Chemotrophic microorganisms gain energy for cellular functions by catalyzing oxidation-reduction (redox) reactions that are out of equilibrium. Calculations of the Gibbs energy (∆ ! ) can identify whether a reaction is thermodynamically favorable, and the accompanying energy yield at the temperature, pressure, and chemical composition in the system of interest. Based on carefully calculated values of ∆ ! , we predict a novel microbial metabolism-sulfur comproportionation (3H 2 S + SO 4 2-+ 2H + = 4S 0 + 4H 2 O).We show that at elevated concentrations of sulfide and sulfate in acidic environments over a broad temperature range, this putative metabolism can be exergonic (∆ ! <0), yielding ~30-50 kJ/mol. We suggest that this may be sufficient energy to support a chemolithotrophic metabolism currently missing in nature. Other versions of this metabolism, to thiosulfate (H 2 S + SO 4 2-= S 2 O 3 2-+ H 2 O) and to sulfite (H 2 S + 3SO 4 2-= 4SO 3 2-+ 2H + ), are only moderately exergonic or endergonic even at ideal geochemical conditions. Natural and impacted environments, including sulfidic karst systems, shallow-sea hydrothermal vents, sites of acid mine drainage, and acid-sulfate crater lakes, may be ideal hunting grounds for finding microbial sulfur comproportionators.