Siderite-based anaerobic iron cycle driven by autotrophic thermophilic microbial consortium
Д. Г. Заварзина, Tatiana V. Kochetkova, Nataliya I. Chistyakova, Maria Gracheva, A. V. Antonova, Alexander Y. Merkel, Anna A. Perevalova, М. С. Чернов, Yury A. Koksharov, E. A. Bonch-Osmolovskaya, Sergey N. Gavrilov, A. Yu. Bychkov
Abstract
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 (FeCO 3 ), with CO 2 /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 N 2 /CO 2 -saturated liquid medium and microoxic (2% O 2 ) headspace. Long-term incubation (56 days) led to the formation of magnetite (Fe 3 O 4 ) instead of green rust as the main product of Fe(II) oxidation, the precipitation of newly formed metabolically induced siderite in the anoxic zone, and the deposition of hematite (Fe 2 O 3 ) on bioreactor walls over the oxycline boundary. Acetate was the only metabolic product of CO 2 /bicarbonate reduction. Thus, we have demonstrated the ability of autotrophic thermophilic microbial consortium to perform a short cycle of iron minerals transformation: siderite–magnetite–siderite, accompanied by magnetite and hematite accumulation. This cycle is believed to have driven the evolution of the early biosphere, leading to primary biomass production and deposition of the main iron mineral association of BIF.