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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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| Publicado no: | Nat Commun |
|---|---|
| Main Authors: | , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2019
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6706372/ https://ncbi.nlm.nih.gov/pubmed/31439843 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-11828-z |
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