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Closure of the Bering Strait caused Mid-Pleistocene Transition cooling
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,...
Autores principales: | Kender, Sev, Ravelo, Ana Christina, Worne, Savannah, Swann, George E. A., Leng, Melanie J., Asahi, Hirofumi, Becker, Julia, Detlef, Henrieka, Aiello, Ivano W., Andreasen, Dyke, Hall, Ian R. |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2018
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6300599/ https://www.ncbi.nlm.nih.gov/pubmed/30568245 http://dx.doi.org/10.1038/s41467-018-07828-0 |
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