Closure of the Bering Strait caused Mid-Pleistocene Transition cooling
Closure of the Bering Strait caused Mid-Pleistocene Transition cooling
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Publisher
London: Nature Publishing Group UK
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Language
English
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Publisher
London: Nature Publishing Group UK
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Contents
The Mid-Pleistocene Transition (MPT) is characterised by cooling and lengthening glacial cycles from 600–1200 ka, thought to be driven by reductions in glacial CO
2
in particular from ~900 ka onwards. Reduced high latitude upwelling, a process that retains CO
2
within the deep ocean over glacials, could have aided drawdown but has so fa...
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Full title
Closure of the Bering Strait caused Mid-Pleistocene Transition cooling
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TN_cdi_doaj_primary_oai_doaj_org_article_66fa5f167de24bb1b71227a993df911e
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_66fa5f167de24bb1b71227a993df911e
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ISSN
2041-1723
E-ISSN
2041-1723
DOI
10.1038/s41467-018-07828-0
