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Minimal biomass deposition in banded iron formations inferred from organic matter and clay relationships

The cycling of iron and organic matter (OM) is thought to have been a major biogeochemical cycle in the early ferruginous oceans which contributed to the deposition of banded iron formations (BIF). However, BIF are deficient in OM, which is postulated to be the result of near-complete oxidation of O...

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Detalles Bibliográficos
Autores principales: Dodd, Matthew S., Papineau, Dominic, Pirajno, Franco, Wan, Yusheng, Karhu, Juha A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6828686/
https://www.ncbi.nlm.nih.gov/pubmed/31685820
http://dx.doi.org/10.1038/s41467-019-12975-z

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