Another chemolithotrophic metabolism missing in nature: sulfur comproportionation

Chemotrophic microorganisms gain energy for cellular functions by catalyzing oxidation–reduction (redox) reactions that are out of equilibrium. Calculations of the Gibbs energy (ΔG(r)) can identify whether a reaction is thermodynamically favourable and quantify the accompanying energy yield at the temperature, pressure and chemical composition in the system of interest. Based on carefully calculated values of ΔG(r), we predict a novel microbial metabolism – sulfur comproportionation (3H(2)S + [Formula: see text] + 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 (ΔG(r)<0), yielding ~30–50 kJ mol(−1). We suggest that this may be sufficient energy to support a chemolithotrophic metabolism currently missing from the literature. Other versions of this metabolism, comproportionation to thiosulfate (H(2)S + [Formula: see text] ⇌ [Formula: see text] + H(2)O) and to sulfite (H(2)S + 3 [Formula: see text] ⇌ 4 [Formula: see text] + 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.