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Oxic Fe(III) reduction could have generated Fe(II) in the photic zone of Precambrian seawater
Many marine Precambrian iron formations (IF) record deep anoxic seawater enriched in Fe(II) (i.e. ferruginous) overlain by mildly oxygenated surface water. This is reflected by iron-rich sediments forming in deep basins, and relatively iron-poor sediments forming in shallow, sunlit waters. Such an i...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2018
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5845006/ https://www.ncbi.nlm.nih.gov/pubmed/29523861 http://dx.doi.org/10.1038/s41598-018-22694-y |