At NB the SRR show a decreasing trend, dropping from 22 nmol cm -3 day -1 in the uppermost sample (0–0.05 mblf) to approximately 1 nmol m -3 day -1 below 0.2 mblf.
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Sulfate reduction controlled by organic matter availability in deep sediment cores from the saline, alkaline Lake Van (Eastern Anatolia, Turkey).
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