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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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| Autors principals: | , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
American Society for Microbiology (ASM)
2001
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC92949/ https://ncbi.nlm.nih.gov/pubmed/11375205 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1128/AEM.67.6.2844-2848.2001 |
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