Mechanism of O2 Activation by Cytochrome P450cam Studied by Isotope Effects and Transient State Kinetics

Abstract

The early steps in dioxygen activation by the monooxygenase cytochrome P450cam (CYP101) include binding of O2 to ferrous P450cam to yield the ferric-superoxo form (oxyP450cam) followed by an irreversible, long-range electron transfer from putidaredoxin to reduce the oxyP450cam. The steady state kinetic parameter kcat/Km(O2) has been studied by a variety of probes that indicate a small D2O solvent isotope effect (1.21 +/- 0.08), a very small solvent viscosogen effect, and a 16O/18O isotope effect of 1.0147 +/- 0.0007. This latter value, which can be compared with the 16O/18O equilibrium isotope effect of 1.0048 +/- 0.0003 measured for oxyP450cam formation, is attributed to a primarily rate-limiting outer-sphere electron transfer from the heme iron center as O2 that has prebound to protein approaches the active site cofactor. The electron transfer from putidaredoxin to oxyP450cam was investigated by rapid mixing at 25 degrees C to complement previous lower-temperature measurements. A rate of 390 +/- 23 s-1 (and a near-unity solvent isotope effect) supports the view that the long-range electron transfer from reduced putidaredoxin to oxyP450cam is rapid relative to dissociation of O2 from the enzyme. P450cam represents the first enzymatic reaction of O2 in which both equilibrium and kinetic 16O/18O isotope effects have been measured.