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Large sulfur isotope fractionation by bacterial sulfide oxidation
A sulfide-oxidizing microorganism, (DA), generates a consistent enrichment of sulfur-34 ( ) 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 enrichments and suggests that sedimentar...
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| Published in: | Science advances 2019-07, Vol.5 (7), p.eaaw1480 |
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| Main Authors: | , , , , , , , |
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| creator | Pellerin, André Antler, Gilad Holm, Simon Agner Findlay, Alyssa J Crockford, Peter W Turchyn, Alexandra V Jørgensen, Bo Barker Finster, Kai |
| description | A sulfide-oxidizing microorganism,
(DA), generates a consistent enrichment of sulfur-34 (
) 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
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
in sediments may be the combined result of three microbial metabolisms: microbial sulfate reduction, the disproportionation of external sulfur intermediates, and microbial sulfide oxidation. |
| doi_str_mv | 10.1126/sciadv.aaw1480 |
| format | article |
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(DA), generates a consistent enrichment of sulfur-34 (
) 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
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
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(DA), generates a consistent enrichment of sulfur-34 (
) 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
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
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) 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
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| source | American Association for the Advancement of Science; PubMed Central（OA） |
| subjects | Chemical Fractionation Deltaproteobacteria - chemistry Deltaproteobacteria - metabolism Geochemistry Metabolic Networks and Pathways Oxidation-Reduction SciAdv r-articles Sulfates - chemistry Sulfates - metabolism Sulfur Isotopes - chemistry Sulfur Isotopes - metabolism |
| title | Large sulfur isotope fractionation by bacterial sulfide oxidation |
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