One-electron reactions in biochemical systems as studied by pulse radiolysis. VI. Stages in the reduction of ferricytochrome c

When ferricytochrome c at pH about 9 is reduced by hydrated electrons and/or CO₂^?, it gives rise to an unstable form of ferrocytochrome c whose absorption spectrum, particularly in the Soret region, differs from that of normal ferrocytochrome c. This form changes intramolecularly (life-time about 0.1 s at ambient temperature) to yield normal ferrocytochrome c, and by 0.5 s the change in absorption spectrum in the range 225–600 nm produced by e^?_aq and/or CO₂^? is identical to the final change produced by reduction with an equivalent amount of sodium dithionite. This shows that both e^?_aq and CO^?₂ reduce cytochrome c with practically 100% efficiency. In the range 600–800 nm the spectrum of the unstable form is the same as that of normal ferrocytochrome c, both having small absorptions at 695 nm as compared with ferricytochrome c. As the unstable form disappears however a further loss of absorption at 695 nm occurs. This is taken to imply that the unstable form decays to a second unstable form which then rapidly donates an electron to the unchanged neutral form of ferricytochrome c, so reducing absorption in the 695 nm band. Subsequent to this process the absorption in the 695 nm band increases over a period of minutes owing to re-equilibration between the neutral and alkaline formes of ferricytochrome c. Between pH 7 and 10 the effect of pH on the absorption changes is consistent with the hypothesis of a second unstable form of ferrocytochrome c. Additional phenomena arise in more alkaline solutions. The rates of the various unimolecular processes are thought to be determined by the rates of change of conformation of the protein parts of the molecule following the change in oxidation state.