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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| Publicado no: | Appl Environ Microbiol |
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| Principais autores: | , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
American Society for Microbiology (ASM)
2001
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| Assuntos: | |
| Acesso em linha: | 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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