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...

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Detalles Bibliográficos
Autores principales: Swanner, Elizabeth D., Maisch, Markus, Wu, Wenfang, Kappler, Andreas
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
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

Internet

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

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