Abstract
The relative importance of three environmental variables known to influence the rate of bacterial sulfate reduction was examined using sediment from a saltmarsh pan. The variables investigated were temperature, electron donor concentration, and electron acceptor concentration. Their relative influence on the rate of bacterial sulfate reduction was examined with multiple replicate sediment samples in which the variables were experimentally adjusted. Sulfate reduction rates were measured with35SO 4 2− . The relative importance of each variable to sulfate reduction rate was assessed with multiple regression analysis by calculating the standardized partial regression coefficients, and the results were compared with the ranges of the three variables encountered in the natural sediment. Temperature proved to have the greatest influence, followed by electron donor and electron acceptor concentrations, in that order. The sulfate concentration was shown to have little influence on sulfate reduction rate at seawater concentrations of sulfate, but its effect increased if sulfate concentrations were diminished compared to those of seawater.