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Transient marine euxinia at the end of the terminal Cryogenian glaciation
Termination of the terminal Cryogenian Marinoan snowball Earth glaciation (~650–635 Ma) is associated with the worldwide deposition of a cap carbonate. Modeling studies suggest that, during and immediately following deglaciation, the ocean may have experienced a rapid rise in pH and physical stratif...
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| I publikationen: | Nat Commun |
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| Huvudupphovsmän: | , , , , , , , , , , , |
| Materialtyp: | Artigo |
| Språk: | Inglês |
| Publicerad: |
Nature Publishing Group UK
2018
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| Ämnen: | |
| Länkar: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6070556/ https://ncbi.nlm.nih.gov/pubmed/30068999 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-05423-x |
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