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.
过氧化氢(H₂O₂)与细胞色素c过氧化物酶反应形成的初级化合物比天然酶氧化态高出两个当量。这两个氧化位点被认为是一个四价铁(Fe(IV))和一个氨基酸自由基。在没有可氧化底物的情况下,Fe(IV)和自由基位点通过表观一级过程衰减,但速率不同。这种衰减可能涉及分子内和分子间的电子转移反应。Fe(IV)位点的还原取决于pH值,在pH 6时最低还原速率为2.9×10⁻⁵ s⁻¹。在pH 4和6时,蛋白质中氨基酸残基的预先氧化促进了Fe(IV)位点的还原。