STOICHIOMETRY OF THE REDOX CHANGES OF MANGANESE DURING THE PHOTOSYNTHETIC WATER OXIDATION CYCLE

Abstract— The UV absorbance change associated with the oxygen-evolution cycle is investigated as to its correlation with the successive redox (S-) states of the system. This change is probably due to a manganese oxidation within a multinuclear Mn-cluster. The stoichiometry of its formation and destruction during the S-cycle has been a matter of controversy: (0,1,0,-1) according to velthuys, B. R. (1981) in Photosynthesis II , (Edited by G. Akoyunoglou), pp. 75–85. Balaban International Science Services, Philadelphia, or (1, 1, 1, -3) according to Dekker, J. P., Van Gorkom, H. J., Wensink, J. and Ouwehand, L. (1984) Biochim. Biophys. Acta 767, 1–9. We show that the data obtained in flash-series experiments on dark-adapted material may be fitted as satisfactorily by both models. More discriminating tests were devised, varying parameters such as the double-hits probability or the initial distribution of the S-states. These experiments clearly indicate that no (or little) absorbance change occurs both upon S₀→S₁ and S₂→S₃ transitions. This suggests that the correct stoichiometry is (0,l,0,-1). The possibility of a non-integer stoichiometry may also be considered.