Abstract

The stoichiometry of vectorial H+ ejection, coupled to ferrocytochrome c oxidation by a three-subunit bacterial cytochrome c oxidase (EC 1.9.3.1) from the thermophilic bacterium PS3, was measured. Three methods of measuring the H+/e- ratio were applied to proteoliposomes containing a relatively small amount of PS3 cytochrome oxidase, which showed a relatively low oxidation rate and a very low H+ leakage, as follows: (a) simultaneous measurements of H+ ejection and cytochrome c oxidation upon addition of a yeast ferrocytochrome c pulse, which enable us to calculate the H+/e- ratio as H+ ejected per cytochrome c oxidized; (b) computer simulations to find out the fit for the pH meter trace by changing the H+/e- ratio and the velocity constant of leakage; and (c) two successive measurements of initial rates of H+ movement in the absence and presence of carbonyl cyanide p-trifluoromethoxyphenylhydrazone. The H+/e- ratios obtained were 1.39, the 10-s value after ferrocytochrome c addition in (a), 1.35 in (b), and 1.33 in (c). This high H+/e- stoichiometry observed, exceeding 1 and as high as 1.4, is discussed with respect to the controversy of the H+/e- ratio at the cytochrome oxidase site.

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