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Strong evidence for a weakly oxygenated ocean–atmosphere system during the Proterozoic
Earth’s surface has undergone a protracted oxygenation, which is commonly assumed to have profoundly affected the biosphere. However, basic aspects of this history are still debated—foremost oxygen (O(2)) levels in the oceans and atmosphere during the billion years leading up to the rise of algae an...
| Autores principales: | , , , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
National Academy of Sciences
2022
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8833159/ https://www.ncbi.nlm.nih.gov/pubmed/35101984 http://dx.doi.org/10.1073/pnas.2116101119 |