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Metabolic potential of microbial communities from ferruginous sediments

Type of publication Peer-reviewed
Publikationsform Original article (peer-reviewed)
Author Vuillemin Aurèle, Horn Fabian, Friese André, Winkel Matthias, Alawi Mashal, Wagner Dirk, Henny Cynthia, Orsi William D, Crowe Sean A, Kallmeyer Jens,
Project Microbial processes in iron-rich sediments of Lake Towuti, Indonesia: Disentangling the methane and iron cycles
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Original article (peer-reviewed)

Journal Environmental Microbiology
Title of proceedings Environmental Microbiology
DOI 10.1111/1462-2920.14343

Open Access

Type of Open Access Publisher (Gold Open Access)


Ferruginous (Fe‐rich, SO4‐poor) conditions are generally restricted to freshwater sediments on Earth today, but were likely widespread during the Archean and Proterozoic Eons. Lake Towuti, Indonesia, is a large ferruginous lake that likely hosts geochemical processes analogous to those that operated in the ferruginous Archean ocean. The metabolic potential of microbial communities and related biogeochemical cycling under such conditions remain largely unknown. We combined geochemical measurements (pore water chemistry, sulfate reduction rates) with metagenomics to link metabolic potential with geochemical processes in the upper 50 cm of sediment. Microbial diversity and quantities of genes for dissimilatory sulfate reduction (dsrAB) and methanogenesis (mcrA) decrease with increasing depth, as do rates of potential sulfate reduction. The presence of taxa affiliated with known iron‐ and sulfate‐reducers implies potential use of ferric iron and sulfate as electron acceptors. Pore water concentrations of acetate imply active production through fermentation. Fermentation likely provides substrates for respiration with iron and sulfate as electron donors and for methanogens that were detected throughout the core. The presence of ANME‐1 16S and mcrA genes suggests potential for anaerobic methane oxidation. Overall our data suggest that microbial community metabolism in anoxic ferruginous sediments support coupled Fe, S, and C biogeochemical cycling.