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  • Title: Large sulfur isotope fractionation by bacterial sulfide oxidation.
    Author: Pellerin A, Antler G, Holm SA, Findlay AJ, Crockford PW, Turchyn AV, Jørgensen BB, Finster K.
    Journal: Sci Adv; 2019 Jul; 5(7):eaaw1480. PubMed ID: 31355330.
    Abstract:
    A sulfide-oxidizing microorganism, Desulfurivibrio alkaliphilus (DA), generates a consistent enrichment of sulfur-34 (34 S) in the produced sulfate of +12.5 per mil or greater. This observation challenges the general consensus that the microbial oxidation of sulfide does not result in large 34 S enrichments and suggests that sedimentary sulfides and sulfates may be influenced by metabolic activity associated with sulfide oxidation. Since the DA-type sulfide oxidation pathway is ubiquitous in sediments, in the modern environment, and throughout Earth history, the enrichments and depletions in 34 S in sediments may be the combined result of three microbial metabolisms: microbial sulfate reduction, the disproportionation of external sulfur intermediates, and microbial sulfide oxidation.
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