Thermococcus onnurineus NA1, a sulfur-reducing hyperthermophilic archaeon, is capable of H 2 -producing growth, considered to be hydrogenogenic carboxydotrophy. Utilization of formate as a sole energy source has been well studied in T. onnurineus NA1. However, whether formate can be used as its carbon source remains unknown. To obtain a global view of the metabolic characteristics of H 2 -producing growth, a quantitative proteome analysis of T. onnurineus NA1 grown on formate, CO, and starch was performed by combining one-dimensional SDS-PAGE with nano UPLC-MS E . A total of 587 proteins corresponding to 29.7% of the encoding genes were identified, and the major metabolic pathways (especially energy metabolism) were characterized at the protein level. Expression of glycolytic enzymes was common but more highly induced in starch-grown cells. In contrast, enzymes involved in key steps of the gluconeogenesis and pentose phosphate pathways were strongly up-regulated in formate-grown cells, suggesting that formate could be utilized as a carbon source by T. onnurineus NA1. In accordance with the genomic analysis, comprehensive proteomic analysis also revealed a number of hydrogenase clusters apparently associated with formate metabolism. On the other hand, CODH and CO-induced hydrogenases belonging to the Hyg4-II cluster, as well as sulfhydrogenase-I and Mbx, were prominently expressed during CO culture. Our data suggest that CO can be utilized as a sole energy source for H 2 production via an electron transport mechanism and that CO 2 produced from catabolism or CO oxidation by CODH and CO-induced hydrogenases may subsequently be assimilated into the organic carbon. Hyperthermophilic archaea can use a wide variety of carbon and energy sources. Hyperthermophiles are widely distributed in extreme habitats such as deep-sea thermal vents, hot springs, and deep oil reservoirs (1-3). So far, the most frequently studied hyperthermophiles are from the genera Thermococcus and Pyrococcus, which belong to the order Thermococcales (4). These are ecologically important hyperthermophilic archaea for understanding the physiology and metabolic activity of microbial consortia within marine hotwater ecosystems. Members of the order Thermococcales are anaerobic heterotrophs that utilize various complex substrates with elemental sulfur (S 0 ) or protons as electron acceptors (4 -6). Unlike other Thermococcales, Thermococcus strain AM4 (7) and Thermococcus onnurineus NA1 (8) are capable of lithotrophic carbon monoxide-dependent hydrogenogenic growth. These Thermococcus strains use CO as a carbon and energy source by converting it into carbon dioxide (CO 2 ). In addition, several hyperthermophilic archaea of the genus Thermococcus can grow with formate as an electron donor, producing hydrogen gas (9). T. onnurineus NA1 is a sulfur-reducing hyperthermophilic archaeon isolated from a deep sea hydrothermal vent area in the Eastern Manus Basin of Papua New Guinea (10). It is one of the more metabolically versatile hyperthermophiles in that it...