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: {\"jsonp\":\"1\",\"folding\":\"1\",\"host\":\"bibbase.org\"},\n      data: [{\"title\":\"Paleo sea-level changes and relative sea-level indicators: Precise measurements, indicative meaning and glacial isostatic adjustment perspectives from Mallorca (Western Mediterranean)\",\"type\":\"article\",\"year\":\"2017\",\"keywords\":\"Beach deposits,Last interglacial,MIS 5e,Morphodynamic modelling\",\"pages\":\"94-107\",\"volume\":\"473\",\"websites\":\"http://linkinghub.elsevier.com/retrieve/pii/S0031018216303753\",\"publisher\":\"Elsevier B.V.\",\"id\":\"7abcfe9b-788b-39f2-8a80-0e128ce6d024\",\"created\":\"2018-02-03T12:42:06.762Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:06.762Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Lorscheid2017\",\"private_publication\":false,\"abstract\":\"Paleo relative sea-level (RSL) indicators formed during the Marine Isotope Stage (MIS) 5e have been reported by a large number of studies worldwide. Despite this, three main aspects are seldom reported: (1) use of high-precision survey techniques applied to MIS 5e RSL indicators; (2) application of modern analogs to understand the indicative meaning of MIS 5e RSL indicators; (3) estimates of the effects of glacial isostatic adjustment (GIA) on the MIS 5e records. In this study, we show how the three points above have been addressed in a focused study on Last Interglacial outcrops on the island of Mallorca. We measured the elevation of several RSL indicators with high-accuracy differential GPS (vertical accuracies down to 0.1 m) and we established the relationship between each RSL indicator and the paleo sea level through calculation of the indicative meaning for each RSL indicator. In particular, we present a novel technique to calculate the indicative meaning of fossil beach deposits with a phase-averaged morphodynamic model (CSHORE). We show how this approach helps overcoming difficulties with the survey of the modern analogs for these indicators. Our results show that two paleo RSLs are imprinted in Mallorca at + 2.9 ± 0.8 m and + 11.3 ± 1.0 m. We then compare our field-based results with modelled paleo RSL, calculated from the predictions of the ice-earth coupled ANICE-SELEN model, using few different ice-sheet melting scenarios during MIS 5e. We conclude that indicative ranges can be derived from relatively simple morphodynamic models and that the comparison of field-derived and modelled RSL values is a good method to validate possible scenarios of MIS 5e sea-level variability, especially in absence of precise dating.\",\"bibtype\":\"article\",\"author\":\"Lorscheid, Thomas and Stocchi, Paolo and Casella, Elisa and Gómez-Pujol, Lluis and Vacchi, Matteo and Mann, Thomas and Rovere, Alessio\",\"doi\":\"10.1016/j.palaeo.2017.02.028\",\"journal\":\"Palaeogeography, Palaeoclimatology, Palaeoecology\",\"bibtex\":\"@article{\\n title = {Paleo sea-level changes and relative sea-level indicators: Precise measurements, indicative meaning and glacial isostatic adjustment perspectives from Mallorca (Western Mediterranean)},\\n type = {article},\\n year = {2017},\\n keywords = {Beach deposits,Last interglacial,MIS 5e,Morphodynamic modelling},\\n pages = {94-107},\\n volume = {473},\\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0031018216303753},\\n publisher = {Elsevier B.V.},\\n id = {7abcfe9b-788b-39f2-8a80-0e128ce6d024},\\n created = {2018-02-03T12:42:06.762Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:06.762Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Lorscheid2017},\\n private_publication = {false},\\n abstract = {Paleo relative sea-level (RSL) indicators formed during the Marine Isotope Stage (MIS) 5e have been reported by a large number of studies worldwide. Despite this, three main aspects are seldom reported: (1) use of high-precision survey techniques applied to MIS 5e RSL indicators; (2) application of modern analogs to understand the indicative meaning of MIS 5e RSL indicators; (3) estimates of the effects of glacial isostatic adjustment (GIA) on the MIS 5e records. In this study, we show how the three points above have been addressed in a focused study on Last Interglacial outcrops on the island of Mallorca. We measured the elevation of several RSL indicators with high-accuracy differential GPS (vertical accuracies down to 0.1 m) and we established the relationship between each RSL indicator and the paleo sea level through calculation of the indicative meaning for each RSL indicator. In particular, we present a novel technique to calculate the indicative meaning of fossil beach deposits with a phase-averaged morphodynamic model (CSHORE). We show how this approach helps overcoming difficulties with the survey of the modern analogs for these indicators. Our results show that two paleo RSLs are imprinted in Mallorca at + 2.9 ± 0.8 m and + 11.3 ± 1.0 m. We then compare our field-based results with modelled paleo RSL, calculated from the predictions of the ice-earth coupled ANICE-SELEN model, using few different ice-sheet melting scenarios during MIS 5e. We conclude that indicative ranges can be derived from relatively simple morphodynamic models and that the comparison of field-derived and modelled RSL values is a good method to validate possible scenarios of MIS 5e sea-level variability, especially in absence of precise dating.},\\n bibtype = {article},\\n author = {Lorscheid, Thomas and Stocchi, Paolo and Casella, Elisa and Gómez-Pujol, Lluis and Vacchi, Matteo and Mann, Thomas and Rovere, Alessio},\\n doi = {10.1016/j.palaeo.2017.02.028},\\n journal = {Palaeogeography, Palaeoclimatology, Palaeoecology}\\n}\",\"author_short\":[\"Lorscheid,  T.\",\"Stocchi,  P.\",\"Casella,  E.\",\"Gómez-Pujol,  L.\",\"Vacchi,  M.\",\"Mann,  T.\",\"Rovere,  A.\"],\"urls\":{\"Website\":\"http://linkinghub.elsevier.com/retrieve/pii/S0031018216303753\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"lorscheid-stocchi-casella-gmezpujol-vacchi-mann-rovere-paleosealevelchangesandrelativesealevelindicatorsprecisemeasurementsindicativemeaningandglacialisostaticadjustmentperspectivesfrommallorcawesternmediterranean-2017\",\"role\":\"author\",\"keyword\":[\"Beach deposits\",\"Last interglacial\",\"MIS 5e\",\"Morphodynamic modelling\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/publications.html\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Resilience of the Marine Animal Forest Lessons from Maldivian Coral Reefs After the Mass Mortality of 1998\",\"type\":\"article\",\"year\":\"2015\",\"pages\":\"1-26\",\"websites\":\"http://link.springer.com/10.1007/978-3-319-17001-5\",\"publisher\":\"Springer International Publishing\",\"city\":\"Cham\",\"id\":\"659f5aa2-00c2-3abe-89b3-8922549dafff\",\"created\":\"2018-02-03T12:42:06.776Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.068Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Bianchi2015\",\"source_type\":\"inbook\",\"private_publication\":false,\"abstract\":\"This chapter reviews the major known monospecific and multispecific sponge aggregations in the world’s oceans. They are shown to occur from the intertidal to abyssal depths, in tropical, temperate, and high latitudes and sometimes to create spectacular formations, such as glass sponge reefs, lithistid reef-like fields, and carnivorous sponge grounds. Sponge aggregations are recognized as singular vulnerable habitats that deserve special research attention and legal protection. However, this review reveals that there is only a poor and fragmentary under- standing of the main biological, environmental, and geochemical factors that favor and maintain these systems, including the food supply, which is funda- mental knowledge. There is also a particular lack of information regarding reproductive biology, growth rates, life spans, and the main factors causing mortality, all crucial drivers for understanding population and community dynamics and for developing conservation strategies. The sponge aggregations have been shown to increase the structural complexity of the habitats, attracting a larger variety of organisms and locally enhancing biodiversity. From the very few cases in which sponge biomass and sponge physiology have been reliably approached jointly, phenomenal fluxes of matter and energy have been inferred. Through their benthic-pelagic coupling, some of the densest sponge aggrega- tions have a significant local or regional impact on major biogeochemical cycles and food webs. Physical damage and habitat destruction derived from man-driven activities along with epidemic diseases facilitated by global envi- ronmental alterations emerge as major threats to the future of the sponge aggregations.\",\"bibtype\":\"article\",\"author\":\"Bianchi, Carlo Nike and Morri, Carla and Lasagna, Roberta and Montefalcone, Monica and Gatti, Giulia and Parravicini, Valeriano and Rovere, Alessio\",\"editor\":\"Rossi, Sergio and Bramanti, Lorenzo and Gori, Andrea and del Valle, Covadonga\",\"doi\":\"10.1007/978-3-319-17001-5\",\"journal\":\"Marine Animal Forests\",\"bibtex\":\"@article{\\n title = {Resilience of the Marine Animal Forest Lessons from Maldivian Coral Reefs After the Mass Mortality of 1998},\\n type = {article},\\n year = {2015},\\n pages = {1-26},\\n websites = {http://link.springer.com/10.1007/978-3-319-17001-5},\\n publisher = {Springer International Publishing},\\n city = {Cham},\\n id = {659f5aa2-00c2-3abe-89b3-8922549dafff},\\n created = {2018-02-03T12:42:06.776Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.068Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Bianchi2015},\\n source_type = {inbook},\\n private_publication = {false},\\n abstract = {This chapter reviews the major known monospecific and multispecific sponge aggregations in the world’s oceans. They are shown to occur from the intertidal to abyssal depths, in tropical, temperate, and high latitudes and sometimes to create spectacular formations, such as glass sponge reefs, lithistid reef-like fields, and carnivorous sponge grounds. Sponge aggregations are recognized as singular vulnerable habitats that deserve special research attention and legal protection. However, this review reveals that there is only a poor and fragmentary under- standing of the main biological, environmental, and geochemical factors that favor and maintain these systems, including the food supply, which is funda- mental knowledge. There is also a particular lack of information regarding reproductive biology, growth rates, life spans, and the main factors causing mortality, all crucial drivers for understanding population and community dynamics and for developing conservation strategies. The sponge aggregations have been shown to increase the structural complexity of the habitats, attracting a larger variety of organisms and locally enhancing biodiversity. From the very few cases in which sponge biomass and sponge physiology have been reliably approached jointly, phenomenal fluxes of matter and energy have been inferred. Through their benthic-pelagic coupling, some of the densest sponge aggrega- tions have a significant local or regional impact on major biogeochemical cycles and food webs. Physical damage and habitat destruction derived from man-driven activities along with epidemic diseases facilitated by global envi- ronmental alterations emerge as major threats to the future of the sponge aggregations.},\\n bibtype = {article},\\n author = {Bianchi, Carlo Nike and Morri, Carla and Lasagna, Roberta and Montefalcone, Monica and Gatti, Giulia and Parravicini, Valeriano and Rovere, Alessio},\\n editor = {Rossi, Sergio and Bramanti, Lorenzo and Gori, Andrea and del Valle, Covadonga},\\n doi = {10.1007/978-3-319-17001-5},\\n journal = {Marine Animal Forests}\\n}\",\"author_short\":[\"Bianchi,  C., N.\",\"Morri,  C.\",\"Lasagna,  R.\",\"Montefalcone,  M.\",\"Gatti,  G.\",\"Parravicini,  V.\",\"Rovere,  A.\"],\"editor_short\":[\"Rossi,  S.\",\"Bramanti,  L.\",\"Gori,  A.\",\"del Valle,  C.\"],\"urls\":{\"Website\":\"http://link.springer.com/10.1007/978-3-319-17001-5\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-resilienceofthemarineanimalforestlessonsfrommaldiviancoralreefsafterthemassmortalityof1998-2015\",\"role\":\"author\",\"metadata\":{\"authorlinks\":{}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Through bleaching and tsunami: Coral reef recovery in the Maldives\",\"type\":\"article\",\"year\":\"2015\",\"keywords\":\"Coral reefs,Hard coral cover,Indian Ocean,Maldives,Recruitment,Resilience\",\"pages\":\"188-200\",\"volume\":\"98\",\"websites\":\"http://linkinghub.elsevier.com/retrieve/pii/S0025326X15004178\",\"publisher\":\"Elsevier Ltd\",\"id\":\"d4572baa-b24e-34a7-8fb4-c42c41fe8b00\",\"created\":\"2018-02-03T12:42:06.777Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.231Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Morri2015\",\"private_publication\":false,\"abstract\":\"Coral reefs are degrading worldwide, but little information exists on their previous conditions for most regions of the world. Since 1989, we have been studying the Maldives, collecting data before, during and after the bleaching and mass mortality event of 1998. As early as 1999, many newly settled colonies were recorded. Recruits shifted from a dominance of massive and encrusting corals in the early stages of recolonisation towards a dominance of Acropora and Pocillopora by 2009. Coral cover, which dropped to less than 10% after the bleaching, returned to pre-bleaching values of around 50% by 2013. The 2004 tsunami had comparatively little effect. In 2014, the coral community was similar to that existing before the bleaching. According to descriptors and metrics adopted, recovery of Maldivian coral reefs took between 6 and 15. years, or may even be considered unachieved, as there are species that had not come back yet.\",\"bibtype\":\"article\",\"author\":\"Morri, Carla and Montefalcone, Monica and Lasagna, Roberta and Gatti, Giulia and Rovere, Alessio and Parravicini, Valeriano and Baldelli, Giuseppe and Colantoni, Paolo and Bianchi, Carlo Nike\",\"doi\":\"10.1016/j.marpolbul.2015.06.050\",\"journal\":\"Marine Pollution Bulletin\",\"number\":\"1-2\",\"bibtex\":\"@article{\\n title = {Through bleaching and tsunami: Coral reef recovery in the Maldives},\\n type = {article},\\n year = {2015},\\n keywords = {Coral reefs,Hard coral cover,Indian Ocean,Maldives,Recruitment,Resilience},\\n pages = {188-200},\\n volume = {98},\\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0025326X15004178},\\n publisher = {Elsevier Ltd},\\n id = {d4572baa-b24e-34a7-8fb4-c42c41fe8b00},\\n created = {2018-02-03T12:42:06.777Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.231Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Morri2015},\\n private_publication = {false},\\n abstract = {Coral reefs are degrading worldwide, but little information exists on their previous conditions for most regions of the world. Since 1989, we have been studying the Maldives, collecting data before, during and after the bleaching and mass mortality event of 1998. As early as 1999, many newly settled colonies were recorded. Recruits shifted from a dominance of massive and encrusting corals in the early stages of recolonisation towards a dominance of Acropora and Pocillopora by 2009. Coral cover, which dropped to less than 10% after the bleaching, returned to pre-bleaching values of around 50% by 2013. The 2004 tsunami had comparatively little effect. In 2014, the coral community was similar to that existing before the bleaching. According to descriptors and metrics adopted, recovery of Maldivian coral reefs took between 6 and 15. years, or may even be considered unachieved, as there are species that had not come back yet.},\\n bibtype = {article},\\n author = {Morri, Carla and Montefalcone, Monica and Lasagna, Roberta and Gatti, Giulia and Rovere, Alessio and Parravicini, Valeriano and Baldelli, Giuseppe and Colantoni, Paolo and Bianchi, Carlo Nike},\\n doi = {10.1016/j.marpolbul.2015.06.050},\\n journal = {Marine Pollution Bulletin},\\n number = {1-2}\\n}\",\"author_short\":[\"Morri,  C.\",\"Montefalcone,  M.\",\"Lasagna,  R.\",\"Gatti,  G.\",\"Rovere,  A.\",\"Parravicini,  V.\",\"Baldelli,  G.\",\"Colantoni,  P.\",\"Bianchi,  C., N.\"],\"urls\":{\"Website\":\"http://linkinghub.elsevier.com/retrieve/pii/S0025326X15004178\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"morri-montefalcone-lasagna-gatti-rovere-parravicini-baldelli-colantoni-etal-throughbleachingandtsunamicoralreefrecoveryinthemaldives-2015\",\"role\":\"author\",\"keyword\":[\"Coral reefs\",\"Hard coral cover\",\"Indian Ocean\",\"Maldives\",\"Recruitment\",\"Resilience\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Multiproxy assessment of Holocene relative sea-level changes in the western Mediterranean: variability in the sea-level histories and redefinition of the isostatic signal.\",\"type\":\"article\",\"year\":\"2016\",\"keywords\":\"Holocene,Isostatic adjustment,Mediterranean Sea,Sea-level database,Sea-level proxy\",\"pages\":\"172-197\",\"volume\":\"155\",\"websites\":\"http://dx.doi.org/10.1016/j.earscirev.2016.02.002\",\"publisher\":\"Elsevier B.V.\",\"city\":\"Vienna, AT\",\"id\":\"87ba1930-b220-369d-8afd-6fdf358bb6d5\",\"created\":\"2018-02-03T12:42:07.277Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:07.277Z\",\"read\":\"true\",\"starred\":\"true\",\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Vacchi\",\"private_publication\":false,\"abstract\":\"A review of 917 relative sea-level (RSL) data-points has resulted in the first quality-controlled database constraining the Holocene sea-level histories of the western Mediterranean Sea (Spain, France, Italy, Slovenia, Croatia, Malta and Tunisia). We reviewed and standardized the geological RSL data-points using a new multi-proxy methodology based on: (1) modern taxa assemblages in Mediterranean lagoons and marshes; (2) beachrock characteristics (cement fabric and chemistry, sedimentary structures); and (3) the modern distribution of Mediterranean fixed biological indicators. These RSL data-points were coupled with the large number of archaeological RSL indicators available for the western Mediterranean. We assessed the spatial variability of RSL histories for 22 regions and compared these with the ICE-5G (VM2) GIA model. In the western Mediterranean, RSL rose continuously for the whole Holocene with a sudden slowdown at ~. 7.5 ka BP and a further deceleration during the last ~. 4.0 ka BP, after which time observed RSL changes are mainly related to variability in isostatic adjustment. The sole exception is southern Tunisia, where data show evidence of a mid-Holocene high-stand compatible with the isostatic impacts of the melting history of the remote Antarctic ice sheet.Our results indicate that late-Holocene sea-level rise was significantly slower than the current one. First estimates of GIA contribution indicate that, at least in the northwestern sector, it accounts at least for the 25-30% of the ongoing sea-level rise recorded by Mediterranean tidal gauges. Such contribution is less constrained at lower latitudes due to the lower quality of the late Holocene index points. Future applications of spatio-temporal statistical techniques are required to better quantify the gradient of the isostatic contribution and to provide improved context for the assessment of 20th century acceleration of Mediterranean sea-level rise.\",\"bibtype\":\"article\",\"author\":\"Vacchi, Matteo and Marriner, Nick and Morhange, Christophe and Spada, Giorgio and Fontana, Alessandro and Rovere, Alessio and Marriner, Nick and Morhange, Christophe and Spada, Giorgio and Fontana, Alessandro\",\"doi\":\"10.1016/j.earscirev.2016.02.002\",\"journal\":\"Earth Science Reviews\",\"bibtex\":\"@article{\\n title = {Multiproxy assessment of Holocene relative sea-level changes in the western Mediterranean: variability in the sea-level histories and redefinition of the isostatic signal.},\\n type = {article},\\n year = {2016},\\n keywords = {Holocene,Isostatic adjustment,Mediterranean Sea,Sea-level database,Sea-level proxy},\\n pages = {172-197},\\n volume = {155},\\n websites = {http://dx.doi.org/10.1016/j.earscirev.2016.02.002},\\n publisher = {Elsevier B.V.},\\n city = {Vienna, AT},\\n id = {87ba1930-b220-369d-8afd-6fdf358bb6d5},\\n created = {2018-02-03T12:42:07.277Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:07.277Z},\\n read = {true},\\n starred = {true},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Vacchi},\\n private_publication = {false},\\n abstract = {A review of 917 relative sea-level (RSL) data-points has resulted in the first quality-controlled database constraining the Holocene sea-level histories of the western Mediterranean Sea (Spain, France, Italy, Slovenia, Croatia, Malta and Tunisia). We reviewed and standardized the geological RSL data-points using a new multi-proxy methodology based on: (1) modern taxa assemblages in Mediterranean lagoons and marshes; (2) beachrock characteristics (cement fabric and chemistry, sedimentary structures); and (3) the modern distribution of Mediterranean fixed biological indicators. These RSL data-points were coupled with the large number of archaeological RSL indicators available for the western Mediterranean. We assessed the spatial variability of RSL histories for 22 regions and compared these with the ICE-5G (VM2) GIA model. In the western Mediterranean, RSL rose continuously for the whole Holocene with a sudden slowdown at ~. 7.5 ka BP and a further deceleration during the last ~. 4.0 ka BP, after which time observed RSL changes are mainly related to variability in isostatic adjustment. The sole exception is southern Tunisia, where data show evidence of a mid-Holocene high-stand compatible with the isostatic impacts of the melting history of the remote Antarctic ice sheet.Our results indicate that late-Holocene sea-level rise was significantly slower than the current one. First estimates of GIA contribution indicate that, at least in the northwestern sector, it accounts at least for the 25-30% of the ongoing sea-level rise recorded by Mediterranean tidal gauges. Such contribution is less constrained at lower latitudes due to the lower quality of the late Holocene index points. Future applications of spatio-temporal statistical techniques are required to better quantify the gradient of the isostatic contribution and to provide improved context for the assessment of 20th century acceleration of Mediterranean sea-level rise.},\\n bibtype = {article},\\n author = {Vacchi, Matteo and Marriner, Nick and Morhange, Christophe and Spada, Giorgio and Fontana, Alessandro and Rovere, Alessio and Marriner, Nick and Morhange, Christophe and Spada, Giorgio and Fontana, Alessandro},\\n doi = {10.1016/j.earscirev.2016.02.002},\\n journal = {Earth Science Reviews}\\n}\",\"author_short\":[\"Vacchi,  M.\",\"Marriner,  N.\",\"Morhange,  C.\",\"Spada,  G.\",\"Fontana,  A.\",\"Rovere,  A.\",\"Marriner,  N.\",\"Morhange,  C.\",\"Spada,  G.\",\"Fontana,  A.\"],\"urls\":{\"Website\":\"http://dx.doi.org/10.1016/j.earscirev.2016.02.002\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"vacchi-marriner-morhange-spada-fontana-rovere-marriner-morhange-etal-multiproxyassessmentofholocenerelativesealevelchangesinthewesternmediterraneanvariabilityinthesealevelhistoriesandredefinitionoftheisostaticsignal-2016\",\"role\":\"author\",\"keyword\":[\"Holocene\",\"Isostatic adjustment\",\"Mediterranean Sea\",\"Sea-level database\",\"Sea-level proxy\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Late holocene sea-level fall and turn-off of reef flat carbonate production: Rethinking bucket fill and coral reef growth models\",\"type\":\"article\",\"year\":\"2015\",\"pages\":\"1-4\",\"volume\":\"43\",\"websites\":\"http://geology.gsapubs.org/cgi/doi/10.1130/G35977.1\",\"month\":\"1\",\"day\":\"7\",\"id\":\"c5ef7744-034e-35cd-a21c-3ccec602d2d1\",\"created\":\"2018-02-03T12:42:07.282Z\",\"accessed\":\"2015-01-14\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:07.282Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Harris2015b\",\"private_publication\":false,\"abstract\":\"Relative sea-level rise has been a major factor driving the evolution of reef systems during the Holocene. Most models of reef evolution suggest that reefs preferentially grow vertically during rising sea level then laterally from windward to leeward, once the reef flat reaches sea level. Continuous lagoonal sedimentation (\\\"bucket fill\\\") and sand apron progradation eventually lead to reef systems with totally filled lagoons. Lagoonal infilling of One Tree Reef (southern Great Barrier Reef) through sand apron accretion was examined in the context of late Holocene relative sea-level change. This analysis was conducted using sedimentological and digital terrain data supported by 50 radiocarbon ages from fossil microatolls, buried patch reefs, foraminifera and shells in sediment cores, and recalibrated previously published radiocarbon ages. This data set challenges the conceptual model of geologically continuous sediment infill during the Holocene through sand apron accretion. Rapid sand apron accretion occurred between 6000 and 3000 calibrated yr before present B.P. (cal. yr B.P.); followed by only small amounts of sedimentation between 3000 cal. yr B.P. and present, with no significant sand apron accretion in the past 2 k.y. This hiatus in sediment infill coincides with a sea-level fall of [~]1-1.3 m during the late Holocene (ca. 2000 cal. yr B.P.), which would have caused the turn-off of highly productive live coral growth on the reef flats currently dominated by less productive rubble and algal flats, resulting in a reduced sediment input to back-reef environments and the cessation in sand apron accretion. Given that relative sea-level variations of [~]1 m were common throughout the Holocene, we suggest that this mode of sand apron development and carbonate production is applicable to most reef systems.\",\"bibtype\":\"article\",\"author\":\"Harris, Daniel L. and Webster, Jody M. and Vila-Concejo, Ana and Hua, Quan and Yokoyama, Yusuke and Reimer, Paula J.\",\"doi\":\"10.1130/G35977.1\",\"journal\":\"Geology\",\"number\":\"2\",\"keywords\":\"SLCC\",\"bibtex\":\"@article{\\n title = {Late holocene sea-level fall and turn-off of reef flat carbonate production: Rethinking bucket fill and coral reef growth models},\\n type = {article},\\n year = {2015},\\n pages = {1-4},\\n volume = {43},\\n websites = {http://geology.gsapubs.org/cgi/doi/10.1130/G35977.1},\\n month = {1},\\n day = {7},\\n id = {c5ef7744-034e-35cd-a21c-3ccec602d2d1},\\n created = {2018-02-03T12:42:07.282Z},\\n accessed = {2015-01-14},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:07.282Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Harris2015b},\\n private_publication = {false},\\n abstract = {Relative sea-level rise has been a major factor driving the evolution of reef systems during the Holocene. Most models of reef evolution suggest that reefs preferentially grow vertically during rising sea level then laterally from windward to leeward, once the reef flat reaches sea level. Continuous lagoonal sedimentation (\\\"bucket fill\\\") and sand apron progradation eventually lead to reef systems with totally filled lagoons. Lagoonal infilling of One Tree Reef (southern Great Barrier Reef) through sand apron accretion was examined in the context of late Holocene relative sea-level change. This analysis was conducted using sedimentological and digital terrain data supported by 50 radiocarbon ages from fossil microatolls, buried patch reefs, foraminifera and shells in sediment cores, and recalibrated previously published radiocarbon ages. This data set challenges the conceptual model of geologically continuous sediment infill during the Holocene through sand apron accretion. Rapid sand apron accretion occurred between 6000 and 3000 calibrated yr before present B.P. (cal. yr B.P.); followed by only small amounts of sedimentation between 3000 cal. yr B.P. and present, with no significant sand apron accretion in the past 2 k.y. This hiatus in sediment infill coincides with a sea-level fall of [~]1-1.3 m during the late Holocene (ca. 2000 cal. yr B.P.), which would have caused the turn-off of highly productive live coral growth on the reef flats currently dominated by less productive rubble and algal flats, resulting in a reduced sediment input to back-reef environments and the cessation in sand apron accretion. Given that relative sea-level variations of [~]1 m were common throughout the Holocene, we suggest that this mode of sand apron development and carbonate production is applicable to most reef systems.},\\n bibtype = {article},\\n author = {Harris, Daniel L. and Webster, Jody M. and Vila-Concejo, Ana and Hua, Quan and Yokoyama, Yusuke and Reimer, Paula J.},\\n doi = {10.1130/G35977.1},\\n journal = {Geology},\\n number = {2},\\n keywords = {SLCC}\\n}\",\"author_short\":[\"Harris,  D., L.\",\"Webster,  J., M.\",\"Vila-Concejo,  A.\",\"Hua,  Q.\",\"Yokoyama,  Y.\",\"Reimer,  P., J.\"],\"urls\":{\"Website\":\"http://geology.gsapubs.org/cgi/doi/10.1130/G35977.1\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"harris-webster-vilaconcejo-hua-yokoyama-reimer-lateholocenesealevelfallandturnoffofreefflatcarbonateproductionrethinkingbucketfillandcoralreefgrowthmodels-2015\",\"role\":\"author\",\"keyword\":[\"SLCC\"],\"metadata\":{\"authorlinks\":{}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Spatial variations in wave transformation and sediment entrainment on a coral reef sand apron\",\"type\":\"article\",\"year\":\"2015\",\"pages\":\"220-229\",\"volume\":\"363\",\"publisher\":\"Elsevier\",\"id\":\"57b0685a-c7b7-348e-834e-0ab865e8b817\",\"created\":\"2018-02-03T12:42:07.347Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:07.347Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"harris2015spatial\",\"source_type\":\"article\",\"private_publication\":false,\"bibtype\":\"article\",\"author\":\"Harris, D L and Vila-Concejo, A and Webster, J M and Power, H E\",\"journal\":\"Marine Geology\",\"bibtex\":\"@article{\\n title = {Spatial variations in wave transformation and sediment entrainment on a coral reef sand apron},\\n type = {article},\\n year = {2015},\\n pages = {220-229},\\n volume = {363},\\n publisher = {Elsevier},\\n id = {57b0685a-c7b7-348e-834e-0ab865e8b817},\\n created = {2018-02-03T12:42:07.347Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:07.347Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {harris2015spatial},\\n source_type = {article},\\n private_publication = {false},\\n bibtype = {article},\\n author = {Harris, D L and Vila-Concejo, A and Webster, J M and Power, H E},\\n journal = {Marine Geology}\\n}\",\"author_short\":[\"Harris,  D., L.\",\"Vila-Concejo,  A.\",\"Webster,  J., M.\",\"Power,  H., E.\"],\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"harris-vilaconcejo-webster-power-spatialvariationsinwavetransformationandsedimententrainmentonacoralreefsandapron-2015\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Influence of hydrodynamic energy on Holocene reef flat accretion, Great Barrier Reef\",\"type\":\"article\",\"year\":\"2016\",\"keywords\":\"Accretion,Great Barrier Reef,Holocene,Reef growth,Sea level,Still-stand\",\"pages\":\"44-53\",\"volume\":\"85\",\"id\":\"80f43001-f620-38f0-834d-7973e06d9e9f\",\"created\":\"2018-02-03T12:42:07.847Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:07.847Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Dechnik2016\",\"private_publication\":false,\"abstract\":\"The response of platform reefs to sea-level stabilization over the past 6 ka is well established for the Great Barrier Reef (GBR), with reefs typically accreting laterally from windward to leeward. However, these observations are based on few cores spread across reef zones and may not accurately reflect a reef's true accretional response to the Holocene stillstand. We present a new record of reef accretion based on 49 U/Th ages from Heron and One Tree reefs in conjunction with re-analyzed data from 14 reefs across the GBR. We demonstrate that hydrodynamic energy is the main driver of accretional direction; exposed reefs accreted primarily lagoon-ward while protected reefs accreted seawards, contrary to the traditional growth model in the GBR. Lateral accretion rates varied from 86.3 m/ka-42.4 m/ka on the exposed One Tree windward reef and 68.35 m/ka-15.7 m/ka on the protected leeward Heron reef, suggesting that wind/wave energy is not a dominant control on lateral accretion rates. This represents the most comprehensive statement of lateral accretion direction and rates from the mid-outer platform reefs of the GBR, confirming great variability in reef flat growth both within and between reef margins over the last 6 ka, and highlighting the need for closely-spaced transects.\",\"bibtype\":\"article\",\"author\":\"Dechnik, Belinda and Webster, Jody M. and Nothdurft, Luke and Webb, Gregory E. and Zhao, Jian xin and Duce, Stephanie and Braga, Juan C. and Harris, Daniel L. and Vila-Concejo, Ana and Puotinen, Marji\",\"doi\":\"10.1016/j.yqres.2015.11.002\",\"journal\":\"Quaternary Research (United States)\",\"number\":\"1\",\"bibtex\":\"@article{\\n title = {Influence of hydrodynamic energy on Holocene reef flat accretion, Great Barrier Reef},\\n type = {article},\\n year = {2016},\\n keywords = {Accretion,Great Barrier Reef,Holocene,Reef growth,Sea level,Still-stand},\\n pages = {44-53},\\n volume = {85},\\n id = {80f43001-f620-38f0-834d-7973e06d9e9f},\\n created = {2018-02-03T12:42:07.847Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:07.847Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Dechnik2016},\\n private_publication = {false},\\n abstract = {The response of platform reefs to sea-level stabilization over the past 6 ka is well established for the Great Barrier Reef (GBR), with reefs typically accreting laterally from windward to leeward. However, these observations are based on few cores spread across reef zones and may not accurately reflect a reef's true accretional response to the Holocene stillstand. We present a new record of reef accretion based on 49 U/Th ages from Heron and One Tree reefs in conjunction with re-analyzed data from 14 reefs across the GBR. We demonstrate that hydrodynamic energy is the main driver of accretional direction; exposed reefs accreted primarily lagoon-ward while protected reefs accreted seawards, contrary to the traditional growth model in the GBR. Lateral accretion rates varied from 86.3 m/ka-42.4 m/ka on the exposed One Tree windward reef and 68.35 m/ka-15.7 m/ka on the protected leeward Heron reef, suggesting that wind/wave energy is not a dominant control on lateral accretion rates. This represents the most comprehensive statement of lateral accretion direction and rates from the mid-outer platform reefs of the GBR, confirming great variability in reef flat growth both within and between reef margins over the last 6 ka, and highlighting the need for closely-spaced transects.},\\n bibtype = {article},\\n author = {Dechnik, Belinda and Webster, Jody M. and Nothdurft, Luke and Webb, Gregory E. and Zhao, Jian xin and Duce, Stephanie and Braga, Juan C. and Harris, Daniel L. and Vila-Concejo, Ana and Puotinen, Marji},\\n doi = {10.1016/j.yqres.2015.11.002},\\n journal = {Quaternary Research (United States)},\\n number = {1}\\n}\",\"author_short\":[\"Dechnik,  B.\",\"Webster,  J., M.\",\"Nothdurft,  L.\",\"Webb,  G., E.\",\"Zhao,  J., x.\",\"Duce,  S.\",\"Braga,  J., C.\",\"Harris,  D., L.\",\"Vila-Concejo,  A.\",\"Puotinen,  M.\"],\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"dechnik-webster-nothdurft-webb-zhao-duce-braga-harris-etal-influenceofhydrodynamicenergyonholocenereefflataccretiongreatbarrierreef-2016\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Accretion\",\"Great Barrier Reef\",\"Holocene\",\"Reef growth\",\"Sea level\",\"Still-stand\"],\"metadata\":{\"authorlinks\":{}},\"downloads\":0,\"html\":\"\"},{\"title\":\"A review of the MIS 5e highstand deposits from Santa Maria Island (Azores, NE Atlantic): Palaeobiodiversity, palaeoecology and palaeobiogeography\",\"type\":\"article\",\"year\":\"2015\",\"keywords\":\"SLCC\",\"pages\":\"126-148\",\"volume\":\"114\",\"id\":\"18675fe6-ef04-3b2a-80ad-0a12239f3f49\",\"created\":\"2018-02-03T12:42:07.872Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.296Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Avila2015\",\"private_publication\":false,\"abstract\":\"The privileged location of Santa Maria Island (Azores archipelago) in the middle of the North Atlantic makes the fossiliferous outcrops on this island of utmost importance to gain a better understanding of how coeval living communities relate to the broader evolutionary and biogeographic history of the Atlantic basin during the late Neogene and the Quaternary. Here we focus on this island's MIS 5e fossil record, offering a comprehensive review on the palaeobiodiversity, palaeoecology and palaeobiogeography of the biota living in the mid North Atlantic during this interglacial. Several studies in oceanic islands stress the huge impact of sea level changes on insular communities. Pleistocene sea-level changes occur during the short-time events known as \\\"Terminations\\\" (associated to glacial/interglacial shifts) as well as with the onset of glaciations (associated to interglacial/glacial shifts). Both are responsible for extinctions and local disappearance of species, bottleneck effects and formation of new species, resulting in community structure changes. This work increases the number of fossil marine taxa reported from the Last Interglacial deposits of Santa Maria to 143 species. All the 19 new records are molluscs (13 gastropods and 6 bivalves), thus increasing the number of fossil molluscs to 136 species. Although thermophilic members of the \\\"Senegalese\\\" tropical fauna were found in these deposits, many of the most emblematic species (e.g., Persististrombus latus (= Strombus bubonius), Cymbula safiana, Harpa doris, Cardita senegalensis, Barbatia plicata, Ctena eburnea or Hyotissa hyotis) are absent, suggesting that they did not reach the Azores. Our results indicate that the main differences between the species composition of the MIS 5e and the present-day shallow-water Azorean communities are probably due to the dropping of sea surface temperature associated with the onset of the last glaciation, which had both direct and indirect effects on species ecology. A group of 21 thermophilic species was directly affected by the lower sea surface temperature, whereas a group of four sand-associated species was indirectly but similarly affected by the lowering of the sea level. Both groups have locally disappeared from the Azores. However, none of the extant endemic species found on the studied MIS 5e outcrops was apparently affected by the lowering SST. In contrast to the biogeographical relationships of the recent Azorean shallow marine molluscs, which are predominantly with the Mediterranean Region, Portugal and with the Madeira and Canary Islands archipelagos, the palaeobiogeographical relationships of the MIS 5e Azorean marine molluscs are mainly with Canaries and West Africa. Despite the general low similarity of the biogeographical relationships between the Azores and Cape Verde Archipelago, on both the recent and the MIS 5e analysis, this similarity is nevertheless higher for the MIS 5e mollusc assemblages, emphasizing the role of Cape Verde as an important source of warm-water species during the Last Interglacial.\",\"bibtype\":\"article\",\"author\":\"Ávila, Sérgio P. and Melo, Carlos and Silva, Luís and Ramalho, Ricardo S. and Quartau, Rui and Hipólito, Ana and Cordeiro, Ricardo and Rebelo, Ana Cristina and Madeira, Patrícia and Rovere, Alessio and Hearty, Paul J. and Henriques, Diamantino and Silva, Carlos Marques da and Martins, António M.de Frias and Zazo, Caridad\",\"doi\":\"10.1016/j.quascirev.2015.02.012\",\"journal\":\"Quaternary Science Reviews\",\"bibtex\":\"@article{\\n title = {A review of the MIS 5e highstand deposits from Santa Maria Island (Azores, NE Atlantic): Palaeobiodiversity, palaeoecology and palaeobiogeography},\\n type = {article},\\n year = {2015},\\n keywords = {SLCC},\\n pages = {126-148},\\n volume = {114},\\n id = {18675fe6-ef04-3b2a-80ad-0a12239f3f49},\\n created = {2018-02-03T12:42:07.872Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.296Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Avila2015},\\n private_publication = {false},\\n abstract = {The privileged location of Santa Maria Island (Azores archipelago) in the middle of the North Atlantic makes the fossiliferous outcrops on this island of utmost importance to gain a better understanding of how coeval living communities relate to the broader evolutionary and biogeographic history of the Atlantic basin during the late Neogene and the Quaternary. Here we focus on this island's MIS 5e fossil record, offering a comprehensive review on the palaeobiodiversity, palaeoecology and palaeobiogeography of the biota living in the mid North Atlantic during this interglacial. Several studies in oceanic islands stress the huge impact of sea level changes on insular communities. Pleistocene sea-level changes occur during the short-time events known as \\\"Terminations\\\" (associated to glacial/interglacial shifts) as well as with the onset of glaciations (associated to interglacial/glacial shifts). Both are responsible for extinctions and local disappearance of species, bottleneck effects and formation of new species, resulting in community structure changes. This work increases the number of fossil marine taxa reported from the Last Interglacial deposits of Santa Maria to 143 species. All the 19 new records are molluscs (13 gastropods and 6 bivalves), thus increasing the number of fossil molluscs to 136 species. Although thermophilic members of the \\\"Senegalese\\\" tropical fauna were found in these deposits, many of the most emblematic species (e.g., Persististrombus latus (= Strombus bubonius), Cymbula safiana, Harpa doris, Cardita senegalensis, Barbatia plicata, Ctena eburnea or Hyotissa hyotis) are absent, suggesting that they did not reach the Azores. Our results indicate that the main differences between the species composition of the MIS 5e and the present-day shallow-water Azorean communities are probably due to the dropping of sea surface temperature associated with the onset of the last glaciation, which had both direct and indirect effects on species ecology. A group of 21 thermophilic species was directly affected by the lower sea surface temperature, whereas a group of four sand-associated species was indirectly but similarly affected by the lowering of the sea level. Both groups have locally disappeared from the Azores. However, none of the extant endemic species found on the studied MIS 5e outcrops was apparently affected by the lowering SST. In contrast to the biogeographical relationships of the recent Azorean shallow marine molluscs, which are predominantly with the Mediterranean Region, Portugal and with the Madeira and Canary Islands archipelagos, the palaeobiogeographical relationships of the MIS 5e Azorean marine molluscs are mainly with Canaries and West Africa. Despite the general low similarity of the biogeographical relationships between the Azores and Cape Verde Archipelago, on both the recent and the MIS 5e analysis, this similarity is nevertheless higher for the MIS 5e mollusc assemblages, emphasizing the role of Cape Verde as an important source of warm-water species during the Last Interglacial.},\\n bibtype = {article},\\n author = {Ávila, Sérgio P. and Melo, Carlos and Silva, Luís and Ramalho, Ricardo S. and Quartau, Rui and Hipólito, Ana and Cordeiro, Ricardo and Rebelo, Ana Cristina and Madeira, Patrícia and Rovere, Alessio and Hearty, Paul J. and Henriques, Diamantino and Silva, Carlos Marques da and Martins, António M.de Frias and Zazo, Caridad},\\n doi = {10.1016/j.quascirev.2015.02.012},\\n journal = {Quaternary Science Reviews}\\n}\",\"author_short\":[\"Ávila,  S., P.\",\"Melo,  C.\",\"Silva,  L.\",\"Ramalho,  R., S.\",\"Quartau,  R.\",\"Hipólito,  A.\",\"Cordeiro,  R.\",\"Rebelo,  A., C.\",\"Madeira,  P.\",\"Rovere,  A.\",\"Hearty,  P., J.\",\"Henriques,  D.\",\"Silva,  C., M., d.\",\"Martins,  A., M., F.\",\"Zazo,  C.\"],\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"vila-melo-silva-ramalho-quartau-hiplito-cordeiro-rebelo-etal-areviewofthemis5ehighstanddepositsfromsantamariaislandazoresneatlanticpalaeobiodiversitypalaeoecologyandpalaeobiogeography-2015\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"SLCC\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Budget of Primary Production and Dinitrogen Fixation in a Highly Seasonal Red Sea Coral Reef\",\"type\":\"article\",\"year\":\"2016\",\"keywords\":\"Biogeochemical cycling,Diazotrophy,Gulf of Aqaba,Nutrient budget,Photosynthesis,Productivity\",\"pages\":\"771-785\",\"volume\":\"19\",\"id\":\"89d9bbe3-e931-365f-9e12-f705ba1067e4\",\"created\":\"2018-02-03T12:42:07.876Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.109Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Cardini\",\"private_publication\":false,\"abstract\":\"Biological dinitrogen (N2) fixation (diazotrophy, BNF) relieves marine primary producers of nitrogen (N) limitation in a large part of the world oceans. N concentrations are particularly low in tropical regions where coral reefs are located, and N is therefore a key limiting nutrient for these productive ecosystems. In this context, the importance of diazotrophy for reef productivity is still not resolved, with studies up to now lacking organismal and seasonal resolution. Here, we present a budget of gross primary production (GPP) and BNF for a highly seasonal Red Sea fringing reef, based on ecophysiological and benthic cover measurements combined with geospatial analyses. Benthic GPP varied from 215 to 262 mmol C m -2 reef d-1, with hard corals making the largest contribution (41-76%). Diazotrophy was omnipresent in space and time, and benthic BNF varied from 0.16 to 0.92 mmol N m-2 reef d-1. Planktonic GPP and BNF rates were respectively approximately 60- and 20-fold lower than those of the benthos, emphasizing the importance of the benthic compartment in reef biogeochemical cycling. BNF showed higher sensitivity to seasonality than GPP, implying greater climatic control on reef BNF. Up to about 20% of net reef primary production could be supported by BNF during summer, suggesting a strong biogeochemical coupling between diazotrophy and the reef carbon cycle. Details\",\"bibtype\":\"article\",\"author\":\"Cardini, Ulisse and Bednarz, Vanessa N. and van Hoytema, Nanne and Rovere, Alessio and Naumann, Malik S. and Al-Rshaidat, Mamoon M.D. and Wild, Christian\",\"doi\":\"10.1007/s10021-016-9966-1\",\"journal\":\"Ecosystems\",\"number\":\"5\",\"bibtex\":\"@article{\\n title = {Budget of Primary Production and Dinitrogen Fixation in a Highly Seasonal Red Sea Coral Reef},\\n type = {article},\\n year = {2016},\\n keywords = {Biogeochemical cycling,Diazotrophy,Gulf of Aqaba,Nutrient budget,Photosynthesis,Productivity},\\n pages = {771-785},\\n volume = {19},\\n id = {89d9bbe3-e931-365f-9e12-f705ba1067e4},\\n created = {2018-02-03T12:42:07.876Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.109Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Cardini},\\n private_publication = {false},\\n abstract = {Biological dinitrogen (N2) fixation (diazotrophy, BNF) relieves marine primary producers of nitrogen (N) limitation in a large part of the world oceans. N concentrations are particularly low in tropical regions where coral reefs are located, and N is therefore a key limiting nutrient for these productive ecosystems. In this context, the importance of diazotrophy for reef productivity is still not resolved, with studies up to now lacking organismal and seasonal resolution. Here, we present a budget of gross primary production (GPP) and BNF for a highly seasonal Red Sea fringing reef, based on ecophysiological and benthic cover measurements combined with geospatial analyses. Benthic GPP varied from 215 to 262 mmol C m -2 reef d-1, with hard corals making the largest contribution (41-76%). Diazotrophy was omnipresent in space and time, and benthic BNF varied from 0.16 to 0.92 mmol N m-2 reef d-1. Planktonic GPP and BNF rates were respectively approximately 60- and 20-fold lower than those of the benthos, emphasizing the importance of the benthic compartment in reef biogeochemical cycling. BNF showed higher sensitivity to seasonality than GPP, implying greater climatic control on reef BNF. Up to about 20% of net reef primary production could be supported by BNF during summer, suggesting a strong biogeochemical coupling between diazotrophy and the reef carbon cycle. Details},\\n bibtype = {article},\\n author = {Cardini, Ulisse and Bednarz, Vanessa N. and van Hoytema, Nanne and Rovere, Alessio and Naumann, Malik S. and Al-Rshaidat, Mamoon M.D. and Wild, Christian},\\n doi = {10.1007/s10021-016-9966-1},\\n journal = {Ecosystems},\\n number = {5}\\n}\",\"author_short\":[\"Cardini,  U.\",\"Bednarz,  V., N.\",\"van Hoytema,  N.\",\"Rovere,  A.\",\"Naumann,  M., S.\",\"Al-Rshaidat,  M., M.\",\"Wild,  C.\"],\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"cardini-bednarz-vanhoytema-rovere-naumann-alrshaidat-wild-budgetofprimaryproductionanddinitrogenfixationinahighlyseasonalredseacoralreef-2016\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"Biogeochemical cycling\",\"Diazotrophy\",\"Gulf of Aqaba\",\"Nutrient budget\",\"Photosynthesis\",\"Productivity\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Late Quaternary sea-level changes and early human societies in the central and eastern Mediterranean Basin: An interdisciplinary review\",\"type\":\"article\",\"year\":\"2017\",\"keywords\":\"Holocene,Mediterranean Archaeology,Pleistocene,Sea-level change\",\"pages\":\"29-57\",\"volume\":\"449\",\"websites\":\"http://linkinghub.elsevier.com/retrieve/pii/S1040618216310928,http://dx.doi.org/10.1016/j.quaint.2017.06.025\",\"publisher\":\"Elsevier Ltd\",\"id\":\"62fca5b4-ded4-330a-a54f-ce02c6217d33\",\"created\":\"2018-02-03T12:42:07.907Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:07.907Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Benjamin2017\",\"private_publication\":false,\"abstract\":\"This article reviews key data and debates focused on relative sea-level changes since the Last Interglacial (approximately the last 132,000 years) in the Mediterranean Basin, and their implications for past human populations. Geological and geomorphological landscape studies are critical to archaeology. Coastal regions provide a wide range of resources to the populations that inhabit them. Coastal landscapes are increasingly the focus of scholarly discussions from the earliest exploitation of littoral resources and early hominin cognition, to the inundation of the earliest permanently settled fishing villages and eventually, formative centres of urbanisation. In the Mediterranean, these would become hubs of maritime transportation that gave rise to the roots of modern seaborne trade. As such, this article represents an original review of both the geo-scientific and archaeological data that specifically relate to sea-level changes and resulting impacts on both physical and cultural landscapes from the Palaeolithic until the emergence of the Classical periods. Our review highlights that the interdisciplinary links between coastal archaeology, geomorphology and sea-level changes are important to explain environmental impacts on coastal human societies and human migration. We review geological indicators of sea level and outline how archaeological features are commonly used as proxies for measuring past sea levels, both gradual changes and catastrophic events. We argue that coastal archaeologists should, as a part of their analyses, incorporate important sea-level concepts, such as indicative meaning. The interpretation of the indicative meaning of Roman fishtanks, for example, plays a critical role in reconstructions of late Holocene Mediterranean sea levels. We identify avenues for future work, which include the consideration of glacial isostatic adjustment (GIA) in addition to coastal tectonics to explain vertical movements of coastlines, more research on Palaeolithic island colonisation, broadening of Palaeolithic studies to include materials from the entire coastal landscape and not just coastal resources, a focus on rescue of archaeological sites under threat by coastal change, and expansion of underwater archaeological explorations in combination with submarine geomorphology. This article presents a collaborative synthesis of data, some of which have been collected and analysed by the authors, as the MEDFLOOD (MEDiterranean sea-level change and projection for future FLOODing) community, and highlights key sites, data, concepts and ongoing debates.\",\"bibtype\":\"article\",\"author\":\"Benjamin, J. and Rovere, A. and Fontana, A. and Furlani, S. and Vacchi, M. and Inglis, R.H. H. and Galili, E. and Antonioli, F. and Sivan, D. and Miko, S. and Mourtzas, N. and Felja, I. and Meredith-Williams, M. and Goodman-Tchernov, B. and Kolaiti, E. and Anzidei, M. and Gehrels, R.\",\"doi\":\"10.1016/j.quaint.2017.06.025\",\"journal\":\"Quaternary International\",\"bibtex\":\"@article{\\n title = {Late Quaternary sea-level changes and early human societies in the central and eastern Mediterranean Basin: An interdisciplinary review},\\n type = {article},\\n year = {2017},\\n keywords = {Holocene,Mediterranean Archaeology,Pleistocene,Sea-level change},\\n pages = {29-57},\\n volume = {449},\\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S1040618216310928,http://dx.doi.org/10.1016/j.quaint.2017.06.025},\\n publisher = {Elsevier Ltd},\\n id = {62fca5b4-ded4-330a-a54f-ce02c6217d33},\\n created = {2018-02-03T12:42:07.907Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:07.907Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Benjamin2017},\\n private_publication = {false},\\n abstract = {This article reviews key data and debates focused on relative sea-level changes since the Last Interglacial (approximately the last 132,000 years) in the Mediterranean Basin, and their implications for past human populations. Geological and geomorphological landscape studies are critical to archaeology. Coastal regions provide a wide range of resources to the populations that inhabit them. Coastal landscapes are increasingly the focus of scholarly discussions from the earliest exploitation of littoral resources and early hominin cognition, to the inundation of the earliest permanently settled fishing villages and eventually, formative centres of urbanisation. In the Mediterranean, these would become hubs of maritime transportation that gave rise to the roots of modern seaborne trade. As such, this article represents an original review of both the geo-scientific and archaeological data that specifically relate to sea-level changes and resulting impacts on both physical and cultural landscapes from the Palaeolithic until the emergence of the Classical periods. Our review highlights that the interdisciplinary links between coastal archaeology, geomorphology and sea-level changes are important to explain environmental impacts on coastal human societies and human migration. We review geological indicators of sea level and outline how archaeological features are commonly used as proxies for measuring past sea levels, both gradual changes and catastrophic events. We argue that coastal archaeologists should, as a part of their analyses, incorporate important sea-level concepts, such as indicative meaning. The interpretation of the indicative meaning of Roman fishtanks, for example, plays a critical role in reconstructions of late Holocene Mediterranean sea levels. We identify avenues for future work, which include the consideration of glacial isostatic adjustment (GIA) in addition to coastal tectonics to explain vertical movements of coastlines, more research on Palaeolithic island colonisation, broadening of Palaeolithic studies to include materials from the entire coastal landscape and not just coastal resources, a focus on rescue of archaeological sites under threat by coastal change, and expansion of underwater archaeological explorations in combination with submarine geomorphology. This article presents a collaborative synthesis of data, some of which have been collected and analysed by the authors, as the MEDFLOOD (MEDiterranean sea-level change and projection for future FLOODing) community, and highlights key sites, data, concepts and ongoing debates.},\\n bibtype = {article},\\n author = {Benjamin, J. and Rovere, A. and Fontana, A. and Furlani, S. and Vacchi, M. and Inglis, R.H. H. and Galili, E. and Antonioli, F. and Sivan, D. and Miko, S. and Mourtzas, N. and Felja, I. and Meredith-Williams, M. and Goodman-Tchernov, B. and Kolaiti, E. and Anzidei, M. and Gehrels, R.},\\n doi = {10.1016/j.quaint.2017.06.025},\\n journal = {Quaternary International}\\n}\",\"author_short\":[\"Benjamin,  J.\",\"Rovere,  A.\",\"Fontana,  A.\",\"Furlani,  S.\",\"Vacchi,  M.\",\"Inglis,  R., H.\",\"Galili,  E.\",\"Antonioli,  F.\",\"Sivan,  D.\",\"Miko,  S.\",\"Mourtzas,  N.\",\"Felja,  I.\",\"Meredith-Williams,  M.\",\"Goodman-Tchernov,  B.\",\"Kolaiti,  E.\",\"Anzidei,  M.\",\"Gehrels,  R.\"],\"urls\":{\"Website\":\"http://linkinghub.elsevier.com/retrieve/pii/S1040618216310928,http://dx.doi.org/10.1016/j.quaint.2017.06.025\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"benjamin-rovere-fontana-furlani-vacchi-inglis-galili-antonioli-etal-latequaternarysealevelchangesandearlyhumansocietiesinthecentralandeasternmediterraneanbasinaninterdisciplinaryreview-2017\",\"role\":\"author\",\"keyword\":[\"Holocene\",\"Mediterranean Archaeology\",\"Pleistocene\",\"Sea-level change\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Giant boulders and Last Interglacial storm intensity in the North Atlantic\",\"type\":\"article\",\"year\":\"2017\",\"keywords\":\"Eemian,Last Interglacial,climate change,extreme waves,superstorms\",\"pages\":\"201712433\",\"volume\":\"114\",\"websites\":\"http://www.ncbi.nlm.nih.gov/pubmed/29087331,http://www.pnas.org/lookup/doi/10.1073/pnas.1712433114\",\"month\":\"10\",\"publisher\":\"National Academy of Sciences\",\"day\":\"30\",\"id\":\"3d249fd7-0f67-34cd-9597-134e27ac4b8c\",\"created\":\"2018-02-03T12:42:07.914Z\",\"accessed\":\"2017-11-10\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:07.914Z\",\"read\":\"true\",\"starred\":\"true\",\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Rovere2017\",\"private_publication\":false,\"abstract\":\"As global climate warms and sea level rises, coastal areas will be subject to more frequent extreme flooding and hurricanes. Geologic evidence for extreme coastal storms during past warm periods has the potential to provide fundamental insights into their future intensity. Recent studies argue that during the Last Interglacial (MIS 5e, ∼128-116 ka) tropical and extratropical North Atlantic cyclones may have been more intense than at present, and may have produced waves larger than those observed historically. Such strong swells are inferred to have created a number of geologic features that can be observed today along the coastlines of Bermuda and the Bahamas. In this paper, we investigate the most iconic among these features: massive boulders atop a cliff in North Eleuthera, Bahamas. We combine geologic field surveys, wave models, and boulder transport equations to test the hypothesis that such boulders must have been emplaced by storms of greater-than-historical intensity. By contrast, our results suggest that with the higher relative sea level (RSL) estimated for the Bahamas during MIS 5e, boulders of this size could have been transported by waves generated by storms of historical intensity. Thus, while the megaboulders of Eleuthera cannot be used as geologic proof for past \\\"superstorms,\\\" they do show that with rising sea levels, cliffs and coastal barriers will be subject to significantly greater erosional energy, even without changes in storm intensity.\",\"bibtype\":\"article\",\"author\":\"Rovere, Alessio and Casella, Elisa and Harris, Daniel L. and Lorscheid, Thomas and Nandasena, Napayalage A. K. and Dyer, Blake and Sandstrom, Michael R. and Stocchi, Paolo and D’Andrea, William J. and Raymo, Maureen E.\",\"doi\":\"10.1073/pnas.1712433114\",\"journal\":\"Proceedings of the National Academy of Sciences\",\"number\":\"46\",\"bibtex\":\"@article{\\n title = {Giant boulders and Last Interglacial storm intensity in the North Atlantic},\\n type = {article},\\n year = {2017},\\n keywords = {Eemian,Last Interglacial,climate change,extreme waves,superstorms},\\n pages = {201712433},\\n volume = {114},\\n websites = {http://www.ncbi.nlm.nih.gov/pubmed/29087331,http://www.pnas.org/lookup/doi/10.1073/pnas.1712433114},\\n month = {10},\\n publisher = {National Academy of Sciences},\\n day = {30},\\n id = {3d249fd7-0f67-34cd-9597-134e27ac4b8c},\\n created = {2018-02-03T12:42:07.914Z},\\n accessed = {2017-11-10},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:07.914Z},\\n read = {true},\\n starred = {true},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Rovere2017},\\n private_publication = {false},\\n abstract = {As global climate warms and sea level rises, coastal areas will be subject to more frequent extreme flooding and hurricanes. Geologic evidence for extreme coastal storms during past warm periods has the potential to provide fundamental insights into their future intensity. Recent studies argue that during the Last Interglacial (MIS 5e, ∼128-116 ka) tropical and extratropical North Atlantic cyclones may have been more intense than at present, and may have produced waves larger than those observed historically. Such strong swells are inferred to have created a number of geologic features that can be observed today along the coastlines of Bermuda and the Bahamas. In this paper, we investigate the most iconic among these features: massive boulders atop a cliff in North Eleuthera, Bahamas. We combine geologic field surveys, wave models, and boulder transport equations to test the hypothesis that such boulders must have been emplaced by storms of greater-than-historical intensity. By contrast, our results suggest that with the higher relative sea level (RSL) estimated for the Bahamas during MIS 5e, boulders of this size could have been transported by waves generated by storms of historical intensity. Thus, while the megaboulders of Eleuthera cannot be used as geologic proof for past \\\"superstorms,\\\" they do show that with rising sea levels, cliffs and coastal barriers will be subject to significantly greater erosional energy, even without changes in storm intensity.},\\n bibtype = {article},\\n author = {Rovere, Alessio and Casella, Elisa and Harris, Daniel L. and Lorscheid, Thomas and Nandasena, Napayalage A. K. and Dyer, Blake and Sandstrom, Michael R. and Stocchi, Paolo and D’Andrea, William J. and Raymo, Maureen E.},\\n doi = {10.1073/pnas.1712433114},\\n journal = {Proceedings of the National Academy of Sciences},\\n number = {46}\\n}\",\"author_short\":[\"Rovere,  A.\",\"Casella,  E.\",\"Harris,  D., L.\",\"Lorscheid,  T.\",\"Nandasena,  N., A., K.\",\"Dyer,  B.\",\"Sandstrom,  M., R.\",\"Stocchi,  P.\",\"D’Andrea,  W., J.\",\"Raymo,  M., E.\"],\"urls\":{\"Website\":\"http://www.ncbi.nlm.nih.gov/pubmed/29087331,http://www.pnas.org/lookup/doi/10.1073/pnas.1712433114\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-giantbouldersandlastinterglacialstormintensityinthenorthatlantic-2017\",\"role\":\"author\",\"keyword\":[\"Eemian\",\"Last Interglacial\",\"climate change\",\"extreme waves\",\"superstorms\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":1,\"html\":\"\"},{\"title\":\"Mapping coral reefs using consumer-grade drones and structure from motion photogrammetry techniques\",\"type\":\"article\",\"year\":\"2017\",\"keywords\":\"Bathymetry from drones,Bathymetry from photogrammetry,Coral reefs,Drone mapping,Structure from motion underwater\",\"pages\":\"269-275\",\"volume\":\"36\",\"websites\":\"http://link.springer.com/10.1007/s00338-016-1522-0\",\"publisher\":\"Springer Berlin Heidelberg\",\"id\":\"014c2903-534c-38d9-8cc6-397276ea0084\",\"created\":\"2018-02-03T12:42:07.996Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:07.996Z\",\"read\":\"true\",\"starred\":\"true\",\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Casella2016\",\"private_publication\":false,\"abstract\":\"We propose a novel technique to measure the small-scale three-dimensional features of a shallow-water coral reef using a small drone equipped with a consumer-grade camera, a handheld GPS and structure from motion (SfM) algorithms. We used a GoPro HERO4 with a modified lens mounted on a DJI Phantom 2 drone (maximum total take-off weight <2 kg) to perform a 10 min flight and collect 306 aerial images with an overlap equal or greater than 90%. We mapped an area of 8380 m2, obtaining as output an ortho-rectified aerial photomosaic and a bathymetric digital elevation model (DEM) with a resolution of 0.78 and 1.56 cm pixel−1, respectively. Through comparison with airborne LiDAR data for the same area, we verified that the location of the ortho-rectified aerial photomosaic is accurate within ~1.4 m. The bathymetric difference between our DEM and the LiDAR dataset is −0.016 ± 0.45 m (1σ). Our results show that it is possible, in conditions of calm waters, low winds and minimal sun glint, to deploy consumer-grade drones as a relatively low-cost and rapid survey technique to produce multispectral and bathymetric data on shallow-water coral reefs. We discuss the utility of such data to monitor temporal changes in topographic complexity of reefs and associated biological processes.\",\"bibtype\":\"article\",\"author\":\"Casella, Elisa and Collin, Antoine and Harris, Daniel and Ferse, Sebastian and Bejarano, Sonia and Parravicini, Valeriano and Hench, James L. and Rovere, Alessio\",\"doi\":\"10.1007/s00338-016-1522-0\",\"journal\":\"Coral Reefs\",\"number\":\"1\",\"bibtex\":\"@article{\\n title = {Mapping coral reefs using consumer-grade drones and structure from motion photogrammetry techniques},\\n type = {article},\\n year = {2017},\\n keywords = {Bathymetry from drones,Bathymetry from photogrammetry,Coral reefs,Drone mapping,Structure from motion underwater},\\n pages = {269-275},\\n volume = {36},\\n websites = {http://link.springer.com/10.1007/s00338-016-1522-0},\\n publisher = {Springer Berlin Heidelberg},\\n id = {014c2903-534c-38d9-8cc6-397276ea0084},\\n created = {2018-02-03T12:42:07.996Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:07.996Z},\\n read = {true},\\n starred = {true},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Casella2016},\\n private_publication = {false},\\n abstract = {We propose a novel technique to measure the small-scale three-dimensional features of a shallow-water coral reef using a small drone equipped with a consumer-grade camera, a handheld GPS and structure from motion (SfM) algorithms. We used a GoPro HERO4 with a modified lens mounted on a DJI Phantom 2 drone (maximum total take-off weight <2 kg) to perform a 10 min flight and collect 306 aerial images with an overlap equal or greater than 90%. We mapped an area of 8380 m2, obtaining as output an ortho-rectified aerial photomosaic and a bathymetric digital elevation model (DEM) with a resolution of 0.78 and 1.56 cm pixel−1, respectively. Through comparison with airborne LiDAR data for the same area, we verified that the location of the ortho-rectified aerial photomosaic is accurate within ~1.4 m. The bathymetric difference between our DEM and the LiDAR dataset is −0.016 ± 0.45 m (1σ). Our results show that it is possible, in conditions of calm waters, low winds and minimal sun glint, to deploy consumer-grade drones as a relatively low-cost and rapid survey technique to produce multispectral and bathymetric data on shallow-water coral reefs. We discuss the utility of such data to monitor temporal changes in topographic complexity of reefs and associated biological processes.},\\n bibtype = {article},\\n author = {Casella, Elisa and Collin, Antoine and Harris, Daniel and Ferse, Sebastian and Bejarano, Sonia and Parravicini, Valeriano and Hench, James L. and Rovere, Alessio},\\n doi = {10.1007/s00338-016-1522-0},\\n journal = {Coral Reefs},\\n number = {1}\\n}\",\"author_short\":[\"Casella,  E.\",\"Collin,  A.\",\"Harris,  D.\",\"Ferse,  S.\",\"Bejarano,  S.\",\"Parravicini,  V.\",\"Hench,  J., L.\",\"Rovere,  A.\"],\"urls\":{\"Website\":\"http://link.springer.com/10.1007/s00338-016-1522-0\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"casella-collin-harris-ferse-bejarano-parravicini-hench-rovere-mappingcoralreefsusingconsumergradedronesandstructurefrommotionphotogrammetrytechniques-2017\",\"role\":\"author\",\"keyword\":[\"Bathymetry from drones\",\"Bathymetry from photogrammetry\",\"Coral reefs\",\"Drone mapping\",\"Structure from motion underwater\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/publications.html\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Tidal notches in Mediterranean Sea: A comprehensive analysis\",\"type\":\"article\",\"year\":\"2015\",\"keywords\":\"MEDFLOOD,SLCC\",\"pages\":\"66-84\",\"volume\":\"119\",\"websites\":\"http://linkinghub.elsevier.com/retrieve/pii/S0277379115001237\",\"id\":\"d4ca0132-0793-3a00-9ab0-363e0f46f1a1\",\"created\":\"2018-02-03T12:42:08.494Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.034Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Antonioli2015\",\"private_publication\":false,\"abstract\":\"Recent works (Evelpidou et al., 2012) suggest that the modern tidal notch is disappearing worldwide due sea level rise over the last century. In order to assess this hypothesis, we measured modern tidal notches in several of sites along the Mediterranean coasts. We report observations on tidal notches cut along carbonate coasts from 73 sites from Italy, France, Croatia, Montenegro, Greece, Malta and Spain, plus additional observations carried outside the Mediterranean. At each site, we measured notch width and depth, and we described the characteristics of the biological rim at the base of the notch. We correlated these parameters with wave energy, tide gauge datasets and rock lithology.Our results suggest that, considering 'the development of tidal notches the consequence of midlittoral bioerosion' (as done in Evelpidou et al., 2012) is a simplification that can lead to misleading results, such as stating that notches are disappearing. Important roles in notch formation can be also played by wave action, rate of karst dissolution, salt weathering and wetting and drying cycles. Of course notch formation can be augmented and favoured also by bioerosion which can, in particular cases, be the main process of notch formation and development.Our dataset shows that notches are carved by an ensemble rather than by a single process, both today and in the past, and that it is difficult, if not impossible, to disentangle them and establish which one is prevailing. We therefore show that tidal notches are still forming, challenging the hypothesis that sea level rise has drowned them.\",\"bibtype\":\"article\",\"author\":\"Antonioli, Fabrizio and Lo Presti, Valeria and Rovere, Alessio and Ferranti, Luigi and Anzidei, Marco and Furlani, Stefano and Mastronuzzi, Giuseppe and Orru, Paolo E. and Scicchitano, Giovanni and Sannino, Gianmaria and Spampinato, Cecilia R. and Pagliarulo, Rossella and Deiana, Giacomo and de Sabata, Eleonora and Sansò, Paolo and Vacchi, Matteo and Vecchio, Antonio\",\"doi\":\"10.1016/j.quascirev.2015.03.016\",\"journal\":\"Quaternary Science Reviews\",\"number\":\"5\",\"bibtex\":\"@article{\\n title = {Tidal notches in Mediterranean Sea: A comprehensive analysis},\\n type = {article},\\n year = {2015},\\n keywords = {MEDFLOOD,SLCC},\\n pages = {66-84},\\n volume = {119},\\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0277379115001237},\\n id = {d4ca0132-0793-3a00-9ab0-363e0f46f1a1},\\n created = {2018-02-03T12:42:08.494Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.034Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Antonioli2015},\\n private_publication = {false},\\n abstract = {Recent works (Evelpidou et al., 2012) suggest that the modern tidal notch is disappearing worldwide due sea level rise over the last century. In order to assess this hypothesis, we measured modern tidal notches in several of sites along the Mediterranean coasts. We report observations on tidal notches cut along carbonate coasts from 73 sites from Italy, France, Croatia, Montenegro, Greece, Malta and Spain, plus additional observations carried outside the Mediterranean. At each site, we measured notch width and depth, and we described the characteristics of the biological rim at the base of the notch. We correlated these parameters with wave energy, tide gauge datasets and rock lithology.Our results suggest that, considering 'the development of tidal notches the consequence of midlittoral bioerosion' (as done in Evelpidou et al., 2012) is a simplification that can lead to misleading results, such as stating that notches are disappearing. Important roles in notch formation can be also played by wave action, rate of karst dissolution, salt weathering and wetting and drying cycles. Of course notch formation can be augmented and favoured also by bioerosion which can, in particular cases, be the main process of notch formation and development.Our dataset shows that notches are carved by an ensemble rather than by a single process, both today and in the past, and that it is difficult, if not impossible, to disentangle them and establish which one is prevailing. We therefore show that tidal notches are still forming, challenging the hypothesis that sea level rise has drowned them.},\\n bibtype = {article},\\n author = {Antonioli, Fabrizio and Lo Presti, Valeria and Rovere, Alessio and Ferranti, Luigi and Anzidei, Marco and Furlani, Stefano and Mastronuzzi, Giuseppe and Orru, Paolo E. and Scicchitano, Giovanni and Sannino, Gianmaria and Spampinato, Cecilia R. and Pagliarulo, Rossella and Deiana, Giacomo and de Sabata, Eleonora and Sansò, Paolo and Vacchi, Matteo and Vecchio, Antonio},\\n doi = {10.1016/j.quascirev.2015.03.016},\\n journal = {Quaternary Science Reviews},\\n number = {5}\\n}\",\"author_short\":[\"Antonioli,  F.\",\"Lo Presti,  V.\",\"Rovere,  A.\",\"Ferranti,  L.\",\"Anzidei,  M.\",\"Furlani,  S.\",\"Mastronuzzi,  G.\",\"Orru,  P., E.\",\"Scicchitano,  G.\",\"Sannino,  G.\",\"Spampinato,  C., R.\",\"Pagliarulo,  R.\",\"Deiana,  G.\",\"de Sabata,  E.\",\"Sansò,  P.\",\"Vacchi,  M.\",\"Vecchio,  A.\"],\"urls\":{\"Website\":\"http://linkinghub.elsevier.com/retrieve/pii/S0277379115001237\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"antonioli-lopresti-rovere-ferranti-anzidei-furlani-mastronuzzi-orru-etal-tidalnotchesinmediterraneanseaacomprehensiveanalysis-2015\",\"role\":\"author\",\"keyword\":[\"MEDFLOOD\",\"SLCC\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Eustatic and Relative Sea Level Changes\",\"type\":\"article\",\"year\":\"2016\",\"keywords\":\"Eustasy,GIA,Isost,Isostasy,Relative sea level,Sea level,Sea level changes,eustasy,gia,isostasy,of the topical collection,on sea level projections,relative sea level,sea level,sea level changes,this article is part\",\"pages\":\"221-231\",\"volume\":\"2\",\"websites\":\"http://link.springer.com/10.1007/s40641-016-0045-7,http://dx.doi.org/10.1007/s40641-016-0045-7\",\"month\":\"12\",\"publisher\":\"Current Climate Change Reports\",\"day\":\"2\",\"id\":\"2e5440fd-63cc-31d6-82b6-b5a3be4b490c\",\"created\":\"2018-02-03T12:42:08.574Z\",\"accessed\":\"2017-04-19\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:08.574Z\",\"read\":\"true\",\"starred\":\"true\",\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Rovere2016\",\"source_type\":\"article\",\"private_publication\":false,\"abstract\":\"Sea level changes can be driven by either variations in the masses or volume of the oceans, or by changes of the land with respect to the sea surface. In the first case, a sea level change is defined `eustatic'; otherwise, it is defined `relative'. Several techniques can be used to observe changes in sea level, from satellite data to tide gauges to geological or archeological proxies. Regardless of the technique used, `eustasy' cannot be measured directly, but only calculated after perturbing factors of different origins are taken into account. In this paper, we review the meaning and main processes that contribute to eustatic and relative sea level changes, and we give an overview of the different techniques used to observe them.\",\"bibtype\":\"article\",\"author\":\"Rovere, Alessio and Stocchi, Paolo and Vacchi, Matteo\",\"doi\":\"10.1007/s40641-016-0045-7\",\"journal\":\"Current Climate Change Reports\",\"number\":\"4\",\"bibtex\":\"@article{\\n title = {Eustatic and Relative Sea Level Changes},\\n type = {article},\\n year = {2016},\\n keywords = {Eustasy,GIA,Isost,Isostasy,Relative sea level,Sea level,Sea level changes,eustasy,gia,isostasy,of the topical collection,on sea level projections,relative sea level,sea level,sea level changes,this article is part},\\n pages = {221-231},\\n volume = {2},\\n websites = {http://link.springer.com/10.1007/s40641-016-0045-7,http://dx.doi.org/10.1007/s40641-016-0045-7},\\n month = {12},\\n publisher = {Current Climate Change Reports},\\n day = {2},\\n id = {2e5440fd-63cc-31d6-82b6-b5a3be4b490c},\\n created = {2018-02-03T12:42:08.574Z},\\n accessed = {2017-04-19},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:08.574Z},\\n read = {true},\\n starred = {true},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Rovere2016},\\n source_type = {article},\\n private_publication = {false},\\n abstract = {Sea level changes can be driven by either variations in the masses or volume of the oceans, or by changes of the land with respect to the sea surface. In the first case, a sea level change is defined `eustatic'; otherwise, it is defined `relative'. Several techniques can be used to observe changes in sea level, from satellite data to tide gauges to geological or archeological proxies. Regardless of the technique used, `eustasy' cannot be measured directly, but only calculated after perturbing factors of different origins are taken into account. In this paper, we review the meaning and main processes that contribute to eustatic and relative sea level changes, and we give an overview of the different techniques used to observe them.},\\n bibtype = {article},\\n author = {Rovere, Alessio and Stocchi, Paolo and Vacchi, Matteo},\\n doi = {10.1007/s40641-016-0045-7},\\n journal = {Current Climate Change Reports},\\n number = {4}\\n}\",\"author_short\":[\"Rovere,  A.\",\"Stocchi,  P.\",\"Vacchi,  M.\"],\"urls\":{\"Website\":\"http://link.springer.com/10.1007/s40641-016-0045-7,http://dx.doi.org/10.1007/s40641-016-0045-7\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"rovere-stocchi-vacchi-eustaticandrelativesealevelchanges-2016\",\"role\":\"author\",\"keyword\":[\"Eustasy\",\"GIA\",\"Isost\",\"Isostasy\",\"Relative sea level\",\"Sea level\",\"Sea level changes\",\"eustasy\",\"gia\",\"isostasy\",\"of the topical collection\",\"on sea level projections\",\"relative sea level\",\"sea level\",\"sea level changes\",\"this article is part\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Ecological Change, Sliding Baselines and the Importance of Historical Data: Lessons from Combing Observational and Quantitative Data on a Temperate Reef Over 70 Years\",\"type\":\"article\",\"year\":\"2015\",\"pages\":\"e0118581\",\"volume\":\"10\",\"websites\":\"http://dx.plos.org/10.1371/journal.pone.0118581\",\"id\":\"8b916ab6-383a-3a2a-9b7b-996ec73ff016\",\"created\":\"2018-02-03T12:42:08.689Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.170Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Gatti2015\",\"private_publication\":false,\"abstract\":\"Understanding the effects of environmental change on ecosystems requires the identifica- tion of baselines that may act as reference conditions. However, the continuous change of these references challenges our ability to define the true natural status of ecosystems. The so-called sliding baseline syndrome can be overcome through the analysis of quantitative time series, which are, however, extremely rare. Here we show how combining historical quantitative data with descriptive ‘naturalistic’ information arranged in a chronological chain allows highlighting long-term trends and can be used to inform present conservation schemes.We analysed the long-term change of a coralligenous reef, a marine habitat en- demic to the Mediterranean Sea. The coralligenous assemblages of Mesco Reef (Ligurian Sea,NWMediterranean) have been studied, although discontinuously, since 1937 thus making available both detailed descriptive information and scanty quantitative data: while the former was useful to understand the natural history of the ecosystem, the analysis of the latter was of paramount importance to provide a formal measure of change over time. Epi- benthic assemblages remained comparatively stable until the 1990s, when species re- placement, invasion by alien algae, and biotic homogenisation occurred within few years, leading to a new and completely different ecosystem state. The shift experienced by the cor- alligenous assemblages of Mesco Reef was probably induced by a combination of seawa- ter warming and local human pressures, the latter mainly resulting in increased water turbidity; in turn, cumulative stress may have favoured the establishment of alien species. This study showed that the combined analysis of quantitative and descriptive historical data represent a precious knowledge to understand ecosystem trends over time and provide help to identify baselines for ecological management.\",\"bibtype\":\"article\",\"author\":\"Gatti, Giulia and Bianchi, Carlo Nike and Parravicini, Valeriano and Rovere, Alessio and Peirano, Andrea and Montefalcone, Monica and Massa, Francesco and Morri, Carla\",\"doi\":\"10.1371/journal.pone.0118581\",\"journal\":\"Plos One\",\"keywords\":\"SLCC\",\"bibtex\":\"@article{\\n title = {Ecological Change, Sliding Baselines and the Importance of Historical Data: Lessons from Combing Observational and Quantitative Data on a Temperate Reef Over 70 Years},\\n type = {article},\\n year = {2015},\\n pages = {e0118581},\\n volume = {10},\\n websites = {http://dx.plos.org/10.1371/journal.pone.0118581},\\n id = {8b916ab6-383a-3a2a-9b7b-996ec73ff016},\\n created = {2018-02-03T12:42:08.689Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.170Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Gatti2015},\\n private_publication = {false},\\n abstract = {Understanding the effects of environmental change on ecosystems requires the identifica- tion of baselines that may act as reference conditions. However, the continuous change of these references challenges our ability to define the true natural status of ecosystems. The so-called sliding baseline syndrome can be overcome through the analysis of quantitative time series, which are, however, extremely rare. Here we show how combining historical quantitative data with descriptive ‘naturalistic’ information arranged in a chronological chain allows highlighting long-term trends and can be used to inform present conservation schemes.We analysed the long-term change of a coralligenous reef, a marine habitat en- demic to the Mediterranean Sea. The coralligenous assemblages of Mesco Reef (Ligurian Sea,NWMediterranean) have been studied, although discontinuously, since 1937 thus making available both detailed descriptive information and scanty quantitative data: while the former was useful to understand the natural history of the ecosystem, the analysis of the latter was of paramount importance to provide a formal measure of change over time. Epi- benthic assemblages remained comparatively stable until the 1990s, when species re- placement, invasion by alien algae, and biotic homogenisation occurred within few years, leading to a new and completely different ecosystem state. The shift experienced by the cor- alligenous assemblages of Mesco Reef was probably induced by a combination of seawa- ter warming and local human pressures, the latter mainly resulting in increased water turbidity; in turn, cumulative stress may have favoured the establishment of alien species. This study showed that the combined analysis of quantitative and descriptive historical data represent a precious knowledge to understand ecosystem trends over time and provide help to identify baselines for ecological management.},\\n bibtype = {article},\\n author = {Gatti, Giulia and Bianchi, Carlo Nike and Parravicini, Valeriano and Rovere, Alessio and Peirano, Andrea and Montefalcone, Monica and Massa, Francesco and Morri, Carla},\\n doi = {10.1371/journal.pone.0118581},\\n journal = {Plos One},\\n keywords = {SLCC}\\n}\",\"author_short\":[\"Gatti,  G.\",\"Bianchi,  C., N.\",\"Parravicini,  V.\",\"Rovere,  A.\",\"Peirano,  A.\",\"Montefalcone,  M.\",\"Massa,  F.\",\"Morri,  C.\"],\"urls\":{\"Website\":\"http://dx.plos.org/10.1371/journal.pone.0118581\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"gatti-bianchi-parravicini-rovere-peirano-montefalcone-massa-morri-ecologicalchangeslidingbaselinesandtheimportanceofhistoricaldatalessonsfromcombingobservationalandquantitativedataonatemperatereefover70years-2015\",\"role\":\"author\",\"keyword\":[\"SLCC\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Mid-Pliocene shorelines of the US Atlantic Coastal Plain — An improved elevation database with comparison to Earth model predictions\",\"type\":\"article\",\"year\":\"2015\",\"keywords\":\"MEDFLOOD,PLIOMAX,SLCC\",\"pages\":\"117-131\",\"volume\":\"145\",\"websites\":\"http://linkinghub.elsevier.com/retrieve/pii/S0012825215000355,http://www.scopus.com/inward/record.url?eid=2-s2.0-84926164528&partnerID=tZOtx3y1\",\"publisher\":\"Elsevier B.V.\",\"id\":\"7c02f629-e8ca-3a22-9339-70cd0d5fd1b8\",\"created\":\"2018-02-03T12:42:08.744Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.267Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Rovere2015\",\"private_publication\":false,\"abstract\":\"For nearly a century, the Atlantic Coastal Plain (ACP) of the United States has been the focus of studies investigating Pliocene and Pleistocene shorelines, however, the mapping of paleoshorelines was primarily done by using elevation contours on topographic maps. Here we review published geologic maps and compare them to paleoshoreline locations obtained through geomorphometric classification and satellite data. We furthermore present the results of an extensive field campaign that measured the mid-Pliocene (~. 3.3-2.9. Ma) shorelines of the Atlantic Coastal Plain using high-accuracy GPS and digital elevation models. We compare our new dataset to positions and elevations extracted from published maps and find that the extracted site information from earlier studies is prone to significant error, both in the location and, more severely, in the elevation of the paleoshoreline. We also investigate, using geophysical modeling, the origin of post-depositional displacement of the shoreline from Georgia to Virginia. In particular, we correct the elevation of our shoreline for glacial isostatic adjustment (GIA) and then compare the corrected elevation to predictions of mantle flow-induced dynamic topography (DT). While a subset of these models does reconcile the general trends in the observed elevation of the mid-Pliocene shoreline, local discrepancies persist. These discrepancies suggests that either (i) the DT and GIA models presented here do not capture the full range of uncertainty in the input parameters; and/or (ii) other influences, such as sediment loading and unloading or local fault-driven tectonics, may have contributed to post-depositional deformation of the mid-Pliocene shoreline that are not captured in the above models. In this context, our field measurements represent an important observational dataset with which to compare future generations of geodynamic models. Improvements in models for DT, GIA and other relevant processes, together with an expanded, geographically distributed set of shoreline records, will ultimately be the key to obtaining more accurate estimates of eustatic sea level not only in the mid-Pliocene but also earlier in the Cenozoic.\",\"bibtype\":\"article\",\"author\":\"Rovere, Alessio and Hearty, P.J. and Austermann, J. and Mitrovica, J.X. and Gale, J. and Moucha, R. and Forte, A.M. and Raymo, M.E.\",\"doi\":\"10.1016/j.earscirev.2015.02.007\",\"journal\":\"Earth-Science Reviews\",\"bibtex\":\"@article{\\n title = {Mid-Pliocene shorelines of the US Atlantic Coastal Plain — An improved elevation database with comparison to Earth model predictions},\\n type = {article},\\n year = {2015},\\n keywords = {MEDFLOOD,PLIOMAX,SLCC},\\n pages = {117-131},\\n volume = {145},\\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0012825215000355,http://www.scopus.com/inward/record.url?eid=2-s2.0-84926164528&partnerID=tZOtx3y1},\\n publisher = {Elsevier B.V.},\\n id = {7c02f629-e8ca-3a22-9339-70cd0d5fd1b8},\\n created = {2018-02-03T12:42:08.744Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.267Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Rovere2015},\\n private_publication = {false},\\n abstract = {For nearly a century, the Atlantic Coastal Plain (ACP) of the United States has been the focus of studies investigating Pliocene and Pleistocene shorelines, however, the mapping of paleoshorelines was primarily done by using elevation contours on topographic maps. Here we review published geologic maps and compare them to paleoshoreline locations obtained through geomorphometric classification and satellite data. We furthermore present the results of an extensive field campaign that measured the mid-Pliocene (~. 3.3-2.9. Ma) shorelines of the Atlantic Coastal Plain using high-accuracy GPS and digital elevation models. We compare our new dataset to positions and elevations extracted from published maps and find that the extracted site information from earlier studies is prone to significant error, both in the location and, more severely, in the elevation of the paleoshoreline. We also investigate, using geophysical modeling, the origin of post-depositional displacement of the shoreline from Georgia to Virginia. In particular, we correct the elevation of our shoreline for glacial isostatic adjustment (GIA) and then compare the corrected elevation to predictions of mantle flow-induced dynamic topography (DT). While a subset of these models does reconcile the general trends in the observed elevation of the mid-Pliocene shoreline, local discrepancies persist. These discrepancies suggests that either (i) the DT and GIA models presented here do not capture the full range of uncertainty in the input parameters; and/or (ii) other influences, such as sediment loading and unloading or local fault-driven tectonics, may have contributed to post-depositional deformation of the mid-Pliocene shoreline that are not captured in the above models. In this context, our field measurements represent an important observational dataset with which to compare future generations of geodynamic models. Improvements in models for DT, GIA and other relevant processes, together with an expanded, geographically distributed set of shoreline records, will ultimately be the key to obtaining more accurate estimates of eustatic sea level not only in the mid-Pliocene but also earlier in the Cenozoic.},\\n bibtype = {article},\\n author = {Rovere, Alessio and Hearty, P.J. and Austermann, J. and Mitrovica, J.X. and Gale, J. and Moucha, R. and Forte, A.M. and Raymo, M.E.},\\n doi = {10.1016/j.earscirev.2015.02.007},\\n journal = {Earth-Science Reviews}\\n}\",\"author_short\":[\"Rovere,  A.\",\"Hearty,  P.\",\"Austermann,  J.\",\"Mitrovica,  J.\",\"Gale,  J.\",\"Moucha,  R.\",\"Forte,  A.\",\"Raymo,  M.\"],\"urls\":{\"Website\":\"http://linkinghub.elsevier.com/retrieve/pii/S0012825215000355,http://www.scopus.com/inward/record.url?eid=2-s2.0-84926164528&partnerID=tZOtx3y1\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"rovere-hearty-austermann-mitrovica-gale-moucha-forte-raymo-midplioceneshorelinesoftheusatlanticcoastalplainanimprovedelevationdatabasewithcomparisontoearthmodelpredictions-2015\",\"role\":\"author\",\"keyword\":[\"MEDFLOOD\",\"PLIOMAX\",\"SLCC\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"The magnitude of a mid-Holocene sea-level highstand in the Strait of Makassar\",\"type\":\"article\",\"year\":\"2016\",\"keywords\":\"Glacial isostatic adjustment,Indo-Pacific,Spermonde Shelf,Sulawesi\",\"pages\":\"155-163\",\"volume\":\"257\",\"websites\":\"http://www.sciencedirect.com/science/article/pii/S0169555X15302427,http://dx.doi.org/10.1016/j.geomorph.2015.12.023\",\"publisher\":\"Elsevier B.V.\",\"id\":\"9954079d-a126-3204-9852-4918ab7f9b80\",\"created\":\"2018-02-03T12:42:08.888Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:08.888Z\",\"read\":\"true\",\"starred\":\"true\",\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"mann2015magnitude\",\"source_type\":\"article\",\"private_publication\":false,\"abstract\":\"Knowledge on the timing and magnitude of past sea-level changes is essential to understand modern and future sea-level variability. Holocene sea-level data from literature on the west coast of Sulawesi, central Indonesia, suggest that this region experienced two relative sea-level highstands over the last 6000years, with magnitudes exceeding two meters. However, recent datasets from the Indo-Pacific region do not support high-magnitude sea-level oscillations during the Holocene in tectonically stable far-field locations. Here we present a new, high-precision, mid-Holocene sea-level dataset from the Spermonde Shelf off southwest Sulawesi. We surveyed 21 fossil microatolls on the reef flats of two coral islands (Pulau Panambungan and Pulau Barrang Lompo) and referred their elevations to local mean sea level and to the height of living coral. Radiometrically calibrated ages from emergent fossil microatolls on Pulau Panambungan indicate a relative sea-level highstand not exceeding 0.5m above present at ca. 5600cal.yrBP. The highstand is followed by a relatively rapid sea-level fall towards present sea level that was reached at around 4000cal.yrBP. Fossil microatolls from nearby Pulau Barrang Lompo show the same trend, however with a coherent negative vertical offset of about 0.8m compared to their equivalents on Pulau Panambungan. The largely consistent gradients of both trends (~−0.14mmyr−1), the consistent elevation of living microatolls in the Spermonde, and a number of instructive geomorphic features indicate a localized, post-formational and probably recent drop of the fossil microatolls on the densely populated island Pulau Barrang Lompo. The relative sea-level trend inferred from Pulau Panambungan is well within the range of geophysical predictions based on ANICE-SELEN ice sheet model, which predict a highstand that is significantly lower than those predicted by other GIA models for this area. Although a complete interpretation of the Holocene sea-level history will require additional high-resolution datasets from this and surrounding territories in SE Asia, our results suggest that there was merely a single Holocene highstand in central Indonesia, the magnitude of which was substantially lower than hitherto assumed.\",\"bibtype\":\"article\",\"author\":\"Mann, Thomas and Rovere, Alessio and Schöne, Tilo and Klicpera, André and Stocchi, Paolo and Lukman, Muhammad and Westphal, Hildegard\",\"doi\":\"10.1016/j.geomorph.2015.12.023\",\"journal\":\"Geomorphology\",\"bibtex\":\"@article{\\n title = {The magnitude of a mid-Holocene sea-level highstand in the Strait of Makassar},\\n type = {article},\\n year = {2016},\\n keywords = {Glacial isostatic adjustment,Indo-Pacific,Spermonde Shelf,Sulawesi},\\n pages = {155-163},\\n volume = {257},\\n websites = {http://www.sciencedirect.com/science/article/pii/S0169555X15302427,http://dx.doi.org/10.1016/j.geomorph.2015.12.023},\\n publisher = {Elsevier B.V.},\\n id = {9954079d-a126-3204-9852-4918ab7f9b80},\\n created = {2018-02-03T12:42:08.888Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:08.888Z},\\n read = {true},\\n starred = {true},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {mann2015magnitude},\\n source_type = {article},\\n private_publication = {false},\\n abstract = {Knowledge on the timing and magnitude of past sea-level changes is essential to understand modern and future sea-level variability. Holocene sea-level data from literature on the west coast of Sulawesi, central Indonesia, suggest that this region experienced two relative sea-level highstands over the last 6000years, with magnitudes exceeding two meters. However, recent datasets from the Indo-Pacific region do not support high-magnitude sea-level oscillations during the Holocene in tectonically stable far-field locations. Here we present a new, high-precision, mid-Holocene sea-level dataset from the Spermonde Shelf off southwest Sulawesi. We surveyed 21 fossil microatolls on the reef flats of two coral islands (Pulau Panambungan and Pulau Barrang Lompo) and referred their elevations to local mean sea level and to the height of living coral. Radiometrically calibrated ages from emergent fossil microatolls on Pulau Panambungan indicate a relative sea-level highstand not exceeding 0.5m above present at ca. 5600cal.yrBP. The highstand is followed by a relatively rapid sea-level fall towards present sea level that was reached at around 4000cal.yrBP. Fossil microatolls from nearby Pulau Barrang Lompo show the same trend, however with a coherent negative vertical offset of about 0.8m compared to their equivalents on Pulau Panambungan. The largely consistent gradients of both trends (~−0.14mmyr−1), the consistent elevation of living microatolls in the Spermonde, and a number of instructive geomorphic features indicate a localized, post-formational and probably recent drop of the fossil microatolls on the densely populated island Pulau Barrang Lompo. The relative sea-level trend inferred from Pulau Panambungan is well within the range of geophysical predictions based on ANICE-SELEN ice sheet model, which predict a highstand that is significantly lower than those predicted by other GIA models for this area. Although a complete interpretation of the Holocene sea-level history will require additional high-resolution datasets from this and surrounding territories in SE Asia, our results suggest that there was merely a single Holocene highstand in central Indonesia, the magnitude of which was substantially lower than hitherto assumed.},\\n bibtype = {article},\\n author = {Mann, Thomas and Rovere, Alessio and Schöne, Tilo and Klicpera, André and Stocchi, Paolo and Lukman, Muhammad and Westphal, Hildegard},\\n doi = {10.1016/j.geomorph.2015.12.023},\\n journal = {Geomorphology}\\n}\",\"author_short\":[\"Mann,  T.\",\"Rovere,  A.\",\"Schöne,  T.\",\"Klicpera,  A.\",\"Stocchi,  P.\",\"Lukman,  M.\",\"Westphal,  H.\"],\"urls\":{\"Website\":\"http://www.sciencedirect.com/science/article/pii/S0169555X15302427,http://dx.doi.org/10.1016/j.geomorph.2015.12.023\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"mann-rovere-schne-klicpera-stocchi-lukman-westphal-themagnitudeofamidholocenesealevelhighstandinthestraitofmakassar-2016\",\"role\":\"author\",\"keyword\":[\"Glacial isostatic adjustment\",\"Indo-Pacific\",\"Spermonde Shelf\",\"Sulawesi\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Palaeo-sea-level and palaeo-ice-sheet databases: problems, strategies, and perspectives\",\"type\":\"article\",\"year\":\"2016\",\"pages\":\"911-921\",\"volume\":\"12\",\"websites\":\"http://www.clim-past.net/12/911/2016/\",\"id\":\"8ca5dd97-7c80-38c9-a445-f8daef1ce5b3\",\"created\":\"2018-02-03T12:42:08.890Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:08.890Z\",\"read\":\"true\",\"starred\":\"true\",\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Dusterhus2016\",\"private_publication\":false,\"abstract\":\"<p>Sea-level and ice-sheet databases have driven numerous advances in understanding the Earth system. We describe the challenges and offer best strategies that can be adopted to build self-consistent and standardised databases of geological and geochemical information used to archive palaeo-sea-levels and palaeo-ice-sheets. There are three phases in the development of a database: (i) measurement, (ii) interpretation, and (iii) database creation. Measurement should include the objective description of the position and age of a sample, description of associated geological features, and quantification of uncertainties. Interpretation of the sample may have a subjective component, but it should always include uncertainties and alternative or contrasting interpretations, with any exclusion of existing interpretations requiring a full justification. During the creation of a database, an approach based on accessibility, transparency, trust, availability, continuity, completeness, and communication of content (ATTAC<sup>3</sup>) must be adopted. It is essential to consider the community that creates and benefits from a database. We conclude that funding agencies should not only consider the creation of original data in specific research-question-oriented projects, but also include the possibility of using part of the funding for IT-related and database creation tasks, which are essential to guarantee accessibility and maintenance of the collected data.</p>\",\"bibtype\":\"article\",\"author\":\"Düsterhus, André and Rovere, Alessio and Carlson, Anders E. and Horton, Benjamin P. and Klemann, Volker and Tarasov, Lev and Barlow, Natasha L. M. and Bradwell, Tom and Clark, Jorie and Dutton, Andrea and Gehrels, W. Roland and Hibbert, Fiona D. and Hijma, Marc P. and Khan, Nicole and Kopp, Robert E. and Sivan, Dorit and Törnqvist, Torbjörn E.\",\"doi\":\"10.5194/cp-12-911-2016\",\"journal\":\"Climate of the Past\",\"number\":\"4\",\"bibtex\":\"@article{\\n title = {Palaeo-sea-level and palaeo-ice-sheet databases: problems, strategies, and perspectives},\\n type = {article},\\n year = {2016},\\n pages = {911-921},\\n volume = {12},\\n websites = {http://www.clim-past.net/12/911/2016/},\\n id = {8ca5dd97-7c80-38c9-a445-f8daef1ce5b3},\\n created = {2018-02-03T12:42:08.890Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:08.890Z},\\n read = {true},\\n starred = {true},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Dusterhus2016},\\n private_publication = {false},\\n abstract = {<p>Sea-level and ice-sheet databases have driven numerous advances in understanding the Earth system. We describe the challenges and offer best strategies that can be adopted to build self-consistent and standardised databases of geological and geochemical information used to archive palaeo-sea-levels and palaeo-ice-sheets. There are three phases in the development of a database: (i) measurement, (ii) interpretation, and (iii) database creation. Measurement should include the objective description of the position and age of a sample, description of associated geological features, and quantification of uncertainties. Interpretation of the sample may have a subjective component, but it should always include uncertainties and alternative or contrasting interpretations, with any exclusion of existing interpretations requiring a full justification. During the creation of a database, an approach based on accessibility, transparency, trust, availability, continuity, completeness, and communication of content (ATTAC<sup>3</sup>) must be adopted. It is essential to consider the community that creates and benefits from a database. We conclude that funding agencies should not only consider the creation of original data in specific research-question-oriented projects, but also include the possibility of using part of the funding for IT-related and database creation tasks, which are essential to guarantee accessibility and maintenance of the collected data.</p>},\\n bibtype = {article},\\n author = {Düsterhus, André and Rovere, Alessio and Carlson, Anders E. and Horton, Benjamin P. and Klemann, Volker and Tarasov, Lev and Barlow, Natasha L. M. and Bradwell, Tom and Clark, Jorie and Dutton, Andrea and Gehrels, W. Roland and Hibbert, Fiona D. and Hijma, Marc P. and Khan, Nicole and Kopp, Robert E. and Sivan, Dorit and Törnqvist, Torbjörn E.},\\n doi = {10.5194/cp-12-911-2016},\\n journal = {Climate of the Past},\\n number = {4}\\n}\",\"author_short\":[\"Düsterhus,  A.\",\"Rovere,  A.\",\"Carlson,  A., E.\",\"Horton,  B., P.\",\"Klemann,  V.\",\"Tarasov,  L.\",\"Barlow,  N., L., M.\",\"Bradwell,  T.\",\"Clark,  J.\",\"Dutton,  A.\",\"Gehrels,  W., R.\",\"Hibbert,  F., D.\",\"Hijma,  M., P.\",\"Khan,  N.\",\"Kopp,  R., E.\",\"Sivan,  D.\",\"Törnqvist,  T., E.\"],\"urls\":{\"Website\":\"http://www.clim-past.net/12/911/2016/\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"dsterhus-rovere-carlson-horton-klemann-tarasov-barlow-bradwell-etal-palaeosealevelandpalaeoicesheetdatabasesproblemsstrategiesandperspectives-2016\",\"role\":\"author\",\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/publications.html\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Drones as tools for monitoring beach topography changes in the Ligurian Sea (NW Mediterranean)\",\"type\":\"article\",\"year\":\"2016\",\"pages\":\"151-163\",\"volume\":\"36\",\"id\":\"78f98a9b-44aa-3790-8deb-9be500fd712d\",\"created\":\"2018-02-03T12:42:08.968Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:08.968Z\",\"read\":\"true\",\"starred\":\"true\",\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Casella\",\"private_publication\":false,\"abstract\":\"The aim of this study was to evaluate topographic changes along a stretch of coastline in the Municipality of Borghetto Santo Spirito (Region of Liguria, Italy, north-western Mediterranean) by means of a remotely piloted aircraft system coupled with structure from motion and multi-view stereo techniques. This sector was surveyed three times over 5 months in the fall–winter of 2013–2014 (1 November 2013, 4 December 2013, 17 March 2014) to obtain digital elevation models and orthophotos of the beach. Changes in beach topography associated with storm action and human activities were assessed in terms of gain/loss of sediments and shifting of the wet–dry boundary defining the shoreline. Between the first and second surveys, the study area was hit by two storms (10–11 November 2013 and 21–22 November 2013) with waves approaching from the E–NNE, causing a shoreline retreat which, in some sectors, reached 7 m. Between the second and third surveys, by contrast, four storms (25–27 December 2013, 5–6 January 2014, 17–18 January 2014 and 6–10 February 2014) with waves propagating from the SE produced a general advancement of the shoreline (up to ~5 m) by deposition of sediments along some parts of the beach. The data also reflect changes in beach topography due to human activity during the 2013 fall season, when private beach managers quarried ~178 m3 of sediments on the emerged beach near the shoreline to accumulate them landwards. The results show that drones can be used for regular beach monitoring activities, and that they can provide new insights into the processes related to natural and/or human-related topographic beach changes.\",\"bibtype\":\"article\",\"author\":\"Casella, Elisa and Rovere, Alessio and Pedroncini, Andrea and Stark, Colin P. and Casella, Marco and Ferrari, Marco and Firpo, Marco\",\"doi\":\"10.1007/s00367-016-0435-9\",\"journal\":\"Geo-Marine Letters\",\"number\":\"2\",\"bibtex\":\"@article{\\n title = {Drones as tools for monitoring beach topography changes in the Ligurian Sea (NW Mediterranean)},\\n type = {article},\\n year = {2016},\\n pages = {151-163},\\n volume = {36},\\n id = {78f98a9b-44aa-3790-8deb-9be500fd712d},\\n created = {2018-02-03T12:42:08.968Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:08.968Z},\\n read = {true},\\n starred = {true},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Casella},\\n private_publication = {false},\\n abstract = {The aim of this study was to evaluate topographic changes along a stretch of coastline in the Municipality of Borghetto Santo Spirito (Region of Liguria, Italy, north-western Mediterranean) by means of a remotely piloted aircraft system coupled with structure from motion and multi-view stereo techniques. This sector was surveyed three times over 5 months in the fall–winter of 2013–2014 (1 November 2013, 4 December 2013, 17 March 2014) to obtain digital elevation models and orthophotos of the beach. Changes in beach topography associated with storm action and human activities were assessed in terms of gain/loss of sediments and shifting of the wet–dry boundary defining the shoreline. Between the first and second surveys, the study area was hit by two storms (10–11 November 2013 and 21–22 November 2013) with waves approaching from the E–NNE, causing a shoreline retreat which, in some sectors, reached 7 m. Between the second and third surveys, by contrast, four storms (25–27 December 2013, 5–6 January 2014, 17–18 January 2014 and 6–10 February 2014) with waves propagating from the SE produced a general advancement of the shoreline (up to ~5 m) by deposition of sediments along some parts of the beach. The data also reflect changes in beach topography due to human activity during the 2013 fall season, when private beach managers quarried ~178 m3 of sediments on the emerged beach near the shoreline to accumulate them landwards. The results show that drones can be used for regular beach monitoring activities, and that they can provide new insights into the processes related to natural and/or human-related topographic beach changes.},\\n bibtype = {article},\\n author = {Casella, Elisa and Rovere, Alessio and Pedroncini, Andrea and Stark, Colin P. and Casella, Marco and Ferrari, Marco and Firpo, Marco},\\n doi = {10.1007/s00367-016-0435-9},\\n journal = {Geo-Marine Letters},\\n number = {2}\\n}\",\"author_short\":[\"Casella,  E.\",\"Rovere,  A.\",\"Pedroncini,  A.\",\"Stark,  C., P.\",\"Casella,  M.\",\"Ferrari,  M.\",\"Firpo,  M.\"],\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"casella-rovere-pedroncini-stark-casella-ferrari-firpo-dronesastoolsformonitoringbeachtopographychangesintheligurianseanwmediterranean-2016\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"The analysis of Last Interglacial (MIS 5e) relative sea-level indicators: Reconstructing sea-level in a warmer world\",\"type\":\"misc\",\"year\":\"2016\",\"source\":\"Earth-Science Reviews\",\"keywords\":\"Ice sheets,Last Interglacial,MIS 5e,Paleo sea-level,Past sea-level changes,Sea-level marker,Sea-level reconstruction\",\"pages\":\"404-427\",\"volume\":\"159\",\"websites\":\"http://linkinghub.elsevier.com/retrieve/pii/S0012825216301246\",\"publisher\":\"Elsevier B.V.\",\"id\":\"6e31994f-6e2d-3da3-af0c-a536ee2529a2\",\"created\":\"2018-02-03T12:42:09.044Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:09.044Z\",\"read\":\"true\",\"starred\":\"true\",\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Rovere2016a\",\"private_publication\":false,\"abstract\":\"The Last Interglacial (MIS 5e, 128–116 ka) is among the most studied past periods in Earth's history. The climate at that time was warmer than today, primarily due to different orbital conditions, with smaller ice sheets and higher sea-level. Field evidence for MIS 5e sea-level was reported from thousands of sites, but often paleo shorelines were measured with low-accuracy techniques and, in some cases, there are contrasting interpretations about paleo sea-level reconstructions. For this reason, large uncertainties still surround both the maximum sea-level attained as well as the pattern of sea-level change throughout MIS 5e. Such uncertainties are exacerbated by the lack of a uniform approach to measuring and interpreting the geological evidence of paleo sea-levels. In this review, we discuss the characteristics of MIS 5e field observations, and we set the basis for a standardized approach to MIS 5e paleo sea-level reconstructions, that is already successfully applied in Holocene sea-level research. Application of the standard definitions and methodologies described in this paper will enhance our ability to compare data from different research groups and different areas, in order to gain deeper insights into MIS 5e sea-level changes. Improving estimates of Last Interglacial sea-level is, in turn, a key to understanding the behavior of ice sheets in a warmer world.\",\"bibtype\":\"misc\",\"author\":\"Rovere, Alessio and Raymo, M.E. Maureen E. and Vacchi, Matteo and Lorscheid, Thomas and Stocchi, Paolo and Gómez-Pujol, Lluís and Harris, Daniel L. D.L. and Casella, Elisa and O'Leary, M.J. Michael J. and Hearty, P.J. Paul J.\",\"doi\":\"10.1016/j.earscirev.2016.06.006\",\"bibtex\":\"@misc{\\n title = {The analysis of Last Interglacial (MIS 5e) relative sea-level indicators: Reconstructing sea-level in a warmer world},\\n type = {misc},\\n year = {2016},\\n source = {Earth-Science Reviews},\\n keywords = {Ice sheets,Last Interglacial,MIS 5e,Paleo sea-level,Past sea-level changes,Sea-level marker,Sea-level reconstruction},\\n pages = {404-427},\\n volume = {159},\\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0012825216301246},\\n publisher = {Elsevier B.V.},\\n id = {6e31994f-6e2d-3da3-af0c-a536ee2529a2},\\n created = {2018-02-03T12:42:09.044Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:09.044Z},\\n read = {true},\\n starred = {true},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Rovere2016a},\\n private_publication = {false},\\n abstract = {The Last Interglacial (MIS 5e, 128–116 ka) is among the most studied past periods in Earth's history. The climate at that time was warmer than today, primarily due to different orbital conditions, with smaller ice sheets and higher sea-level. Field evidence for MIS 5e sea-level was reported from thousands of sites, but often paleo shorelines were measured with low-accuracy techniques and, in some cases, there are contrasting interpretations about paleo sea-level reconstructions. For this reason, large uncertainties still surround both the maximum sea-level attained as well as the pattern of sea-level change throughout MIS 5e. Such uncertainties are exacerbated by the lack of a uniform approach to measuring and interpreting the geological evidence of paleo sea-levels. In this review, we discuss the characteristics of MIS 5e field observations, and we set the basis for a standardized approach to MIS 5e paleo sea-level reconstructions, that is already successfully applied in Holocene sea-level research. Application of the standard definitions and methodologies described in this paper will enhance our ability to compare data from different research groups and different areas, in order to gain deeper insights into MIS 5e sea-level changes. Improving estimates of Last Interglacial sea-level is, in turn, a key to understanding the behavior of ice sheets in a warmer world.},\\n bibtype = {misc},\\n author = {Rovere, Alessio and Raymo, M.E. Maureen E. and Vacchi, Matteo and Lorscheid, Thomas and Stocchi, Paolo and Gómez-Pujol, Lluís and Harris, Daniel L. D.L. and Casella, Elisa and O'Leary, M.J. Michael J. and Hearty, P.J. Paul J.},\\n doi = {10.1016/j.earscirev.2016.06.006}\\n}\",\"author_short\":[\"Rovere,  A.\",\"Raymo,  M., M., E.\",\"Vacchi,  M.\",\"Lorscheid,  T.\",\"Stocchi,  P.\",\"Gómez-Pujol,  L.\",\"Harris,  D., L., D.\",\"Casella,  E.\",\"O'Leary,  M., M., J.\",\"Hearty,  P., P., J.\"],\"urls\":{\"Website\":\"http://linkinghub.elsevier.com/retrieve/pii/S0012825216301246\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"rovere-raymo-vacchi-lorscheid-stocchi-gmezpujol-harris-casella-etal-theanalysisoflastinterglacialmis5erelativesealevelindicatorsreconstructingsealevelinawarmerworld-2016\",\"role\":\"author\",\"keyword\":[\"Ice sheets\",\"Last Interglacial\",\"MIS 5e\",\"Paleo sea-level\",\"Past sea-level changes\",\"Sea-level marker\",\"Sea-level reconstruction\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":1,\"html\":\"\"},{\"title\":\"Study of wave runup using numerical models and low-altitude aerial photogrammetry: A tool for coastal management\",\"type\":\"article\",\"year\":\"2014\",\"keywords\":\"MEDFLOOD,MIRAMAR,PLIOMAX,SEAMAP,SLCC\",\"pages\":\"160-167\",\"volume\":\"149\",\"websites\":\"http://linkinghub.elsevier.com/retrieve/pii/S0272771414002273,http://dx.doi.org/10.1016/j.ecss.2014.08.012\",\"month\":\"8\",\"publisher\":\"Elsevier Ltd\",\"id\":\"8fb8ca01-2971-312e-8c98-3107d0542aff\",\"created\":\"2018-02-03T12:42:09.112Z\",\"accessed\":\"2014-09-25\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.243Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Casella2014\",\"private_publication\":false,\"abstract\":\"Monitoring the impact of sea storms on coastal areas is fundamental to study beach evolution and the vulnerability of low-lying coasts to erosion and flooding. Modelling wave runup on a beach is possible, but it requires accurate topographic data and model tuning, that can be done comparing observed and modeled runup. In this study we collected aerial photos using an Unmanned Aerial Vehicle after two different swells on the same study area. We merged the point cloud obtained with photogrammetry with multibeam data, in order to obtain a complete beach topography. Then, on each set of rectified and georeferenced UAV orthophotos, we identified the maximum wave runup for both events recognizing the wet area left by the waves. We then used our topography and numerical models to simulate the wave runup and compare the model results to observed values during the two events. Our results highlight the potential of the methodology presented, which integrates UAV platforms, photogrammetry and Geographic Information Systems to provide faster and cheaper information on beach topography and geomorphology compared with traditional techniques without losing in accuracy. We use the results obtained from this technique as a topographic base for a model that calculates runup for the two swells. The observed and modeled runups are consistent, and open new directions for future research.\",\"bibtype\":\"article\",\"author\":\"Casella, Elisa and Rovere, Alessio and Pedroncini, Andrea and Mucerino, Luigi and Casella, Marco and Cusati, Luis Alberto and Vacchi, Matteo and Ferrari, Marco and Firpo, Marco\",\"doi\":\"10.1016/j.ecss.2014.08.012\",\"journal\":\"Estuarine, Coastal and Shelf Science\",\"bibtex\":\"@article{\\n title = {Study of wave runup using numerical models and low-altitude aerial photogrammetry: A tool for coastal management},\\n type = {article},\\n year = {2014},\\n keywords = {MEDFLOOD,MIRAMAR,PLIOMAX,SEAMAP,SLCC},\\n pages = {160-167},\\n volume = {149},\\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0272771414002273,http://dx.doi.org/10.1016/j.ecss.2014.08.012},\\n month = {8},\\n publisher = {Elsevier Ltd},\\n id = {8fb8ca01-2971-312e-8c98-3107d0542aff},\\n created = {2018-02-03T12:42:09.112Z},\\n accessed = {2014-09-25},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.243Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Casella2014},\\n private_publication = {false},\\n abstract = {Monitoring the impact of sea storms on coastal areas is fundamental to study beach evolution and the vulnerability of low-lying coasts to erosion and flooding. Modelling wave runup on a beach is possible, but it requires accurate topographic data and model tuning, that can be done comparing observed and modeled runup. In this study we collected aerial photos using an Unmanned Aerial Vehicle after two different swells on the same study area. We merged the point cloud obtained with photogrammetry with multibeam data, in order to obtain a complete beach topography. Then, on each set of rectified and georeferenced UAV orthophotos, we identified the maximum wave runup for both events recognizing the wet area left by the waves. We then used our topography and numerical models to simulate the wave runup and compare the model results to observed values during the two events. Our results highlight the potential of the methodology presented, which integrates UAV platforms, photogrammetry and Geographic Information Systems to provide faster and cheaper information on beach topography and geomorphology compared with traditional techniques without losing in accuracy. We use the results obtained from this technique as a topographic base for a model that calculates runup for the two swells. The observed and modeled runups are consistent, and open new directions for future research.},\\n bibtype = {article},\\n author = {Casella, Elisa and Rovere, Alessio and Pedroncini, Andrea and Mucerino, Luigi and Casella, Marco and Cusati, Luis Alberto and Vacchi, Matteo and Ferrari, Marco and Firpo, Marco},\\n doi = {10.1016/j.ecss.2014.08.012},\\n journal = {Estuarine, Coastal and Shelf Science}\\n}\",\"author_short\":[\"Casella,  E.\",\"Rovere,  A.\",\"Pedroncini,  A.\",\"Mucerino,  L.\",\"Casella,  M.\",\"Cusati,  L., A.\",\"Vacchi,  M.\",\"Ferrari,  M.\",\"Firpo,  M.\"],\"urls\":{\"Website\":\"http://linkinghub.elsevier.com/retrieve/pii/S0272771414002273,http://dx.doi.org/10.1016/j.ecss.2014.08.012\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"casella-rovere-pedroncini-mucerino-casella-cusati-vacchi-ferrari-etal-studyofwaverunupusingnumericalmodelsandlowaltitudeaerialphotogrammetryatoolforcoastalmanagement-2014\",\"role\":\"author\",\"keyword\":[\"MEDFLOOD\",\"MIRAMAR\",\"PLIOMAX\",\"SEAMAP\",\"SLCC\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/publications.html\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Chapter 18 Fixed biological indicators\",\"type\":\"article\",\"year\":\"2015\",\"keywords\":\"MEDFLOOD,PLIOMAX,SLCC\",\"pages\":\"268-280\",\"publisher\":\"Wiley Online Library\",\"chapter\":\"18\",\"id\":\"88d36d15-b4c4-3042-bbdf-5b2ba9c1033d\",\"created\":\"2018-02-03T12:42:09.156Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.173Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Rovere2015c\",\"private_publication\":false,\"abstract\":\"Fixed biological indicators are organisms that live fixed to hard substrates and their living range or the upper part of it is located near or at sea level. In this chapter, the main fixed biological indicators are described and their value as indicators of former sea levels is discussed.\",\"bibtype\":\"article\",\"author\":\"Rovere, Alessio and Antonioli, Fabrizio and Bianchi, Carlo Nike\",\"editor\":\"Shennan, Ian and Long, Antony J. and Horton, Benjamin P\",\"journal\":\"Handbook of Sea-Level Research\",\"bibtex\":\"@article{\\n title = {Chapter 18 Fixed biological indicators},\\n type = {article},\\n year = {2015},\\n keywords = {MEDFLOOD,PLIOMAX,SLCC},\\n pages = {268-280},\\n publisher = {Wiley Online Library},\\n chapter = {18},\\n id = {88d36d15-b4c4-3042-bbdf-5b2ba9c1033d},\\n created = {2018-02-03T12:42:09.156Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.173Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Rovere2015c},\\n private_publication = {false},\\n abstract = {Fixed biological indicators are organisms that live fixed to hard substrates and their living range or the upper part of it is located near or at sea level. In this chapter, the main fixed biological indicators are described and their value as indicators of former sea levels is discussed.},\\n bibtype = {article},\\n author = {Rovere, Alessio and Antonioli, Fabrizio and Bianchi, Carlo Nike},\\n editor = {Shennan, Ian and Long, Antony J. and Horton, Benjamin P},\\n journal = {Handbook of Sea-Level Research}\\n}\",\"author_short\":[\"Rovere,  A.\",\"Antonioli,  F.\",\"Bianchi,  C., N.\"],\"editor_short\":[\"Shennan,  I.\",\"Long,  A., J.\",\"Horton,  B., P.\"],\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"rovere-antonioli-bianchi-chapter18fixedbiologicalindicators-2015\",\"role\":\"author\",\"urls\":{},\"keyword\":[\"MEDFLOOD\",\"PLIOMAX\",\"SLCC\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/publications.html\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"type\":\"inbook\",\"year\":\"2015\",\"pages\":\"1-30\",\"websites\":\"http://dx.doi.org/10.1007/978-3-319-17001-5_35-1\",\"publisher\":\"Springer International Publishing\",\"city\":\"Cham\",\"id\":\"8d9ac960-e7f9-3635-a6bf-13ec1d22a9f2\",\"created\":\"2018-02-03T12:42:09.165Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.136Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Bianchi2015\",\"source_type\":\"inbook\",\"private_publication\":false,\"bibtype\":\"inbook\",\"author\":\"Bianchi, Carlo Nike and Morri, Carla and Lasagna, Roberta and Montefalcone, Monica and Gatti, Giulia and Parravicini, Valeriano and Rovere, Alessio\",\"editor\":\"Rossi, Sergio and Bramanti, Lorenzo and Gori, Andrea and del Valle, Covadonga\",\"doi\":\"10.1007/978-3-319-17001-5_35-1\",\"chapter\":\"Resilience of the Marine Animal Forest\",\"title\":\"Marine Animal Forests: The Ecology of Benthic Biodiversity Hotspots\",\"bibtex\":\"@inbook{\\n type = {inbook},\\n year = {2015},\\n pages = {1-30},\\n websites = {http://dx.doi.org/10.1007/978-3-319-17001-5_35-1},\\n publisher = {Springer International Publishing},\\n city = {Cham},\\n id = {8d9ac960-e7f9-3635-a6bf-13ec1d22a9f2},\\n created = {2018-02-03T12:42:09.165Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.136Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Bianchi2015},\\n source_type = {inbook},\\n private_publication = {false},\\n bibtype = {inbook},\\n author = {Bianchi, Carlo Nike and Morri, Carla and Lasagna, Roberta and Montefalcone, Monica and Gatti, Giulia and Parravicini, Valeriano and Rovere, Alessio},\\n editor = {Rossi, Sergio and Bramanti, Lorenzo and Gori, Andrea and del Valle, Covadonga},\\n doi = {10.1007/978-3-319-17001-5_35-1},\\n chapter = {Resilience of the Marine Animal Forest},\\n title = {Marine Animal Forests: The Ecology of Benthic Biodiversity Hotspots}\\n}\",\"author_short\":[\"Bianchi,  C., N.\",\"Morri,  C.\",\"Lasagna,  R.\",\"Montefalcone,  M.\",\"Gatti,  G.\",\"Parravicini,  V.\",\"Rovere,  A.\"],\"editor_short\":[\"Rossi,  S.\",\"Bramanti,  L.\",\"Gori,  A.\",\"del Valle,  C.\"],\"urls\":{\"Website\":\"http://dx.doi.org/10.1007/978-3-319-17001-5_35-1\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-marineanimalforeststheecologyofbenthicbiodiversityhotspots-2015\",\"role\":\"author\",\"metadata\":{\"authorlinks\":{}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy)\",\"type\":\"article\",\"year\":\"2015\",\"keywords\":\"MIRAMAR,SEAMAP,SLCC\",\"pages\":\"278-286\",\"volume\":\"11\",\"websites\":\"http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134\",\"month\":\"6\",\"day\":\"24\",\"id\":\"4764317f-01f8-36bf-9eff-783fcb4dfc8b\",\"created\":\"2018-02-03T12:42:09.171Z\",\"accessed\":\"2014-09-15\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.118Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Rovere2014\",\"private_publication\":false,\"abstract\":\"In this paper, we present a map describing the main geomorphological features of the coastal and marine area between the towns of Albenga and Savona (Ligurian Sea, NW Mediterranean) corresponding to a coastal stretch of ∼40 km. To produce this map, we collated data from the literature, orthophotos, perspective photos, multibeam and side scan sonar data, and undertook direct surveys to ground truth data obtained using indirect techniques. We divided the information into nine thematic layers, including bathymetry, natural coastal types, geomorphological elements, seafloor coverage (both geological and biological), coastal and nearshore dynamics, human influence on coastal and marine environments, coastal occupation and protected areas.\",\"bibtype\":\"article\",\"author\":\"Rovere, A. and Casella, E. and Vacchi, M. and Parravicini, V. and Firpo, M. and Ferrari, M. and Morri, C. and Bianchi, C. N.\",\"doi\":\"10.1080/17445647.2014.933134\",\"journal\":\"Journal of Maps\",\"number\":\"2\",\"bibtex\":\"@article{\\n title = {Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy)},\\n type = {article},\\n year = {2015},\\n keywords = {MIRAMAR,SEAMAP,SLCC},\\n pages = {278-286},\\n volume = {11},\\n websites = {http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134},\\n month = {6},\\n day = {24},\\n id = {4764317f-01f8-36bf-9eff-783fcb4dfc8b},\\n created = {2018-02-03T12:42:09.171Z},\\n accessed = {2014-09-15},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.118Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Rovere2014},\\n private_publication = {false},\\n abstract = {In this paper, we present a map describing the main geomorphological features of the coastal and marine area between the towns of Albenga and Savona (Ligurian Sea, NW Mediterranean) corresponding to a coastal stretch of ∼40 km. To produce this map, we collated data from the literature, orthophotos, perspective photos, multibeam and side scan sonar data, and undertook direct surveys to ground truth data obtained using indirect techniques. We divided the information into nine thematic layers, including bathymetry, natural coastal types, geomorphological elements, seafloor coverage (both geological and biological), coastal and nearshore dynamics, human influence on coastal and marine environments, coastal occupation and protected areas.},\\n bibtype = {article},\\n author = {Rovere, A. and Casella, E. and Vacchi, M. and Parravicini, V. and Firpo, M. and Ferrari, M. and Morri, C. and Bianchi, C. N.},\\n doi = {10.1080/17445647.2014.933134},\\n journal = {Journal of Maps},\\n number = {2}\\n}\",\"author_short\":[\"Rovere,  A.\",\"Casella,  E.\",\"Vacchi,  M.\",\"Parravicini,  V.\",\"Firpo,  M.\",\"Ferrari,  M.\",\"Morri,  C.\",\"Bianchi,  C., N.\"],\"urls\":{\"Website\":\"http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-2015\",\"role\":\"author\",\"keyword\":[\"MIRAMAR\",\"SEAMAP\",\"SLCC\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/publications.html\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Detection of a dynamic topography signal in last interglacial sea-level records\",\"type\":\"article\",\"year\":\"2017\",\"pages\":\"e1700457\",\"volume\":\"3\",\"websites\":\"http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.1700457\",\"id\":\"ba87cc47-ab64-3a6b-9d47-f1fd1ea653c2\",\"created\":\"2018-02-03T12:42:09.180Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:09.180Z\",\"read\":\"true\",\"starred\":\"true\",\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"austermann2017detection\",\"source_type\":\"inproceedings\",\"private_publication\":false,\"abstract\":\"Estimating minimum ice volume during the last interglacial based on local sea-level indicators requires that these indicators are corrected for processes that alter local sea level relative to the global average. Although glacial isostatic adjustment is generally accounted for, global scale dynamic changes in topography driven by convective mantle flow are generally not considered. We use numerical models of mantle flow to quantify vertical deflections caused by dynamic topography and compare predictions at passive margins to a globally distributed set of last interglacial sea-level markers. The deflections predicted as a result of dynamic topography are significantly correlated with marker elevations (>95% probability) and are consistent with construction and preservation attributes across marker types. We conclude that a dynamic topography signal is present in the elevation of last interglacial sea-level records and that the signal must be accounted for in any effort to determine peak global mean sea level during the last interglacial to within an accuracy of several meters.\",\"bibtype\":\"article\",\"author\":\"Austermann, Jacqueline and Mitrovica, Jerry X and Huybers, Peter and Rovere, Alessio\",\"doi\":\"10.1126/sciadv.1700457\",\"journal\":\"Science Advances\",\"number\":\"7\",\"bibtex\":\"@article{\\n title = {Detection of a dynamic topography signal in last interglacial sea-level records},\\n type = {article},\\n year = {2017},\\n pages = {e1700457},\\n volume = {3},\\n websites = {http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.1700457},\\n id = {ba87cc47-ab64-3a6b-9d47-f1fd1ea653c2},\\n created = {2018-02-03T12:42:09.180Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:09.180Z},\\n read = {true},\\n starred = {true},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {austermann2017detection},\\n source_type = {inproceedings},\\n private_publication = {false},\\n abstract = {Estimating minimum ice volume during the last interglacial based on local sea-level indicators requires that these indicators are corrected for processes that alter local sea level relative to the global average. Although glacial isostatic adjustment is generally accounted for, global scale dynamic changes in topography driven by convective mantle flow are generally not considered. We use numerical models of mantle flow to quantify vertical deflections caused by dynamic topography and compare predictions at passive margins to a globally distributed set of last interglacial sea-level markers. The deflections predicted as a result of dynamic topography are significantly correlated with marker elevations (>95% probability) and are consistent with construction and preservation attributes across marker types. We conclude that a dynamic topography signal is present in the elevation of last interglacial sea-level records and that the signal must be accounted for in any effort to determine peak global mean sea level during the last interglacial to within an accuracy of several meters.},\\n bibtype = {article},\\n author = {Austermann, Jacqueline and Mitrovica, Jerry X and Huybers, Peter and Rovere, Alessio},\\n doi = {10.1126/sciadv.1700457},\\n journal = {Science Advances},\\n number = {7}\\n}\",\"author_short\":[\"Austermann,  J.\",\"Mitrovica,  J., X.\",\"Huybers,  P.\",\"Rovere,  A.\"],\"urls\":{\"Website\":\"http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.1700457\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"austermann-mitrovica-huybers-rovere-detectionofadynamictopographysignalinlastinterglacialsealevelrecords-2017\",\"role\":\"author\",\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/publications.html\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Emergence and evolution of Santa Maria Island (azores)- The conundrum of uplifted islands revisited\",\"type\":\"article\",\"year\":\"2017\",\"pages\":\"372-391\",\"volume\":\"129\",\"id\":\"1b95bc57-9756-342d-9c36-37e15aca8e39\",\"created\":\"2018-02-03T12:42:09.288Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-02-03T12:42:09.288Z\",\"read\":\"true\",\"starred\":\"true\",\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Ramalho2016\",\"private_publication\":false,\"abstract\":\"The growth and decay of ocean island volcanoes is intrinsically linked to vertical movements; whilst mechanisms for subsidence are well understood, uplift mechanisms are still very enigmatic. Santa Maria Island in the Azores is an ocean island volcano with a complex evolutionary history with subsidence followed by uplift. The island emerged by surtseyan activity at approximately 6 Ma, entailing in the formation of a subaerial shield volcano that was fully developed by ~5.6 Ma. The edifice then experienced a period of intense erosion and subsidence, during which it was partially or completely truncated to a shallow submarine bank. Around 5 Ma, volcanism resumed on the eastern side of the edifice, with occasional submarine/surtseyan activity synchronous with marine deposition. By ~4.3 Ma, volcanism grew in intensity forming a new edifice centred on the eastern flank of the underlying edifice. This new volcanic edifice started as submarine and then, as it gradually grew upwards and outpaced subsidence, breached sea level and formed a new island. The new edifice kept growing eastwards and northwards until ~3.5 Ma, when volcanic activity waned. At 3.5-3.2 Ma, however, subsidence reversed to an uplift trend that extended throughout the Upper Pleistocene into the present. This uplift trend is responsible for the generation of a staircase of shore platforms on the windward side of the island, which extends up to ~230 m in elevation. The fact that an island located in very young lithosphere experienced such a pronounced uplift trend is remarkable and raises important questions concerning possible uplift mechanisms. The loading of the neighbouring island of São Miguel may account for part of the uplift, but not the majority. Vertical tectonics along the nearby Gloria Fault is not completely implausible but unlikely to be a source of significant uplift due to its dominant strike-slip character. Thus, other mechanisms need to be considered, most notably intrusions at the base of the edifice and crustal thickening, suggesting that these play a significant role even on islands standing on a young lithosphere, such as in the Azores.\",\"bibtype\":\"article\",\"author\":\"Ramalho, Ricardo S. and Helffrich, George and Madeira, José and Cosca, Michael and Thomas, Christine and Quartau, Rui and Hipólito, Ana and Rovere, Alessio and Hearty, Paul J. and Ávila, Sérgio P.\",\"doi\":\"10.1130/B31538.1\",\"journal\":\"Bulletin of the Geological Society of America\",\"number\":\"3-4\",\"bibtex\":\"@article{\\n title = {Emergence and evolution of Santa Maria Island (azores)- The conundrum of uplifted islands revisited},\\n type = {article},\\n year = {2017},\\n pages = {372-391},\\n volume = {129},\\n id = {1b95bc57-9756-342d-9c36-37e15aca8e39},\\n created = {2018-02-03T12:42:09.288Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-02-03T12:42:09.288Z},\\n read = {true},\\n starred = {true},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Ramalho2016},\\n private_publication = {false},\\n abstract = {The growth and decay of ocean island volcanoes is intrinsically linked to vertical movements; whilst mechanisms for subsidence are well understood, uplift mechanisms are still very enigmatic. Santa Maria Island in the Azores is an ocean island volcano with a complex evolutionary history with subsidence followed by uplift. The island emerged by surtseyan activity at approximately 6 Ma, entailing in the formation of a subaerial shield volcano that was fully developed by ~5.6 Ma. The edifice then experienced a period of intense erosion and subsidence, during which it was partially or completely truncated to a shallow submarine bank. Around 5 Ma, volcanism resumed on the eastern side of the edifice, with occasional submarine/surtseyan activity synchronous with marine deposition. By ~4.3 Ma, volcanism grew in intensity forming a new edifice centred on the eastern flank of the underlying edifice. This new volcanic edifice started as submarine and then, as it gradually grew upwards and outpaced subsidence, breached sea level and formed a new island. The new edifice kept growing eastwards and northwards until ~3.5 Ma, when volcanic activity waned. At 3.5-3.2 Ma, however, subsidence reversed to an uplift trend that extended throughout the Upper Pleistocene into the present. This uplift trend is responsible for the generation of a staircase of shore platforms on the windward side of the island, which extends up to ~230 m in elevation. The fact that an island located in very young lithosphere experienced such a pronounced uplift trend is remarkable and raises important questions concerning possible uplift mechanisms. The loading of the neighbouring island of São Miguel may account for part of the uplift, but not the majority. Vertical tectonics along the nearby Gloria Fault is not completely implausible but unlikely to be a source of significant uplift due to its dominant strike-slip character. Thus, other mechanisms need to be considered, most notably intrusions at the base of the edifice and crustal thickening, suggesting that these play a significant role even on islands standing on a young lithosphere, such as in the Azores.},\\n bibtype = {article},\\n author = {Ramalho, Ricardo S. and Helffrich, George and Madeira, José and Cosca, Michael and Thomas, Christine and Quartau, Rui and Hipólito, Ana and Rovere, Alessio and Hearty, Paul J. and Ávila, Sérgio P.},\\n doi = {10.1130/B31538.1},\\n journal = {Bulletin of the Geological Society of America},\\n number = {3-4}\\n}\",\"author_short\":[\"Ramalho,  R., S.\",\"Helffrich,  G.\",\"Madeira,  J.\",\"Cosca,  M.\",\"Thomas,  C.\",\"Quartau,  R.\",\"Hipólito,  A.\",\"Rovere,  A.\",\"Hearty,  P., J.\",\"Ávila,  S., P.\"],\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"ramalho-helffrich-madeira-cosca-thomas-quartau-hiplito-rovere-etal-emergenceandevolutionofsantamariaislandazorestheconundrumofupliftedislandsrevisited-2017\",\"role\":\"author\",\"urls\":{},\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Tides in the Last Interglacial: Insights from notch geometry and palaeo tidal models in Bonaire, Netherland Antilles\",\"type\":\"article\",\"year\":\"2017\",\"pages\":\"1-9\",\"volume\":\"7\",\"websites\":\"http://dx.doi.org/10.1038/s41598-017-16285-6\",\"publisher\":\"Springer US\",\"id\":\"cb5bca11-8cb9-3f21-8351-097d44faa054\",\"created\":\"2018-02-03T12:42:09.295Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-09-14T15:34:15.866Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Lorscheid2017d\",\"private_publication\":false,\"abstract\":\"The study of past sea levels relies largely on the interpretation of sea-level indicators. Palaeo tidal notches are considered as one of the most precise sea-level indicators as their formation is closely tied to the local tidal range. We present geometric measurements of modern and palaeo (Marine Isotope Stage (MIS) 5e) tidal notches on Bonaire (southern Caribbean Sea) and results from two tidal simulations, using the present-day bathymetry and a palaeo-bathymetry. We use these two tools to investigate changes in the tidal range since MIS 5e. Our models show that the tidal range changes most significantly in shallow areas, whereas both, notch geometry and models results, suggest that steeper continental shelves, such as the ones bordering the island of Bonaire, are less affected to changes in tidal range in conditions of MIS 5e sea levels. We use our data and results to discuss the importance of considering changes in tidal range while reconstructing MIS 5e sea level histories, and we remark that it is possible to use hydrodynamic modelling and notch geometry as first-order proxies to assess whether, in a particular area, tidal range might have been different in MIS 5e with respect to today. Fossil\",\"bibtype\":\"article\",\"author\":\"Lorscheid, Thomas and Felis, Thomas and Stocchi, Paolo and Obert, J.C. Christina and Scholz, Denis and Rovere, Alessio\",\"doi\":\"10.1038/s41598-017-16285-6\",\"journal\":\"Scientific Reports\",\"number\":\"1\",\"bibtex\":\"@article{\\n title = {Tides in the Last Interglacial: Insights from notch geometry and palaeo tidal models in Bonaire, Netherland Antilles},\\n type = {article},\\n year = {2017},\\n pages = {1-9},\\n volume = {7},\\n websites = {http://dx.doi.org/10.1038/s41598-017-16285-6},\\n publisher = {Springer US},\\n id = {cb5bca11-8cb9-3f21-8351-097d44faa054},\\n created = {2018-02-03T12:42:09.295Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-09-14T15:34:15.866Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Lorscheid2017d},\\n private_publication = {false},\\n abstract = {The study of past sea levels relies largely on the interpretation of sea-level indicators. Palaeo tidal notches are considered as one of the most precise sea-level indicators as their formation is closely tied to the local tidal range. We present geometric measurements of modern and palaeo (Marine Isotope Stage (MIS) 5e) tidal notches on Bonaire (southern Caribbean Sea) and results from two tidal simulations, using the present-day bathymetry and a palaeo-bathymetry. We use these two tools to investigate changes in the tidal range since MIS 5e. Our models show that the tidal range changes most significantly in shallow areas, whereas both, notch geometry and models results, suggest that steeper continental shelves, such as the ones bordering the island of Bonaire, are less affected to changes in tidal range in conditions of MIS 5e sea levels. We use our data and results to discuss the importance of considering changes in tidal range while reconstructing MIS 5e sea level histories, and we remark that it is possible to use hydrodynamic modelling and notch geometry as first-order proxies to assess whether, in a particular area, tidal range might have been different in MIS 5e with respect to today. Fossil},\\n bibtype = {article},\\n author = {Lorscheid, Thomas and Felis, Thomas and Stocchi, Paolo and Obert, J.C. Christina and Scholz, Denis and Rovere, Alessio},\\n doi = {10.1038/s41598-017-16285-6},\\n journal = {Scientific Reports},\\n number = {1}\\n}\",\"author_short\":[\"Lorscheid,  T.\",\"Felis,  T.\",\"Stocchi,  P.\",\"Obert,  J., C.\",\"Scholz,  D.\",\"Rovere,  A.\"],\"urls\":{\"Website\":\"http://dx.doi.org/10.1038/s41598-017-16285-6\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"lorscheid-felis-stocchi-obert-scholz-rovere-tidesinthelastinterglacialinsightsfromnotchgeometryandpalaeotidalmodelsinbonairenetherlandantilles-2017\",\"role\":\"author\",\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Patterns of Sediment Transport Using Foraminifera Tracers across Sand Aprons on the Great Barrier Reef\",\"type\":\"article\",\"year\":\"2017\",\"pages\":\"864-873\",\"volume\":\"33\",\"websites\":\"http://www.bioone.org/doi/10.2112/JCOASTRES-D-16-00082.1\",\"id\":\"f1b13efb-e7ec-3abf-be89-0b240ef77579\",\"created\":\"2018-02-03T12:42:09.320Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-09-14T15:34:15.852Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Fellowes2017\",\"private_publication\":false,\"abstract\":\"© Coastal Education and Research Foundation, Inc. 2017. Sediment dynamics exert large control over coral reef geomorphological evolution and are vital to understanding past and present geomorphic responses. Large benthic foraminifera (LBF) live in the algal reef flats, and their tests (shells) are transported post-mortem by waves and currents onto back-reef environments, including sand aprons. This study investigated the patterns of transport linking surficial and downcore sediments in samples from three sand aprons with different wave exposures at One Tree Reef on the southern Great Barrier Reef (Australia). Six LBF genera represented up to 32% of the sediments analysed. Lagoonward transport increased LBF test abrasion and sediment bulk density. Sediment grain size and LBF abundance in sediments also decreased with lagoonward transport. Sediment transport patterns indicated by LBF species used as tracer were consistent with the prominent E-SE wave environment. A novel taphofacies approach was used to describe stratigraphic layers in downcore sediments based on LBF test abrasion and abundance. Varied sediment deposition rates did not affect the LBF test abrasion signature downcore. It appears that Baculogypsina sphaerulata has been the dominant species for at least 3 ka. Tests that were deposited slowly exhibited less or the same levels of abrasion than those that were rapidly deposited. It appears that test abrasion is primarily determined by the distance travelled rather than the influence of increased age or chemical dissolution.\",\"bibtype\":\"article\",\"author\":\"Fellowes, Thomas E. and Gacutan, Jordan and Harris, Daniel L. and Vila-Concejo, Ana and Webster, Jody M. and Byrne, Maria\",\"doi\":\"10.2112/JCOASTRES-D-16-00082.1\",\"journal\":\"Journal of Coastal Research\",\"number\":\"4\",\"bibtex\":\"@article{\\n title = {Patterns of Sediment Transport Using Foraminifera Tracers across Sand Aprons on the Great Barrier Reef},\\n type = {article},\\n year = {2017},\\n pages = {864-873},\\n volume = {33},\\n websites = {http://www.bioone.org/doi/10.2112/JCOASTRES-D-16-00082.1},\\n id = {f1b13efb-e7ec-3abf-be89-0b240ef77579},\\n created = {2018-02-03T12:42:09.320Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-09-14T15:34:15.852Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Fellowes2017},\\n private_publication = {false},\\n abstract = {© Coastal Education and Research Foundation, Inc. 2017. Sediment dynamics exert large control over coral reef geomorphological evolution and are vital to understanding past and present geomorphic responses. Large benthic foraminifera (LBF) live in the algal reef flats, and their tests (shells) are transported post-mortem by waves and currents onto back-reef environments, including sand aprons. This study investigated the patterns of transport linking surficial and downcore sediments in samples from three sand aprons with different wave exposures at One Tree Reef on the southern Great Barrier Reef (Australia). Six LBF genera represented up to 32% of the sediments analysed. Lagoonward transport increased LBF test abrasion and sediment bulk density. Sediment grain size and LBF abundance in sediments also decreased with lagoonward transport. Sediment transport patterns indicated by LBF species used as tracer were consistent with the prominent E-SE wave environment. A novel taphofacies approach was used to describe stratigraphic layers in downcore sediments based on LBF test abrasion and abundance. Varied sediment deposition rates did not affect the LBF test abrasion signature downcore. It appears that Baculogypsina sphaerulata has been the dominant species for at least 3 ka. Tests that were deposited slowly exhibited less or the same levels of abrasion than those that were rapidly deposited. It appears that test abrasion is primarily determined by the distance travelled rather than the influence of increased age or chemical dissolution.},\\n bibtype = {article},\\n author = {Fellowes, Thomas E. and Gacutan, Jordan and Harris, Daniel L. and Vila-Concejo, Ana and Webster, Jody M. and Byrne, Maria},\\n doi = {10.2112/JCOASTRES-D-16-00082.1},\\n journal = {Journal of Coastal Research},\\n number = {4}\\n}\",\"author_short\":[\"Fellowes,  T., E.\",\"Gacutan,  J.\",\"Harris,  D., L.\",\"Vila-Concejo,  A.\",\"Webster,  J., M.\",\"Byrne,  M.\"],\"urls\":{\"Website\":\"http://www.bioone.org/doi/10.2112/JCOASTRES-D-16-00082.1\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"fellowes-gacutan-harris-vilaconcejo-webster-byrne-patternsofsedimenttransportusingforaminiferatracersacrosssandapronsonthegreatbarrierreef-2017\",\"role\":\"author\",\"metadata\":{\"authorlinks\":{}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Geomorphic changes of a coral shingle cay measured using Kite Aerial Photography\",\"type\":\"article\",\"year\":\"2016\",\"keywords\":\"3D topography,Coral reef morphodynamics,Kite Aerial Photography\",\"pages\":\"1-8\",\"volume\":\"270\",\"websites\":\"http://dx.doi.org/10.1016/j.geomorph.2016.06.018\",\"publisher\":\"Elsevier B.V.\",\"id\":\"4bf2fa14-782a-38ea-99cf-8df4b476f09d\",\"created\":\"2018-02-03T12:42:09.330Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-09-14T15:34:15.863Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Bryson2016e\",\"private_publication\":false,\"abstract\":\"Measurements of geomorphic change in the intertidal zones of coral reefs are made using a variety of remote sensing and in-situ techniques, where variations in the coverage and spatial-temporal precision achieved are directly related to the cost of data acquisition. We present a novel, low-cost technique for measuring high-resolution changes in reef environments based on Kite Aerial Photography (KAP) and photogrammetry/structure-from-motion post-processing. KAP images are used to measure fine-scale changes in intertidal topography and sediment texture characteristics, including rubble particle size, of a coral shingle cay at One Tree Island, Great Barrier Reef in the context of storm activity. Validation using Real Time Kinematic DGPS demonstrates the ability to measure topographic elevation with an error of 5.53 cm (RMSE) and a spatial resolution of 5 cm per point, an accuracy/resolution that is superior to airborne LiDAR and equivalent to terrestrial LiDAR, but at a fraction of the equipment cost.\",\"bibtype\":\"article\",\"author\":\"Bryson, Mitch and Duce, Stephanie and Harris, Dan and Webster, Jody M. and Thompson, Alisha and Vila-Concejo, Ana and Williams, Stefan B.\",\"doi\":\"10.1016/j.geomorph.2016.06.018\",\"journal\":\"Geomorphology\",\"bibtex\":\"@article{\\n title = {Geomorphic changes of a coral shingle cay measured using Kite Aerial Photography},\\n type = {article},\\n year = {2016},\\n keywords = {3D topography,Coral reef morphodynamics,Kite Aerial Photography},\\n pages = {1-8},\\n volume = {270},\\n websites = {http://dx.doi.org/10.1016/j.geomorph.2016.06.018},\\n publisher = {Elsevier B.V.},\\n id = {4bf2fa14-782a-38ea-99cf-8df4b476f09d},\\n created = {2018-02-03T12:42:09.330Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-09-14T15:34:15.863Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Bryson2016e},\\n private_publication = {false},\\n abstract = {Measurements of geomorphic change in the intertidal zones of coral reefs are made using a variety of remote sensing and in-situ techniques, where variations in the coverage and spatial-temporal precision achieved are directly related to the cost of data acquisition. We present a novel, low-cost technique for measuring high-resolution changes in reef environments based on Kite Aerial Photography (KAP) and photogrammetry/structure-from-motion post-processing. KAP images are used to measure fine-scale changes in intertidal topography and sediment texture characteristics, including rubble particle size, of a coral shingle cay at One Tree Island, Great Barrier Reef in the context of storm activity. Validation using Real Time Kinematic DGPS demonstrates the ability to measure topographic elevation with an error of 5.53 cm (RMSE) and a spatial resolution of 5 cm per point, an accuracy/resolution that is superior to airborne LiDAR and equivalent to terrestrial LiDAR, but at a fraction of the equipment cost.},\\n bibtype = {article},\\n author = {Bryson, Mitch and Duce, Stephanie and Harris, Dan and Webster, Jody M. and Thompson, Alisha and Vila-Concejo, Ana and Williams, Stefan B.},\\n doi = {10.1016/j.geomorph.2016.06.018},\\n journal = {Geomorphology}\\n}\",\"author_short\":[\"Bryson,  M.\",\"Duce,  S.\",\"Harris,  D.\",\"Webster,  J., M.\",\"Thompson,  A.\",\"Vila-Concejo,  A.\",\"Williams,  S., B.\"],\"urls\":{\"Website\":\"http://dx.doi.org/10.1016/j.geomorph.2016.06.018\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"bryson-duce-harris-webster-thompson-vilaconcejo-williams-geomorphicchangesofacoralshinglecaymeasuredusingkiteaerialphotography-2016\",\"role\":\"author\",\"keyword\":[\"3D topography\",\"Coral reef morphodynamics\",\"Kite Aerial Photography\"],\"metadata\":{\"authorlinks\":{}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Sediment Composition and Facies of Coral Reef Islands in the Spermonde Archipelago, Indonesia\",\"type\":\"article\",\"year\":\"2017\",\"keywords\":\"carbonate sediments, grain size, skeletal constitu\",\"pages\":\"1-13\",\"volume\":\"4\",\"websites\":\"http://journal.frontiersin.org/article/10.3389/fmars.2017.00144/full\",\"id\":\"c0dff020-5319-3fd2-93e8-d982132be5aa\",\"created\":\"2018-02-03T12:42:09.395Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-09-14T15:34:15.991Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Janßen2017a\",\"private_publication\":false,\"bibtype\":\"article\",\"author\":\"Janßen, Alexander and Wizemann, André and Klicpera, André and Satari, Dewi Y. and Westphal, Hildegard and Mann, Thomas\",\"doi\":\"10.3389/fmars.2017.00144\",\"journal\":\"Frontiers in Marine Science\",\"number\":\"May\",\"bibtex\":\"@article{\\n title = {Sediment Composition and Facies of Coral Reef Islands in the Spermonde Archipelago, Indonesia},\\n type = {article},\\n year = {2017},\\n keywords = {carbonate sediments, grain size, skeletal constitu},\\n pages = {1-13},\\n volume = {4},\\n websites = {http://journal.frontiersin.org/article/10.3389/fmars.2017.00144/full},\\n id = {c0dff020-5319-3fd2-93e8-d982132be5aa},\\n created = {2018-02-03T12:42:09.395Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-09-14T15:34:15.991Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Janßen2017a},\\n private_publication = {false},\\n bibtype = {article},\\n author = {Janßen, Alexander and Wizemann, André and Klicpera, André and Satari, Dewi Y. and Westphal, Hildegard and Mann, Thomas},\\n doi = {10.3389/fmars.2017.00144},\\n journal = {Frontiers in Marine Science},\\n number = {May}\\n}\",\"author_short\":[\"Janßen,  A.\",\"Wizemann,  A.\",\"Klicpera,  A.\",\"Satari,  D., Y.\",\"Westphal,  H.\",\"Mann,  T.\"],\"urls\":{\"Website\":\"http://journal.frontiersin.org/article/10.3389/fmars.2017.00144/full\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"janen-wizemann-klicpera-satari-westphal-mann-sedimentcompositionandfaciesofcoralreefislandsinthespermondearchipelagoindonesia-2017\",\"role\":\"author\",\"keyword\":[\"carbonate sediments\",\"grain size\",\"skeletal constitu\"],\"metadata\":{\"authorlinks\":{}},\"downloads\":0,\"html\":\"\"},{\"title\":\"The Mid-Pliocene sea-level conundrum: Glacial isostasy, eustasy and dynamic topography\",\"type\":\"article\",\"year\":\"2014\",\"keywords\":\"MEDFLOOD,PLIOMAX\",\"pages\":\"27-33\",\"volume\":\"387\",\"websites\":\"http://linkinghub.elsevier.com/retrieve/pii/S0012821X13006006,papers2://publication/doi/10.1016/j.epsl.2013.10.030\",\"publisher\":\"Elsevier B.V.\",\"day\":\"1\",\"id\":\"97905946-5bca-31d9-be05-3770c4ddacfc\",\"created\":\"2018-02-03T12:46:08.757Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.049Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Rovere2014f\",\"source_type\":\"JOUR\",\"private_publication\":false,\"abstract\":\"Determining eustatic sea level during the Mid-Pliocene warm period (~3.3 to 2.9 Ma) has been a central but elusive goal in the study of past warm climates. Estimates of eustatic sea level based on geologic data span a broad range; variation that we now recognize is due in part to geographically varying post-depositional displacement caused by glacial isostatic adjustment and dynamic topography. In this study, we combine field observations and glacial isostatic adjustment modeling to estimate the dynamic topography signal in three areas that are important to paleo-sea level studies of the Mid-Pliocene warm period (South Africa, West Australia and southeastern United States). We show that dynamic topography played a significant role in the post-depositional displacement of Pliocene, and even younger Pleistocene, shorelines. In this regard, we provide a robust paleo-sea level elevation data set, corrected for glacial isostatic adjustment, that can be used to evaluate predictions from mantle flow models of dynamic topography. © 2013 Elsevier B.V.\",\"bibtype\":\"article\",\"author\":\"Rovere, Alessio and Raymo, Maureen E and Mitrovica, Jerry X and Hearty, Paul J and O'Leary, M. J. and Inglis, J D\",\"doi\":\"10.1016/j.epsl.2013.10.030\",\"journal\":\"Earth and Planetary Science Letters\",\"bibtex\":\"@article{\\n title = {The Mid-Pliocene sea-level conundrum: Glacial isostasy, eustasy and dynamic topography},\\n type = {article},\\n year = {2014},\\n keywords = {MEDFLOOD,PLIOMAX},\\n pages = {27-33},\\n volume = {387},\\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0012821X13006006,papers2://publication/doi/10.1016/j.epsl.2013.10.030},\\n publisher = {Elsevier B.V.},\\n day = {1},\\n id = {97905946-5bca-31d9-be05-3770c4ddacfc},\\n created = {2018-02-03T12:46:08.757Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.049Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Rovere2014f},\\n source_type = {JOUR},\\n private_publication = {false},\\n abstract = {Determining eustatic sea level during the Mid-Pliocene warm period (~3.3 to 2.9 Ma) has been a central but elusive goal in the study of past warm climates. Estimates of eustatic sea level based on geologic data span a broad range; variation that we now recognize is due in part to geographically varying post-depositional displacement caused by glacial isostatic adjustment and dynamic topography. In this study, we combine field observations and glacial isostatic adjustment modeling to estimate the dynamic topography signal in three areas that are important to paleo-sea level studies of the Mid-Pliocene warm period (South Africa, West Australia and southeastern United States). We show that dynamic topography played a significant role in the post-depositional displacement of Pliocene, and even younger Pleistocene, shorelines. In this regard, we provide a robust paleo-sea level elevation data set, corrected for glacial isostatic adjustment, that can be used to evaluate predictions from mantle flow models of dynamic topography. © 2013 Elsevier B.V.},\\n bibtype = {article},\\n author = {Rovere, Alessio and Raymo, Maureen E and Mitrovica, Jerry X and Hearty, Paul J and O'Leary, M. J. and Inglis, J D},\\n doi = {10.1016/j.epsl.2013.10.030},\\n journal = {Earth and Planetary Science Letters}\\n}\",\"author_short\":[\"Rovere,  A.\",\"Raymo,  M., E.\",\"Mitrovica,  J., X.\",\"Hearty,  P., J.\",\"O'Leary,  M., J.\",\"Inglis,  J., D.\"],\"urls\":{\"Website\":\"http://linkinghub.elsevier.com/retrieve/pii/S0012821X13006006,papers2://publication/doi/10.1016/j.epsl.2013.10.030\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"rovere-raymo-mitrovica-hearty-oleary-inglis-themidpliocenesealevelconundrumglacialisostasyeustasyanddynamictopography-2014\",\"role\":\"author\",\"keyword\":[\"MEDFLOOD\",\"PLIOMAX\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/publications.html\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy)\",\"type\":\"article\",\"year\":\"2015\",\"keywords\":\"MIRAMAR,SEAMAP,SLCC\",\"pages\":\"278-286\",\"volume\":\"11\",\"websites\":\"http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134\",\"month\":\"6\",\"day\":\"24\",\"id\":\"c344b1c9-df37-392f-9269-db1a39f0056e\",\"created\":\"2018-02-03T12:46:08.766Z\",\"accessed\":\"2014-09-15\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2019-05-09T11:32:24.165Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Rovere2014\",\"private_publication\":false,\"abstract\":\"In this paper, we present a map describing the main geomorphological features of the coastal and marine area between the towns of Albenga and Savona (Ligurian Sea, NW Mediterranean) corresponding to a coastal stretch of ∼40 km. To produce this map, we collated data from the literature, orthophotos, perspective photos, multibeam and side scan sonar data, and undertook direct surveys to ground truth data obtained using indirect techniques. We divided the information into nine thematic layers, including bathymetry, natural coastal types, geomorphological elements, seafloor coverage (both geological and biological), coastal and nearshore dynamics, human influence on coastal and marine environments, coastal occupation and protected areas.\",\"bibtype\":\"article\",\"author\":\"Rovere, A. and Casella, E. and Vacchi, M. and Parravicini, V. and Firpo, M. and Ferrari, M. and Morri, C. and Bianchi, C. N.\",\"doi\":\"10.1080/17445647.2014.933134\",\"journal\":\"Journal of Maps\",\"number\":\"2\",\"bibtex\":\"@article{\\n title = {Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy)},\\n type = {article},\\n year = {2015},\\n keywords = {MIRAMAR,SEAMAP,SLCC},\\n pages = {278-286},\\n volume = {11},\\n websites = {http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134},\\n month = {6},\\n day = {24},\\n id = {c344b1c9-df37-392f-9269-db1a39f0056e},\\n created = {2018-02-03T12:46:08.766Z},\\n accessed = {2014-09-15},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2019-05-09T11:32:24.165Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Rovere2014},\\n private_publication = {false},\\n abstract = {In this paper, we present a map describing the main geomorphological features of the coastal and marine area between the towns of Albenga and Savona (Ligurian Sea, NW Mediterranean) corresponding to a coastal stretch of ∼40 km. To produce this map, we collated data from the literature, orthophotos, perspective photos, multibeam and side scan sonar data, and undertook direct surveys to ground truth data obtained using indirect techniques. We divided the information into nine thematic layers, including bathymetry, natural coastal types, geomorphological elements, seafloor coverage (both geological and biological), coastal and nearshore dynamics, human influence on coastal and marine environments, coastal occupation and protected areas.},\\n bibtype = {article},\\n author = {Rovere, A. and Casella, E. and Vacchi, M. and Parravicini, V. and Firpo, M. and Ferrari, M. and Morri, C. and Bianchi, C. N.},\\n doi = {10.1080/17445647.2014.933134},\\n journal = {Journal of Maps},\\n number = {2}\\n}\",\"author_short\":[\"Rovere,  A.\",\"Casella,  E.\",\"Vacchi,  M.\",\"Parravicini,  V.\",\"Firpo,  M.\",\"Ferrari,  M.\",\"Morri,  C.\",\"Bianchi,  C., N.\"],\"urls\":{\"Website\":\"http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-2015\",\"role\":\"author\",\"keyword\":[\"MIRAMAR\",\"SEAMAP\",\"SLCC\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/publications.html\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Coral reef structural complexity provides important coastal protection from waves under rising sea levels\",\"type\":\"article\",\"year\":\"2018\",\"pages\":\"eaao4350\",\"volume\":\"4\",\"websites\":\"http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.aao4350\",\"id\":\"c59b8d33-524b-3a4c-9af1-75c525bbf1b7\",\"created\":\"2018-03-12T08:49:53.423Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-09-14T15:34:15.877Z\",\"read\":false,\"starred\":\"true\",\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Harris2018a\",\"private_publication\":false,\"abstract\":\"Coral reefs are diverse ecosystems that support millions of people worldwide by providing coastal protection from waves.Climate change andhumanimpacts are leading todegraded coral reefs and to rising sea levels, posing concerns for the protection of tropical coastal regions in the near future. We use a wave dissipation model calibrated with empirical wave data to calculate the future increase of back-reef wave height. We showthat, in the near future, the structuralcomplexity of coral reefs ismore important than sea-level rise in determining the coastal protection provided by coral reefs from average waves. We also show that a significant increase in average wave heights could occur at present sea level if there is sustained degradation of benthic structural complexity. Our results highlight thatmaintain- ing the structural complexity of coral reefs is key to ensure coastal protection on tropical coastlines in the future.\",\"bibtype\":\"article\",\"author\":\"Harris, Daniel L. and Rovere, Alessio and Casella, Elisa and Power, Hannah and Canavesio, Remy and Collin, Antoine and Pomeroy, Andrew and Webster, Jody M. and Parravicini, Valeriano\",\"doi\":\"10.1126/sciadv.aao4350\",\"journal\":\"Science Advances\",\"number\":\"2\",\"bibtex\":\"@article{\\n title = {Coral reef structural complexity provides important coastal protection from waves under rising sea levels},\\n type = {article},\\n year = {2018},\\n pages = {eaao4350},\\n volume = {4},\\n websites = {http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.aao4350},\\n id = {c59b8d33-524b-3a4c-9af1-75c525bbf1b7},\\n created = {2018-03-12T08:49:53.423Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-09-14T15:34:15.877Z},\\n read = {false},\\n starred = {true},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Harris2018a},\\n private_publication = {false},\\n abstract = {Coral reefs are diverse ecosystems that support millions of people worldwide by providing coastal protection from waves.Climate change andhumanimpacts are leading todegraded coral reefs and to rising sea levels, posing concerns for the protection of tropical coastal regions in the near future. We use a wave dissipation model calibrated with empirical wave data to calculate the future increase of back-reef wave height. We showthat, in the near future, the structuralcomplexity of coral reefs ismore important than sea-level rise in determining the coastal protection provided by coral reefs from average waves. We also show that a significant increase in average wave heights could occur at present sea level if there is sustained degradation of benthic structural complexity. Our results highlight thatmaintain- ing the structural complexity of coral reefs is key to ensure coastal protection on tropical coastlines in the future.},\\n bibtype = {article},\\n author = {Harris, Daniel L. and Rovere, Alessio and Casella, Elisa and Power, Hannah and Canavesio, Remy and Collin, Antoine and Pomeroy, Andrew and Webster, Jody M. and Parravicini, Valeriano},\\n doi = {10.1126/sciadv.aao4350},\\n journal = {Science Advances},\\n number = {2}\\n}\",\"author_short\":[\"Harris,  D., L.\",\"Rovere,  A.\",\"Casella,  E.\",\"Power,  H.\",\"Canavesio,  R.\",\"Collin,  A.\",\"Pomeroy,  A.\",\"Webster,  J., M.\",\"Parravicini,  V.\"],\"urls\":{\"Website\":\"http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.aao4350\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"harris-rovere-casella-power-canavesio-collin-pomeroy-webster-etal-coralreefstructuralcomplexityprovidesimportantcoastalprotectionfromwavesunderrisingsealevels-2018\",\"role\":\"author\",\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/publications.html\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":1,\"html\":\"\"},{\"title\":\"MIS 5e relative sea-level changes in the Mediterranean Sea : Contribution of isostatic disequilibrium\",\"type\":\"article\",\"year\":\"2018\",\"pages\":\"122-134\",\"volume\":\"185\",\"websites\":\"https://doi.org/10.1016/j.quascirev.2018.01.004\",\"publisher\":\"Elsevier Ltd\",\"id\":\"96373c82-3999-3443-83f0-80ebf8af4bde\",\"created\":\"2018-04-19T09:43:34.364Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-09-14T15:34:15.974Z\",\"read\":\"true\",\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Stocchi2018c\",\"private_publication\":false,\"bibtype\":\"article\",\"author\":\"Stocchi, Paolo and Vacchi, Matteo and Lorscheid, Thomas and Boer, Bas De and Simms, Alexander R and Van de Wal, Roderik S and Vermeersen, Bert L A and Pappalardo, Marta and Rovere, Alessio\",\"doi\":\"10.1016/j.quascirev.2018.01.004\",\"journal\":\"Quaternary Science Reviews\",\"bibtex\":\"@article{\\n title = {MIS 5e relative sea-level changes in the Mediterranean Sea : Contribution of isostatic disequilibrium},\\n type = {article},\\n year = {2018},\\n pages = {122-134},\\n volume = {185},\\n websites = {https://doi.org/10.1016/j.quascirev.2018.01.004},\\n publisher = {Elsevier Ltd},\\n id = {96373c82-3999-3443-83f0-80ebf8af4bde},\\n created = {2018-04-19T09:43:34.364Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-09-14T15:34:15.974Z},\\n read = {true},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Stocchi2018c},\\n private_publication = {false},\\n bibtype = {article},\\n author = {Stocchi, Paolo and Vacchi, Matteo and Lorscheid, Thomas and Boer, Bas De and Simms, Alexander R and Van de Wal, Roderik S and Vermeersen, Bert L A and Pappalardo, Marta and Rovere, Alessio},\\n doi = {10.1016/j.quascirev.2018.01.004},\\n journal = {Quaternary Science Reviews}\\n}\",\"author_short\":[\"Stocchi,  P.\",\"Vacchi,  M.\",\"Lorscheid,  T.\",\"Boer,  B., D.\",\"Simms,  A., R.\",\"Van de Wal,  R., S.\",\"Vermeersen,  B., L., A.\",\"Pappalardo,  M.\",\"Rovere,  A.\"],\"urls\":{\"Website\":\"https://doi.org/10.1016/j.quascirev.2018.01.004\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"stocchi-vacchi-lorscheid-boer-simms-vandewal-vermeersen-pappalardo-etal-mis5erelativesealevelchangesinthemediterraneanseacontributionofisostaticdisequilibrium-2018\",\"role\":\"author\",\"metadata\":{\"authorlinks\":{}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Submerged reef terraces in the Maldivian Archipelago (Indian Ocean)\",\"type\":\"article\",\"year\":\"2018\",\"keywords\":\"Maldives,Multibeam bathymetry,Scuba diving,Submerged reef terraces\",\"pages\":\"218-232\",\"volume\":\"317\",\"websites\":\"https://doi.org/10.1016/j.geomorph.2018.05.026\",\"publisher\":\"Elsevier B.V.\",\"id\":\"624c972e-28f2-3894-ac6c-1bbcfe9f8e2e\",\"created\":\"2018-06-19T09:16:48.732Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-09-14T15:34:15.876Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Rovere2018c\",\"private_publication\":false,\"abstract\":\"Sea-level changes have shaped the world's carbonate platform margins and continental shelves, leaving typical geomorphic imprints, such as drowned reef terraces. In this paper, we present the results of 112 scuba diving transects across seven different Maldivian atolls and one multibeam survey around Malé Island, the capital of Maldives. We report on the occurrence of drowned reef terraces down to 120 m depth. In total, we identified six levels of submerged terraces that we consider as indicative of periods of time with stable or slowly rising sea level that can be attributed either to deceleration of the last deglacial sea-level rise or to Late Quaternary sea-level highstands. We compare our dataset to the depth of reef terraces reported globally, and we discuss the reasons why common global submerged terrace levels are difficult to identify in the field record.\",\"bibtype\":\"article\",\"author\":\"Rovere, Alessio and Khanna, Pankaj and Bianchi, Carlo Nike and Droxler, André W. and Morri, Carla and Naar, David F.\",\"doi\":\"10.1016/j.geomorph.2018.05.026\",\"journal\":\"Geomorphology\",\"bibtex\":\"@article{\\n title = {Submerged reef terraces in the Maldivian Archipelago (Indian Ocean)},\\n type = {article},\\n year = {2018},\\n keywords = {Maldives,Multibeam bathymetry,Scuba diving,Submerged reef terraces},\\n pages = {218-232},\\n volume = {317},\\n websites = {https://doi.org/10.1016/j.geomorph.2018.05.026},\\n publisher = {Elsevier B.V.},\\n id = {624c972e-28f2-3894-ac6c-1bbcfe9f8e2e},\\n created = {2018-06-19T09:16:48.732Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-09-14T15:34:15.876Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Rovere2018c},\\n private_publication = {false},\\n abstract = {Sea-level changes have shaped the world's carbonate platform margins and continental shelves, leaving typical geomorphic imprints, such as drowned reef terraces. In this paper, we present the results of 112 scuba diving transects across seven different Maldivian atolls and one multibeam survey around Malé Island, the capital of Maldives. We report on the occurrence of drowned reef terraces down to 120 m depth. In total, we identified six levels of submerged terraces that we consider as indicative of periods of time with stable or slowly rising sea level that can be attributed either to deceleration of the last deglacial sea-level rise or to Late Quaternary sea-level highstands. We compare our dataset to the depth of reef terraces reported globally, and we discuss the reasons why common global submerged terrace levels are difficult to identify in the field record.},\\n bibtype = {article},\\n author = {Rovere, Alessio and Khanna, Pankaj and Bianchi, Carlo Nike and Droxler, André W. and Morri, Carla and Naar, David F.},\\n doi = {10.1016/j.geomorph.2018.05.026},\\n journal = {Geomorphology}\\n}\",\"author_short\":[\"Rovere,  A.\",\"Khanna,  P.\",\"Bianchi,  C., N.\",\"Droxler,  A., W.\",\"Morri,  C.\",\"Naar,  D., F.\"],\"urls\":{\"Website\":\"https://doi.org/10.1016/j.geomorph.2018.05.026\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"rovere-khanna-bianchi-droxler-morri-naar-submergedreefterracesinthemaldivianarchipelagoindianocean-2018\",\"role\":\"author\",\"keyword\":[\"Maldives\",\"Multibeam bathymetry\",\"Scuba diving\",\"Submerged reef terraces\"],\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Very high resolution mapping of coral reef state using airborne bathymetric LiDAR surface-intensity and drone imagery\",\"type\":\"article\",\"year\":\"2018\",\"pages\":\"1-13\",\"volume\":\"00\",\"websites\":\"https://www.tandfonline.com/doi/full/10.1080/01431161.2018.1500072\",\"publisher\":\"Taylor & Francis\",\"id\":\"d7e17a9b-2188-3ee3-971f-15b820214d88\",\"created\":\"2018-07-24T12:51:35.662Z\",\"file_attached\":false,\"profile_id\":\"58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"group_id\":\"c506fd31-7f0e-3486-8ab7-d996efa2ef2a\",\"last_modified\":\"2018-09-14T15:34:15.965Z\",\"read\":false,\"starred\":false,\"authored\":false,\"confirmed\":\"true\",\"hidden\":false,\"citation_key\":\"Collin2018a\",\"private_publication\":false,\"bibtype\":\"article\",\"author\":\"Collin, Antoine and Ramambason, Camille and Pastol, Yves and Casella, Elisa and Rovere, Alessio and Thiault, Lauric and Espiau, Benoît and Siu, Gilles and Lerouvreur, Franck and Nakamura, Nao and Hench, James L. and Schmitt, Russell J. and Holbrook, Sally J. and Troyer, Matthias and Davies, Neil\",\"doi\":\"10.1080/01431161.2018.1500072\",\"journal\":\"International Journal of Remote Sensing\",\"number\":\"00\",\"bibtex\":\"@article{\\n title = {Very high resolution mapping of coral reef state using airborne bathymetric LiDAR surface-intensity and drone imagery},\\n type = {article},\\n year = {2018},\\n pages = {1-13},\\n volume = {00},\\n websites = {https://www.tandfonline.com/doi/full/10.1080/01431161.2018.1500072},\\n publisher = {Taylor & Francis},\\n id = {d7e17a9b-2188-3ee3-971f-15b820214d88},\\n created = {2018-07-24T12:51:35.662Z},\\n file_attached = {false},\\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\\n last_modified = {2018-09-14T15:34:15.965Z},\\n read = {false},\\n starred = {false},\\n authored = {false},\\n confirmed = {true},\\n hidden = {false},\\n citation_key = {Collin2018a},\\n private_publication = {false},\\n bibtype = {article},\\n author = {Collin, Antoine and Ramambason, Camille and Pastol, Yves and Casella, Elisa and Rovere, Alessio and Thiault, Lauric and Espiau, Benoît and Siu, Gilles and Lerouvreur, Franck and Nakamura, Nao and Hench, James L. and Schmitt, Russell J. and Holbrook, Sally J. and Troyer, Matthias and Davies, Neil},\\n doi = {10.1080/01431161.2018.1500072},\\n journal = {International Journal of Remote Sensing},\\n number = {00}\\n}\",\"author_short\":[\"Collin,  A.\",\"Ramambason,  C.\",\"Pastol,  Y.\",\"Casella,  E.\",\"Rovere,  A.\",\"Thiault,  L.\",\"Espiau,  B.\",\"Siu,  G.\",\"Lerouvreur,  F.\",\"Nakamura,  N.\",\"Hench,  J., L.\",\"Schmitt,  R., J.\",\"Holbrook,  S., J.\",\"Troyer,  M.\",\"Davies,  N.\"],\"urls\":{\"Website\":\"https://www.tandfonline.com/doi/full/10.1080/01431161.2018.1500072\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"collin-ramambason-pastol-casella-rovere-thiault-espiau-siu-etal-veryhighresolutionmappingofcoralreefstateusingairbornebathymetriclidarsurfaceintensityanddroneimagery-2018\",\"role\":\"author\",\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/publications.html\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":0,\"html\":\"\"},{\"title\":\"Coral reef structural complexity provides important coastal protection from waves under rising sea 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Although past intervals of warming were forced differently than future anthropogenic change, such periods can provide insights into potential future climate impacts and ecosystem feedbacks, especially over centennial-to-millennial timescales that are often not covered by climate model simulations. Our observation-based synthesis of the understanding of past intervals with temperatures within the range of projected future warming suggests that there is a low risk of runaway greenhouse gas feedbacks for global warming of no more than 2 °C. However, substantial regional environmental impacts can occur. A global average warming of 1–2 °C with strong polar amplification has, in the past, been accompanied by significant shifts in climate zones and the spatial distribution of land and ocean ecosystems. Sustained warming at this level has also led to substantial reductions of the Greenland and Antarctic ice sheets, with sea-level increases of at least several metres on millennial timescales. Comparison of palaeo observations with climate model results suggests that, due to the lack of certain feedback processes, model-based climate projections may underestimate long-term warming in response to future radiative forcing by as much as a factor of two, and thus may also underestimate centennial-to-millennial-scale sea-level rise.},\\n bibtype = {misc},\\n author = {Fischer, Hubertus and Meissner, Katrin J and Mix, Alan C and Abram, Nerilie J and Austermann, Jacqueline and Brovkin, Victor and Capron, Emilie and Colombaroli, Daniele and Daniau, Anne Laure and Dyez, Kelsey A and Felis, Thomas and Finkelstein, Sarah A and Jaccard, Samuel L and McClymont, Erin L and Rovere, Alessio and Sutter, Johannes and Wolff, Eric W and Affolter, Stéphane and Bakker, Pepijn and Ballesteros-Cánovas, Juan Antonio and Barbante, Carlo and Caley, Thibaut and Carlson, Anders E and Churakova, Olga and Cortese, Giuseppe and Cumming, Brian F and Davis, Basil A.S. and De Vernal, Anne and Emile-Geay, Julien and Fritz, Sherilyn C and Gierz, Paul and Gottschalk, Julia and Holloway, Max D and Joos, Fortunat and Kucera, Michal and Loutre, Marie France and Lunt, Daniel J and Marcisz, Katarzyna and Marlon, Jennifer R and Martinez, Philippe and Masson-Delmotte, Valerie and Nehrbass-Ahles, Christoph and Otto-Bliesner, Bette L and Raible, Christoph C and Risebrobakken, Bjørg and Sánchez Goñi, Mariá F. and Arrigo, Jennifer Saleem and Sarnthein, Michael and Sjolte, Jesper and Stocker, Thomas F and Velasquez Alvárez, Patricio A. and Tinner, Willy and Valdes, Paul J and Vogel, Hendrik and Wanner, Heinz and Yan, Qing and Yu, Zicheng and Ziegler, Martin and Zhou, Liping},\\n doi = {10.1038/s41561-018-0146-0}\\n}\",\"author_short\":[\"Fischer,  H.\",\"Meissner,  K., J.\",\"Mix,  A., C.\",\"Abram,  N., J.\",\"Austermann,  J.\",\"Brovkin,  V.\",\"Capron,  E.\",\"Colombaroli,  D.\",\"Daniau,  A., L.\",\"Dyez,  K., A.\",\"Felis,  T.\",\"Finkelstein,  S., A.\",\"Jaccard,  S., L.\",\"McClymont,  E., L.\",\"Rovere,  A.\",\"Sutter,  J.\",\"Wolff,  E., W.\",\"Affolter,  S.\",\"Bakker,  P.\",\"Ballesteros-Cánovas,  J., A.\",\"Barbante,  C.\",\"Caley,  T.\",\"Carlson,  A., E.\",\"Churakova,  O.\",\"Cortese,  G.\",\"Cumming,  B., F.\",\"Davis,  B., A.\",\"De Vernal,  A.\",\"Emile-Geay,  J.\",\"Fritz,  S., C.\",\"Gierz,  P.\",\"Gottschalk,  J.\",\"Holloway,  M., D.\",\"Joos,  F.\",\"Kucera,  M.\",\"Loutre,  M., F.\",\"Lunt,  D., J.\",\"Marcisz,  K.\",\"Marlon,  J., R.\",\"Martinez,  P.\",\"Masson-Delmotte,  V.\",\"Nehrbass-Ahles,  C.\",\"Otto-Bliesner,  B., L.\",\"Raible,  C., C.\",\"Risebrobakken,  B.\",\"Sánchez Goñi,  M., F.\",\"Arrigo,  J., S.\",\"Sarnthein,  M.\",\"Sjolte,  J.\",\"Stocker,  T., F.\",\"Velasquez Alvárez,  P., A.\",\"Tinner,  W.\",\"Valdes,  P., J.\",\"Vogel,  H.\",\"Wanner,  H.\",\"Yan,  Q.\",\"Yu,  Z.\",\"Ziegler,  M.\",\"Zhou,  L.\"],\"urls\":{\"Website\":\"file:///home/lmjong/Downloads/2018 - Natgeo - Fischer - PAGES palaeo constraints 2 degrees.pdf\"},\"biburl\":\"https://bibbase.org/service/mendeley/58d47d98-a4f4-3ac1-a79d-2d252a797376\",\"bibbaseid\":\"fischer-meissner-mix-abram-austermann-brovkin-capron-colombaroli-etal-palaeoclimateconstraintsontheimpactof2canthropogenicwarmingandbeyond-2018\",\"role\":\"author\",\"metadata\":{\"authorlinks\":{\"rovere, a\":\"https://alerov.weebly.com/\",\"rovere,  a\":\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\"}},\"downloads\":4,\"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; margin-right: 10px; margin-top: 10px; text-align: right; font-size: 12px\">\n    generated by\n    <a href=\"//bibbase.org\"\n       onclick=\"trackOutboundLink('bibbase', 'logo clicked', window.location.href, '//bibbase.org'); return false;\">\n      <img src=\"//bibbase.org/img/logo.svg\"\n           style=\"vertical-align: middle; margin-left: 3px; height: 16px;\"/\n           alt=\"bibbase.org\"\n           title=\"BibBase – The easiest way to maintain your publications page.\"\n        ></a>\n    \n  </div>\n  \n\n  <div id=\"bibbase_header\" class=\"dontprint\" style=\"\">\n\n    <ul class=\"nav nav-pills\" style=\"margin: 0px;\">\n\n      <li class=\"dropdown\" id=\"groupby_dropdown\">\n      <a class=\"dropdown-toggle\"\n         data-toggle=\"dropdown\"\n         href=\"#\">\n          Group by\n          <b class=\"caret\"></b>\n      </a>\n      <ul class=\"dropdown-menu\">\n        <li class=\"groupby year\"><a onclick=\"groupby('year')\">\n            Year</a>\n        </li>\n        <li class=\"groupby author\"><a onclick=\"groupby('author_short')\">\n            Author</a>\n        </li>\n        <li class=\"groupby type\"><a onclick=\"groupby('type')\">\n            Type</a>\n        </li>\n        <li class=\"groupby keyword\"><a onclick=\"groupby('keyword')\">\n            Keyword</a>\n        </li>\n        <li class=\"groupby downloads\"><a onclick=\"groupby('downloads')\">\n            Downloads</a>\n        </li>\n      </ul>\n      </li>\n\n\n      <li class=\"dropdown\" id=\"menu_dropdown\">\n      <a class=\"dropdown-toggle\"\n         data-toggle=\"dropdown\"\n         href=\"#\" alt=\"controls\">\n          <i class=\"fa fa-reorder\" alt=\"controls\"></i>\n          <b class=\"caret\"></b>\n      </a>\n      <ul class=\"dropdown-menu\">\n        <li>\n          <a onclick=\"toggleAll()\">\n            <i class=\"fa fa-chevron-down fa-fw\"></i> Expand/Collapse All\n          </a>\n        </li>\n        <li>\n          <a download=\"all.bib\" href=\"data:text/bibtex;base64,@article{
 title = {Paleo sea-level changes and relative sea-level indicators: Precise measurements, indicative meaning and glacial isostatic adjustment perspectives from Mallorca (Western Mediterranean)},
 type = {article},
 year = {2017},
 keywords = {Beach deposits,Last interglacial,MIS 5e,Morphodynamic modelling},
 pages = {94-107},
 volume = {473},
 websites = {http://linkinghub.elsevier.com/retrieve/pii/S0031018216303753},
 publisher = {Elsevier B.V.},
 id = {7abcfe9b-788b-39f2-8a80-0e128ce6d024},
 created = {2018-02-03T12:42:06.762Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:06.762Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Lorscheid2017},
 private_publication = {false},
 abstract = {Paleo relative sea-level (RSL) indicators formed during the Marine Isotope Stage (MIS) 5e have been reported by a large number of studies worldwide. Despite this, three main aspects are seldom reported: (1) use of high-precision survey techniques applied to MIS 5e RSL indicators; (2) application of modern analogs to understand the indicative meaning of MIS 5e RSL indicators; (3) estimates of the effects of glacial isostatic adjustment (GIA) on the MIS 5e records. In this study, we show how the three points above have been addressed in a focused study on Last Interglacial outcrops on the island of Mallorca. We measured the elevation of several RSL indicators with high-accuracy differential GPS (vertical accuracies down to 0.1 m) and we established the relationship between each RSL indicator and the paleo sea level through calculation of the indicative meaning for each RSL indicator. In particular, we present a novel technique to calculate the indicative meaning of fossil beach deposits with a phase-averaged morphodynamic model (CSHORE). We show how this approach helps overcoming difficulties with the survey of the modern analogs for these indicators. Our results show that two paleo RSLs are imprinted in Mallorca at + 2.9 ± 0.8 m and + 11.3 ± 1.0 m. We then compare our field-based results with modelled paleo RSL, calculated from the predictions of the ice-earth coupled ANICE-SELEN model, using few different ice-sheet melting scenarios during MIS 5e. We conclude that indicative ranges can be derived from relatively simple morphodynamic models and that the comparison of field-derived and modelled RSL values is a good method to validate possible scenarios of MIS 5e sea-level variability, especially in absence of precise dating.},
 bibtype = {article},
 author = {Lorscheid, Thomas and Stocchi, Paolo and Casella, Elisa and Gómez-Pujol, Lluis and Vacchi, Matteo and Mann, Thomas and Rovere, Alessio},
 doi = {10.1016/j.palaeo.2017.02.028},
 journal = {Palaeogeography, Palaeoclimatology, Palaeoecology}
}

@article{
 title = {Resilience of the Marine Animal Forest Lessons from Maldivian Coral Reefs After the Mass Mortality of 1998},
 type = {article},
 year = {2015},
 pages = {1-26},
 websites = {http://link.springer.com/10.1007/978-3-319-17001-5},
 publisher = {Springer International Publishing},
 city = {Cham},
 id = {659f5aa2-00c2-3abe-89b3-8922549dafff},
 created = {2018-02-03T12:42:06.776Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.068Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Bianchi2015},
 source_type = {inbook},
 private_publication = {false},
 abstract = {This chapter reviews the major known monospecific and multispecific sponge aggregations in the world’s oceans. They are shown to occur from the intertidal to abyssal depths, in tropical, temperate, and high latitudes and sometimes to create spectacular formations, such as glass sponge reefs, lithistid reef-like fields, and carnivorous sponge grounds. Sponge aggregations are recognized as singular vulnerable habitats that deserve special research attention and legal protection. However, this review reveals that there is only a poor and fragmentary under- standing of the main biological, environmental, and geochemical factors that favor and maintain these systems, including the food supply, which is funda- mental knowledge. There is also a particular lack of information regarding reproductive biology, growth rates, life spans, and the main factors causing mortality, all crucial drivers for understanding population and community dynamics and for developing conservation strategies. The sponge aggregations have been shown to increase the structural complexity of the habitats, attracting a larger variety of organisms and locally enhancing biodiversity. From the very few cases in which sponge biomass and sponge physiology have been reliably approached jointly, phenomenal fluxes of matter and energy have been inferred. Through their benthic-pelagic coupling, some of the densest sponge aggrega- tions have a significant local or regional impact on major biogeochemical cycles and food webs. Physical damage and habitat destruction derived from man-driven activities along with epidemic diseases facilitated by global envi- ronmental alterations emerge as major threats to the future of the sponge aggregations.},
 bibtype = {article},
 author = {Bianchi, Carlo Nike and Morri, Carla and Lasagna, Roberta and Montefalcone, Monica and Gatti, Giulia and Parravicini, Valeriano and Rovere, Alessio},
 editor = {Rossi, Sergio and Bramanti, Lorenzo and Gori, Andrea and del Valle, Covadonga},
 doi = {10.1007/978-3-319-17001-5},
 journal = {Marine Animal Forests}
}

@article{
 title = {Through bleaching and tsunami: Coral reef recovery in the Maldives},
 type = {article},
 year = {2015},
 keywords = {Coral reefs,Hard coral cover,Indian Ocean,Maldives,Recruitment,Resilience},
 pages = {188-200},
 volume = {98},
 websites = {http://linkinghub.elsevier.com/retrieve/pii/S0025326X15004178},
 publisher = {Elsevier Ltd},
 id = {d4572baa-b24e-34a7-8fb4-c42c41fe8b00},
 created = {2018-02-03T12:42:06.777Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.231Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Morri2015},
 private_publication = {false},
 abstract = {Coral reefs are degrading worldwide, but little information exists on their previous conditions for most regions of the world. Since 1989, we have been studying the Maldives, collecting data before, during and after the bleaching and mass mortality event of 1998. As early as 1999, many newly settled colonies were recorded. Recruits shifted from a dominance of massive and encrusting corals in the early stages of recolonisation towards a dominance of Acropora and Pocillopora by 2009. Coral cover, which dropped to less than 10% after the bleaching, returned to pre-bleaching values of around 50% by 2013. The 2004 tsunami had comparatively little effect. In 2014, the coral community was similar to that existing before the bleaching. According to descriptors and metrics adopted, recovery of Maldivian coral reefs took between 6 and 15. years, or may even be considered unachieved, as there are species that had not come back yet.},
 bibtype = {article},
 author = {Morri, Carla and Montefalcone, Monica and Lasagna, Roberta and Gatti, Giulia and Rovere, Alessio and Parravicini, Valeriano and Baldelli, Giuseppe and Colantoni, Paolo and Bianchi, Carlo Nike},
 doi = {10.1016/j.marpolbul.2015.06.050},
 journal = {Marine Pollution Bulletin},
 number = {1-2}
}

@article{
 title = {Multiproxy assessment of Holocene relative sea-level changes in the western Mediterranean: variability in the sea-level histories and redefinition of the isostatic signal.},
 type = {article},
 year = {2016},
 keywords = {Holocene,Isostatic adjustment,Mediterranean Sea,Sea-level database,Sea-level proxy},
 pages = {172-197},
 volume = {155},
 websites = {http://dx.doi.org/10.1016/j.earscirev.2016.02.002},
 publisher = {Elsevier B.V.},
 city = {Vienna, AT},
 id = {87ba1930-b220-369d-8afd-6fdf358bb6d5},
 created = {2018-02-03T12:42:07.277Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:07.277Z},
 read = {true},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Vacchi},
 private_publication = {false},
 abstract = {A review of 917 relative sea-level (RSL) data-points has resulted in the first quality-controlled database constraining the Holocene sea-level histories of the western Mediterranean Sea (Spain, France, Italy, Slovenia, Croatia, Malta and Tunisia). We reviewed and standardized the geological RSL data-points using a new multi-proxy methodology based on: (1) modern taxa assemblages in Mediterranean lagoons and marshes; (2) beachrock characteristics (cement fabric and chemistry, sedimentary structures); and (3) the modern distribution of Mediterranean fixed biological indicators. These RSL data-points were coupled with the large number of archaeological RSL indicators available for the western Mediterranean. We assessed the spatial variability of RSL histories for 22 regions and compared these with the ICE-5G (VM2) GIA model. In the western Mediterranean, RSL rose continuously for the whole Holocene with a sudden slowdown at ~. 7.5 ka BP and a further deceleration during the last ~. 4.0 ka BP, after which time observed RSL changes are mainly related to variability in isostatic adjustment. The sole exception is southern Tunisia, where data show evidence of a mid-Holocene high-stand compatible with the isostatic impacts of the melting history of the remote Antarctic ice sheet.Our results indicate that late-Holocene sea-level rise was significantly slower than the current one. First estimates of GIA contribution indicate that, at least in the northwestern sector, it accounts at least for the 25-30% of the ongoing sea-level rise recorded by Mediterranean tidal gauges. Such contribution is less constrained at lower latitudes due to the lower quality of the late Holocene index points. Future applications of spatio-temporal statistical techniques are required to better quantify the gradient of the isostatic contribution and to provide improved context for the assessment of 20th century acceleration of Mediterranean sea-level rise.},
 bibtype = {article},
 author = {Vacchi, Matteo and Marriner, Nick and Morhange, Christophe and Spada, Giorgio and Fontana, Alessandro and Rovere, Alessio and Marriner, Nick and Morhange, Christophe and Spada, Giorgio and Fontana, Alessandro},
 doi = {10.1016/j.earscirev.2016.02.002},
 journal = {Earth Science Reviews}
}

@article{
 title = {Late holocene sea-level fall and turn-off of reef flat carbonate production: Rethinking bucket fill and coral reef growth models},
 type = {article},
 year = {2015},
 pages = {1-4},
 volume = {43},
 websites = {http://geology.gsapubs.org/cgi/doi/10.1130/G35977.1},
 month = {1},
 day = {7},
 id = {c5ef7744-034e-35cd-a21c-3ccec602d2d1},
 created = {2018-02-03T12:42:07.282Z},
 accessed = {2015-01-14},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:07.282Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Harris2015b},
 private_publication = {false},
 abstract = {Relative sea-level rise has been a major factor driving the evolution of reef systems during the Holocene. Most models of reef evolution suggest that reefs preferentially grow vertically during rising sea level then laterally from windward to leeward, once the reef flat reaches sea level. Continuous lagoonal sedimentation ("bucket fill") and sand apron progradation eventually lead to reef systems with totally filled lagoons. Lagoonal infilling of One Tree Reef (southern Great Barrier Reef) through sand apron accretion was examined in the context of late Holocene relative sea-level change. This analysis was conducted using sedimentological and digital terrain data supported by 50 radiocarbon ages from fossil microatolls, buried patch reefs, foraminifera and shells in sediment cores, and recalibrated previously published radiocarbon ages. This data set challenges the conceptual model of geologically continuous sediment infill during the Holocene through sand apron accretion. Rapid sand apron accretion occurred between 6000 and 3000 calibrated yr before present B.P. (cal. yr B.P.); followed by only small amounts of sedimentation between 3000 cal. yr B.P. and present, with no significant sand apron accretion in the past 2 k.y. This hiatus in sediment infill coincides with a sea-level fall of [~]1-1.3 m during the late Holocene (ca. 2000 cal. yr B.P.), which would have caused the turn-off of highly productive live coral growth on the reef flats currently dominated by less productive rubble and algal flats, resulting in a reduced sediment input to back-reef environments and the cessation in sand apron accretion. Given that relative sea-level variations of [~]1 m were common throughout the Holocene, we suggest that this mode of sand apron development and carbonate production is applicable to most reef systems.},
 bibtype = {article},
 author = {Harris, Daniel L. and Webster, Jody M. and Vila-Concejo, Ana and Hua, Quan and Yokoyama, Yusuke and Reimer, Paula J.},
 doi = {10.1130/G35977.1},
 journal = {Geology},
 number = {2},
 keywords = {SLCC}
}

@article{
 title = {Spatial variations in wave transformation and sediment entrainment on a coral reef sand apron},
 type = {article},
 year = {2015},
 pages = {220-229},
 volume = {363},
 publisher = {Elsevier},
 id = {57b0685a-c7b7-348e-834e-0ab865e8b817},
 created = {2018-02-03T12:42:07.347Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:07.347Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {harris2015spatial},
 source_type = {article},
 private_publication = {false},
 bibtype = {article},
 author = {Harris, D L and Vila-Concejo, A and Webster, J M and Power, H E},
 journal = {Marine Geology}
}

@article{
 title = {Influence of hydrodynamic energy on Holocene reef flat accretion, Great Barrier Reef},
 type = {article},
 year = {2016},
 keywords = {Accretion,Great Barrier Reef,Holocene,Reef growth,Sea level,Still-stand},
 pages = {44-53},
 volume = {85},
 id = {80f43001-f620-38f0-834d-7973e06d9e9f},
 created = {2018-02-03T12:42:07.847Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:07.847Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Dechnik2016},
 private_publication = {false},
 abstract = {The response of platform reefs to sea-level stabilization over the past 6 ka is well established for the Great Barrier Reef (GBR), with reefs typically accreting laterally from windward to leeward. However, these observations are based on few cores spread across reef zones and may not accurately reflect a reef's true accretional response to the Holocene stillstand. We present a new record of reef accretion based on 49 U/Th ages from Heron and One Tree reefs in conjunction with re-analyzed data from 14 reefs across the GBR. We demonstrate that hydrodynamic energy is the main driver of accretional direction; exposed reefs accreted primarily lagoon-ward while protected reefs accreted seawards, contrary to the traditional growth model in the GBR. Lateral accretion rates varied from 86.3 m/ka-42.4 m/ka on the exposed One Tree windward reef and 68.35 m/ka-15.7 m/ka on the protected leeward Heron reef, suggesting that wind/wave energy is not a dominant control on lateral accretion rates. This represents the most comprehensive statement of lateral accretion direction and rates from the mid-outer platform reefs of the GBR, confirming great variability in reef flat growth both within and between reef margins over the last 6 ka, and highlighting the need for closely-spaced transects.},
 bibtype = {article},
 author = {Dechnik, Belinda and Webster, Jody M. and Nothdurft, Luke and Webb, Gregory E. and Zhao, Jian xin and Duce, Stephanie and Braga, Juan C. and Harris, Daniel L. and Vila-Concejo, Ana and Puotinen, Marji},
 doi = {10.1016/j.yqres.2015.11.002},
 journal = {Quaternary Research (United States)},
 number = {1}
}

@article{
 title = {A review of the MIS 5e highstand deposits from Santa Maria Island (Azores, NE Atlantic): Palaeobiodiversity, palaeoecology and palaeobiogeography},
 type = {article},
 year = {2015},
 keywords = {SLCC},
 pages = {126-148},
 volume = {114},
 id = {18675fe6-ef04-3b2a-80ad-0a12239f3f49},
 created = {2018-02-03T12:42:07.872Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.296Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Avila2015},
 private_publication = {false},
 abstract = {The privileged location of Santa Maria Island (Azores archipelago) in the middle of the North Atlantic makes the fossiliferous outcrops on this island of utmost importance to gain a better understanding of how coeval living communities relate to the broader evolutionary and biogeographic history of the Atlantic basin during the late Neogene and the Quaternary. Here we focus on this island's MIS 5e fossil record, offering a comprehensive review on the palaeobiodiversity, palaeoecology and palaeobiogeography of the biota living in the mid North Atlantic during this interglacial. Several studies in oceanic islands stress the huge impact of sea level changes on insular communities. Pleistocene sea-level changes occur during the short-time events known as "Terminations" (associated to glacial/interglacial shifts) as well as with the onset of glaciations (associated to interglacial/glacial shifts). Both are responsible for extinctions and local disappearance of species, bottleneck effects and formation of new species, resulting in community structure changes. This work increases the number of fossil marine taxa reported from the Last Interglacial deposits of Santa Maria to 143 species. All the 19 new records are molluscs (13 gastropods and 6 bivalves), thus increasing the number of fossil molluscs to 136 species. Although thermophilic members of the "Senegalese" tropical fauna were found in these deposits, many of the most emblematic species (e.g., Persististrombus latus (= Strombus bubonius), Cymbula safiana, Harpa doris, Cardita senegalensis, Barbatia plicata, Ctena eburnea or Hyotissa hyotis) are absent, suggesting that they did not reach the Azores. Our results indicate that the main differences between the species composition of the MIS 5e and the present-day shallow-water Azorean communities are probably due to the dropping of sea surface temperature associated with the onset of the last glaciation, which had both direct and indirect effects on species ecology. A group of 21 thermophilic species was directly affected by the lower sea surface temperature, whereas a group of four sand-associated species was indirectly but similarly affected by the lowering of the sea level. Both groups have locally disappeared from the Azores. However, none of the extant endemic species found on the studied MIS 5e outcrops was apparently affected by the lowering SST. In contrast to the biogeographical relationships of the recent Azorean shallow marine molluscs, which are predominantly with the Mediterranean Region, Portugal and with the Madeira and Canary Islands archipelagos, the palaeobiogeographical relationships of the MIS 5e Azorean marine molluscs are mainly with Canaries and West Africa. Despite the general low similarity of the biogeographical relationships between the Azores and Cape Verde Archipelago, on both the recent and the MIS 5e analysis, this similarity is nevertheless higher for the MIS 5e mollusc assemblages, emphasizing the role of Cape Verde as an important source of warm-water species during the Last Interglacial.},
 bibtype = {article},
 author = {Ávila, Sérgio P. and Melo, Carlos and Silva, Luís and Ramalho, Ricardo S. and Quartau, Rui and Hipólito, Ana and Cordeiro, Ricardo and Rebelo, Ana Cristina and Madeira, Patrícia and Rovere, Alessio and Hearty, Paul J. and Henriques, Diamantino and Silva, Carlos Marques da and Martins, António M.de Frias and Zazo, Caridad},
 doi = {10.1016/j.quascirev.2015.02.012},
 journal = {Quaternary Science Reviews}
}

@article{
 title = {Budget of Primary Production and Dinitrogen Fixation in a Highly Seasonal Red Sea Coral Reef},
 type = {article},
 year = {2016},
 keywords = {Biogeochemical cycling,Diazotrophy,Gulf of Aqaba,Nutrient budget,Photosynthesis,Productivity},
 pages = {771-785},
 volume = {19},
 id = {89d9bbe3-e931-365f-9e12-f705ba1067e4},
 created = {2018-02-03T12:42:07.876Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.109Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Cardini},
 private_publication = {false},
 abstract = {Biological dinitrogen (N2) fixation (diazotrophy, BNF) relieves marine primary producers of nitrogen (N) limitation in a large part of the world oceans. N concentrations are particularly low in tropical regions where coral reefs are located, and N is therefore a key limiting nutrient for these productive ecosystems. In this context, the importance of diazotrophy for reef productivity is still not resolved, with studies up to now lacking organismal and seasonal resolution. Here, we present a budget of gross primary production (GPP) and BNF for a highly seasonal Red Sea fringing reef, based on ecophysiological and benthic cover measurements combined with geospatial analyses. Benthic GPP varied from 215 to 262 mmol C m -2 reef d-1, with hard corals making the largest contribution (41-76%). Diazotrophy was omnipresent in space and time, and benthic BNF varied from 0.16 to 0.92 mmol N m-2 reef d-1. Planktonic GPP and BNF rates were respectively approximately 60- and 20-fold lower than those of the benthos, emphasizing the importance of the benthic compartment in reef biogeochemical cycling. BNF showed higher sensitivity to seasonality than GPP, implying greater climatic control on reef BNF. Up to about 20% of net reef primary production could be supported by BNF during summer, suggesting a strong biogeochemical coupling between diazotrophy and the reef carbon cycle. Details},
 bibtype = {article},
 author = {Cardini, Ulisse and Bednarz, Vanessa N. and van Hoytema, Nanne and Rovere, Alessio and Naumann, Malik S. and Al-Rshaidat, Mamoon M.D. and Wild, Christian},
 doi = {10.1007/s10021-016-9966-1},
 journal = {Ecosystems},
 number = {5}
}

@article{
 title = {Late Quaternary sea-level changes and early human societies in the central and eastern Mediterranean Basin: An interdisciplinary review},
 type = {article},
 year = {2017},
 keywords = {Holocene,Mediterranean Archaeology,Pleistocene,Sea-level change},
 pages = {29-57},
 volume = {449},
 websites = {http://linkinghub.elsevier.com/retrieve/pii/S1040618216310928,http://dx.doi.org/10.1016/j.quaint.2017.06.025},
 publisher = {Elsevier Ltd},
 id = {62fca5b4-ded4-330a-a54f-ce02c6217d33},
 created = {2018-02-03T12:42:07.907Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:07.907Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Benjamin2017},
 private_publication = {false},
 abstract = {This article reviews key data and debates focused on relative sea-level changes since the Last Interglacial (approximately the last 132,000 years) in the Mediterranean Basin, and their implications for past human populations. Geological and geomorphological landscape studies are critical to archaeology. Coastal regions provide a wide range of resources to the populations that inhabit them. Coastal landscapes are increasingly the focus of scholarly discussions from the earliest exploitation of littoral resources and early hominin cognition, to the inundation of the earliest permanently settled fishing villages and eventually, formative centres of urbanisation. In the Mediterranean, these would become hubs of maritime transportation that gave rise to the roots of modern seaborne trade. As such, this article represents an original review of both the geo-scientific and archaeological data that specifically relate to sea-level changes and resulting impacts on both physical and cultural landscapes from the Palaeolithic until the emergence of the Classical periods. Our review highlights that the interdisciplinary links between coastal archaeology, geomorphology and sea-level changes are important to explain environmental impacts on coastal human societies and human migration. We review geological indicators of sea level and outline how archaeological features are commonly used as proxies for measuring past sea levels, both gradual changes and catastrophic events. We argue that coastal archaeologists should, as a part of their analyses, incorporate important sea-level concepts, such as indicative meaning. The interpretation of the indicative meaning of Roman fishtanks, for example, plays a critical role in reconstructions of late Holocene Mediterranean sea levels. We identify avenues for future work, which include the consideration of glacial isostatic adjustment (GIA) in addition to coastal tectonics to explain vertical movements of coastlines, more research on Palaeolithic island colonisation, broadening of Palaeolithic studies to include materials from the entire coastal landscape and not just coastal resources, a focus on rescue of archaeological sites under threat by coastal change, and expansion of underwater archaeological explorations in combination with submarine geomorphology. This article presents a collaborative synthesis of data, some of which have been collected and analysed by the authors, as the MEDFLOOD (MEDiterranean sea-level change and projection for future FLOODing) community, and highlights key sites, data, concepts and ongoing debates.},
 bibtype = {article},
 author = {Benjamin, J. and Rovere, A. and Fontana, A. and Furlani, S. and Vacchi, M. and Inglis, R.H. H. and Galili, E. and Antonioli, F. and Sivan, D. and Miko, S. and Mourtzas, N. and Felja, I. and Meredith-Williams, M. and Goodman-Tchernov, B. and Kolaiti, E. and Anzidei, M. and Gehrels, R.},
 doi = {10.1016/j.quaint.2017.06.025},
 journal = {Quaternary International}
}

@article{
 title = {Giant boulders and Last Interglacial storm intensity in the North Atlantic},
 type = {article},
 year = {2017},
 keywords = {Eemian,Last Interglacial,climate change,extreme waves,superstorms},
 pages = {201712433},
 volume = {114},
 websites = {http://www.ncbi.nlm.nih.gov/pubmed/29087331,http://www.pnas.org/lookup/doi/10.1073/pnas.1712433114},
 month = {10},
 publisher = {National Academy of Sciences},
 day = {30},
 id = {3d249fd7-0f67-34cd-9597-134e27ac4b8c},
 created = {2018-02-03T12:42:07.914Z},
 accessed = {2017-11-10},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:07.914Z},
 read = {true},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Rovere2017},
 private_publication = {false},
 abstract = {As global climate warms and sea level rises, coastal areas will be subject to more frequent extreme flooding and hurricanes. Geologic evidence for extreme coastal storms during past warm periods has the potential to provide fundamental insights into their future intensity. Recent studies argue that during the Last Interglacial (MIS 5e, ∼128-116 ka) tropical and extratropical North Atlantic cyclones may have been more intense than at present, and may have produced waves larger than those observed historically. Such strong swells are inferred to have created a number of geologic features that can be observed today along the coastlines of Bermuda and the Bahamas. In this paper, we investigate the most iconic among these features: massive boulders atop a cliff in North Eleuthera, Bahamas. We combine geologic field surveys, wave models, and boulder transport equations to test the hypothesis that such boulders must have been emplaced by storms of greater-than-historical intensity. By contrast, our results suggest that with the higher relative sea level (RSL) estimated for the Bahamas during MIS 5e, boulders of this size could have been transported by waves generated by storms of historical intensity. Thus, while the megaboulders of Eleuthera cannot be used as geologic proof for past "superstorms," they do show that with rising sea levels, cliffs and coastal barriers will be subject to significantly greater erosional energy, even without changes in storm intensity.},
 bibtype = {article},
 author = {Rovere, Alessio and Casella, Elisa and Harris, Daniel L. and Lorscheid, Thomas and Nandasena, Napayalage A. K. and Dyer, Blake and Sandstrom, Michael R. and Stocchi, Paolo and D’Andrea, William J. and Raymo, Maureen E.},
 doi = {10.1073/pnas.1712433114},
 journal = {Proceedings of the National Academy of Sciences},
 number = {46}
}

@article{
 title = {Mapping coral reefs using consumer-grade drones and structure from motion photogrammetry techniques},
 type = {article},
 year = {2017},
 keywords = {Bathymetry from drones,Bathymetry from photogrammetry,Coral reefs,Drone mapping,Structure from motion underwater},
 pages = {269-275},
 volume = {36},
 websites = {http://link.springer.com/10.1007/s00338-016-1522-0},
 publisher = {Springer Berlin Heidelberg},
 id = {014c2903-534c-38d9-8cc6-397276ea0084},
 created = {2018-02-03T12:42:07.996Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:07.996Z},
 read = {true},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Casella2016},
 private_publication = {false},
 abstract = {We propose a novel technique to measure the small-scale three-dimensional features of a shallow-water coral reef using a small drone equipped with a consumer-grade camera, a handheld GPS and structure from motion (SfM) algorithms. We used a GoPro HERO4 with a modified lens mounted on a DJI Phantom 2 drone (maximum total take-off weight <2 kg) to perform a 10 min flight and collect 306 aerial images with an overlap equal or greater than 90%. We mapped an area of 8380 m2, obtaining as output an ortho-rectified aerial photomosaic and a bathymetric digital elevation model (DEM) with a resolution of 0.78 and 1.56 cm pixel−1, respectively. Through comparison with airborne LiDAR data for the same area, we verified that the location of the ortho-rectified aerial photomosaic is accurate within ~1.4 m. The bathymetric difference between our DEM and the LiDAR dataset is −0.016 ± 0.45 m (1σ). Our results show that it is possible, in conditions of calm waters, low winds and minimal sun glint, to deploy consumer-grade drones as a relatively low-cost and rapid survey technique to produce multispectral and bathymetric data on shallow-water coral reefs. We discuss the utility of such data to monitor temporal changes in topographic complexity of reefs and associated biological processes.},
 bibtype = {article},
 author = {Casella, Elisa and Collin, Antoine and Harris, Daniel and Ferse, Sebastian and Bejarano, Sonia and Parravicini, Valeriano and Hench, James L. and Rovere, Alessio},
 doi = {10.1007/s00338-016-1522-0},
 journal = {Coral Reefs},
 number = {1}
}

@article{
 title = {Tidal notches in Mediterranean Sea: A comprehensive analysis},
 type = {article},
 year = {2015},
 keywords = {MEDFLOOD,SLCC},
 pages = {66-84},
 volume = {119},
 websites = {http://linkinghub.elsevier.com/retrieve/pii/S0277379115001237},
 id = {d4ca0132-0793-3a00-9ab0-363e0f46f1a1},
 created = {2018-02-03T12:42:08.494Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.034Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Antonioli2015},
 private_publication = {false},
 abstract = {Recent works (Evelpidou et al., 2012) suggest that the modern tidal notch is disappearing worldwide due sea level rise over the last century. In order to assess this hypothesis, we measured modern tidal notches in several of sites along the Mediterranean coasts. We report observations on tidal notches cut along carbonate coasts from 73 sites from Italy, France, Croatia, Montenegro, Greece, Malta and Spain, plus additional observations carried outside the Mediterranean. At each site, we measured notch width and depth, and we described the characteristics of the biological rim at the base of the notch. We correlated these parameters with wave energy, tide gauge datasets and rock lithology.Our results suggest that, considering 'the development of tidal notches the consequence of midlittoral bioerosion' (as done in Evelpidou et al., 2012) is a simplification that can lead to misleading results, such as stating that notches are disappearing. Important roles in notch formation can be also played by wave action, rate of karst dissolution, salt weathering and wetting and drying cycles. Of course notch formation can be augmented and favoured also by bioerosion which can, in particular cases, be the main process of notch formation and development.Our dataset shows that notches are carved by an ensemble rather than by a single process, both today and in the past, and that it is difficult, if not impossible, to disentangle them and establish which one is prevailing. We therefore show that tidal notches are still forming, challenging the hypothesis that sea level rise has drowned them.},
 bibtype = {article},
 author = {Antonioli, Fabrizio and Lo Presti, Valeria and Rovere, Alessio and Ferranti, Luigi and Anzidei, Marco and Furlani, Stefano and Mastronuzzi, Giuseppe and Orru, Paolo E. and Scicchitano, Giovanni and Sannino, Gianmaria and Spampinato, Cecilia R. and Pagliarulo, Rossella and Deiana, Giacomo and de Sabata, Eleonora and Sansò, Paolo and Vacchi, Matteo and Vecchio, Antonio},
 doi = {10.1016/j.quascirev.2015.03.016},
 journal = {Quaternary Science Reviews},
 number = {5}
}

@article{
 title = {Eustatic and Relative Sea Level Changes},
 type = {article},
 year = {2016},
 keywords = {Eustasy,GIA,Isost,Isostasy,Relative sea level,Sea level,Sea level changes,eustasy,gia,isostasy,of the topical collection,on sea level projections,relative sea level,sea level,sea level changes,this article is part},
 pages = {221-231},
 volume = {2},
 websites = {http://link.springer.com/10.1007/s40641-016-0045-7,http://dx.doi.org/10.1007/s40641-016-0045-7},
 month = {12},
 publisher = {Current Climate Change Reports},
 day = {2},
 id = {2e5440fd-63cc-31d6-82b6-b5a3be4b490c},
 created = {2018-02-03T12:42:08.574Z},
 accessed = {2017-04-19},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:08.574Z},
 read = {true},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Rovere2016},
 source_type = {article},
 private_publication = {false},
 abstract = {Sea level changes can be driven by either variations in the masses or volume of the oceans, or by changes of the land with respect to the sea surface. In the first case, a sea level change is defined `eustatic'; otherwise, it is defined `relative'. Several techniques can be used to observe changes in sea level, from satellite data to tide gauges to geological or archeological proxies. Regardless of the technique used, `eustasy' cannot be measured directly, but only calculated after perturbing factors of different origins are taken into account. In this paper, we review the meaning and main processes that contribute to eustatic and relative sea level changes, and we give an overview of the different techniques used to observe them.},
 bibtype = {article},
 author = {Rovere, Alessio and Stocchi, Paolo and Vacchi, Matteo},
 doi = {10.1007/s40641-016-0045-7},
 journal = {Current Climate Change Reports},
 number = {4}
}

@article{
 title = {Ecological Change, Sliding Baselines and the Importance of Historical Data: Lessons from Combing Observational and Quantitative Data on a Temperate Reef Over 70 Years},
 type = {article},
 year = {2015},
 pages = {e0118581},
 volume = {10},
 websites = {http://dx.plos.org/10.1371/journal.pone.0118581},
 id = {8b916ab6-383a-3a2a-9b7b-996ec73ff016},
 created = {2018-02-03T12:42:08.689Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.170Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Gatti2015},
 private_publication = {false},
 abstract = {Understanding the effects of environmental change on ecosystems requires the identifica- tion of baselines that may act as reference conditions. However, the continuous change of these references challenges our ability to define the true natural status of ecosystems. The so-called sliding baseline syndrome can be overcome through the analysis of quantitative time series, which are, however, extremely rare. Here we show how combining historical quantitative data with descriptive ‘naturalistic’ information arranged in a chronological chain allows highlighting long-term trends and can be used to inform present conservation schemes.We analysed the long-term change of a coralligenous reef, a marine habitat en- demic to the Mediterranean Sea. The coralligenous assemblages of Mesco Reef (Ligurian Sea,NWMediterranean) have been studied, although discontinuously, since 1937 thus making available both detailed descriptive information and scanty quantitative data: while the former was useful to understand the natural history of the ecosystem, the analysis of the latter was of paramount importance to provide a formal measure of change over time. Epi- benthic assemblages remained comparatively stable until the 1990s, when species re- placement, invasion by alien algae, and biotic homogenisation occurred within few years, leading to a new and completely different ecosystem state. The shift experienced by the cor- alligenous assemblages of Mesco Reef was probably induced by a combination of seawa- ter warming and local human pressures, the latter mainly resulting in increased water turbidity; in turn, cumulative stress may have favoured the establishment of alien species. This study showed that the combined analysis of quantitative and descriptive historical data represent a precious knowledge to understand ecosystem trends over time and provide help to identify baselines for ecological management.},
 bibtype = {article},
 author = {Gatti, Giulia and Bianchi, Carlo Nike and Parravicini, Valeriano and Rovere, Alessio and Peirano, Andrea and Montefalcone, Monica and Massa, Francesco and Morri, Carla},
 doi = {10.1371/journal.pone.0118581},
 journal = {Plos One},
 keywords = {SLCC}
}

@article{
 title = {Mid-Pliocene shorelines of the US Atlantic Coastal Plain — An improved elevation database with comparison to Earth model predictions},
 type = {article},
 year = {2015},
 keywords = {MEDFLOOD,PLIOMAX,SLCC},
 pages = {117-131},
 volume = {145},
 websites = {http://linkinghub.elsevier.com/retrieve/pii/S0012825215000355,http://www.scopus.com/inward/record.url?eid=2-s2.0-84926164528&partnerID=tZOtx3y1},
 publisher = {Elsevier B.V.},
 id = {7c02f629-e8ca-3a22-9339-70cd0d5fd1b8},
 created = {2018-02-03T12:42:08.744Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.267Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Rovere2015},
 private_publication = {false},
 abstract = {For nearly a century, the Atlantic Coastal Plain (ACP) of the United States has been the focus of studies investigating Pliocene and Pleistocene shorelines, however, the mapping of paleoshorelines was primarily done by using elevation contours on topographic maps. Here we review published geologic maps and compare them to paleoshoreline locations obtained through geomorphometric classification and satellite data. We furthermore present the results of an extensive field campaign that measured the mid-Pliocene (~. 3.3-2.9. Ma) shorelines of the Atlantic Coastal Plain using high-accuracy GPS and digital elevation models. We compare our new dataset to positions and elevations extracted from published maps and find that the extracted site information from earlier studies is prone to significant error, both in the location and, more severely, in the elevation of the paleoshoreline. We also investigate, using geophysical modeling, the origin of post-depositional displacement of the shoreline from Georgia to Virginia. In particular, we correct the elevation of our shoreline for glacial isostatic adjustment (GIA) and then compare the corrected elevation to predictions of mantle flow-induced dynamic topography (DT). While a subset of these models does reconcile the general trends in the observed elevation of the mid-Pliocene shoreline, local discrepancies persist. These discrepancies suggests that either (i) the DT and GIA models presented here do not capture the full range of uncertainty in the input parameters; and/or (ii) other influences, such as sediment loading and unloading or local fault-driven tectonics, may have contributed to post-depositional deformation of the mid-Pliocene shoreline that are not captured in the above models. In this context, our field measurements represent an important observational dataset with which to compare future generations of geodynamic models. Improvements in models for DT, GIA and other relevant processes, together with an expanded, geographically distributed set of shoreline records, will ultimately be the key to obtaining more accurate estimates of eustatic sea level not only in the mid-Pliocene but also earlier in the Cenozoic.},
 bibtype = {article},
 author = {Rovere, Alessio and Hearty, P.J. and Austermann, J. and Mitrovica, J.X. and Gale, J. and Moucha, R. and Forte, A.M. and Raymo, M.E.},
 doi = {10.1016/j.earscirev.2015.02.007},
 journal = {Earth-Science Reviews}
}

@article{
 title = {The magnitude of a mid-Holocene sea-level highstand in the Strait of Makassar},
 type = {article},
 year = {2016},
 keywords = {Glacial isostatic adjustment,Indo-Pacific,Spermonde Shelf,Sulawesi},
 pages = {155-163},
 volume = {257},
 websites = {http://www.sciencedirect.com/science/article/pii/S0169555X15302427,http://dx.doi.org/10.1016/j.geomorph.2015.12.023},
 publisher = {Elsevier B.V.},
 id = {9954079d-a126-3204-9852-4918ab7f9b80},
 created = {2018-02-03T12:42:08.888Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:08.888Z},
 read = {true},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {mann2015magnitude},
 source_type = {article},
 private_publication = {false},
 abstract = {Knowledge on the timing and magnitude of past sea-level changes is essential to understand modern and future sea-level variability. Holocene sea-level data from literature on the west coast of Sulawesi, central Indonesia, suggest that this region experienced two relative sea-level highstands over the last 6000years, with magnitudes exceeding two meters. However, recent datasets from the Indo-Pacific region do not support high-magnitude sea-level oscillations during the Holocene in tectonically stable far-field locations. Here we present a new, high-precision, mid-Holocene sea-level dataset from the Spermonde Shelf off southwest Sulawesi. We surveyed 21 fossil microatolls on the reef flats of two coral islands (Pulau Panambungan and Pulau Barrang Lompo) and referred their elevations to local mean sea level and to the height of living coral. Radiometrically calibrated ages from emergent fossil microatolls on Pulau Panambungan indicate a relative sea-level highstand not exceeding 0.5m above present at ca. 5600cal.yrBP. The highstand is followed by a relatively rapid sea-level fall towards present sea level that was reached at around 4000cal.yrBP. Fossil microatolls from nearby Pulau Barrang Lompo show the same trend, however with a coherent negative vertical offset of about 0.8m compared to their equivalents on Pulau Panambungan. The largely consistent gradients of both trends (~−0.14mmyr−1), the consistent elevation of living microatolls in the Spermonde, and a number of instructive geomorphic features indicate a localized, post-formational and probably recent drop of the fossil microatolls on the densely populated island Pulau Barrang Lompo. The relative sea-level trend inferred from Pulau Panambungan is well within the range of geophysical predictions based on ANICE-SELEN ice sheet model, which predict a highstand that is significantly lower than those predicted by other GIA models for this area. Although a complete interpretation of the Holocene sea-level history will require additional high-resolution datasets from this and surrounding territories in SE Asia, our results suggest that there was merely a single Holocene highstand in central Indonesia, the magnitude of which was substantially lower than hitherto assumed.},
 bibtype = {article},
 author = {Mann, Thomas and Rovere, Alessio and Schöne, Tilo and Klicpera, André and Stocchi, Paolo and Lukman, Muhammad and Westphal, Hildegard},
 doi = {10.1016/j.geomorph.2015.12.023},
 journal = {Geomorphology}
}

@article{
 title = {Palaeo-sea-level and palaeo-ice-sheet databases: problems, strategies, and perspectives},
 type = {article},
 year = {2016},
 pages = {911-921},
 volume = {12},
 websites = {http://www.clim-past.net/12/911/2016/},
 id = {8ca5dd97-7c80-38c9-a445-f8daef1ce5b3},
 created = {2018-02-03T12:42:08.890Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:08.890Z},
 read = {true},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Dusterhus2016},
 private_publication = {false},
 abstract = {<p>Sea-level and ice-sheet databases have driven numerous advances in understanding the Earth system. We describe the challenges and offer best strategies that can be adopted to build self-consistent and standardised databases of geological and geochemical information used to archive palaeo-sea-levels and palaeo-ice-sheets. There are three phases in the development of a database: (i) measurement, (ii) interpretation, and (iii) database creation. Measurement should include the objective description of the position and age of a sample, description of associated geological features, and quantification of uncertainties. Interpretation of the sample may have a subjective component, but it should always include uncertainties and alternative or contrasting interpretations, with any exclusion of existing interpretations requiring a full justification. During the creation of a database, an approach based on accessibility, transparency, trust, availability, continuity, completeness, and communication of content (ATTAC<sup>3</sup>) must be adopted. It is essential to consider the community that creates and benefits from a database. We conclude that funding agencies should not only consider the creation of original data in specific research-question-oriented projects, but also include the possibility of using part of the funding for IT-related and database creation tasks, which are essential to guarantee accessibility and maintenance of the collected data.</p>},
 bibtype = {article},
 author = {Düsterhus, André and Rovere, Alessio and Carlson, Anders E. and Horton, Benjamin P. and Klemann, Volker and Tarasov, Lev and Barlow, Natasha L. M. and Bradwell, Tom and Clark, Jorie and Dutton, Andrea and Gehrels, W. Roland and Hibbert, Fiona D. and Hijma, Marc P. and Khan, Nicole and Kopp, Robert E. and Sivan, Dorit and Törnqvist, Torbjörn E.},
 doi = {10.5194/cp-12-911-2016},
 journal = {Climate of the Past},
 number = {4}
}

@article{
 title = {Drones as tools for monitoring beach topography changes in the Ligurian Sea (NW Mediterranean)},
 type = {article},
 year = {2016},
 pages = {151-163},
 volume = {36},
 id = {78f98a9b-44aa-3790-8deb-9be500fd712d},
 created = {2018-02-03T12:42:08.968Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:08.968Z},
 read = {true},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Casella},
 private_publication = {false},
 abstract = {The aim of this study was to evaluate topographic changes along a stretch of coastline in the Municipality of Borghetto Santo Spirito (Region of Liguria, Italy, north-western Mediterranean) by means of a remotely piloted aircraft system coupled with structure from motion and multi-view stereo techniques. This sector was surveyed three times over 5 months in the fall–winter of 2013–2014 (1 November 2013, 4 December 2013, 17 March 2014) to obtain digital elevation models and orthophotos of the beach. Changes in beach topography associated with storm action and human activities were assessed in terms of gain/loss of sediments and shifting of the wet–dry boundary defining the shoreline. Between the first and second surveys, the study area was hit by two storms (10–11 November 2013 and 21–22 November 2013) with waves approaching from the E–NNE, causing a shoreline retreat which, in some sectors, reached 7 m. Between the second and third surveys, by contrast, four storms (25–27 December 2013, 5–6 January 2014, 17–18 January 2014 and 6–10 February 2014) with waves propagating from the SE produced a general advancement of the shoreline (up to ~5 m) by deposition of sediments along some parts of the beach. The data also reflect changes in beach topography due to human activity during the 2013 fall season, when private beach managers quarried ~178 m3 of sediments on the emerged beach near the shoreline to accumulate them landwards. The results show that drones can be used for regular beach monitoring activities, and that they can provide new insights into the processes related to natural and/or human-related topographic beach changes.},
 bibtype = {article},
 author = {Casella, Elisa and Rovere, Alessio and Pedroncini, Andrea and Stark, Colin P. and Casella, Marco and Ferrari, Marco and Firpo, Marco},
 doi = {10.1007/s00367-016-0435-9},
 journal = {Geo-Marine Letters},
 number = {2}
}

@misc{
 title = {The analysis of Last Interglacial (MIS 5e) relative sea-level indicators: Reconstructing sea-level in a warmer world},
 type = {misc},
 year = {2016},
 source = {Earth-Science Reviews},
 keywords = {Ice sheets,Last Interglacial,MIS 5e,Paleo sea-level,Past sea-level changes,Sea-level marker,Sea-level reconstruction},
 pages = {404-427},
 volume = {159},
 websites = {http://linkinghub.elsevier.com/retrieve/pii/S0012825216301246},
 publisher = {Elsevier B.V.},
 id = {6e31994f-6e2d-3da3-af0c-a536ee2529a2},
 created = {2018-02-03T12:42:09.044Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:09.044Z},
 read = {true},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Rovere2016a},
 private_publication = {false},
 abstract = {The Last Interglacial (MIS 5e, 128–116 ka) is among the most studied past periods in Earth's history. The climate at that time was warmer than today, primarily due to different orbital conditions, with smaller ice sheets and higher sea-level. Field evidence for MIS 5e sea-level was reported from thousands of sites, but often paleo shorelines were measured with low-accuracy techniques and, in some cases, there are contrasting interpretations about paleo sea-level reconstructions. For this reason, large uncertainties still surround both the maximum sea-level attained as well as the pattern of sea-level change throughout MIS 5e. Such uncertainties are exacerbated by the lack of a uniform approach to measuring and interpreting the geological evidence of paleo sea-levels. In this review, we discuss the characteristics of MIS 5e field observations, and we set the basis for a standardized approach to MIS 5e paleo sea-level reconstructions, that is already successfully applied in Holocene sea-level research. Application of the standard definitions and methodologies described in this paper will enhance our ability to compare data from different research groups and different areas, in order to gain deeper insights into MIS 5e sea-level changes. Improving estimates of Last Interglacial sea-level is, in turn, a key to understanding the behavior of ice sheets in a warmer world.},
 bibtype = {misc},
 author = {Rovere, Alessio and Raymo, M.E. Maureen E. and Vacchi, Matteo and Lorscheid, Thomas and Stocchi, Paolo and Gómez-Pujol, Lluís and Harris, Daniel L. D.L. and Casella, Elisa and O'Leary, M.J. Michael J. and Hearty, P.J. Paul J.},
 doi = {10.1016/j.earscirev.2016.06.006}
}

@article{
 title = {Study of wave runup using numerical models and low-altitude aerial photogrammetry: A tool for coastal management},
 type = {article},
 year = {2014},
 keywords = {MEDFLOOD,MIRAMAR,PLIOMAX,SEAMAP,SLCC},
 pages = {160-167},
 volume = {149},
 websites = {http://linkinghub.elsevier.com/retrieve/pii/S0272771414002273,http://dx.doi.org/10.1016/j.ecss.2014.08.012},
 month = {8},
 publisher = {Elsevier Ltd},
 id = {8fb8ca01-2971-312e-8c98-3107d0542aff},
 created = {2018-02-03T12:42:09.112Z},
 accessed = {2014-09-25},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.243Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Casella2014},
 private_publication = {false},
 abstract = {Monitoring the impact of sea storms on coastal areas is fundamental to study beach evolution and the vulnerability of low-lying coasts to erosion and flooding. Modelling wave runup on a beach is possible, but it requires accurate topographic data and model tuning, that can be done comparing observed and modeled runup. In this study we collected aerial photos using an Unmanned Aerial Vehicle after two different swells on the same study area. We merged the point cloud obtained with photogrammetry with multibeam data, in order to obtain a complete beach topography. Then, on each set of rectified and georeferenced UAV orthophotos, we identified the maximum wave runup for both events recognizing the wet area left by the waves. We then used our topography and numerical models to simulate the wave runup and compare the model results to observed values during the two events. Our results highlight the potential of the methodology presented, which integrates UAV platforms, photogrammetry and Geographic Information Systems to provide faster and cheaper information on beach topography and geomorphology compared with traditional techniques without losing in accuracy. We use the results obtained from this technique as a topographic base for a model that calculates runup for the two swells. The observed and modeled runups are consistent, and open new directions for future research.},
 bibtype = {article},
 author = {Casella, Elisa and Rovere, Alessio and Pedroncini, Andrea and Mucerino, Luigi and Casella, Marco and Cusati, Luis Alberto and Vacchi, Matteo and Ferrari, Marco and Firpo, Marco},
 doi = {10.1016/j.ecss.2014.08.012},
 journal = {Estuarine, Coastal and Shelf Science}
}

@article{
 title = {Chapter 18 Fixed biological indicators},
 type = {article},
 year = {2015},
 keywords = {MEDFLOOD,PLIOMAX,SLCC},
 pages = {268-280},
 publisher = {Wiley Online Library},
 chapter = {18},
 id = {88d36d15-b4c4-3042-bbdf-5b2ba9c1033d},
 created = {2018-02-03T12:42:09.156Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.173Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Rovere2015c},
 private_publication = {false},
 abstract = {Fixed biological indicators are organisms that live fixed to hard substrates and their living range or the upper part of it is located near or at sea level. In this chapter, the main fixed biological indicators are described and their value as indicators of former sea levels is discussed.},
 bibtype = {article},
 author = {Rovere, Alessio and Antonioli, Fabrizio and Bianchi, Carlo Nike},
 editor = {Shennan, Ian and Long, Antony J. and Horton, Benjamin P},
 journal = {Handbook of Sea-Level Research}
}

@inbook{
 type = {inbook},
 year = {2015},
 pages = {1-30},
 websites = {http://dx.doi.org/10.1007/978-3-319-17001-5_35-1},
 publisher = {Springer International Publishing},
 city = {Cham},
 id = {8d9ac960-e7f9-3635-a6bf-13ec1d22a9f2},
 created = {2018-02-03T12:42:09.165Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.136Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Bianchi2015},
 source_type = {inbook},
 private_publication = {false},
 bibtype = {inbook},
 author = {Bianchi, Carlo Nike and Morri, Carla and Lasagna, Roberta and Montefalcone, Monica and Gatti, Giulia and Parravicini, Valeriano and Rovere, Alessio},
 editor = {Rossi, Sergio and Bramanti, Lorenzo and Gori, Andrea and del Valle, Covadonga},
 doi = {10.1007/978-3-319-17001-5_35-1},
 chapter = {Resilience of the Marine Animal Forest},
 title = {Marine Animal Forests: The Ecology of Benthic Biodiversity Hotspots}
}

@article{
 title = {Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy)},
 type = {article},
 year = {2015},
 keywords = {MIRAMAR,SEAMAP,SLCC},
 pages = {278-286},
 volume = {11},
 websites = {http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134},
 month = {6},
 day = {24},
 id = {4764317f-01f8-36bf-9eff-783fcb4dfc8b},
 created = {2018-02-03T12:42:09.171Z},
 accessed = {2014-09-15},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.118Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Rovere2014},
 private_publication = {false},
 abstract = {In this paper, we present a map describing the main geomorphological features of the coastal and marine area between the towns of Albenga and Savona (Ligurian Sea, NW Mediterranean) corresponding to a coastal stretch of ∼40 km. To produce this map, we collated data from the literature, orthophotos, perspective photos, multibeam and side scan sonar data, and undertook direct surveys to ground truth data obtained using indirect techniques. We divided the information into nine thematic layers, including bathymetry, natural coastal types, geomorphological elements, seafloor coverage (both geological and biological), coastal and nearshore dynamics, human influence on coastal and marine environments, coastal occupation and protected areas.},
 bibtype = {article},
 author = {Rovere, A. and Casella, E. and Vacchi, M. and Parravicini, V. and Firpo, M. and Ferrari, M. and Morri, C. and Bianchi, C. N.},
 doi = {10.1080/17445647.2014.933134},
 journal = {Journal of Maps},
 number = {2}
}

@article{
 title = {Detection of a dynamic topography signal in last interglacial sea-level records},
 type = {article},
 year = {2017},
 pages = {e1700457},
 volume = {3},
 websites = {http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.1700457},
 id = {ba87cc47-ab64-3a6b-9d47-f1fd1ea653c2},
 created = {2018-02-03T12:42:09.180Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:09.180Z},
 read = {true},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {austermann2017detection},
 source_type = {inproceedings},
 private_publication = {false},
 abstract = {Estimating minimum ice volume during the last interglacial based on local sea-level indicators requires that these indicators are corrected for processes that alter local sea level relative to the global average. Although glacial isostatic adjustment is generally accounted for, global scale dynamic changes in topography driven by convective mantle flow are generally not considered. We use numerical models of mantle flow to quantify vertical deflections caused by dynamic topography and compare predictions at passive margins to a globally distributed set of last interglacial sea-level markers. The deflections predicted as a result of dynamic topography are significantly correlated with marker elevations (>95% probability) and are consistent with construction and preservation attributes across marker types. We conclude that a dynamic topography signal is present in the elevation of last interglacial sea-level records and that the signal must be accounted for in any effort to determine peak global mean sea level during the last interglacial to within an accuracy of several meters.},
 bibtype = {article},
 author = {Austermann, Jacqueline and Mitrovica, Jerry X and Huybers, Peter and Rovere, Alessio},
 doi = {10.1126/sciadv.1700457},
 journal = {Science Advances},
 number = {7}
}

@article{
 title = {Emergence and evolution of Santa Maria Island (azores)- The conundrum of uplifted islands revisited},
 type = {article},
 year = {2017},
 pages = {372-391},
 volume = {129},
 id = {1b95bc57-9756-342d-9c36-37e15aca8e39},
 created = {2018-02-03T12:42:09.288Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-02-03T12:42:09.288Z},
 read = {true},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Ramalho2016},
 private_publication = {false},
 abstract = {The growth and decay of ocean island volcanoes is intrinsically linked to vertical movements; whilst mechanisms for subsidence are well understood, uplift mechanisms are still very enigmatic. Santa Maria Island in the Azores is an ocean island volcano with a complex evolutionary history with subsidence followed by uplift. The island emerged by surtseyan activity at approximately 6 Ma, entailing in the formation of a subaerial shield volcano that was fully developed by ~5.6 Ma. The edifice then experienced a period of intense erosion and subsidence, during which it was partially or completely truncated to a shallow submarine bank. Around 5 Ma, volcanism resumed on the eastern side of the edifice, with occasional submarine/surtseyan activity synchronous with marine deposition. By ~4.3 Ma, volcanism grew in intensity forming a new edifice centred on the eastern flank of the underlying edifice. This new volcanic edifice started as submarine and then, as it gradually grew upwards and outpaced subsidence, breached sea level and formed a new island. The new edifice kept growing eastwards and northwards until ~3.5 Ma, when volcanic activity waned. At 3.5-3.2 Ma, however, subsidence reversed to an uplift trend that extended throughout the Upper Pleistocene into the present. This uplift trend is responsible for the generation of a staircase of shore platforms on the windward side of the island, which extends up to ~230 m in elevation. The fact that an island located in very young lithosphere experienced such a pronounced uplift trend is remarkable and raises important questions concerning possible uplift mechanisms. The loading of the neighbouring island of São Miguel may account for part of the uplift, but not the majority. Vertical tectonics along the nearby Gloria Fault is not completely implausible but unlikely to be a source of significant uplift due to its dominant strike-slip character. Thus, other mechanisms need to be considered, most notably intrusions at the base of the edifice and crustal thickening, suggesting that these play a significant role even on islands standing on a young lithosphere, such as in the Azores.},
 bibtype = {article},
 author = {Ramalho, Ricardo S. and Helffrich, George and Madeira, José and Cosca, Michael and Thomas, Christine and Quartau, Rui and Hipólito, Ana and Rovere, Alessio and Hearty, Paul J. and Ávila, Sérgio P.},
 doi = {10.1130/B31538.1},
 journal = {Bulletin of the Geological Society of America},
 number = {3-4}
}

@article{
 title = {Tides in the Last Interglacial: Insights from notch geometry and palaeo tidal models in Bonaire, Netherland Antilles},
 type = {article},
 year = {2017},
 pages = {1-9},
 volume = {7},
 websites = {http://dx.doi.org/10.1038/s41598-017-16285-6},
 publisher = {Springer US},
 id = {cb5bca11-8cb9-3f21-8351-097d44faa054},
 created = {2018-02-03T12:42:09.295Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-09-14T15:34:15.866Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Lorscheid2017d},
 private_publication = {false},
 abstract = {The study of past sea levels relies largely on the interpretation of sea-level indicators. Palaeo tidal notches are considered as one of the most precise sea-level indicators as their formation is closely tied to the local tidal range. We present geometric measurements of modern and palaeo (Marine Isotope Stage (MIS) 5e) tidal notches on Bonaire (southern Caribbean Sea) and results from two tidal simulations, using the present-day bathymetry and a palaeo-bathymetry. We use these two tools to investigate changes in the tidal range since MIS 5e. Our models show that the tidal range changes most significantly in shallow areas, whereas both, notch geometry and models results, suggest that steeper continental shelves, such as the ones bordering the island of Bonaire, are less affected to changes in tidal range in conditions of MIS 5e sea levels. We use our data and results to discuss the importance of considering changes in tidal range while reconstructing MIS 5e sea level histories, and we remark that it is possible to use hydrodynamic modelling and notch geometry as first-order proxies to assess whether, in a particular area, tidal range might have been different in MIS 5e with respect to today. Fossil},
 bibtype = {article},
 author = {Lorscheid, Thomas and Felis, Thomas and Stocchi, Paolo and Obert, J.C. Christina and Scholz, Denis and Rovere, Alessio},
 doi = {10.1038/s41598-017-16285-6},
 journal = {Scientific Reports},
 number = {1}
}

@article{
 title = {Patterns of Sediment Transport Using Foraminifera Tracers across Sand Aprons on the Great Barrier Reef},
 type = {article},
 year = {2017},
 pages = {864-873},
 volume = {33},
 websites = {http://www.bioone.org/doi/10.2112/JCOASTRES-D-16-00082.1},
 id = {f1b13efb-e7ec-3abf-be89-0b240ef77579},
 created = {2018-02-03T12:42:09.320Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-09-14T15:34:15.852Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Fellowes2017},
 private_publication = {false},
 abstract = {© Coastal Education and Research Foundation, Inc. 2017. Sediment dynamics exert large control over coral reef geomorphological evolution and are vital to understanding past and present geomorphic responses. Large benthic foraminifera (LBF) live in the algal reef flats, and their tests (shells) are transported post-mortem by waves and currents onto back-reef environments, including sand aprons. This study investigated the patterns of transport linking surficial and downcore sediments in samples from three sand aprons with different wave exposures at One Tree Reef on the southern Great Barrier Reef (Australia). Six LBF genera represented up to 32% of the sediments analysed. Lagoonward transport increased LBF test abrasion and sediment bulk density. Sediment grain size and LBF abundance in sediments also decreased with lagoonward transport. Sediment transport patterns indicated by LBF species used as tracer were consistent with the prominent E-SE wave environment. A novel taphofacies approach was used to describe stratigraphic layers in downcore sediments based on LBF test abrasion and abundance. Varied sediment deposition rates did not affect the LBF test abrasion signature downcore. It appears that Baculogypsina sphaerulata has been the dominant species for at least 3 ka. Tests that were deposited slowly exhibited less or the same levels of abrasion than those that were rapidly deposited. It appears that test abrasion is primarily determined by the distance travelled rather than the influence of increased age or chemical dissolution.},
 bibtype = {article},
 author = {Fellowes, Thomas E. and Gacutan, Jordan and Harris, Daniel L. and Vila-Concejo, Ana and Webster, Jody M. and Byrne, Maria},
 doi = {10.2112/JCOASTRES-D-16-00082.1},
 journal = {Journal of Coastal Research},
 number = {4}
}

@article{
 title = {Geomorphic changes of a coral shingle cay measured using Kite Aerial Photography},
 type = {article},
 year = {2016},
 keywords = {3D topography,Coral reef morphodynamics,Kite Aerial Photography},
 pages = {1-8},
 volume = {270},
 websites = {http://dx.doi.org/10.1016/j.geomorph.2016.06.018},
 publisher = {Elsevier B.V.},
 id = {4bf2fa14-782a-38ea-99cf-8df4b476f09d},
 created = {2018-02-03T12:42:09.330Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-09-14T15:34:15.863Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Bryson2016e},
 private_publication = {false},
 abstract = {Measurements of geomorphic change in the intertidal zones of coral reefs are made using a variety of remote sensing and in-situ techniques, where variations in the coverage and spatial-temporal precision achieved are directly related to the cost of data acquisition. We present a novel, low-cost technique for measuring high-resolution changes in reef environments based on Kite Aerial Photography (KAP) and photogrammetry/structure-from-motion post-processing. KAP images are used to measure fine-scale changes in intertidal topography and sediment texture characteristics, including rubble particle size, of a coral shingle cay at One Tree Island, Great Barrier Reef in the context of storm activity. Validation using Real Time Kinematic DGPS demonstrates the ability to measure topographic elevation with an error of 5.53 cm (RMSE) and a spatial resolution of 5 cm per point, an accuracy/resolution that is superior to airborne LiDAR and equivalent to terrestrial LiDAR, but at a fraction of the equipment cost.},
 bibtype = {article},
 author = {Bryson, Mitch and Duce, Stephanie and Harris, Dan and Webster, Jody M. and Thompson, Alisha and Vila-Concejo, Ana and Williams, Stefan B.},
 doi = {10.1016/j.geomorph.2016.06.018},
 journal = {Geomorphology}
}

@article{
 title = {Sediment Composition and Facies of Coral Reef Islands in the Spermonde Archipelago, Indonesia},
 type = {article},
 year = {2017},
 keywords = {carbonate sediments, grain size, skeletal constitu},
 pages = {1-13},
 volume = {4},
 websites = {http://journal.frontiersin.org/article/10.3389/fmars.2017.00144/full},
 id = {c0dff020-5319-3fd2-93e8-d982132be5aa},
 created = {2018-02-03T12:42:09.395Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-09-14T15:34:15.991Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Janßen2017a},
 private_publication = {false},
 bibtype = {article},
 author = {Janßen, Alexander and Wizemann, André and Klicpera, André and Satari, Dewi Y. and Westphal, Hildegard and Mann, Thomas},
 doi = {10.3389/fmars.2017.00144},
 journal = {Frontiers in Marine Science},
 number = {May}
}

@article{
 title = {The Mid-Pliocene sea-level conundrum: Glacial isostasy, eustasy and dynamic topography},
 type = {article},
 year = {2014},
 keywords = {MEDFLOOD,PLIOMAX},
 pages = {27-33},
 volume = {387},
 websites = {http://linkinghub.elsevier.com/retrieve/pii/S0012821X13006006,papers2://publication/doi/10.1016/j.epsl.2013.10.030},
 publisher = {Elsevier B.V.},
 day = {1},
 id = {97905946-5bca-31d9-be05-3770c4ddacfc},
 created = {2018-02-03T12:46:08.757Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.049Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Rovere2014f},
 source_type = {JOUR},
 private_publication = {false},
 abstract = {Determining eustatic sea level during the Mid-Pliocene warm period (~3.3 to 2.9 Ma) has been a central but elusive goal in the study of past warm climates. Estimates of eustatic sea level based on geologic data span a broad range; variation that we now recognize is due in part to geographically varying post-depositional displacement caused by glacial isostatic adjustment and dynamic topography. In this study, we combine field observations and glacial isostatic adjustment modeling to estimate the dynamic topography signal in three areas that are important to paleo-sea level studies of the Mid-Pliocene warm period (South Africa, West Australia and southeastern United States). We show that dynamic topography played a significant role in the post-depositional displacement of Pliocene, and even younger Pleistocene, shorelines. In this regard, we provide a robust paleo-sea level elevation data set, corrected for glacial isostatic adjustment, that can be used to evaluate predictions from mantle flow models of dynamic topography. © 2013 Elsevier B.V.},
 bibtype = {article},
 author = {Rovere, Alessio and Raymo, Maureen E and Mitrovica, Jerry X and Hearty, Paul J and O'Leary, M. J. and Inglis, J D},
 doi = {10.1016/j.epsl.2013.10.030},
 journal = {Earth and Planetary Science Letters}
}

@article{
 title = {Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy)},
 type = {article},
 year = {2015},
 keywords = {MIRAMAR,SEAMAP,SLCC},
 pages = {278-286},
 volume = {11},
 websites = {http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134},
 month = {6},
 day = {24},
 id = {c344b1c9-df37-392f-9269-db1a39f0056e},
 created = {2018-02-03T12:46:08.766Z},
 accessed = {2014-09-15},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:24.165Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Rovere2014},
 private_publication = {false},
 abstract = {In this paper, we present a map describing the main geomorphological features of the coastal and marine area between the towns of Albenga and Savona (Ligurian Sea, NW Mediterranean) corresponding to a coastal stretch of ∼40 km. To produce this map, we collated data from the literature, orthophotos, perspective photos, multibeam and side scan sonar data, and undertook direct surveys to ground truth data obtained using indirect techniques. We divided the information into nine thematic layers, including bathymetry, natural coastal types, geomorphological elements, seafloor coverage (both geological and biological), coastal and nearshore dynamics, human influence on coastal and marine environments, coastal occupation and protected areas.},
 bibtype = {article},
 author = {Rovere, A. and Casella, E. and Vacchi, M. and Parravicini, V. and Firpo, M. and Ferrari, M. and Morri, C. and Bianchi, C. N.},
 doi = {10.1080/17445647.2014.933134},
 journal = {Journal of Maps},
 number = {2}
}

@article{
 title = {Coral reef structural complexity provides important coastal protection from waves under rising sea levels},
 type = {article},
 year = {2018},
 pages = {eaao4350},
 volume = {4},
 websites = {http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.aao4350},
 id = {c59b8d33-524b-3a4c-9af1-75c525bbf1b7},
 created = {2018-03-12T08:49:53.423Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-09-14T15:34:15.877Z},
 read = {false},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Harris2018a},
 private_publication = {false},
 abstract = {Coral reefs are diverse ecosystems that support millions of people worldwide by providing coastal protection from waves.Climate change andhumanimpacts are leading todegraded coral reefs and to rising sea levels, posing concerns for the protection of tropical coastal regions in the near future. We use a wave dissipation model calibrated with empirical wave data to calculate the future increase of back-reef wave height. We showthat, in the near future, the structuralcomplexity of coral reefs ismore important than sea-level rise in determining the coastal protection provided by coral reefs from average waves. We also show that a significant increase in average wave heights could occur at present sea level if there is sustained degradation of benthic structural complexity. Our results highlight thatmaintain- ing the structural complexity of coral reefs is key to ensure coastal protection on tropical coastlines in the future.},
 bibtype = {article},
 author = {Harris, Daniel L. and Rovere, Alessio and Casella, Elisa and Power, Hannah and Canavesio, Remy and Collin, Antoine and Pomeroy, Andrew and Webster, Jody M. and Parravicini, Valeriano},
 doi = {10.1126/sciadv.aao4350},
 journal = {Science Advances},
 number = {2}
}

@article{
 title = {MIS 5e relative sea-level changes in the Mediterranean Sea : Contribution of isostatic disequilibrium},
 type = {article},
 year = {2018},
 pages = {122-134},
 volume = {185},
 websites = {https://doi.org/10.1016/j.quascirev.2018.01.004},
 publisher = {Elsevier Ltd},
 id = {96373c82-3999-3443-83f0-80ebf8af4bde},
 created = {2018-04-19T09:43:34.364Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-09-14T15:34:15.974Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Stocchi2018c},
 private_publication = {false},
 bibtype = {article},
 author = {Stocchi, Paolo and Vacchi, Matteo and Lorscheid, Thomas and Boer, Bas De and Simms, Alexander R and Van de Wal, Roderik S and Vermeersen, Bert L A and Pappalardo, Marta and Rovere, Alessio},
 doi = {10.1016/j.quascirev.2018.01.004},
 journal = {Quaternary Science Reviews}
}

@article{
 title = {Submerged reef terraces in the Maldivian Archipelago (Indian Ocean)},
 type = {article},
 year = {2018},
 keywords = {Maldives,Multibeam bathymetry,Scuba diving,Submerged reef terraces},
 pages = {218-232},
 volume = {317},
 websites = {https://doi.org/10.1016/j.geomorph.2018.05.026},
 publisher = {Elsevier B.V.},
 id = {624c972e-28f2-3894-ac6c-1bbcfe9f8e2e},
 created = {2018-06-19T09:16:48.732Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-09-14T15:34:15.876Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Rovere2018c},
 private_publication = {false},
 abstract = {Sea-level changes have shaped the world's carbonate platform margins and continental shelves, leaving typical geomorphic imprints, such as drowned reef terraces. In this paper, we present the results of 112 scuba diving transects across seven different Maldivian atolls and one multibeam survey around Malé Island, the capital of Maldives. We report on the occurrence of drowned reef terraces down to 120 m depth. In total, we identified six levels of submerged terraces that we consider as indicative of periods of time with stable or slowly rising sea level that can be attributed either to deceleration of the last deglacial sea-level rise or to Late Quaternary sea-level highstands. We compare our dataset to the depth of reef terraces reported globally, and we discuss the reasons why common global submerged terrace levels are difficult to identify in the field record.},
 bibtype = {article},
 author = {Rovere, Alessio and Khanna, Pankaj and Bianchi, Carlo Nike and Droxler, André W. and Morri, Carla and Naar, David F.},
 doi = {10.1016/j.geomorph.2018.05.026},
 journal = {Geomorphology}
}

@article{
 title = {Very high resolution mapping of coral reef state using airborne bathymetric LiDAR surface-intensity and drone imagery},
 type = {article},
 year = {2018},
 pages = {1-13},
 volume = {00},
 websites = {https://www.tandfonline.com/doi/full/10.1080/01431161.2018.1500072},
 publisher = {Taylor & Francis},
 id = {d7e17a9b-2188-3ee3-971f-15b820214d88},
 created = {2018-07-24T12:51:35.662Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2018-09-14T15:34:15.965Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Collin2018a},
 private_publication = {false},
 bibtype = {article},
 author = {Collin, Antoine and Ramambason, Camille and Pastol, Yves and Casella, Elisa and Rovere, Alessio and Thiault, Lauric and Espiau, Benoît and Siu, Gilles and Lerouvreur, Franck and Nakamura, Nao and Hench, James L. and Schmitt, Russell J. and Holbrook, Sally J. and Troyer, Matthias and Davies, Neil},
 doi = {10.1080/01431161.2018.1500072},
 journal = {International Journal of Remote Sensing},
 number = {00}
}

@article{
 title = {Coral reef structural complexity provides important coastal protection from waves under rising sea levels},
 type = {article},
 year = {2018},
 pages = {eaao4350},
 volume = {4},
 id = {aad1adc5-4385-32fe-b1e7-72611459d5bc},
 created = {2019-05-09T11:32:03.381Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:03.381Z},
 read = {true},
 starred = {true},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Harris2018},
 private_publication = {false},
 bibtype = {article},
 author = {Harris, Daniel L. and Rovere, Alessio and Casella, Elisa and Power, Hannah and Canavesio, Remy and Collin, Antoine and Pomeroy, Andrew and Webster, Jody M. and Parravicini, Valeriano},
 doi = {10.1126/sciadv.aao4350},
 journal = {Science Advances},
 number = {2}
}

@article{
 title = {Reply to Hearty and Tormey: Use the scientific method to test geologic hypotheses, because rocks do not whisper},
 type = {article},
 year = {2018},
 pages = {201800534},
 websites = {http://www.pnas.org/lookup/doi/10.1073/pnas.1800534115},
 id = {64b225df-3214-3f99-b240-8fbf8f9c2b05},
 created = {2019-05-09T11:32:03.455Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:03.455Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Rovere2018},
 private_publication = {false},
 bibtype = {article},
 author = {Rovere, Alessio and Casella, Elisa and Harris, Daniel L. and Lorscheid, Thomas and Nandasena, Napayalage A. K. and Dyer, Blake and Sandstrom, Michael R. and Stocchi, Paolo and D’Andrea, William J. and Raymo, Maureen E.},
 doi = {10.1073/pnas.1800534115},
 journal = {Proceedings of the National Academy of Sciences}
}

@article{
 title = {New relative sea-level insights into the isostatic history of the Western Mediterranean},
 type = {article},
 year = {2018},
 pages = {396-408},
 volume = {201},
 websites = {https://linkinghub.elsevier.com/retrieve/pii/S0277379118300258},
 publisher = {Elsevier Ltd},
 id = {f6eede31-d00d-3755-8ae8-406b18d9e36a},
 created = {2019-05-09T11:32:03.462Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:03.462Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Vacchi2018},
 private_publication = {false},
 bibtype = {article},
 author = {Vacchi, Matteo and Ghilardi, Matthieu and Melis, Rita T. and Spada, Giorgio and Giaime, Matthieu and Marriner, Nick and Lorscheid, Thomas and Morhange, Christophe and Burjachs, Francesc and Rovere, Alessio},
 doi = {10.1016/j.quascirev.2018.10.025},
 journal = {Quaternary Science Reviews}
}

@article{
 title = {The park never born: Outcome of a quarter of a century of inaction on the sea-floor integrity of a proposed but not established Marine Protected Area},
 type = {article},
 year = {2018},
 pages = {1-20},
 websites = {http://doi.wiley.com/10.1002/aqc.2918},
 id = {0f532705-b047-337d-a91a-49ef26cb036b},
 created = {2019-05-09T11:32:03.510Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:03.510Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Bianchi2018},
 private_publication = {false},
 bibtype = {article},
 author = {Bianchi, Carlo Nike and Cocito, Silvia and Diviacco, Giovanni and Dondi, Nicolò and Fratangeli, Francesca and Montefalcone, Monica and Parravicini, Valeriano and Rovere, Alessio and Sgorbini, Sergio and Vacchi, Matteo and Morri, Carla},
 doi = {10.1002/aqc.2918},
 journal = {Aquatic Conservation: Marine and Freshwater Ecosystems},
 number = {February}
}

@misc{
 title = {Palaeoclimate constraints on the impact of 2 °c anthropogenic warming and beyond},
 type = {misc},
 year = {2018},
 source = {Nature Geoscience},
 pages = {474-485},
 volume = {11},
 issue = {7},
 websites = {file:///home/lmjong/Downloads/2018 - Natgeo - Fischer - PAGES palaeo constraints 2 degrees.pdf},
 publisher = {Springer US},
 id = {6a61807b-e8c8-3eb8-bf1d-cf948032db58},
 created = {2019-05-09T11:32:03.536Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},
 last_modified = {2019-05-09T11:32:03.536Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Fischer2018a},
 private_publication = {false},
 abstract = {Over the past 3.5 million years, there have been several intervals when climate conditions were warmer than during the pre-industrial Holocene. Although past intervals of warming were forced differently than future anthropogenic change, such periods can provide insights into potential future climate impacts and ecosystem feedbacks, especially over centennial-to-millennial timescales that are often not covered by climate model simulations. Our observation-based synthesis of the understanding of past intervals with temperatures within the range of projected future warming suggests that there is a low risk of runaway greenhouse gas feedbacks for global warming of no more than 2 °C. However, substantial regional environmental impacts can occur. A global average warming of 1–2 °C with strong polar amplification has, in the past, been accompanied by significant shifts in climate zones and the spatial distribution of land and ocean ecosystems. Sustained warming at this level has also led to substantial reductions of the Greenland and Antarctic ice sheets, with sea-level increases of at least several metres on millennial timescales. Comparison of palaeo observations with climate model results suggests that, due to the lack of certain feedback processes, model-based climate projections may underestimate long-term warming in response to future radiative forcing by as much as a factor of two, and thus may also underestimate centennial-to-millennial-scale sea-level rise.},
 bibtype = {misc},
 author = {Fischer, Hubertus and Meissner, Katrin J and Mix, Alan C and Abram, Nerilie J and Austermann, Jacqueline and Brovkin, Victor and Capron, Emilie and Colombaroli, Daniele and Daniau, Anne Laure and Dyez, Kelsey A and Felis, Thomas and Finkelstein, Sarah A and Jaccard, Samuel L and McClymont, Erin L and Rovere, Alessio and Sutter, Johannes and Wolff, Eric W and Affolter, Stéphane and Bakker, Pepijn and Ballesteros-Cánovas, Juan Antonio and Barbante, Carlo and Caley, Thibaut and Carlson, Anders E and Churakova, Olga and Cortese, Giuseppe and Cumming, Brian F and Davis, Basil A.S. and De Vernal, Anne and Emile-Geay, Julien and Fritz, Sherilyn C and Gierz, Paul and Gottschalk, Julia and Holloway, Max D and Joos, Fortunat and Kucera, Michal and Loutre, Marie France and Lunt, Daniel J and Marcisz, Katarzyna and Marlon, Jennifer R and Martinez, Philippe and Masson-Delmotte, Valerie and Nehrbass-Ahles, Christoph and Otto-Bliesner, Bette L and Raible, Christoph C and Risebrobakken, Bjørg and Sánchez Goñi, Mariá F. and Arrigo, Jennifer Saleem and Sarnthein, Michael and Sjolte, Jesper and Stocker, Thomas F and Velasquez Alvárez, Patricio A. and Tinner, Willy and Valdes, Paul J and Vogel, Hendrik and Wanner, Heinz and Yan, Qing and Yu, Zicheng and Ziegler, Martin and Zhou, Liping},
 doi = {10.1038/s41561-018-0146-0}
}\">\n            <i class=\"fa fa-download fa-fw\"></i> Download BibTeX\n          </a>\n        </li>\n        <li>\n          <a href=\"//bibbase.org/rss?bib=\">\n            <i class=\"fa fa-rss fa-fw\"></i> RSS Feed\n          </a>\n          </li>\n      </ul>\n      </li>\n\n      \n\n\n      \n    </ul>\n\n\n    <div class=\"alert alert-success bibbase_msg\" id=\"bibbase_msg_embed\"\n         style=\"display: none;\">\n\n      Excellent! 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In order to keep using Mendeley with BibBase past April\n        14th, you need to:\n        <ol>\n          <li>renew the authorization for BibBase on Mendeley, and</li>\n          <li>update the BibBase URL\n            in your page the same way you did when you initially set up\n            this page.\n          </li>\n        </ol>\n      </p>\n\n      <p>\n        <a href=\"http://bibbase.org/cgi-bin/mendeley2/get.py\">\n          <i class=\"fa fa-angle-double-right\"></i>\n          Fix it now</a>\n      </p>\n    </div>\n\n  </div>\n\n\n  <div id=\"bibbase_body\">\n    \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        (9)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"harris-rovere-casella-power-canavesio-collin-pomeroy-webster-etal-coralreefstructuralcomplexityprovidesimportantcoastalprotectionfromwavesunderrisingsealevels-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.aao4350\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'harris-rovere-casella-power-canavesio-collin-pomeroy-webster-etal-coralreefstructuralcomplexityprovidesimportantcoastalprotectionfromwavesunderrisingsealevels-2018', 'http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.aao4350', event);\">\n    Coral reef structural complexity provides important coastal protection from waves under rising sea levels.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Harris,  D., L.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Casella,  E.; Power,  H.; Canavesio,  R.; Collin,  A.; Pomeroy,  A.; Webster,  J., M.;  and Parravicini,  V.\n</span>\n\n  \n\n</span>\n\n  <i>Science Advances</i>, 4(2): eaao4350.  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  <a href=\"http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.aao4350\"\n     onclick=\"log_download('harris-rovere-casella-power-canavesio-collin-pomeroy-webster-etal-coralreefstructuralcomplexityprovidesimportantcoastalprotectionfromwavesunderrisingsealevels-2018', 'http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.aao4350', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Coral reef structural complexity provides important coastal protection from waves under rising sea levels [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1126/sciadv.aao4350\"\n     onclick=\"log_download('harris-rovere-casella-power-canavesio-collin-pomeroy-webster-etal-coralreefstructuralcomplexityprovidesimportantcoastalprotectionfromwavesunderrisingsealevels-2018', 'http://doi.org/10.1126/sciadv.aao4350', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/harris-rovere-casella-power-canavesio-collin-pomeroy-webster-etal-coralreefstructuralcomplexityprovidesimportantcoastalprotectionfromwavesunderrisingsealevels-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>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('harris-rovere-casella-power-canavesio-collin-pomeroy-webster-etal-coralreefstructuralcomplexityprovidesimportantcoastalprotectionfromwavesunderrisingsealevels-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{\n title = {Coral reef structural complexity provides important coastal protection from waves under rising sea levels},\n type = {article},\n year = {2018},\n pages = {eaao4350},\n volume = {4},\n websites = {http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.aao4350},\n id = {c59b8d33-524b-3a4c-9af1-75c525bbf1b7},\n created = {2018-03-12T08:49:53.423Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-09-14T15:34:15.877Z},\n read = {false},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Harris2018a},\n private_publication = {false},\n abstract = {Coral reefs are diverse ecosystems that support millions of people worldwide by providing coastal protection from waves.Climate change andhumanimpacts are leading todegraded coral reefs and to rising sea levels, posing concerns for the protection of tropical coastal regions in the near future. We use a wave dissipation model calibrated with empirical wave data to calculate the future increase of back-reef wave height. We showthat, in the near future, the structuralcomplexity of coral reefs ismore important than sea-level rise in determining the coastal protection provided by coral reefs from average waves. We also show that a significant increase in average wave heights could occur at present sea level if there is sustained degradation of benthic structural complexity. Our results highlight thatmaintain- ing the structural complexity of coral reefs is key to ensure coastal protection on tropical coastlines in the future.},\n bibtype = {article},\n author = {Harris, Daniel L. and Rovere, Alessio and Casella, Elisa and Power, Hannah and Canavesio, Remy and Collin, Antoine and Pomeroy, Andrew and Webster, Jody M. and Parravicini, Valeriano},\n doi = {10.1126/sciadv.aao4350},\n journal = {Science Advances},\n number = {2}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Coral reefs are diverse ecosystems that support millions of people worldwide by providing coastal protection from waves.Climate change andhumanimpacts are leading todegraded coral reefs and to rising sea levels, posing concerns for the protection of tropical coastal regions in the near future. We use a wave dissipation model calibrated with empirical wave data to calculate the future increase of back-reef wave height. We showthat, in the near future, the structuralcomplexity of coral reefs ismore important than sea-level rise in determining the coastal protection provided by coral reefs from average waves. We also show that a significant increase in average wave heights could occur at present sea level if there is sustained degradation of benthic structural complexity. Our results highlight thatmaintain- ing the structural complexity of coral reefs is key to ensure coastal protection on tropical coastlines in the future.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"stocchi-vacchi-lorscheid-boer-simms-vandewal-vermeersen-pappalardo-etal-mis5erelativesealevelchangesinthemediterraneanseacontributionofisostaticdisequilibrium-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.1016/j.quascirev.2018.01.004\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'stocchi-vacchi-lorscheid-boer-simms-vandewal-vermeersen-pappalardo-etal-mis5erelativesealevelchangesinthemediterraneanseacontributionofisostaticdisequilibrium-2018', 'https://doi.org/10.1016/j.quascirev.2018.01.004', event);\">\n    MIS 5e relative sea-level changes in the Mediterranean Sea : Contribution of isostatic disequilibrium.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Stocchi,  P.; Vacchi,  M.; Lorscheid,  T.; Boer,  B., D.; Simms,  A., R.; Van de Wal,  R., S.; Vermeersen,  B., L., A.; Pappalardo,  M.;  and Rovere,  A.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Science Reviews</i>, 185: 122-134.  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  <a href=\"https://doi.org/10.1016/j.quascirev.2018.01.004\"\n     onclick=\"log_download('stocchi-vacchi-lorscheid-boer-simms-vandewal-vermeersen-pappalardo-etal-mis5erelativesealevelchangesinthemediterraneanseacontributionofisostaticdisequilibrium-2018', 'https://doi.org/10.1016/j.quascirev.2018.01.004', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"MIS 5e relative sea-level changes in the Mediterranean Sea : Contribution of isostatic disequilibrium [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quascirev.2018.01.004\"\n     onclick=\"log_download('stocchi-vacchi-lorscheid-boer-simms-vandewal-vermeersen-pappalardo-etal-mis5erelativesealevelchangesinthemediterraneanseacontributionofisostaticdisequilibrium-2018', 'http://doi.org/10.1016/j.quascirev.2018.01.004', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/stocchi-vacchi-lorscheid-boer-simms-vandewal-vermeersen-pappalardo-etal-mis5erelativesealevelchangesinthemediterraneanseacontributionofisostaticdisequilibrium-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\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('stocchi-vacchi-lorscheid-boer-simms-vandewal-vermeersen-pappalardo-etal-mis5erelativesealevelchangesinthemediterraneanseacontributionofisostaticdisequilibrium-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{\n title = {MIS 5e relative sea-level changes in the Mediterranean Sea : Contribution of isostatic disequilibrium},\n type = {article},\n year = {2018},\n pages = {122-134},\n volume = {185},\n websites = {https://doi.org/10.1016/j.quascirev.2018.01.004},\n publisher = {Elsevier Ltd},\n id = {96373c82-3999-3443-83f0-80ebf8af4bde},\n created = {2018-04-19T09:43:34.364Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-09-14T15:34:15.974Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Stocchi2018c},\n private_publication = {false},\n bibtype = {article},\n author = {Stocchi, Paolo and Vacchi, Matteo and Lorscheid, Thomas and Boer, Bas De and Simms, Alexander R and Van de Wal, Roderik S and Vermeersen, Bert L A and Pappalardo, Marta and Rovere, Alessio},\n doi = {10.1016/j.quascirev.2018.01.004},\n journal = {Quaternary Science Reviews}\n}</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"rovere-khanna-bianchi-droxler-morri-naar-submergedreefterracesinthemaldivianarchipelagoindianocean-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://doi.org/10.1016/j.geomorph.2018.05.026\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'rovere-khanna-bianchi-droxler-morri-naar-submergedreefterracesinthemaldivianarchipelagoindianocean-2018', 'https://doi.org/10.1016/j.geomorph.2018.05.026', event);\">\n    Submerged reef terraces in the Maldivian Archipelago (Indian Ocean).\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Khanna,  P.; Bianchi,  C., N.; Droxler,  A., W.; Morri,  C.;  and Naar,  D., F.\n</span>\n\n  \n\n</span>\n\n  <i>Geomorphology</i>, 317: 218-232.  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  <a href=\"https://doi.org/10.1016/j.geomorph.2018.05.026\"\n     onclick=\"log_download('rovere-khanna-bianchi-droxler-morri-naar-submergedreefterracesinthemaldivianarchipelagoindianocean-2018', 'https://doi.org/10.1016/j.geomorph.2018.05.026', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Submerged reef terraces in the Maldivian Archipelago (Indian Ocean) [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.geomorph.2018.05.026\"\n     onclick=\"log_download('rovere-khanna-bianchi-droxler-morri-naar-submergedreefterracesinthemaldivianarchipelagoindianocean-2018', 'http://doi.org/10.1016/j.geomorph.2018.05.026', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/rovere-khanna-bianchi-droxler-morri-naar-submergedreefterracesinthemaldivianarchipelagoindianocean-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('rovere-khanna-bianchi-droxler-morri-naar-submergedreefterracesinthemaldivianarchipelagoindianocean-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Submerged reef terraces in the Maldivian Archipelago (Indian Ocean)},\n type = {article},\n year = {2018},\n keywords = {Maldives,Multibeam bathymetry,Scuba diving,Submerged reef terraces},\n pages = {218-232},\n volume = {317},\n websites = {https://doi.org/10.1016/j.geomorph.2018.05.026},\n publisher = {Elsevier B.V.},\n id = {624c972e-28f2-3894-ac6c-1bbcfe9f8e2e},\n created = {2018-06-19T09:16:48.732Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-09-14T15:34:15.876Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Rovere2018c},\n private_publication = {false},\n abstract = {Sea-level changes have shaped the world&#x27;s carbonate platform margins and continental shelves, leaving typical geomorphic imprints, such as drowned reef terraces. In this paper, we present the results of 112 scuba diving transects across seven different Maldivian atolls and one multibeam survey around Malé Island, the capital of Maldives. We report on the occurrence of drowned reef terraces down to 120 m depth. In total, we identified six levels of submerged terraces that we consider as indicative of periods of time with stable or slowly rising sea level that can be attributed either to deceleration of the last deglacial sea-level rise or to Late Quaternary sea-level highstands. We compare our dataset to the depth of reef terraces reported globally, and we discuss the reasons why common global submerged terrace levels are difficult to identify in the field record.},\n bibtype = {article},\n author = {Rovere, Alessio and Khanna, Pankaj and Bianchi, Carlo Nike and Droxler, André W. and Morri, Carla and Naar, David F.},\n doi = {10.1016/j.geomorph.2018.05.026},\n journal = {Geomorphology}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Sea-level changes have shaped the world's carbonate platform margins and continental shelves, leaving typical geomorphic imprints, such as drowned reef terraces. In this paper, we present the results of 112 scuba diving transects across seven different Maldivian atolls and one multibeam survey around Malé Island, the capital of Maldives. We report on the occurrence of drowned reef terraces down to 120 m depth. In total, we identified six levels of submerged terraces that we consider as indicative of periods of time with stable or slowly rising sea level that can be attributed either to deceleration of the last deglacial sea-level rise or to Late Quaternary sea-level highstands. We compare our dataset to the depth of reef terraces reported globally, and we discuss the reasons why common global submerged terrace levels are difficult to identify in the field record.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"collin-ramambason-pastol-casella-rovere-thiault-espiau-siu-etal-veryhighresolutionmappingofcoralreefstateusingairbornebathymetriclidarsurfaceintensityanddroneimagery-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://www.tandfonline.com/doi/full/10.1080/01431161.2018.1500072\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'collin-ramambason-pastol-casella-rovere-thiault-espiau-siu-etal-veryhighresolutionmappingofcoralreefstateusingairbornebathymetriclidarsurfaceintensityanddroneimagery-2018', 'https://www.tandfonline.com/doi/full/10.1080/01431161.2018.1500072', event);\">\n    Very high resolution mapping of coral reef state using airborne bathymetric LiDAR surface-intensity and drone imagery.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Collin,  A.; Ramambason,  C.; Pastol,  Y.; Casella,  E.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Thiault,  L.; Espiau,  B.; Siu,  G.; Lerouvreur,  F.; Nakamura,  N.; Hench,  J., L.; Schmitt,  R., J.; Holbrook,  S., J.; Troyer,  M.;  and Davies,  N.\n</span>\n\n  \n\n</span>\n\n  <i>International Journal of Remote Sensing</i>, 00(00): 1-13.  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  <a href=\"https://www.tandfonline.com/doi/full/10.1080/01431161.2018.1500072\"\n     onclick=\"log_download('collin-ramambason-pastol-casella-rovere-thiault-espiau-siu-etal-veryhighresolutionmappingofcoralreefstateusingairbornebathymetriclidarsurfaceintensityanddroneimagery-2018', 'https://www.tandfonline.com/doi/full/10.1080/01431161.2018.1500072', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Very high resolution mapping of coral reef state using airborne bathymetric LiDAR surface-intensity and drone imagery [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1080/01431161.2018.1500072\"\n     onclick=\"log_download('collin-ramambason-pastol-casella-rovere-thiault-espiau-siu-etal-veryhighresolutionmappingofcoralreefstateusingairbornebathymetriclidarsurfaceintensityanddroneimagery-2018', 'http://doi.org/10.1080/01431161.2018.1500072', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/collin-ramambason-pastol-casella-rovere-thiault-espiau-siu-etal-veryhighresolutionmappingofcoralreefstateusingairbornebathymetriclidarsurfaceintensityanddroneimagery-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\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('collin-ramambason-pastol-casella-rovere-thiault-espiau-siu-etal-veryhighresolutionmappingofcoralreefstateusingairbornebathymetriclidarsurfaceintensityanddroneimagery-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{\n title = {Very high resolution mapping of coral reef state using airborne bathymetric LiDAR surface-intensity and drone imagery},\n type = {article},\n year = {2018},\n pages = {1-13},\n volume = {00},\n websites = {https://www.tandfonline.com/doi/full/10.1080/01431161.2018.1500072},\n publisher = {Taylor &amp; Francis},\n id = {d7e17a9b-2188-3ee3-971f-15b820214d88},\n created = {2018-07-24T12:51:35.662Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-09-14T15:34:15.965Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Collin2018a},\n private_publication = {false},\n bibtype = {article},\n author = {Collin, Antoine and Ramambason, Camille and Pastol, Yves and Casella, Elisa and Rovere, Alessio and Thiault, Lauric and Espiau, Benoît and Siu, Gilles and Lerouvreur, Franck and Nakamura, Nao and Hench, James L. and Schmitt, Russell J. and Holbrook, Sally J. and Troyer, Matthias and Davies, Neil},\n doi = {10.1080/01431161.2018.1500072},\n journal = {International Journal of Remote Sensing},\n number = {00}\n}</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"harris-rovere-casella-power-canavesio-collin-pomeroy-webster-etal-coralreefstructuralcomplexityprovidesimportantcoastalprotectionfromwavesunderrisingsealevels-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Coral reef structural complexity provides important coastal protection from waves under rising sea levels.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Harris,  D., L.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Casella,  E.; Power,  H.; Canavesio,  R.; Collin,  A.; Pomeroy,  A.; Webster,  J., M.;  and Parravicini,  V.\n</span>\n\n  \n\n</span>\n\n  <i>Science Advances</i>, 4(2): eaao4350.  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/10.1126/sciadv.aao4350\"\n     onclick=\"log_download('harris-rovere-casella-power-canavesio-collin-pomeroy-webster-etal-coralreefstructuralcomplexityprovidesimportantcoastalprotectionfromwavesunderrisingsealevels-2018', 'http://doi.org/10.1126/sciadv.aao4350', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/harris-rovere-casella-power-canavesio-collin-pomeroy-webster-etal-coralreefstructuralcomplexityprovidesimportantcoastalprotectionfromwavesunderrisingsealevels-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\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('harris-rovere-casella-power-canavesio-collin-pomeroy-webster-etal-coralreefstructuralcomplexityprovidesimportantcoastalprotectionfromwavesunderrisingsealevels-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{\n title = {Coral reef structural complexity provides important coastal protection from waves under rising sea levels},\n type = {article},\n year = {2018},\n pages = {eaao4350},\n volume = {4},\n id = {aad1adc5-4385-32fe-b1e7-72611459d5bc},\n created = {2019-05-09T11:32:03.381Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:03.381Z},\n read = {true},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Harris2018},\n private_publication = {false},\n bibtype = {article},\n author = {Harris, Daniel L. and Rovere, Alessio and Casella, Elisa and Power, Hannah and Canavesio, Remy and Collin, Antoine and Pomeroy, Andrew and Webster, Jody M. and Parravicini, Valeriano},\n doi = {10.1126/sciadv.aao4350},\n journal = {Science Advances},\n number = {2}\n}</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-replytoheartyandtormeyusethescientificmethodtotestgeologichypothesesbecauserocksdonotwhisper-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.pnas.org/lookup/doi/10.1073/pnas.1800534115\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-replytoheartyandtormeyusethescientificmethodtotestgeologichypothesesbecauserocksdonotwhisper-2018', 'http://www.pnas.org/lookup/doi/10.1073/pnas.1800534115', event);\">\n    Reply to Hearty and Tormey: Use the scientific method to test geologic hypotheses, because rocks do not whisper.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Casella,  E.; Harris,  D., L.; Lorscheid,  T.; Nandasena,  N., A., K.; Dyer,  B.; Sandstrom,  M., R.; Stocchi,  P.; D’Andrea,  W., J.;  and Raymo,  M., E.\n</span>\n\n  \n\n</span>\n\n  <i>Proceedings of the National Academy of Sciences</i>,201800534.  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  <a href=\"http://www.pnas.org/lookup/doi/10.1073/pnas.1800534115\"\n     onclick=\"log_download('rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-replytoheartyandtormeyusethescientificmethodtotestgeologichypothesesbecauserocksdonotwhisper-2018', 'http://www.pnas.org/lookup/doi/10.1073/pnas.1800534115', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Reply to Hearty and Tormey: Use the scientific method to test geologic hypotheses, because rocks do not whisper [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1073/pnas.1800534115\"\n     onclick=\"log_download('rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-replytoheartyandtormeyusethescientificmethodtotestgeologichypothesesbecauserocksdonotwhisper-2018', 'http://doi.org/10.1073/pnas.1800534115', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-replytoheartyandtormeyusethescientificmethodtotestgeologichypothesesbecauserocksdonotwhisper-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\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('rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-replytoheartyandtormeyusethescientificmethodtotestgeologichypothesesbecauserocksdonotwhisper-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{\n title = {Reply to Hearty and Tormey: Use the scientific method to test geologic hypotheses, because rocks do not whisper},\n type = {article},\n year = {2018},\n pages = {201800534},\n websites = {http://www.pnas.org/lookup/doi/10.1073/pnas.1800534115},\n id = {64b225df-3214-3f99-b240-8fbf8f9c2b05},\n created = {2019-05-09T11:32:03.455Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:03.455Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Rovere2018},\n private_publication = {false},\n bibtype = {article},\n author = {Rovere, Alessio and Casella, Elisa and Harris, Daniel L. and Lorscheid, Thomas and Nandasena, Napayalage A. K. and Dyer, Blake and Sandstrom, Michael R. and Stocchi, Paolo and D’Andrea, William J. and Raymo, Maureen E.},\n doi = {10.1073/pnas.1800534115},\n journal = {Proceedings of the National Academy of Sciences}\n}</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"vacchi-ghilardi-melis-spada-giaime-marriner-lorscheid-morhange-etal-newrelativesealevelinsightsintotheisostatichistoryofthewesternmediterranean-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"https://linkinghub.elsevier.com/retrieve/pii/S0277379118300258\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'vacchi-ghilardi-melis-spada-giaime-marriner-lorscheid-morhange-etal-newrelativesealevelinsightsintotheisostatichistoryofthewesternmediterranean-2018', 'https://linkinghub.elsevier.com/retrieve/pii/S0277379118300258', event);\">\n    New relative sea-level insights into the isostatic history of the Western Mediterranean.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Vacchi,  M.; Ghilardi,  M.; Melis,  R., T.; Spada,  G.; Giaime,  M.; Marriner,  N.; Lorscheid,  T.; Morhange,  C.; Burjachs,  F.;  and <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Science Reviews</i>, 201: 396-408.  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  <a href=\"https://linkinghub.elsevier.com/retrieve/pii/S0277379118300258\"\n     onclick=\"log_download('vacchi-ghilardi-melis-spada-giaime-marriner-lorscheid-morhange-etal-newrelativesealevelinsightsintotheisostatichistoryofthewesternmediterranean-2018', 'https://linkinghub.elsevier.com/retrieve/pii/S0277379118300258', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"New relative sea-level insights into the isostatic history of the Western Mediterranean [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quascirev.2018.10.025\"\n     onclick=\"log_download('vacchi-ghilardi-melis-spada-giaime-marriner-lorscheid-morhange-etal-newrelativesealevelinsightsintotheisostatichistoryofthewesternmediterranean-2018', 'http://doi.org/10.1016/j.quascirev.2018.10.025', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/vacchi-ghilardi-melis-spada-giaime-marriner-lorscheid-morhange-etal-newrelativesealevelinsightsintotheisostatichistoryofthewesternmediterranean-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\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('vacchi-ghilardi-melis-spada-giaime-marriner-lorscheid-morhange-etal-newrelativesealevelinsightsintotheisostatichistoryofthewesternmediterranean-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{\n title = {New relative sea-level insights into the isostatic history of the Western Mediterranean},\n type = {article},\n year = {2018},\n pages = {396-408},\n volume = {201},\n websites = {https://linkinghub.elsevier.com/retrieve/pii/S0277379118300258},\n publisher = {Elsevier Ltd},\n id = {f6eede31-d00d-3755-8ae8-406b18d9e36a},\n created = {2019-05-09T11:32:03.462Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:03.462Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Vacchi2018},\n private_publication = {false},\n bibtype = {article},\n author = {Vacchi, Matteo and Ghilardi, Matthieu and Melis, Rita T. and Spada, Giorgio and Giaime, Matthieu and Marriner, Nick and Lorscheid, Thomas and Morhange, Christophe and Burjachs, Francesc and Rovere, Alessio},\n doi = {10.1016/j.quascirev.2018.10.025},\n journal = {Quaternary Science Reviews}\n}</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"bianchi-cocito-diviacco-dondi-fratangeli-montefalcone-parravicini-rovere-etal-theparkneverbornoutcomeofaquarterofacenturyofinactionontheseafloorintegrityofaproposedbutnotestablishedmarineprotectedarea-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://doi.wiley.com/10.1002/aqc.2918\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'bianchi-cocito-diviacco-dondi-fratangeli-montefalcone-parravicini-rovere-etal-theparkneverbornoutcomeofaquarterofacenturyofinactionontheseafloorintegrityofaproposedbutnotestablishedmarineprotectedarea-2018', 'http://doi.wiley.com/10.1002/aqc.2918', event);\">\n    The park never born: Outcome of a quarter of a century of inaction on the sea-floor integrity of a proposed but not established Marine Protected Area.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Bianchi,  C., N.; Cocito,  S.; Diviacco,  G.; Dondi,  N.; Fratangeli,  F.; Montefalcone,  M.; Parravicini,  V.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Sgorbini,  S.; Vacchi,  M.;  and Morri,  C.\n</span>\n\n  \n\n</span>\n\n  <i>Aquatic Conservation: Marine and Freshwater Ecosystems</i>, (February): 1-20.  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  <a href=\"http://doi.wiley.com/10.1002/aqc.2918\"\n     onclick=\"log_download('bianchi-cocito-diviacco-dondi-fratangeli-montefalcone-parravicini-rovere-etal-theparkneverbornoutcomeofaquarterofacenturyofinactionontheseafloorintegrityofaproposedbutnotestablishedmarineprotectedarea-2018', 'http://doi.wiley.com/10.1002/aqc.2918', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"The park never born: Outcome of a quarter of a century of inaction on the sea-floor integrity of a proposed but not established Marine Protected Area [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1002/aqc.2918\"\n     onclick=\"log_download('bianchi-cocito-diviacco-dondi-fratangeli-montefalcone-parravicini-rovere-etal-theparkneverbornoutcomeofaquarterofacenturyofinactionontheseafloorintegrityofaproposedbutnotestablishedmarineprotectedarea-2018', 'http://doi.org/10.1002/aqc.2918', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/bianchi-cocito-diviacco-dondi-fratangeli-montefalcone-parravicini-rovere-etal-theparkneverbornoutcomeofaquarterofacenturyofinactionontheseafloorintegrityofaproposedbutnotestablishedmarineprotectedarea-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\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('bianchi-cocito-diviacco-dondi-fratangeli-montefalcone-parravicini-rovere-etal-theparkneverbornoutcomeofaquarterofacenturyofinactionontheseafloorintegrityofaproposedbutnotestablishedmarineprotectedarea-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{\n title = {The park never born: Outcome of a quarter of a century of inaction on the sea-floor integrity of a proposed but not established Marine Protected Area},\n type = {article},\n year = {2018},\n pages = {1-20},\n websites = {http://doi.wiley.com/10.1002/aqc.2918},\n id = {0f532705-b047-337d-a91a-49ef26cb036b},\n created = {2019-05-09T11:32:03.510Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:03.510Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Bianchi2018},\n private_publication = {false},\n bibtype = {article},\n author = {Bianchi, Carlo Nike and Cocito, Silvia and Diviacco, Giovanni and Dondi, Nicolò and Fratangeli, Francesca and Montefalcone, Monica and Parravicini, Valeriano and Rovere, Alessio and Sgorbini, Sergio and Vacchi, Matteo and Morri, Carla},\n doi = {10.1002/aqc.2918},\n journal = {Aquatic Conservation: Marine and Freshwater Ecosystems},\n number = {February}\n}</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"fischer-meissner-mix-abram-austermann-brovkin-capron-colombaroli-etal-palaeoclimateconstraintsontheimpactof2canthropogenicwarmingandbeyond-2018\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"file:///home/lmjong/Downloads/2018 - Natgeo - Fischer - PAGES palaeo constraints 2 degrees.pdf\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'fischer-meissner-mix-abram-austermann-brovkin-capron-colombaroli-etal-palaeoclimateconstraintsontheimpactof2canthropogenicwarmingandbeyond-2018', 'file:///home/lmjong/Downloads/2018 - Natgeo - Fischer - PAGES palaeo constraints 2 degrees.pdf', event);\">\n    Palaeoclimate constraints on the impact of 2 °c anthropogenic warming and beyond.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Fischer,  H.; Meissner,  K., J.; Mix,  A., C.; Abram,  N., J.; Austermann,  J.; Brovkin,  V.; Capron,  E.; Colombaroli,  D.; Daniau,  A., L.; Dyez,  K., A.; Felis,  T.; Finkelstein,  S., A.; Jaccard,  S., L.; McClymont,  E., L.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Sutter,  J.; Wolff,  E., W.; Affolter,  S.; Bakker,  P.; Ballesteros-Cánovas,  J., A.; Barbante,  C.; Caley,  T.; Carlson,  A., E.; Churakova,  O.; Cortese,  G.; Cumming,  B., F.; Davis,  B., A.; De Vernal,  A.; Emile-Geay,  J.; Fritz,  S., C.; Gierz,  P.; Gottschalk,  J.; Holloway,  M., D.; Joos,  F.; Kucera,  M.; Loutre,  M., F.; Lunt,  D., J.; Marcisz,  K.; Marlon,  J., R.; Martinez,  P.; Masson-Delmotte,  V.; Nehrbass-Ahles,  C.; Otto-Bliesner,  B., L.; Raible,  C., C.; Risebrobakken,  B.; Sánchez Goñi,  M., F.; Arrigo,  J., S.; Sarnthein,  M.; Sjolte,  J.; Stocker,  T., F.; Velasquez Alvárez,  P., A.; Tinner,  W.; Valdes,  P., J.; Vogel,  H.; Wanner,  H.; Yan,  Q.; Yu,  Z.; Ziegler,  M.;  and Zhou,  L.\n</span>\n\n  \n\n</span>\n\n   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  <a href=\"file:///home/lmjong/Downloads/2018 - Natgeo - Fischer - PAGES palaeo constraints 2 degrees.pdf\"\n     onclick=\"log_download('fischer-meissner-mix-abram-austermann-brovkin-capron-colombaroli-etal-palaeoclimateconstraintsontheimpactof2canthropogenicwarmingandbeyond-2018', 'file:///home/lmjong/Downloads/2018 - Natgeo - Fischer - PAGES palaeo constraints 2 degrees.pdf', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/pdf.svg\"\n\t     alt=\"Palaeoclimate constraints on the impact of 2 °c anthropogenic warming and beyond [pdf]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1038/s41561-018-0146-0\"\n     onclick=\"log_download('fischer-meissner-mix-abram-austermann-brovkin-capron-colombaroli-etal-palaeoclimateconstraintsontheimpactof2canthropogenicwarmingandbeyond-2018', 'http://doi.org/10.1038/s41561-018-0146-0', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/fischer-meissner-mix-abram-austermann-brovkin-capron-colombaroli-etal-palaeoclimateconstraintsontheimpactof2canthropogenicwarmingandbeyond-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>4 downloads</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('fischer-meissner-mix-abram-austermann-brovkin-capron-colombaroli-etal-palaeoclimateconstraintsontheimpactof2canthropogenicwarmingandbeyond-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;\">@misc{\n title = {Palaeoclimate constraints on the impact of 2 °c anthropogenic warming and beyond},\n type = {misc},\n year = {2018},\n source = {Nature Geoscience},\n pages = {474-485},\n volume = {11},\n issue = {7},\n websites = {file:///home/lmjong/Downloads/2018 - Natgeo - Fischer - PAGES palaeo constraints 2 degrees.pdf},\n publisher = {Springer US},\n id = {6a61807b-e8c8-3eb8-bf1d-cf948032db58},\n created = {2019-05-09T11:32:03.536Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:03.536Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Fischer2018a},\n private_publication = {false},\n abstract = {Over the past 3.5 million years, there have been several intervals when climate conditions were warmer than during the pre-industrial Holocene. Although past intervals of warming were forced differently than future anthropogenic change, such periods can provide insights into potential future climate impacts and ecosystem feedbacks, especially over centennial-to-millennial timescales that are often not covered by climate model simulations. Our observation-based synthesis of the understanding of past intervals with temperatures within the range of projected future warming suggests that there is a low risk of runaway greenhouse gas feedbacks for global warming of no more than 2 °C. However, substantial regional environmental impacts can occur. A global average warming of 1–2 °C with strong polar amplification has, in the past, been accompanied by significant shifts in climate zones and the spatial distribution of land and ocean ecosystems. Sustained warming at this level has also led to substantial reductions of the Greenland and Antarctic ice sheets, with sea-level increases of at least several metres on millennial timescales. Comparison of palaeo observations with climate model results suggests that, due to the lack of certain feedback processes, model-based climate projections may underestimate long-term warming in response to future radiative forcing by as much as a factor of two, and thus may also underestimate centennial-to-millennial-scale sea-level rise.},\n bibtype = {misc},\n author = {Fischer, Hubertus and Meissner, Katrin J and Mix, Alan C and Abram, Nerilie J and Austermann, Jacqueline and Brovkin, Victor and Capron, Emilie and Colombaroli, Daniele and Daniau, Anne Laure and Dyez, Kelsey A and Felis, Thomas and Finkelstein, Sarah A and Jaccard, Samuel L and McClymont, Erin L and Rovere, Alessio and Sutter, Johannes and Wolff, Eric W and Affolter, Stéphane and Bakker, Pepijn and Ballesteros-Cánovas, Juan Antonio and Barbante, Carlo and Caley, Thibaut and Carlson, Anders E and Churakova, Olga and Cortese, Giuseppe and Cumming, Brian F and Davis, Basil A.S. and De Vernal, Anne and Emile-Geay, Julien and Fritz, Sherilyn C and Gierz, Paul and Gottschalk, Julia and Holloway, Max D and Joos, Fortunat and Kucera, Michal and Loutre, Marie France and Lunt, Daniel J and Marcisz, Katarzyna and Marlon, Jennifer R and Martinez, Philippe and Masson-Delmotte, Valerie and Nehrbass-Ahles, Christoph and Otto-Bliesner, Bette L and Raible, Christoph C and Risebrobakken, Bjørg and Sánchez Goñi, Mariá F. and Arrigo, Jennifer Saleem and Sarnthein, Michael and Sjolte, Jesper and Stocker, Thomas F and Velasquez Alvárez, Patricio A. and Tinner, Willy and Valdes, Paul J and Vogel, Hendrik and Wanner, Heinz and Yan, Qing and Yu, Zicheng and Ziegler, Martin and Zhou, Liping},\n doi = {10.1038/s41561-018-0146-0}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Over the past 3.5 million years, there have been several intervals when climate conditions were warmer than during the pre-industrial Holocene. Although past intervals of warming were forced differently than future anthropogenic change, such periods can provide insights into potential future climate impacts and ecosystem feedbacks, especially over centennial-to-millennial timescales that are often not covered by climate model simulations. Our observation-based synthesis of the understanding of past intervals with temperatures within the range of projected future warming suggests that there is a low risk of runaway greenhouse gas feedbacks for global warming of no more than 2 °C. However, substantial regional environmental impacts can occur. A global average warming of 1–2 °C with strong polar amplification has, in the past, been accompanied by significant shifts in climate zones and the spatial distribution of land and ocean ecosystems. Sustained warming at this level has also led to substantial reductions of the Greenland and Antarctic ice sheets, with sea-level increases of at least several metres on millennial timescales. Comparison of palaeo observations with climate model results suggests that, due to the lack of certain feedback processes, model-based climate projections may underestimate long-term warming in response to future radiative forcing by as much as a factor of two, and thus may also underestimate centennial-to-millennial-scale sea-level rise.\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        (9)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"lorscheid-stocchi-casella-gmezpujol-vacchi-mann-rovere-paleosealevelchangesandrelativesealevelindicatorsprecisemeasurementsindicativemeaningandglacialisostaticadjustmentperspectivesfrommallorcawesternmediterranean-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://linkinghub.elsevier.com/retrieve/pii/S0031018216303753\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'lorscheid-stocchi-casella-gmezpujol-vacchi-mann-rovere-paleosealevelchangesandrelativesealevelindicatorsprecisemeasurementsindicativemeaningandglacialisostaticadjustmentperspectivesfrommallorcawesternmediterranean-2017', 'http://linkinghub.elsevier.com/retrieve/pii/S0031018216303753', event);\">\n    Paleo sea-level changes and relative sea-level indicators: Precise measurements, indicative meaning and glacial isostatic adjustment perspectives from Mallorca (Western Mediterranean).\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Lorscheid,  T.; Stocchi,  P.; Casella,  E.; Gómez-Pujol,  L.; Vacchi,  M.; Mann,  T.;  and <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>\n</span>\n\n  \n\n</span>\n\n  <i>Palaeogeography, Palaeoclimatology, Palaeoecology</i>, 473: 94-107.  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=\"http://linkinghub.elsevier.com/retrieve/pii/S0031018216303753\"\n     onclick=\"log_download('lorscheid-stocchi-casella-gmezpujol-vacchi-mann-rovere-paleosealevelchangesandrelativesealevelindicatorsprecisemeasurementsindicativemeaningandglacialisostaticadjustmentperspectivesfrommallorcawesternmediterranean-2017', 'http://linkinghub.elsevier.com/retrieve/pii/S0031018216303753', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Paleo sea-level changes and relative sea-level indicators: Precise measurements, indicative meaning and glacial isostatic adjustment perspectives from Mallorca (Western Mediterranean) [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.palaeo.2017.02.028\"\n     onclick=\"log_download('lorscheid-stocchi-casella-gmezpujol-vacchi-mann-rovere-paleosealevelchangesandrelativesealevelindicatorsprecisemeasurementsindicativemeaningandglacialisostaticadjustmentperspectivesfrommallorcawesternmediterranean-2017', 'http://doi.org/10.1016/j.palaeo.2017.02.028', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/lorscheid-stocchi-casella-gmezpujol-vacchi-mann-rovere-paleosealevelchangesandrelativesealevelindicatorsprecisemeasurementsindicativemeaningandglacialisostaticadjustmentperspectivesfrommallorcawesternmediterranean-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('lorscheid-stocchi-casella-gmezpujol-vacchi-mann-rovere-paleosealevelchangesandrelativesealevelindicatorsprecisemeasurementsindicativemeaningandglacialisostaticadjustmentperspectivesfrommallorcawesternmediterranean-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Paleo sea-level changes and relative sea-level indicators: Precise measurements, indicative meaning and glacial isostatic adjustment perspectives from Mallorca (Western Mediterranean)},\n type = {article},\n year = {2017},\n keywords = {Beach deposits,Last interglacial,MIS 5e,Morphodynamic modelling},\n pages = {94-107},\n volume = {473},\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0031018216303753},\n publisher = {Elsevier B.V.},\n id = {7abcfe9b-788b-39f2-8a80-0e128ce6d024},\n created = {2018-02-03T12:42:06.762Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:06.762Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Lorscheid2017},\n private_publication = {false},\n abstract = {Paleo relative sea-level (RSL) indicators formed during the Marine Isotope Stage (MIS) 5e have been reported by a large number of studies worldwide. Despite this, three main aspects are seldom reported: (1) use of high-precision survey techniques applied to MIS 5e RSL indicators; (2) application of modern analogs to understand the indicative meaning of MIS 5e RSL indicators; (3) estimates of the effects of glacial isostatic adjustment (GIA) on the MIS 5e records. In this study, we show how the three points above have been addressed in a focused study on Last Interglacial outcrops on the island of Mallorca. We measured the elevation of several RSL indicators with high-accuracy differential GPS (vertical accuracies down to 0.1 m) and we established the relationship between each RSL indicator and the paleo sea level through calculation of the indicative meaning for each RSL indicator. In particular, we present a novel technique to calculate the indicative meaning of fossil beach deposits with a phase-averaged morphodynamic model (CSHORE). We show how this approach helps overcoming difficulties with the survey of the modern analogs for these indicators. Our results show that two paleo RSLs are imprinted in Mallorca at + 2.9 ± 0.8 m and + 11.3 ± 1.0 m. We then compare our field-based results with modelled paleo RSL, calculated from the predictions of the ice-earth coupled ANICE-SELEN model, using few different ice-sheet melting scenarios during MIS 5e. We conclude that indicative ranges can be derived from relatively simple morphodynamic models and that the comparison of field-derived and modelled RSL values is a good method to validate possible scenarios of MIS 5e sea-level variability, especially in absence of precise dating.},\n bibtype = {article},\n author = {Lorscheid, Thomas and Stocchi, Paolo and Casella, Elisa and Gómez-Pujol, Lluis and Vacchi, Matteo and Mann, Thomas and Rovere, Alessio},\n doi = {10.1016/j.palaeo.2017.02.028},\n journal = {Palaeogeography, Palaeoclimatology, Palaeoecology}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Paleo relative sea-level (RSL) indicators formed during the Marine Isotope Stage (MIS) 5e have been reported by a large number of studies worldwide. Despite this, three main aspects are seldom reported: (1) use of high-precision survey techniques applied to MIS 5e RSL indicators; (2) application of modern analogs to understand the indicative meaning of MIS 5e RSL indicators; (3) estimates of the effects of glacial isostatic adjustment (GIA) on the MIS 5e records. In this study, we show how the three points above have been addressed in a focused study on Last Interglacial outcrops on the island of Mallorca. We measured the elevation of several RSL indicators with high-accuracy differential GPS (vertical accuracies down to 0.1 m) and we established the relationship between each RSL indicator and the paleo sea level through calculation of the indicative meaning for each RSL indicator. In particular, we present a novel technique to calculate the indicative meaning of fossil beach deposits with a phase-averaged morphodynamic model (CSHORE). We show how this approach helps overcoming difficulties with the survey of the modern analogs for these indicators. Our results show that two paleo RSLs are imprinted in Mallorca at + 2.9 ± 0.8 m and + 11.3 ± 1.0 m. We then compare our field-based results with modelled paleo RSL, calculated from the predictions of the ice-earth coupled ANICE-SELEN model, using few different ice-sheet melting scenarios during MIS 5e. We conclude that indicative ranges can be derived from relatively simple morphodynamic models and that the comparison of field-derived and modelled RSL values is a good method to validate possible scenarios of MIS 5e sea-level variability, especially in absence of precise dating.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"benjamin-rovere-fontana-furlani-vacchi-inglis-galili-antonioli-etal-latequaternarysealevelchangesandearlyhumansocietiesinthecentralandeasternmediterraneanbasinaninterdisciplinaryreview-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://linkinghub.elsevier.com/retrieve/pii/S1040618216310928,http://dx.doi.org/10.1016/j.quaint.2017.06.025\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'benjamin-rovere-fontana-furlani-vacchi-inglis-galili-antonioli-etal-latequaternarysealevelchangesandearlyhumansocietiesinthecentralandeasternmediterraneanbasinaninterdisciplinaryreview-2017', 'http://linkinghub.elsevier.com/retrieve/pii/S1040618216310928,http://dx.doi.org/10.1016/j.quaint.2017.06.025', event);\">\n    Late Quaternary sea-level changes and early human societies in the central and eastern Mediterranean Basin: An interdisciplinary review.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Benjamin,  J.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Fontana,  A.; Furlani,  S.; Vacchi,  M.; Inglis,  R., H.; Galili,  E.; Antonioli,  F.; Sivan,  D.; Miko,  S.; Mourtzas,  N.; Felja,  I.; Meredith-Williams,  M.; Goodman-Tchernov,  B.; Kolaiti,  E.; Anzidei,  M.;  and Gehrels,  R.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary International</i>, 449: 29-57.  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=\"http://linkinghub.elsevier.com/retrieve/pii/S1040618216310928,http://dx.doi.org/10.1016/j.quaint.2017.06.025\"\n     onclick=\"log_download('benjamin-rovere-fontana-furlani-vacchi-inglis-galili-antonioli-etal-latequaternarysealevelchangesandearlyhumansocietiesinthecentralandeasternmediterraneanbasinaninterdisciplinaryreview-2017', 'http://linkinghub.elsevier.com/retrieve/pii/S1040618216310928,http://dx.doi.org/10.1016/j.quaint.2017.06.025', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Late Quaternary sea-level changes and early human societies in the central and eastern Mediterranean Basin: An interdisciplinary review [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quaint.2017.06.025\"\n     onclick=\"log_download('benjamin-rovere-fontana-furlani-vacchi-inglis-galili-antonioli-etal-latequaternarysealevelchangesandearlyhumansocietiesinthecentralandeasternmediterraneanbasinaninterdisciplinaryreview-2017', 'http://doi.org/10.1016/j.quaint.2017.06.025', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/benjamin-rovere-fontana-furlani-vacchi-inglis-galili-antonioli-etal-latequaternarysealevelchangesandearlyhumansocietiesinthecentralandeasternmediterraneanbasinaninterdisciplinaryreview-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('benjamin-rovere-fontana-furlani-vacchi-inglis-galili-antonioli-etal-latequaternarysealevelchangesandearlyhumansocietiesinthecentralandeasternmediterraneanbasinaninterdisciplinaryreview-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Late Quaternary sea-level changes and early human societies in the central and eastern Mediterranean Basin: An interdisciplinary review},\n type = {article},\n year = {2017},\n keywords = {Holocene,Mediterranean Archaeology,Pleistocene,Sea-level change},\n pages = {29-57},\n volume = {449},\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S1040618216310928,http://dx.doi.org/10.1016/j.quaint.2017.06.025},\n publisher = {Elsevier Ltd},\n id = {62fca5b4-ded4-330a-a54f-ce02c6217d33},\n created = {2018-02-03T12:42:07.907Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:07.907Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Benjamin2017},\n private_publication = {false},\n abstract = {This article reviews key data and debates focused on relative sea-level changes since the Last Interglacial (approximately the last 132,000 years) in the Mediterranean Basin, and their implications for past human populations. Geological and geomorphological landscape studies are critical to archaeology. Coastal regions provide a wide range of resources to the populations that inhabit them. Coastal landscapes are increasingly the focus of scholarly discussions from the earliest exploitation of littoral resources and early hominin cognition, to the inundation of the earliest permanently settled fishing villages and eventually, formative centres of urbanisation. In the Mediterranean, these would become hubs of maritime transportation that gave rise to the roots of modern seaborne trade. As such, this article represents an original review of both the geo-scientific and archaeological data that specifically relate to sea-level changes and resulting impacts on both physical and cultural landscapes from the Palaeolithic until the emergence of the Classical periods. Our review highlights that the interdisciplinary links between coastal archaeology, geomorphology and sea-level changes are important to explain environmental impacts on coastal human societies and human migration. We review geological indicators of sea level and outline how archaeological features are commonly used as proxies for measuring past sea levels, both gradual changes and catastrophic events. We argue that coastal archaeologists should, as a part of their analyses, incorporate important sea-level concepts, such as indicative meaning. The interpretation of the indicative meaning of Roman fishtanks, for example, plays a critical role in reconstructions of late Holocene Mediterranean sea levels. We identify avenues for future work, which include the consideration of glacial isostatic adjustment (GIA) in addition to coastal tectonics to explain vertical movements of coastlines, more research on Palaeolithic island colonisation, broadening of Palaeolithic studies to include materials from the entire coastal landscape and not just coastal resources, a focus on rescue of archaeological sites under threat by coastal change, and expansion of underwater archaeological explorations in combination with submarine geomorphology. This article presents a collaborative synthesis of data, some of which have been collected and analysed by the authors, as the MEDFLOOD (MEDiterranean sea-level change and projection for future FLOODing) community, and highlights key sites, data, concepts and ongoing debates.},\n bibtype = {article},\n author = {Benjamin, J. and Rovere, A. and Fontana, A. and Furlani, S. and Vacchi, M. and Inglis, R.H. H. and Galili, E. and Antonioli, F. and Sivan, D. and Miko, S. and Mourtzas, N. and Felja, I. and Meredith-Williams, M. and Goodman-Tchernov, B. and Kolaiti, E. and Anzidei, M. and Gehrels, R.},\n doi = {10.1016/j.quaint.2017.06.025},\n journal = {Quaternary International}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  This article reviews key data and debates focused on relative sea-level changes since the Last Interglacial (approximately the last 132,000 years) in the Mediterranean Basin, and their implications for past human populations. Geological and geomorphological landscape studies are critical to archaeology. Coastal regions provide a wide range of resources to the populations that inhabit them. Coastal landscapes are increasingly the focus of scholarly discussions from the earliest exploitation of littoral resources and early hominin cognition, to the inundation of the earliest permanently settled fishing villages and eventually, formative centres of urbanisation. In the Mediterranean, these would become hubs of maritime transportation that gave rise to the roots of modern seaborne trade. As such, this article represents an original review of both the geo-scientific and archaeological data that specifically relate to sea-level changes and resulting impacts on both physical and cultural landscapes from the Palaeolithic until the emergence of the Classical periods. Our review highlights that the interdisciplinary links between coastal archaeology, geomorphology and sea-level changes are important to explain environmental impacts on coastal human societies and human migration. We review geological indicators of sea level and outline how archaeological features are commonly used as proxies for measuring past sea levels, both gradual changes and catastrophic events. We argue that coastal archaeologists should, as a part of their analyses, incorporate important sea-level concepts, such as indicative meaning. The interpretation of the indicative meaning of Roman fishtanks, for example, plays a critical role in reconstructions of late Holocene Mediterranean sea levels. We identify avenues for future work, which include the consideration of glacial isostatic adjustment (GIA) in addition to coastal tectonics to explain vertical movements of coastlines, more research on Palaeolithic island colonisation, broadening of Palaeolithic studies to include materials from the entire coastal landscape and not just coastal resources, a focus on rescue of archaeological sites under threat by coastal change, and expansion of underwater archaeological explorations in combination with submarine geomorphology. This article presents a collaborative synthesis of data, some of which have been collected and analysed by the authors, as the MEDFLOOD (MEDiterranean sea-level change and projection for future FLOODing) community, and highlights key sites, data, concepts and ongoing debates.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-giantbouldersandlastinterglacialstormintensityinthenorthatlantic-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.ncbi.nlm.nih.gov/pubmed/29087331,http://www.pnas.org/lookup/doi/10.1073/pnas.1712433114\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-giantbouldersandlastinterglacialstormintensityinthenorthatlantic-2017', 'http://www.ncbi.nlm.nih.gov/pubmed/29087331,http://www.pnas.org/lookup/doi/10.1073/pnas.1712433114', event);\">\n    Giant boulders and Last Interglacial storm intensity in the North Atlantic.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Casella,  E.; Harris,  D., L.; Lorscheid,  T.; Nandasena,  N., A., K.; Dyer,  B.; Sandstrom,  M., R.; Stocchi,  P.; D’Andrea,  W., J.;  and Raymo,  M., E.\n</span>\n\n  \n\n</span>\n\n  <i>Proceedings of the National Academy of Sciences</i>, 114(46): 201712433. 10 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=\"http://www.ncbi.nlm.nih.gov/pubmed/29087331,http://www.pnas.org/lookup/doi/10.1073/pnas.1712433114\"\n     onclick=\"log_download('rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-giantbouldersandlastinterglacialstormintensityinthenorthatlantic-2017', 'http://www.ncbi.nlm.nih.gov/pubmed/29087331,http://www.pnas.org/lookup/doi/10.1073/pnas.1712433114', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Giant boulders and Last Interglacial storm intensity in the North Atlantic [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1073/pnas.1712433114\"\n     onclick=\"log_download('rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-giantbouldersandlastinterglacialstormintensityinthenorthatlantic-2017', 'http://doi.org/10.1073/pnas.1712433114', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-giantbouldersandlastinterglacialstormintensityinthenorthatlantic-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>1 download</span>\n  </span>\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('rovere-casella-harris-lorscheid-nandasena-dyer-sandstrom-stocchi-etal-giantbouldersandlastinterglacialstormintensityinthenorthatlantic-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Giant boulders and Last Interglacial storm intensity in the North Atlantic},\n type = {article},\n year = {2017},\n keywords = {Eemian,Last Interglacial,climate change,extreme waves,superstorms},\n pages = {201712433},\n volume = {114},\n websites = {http://www.ncbi.nlm.nih.gov/pubmed/29087331,http://www.pnas.org/lookup/doi/10.1073/pnas.1712433114},\n month = {10},\n publisher = {National Academy of Sciences},\n day = {30},\n id = {3d249fd7-0f67-34cd-9597-134e27ac4b8c},\n created = {2018-02-03T12:42:07.914Z},\n accessed = {2017-11-10},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:07.914Z},\n read = {true},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Rovere2017},\n private_publication = {false},\n abstract = {As global climate warms and sea level rises, coastal areas will be subject to more frequent extreme flooding and hurricanes. Geologic evidence for extreme coastal storms during past warm periods has the potential to provide fundamental insights into their future intensity. Recent studies argue that during the Last Interglacial (MIS 5e, ∼128-116 ka) tropical and extratropical North Atlantic cyclones may have been more intense than at present, and may have produced waves larger than those observed historically. Such strong swells are inferred to have created a number of geologic features that can be observed today along the coastlines of Bermuda and the Bahamas. In this paper, we investigate the most iconic among these features: massive boulders atop a cliff in North Eleuthera, Bahamas. We combine geologic field surveys, wave models, and boulder transport equations to test the hypothesis that such boulders must have been emplaced by storms of greater-than-historical intensity. By contrast, our results suggest that with the higher relative sea level (RSL) estimated for the Bahamas during MIS 5e, boulders of this size could have been transported by waves generated by storms of historical intensity. Thus, while the megaboulders of Eleuthera cannot be used as geologic proof for past &quot;superstorms,&quot; they do show that with rising sea levels, cliffs and coastal barriers will be subject to significantly greater erosional energy, even without changes in storm intensity.},\n bibtype = {article},\n author = {Rovere, Alessio and Casella, Elisa and Harris, Daniel L. and Lorscheid, Thomas and Nandasena, Napayalage A. K. and Dyer, Blake and Sandstrom, Michael R. and Stocchi, Paolo and D’Andrea, William J. and Raymo, Maureen E.},\n doi = {10.1073/pnas.1712433114},\n journal = {Proceedings of the National Academy of Sciences},\n number = {46}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  As global climate warms and sea level rises, coastal areas will be subject to more frequent extreme flooding and hurricanes. Geologic evidence for extreme coastal storms during past warm periods has the potential to provide fundamental insights into their future intensity. Recent studies argue that during the Last Interglacial (MIS 5e, ∼128-116 ka) tropical and extratropical North Atlantic cyclones may have been more intense than at present, and may have produced waves larger than those observed historically. Such strong swells are inferred to have created a number of geologic features that can be observed today along the coastlines of Bermuda and the Bahamas. In this paper, we investigate the most iconic among these features: massive boulders atop a cliff in North Eleuthera, Bahamas. We combine geologic field surveys, wave models, and boulder transport equations to test the hypothesis that such boulders must have been emplaced by storms of greater-than-historical intensity. By contrast, our results suggest that with the higher relative sea level (RSL) estimated for the Bahamas during MIS 5e, boulders of this size could have been transported by waves generated by storms of historical intensity. Thus, while the megaboulders of Eleuthera cannot be used as geologic proof for past \"superstorms,\" they do show that with rising sea levels, cliffs and coastal barriers will be subject to significantly greater erosional energy, even without changes in storm intensity.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"casella-collin-harris-ferse-bejarano-parravicini-hench-rovere-mappingcoralreefsusingconsumergradedronesandstructurefrommotionphotogrammetrytechniques-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://link.springer.com/10.1007/s00338-016-1522-0\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'casella-collin-harris-ferse-bejarano-parravicini-hench-rovere-mappingcoralreefsusingconsumergradedronesandstructurefrommotionphotogrammetrytechniques-2017', 'http://link.springer.com/10.1007/s00338-016-1522-0', event);\">\n    Mapping coral reefs using consumer-grade drones and structure from motion photogrammetry techniques.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Casella,  E.; Collin,  A.; Harris,  D.; Ferse,  S.; Bejarano,  S.; Parravicini,  V.; Hench,  J., L.;  and <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>\n</span>\n\n  \n\n</span>\n\n  <i>Coral Reefs</i>, 36(1): 269-275.  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=\"http://link.springer.com/10.1007/s00338-016-1522-0\"\n     onclick=\"log_download('casella-collin-harris-ferse-bejarano-parravicini-hench-rovere-mappingcoralreefsusingconsumergradedronesandstructurefrommotionphotogrammetrytechniques-2017', 'http://link.springer.com/10.1007/s00338-016-1522-0', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Mapping coral reefs using consumer-grade drones and structure from motion photogrammetry techniques [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s00338-016-1522-0\"\n     onclick=\"log_download('casella-collin-harris-ferse-bejarano-parravicini-hench-rovere-mappingcoralreefsusingconsumergradedronesandstructurefrommotionphotogrammetrytechniques-2017', 'http://doi.org/10.1007/s00338-016-1522-0', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/casella-collin-harris-ferse-bejarano-parravicini-hench-rovere-mappingcoralreefsusingconsumergradedronesandstructurefrommotionphotogrammetrytechniques-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('casella-collin-harris-ferse-bejarano-parravicini-hench-rovere-mappingcoralreefsusingconsumergradedronesandstructurefrommotionphotogrammetrytechniques-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Mapping coral reefs using consumer-grade drones and structure from motion photogrammetry techniques},\n type = {article},\n year = {2017},\n keywords = {Bathymetry from drones,Bathymetry from photogrammetry,Coral reefs,Drone mapping,Structure from motion underwater},\n pages = {269-275},\n volume = {36},\n websites = {http://link.springer.com/10.1007/s00338-016-1522-0},\n publisher = {Springer Berlin Heidelberg},\n id = {014c2903-534c-38d9-8cc6-397276ea0084},\n created = {2018-02-03T12:42:07.996Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:07.996Z},\n read = {true},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Casella2016},\n private_publication = {false},\n abstract = {We propose a novel technique to measure the small-scale three-dimensional features of a shallow-water coral reef using a small drone equipped with a consumer-grade camera, a handheld GPS and structure from motion (SfM) algorithms. We used a GoPro HERO4 with a modified lens mounted on a DJI Phantom 2 drone (maximum total take-off weight &lt;2 kg) to perform a 10 min flight and collect 306 aerial images with an overlap equal or greater than 90%. We mapped an area of 8380 m2, obtaining as output an ortho-rectified aerial photomosaic and a bathymetric digital elevation model (DEM) with a resolution of 0.78 and 1.56 cm pixel−1, respectively. Through comparison with airborne LiDAR data for the same area, we verified that the location of the ortho-rectified aerial photomosaic is accurate within ~1.4 m. The bathymetric difference between our DEM and the LiDAR dataset is −0.016 ± 0.45 m (1σ). Our results show that it is possible, in conditions of calm waters, low winds and minimal sun glint, to deploy consumer-grade drones as a relatively low-cost and rapid survey technique to produce multispectral and bathymetric data on shallow-water coral reefs. We discuss the utility of such data to monitor temporal changes in topographic complexity of reefs and associated biological processes.},\n bibtype = {article},\n author = {Casella, Elisa and Collin, Antoine and Harris, Daniel and Ferse, Sebastian and Bejarano, Sonia and Parravicini, Valeriano and Hench, James L. and Rovere, Alessio},\n doi = {10.1007/s00338-016-1522-0},\n journal = {Coral Reefs},\n number = {1}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  We propose a novel technique to measure the small-scale three-dimensional features of a shallow-water coral reef using a small drone equipped with a consumer-grade camera, a handheld GPS and structure from motion (SfM) algorithms. We used a GoPro HERO4 with a modified lens mounted on a DJI Phantom 2 drone (maximum total take-off weight <2 kg) to perform a 10 min flight and collect 306 aerial images with an overlap equal or greater than 90%. We mapped an area of 8380 m2, obtaining as output an ortho-rectified aerial photomosaic and a bathymetric digital elevation model (DEM) with a resolution of 0.78 and 1.56 cm pixel−1, respectively. Through comparison with airborne LiDAR data for the same area, we verified that the location of the ortho-rectified aerial photomosaic is accurate within ~1.4 m. The bathymetric difference between our DEM and the LiDAR dataset is −0.016 ± 0.45 m (1σ). Our results show that it is possible, in conditions of calm waters, low winds and minimal sun glint, to deploy consumer-grade drones as a relatively low-cost and rapid survey technique to produce multispectral and bathymetric data on shallow-water coral reefs. We discuss the utility of such data to monitor temporal changes in topographic complexity of reefs and associated biological processes.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"austermann-mitrovica-huybers-rovere-detectionofadynamictopographysignalinlastinterglacialsealevelrecords-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.1700457\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'austermann-mitrovica-huybers-rovere-detectionofadynamictopographysignalinlastinterglacialsealevelrecords-2017', 'http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.1700457', event);\">\n    Detection of a dynamic topography signal in last interglacial sea-level records.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Austermann,  J.; Mitrovica,  J., X.; Huybers,  P.;  and <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>\n</span>\n\n  \n\n</span>\n\n  <i>Science Advances</i>, 3(7): e1700457.  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=\"http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.1700457\"\n     onclick=\"log_download('austermann-mitrovica-huybers-rovere-detectionofadynamictopographysignalinlastinterglacialsealevelrecords-2017', 'http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.1700457', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Detection of a dynamic topography signal in last interglacial sea-level records [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1126/sciadv.1700457\"\n     onclick=\"log_download('austermann-mitrovica-huybers-rovere-detectionofadynamictopographysignalinlastinterglacialsealevelrecords-2017', 'http://doi.org/10.1126/sciadv.1700457', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/austermann-mitrovica-huybers-rovere-detectionofadynamictopographysignalinlastinterglacialsealevelrecords-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('austermann-mitrovica-huybers-rovere-detectionofadynamictopographysignalinlastinterglacialsealevelrecords-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Detection of a dynamic topography signal in last interglacial sea-level records},\n type = {article},\n year = {2017},\n pages = {e1700457},\n volume = {3},\n websites = {http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.1700457},\n id = {ba87cc47-ab64-3a6b-9d47-f1fd1ea653c2},\n created = {2018-02-03T12:42:09.180Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:09.180Z},\n read = {true},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {austermann2017detection},\n source_type = {inproceedings},\n private_publication = {false},\n abstract = {Estimating minimum ice volume during the last interglacial based on local sea-level indicators requires that these indicators are corrected for processes that alter local sea level relative to the global average. Although glacial isostatic adjustment is generally accounted for, global scale dynamic changes in topography driven by convective mantle flow are generally not considered. We use numerical models of mantle flow to quantify vertical deflections caused by dynamic topography and compare predictions at passive margins to a globally distributed set of last interglacial sea-level markers. The deflections predicted as a result of dynamic topography are significantly correlated with marker elevations (&gt;95% probability) and are consistent with construction and preservation attributes across marker types. We conclude that a dynamic topography signal is present in the elevation of last interglacial sea-level records and that the signal must be accounted for in any effort to determine peak global mean sea level during the last interglacial to within an accuracy of several meters.},\n bibtype = {article},\n author = {Austermann, Jacqueline and Mitrovica, Jerry X and Huybers, Peter and Rovere, Alessio},\n doi = {10.1126/sciadv.1700457},\n journal = {Science Advances},\n number = {7}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Estimating minimum ice volume during the last interglacial based on local sea-level indicators requires that these indicators are corrected for processes that alter local sea level relative to the global average. Although glacial isostatic adjustment is generally accounted for, global scale dynamic changes in topography driven by convective mantle flow are generally not considered. We use numerical models of mantle flow to quantify vertical deflections caused by dynamic topography and compare predictions at passive margins to a globally distributed set of last interglacial sea-level markers. The deflections predicted as a result of dynamic topography are significantly correlated with marker elevations (>95% probability) and are consistent with construction and preservation attributes across marker types. We conclude that a dynamic topography signal is present in the elevation of last interglacial sea-level records and that the signal must be accounted for in any effort to determine peak global mean sea level during the last interglacial to within an accuracy of several meters.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"ramalho-helffrich-madeira-cosca-thomas-quartau-hiplito-rovere-etal-emergenceandevolutionofsantamariaislandazorestheconundrumofupliftedislandsrevisited-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Emergence and evolution of Santa Maria Island (azores)- The conundrum of uplifted islands revisited.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Ramalho,  R., S.; Helffrich,  G.; Madeira,  J.; Cosca,  M.; Thomas,  C.; Quartau,  R.; Hipólito,  A.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Hearty,  P., J.;  and Ávila,  S., P.\n</span>\n\n  \n\n</span>\n\n  <i>Bulletin of the Geological Society of America</i>, 129(3-4): 372-391.  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\n  \n  <a href=\"http://doi.org/10.1130/B31538.1\"\n     onclick=\"log_download('ramalho-helffrich-madeira-cosca-thomas-quartau-hiplito-rovere-etal-emergenceandevolutionofsantamariaislandazorestheconundrumofupliftedislandsrevisited-2017', 'http://doi.org/10.1130/B31538.1', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/ramalho-helffrich-madeira-cosca-thomas-quartau-hiplito-rovere-etal-emergenceandevolutionofsantamariaislandazorestheconundrumofupliftedislandsrevisited-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('ramalho-helffrich-madeira-cosca-thomas-quartau-hiplito-rovere-etal-emergenceandevolutionofsantamariaislandazorestheconundrumofupliftedislandsrevisited-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Emergence and evolution of Santa Maria Island (azores)- The conundrum of uplifted islands revisited},\n type = {article},\n year = {2017},\n pages = {372-391},\n volume = {129},\n id = {1b95bc57-9756-342d-9c36-37e15aca8e39},\n created = {2018-02-03T12:42:09.288Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:09.288Z},\n read = {true},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Ramalho2016},\n private_publication = {false},\n abstract = {The growth and decay of ocean island volcanoes is intrinsically linked to vertical movements; whilst mechanisms for subsidence are well understood, uplift mechanisms are still very enigmatic. Santa Maria Island in the Azores is an ocean island volcano with a complex evolutionary history with subsidence followed by uplift. The island emerged by surtseyan activity at approximately 6 Ma, entailing in the formation of a subaerial shield volcano that was fully developed by ~5.6 Ma. The edifice then experienced a period of intense erosion and subsidence, during which it was partially or completely truncated to a shallow submarine bank. Around 5 Ma, volcanism resumed on the eastern side of the edifice, with occasional submarine/surtseyan activity synchronous with marine deposition. By ~4.3 Ma, volcanism grew in intensity forming a new edifice centred on the eastern flank of the underlying edifice. This new volcanic edifice started as submarine and then, as it gradually grew upwards and outpaced subsidence, breached sea level and formed a new island. The new edifice kept growing eastwards and northwards until ~3.5 Ma, when volcanic activity waned. At 3.5-3.2 Ma, however, subsidence reversed to an uplift trend that extended throughout the Upper Pleistocene into the present. This uplift trend is responsible for the generation of a staircase of shore platforms on the windward side of the island, which extends up to ~230 m in elevation. The fact that an island located in very young lithosphere experienced such a pronounced uplift trend is remarkable and raises important questions concerning possible uplift mechanisms. The loading of the neighbouring island of São Miguel may account for part of the uplift, but not the majority. Vertical tectonics along the nearby Gloria Fault is not completely implausible but unlikely to be a source of significant uplift due to its dominant strike-slip character. Thus, other mechanisms need to be considered, most notably intrusions at the base of the edifice and crustal thickening, suggesting that these play a significant role even on islands standing on a young lithosphere, such as in the Azores.},\n bibtype = {article},\n author = {Ramalho, Ricardo S. and Helffrich, George and Madeira, José and Cosca, Michael and Thomas, Christine and Quartau, Rui and Hipólito, Ana and Rovere, Alessio and Hearty, Paul J. and Ávila, Sérgio P.},\n doi = {10.1130/B31538.1},\n journal = {Bulletin of the Geological Society of America},\n number = {3-4}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The growth and decay of ocean island volcanoes is intrinsically linked to vertical movements; whilst mechanisms for subsidence are well understood, uplift mechanisms are still very enigmatic. Santa Maria Island in the Azores is an ocean island volcano with a complex evolutionary history with subsidence followed by uplift. The island emerged by surtseyan activity at approximately 6 Ma, entailing in the formation of a subaerial shield volcano that was fully developed by ~5.6 Ma. The edifice then experienced a period of intense erosion and subsidence, during which it was partially or completely truncated to a shallow submarine bank. Around 5 Ma, volcanism resumed on the eastern side of the edifice, with occasional submarine/surtseyan activity synchronous with marine deposition. By ~4.3 Ma, volcanism grew in intensity forming a new edifice centred on the eastern flank of the underlying edifice. This new volcanic edifice started as submarine and then, as it gradually grew upwards and outpaced subsidence, breached sea level and formed a new island. The new edifice kept growing eastwards and northwards until ~3.5 Ma, when volcanic activity waned. At 3.5-3.2 Ma, however, subsidence reversed to an uplift trend that extended throughout the Upper Pleistocene into the present. This uplift trend is responsible for the generation of a staircase of shore platforms on the windward side of the island, which extends up to ~230 m in elevation. The fact that an island located in very young lithosphere experienced such a pronounced uplift trend is remarkable and raises important questions concerning possible uplift mechanisms. The loading of the neighbouring island of São Miguel may account for part of the uplift, but not the majority. Vertical tectonics along the nearby Gloria Fault is not completely implausible but unlikely to be a source of significant uplift due to its dominant strike-slip character. Thus, other mechanisms need to be considered, most notably intrusions at the base of the edifice and crustal thickening, suggesting that these play a significant role even on islands standing on a young lithosphere, such as in the Azores.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"lorscheid-felis-stocchi-obert-scholz-rovere-tidesinthelastinterglacialinsightsfromnotchgeometryandpalaeotidalmodelsinbonairenetherlandantilles-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://dx.doi.org/10.1038/s41598-017-16285-6\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'lorscheid-felis-stocchi-obert-scholz-rovere-tidesinthelastinterglacialinsightsfromnotchgeometryandpalaeotidalmodelsinbonairenetherlandantilles-2017', 'http://dx.doi.org/10.1038/s41598-017-16285-6', event);\">\n    Tides in the Last Interglacial: Insights from notch geometry and palaeo tidal models in Bonaire, Netherland Antilles.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Lorscheid,  T.; Felis,  T.; Stocchi,  P.; Obert,  J., C.; Scholz,  D.;  and <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>\n</span>\n\n  \n\n</span>\n\n  <i>Scientific Reports</i>, 7(1): 1-9.  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=\"http://dx.doi.org/10.1038/s41598-017-16285-6\"\n     onclick=\"log_download('lorscheid-felis-stocchi-obert-scholz-rovere-tidesinthelastinterglacialinsightsfromnotchgeometryandpalaeotidalmodelsinbonairenetherlandantilles-2017', 'http://dx.doi.org/10.1038/s41598-017-16285-6', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Tides in the Last Interglacial: Insights from notch geometry and palaeo tidal models in Bonaire, Netherland Antilles [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1038/s41598-017-16285-6\"\n     onclick=\"log_download('lorscheid-felis-stocchi-obert-scholz-rovere-tidesinthelastinterglacialinsightsfromnotchgeometryandpalaeotidalmodelsinbonairenetherlandantilles-2017', 'http://doi.org/10.1038/s41598-017-16285-6', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/lorscheid-felis-stocchi-obert-scholz-rovere-tidesinthelastinterglacialinsightsfromnotchgeometryandpalaeotidalmodelsinbonairenetherlandantilles-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('lorscheid-felis-stocchi-obert-scholz-rovere-tidesinthelastinterglacialinsightsfromnotchgeometryandpalaeotidalmodelsinbonairenetherlandantilles-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Tides in the Last Interglacial: Insights from notch geometry and palaeo tidal models in Bonaire, Netherland Antilles},\n type = {article},\n year = {2017},\n pages = {1-9},\n volume = {7},\n websites = {http://dx.doi.org/10.1038/s41598-017-16285-6},\n publisher = {Springer US},\n id = {cb5bca11-8cb9-3f21-8351-097d44faa054},\n created = {2018-02-03T12:42:09.295Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-09-14T15:34:15.866Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Lorscheid2017d},\n private_publication = {false},\n abstract = {The study of past sea levels relies largely on the interpretation of sea-level indicators. Palaeo tidal notches are considered as one of the most precise sea-level indicators as their formation is closely tied to the local tidal range. We present geometric measurements of modern and palaeo (Marine Isotope Stage (MIS) 5e) tidal notches on Bonaire (southern Caribbean Sea) and results from two tidal simulations, using the present-day bathymetry and a palaeo-bathymetry. We use these two tools to investigate changes in the tidal range since MIS 5e. Our models show that the tidal range changes most significantly in shallow areas, whereas both, notch geometry and models results, suggest that steeper continental shelves, such as the ones bordering the island of Bonaire, are less affected to changes in tidal range in conditions of MIS 5e sea levels. We use our data and results to discuss the importance of considering changes in tidal range while reconstructing MIS 5e sea level histories, and we remark that it is possible to use hydrodynamic modelling and notch geometry as first-order proxies to assess whether, in a particular area, tidal range might have been different in MIS 5e with respect to today. Fossil},\n bibtype = {article},\n author = {Lorscheid, Thomas and Felis, Thomas and Stocchi, Paolo and Obert, J.C. Christina and Scholz, Denis and Rovere, Alessio},\n doi = {10.1038/s41598-017-16285-6},\n journal = {Scientific Reports},\n number = {1}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The study of past sea levels relies largely on the interpretation of sea-level indicators. Palaeo tidal notches are considered as one of the most precise sea-level indicators as their formation is closely tied to the local tidal range. We present geometric measurements of modern and palaeo (Marine Isotope Stage (MIS) 5e) tidal notches on Bonaire (southern Caribbean Sea) and results from two tidal simulations, using the present-day bathymetry and a palaeo-bathymetry. We use these two tools to investigate changes in the tidal range since MIS 5e. Our models show that the tidal range changes most significantly in shallow areas, whereas both, notch geometry and models results, suggest that steeper continental shelves, such as the ones bordering the island of Bonaire, are less affected to changes in tidal range in conditions of MIS 5e sea levels. We use our data and results to discuss the importance of considering changes in tidal range while reconstructing MIS 5e sea level histories, and we remark that it is possible to use hydrodynamic modelling and notch geometry as first-order proxies to assess whether, in a particular area, tidal range might have been different in MIS 5e with respect to today. Fossil\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"fellowes-gacutan-harris-vilaconcejo-webster-byrne-patternsofsedimenttransportusingforaminiferatracersacrosssandapronsonthegreatbarrierreef-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.bioone.org/doi/10.2112/JCOASTRES-D-16-00082.1\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'fellowes-gacutan-harris-vilaconcejo-webster-byrne-patternsofsedimenttransportusingforaminiferatracersacrosssandapronsonthegreatbarrierreef-2017', 'http://www.bioone.org/doi/10.2112/JCOASTRES-D-16-00082.1', event);\">\n    Patterns of Sediment Transport Using Foraminifera Tracers across Sand Aprons on the Great Barrier Reef.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Fellowes,  T., E.; Gacutan,  J.; Harris,  D., L.; Vila-Concejo,  A.; Webster,  J., M.;  and Byrne,  M.\n</span>\n\n  \n\n</span>\n\n  <i>Journal of Coastal Research</i>, 33(4): 864-873.  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=\"http://www.bioone.org/doi/10.2112/JCOASTRES-D-16-00082.1\"\n     onclick=\"log_download('fellowes-gacutan-harris-vilaconcejo-webster-byrne-patternsofsedimenttransportusingforaminiferatracersacrosssandapronsonthegreatbarrierreef-2017', 'http://www.bioone.org/doi/10.2112/JCOASTRES-D-16-00082.1', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Patterns of Sediment Transport Using Foraminifera Tracers across Sand Aprons on the Great Barrier Reef [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.2112/JCOASTRES-D-16-00082.1\"\n     onclick=\"log_download('fellowes-gacutan-harris-vilaconcejo-webster-byrne-patternsofsedimenttransportusingforaminiferatracersacrosssandapronsonthegreatbarrierreef-2017', 'http://doi.org/10.2112/JCOASTRES-D-16-00082.1', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/fellowes-gacutan-harris-vilaconcejo-webster-byrne-patternsofsedimenttransportusingforaminiferatracersacrosssandapronsonthegreatbarrierreef-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('fellowes-gacutan-harris-vilaconcejo-webster-byrne-patternsofsedimenttransportusingforaminiferatracersacrosssandapronsonthegreatbarrierreef-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Patterns of Sediment Transport Using Foraminifera Tracers across Sand Aprons on the Great Barrier Reef},\n type = {article},\n year = {2017},\n pages = {864-873},\n volume = {33},\n websites = {http://www.bioone.org/doi/10.2112/JCOASTRES-D-16-00082.1},\n id = {f1b13efb-e7ec-3abf-be89-0b240ef77579},\n created = {2018-02-03T12:42:09.320Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-09-14T15:34:15.852Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Fellowes2017},\n private_publication = {false},\n abstract = {© Coastal Education and Research Foundation, Inc. 2017. Sediment dynamics exert large control over coral reef geomorphological evolution and are vital to understanding past and present geomorphic responses. Large benthic foraminifera (LBF) live in the algal reef flats, and their tests (shells) are transported post-mortem by waves and currents onto back-reef environments, including sand aprons. This study investigated the patterns of transport linking surficial and downcore sediments in samples from three sand aprons with different wave exposures at One Tree Reef on the southern Great Barrier Reef (Australia). Six LBF genera represented up to 32% of the sediments analysed. Lagoonward transport increased LBF test abrasion and sediment bulk density. Sediment grain size and LBF abundance in sediments also decreased with lagoonward transport. Sediment transport patterns indicated by LBF species used as tracer were consistent with the prominent E-SE wave environment. A novel taphofacies approach was used to describe stratigraphic layers in downcore sediments based on LBF test abrasion and abundance. Varied sediment deposition rates did not affect the LBF test abrasion signature downcore. It appears that Baculogypsina sphaerulata has been the dominant species for at least 3 ka. Tests that were deposited slowly exhibited less or the same levels of abrasion than those that were rapidly deposited. It appears that test abrasion is primarily determined by the distance travelled rather than the influence of increased age or chemical dissolution.},\n bibtype = {article},\n author = {Fellowes, Thomas E. and Gacutan, Jordan and Harris, Daniel L. and Vila-Concejo, Ana and Webster, Jody M. and Byrne, Maria},\n doi = {10.2112/JCOASTRES-D-16-00082.1},\n journal = {Journal of Coastal Research},\n number = {4}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  © Coastal Education and Research Foundation, Inc. 2017. Sediment dynamics exert large control over coral reef geomorphological evolution and are vital to understanding past and present geomorphic responses. Large benthic foraminifera (LBF) live in the algal reef flats, and their tests (shells) are transported post-mortem by waves and currents onto back-reef environments, including sand aprons. This study investigated the patterns of transport linking surficial and downcore sediments in samples from three sand aprons with different wave exposures at One Tree Reef on the southern Great Barrier Reef (Australia). Six LBF genera represented up to 32% of the sediments analysed. Lagoonward transport increased LBF test abrasion and sediment bulk density. Sediment grain size and LBF abundance in sediments also decreased with lagoonward transport. Sediment transport patterns indicated by LBF species used as tracer were consistent with the prominent E-SE wave environment. A novel taphofacies approach was used to describe stratigraphic layers in downcore sediments based on LBF test abrasion and abundance. Varied sediment deposition rates did not affect the LBF test abrasion signature downcore. It appears that Baculogypsina sphaerulata has been the dominant species for at least 3 ka. Tests that were deposited slowly exhibited less or the same levels of abrasion than those that were rapidly deposited. It appears that test abrasion is primarily determined by the distance travelled rather than the influence of increased age or chemical dissolution.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"janen-wizemann-klicpera-satari-westphal-mann-sedimentcompositionandfaciesofcoralreefislandsinthespermondearchipelagoindonesia-2017\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://journal.frontiersin.org/article/10.3389/fmars.2017.00144/full\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'janen-wizemann-klicpera-satari-westphal-mann-sedimentcompositionandfaciesofcoralreefislandsinthespermondearchipelagoindonesia-2017', 'http://journal.frontiersin.org/article/10.3389/fmars.2017.00144/full', event);\">\n    Sediment Composition and Facies of Coral Reef Islands in the Spermonde Archipelago, Indonesia.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Janßen,  A.; Wizemann,  A.; Klicpera,  A.; Satari,  D., Y.; Westphal,  H.;  and Mann,  T.\n</span>\n\n  \n\n</span>\n\n  <i>Frontiers in Marine Science</i>, 4(May): 1-13.  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=\"http://journal.frontiersin.org/article/10.3389/fmars.2017.00144/full\"\n     onclick=\"log_download('janen-wizemann-klicpera-satari-westphal-mann-sedimentcompositionandfaciesofcoralreefislandsinthespermondearchipelagoindonesia-2017', 'http://journal.frontiersin.org/article/10.3389/fmars.2017.00144/full', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Sediment Composition and Facies of Coral Reef Islands in the Spermonde Archipelago, Indonesia [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.3389/fmars.2017.00144\"\n     onclick=\"log_download('janen-wizemann-klicpera-satari-westphal-mann-sedimentcompositionandfaciesofcoralreefislandsinthespermondearchipelagoindonesia-2017', 'http://doi.org/10.3389/fmars.2017.00144', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/janen-wizemann-klicpera-satari-westphal-mann-sedimentcompositionandfaciesofcoralreefislandsinthespermondearchipelagoindonesia-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\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('janen-wizemann-klicpera-satari-westphal-mann-sedimentcompositionandfaciesofcoralreefislandsinthespermondearchipelagoindonesia-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Sediment Composition and Facies of Coral Reef Islands in the Spermonde Archipelago, Indonesia},\n type = {article},\n year = {2017},\n keywords = {carbonate sediments, grain size, skeletal constitu},\n pages = {1-13},\n volume = {4},\n websites = {http://journal.frontiersin.org/article/10.3389/fmars.2017.00144/full},\n id = {c0dff020-5319-3fd2-93e8-d982132be5aa},\n created = {2018-02-03T12:42:09.395Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-09-14T15:34:15.991Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Janßen2017a},\n private_publication = {false},\n bibtype = {article},\n author = {Janßen, Alexander and Wizemann, André and Klicpera, André and Satari, Dewi Y. and Westphal, Hildegard and Mann, Thomas},\n doi = {10.3389/fmars.2017.00144},\n journal = {Frontiers in Marine Science},\n number = {May}\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_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        (9)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"vacchi-marriner-morhange-spada-fontana-rovere-marriner-morhange-etal-multiproxyassessmentofholocenerelativesealevelchangesinthewesternmediterraneanvariabilityinthesealevelhistoriesandredefinitionoftheisostaticsignal-2016\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://dx.doi.org/10.1016/j.earscirev.2016.02.002\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'vacchi-marriner-morhange-spada-fontana-rovere-marriner-morhange-etal-multiproxyassessmentofholocenerelativesealevelchangesinthewesternmediterraneanvariabilityinthesealevelhistoriesandredefinitionoftheisostaticsignal-2016', 'http://dx.doi.org/10.1016/j.earscirev.2016.02.002', event);\">\n    Multiproxy assessment of Holocene relative sea-level changes in the western Mediterranean: variability in the sea-level histories and redefinition of the isostatic signal.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Vacchi,  M.; Marriner,  N.; Morhange,  C.; Spada,  G.; Fontana,  A.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Marriner,  N.; Morhange,  C.; Spada,  G.;  and Fontana,  A.\n</span>\n\n  \n\n</span>\n\n  <i>Earth Science Reviews</i>, 155: 172-197.  2016.\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://dx.doi.org/10.1016/j.earscirev.2016.02.002\"\n     onclick=\"log_download('vacchi-marriner-morhange-spada-fontana-rovere-marriner-morhange-etal-multiproxyassessmentofholocenerelativesealevelchangesinthewesternmediterraneanvariabilityinthesealevelhistoriesandredefinitionoftheisostaticsignal-2016', 'http://dx.doi.org/10.1016/j.earscirev.2016.02.002', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Multiproxy assessment of Holocene relative sea-level changes in the western Mediterranean: variability in the sea-level histories and redefinition of the isostatic signal. [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.earscirev.2016.02.002\"\n     onclick=\"log_download('vacchi-marriner-morhange-spada-fontana-rovere-marriner-morhange-etal-multiproxyassessmentofholocenerelativesealevelchangesinthewesternmediterraneanvariabilityinthesealevelhistoriesandredefinitionoftheisostaticsignal-2016', 'http://doi.org/10.1016/j.earscirev.2016.02.002', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/vacchi-marriner-morhange-spada-fontana-rovere-marriner-morhange-etal-multiproxyassessmentofholocenerelativesealevelchangesinthewesternmediterraneanvariabilityinthesealevelhistoriesandredefinitionoftheisostaticsignal-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('vacchi-marriner-morhange-spada-fontana-rovere-marriner-morhange-etal-multiproxyassessmentofholocenerelativesealevelchangesinthewesternmediterraneanvariabilityinthesealevelhistoriesandredefinitionoftheisostaticsignal-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{\n title = {Multiproxy assessment of Holocene relative sea-level changes in the western Mediterranean: variability in the sea-level histories and redefinition of the isostatic signal.},\n type = {article},\n year = {2016},\n keywords = {Holocene,Isostatic adjustment,Mediterranean Sea,Sea-level database,Sea-level proxy},\n pages = {172-197},\n volume = {155},\n websites = {http://dx.doi.org/10.1016/j.earscirev.2016.02.002},\n publisher = {Elsevier B.V.},\n city = {Vienna, AT},\n id = {87ba1930-b220-369d-8afd-6fdf358bb6d5},\n created = {2018-02-03T12:42:07.277Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:07.277Z},\n read = {true},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Vacchi},\n private_publication = {false},\n abstract = {A review of 917 relative sea-level (RSL) data-points has resulted in the first quality-controlled database constraining the Holocene sea-level histories of the western Mediterranean Sea (Spain, France, Italy, Slovenia, Croatia, Malta and Tunisia). We reviewed and standardized the geological RSL data-points using a new multi-proxy methodology based on: (1) modern taxa assemblages in Mediterranean lagoons and marshes; (2) beachrock characteristics (cement fabric and chemistry, sedimentary structures); and (3) the modern distribution of Mediterranean fixed biological indicators. These RSL data-points were coupled with the large number of archaeological RSL indicators available for the western Mediterranean. We assessed the spatial variability of RSL histories for 22 regions and compared these with the ICE-5G (VM2) GIA model. In the western Mediterranean, RSL rose continuously for the whole Holocene with a sudden slowdown at ~. 7.5 ka BP and a further deceleration during the last ~. 4.0 ka BP, after which time observed RSL changes are mainly related to variability in isostatic adjustment. The sole exception is southern Tunisia, where data show evidence of a mid-Holocene high-stand compatible with the isostatic impacts of the melting history of the remote Antarctic ice sheet.Our results indicate that late-Holocene sea-level rise was significantly slower than the current one. First estimates of GIA contribution indicate that, at least in the northwestern sector, it accounts at least for the 25-30% of the ongoing sea-level rise recorded by Mediterranean tidal gauges. Such contribution is less constrained at lower latitudes due to the lower quality of the late Holocene index points. Future applications of spatio-temporal statistical techniques are required to better quantify the gradient of the isostatic contribution and to provide improved context for the assessment of 20th century acceleration of Mediterranean sea-level rise.},\n bibtype = {article},\n author = {Vacchi, Matteo and Marriner, Nick and Morhange, Christophe and Spada, Giorgio and Fontana, Alessandro and Rovere, Alessio and Marriner, Nick and Morhange, Christophe and Spada, Giorgio and Fontana, Alessandro},\n doi = {10.1016/j.earscirev.2016.02.002},\n journal = {Earth Science Reviews}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  A review of 917 relative sea-level (RSL) data-points has resulted in the first quality-controlled database constraining the Holocene sea-level histories of the western Mediterranean Sea (Spain, France, Italy, Slovenia, Croatia, Malta and Tunisia). We reviewed and standardized the geological RSL data-points using a new multi-proxy methodology based on: (1) modern taxa assemblages in Mediterranean lagoons and marshes; (2) beachrock characteristics (cement fabric and chemistry, sedimentary structures); and (3) the modern distribution of Mediterranean fixed biological indicators. These RSL data-points were coupled with the large number of archaeological RSL indicators available for the western Mediterranean. We assessed the spatial variability of RSL histories for 22 regions and compared these with the ICE-5G (VM2) GIA model. In the western Mediterranean, RSL rose continuously for the whole Holocene with a sudden slowdown at ~. 7.5 ka BP and a further deceleration during the last ~. 4.0 ka BP, after which time observed RSL changes are mainly related to variability in isostatic adjustment. The sole exception is southern Tunisia, where data show evidence of a mid-Holocene high-stand compatible with the isostatic impacts of the melting history of the remote Antarctic ice sheet.Our results indicate that late-Holocene sea-level rise was significantly slower than the current one. First estimates of GIA contribution indicate that, at least in the northwestern sector, it accounts at least for the 25-30% of the ongoing sea-level rise recorded by Mediterranean tidal gauges. Such contribution is less constrained at lower latitudes due to the lower quality of the late Holocene index points. Future applications of spatio-temporal statistical techniques are required to better quantify the gradient of the isostatic contribution and to provide improved context for the assessment of 20th century acceleration of Mediterranean sea-level rise.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"dechnik-webster-nothdurft-webb-zhao-duce-braga-harris-etal-influenceofhydrodynamicenergyonholocenereefflataccretiongreatbarrierreef-2016\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Influence of hydrodynamic energy on Holocene reef flat accretion, Great Barrier Reef.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Dechnik,  B.; Webster,  J., M.; Nothdurft,  L.; Webb,  G., E.; Zhao,  J., x.; Duce,  S.; Braga,  J., C.; Harris,  D., L.; Vila-Concejo,  A.;  and Puotinen,  M.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Research (United States)</i>, 85(1): 44-53.  2016.\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.yqres.2015.11.002\"\n     onclick=\"log_download('dechnik-webster-nothdurft-webb-zhao-duce-braga-harris-etal-influenceofhydrodynamicenergyonholocenereefflataccretiongreatbarrierreef-2016', 'http://doi.org/10.1016/j.yqres.2015.11.002', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/dechnik-webster-nothdurft-webb-zhao-duce-braga-harris-etal-influenceofhydrodynamicenergyonholocenereefflataccretiongreatbarrierreef-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('dechnik-webster-nothdurft-webb-zhao-duce-braga-harris-etal-influenceofhydrodynamicenergyonholocenereefflataccretiongreatbarrierreef-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Influence of hydrodynamic energy on Holocene reef flat accretion, Great Barrier Reef},\n type = {article},\n year = {2016},\n keywords = {Accretion,Great Barrier Reef,Holocene,Reef growth,Sea level,Still-stand},\n pages = {44-53},\n volume = {85},\n id = {80f43001-f620-38f0-834d-7973e06d9e9f},\n created = {2018-02-03T12:42:07.847Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:07.847Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Dechnik2016},\n private_publication = {false},\n abstract = {The response of platform reefs to sea-level stabilization over the past 6 ka is well established for the Great Barrier Reef (GBR), with reefs typically accreting laterally from windward to leeward. However, these observations are based on few cores spread across reef zones and may not accurately reflect a reef&#x27;s true accretional response to the Holocene stillstand. We present a new record of reef accretion based on 49 U/Th ages from Heron and One Tree reefs in conjunction with re-analyzed data from 14 reefs across the GBR. We demonstrate that hydrodynamic energy is the main driver of accretional direction; exposed reefs accreted primarily lagoon-ward while protected reefs accreted seawards, contrary to the traditional growth model in the GBR. Lateral accretion rates varied from 86.3 m/ka-42.4 m/ka on the exposed One Tree windward reef and 68.35 m/ka-15.7 m/ka on the protected leeward Heron reef, suggesting that wind/wave energy is not a dominant control on lateral accretion rates. This represents the most comprehensive statement of lateral accretion direction and rates from the mid-outer platform reefs of the GBR, confirming great variability in reef flat growth both within and between reef margins over the last 6 ka, and highlighting the need for closely-spaced transects.},\n bibtype = {article},\n author = {Dechnik, Belinda and Webster, Jody M. and Nothdurft, Luke and Webb, Gregory E. and Zhao, Jian xin and Duce, Stephanie and Braga, Juan C. and Harris, Daniel L. and Vila-Concejo, Ana and Puotinen, Marji},\n doi = {10.1016/j.yqres.2015.11.002},\n journal = {Quaternary Research (United States)},\n number = {1}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The response of platform reefs to sea-level stabilization over the past 6 ka is well established for the Great Barrier Reef (GBR), with reefs typically accreting laterally from windward to leeward. However, these observations are based on few cores spread across reef zones and may not accurately reflect a reef's true accretional response to the Holocene stillstand. We present a new record of reef accretion based on 49 U/Th ages from Heron and One Tree reefs in conjunction with re-analyzed data from 14 reefs across the GBR. We demonstrate that hydrodynamic energy is the main driver of accretional direction; exposed reefs accreted primarily lagoon-ward while protected reefs accreted seawards, contrary to the traditional growth model in the GBR. Lateral accretion rates varied from 86.3 m/ka-42.4 m/ka on the exposed One Tree windward reef and 68.35 m/ka-15.7 m/ka on the protected leeward Heron reef, suggesting that wind/wave energy is not a dominant control on lateral accretion rates. This represents the most comprehensive statement of lateral accretion direction and rates from the mid-outer platform reefs of the GBR, confirming great variability in reef flat growth both within and between reef margins over the last 6 ka, and highlighting the need for closely-spaced transects.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"cardini-bednarz-vanhoytema-rovere-naumann-alrshaidat-wild-budgetofprimaryproductionanddinitrogenfixationinahighlyseasonalredseacoralreef-2016\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Budget of Primary Production and Dinitrogen Fixation in a Highly Seasonal Red Sea Coral Reef.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Cardini,  U.; Bednarz,  V., N.; van Hoytema,  N.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Naumann,  M., S.; Al-Rshaidat,  M., M.;  and Wild,  C.\n</span>\n\n  \n\n</span>\n\n  <i>Ecosystems</i>, 19(5): 771-785.  2016.\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/s10021-016-9966-1\"\n     onclick=\"log_download('cardini-bednarz-vanhoytema-rovere-naumann-alrshaidat-wild-budgetofprimaryproductionanddinitrogenfixationinahighlyseasonalredseacoralreef-2016', 'http://doi.org/10.1007/s10021-016-9966-1', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/cardini-bednarz-vanhoytema-rovere-naumann-alrshaidat-wild-budgetofprimaryproductionanddinitrogenfixationinahighlyseasonalredseacoralreef-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('cardini-bednarz-vanhoytema-rovere-naumann-alrshaidat-wild-budgetofprimaryproductionanddinitrogenfixationinahighlyseasonalredseacoralreef-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Budget of Primary Production and Dinitrogen Fixation in a Highly Seasonal Red Sea Coral Reef},\n type = {article},\n year = {2016},\n keywords = {Biogeochemical cycling,Diazotrophy,Gulf of Aqaba,Nutrient budget,Photosynthesis,Productivity},\n pages = {771-785},\n volume = {19},\n id = {89d9bbe3-e931-365f-9e12-f705ba1067e4},\n created = {2018-02-03T12:42:07.876Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.109Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Cardini},\n private_publication = {false},\n abstract = {Biological dinitrogen (N2) fixation (diazotrophy, BNF) relieves marine primary producers of nitrogen (N) limitation in a large part of the world oceans. N concentrations are particularly low in tropical regions where coral reefs are located, and N is therefore a key limiting nutrient for these productive ecosystems. In this context, the importance of diazotrophy for reef productivity is still not resolved, with studies up to now lacking organismal and seasonal resolution. Here, we present a budget of gross primary production (GPP) and BNF for a highly seasonal Red Sea fringing reef, based on ecophysiological and benthic cover measurements combined with geospatial analyses. Benthic GPP varied from 215 to 262 mmol C m -2 reef d-1, with hard corals making the largest contribution (41-76%). Diazotrophy was omnipresent in space and time, and benthic BNF varied from 0.16 to 0.92 mmol N m-2 reef d-1. Planktonic GPP and BNF rates were respectively approximately 60- and 20-fold lower than those of the benthos, emphasizing the importance of the benthic compartment in reef biogeochemical cycling. BNF showed higher sensitivity to seasonality than GPP, implying greater climatic control on reef BNF. Up to about 20% of net reef primary production could be supported by BNF during summer, suggesting a strong biogeochemical coupling between diazotrophy and the reef carbon cycle. Details},\n bibtype = {article},\n author = {Cardini, Ulisse and Bednarz, Vanessa N. and van Hoytema, Nanne and Rovere, Alessio and Naumann, Malik S. and Al-Rshaidat, Mamoon M.D. and Wild, Christian},\n doi = {10.1007/s10021-016-9966-1},\n journal = {Ecosystems},\n number = {5}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Biological dinitrogen (N2) fixation (diazotrophy, BNF) relieves marine primary producers of nitrogen (N) limitation in a large part of the world oceans. N concentrations are particularly low in tropical regions where coral reefs are located, and N is therefore a key limiting nutrient for these productive ecosystems. In this context, the importance of diazotrophy for reef productivity is still not resolved, with studies up to now lacking organismal and seasonal resolution. Here, we present a budget of gross primary production (GPP) and BNF for a highly seasonal Red Sea fringing reef, based on ecophysiological and benthic cover measurements combined with geospatial analyses. Benthic GPP varied from 215 to 262 mmol C m -2 reef d-1, with hard corals making the largest contribution (41-76%). Diazotrophy was omnipresent in space and time, and benthic BNF varied from 0.16 to 0.92 mmol N m-2 reef d-1. Planktonic GPP and BNF rates were respectively approximately 60- and 20-fold lower than those of the benthos, emphasizing the importance of the benthic compartment in reef biogeochemical cycling. BNF showed higher sensitivity to seasonality than GPP, implying greater climatic control on reef BNF. Up to about 20% of net reef primary production could be supported by BNF during summer, suggesting a strong biogeochemical coupling between diazotrophy and the reef carbon cycle. Details\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"rovere-stocchi-vacchi-eustaticandrelativesealevelchanges-2016\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://link.springer.com/10.1007/s40641-016-0045-7,http://dx.doi.org/10.1007/s40641-016-0045-7\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'rovere-stocchi-vacchi-eustaticandrelativesealevelchanges-2016', 'http://link.springer.com/10.1007/s40641-016-0045-7,http://dx.doi.org/10.1007/s40641-016-0045-7', event);\">\n    Eustatic and Relative Sea Level Changes.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Stocchi,  P.;  and Vacchi,  M.\n</span>\n\n  \n\n</span>\n\n  <i>Current Climate Change Reports</i>, 2(4): 221-231. 12 2016.\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://link.springer.com/10.1007/s40641-016-0045-7,http://dx.doi.org/10.1007/s40641-016-0045-7\"\n     onclick=\"log_download('rovere-stocchi-vacchi-eustaticandrelativesealevelchanges-2016', 'http://link.springer.com/10.1007/s40641-016-0045-7,http://dx.doi.org/10.1007/s40641-016-0045-7', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Eustatic and Relative Sea Level Changes [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1007/s40641-016-0045-7\"\n     onclick=\"log_download('rovere-stocchi-vacchi-eustaticandrelativesealevelchanges-2016', 'http://doi.org/10.1007/s40641-016-0045-7', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/rovere-stocchi-vacchi-eustaticandrelativesealevelchanges-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('rovere-stocchi-vacchi-eustaticandrelativesealevelchanges-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  \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{\n title = {Eustatic and Relative Sea Level Changes},\n type = {article},\n year = {2016},\n keywords = {Eustasy,GIA,Isost,Isostasy,Relative sea level,Sea level,Sea level changes,eustasy,gia,isostasy,of the topical collection,on sea level projections,relative sea level,sea level,sea level changes,this article is part},\n pages = {221-231},\n volume = {2},\n websites = {http://link.springer.com/10.1007/s40641-016-0045-7,http://dx.doi.org/10.1007/s40641-016-0045-7},\n month = {12},\n publisher = {Current Climate Change Reports},\n day = {2},\n id = {2e5440fd-63cc-31d6-82b6-b5a3be4b490c},\n created = {2018-02-03T12:42:08.574Z},\n accessed = {2017-04-19},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:08.574Z},\n read = {true},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Rovere2016},\n source_type = {article},\n private_publication = {false},\n abstract = {Sea level changes can be driven by either variations in the masses or volume of the oceans, or by changes of the land with respect to the sea surface. In the first case, a sea level change is defined &#x60;eustatic&#x27;; otherwise, it is defined &#x60;relative&#x27;. Several techniques can be used to observe changes in sea level, from satellite data to tide gauges to geological or archeological proxies. Regardless of the technique used, &#x60;eustasy&#x27; cannot be measured directly, but only calculated after perturbing factors of different origins are taken into account. In this paper, we review the meaning and main processes that contribute to eustatic and relative sea level changes, and we give an overview of the different techniques used to observe them.},\n bibtype = {article},\n author = {Rovere, Alessio and Stocchi, Paolo and Vacchi, Matteo},\n doi = {10.1007/s40641-016-0045-7},\n journal = {Current Climate Change Reports},\n number = {4}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Sea level changes can be driven by either variations in the masses or volume of the oceans, or by changes of the land with respect to the sea surface. In the first case, a sea level change is defined `eustatic'; otherwise, it is defined `relative'. Several techniques can be used to observe changes in sea level, from satellite data to tide gauges to geological or archeological proxies. Regardless of the technique used, `eustasy' cannot be measured directly, but only calculated after perturbing factors of different origins are taken into account. In this paper, we review the meaning and main processes that contribute to eustatic and relative sea level changes, and we give an overview of the different techniques used to observe them.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"mann-rovere-schne-klicpera-stocchi-lukman-westphal-themagnitudeofamidholocenesealevelhighstandinthestraitofmakassar-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/S0169555X15302427,http://dx.doi.org/10.1016/j.geomorph.2015.12.023\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'mann-rovere-schne-klicpera-stocchi-lukman-westphal-themagnitudeofamidholocenesealevelhighstandinthestraitofmakassar-2016', 'http://www.sciencedirect.com/science/article/pii/S0169555X15302427,http://dx.doi.org/10.1016/j.geomorph.2015.12.023', event);\">\n    The magnitude of a mid-Holocene sea-level highstand in the Strait of Makassar.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Mann,  T.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Schöne,  T.; Klicpera,  A.; Stocchi,  P.; Lukman,  M.;  and Westphal,  H.\n</span>\n\n  \n\n</span>\n\n  <i>Geomorphology</i>, 257: 155-163.  2016.\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/S0169555X15302427,http://dx.doi.org/10.1016/j.geomorph.2015.12.023\"\n     onclick=\"log_download('mann-rovere-schne-klicpera-stocchi-lukman-westphal-themagnitudeofamidholocenesealevelhighstandinthestraitofmakassar-2016', 'http://www.sciencedirect.com/science/article/pii/S0169555X15302427,http://dx.doi.org/10.1016/j.geomorph.2015.12.023', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"The magnitude of a mid-Holocene sea-level highstand in the Strait of Makassar [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.geomorph.2015.12.023\"\n     onclick=\"log_download('mann-rovere-schne-klicpera-stocchi-lukman-westphal-themagnitudeofamidholocenesealevelhighstandinthestraitofmakassar-2016', 'http://doi.org/10.1016/j.geomorph.2015.12.023', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/mann-rovere-schne-klicpera-stocchi-lukman-westphal-themagnitudeofamidholocenesealevelhighstandinthestraitofmakassar-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('mann-rovere-schne-klicpera-stocchi-lukman-westphal-themagnitudeofamidholocenesealevelhighstandinthestraitofmakassar-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {The magnitude of a mid-Holocene sea-level highstand in the Strait of Makassar},\n type = {article},\n year = {2016},\n keywords = {Glacial isostatic adjustment,Indo-Pacific,Spermonde Shelf,Sulawesi},\n pages = {155-163},\n volume = {257},\n websites = {http://www.sciencedirect.com/science/article/pii/S0169555X15302427,http://dx.doi.org/10.1016/j.geomorph.2015.12.023},\n publisher = {Elsevier B.V.},\n id = {9954079d-a126-3204-9852-4918ab7f9b80},\n created = {2018-02-03T12:42:08.888Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:08.888Z},\n read = {true},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {mann2015magnitude},\n source_type = {article},\n private_publication = {false},\n abstract = {Knowledge on the timing and magnitude of past sea-level changes is essential to understand modern and future sea-level variability. Holocene sea-level data from literature on the west coast of Sulawesi, central Indonesia, suggest that this region experienced two relative sea-level highstands over the last 6000years, with magnitudes exceeding two meters. However, recent datasets from the Indo-Pacific region do not support high-magnitude sea-level oscillations during the Holocene in tectonically stable far-field locations. Here we present a new, high-precision, mid-Holocene sea-level dataset from the Spermonde Shelf off southwest Sulawesi. We surveyed 21 fossil microatolls on the reef flats of two coral islands (Pulau Panambungan and Pulau Barrang Lompo) and referred their elevations to local mean sea level and to the height of living coral. Radiometrically calibrated ages from emergent fossil microatolls on Pulau Panambungan indicate a relative sea-level highstand not exceeding 0.5m above present at ca. 5600cal.yrBP. The highstand is followed by a relatively rapid sea-level fall towards present sea level that was reached at around 4000cal.yrBP. Fossil microatolls from nearby Pulau Barrang Lompo show the same trend, however with a coherent negative vertical offset of about 0.8m compared to their equivalents on Pulau Panambungan. The largely consistent gradients of both trends (~−0.14mmyr−1), the consistent elevation of living microatolls in the Spermonde, and a number of instructive geomorphic features indicate a localized, post-formational and probably recent drop of the fossil microatolls on the densely populated island Pulau Barrang Lompo. The relative sea-level trend inferred from Pulau Panambungan is well within the range of geophysical predictions based on ANICE-SELEN ice sheet model, which predict a highstand that is significantly lower than those predicted by other GIA models for this area. Although a complete interpretation of the Holocene sea-level history will require additional high-resolution datasets from this and surrounding territories in SE Asia, our results suggest that there was merely a single Holocene highstand in central Indonesia, the magnitude of which was substantially lower than hitherto assumed.},\n bibtype = {article},\n author = {Mann, Thomas and Rovere, Alessio and Schöne, Tilo and Klicpera, André and Stocchi, Paolo and Lukman, Muhammad and Westphal, Hildegard},\n doi = {10.1016/j.geomorph.2015.12.023},\n journal = {Geomorphology}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Knowledge on the timing and magnitude of past sea-level changes is essential to understand modern and future sea-level variability. Holocene sea-level data from literature on the west coast of Sulawesi, central Indonesia, suggest that this region experienced two relative sea-level highstands over the last 6000years, with magnitudes exceeding two meters. However, recent datasets from the Indo-Pacific region do not support high-magnitude sea-level oscillations during the Holocene in tectonically stable far-field locations. Here we present a new, high-precision, mid-Holocene sea-level dataset from the Spermonde Shelf off southwest Sulawesi. We surveyed 21 fossil microatolls on the reef flats of two coral islands (Pulau Panambungan and Pulau Barrang Lompo) and referred their elevations to local mean sea level and to the height of living coral. Radiometrically calibrated ages from emergent fossil microatolls on Pulau Panambungan indicate a relative sea-level highstand not exceeding 0.5m above present at ca. 5600cal.yrBP. The highstand is followed by a relatively rapid sea-level fall towards present sea level that was reached at around 4000cal.yrBP. Fossil microatolls from nearby Pulau Barrang Lompo show the same trend, however with a coherent negative vertical offset of about 0.8m compared to their equivalents on Pulau Panambungan. The largely consistent gradients of both trends (~−0.14mmyr−1), the consistent elevation of living microatolls in the Spermonde, and a number of instructive geomorphic features indicate a localized, post-formational and probably recent drop of the fossil microatolls on the densely populated island Pulau Barrang Lompo. The relative sea-level trend inferred from Pulau Panambungan is well within the range of geophysical predictions based on ANICE-SELEN ice sheet model, which predict a highstand that is significantly lower than those predicted by other GIA models for this area. Although a complete interpretation of the Holocene sea-level history will require additional high-resolution datasets from this and surrounding territories in SE Asia, our results suggest that there was merely a single Holocene highstand in central Indonesia, the magnitude of which was substantially lower than hitherto assumed.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"dsterhus-rovere-carlson-horton-klemann-tarasov-barlow-bradwell-etal-palaeosealevelandpalaeoicesheetdatabasesproblemsstrategiesandperspectives-2016\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.clim-past.net/12/911/2016/\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'dsterhus-rovere-carlson-horton-klemann-tarasov-barlow-bradwell-etal-palaeosealevelandpalaeoicesheetdatabasesproblemsstrategiesandperspectives-2016', 'http://www.clim-past.net/12/911/2016/', event);\">\n    Palaeo-sea-level and palaeo-ice-sheet databases: problems, strategies, and perspectives.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Düsterhus,  A.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Carlson,  A., E.; Horton,  B., P.; Klemann,  V.; Tarasov,  L.; Barlow,  N., L., M.; Bradwell,  T.; Clark,  J.; Dutton,  A.; Gehrels,  W., R.; Hibbert,  F., D.; Hijma,  M., P.; Khan,  N.; Kopp,  R., E.; Sivan,  D.;  and Törnqvist,  T., E.\n</span>\n\n  \n\n</span>\n\n  <i>Climate of the Past</i>, 12(4): 911-921.  2016.\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.clim-past.net/12/911/2016/\"\n     onclick=\"log_download('dsterhus-rovere-carlson-horton-klemann-tarasov-barlow-bradwell-etal-palaeosealevelandpalaeoicesheetdatabasesproblemsstrategiesandperspectives-2016', 'http://www.clim-past.net/12/911/2016/', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Palaeo-sea-level and palaeo-ice-sheet databases: problems, strategies, and perspectives [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.5194/cp-12-911-2016\"\n     onclick=\"log_download('dsterhus-rovere-carlson-horton-klemann-tarasov-barlow-bradwell-etal-palaeosealevelandpalaeoicesheetdatabasesproblemsstrategiesandperspectives-2016', 'http://doi.org/10.5194/cp-12-911-2016', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/dsterhus-rovere-carlson-horton-klemann-tarasov-barlow-bradwell-etal-palaeosealevelandpalaeoicesheetdatabasesproblemsstrategiesandperspectives-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('dsterhus-rovere-carlson-horton-klemann-tarasov-barlow-bradwell-etal-palaeosealevelandpalaeoicesheetdatabasesproblemsstrategiesandperspectives-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Palaeo-sea-level and palaeo-ice-sheet databases: problems, strategies, and perspectives},\n type = {article},\n year = {2016},\n pages = {911-921},\n volume = {12},\n websites = {http://www.clim-past.net/12/911/2016/},\n id = {8ca5dd97-7c80-38c9-a445-f8daef1ce5b3},\n created = {2018-02-03T12:42:08.890Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:08.890Z},\n read = {true},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Dusterhus2016},\n private_publication = {false},\n abstract = {&lt;p&gt;Sea-level and ice-sheet databases have driven numerous advances in understanding the Earth system. We describe the challenges and offer best strategies that can be adopted to build self-consistent and standardised databases of geological and geochemical information used to archive palaeo-sea-levels and palaeo-ice-sheets. There are three phases in the development of a database: (i) measurement, (ii) interpretation, and (iii) database creation. Measurement should include the objective description of the position and age of a sample, description of associated geological features, and quantification of uncertainties. Interpretation of the sample may have a subjective component, but it should always include uncertainties and alternative or contrasting interpretations, with any exclusion of existing interpretations requiring a full justification. During the creation of a database, an approach based on accessibility, transparency, trust, availability, continuity, completeness, and communication of content (ATTAC&lt;sup&gt;3&lt;/sup&gt;) must be adopted. It is essential to consider the community that creates and benefits from a database. We conclude that funding agencies should not only consider the creation of original data in specific research-question-oriented projects, but also include the possibility of using part of the funding for IT-related and database creation tasks, which are essential to guarantee accessibility and maintenance of the collected data.&lt;/p&gt;},\n bibtype = {article},\n author = {Düsterhus, André and Rovere, Alessio and Carlson, Anders E. and Horton, Benjamin P. and Klemann, Volker and Tarasov, Lev and Barlow, Natasha L. M. and Bradwell, Tom and Clark, Jorie and Dutton, Andrea and Gehrels, W. Roland and Hibbert, Fiona D. and Hijma, Marc P. and Khan, Nicole and Kopp, Robert E. and Sivan, Dorit and Törnqvist, Torbjörn E.},\n doi = {10.5194/cp-12-911-2016},\n journal = {Climate of the Past},\n number = {4}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  <p>Sea-level and ice-sheet databases have driven numerous advances in understanding the Earth system. We describe the challenges and offer best strategies that can be adopted to build self-consistent and standardised databases of geological and geochemical information used to archive palaeo-sea-levels and palaeo-ice-sheets. There are three phases in the development of a database: (i) measurement, (ii) interpretation, and (iii) database creation. Measurement should include the objective description of the position and age of a sample, description of associated geological features, and quantification of uncertainties. Interpretation of the sample may have a subjective component, but it should always include uncertainties and alternative or contrasting interpretations, with any exclusion of existing interpretations requiring a full justification. During the creation of a database, an approach based on accessibility, transparency, trust, availability, continuity, completeness, and communication of content (ATTAC<sup>3</sup>) must be adopted. It is essential to consider the community that creates and benefits from a database. We conclude that funding agencies should not only consider the creation of original data in specific research-question-oriented projects, but also include the possibility of using part of the funding for IT-related and database creation tasks, which are essential to guarantee accessibility and maintenance of the collected data.</p>\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"casella-rovere-pedroncini-stark-casella-ferrari-firpo-dronesastoolsformonitoringbeachtopographychangesintheligurianseanwmediterranean-2016\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Drones as tools for monitoring beach topography changes in the Ligurian Sea (NW Mediterranean).\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Casella,  E.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Pedroncini,  A.; Stark,  C., P.; Casella,  M.; Ferrari,  M.;  and Firpo,  M.\n</span>\n\n  \n\n</span>\n\n  <i>Geo-Marine Letters</i>, 36(2): 151-163.  2016.\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/s00367-016-0435-9\"\n     onclick=\"log_download('casella-rovere-pedroncini-stark-casella-ferrari-firpo-dronesastoolsformonitoringbeachtopographychangesintheligurianseanwmediterranean-2016', 'http://doi.org/10.1007/s00367-016-0435-9', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/casella-rovere-pedroncini-stark-casella-ferrari-firpo-dronesastoolsformonitoringbeachtopographychangesintheligurianseanwmediterranean-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('casella-rovere-pedroncini-stark-casella-ferrari-firpo-dronesastoolsformonitoringbeachtopographychangesintheligurianseanwmediterranean-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Drones as tools for monitoring beach topography changes in the Ligurian Sea (NW Mediterranean)},\n type = {article},\n year = {2016},\n pages = {151-163},\n volume = {36},\n id = {78f98a9b-44aa-3790-8deb-9be500fd712d},\n created = {2018-02-03T12:42:08.968Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:08.968Z},\n read = {true},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Casella},\n private_publication = {false},\n abstract = {The aim of this study was to evaluate topographic changes along a stretch of coastline in the Municipality of Borghetto Santo Spirito (Region of Liguria, Italy, north-western Mediterranean) by means of a remotely piloted aircraft system coupled with structure from motion and multi-view stereo techniques. This sector was surveyed three times over 5 months in the fall–winter of 2013–2014 (1 November 2013, 4 December 2013, 17 March 2014) to obtain digital elevation models and orthophotos of the beach. Changes in beach topography associated with storm action and human activities were assessed in terms of gain/loss of sediments and shifting of the wet–dry boundary defining the shoreline. Between the first and second surveys, the study area was hit by two storms (10–11 November 2013 and 21–22 November 2013) with waves approaching from the E–NNE, causing a shoreline retreat which, in some sectors, reached 7 m. Between the second and third surveys, by contrast, four storms (25–27 December 2013, 5–6 January 2014, 17–18 January 2014 and 6–10 February 2014) with waves propagating from the SE produced a general advancement of the shoreline (up to ~5 m) by deposition of sediments along some parts of the beach. The data also reflect changes in beach topography due to human activity during the 2013 fall season, when private beach managers quarried ~178 m3 of sediments on the emerged beach near the shoreline to accumulate them landwards. The results show that drones can be used for regular beach monitoring activities, and that they can provide new insights into the processes related to natural and/or human-related topographic beach changes.},\n bibtype = {article},\n author = {Casella, Elisa and Rovere, Alessio and Pedroncini, Andrea and Stark, Colin P. and Casella, Marco and Ferrari, Marco and Firpo, Marco},\n doi = {10.1007/s00367-016-0435-9},\n journal = {Geo-Marine Letters},\n number = {2}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The aim of this study was to evaluate topographic changes along a stretch of coastline in the Municipality of Borghetto Santo Spirito (Region of Liguria, Italy, north-western Mediterranean) by means of a remotely piloted aircraft system coupled with structure from motion and multi-view stereo techniques. This sector was surveyed three times over 5 months in the fall–winter of 2013–2014 (1 November 2013, 4 December 2013, 17 March 2014) to obtain digital elevation models and orthophotos of the beach. Changes in beach topography associated with storm action and human activities were assessed in terms of gain/loss of sediments and shifting of the wet–dry boundary defining the shoreline. Between the first and second surveys, the study area was hit by two storms (10–11 November 2013 and 21–22 November 2013) with waves approaching from the E–NNE, causing a shoreline retreat which, in some sectors, reached 7 m. Between the second and third surveys, by contrast, four storms (25–27 December 2013, 5–6 January 2014, 17–18 January 2014 and 6–10 February 2014) with waves propagating from the SE produced a general advancement of the shoreline (up to ~5 m) by deposition of sediments along some parts of the beach. The data also reflect changes in beach topography due to human activity during the 2013 fall season, when private beach managers quarried ~178 m3 of sediments on the emerged beach near the shoreline to accumulate them landwards. The results show that drones can be used for regular beach monitoring activities, and that they can provide new insights into the processes related to natural and/or human-related topographic beach changes.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"rovere-raymo-vacchi-lorscheid-stocchi-gmezpujol-harris-casella-etal-theanalysisoflastinterglacialmis5erelativesealevelindicatorsreconstructingsealevelinawarmerworld-2016\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://linkinghub.elsevier.com/retrieve/pii/S0012825216301246\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'rovere-raymo-vacchi-lorscheid-stocchi-gmezpujol-harris-casella-etal-theanalysisoflastinterglacialmis5erelativesealevelindicatorsreconstructingsealevelinawarmerworld-2016', 'http://linkinghub.elsevier.com/retrieve/pii/S0012825216301246', event);\">\n    The analysis of Last Interglacial (MIS 5e) relative sea-level indicators: Reconstructing sea-level in a warmer world.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Raymo,  M., M., E.; Vacchi,  M.; Lorscheid,  T.; Stocchi,  P.; Gómez-Pujol,  L.; Harris,  D., L., D.; Casella,  E.; O'Leary,  M., M., J.;  and Hearty,  P., P., J.\n</span>\n\n  \n\n</span>\n\n   2016.\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://linkinghub.elsevier.com/retrieve/pii/S0012825216301246\"\n     onclick=\"log_download('rovere-raymo-vacchi-lorscheid-stocchi-gmezpujol-harris-casella-etal-theanalysisoflastinterglacialmis5erelativesealevelindicatorsreconstructingsealevelinawarmerworld-2016', 'http://linkinghub.elsevier.com/retrieve/pii/S0012825216301246', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"The analysis of Last Interglacial (MIS 5e) relative sea-level indicators: Reconstructing sea-level in a warmer world [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.earscirev.2016.06.006\"\n     onclick=\"log_download('rovere-raymo-vacchi-lorscheid-stocchi-gmezpujol-harris-casella-etal-theanalysisoflastinterglacialmis5erelativesealevelindicatorsreconstructingsealevelinawarmerworld-2016', 'http://doi.org/10.1016/j.earscirev.2016.06.006', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/rovere-raymo-vacchi-lorscheid-stocchi-gmezpujol-harris-casella-etal-theanalysisoflastinterglacialmis5erelativesealevelindicatorsreconstructingsealevelinawarmerworld-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  &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('rovere-raymo-vacchi-lorscheid-stocchi-gmezpujol-harris-casella-etal-theanalysisoflastinterglacialmis5erelativesealevelindicatorsreconstructingsealevelinawarmerworld-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@misc{\n title = {The analysis of Last Interglacial (MIS 5e) relative sea-level indicators: Reconstructing sea-level in a warmer world},\n type = {misc},\n year = {2016},\n source = {Earth-Science Reviews},\n keywords = {Ice sheets,Last Interglacial,MIS 5e,Paleo sea-level,Past sea-level changes,Sea-level marker,Sea-level reconstruction},\n pages = {404-427},\n volume = {159},\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0012825216301246},\n publisher = {Elsevier B.V.},\n id = {6e31994f-6e2d-3da3-af0c-a536ee2529a2},\n created = {2018-02-03T12:42:09.044Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:09.044Z},\n read = {true},\n starred = {true},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Rovere2016a},\n private_publication = {false},\n abstract = {The Last Interglacial (MIS 5e, 128–116 ka) is among the most studied past periods in Earth&#x27;s history. The climate at that time was warmer than today, primarily due to different orbital conditions, with smaller ice sheets and higher sea-level. Field evidence for MIS 5e sea-level was reported from thousands of sites, but often paleo shorelines were measured with low-accuracy techniques and, in some cases, there are contrasting interpretations about paleo sea-level reconstructions. For this reason, large uncertainties still surround both the maximum sea-level attained as well as the pattern of sea-level change throughout MIS 5e. Such uncertainties are exacerbated by the lack of a uniform approach to measuring and interpreting the geological evidence of paleo sea-levels. In this review, we discuss the characteristics of MIS 5e field observations, and we set the basis for a standardized approach to MIS 5e paleo sea-level reconstructions, that is already successfully applied in Holocene sea-level research. Application of the standard definitions and methodologies described in this paper will enhance our ability to compare data from different research groups and different areas, in order to gain deeper insights into MIS 5e sea-level changes. Improving estimates of Last Interglacial sea-level is, in turn, a key to understanding the behavior of ice sheets in a warmer world.},\n bibtype = {misc},\n author = {Rovere, Alessio and Raymo, M.E. Maureen E. and Vacchi, Matteo and Lorscheid, Thomas and Stocchi, Paolo and Gómez-Pujol, Lluís and Harris, Daniel L. D.L. and Casella, Elisa and O&#x27;Leary, M.J. Michael J. and Hearty, P.J. Paul J.},\n doi = {10.1016/j.earscirev.2016.06.006}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The Last Interglacial (MIS 5e, 128–116 ka) is among the most studied past periods in Earth's history. The climate at that time was warmer than today, primarily due to different orbital conditions, with smaller ice sheets and higher sea-level. Field evidence for MIS 5e sea-level was reported from thousands of sites, but often paleo shorelines were measured with low-accuracy techniques and, in some cases, there are contrasting interpretations about paleo sea-level reconstructions. For this reason, large uncertainties still surround both the maximum sea-level attained as well as the pattern of sea-level change throughout MIS 5e. Such uncertainties are exacerbated by the lack of a uniform approach to measuring and interpreting the geological evidence of paleo sea-levels. In this review, we discuss the characteristics of MIS 5e field observations, and we set the basis for a standardized approach to MIS 5e paleo sea-level reconstructions, that is already successfully applied in Holocene sea-level research. Application of the standard definitions and methodologies described in this paper will enhance our ability to compare data from different research groups and different areas, in order to gain deeper insights into MIS 5e sea-level changes. Improving estimates of Last Interglacial sea-level is, in turn, a key to understanding the behavior of ice sheets in a warmer world.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"bryson-duce-harris-webster-thompson-vilaconcejo-williams-geomorphicchangesofacoralshinglecaymeasuredusingkiteaerialphotography-2016\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://dx.doi.org/10.1016/j.geomorph.2016.06.018\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'bryson-duce-harris-webster-thompson-vilaconcejo-williams-geomorphicchangesofacoralshinglecaymeasuredusingkiteaerialphotography-2016', 'http://dx.doi.org/10.1016/j.geomorph.2016.06.018', event);\">\n    Geomorphic changes of a coral shingle cay measured using Kite Aerial Photography.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Bryson,  M.; Duce,  S.; Harris,  D.; Webster,  J., M.; Thompson,  A.; Vila-Concejo,  A.;  and Williams,  S., B.\n</span>\n\n  \n\n</span>\n\n  <i>Geomorphology</i>, 270: 1-8.  2016.\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://dx.doi.org/10.1016/j.geomorph.2016.06.018\"\n     onclick=\"log_download('bryson-duce-harris-webster-thompson-vilaconcejo-williams-geomorphicchangesofacoralshinglecaymeasuredusingkiteaerialphotography-2016', 'http://dx.doi.org/10.1016/j.geomorph.2016.06.018', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Geomorphic changes of a coral shingle cay measured using Kite Aerial Photography [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.geomorph.2016.06.018\"\n     onclick=\"log_download('bryson-duce-harris-webster-thompson-vilaconcejo-williams-geomorphicchangesofacoralshinglecaymeasuredusingkiteaerialphotography-2016', 'http://doi.org/10.1016/j.geomorph.2016.06.018', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/bryson-duce-harris-webster-thompson-vilaconcejo-williams-geomorphicchangesofacoralshinglecaymeasuredusingkiteaerialphotography-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('bryson-duce-harris-webster-thompson-vilaconcejo-williams-geomorphicchangesofacoralshinglecaymeasuredusingkiteaerialphotography-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Geomorphic changes of a coral shingle cay measured using Kite Aerial Photography},\n type = {article},\n year = {2016},\n keywords = {3D topography,Coral reef morphodynamics,Kite Aerial Photography},\n pages = {1-8},\n volume = {270},\n websites = {http://dx.doi.org/10.1016/j.geomorph.2016.06.018},\n publisher = {Elsevier B.V.},\n id = {4bf2fa14-782a-38ea-99cf-8df4b476f09d},\n created = {2018-02-03T12:42:09.330Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-09-14T15:34:15.863Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Bryson2016e},\n private_publication = {false},\n abstract = {Measurements of geomorphic change in the intertidal zones of coral reefs are made using a variety of remote sensing and in-situ techniques, where variations in the coverage and spatial-temporal precision achieved are directly related to the cost of data acquisition. We present a novel, low-cost technique for measuring high-resolution changes in reef environments based on Kite Aerial Photography (KAP) and photogrammetry/structure-from-motion post-processing. KAP images are used to measure fine-scale changes in intertidal topography and sediment texture characteristics, including rubble particle size, of a coral shingle cay at One Tree Island, Great Barrier Reef in the context of storm activity. Validation using Real Time Kinematic DGPS demonstrates the ability to measure topographic elevation with an error of 5.53 cm (RMSE) and a spatial resolution of 5 cm per point, an accuracy/resolution that is superior to airborne LiDAR and equivalent to terrestrial LiDAR, but at a fraction of the equipment cost.},\n bibtype = {article},\n author = {Bryson, Mitch and Duce, Stephanie and Harris, Dan and Webster, Jody M. and Thompson, Alisha and Vila-Concejo, Ana and Williams, Stefan B.},\n doi = {10.1016/j.geomorph.2016.06.018},\n journal = {Geomorphology}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Measurements of geomorphic change in the intertidal zones of coral reefs are made using a variety of remote sensing and in-situ techniques, where variations in the coverage and spatial-temporal precision achieved are directly related to the cost of data acquisition. We present a novel, low-cost technique for measuring high-resolution changes in reef environments based on Kite Aerial Photography (KAP) and photogrammetry/structure-from-motion post-processing. KAP images are used to measure fine-scale changes in intertidal topography and sediment texture characteristics, including rubble particle size, of a coral shingle cay at One Tree Island, Great Barrier Reef in the context of storm activity. Validation using Real Time Kinematic DGPS demonstrates the ability to measure topographic elevation with an error of 5.53 cm (RMSE) and a spatial resolution of 5 cm per point, an accuracy/resolution that is superior to airborne LiDAR and equivalent to terrestrial LiDAR, but at a fraction of the equipment cost.\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        (12)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-resilienceofthemarineanimalforestlessonsfrommaldiviancoralreefsafterthemassmortalityof1998-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://link.springer.com/10.1007/978-3-319-17001-5\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-resilienceofthemarineanimalforestlessonsfrommaldiviancoralreefsafterthemassmortalityof1998-2015', 'http://link.springer.com/10.1007/978-3-319-17001-5', event);\">\n    Resilience of the Marine Animal Forest Lessons from Maldivian Coral Reefs After the Mass Mortality of 1998.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Bianchi,  C., N.; Morri,  C.; Lasagna,  R.; Montefalcone,  M.; Gatti,  G.; Parravicini,  V.;  and Rovere,  A.\n</span>\n\n  \n\n</span>\n\n  <i>Marine Animal Forests</i>,1-26.  2015.\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://link.springer.com/10.1007/978-3-319-17001-5\"\n     onclick=\"log_download('bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-resilienceofthemarineanimalforestlessonsfrommaldiviancoralreefsafterthemassmortalityof1998-2015', 'http://link.springer.com/10.1007/978-3-319-17001-5', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Resilience of the Marine Animal Forest Lessons from Maldivian Coral Reefs After the Mass Mortality of 1998 [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1007/978-3-319-17001-5\"\n     onclick=\"log_download('bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-resilienceofthemarineanimalforestlessonsfrommaldiviancoralreefsafterthemassmortalityof1998-2015', 'http://doi.org/10.1007/978-3-319-17001-5', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-resilienceofthemarineanimalforestlessonsfrommaldiviancoralreefsafterthemassmortalityof1998-2015\"\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\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-resilienceofthemarineanimalforestlessonsfrommaldiviancoralreefsafterthemassmortalityof1998-2015')\" -->\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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Resilience of the Marine Animal Forest Lessons from Maldivian Coral Reefs After the Mass Mortality of 1998},\n type = {article},\n year = {2015},\n pages = {1-26},\n websites = {http://link.springer.com/10.1007/978-3-319-17001-5},\n publisher = {Springer International Publishing},\n city = {Cham},\n id = {659f5aa2-00c2-3abe-89b3-8922549dafff},\n created = {2018-02-03T12:42:06.776Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.068Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Bianchi2015},\n source_type = {inbook},\n private_publication = {false},\n abstract = {This chapter reviews the major known monospecific and multispecific sponge aggregations in the world’s oceans. They are shown to occur from the intertidal to abyssal depths, in tropical, temperate, and high latitudes and sometimes to create spectacular formations, such as glass sponge reefs, lithistid reef-like fields, and carnivorous sponge grounds. Sponge aggregations are recognized as singular vulnerable habitats that deserve special research attention and legal protection. However, this review reveals that there is only a poor and fragmentary under- standing of the main biological, environmental, and geochemical factors that favor and maintain these systems, including the food supply, which is funda- mental knowledge. There is also a particular lack of information regarding reproductive biology, growth rates, life spans, and the main factors causing mortality, all crucial drivers for understanding population and community dynamics and for developing conservation strategies. The sponge aggregations have been shown to increase the structural complexity of the habitats, attracting a larger variety of organisms and locally enhancing biodiversity. From the very few cases in which sponge biomass and sponge physiology have been reliably approached jointly, phenomenal fluxes of matter and energy have been inferred. Through their benthic-pelagic coupling, some of the densest sponge aggrega- tions have a significant local or regional impact on major biogeochemical cycles and food webs. Physical damage and habitat destruction derived from man-driven activities along with epidemic diseases facilitated by global envi- ronmental alterations emerge as major threats to the future of the sponge aggregations.},\n bibtype = {article},\n author = {Bianchi, Carlo Nike and Morri, Carla and Lasagna, Roberta and Montefalcone, Monica and Gatti, Giulia and Parravicini, Valeriano and Rovere, Alessio},\n editor = {Rossi, Sergio and Bramanti, Lorenzo and Gori, Andrea and del Valle, Covadonga},\n doi = {10.1007/978-3-319-17001-5},\n journal = {Marine Animal Forests}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  This chapter reviews the major known monospecific and multispecific sponge aggregations in the world’s oceans. They are shown to occur from the intertidal to abyssal depths, in tropical, temperate, and high latitudes and sometimes to create spectacular formations, such as glass sponge reefs, lithistid reef-like fields, and carnivorous sponge grounds. Sponge aggregations are recognized as singular vulnerable habitats that deserve special research attention and legal protection. However, this review reveals that there is only a poor and fragmentary under- standing of the main biological, environmental, and geochemical factors that favor and maintain these systems, including the food supply, which is funda- mental knowledge. There is also a particular lack of information regarding reproductive biology, growth rates, life spans, and the main factors causing mortality, all crucial drivers for understanding population and community dynamics and for developing conservation strategies. The sponge aggregations have been shown to increase the structural complexity of the habitats, attracting a larger variety of organisms and locally enhancing biodiversity. From the very few cases in which sponge biomass and sponge physiology have been reliably approached jointly, phenomenal fluxes of matter and energy have been inferred. Through their benthic-pelagic coupling, some of the densest sponge aggrega- tions have a significant local or regional impact on major biogeochemical cycles and food webs. Physical damage and habitat destruction derived from man-driven activities along with epidemic diseases facilitated by global envi- ronmental alterations emerge as major threats to the future of the sponge aggregations.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"morri-montefalcone-lasagna-gatti-rovere-parravicini-baldelli-colantoni-etal-throughbleachingandtsunamicoralreefrecoveryinthemaldives-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://linkinghub.elsevier.com/retrieve/pii/S0025326X15004178\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'morri-montefalcone-lasagna-gatti-rovere-parravicini-baldelli-colantoni-etal-throughbleachingandtsunamicoralreefrecoveryinthemaldives-2015', 'http://linkinghub.elsevier.com/retrieve/pii/S0025326X15004178', event);\">\n    Through bleaching and tsunami: Coral reef recovery in the Maldives.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Morri,  C.; Montefalcone,  M.; Lasagna,  R.; Gatti,  G.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Parravicini,  V.; Baldelli,  G.; Colantoni,  P.;  and Bianchi,  C., N.\n</span>\n\n  \n\n</span>\n\n  <i>Marine Pollution Bulletin</i>, 98(1-2): 188-200.  2015.\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://linkinghub.elsevier.com/retrieve/pii/S0025326X15004178\"\n     onclick=\"log_download('morri-montefalcone-lasagna-gatti-rovere-parravicini-baldelli-colantoni-etal-throughbleachingandtsunamicoralreefrecoveryinthemaldives-2015', 'http://linkinghub.elsevier.com/retrieve/pii/S0025326X15004178', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Through bleaching and tsunami: Coral reef recovery in the Maldives [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.marpolbul.2015.06.050\"\n     onclick=\"log_download('morri-montefalcone-lasagna-gatti-rovere-parravicini-baldelli-colantoni-etal-throughbleachingandtsunamicoralreefrecoveryinthemaldives-2015', 'http://doi.org/10.1016/j.marpolbul.2015.06.050', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/morri-montefalcone-lasagna-gatti-rovere-parravicini-baldelli-colantoni-etal-throughbleachingandtsunamicoralreefrecoveryinthemaldives-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\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('morri-montefalcone-lasagna-gatti-rovere-parravicini-baldelli-colantoni-etal-throughbleachingandtsunamicoralreefrecoveryinthemaldives-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Through bleaching and tsunami: Coral reef recovery in the Maldives},\n type = {article},\n year = {2015},\n keywords = {Coral reefs,Hard coral cover,Indian Ocean,Maldives,Recruitment,Resilience},\n pages = {188-200},\n volume = {98},\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0025326X15004178},\n publisher = {Elsevier Ltd},\n id = {d4572baa-b24e-34a7-8fb4-c42c41fe8b00},\n created = {2018-02-03T12:42:06.777Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.231Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Morri2015},\n private_publication = {false},\n abstract = {Coral reefs are degrading worldwide, but little information exists on their previous conditions for most regions of the world. Since 1989, we have been studying the Maldives, collecting data before, during and after the bleaching and mass mortality event of 1998. As early as 1999, many newly settled colonies were recorded. Recruits shifted from a dominance of massive and encrusting corals in the early stages of recolonisation towards a dominance of Acropora and Pocillopora by 2009. Coral cover, which dropped to less than 10% after the bleaching, returned to pre-bleaching values of around 50% by 2013. The 2004 tsunami had comparatively little effect. In 2014, the coral community was similar to that existing before the bleaching. According to descriptors and metrics adopted, recovery of Maldivian coral reefs took between 6 and 15. years, or may even be considered unachieved, as there are species that had not come back yet.},\n bibtype = {article},\n author = {Morri, Carla and Montefalcone, Monica and Lasagna, Roberta and Gatti, Giulia and Rovere, Alessio and Parravicini, Valeriano and Baldelli, Giuseppe and Colantoni, Paolo and Bianchi, Carlo Nike},\n doi = {10.1016/j.marpolbul.2015.06.050},\n journal = {Marine Pollution Bulletin},\n number = {1-2}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Coral reefs are degrading worldwide, but little information exists on their previous conditions for most regions of the world. Since 1989, we have been studying the Maldives, collecting data before, during and after the bleaching and mass mortality event of 1998. As early as 1999, many newly settled colonies were recorded. Recruits shifted from a dominance of massive and encrusting corals in the early stages of recolonisation towards a dominance of Acropora and Pocillopora by 2009. Coral cover, which dropped to less than 10% after the bleaching, returned to pre-bleaching values of around 50% by 2013. The 2004 tsunami had comparatively little effect. In 2014, the coral community was similar to that existing before the bleaching. According to descriptors and metrics adopted, recovery of Maldivian coral reefs took between 6 and 15. years, or may even be considered unachieved, as there are species that had not come back yet.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"harris-webster-vilaconcejo-hua-yokoyama-reimer-lateholocenesealevelfallandturnoffofreefflatcarbonateproductionrethinkingbucketfillandcoralreefgrowthmodels-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://geology.gsapubs.org/cgi/doi/10.1130/G35977.1\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'harris-webster-vilaconcejo-hua-yokoyama-reimer-lateholocenesealevelfallandturnoffofreefflatcarbonateproductionrethinkingbucketfillandcoralreefgrowthmodels-2015', 'http://geology.gsapubs.org/cgi/doi/10.1130/G35977.1', event);\">\n    Late holocene sea-level fall and turn-off of reef flat carbonate production: Rethinking bucket fill and coral reef growth models.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Harris,  D., L.; Webster,  J., M.; Vila-Concejo,  A.; Hua,  Q.; Yokoyama,  Y.;  and Reimer,  P., J.\n</span>\n\n  \n\n</span>\n\n  <i>Geology</i>, 43(2): 1-4. 1 2015.\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://geology.gsapubs.org/cgi/doi/10.1130/G35977.1\"\n     onclick=\"log_download('harris-webster-vilaconcejo-hua-yokoyama-reimer-lateholocenesealevelfallandturnoffofreefflatcarbonateproductionrethinkingbucketfillandcoralreefgrowthmodels-2015', 'http://geology.gsapubs.org/cgi/doi/10.1130/G35977.1', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Late holocene sea-level fall and turn-off of reef flat carbonate production: Rethinking bucket fill and coral reef growth models [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1130/G35977.1\"\n     onclick=\"log_download('harris-webster-vilaconcejo-hua-yokoyama-reimer-lateholocenesealevelfallandturnoffofreefflatcarbonateproductionrethinkingbucketfillandcoralreefgrowthmodels-2015', 'http://doi.org/10.1130/G35977.1', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/harris-webster-vilaconcejo-hua-yokoyama-reimer-lateholocenesealevelfallandturnoffofreefflatcarbonateproductionrethinkingbucketfillandcoralreefgrowthmodels-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\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('harris-webster-vilaconcejo-hua-yokoyama-reimer-lateholocenesealevelfallandturnoffofreefflatcarbonateproductionrethinkingbucketfillandcoralreefgrowthmodels-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Late holocene sea-level fall and turn-off of reef flat carbonate production: Rethinking bucket fill and coral reef growth models},\n type = {article},\n year = {2015},\n pages = {1-4},\n volume = {43},\n websites = {http://geology.gsapubs.org/cgi/doi/10.1130/G35977.1},\n month = {1},\n day = {7},\n id = {c5ef7744-034e-35cd-a21c-3ccec602d2d1},\n created = {2018-02-03T12:42:07.282Z},\n accessed = {2015-01-14},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:07.282Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Harris2015b},\n private_publication = {false},\n abstract = {Relative sea-level rise has been a major factor driving the evolution of reef systems during the Holocene. Most models of reef evolution suggest that reefs preferentially grow vertically during rising sea level then laterally from windward to leeward, once the reef flat reaches sea level. Continuous lagoonal sedimentation (&quot;bucket fill&quot;) and sand apron progradation eventually lead to reef systems with totally filled lagoons. Lagoonal infilling of One Tree Reef (southern Great Barrier Reef) through sand apron accretion was examined in the context of late Holocene relative sea-level change. This analysis was conducted using sedimentological and digital terrain data supported by 50 radiocarbon ages from fossil microatolls, buried patch reefs, foraminifera and shells in sediment cores, and recalibrated previously published radiocarbon ages. This data set challenges the conceptual model of geologically continuous sediment infill during the Holocene through sand apron accretion. Rapid sand apron accretion occurred between 6000 and 3000 calibrated yr before present B.P. (cal. yr B.P.); followed by only small amounts of sedimentation between 3000 cal. yr B.P. and present, with no significant sand apron accretion in the past 2 k.y. This hiatus in sediment infill coincides with a sea-level fall of [~]1-1.3 m during the late Holocene (ca. 2000 cal. yr B.P.), which would have caused the turn-off of highly productive live coral growth on the reef flats currently dominated by less productive rubble and algal flats, resulting in a reduced sediment input to back-reef environments and the cessation in sand apron accretion. Given that relative sea-level variations of [~]1 m were common throughout the Holocene, we suggest that this mode of sand apron development and carbonate production is applicable to most reef systems.},\n bibtype = {article},\n author = {Harris, Daniel L. and Webster, Jody M. and Vila-Concejo, Ana and Hua, Quan and Yokoyama, Yusuke and Reimer, Paula J.},\n doi = {10.1130/G35977.1},\n journal = {Geology},\n number = {2},\n keywords = {SLCC}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Relative sea-level rise has been a major factor driving the evolution of reef systems during the Holocene. Most models of reef evolution suggest that reefs preferentially grow vertically during rising sea level then laterally from windward to leeward, once the reef flat reaches sea level. Continuous lagoonal sedimentation (\"bucket fill\") and sand apron progradation eventually lead to reef systems with totally filled lagoons. Lagoonal infilling of One Tree Reef (southern Great Barrier Reef) through sand apron accretion was examined in the context of late Holocene relative sea-level change. This analysis was conducted using sedimentological and digital terrain data supported by 50 radiocarbon ages from fossil microatolls, buried patch reefs, foraminifera and shells in sediment cores, and recalibrated previously published radiocarbon ages. This data set challenges the conceptual model of geologically continuous sediment infill during the Holocene through sand apron accretion. Rapid sand apron accretion occurred between 6000 and 3000 calibrated yr before present B.P. (cal. yr B.P.); followed by only small amounts of sedimentation between 3000 cal. yr B.P. and present, with no significant sand apron accretion in the past 2 k.y. This hiatus in sediment infill coincides with a sea-level fall of [~]1-1.3 m during the late Holocene (ca. 2000 cal. yr B.P.), which would have caused the turn-off of highly productive live coral growth on the reef flats currently dominated by less productive rubble and algal flats, resulting in a reduced sediment input to back-reef environments and the cessation in sand apron accretion. Given that relative sea-level variations of [~]1 m were common throughout the Holocene, we suggest that this mode of sand apron development and carbonate production is applicable to most reef systems.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"harris-vilaconcejo-webster-power-spatialvariationsinwavetransformationandsedimententrainmentonacoralreefsandapron-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Spatial variations in wave transformation and sediment entrainment on a coral reef sand apron.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Harris,  D., L.; Vila-Concejo,  A.; Webster,  J., M.;  and Power,  H., E.\n</span>\n\n  \n\n</span>\n\n  <i>Marine Geology</i>, 363: 220-229.  2015.\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/harris-vilaconcejo-webster-power-spatialvariationsinwavetransformationandsedimententrainmentonacoralreefsandapron-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\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('harris-vilaconcejo-webster-power-spatialvariationsinwavetransformationandsedimententrainmentonacoralreefsandapron-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Spatial variations in wave transformation and sediment entrainment on a coral reef sand apron},\n type = {article},\n year = {2015},\n pages = {220-229},\n volume = {363},\n publisher = {Elsevier},\n id = {57b0685a-c7b7-348e-834e-0ab865e8b817},\n created = {2018-02-03T12:42:07.347Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2018-02-03T12:42:07.347Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {harris2015spatial},\n source_type = {article},\n private_publication = {false},\n bibtype = {article},\n author = {Harris, D L and Vila-Concejo, A and Webster, J M and Power, H E},\n journal = {Marine Geology}\n}</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"vila-melo-silva-ramalho-quartau-hiplito-cordeiro-rebelo-etal-areviewofthemis5ehighstanddepositsfromsantamariaislandazoresneatlanticpalaeobiodiversitypalaeoecologyandpalaeobiogeography-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  A review of the MIS 5e highstand deposits from Santa Maria Island (Azores, NE Atlantic): Palaeobiodiversity, palaeoecology and palaeobiogeography.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Ávila,  S., P.; Melo,  C.; Silva,  L.; Ramalho,  R., S.; Quartau,  R.; Hipólito,  A.; Cordeiro,  R.; Rebelo,  A., C.; Madeira,  P.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Hearty,  P., J.; Henriques,  D.; Silva,  C., M., d.; Martins,  A., M., F.;  and Zazo,  C.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Science Reviews</i>, 114: 126-148.  2015.\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.2015.02.012\"\n     onclick=\"log_download('vila-melo-silva-ramalho-quartau-hiplito-cordeiro-rebelo-etal-areviewofthemis5ehighstanddepositsfromsantamariaislandazoresneatlanticpalaeobiodiversitypalaeoecologyandpalaeobiogeography-2015', 'http://doi.org/10.1016/j.quascirev.2015.02.012', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/vila-melo-silva-ramalho-quartau-hiplito-cordeiro-rebelo-etal-areviewofthemis5ehighstanddepositsfromsantamariaislandazoresneatlanticpalaeobiodiversitypalaeoecologyandpalaeobiogeography-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\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('vila-melo-silva-ramalho-quartau-hiplito-cordeiro-rebelo-etal-areviewofthemis5ehighstanddepositsfromsantamariaislandazoresneatlanticpalaeobiodiversitypalaeoecologyandpalaeobiogeography-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {A review of the MIS 5e highstand deposits from Santa Maria Island (Azores, NE Atlantic): Palaeobiodiversity, palaeoecology and palaeobiogeography},\n type = {article},\n year = {2015},\n keywords = {SLCC},\n pages = {126-148},\n volume = {114},\n id = {18675fe6-ef04-3b2a-80ad-0a12239f3f49},\n created = {2018-02-03T12:42:07.872Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.296Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Avila2015},\n private_publication = {false},\n abstract = {The privileged location of Santa Maria Island (Azores archipelago) in the middle of the North Atlantic makes the fossiliferous outcrops on this island of utmost importance to gain a better understanding of how coeval living communities relate to the broader evolutionary and biogeographic history of the Atlantic basin during the late Neogene and the Quaternary. Here we focus on this island&#x27;s MIS 5e fossil record, offering a comprehensive review on the palaeobiodiversity, palaeoecology and palaeobiogeography of the biota living in the mid North Atlantic during this interglacial. Several studies in oceanic islands stress the huge impact of sea level changes on insular communities. Pleistocene sea-level changes occur during the short-time events known as &quot;Terminations&quot; (associated to glacial/interglacial shifts) as well as with the onset of glaciations (associated to interglacial/glacial shifts). Both are responsible for extinctions and local disappearance of species, bottleneck effects and formation of new species, resulting in community structure changes. This work increases the number of fossil marine taxa reported from the Last Interglacial deposits of Santa Maria to 143 species. All the 19 new records are molluscs (13 gastropods and 6 bivalves), thus increasing the number of fossil molluscs to 136 species. Although thermophilic members of the &quot;Senegalese&quot; tropical fauna were found in these deposits, many of the most emblematic species (e.g., Persististrombus latus (= Strombus bubonius), Cymbula safiana, Harpa doris, Cardita senegalensis, Barbatia plicata, Ctena eburnea or Hyotissa hyotis) are absent, suggesting that they did not reach the Azores. Our results indicate that the main differences between the species composition of the MIS 5e and the present-day shallow-water Azorean communities are probably due to the dropping of sea surface temperature associated with the onset of the last glaciation, which had both direct and indirect effects on species ecology. A group of 21 thermophilic species was directly affected by the lower sea surface temperature, whereas a group of four sand-associated species was indirectly but similarly affected by the lowering of the sea level. Both groups have locally disappeared from the Azores. However, none of the extant endemic species found on the studied MIS 5e outcrops was apparently affected by the lowering SST. In contrast to the biogeographical relationships of the recent Azorean shallow marine molluscs, which are predominantly with the Mediterranean Region, Portugal and with the Madeira and Canary Islands archipelagos, the palaeobiogeographical relationships of the MIS 5e Azorean marine molluscs are mainly with Canaries and West Africa. Despite the general low similarity of the biogeographical relationships between the Azores and Cape Verde Archipelago, on both the recent and the MIS 5e analysis, this similarity is nevertheless higher for the MIS 5e mollusc assemblages, emphasizing the role of Cape Verde as an important source of warm-water species during the Last Interglacial.},\n bibtype = {article},\n author = {Ávila, Sérgio P. and Melo, Carlos and Silva, Luís and Ramalho, Ricardo S. and Quartau, Rui and Hipólito, Ana and Cordeiro, Ricardo and Rebelo, Ana Cristina and Madeira, Patrícia and Rovere, Alessio and Hearty, Paul J. and Henriques, Diamantino and Silva, Carlos Marques da and Martins, António M.de Frias and Zazo, Caridad},\n doi = {10.1016/j.quascirev.2015.02.012},\n journal = {Quaternary Science Reviews}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  The privileged location of Santa Maria Island (Azores archipelago) in the middle of the North Atlantic makes the fossiliferous outcrops on this island of utmost importance to gain a better understanding of how coeval living communities relate to the broader evolutionary and biogeographic history of the Atlantic basin during the late Neogene and the Quaternary. Here we focus on this island's MIS 5e fossil record, offering a comprehensive review on the palaeobiodiversity, palaeoecology and palaeobiogeography of the biota living in the mid North Atlantic during this interglacial. Several studies in oceanic islands stress the huge impact of sea level changes on insular communities. Pleistocene sea-level changes occur during the short-time events known as \"Terminations\" (associated to glacial/interglacial shifts) as well as with the onset of glaciations (associated to interglacial/glacial shifts). Both are responsible for extinctions and local disappearance of species, bottleneck effects and formation of new species, resulting in community structure changes. This work increases the number of fossil marine taxa reported from the Last Interglacial deposits of Santa Maria to 143 species. All the 19 new records are molluscs (13 gastropods and 6 bivalves), thus increasing the number of fossil molluscs to 136 species. Although thermophilic members of the \"Senegalese\" tropical fauna were found in these deposits, many of the most emblematic species (e.g., Persististrombus latus (= Strombus bubonius), Cymbula safiana, Harpa doris, Cardita senegalensis, Barbatia plicata, Ctena eburnea or Hyotissa hyotis) are absent, suggesting that they did not reach the Azores. Our results indicate that the main differences between the species composition of the MIS 5e and the present-day shallow-water Azorean communities are probably due to the dropping of sea surface temperature associated with the onset of the last glaciation, which had both direct and indirect effects on species ecology. A group of 21 thermophilic species was directly affected by the lower sea surface temperature, whereas a group of four sand-associated species was indirectly but similarly affected by the lowering of the sea level. Both groups have locally disappeared from the Azores. However, none of the extant endemic species found on the studied MIS 5e outcrops was apparently affected by the lowering SST. In contrast to the biogeographical relationships of the recent Azorean shallow marine molluscs, which are predominantly with the Mediterranean Region, Portugal and with the Madeira and Canary Islands archipelagos, the palaeobiogeographical relationships of the MIS 5e Azorean marine molluscs are mainly with Canaries and West Africa. Despite the general low similarity of the biogeographical relationships between the Azores and Cape Verde Archipelago, on both the recent and the MIS 5e analysis, this similarity is nevertheless higher for the MIS 5e mollusc assemblages, emphasizing the role of Cape Verde as an important source of warm-water species during the Last Interglacial.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"antonioli-lopresti-rovere-ferranti-anzidei-furlani-mastronuzzi-orru-etal-tidalnotchesinmediterraneanseaacomprehensiveanalysis-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://linkinghub.elsevier.com/retrieve/pii/S0277379115001237\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'antonioli-lopresti-rovere-ferranti-anzidei-furlani-mastronuzzi-orru-etal-tidalnotchesinmediterraneanseaacomprehensiveanalysis-2015', 'http://linkinghub.elsevier.com/retrieve/pii/S0277379115001237', event);\">\n    Tidal notches in Mediterranean Sea: A comprehensive analysis.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Antonioli,  F.; Lo Presti,  V.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Ferranti,  L.; Anzidei,  M.; Furlani,  S.; Mastronuzzi,  G.; Orru,  P., E.; Scicchitano,  G.; Sannino,  G.; Spampinato,  C., R.; Pagliarulo,  R.; Deiana,  G.; de Sabata,  E.; Sansò,  P.; Vacchi,  M.;  and Vecchio,  A.\n</span>\n\n  \n\n</span>\n\n  <i>Quaternary Science Reviews</i>, 119(5): 66-84.  2015.\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://linkinghub.elsevier.com/retrieve/pii/S0277379115001237\"\n     onclick=\"log_download('antonioli-lopresti-rovere-ferranti-anzidei-furlani-mastronuzzi-orru-etal-tidalnotchesinmediterraneanseaacomprehensiveanalysis-2015', 'http://linkinghub.elsevier.com/retrieve/pii/S0277379115001237', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Tidal notches in Mediterranean Sea: A comprehensive analysis [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.quascirev.2015.03.016\"\n     onclick=\"log_download('antonioli-lopresti-rovere-ferranti-anzidei-furlani-mastronuzzi-orru-etal-tidalnotchesinmediterraneanseaacomprehensiveanalysis-2015', 'http://doi.org/10.1016/j.quascirev.2015.03.016', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/antonioli-lopresti-rovere-ferranti-anzidei-furlani-mastronuzzi-orru-etal-tidalnotchesinmediterraneanseaacomprehensiveanalysis-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\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('antonioli-lopresti-rovere-ferranti-anzidei-furlani-mastronuzzi-orru-etal-tidalnotchesinmediterraneanseaacomprehensiveanalysis-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Tidal notches in Mediterranean Sea: A comprehensive analysis},\n type = {article},\n year = {2015},\n keywords = {MEDFLOOD,SLCC},\n pages = {66-84},\n volume = {119},\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0277379115001237},\n id = {d4ca0132-0793-3a00-9ab0-363e0f46f1a1},\n created = {2018-02-03T12:42:08.494Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.034Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Antonioli2015},\n private_publication = {false},\n abstract = {Recent works (Evelpidou et al., 2012) suggest that the modern tidal notch is disappearing worldwide due sea level rise over the last century. In order to assess this hypothesis, we measured modern tidal notches in several of sites along the Mediterranean coasts. We report observations on tidal notches cut along carbonate coasts from 73 sites from Italy, France, Croatia, Montenegro, Greece, Malta and Spain, plus additional observations carried outside the Mediterranean. At each site, we measured notch width and depth, and we described the characteristics of the biological rim at the base of the notch. We correlated these parameters with wave energy, tide gauge datasets and rock lithology.Our results suggest that, considering &#x27;the development of tidal notches the consequence of midlittoral bioerosion&#x27; (as done in Evelpidou et al., 2012) is a simplification that can lead to misleading results, such as stating that notches are disappearing. Important roles in notch formation can be also played by wave action, rate of karst dissolution, salt weathering and wetting and drying cycles. Of course notch formation can be augmented and favoured also by bioerosion which can, in particular cases, be the main process of notch formation and development.Our dataset shows that notches are carved by an ensemble rather than by a single process, both today and in the past, and that it is difficult, if not impossible, to disentangle them and establish which one is prevailing. We therefore show that tidal notches are still forming, challenging the hypothesis that sea level rise has drowned them.},\n bibtype = {article},\n author = {Antonioli, Fabrizio and Lo Presti, Valeria and Rovere, Alessio and Ferranti, Luigi and Anzidei, Marco and Furlani, Stefano and Mastronuzzi, Giuseppe and Orru, Paolo E. and Scicchitano, Giovanni and Sannino, Gianmaria and Spampinato, Cecilia R. and Pagliarulo, Rossella and Deiana, Giacomo and de Sabata, Eleonora and Sansò, Paolo and Vacchi, Matteo and Vecchio, Antonio},\n doi = {10.1016/j.quascirev.2015.03.016},\n journal = {Quaternary Science Reviews},\n number = {5}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Recent works (Evelpidou et al., 2012) suggest that the modern tidal notch is disappearing worldwide due sea level rise over the last century. In order to assess this hypothesis, we measured modern tidal notches in several of sites along the Mediterranean coasts. We report observations on tidal notches cut along carbonate coasts from 73 sites from Italy, France, Croatia, Montenegro, Greece, Malta and Spain, plus additional observations carried outside the Mediterranean. At each site, we measured notch width and depth, and we described the characteristics of the biological rim at the base of the notch. We correlated these parameters with wave energy, tide gauge datasets and rock lithology.Our results suggest that, considering 'the development of tidal notches the consequence of midlittoral bioerosion' (as done in Evelpidou et al., 2012) is a simplification that can lead to misleading results, such as stating that notches are disappearing. Important roles in notch formation can be also played by wave action, rate of karst dissolution, salt weathering and wetting and drying cycles. Of course notch formation can be augmented and favoured also by bioerosion which can, in particular cases, be the main process of notch formation and development.Our dataset shows that notches are carved by an ensemble rather than by a single process, both today and in the past, and that it is difficult, if not impossible, to disentangle them and establish which one is prevailing. We therefore show that tidal notches are still forming, challenging the hypothesis that sea level rise has drowned them.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"gatti-bianchi-parravicini-rovere-peirano-montefalcone-massa-morri-ecologicalchangeslidingbaselinesandtheimportanceofhistoricaldatalessonsfromcombingobservationalandquantitativedataonatemperatereefover70years-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://dx.plos.org/10.1371/journal.pone.0118581\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'gatti-bianchi-parravicini-rovere-peirano-montefalcone-massa-morri-ecologicalchangeslidingbaselinesandtheimportanceofhistoricaldatalessonsfromcombingobservationalandquantitativedataonatemperatereefover70years-2015', 'http://dx.plos.org/10.1371/journal.pone.0118581', event);\">\n    Ecological Change, Sliding Baselines and the Importance of Historical Data: Lessons from Combing Observational and Quantitative Data on a Temperate Reef Over 70 Years.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Gatti,  G.; Bianchi,  C., N.; Parravicini,  V.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Peirano,  A.; Montefalcone,  M.; Massa,  F.;  and Morri,  C.\n</span>\n\n  \n\n</span>\n\n  <i>Plos One</i>, 10: e0118581.  2015.\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://dx.plos.org/10.1371/journal.pone.0118581\"\n     onclick=\"log_download('gatti-bianchi-parravicini-rovere-peirano-montefalcone-massa-morri-ecologicalchangeslidingbaselinesandtheimportanceofhistoricaldatalessonsfromcombingobservationalandquantitativedataonatemperatereefover70years-2015', 'http://dx.plos.org/10.1371/journal.pone.0118581', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Ecological Change, Sliding Baselines and the Importance of Historical Data: Lessons from Combing Observational and Quantitative Data on a Temperate Reef Over 70 Years [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1371/journal.pone.0118581\"\n     onclick=\"log_download('gatti-bianchi-parravicini-rovere-peirano-montefalcone-massa-morri-ecologicalchangeslidingbaselinesandtheimportanceofhistoricaldatalessonsfromcombingobservationalandquantitativedataonatemperatereefover70years-2015', 'http://doi.org/10.1371/journal.pone.0118581', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/gatti-bianchi-parravicini-rovere-peirano-montefalcone-massa-morri-ecologicalchangeslidingbaselinesandtheimportanceofhistoricaldatalessonsfromcombingobservationalandquantitativedataonatemperatereefover70years-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\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('gatti-bianchi-parravicini-rovere-peirano-montefalcone-massa-morri-ecologicalchangeslidingbaselinesandtheimportanceofhistoricaldatalessonsfromcombingobservationalandquantitativedataonatemperatereefover70years-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Ecological Change, Sliding Baselines and the Importance of Historical Data: Lessons from Combing Observational and Quantitative Data on a Temperate Reef Over 70 Years},\n type = {article},\n year = {2015},\n pages = {e0118581},\n volume = {10},\n websites = {http://dx.plos.org/10.1371/journal.pone.0118581},\n id = {8b916ab6-383a-3a2a-9b7b-996ec73ff016},\n created = {2018-02-03T12:42:08.689Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.170Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Gatti2015},\n private_publication = {false},\n abstract = {Understanding the effects of environmental change on ecosystems requires the identifica- tion of baselines that may act as reference conditions. However, the continuous change of these references challenges our ability to define the true natural status of ecosystems. The so-called sliding baseline syndrome can be overcome through the analysis of quantitative time series, which are, however, extremely rare. Here we show how combining historical quantitative data with descriptive ‘naturalistic’ information arranged in a chronological chain allows highlighting long-term trends and can be used to inform present conservation schemes.We analysed the long-term change of a coralligenous reef, a marine habitat en- demic to the Mediterranean Sea. The coralligenous assemblages of Mesco Reef (Ligurian Sea,NWMediterranean) have been studied, although discontinuously, since 1937 thus making available both detailed descriptive information and scanty quantitative data: while the former was useful to understand the natural history of the ecosystem, the analysis of the latter was of paramount importance to provide a formal measure of change over time. Epi- benthic assemblages remained comparatively stable until the 1990s, when species re- placement, invasion by alien algae, and biotic homogenisation occurred within few years, leading to a new and completely different ecosystem state. The shift experienced by the cor- alligenous assemblages of Mesco Reef was probably induced by a combination of seawa- ter warming and local human pressures, the latter mainly resulting in increased water turbidity; in turn, cumulative stress may have favoured the establishment of alien species. This study showed that the combined analysis of quantitative and descriptive historical data represent a precious knowledge to understand ecosystem trends over time and provide help to identify baselines for ecological management.},\n bibtype = {article},\n author = {Gatti, Giulia and Bianchi, Carlo Nike and Parravicini, Valeriano and Rovere, Alessio and Peirano, Andrea and Montefalcone, Monica and Massa, Francesco and Morri, Carla},\n doi = {10.1371/journal.pone.0118581},\n journal = {Plos One},\n keywords = {SLCC}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Understanding the effects of environmental change on ecosystems requires the identifica- tion of baselines that may act as reference conditions. However, the continuous change of these references challenges our ability to define the true natural status of ecosystems. The so-called sliding baseline syndrome can be overcome through the analysis of quantitative time series, which are, however, extremely rare. Here we show how combining historical quantitative data with descriptive ‘naturalistic’ information arranged in a chronological chain allows highlighting long-term trends and can be used to inform present conservation schemes.We analysed the long-term change of a coralligenous reef, a marine habitat en- demic to the Mediterranean Sea. The coralligenous assemblages of Mesco Reef (Ligurian Sea,NWMediterranean) have been studied, although discontinuously, since 1937 thus making available both detailed descriptive information and scanty quantitative data: while the former was useful to understand the natural history of the ecosystem, the analysis of the latter was of paramount importance to provide a formal measure of change over time. Epi- benthic assemblages remained comparatively stable until the 1990s, when species re- placement, invasion by alien algae, and biotic homogenisation occurred within few years, leading to a new and completely different ecosystem state. The shift experienced by the cor- alligenous assemblages of Mesco Reef was probably induced by a combination of seawa- ter warming and local human pressures, the latter mainly resulting in increased water turbidity; in turn, cumulative stress may have favoured the establishment of alien species. This study showed that the combined analysis of quantitative and descriptive historical data represent a precious knowledge to understand ecosystem trends over time and provide help to identify baselines for ecological management.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"rovere-hearty-austermann-mitrovica-gale-moucha-forte-raymo-midplioceneshorelinesoftheusatlanticcoastalplainanimprovedelevationdatabasewithcomparisontoearthmodelpredictions-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://linkinghub.elsevier.com/retrieve/pii/S0012825215000355,http://www.scopus.com/inward/record.url?eid=2-s2.0-84926164528&amp;partnerID=tZOtx3y1\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'rovere-hearty-austermann-mitrovica-gale-moucha-forte-raymo-midplioceneshorelinesoftheusatlanticcoastalplainanimprovedelevationdatabasewithcomparisontoearthmodelpredictions-2015', 'http://linkinghub.elsevier.com/retrieve/pii/S0012825215000355,http://www.scopus.com/inward/record.url?eid=2-s2.0-84926164528&amp;partnerID=tZOtx3y1', event);\">\n    Mid-Pliocene shorelines of the US Atlantic Coastal Plain — An improved elevation database with comparison to Earth model predictions.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Hearty,  P.; Austermann,  J.; Mitrovica,  J.; Gale,  J.; Moucha,  R.; Forte,  A.;  and Raymo,  M.\n</span>\n\n  \n\n</span>\n\n  <i>Earth-Science Reviews</i>, 145: 117-131.  2015.\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://linkinghub.elsevier.com/retrieve/pii/S0012825215000355,http://www.scopus.com/inward/record.url?eid=2-s2.0-84926164528&amp;partnerID=tZOtx3y1\"\n     onclick=\"log_download('rovere-hearty-austermann-mitrovica-gale-moucha-forte-raymo-midplioceneshorelinesoftheusatlanticcoastalplainanimprovedelevationdatabasewithcomparisontoearthmodelpredictions-2015', 'http://linkinghub.elsevier.com/retrieve/pii/S0012825215000355,http://www.scopus.com/inward/record.url?eid=2-s2.0-84926164528&amp;partnerID=tZOtx3y1', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Mid-Pliocene shorelines of the US Atlantic Coastal Plain — An improved elevation database with comparison to Earth model predictions [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.earscirev.2015.02.007\"\n     onclick=\"log_download('rovere-hearty-austermann-mitrovica-gale-moucha-forte-raymo-midplioceneshorelinesoftheusatlanticcoastalplainanimprovedelevationdatabasewithcomparisontoearthmodelpredictions-2015', 'http://doi.org/10.1016/j.earscirev.2015.02.007', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/rovere-hearty-austermann-mitrovica-gale-moucha-forte-raymo-midplioceneshorelinesoftheusatlanticcoastalplainanimprovedelevationdatabasewithcomparisontoearthmodelpredictions-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\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('rovere-hearty-austermann-mitrovica-gale-moucha-forte-raymo-midplioceneshorelinesoftheusatlanticcoastalplainanimprovedelevationdatabasewithcomparisontoearthmodelpredictions-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Mid-Pliocene shorelines of the US Atlantic Coastal Plain — An improved elevation database with comparison to Earth model predictions},\n type = {article},\n year = {2015},\n keywords = {MEDFLOOD,PLIOMAX,SLCC},\n pages = {117-131},\n volume = {145},\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0012825215000355,http://www.scopus.com/inward/record.url?eid=2-s2.0-84926164528&amp;partnerID=tZOtx3y1},\n publisher = {Elsevier B.V.},\n id = {7c02f629-e8ca-3a22-9339-70cd0d5fd1b8},\n created = {2018-02-03T12:42:08.744Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.267Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Rovere2015},\n private_publication = {false},\n abstract = {For nearly a century, the Atlantic Coastal Plain (ACP) of the United States has been the focus of studies investigating Pliocene and Pleistocene shorelines, however, the mapping of paleoshorelines was primarily done by using elevation contours on topographic maps. Here we review published geologic maps and compare them to paleoshoreline locations obtained through geomorphometric classification and satellite data. We furthermore present the results of an extensive field campaign that measured the mid-Pliocene (~. 3.3-2.9. Ma) shorelines of the Atlantic Coastal Plain using high-accuracy GPS and digital elevation models. We compare our new dataset to positions and elevations extracted from published maps and find that the extracted site information from earlier studies is prone to significant error, both in the location and, more severely, in the elevation of the paleoshoreline. We also investigate, using geophysical modeling, the origin of post-depositional displacement of the shoreline from Georgia to Virginia. In particular, we correct the elevation of our shoreline for glacial isostatic adjustment (GIA) and then compare the corrected elevation to predictions of mantle flow-induced dynamic topography (DT). While a subset of these models does reconcile the general trends in the observed elevation of the mid-Pliocene shoreline, local discrepancies persist. These discrepancies suggests that either (i) the DT and GIA models presented here do not capture the full range of uncertainty in the input parameters; and/or (ii) other influences, such as sediment loading and unloading or local fault-driven tectonics, may have contributed to post-depositional deformation of the mid-Pliocene shoreline that are not captured in the above models. In this context, our field measurements represent an important observational dataset with which to compare future generations of geodynamic models. Improvements in models for DT, GIA and other relevant processes, together with an expanded, geographically distributed set of shoreline records, will ultimately be the key to obtaining more accurate estimates of eustatic sea level not only in the mid-Pliocene but also earlier in the Cenozoic.},\n bibtype = {article},\n author = {Rovere, Alessio and Hearty, P.J. and Austermann, J. and Mitrovica, J.X. and Gale, J. and Moucha, R. and Forte, A.M. and Raymo, M.E.},\n doi = {10.1016/j.earscirev.2015.02.007},\n journal = {Earth-Science Reviews}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  For nearly a century, the Atlantic Coastal Plain (ACP) of the United States has been the focus of studies investigating Pliocene and Pleistocene shorelines, however, the mapping of paleoshorelines was primarily done by using elevation contours on topographic maps. Here we review published geologic maps and compare them to paleoshoreline locations obtained through geomorphometric classification and satellite data. We furthermore present the results of an extensive field campaign that measured the mid-Pliocene (~. 3.3-2.9. Ma) shorelines of the Atlantic Coastal Plain using high-accuracy GPS and digital elevation models. We compare our new dataset to positions and elevations extracted from published maps and find that the extracted site information from earlier studies is prone to significant error, both in the location and, more severely, in the elevation of the paleoshoreline. We also investigate, using geophysical modeling, the origin of post-depositional displacement of the shoreline from Georgia to Virginia. In particular, we correct the elevation of our shoreline for glacial isostatic adjustment (GIA) and then compare the corrected elevation to predictions of mantle flow-induced dynamic topography (DT). While a subset of these models does reconcile the general trends in the observed elevation of the mid-Pliocene shoreline, local discrepancies persist. These discrepancies suggests that either (i) the DT and GIA models presented here do not capture the full range of uncertainty in the input parameters; and/or (ii) other influences, such as sediment loading and unloading or local fault-driven tectonics, may have contributed to post-depositional deformation of the mid-Pliocene shoreline that are not captured in the above models. In this context, our field measurements represent an important observational dataset with which to compare future generations of geodynamic models. Improvements in models for DT, GIA and other relevant processes, together with an expanded, geographically distributed set of shoreline records, will ultimately be the key to obtaining more accurate estimates of eustatic sea level not only in the mid-Pliocene but also earlier in the Cenozoic.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"rovere-antonioli-bianchi-chapter18fixedbiologicalindicators-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  Chapter 18 Fixed biological indicators.\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Antonioli,  F.;  and Bianchi,  C., N.\n</span>\n\n  \n\n</span>\n\n  <i>Handbook of Sea-Level Research</i>,268-280.  2015.\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/rovere-antonioli-bianchi-chapter18fixedbiologicalindicators-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\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('rovere-antonioli-bianchi-chapter18fixedbiologicalindicators-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Chapter 18 Fixed biological indicators},\n type = {article},\n year = {2015},\n keywords = {MEDFLOOD,PLIOMAX,SLCC},\n pages = {268-280},\n publisher = {Wiley Online Library},\n chapter = {18},\n id = {88d36d15-b4c4-3042-bbdf-5b2ba9c1033d},\n created = {2018-02-03T12:42:09.156Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.173Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Rovere2015c},\n private_publication = {false},\n abstract = {Fixed biological indicators are organisms that live fixed to hard substrates and their living range or the upper part of it is located near or at sea level. In this chapter, the main fixed biological indicators are described and their value as indicators of former sea levels is discussed.},\n bibtype = {article},\n author = {Rovere, Alessio and Antonioli, Fabrizio and Bianchi, Carlo Nike},\n editor = {Shennan, Ian and Long, Antony J. and Horton, Benjamin P},\n journal = {Handbook of Sea-Level Research}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Fixed biological indicators are organisms that live fixed to hard substrates and their living range or the upper part of it is located near or at sea level. In this chapter, the main fixed biological indicators are described and their value as indicators of former sea levels is discussed.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-marineanimalforeststheecologyofbenthicbiodiversityhotspots-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://dx.doi.org/10.1007/978-3-319-17001-5_35-1\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-marineanimalforeststheecologyofbenthicbiodiversityhotspots-2015', 'http://dx.doi.org/10.1007/978-3-319-17001-5_35-1', event);\">\n    Resilience of the Marine Animal Forest.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Bianchi,  C., N.; Morri,  C.; Lasagna,  R.; Montefalcone,  M.; Gatti,  G.; Parravicini,  V.;  and Rovere,  A.\n</span>\n\n  \n\n</span>\n\n  Marine Animal Forests: The Ecology of Benthic Biodiversity Hotspots, pages 1-30. Rossi,  S.; Bramanti,  L.; Gori,  A.;  and del Valle,  C., editor(s). Springer International Publishing,  2015.\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://dx.doi.org/10.1007/978-3-319-17001-5_35-1\"\n     onclick=\"log_download('bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-marineanimalforeststheecologyofbenthicbiodiversityhotspots-2015', 'http://dx.doi.org/10.1007/978-3-319-17001-5_35-1', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Marine Animal Forests: The Ecology of Benthic Biodiversity Hotspots [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1007/978-3-319-17001-5_35-1\"\n     onclick=\"log_download('bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-marineanimalforeststheecologyofbenthicbiodiversityhotspots-2015', 'http://doi.org/10.1007/978-3-319-17001-5_35-1', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-marineanimalforeststheecologyofbenthicbiodiversityhotspots-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\n  \n\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('bianchi-morri-lasagna-montefalcone-gatti-parravicini-rovere-marineanimalforeststheecologyofbenthicbiodiversityhotspots-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@inbook{\n type = {inbook},\n year = {2015},\n pages = {1-30},\n websites = {http://dx.doi.org/10.1007/978-3-319-17001-5_35-1},\n publisher = {Springer International Publishing},\n city = {Cham},\n id = {8d9ac960-e7f9-3635-a6bf-13ec1d22a9f2},\n created = {2018-02-03T12:42:09.165Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.136Z},\n read = {false},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Bianchi2015},\n source_type = {inbook},\n private_publication = {false},\n bibtype = {inbook},\n author = {Bianchi, Carlo Nike and Morri, Carla and Lasagna, Roberta and Montefalcone, Monica and Gatti, Giulia and Parravicini, Valeriano and Rovere, Alessio},\n editor = {Rossi, Sergio and Bramanti, Lorenzo and Gori, Andrea and del Valle, Covadonga},\n doi = {10.1007/978-3-319-17001-5_35-1},\n chapter = {Resilience of the Marine Animal Forest},\n title = {Marine Animal Forests: The Ecology of Benthic Biodiversity Hotspots}\n}</pre>\n</div>\n\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-2015', 'http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134', event);\">\n    Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy).\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Casella,  E.; Vacchi,  M.; Parravicini,  V.; Firpo,  M.; Ferrari,  M.; Morri,  C.;  and Bianchi,  C., N.\n</span>\n\n  \n\n</span>\n\n  <i>Journal of Maps</i>, 11(2): 278-286. 6 2015.\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.tandfonline.com/doi/abs/10.1080/17445647.2014.933134\"\n     onclick=\"log_download('rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-2015', 'http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy) [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1080/17445647.2014.933134\"\n     onclick=\"log_download('rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-2015', 'http://doi.org/10.1080/17445647.2014.933134', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-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\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy)},\n type = {article},\n year = {2015},\n keywords = {MIRAMAR,SEAMAP,SLCC},\n pages = {278-286},\n volume = {11},\n websites = {http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134},\n month = {6},\n day = {24},\n id = {4764317f-01f8-36bf-9eff-783fcb4dfc8b},\n created = {2018-02-03T12:42:09.171Z},\n accessed = {2014-09-15},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.118Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Rovere2014},\n private_publication = {false},\n abstract = {In this paper, we present a map describing the main geomorphological features of the coastal and marine area between the towns of Albenga and Savona (Ligurian Sea, NW Mediterranean) corresponding to a coastal stretch of ∼40 km. To produce this map, we collated data from the literature, orthophotos, perspective photos, multibeam and side scan sonar data, and undertook direct surveys to ground truth data obtained using indirect techniques. We divided the information into nine thematic layers, including bathymetry, natural coastal types, geomorphological elements, seafloor coverage (both geological and biological), coastal and nearshore dynamics, human influence on coastal and marine environments, coastal occupation and protected areas.},\n bibtype = {article},\n author = {Rovere, A. and Casella, E. and Vacchi, M. and Parravicini, V. and Firpo, M. and Ferrari, M. and Morri, C. and Bianchi, C. N.},\n doi = {10.1080/17445647.2014.933134},\n journal = {Journal of Maps},\n number = {2}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  In this paper, we present a map describing the main geomorphological features of the coastal and marine area between the towns of Albenga and Savona (Ligurian Sea, NW Mediterranean) corresponding to a coastal stretch of ∼40 km. To produce this map, we collated data from the literature, orthophotos, perspective photos, multibeam and side scan sonar data, and undertook direct surveys to ground truth data obtained using indirect techniques. We divided the information into nine thematic layers, including bathymetry, natural coastal types, geomorphological elements, seafloor coverage (both geological and biological), coastal and nearshore dynamics, human influence on coastal and marine environments, coastal occupation and protected areas.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-2015\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-2015', 'http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134', event);\">\n    Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy).\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Casella,  E.; Vacchi,  M.; Parravicini,  V.; Firpo,  M.; Ferrari,  M.; Morri,  C.;  and Bianchi,  C., N.\n</span>\n\n  \n\n</span>\n\n  <i>Journal of Maps</i>, 11(2): 278-286. 6 2015.\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.tandfonline.com/doi/abs/10.1080/17445647.2014.933134\"\n     onclick=\"log_download('rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-2015', 'http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy) [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1080/17445647.2014.933134\"\n     onclick=\"log_download('rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-2015', 'http://doi.org/10.1080/17445647.2014.933134', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-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\n  <!-- <a class=\"bibbase read link hidden\" -->\n  <!--    href=\"javascript:toggleRead('rovere-casella-vacchi-parravicini-firpo-ferrari-morri-bianchi-coastalandmarinegeomorphologybetweenalbengaandsavonanwmediterraneanseaitaly-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {Coastal and marine geomorphology between Albenga and Savona(NW Mediterranean Sea, Italy)},\n type = {article},\n year = {2015},\n keywords = {MIRAMAR,SEAMAP,SLCC},\n pages = {278-286},\n volume = {11},\n websites = {http://www.tandfonline.com/doi/abs/10.1080/17445647.2014.933134},\n month = {6},\n day = {24},\n id = {c344b1c9-df37-392f-9269-db1a39f0056e},\n created = {2018-02-03T12:46:08.766Z},\n accessed = {2014-09-15},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.165Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Rovere2014},\n private_publication = {false},\n abstract = {In this paper, we present a map describing the main geomorphological features of the coastal and marine area between the towns of Albenga and Savona (Ligurian Sea, NW Mediterranean) corresponding to a coastal stretch of ∼40 km. To produce this map, we collated data from the literature, orthophotos, perspective photos, multibeam and side scan sonar data, and undertook direct surveys to ground truth data obtained using indirect techniques. We divided the information into nine thematic layers, including bathymetry, natural coastal types, geomorphological elements, seafloor coverage (both geological and biological), coastal and nearshore dynamics, human influence on coastal and marine environments, coastal occupation and protected areas.},\n bibtype = {article},\n author = {Rovere, A. and Casella, E. and Vacchi, M. and Parravicini, V. and Firpo, M. and Ferrari, M. and Morri, C. and Bianchi, C. N.},\n doi = {10.1080/17445647.2014.933134},\n journal = {Journal of Maps},\n number = {2}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  In this paper, we present a map describing the main geomorphological features of the coastal and marine area between the towns of Albenga and Savona (Ligurian Sea, NW Mediterranean) corresponding to a coastal stretch of ∼40 km. To produce this map, we collated data from the literature, orthophotos, perspective photos, multibeam and side scan sonar data, and undertook direct surveys to ground truth data obtained using indirect techniques. We divided the information into nine thematic layers, including bathymetry, natural coastal types, geomorphological elements, seafloor coverage (both geological and biological), coastal and nearshore dynamics, human influence on coastal and marine environments, coastal occupation and protected areas.\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        (2)\n        \n      </span>\n    </div>\n    <div class=\"bibbase_group_body\">\n      \n  \n  <div class=\"bibbase_paper\" id=\"casella-rovere-pedroncini-mucerino-casella-cusati-vacchi-ferrari-etal-studyofwaverunupusingnumericalmodelsandlowaltitudeaerialphotogrammetryatoolforcoastalmanagement-2014\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://linkinghub.elsevier.com/retrieve/pii/S0272771414002273,http://dx.doi.org/10.1016/j.ecss.2014.08.012\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'casella-rovere-pedroncini-mucerino-casella-cusati-vacchi-ferrari-etal-studyofwaverunupusingnumericalmodelsandlowaltitudeaerialphotogrammetryatoolforcoastalmanagement-2014', 'http://linkinghub.elsevier.com/retrieve/pii/S0272771414002273,http://dx.doi.org/10.1016/j.ecss.2014.08.012', event);\">\n    Study of wave runup using numerical models and low-altitude aerial photogrammetry: A tool for coastal management.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  Casella,  E.; <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Pedroncini,  A.; Mucerino,  L.; Casella,  M.; Cusati,  L., A.; Vacchi,  M.; Ferrari,  M.;  and Firpo,  M.\n</span>\n\n  \n\n</span>\n\n  <i>Estuarine, Coastal and Shelf Science</i>, 149: 160-167. 8 2014.\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://linkinghub.elsevier.com/retrieve/pii/S0272771414002273,http://dx.doi.org/10.1016/j.ecss.2014.08.012\"\n     onclick=\"log_download('casella-rovere-pedroncini-mucerino-casella-cusati-vacchi-ferrari-etal-studyofwaverunupusingnumericalmodelsandlowaltitudeaerialphotogrammetryatoolforcoastalmanagement-2014', 'http://linkinghub.elsevier.com/retrieve/pii/S0272771414002273,http://dx.doi.org/10.1016/j.ecss.2014.08.012', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"Study of wave runup using numerical models and low-altitude aerial photogrammetry: A tool for coastal management [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.ecss.2014.08.012\"\n     onclick=\"log_download('casella-rovere-pedroncini-mucerino-casella-cusati-vacchi-ferrari-etal-studyofwaverunupusingnumericalmodelsandlowaltitudeaerialphotogrammetryatoolforcoastalmanagement-2014', 'http://doi.org/10.1016/j.ecss.2014.08.012', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/casella-rovere-pedroncini-mucerino-casella-cusati-vacchi-ferrari-etal-studyofwaverunupusingnumericalmodelsandlowaltitudeaerialphotogrammetryatoolforcoastalmanagement-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('casella-rovere-pedroncini-mucerino-casella-cusati-vacchi-ferrari-etal-studyofwaverunupusingnumericalmodelsandlowaltitudeaerialphotogrammetryatoolforcoastalmanagement-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{\n title = {Study of wave runup using numerical models and low-altitude aerial photogrammetry: A tool for coastal management},\n type = {article},\n year = {2014},\n keywords = {MEDFLOOD,MIRAMAR,PLIOMAX,SEAMAP,SLCC},\n pages = {160-167},\n volume = {149},\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0272771414002273,http://dx.doi.org/10.1016/j.ecss.2014.08.012},\n month = {8},\n publisher = {Elsevier Ltd},\n id = {8fb8ca01-2971-312e-8c98-3107d0542aff},\n created = {2018-02-03T12:42:09.112Z},\n accessed = {2014-09-25},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.243Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Casella2014},\n private_publication = {false},\n abstract = {Monitoring the impact of sea storms on coastal areas is fundamental to study beach evolution and the vulnerability of low-lying coasts to erosion and flooding. Modelling wave runup on a beach is possible, but it requires accurate topographic data and model tuning, that can be done comparing observed and modeled runup. In this study we collected aerial photos using an Unmanned Aerial Vehicle after two different swells on the same study area. We merged the point cloud obtained with photogrammetry with multibeam data, in order to obtain a complete beach topography. Then, on each set of rectified and georeferenced UAV orthophotos, we identified the maximum wave runup for both events recognizing the wet area left by the waves. We then used our topography and numerical models to simulate the wave runup and compare the model results to observed values during the two events. Our results highlight the potential of the methodology presented, which integrates UAV platforms, photogrammetry and Geographic Information Systems to provide faster and cheaper information on beach topography and geomorphology compared with traditional techniques without losing in accuracy. We use the results obtained from this technique as a topographic base for a model that calculates runup for the two swells. The observed and modeled runups are consistent, and open new directions for future research.},\n bibtype = {article},\n author = {Casella, Elisa and Rovere, Alessio and Pedroncini, Andrea and Mucerino, Luigi and Casella, Marco and Cusati, Luis Alberto and Vacchi, Matteo and Ferrari, Marco and Firpo, Marco},\n doi = {10.1016/j.ecss.2014.08.012},\n journal = {Estuarine, Coastal and Shelf Science}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Monitoring the impact of sea storms on coastal areas is fundamental to study beach evolution and the vulnerability of low-lying coasts to erosion and flooding. Modelling wave runup on a beach is possible, but it requires accurate topographic data and model tuning, that can be done comparing observed and modeled runup. In this study we collected aerial photos using an Unmanned Aerial Vehicle after two different swells on the same study area. We merged the point cloud obtained with photogrammetry with multibeam data, in order to obtain a complete beach topography. Then, on each set of rectified and georeferenced UAV orthophotos, we identified the maximum wave runup for both events recognizing the wet area left by the waves. We then used our topography and numerical models to simulate the wave runup and compare the model results to observed values during the two events. Our results highlight the potential of the methodology presented, which integrates UAV platforms, photogrammetry and Geographic Information Systems to provide faster and cheaper information on beach topography and geomorphology compared with traditional techniques without losing in accuracy. We use the results obtained from this technique as a topographic base for a model that calculates runup for the two swells. The observed and modeled runups are consistent, and open new directions for future research.\n</div>\n\n\n</div>\n\n\n  <div class=\"bibbase_paper\" id=\"rovere-raymo-mitrovica-hearty-oleary-inglis-themidpliocenesealevelconundrumglacialisostasyeustasyanddynamictopography-2014\">\n  <span class=\"bibbase_paper_titleauthoryear\">\n\n  \n  <span class=\"bibbase_paper_title\">\n  \n  \n  \n  <a href=\"http://linkinghub.elsevier.com/retrieve/pii/S0012821X13006006,papers2://publication/doi/10.1016/j.epsl.2013.10.030\"\n     onclick=\"return trackOutboundLink('publications', 'click', 'rovere-raymo-mitrovica-hearty-oleary-inglis-themidpliocenesealevelconundrumglacialisostasyeustasyanddynamictopography-2014', 'http://linkinghub.elsevier.com/retrieve/pii/S0012821X13006006,papers2://publication/doi/10.1016/j.epsl.2013.10.030', event);\">\n    The Mid-Pliocene sea-level conundrum: Glacial isostasy, eustasy and dynamic topography.\n  </a>\n  \n  \n  \n</span>\n\n  <span class=\"bibbase_paper_author\">\n  <a class=\"bibbase author link\" href=\"https://www.marum.de/Prof.-Dr.-alessio-rovere.html\">Rovere,  A.</a>; Raymo,  M., E.; Mitrovica,  J., X.; Hearty,  P., J.; O'Leary,  M., J.;  and Inglis,  J., D.\n</span>\n\n  \n\n</span>\n\n  <i>Earth and Planetary Science Letters</i>, 387: 27-33.  2014.\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://linkinghub.elsevier.com/retrieve/pii/S0012821X13006006,papers2://publication/doi/10.1016/j.epsl.2013.10.030\"\n     onclick=\"log_download('rovere-raymo-mitrovica-hearty-oleary-inglis-themidpliocenesealevelconundrumglacialisostasyeustasyanddynamictopography-2014', 'http://linkinghub.elsevier.com/retrieve/pii/S0012821X13006006,papers2://publication/doi/10.1016/j.epsl.2013.10.030', event.ctrlKey, event)\">\n    <img src=\"//bibbase.org/img/filetypes/link.svg\"\n\t     alt=\"The Mid-Pliocene sea-level conundrum: Glacial isostasy, eustasy and dynamic topography [link]\"\n       title=\"Website\"\n\t     class=\"bibbase_icon\"\n         ><span class=\"bibbase_icon_text\">Website</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"http://doi.org/10.1016/j.epsl.2013.10.030\"\n     onclick=\"log_download('rovere-raymo-mitrovica-hearty-oleary-inglis-themidpliocenesealevelconundrumglacialisostasyeustasyanddynamictopography-2014', 'http://doi.org/10.1016/j.epsl.2013.10.030', event.ctrlKey)\"\n     class=\"bibbase doi link\">\n    <span>doi</span></a>\n  &nbsp;\n  \n\n  \n  <a href=\"//bibbase.org/network/publication/rovere-raymo-mitrovica-hearty-oleary-inglis-themidpliocenesealevelconundrumglacialisostasyeustasyanddynamictopography-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('rovere-raymo-mitrovica-hearty-oleary-inglis-themidpliocenesealevelconundrumglacialisostasyeustasyanddynamictopography-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</span>\n\n<div class=\"well well-small bibbase\" data-type=\"bibtex\"\n     style=\"display:none\">\n  <pre style=\"white-space: pre-wrap;\">@article{\n title = {The Mid-Pliocene sea-level conundrum: Glacial isostasy, eustasy and dynamic topography},\n type = {article},\n year = {2014},\n keywords = {MEDFLOOD,PLIOMAX},\n pages = {27-33},\n volume = {387},\n websites = {http://linkinghub.elsevier.com/retrieve/pii/S0012821X13006006,papers2://publication/doi/10.1016/j.epsl.2013.10.030},\n publisher = {Elsevier B.V.},\n day = {1},\n id = {97905946-5bca-31d9-be05-3770c4ddacfc},\n created = {2018-02-03T12:46:08.757Z},\n file_attached = {false},\n profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},\n group_id = {c506fd31-7f0e-3486-8ab7-d996efa2ef2a},\n last_modified = {2019-05-09T11:32:24.049Z},\n read = {true},\n starred = {false},\n authored = {false},\n confirmed = {true},\n hidden = {false},\n citation_key = {Rovere2014f},\n source_type = {JOUR},\n private_publication = {false},\n abstract = {Determining eustatic sea level during the Mid-Pliocene warm period (~3.3 to 2.9 Ma) has been a central but elusive goal in the study of past warm climates. Estimates of eustatic sea level based on geologic data span a broad range; variation that we now recognize is due in part to geographically varying post-depositional displacement caused by glacial isostatic adjustment and dynamic topography. In this study, we combine field observations and glacial isostatic adjustment modeling to estimate the dynamic topography signal in three areas that are important to paleo-sea level studies of the Mid-Pliocene warm period (South Africa, West Australia and southeastern United States). We show that dynamic topography played a significant role in the post-depositional displacement of Pliocene, and even younger Pleistocene, shorelines. In this regard, we provide a robust paleo-sea level elevation data set, corrected for glacial isostatic adjustment, that can be used to evaluate predictions from mantle flow models of dynamic topography. © 2013 Elsevier B.V.},\n bibtype = {article},\n author = {Rovere, Alessio and Raymo, Maureen E and Mitrovica, Jerry X and Hearty, Paul J and O&#x27;Leary, M. J. and Inglis, J D},\n doi = {10.1016/j.epsl.2013.10.030},\n journal = {Earth and Planetary Science Letters}\n}</pre>\n</div>\n\n\n<div class=\"well well-small bibbase\" data-type=\"abstract\"\n     style=\"display:none\">\n  Determining eustatic sea level during the Mid-Pliocene warm period (~3.3 to 2.9 Ma) has been a central but elusive goal in the study of past warm climates. Estimates of eustatic sea level based on geologic data span a broad range; variation that we now recognize is due in part to geographically varying post-depositional displacement caused by glacial isostatic adjustment and dynamic topography. In this study, we combine field observations and glacial isostatic adjustment modeling to estimate the dynamic topography signal in three areas that are important to paleo-sea level studies of the Mid-Pliocene warm period (South Africa, West Australia and southeastern United States). We show that dynamic topography played a significant role in the post-depositional displacement of Pliocene, and even younger Pleistocene, shorelines. In this regard, we provide a robust paleo-sea level elevation data set, corrected for glacial isostatic adjustment, that can be used to evaluate predictions from mantle flow models of dynamic topography. © 2013 Elsevier B.V.\n</div>\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);