Manganese Oxyl Radical Intermediates and O−O Bond Formation in Photosynthetic Oxygen Evolution and a Proposed Role for the Calcium Cofactor in Photosystem II

Abstract

Spin state considerations are proposed to sharply limit the possible O−O bond-forming steps in water oxidation by the oxygen evolving center of Photosystem II. A series of intermediates are proposed for the Kok S states on the basis of quantum chemical studies on simple model complexes; these are also consistent with the main biophysical data. Only one Mn atom in the active site cluster is thought to be redox-active and mediate O−O bond formation. A key concept is the formation of an unreactive Mn O oxo at the S 2 state, followed by its conversion to a reactive Mn−O• oxyl form at the S 3 level, with radical character on the oxyl oxygen, at which point O−O bond formation can occur by a coupling between the oxyl and an outer-sphere water molecule. An MnOOH intermediate at S 3 is proposed to lose a hydrogen atom to give O 2 . The role of the Ca cofactor is to bring about a 5- to 6-coordination change at S 2, necessary for formation of a reactive oxo in S 3 . The chloride cofactor is assigned the role of charge neutralization.