Biogenic Magnetite Formation through Anaerobic Biooxidation of Fe(II)

The presence of isotopically light carbonates in association with fine-grained magnetite is considered to be primarily due to the reduction of Fe(III) by Fe(III)-reducing bacteria in the environment. Here, we report on magnetite formation by biooxidation of Fe(II) coupled to denitrification. This me...

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Manylion Llyfryddiaeth

Cyhoeddwyd yn:	Appl Environ Microbiol
Prif Awduron:	Chaudhuri, Swades K., Lack, Joseph G., Coates, John D.
Fformat:	Artigo
Iaith:	Inglês
Cyhoeddwyd:	American Society for Microbiology (ASM) 2001
Pynciau:	Geomicrobiology
Mynediad Ar-lein:	https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC92949/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/11375205/ https://ncbi.nlm.nih.govhttps://doi.org/10.1128/AEM.67.6.2844-2848.2001
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