The 18 O exchange rates for the substrate water bound in the S 3 state were determined in different photosystem II sample types using time-resolved mass spectrometry. The samples included thylakoid membranes, saltwashed Triton X-100-prepared membrane fragments, and purified core complexes from spinach and cyanobacteria. For each sample type, two kinetically distinct isotopic exchange rates could be resolved, indicating that the biphasic exchange behavior for the substrate water is inherent to the O 2 -evolving catalytic site in the S 3 state. However, the fast phase of exchange became somewhat slower (by a factor of ϳ2) in NaClwashed membrane fragments and core complexes from spinach in which the 16-and 23-kDa extrinsic proteins have been removed, compared with the corresponding rate for the intact samples. For CaCl 2 -washed membrane fragments in which the 33-kDa manganese stabilizing protein (MSP) has also been removed, the fast phase of exchange slowed down even further (by a factor of ϳ3). Interestingly, the slow phase of exchange was little affected in the samples from spinach. For core complexes prepared from Synechocystis PCC 6803 and Synechococcus elongatus, the fast and slow exchange rates were variously affected. Nevertheless, within the experimental error, nearly the same exchange rates were measured for thylakoid samples made from wild type and an MSP-lacking mutant of Synechocystis PCC 6803. This result could indicate that the MSP has a slightly different function in eukaryotic organisms compared with prokaryotic organisms. In all samples, however, the differences in the exchange rates are relatively small. Such small differences are unlikely to arise from major changes in the metal-ligand structure at the catalytic site. Rather, the observed differences may reflect subtle long range effects in which the exchange reaction coordinates become slightly altered. We discuss the results in terms of solvent penetration into photosystem II and the regional dielectric around the catalytic site.The oxidation of water during photosynthesis is catalyzed by the membrane-bound pigment protein complex photosystem II (PSII).1 In the net reaction, four electrons, four protons, and one molecule of O 2 are liberated from the splitting of two water molecules. A key insight into the reaction mechanism was the observation that the O 2 produced in brief, saturating light flashes follows a periodicity of four (1). The period four phenomenon is now universally interpreted in terms of the S-state model, in which the catalytic site cycles through five intermediary S n states (n ϭ 0 -4) (2). Beginning in S 0 and traversing to S 4 , each S n state is driven forward by a single quantum event at the PSII reaction center. Upon reaching the S 4 state (which may be equivalent to S 3 Y Z ⅐ ) O 2 is released, S 0 is regenerated, and the cycle begins anew. The catalytic site for water oxidation involves an inorganic metal cluster consisting of four manganese ions, one Ca 2ϩ ion, possibly one Cl Ϫ ion, and the redox-active Tyr-161 resid...