The role of Cl − in photosynthetic O 2 evolution has been investigated by measurement of the steady-state O 2 rate and EPR of the electron donors responsible for the S 2 multiline signal and Signal II s upon Cl − depletion and substitution in Photosystem II membranes. Cl − removal has three effects upon the donor side of Photosystem II. (1) It abolishes O 2 evolution reversibly, while decreasing the yield of the S 2 multiline signal indicative of the manganese site of the O 2-evolving complex in the S 2 oxidation state. This decrease is brought about by (2) the reversible disconnection of the manganese complex from the reaction center; and by (3) deactivation of S 1 centers having reduced primary acceptor Q A to form S 0 centers having a reduced Signal II s species. Reactivation of O 2 evolution by anions confirms earlier work showing a requirement for a univalent anion of optimum charge density. The observed order of reactivation is Cl − > Br − ∼ NO 3 − ⪢ OH − ∼ F −. Reactivation of the S 2 multiline signal follows Cl − ∼ Br − > NO 3 − ∼ OH − > F −, in near correspondence with reactivation of O 2-evolution rates. Cl − titrations of F −-inhibited samples reveal two binding sites for Cl − which differ in binding affinity by 11-fold. The higher-affinity site reactivates the S 1 → S 2 light reaction, while the lower-affinity site reactivates the S 3 → S 0 light reaction. The high-affinity site is located within the O 2-evolving complex at an undetermined site, while the lower-affinity site functions in coupling the reaction center photochemistry to the O 2-evolving complex. The results are compared with Cl −/F − exchange equilibria for Mn 3+ in solution. A model for the lower S-state transitions is presented in which specific oxidation state assignments are made for some of the donors and acceptors of Photosystem II.