Methanogenic archaea conserve energy for growth by reducing some one- and two-carbon compounds to methane and concomitantly generating an ion motive force. Growth of Methanosarcina acetivorans on carbon monoxide (CO) is peculiar as it involves formation of, besides methane, formate, acetate and methylated thiols. It has been argued that methane formation is partially inhibited under carboxidotrophic conditions and that the other products result from either detoxification of CO or from bypassing methanogenesis with other pathways for energy conservation. To gain a deeper understanding of the CO-dependent physiology of M. acetivorans we analyzed metabolite formation in resting cells. The initial rates of methane, acetate, formate, and dimethylsulfide formation increased differentially with increasing CO concentrations but were maximal already at the same moderate CO partial pressure. Strikingly, further increase of the amount of CO was not inhibitory. The maximal rate of methane formation from CO was approximately fivefold lower than that from methanol, consistent with the previously observed significant downregulation of the energy converting sodium-dependent methyltransferase. The rate of dimethylsulfide formation from CO was only 1-2% of that of methane formation under any conditions tested. Implications of the data presented for previously proposed pathways of CO utilization are discussed.