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Sedimentary constraints on the duration of the Marinoan Oxygen-17 Depletion (MOSD) event
The ∼635 Ma Marinoan glaciation is marked by dramatic Earth system perturbations. Deposition of nonmass-dependently (17)O-depleted sulfate (SO(4)(2−)) in worldwide postglacial sediments is, thus far, unique to this glaciation. It is proposed that an extremely high-pCO(2) atmosphere can result in hig...
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| Main Authors: | , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2013
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3816407/ https://ncbi.nlm.nih.gov/pubmed/23386719 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1213154110 |
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