“…Dimethylsulfoniopropionate (DMSP), as a DMS precursor, is primarily produced by a variety of phytoplankton in the euphotic layer (Simóet al, 1998;Bullock et al, 2017). Most DMSP released into seawater is utilized by bacteria through demethylation or demethiolation pathways leading to production of methanethiol, which represents a source of energy, carbon, and reduced sulfur, while the proportion utilized by the bacterial lyase pathway to produce DMS is minor, i.e.,<20% (Kiene et al, 1999;Boden and Hutt, 2019). In addition to microbial metabolism, certain algae such as Phaeocystis that have highly active DMSP lyases, can degrade DMSP to DMS, which is released into seawater (Keller et al, 1989;Steinke et al, 2007).…”