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,...

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Detalles Bibliográficos
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.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
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

Internet

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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