TY - GEN A1 - Foster, William J. A1 - Garvie, Christopher L. A1 - Weiss, Anna M. A1 - Muscente, A. Drew A1 - Aberhan, Martin A1 - Counts, John W. A1 - Martindale, Rowan C. T1 - Resilience of marine invertebrate communities during the early Cenozoic hyperthermals T2 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe N2 - The hyperthermal events of the Cenozoic, including the Paleocene-Eocene Thermal Maximum, provide an opportunity to investigate the potential effects of climate warming on marine ecosystems. Here, we examine the shallow benthic marine communities preserved in the late Cretaceous to Eocene strata on the Gulf Coastal Plain (United States). In stark contrast to the ecological shifts following the end-Cretaceous mass extinction, our data show that the early Cenozoic hyperthermals did not have a long-term impact on the generic diversity nor composition of the Gulf Coastal Plain molluscan communities. We propose that these communities were resilient to climate change because molluscs are better adapted to high temperatures than other taxa, as demonstrated by their physiology and evolutionary history. In terms of resilience, these communities differ from other shallow-water carbonate ecosystems, such as reef communities, which record significant changes during the early Cenozoic hyperthermals. These data highlight the strikingly different responses of community types, i.e., the almost imperceptible response of molluscs versus the marked turnover of foraminifera and reef faunas. The impact on molluscan communities may have been low because detrimental conditions did not devastate the entire Gulf Coastal Plain, allowing molluscs to rapidly recolonise vacated areas once harsh environmental conditions ameliorated. T3 - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 1410 KW - eocene thermal maximum KW - gulf coastal plain KW - climate-change KW - ocean acidification KW - extinction event KW - carbon-cycle KW - heat-stress KW - origination KW - ecosystems KW - diversity Y1 - 2020 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-516011 SN - 1866-8372 IS - 1 ER - TY - JOUR A1 - Foster, William J. A1 - Garvie, Christopher L. A1 - Weiss, Anna M. A1 - Muscente, A. Drew A1 - Aberhan, Martin A1 - Counts, John W. A1 - Martindale, Rowan C. T1 - Resilience of marine invertebrate communities during the early Cenozoic hyperthermals JF - Scientific Reports N2 - The hyperthermal events of the Cenozoic, including the Paleocene-Eocene Thermal Maximum, provide an opportunity to investigate the potential effects of climate warming on marine ecosystems. Here, we examine the shallow benthic marine communities preserved in the late Cretaceous to Eocene strata on the Gulf Coastal Plain (United States). In stark contrast to the ecological shifts following the end-Cretaceous mass extinction, our data show that the early Cenozoic hyperthermals did not have a long-term impact on the generic diversity nor composition of the Gulf Coastal Plain molluscan communities. We propose that these communities were resilient to climate change because molluscs are better adapted to high temperatures than other taxa, as demonstrated by their physiology and evolutionary history. In terms of resilience, these communities differ from other shallow-water carbonate ecosystems, such as reef communities, which record significant changes during the early Cenozoic hyperthermals. These data highlight the strikingly different responses of community types, i.e., the almost imperceptible response of molluscs versus the marked turnover of foraminifera and reef faunas. The impact on molluscan communities may have been low because detrimental conditions did not devastate the entire Gulf Coastal Plain, allowing molluscs to rapidly recolonise vacated areas once harsh environmental conditions ameliorated. KW - eocene thermal maximum KW - gulf coastal plain KW - climate-change KW - ocean acidification KW - extinction event KW - carbon-cycle KW - heat-stress KW - origination KW - ecosystems KW - diversity Y1 - 2020 U6 - https://doi.org/10.1038/s41598-020-58986-5 SN - 2045-2322 VL - 10 IS - 1 SP - 1 EP - 11 PB - Springer Nature CY - London ER - TY - JOUR A1 - Huang, Sichao A1 - Herzschuh, Ulrike A1 - Pestryakova, Luidmila Agafyevna A1 - Zimmermann, Heike Hildegard A1 - Davydova, Paraskovya A1 - Biskaborn, Boris A1 - Shevtsova, Iuliia A1 - Stoof-Leichsenring, Kathleen Rosemarie T1 - Genetic and morphologic determination of diatom community composition in surface sediments from glacial and thermokarst lakes in the Siberian Arctic JF - Journal of paleolimnolog N2 - Lakes cover large parts of the climatically sensitive Arctic landscape and respond rapidly to environmental change. Arctic lakes have different origins and include the predominant thermokarst lakes, which are small, young and highly dynamic, as well as large, old and stable glacial lakes. Freshwater diatoms dominate the primary producer community in these lakes and can be used to detect biotic responses to climate and environmental change. We used specific diatom metabarcoding on sedimentary DNA, combined with next-generation sequencing and diatom morphology, to assess diatom diversity in five glacial and 15 thermokarst lakes within the easternmost expanse of the Siberian treeline ecotone in Chukotka, Russia. We obtained 163 verified diatom sequence types and identified 176 diatom species morphologically. Although there were large differences in taxonomic assignment using the two approaches, they showed similar high abundances and diversity of Fragilariceae and Aulacoseiraceae. In particular, the genetic approach detected hidden within-lake variations of fragilarioids in glacial lakes and dominance of centric Aulacoseira species, whereas Lindavia ocellata was predominant using morphology. In thermokarst lakes, sequence types and valve counts also detected high diversity of Fragilariaceae, which followed the vegetation gradient along the treeline. Ordination analyses of the genetic data from glacial and thermokarst lakes suggest that concentrations of sulfate (SO42-), an indicator of the activity of sulfate-reducing microbes under anoxic conditions, and bicarbonate (HCO3-), which relates to surrounding vegetation, have a significant influence on diatom community composition. For thermokarst lakes, we also identified lake depth as an important variable, but SO42- best explains diatom diversity derived from genetic data, whereas HCO3- best explains the data from valve counts. Higher diatom diversity was detected in glacial lakes, most likely related to greater lake age and different edaphic settings, which gave rise to diversification and endemism. In contrast, small, dynamic thermokarst lakes are inhabited by stress-tolerant fragilarioids and are related to different vegetation types along the treeline ecotone. Our study demonstrated that genetic investigations of lake sediments can be used to interpret climate and environmental responses of diatoms. It also showed how lake type affects diatom diversity, and that such genetic analyses can be used to track diatom community changes under ongoing warming in the Arctic. KW - diatoms KW - diversity KW - glacial lakes KW - sedimentary DNA KW - Siberian arctic KW - thermokarst Y1 - 2020 U6 - https://doi.org/10.1007/s10933-020-00133-1 SN - 0921-2728 SN - 1573-0417 VL - 64 IS - 3 SP - 225 EP - 242 PB - Springer CY - Dordrecht ER -