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Abstract Unlike biologically available nitrogen and phosphorus, which are often at limiting concentrations in surface seawater, sulfur in the form of sulfate is plentiful and not considered to constrain marine microbial activity. Nonetheless, in a model system in which a marine bacterium obtains all of its carbon from co-cultured phytoplankton, bacterial gene expression suggests that at least seven dissolved organic sulfur (DOS) metabolites support bacterial heterotrophy. These labile exometabolites of marine dinoflagellates and diatoms include taurine, N-acetyltaurine, isethionate, choline-O-sulfate, cysteate, 2,3-dihydroxypropane-1-sulfonate (DHPS), and dimethylsulfoniopropionate (DMSP). Leveraging from the compounds identified in this model system, we assessed the role of sulfur metabolites in the ocean carbon cycle by mining the Tara Oceans dataset for diagnostic genes. In the 1.4 million bacterial genome equivalents surveyed, estimates of the frequency of genomes harboring the capability for DOS metabolite utilization ranged broadly, from only 1 out of every 190 genomes (for the C2 sulfonate isethionate) to 1 out of every 5 (for the sulfonium compound DMSP). Bacteria able to participate in DOS transformations are dominated by Alphaproteobacteria in the surface ocean, but by SAR324, Acidimicrobiia, and Gammaproteobacteria at mesopelagic depths, where the capability for utilization occurs in higher frequency than in surface bacteria for more than half the sulfur metabolites. The discovery of an abundant and diverse suite of marine bacteria with the genetic capacity for DOS transformation argues for an important role for sulfur metabolites in the pelagic ocean carbon cycle. 

Dimethylsulfoniopropionate (DMSP) is produced by many species of marine phytoplankton and has been reported to provide a variety of beneficial functions including osmoregulation. Dinoflagellates are recognized as majorDMSPproducers; however, accumulation has been shown to be highly variable in this group. We explored the effect of hyposaline transfer inGambierdiscus belizeanusbetween ecologically relevant salinities (36 and 31) onDMSPaccumulation, Chla, cell growth, and cell volume, over 12 d. Our results showed thatG. belizeanusmaintained an intracellularDMSPcontent of 16.3 pmol cell⁻¹and concentration of 139 mMin both salinities. Although this intracellular concentration was near the median reported for other dinoflagellates, the cellular content achieved byG. belizeanuswas the highest reported of any dinoflagellate thus far, owing mainly to its large size.DMSPlevels were not significantly affected by salinity treatment but did change over time during the experiment. Salinity, however, did have a significant effect on the ratio ofDMSP:Chla, suggesting that salinity transfer ofG. belizeanusinduced a physiological response other thanDMSPadjustment. A survey ofDMSPcontent in a variety ofGambierdiscusspecies and strains revealed relatively highDMSPconcentrations (1.0–16.4 pmol cell⁻¹) as well as high intrageneric and intraspecific variation. We conclude that, althoughDMSPmay not be involved in long‐term (3–12 d) osmoregulation in this species,G. belizeanusand otherGambierdiscusspecies may be important contributors toDMSPproduction in tropical benthic microalgal communities due to their large size and high cellular content.