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Climate transition at the Eocene–Oligocene influenced by bathymetric changes to the Atlantic–Arctic oceanic gateways

The Eocene–Oligocene Transition (∼33.9 Ma) marks the largest step transformation within the Cenozoic cooling trend and is characterized by a sudden growth of the Antarctic ice sheets, cooling of the interior ocean, and the establishment of strong meridional temperature gradients. Here we examine the...

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Detalles Bibliográficos
Autores principales:	Straume, Eivind O., Nummelin, Aleksi, Gaina, Carmen, Nisancioglu, Kerim H.
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	National Academy of Sciences 2022
Materias:	Physical Sciences
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9169914/ https://www.ncbi.nlm.nih.gov/pubmed/35446685 http://dx.doi.org/10.1073/pnas.2115346119

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