Complexes of trivalent oxygenated phosphorus compounds with cytochrome P-450 and cytochrome P-420: the origin of double Soret spectra.
Trivalent oxygenated phosphorus ligands include alkyl and aryl phosphites, (RO)3P, phosphonites, (RO)2PR, and phosphinites, ROPR2. All such compounds tested, with the exception of triphenyl phosphite, interact with ferrous cytochrome P-450 and its denatured form, cytochrome P-420, to produce complexes having two peaks in the Soret region of their optical difference spectra. Careful evaluation of these spectra indicate that they arise for different reasons for each of the two cytochromes. Clear evidence shows that cytochrome P-450 is not denatured by these ligands. The high affinity of these ligands for heme iron is indicated by small Ks values. The experimental results are used to substantiate a theory of the origin of microsomal double Soret spectra and the nature of the environments available for microsomal cytochromes P-450 and P-420.
Complexes of trivalent oxygenated phosphorus compounds with cytochrome P-450 and cytochrome P-420: the origin of double Soret spectra. Trivalent oxygenated phosphorus ligands include alkyl and aryl phosphites, (RO)3P, phosphonites, (RO)2PR, and phosphinites, ROPR2. All such compounds tested, with the exception of triphenyl phosphite, interact with ferrous cytochrome P-450 and its denatured form, cytochrome P-420, to produce complexes having two peaks in the Soret region of their optical difference spectra. Careful evaluation of these spectra indicate that they arise for different reasons for each of the two cytochromes. Clear evidence shows that cytochrome P-450 is not denatured by these ligands. The high affinity of these ligands for heme iron is indicated by small Ks values. The experimental results are used to substantiate a theory of the origin of microsomal double Soret spectra and the nature of the environments available for microsomal cytochromes P-450 and P-420.