Thermococcus onnurineus NA1 is known to grow by the anaerobic oxidation of formate to CO 2 and H 2 , a reaction that operates near thermodynamic equilibrium. Here we demonstrate that this reaction is coupled to ATP synthesis by a transmembrane ion current. Formate oxidation leads to H + translocation across the cytoplasmic membrane that then drives Na + translocation. The ion-translocating electron transfer system is rather simple, consisting of only a formate dehydrogenase module, a membrane-bound hydrogenase module, and a multisubunit Na + /H + antiporter module. The electrochemical Na + gradient established then drives ATP synthesis. These data give a mechanistic explanation for chemiosmotic energy conservation coupled to formate oxidation to CO 2 and H 2 . Because it is discussed that the membrane-bound hydrogenase with the Naantiporter module are ancestors of complex I of mitochondrial and bacterial electron transport these data also shed light on the evolution of ion transport in complex I-like electron transport chains.ormate is a common end product of bacterial fermentation and is liberated into the environment. It does not accumulate but is oxidized under oxic as well as anoxic conditions. Oxidation of formate to CO 2 and H 2 under anoxic conditions according tois an endergonic process under standard conditions at 25°C. Nevertheless, some anaerobic microbes can grow by this reaction. In anaerobic syntrophic formate oxidation the reaction is made thermodynamically possible by removal of the end product H 2 by a methanogenic or sulfate-reducing partner (1-4). For pure cultures, growth at the expense of Eq. 1 was considered impossible owing to the thermodynamic constraints (2, 3). However, recently we reported that several hyperthermophilic archaea belonging to the family Thermococcales, including Thermococcus onnurineus NA1, are able to grow by oxidation of formate to molecular hydrogen (5, 6). At 80°C, the optimum growth temperature for these hyperthermophiles, the reaction becomes slightly exergonic (ΔG 0 = −2.6 kJ/mol), according to the Van't Hoff equation (7). Measurements of pool sizes of products and educts of the reaction catalyzed by whole cells at 80°C revealed that the ΔG was more negative and growth occurred within a range of concentrations of products and educts that equals −20 to −8 kJ/mol (5), indicating that the reaction is potentially able to drive formation of an electrochemical ion gradient across the membrane.Molecular and genetic analyses revealed that the hydrogenase genes in the fdh2-mfh2-mnh2 gene cluster are essential for growth coupled to formate oxidization and hydrogen production (5, 8). Based on these findings a model was developed in which the formate dehydrogenase (Fdh2) module oxidizes formate; the hydrogenase (Mfh2) module transfers electrons to protons, thereby generating a proton gradient across the membrane that is then used by the Mnh2 module to produce a secondary sodium ion gradient that then drives ATP synthesis, catalyzed by a Na + -ATP synthase (2, 5). In this work...