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DOI | 10.1073/pnas.1916923117 |
Past and future decline of tropical pelagic biodiversity | |
Yasuhara M.; Wei C.-L.; Kucera M.; Costello M.J.; Tittensor D.P.; Kiessling W.; Bonebrake T.C.; Tabor C.R.; Feng R.; Baselga A.; Kretschmer K.; Kusumoto B.; Kubota Y. | |
发表日期 | 2020 |
ISSN | 0027-8424 |
起始页码 | 12891 |
结束页码 | 12896 |
卷号 | 117期号:23 |
英文摘要 | A major research question concerning global pelagic biodiversity remains unanswered: when did the apparent tropical biodiversity depression (i.e., bimodality of latitudinal diversity gradient [LDG]) begin? The bimodal LDG may be a consequence of recent ocean warming or of deep-time evolutionary speciation and extinction processes. Using rich fossil datasets of planktonic foraminifers, we show here that a unimodal (or only weakly bimodal) diversity gradient, with a plateau in the tropics, occurred during the last ice age and has since then developed into a bimodal gradient through species distribution shifts driven by postglacial ocean warming. The bimodal LDG likely emerged before the Anthropocene and industrialization, and perhaps ∼15,000 y ago, indicating a strong environmental control of tropical diversity even before the start of anthropogenic warming. However, our model projections suggest that future anthropogenic warming further diminishes tropical pelagic diversity to a level not seen in millions of years. © 2020 National Academy of Sciences. All rights reserved. |
英文关键词 | Climate change; Last Glacial Maximum; Latitudinal diversity gradients; Planktonic foraminifera; Temperature |
语种 | 英语 |
scopus关键词 | article; biodiversity; climate change; foraminifer; fossil; ice age; industrialization; last glacial maximum; nonhuman; planktonic foraminifera; sea; species distribution; tropics; warming; animal; physiology; plankton; sediment; tropic climate; Animals; Biodiversity; Climate Change; Fossils; Geologic Sediments; Plankton; Tropical Climate |
来源期刊 | Proceedings of the National Academy of Sciences of the United States of America
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/160927 |
作者单位 | Yasuhara, M., Swire Institute of Marine Science, University of Hong Kong, Hong Kong Special Administrative, Region, China, School of Biological Sciences, University of Hong Kong, Hong Kong Special Administrative, Region, China; Wei, C.-L., Institute of Oceanography, National Taiwan University, Taipei, 106, Taiwan; Kucera, M., MARUM–Center for Marine Environmental Sciences, University of Bremen, Bremen, 28359, Germany, Faculty of Geosciences, University of Bremen, Bremen, 28359, Germany; Costello, M.J., School of Environment, University of Auckland, Auckland, 1142, New Zealand, Faculty of Biosciences and Aquaculture, Nord University, Bodø, 8049, Norway; Tittensor, D.P., Department of Biology, Dalhousie University, Halifax, NS B3H 4R2, Canada, United Nations Environment Programme World Conservation Monitoring Centre, Cambridge, CB3 0DL, United Kingdom; Kiessling, W., GeoZentrum Nordbayern, Department of Geography and Geosciences, Friedrich-Alexander Universität Erlangen–Nürnberg, Erlangen, 91054, Germany; ... |
推荐引用方式 GB/T 7714 | Yasuhara M.,Wei C.-L.,Kucera M.,et al. Past and future decline of tropical pelagic biodiversity[J],2020,117(23). |
APA | Yasuhara M..,Wei C.-L..,Kucera M..,Costello M.J..,Tittensor D.P..,...&Kubota Y..(2020).Past and future decline of tropical pelagic biodiversity.Proceedings of the National Academy of Sciences of the United States of America,117(23). |
MLA | Yasuhara M.,et al."Past and future decline of tropical pelagic biodiversity".Proceedings of the National Academy of Sciences of the United States of America 117.23(2020). |
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