Middle Holocene expansion of Pacific Deep Water into the Southern Ocean.

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第一作者： Torben,Struve

第一单位： Department of Earth Science and Engineering, Imperial College London, SW7 2AZ London, United Kingdom; t.struve@icbm.de.

作者： Torben,Struve ^[1] ; David J,Wilson ^[2] ; Tina,van de Flierdt ^[3] ; Naomi,Pratt ^[4] ; Kirsty C,Crocket ^[3]

作者单位： Department of Earth Science and Engineering, Imperial College London, SW7 2AZ London, United Kingdom; t.struve@icbm.de. ^[1] The Grantham Institute for Climate Change and the Environment, Imperial College London, SW7 2AZ London, United Kingdom. ^[2] Department of Earth Science and Engineering, Imperial College London, SW7 2AZ London, United Kingdom. ^[3] Institute of Earth and Planetary Sciences, University College London and Birkbeck, University of London, WC1E 6BT London, United Kingdom. ^[4] School of Geosciences, University of Edinburgh, EH9 3FE Edinburgh, United Kingdom. ^[5]

关键词 Holocene Southern Ocean cold-water corals neodymium isotopes water mass mixing

DOI 10.1073/pnas.1908138117

PMID 31888997

发布时间 2020-06-30

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