“…Mirroring the sulfate-reducing populations, the diversity of detected methanogens suggests that a wide range of substrates—including acetate, hydrogen and formate, C1 compounds, and primary and secondary alcohols—could potentially be utilized for methanogenesis. While Arc I group archaea have been hypothesized to produce methane from methylated thiol groups [ 71 ], Methanosarcina species can utilize H 2 /CO 2 , acetate, dimethylsulfide, methanol, monomethylamine, dimethylamine, and trimethylamine [ 72 , 73 ], and Methanomassiliicoccus luminyensis is able to grow on methanol, mono-, di-, or trimethylamine with hydrogen [ 74 ]. Moreover, Methanofollis ethanolicus can utilize ethanol/CO 2 , 1-propanol/CO 2 , 1-butanol/CO 2 , H 2 /CO 2 , and formate for growth and methane production, converting ethanol to methane and acetate [ 75 ], while Methanofollis liminatans can utilize formate, H 2 /CO 2 , 2-propanol/CO 2 , 2-butanol/CO 2 , and cyclopentanol/CO 2 , converting these secondary and cyclic alcohols to their respective ketones [ 76 ].…”