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Identifying the two substrate water sites of nature’s water-splitting cofactor (Mn 4 CaO 5 cluster) provides important information toward resolving the mechanism of O-O bond formation in Photosystem II (PSII). To this end, we have performed parallel substrate water exchange experiments in the S 1 state of native Ca-PSII and biosynthetically substituted Sr-PSII employing Time-Resolved Membrane Inlet Mass Spectrometry (TR-MIMS) and a Time-Resolved 17 O-Electron-electron Double resonance detected NMR (TR- 17 O-EDNMR) approach. TR-MIMS resolves the kinetics for incorporation of the oxygen-isotope label into the substrate sites after addition of H 2 18 O to the medium, while the magnetic resonance technique allows, in principle, the characterization of all exchangeable oxygen ligands of the Mn 4 CaO 5 cofactor after mixing with H 2 17 O. This unique combination shows i) that the central oxygen bridge (O5) of Ca-PSII core complexes isolated from Thermosynechococcus vestitus has, within experimental conditions, the same rate of exchange as the slowly exchanging substrate water (W S ) in the TR-MIMS experiments and ii) that the exchange rates of O5 and W S are both enhanced by Ca 2+ →Sr 2+ substitution in a similar manner. In the context of previous TR-MIMS results, this shows that only O5 fulfills all criteria for being W S . This strongly restricts options for the mechanism of water oxidation.
Lichtenberg et al. (Mon,) studied this question.