Photosynthetic water oxidation is catalyzed by the Mn 4 CaO 5 cluster of photosystem II. Recent studies implicate an oxo bridge atom, O5, of the Mn 4 CaO 5 cluster, as the "slowly exchanging" substrate water molecule. The D1-V185N mutant is in close vicinity of O5 and known to extend the lag phase and retard the O 2 release phase (slow phase) in this critical last S + 3 → S 0 transition of water oxidation. The pH dependence, hydrogen/deuterium (H/D) isotope effect, and temperature dependence on the O 2 release kinetics for this mutant were studied using time-resolved O 2 polarography, and comparisons were made with WT and two mutants of the putative proton gate D1-D61. Both kinetic phases in V185N are independent of pH and buffer concentration and have weaker H/D kinetic isotope effects. Each phase is characterized by a parallel or even lower activation enthalpy but a less favorable activation entropy than the WT. The results indicate new rate-determining steps for both phases. It is concluded that the lag does not represent inhibition of proton release but rather, slowing of a previously unrecognized kinetic phase involving a structural rearrangement or tautomerism of the S 3 + ground state as it approaches a configuration conducive to dioxygen formation. The parallel impacts on both the lag and O 2 formation phases suggest a common origin for the defects surmised to be perturbations of the H-bond network and the water cluster adjacent to O5.photosynthesis | water oxidation | oxygen release kinetics | photosystem II | activation energy O xygenic photosynthesis depends on the light-driven waterplastoquinone oxidoreductase, photosystem II (PSII), which catalyzes the complete oxidation of H 2 O molecules to O 2 . The electrons extracted from H 2 O oxidation are the reductant for autotrophic metabolism, and the liberated protons contribute to the transmembrane proton motive force powering ATP production (reviewed in refs. 1-4). The byproduct, O 2 , has transformed our Earth's atmosphere and makes heterotrophic life in the biosphere possible. A metal cluster, the Mn 4 CaO 5 , functions as the catalytic site of H 2 O oxidation and is buried in a protein domain of PSII referred to as the H 2 O oxidation complex (WOC). The primary photochemical electron donor of the reaction center (RC) complex is a dimeric chlorophyll moiety designated P 680 that is coordinated by the pseudosymmetrically arranged D1 and D2 polypeptides. Together, the D1/D2 heterodimer are responsible for the coordination of most of the photochemically active cofactors of the RC. Photoexcitation of P 680 initiates transmembrane charge separation with the activated electron moving to plastoquinone species, Q A and Q B , on the acceptor side of the RC. The resultant electron hole ðP +• 680 Þ functions as the powerful oxidant for the extraction of electrons from substrate H 2 O bound to the Mn 4 CaO 5 (Fig. 1A). However, the oxidation of the Mn 4 CaO 5 occurs through a redox active tyrosyl of the D1 protein, D1-Tyr161 (Y Z ), located between P 680 and the...