The production of dimethylsulfoniopropionate (DMSP) by marine phytoplankton and the fate of the produced DMSP and dimethylsulfide (DMS) were studied in 4 pelagic mesocosms during a n algal bloon~ over a period of 1 mo. Bacterial numbers, concentrations of particulate a n d dissolved DMSP, DMS, and chlorophyll a were mon~tored, as well as the turnover rates of DMS and DMSP Of the total amount of DMSP produced, only a fracbon could be detected as DhdS In the water column DMS production in the water column did not necessarily correlate with algal senescence, but also occurred during the maximum of the algal bloom. The flux of DMS to the atmosphere played a minor role a s a sink for DMS. Evidence is presented that shows bacterial consumption to be a major sink for DMS, under conditions of both high and lot\-[)MS water concentrations. DMSP was degraded either via cleavage or via demethylation; the results indicate a predominant role for the latter route.
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Kwint et al. (1996) studied this question.
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