作者: Y. Roh , C.-L. Zhang , H. Vali , R. J. Lauf , J. Zhou
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摘要: The formation of siderite and magnetite by Fe(III)-reducing bacteria may play an important role in C Fe geochemistry subsurface ocean sediments. objective this study was to identify environmental factors that control the (FeCO 3 ) (Fe O 4 bacteria. Psychrotolerant ( 45°C) were used examine reduction a poorly crystalline iron oxide, akaganeite (β-FeOOH), without soluble electron shuttle, anthraquinone disulfuonate (AQDS), presence N 2 , -CO (80:20, V:V), H V:V) headspace gases as well HCO − -buffered medium (30–210 mM) under atmosphere. Iron biomineralization also examined different growth conditions such salinity, pH, incubation time, temperature donors. Magnetite dominant Siderite A mixture formed headspace. Akaganeite reduced transformed (>120 with lactate donor Biogeochemical controlling phases secondary mineral suite include donors, atmospheric composition time. These results indicate microbial Fe(III) biogeochemistry sequestration natural environments.