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Sedimentary sulfur isotopes and Neoarchean ocean oxygenation
Abrupt disappearance of mass-independent fractionation of sulfur isotopes (MIF-S) from the geologic record and an apparent ingrowth in seawater sulfate around 2.45 billion years ago (Ga) signal the first large-scale oxygenation of the atmosphere [the Great Oxygenation Event (GOE)]. Pre-GOE O(2) prod...
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| Yayımlandı: | Sci Adv |
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| Asıl Yazarlar: | , , |
| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
American Association for the Advancement of Science
2018
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| Konular: | |
| Online Erişim: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5783677/ https://ncbi.nlm.nih.gov/pubmed/29376118 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.1701835 |
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