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Biogenic Magnetite Formation through Anaerobic Biooxidation of Fe(II)

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PubMed Central2026-05-16 收录
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https://pmc.ncbi.nlm.nih.gov/articles/PMC92949/
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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 metabolism offers an alternative environmental source of biogenic magnetite.
提供机构:
American Society for Microbiology (ASM)
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