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Effect of a Jurassic oceanic anoxic event on belemnite ecology and evolution
The Toarcian oceanic anoxic event (T-OAE; ∼183 million y ago) is possibly the most extreme episode of widespread ocean oxygen deficiency in the Phanerozoic, coinciding with rapid atmospheric pCO(2) increase and significant loss of biodiversity in marine faunas. The event is a unique past tipping poi...
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| Hlavní autoři: | , , , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
2014
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4104856/ https://ncbi.nlm.nih.gov/pubmed/24982187 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1320156111 |
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