Past and future decline of tropical pelagic biodiversity

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  • Moriaki Yasuhara
    Swire Institute of Marine Science, The University of Hong Kong, Hong Kong Special Administrative Region, China;
  • Chih-Lin Wei
    Institute of Oceanography, National Taiwan University, 106 Taipei, Taiwan;
  • Michal Kucera
    MARUM–Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany;
  • Mark J. Costello
    School of Environment, The University of Auckland, 1142 Auckland, New Zealand;
  • Derek P. Tittensor
    Department of Biology, Dalhousie University, Halifax, NS, B3H 4R2 Canada;
  • Wolfgang Kiessling
    GeoZentrum Nordbayern, Department of Geography and Geosciences, Friedrich-Alexander Universität Erlangen–Nürnberg, 91054 Erlangen, Germany;
  • Timothy C. Bonebrake
    School of Biological Sciences, The University of Hong Kong, Hong Kong Special Administrative Region, China;
  • Clay R. Tabor
    Department of Geosciences, University of Connecticut, Storrs, CT 06269;
  • Ran Feng
    Department of Geosciences, University of Connecticut, Storrs, CT 06269;
  • Andrés Baselga
    Departamento de Zoología, Genética y Antropología Física, Facultad de Biología, Universidad de Santiago de Compostela, 15782 Santiago de Compostela, Spain;
  • Kerstin Kretschmer
    MARUM–Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany;
  • Buntarou Kusumoto
    Faculty of Science, University of the Ryukyus, 903-0213 Okinawa, Japan
  • Yasuhiro Kubota
    Faculty of Science, University of the Ryukyus, 903-0213 Okinawa, Japan

書誌事項

公開日
2020-05-26
権利情報
  • https://www.pnas.org/site/aboutpnas/licenses.xhtml
DOI
  • 10.1073/pnas.1916923117
公開者
Proceedings of the National Academy of Sciences

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<jats:title>Significance</jats:title><jats:p>We discovered that the tropical oceanic diversity depression is not a recent phenomenon nor very deep time in origin by using a comprehensive global dataset of the calcified shells of planktonic foraminifers, abundant unicellular organisms in the world's oceans, which are exceptionally well preserved in marine sediments as fossils. The diversity decline in the lowest latitudes may have started due to rapid post–ice-age warming around 15,000 y ago. Warming may by the end of this century diminish tropical oceanic diversity to an unprecedented level in human history.</jats:p>

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