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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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| Izdano u: | Nat Commun |
|---|---|
| Glavni autori: | , , , , |
| Format: | Artigo |
| Jezik: | Inglês |
| Izdano: |
Nature Publishing Group
2016
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| Teme: | |
| Online pristup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4735640/ https://ncbi.nlm.nih.gov/pubmed/26777897 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms10316 |
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