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Biogenic magnetite formation through anaerobic biooxidation of Fe(II)
S K Chaudhuri1, J G Lack, J D Coates
1Department of Microbiology, Southern Illinois University, Carbondale, Illinois 62901, USA.
Abstract:
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.
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