The iron–quinone complex in
photosystem II (PSII) consists
of the two plastoquinone electron acceptors, QA and QB, and a non-heme iron connecting them. It has been suggested
that nearby histidine residues play important roles in the electron
and proton transfer reactions of the iron–quinone complex in
PSII. In this study, we investigated the protonation/deprotonation
reaction of D1-H215, which bridges the non-heme iron and QB, using attenuated total reflection Fourier transform infrared (ATR-FTIR)
spectroscopy. Flash-induced Fe2+/Fe3+ ATR-FTIR
difference spectra were measured with PSII membranes in the pH range
of 5.0–7.5. In the CN stretching region of histidine, the intensity
of a negative peak at 1094 cm–1, which was assigned
to the deprotonated anion form of D1-H215, increased as the pH increased.
Singular-value decomposition analysis provided a component due to
deprotonation of D1-H215 with a pK
a of
∼5.5 in the Fe3+ state, whereas no component of
histidine deprotonation was resolved in the Fe2+ state.
This observation supports the previous proposal that D1-H215 is responsible
for the proton release upon Fe2+ oxidation [Berthomieu,
C., and Hienerwadel, R. (2001) Biochemistry 40, 4044–4052].
The pH dependence of the 13C isotope-edited bands of the
bicarbonate ligand to the non-heme iron further showed that deprotonation
of bicarbonate to carbonate does not take place at pH <8 in the
Fe2+ or Fe3+ state. These results suggest that
the putative mechanism of proton transfer to QBH– through D1-H215 and bicarbonate around Fe2+ functions
throughout the physiological pH range.