Photoinduced water oxidation at the O 2 -evolving complex (OEC) of photosystem II (PSII) is a complex process involving a tetramanganesecalcium cluster that is surrounded by a hydrogenbonded network of water molecules, chloride ions, and amino-acid residues. Although the structure of the OEC has remained conserved over eons of evolution, significant differences in the chloride-binding characteristics exist between cyanobacteria and higher plants. An analysis of amino-acid residues in and around the OEC has identified residue 87 in the D1 subunit as the only significant difference between PSII in cyanobacteria and higher plants. We substituted the D1-N87 residue in the cyanobacterium Synechocystis sp. PCC 6803 (wild-type) with alanine, present in higher plants, or with aspartic acid. We studied PSII core complexes purified from D1-N87A and D1-N87D variant strains to probe the function of the D1-N87 residue in the water-oxidation mechanism. EPR spectra of the S 2 state and flash-induced FTIR spectra of both D1-N87A and D1-N87D PSII core complexes exhibited characteristics similar to those of wildtype Synechocystis PSII core complexes. However, flash-induced O 2 -evolution studies revealed a decreased cycling efficiency of the D1-N87D variant, whereas the cycling efficiency of the D1-N87A PSII variant was similar to that of wild-type PSII. Steady-state O 2 -evolution activity assays revealed that substitution of the D1-87 residue with alanine perturbs the chloridebinding site in the proton-exit channel. These findings provide new insight into the role of the D1-N87 site in the water-oxidation mechanism and explain the difference in the chloride-binding properties of cyanobacterial and higher-plant PSII.Photosystem II (PSII) is a 700 kDa pigmentprotein complex responsible for water oxidation in photoautotrophic organisms. The site of water oxidation, known as the oxygen-evolving complex (OEC), consists of a µ-oxo-bridged tetramanganese-calcium cluster ligated by a number of amino-acid residues and water molecules (1). The OEC is surrounded by a network of hydrogen-bonded amino-acid residues and water molecules that, along with Cl -ions, play a pivotal role in water oxidation (2,3). This process is initiated by photoinduced charge separation via a chlorophyll molecule called P 680 . The P 680 ⦁ + species thus formed is reduced by oxidation of the tetramanganese cluster, thereby building up oxidizing equivalents that are used for water oxidation (4). The process of water oxidation has been shown to proceed via a fourflash cycle called the Kok cycle with the intermediates formed at each step being referred to as S i states (i = 0 -4) (5). has remained elusive so far while the remaining S states have been studied using many experimental methods, especially electron paramagnetic resonance (EPR), Fourier transform infrared (FTIR), and extended X-ray absorption fine structure (EXAFS) spectroscopy. Information about the S 0 -S 3 states provides valuable insights about water oxidation.Due to the ease of generation an...