Dimethyl sulfide (DMS) or methylthiomethane is an organosulfur compound with the formula (CH3)2S. Dimethyl sulfide is a water-insoluble flammable liquid that boils at 37°C and has a characteristic disagreeable odor. It is a component of the smell produced from cooking of certain vegetables, notably corn, cabbage, beetroot and seafoods. It is also an indication of bacterial infection in malt production and brewing. It is a breakdown product of dimethylsulfoniopropionate (DMSP), and is also produced by the bacterial metabolism of methanethiol.
DMS is oxidized in the marine atmosphere to various sulfur-containing compounds, such as sulfur dioxide, dimethyl sulfoxide (DMSO), dimethyl sulfone, methane sulfonic acid and sulfuric acid. Among these compounds, sulfuric acid has the potential to create new aerosols which act as cloud condensation nuclei. Through this interaction with cloud formation, the massive production of atmospheric DMS over the oceans may have a significant impact on the Earth's climate. The CLAW hypothesis suggests that in this manner DMS may play a role in planetary homeostasis.
Marine phytoplankton also produces dimethyl sulfide. Andrew Johnston, of the University of East Anglia, has characterized DMS as being the "smell of the sea". It would be more accurate to say that DMS is a component of the "smell of the sea," another being pheromones of algae called dictyopterenes.
Dimethyl sulfide is also an odorant emitted by kraft pulping mills, and a byproduct of Swern oxidation.
The largest single commercial producer of DMS in the world is Gaylord Chemical Corporation, which is a significant economic component of the paper industry of Bogalusa, Louisiana.