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Decreasing extents of Archean serpentinization contributed to the rise of an oxidized atmosphere
At present, molecular hydrogen (H(2)) produced through Fe(II) oxidation during serpentinization of ultramafic rocks represents a small fraction of the global sink for O(2) due to limited exposures of ultramafic rocks. In contrast, ultramafic rocks such as komatiites were much more common in the Earl...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2021
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8688491/ https://www.ncbi.nlm.nih.gov/pubmed/34930924 http://dx.doi.org/10.1038/s41467-021-27589-7 |