Erman J E, Yonetani T
Biochim Biophys Acta. 1975 Jun 26;393(2):350-7. doi: 10.1016/0005-2795(75)90061-6.
The primatry compound formed in the reaction between H2O2 and cytochrome c peroxidase is oxidized two equivalents above the native enzyme. The two oxidized sites are thought to be an Fe(IV) and an amino acid radical. In the absence of oxidizable substrate, the Fe(IV) and radical sites decay by apparent first-order processes but at different rates. It is likely that the decay involves both intra- and intermolecular electron-transfer reactions. The reduction of the Fe(IV) site depends upon the pH with a minimum reduction rate of 2.9-10(-5)s(-1) at pH 6. At pH 4 and 6, the reduction of the Fe(IV) site is facilitated by prior oxidation of amino acid residues in the protein.