Microbial processes during deposition and diagenesis of Banded Iron Formations

Banded Iron Formations (BIFs) are marine chemical sediments consisting of alternating iron (Fe)-rich and silica (Si)-rich bands which were deposited throughout much of the Precambrian era. BIFs represent important proxies for the geochemical composition of Precambrian seawater and provide evidence f...

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Detalles Bibliográficos
Autores principales: Dreher, Carolin L., Schad, Manuel, Robbins, Leslie J., Konhauser, Kurt O., Kappler, Andreas, Joshi, Prachi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2021
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8724090/
https://www.ncbi.nlm.nih.gov/pubmed/35034981
http://dx.doi.org/10.1007/s12542-021-00598-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8724090/
https://www.ncbi.nlm.nih.gov/pubmed/35034981
http://dx.doi.org/10.1007/s12542-021-00598-z

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