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Proton Release Process during the S2‑to‑S3 Transition of Photosynthetic Water Oxidation As Revealed by the pH Dependence of Kinetics Monitored by Time-Resolved Infrared Spectroscopy
journal contribution
posted on 2019-10-09, 14:03 authored by Hiroshi Takemoto, Miwa Sugiura, Takumi NoguchiPhotosynthetic
water oxidation takes place at the Mn4CaO5 cluster
in photosystem II via a light-driven cycle
of intermediates called S states (S0–S4). Clarifying how electron and proton transfer reactions are coupled
with each other in the S2 → S3 transition,
which occurs just before O–O bond formation, is crucial for
understanding the water oxidation mechanism. Here, we investigated
the pH dependence of the kinetics of the S2 → S3 transition using time-resolved infrared (TRIR) spectroscopy
to identify the proton release phase in this transition. TRIR measurements
of YD-less PSII core complexes from the D2-Y160F mutant
of Thermosynechococcus elongatus showed that the
last phase in this transition (τ ∼ 350 μs at pH
6) was strongly dependent on pH, and its time constant at pH 5 was
larger than that at pH 8 by a factor of >3. In contrast, the earlier
phase with a time constant of ∼100 μs was virtually independent
of pH. These results strongly support the view that proton release
is a rate-limiting step of the proton-coupled electron transfer in
the last phase of the S2 → S3 transition.
This proton release enables electron transfer by removing an excessive
positive charge from the catalytic center and hence decreasing its
redox potential.