4.4 Article

FTIR detection of water reactions during the flash-induced S-state cycle of the photosynthetic water-oxidizing complex

Journal

BIOCHEMISTRY
Volume 41, Issue 52, Pages 15706-15712

Publisher

AMER CHEMICAL SOC
DOI: 10.1021/bi020603i

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Photosynthetic water oxidation is performed via the light-driven S-state cycle in the water-oxidizing complex (WOC) of photosystem II (PS II). To understand its molecular mechanism, monitoring the reaction of substrate water in each S-state transition is essential. We have for the first time detected the reactions of water molecules in WOC throughout the S-state cycle by observing the OH vibrations of water using flash-induced Fourier transform infrared (FTIR) difference spectroscopy. Moderately hydrated (or deuterated) PS II core films from Synechococcus elongatus were used to obtain the FTIR difference spectra upon the first, second, third, and fourth flash illumination, representing the structural changes in the S-1 --> S-2, S-2 --> S-3, S-3 --> S-0, and S-0 --> S-1 transitions, respectively. In the weakly H-bonded OH region, bands appeared at 3617/3588 cm(-1) as a differential signal in the first-flash spectrum and at 3634, 3621, and 3612 cm(-1) with negative intensities in the second-, third-, and fourth-flash spectra, respectively. These bands shifted down by similar to940 cm(-1) upon deuteration and by similar to10 cm(-1) upon (HO)-O-18 substitution, indicating that they arise from the OH stretches of water including the substrate and its intermediates. Stronuly D-bonded OD bands of water were also identified as broad features in the range of 2600-2200 cm(-1) by taking the double difference between the spectra of (D2O)-O-16- and (D2O)-O-18-deuterated films. In addition, broad continuum features that probably arise from the large proton polarizability of H-bonds were observed around 3000, 2700, 2550, and 2600 cm(-1) in the first-, second-, third-, and fourth-flash spectra, respectively, of the hydrated PS II film, revealing changes in the H-bond network of the protein. The negative OH intensities upon the second to fourth flashes might be related to proton release from substrate water. The results presented here showed that FTIR detection of water OH(D) bands can be a powerful method for investigating the mechanism of photosynthetic water oxidation.

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