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Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery
The end-Permian mass extinction, ∼252 million years ago, is notable for a complex recovery period of ∼5 Myr. Widespread euxinic (anoxic and sulfidic) oceanic conditions have been proposed as both extinction mechanism and explanation for the protracted recovery period, yet the vertical distribution o...
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| Izdano u: | Nat Commun |
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| 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/PMC4960316/ https://ncbi.nlm.nih.gov/pubmed/27433855 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms12236 |
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