Manganese sulfide formation via concomitant microbial manganese oxide and thiosulfate reduction

Abstract

Summary The dissimilatory metal‐reducing bacterium, Shewanella oneidensis MR‐1 produced γ‐MnS (rambergite) nanoparticles during the concurrent reduction of MnO 2 and thiosulfate coupled to H 2 oxidation. To investigate effect of direct microbial reduction of MnO 2 on MnS formation, two MR‐1 mutants defective in outer membrane c ‐type cytochromes (Δ mtrC /Δ omcA and Δ mtrC /Δ omcA /Δ mtrF ) were also used and it was determined that direct reduction of MnO 2 was dominant relative to chemical reduction by biogenic sulfide generated from thiosulfate reduction. Although bicarbonate was excluded from the medium, incubations of strain MR‐1 with lactate as the electron donor produced MnCO 3 (rhodochrosite) as well as MnS in nearly equivalent amounts as estimated by micro X‐ray diffraction (micro‐XRD) analysis. It was concluded that carbonate released from lactate metabolism promoted MnCO 3 formation and that Mn(II) mineralogy was strongly affected by carbonate ions even in the presence of abundant sulfide and weakly alkaline conditions expected to favour the precipitation of MnS. Formation of MnS, as determined by a combination of micro‐XRD, transmission electron microscopy, energy dispersive X‐ray spectroscopy, and selected area electron diffraction analyses was consistent with equilibrium speciation modelling predictions. Biogenic manganese sulfide may be a manganese sink in the Mn biogeochemical cycle in select environments such as deep anoxic marine basins within the Baltic Sea.

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