THE MANGANESE SITE OF THE PHOTOSYNTHETIC OXYGEN-EVOLVING COMPLEX PROBED BY EPR SPECTROSCOPY OF ORIENTED PHOTOSYSTEM-II MEMBRANES - THE G = 4 AND G = 2 MULTILINE SIGNALS

The g = 4 and g = 2 multiline EPR signals arising from the Mn cluster of the photosynthetic oxygen-evolving complex (OEC) in the S2 state were studied in preparations of oriented photosystem Il (PSII) membranes. The ammonia-modified forms of these two signals were also examined. The g = 4 signal obtained in oriented PSII membranes treated with NH4Cl at pH 7.5 displays at least 16 partially resolved Mn hyperfine transitions with a regular spacing of 36 G [Kim, D. H., Britt, R. D., Klein, M. P., & Sauer, K. (1990) J. Am. Chem. Soc. 112, 9389-9391]. The observation of this g = 4 "multiline signal" provides strong spectral evidence for a tetranuclear Mn origin for the g = 4 signal and is strongly suggestive of a model in which different spin state configurations of a single exchange-coupled Mn cluster give rise to the g = 4 and g = 2 multiline signals. A simulation shows the observed spectrum to be consistent with an S = 3/2 or S = 5/2 state of a tetranuclear Mn complex. The resolution of hyperfine structure on the NH3-modified g = 4 signal is strongly dependent on sample orientation, with no resolved hyperfine structure when the membrane normal is oriented perpendicular to the applied magnetic field. The dramatic NH3-induced changes in the g = 4 signal resolved in the spectra of oriented samples are suggestive that NH3 binding at the Cl- site of the OEC may represent direct coordination of NH3 to the Mn cluster. Orientation dependence data on the g = 2 multiline signal show that the hyperfine transitions in the wings of the signal are anisotropic. These peaks remain unresolved in the powder spectrum of the g = 2 multiline signal. The g tensor for the g = 2 multiline signal may be more anisotropic than previously thought.