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Transient surface ocean oxygenation recorded in the ∼2.66-Ga Jeerinah Formation, Australia
Many paleoredox proxies indicate low-level and dynamic incipient oxygenation of Earth’s surface environments during the Neoarchean (2.8–2.5 Ga) before the Great Oxidation Event (GOE) at ∼2.4 Ga. The mode, tempo, and scale of these redox changes are poorly understood, because data from various locati...
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| Publicat a: | Proc Natl Acad Sci U S A |
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| Autors principals: | , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2018
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6065012/ https://ncbi.nlm.nih.gov/pubmed/29987010 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1720820115 |
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