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Hydrologic Alteration and Enhanced Microbial Reductive Dissolution of Fe(III) (hydr)oxides Under Flow Conditions in Fe(III)-Rich Rocks: Contribution to Cave-Forming Processes

Previous work demonstrated that microbial Fe(III)-reduction contributes to void formation, and potentially cave formation within Fe(III)-rich rocks, such as banded iron formation (BIF), iron ore and canga (a surficial duricrust), based on field observations and static batch cultures. Microbiological...

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Detalles Bibliográficos
Autores principales: Calapa, Kayla A., Mulford, Melissa K., Rieman, Tyler D., Senko, John M., Auler, Augusto S., Parker, Ceth W., Barton, Hazel A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8317133/
https://www.ncbi.nlm.nih.gov/pubmed/34335526
http://dx.doi.org/10.3389/fmicb.2021.696534

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