Dimethylated Sulfur, Methane and Aerobic Methane Production in the Yellow Sea and Bohai Sea

Abstract This paper presents a comprehensive study of biogenic dimethylated sulfur compounds and methane (CH 4 ) from 27 March to 16 April 2018 (spring) and from 24 July to 10 August 2018 (summer) in the Yellow Sea and Bohai Sea. The overall distributions of dimethylsulfide (DMS), dimethylsulfoniopropionate (DMSP, precursor of DMS), dimethylsulfoxide (DMSO, oxidation product of DMS) and CH 4 in surface waters were characterized by elevated concentrations in summer and in coastal waters, coupled to phytoplankton biomass and terrestrially sourced inputs. Surface waters were oversaturated with CH 4 . The flux distributions of DMS and CH 4 were generally consistent with their concentration distributions. In situ incubation experiments revealed that microbial consumption was the main removal mechanism for DMS, which could remove up to 72.1% of the total DMS compared to sea‐to‐air exchange in the surface layer. High DMS release and enhanced DMS yields (34%–62%) suggested more obvious influence from high DMSP concentrations (1 or 5 μm L −1 ) on DMS production in oligotrophic waters with lower bacterial sulfur demand in contrast to near‐shore waters. Positive correlations were found between CH 4 and DMSP (dissolved) in summer and DMSO (particulate and dissolved) in spring. A DMSP addition experiment suggested that DMSP could act as a precursor for aerobic methanogenesis, and CH 4 preferentially occurs under nitrogen‐stressed conditions in the surface layers of the Yellow Sea and Bohai Sea.