Item talk:Q256819

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   "name": "Big Soda Lake (Nevada). 2. Pelagic sulfate reduction",
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   "abstract": "The epilimnion of hypersaline, alkaline, meromictic Big Soda Lake contains an average 58 mmol sulfate liter\u22121\u00a0and 0.4\u00a0\u00b5mol dissolved iron liter\u22121. The monimolimnion, which is permanently anoxic, has a sulfide concentration ranging seasonally from 4 to 7 mmol liter\u22121. Depth profiles of sulfate reduction in the monimolimnion, assayed with a\u00a035S tracer technique and in situ incubations, demonstrated that sulfate reduction occurs within the water column of this extreme environment. The average rate of reduction in the monimolimnion was 3\u00a0\u00b5mol sulfate liter\u22121\u00a0d\u22121in May compared to 0.9 in October. These values are comparable to rates of sulfate reduction reported for anoxic waters of more moderate environments. Sulfate reduction also occurred in the anoxic zone of the mixolimnion, though at significantly lower rates (0.025\u20130.090\u00a0\u00b5mol liter\u22121\u00a0d\u22121\u00a0at 25 m). Additions of FeS (1.0 mmol liter\u22121) doubled the endogenous rate of sulfate reduction in the monimolimnion, while MnS and kaolinite had no effect. These results suggest that sulfate reduction in Big Soda Lake is iron limited and controlled by seasonal variables other than temperature. Estimates of the organic carbon mineralized by sulfate reduction exceed measured fluxes of particulate organic carbon sinking from the mixolimnion. Thus, additional sources of electron donors (other than those derived from the sinking of pelagic autotrophs) may also fuel monimolimnetic sulfate reduction in the lake.",
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