Abstract

Changes in the chemical structure of alpha-carboxylate of the D1 C-terminal Ala-344 during S-state cycling of photosynthetic oxygen-evolving complex were selectively measured using light-induced Fourier transform infrared (FTIR) difference spectroscopy in combination with specific [(13)C]alanine labeling and site-directed mutagenesis in photosystem II core particles from Synechocystis sp. PCC 6803. Several bands for carboxylate symmetric stretching modes in an S(2)/S(1) FTIR difference spectrum were affected by selective (13)C labeling of the alpha-carboxylate of Ala with l-[1-(13)C]alanine, whereas most of the isotopic effects failed to be induced in a site-directed mutant in which Ala-344 was replaced with Gly. Labeling of the alpha-methyl of Ala with l-[3-(13)C]alanine had much smaller effects on the spectrum to induce isotopic bands due to a symmetric CH(3) deformation coupled with the alpha-carboxylate. The isotopic bands for the alpha-carboxylate of Ala-344 showed characteristic changes during S-state cycling. The bands appeared prominently upon the S(1)-to-S(2) transition and to a lesser extent upon the S(2)-to-S(3) transition but reappeared at slightly upshifted frequencies with the opposite sign upon the S(3)-to-S(0) transition. No obvious isotopic band appeared upon the S(0)-to-S(1) transition. These results indicate that the alpha-carboxylate of C-terminal Ala-344 is structurally associated with a manganese ion that becomes oxidized upon the S(1)-to-S(2) transition and reduced reversely upon the S(3)-to-S(0) transition but is not associated with manganese ion(s) oxidized during the S(0)-to-S(1) (and S(2)-to-S(3)) transition(s). Consistently, l-[1-(13)C]alanine labeling also induced spectral changes in the low frequency (670-350 cm(-1)) S(2)/S(1) FTIR difference spectrum.

Highlights

  • Photosynthetic water oxidation takes place in an oxygenevolving complex (OEC)1 in which the catalytic metal cluster located on the lumenal side of the D1 protein is composed of four manganese ions and one Ca2ϩ ion

  • Mid-frequency Fourier transform infrared (FTIR) difference spectroscopy has been applied to studies on oxygen evolution for elucidating S-state-dependent changes in protein backbone and amino acid side groups, which structurally associate with the manganese/Ca2ϩ cluster in a direct or indirect manner [21,22,23,24,25]

  • Extended x-ray absorption fine structure measurements indicate that the core structure of the manganese/ Ca2ϩ cluster remains almost same during the S1-to-S2 transition but changes considerably during the S2-to-S3 transition [28]

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Summary

Introduction

Photosynthetic water oxidation takes place in an oxygenevolving complex (OEC)1 in which the catalytic metal cluster located on the lumenal side of the D1 protein is composed of four manganese ions and one Ca2ϩ ion. Changes in the chemical structure of ␣-carboxylate of the D1 C-terminal Ala-344 during S-state cycling of photosynthetic oxygen-evolving complex were selectively measured using light-induced Fourier transform infrared (FTIR) difference spectroscopy in combination with specific [13C]alanine labeling and site-directed mutagenesis in photosystem II core particles from Synechocystis sp.

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