Siderite-based anaerobic iron cycle driven by autotrophic thermophilic microbial consortium.

ABSTRACT: Using a sample from a terrestrial hot spring (pH 6.8, 60 °C), we enriched a thermophilic microbial consortium performing anaerobic autotrophic oxidation of hydrothermal siderite (FeCO₃), with CO₂/bicarbonate as the electron acceptor and the only carbon source, producing green rust and acetate. In order to reproduce Proterozoic environmental conditions during the deposition of banded iron formation (BIF), we incubated the microbial consortium in a bioreactor that contained an unmixed anoxic layer of siderite, perfectly mixed N₂/CO₂-saturated liquid medium and microoxic (2% O₂) headspace. Long-term incubation (56 days) led to the formation of magnetite (Fe₃O₄) instead of green rust as the main product of Fe(II) oxid

SUBMITTER: Zavarzina DG 

PROVIDER: S-EPMC7729950 | biostudies-literature | 2020 Dec

REPOSITORIES: biostudies-literature