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Elevated CO(2) degassing rates prevented the return of Snowball Earth during the Phanerozoic
The Cryogenian period (~720–635 Ma) is marked by extensive Snowball Earth glaciations. These have previously been linked to CO(2) draw-down, but the severe cold climates of the Cryogenian have never been replicated during the Phanerozoic despite similar, and sometimes more dramatic changes to carbon...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2017
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5736558/ https://www.ncbi.nlm.nih.gov/pubmed/29062095 http://dx.doi.org/10.1038/s41467-017-01456-w |