The production of 34S-depleted sulfide during bacterial disproportionation of elemental sulfur.

Abstract

Bacteria that disproportionate elemental sulfur fractionate sulfur isotopes such that sulfate is enriched in sulfur-34 by 12.6 to 15.3 per mil and sulfide is depleted in sulfur-34 by 7.3 to 8.6 per mil. Through a repeated cycle of sulfide oxidation to S0 and subsequent disproportionation, these bacteria can deplete sedimentary sulfides in sulfur-34. A prediction, borne out by observation, is that more extensive sulfide oxidation will lead to sulfides that are more depleted in sulfur-34. Thus, the oxidative part of the sulfur cycle creates circumstances by which sulfides become more depleted in sulfur-34 than would be possible with sulfate-reducing bacteria alone.

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@article{Canfield1994ThePO, title={The production of 34S-depleted sulfide during bacterial disproportionation of elemental sulfur.}, author={Donald Eugene Canfield and Bo Thamdrup}, journal={Science}, year={1994}, volume={266}, pages={1973-5} }