoarchaeologicalsiteczechrepublic-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.sciencedirect.com/science/article/pii/S1040618217309503\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'petk-petr-adamekov-prikov-potkov-lenkov-frczek-dresler-etal-disruptioninanalluviallandscapesettlementandenvironmentdynamicsonthealluviumoftheriverdyjeatthepohanskoarchaeologicalsiteczechrepublic-2019', 'http://www.sciencedirect.com/science/article/pii/S1040618217309503', event);\">\n    Disruption in an alluvial landscape: Settlement and environment dynamics on the alluvium of the river Dyje at the Pohansko archaeological site (Czech Republic).\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Petřík, J.; Petr, L.; Adameková, K.; Prišťáková, M.; Potůčková, A.; Lenďáková, Z.; Frączek, M.; Dresler, P.; Macháček, J.; Kalicki, T.;  and Lisá, L.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary International</i>, 511: 124–139. March 2019.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"http://www.sciencedirect.com/science/article/pii/S1040618217309503\"\n     onclick=\"log_download('petk-petr-adamekov-prikov-potkov-lenkov-frczek-dresler-etal-disruptioninanalluviallandscapesettlementandenvironmentdynamicsonthealluviumoftheriverdyjeatthepohanskoarchaeologicalsiteczechrepublic-2019', 'http://www.sciencedirect.com/science/article/pii/S1040618217309503', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Disruption in an alluvial landscape: Settlement and environment dynamics on the alluvium of the river Dyje at the Pohansko archaeological site (Czech Republic) [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quaint.2018.04.013\"\n     onclick=\"log_download('petk-petr-adamekov-prikov-potkov-lenkov-frczek-dresler-etal-disruptioninanalluviallandscapesettlementandenvironmentdynamicsonthealluviumoftheriverdyjeatthepohanskoarchaeologicalsiteczechrepublic-2019', 'http://doi.org/10.1016/j.quaint.2018.04.013', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/petk-petr-adamekov-prikov-potkov-lenkov-frczek-dresler-etal-disruptioninanalluviallandscapesettlementandenvironmentdynamicsonthealluviumoftheriverdyjeatthepohanskoarchaeologicalsiteczechrepublic-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('petk-petr-adamekov-prikov-potkov-lenkov-frczek-dresler-etal-disruptioninanalluviallandscapesettlementandenvironmentdynamicsonthealluviumoftheriverdyjeatthepohanskoarchaeologicalsiteczechrepublic-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{petrik_disruption_2019,\n\ttitle = {Disruption in an alluvial landscape: {Settlement} and environment dynamics on the alluvium of the river {Dyje} at the {Pohansko} archaeological site ({Czech} {Republic})},\n\tvolume = {511},\n\tissn = {1040-6182},\n\tshorttitle = {Disruption in an alluvial landscape},\n\turl = {http://www.sciencedirect.com/science/article/pii/S1040618217309503},\n\tdoi = {10.1016/j.quaint.2018.04.013},\n\tabstract = {Floodplain alluvia can provide a combination of natural and anthropogenic evidence of environmental changes, allowing to directly examine their evolution in relation to settlement dynamics. Such evidence is recorded, for example, at the archaeological site Pohansko by the town of Břeclav, a former centre of the Great Moravian Empire. The aim of our research was to explore what conditions on the floodplain could have caused the abandonment of this environment. Special attention was paid to the climax of the floodplain&#x27;s occupation during the times of the Great Moravian Empire (AD 836–906) and to the decline of its occupation in the following centuries. The environmental record at the Pohansko site starts in the 7th century BC. From the Iron Age onwards (Hallstatt and La Tène periods) there is evidence of non-agricultural human activities. Since the 3rd and 2nd centuries BC to at least the second half of the 10th century AD, there is no record of any floodplain aggradation or flooding at the site. Later, both the archaeological and palaeoecological records on the floodplain probably got exposed and redeposited. The result is a mechanically disturbed layer that is synchronous with soil horizons and subsequent Early Mediaeval cultural layers covering sandy elevations. For an unknown reason, the site was deserted for many centuries after the end of the 10th century AD. During the High Mediaeval period and the early Modern Era, especially since the 15th century AD, overbank deposits covered the floodplain. Intensified human impact in the river catchment and climate change during the Little Ice Age were the main triggers of this change. The results correlate with the written historical sources pertaining to this area, which speak about an increasing frequency of flooding in the Czech lands since the 14th century, and especially in the second half of the 16th century. As a result, these sites became unsuitable for settlement and abandoned.},\n\tlanguage = {en},\n\turldate = {2020-03-05},\n\tjournal = {Quaternary International},\n\tauthor = {Petřík, Jan and Petr, Libor and Adameková, Katarína and Prišťáková, Michaela and Potůčková, Anna and Lenďáková, Zuzana and Frączek, Marcin and Dresler, Petr and Macháček, Jiří and Kalicki, Tomasz and Lisá, Lenka},\n\tmonth = mar,\n\tyear = {2019},\n\tkeywords = {Aggradation, Early Middle Ages, Floodplain, Floodplain occupation, Great Moravian Empire, Human impact, Iron Age, Late Holocene},\n\tpages = {124--139},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Floodplain alluvia can provide a combination of natural and anthropogenic evidence of environmental changes, allowing to directly examine their evolution in relation to settlement dynamics. Such evidence is recorded, for example, at the archaeological site Pohansko by the town of Břeclav, a former centre of the Great Moravian Empire. The aim of our research was to explore what conditions on the floodplain could have caused the abandonment of this environment. Special attention was paid to the climax of the floodplain's occupation during the times of the Great Moravian Empire (AD 836–906) and to the decline of its occupation in the following centuries. The environmental record at the Pohansko site starts in the 7th century BC. From the Iron Age onwards (Hallstatt and La Tène periods) there is evidence of non-agricultural human activities. Since the 3rd and 2nd centuries BC to at least the second half of the 10th century AD, there is no record of any floodplain aggradation or flooding at the site. Later, both the archaeological and palaeoecological records on the floodplain probably got exposed and redeposited. The result is a mechanically disturbed layer that is synchronous with soil horizons and subsequent Early Mediaeval cultural layers covering sandy elevations. For an unknown reason, the site was deserted for many centuries after the end of the 10th century AD. During the High Mediaeval period and the early Modern Era, especially since the 15th century AD, overbank deposits covered the floodplain. Intensified human impact in the river catchment and climate change during the Little Ice Age were the main triggers of this change. The results correlate with the written historical sources pertaining to this area, which speak about an increasing frequency of flooding in the Czech lands since the 14th century, and especially in the second half of the 16th century. As a result, these sites became unsuitable for settlement and abandoned.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"novk-roleek-dresler-hjek-soilcharcoalelucidatestheroleofhumansinthedevelopmentoflandscapeofextremebiodiversity-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://onlinelibrary.wiley.com/doi/abs/10.1002/ldr.3350\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'novk-roleek-dresler-hjek-soilcharcoalelucidatestheroleofhumansinthedevelopmentoflandscapeofextremebiodiversity-2019', 'https://onlinelibrary.wiley.com/doi/abs/10.1002/ldr.3350', event);\">\n    Soil charcoal elucidates the role of humans in the development of landscape of extreme biodiversity.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Novák, J.; Roleček, J.; Dresler, P.;  and Hájek, M.\n</span>\n\n  \n\n</span>\n\n  <i>Land Degradation & Development</i>, 30(13): 1607–1619.  2019.\n  <span class=\"note\">_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/ldr.3350</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://onlinelibrary.wiley.com/doi/abs/10.1002/ldr.3350\"\n     onclick=\"log_download('novk-roleek-dresler-hjek-soilcharcoalelucidatestheroleofhumansinthedevelopmentoflandscapeofextremebiodiversity-2019', 'https://onlinelibrary.wiley.com/doi/abs/10.1002/ldr.3350', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Soil charcoal elucidates the role of humans in the development of landscape of extreme biodiversity [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1002/ldr.3350\"\n     onclick=\"log_download('novk-roleek-dresler-hjek-soilcharcoalelucidatestheroleofhumansinthedevelopmentoflandscapeofextremebiodiversity-2019', 'http://doi.org/10.1002/ldr.3350', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/novk-roleek-dresler-hjek-soilcharcoalelucidatestheroleofhumansinthedevelopmentoflandscapeofextremebiodiversity-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('novk-roleek-dresler-hjek-soilcharcoalelucidatestheroleofhumansinthedevelopmentoflandscapeofextremebiodiversity-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{novak_soil_2019,\n\ttitle = {Soil charcoal elucidates the role of humans in the development of landscape of extreme biodiversity},\n\tvolume = {30},\n\tcopyright = {© 2019 John Wiley \\&amp; Sons, Ltd.},\n\tissn = {1099-145X},\n\turl = {https://onlinelibrary.wiley.com/doi/abs/10.1002/ldr.3350},\n\tdoi = {10.1002/ldr.3350},\n\tabstract = {The south-western White Carpathians (Czech Republic, Slovakia) are one of the few places in low-elevation Central Europe where a diverse landscape, including extremely species rich meadows, scattered oak trees, and mixed oak woodlands, has escaped modern transformation. We studied C14-dated and taxonomically identified macroscopic soil charcoal record to elucidate the genesis of this landscape. Thirteen soil profiles were sampled in grasslands along a gradient of elevation and history of human settlement. We identified clear pattern in the taxonomic composition of woody soil charcoal and anthracomass along this gradient, which we ascribe to different pathways of landscape development. Charcoal assemblages of chernozem-like soils in the promontories of the mountain range have a low anthracomass and are dominated by heliophilous and semishade species (Quercus, Pinus), with the oldest charcoals dated to pre-Neolithic times. Soils of the middle elevations have a high anthracomass and often show pronounced differences in charcoal composition at different soil depths; the oldest charcoal samples date back between the Neolithic and Early Middle Ages, and heliophilous species increase towards the topsoil. The soil of the summit area shows a medium anthracomass and charcoal assemblage dominated by shade-tolerant trees; the charcoal dates from the Middle Ages. Our results suggest continuity of an open to semiopen landscape in lower elevations of the White Carpathians, whereas middle and higher elevations experienced a forested period. Humans and fire played an important role in landscape development, as indicated by both soil charcoal and available palaeoecological and archaeological evidence. Local meadows with extremely high biodiversity thus appear to be a continuation of an ancient forest-steppe-like ecosystem.},\n\tlanguage = {en},\n\tnumber = {13},\n\turldate = {2020-03-05},\n\tjournal = {Land Degradation \\&amp; Development},\n\tauthor = {Novák, Jan and Roleček, Jan and Dresler, Petr and Hájek, Michal},\n\tyear = {2019},\n\tnote = {\\_eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/ldr.3350},\n\tkeywords = {Holocene, biodiversity, forest-steppe, human settlement, soil charcoal},\n\tpages = {1607--1619},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The south-western White Carpathians (Czech Republic, Slovakia) are one of the few places in low-elevation Central Europe where a diverse landscape, including extremely species rich meadows, scattered oak trees, and mixed oak woodlands, has escaped modern transformation. We studied C14-dated and taxonomically identified macroscopic soil charcoal record to elucidate the genesis of this landscape. Thirteen soil profiles were sampled in grasslands along a gradient of elevation and history of human settlement. We identified clear pattern in the taxonomic composition of woody soil charcoal and anthracomass along this gradient, which we ascribe to different pathways of landscape development. Charcoal assemblages of chernozem-like soils in the promontories of the mountain range have a low anthracomass and are dominated by heliophilous and semishade species (Quercus, Pinus), with the oldest charcoals dated to pre-Neolithic times. Soils of the middle elevations have a high anthracomass and often show pronounced differences in charcoal composition at different soil depths; the oldest charcoal samples date back between the Neolithic and Early Middle Ages, and heliophilous species increase towards the topsoil. The soil of the summit area shows a medium anthracomass and charcoal assemblage dominated by shade-tolerant trees; the charcoal dates from the Middle Ages. Our results suggest continuity of an open to semiopen landscape in lower elevations of the White Carpathians, whereas middle and higher elevations experienced a forested period. Humans and fire played an important role in landscape development, as indicated by both soil charcoal and available palaeoecological and archaeological evidence. Local meadows with extremely high biodiversity thus appear to be a continuation of an ancient forest-steppe-like ecosystem.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"novk-abraham-da-pokorn-holoceneforesttransformationsinsandstonelandscapesoftheczechrepublicstandscalecomparisonofcharcoalandpollenrecords-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://journals.sagepub.com/doi/10.1177/0959683619854510\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'novk-abraham-da-pokorn-holoceneforesttransformationsinsandstonelandscapesoftheczechrepublicstandscalecomparisonofcharcoalandpollenrecords-2019', 'https://journals.sagepub.com/doi/10.1177/0959683619854510', event);\">\n    Holocene forest transformations in sandstone landscapes of the Czech Republic: Stand-scale comparison of charcoal and pollen records:.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Novák, J.; Abraham, V.; Šída, P.;  and Pokorný, P.\n</span>\n\n  \n\n</span>\n\n  <i>The Holocene</i>. June 2019.\n  <span class=\"note\">Publisher: SAGE PublicationsSage UK: London, England</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://journals.sagepub.com/doi/10.1177/0959683619854510\"\n     onclick=\"log_download('novk-abraham-da-pokorn-holoceneforesttransformationsinsandstonelandscapesoftheczechrepublicstandscalecomparisonofcharcoalandpollenrecords-2019', 'https://journals.sagepub.com/doi/10.1177/0959683619854510', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Holocene forest transformations in sandstone landscapes of the Czech Republic: Stand-scale comparison of charcoal and pollen records: [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1177/0959683619854510\"\n     onclick=\"log_download('novk-abraham-da-pokorn-holoceneforesttransformationsinsandstonelandscapesoftheczechrepublicstandscalecomparisonofcharcoalandpollenrecords-2019', 'http://doi.org/10.1177/0959683619854510', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/novk-abraham-da-pokorn-holoceneforesttransformationsinsandstonelandscapesoftheczechrepublicstandscalecomparisonofcharcoalandpollenrecords-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('novk-abraham-da-pokorn-holoceneforesttransformationsinsandstonelandscapesoftheczechrepublicstandscalecomparisonofcharcoalandpollenrecords-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{novak_holocene_2019,\n\ttitle = {Holocene forest transformations in sandstone landscapes of the {Czech} {Republic}: {Stand}-scale comparison of charcoal and pollen records:},\n\tshorttitle = {Holocene forest transformations in sandstone landscapes of the {Czech} {Republic}},\n\turl = {https://journals.sagepub.com/doi/10.1177/0959683619854510},\n\tdoi = {10.1177/0959683619854510},\n\tabstract = {Stand-scale palaeoecology in sandstone landscapes provides insight into contrasting Holocene forest succession trajectories. Sharp geomorphological gradients in...},\n\tlanguage = {en},\n\turldate = {2020-03-05},\n\tjournal = {The Holocene},\n\tauthor = {Novák, Jan and Abraham, Vojtěch and Šída, Petr and Pokorný, Petr},\n\tmonth = jun,\n\tyear = {2019},\n\tnote = {Publisher: SAGE PublicationsSage UK: London, England},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Stand-scale palaeoecology in sandstone landscapes provides insight into contrasting Holocene forest succession trajectories. Sharp geomorphological gradients in...\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"hoek-prach-kek-da-moska-pokorn-buriedlateweichselianthermokarstlandscapediscoveredintheczechrepubliccentraleurope-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Buried Late Weichselian thermokarst landscape discovered in the Czech Republic, central Europe.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Hošek, J.; Prach, J.; Křížek, M.; Šída, P.; Moska, P.;  and Pokorný, P.\n</span>\n\n  \n\n</span>\n\n  <i>Boreas</i>, 48(4): 988–1005.  2019.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1111/bor.12404\"\n     onclick=\"log_download('hoek-prach-kek-da-moska-pokorn-buriedlateweichselianthermokarstlandscapediscoveredintheczechrepubliccentraleurope-2019', 'http://doi.org/10.1111/bor.12404', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/hoek-prach-kek-da-moska-pokorn-buriedlateweichselianthermokarstlandscapediscoveredintheczechrepubliccentraleurope-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('hoek-prach-kek-da-moska-pokorn-buriedlateweichselianthermokarstlandscapediscoveredintheczechrepubliccentraleurope-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{hosek_buried_2019,\n\ttitle = {Buried {Late} {Weichselian} thermokarst landscape discovered in the {Czech} {Republic}, central {Europe}},\n\tvolume = {48},\n\tcopyright = {© 2019 Collegium Boreas. Published by John Wiley \\&amp; Sons Ltd},\n\tissn = {1502-3885},\n\tdoi = {10.1111/bor.12404},\n\tabstract = {Pronounced climatic warming associated with the Late Weichselian Pleniglacial-to-Lateglacial transition caused considerable environmental changes throughout the former periglacial zones (in Europe 53°–46°N). During permafrost degradation and subsequent ground subsidence (i.e. thermokarst processes), the landscape changed rapidly. In this study we investigated a flat mid-altitude area in south Bohemia, Czech Republic, lying close to the southern limit of the Weichselian permafrost. We discovered palaeo-lake basins with sedimentary infillings up to 11 m in depth. According to radiocarbon and palynostratigraphical dating, these basins were formed at the onset of the Late Pleniglacial-to-Lateglacial transition, whereas the smaller depressions were formed later. We suggest that the basins resulted from thermal and fluvio-thermal erosion of the former permafrost and represent remnants of discontinuous gullies and possibly collapsed frost mounds (pingo/lithalsa scars). The formation of this a fossil thermokarst landscape was climatically driven and multiple phased, with the major phase during the climatic warming and wetting at the onset of GI-1e (Bølling) and the minor phase during GI-1c (Allerød). This study enhances knowledge of the palaeogeography of the former European periglacial zone by showing that Late Pleistocene thermokarst activity could have had a significant impact on the evolution of the landscape of at least some regions of central Europe along the southern limit of the continuous permafrost zone. The research also points to a similar history for the physical transformation of the landscape of the former European periglacial zone and current thermokarst landscapes and could be a valuable source of information with respect to the future transformation of the Arctic under conditions of ongoing global warming.},\n\tlanguage = {English},\n\tnumber = {4},\n\turldate = {2020-03-05},\n\tjournal = {Boreas},\n\tauthor = {Hošek, Jan and Prach, Jindřich and Křížek, Marek and Šída, Petr and Moska, Piotr and Pokorný, Petr},\n\tyear = {2019},\n\tpages = {988--1005},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Pronounced climatic warming associated with the Late Weichselian Pleniglacial-to-Lateglacial transition caused considerable environmental changes throughout the former periglacial zones (in Europe 53°–46°N). During permafrost degradation and subsequent ground subsidence (i.e. thermokarst processes), the landscape changed rapidly. In this study we investigated a flat mid-altitude area in south Bohemia, Czech Republic, lying close to the southern limit of the Weichselian permafrost. We discovered palaeo-lake basins with sedimentary infillings up to 11 m in depth. According to radiocarbon and palynostratigraphical dating, these basins were formed at the onset of the Late Pleniglacial-to-Lateglacial transition, whereas the smaller depressions were formed later. We suggest that the basins resulted from thermal and fluvio-thermal erosion of the former permafrost and represent remnants of discontinuous gullies and possibly collapsed frost mounds (pingo/lithalsa scars). The formation of this a fossil thermokarst landscape was climatically driven and multiple phased, with the major phase during the climatic warming and wetting at the onset of GI-1e (Bølling) and the minor phase during GI-1c (Allerød). This study enhances knowledge of the palaeogeography of the former European periglacial zone by showing that Late Pleistocene thermokarst activity could have had a significant impact on the evolution of the landscape of at least some regions of central Europe along the southern limit of the continuous permafrost zone. The research also points to a similar history for the physical transformation of the landscape of the former European periglacial zone and current thermokarst landscapes and could be a valuable source of information with respect to the future transformation of the Arctic under conditions of ongoing global warming.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"lkov-chvojka-hlsek-jik-john-novk-kovaikov-bene-cropsalongthetraderoutesarchaeobotanyofthebronzeageintheregionofsouthbohemiaczechrepublicincontextwithlongerdistancetradeandexchangenetworks-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Crops along the trade routes? Archaeobotany of the Bronze Age in the region of South Bohemia (Czech Republic) in context with longer distance trade and exchange networks.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Šálková, T.; Chvojka, O.; Hlásek, D.; Jiřík, J.; John, J.; Novák, J.; Kovačiková, L.;  and Beneš, J.\n</span>\n\n  \n\n</span>\n\n  <i>Archaeological and Anthropological Sciences</i>, 11(10): 5569–5590. October 2019.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s12520-019-00893-6\"\n     onclick=\"log_download('lkov-chvojka-hlsek-jik-john-novk-kovaikov-bene-cropsalongthetraderoutesarchaeobotanyofthebronzeageintheregionofsouthbohemiaczechrepublicincontextwithlongerdistancetradeandexchangenetworks-2019', 'http://doi.org/10.1007/s12520-019-00893-6', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/lkov-chvojka-hlsek-jik-john-novk-kovaikov-bene-cropsalongthetraderoutesarchaeobotanyofthebronzeageintheregionofsouthbohemiaczechrepublicincontextwithlongerdistancetradeandexchangenetworks-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('lkov-chvojka-hlsek-jik-john-novk-kovaikov-bene-cropsalongthetraderoutesarchaeobotanyofthebronzeageintheregionofsouthbohemiaczechrepublicincontextwithlongerdistancetradeandexchangenetworks-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{salkova_crops_2019,\n\ttitle = {Crops along the trade routes? {Archaeobotany} of the {Bronze} {Age} in the region of {South} {Bohemia} ({Czech} {Republic}) in context with longer distance trade and exchange networks},\n\tvolume = {11},\n\tissn = {1866-9565},\n\tshorttitle = {Crops along the trade routes?},\n\tdoi = {10.1007/s12520-019-00893-6},\n\tabstract = {The number of species of crop plants in Central Europe increased constantly during the Bronze Age. The structure of the composition of cultivated plants was probably connected to the cultural contacts of human populations. During the Bronze Age (2300/2000–800 BC), the region of South Bohemia (Czech Republic) increasingly became the focus of long-distance trade and exchange networks with regions to the east and many other regions (the Eastern Alps, the Alpine Foreland, the central lowlands of the Czech Republic, Hungary and Western Slovakia). The aim of the paper is to examine archaeobotanical assemblages of charred plant remains to see if these changes within Bronze Age societies, and their spheres of interaction, are also recorded within their agricultural practices. In particular, the importance of specific individual crop species can be reflected in the study region in comparison with other individual regions of Central Europe. Humans in the region of South Bohemia had more connections with the Eastern Alps and the Alpine Foreland region during the Early and Middle Bronze Ages. Regarding the structure of crop species, the composition of sub/dominant crops in South Bohemia and the Eastern Alps and the Alpine Foreland had many similarities. The cultural trajectory of the human populations of the South Bohemian region changed substantially in the Late and Final Bronze Ages: intensive contacts are documented, primarily with the region of Central Bohemia. This is reflected in the composition of the sub/dominant crops in South Bohemia, which shows many similarities to the other regions of the Czech Republic. Changes in migration and exchange networks—in particular those that involved more formalised trade—are associated with a large number of innovations and specific goods and led to much wider levels of cultural and social integration within Bronze Age Europe than had been previously seen.},\n\tlanguage = {English},\n\tnumber = {10},\n\turldate = {2020-03-05},\n\tjournal = {Archaeological and Anthropological Sciences},\n\tauthor = {Šálková, Tereza and Chvojka, Ondřej and Hlásek, Daniel and Jiřík, Jaroslav and John, Jan and Novák, Jan and Kovačiková, Lenka and Beneš, Jaromír},\n\tmonth = oct,\n\tyear = {2019},\n\tpages = {5569--5590},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The number of species of crop plants in Central Europe increased constantly during the Bronze Age. The structure of the composition of cultivated plants was probably connected to the cultural contacts of human populations. During the Bronze Age (2300/2000–800 BC), the region of South Bohemia (Czech Republic) increasingly became the focus of long-distance trade and exchange networks with regions to the east and many other regions (the Eastern Alps, the Alpine Foreland, the central lowlands of the Czech Republic, Hungary and Western Slovakia). The aim of the paper is to examine archaeobotanical assemblages of charred plant remains to see if these changes within Bronze Age societies, and their spheres of interaction, are also recorded within their agricultural practices. In particular, the importance of specific individual crop species can be reflected in the study region in comparison with other individual regions of Central Europe. Humans in the region of South Bohemia had more connections with the Eastern Alps and the Alpine Foreland region during the Early and Middle Bronze Ages. Regarding the structure of crop species, the composition of sub/dominant crops in South Bohemia and the Eastern Alps and the Alpine Foreland had many similarities. The cultural trajectory of the human populations of the South Bohemian region changed substantially in the Late and Final Bronze Ages: intensive contacts are documented, primarily with the region of Central Bohemia. This is reflected in the composition of the sub/dominant crops in South Bohemia, which shows many similarities to the other regions of the Czech Republic. Changes in migration and exchange networks—in particular those that involved more formalised trade—are associated with a large number of innovations and specific goods and led to much wider levels of cultural and social integration within Bronze Age Europe than had been previously seen.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"tich-beta-vondrk-houfkov-jankovsk-nutrientavailabilityaffectedshallowlakeecosystemresponsealongthelateglacialholocenetransition-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Nutrient availability affected shallow-lake ecosystem response along the Late-Glacial/Holocene transition.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Tichá, A.; Bešta, T.; Vondrák, D.; Houfková, P.;  and Jankovská, V.\n</span>\n\n  \n\n</span>\n\n  <i>Hydrobiologia</i>, 846(1): 87–108. December 2019.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s10750-019-04054-7\"\n     onclick=\"log_download('tich-beta-vondrk-houfkov-jankovsk-nutrientavailabilityaffectedshallowlakeecosystemresponsealongthelateglacialholocenetransition-2019', 'http://doi.org/10.1007/s10750-019-04054-7', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/tich-beta-vondrk-houfkov-jankovsk-nutrientavailabilityaffectedshallowlakeecosystemresponsealongthelateglacialholocenetransition-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('tich-beta-vondrk-houfkov-jankovsk-nutrientavailabilityaffectedshallowlakeecosystemresponsealongthelateglacialholocenetransition-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{ticha_nutrient_2019,\n\ttitle = {Nutrient availability affected shallow-lake ecosystem response along the {Late}-{Glacial}/{Holocene} transition},\n\tvolume = {846},\n\tissn = {1573-5117},\n\tdoi = {10.1007/s10750-019-04054-7},\n\tabstract = {Shallow lowland lakes undergo long-lasting natural eutrophication processes, which can be studied through the development of communities of aquatic organisms. However, records showing millennial-scale trophic status variability in these water bodies are rare. Two radiocarbon-dated sedimentary profiles from former (now destroyed by brown coal mining) Lake Komořany (Central Europe, Czech Republic) served for a multi-proxy study of biological remains (diatoms, chironomids, pollen) supplemented by X-ray fluorescence (XRF) and loss-on-ignition (LOI). The age–depth model and palynostratigraphy confirm a continuous Late-Glacial to Early-Holocene record. The results suggest consistent in-lake conditions with high nutrient availability since the lake origin in the Late-Glacial period. A distinct shift at the Late-Glacial/Holocene boundary evidenced by an enhancement in diatom valve concentration and a lithological interface was foregone by a qualitative change in diatom and chironomid assemblages along with rise in LOI. It suggests that a major transformation occurred before the onset of the Holocene. As this qualitative change was characterized by a decrease in relative abundance of nutrient-demanding species, we propose an indirect climatic control by means of nutrient availability as the main driver of the aquatic species composition.},\n\tlanguage = {English},\n\tnumber = {1},\n\turldate = {2020-03-05},\n\tjournal = {Hydrobiologia},\n\tauthor = {Tichá, Anna and Bešta, Tomáš and Vondrák, Daniel and Houfková, Petra and Jankovská, Vlasta},\n\tmonth = dec,\n\tyear = {2019},\n\tpages = {87--108},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Shallow lowland lakes undergo long-lasting natural eutrophication processes, which can be studied through the development of communities of aquatic organisms. However, records showing millennial-scale trophic status variability in these water bodies are rare. Two radiocarbon-dated sedimentary profiles from former (now destroyed by brown coal mining) Lake Komořany (Central Europe, Czech Republic) served for a multi-proxy study of biological remains (diatoms, chironomids, pollen) supplemented by X-ray fluorescence (XRF) and loss-on-ignition (LOI). The age–depth model and palynostratigraphy confirm a continuous Late-Glacial to Early-Holocene record. The results suggest consistent in-lake conditions with high nutrient availability since the lake origin in the Late-Glacial period. A distinct shift at the Late-Glacial/Holocene boundary evidenced by an enhancement in diatom valve concentration and a lithological interface was foregone by a qualitative change in diatom and chironomid assemblages along with rise in LOI. It suggests that a major transformation occurred before the onset of the Holocene. As this qualitative change was characterized by a decrease in relative abundance of nutrient-demanding species, we propose an indirect climatic control by means of nutrient availability as the main driver of the aquatic species composition.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"houfkov-hork-pokorn-beta-pravcov-novk-klr-thedynamicsofanonforestedstandinthekrunmtstheeffectofashortlivedmedievalvillageonthelocalenvironment-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.1007/s00334-019-00718-5\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'houfkov-hork-pokorn-beta-pravcov-novk-klr-thedynamicsofanonforestedstandinthekrunmtstheeffectofashortlivedmedievalvillageonthelocalenvironment-2019', 'https://doi.org/10.1007/s00334-019-00718-5', event);\">\n    The dynamics of a non-forested stand in the Krušné Mts.: the effect of a short-lived medieval village on the local environment.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Houfková, P.; Horák, J.; Pokorná, A.; Bešta, T.; Pravcová, I.; Novák, J.;  and Klír, T.\n</span>\n\n  \n\n</span>\n\n  <i>Vegetation History and Archaeobotany</i>, 28(6): 607–621. November 2019.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://doi.org/10.1007/s00334-019-00718-5\"\n     onclick=\"log_download('houfkov-hork-pokorn-beta-pravcov-novk-klr-thedynamicsofanonforestedstandinthekrunmtstheeffectofashortlivedmedievalvillageonthelocalenvironment-2019', 'https://doi.org/10.1007/s00334-019-00718-5', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"The dynamics of a non-forested stand in the Krušné Mts.: the effect of a short-lived medieval village on the local environment [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s00334-019-00718-5\"\n     onclick=\"log_download('houfkov-hork-pokorn-beta-pravcov-novk-klr-thedynamicsofanonforestedstandinthekrunmtstheeffectofashortlivedmedievalvillageonthelocalenvironment-2019', 'http://doi.org/10.1007/s00334-019-00718-5', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/houfkov-hork-pokorn-beta-pravcov-novk-klr-thedynamicsofanonforestedstandinthekrunmtstheeffectofashortlivedmedievalvillageonthelocalenvironment-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('houfkov-hork-pokorn-beta-pravcov-novk-klr-thedynamicsofanonforestedstandinthekrunmtstheeffectofashortlivedmedievalvillageonthelocalenvironment-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{houfkova_dynamics_2019,\n\ttitle = {The dynamics of a non-forested stand in the {Krušné} {Mts}.: the effect of a short-lived medieval village on the local environment},\n\tvolume = {28},\n\tissn = {1617-6278},\n\tshorttitle = {The dynamics of a non-forested stand in the {Krušné} {Mts}.},\n\turl = {https://doi.org/10.1007/s00334-019-00718-5},\n\tdoi = {10.1007/s00334-019-00718-5},\n\tabstract = {Medieval vegetation–human–climate interactions were studied from a sediment profile situated in the centre of a short-lived medieval village located above 800 m a.s.l. on the ridge of the Krušné Mts., NW Bohemia, Central Europe. Analyses of pollen, seeds/fruits, micro- and macro-charcoals, diatoms and concentrations of microelements in connection with written sources revealed a significant human-induced deforestation in the second half of the 14th century. This deforestation occurred sooner than supposed and the area did not revert after ad 1347 as elsewhere in Europe. Arable fields probably enabled basic self-sustaining cultivation of winter cereals even at such elevations in the climatically favourable years of the Medieval Warm Period. The village presumably collapsed due to a combination of weather fluctuations at the onset of the Little Ice Age, simultaneous socioeconomic stagnation in the Czech Lands and exploitation of the surrounding forest. The dynamics of wet stand vegetation and Calthion palustris montane wet meadows were driven by fluctuating human and grazing impacts. Annual and biennial herbaceous species that peaked after village abandonment were rapidly replaced by Filipendula ulmaria and Salix stands. The secondary forest developed towards Picea stands. Only later, mesic montane meadows of medium tall grasses combined with Meum athamanticum and mountain dry pastures developed on nutrient poor patches.},\n\tlanguage = {en},\n\tnumber = {6},\n\turldate = {2020-03-05},\n\tjournal = {Vegetation History and Archaeobotany},\n\tauthor = {Houfková, Petra and Horák, Jan and Pokorná, Adéla and Bešta, Tomáš and Pravcová, Ivana and Novák, Jan and Klír, Tomáš},\n\tmonth = nov,\n\tyear = {2019},\n\tpages = {607--621},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Medieval vegetation–human–climate interactions were studied from a sediment profile situated in the centre of a short-lived medieval village located above 800 m a.s.l. on the ridge of the Krušné Mts., NW Bohemia, Central Europe. Analyses of pollen, seeds/fruits, micro- and macro-charcoals, diatoms and concentrations of microelements in connection with written sources revealed a significant human-induced deforestation in the second half of the 14th century. This deforestation occurred sooner than supposed and the area did not revert after ad 1347 as elsewhere in Europe. Arable fields probably enabled basic self-sustaining cultivation of winter cereals even at such elevations in the climatically favourable years of the Medieval Warm Period. The village presumably collapsed due to a combination of weather fluctuations at the onset of the Little Ice Age, simultaneous socioeconomic stagnation in the Czech Lands and exploitation of the surrounding forest. The dynamics of wet stand vegetation and Calthion palustris montane wet meadows were driven by fluctuating human and grazing impacts. Annual and biennial herbaceous species that peaked after village abandonment were rapidly replaced by Filipendula ulmaria and Salix stands. The secondary forest developed towards Picea stands. Only later, mesic montane meadows of medium tall grasses combined with Meum athamanticum and mountain dry pastures developed on nutrient poor patches.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"jamrichov-bobek-olcov-tk-hdl-valachovi-lowlandpineforestsinthenorthwesternpannonianbasinbetweennaturalvegetationandmodernplantations-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Lowland pine forests in the northwestern Pannonian Basin: between natural vegetation and modern plantations.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Jamrichová, E.; Bobek, P.; Šolcová, A.; Tkáč, P.; Hédl, R.;  and Valachovič, M.\n</span>\n\n  \n\n</span>\n\n  <i>Regional Environmental Change</i>, 19(8): 2395–2409. December 2019.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s10113-019-01555-y\"\n     onclick=\"log_download('jamrichov-bobek-olcov-tk-hdl-valachovi-lowlandpineforestsinthenorthwesternpannonianbasinbetweennaturalvegetationandmodernplantations-2019', 'http://doi.org/10.1007/s10113-019-01555-y', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/jamrichov-bobek-olcov-tk-hdl-valachovi-lowlandpineforestsinthenorthwesternpannonianbasinbetweennaturalvegetationandmodernplantations-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('jamrichov-bobek-olcov-tk-hdl-valachovi-lowlandpineforestsinthenorthwesternpannonianbasinbetweennaturalvegetationandmodernplantations-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{jamrichova_lowland_2019,\n\ttitle = {Lowland pine forests in the northwestern {Pannonian} {Basin}: between natural vegetation and modern plantations},\n\tvolume = {19},\n\tissn = {1436-378X},\n\tshorttitle = {Lowland pine forests in the northwestern {Pannonian} {Basin}},\n\tdoi = {10.1007/s10113-019-01555-y},\n\tabstract = {Lowland Scots pine (Pinus sylvestris L.) forests cover extensive areas in Central Europe. Most of them are considered to be the results of relatively recent plantation-oriented forest management. We investigated the long-term history of lowland pine forests in the Záhorská Lowland region of aeolian sands in the northern margin of the Pannonian Basin. Pine monocultures were planted there already in the mid-seventeenth century and currently prevail in the land cover of the region. Our aim was to challenge the commonly accepted idea that the present pine-dominated forests lack connections to pre-plantation pine forests of the Early Holocene. Using multi-proxy data, we compared palaeoeocological data with archaeobotanical data, anthracological finds and evidence on past human settlement. Palaeoecological results suggested a distinct compositional linkage of recent pine-dominated forests with their Early Holocene predecessors. Moreover, no significant change was detected in tree dominants in at least the past two millennia. Contrary to palaeoecology, archeaeobotany suggested that broadleaved trees (mostly oak) dominated during the past 4000 years. However, this result is probably strongly biased by human preferences for wood for specific purposes. On the other hand, pine in palaeoecological data is doubtless overrepresented because of its abundant pollen production. We conclude that pine forests with a significant admixture of oak continuously covered the sandy substrates of the Záhorská Lowland throughout the Holocene. The present pine forests can therefore be considered fairly close to the original vegetation of the study region.},\n\tlanguage = {English},\n\tnumber = {8},\n\turldate = {2020-03-05},\n\tjournal = {Regional Environmental Change},\n\tauthor = {Jamrichová, Eva and Bobek, Přemysl and Šolcová, Anna and Tkáč, Peter and Hédl, Radim and Valachovič, Milan},\n\tmonth = dec,\n\tyear = {2019},\n\tpages = {2395--2409},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Lowland Scots pine (Pinus sylvestris L.) forests cover extensive areas in Central Europe. Most of them are considered to be the results of relatively recent plantation-oriented forest management. We investigated the long-term history of lowland pine forests in the Záhorská Lowland region of aeolian sands in the northern margin of the Pannonian Basin. Pine monocultures were planted there already in the mid-seventeenth century and currently prevail in the land cover of the region. Our aim was to challenge the commonly accepted idea that the present pine-dominated forests lack connections to pre-plantation pine forests of the Early Holocene. Using multi-proxy data, we compared palaeoeocological data with archaeobotanical data, anthracological finds and evidence on past human settlement. Palaeoecological results suggested a distinct compositional linkage of recent pine-dominated forests with their Early Holocene predecessors. Moreover, no significant change was detected in tree dominants in at least the past two millennia. Contrary to palaeoecology, archeaeobotany suggested that broadleaved trees (mostly oak) dominated during the past 4000 years. However, this result is probably strongly biased by human preferences for wood for specific purposes. On the other hand, pine in palaeoecological data is doubtless overrepresented because of its abundant pollen production. We conclude that pine forests with a significant admixture of oak continuously covered the sandy substrates of the Záhorská Lowland throughout the Holocene. The present pine forests can therefore be considered fairly close to the original vegetation of the study region.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"kune-abraham-herben-changingdisturbancediversityrelationshipsintemperateecosystemsoverthepast12000years-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Changing disturbance-diversity relationships in temperate ecosystems over the past 12000 years.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Abraham, V.;  and Herben, T.\n</span>\n\n  \n\n</span>\n\n  <i>Journal of Ecology</i>, 107(4): 1678–1688.  2019.\n  <span class=\"note\">[IF2018=5.687]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1111/1365-2745.13136\"\n     onclick=\"log_download('kune-abraham-herben-changingdisturbancediversityrelationshipsintemperateecosystemsoverthepast12000years-2019', 'http://doi.org/10.1111/1365-2745.13136', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kune-abraham-herben-changingdisturbancediversityrelationshipsintemperateecosystemsoverthepast12000years-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>4 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kune-abraham-herben-changingdisturbancediversityrelationshipsintemperateecosystemsoverthepast12000years-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{kunes_changing_2019,\n\ttitle = {Changing disturbance-diversity relationships in temperate ecosystems over the past 12000 years},\n\tvolume = {107},\n\tcopyright = {© 2019 The Authors. Journal of Ecology © 2019 British Ecological Society},\n\tissn = {1365-2745},\n\tdoi = {10.1111/1365-2745.13136},\n\tabstract = {Disturbances such as fires and grazing have major impacts on biodiversity. While it has been suggested that species richness is highest with intermediate levels of disturbance, currently there is no consensus due to an absence of data covering large temporal and spatial scales. We developed a new method to examine disturbance-diversity relationships (DDR) using sedimentary pollen data linked with species’ disturbance ecology. We reconstructed disturbance and diversity dynamics in the region of the European temperate zone over the last 12,000 years and calculated DDR for 900-year sequential temporal windows. Disturbance frequency was highest in the early and late Holocene, while remaining low in the mid-Holocene. Diversity increased continuously from the start of the Holocene. Our results demonstrate that over the past 12,000 years DDR changed from hump-shaped into monotonic increasing pattern. While both highly disturbed and undisturbed sites were strongly impoverished in the early Holocene, as species migrated, biodiversity levels have subsequently affected disturbance regimes with highly disturbed sites now being the highest in species richness. Synthesis. Land-use changes in the last 4,000 years created an increasingly patchy landscape, allowing invasive species adapted to high-frequency disturbance to migrate across the landscape. The link between high diversity and disturbed areas is relatively recent and may anticipate even greater disturbance frequencies in future. Our findings also support a hypothesis that species migration, and the structure of the species pool critically determines the response of biota to external factors such as disturbance.},\n\tlanguage = {English},\n\tnumber = {4},\n\turldate = {2019-06-28},\n\tjournal = {Journal of Ecology},\n\tauthor = {Kuneš, Petr and Abraham, Vojtěch and Herben, Tomáš},\n\tyear = {2019},\n\tnote = {[IF2018=5.687]},\n\tkeywords = {Central Europe, Holocene, disturbance, disturbance frequency, pollen, richness, vegetation},\n\tpages = {1678--1688},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Disturbances such as fires and grazing have major impacts on biodiversity. While it has been suggested that species richness is highest with intermediate levels of disturbance, currently there is no consensus due to an absence of data covering large temporal and spatial scales. We developed a new method to examine disturbance-diversity relationships (DDR) using sedimentary pollen data linked with species’ disturbance ecology. We reconstructed disturbance and diversity dynamics in the region of the European temperate zone over the last 12,000 years and calculated DDR for 900-year sequential temporal windows. Disturbance frequency was highest in the early and late Holocene, while remaining low in the mid-Holocene. Diversity increased continuously from the start of the Holocene. Our results demonstrate that over the past 12,000 years DDR changed from hump-shaped into monotonic increasing pattern. While both highly disturbed and undisturbed sites were strongly impoverished in the early Holocene, as species migrated, biodiversity levels have subsequently affected disturbance regimes with highly disturbed sites now being the highest in species richness. Synthesis. Land-use changes in the last 4,000 years created an increasingly patchy landscape, allowing invasive species adapted to high-frequency disturbance to migrate across the landscape. The link between high diversity and disturbed areas is relatively recent and may anticipate even greater disturbance frequencies in future. Our findings also support a hypothesis that species migration, and the structure of the species pool critically determines the response of biota to external factors such as disturbance.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"florescu-brown-carter-kune-veski-feurdean-holocenerapidclimatechangesandiceraftingdebriseventsreflectedinhighresolutioneuropeancharcoalrecords-2019\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Holocene rapid climate changes and ice-rafting debris events reflected in high-resolution European charcoal records.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Florescu, G.; Brown, K. J.; Carter, V. A.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Veski, S.;  and Feurdean, A.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Science Reviews</i>, 222: 105877. October 2019.\n  <span class=\"note\">[IF2018=4.641]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quascirev.2019.105877\"\n     onclick=\"log_download('florescu-brown-carter-kune-veski-feurdean-holocenerapidclimatechangesandiceraftingdebriseventsreflectedinhighresolutioneuropeancharcoalrecords-2019', 'http://doi.org/10.1016/j.quascirev.2019.105877', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/florescu-brown-carter-kune-veski-feurdean-holocenerapidclimatechangesandiceraftingdebriseventsreflectedinhighresolutioneuropeancharcoalrecords-2019\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('florescu-brown-carter-kune-veski-feurdean-holocenerapidclimatechangesandiceraftingdebriseventsreflectedinhighresolutioneuropeancharcoalrecords-2019')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{florescu_holocene_2019,\n\ttitle = {Holocene rapid climate changes and ice-rafting debris events reflected in high-resolution {European} charcoal records},\n\tvolume = {222},\n\tissn = {0277-3791},\n\tdoi = {10.1016/j.quascirev.2019.105877},\n\tabstract = {In contrast to marked climate change across glacial-interglacial cycles, the Holocene epoch represents a relatively warm, stable interval. However, on finer temporal scales, it too has experienced both gradual and rapid changes in climate. In the North Atlantic region, many rapid climate changes (RCCs) coincide with ice-rafted debris (IRD) or Bond events, which are associated with cooling and suggested to occur with periodicities of 1370 ± 500 years. Given that climate is a dominant control of fire activity, regulating both vegetation productivity and fuel moisture, this study investigated the linkage between Holocene fire, IRD episodes and associated RCCs in seven high-resolution charcoal records distributed across Europe. Results show low-frequency fire periodicities of 500–600 years, 900–1400 and 2400 years that occurred simultaneously across northern and mid-latitude Europe, suggesting that regional fire disturbance responded to large-scale climate drivers. The 900–1400 year periodicity is most common among sites and of similar frequency to IRD episodes, potentially reflecting a connection between mechanisms regulating IRD flux in the North Atlantic and wildfire activity in Europe. Although the data indicate some spatial variability in fire induced by local drivers (such as vegetation and human impact) during RCC events associated with IRD peaks, broad-scale patterns are discernible. Specifically, Northern Europe burned more during the 10.2, 9.4, 8.2, 5.9 and 4.2 kiloannum before present (ka) RCC events when climate was drier, and less during the 2.9 and 1.4 ka events when climate was moister. In contrast, in mid-latitude Europe, a higher incidence of fire is documented at 8.2 and 1.4 ka when climate was drier and a lower incidence of fire is associated with moister conditions at 10.2, 9.4 and 2.9 ka. Spatial heterogeneity is evident in mid-latitude Europe during the 5.9, 4.2 and 0.4 ka events. These spatially explicit sub-continental scale differences in fire activity may be related to differences in moisture availability resulting from shifts in associated atmospheric circulation patterns.},\n\tlanguage = {English},\n\turldate = {2019-09-08},\n\tjournal = {Quaternary Science Reviews},\n\tauthor = {Florescu, Gabriela and Brown, Kendrick J. and Carter, Vachel A. and Kuneš, Petr and Veski, Siim and Feurdean, Angelica},\n\tmonth = oct,\n\tyear = {2019},\n\tnote = {[IF2018=4.641]},\n\tkeywords = {Europe, Fire cycles, Holocene, Ice rafted debris events, Macroscopic charcoal, Rapid climate change, disturbance},\n\tpages = {105877},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  In contrast to marked climate change across glacial-interglacial cycles, the Holocene epoch represents a relatively warm, stable interval. However, on finer temporal scales, it too has experienced both gradual and rapid changes in climate. In the North Atlantic region, many rapid climate changes (RCCs) coincide with ice-rafted debris (IRD) or Bond events, which are associated with cooling and suggested to occur with periodicities of 1370 ± 500 years. Given that climate is a dominant control of fire activity, regulating both vegetation productivity and fuel moisture, this study investigated the linkage between Holocene fire, IRD episodes and associated RCCs in seven high-resolution charcoal records distributed across Europe. Results show low-frequency fire periodicities of 500–600 years, 900–1400 and 2400 years that occurred simultaneously across northern and mid-latitude Europe, suggesting that regional fire disturbance responded to large-scale climate drivers. The 900–1400 year periodicity is most common among sites and of similar frequency to IRD episodes, potentially reflecting a connection between mechanisms regulating IRD flux in the North Atlantic and wildfire activity in Europe. Although the data indicate some spatial variability in fire induced by local drivers (such as vegetation and human impact) during RCC events associated with IRD peaks, broad-scale patterns are discernible. Specifically, Northern Europe burned more during the 10.2, 9.4, 8.2, 5.9 and 4.2 kiloannum before present (ka) RCC events when climate was drier, and less during the 2.9 and 1.4 ka events when climate was moister. In contrast, in mid-latitude Europe, a higher incidence of fire is documented at 8.2 and 1.4 ka when climate was drier and a lower incidence of fire is associated with moister conditions at 10.2, 9.4 and 2.9 ka. Spatial heterogeneity is evident in mid-latitude Europe during the 5.9, 4.2 and 0.4 ka events. These spatially explicit sub-continental scale differences in fire activity may be related to differences in moisture availability resulting from shifts in associated atmospheric circulation patterns.\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2018\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2018')\"\n      onkeypress=\"toggleGroup('group_2018')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2018</span>\n      <span class=\"bibbase_group_count\">\n        \n        (7)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"kol-kune-szab-hajnalov-svobodov-macek-tk-populationandforestdynamicsduringthecentraleuropeaneneolithic45002000bc-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Population and forest dynamics during the Central European Eneolithic (4500–2000 BC).\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Kolář, J.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Szabó, P.; Hajnalová, M.; Svobodová, H. S.; Macek, M.;  and Tkáč, P.\n</span>\n\n  \n\n</span>\n\n  <i>Archaeological and Anthropological Sciences</i>, 10(5): 1153–1164. August 2018.\n  <span class=\"note\">[IF2017=2.414]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s12520-016-0446-5\"\n     onclick=\"log_download('kol-kune-szab-hajnalov-svobodov-macek-tk-populationandforestdynamicsduringthecentraleuropeaneneolithic45002000bc-2018', 'http://doi.org/10.1007/s12520-016-0446-5', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kol-kune-szab-hajnalov-svobodov-macek-tk-populationandforestdynamicsduringthecentraleuropeaneneolithic45002000bc-2018\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kol-kune-szab-hajnalov-svobodov-macek-tk-populationandforestdynamicsduringthecentraleuropeaneneolithic45002000bc-2018')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{kolar_population_2018,\n\ttitle = {Population and forest dynamics during the {Central} {European} {Eneolithic} (4500–2000 {BC})},\n\tvolume = {10},\n\tcopyright = {All rights reserved},\n\tissn = {1866-9557, 1866-9565},\n\tdoi = {10.1007/s12520-016-0446-5},\n\tabstract = {The population boom-and-bust during the European Neolithic (7000–2000 BC) has been the subject of lively discussion for the past decade. Most of the research on this topic was carried out with help of summed radiocarbon probability distributions. We aim to reconstruct population dynamics within the catchment of a medium sized lake on the basis of information on the presence of all known past human activities. We calculated a human activity model based on Monte Carlo simulations. The model showed the lowest level of human activity between 4000 and 3000 BC. For a better understanding of long-term socio-environmental dynamics, we also used the results of a pollen-based quantitative vegetation model, as well as a local macrophysical climate model. The beginning of the decline of archaeologically visible human activities corresponds with climatic changes and an increase in secondary forest taxa probably indicating more extensive land use. In addition, social and technological innovations are important, such as the introduction of the ard, wheel, animal traction and metallurgy, as well as changes in social hierarchy characterizing the same period.},\n\tlanguage = {English},\n\tnumber = {5},\n\turldate = {2016-12-14},\n\tjournal = {Archaeological and Anthropological Sciences},\n\tauthor = {Kolář, Jan and Kuneš, Petr and Szabó, Péter and Hajnalová, Mária and Svobodová, Helena Svitavská and Macek, Martin and Tkáč, Peter},\n\tmonth = aug,\n\tyear = {2018},\n\tnote = {[IF2017=2.414]},\n\tkeywords = {Czech Republic, MCM model, Neolithic, Population density, REVEALS, climate, conservation, cultural landscape, reconstruction},\n\tpages = {1153--1164},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The population boom-and-bust during the European Neolithic (7000–2000 BC) has been the subject of lively discussion for the past decade. Most of the research on this topic was carried out with help of summed radiocarbon probability distributions. We aim to reconstruct population dynamics within the catchment of a medium sized lake on the basis of information on the presence of all known past human activities. We calculated a human activity model based on Monte Carlo simulations. The model showed the lowest level of human activity between 4000 and 3000 BC. For a better understanding of long-term socio-environmental dynamics, we also used the results of a pollen-based quantitative vegetation model, as well as a local macrophysical climate model. The beginning of the decline of archaeologically visible human activities corresponds with climatic changes and an increase in secondary forest taxa probably indicating more extensive land use. In addition, social and technological innovations are important, such as the introduction of the ard, wheel, animal traction and metallurgy, as well as changes in social hierarchy characterizing the same period.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"carter-chiverrell-clear-kuosmanen-moravcov-svoboda-svobodovsvitavsk-leeuwen-etal-quantitativepalynologyinformingconservationecologyinthebohemianbavarianforestsofcentraleurope-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Quantitative palynology informing conservation ecology in the Bohemian/Bavarian Forests of Central Europe.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Carter, V. A.; Chiverrell, R. C.; Clear, J. L.; Kuosmanen, N.; Moravcová, A.; Svoboda, M.; Svobodová-Svitavská, H.; Leeuwen, V.; Van Leeuwen, J.; van der Knaap, W. O.;  and <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>\n</span>\n\n  \n\n</span>\n\n  <i>Frontiers in Plant Science</i>, 8(Article 2268): 1–14.  2018.\n  <span class=\"note\">[IF2017=3.678]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.3389/fpls.2017.02268\"\n     onclick=\"log_download('carter-chiverrell-clear-kuosmanen-moravcov-svoboda-svobodovsvitavsk-leeuwen-etal-quantitativepalynologyinformingconservationecologyinthebohemianbavarianforestsofcentraleurope-2018', 'http://doi.org/10.3389/fpls.2017.02268', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/carter-chiverrell-clear-kuosmanen-moravcov-svoboda-svobodovsvitavsk-leeuwen-etal-quantitativepalynologyinformingconservationecologyinthebohemianbavarianforestsofcentraleurope-2018\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>2 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('carter-chiverrell-clear-kuosmanen-moravcov-svoboda-svobodovsvitavsk-leeuwen-etal-quantitativepalynologyinformingconservationecologyinthebohemianbavarianforestsofcentraleurope-2018')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{carter_quantitative_2018,\n\ttitle = {Quantitative palynology informing conservation ecology in the {Bohemian}/{Bavarian} {Forests} of {Central} {Europe}},\n\tvolume = {8},\n\tissn = {1664-462X},\n\tdoi = {10.3389/fpls.2017.02268},\n\tabstract = {In 1927, the first pollen diagram was published from the Bohemian/Bavarian Forest region of Central Europe, providing one of the first qualitative views of the long-term vegetation development in the region. Since then significant methodological advances in quantitative approaches such as pollen influx and pollen-based vegetation models (e.g., Landscape Reconstruction Algorithm, LRA) have contributed to enhance our understanding of temporal and spatial ecology. These types of quantitative reconstructions are fundamental for conservation and restoration ecology because they provide long-term perspectives on ecosystem functioning. In the Bohemian/Bavarian Forests, forest managers have a goal to restore the original forest composition at mid-elevation forests, yet they rely on natural potential vegetation maps that do not take into account long-term vegetation dynamics. Here we reconstruct the Holocene history of forest composition and discuss the implications the LRA has for regional forest management and conservation. Two newly analysed pollen records from Prášilské jezero and Rachelsee were compared to 10 regional peat bogs/mires and two other regional lakes to reconstruct total land-cover abundance at both the regional- and local-scales. The results demonstrate that spruce has been the dominate canopy cover across the region for the past 9000 years at both high- ({\\textgreater}900 m) and mid-elevations ({\\textgreater}700-900 m) elevations. At the regional-scale, inferred from lake records, spruce has comprised an average of {\\textasciitilde}50\\% of the total forest canopy; whereas at the more local-scale at mid-elevations, spruce formed {\\textasciitilde}59\\%. Beech established {\\textasciitilde}6000 cal yr BP while fir established {\\textasciitilde}5500 cal yr BP, and reached a maximum land-cover abundance of 24\\% and 13\\% roughly 1000 years ago at mid-elevations. Over the past 500 years spruce has comprised {\\textasciitilde}47\\% land-cover, while beech and fir comprised {\\textasciitilde}8\\% and {\\textless}5\\% at mid-elevations. This approach argues for the ‘natural’ development of spruce and fir locally in zones where the paleoecology indicates the persistence of these species for millennia. Contrasting local and regional reconstructions of forest canopy cover points to a patchwork mosaic with local variability in the dominant taxa. Incorporation of paleoecological data in dialogues about biodiversity and ecosystem management is an approach that has wider utility.},\n\tlanguage = {English},\n\tnumber = {Article 2268},\n\turldate = {2017-12-28},\n\tjournal = {Frontiers in Plant Science},\n\tauthor = {Carter, Vachel A. and Chiverrell, Richard C. and Clear, Jennifer L. and Kuosmanen, Niina and Moravcová, Alice and Svoboda, Miroslav and Svobodová-Svitavská, Helena and Leeuwen, Van and Van Leeuwen, Jacqueline and van der Knaap, Willem O. and Kuneš, Petr},\n\tyear = {2018},\n\tnote = {[IF2017=3.678]},\n\tkeywords = {Abies alba, Fagus sylvatica, Holocene, Picea abies, Pollen, Reveals, disturbance, landcover, palynology, reconstruction},\n\tpages = {1--14},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  In 1927, the first pollen diagram was published from the Bohemian/Bavarian Forest region of Central Europe, providing one of the first qualitative views of the long-term vegetation development in the region. Since then significant methodological advances in quantitative approaches such as pollen influx and pollen-based vegetation models (e.g., Landscape Reconstruction Algorithm, LRA) have contributed to enhance our understanding of temporal and spatial ecology. These types of quantitative reconstructions are fundamental for conservation and restoration ecology because they provide long-term perspectives on ecosystem functioning. In the Bohemian/Bavarian Forests, forest managers have a goal to restore the original forest composition at mid-elevation forests, yet they rely on natural potential vegetation maps that do not take into account long-term vegetation dynamics. Here we reconstruct the Holocene history of forest composition and discuss the implications the LRA has for regional forest management and conservation. Two newly analysed pollen records from Prášilské jezero and Rachelsee were compared to 10 regional peat bogs/mires and two other regional lakes to reconstruct total land-cover abundance at both the regional- and local-scales. The results demonstrate that spruce has been the dominate canopy cover across the region for the past 9000 years at both high- (\\textgreater900 m) and mid-elevations (\\textgreater700-900 m) elevations. At the regional-scale, inferred from lake records, spruce has comprised an average of ~50% of the total forest canopy; whereas at the more local-scale at mid-elevations, spruce formed ~59%. Beech established ~6000 cal yr BP while fir established ~5500 cal yr BP, and reached a maximum land-cover abundance of 24% and 13% roughly 1000 years ago at mid-elevations. Over the past 500 years spruce has comprised ~47% land-cover, while beech and fir comprised ~8% and \\textless5% at mid-elevations. This approach argues for the ‘natural’ development of spruce and fir locally in zones where the paleoecology indicates the persistence of these species for millennia. Contrasting local and regional reconstructions of forest canopy cover points to a patchwork mosaic with local variability in the dominant taxa. Incorporation of paleoecological data in dialogues about biodiversity and ecosystem management is an approach that has wider utility.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"bobek-svitavsksvobodov-werchan-varcov-kune-humaninducedchangesinfireregimeandsubsequentalterationofthesandstonelandscapeofnorthernbohemiaczechrepublic-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Human-induced changes in fire regime and subsequent alteration of the sandstone landscape of Northern Bohemia (Czech Republic).\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Bobek, P.; Svitavská Svobodová, H.; Werchan, B.; Švarcová, M. G.;  and <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>\n</span>\n\n  \n\n</span>\n\n  <i>The Holocene</i>, 28(3): 427–443. March 2018.\n  <span class=\"note\">[IF2017=2.419]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1177/0959683617729443\"\n     onclick=\"log_download('bobek-svitavsksvobodov-werchan-varcov-kune-humaninducedchangesinfireregimeandsubsequentalterationofthesandstonelandscapeofnorthernbohemiaczechrepublic-2018', 'http://doi.org/10.1177/0959683617729443', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/bobek-svitavsksvobodov-werchan-varcov-kune-humaninducedchangesinfireregimeandsubsequentalterationofthesandstonelandscapeofnorthernbohemiaczechrepublic-2018\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('bobek-svitavsksvobodov-werchan-varcov-kune-humaninducedchangesinfireregimeandsubsequentalterationofthesandstonelandscapeofnorthernbohemiaczechrepublic-2018')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{bobek_human-induced_2018,\n\ttitle = {Human-induced changes in fire regime and subsequent alteration of the sandstone landscape of {Northern} {Bohemia} ({Czech} {Republic})},\n\tvolume = {28},\n\tissn = {0959-6836},\n\tdoi = {10.1177/0959683617729443},\n\tabstract = {Multiproxy palaeoecological evidence from a sandstone region in northern Czech Republic was collected to explore the impact of fire disturbances on the decline of the broadleaved forests during the Late Bronze Age (3250–3050 cal. BP). It has been hypothesized that human-accelerated soil leaching affected the nutrient availability in the sandstone area, thus promoting the expansion of oligotrophic-adapted plant communities in the late-Holocene. Little is known about the mechanisms which induced such large-scale vegetation transformation. We sought to determine which driving forces were involved using independent proxy records – soil and sedimentary charcoal, pollen and fungal spores. Local fire history was derived from the variation in charcoal accumulation rates (CHAR) preserved in Eustach peatbog. The fire frequency (FF) estimation over the past {\\textasciitilde}7500 years revealed distinct phases of increased burning between 3100 and 2120 cal. BP (3.0 fires 1000 yr−1) and 1400–600 cal. BP (4.3 fires 1000 yr−1). Rapid compositional changes in the pollen assemblage were documented during the Late Bronze Age period, suggesting vegetation responded to increased fire disturbances. The human influence on the fire regime is implied by the short-term increase in cereal pollen concurrent with a major fire event, indicating possible use of slash-and-burn cultivation by Late Bronze societies. This type of human subsistence strategy practised in the sandstone landscape further evolved to pastoralism as suggested by continuous presence of coprophilous fungi Sporormiella and Sordaria, which occurred since the Hallstatt/La Tène period (2750–1950 cal. BP). Our study documents, for the first time, the intentional, human-caused biomass burning from densely forested areas of Northern Bohemian sandstone region. Our results imply that increased rate of fire disturbances contributed to the Late Bronze Age transformation of broadleaved forests to oligotrophic forest communities of late-Holocene.},\n\tlanguage = {English},\n\tnumber = {3},\n\turldate = {2018-03-31},\n\tjournal = {The Holocene},\n\tauthor = {Bobek, Přemysl and Svitavská Svobodová, Helena and Werchan, Barbora and Švarcová, Markéta Gabriela and Kuneš, Petr},\n\tmonth = mar,\n\tyear = {2018},\n\tnote = {[IF2017=2.419]},\n\tkeywords = {disturbance},\n\tpages = {427--443},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Multiproxy palaeoecological evidence from a sandstone region in northern Czech Republic was collected to explore the impact of fire disturbances on the decline of the broadleaved forests during the Late Bronze Age (3250–3050 cal. BP). It has been hypothesized that human-accelerated soil leaching affected the nutrient availability in the sandstone area, thus promoting the expansion of oligotrophic-adapted plant communities in the late-Holocene. Little is known about the mechanisms which induced such large-scale vegetation transformation. We sought to determine which driving forces were involved using independent proxy records – soil and sedimentary charcoal, pollen and fungal spores. Local fire history was derived from the variation in charcoal accumulation rates (CHAR) preserved in Eustach peatbog. The fire frequency (FF) estimation over the past ~7500 years revealed distinct phases of increased burning between 3100 and 2120 cal. BP (3.0 fires 1000 yr−1) and 1400–600 cal. BP (4.3 fires 1000 yr−1). Rapid compositional changes in the pollen assemblage were documented during the Late Bronze Age period, suggesting vegetation responded to increased fire disturbances. The human influence on the fire regime is implied by the short-term increase in cereal pollen concurrent with a major fire event, indicating possible use of slash-and-burn cultivation by Late Bronze societies. This type of human subsistence strategy practised in the sandstone landscape further evolved to pastoralism as suggested by continuous presence of coprophilous fungi Sporormiella and Sordaria, which occurred since the Hallstatt/La Tène period (2750–1950 cal. BP). Our study documents, for the first time, the intentional, human-caused biomass burning from densely forested areas of Northern Bohemian sandstone region. Our results imply that increased rate of fire disturbances contributed to the Late Bronze Age transformation of broadleaved forests to oligotrophic forest communities of late-Holocene.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"carter-moravcov-chiverrell-clear-finsinger-dreslerov-halsall-kune-holocenescalefiredynamicsofcentraleuropeantemperatesprucebeechforests-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Holocene-scale fire dynamics of central European temperate spruce-beech forests.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Carter, V. A.; Moravcová, A.; Chiverrell, R. C.; Clear, J. L.; Finsinger, W.; Dreslerová, D.; Halsall, K.;  and <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Science Reviews</i>, 191: 15–30. July 2018.\n  <span class=\"note\">[IF2017=4.334]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quascirev.2018.05.001\"\n     onclick=\"log_download('carter-moravcov-chiverrell-clear-finsinger-dreslerov-halsall-kune-holocenescalefiredynamicsofcentraleuropeantemperatesprucebeechforests-2018', 'http://doi.org/10.1016/j.quascirev.2018.05.001', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/carter-moravcov-chiverrell-clear-finsinger-dreslerov-halsall-kune-holocenescalefiredynamicsofcentraleuropeantemperatesprucebeechforests-2018\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>2 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('carter-moravcov-chiverrell-clear-finsinger-dreslerov-halsall-kune-holocenescalefiredynamicsofcentraleuropeantemperatesprucebeechforests-2018')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{carter_holocene-scale_2018,\n\ttitle = {Holocene-scale fire dynamics of central {European} temperate spruce-beech forests},\n\tvolume = {191},\n\tissn = {0277-3791},\n\tdoi = {10.1016/j.quascirev.2018.05.001},\n\tabstract = {This study investigated the long-term role and drivers of fire in the central European temperate spruce-beech forests from Prášilské jezero, Czech Republic. The results illustrate the complex relationship between broad-scale climate, vegetation composition, and local human activities on fire throughout the Holocene. Biomass burning was the highest (average 3 fires/1000 years) and most severe during the early Holocene when fire resistant taxa (Pinus, Corylus and Betula) dominated. Using a Generalized Additive Model to assess the response of dominant canopy taxa to changes in biomass burning and fire severity, response curves demonstrate a positive relationship (p \\&amp;lt; 0.01) between fire resistant taxa and increases in biomass burning. Norway spruce (Picea abies) established ∼10,000 cal yr BP and expanded during peak biomass burning. Response curves show a slight negative relationship with Picea and increasing biomass burning, and a positive relationship with increasing fire severity. This suggests that central European spruce forests may not be significantly impacted by fire. Regional biomass burning dramatically decreased with the expansion of fire sensitive taxa (e.g. Fagus sylvatica) ∼6500 cal yr BP, yet no dramatic reduction in local fire frequency occurred. This suggests either human activities or rare fire-promoting climatic events were important in shaping local fire regimes. Fire activity peaked (6 fires/1000 years) ∼2500 cal yr BP and paralleled increases in anthropogenic pollen indicators. Fagus response curves illustrates a negative (p \\&amp;lt; 0.01) relationship with increasing biomass burning and fire severity suggesting that natural Fagus forests may be increasingly vulnerable to projected increases in wildfire occurrence.},\n\tlanguage = {English},\n\turldate = {2018-05-26},\n\tjournal = {Quaternary Science Reviews},\n\tauthor = {Carter, Vachel A. and Moravcová, Alice and Chiverrell, Richard C. and Clear, Jennifer L. and Finsinger, Walter and Dreslerová, Dagmar and Halsall, Karen and Kuneš, Petr},\n\tmonth = jul,\n\tyear = {2018},\n\tnote = {[IF2017=4.334]},\n\tkeywords = {Climate, Fire, Holocene, Macrofossils, Paleoecology, Pollen, Sedimentary charcoal, disturbance},\n\tpages = {15--30},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  This study investigated the long-term role and drivers of fire in the central European temperate spruce-beech forests from Prášilské jezero, Czech Republic. The results illustrate the complex relationship between broad-scale climate, vegetation composition, and local human activities on fire throughout the Holocene. Biomass burning was the highest (average 3 fires/1000 years) and most severe during the early Holocene when fire resistant taxa (Pinus, Corylus and Betula) dominated. Using a Generalized Additive Model to assess the response of dominant canopy taxa to changes in biomass burning and fire severity, response curves demonstrate a positive relationship (p &lt; 0.01) between fire resistant taxa and increases in biomass burning. Norway spruce (Picea abies) established ∼10,000 cal yr BP and expanded during peak biomass burning. Response curves show a slight negative relationship with Picea and increasing biomass burning, and a positive relationship with increasing fire severity. This suggests that central European spruce forests may not be significantly impacted by fire. Regional biomass burning dramatically decreased with the expansion of fire sensitive taxa (e.g. Fagus sylvatica) ∼6500 cal yr BP, yet no dramatic reduction in local fire frequency occurred. This suggests either human activities or rare fire-promoting climatic events were important in shaping local fire regimes. Fire activity peaked (6 fires/1000 years) ∼2500 cal yr BP and paralleled increases in anthropogenic pollen indicators. Fagus response curves illustrates a negative (p &lt; 0.01) relationship with increasing biomass burning and fire severity suggesting that natural Fagus forests may be increasingly vulnerable to projected increases in wildfire occurrence.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"olcov-petr-hjkov-petk-tth-rohovec-btora-horsk-earlyandmiddleholoceneecosystemchangesatthewesterncarpathianpannonianborderdrivenbyclimateandneolithicimpact-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Early and middle Holocene ecosystem changes at the Western Carpathian/Pannonian border driven by climate and Neolithic impact.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Šolcová, A.; Petr, L.; Hájková, P.; Petřík, J.; Tóth, P.; Rohovec, J.; BáTORA, J.;  and Horsák, M.\n</span>\n\n  \n\n</span>\n\n  <i>Boreas</i>, 47(3): 897–909.  2018.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1111/bor.12309\"\n     onclick=\"log_download('olcov-petr-hjkov-petk-tth-rohovec-btora-horsk-earlyandmiddleholoceneecosystemchangesatthewesterncarpathianpannonianborderdrivenbyclimateandneolithicimpact-2018', 'http://doi.org/10.1111/bor.12309', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/olcov-petr-hjkov-petk-tth-rohovec-btora-horsk-earlyandmiddleholoceneecosystemchangesatthewesterncarpathianpannonianborderdrivenbyclimateandneolithicimpact-2018\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('olcov-petr-hjkov-petk-tth-rohovec-btora-horsk-earlyandmiddleholoceneecosystemchangesatthewesterncarpathianpannonianborderdrivenbyclimateandneolithicimpact-2018')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{solcova_early_2018,\n\ttitle = {Early and middle {Holocene} ecosystem changes at the {Western} {Carpathian}/{Pannonian} border driven by climate and {Neolithic} impact},\n\tvolume = {47},\n\tcopyright = {© 2018 Collegium Boreas. Published by John Wiley \\&amp; Sons Ltd},\n\tissn = {1502-3885},\n\tdoi = {10.1111/bor.12309},\n\tabstract = {Travertine deposits are unique archives for multidisciplinary studies of past climate changes, associated vegetation development and the evolution of human societies. Despite their high potential in palaeoecological and palaeoclimate reconstructions, investigations of travertines are rather scarce in central Europe and particularly in Slovakia. Therefore, this study focused on a travertine deposit situated on the border between the Pannonian Basin and the Western Carpathians in a small valley in Santovka village (SW Slovakia), which is unique due to the presence of archaeological artefacts with known radiocarbon ages in the palaeoecological profile. Using a multidisciplinary approach combining macrofossil, pollen, mollusc, lithological and geochemical analyses, this study investigated climate–human–vegetation interactions. The Holocene onset was marked by the early arrival of oak trees; however, forest-steppe with a high representation of pine predominated until 9880 cal. a BP, followed by an expansion of temperate trees. The local ecosystem changed around 8600 cal. a BP when the valley was probably dammed by a travertine accumulation, probably resulting in the existence of a small travertine lake. This was associated with wetter climatic conditions, which were also documented in other sites in the Western Carpathians at that time. Surrounding temperate forest possibly retained a certain degree of openness, or local steppe habitat may have persisted on adjacent loess terraces until the neolithization of the area. Archaeological evidence represented by a ceramic shard dated to 7339 cal. a BP suggests the first appearance of humans at the site, yet pollen analysis records a significant change in vegetation first at 6650 cal. a BP. The local ecosystem records an abrupt change linked with human settlement earlier, at c. 7000 cal. a BP. Deforestation activities of the Neolithics resulted in the formation of an open calcareous fen occupied by numerous light-demanding mollusc species. The present study provides new important data about the spread of temperate trees at the onset of the Holocene, about further vegetation changes caused by activities of the first Neolithic farmers and about climate changes in the region of southwestern Slovakia.},\n\tlanguage = {English},\n\tnumber = {3},\n\turldate = {2019-01-22},\n\tjournal = {Boreas},\n\tauthor = {Šolcová, Anna and Petr, Libor and Hájková, Petra and Petřík, Jan and Tóth, Peter and Rohovec, Jan and BáTORA, Jozef and Horsák, Michal},\n\tyear = {2018},\n\tpages = {897--909},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Travertine deposits are unique archives for multidisciplinary studies of past climate changes, associated vegetation development and the evolution of human societies. Despite their high potential in palaeoecological and palaeoclimate reconstructions, investigations of travertines are rather scarce in central Europe and particularly in Slovakia. Therefore, this study focused on a travertine deposit situated on the border between the Pannonian Basin and the Western Carpathians in a small valley in Santovka village (SW Slovakia), which is unique due to the presence of archaeological artefacts with known radiocarbon ages in the palaeoecological profile. Using a multidisciplinary approach combining macrofossil, pollen, mollusc, lithological and geochemical analyses, this study investigated climate–human–vegetation interactions. The Holocene onset was marked by the early arrival of oak trees; however, forest-steppe with a high representation of pine predominated until 9880 cal. a BP, followed by an expansion of temperate trees. The local ecosystem changed around 8600 cal. a BP when the valley was probably dammed by a travertine accumulation, probably resulting in the existence of a small travertine lake. This was associated with wetter climatic conditions, which were also documented in other sites in the Western Carpathians at that time. Surrounding temperate forest possibly retained a certain degree of openness, or local steppe habitat may have persisted on adjacent loess terraces until the neolithization of the area. Archaeological evidence represented by a ceramic shard dated to 7339 cal. a BP suggests the first appearance of humans at the site, yet pollen analysis records a significant change in vegetation first at 6650 cal. a BP. The local ecosystem records an abrupt change linked with human settlement earlier, at c. 7000 cal. a BP. Deforestation activities of the Neolithics resulted in the formation of an open calcareous fen occupied by numerous light-demanding mollusc species. The present study provides new important data about the spread of temperate trees at the onset of the Holocene, about further vegetation changes caused by activities of the first Neolithic farmers and about climate changes in the region of southwestern Slovakia.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"carter-power-lundeen-morris-petersen-brunelle-anderson-shinker-etal-a1500yearsynthesisofwildfireactivitystratifiedbyelevationfromtheusrockymountains-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  A 1,500-year synthesis of wildfire activity stratified by elevation from the U.S. Rocky Mountains.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Carter, V. A.; Power, M. J.; Lundeen, Z. J.; Morris, J. L.; Petersen, K. L.; Brunelle, A.; Anderson, R. S.; Shinker, J. J.; Turney, L.; Koll, R.;  and Bartlein, P. J.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary International</i>, 488: 107–119. September 2018.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quaint.2017.06.051\"\n     onclick=\"log_download('carter-power-lundeen-morris-petersen-brunelle-anderson-shinker-etal-a1500yearsynthesisofwildfireactivitystratifiedbyelevationfromtheusrockymountains-2018', 'http://doi.org/10.1016/j.quaint.2017.06.051', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/carter-power-lundeen-morris-petersen-brunelle-anderson-shinker-etal-a1500yearsynthesisofwildfireactivitystratifiedbyelevationfromtheusrockymountains-2018\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('carter-power-lundeen-morris-petersen-brunelle-anderson-shinker-etal-a1500yearsynthesisofwildfireactivitystratifiedbyelevationfromtheusrockymountains-2018')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{carter_1500-year_2018,\n\tseries = {The {Fire}-{Human}-{Climate}-{Vegetation} {Nexus}},\n\ttitle = {A 1,500-year synthesis of wildfire activity stratified by elevation from the {U}.{S}. {Rocky} {Mountains}},\n\tvolume = {488},\n\tissn = {1040-6182},\n\tdoi = {10.1016/j.quaint.2017.06.051},\n\tabstract = {A key task in fire-climate research in the western United States is to characterize potential future fire-climate linkages across different elevational gradients. Using thirty-seven sedimentary charcoal records, here we present a 1500-year synthesis of wildfire activity across different elevational gradients to characterize fire-climate linkages. From our results, we have identified three periods of elevated fire occurrence centered on the 20th century, 900 cal yr BP, and 1350 cal yr BP. During the 20th century, fire activity has occurred primarily in the northern Rocky Mountains, with mid-elevations experiencing the greatest increase in wildfire activity. While wildfires occurred primarily in the SRM region ∼900 cal yr BP, the greatest increase in high-elevations occurred in the NRM at this time. Finally, synchronous wildfires occurred in both northern and southern Rocky Mountain mid-elevations ∼1350 cal yr BP, suggesting a potential analog for future wildfire conditions in response to warmer temperatures and more protracted droughts. We conclude that wildfire activity increased in most elevations during periods of protracted summer drought, warmer-than-average temperatures, and based on modern climate analogs, reduced atmospheric humidity.},\n\turldate = {2019-01-22},\n\tjournal = {Quaternary International},\n\tauthor = {Carter, Vachel A. and Power, Mitchell J. and Lundeen, Zachary J. and Morris, Jesse L. and Petersen, Kenneth L. and Brunelle, Andrea and Anderson, R. Scott and Shinker, Jacqueline J. and Turney, Lovina and Koll, Rebecca and Bartlein, Patrick J.},\n\tmonth = sep,\n\tyear = {2018},\n\tkeywords = {Charcoal, Climate, Fire, Paleofire, Rocky Mountains},\n\tpages = {107--119},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  A key task in fire-climate research in the western United States is to characterize potential future fire-climate linkages across different elevational gradients. Using thirty-seven sedimentary charcoal records, here we present a 1500-year synthesis of wildfire activity across different elevational gradients to characterize fire-climate linkages. From our results, we have identified three periods of elevated fire occurrence centered on the 20th century, 900 cal yr BP, and 1350 cal yr BP. During the 20th century, fire activity has occurred primarily in the northern Rocky Mountains, with mid-elevations experiencing the greatest increase in wildfire activity. While wildfires occurred primarily in the SRM region ∼900 cal yr BP, the greatest increase in high-elevations occurred in the NRM at this time. Finally, synchronous wildfires occurred in both northern and southern Rocky Mountain mid-elevations ∼1350 cal yr BP, suggesting a potential analog for future wildfire conditions in response to warmer temperatures and more protracted droughts. We conclude that wildfire activity increased in most elevations during periods of protracted summer drought, warmer-than-average temperatures, and based on modern climate analogs, reduced atmospheric humidity.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"carter-shinker-preece-droughtandvegetationchangeinthecentralrockymountainsandwesterngreatplainspotentialclimaticmechanismsassociatedwithmegadroughtconditionsat4200thinspcalthinspyrthinspbp-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Drought and vegetation change in the central Rocky Mountains and western Great Plains: potential climatic mechanisms associated with megadrought conditions at 4200&thinsp;cal&thinsp;yr&thinsp;BP.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Carter, V. A.; Shinker, J. J.;  and Preece, J.\n</span>\n\n  \n\n</span>\n\n  <i>Climate of the Past</i>, 14(8): 1195–1212. August 2018.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.5194/cp-14-1195-2018\"\n     onclick=\"log_download('carter-shinker-preece-droughtandvegetationchangeinthecentralrockymountainsandwesterngreatplainspotentialclimaticmechanismsassociatedwithmegadroughtconditionsat4200thinspcalthinspyrthinspbp-2018', 'http://doi.org/10.5194/cp-14-1195-2018', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/carter-shinker-preece-droughtandvegetationchangeinthecentralrockymountainsandwesterngreatplainspotentialclimaticmechanismsassociatedwithmegadroughtconditionsat4200thinspcalthinspyrthinspbp-2018\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('carter-shinker-preece-droughtandvegetationchangeinthecentralrockymountainsandwesterngreatplainspotentialclimaticmechanismsassociatedwithmegadroughtconditionsat4200thinspcalthinspyrthinspbp-2018')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{carter_drought_2018,\n\ttitle = {Drought and vegetation change in the central {Rocky} {Mountains} and western {Great} {Plains}: potential climatic mechanisms associated with megadrought conditions at 4200\\&amp;thinsp;cal\\&amp;thinsp;yr\\&amp;thinsp;{BP}},\n\tvolume = {14},\n\tissn = {1814-9324},\n\tshorttitle = {Drought and vegetation change in the central {Rocky} {Mountains} and western {Great} {Plains}},\n\tdoi = {10.5194/cp-14-1195-2018},\n\tabstract = {{\\textless}p{\\textgreater}{\\textless}strong{\\textgreater}Abstract.{\\textless}/strong{\\textgreater} Droughts are a naturally re-occurring phenomena that result in economic and societal losses. Yet, the most historic droughts that occurred in the 1930s and 1950s in the Great Plains and western United States were both shorter in duration and less severe than megadroughts that have plagued the region in the past. Roughly 4200 years ago, a ∼ 150-year long megadrought occurred in the central Rocky Mountains, as indicated by sedimentary pollen evidence documenting a brief and unique change in vegetation composition from Long Lake, southeastern Wyoming. Neighbouring the central Rocky Mountains, several dune fields reactivated in the western Great Plains around this time period illustrating a severe regional drought. While sedimentary pollen provides evidence of past drought, paleoecological evidence does not provide context for the climate mechanisms that may have caused the drought. Thus, a modern climate analogue technique was applied to the sedimentary pollen and regional dune reactivation evidence identified from the region to provide a conceptual framework for exploring possible mechanisms responsible for the observed ecological changes. The modern climate analogues of 2002/2012 illustrate that warm and dry conditions persisted through the growing season and were associated with anomalously higher-than-normal geopotential heights centred over the Great Plains. In the spring, higher-than-normal heights suppressed moisture transport via the low-level jet from the Gulf of Mexico creating a more southwesterly component of flow. In the summer, higher-than-normal heights persisted over the northern Great Plains resulting in a wind shift with an easterly component of flow, drawing in dry continental air into the study region. In both cases, lower-than-normal moisture in the atmosphere (via 850{\\textless}span class=&quot;thinspace&quot;{\\textgreater}{\\textless}/span{\\textgreater}mbar specific humidity) inhibited uplift and potential precipitation. Thus, if the present scenario existed during the 4.2{\\textless}span class=&quot;thinspace&quot;{\\textgreater}{\\textless}/span{\\textgreater}ka drought, the associated climatic responses are consistent with local and regional proxy data suggesting regional drought conditions in the central Rocky Mountains and western Great Plains.{\\textless}/p{\\textgreater}},\n\tlanguage = {English},\n\tnumber = {8},\n\turldate = {2019-01-22},\n\tjournal = {Climate of the Past},\n\tauthor = {Carter, Vachel A. and Shinker, Jacqueline J. and Preece, Jonathon},\n\tmonth = aug,\n\tyear = {2018},\n\tpages = {1195--1212},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  \\textlessp\\textgreater\\textlessstrong\\textgreaterAbstract.\\textless/strong\\textgreater Droughts are a naturally re-occurring phenomena that result in economic and societal losses. Yet, the most historic droughts that occurred in the 1930s and 1950s in the Great Plains and western United States were both shorter in duration and less severe than megadroughts that have plagued the region in the past. Roughly 4200 years ago, a ∼ 150-year long megadrought occurred in the central Rocky Mountains, as indicated by sedimentary pollen evidence documenting a brief and unique change in vegetation composition from Long Lake, southeastern Wyoming. Neighbouring the central Rocky Mountains, several dune fields reactivated in the western Great Plains around this time period illustrating a severe regional drought. While sedimentary pollen provides evidence of past drought, paleoecological evidence does not provide context for the climate mechanisms that may have caused the drought. Thus, a modern climate analogue technique was applied to the sedimentary pollen and regional dune reactivation evidence identified from the region to provide a conceptual framework for exploring possible mechanisms responsible for the observed ecological changes. The modern climate analogues of 2002/2012 illustrate that warm and dry conditions persisted through the growing season and were associated with anomalously higher-than-normal geopotential heights centred over the Great Plains. In the spring, higher-than-normal heights suppressed moisture transport via the low-level jet from the Gulf of Mexico creating a more southwesterly component of flow. In the summer, higher-than-normal heights persisted over the northern Great Plains resulting in a wind shift with an easterly component of flow, drawing in dry continental air into the study region. In both cases, lower-than-normal moisture in the atmosphere (via 850\\textlessspan class=\"thinspace\"\\textgreater\\textless/span\\textgreatermbar specific humidity) inhibited uplift and potential precipitation. Thus, if the present scenario existed during the 4.2\\textlessspan class=\"thinspace\"\\textgreater\\textless/span\\textgreaterka drought, the associated climatic responses are consistent with local and regional proxy data suggesting regional drought conditions in the central Rocky Mountains and western Great Plains.\\textless/p\\textgreater\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2017\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2017')\"\n      onkeypress=\"toggleGroup('group_2017')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2017</span>\n      <span class=\"bibbase_group_count\">\n        \n        (3)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"szab-kune-svobodovsvitavsk-varcov-kov-suchnkov-mllerov-hdl-usinghistoricalecologytoreassesstheconservationstatusofconiferousforestsincentraleurope-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Using historical ecology to reassess the conservation status of coniferous forests in Central Europe.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Szabó, P.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Svobodová‐Svitavská, H.; Švarcová, M. G.; Křížová, L.; Suchánková, S.; Müllerová, J.;  and Hédl, R.\n</span>\n\n  \n\n</span>\n\n  <i>Conservation Biology</i>, 31(1): 150–160. February 2017.\n  <span class=\"note\">[IF2016=4.842]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1111/cobi.12763\"\n     onclick=\"log_download('szab-kune-svobodovsvitavsk-varcov-kov-suchnkov-mllerov-hdl-usinghistoricalecologytoreassesstheconservationstatusofconiferousforestsincentraleurope-2017', 'http://doi.org/10.1111/cobi.12763', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/szab-kune-svobodovsvitavsk-varcov-kov-suchnkov-mllerov-hdl-usinghistoricalecologytoreassesstheconservationstatusofconiferousforestsincentraleurope-2017\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>3 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('szab-kune-svobodovsvitavsk-varcov-kov-suchnkov-mllerov-hdl-usinghistoricalecologytoreassesstheconservationstatusofconiferousforestsincentraleurope-2017')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{szabo_using_2017,\n\ttitle = {Using historical ecology to reassess the conservation status of coniferous forests in {Central} {Europe}},\n\tvolume = {31},\n\tcopyright = {All rights reserved},\n\tissn = {1523-1739},\n\tdoi = {10.1111/cobi.12763},\n\tabstract = {Forests cover approximately one-third of Central Europe. Oak (Quercus) and European beech (Fagus sylvatica) are considered the natural dominants at low and middle elevations, respectively. Many coniferous forests (especially of Picea abies) occur primarily at midelevations, but these are thought to have resulted from forestry plantations planted over the past 200 years. Nature conservation and forestry policy seek to promote broadleaved trees over conifers. However, there are discrepancies between conservation guidelines (included in Natura 2000) and historical and palaeoecological data with regard to the distribution of conifers. Our aim was to bring new evidence to the debate on the conservation of conifers versus broadleaved trees at midelevations in Central Europe. We created a vegetation and land-cover model based on pollen data for a highland area of 11,300 km2 in the Czech Republic and assessed tree species composition in the forests before the onset of modern forestry based on 18th-century archival sources. Conifers dominated the study region throughout the entire Holocene (approximately 40–60\\% of the area). Broadleaved trees were present in a much smaller area than envisaged by current ideas of natural vegetation. Rather than casting doubt on the principles of Central European nature conservation in general, our results highlight the necessity of detailed regional investigations and the importance of historical data in challenging established notions on the natural distribution of tree species.},\n\tlanguage = {English},\n\tnumber = {1},\n\turldate = {2017-01-26},\n\tjournal = {Conservation Biology},\n\tauthor = {Szabó, Péter and Kuneš, Petr and Svobodová‐Svitavská, Helena and Švarcová, Markéta Gabriela and Křížová, Lucie and Suchánková, Silvie and Müllerová, Jana and Hédl, Radim},\n\tmonth = feb,\n\tyear = {2017},\n\tnote = {[IF2016=4.842]},\n\tkeywords = {Czech Republic, Historical ecology, Holocene, LRA, REVEALS, conservation, interdisciplinarity, potential natural vegetation, reconstruction},\n\tpages = {150--160},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Forests cover approximately one-third of Central Europe. Oak (Quercus) and European beech (Fagus sylvatica) are considered the natural dominants at low and middle elevations, respectively. Many coniferous forests (especially of Picea abies) occur primarily at midelevations, but these are thought to have resulted from forestry plantations planted over the past 200 years. Nature conservation and forestry policy seek to promote broadleaved trees over conifers. However, there are discrepancies between conservation guidelines (included in Natura 2000) and historical and palaeoecological data with regard to the distribution of conifers. Our aim was to bring new evidence to the debate on the conservation of conifers versus broadleaved trees at midelevations in Central Europe. We created a vegetation and land-cover model based on pollen data for a highland area of 11,300 km2 in the Czech Republic and assessed tree species composition in the forests before the onset of modern forestry based on 18th-century archival sources. Conifers dominated the study region throughout the entire Holocene (approximately 40–60% of the area). Broadleaved trees were present in a much smaller area than envisaged by current ideas of natural vegetation. Rather than casting doubt on the principles of Central European nature conservation in general, our results highlight the necessity of detailed regional investigations and the importance of historical data in challenging established notions on the natural distribution of tree species.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"kune-abraham-historyofczechvegetationsincethelatepleistocene-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://link.springer.com/chapter/10.1007/978-3-319-63181-3_6\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'kune-abraham-historyofczechvegetationsincethelatepleistocene-2017', 'https://link.springer.com/chapter/10.1007/978-3-319-63181-3_6', event);\">\n    History of Czech vegetation since the Late Pleistocene.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>;  and Abraham, V.\n</span>\n\n  \n\n</span>\n\n  In Chytrý, M.; Danihelka, J.; Kaplan, Z.;  and Pyšek, P., editor(s), <i>Flora and Vegetation of the Czech Republic</i>, of Plant and Vegetation, pages 193–227. Springer, Cham, 1 edition,  2017.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"https://link.springer.com/chapter/10.1007/978-3-319-63181-3_6\"\n     onclick=\"log_download('kune-abraham-historyofczechvegetationsincethelatepleistocene-2017', 'https://link.springer.com/chapter/10.1007/978-3-319-63181-3_6', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"History of Czech vegetation since the Late Pleistocene [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kune-abraham-historyofczechvegetationsincethelatepleistocene-2017\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kune-abraham-historyofczechvegetationsincethelatepleistocene-2017')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@incollection{kunes_history_2017,\n\taddress = {Cham},\n\tedition = {1},\n\tseries = {Plant and {Vegetation}},\n\ttitle = {History of {Czech} vegetation since the {Late} {Pleistocene}},\n\tcopyright = {All rights reserved},\n\tisbn = {978-3-319-63180-6},\n\turl = {https://link.springer.com/chapter/10.1007/978-3-319-63181-3_6},\n\tabstract = {A long-term perspective is a crucial dimension for understanding the present-day composition and structure of the Czech flora and vegetation. We outline processes that were important for the development of the present-day diversity of flora and vegetation including extinctions of taxa and ecological mechanisms operating within glacial-interglacial cycles. Further, we present the history of vegetation during the key stages in the glacial and postglacial periods. First, we outline the pattern in the vegetation during the last glacial, including a discussion of the existence of refugia for trees. We further describe the changes in vegetation during the Late Glacial, which were mostly the results of abrupt climatic events. We also present a new synthesis of the Holocene regional development in vegetation based on a Landscape Reconstruction Algorithm, which results in different regional vegetation trajectories and three main phases in the development of vegetation. Finally, we give some examples of the histories of local vegetation at several sites mainly based on plant macrofossils.},\n\tlanguage = {English},\n\tnumber = {14},\n\tbooktitle = {Flora and {Vegetation} of the {Czech} {Republic}},\n\tpublisher = {Springer},\n\tauthor = {Kuneš, Petr and Abraham, Vojtěch},\n\teditor = {Chytrý, Milan and Danihelka, Jiří and Kaplan, Zdeněk and Pyšek, Petr},\n\tyear = {2017},\n\tkeywords = {Czech Republic, Holocene, Late Glacial, Plant macroremains, glacial, interglacial, pollen analysis, reconstruction, vegetation history},\n\tpages = {193--227},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  A long-term perspective is a crucial dimension for understanding the present-day composition and structure of the Czech flora and vegetation. We outline processes that were important for the development of the present-day diversity of flora and vegetation including extinctions of taxa and ecological mechanisms operating within glacial-interglacial cycles. Further, we present the history of vegetation during the key stages in the glacial and postglacial periods. First, we outline the pattern in the vegetation during the last glacial, including a discussion of the existence of refugia for trees. We further describe the changes in vegetation during the Late Glacial, which were mostly the results of abrupt climatic events. We also present a new synthesis of the Holocene regional development in vegetation based on a Landscape Reconstruction Algorithm, which results in different regional vegetation trajectories and three main phases in the development of vegetation. Finally, we give some examples of the histories of local vegetation at several sites mainly based on plant macrofossils.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"mariani-connor-fletcher-theuerkauf-kune-jacobsen-saunders-zawadzki-howoldisthetasmanianculturallandscapeatestoflandscapeopennessusingquantitativelandcoverreconstructions-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  How old is the Tasmanian cultural landscape? A test of landscape openness using quantitative land-cover reconstructions.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Mariani, M.; Connor, S. E.; Fletcher, M.; Theuerkauf, M.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Jacobsen, G.; Saunders, K. M.;  and Zawadzki, A.\n</span>\n\n  \n\n</span>\n\n  <i>Journal of Biogeography</i>, 44(10): 2410–2420.  2017.\n  <span class=\"note\">[IF2016=4.248]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1111/jbi.13040\"\n     onclick=\"log_download('mariani-connor-fletcher-theuerkauf-kune-jacobsen-saunders-zawadzki-howoldisthetasmanianculturallandscapeatestoflandscapeopennessusingquantitativelandcoverreconstructions-2017', 'http://doi.org/10.1111/jbi.13040', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/mariani-connor-fletcher-theuerkauf-kune-jacobsen-saunders-zawadzki-howoldisthetasmanianculturallandscapeatestoflandscapeopennessusingquantitativelandcoverreconstructions-2017\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('mariani-connor-fletcher-theuerkauf-kune-jacobsen-saunders-zawadzki-howoldisthetasmanianculturallandscapeatestoflandscapeopennessusingquantitativelandcoverreconstructions-2017')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{mariani_how_2017,\n\ttitle = {How old is the {Tasmanian} cultural landscape? {A} test of landscape openness using quantitative land-cover reconstructions},\n\tvolume = {44},\n\tcopyright = {All rights reserved},\n\tissn = {1365–2699},\n\tshorttitle = {How old is the {Tasmanian} cultural landscape?},\n\tdoi = {10.1111/jbi.13040},\n\tabstract = {Aim: To test competing hypotheses about the timing and extent of Holocene landscape opening using pollen-based quantitative land-cover estimates.\nLocation: Dove Lake, Tasmanian Wilderness World Heritage Area, Australia.\nMethods: Fossil pollen data were incorporated into pollen dispersal models and corrected for differences in pollen productivity among key plant taxa. Mechanistic models (REVEALS—Regional Estimates of VEgetation Abundance from Large Sites) employing different models for pollen dispersal (Gaussian plume and Lagrangian stochastic models) were evaluated and applied in the Southern Hemisphere for the first time.\nResults: Validation of the REVEALS model with vegetation cover data suggests an overall better performance of the Lagrangian stochastic model. Regional land-cover estimates for forest and non-forest plant taxa show persistent landscape openness throughout the Holocene (average landscape openness {\\textasciitilde}50\\%). Gymnoschoenus sphaerocephalus, an indicator of moorland vegetation, shows higher values during the early Holocene (11.7–9 ka) and declines slightly through the mid-Holocene (9–4.5 ka) during a phase of partial landscape afforestation. Rain forest cover reduced (from {\\textasciitilde}40\\% to {\\textasciitilde}20\\%) during the period between 4.2–3.5 ka.\nMain conclusions: Pollen percentages severely under-represent landscape openness in western Tasmania and this bias has fostered an over-estimation of Holocene forest cover from pollen data. Treeless vegetation dominated Holocene landscapes of the Dove Lake area, allowing us to reject models of landscape evolution that invoke late-Holocene replacement of a rain forest-dominated landscape by moorland. Instead, we confirm a model of Late Pleistocene inheritance of open vegetation. Rapid forest decline occurred after c. 4 ka, likely in response to regional moisture decline.},\n\tlanguage = {English},\n\tnumber = {10},\n\tjournal = {Journal of Biogeography},\n\tauthor = {Mariani, Michela and Connor, Simon E. and Fletcher, Michael-S. and Theuerkauf, Martin and Kuneš, Petr and Jacobsen, Geraldine and Saunders, Krystyna M. and Zawadzki, Atun},\n\tyear = {2017},\n\tnote = {[IF2016=4.248]},\n\tkeywords = {Australia, Holocene, REVEALS, Tasmania, cultural landscape, dispersal models, fire, landcover reconstruction, moorland, rain forest, reconstruction},\n\tpages = {2410--2420},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Aim: To test competing hypotheses about the timing and extent of Holocene landscape opening using pollen-based quantitative land-cover estimates. Location: Dove Lake, Tasmanian Wilderness World Heritage Area, Australia. Methods: Fossil pollen data were incorporated into pollen dispersal models and corrected for differences in pollen productivity among key plant taxa. Mechanistic models (REVEALS—Regional Estimates of VEgetation Abundance from Large Sites) employing different models for pollen dispersal (Gaussian plume and Lagrangian stochastic models) were evaluated and applied in the Southern Hemisphere for the first time. Results: Validation of the REVEALS model with vegetation cover data suggests an overall better performance of the Lagrangian stochastic model. Regional land-cover estimates for forest and non-forest plant taxa show persistent landscape openness throughout the Holocene (average landscape openness ~50%). Gymnoschoenus sphaerocephalus, an indicator of moorland vegetation, shows higher values during the early Holocene (11.7–9 ka) and declines slightly through the mid-Holocene (9–4.5 ka) during a phase of partial landscape afforestation. Rain forest cover reduced (from ~40% to ~20%) during the period between 4.2–3.5 ka. Main conclusions: Pollen percentages severely under-represent landscape openness in western Tasmania and this bias has fostered an over-estimation of Holocene forest cover from pollen data. Treeless vegetation dominated Holocene landscapes of the Dove Lake area, allowing us to reject models of landscape evolution that invoke late-Holocene replacement of a rain forest-dominated landscape by moorland. Instead, we confirm a model of Late Pleistocene inheritance of open vegetation. Rapid forest decline occurred after c. 4 ka, likely in response to regional moisture decline.\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2016\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2016')\"\n      onkeypress=\"toggleGroup('group_2016')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2016</span>\n      <span class=\"bibbase_group_count\">\n        \n        (2)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"abraham-kune-petr-svitavsksvobodov-kozkov-jamrichov-varcov-pokorn-apollenbasedquantitativereconstructionoftheholocenevegetationupdatesaperspectiveonthenaturalvegetationintheczechrepublicandslovakia-2016\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.preslia.cz/P164Abraham.pdf\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'abraham-kune-petr-svitavsksvobodov-kozkov-jamrichov-varcov-pokorn-apollenbasedquantitativereconstructionoftheholocenevegetationupdatesaperspectiveonthenaturalvegetationintheczechrepublicandslovakia-2016', 'http://www.preslia.cz/P164Abraham.pdf', event);\">\n    A pollen-based quantitative reconstruction of the Holocene vegetation updates a perspective on the natural vegetation in the Czech Republic and Slovakia.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Abraham, V.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Petr, L.; Svitavská-Svobodová, H.; Kozáková, R.; Jamrichová, E.; Švarcová, M. G.;  and Pokorný, P.\n</span>\n\n  \n\n</span>\n\n  <i>Preslia</i>, 88(4): 409–434.  2016.\n  <span class=\"note\">[IF2015=2.711]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"http://www.preslia.cz/P164Abraham.pdf\"\n     onclick=\"log_download('abraham-kune-petr-svitavsksvobodov-kozkov-jamrichov-varcov-pokorn-apollenbasedquantitativereconstructionoftheholocenevegetationupdatesaperspectiveonthenaturalvegetationintheczechrepublicandslovakia-2016', 'http://www.preslia.cz/P164Abraham.pdf', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/pdf.svg\"\n\t     alt=\"A pollen-based quantitative reconstruction of the Holocene vegetation updates a perspective on the natural vegetation in the Czech Republic and Slovakia [pdf]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/abraham-kune-petr-svitavsksvobodov-kozkov-jamrichov-varcov-pokorn-apollenbasedquantitativereconstructionoftheholocenevegetationupdatesaperspectiveonthenaturalvegetationintheczechrepublicandslovakia-2016\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('abraham-kune-petr-svitavsksvobodov-kozkov-jamrichov-varcov-pokorn-apollenbasedquantitativereconstructionoftheholocenevegetationupdatesaperspectiveonthenaturalvegetationintheczechrepublicandslovakia-2016')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{abraham_pollen-based_2016,\n\ttitle = {A pollen-based quantitative reconstruction of the {Holocene} vegetation updates a perspective on the natural vegetation in the {Czech} {Republic} and {Slovakia}},\n\tvolume = {88},\n\tcopyright = {All rights reserved},\n\turl = {http://www.preslia.cz/P164Abraham.pdf},\n\tlanguage = {English},\n\tnumber = {4},\n\tjournal = {Preslia},\n\tauthor = {Abraham, Vojtěch and Kuneš, Petr and Petr, Libor and Svitavská-Svobodová, Helena and Kozáková, Radka and Jamrichová, Eva and Švarcová, Markéta Gabriela and Pokorný, Petr},\n\tyear = {2016},\n\tnote = {[IF2015=2.711]},\n\tkeywords = {Czech Republic, Database, Holocene, LRA, REVEALS, Slovakia, conservation, pollen data, potential natural vegetation, reconstruction},\n\tpages = {409--434},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"mariani-connor-theuerkauf-kune-fletcher-testingquantitativepollendispersalmodelsinanimalpollinatedvegetationmosaicsanexamplefromtemperatetasmaniaaustralia-2016\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.sciencedirect.com/science/article/pii/S0277379116304851\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'mariani-connor-theuerkauf-kune-fletcher-testingquantitativepollendispersalmodelsinanimalpollinatedvegetationmosaicsanexamplefromtemperatetasmaniaaustralia-2016', 'http://www.sciencedirect.com/science/article/pii/S0277379116304851', event);\">\n    Testing quantitative pollen dispersal models in animal-pollinated vegetation mosaics: An example from temperate Tasmania, Australia.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Mariani, M.; Connor, S. E.; Theuerkauf, M.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>;  and Fletcher, M. -.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Science Reviews</i>, 154: 214–225. December 2016.\n  <span class=\"note\">[IF2015=4.521]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"http://www.sciencedirect.com/science/article/pii/S0277379116304851\"\n     onclick=\"log_download('mariani-connor-theuerkauf-kune-fletcher-testingquantitativepollendispersalmodelsinanimalpollinatedvegetationmosaicsanexamplefromtemperatetasmaniaaustralia-2016', 'http://www.sciencedirect.com/science/article/pii/S0277379116304851', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Testing quantitative pollen dispersal models in animal-pollinated vegetation mosaics: An example from temperate Tasmania, Australia [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quascirev.2016.10.020\"\n     onclick=\"log_download('mariani-connor-theuerkauf-kune-fletcher-testingquantitativepollendispersalmodelsinanimalpollinatedvegetationmosaicsanexamplefromtemperatetasmaniaaustralia-2016', 'http://doi.org/10.1016/j.quascirev.2016.10.020', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/mariani-connor-theuerkauf-kune-fletcher-testingquantitativepollendispersalmodelsinanimalpollinatedvegetationmosaicsanexamplefromtemperatetasmaniaaustralia-2016\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('mariani-connor-theuerkauf-kune-fletcher-testingquantitativepollendispersalmodelsinanimalpollinatedvegetationmosaicsanexamplefromtemperatetasmaniaaustralia-2016')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{mariani_testing_2016,\n\ttitle = {Testing quantitative pollen dispersal models in animal-pollinated vegetation mosaics: {An} example from temperate {Tasmania}, {Australia}},\n\tvolume = {154},\n\tcopyright = {All rights reserved},\n\tissn = {0277-3791},\n\tshorttitle = {Testing quantitative pollen dispersal models in animal-pollinated vegetation mosaics},\n\turl = {http://www.sciencedirect.com/science/article/pii/S0277379116304851},\n\tdoi = {10.1016/j.quascirev.2016.10.020},\n\tabstract = {Reconstructing past vegetation abundance and land-cover changes through time has important implications in land management and climate modelling. To date palaeovegetation reconstructions in Australia have been limited to qualitative or semi-quantitative inferences from pollen data. Testing pollen dispersal models constitutes a crucial step in developing quantitative past vegetation and land cover reconstructions. Thus far, the application of quantitative pollen dispersal models has been restricted to regions dominated by wind-pollinated plants (e.g. Europe) and their performance in a landscape dominated by animal-pollinated plant taxa is still unexplored. Here we test, for the first time in Australia, two well-known pollen dispersal models to assess their performance in the wind- and animal-pollinated vegetation mosaics of western Tasmania. We focus on a mix of wind- (6 taxa) and animal- (7 taxa) pollinated species that comprise the most common pollen types and key representatives of the dominant vegetation formations. Pollen Productivity Estimates and Relevant Source Area of Pollen obtained using Lagrangian Stochastic turbulent simulations appear to be more realistic when compared to the results from the widely used Gaussian Plume Model.},\n\turldate = {2016-11-18},\n\tjournal = {Quaternary Science Reviews},\n\tauthor = {Mariani, M. and Connor, S. E. and Theuerkauf, M. and Kuneš, P. and Fletcher, M. -S.},\n\tmonth = dec,\n\tyear = {2016},\n\tnote = {[IF2015=4.521]},\n\tkeywords = {Australia, Pollen dispersal, Pollen production estimate (PPE), Tasmania, reconstruction},\n\tpages = {214--225},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Reconstructing past vegetation abundance and land-cover changes through time has important implications in land management and climate modelling. To date palaeovegetation reconstructions in Australia have been limited to qualitative or semi-quantitative inferences from pollen data. Testing pollen dispersal models constitutes a crucial step in developing quantitative past vegetation and land cover reconstructions. Thus far, the application of quantitative pollen dispersal models has been restricted to regions dominated by wind-pollinated plants (e.g. Europe) and their performance in a landscape dominated by animal-pollinated plant taxa is still unexplored. Here we test, for the first time in Australia, two well-known pollen dispersal models to assess their performance in the wind- and animal-pollinated vegetation mosaics of western Tasmania. We focus on a mix of wind- (6 taxa) and animal- (7 taxa) pollinated species that comprise the most common pollen types and key representatives of the dominant vegetation formations. Pollen Productivity Estimates and Relevant Source Area of Pollen obtained using Lagrangian Stochastic turbulent simulations appear to be more realistic when compared to the results from the widely used Gaussian Plume Model.\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2015\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2015')\"\n      onkeypress=\"toggleGroup('group_2015')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2015</span>\n      <span class=\"bibbase_group_count\">\n        \n        (1)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"kune-svobodovsvitavsk-kol-hajnalov-abraham-macek-tk-szab-theoriginofgrasslandsinthetemperateforestzoneofeastcentraleuropelongtermlegacyofclimateandhumanimpact-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  The origin of grasslands in the temperate forest zone of east-central Europe: long-term legacy of climate and human impact.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Svobodová-Svitavská, H.; Kolář, J.; Hajnalová, M.; Abraham, V.; Macek, M.; Tkáč, P.;  and Szabó, P.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Science Reviews</i>, 116: 15–27. May 2015.\n  <span class=\"note\">[IF2014=4.572]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quascirev.2015.03.014\"\n     onclick=\"log_download('kune-svobodovsvitavsk-kol-hajnalov-abraham-macek-tk-szab-theoriginofgrasslandsinthetemperateforestzoneofeastcentraleuropelongtermlegacyofclimateandhumanimpact-2015', 'http://doi.org/10.1016/j.quascirev.2015.03.014', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kune-svobodovsvitavsk-kol-hajnalov-abraham-macek-tk-szab-theoriginofgrasslandsinthetemperateforestzoneofeastcentraleuropelongtermlegacyofclimateandhumanimpact-2015\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>2 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kune-svobodovsvitavsk-kol-hajnalov-abraham-macek-tk-szab-theoriginofgrasslandsinthetemperateforestzoneofeastcentraleuropelongtermlegacyofclimateandhumanimpact-2015')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{kunes_origin_2015,\n\ttitle = {The origin of grasslands in the temperate forest zone of east-central {Europe}: long-term legacy of climate and human impact},\n\tvolume = {116},\n\tcopyright = {All rights reserved},\n\tissn = {0277-3791},\n\tshorttitle = {The origin of grasslands in the temperate forest zone of east-central {Europe}},\n\tdoi = {10.1016/j.quascirev.2015.03.014},\n\tabstract = {The post-glacial fate of central European grasslands has stimulated palaeoecological debates for a century. Some argued for the continuous survival of open land, while others claimed that closed forest had developed during the Middle Holocene. The reasons behind stability or changes in the proportion of open land are also unclear. We aim to reconstruct regional vegetation openness and test the effects of climate and human impact on vegetation change throughout the Holocene. We present a newly dated pollen record from north-western fringes of the Pannonian Plain, east-central Europe, and reconstruct Holocene regional vegetation development by the REVEALS model for 27 pollen-equivalent taxa. Estimated vegetation is correlated in the same area with a human activity model based on all available archaeological information and a macrophysical climate model. The palaeovegetation record indicates the continuous presence of open land throughout the Holocene. Grasslands and open woodlands were probably maintained by local arid climatic conditions during the early Holocene delaying the spread of deciduous (oak) forests. Significantly detectable human-made landscape transformation started only after 2000 BC. Our analyses suggest that Neolithic people spread into a landscape that was already open. Humans probably contributed to the spread of oak, and influenced the dynamics of hazel and hornbeam.},\n\tlanguage = {English},\n\turldate = {2015-04-09},\n\tjournal = {Quaternary Science Reviews},\n\tauthor = {Kuneš, Petr and Svobodová-Svitavská, Helena and Kolář, Jan and Hajnalová, Mária and Abraham, Vojtěch and Macek, Martin and Tkáč, Peter and Szabó, Péter},\n\tmonth = may,\n\tyear = {2015},\n\tnote = {[IF2014=4.572]},\n\tkeywords = {Carpathian Basin, Czech Republic, Holocene, LRA, MCM model, REVEALS, conservation, pollen analysis, quantitative vegetation reconstruction},\n\tpages = {15--27},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The post-glacial fate of central European grasslands has stimulated palaeoecological debates for a century. Some argued for the continuous survival of open land, while others claimed that closed forest had developed during the Middle Holocene. The reasons behind stability or changes in the proportion of open land are also unclear. We aim to reconstruct regional vegetation openness and test the effects of climate and human impact on vegetation change throughout the Holocene. We present a newly dated pollen record from north-western fringes of the Pannonian Plain, east-central Europe, and reconstruct Holocene regional vegetation development by the REVEALS model for 27 pollen-equivalent taxa. Estimated vegetation is correlated in the same area with a human activity model based on all available archaeological information and a macrophysical climate model. The palaeovegetation record indicates the continuous presence of open land throughout the Holocene. Grasslands and open woodlands were probably maintained by local arid climatic conditions during the early Holocene delaying the spread of deciduous (oak) forests. Significantly detectable human-made landscape transformation started only after 2000 BC. Our analyses suggest that Neolithic people spread into a landscape that was already open. Humans probably contributed to the spread of oak, and influenced the dynamics of hazel and hornbeam.\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2014\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2014')\"\n      onkeypress=\"toggleGroup('group_2014')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2014</span>\n      <span class=\"bibbase_group_count\">\n        \n        (4)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"jamrichov-potkov-horsk-hajnalov-barta-tth-kune-earlyoccurrenceoftemperateoakdominatedforestinthenorthernpartofthelittlehungarianplainswslovakia-2014\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Early occurrence of temperate oak-dominated forest in the northern part of the Little Hungarian Plain, SW Slovakia.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Jamrichová, E.; Potůčková, A.; Horsák, M.; Hajnalová, M.; Barta, P.; Tóth, P.;  and <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>\n</span>\n\n  \n\n</span>\n\n  <i>The Holocene</i>, 24(12): 1810–1824. December 2014.\n  <span class=\"note\">[IF2013=3.794]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1177/0959683614551225\"\n     onclick=\"log_download('jamrichov-potkov-horsk-hajnalov-barta-tth-kune-earlyoccurrenceoftemperateoakdominatedforestinthenorthernpartofthelittlehungarianplainswslovakia-2014', 'http://doi.org/10.1177/0959683614551225', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/jamrichov-potkov-horsk-hajnalov-barta-tth-kune-earlyoccurrenceoftemperateoakdominatedforestinthenorthernpartofthelittlehungarianplainswslovakia-2014\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('jamrichov-potkov-horsk-hajnalov-barta-tth-kune-earlyoccurrenceoftemperateoakdominatedforestinthenorthernpartofthelittlehungarianplainswslovakia-2014')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{jamrichova_early_2014,\n\ttitle = {Early occurrence of temperate oak-dominated forest in the northern part of the {Little} {Hungarian} {Plain}, {SW} {Slovakia}},\n\tvolume = {24},\n\tcopyright = {All rights reserved},\n\tissn = {0959-6836, 1477-0911},\n\tdoi = {10.1177/0959683614551225},\n\tabstract = {Using a multi-proxy analysis of a postglacial sedimentary sequence from a lowland wetland, we address the possible drivers of change in the wetland habitats and surrounding landscapes of southwestern Slovakia. A 5 m-deep core in the Parížske močiare marshes was investigated for pollen, plant macro-remains, molluscs, organic content and magnetic susceptibility. The palaeoecological record extends from the Pleistocene–Holocene transition (≥11,200 cal. BP) to the 5th millennium cal. BP and was correlated with a macrophysical climate model (MCM) and archaeological data. Our results show the transformation of an open parkland landscape with patches of coniferous forest to a temperate deciduous forest at the onset of the Holocene. The record is remarkable for an early occurrence of Quercus pollen and macro-remains around 11,200 cal. BP and its early expansion (10,390 cal. BP) in the vegetation. Such an early spread of Quercus has not previously been recorded in the region, where Corylus is usually the first to expand among temperate trees. This unusual development of forest communities was most probably triggered by a short-lived increase in precipitation and decrease in temperature, as reconstructed by the MCM model. Higher moisture availability and low temperature inhibited Corylus and favoured the spread of Quercus. Later, the climate became drier and warmer, which, together with fires, supported the expansion of Corylus. Since 7300 cal. BP, human activities became most likely the dominant influence on the landscape. Deforestation contributed to soil erosion, which halted the accumulation of organic material after 5520 cal. BP, followed by the accumulation of clay sediments.},\n\tlanguage = {English},\n\tnumber = {12},\n\turldate = {2014-12-10},\n\tjournal = {The Holocene},\n\tauthor = {Jamrichová, Eva and Potůčková, Anna and Horsák, Michal and Hajnalová, Mária and Barta, Peter and Tóth, Peter and Kuneš, Petr},\n\tmonth = dec,\n\tyear = {2014},\n\tnote = {[IF2013=3.794]},\n\tkeywords = {Lowland vegetation, MCM model, Palaeoecology, Plant macroremains, Slovakia, climate, conservation, cultural landscape, human impact, multi-proxy, pollen analysis},\n\tpages = {1810--1824},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Using a multi-proxy analysis of a postglacial sedimentary sequence from a lowland wetland, we address the possible drivers of change in the wetland habitats and surrounding landscapes of southwestern Slovakia. A 5 m-deep core in the Parížske močiare marshes was investigated for pollen, plant macro-remains, molluscs, organic content and magnetic susceptibility. The palaeoecological record extends from the Pleistocene–Holocene transition (≥11,200 cal. BP) to the 5th millennium cal. BP and was correlated with a macrophysical climate model (MCM) and archaeological data. Our results show the transformation of an open parkland landscape with patches of coniferous forest to a temperate deciduous forest at the onset of the Holocene. The record is remarkable for an early occurrence of Quercus pollen and macro-remains around 11,200 cal. BP and its early expansion (10,390 cal. BP) in the vegetation. Such an early spread of Quercus has not previously been recorded in the region, where Corylus is usually the first to expand among temperate trees. This unusual development of forest communities was most probably triggered by a short-lived increase in precipitation and decrease in temperature, as reconstructed by the MCM model. Higher moisture availability and low temperature inhibited Corylus and favoured the spread of Quercus. Later, the climate became drier and warmer, which, together with fires, supported the expansion of Corylus. Since 7300 cal. BP, human activities became most likely the dominant influence on the landscape. Deforestation contributed to soil erosion, which halted the accumulation of organic material after 5520 cal. BP, followed by the accumulation of clay sediments.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"abraham-oukov-kune-presentdayvegetationhelpsquantifyingpastlandcoverinselectedregionsoftheczechrepublic-2014\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Present-day vegetation helps quantifying past land cover in selected regions of the Czech Republic.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Abraham, V.; Oušková, V.;  and <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>\n</span>\n\n  \n\n</span>\n\n  <i>PLoS ONE</i>, 9(6): e100117. June 2014.\n  <span class=\"note\">[IF2013=3.534]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1371/journal.pone.0100117\"\n     onclick=\"log_download('abraham-oukov-kune-presentdayvegetationhelpsquantifyingpastlandcoverinselectedregionsoftheczechrepublic-2014', 'http://doi.org/10.1371/journal.pone.0100117', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/abraham-oukov-kune-presentdayvegetationhelpsquantifyingpastlandcoverinselectedregionsoftheczechrepublic-2014\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('abraham-oukov-kune-presentdayvegetationhelpsquantifyingpastlandcoverinselectedregionsoftheczechrepublic-2014')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{abraham_present-day_2014,\n\ttitle = {Present-day vegetation helps quantifying past land cover in selected regions of the {Czech} {Republic}},\n\tvolume = {9},\n\tcopyright = {All rights reserved},\n\tdoi = {10.1371/journal.pone.0100117},\n\tabstract = {The REVEALS model is a tool for recalculating pollen data into vegetation abundances on a regional scale. We explored the general effect of selected parameters by performing simulations and ascertained the best model setting for the Czech Republic using the shallowest samples from 120 fossil sites and data on actual regional vegetation (60 km radius). Vegetation proportions of 17 taxa were obtained by combining the CORINE Land Cover map with forest inventories, agricultural statistics and habitat mapping data. Our simulation shows that changing the site radius for all taxa substantially affects REVEALS estimates of taxa with heavy or light pollen grains. Decreasing the site radius has a similar effect as increasing the wind speed parameter. However, adjusting the site radius to 1 m for local taxa only (even taxa with light pollen) yields lower, more correct estimates despite their high pollen signal. Increasing the background radius does not affect the estimates significantly. Our comparison of estimates with actual vegetation in seven regions shows that the most accurate relative pollen productivity estimates (PPEs) come from Central Europe and Southern Sweden. The initial simulation and pollen data yielded unrealistic estimates for Abies under the default setting of the wind speed parameter (3 m/s). We therefore propose the setting of 4 m/s, which corresponds to the spring average in most regions of the Czech Republic studied. Ad hoc adjustment of PPEs with this setting improves the match 3–4-fold. We consider these values (apart from four exceptions) to be appropriate, because they are within the ranges of standard errors, so they are related to original PPEs. Setting a 1 m radius for local taxa (Alnus, Salix, Poaceae) significantly improves the match between estimates and actual vegetation. However, further adjustments to PPEs exceed the ranges of original values, so their relevance is uncertain.},\n\tlanguage = {English},\n\tnumber = {6},\n\turldate = {2014-06-18},\n\tjournal = {PLoS ONE},\n\tauthor = {Abraham, Vojtěch and Oušková, Veronika and Kuneš, Petr},\n\tmonth = jun,\n\tyear = {2014},\n\tnote = {[IF2013=3.534]},\n\tkeywords = {Czech Republic, LRA, Pollen dispersal, Pollen production estimate (PPE), REVEALS, reconstruction, vegetation},\n\tpages = {e100117},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The REVEALS model is a tool for recalculating pollen data into vegetation abundances on a regional scale. We explored the general effect of selected parameters by performing simulations and ascertained the best model setting for the Czech Republic using the shallowest samples from 120 fossil sites and data on actual regional vegetation (60 km radius). Vegetation proportions of 17 taxa were obtained by combining the CORINE Land Cover map with forest inventories, agricultural statistics and habitat mapping data. Our simulation shows that changing the site radius for all taxa substantially affects REVEALS estimates of taxa with heavy or light pollen grains. Decreasing the site radius has a similar effect as increasing the wind speed parameter. However, adjusting the site radius to 1 m for local taxa only (even taxa with light pollen) yields lower, more correct estimates despite their high pollen signal. Increasing the background radius does not affect the estimates significantly. Our comparison of estimates with actual vegetation in seven regions shows that the most accurate relative pollen productivity estimates (PPEs) come from Central Europe and Southern Sweden. The initial simulation and pollen data yielded unrealistic estimates for Abies under the default setting of the wind speed parameter (3 m/s). We therefore propose the setting of 4 m/s, which corresponds to the spring average in most regions of the Czech Republic studied. Ad hoc adjustment of PPEs with this setting improves the match 3–4-fold. We consider these values (apart from four exceptions) to be appropriate, because they are within the ranges of standard errors, so they are related to original PPEs. Setting a 1 m radius for local taxa (Alnus, Salix, Poaceae) significantly improves the match between estimates and actual vegetation. However, further adjustments to PPEs exceed the ranges of original values, so their relevance is uncertain.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"strandberg-kjellstrm-poska-wagner-gaillard-trondman-mauri-davis-etal-regionalclimatemodelsimulationsforeuropeat6and02kbpsensitivitytochangesinanthropogenicdeforestation-2014\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Regional climate model simulations for Europe at 6 and 0.2 k BP: sensitivity to changes in anthropogenic deforestation.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Strandberg, G.; Kjellström, E.; Poska, A.; Wagner, S.; Gaillard, M.; Trondman, A.; Mauri, A.; Davis, B. A. S.; Kaplan, J. O.; Birks, H. J. B.; Bjune, A. E.; Fyfe, R.; Giesecke, T.; Kalnina, L.; Kangur, M.; van der Knaap, W. O.; Kokfelt, U.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Latałova, M.; Marquer, L.; Mazier, F.; Nielsen, A. B.; Smith, B.; Seppä, H.;  and Sugita, S.\n</span>\n\n  \n\n</span>\n\n  <i>Climate of the Past</i>, 10(2): 661–680. March 2014.\n  <span class=\"note\">[IF2013=3.482]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.5194/cp-10-661-2014\"\n     onclick=\"log_download('strandberg-kjellstrm-poska-wagner-gaillard-trondman-mauri-davis-etal-regionalclimatemodelsimulationsforeuropeat6and02kbpsensitivitytochangesinanthropogenicdeforestation-2014', 'http://doi.org/10.5194/cp-10-661-2014', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/strandberg-kjellstrm-poska-wagner-gaillard-trondman-mauri-davis-etal-regionalclimatemodelsimulationsforeuropeat6and02kbpsensitivitytochangesinanthropogenicdeforestation-2014\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('strandberg-kjellstrm-poska-wagner-gaillard-trondman-mauri-davis-etal-regionalclimatemodelsimulationsforeuropeat6and02kbpsensitivitytochangesinanthropogenicdeforestation-2014')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{strandberg_regional_2014,\n\ttitle = {Regional climate model simulations for {Europe} at 6 and 0.2 k {BP}: sensitivity to changes in anthropogenic deforestation},\n\tvolume = {10},\n\tcopyright = {All rights reserved},\n\tissn = {1814-9332},\n\tshorttitle = {Regional climate model simulations for {Europe} at 6 and 0.2 k {BP}},\n\tdoi = {10.5194/cp-10-661-2014},\n\tlanguage = {English},\n\tnumber = {2},\n\turldate = {2014-03-28},\n\tjournal = {Climate of the Past},\n\tauthor = {Strandberg, G. and Kjellström, E. and Poska, A. and Wagner, S. and Gaillard, M.-J. and Trondman, A.-K. and Mauri, A. and Davis, B. A. S. and Kaplan, J. O. and Birks, H. J. B. and Bjune, A. E. and Fyfe, R. and Giesecke, T. and Kalnina, L. and Kangur, M. and van der Knaap, W. O. and Kokfelt, U. and Kuneš, P. and Latałova, M. and Marquer, L. and Mazier, F. and Nielsen, A. B. and Smith, B. and Seppä, H. and Sugita, S.},\n\tmonth = mar,\n\tyear = {2014},\n\tnote = {[IF2013=3.482]},\n\tkeywords = {Europe, REVEALS, climate model, human impact, reconstruction},\n\tpages = {661--680},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"giesecke-davis-brewer-finsinger-wolters-blaauw-beaulieu-binney-etal-towardsmappingthelatequaternaryvegetationchangeofeurope-2014\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Towards mapping the late Quaternary vegetation change of Europe.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Giesecke, T.; Davis, B.; Brewer, S.; Finsinger, W.; Wolters, S.; Blaauw, M.; Beaulieu, J. d.; Binney, H.; Fyfe, R. M.; Gaillard, M.; Gil-Romera, G.; Knaap, W. O. v. d.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Kühl, N.; Leeuwen, J. F. N. v.; Leydet, M.; Lotter, A. F.; Ortu, E.; Semmler, M.;  and Bradshaw, R. H. W.\n</span>\n\n  \n\n</span>\n\n  <i>Vegetation History and Archaeobotany</i>, 23(1): 75–86. January 2014.\n  <span class=\"note\">[IF2013=2.061]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s00334-012-0390-y\"\n     onclick=\"log_download('giesecke-davis-brewer-finsinger-wolters-blaauw-beaulieu-binney-etal-towardsmappingthelatequaternaryvegetationchangeofeurope-2014', 'http://doi.org/10.1007/s00334-012-0390-y', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/giesecke-davis-brewer-finsinger-wolters-blaauw-beaulieu-binney-etal-towardsmappingthelatequaternaryvegetationchangeofeurope-2014\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('giesecke-davis-brewer-finsinger-wolters-blaauw-beaulieu-binney-etal-towardsmappingthelatequaternaryvegetationchangeofeurope-2014')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{giesecke_towards_2014,\n\ttitle = {Towards mapping the late {Quaternary} vegetation change of {Europe}},\n\tvolume = {23},\n\tcopyright = {All rights reserved},\n\tissn = {0939-6314, 1617-6278},\n\tdoi = {10.1007/s00334-012-0390-y},\n\tabstract = {The number of well-dated pollen diagrams in Europe has increased considerably over the last 30 years and many of them have been submitted to the European Pollen Database (EPD). This allows for the construction of increasingly precise maps of Holocene vegetation change across the continent. Chronological information in the EPD has been expressed in uncalibrated radiocarbon years, and most chronologies to date are based on this time scale. Here we present new chronologies for most of the datasets stored in the EPD based on calibrated radiocarbon years. Age information associated with pollen diagrams is often derived from the pollen stratigraphy itself or from other sedimentological information. We reviewed these chronological tie points and assigned uncertainties to them. The steps taken to generate the new chronologies are described and the rationale for a new classification system for age uncertainties is introduced. The resulting chronologies are fit for most continental-scale questions. They may not provide the best age model for particular sites, but may be viewed as general purpose chronologies. Taxonomic particularities of the data stored in the EPD are explained. An example is given of how the database can be queried to select samples with appropriate age control as well as the suitable taxonomic level to answer a specific research question.},\n\tlanguage = {English},\n\tnumber = {1},\n\turldate = {2014-01-08},\n\tjournal = {Vegetation History and Archaeobotany},\n\tauthor = {Giesecke, Thomas and Davis, Basil and Brewer, Simon and Finsinger, Walter and Wolters, Steffen and Blaauw, Maarten and Beaulieu, Jacques-Louis de and Binney, Heather and Fyfe, Ralph M. and Gaillard, Marie-José and Gil-Romera, Graciela and Knaap, W. O. van der and Kuneš, Petr and Kühl, Norbert and Leeuwen, Jacqueline F. N. van and Leydet, Michelle and Lotter, André F. and Ortu, Elena and Semmler, Malte and Bradshaw, Richard H. W.},\n\tmonth = jan,\n\tyear = {2014},\n\tnote = {[IF2013=2.061]},\n\tkeywords = {Age-depth relationships, Chronology, Database, European pollen database, climate, pollen data},\n\tpages = {75--86},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The number of well-dated pollen diagrams in Europe has increased considerably over the last 30 years and many of them have been submitted to the European Pollen Database (EPD). This allows for the construction of increasingly precise maps of Holocene vegetation change across the continent. Chronological information in the EPD has been expressed in uncalibrated radiocarbon years, and most chronologies to date are based on this time scale. Here we present new chronologies for most of the datasets stored in the EPD based on calibrated radiocarbon years. Age information associated with pollen diagrams is often derived from the pollen stratigraphy itself or from other sedimentological information. We reviewed these chronological tie points and assigned uncertainties to them. The steps taken to generate the new chronologies are described and the rationale for a new classification system for age uncertainties is introduced. The resulting chronologies are fit for most continental-scale questions. They may not provide the best age model for particular sites, but may be viewed as general purpose chronologies. Taxonomic particularities of the data stored in the EPD are explained. An example is given of how the database can be queried to select samples with appropriate age control as well as the suitable taxonomic level to answer a specific research question.\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2013\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2013')\"\n      onkeypress=\"toggleGroup('group_2013')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2013</span>\n      <span class=\"bibbase_group_count\">\n        \n        (2)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"kune-kjrsgaardsrensen-buylaert-murray-houmarknielsen-odgaard-anewmiddlepleistoceneinterglacialrecordfromdenmarkchronostratigraphiccorrelationpalaeovegetationandfiredynamics-2013\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  A new Middle Pleistocene interglacial record from Denmark: Chronostratigraphic correlation, palaeovegetation and fire dynamics.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Kuneš, P.; Kjærsgaard Sørensen, M.; Buylaert, J.; Murray, A. S.; Houmark-Nielsen, M.;  and Odgaard, B. V.\n</span>\n\n  \n\n</span>\n\n  <i>Boreas</i>, 42(3): 596–612.  2013.\n  <span class=\"note\">[IF2012=2.457]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1111/bor.12002\"\n     onclick=\"log_download('kune-kjrsgaardsrensen-buylaert-murray-houmarknielsen-odgaard-anewmiddlepleistoceneinterglacialrecordfromdenmarkchronostratigraphiccorrelationpalaeovegetationandfiredynamics-2013', 'http://doi.org/10.1111/bor.12002', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kune-kjrsgaardsrensen-buylaert-murray-houmarknielsen-odgaard-anewmiddlepleistoceneinterglacialrecordfromdenmarkchronostratigraphiccorrelationpalaeovegetationandfiredynamics-2013\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kune-kjrsgaardsrensen-buylaert-murray-houmarknielsen-odgaard-anewmiddlepleistoceneinterglacialrecordfromdenmarkchronostratigraphiccorrelationpalaeovegetationandfiredynamics-2013')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{kunes_new_2013,\n\ttitle = {A new {Middle} {Pleistocene} interglacial record from {Denmark}: {Chronostratigraphic} correlation, palaeovegetation and fire dynamics},\n\tvolume = {42},\n\tcopyright = {© 2013 The Authors. Boreas © 2013 The Boreas Collegium},\n\tissn = {1502-3885},\n\tshorttitle = {A new {Middle} {Pleistocene} interglacial record from {Denmark}},\n\tdoi = {10.1111/bor.12002},\n\tabstract = {Previously only three terrestrial interglacial periods were known from southern Scandinavia, all of which could be relatively easily correlated within the central European stratigraphical framework. Here, we present a new interglacial–interstadial pollen, plant macrofossil and charcoal record from Trelde Klint, Denmark, and analyse its biostratigraphy, correlation with other European records, vegetation development, fire dynamics and absolute dating. Except for a slight truncation of the early part of the record, the pollen stratigraphy exhibits a full interglacial succession, including temperate trees (Quercus, Ulmus and Tilia) during its mesocratic stage. Macrofossil analysis allowed identification to species level for Quercus robur, Picea abies and two mosses. Conifers (Pinus and Picea) dominate the pollen record of the interglacial sequence, and the occurrence of Larix pollen in the top part of the interglacial record as well as in the interstadial sediments is especially indicative of this interglacial. The overall diversity of tree genera is rather low. These biostratigraphical features suggest that Trelde Klint is unique among Danish records, but it is similar to records from northern Germany. Numerical analyses (REVEALS and DCA) indicate that forests during the temperate stage were dense and that vegetation openness increased only towards the end of the interglacial, accompanied by increased fire occurrence. A short interstadial sequence with a dominance of Pinus and Betula and the presence of Larix is present above the interglacial deposit. We argue that lack of attention to differences in fire regimes may hamper understanding of between-site correlations of interglacial pollen records. OSL dating, using a novel feldspar technique, yields an average age of 350±20 ka for the sandy sediments above the interglacial layers at Trelde Klint, suggesting that the whole interglacial–interstadial succession belongs to Marine Isotope Stage 11.},\n\tlanguage = {English},\n\tnumber = {3},\n\turldate = {2013-06-23},\n\tjournal = {Boreas},\n\tauthor = {Kuneš, Petr and Kjærsgaard Sørensen, Malene and Buylaert, Jan-Pieter and Murray, Andrew S. and Houmark-Nielsen, Michael and Odgaard, Bent Vad},\n\tyear = {2013},\n\tnote = {[IF2012=2.457]},\n\tkeywords = {Denmark, OSL dating, Plant macroremains, REVEALS, charcoal, interglacial, pollen analysis},\n\tpages = {596--612},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Previously only three terrestrial interglacial periods were known from southern Scandinavia, all of which could be relatively easily correlated within the central European stratigraphical framework. Here, we present a new interglacial–interstadial pollen, plant macrofossil and charcoal record from Trelde Klint, Denmark, and analyse its biostratigraphy, correlation with other European records, vegetation development, fire dynamics and absolute dating. Except for a slight truncation of the early part of the record, the pollen stratigraphy exhibits a full interglacial succession, including temperate trees (Quercus, Ulmus and Tilia) during its mesocratic stage. Macrofossil analysis allowed identification to species level for Quercus robur, Picea abies and two mosses. Conifers (Pinus and Picea) dominate the pollen record of the interglacial sequence, and the occurrence of Larix pollen in the top part of the interglacial record as well as in the interstadial sediments is especially indicative of this interglacial. The overall diversity of tree genera is rather low. These biostratigraphical features suggest that Trelde Klint is unique among Danish records, but it is similar to records from northern Germany. Numerical analyses (REVEALS and DCA) indicate that forests during the temperate stage were dense and that vegetation openness increased only towards the end of the interglacial, accompanied by increased fire occurrence. A short interstadial sequence with a dominance of Pinus and Betula and the presence of Larix is present above the interglacial deposit. We argue that lack of attention to differences in fire regimes may hamper understanding of between-site correlations of interglacial pollen records. OSL dating, using a novel feldspar technique, yields an average age of 350±20 ka for the sandy sediments above the interglacial layers at Trelde Klint, suggesting that the whole interglacial–interstadial succession belongs to Marine Isotope Stage 11.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"jamrichov-szab-hdl-kune-bobek-pelnkov-continuityandchangeinthevegetationofacentraleuropeanoakwood-2013\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Continuity and change in the vegetation of a Central European oakwood.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Jamrichová, E.; Szabó, P.; Hédl, R.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Bobek, P.;  and Pelánková, B.\n</span>\n\n  \n\n</span>\n\n  <i>The Holocene</i>, 23(1): 46–56. January 2013.\n  <span class=\"note\">[IF2012=3.218]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1177/0959683612450200\"\n     onclick=\"log_download('jamrichov-szab-hdl-kune-bobek-pelnkov-continuityandchangeinthevegetationofacentraleuropeanoakwood-2013', 'http://doi.org/10.1177/0959683612450200', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/jamrichov-szab-hdl-kune-bobek-pelnkov-continuityandchangeinthevegetationofacentraleuropeanoakwood-2013\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('jamrichov-szab-hdl-kune-bobek-pelnkov-continuityandchangeinthevegetationofacentraleuropeanoakwood-2013')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{jamrichova_continuity_2013,\n\ttitle = {Continuity and change in the vegetation of a {Central} {European} oakwood},\n\tvolume = {23},\n\tcopyright = {All rights reserved},\n\tissn = {0959-6836, 1477-0911},\n\tdoi = {10.1177/0959683612450200},\n\tabstract = {The issue of continuity in deciduous oakwood vegetation has been in the forefront of woodland ecological studies for many decades. The two basic questions that emerge from existing research are whether or not oakwoods can be characterized by long-term stability and what may be the driving forces of the observed stability or change. To answer these questions in a well-defined case study, we examined the history of a large subcontinental oakwood (Dúbrava) in the southeastern Czech Republic with interdisciplinary methods using palaeoecological and archival sources. Palaeoecology allowed us to reconstruct the vegetation composition and fire disturbances in Dúbrava in the past 2000 years, while written sources provided information about tree composition and management from the 14th century onwards. The pollen profiles show that the present oakwood was established in the mid-14th century with an abrupt change from shrubby, hazel-dominated vegetation to oak forest. This change was most probably caused by a ban on oak felling in ad 1350. From the 14th to the late 18th centuries Dúbrava had multiple uses, of which wood-pasture and hay-cutting kept the forest considerably open. The second remarkable change was dated to the late 18th century, when multiple-use management was abandoned and Dúbrava was divided into pasture-only and coppice-only parts. The last major shift occurred in the mid-19th century, when modern forestry and Scotch pine plantation became dominant. We conclude that Dúbrava Wood did not show stability in the long run and that its species composition has dramatically changed during the last two millennia. The most important driving force in the shaping and maintenance of the unique vegetation of Dúbrava was human management.},\n\tlanguage = {English},\n\tnumber = {1},\n\turldate = {2012-12-20},\n\tjournal = {The Holocene},\n\tauthor = {Jamrichová, Eva and Szabó, Péter and Hédl, Radim and Kuneš, Petr and Bobek, Přemysl and Pelánková, Barbora},\n\tmonth = jan,\n\tyear = {2013},\n\tnote = {[IF2012=3.218]},\n\tkeywords = {Historical ecology, conservation, ecosystem stability, management history, pollen analysis, temperate oakwood},\n\tpages = {46--56},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The issue of continuity in deciduous oakwood vegetation has been in the forefront of woodland ecological studies for many decades. The two basic questions that emerge from existing research are whether or not oakwoods can be characterized by long-term stability and what may be the driving forces of the observed stability or change. To answer these questions in a well-defined case study, we examined the history of a large subcontinental oakwood (Dúbrava) in the southeastern Czech Republic with interdisciplinary methods using palaeoecological and archival sources. Palaeoecology allowed us to reconstruct the vegetation composition and fire disturbances in Dúbrava in the past 2000 years, while written sources provided information about tree composition and management from the 14th century onwards. The pollen profiles show that the present oakwood was established in the mid-14th century with an abrupt change from shrubby, hazel-dominated vegetation to oak forest. This change was most probably caused by a ban on oak felling in ad 1350. From the 14th to the late 18th centuries Dúbrava had multiple uses, of which wood-pasture and hay-cutting kept the forest considerably open. The second remarkable change was dated to the late 18th century, when multiple-use management was abandoned and Dúbrava was divided into pasture-only and coppice-only parts. The last major shift occurred in the mid-19th century, when modern forestry and Scotch pine plantation became dominant. We conclude that Dúbrava Wood did not show stability in the long run and that its species composition has dramatically changed during the last two millennia. The most important driving force in the shaping and maintenance of the unique vegetation of Dúbrava was human management.\n</div>\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2011\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2011')\"\n      onkeypress=\"toggleGroup('group_2011')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2011</span>\n      <span class=\"bibbase_group_count\">\n        \n        (1)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"da-prostednk-kune-newradiocarbondataforthenorthbohemianmesolithic-2011\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.iansa.eu/papers/IANSA-2011-02-sida.pdf\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'da-prostednk-kune-newradiocarbondataforthenorthbohemianmesolithic-2011', 'http://www.iansa.eu/papers/IANSA-2011-02-sida.pdf', event);\">\n    New Radiocarbon Data for the North Bohemian Mesolithic.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Šída, P.; Prostředník, J.;  and <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>\n</span>\n\n  \n\n</span>\n\n  <i>Interdisciplinaria Archaeologica</i>, 2(2): 151–157.  2011.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"http://www.iansa.eu/papers/IANSA-2011-02-sida.pdf\"\n     onclick=\"log_download('da-prostednk-kune-newradiocarbondataforthenorthbohemianmesolithic-2011', 'http://www.iansa.eu/papers/IANSA-2011-02-sida.pdf', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/pdf.svg\"\n\t     alt=\"New Radiocarbon Data for the North Bohemian Mesolithic [pdf]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/da-prostednk-kune-newradiocarbondataforthenorthbohemianmesolithic-2011\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('da-prostednk-kune-newradiocarbondataforthenorthbohemianmesolithic-2011')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{sida_new_2011,\n\ttitle = {New {Radiocarbon} {Data} for the {North} {Bohemian} {Mesolithic}},\n\tvolume = {2},\n\tcopyright = {All rights reserved},\n\turl = {http://www.iansa.eu/papers/IANSA-2011-02-sida.pdf},\n\tlanguage = {English},\n\tnumber = {2},\n\tjournal = {Interdisciplinaria Archaeologica},\n\tauthor = {Šída, P. and Prostředník, J. and Kuneš, P.},\n\tyear = {2011},\n\tkeywords = {Czech Republic, Mesolithic, archeology, pre-Neolithic, radiocarbon AMS dating},\n\tpages = {151--157},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2010\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2010')\"\n      onkeypress=\"toggleGroup('group_2010')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2010</span>\n      <span class=\"bibbase_group_count\">\n        \n        (1)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"pokorn-da-chvojka-kov-kune-svtlk-vesel-palaeoenvironmentalresearchoftheschwarzenberglakesouthernbohemiaandexploratoryexcavationsofthiskeymesolithicarchaeologicalarea-2010\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Palaeoenvironmental research of the Schwarzenberg Lake, southern Bohemia, and exploratory excavations of this key Mesolithic archaeological area.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Pokorný, P.; Šída, P.; Chvojka, O.; Žáčková, P.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Světlík, I.;  and Veselý, J.\n</span>\n\n  \n\n</span>\n\n  <i>Památky archeologické</i>, 101: 5–38.  2010.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/pokorn-da-chvojka-kov-kune-svtlk-vesel-palaeoenvironmentalresearchoftheschwarzenberglakesouthernbohemiaandexploratoryexcavationsofthiskeymesolithicarchaeologicalarea-2010\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('pokorn-da-chvojka-kov-kune-svtlk-vesel-palaeoenvironmentalresearchoftheschwarzenberglakesouthernbohemiaandexploratoryexcavationsofthiskeymesolithicarchaeologicalarea-2010')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{pokorny_palaeoenvironmental_2010,\n\ttitle = {Palaeoenvironmental research of the {Schwarzenberg} {Lake}, southern {Bohemia}, and exploratory excavations of this key {Mesolithic} archaeological area},\n\tvolume = {101},\n\tcopyright = {All rights reserved},\n\tlanguage = {English},\n\tjournal = {Památky archeologické},\n\tauthor = {Pokorný, Petr and Šída, Petr and Chvojka, Ondřej and Žáčková, Pavla and Kuneš, Petr and Světlík, Ivo and Veselý, Josef},\n\tyear = {2010},\n\tkeywords = {Czech Republic, Mesolithic, Plant macroremains, archeology, pollen analysis, pre-Neolithic},\n\tpages = {5--38},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2009\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2009')\"\n      onkeypress=\"toggleGroup('group_2009')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2009</span>\n      <span class=\"bibbase_group_count\">\n        \n        (1)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"kune-abraham-kovk-kopeck-palyczcontributors-czechquaternarypalynologicaldatabasepalyczreviewandbasicstatisticsofthedata-2009\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Czech Quaternary Palynological Database – PALYCZ: review and basic statistics of the data.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Abraham, V.; Kovářík, O.; Kopecký, M.;  and PALYCZcontributors\n</span>\n\n  \n\n</span>\n\n  <i>Preslia</i>, 81(3): 209–238.  2009.\n  <span class=\"note\">[IF2008=2.396]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kune-abraham-kovk-kopeck-palyczcontributors-czechquaternarypalynologicaldatabasepalyczreviewandbasicstatisticsofthedata-2009\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kune-abraham-kovk-kopeck-palyczcontributors-czechquaternarypalynologicaldatabasepalyczreviewandbasicstatisticsofthedata-2009')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{kunes_czech_2009,\n\ttitle = {Czech {Quaternary} {Palynological} {Database} – {PALYCZ}: review and basic statistics of the data},\n\tvolume = {81},\n\tcopyright = {All rights reserved},\n\tissn = {0032-7786},\n\tlanguage = {English},\n\tnumber = {3},\n\tjournal = {Preslia},\n\tauthor = {Kuneš, Petr and Abraham, Vojtěch and Kovářík, Oleg and Kopecký, Martin and PALYCZcontributors},\n\tyear = {2009},\n\tnote = {[IF2008=2.396]},\n\tkeywords = {Czech Republic, Database, Holocene, Late Glacial, Pollen, Slovakia, numerical methods},\n\tpages = {209--238},\n}\n</pre>\n</div>\n\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2008\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2008')\"\n      onkeypress=\"toggleGroup('group_2008')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2008</span>\n      <span class=\"bibbase_group_count\">\n        \n        (3)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"kune-pelnkov-chytr-jankovsk-pokorn-petr-interpretationofthelastglacialvegetationofeasterncentraleuropeusingmodernanaloguesfromsouthernsiberia-2008\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Interpretation of the last-glacial vegetation of eastern-central Europe using modern analogues from southern Siberia.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Pelánková, B.; Chytrý, M.; Jankovská, V.; Pokorný, P.;  and Petr, L.\n</span>\n\n  \n\n</span>\n\n  <i>Journal of Biogeography</i>, 35(12): 2223–2236.  2008.\n  <span class=\"note\">[IF2007=3.539]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1111/j.1365-2699.2008.01974.x\"\n     onclick=\"log_download('kune-pelnkov-chytr-jankovsk-pokorn-petr-interpretationofthelastglacialvegetationofeasterncentraleuropeusingmodernanaloguesfromsouthernsiberia-2008', 'http://doi.org/10.1111/j.1365-2699.2008.01974.x', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kune-pelnkov-chytr-jankovsk-pokorn-petr-interpretationofthelastglacialvegetationofeasterncentraleuropeusingmodernanaloguesfromsouthernsiberia-2008\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>2 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kune-pelnkov-chytr-jankovsk-pokorn-petr-interpretationofthelastglacialvegetationofeasterncentraleuropeusingmodernanaloguesfromsouthernsiberia-2008')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{kunes_interpretation_2008,\n\ttitle = {Interpretation of the last-glacial vegetation of eastern-central {Europe} using modern analogues from southern {Siberia}},\n\tvolume = {35},\n\tcopyright = {All rights reserved},\n\tissn = {1365-2699},\n\tdoi = {10.1111/j.1365-2699.2008.01974.x},\n\tlanguage = {English},\n\tnumber = {12},\n\tjournal = {Journal of Biogeography},\n\tauthor = {Kuneš, Petr and Pelánková, Barbora and Chytrý, Milan and Jankovská, Vlasta and Pokorný, Petr and Petr, Libor},\n\tyear = {2008},\n\tnote = {[IF2007=3.539]},\n\tkeywords = {Central Europe, Late Glacial, Pollen, Siberia, Surface sample, glacial, modern analogue, pre-Neolithic, steppe},\n\tpages = {2223--2236},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"kune-pokorn-da-detectionoftheimpactofearlyholocenehuntergatherersonvegetationintheczechrepublicusingmultivariateanalysisofpollendata-2008\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Detection of the impact of early Holocene hunter-gatherers on vegetation in the Czech Republic, using multivariate analysis of pollen data.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Pokorný, P.;  and Šída, P.\n</span>\n\n  \n\n</span>\n\n  <i>Vegetation History and Archaeobotany</i>, 17(3): 269–287. May 2008.\n  <span class=\"note\">[IF2007=1.076]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s00334-007-0119-5\"\n     onclick=\"log_download('kune-pokorn-da-detectionoftheimpactofearlyholocenehuntergatherersonvegetationintheczechrepublicusingmultivariateanalysisofpollendata-2008', 'http://doi.org/10.1007/s00334-007-0119-5', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kune-pokorn-da-detectionoftheimpactofearlyholocenehuntergatherersonvegetationintheczechrepublicusingmultivariateanalysisofpollendata-2008\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n  &nbsp;\n  <a class=\"bibbase_abstract_link bibbase link\"\n     href=\"#\"\n     onclick=\"showAbstract(event); return false;\">\n    abstract <i class=\"fa fa-caret-down\"></i></a>\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kune-pokorn-da-detectionoftheimpactofearlyholocenehuntergatherersonvegetationintheczechrepublicusingmultivariateanalysisofpollendata-2008')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{kunes_detection_2008,\n\ttitle = {Detection of the impact of early {Holocene} hunter-gatherers on vegetation in the {Czech} {Republic}, using multivariate analysis of pollen data},\n\tvolume = {17},\n\tcopyright = {All rights reserved},\n\tissn = {0939-6314, 1617-6278},\n\tdoi = {10.1007/s00334-007-0119-5},\n\tabstract = {Pollen data from the Czech Republic was used to detect the early Holocene impact of hunter-gatherers on vegetation based on a selection of 19 early Holocene pollen profiles, complemented with archaeological information regarding the intensity of local and regional Mesolithic human habitation. Archaeological evidence was assigned to simple categories reflecting the intensity of habitation and distance from pollen sites. Multivariate methods (PCA and RDA) were used to determine relationships between sites and possible anthropogenic pollen indicators and to test how these indicators relate to the archaeological evidence. In several profiles the pollen signal was influenced by local Mesolithic settlement. Specific pollen types (e.g. Calluna vulgaris, Plantago lanceolata, Solanum and Pteridium aquilinum) were found to be significantly correlated with human activity. The role of settlement proximity to the investigation site, the statistical significance of pollen indicators of human activity, as well as the early occurrence of Corylus avellana and its possible anthropogenic dispersal, are discussed.},\n\tlanguage = {English},\n\tnumber = {3},\n\tjournal = {Vegetation History and Archaeobotany},\n\tauthor = {Kuneš, Petr and Pokorný, Petr and Šída, Petr},\n\tmonth = may,\n\tyear = {2008},\n\tnote = {[IF2007=1.076]},\n\tkeywords = {Database, Mesolithic, Multivariate analysis, Pollen, archeology, climate change, human impact, pre-Neolithic},\n\tpages = {269--287},\n}\n\n</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Pollen data from the Czech Republic was used to detect the early Holocene impact of hunter-gatherers on vegetation based on a selection of 19 early Holocene pollen profiles, complemented with archaeological information regarding the intensity of local and regional Mesolithic human habitation. Archaeological evidence was assigned to simple categories reflecting the intensity of habitation and distance from pollen sites. Multivariate methods (PCA and RDA) were used to determine relationships between sites and possible anthropogenic pollen indicators and to test how these indicators relate to the archaeological evidence. In several profiles the pollen signal was influenced by local Mesolithic settlement. Specific pollen types (e.g. Calluna vulgaris, Plantago lanceolata, Solanum and Pteridium aquilinum) were found to be significantly correlated with human activity. The role of settlement proximity to the investigation site, the statistical significance of pollen indicators of human activity, as well as the early occurrence of Corylus avellana and its possible anthropogenic dispersal, are discussed.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"pelnkov-kune-jankovsk-chytr-ermakov-svobodovsvitavsk-therelationshipofmodernpollenspectratovegetationandclimatealongasteppeforesttundratransitioninsouthernsiberiaexploredbydecisiontrees-2008\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  The relationship of modern pollen spectra to vegetation and climate along a steppe-forest-tundra transition in southern Siberia, explored by decision trees.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Pelánková, B.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Jankovská, V.; Chytrý, M.; Ermakov, N.;  and Svobodová-Svitavská, H.\n</span>\n\n  \n\n</span>\n\n  <i>The Holocene</i>, 18(8): 1259–1271.  2008.\n  <span class=\"note\">[IF2007=2.343]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1177/0959683608096600\"\n     onclick=\"log_download('pelnkov-kune-jankovsk-chytr-ermakov-svobodovsvitavsk-therelationshipofmodernpollenspectratovegetationandclimatealongasteppeforesttundratransitioninsouthernsiberiaexploredbydecisiontrees-2008', 'http://doi.org/10.1177/0959683608096600', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/pelnkov-kune-jankovsk-chytr-ermakov-svobodovsvitavsk-therelationshipofmodernpollenspectratovegetationandclimatealongasteppeforesttundratransitioninsouthernsiberiaexploredbydecisiontrees-2008\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n  &nbsp;\n  <span class=\"bibbase_stats_paper\" style=\"color: #777;\">\n    <span>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('pelnkov-kune-jankovsk-chytr-ermakov-svobodovsvitavsk-therelationshipofmodernpollenspectratovegetationandclimatealongasteppeforesttundratransitioninsouthernsiberiaexploredbydecisiontrees-2008')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{pelankova_relationship_2008,\n\ttitle = {The relationship of modern pollen spectra to vegetation and climate along a steppe-forest-tundra transition in southern {Siberia}, explored by decision trees},\n\tvolume = {18},\n\tcopyright = {All rights reserved},\n\tdoi = {10.1177/0959683608096600},\n\tlanguage = {English},\n\tnumber = {8},\n\tjournal = {The Holocene},\n\tauthor = {Pelánková, Barbora and Kuneš, Petr and Jankovská, Vlasta and Chytrý, Milan and Ermakov, Nikolai and Svobodová-Svitavská, Helena},\n\tyear = {2008},\n\tnote = {[IF2007=2.343]},\n\tkeywords = {Pollen, Siberia, Surface sample, modern analogue, pre-Neolithic},\n\tpages = {1259--1271},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2007\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2007')\"\n      onkeypress=\"toggleGroup('group_2007')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2007</span>\n      <span class=\"bibbase_group_count\">\n        \n        (3)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"kune-pokorn-jankovsk-postglacialvegetationdevelopmentinsandstoneareasoftheczechrepublic-2007\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Post-glacial vegetation development in sandstone areas of the Czech Republic.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>; Pokorný, P.;  and Jankovská, V.\n</span>\n\n  \n\n</span>\n\n  In Härtel, H.; Cílek, V.; Herben, T.; Jackson, A.;  and Williams, R., editor(s), <i>Sandstone Landscapes</i>, pages 244–257. Academia, Praha,  2007.\n  <span class=\"note\"></span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/kune-pokorn-jankovsk-postglacialvegetationdevelopmentinsandstoneareasoftheczechrepublic-2007\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('kune-pokorn-jankovsk-postglacialvegetationdevelopmentinsandstoneareasoftheczechrepublic-2007')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@incollection{kunes_post-glacial_2007,\n\taddress = {Praha},\n\ttitle = {Post-glacial vegetation development in sandstone areas of the {Czech} {Republic}},\n\tcopyright = {All rights reserved},\n\tisbn = {978-80-200-1577-8},\n\tlanguage = {English},\n\tbooktitle = {Sandstone {Landscapes}},\n\tpublisher = {Academia},\n\tauthor = {Kuneš, Petr and Pokorný, Petr and Jankovská, Vlasta},\n\teditor = {Härtel, Handrij and Cílek, Václav and Herben, Tomáš and Jackson, Andrew and Williams, Rendel},\n\tyear = {2007},\n\tkeywords = {Czech Republic, Holocene, Late Glacial, human impact, pollen analysis, sandstone, vegetation history},\n\tpages = {244--257},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"da-pokorn-kune-devnartefaktyranholocennhostzlitorluzaniklhojezeravarcenberkearlyholocenewoodenartifactsfromthelakevarcenberk-2007\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Dřevěné artefakty raně holocenního stáří z litorálu zaniklého jezera Švarcenberk [Early Holocene wooden artifacts from the Lake Švarcenberk].\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Šída, P.; Pokorný, P.;  and <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>\n</span>\n\n  \n\n</span>\n\n  <i>Přehled výzkumů</i>, 48: 55–64.  2007.\n  <span class=\"note\">In Czech</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/da-pokorn-kune-devnartefaktyranholocennhostzlitorluzaniklhojezeravarcenberkearlyholocenewoodenartifactsfromthelakevarcenberk-2007\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('da-pokorn-kune-devnartefaktyranholocennhostzlitorluzaniklhojezeravarcenberkearlyholocenewoodenartifactsfromthelakevarcenberk-2007')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{sida_drevene_2007,\n\ttitle = {Dřevěné artefakty raně holocenního stáří z litorálu zaniklého jezera Švarcenberk [{Early} {Holocene} wooden artifacts from the {Lake} Švarcenberk]},\n\tvolume = {48},\n\tcopyright = {All rights reserved},\n\tlanguage = {Czech},\n\tjournal = {Přehled výzkumů},\n\tauthor = {Šída, Petr and Pokorný, Petr and Kuneš, Petr},\n\tyear = {2007},\n\tnote = {In Czech},\n\tkeywords = {Holocene, Mesolithic, archeology, pre-Neolithic},\n\tpages = {55--64},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"jankovsk-kune-vanderknaap-1fljekiefernkrunhorymountainslateglacialandholocenevegetationdevelopment-2007\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.informaworld.com/10.1080/00173130701526341\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'jankovsk-kune-vanderknaap-1fljekiefernkrunhorymountainslateglacialandholocenevegetationdevelopment-2007', 'http://www.informaworld.com/10.1080/00173130701526341', event);\">\n    1. Fláje-Kiefern (Krušné Hory Mountains): Late Glacial and Holocene vegetation development.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Jankovská, V.; <a class=\"bibbase author link\" href=\"https://petr.kunes.net/disturbance-dynamics/\">Kuneš, P.</a>;  and van der Knaap, W. O.\n</span>\n\n  \n\n</span>\n\n  <i>Grana</i>, 46(3): 214–216. November 2007.\n  <span class=\"note\">[IF2006=0.689]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n  <a href=\"http://www.informaworld.com/10.1080/00173130701526341\"\n     onclick=\"log_download('jankovsk-kune-vanderknaap-1fljekiefernkrunhorymountainslateglacialandholocenevegetationdevelopment-2007', 'http://www.informaworld.com/10.1080/00173130701526341', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"1. Fláje-Kiefern (Krušné Hory Mountains): Late Glacial and Holocene vegetation development [link]\"\n       title=\"Paper\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Paper</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1080/00173130701526341\"\n     onclick=\"log_download('jankovsk-kune-vanderknaap-1fljekiefernkrunhorymountainslateglacialandholocenevegetationdevelopment-2007', 'http://doi.org/10.1080/00173130701526341', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/jankovsk-kune-vanderknaap-1fljekiefernkrunhorymountainslateglacialandholocenevegetationdevelopment-2007\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('jankovsk-kune-vanderknaap-1fljekiefernkrunhorymountainslateglacialandholocenevegetationdevelopment-2007')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{jankovska_1._2007,\n\ttitle = {1. {Fláje}-{Kiefern} ({Krušné} {Hory} {Mountains}): {Late} {Glacial} and {Holocene} vegetation development},\n\tvolume = {46},\n\tcopyright = {All rights reserved},\n\tissn = {0017-3134},\n\turl = {http://www.informaworld.com/10.1080/00173130701526341},\n\tdoi = {10.1080/00173130701526341},\n\tlanguage = {English},\n\tnumber = {3},\n\tjournal = {Grana},\n\tauthor = {Jankovská, Vlasta and Kuneš, Petr and van der Knaap, Willem O.},\n\tmonth = nov,\n\tyear = {2007},\n\tnote = {[IF2006=0.689]},\n\tkeywords = {Czech Republic, Database, Holocene, pollen analysis, vegetation history},\n\tpages = {214--216},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n  <div class=\"bibbase_group_whole\" id=\"group_2006\">\n    <div class=\"bibbase_group\"\n      onclick=\"toggleGroup('group_2006')\"\n      onkeypress=\"toggleGroup('group_2006')\"\n      tabindex=\"0\">\n      <i class=\"fa fa-angle-down bibbase_group_head_icon\"></i>&nbsp;\n      <span>2006</span>\n      <span class=\"bibbase_group_count\">\n        \n        (1)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"pokorn-boenke-chytrek-novkov-sdlo-vesel-kune-jankovsk-insightintotheenvironmentofapreromanironagehillfortatvladaczechrepublicusingamultiproxyapproach-2006\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Insight into the environment of a pre-Roman Iron Age hillfort at Vladař, Czech Republic, using a multi-proxy approach.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Pokorný, P.; Boenke, N.; Chytráček, M.; Nováková, K.; Sádlo, J.; Veselý, J.; Kuneš, P.;  and Jankovská, V.\n</span>\n\n  \n\n</span>\n\n  <i>Vegetation History and Archaeobotany</i>, 15(4): 419–433. July 2006.\n  <span class=\"note\">[IF2005=0.739]</span>\n\n<span class=\"bibbase_note\"></span>\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content dontprint\">\n\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s00334-006-0064-8\"\n     onclick=\"log_download('pokorn-boenke-chytrek-novkov-sdlo-vesel-kune-jankovsk-insightintotheenvironmentofapreromanironagehillfortatvladaczechrepublicusingamultiproxyapproach-2006', 'http://doi.org/10.1007/s00334-006-0064-8', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/pokorn-boenke-chytrek-novkov-sdlo-vesel-kune-jankovsk-insightintotheenvironmentofapreromanironagehillfortatvladaczechrepublicusingamultiproxyapproach-2006\"\n     class=\"bibbase bibbase_page link\">link</a>\n  &nbsp;\n  \n\n  <a href=\"#\"\n     onclick=\"showBib(event); return false;\"\n     class=\"bibbase bibtex link\">bibtex\n    <i class=\"fa fa-caret-down\"></i></a>\n\n  \n\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('pokorn-boenke-chytrek-novkov-sdlo-vesel-kune-jankovsk-insightintotheenvironmentofapreromanironagehillfortatvladaczechrepublicusingamultiproxyapproach-2006')\" -->\n  <!--    title=\"Marking this paper as read adds it to your library on BibBase.\" -->\n  <!--    > -->\n  <!--   <i class=\"fa fa-check\"></i>&nbsp; -->\n  <!--   <span>mark as read</span> -->\n  <!-- </a> -->\n\n  &nbsp;\n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n  \n\n</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{pokorny_insight_2006,\n\ttitle = {Insight into the environment of a pre-{Roman} {Iron} {Age} hillfort at {Vladař}, {Czech} {Republic}, using a multi-proxy approach},\n\tvolume = {15},\n\tcopyright = {All rights reserved},\n\tissn = {0939-6314, 1617-6278},\n\tdoi = {10.1007/s00334-006-0064-8},\n\tlanguage = {English},\n\tnumber = {4},\n\turldate = {2012-01-05},\n\tjournal = {Vegetation History and Archaeobotany},\n\tauthor = {Pokorný, Petr and Boenke, Nicole and Chytráček, Miloslav and Nováková, Kateřina and Sádlo, Jiří and Veselý, Josef and Kuneš, Petr and Jankovská, Vlasta},\n\tmonth = jul,\n\tyear = {2006},\n\tnote = {[IF2005=0.739]},\n\tkeywords = {Czech Republic, Plant macroremains, archeology, cladocera, human impact, pollen analysis},\n\tpages = {419--433},\n}\n\n</pre>\n</div>\n\n\n\n</div>\n\n\n\n\n\n    </div>\n  </div>\n\n\n\n\n  </div>\n\n\n  <!-- Modal -->\n\n  <!-- <iframe id=\"bibbase_network_frame\" -->\n  <!--         src=\"//bibbase.org/network/control\" -->\n  <!--         style=\"display: none;\"> -->\n  <!-- </iframe> -->\n\n</div>\n"}; document.write(bibbase_data.data);