Comparative properties of hydroquinone and hydroxylamine reduction of the Ca(2+)-stabilized O2-evolving complex of photosystem II: reductant-dependent Mn2+ formation and activity inhibition.

Calcium binding to photosystem II slows NH2OH inhibition of O2 evolution; Mn2+ is retained by the O2-evolving complex [Mei, R., & Yocum, C. F. (1991) Biochemistry 30, 7836-7842]. This Ca(2+)-induced stability has been further characterized using the large reductant hydroquinone. Salt-washed photosystem II membranes reduced by hydroquinone in the presence of Ca2+ retain 80% of steady-state O2 evolution activity and contain about 2 Mn2+/reaction center that can be detected at room temperature by electron paramagnetic resonance. This Mn2+ produces a weak enhancement of H2O proton spin-lattice relaxation rates, cannot be easily extracted by a chelator, and is reincorporated into the O2-evolving complex upon illumination. A comparison of the properties of Ca(2+)-supplemented photosystem II samples reduced by hydroquinone or NH2OH alone or in sequence reveals the presence of a subpopulation of manganese atoms at the active site of H2O oxidation that is not accessible to facile hydroquinone reduction. At least one of these manganese atoms can be readily reduced by NH2OH following a noninhibitory hydroquinone reduction step. Under these conditions, about 3 Mn2+/reaction center are lost and O2 evolution activity is irreversibly inhibited. We interpret the existence of distinct sites of reductant action on manganese as further evidence that the Ca(2+)-binding site in photosystem II participates in regulation of the organization of manganese-binding ligands and the overall structure of the O2-evolving complex.