Demethylation and cleavage of dimethylsulfoniopropionate and reduction of dimethyl sulfoxide by sulfate‐reducing bacteria

Abstract

Many marine algae contain high concentrations of dimethylsulfoniopropionate (DMSP); most likely this compound functions mainly as an osmolyte. In anoxic marine sediments DMSP can be degraded in two ways: via an initial demethylation, or via a cleavage to dimethyl sulfide (DMS) and acrylate. Although the occurrence of these processes in sediments was known, the types of organisms responsible for them were not. Recent data from our laboratory, however, have shown that certain types of sulfate‐reducing bacteria can carry out a demethylation of DMSP, whereas another sulfate reducer was found to cleave DMSP to DMS and acrylate, which was reduced to propionate. Thus, sulfate‐reducing bacteria might be responsible for at least a part of the observed DMSP transformations in anoxic sediments. It was also shown that a well‐known oxidation product of DMS, dimethyl sulfoxide, can function as an alternative electron acceptor in the metabolism of some marine sulfate reducers. These data are reviewed in the present article.