A better-ventilated ocean triggered by Late Cretaceous changes in continental configuration

Oceanic anoxic events (OAEs) are large-scale events of oxygen depletion in the deep ocean that happened during pre-Cenozoic periods of extreme warmth. Here, to assess the role of major continental configuration changes occurring during the Late Cretaceous on oceanic circulation modes, which in turn...

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Detalles Bibliográficos
Autores principales: Donnadieu, Yannick, Pucéat, Emmanuelle, Moiroud, Mathieu, Guillocheau, François, Deconinck, Jean- François
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4735640/
https://www.ncbi.nlm.nih.gov/pubmed/26777897
http://dx.doi.org/10.1038/ncomms10316

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4735640/
https://www.ncbi.nlm.nih.gov/pubmed/26777897
http://dx.doi.org/10.1038/ncomms10316

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