Hydrogen as an electron donor for sulfate-reducing bacteria in slurries of salt marsh sediment.

Experiments with a Warburg respirometer showed that a sediment slurry consumed hydrogen from a hydrogen atmosphere, and this consumption was not due to the activity of methanogenic bacteria. The hydrogren uptake was inhibited by the addition of 20 mM molybdate. Further experiments with sediment slurry held in conical flasks under an atmosphere of nitrogen showed that hydrogen accumulated in the headspace when bacterial sulfate reduction was inhibited either by the addition of 20 mM molybdate or by low (<5 mM) sulfate concentrations in the slurry. Methanogenesis was stimulated in the presence of a hydrogen atmosphere or by the addition of 20 mM molybdate. The results confirmed that hydrogren was an important electron donor for sulfate-reducing bacteria present in the sediment. The stimulation of methanogenesis by molybdate could be explained in part by a competition for hydrogen between sulfate-reducing bacteria and hydrogen-metabolizing methanogenic bacteria, but competition for another common substrate, possibly acetate, could also be significant.