UNLABELLED: 2-mercaptoethanesulfonate (Coenzyme M, CoM) is an organic sulfur-containing cofactor used for hydrocarbon metabolism in Archaea and Bacteria. In Archaea, CoM serves as an alkyl group carrier for enzymes belonging to the alkyl-CoM reductase family, including methyl-CoM reductase, which catalyzes methane formation in methanogens. Two pathways for the biosynthesis of CoM are present in methanogenic archaea. The initial steps of these pathways are distinct but the last two reactions, leading up to CoM formation, are universally conserved. The final step is proposed to be mediated by methanogenesis marker metalloprotein 16 (MMP16), a putative sulfurtransferase, that replaces the aldehyde group of sulfoacetaldehyde with a thiol to generate CoM. The assignment of MMP16 as CoM synthase (ComF) is not widely accepted as deletion mutants have been shown to grow without any CoM dependence. Here, we investigate the role of MMP16 in the model methanogen, AUTHOR SUMMARY: Methane is a high energy renewable fuel that is the primary constituent of natural gas and a potent greenhouse gas. A significant fraction of global methane emissions is generated by the activity of methanogenic archaea. These microorganisms use a cofactor called Coenzyme M (CoM) as a methyl carrier for methane production mediated by the enzyme Methyl-Coenzyme M reductase. Since methane production is essential for energy conservation in methanogens, they need to synthesize or import CoM. Accordingly, most methanogens encode either one of two CoM biosynthesis pathways. Methanogenesis marker 16 metalloprotein (MMP16) is proposed to catalyze the last step of CoM biosynthesis in both pathways however experimental evidence to this effect is lacking. Here we demonstrate that MMP16 is, indeed, the primary CoM synthase (ComF) in the model methanogen,