Dimethyl sulfide (DMS) is the main biogenic sulfur compound emitted to the atmosphere from seawater and likely affects the global climate (Andreae, 1990;Charlson et al., 1987). The oxidation products of DMS form cloud condensation nuclei, which changes the backscattering effect of sunlight and potentially affects the global environment (Charlson et al., 1987;Nguyen et al., 1992). The DMS precursor dimethylsulfoniopropionate (DMSP) is synthesized by marine phytoplankton (Keller et al., 1989) and bacteria (Curson et al., 2017(Curson et al., , 2018. DMSP is ubiquitous in the marine environment and serves numerous physiological and biological functions as an osmolyte (Kirst, 1989), a cryoprotectant (Sunda et al., 2002), and an antioxidant (Karsten et al., 1996). The DMS and DMSP sources and sinks in the ocean are closely related to marine organisms (i.e., bacteria, phytoplankton, and zooplankton) (Stefels et al., 2007). DMSP supplies sulfur and carbon to marine bacteria and zooplankton in the food web (Levasseur, 2013;Vila-Costa et al., 2006). DMSP dissolves in the water column and is catabolized by marine bacteria, mainly those from the classes α-Proteobacteria and γ-Proteobacteria (Curson et al., 2008;