Response of the Pacific inter-tropical convergence zone to global cooling and initiation of Antarctic glaciation across the Eocene Oligocene Transition

Approximately 34 million years ago across the Eocene–Oligocene transition (EOT), Earth’s climate tipped from a largely unglaciated state into one that sustained large ice sheets on Antarctica. Antarctic glaciation is attributed to a threshold response to slow decline in atmospheric CO(2) but our und...

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Detalles Bibliográficos
Autores principales: Hyeong, Kiseong, Kuroda, Junichiro, Seo, Inah, Wilson, Paul A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4979033/
https://www.ncbi.nlm.nih.gov/pubmed/27507793
http://dx.doi.org/10.1038/srep30647

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4979033/
https://www.ncbi.nlm.nih.gov/pubmed/27507793
http://dx.doi.org/10.1038/srep30647

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