Arctic closure as a trigger for Atlantic overturning at the Eocene-Oligocene Transition

The Eocene-Oligocene Transition (EOT), approximately 34 Ma ago, marks a period of major global cooling and inception of the Antarctic ice sheet. Proxies of deep circulation suggest a contemporaneous onset or strengthening of the Atlantic meridional overturning circulation (AMOC). Proxy evidence of g...

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Detalles Bibliográficos
Autores principales: Hutchinson, David K., Coxall, Helen K., OʹRegan, Matt, Nilsson, Johan, Caballero, Rodrigo, de Boer, Agatha M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6706372/
https://www.ncbi.nlm.nih.gov/pubmed/31439843
http://dx.doi.org/10.1038/s41467-019-11828-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6706372/
https://www.ncbi.nlm.nih.gov/pubmed/31439843
http://dx.doi.org/10.1038/s41467-019-11828-z

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