Gateway-driven weakening of ocean gyres leads to Southern Ocean cooling

Declining atmospheric CO(2) concentrations are considered the primary driver for the Cenozoic Greenhouse-Icehouse transition, ~34 million years ago. A role for tectonically opening Southern Ocean gateways, initiating the onset of a thermally isolating Antarctic Circumpolar Current, has been disputed...

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Detalles Bibliográficos
Autores principales: Sauermilch, Isabel, Whittaker, Joanne M., Klocker, Andreas, Munday, David R., Hochmuth, Katharina, Bijl, Peter K., LaCasce, Joseph H.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8578591/
https://www.ncbi.nlm.nih.gov/pubmed/34753912
http://dx.doi.org/10.1038/s41467-021-26658-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8578591/
https://www.ncbi.nlm.nih.gov/pubmed/34753912
http://dx.doi.org/10.1038/s41467-021-26658-1

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