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Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago
Molecular oxygen (O(2)) is, and has been, a primary driver of biological evolution and shapes the contemporary landscape of Earth’s biogeochemical cycles. Although “whiffs” of oxygen have been documented in the Archean atmosphere, substantial O(2) did not accumulate irreversibly until the Early Pale...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
American Association for the Advancement of Science
2016
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4928975/ https://www.ncbi.nlm.nih.gov/pubmed/27386544 http://dx.doi.org/10.1126/sciadv.1600134 |