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\n  \n 2020\n \n \n (3)\n \n \n
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\n \n\n \n \n \n \n \n Can relict-rich communities be of an anthropogenic origin? Palaeoecological insight into conservation strategy for endangered Carpathian travertine fens.\n \n \n \n\n\n \n Hájková, P.; Jamrichová, E.; Šolcová, A.; Frodlová, J.; Petr, L.; Dítě, D.; Hájek, M.; and Horsák, M.\n\n\n \n\n\n\n Quaternary Science Reviews, 234. 2020.\n \n\n\n\n
\n\n\n\n \n\n \n \n doi\n  \n \n\n \n link\n  \n \n\n bibtex\n \n\n \n  \n \n abstract \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 \n \n\n\n\n
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@article{\n title = {Can relict-rich communities be of an anthropogenic origin? Palaeoecological insight into conservation strategy for endangered Carpathian travertine fens},\n type = {article},\n year = {2020},\n keywords = {Active management,Human influence,Macrofossil analysis,Molluscs,Phragmites australis,Pollen},\n volume = {234},\n id = {d4841926-1535-353b-8414-98e1b4d9cee7},\n created = {2020-10-27T07:27:47.670Z},\n file_attached = {false},\n profile_id = {eb02e700-d0d6-3850-bf58-0ab82dfdbfcf},\n last_modified = {2020-10-27T07:27:47.670Z},\n read = {false},\n starred = {false},\n authored = {true},\n confirmed = {false},\n hidden = {false},\n private_publication = {false},\n abstract = {© 2020 Elsevier Ltd Western-Carpathian travertine fens developed on deep-circulation groundwater are highly localised and harbour unique communities that combine rare species of calcareous fens and salt marshes, with many species considered glacial or Early-Holocene relicts. Using a multi-proxy palaeoecological approach, we tested the assumption of naturalness and Holocene continuity of the current plant and mollusc communities occupying one of the best-preserved travertine fens in Europe. Our novel results, based on two complete cores throughout the fen deposits, document an anthropogenic origin of the current communities, despite their richness in rare and relict species. The habitat originated in the very beginning of the Holocene, later it was encroached by a semi-open woodland with spruce and alder and then by a dense reed bed that suppressed fen species even more than woodland encroachment. When compared with a fen site on shallow-circulation groundwater, the Holocene succession to woodlands has been blocked by travertine formation, allowing survival of light-demanding relicts in small patches. The current communities were established once the woody plants, and especially reed, were reduced by medieval land use. The community itself is therefore not relict, but it harbours probable descendants of relict populations that survived in neighbouring small refugia throughout the Holocene. Our results strongly support the need for active conservation actions as mowing and extensive grazing, mimicking the traditional type of land use, which has conditioned the recent travertine assemblages in the past.},\n bibtype = {article},\n author = {Hájková, P. and Jamrichová, E. and Šolcová, A. and Frodlová, J. and Petr, L. and Dítě, D. and Hájek, M. and Horsák, M.},\n doi = {10.1016/j.quascirev.2020.106241},\n journal = {Quaternary Science Reviews}\n}
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\n © 2020 Elsevier Ltd Western-Carpathian travertine fens developed on deep-circulation groundwater are highly localised and harbour unique communities that combine rare species of calcareous fens and salt marshes, with many species considered glacial or Early-Holocene relicts. Using a multi-proxy palaeoecological approach, we tested the assumption of naturalness and Holocene continuity of the current plant and mollusc communities occupying one of the best-preserved travertine fens in Europe. Our novel results, based on two complete cores throughout the fen deposits, document an anthropogenic origin of the current communities, despite their richness in rare and relict species. The habitat originated in the very beginning of the Holocene, later it was encroached by a semi-open woodland with spruce and alder and then by a dense reed bed that suppressed fen species even more than woodland encroachment. When compared with a fen site on shallow-circulation groundwater, the Holocene succession to woodlands has been blocked by travertine formation, allowing survival of light-demanding relicts in small patches. The current communities were established once the woody plants, and especially reed, were reduced by medieval land use. The community itself is therefore not relict, but it harbours probable descendants of relict populations that survived in neighbouring small refugia throughout the Holocene. Our results strongly support the need for active conservation actions as mowing and extensive grazing, mimicking the traditional type of land use, which has conditioned the recent travertine assemblages in the past.\n
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\n \n\n \n \n \n \n \n Abrupt vegetation and environmental change since the MIS 2: A unique paleorecord from Slovakia (Central Europe).\n \n \n \n\n\n \n Šolcová, A.; Jamrichová, E.; Horsák, M.; Pařil, P.; Petr, L.; Heiri, O.; Květoň, J.; Křížek, M.; Hartvich, F.; Hájek, M.; and Hájková, P.\n\n\n \n\n\n\n Quaternary Science Reviews, 230. 2020.\n \n\n\n\n
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@article{\n title = {Abrupt vegetation and environmental change since the MIS 2: A unique paleorecord from Slovakia (Central Europe)},\n type = {article},\n year = {2020},\n keywords = {Central Europe,Chironomids,Holocene,Lateglacial,MIS 2/MIS 1 transition,Paleoclimatology,Paleolimnology,Stable isotopes,Travertine,Vegetation dynamics},\n volume = {230},\n id = {5039f226-88c5-393f-8d64-c3e77117f83d},\n created = {2020-10-27T07:27:47.732Z},\n file_attached = {false},\n profile_id = {eb02e700-d0d6-3850-bf58-0ab82dfdbfcf},\n last_modified = {2020-10-27T07:27:47.732Z},\n read = {false},\n starred = {false},\n authored = {true},\n confirmed = {false},\n hidden = {false},\n private_publication = {false},\n abstract = {© 2020 Elsevier Ltd Research on past abrupt climate change and linked biotic response is essential for understanding of the future development of biota under changing climatic conditions, which, in turn, is necessary for adequate progress in ecosystem management and nature conservation. The present study presents the first comprehensive reconstruction of local and regional environment at the Western Carpathian/Pannonian Basin border, including a first chironomid-based paleoclimate reconstruction and δ18O and δ13C records from travertine, to investigate abrupt biota and climate shifts since the Marine Isotope Stage (MIS) 2. A range of biotic and abiotic proxy data in organic-calcareous sediment sequence were analysed using a multi-proxy approach to produce a detailed reconstruction of past ecosystem conditions. The results illustrate that the most prominent abrupt change in the local environment occurred directly at the MIS 2/MIS 1 transition at 14,560 cal BP as a consequence of increased precipitation and an increase in reconstructed mean July temperature by ∼2.2 °C. Abrupt changes in local environment during the early Holocene were closely linked to travertine precipitation rate around thermal springs and thus indirectly to the climate until the arrival of the Late Neolithics around 6400 cal BP. Regional vegetation response (derived from pollen data) to the climatic fluctuations lagged, with the most prominent changes around 14,410 cal BP and 10,140 cal BP. Our data suggest the presence of a steppe-tundra ecosystem with evidence for low amounts of temperate broadleaf trees during the MIS 2, indicating close proximity to their northern glacial refugium. We demonstrate the ability of δ18O and δ13C stable isotope record from travertine to reflect abrupt climatic and environmental changes. The study provides evidence about benefits using travertine deposits coupled with high-resolution paleoecological data to investigate past biotic and abiotic responses to abrupt climate change.},\n bibtype = {article},\n author = {Šolcová, A. and Jamrichová, E. and Horsák, M. and Pařil, P. and Petr, L. and Heiri, O. and Květoň, J. and Křížek, M. and Hartvich, F. and Hájek, M. and Hájková, P.},\n doi = {10.1016/j.quascirev.2020.106170},\n journal = {Quaternary Science Reviews}\n}
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\n © 2020 Elsevier Ltd Research on past abrupt climate change and linked biotic response is essential for understanding of the future development of biota under changing climatic conditions, which, in turn, is necessary for adequate progress in ecosystem management and nature conservation. The present study presents the first comprehensive reconstruction of local and regional environment at the Western Carpathian/Pannonian Basin border, including a first chironomid-based paleoclimate reconstruction and δ18O and δ13C records from travertine, to investigate abrupt biota and climate shifts since the Marine Isotope Stage (MIS) 2. A range of biotic and abiotic proxy data in organic-calcareous sediment sequence were analysed using a multi-proxy approach to produce a detailed reconstruction of past ecosystem conditions. The results illustrate that the most prominent abrupt change in the local environment occurred directly at the MIS 2/MIS 1 transition at 14,560 cal BP as a consequence of increased precipitation and an increase in reconstructed mean July temperature by ∼2.2 °C. Abrupt changes in local environment during the early Holocene were closely linked to travertine precipitation rate around thermal springs and thus indirectly to the climate until the arrival of the Late Neolithics around 6400 cal BP. Regional vegetation response (derived from pollen data) to the climatic fluctuations lagged, with the most prominent changes around 14,410 cal BP and 10,140 cal BP. Our data suggest the presence of a steppe-tundra ecosystem with evidence for low amounts of temperate broadleaf trees during the MIS 2, indicating close proximity to their northern glacial refugium. We demonstrate the ability of δ18O and δ13C stable isotope record from travertine to reflect abrupt climatic and environmental changes. The study provides evidence about benefits using travertine deposits coupled with high-resolution paleoecological data to investigate past biotic and abiotic responses to abrupt climate change.\n
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\n \n\n \n \n \n \n \n The role of climate-fuel feedbacks on Holocene biomass burning in upper-montane Carpathian forests.\n \n \n \n\n\n \n Carter, V.; Bobek, P.; Moravcová, A.; Šolcová, A.; Chiverrell, R.; Clear, J.; Finsinger, W.; Feurdean, A.; Tanţău, I.; Magyari, E.; Brussel, T.; and Kuneš, P.\n\n\n \n\n\n\n Global and Planetary Change, 193. 2020.\n \n\n\n\n
\n\n\n\n \n\n \n \n doi\n  \n \n\n \n link\n  \n \n\n bibtex\n \n\n \n  \n \n abstract \n \n\n \n  \n \n 5 downloads\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 \n \n \n \n \n \n \n \n \n\n\n\n
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@article{\n title = {The role of climate-fuel feedbacks on Holocene biomass burning in upper-montane Carpathian forests},\n type = {article},\n year = {2020},\n keywords = {Carpathians,Fire,Forest composition,Forest density,Holocene,Macrofossils,Picea abies,Pollen,Sedimentary charcoal,Upper-montane},\n volume = {193},\n id = {f138466f-a598-316d-8e6e-397149152533},\n created = {2020-10-27T07:27:47.787Z},\n file_attached = {false},\n profile_id = {eb02e700-d0d6-3850-bf58-0ab82dfdbfcf},\n last_modified = {2020-10-27T07:27:47.787Z},\n read = {false},\n starred = {false},\n authored = {true},\n confirmed = {false},\n hidden = {false},\n private_publication = {false},\n abstract = {© 2020 Elsevier B.V. Over the past few decades, mean summer temperatures within the Carpathian Mountains have increased by as much as 2 °C leading to a projected increased forest fire risk. Currently, there are no paleofire records from the Western Carpathians that provide the long-term range of natural variability to contextualise the response of upper-montane forests to future environmental change and disturbance regimes. We present the first high-resolution Holocene fire history record from the upper-montane ecotone from the High Tatra Mountains, Slovakia, as well as provide a regional synthesis of pan-Carpathian drivers of biomass burning in upper-montane forests. Our results illustrate that forest composition and density both greatly influence biomass burning, creating two different climate-fuel feedbacks. First, warmer conditions in the early Holocene, coupled with generally higher abundances of Pinus sp., either P. cembra and/or P. mugo/sylvestris, created a positive climate-fuel relationship that resulted in higher amounts of biomass burning. Second, cooler and wetter late Holocene conditions led to denser Picea abies upper-montane forests, creating a negative climate-fuel feedback that reduced biomass burning in upper-montane forests across the Carpathians. Given that warmer and drier conditions are expected across the entire Carpathian region in the future, our results illustrate how future climate change could potentially create a positive climate-fuel relationship within upper-montane forests dominated by Picea abies and Pinus cembra and/or P. mugo/sylvestris.},\n bibtype = {article},\n author = {Carter, V.A. and Bobek, P. and Moravcová, A. and Šolcová, A. and Chiverrell, R.C. and Clear, J.L. and Finsinger, W. and Feurdean, A. and Tanţău, I. and Magyari, E. and Brussel, T. and Kuneš, P.},\n doi = {10.1016/j.gloplacha.2020.103264},\n journal = {Global and Planetary Change}\n}
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\n © 2020 Elsevier B.V. Over the past few decades, mean summer temperatures within the Carpathian Mountains have increased by as much as 2 °C leading to a projected increased forest fire risk. Currently, there are no paleofire records from the Western Carpathians that provide the long-term range of natural variability to contextualise the response of upper-montane forests to future environmental change and disturbance regimes. We present the first high-resolution Holocene fire history record from the upper-montane ecotone from the High Tatra Mountains, Slovakia, as well as provide a regional synthesis of pan-Carpathian drivers of biomass burning in upper-montane forests. Our results illustrate that forest composition and density both greatly influence biomass burning, creating two different climate-fuel feedbacks. First, warmer conditions in the early Holocene, coupled with generally higher abundances of Pinus sp., either P. cembra and/or P. mugo/sylvestris, created a positive climate-fuel relationship that resulted in higher amounts of biomass burning. Second, cooler and wetter late Holocene conditions led to denser Picea abies upper-montane forests, creating a negative climate-fuel feedback that reduced biomass burning in upper-montane forests across the Carpathians. Given that warmer and drier conditions are expected across the entire Carpathian region in the future, our results illustrate how future climate change could potentially create a positive climate-fuel relationship within upper-montane forests dominated by Picea abies and Pinus cembra and/or P. mugo/sylvestris.\n
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\n \n\n \n \n \n \n \n Lowland pine forests in the northwestern Pannonian Basin: between natural vegetation and modern plantations.\n \n \n \n\n\n \n Jamrichová, E.; Bobek, P.; Šolcová, A.; Tkáč, P.; Hédl, R.; and Valachovič, M.\n\n\n \n\n\n\n Regional Environmental Change, 19(8). 2019.\n \n\n\n\n
\n\n\n\n \n\n \n \n doi\n  \n \n\n \n link\n  \n \n\n bibtex\n \n\n \n  \n \n abstract \n \n\n \n  \n \n 1 download\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 \n\n\n\n
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@article{\n title = {Lowland pine forests in the northwestern Pannonian Basin: between natural vegetation and modern plantations},\n type = {article},\n year = {2019},\n keywords = {Conifer plantations,Lowland pine forest,Multi-proxy data,Palaeoecology,Pinus,Quercus},\n volume = {19},\n id = {73d9d60b-f2df-3ba3-8346-0fbf475b709a},\n created = {2020-10-27T07:27:47.667Z},\n file_attached = {false},\n profile_id = {eb02e700-d0d6-3850-bf58-0ab82dfdbfcf},\n last_modified = {2020-10-27T07:27:47.667Z},\n read = {false},\n starred = {false},\n authored = {true},\n confirmed = {false},\n hidden = {false},\n private_publication = {false},\n abstract = {© 2019, Springer-Verlag GmbH Germany, part of Springer Nature. 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 bibtype = {article},\n author = {Jamrichová, E. and Bobek, P. and Šolcová, A. and Tkáč, P. and Hédl, R. and Valachovič, M.},\n doi = {10.1007/s10113-019-01555-y},\n journal = {Regional Environmental Change},\n number = {8}\n}
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\n © 2019, Springer-Verlag GmbH Germany, part of Springer Nature. 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
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\n \n\n \n \n \n \n \n \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 \n \n \n \n\n\n \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\n\n \n\n\n\n Quaternary International, 511: 124-139. 3 2019.\n \n\n\n\n
\n\n\n\n \n \n \"DisruptionWebsite\n  \n \n\n \n \n doi\n  \n \n\n \n link\n  \n \n\n bibtex\n \n\n \n\n \n  \n \n 1 download\n \n \n\n \n \n \n \n \n \n \n\n  \n \n \n\n\n\n
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@article{\n title = {Disruption in an alluvial landscape: Settlement and environment dynamics on the alluvium of the river Dyje at the Pohansko archaeological site (Czech Republic)},\n type = {article},\n year = {2019},\n pages = {124-139},\n volume = {511},\n websites = {https://linkinghub.elsevier.com/retrieve/pii/S1040618217309503},\n month = {3},\n id = {610bdf60-31cb-3a36-bc3b-c263c5f1f47f},\n created = {2020-12-08T03:50:46.296Z},\n file_attached = {false},\n profile_id = {eb02e700-d0d6-3850-bf58-0ab82dfdbfcf},\n last_modified = {2020-12-08T03:50:46.296Z},\n read = {false},\n starred = {false},\n authored = {true},\n confirmed = {true},\n hidden = {false},\n private_publication = {false},\n bibtype = {article},\n 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},\n doi = {10.1016/j.quaint.2018.04.013},\n journal = {Quaternary International}\n}
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\n \n\n \n \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\n\n \n Šolcová, A.; Petr, L.; Hájková, P.; Petřík, J.; Tóth, P.; Rohovec, J.; Bátora, J.; and Horsák, M.\n\n\n \n\n\n\n Boreas, 47(3). 2018.\n \n\n\n\n
\n\n\n\n \n\n \n \n doi\n  \n \n\n \n link\n  \n \n\n bibtex\n \n\n \n  \n \n abstract \n \n\n \n\n \n \n \n \n \n \n \n\n  \n \n \n\n\n\n
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@article{\n title = {Early and middle Holocene ecosystem changes at the Western Carpathian/Pannonian border driven by climate and Neolithic impact},\n type = {article},\n year = {2018},\n volume = {47},\n id = {53f11e42-7dfc-357b-98d0-4a15a5352a29},\n created = {2020-10-27T07:27:47.727Z},\n file_attached = {false},\n profile_id = {eb02e700-d0d6-3850-bf58-0ab82dfdbfcf},\n last_modified = {2020-10-27T07:27:47.727Z},\n read = {false},\n starred = {false},\n authored = {true},\n confirmed = {false},\n hidden = {false},\n private_publication = {false},\n abstract = {© 2018 Collegium Boreas. Published by John Wiley  &  Sons Ltd 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 bibtype = {article},\n author = {Šolcová, A. and Petr, L. and Hájková, P. and Petřík, J. and Tóth, P. and Rohovec, J. and Bátora, J. and Horsák, M.},\n doi = {10.1111/bor.12309},\n journal = {Boreas},\n number = {3}\n}
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\n © 2018 Collegium Boreas. Published by John Wiley & Sons Ltd 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
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\n \n\n \n \n \n \n \n \n Spatiotemporal heterogeneity of the palaeoecological record in a large temperate palaeolake, Šúr, southwest Slovakia: Comparison of pollen, macrofossil and geochemical data.\n \n \n \n \n\n\n \n Potůčková, A.; Hájková, P.; Žáčková, P.; Petr, L.; Grygar, T., M.; and Weiser, M.\n\n\n \n\n\n\n Palaeogeography, Palaeoclimatology, Palaeoecology, 489: 52-63. 1 2018.\n \n\n\n\n
\n\n\n\n \n \n \"SpatiotemporalWebsite\n  \n \n\n \n \n doi\n  \n \n\n \n link\n  \n \n\n bibtex\n \n\n \n\n \n\n \n \n \n \n \n \n \n\n  \n \n \n\n\n\n
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@article{\n title = {Spatiotemporal heterogeneity of the palaeoecological record in a large temperate palaeolake, Šúr, southwest Slovakia: Comparison of pollen, macrofossil and geochemical data},\n type = {article},\n year = {2018},\n pages = {52-63},\n volume = {489},\n websites = {https://linkinghub.elsevier.com/retrieve/pii/S0031018217301219},\n month = {1},\n id = {6fed15d4-cbc5-3b4e-a2b1-5a12289725d3},\n created = {2020-12-08T03:50:46.399Z},\n file_attached = {false},\n profile_id = {eb02e700-d0d6-3850-bf58-0ab82dfdbfcf},\n last_modified = {2020-12-08T03:50:46.399Z},\n read = {false},\n starred = {false},\n authored = {true},\n confirmed = {true},\n hidden = {false},\n private_publication = {false},\n bibtype = {article},\n author = {Potůčková, Anna and Hájková, Petra and Žáčková, Pavla and Petr, Libor and Grygar, Tomáš Matys and Weiser, Martin},\n doi = {10.1016/j.palaeo.2017.09.010},\n journal = {Palaeogeography, Palaeoclimatology, Palaeoecology}\n}
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\n  \n 2017\n \n \n (1)\n \n \n
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\n \n\n \n \n \n \n \n \n Refugial occurrence and ecology of the land snail Vertigo lilljeborgi in fen habitats in temperate mainland Europe.\n \n \n \n \n\n\n \n Horsák, M.; Hájek, M.; Horsáková, V.; Hlaváč, J.; Hájková, P.; Dítě, D.; Peterka, T.; Divíšek, J.; Potůčková, A.; and Preece, R., C.\n\n\n \n\n\n\n Journal of Molluscan Studies, 83(4): 451-460. 11 2017.\n \n\n\n\n
\n\n\n\n \n \n \"RefugialWebsite\n  \n \n\n \n \n doi\n  \n \n\n \n link\n  \n \n\n bibtex\n \n\n \n\n \n\n \n \n \n \n \n \n \n\n  \n \n \n\n\n\n
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@article{\n title = {Refugial occurrence and ecology of the land snail Vertigo lilljeborgi in fen habitats in temperate mainland Europe},\n type = {article},\n year = {2017},\n pages = {451-460},\n volume = {83},\n websites = {https://doi.org/10.17863/CAM.18876,https://academic.oup.com/mollus/article/83/4/451/3978663},\n month = {11},\n day = {1},\n id = {7dcdc9ec-b79a-3187-ae59-b0eb0c360ed5},\n created = {2020-12-08T03:57:30.327Z},\n file_attached = {false},\n profile_id = {eb02e700-d0d6-3850-bf58-0ab82dfdbfcf},\n last_modified = {2020-12-08T04:04:16.399Z},\n read = {false},\n starred = {false},\n authored = {true},\n confirmed = {true},\n hidden = {false},\n private_publication = {false},\n bibtype = {article},\n author = {Horsák, Michal and Hájek, Michal and Horsáková, Veronika and Hlaváč, Jaroslav and Hájková, Petra and Dítě, Daniel and Peterka, Tomáš and Divíšek, Jan and Potůčková, Anna and Preece, Richard Charles},\n doi = {10.1093/mollus/eyx028},\n journal = {Journal of Molluscan Studies},\n number = {4}\n}
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\n  \n 2014\n \n \n (1)\n \n \n
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\n \n\n \n \n \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 \n\n\n \n Jamrichová, E.; Potůčková, A.; Horsák, M.; Hajnalová, M.; Barta, P.; Tóth, P.; and Kuneš, P.\n\n\n \n\n\n\n The Holocene, 24(12): 1810-1824. 12 2014.\n \n\n\n\n
\n\n\n\n \n \n \"EarlyWebsite\n  \n \n\n \n \n doi\n  \n \n\n \n link\n  \n \n\n bibtex\n \n\n \n\n \n\n \n \n \n \n \n \n \n\n  \n \n \n\n\n\n
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@article{\n title = {Early occurrence of temperate oak-dominated forest in the northern part of the Little Hungarian Plain, SW Slovakia},\n type = {article},\n year = {2014},\n pages = {1810-1824},\n volume = {24},\n websites = {http://journals.sagepub.com/doi/10.1177/0959683614551225},\n month = {12},\n day = {30},\n id = {c11900a5-b03b-3895-a137-10429824174c},\n created = {2020-12-08T03:50:46.398Z},\n file_attached = {false},\n profile_id = {eb02e700-d0d6-3850-bf58-0ab82dfdbfcf},\n last_modified = {2020-12-08T03:50:46.398Z},\n read = {false},\n starred = {false},\n authored = {true},\n confirmed = {true},\n hidden = {false},\n private_publication = {false},\n bibtype = {article},\n author = {Jamrichová, Eva and Potůčková, Anna and Horsák, Michal and Hajnalová, Mária and Barta, Peter and Tóth, Peter and Kuneš, Petr},\n doi = {10.1177/0959683614551225},\n journal = {The Holocene},\n number = {12}\n}
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