Concurrent low- and high-affinity sulfate reduction kinetics in marine sediment

Abstract

Bacterial sulfate reduction in marine sediments generally occurs in the presence of high millimolar concentrations of sulfate. Published data indicate that low sulfate concentrations may limit sulfate reduction rates below 0.2–2 mM. Yet, high sulfate reduction rates occur in the 1–100 μM range in freshwater sediments and at the sulfate–methane transition in marine sediments. Through a combination of 35S-tracer experiments, including initial velocity experiments and time course experiments, we searched for different sulfate affinities in the mixed community of sulfate reducers in a marine sediment. We supported the radiotracer experiments with a highly sensitive ion chromatographic technique for sulfate with a detection limit of 0.15 μM SO 4 2− in marine pore water. Our results showed that high and low affinities for sulfate co-occur and that the applied experimental approach may determine the observed apparent half saturation constant, K m. Our experimental and model data both show that sulfate reduction in the studied marine sediment could be explained by two dominating affinities for sulfate: a low affinity with a mean half saturation constant, K m, of 430 μM SO 4 2− and a high affinity with a mean K m of 2.6 μM SO 4 2−. The high-affinity sulfate reduction was thermodynamically un-constrained down to <1 μM SO 4 2−, both in our experiments and under in situ conditions. The reduction of radio-labeled sulfate was partly reversible due to concurrent re-oxidation of sulfide by Fe(III) and possibly due to a reversibility of the enzymatic pathway of sulfate reduction. A literature survey of apparent K m values for sediments and pure cultures is presented and discussed.