Despite its toxicity for the majority of living matter on our planet, numerous microorganisms, both aerobic and anaerobic, can use carbon monoxide (CO) as a source of carbon and/or energy for growth. The capacity to employ carboxidotrophic energy metabolism anaerobically is found in phylogenetically diverse members of the Bacteria and the Archaea. The oxidation of CO is coupled to numerous respiratory processes, such as desulfurication, hydrogenogenesis, acetogenesis, and methanogenesis. Although as diverse as the organisms capable of it, any CO-dependent energy metabolism known depends on the presence of carbon monoxide dehydrogenase. This review summarizes recent insights into the CO-dependent physiology of anaerobic microorganisms with a focus on methanogenic archaea. Carboxidotrophic growth of Methanosarcina acetivorans, thought to strictly rely on the process of methanogenesis, also involves formation of methylated thiols, formate, and even acetogenesis, and, thus, exemplifies how the beneficial redox properties of CO can be exploited in unexpected ways by anaerobic microorganisms.

SummaryMethanosarcina acetivorans is able to use carbon monoxide (CO) as the sole source of energy for growth. Its carboxidotrophic growth is peculiar as it involves formation of acetate, formate and methylated thiols, besides methane. Under this condition three proteins homologous to both corrinoid proteins and methyltransferases (MA0859, MA4384 and MA4558) are highly abundant. To address their role in M. acetivorans, a set of single and double mutants, and the triple mutant, was constructed by deletion/ disruption of the encoding genes. Phenotypic analysis of the mutants rules out an important role of the methyltransferase homologues in the CO 2 reduction pathway of methanogenesis. Instead, the single and double mutants were affected to various degrees in their capacity to generate dimethylsulphide (DMS) from CO and to form methane from DMS. The triple mutant was unable to produce or metabolize DMS, and could not grow with DMS as the sole energy source, which demonstrates that MA0859, MA4384 and MA4558 are involved in, and required for, methylsulphide metabolism of M. acetivorans. Based on these findings we propose to designate MA0859, MA4384 and MA4558 as methyltransferases specific for methylsulphides, MtsD, MtsF and MtsH respectively.

Methanosarcina acetivorans, a member of the methanogenic archaea, can grow with carbon monoxide (CO) as the sole energy source and generates, unlike other methanogens, substantial amounts of acetate and formate in addition to methane. Phenotypic analyses of mutant strains lacking the cooS1F operon and the cooS2 gene suggest that the monofunctional carbon monoxide dehydrogenase (CODH) system contributes to, but is not required for, carboxidotrophic growth of M. acetivorans. Further, qualitative proteomic analyses confirm a recent report (Lessner et al., Proc Natl Acad Sci USA, 103:17921-17926, 2006) in showing that the bifunctional CODH/acetyl-CoA synthase (ACS) system, two enzymes involved in CO(2)-reduction, and a peculiar protein homologous to both corrinoid proteins and methyltransferases are synthesized at elevated levels in response to CO; however, the finding that the latter protein is also abundant when trimethylamine serves as growth substrate questions its proposed involvement in the reduction of methyl-groups to methane. Potential catabolic mechanisms and metabolic adaptations employed by M. acetivorans to effectively utilize CO are discussed.

Conversion of acetate to methane (aceticlastic methanogenesis) is an ecologically important process carried out exclusively by methanogenic archaea. An important enzyme for this process as well as for methanogenic growth on carbon monoxide is the five-subunit archaeal CO dehydrogenase/acetyl coenzyme A (CoA) synthase multienzyme complex (CODH/ACS) catalyzing both CO oxidation/CO 2 reduction and cleavage/synthesis of acetyl-CoA. Methanosarcina acetivorans C2A contains two very similar copies of a six-gene operon (cdh genes) encoding two isoforms of CODH/ACS (Cdh1 and Cdh2) and a single CdhA subunit, CdhA3. To address the role of the CODH/ACS system in M. acetivorans, mutational as well as promoter/reporter gene fusion analyses were conducted. Phenotypic characterization of cdh disruption mutants (three single and double mutants, as well as the triple mutant) revealed a strict requirement of either Cdh1 or Cdh2 for acetotrophic or carboxidotrophic growth, as well as for autotrophy, which demonstrated that both isoforms are bona fide CODH/ACS. While expression of the Cdh2-encoding genes was generally higher than that of genes encoding Cdh1, both appeared to be regulated differentially in response to growth phase and to changing substrate conditions. While dispensable for growth, CdhA3 clearly affected expression of cdh1, suggesting that it functions in signal perception and transduction rather than in catabolism. The data obtained argue for a functional hierarchy and regulatory cross talk of the CODH/ACS isoforms.

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.