The production of O/sub 2/ from water requires the collaboration of four oxidizing equivalents. When dark-adapted O/sub 2/ evolving photosynthetic material is illuminated by a sequence of short (less than 2 ..mu..sec) saturating flashes, the amount of O/sub 2/ evolved per flash oscillates with a period of four. This indicates that a charge-collector, operating with its own reaction center, successively collects and stores four oxidizing equivalents, which are used in a concerted oxidation of two water molecules. Luminescence, fluorescence, and pH changes also reflect this cycle of four. The O/sub 2/ precursor states are quite stable; under some conditions they can have a lifetime of several minutes. The O/sub 2/-yielding reactions and reactions associated with trap recovery are fast relative to the rate-limiting step of photosynthesis. The molecular identity of the charge-collector is unknown, but correlative evidence suggests that a manganese containing catalyst (approximately 4 Mn/charge collector) participates, possibly directly. Formation of the active Mn-containing catalyst occurs via a multi-quantum process occurring within the System II reaction center. The photoactivated catalyst, located on the inner face of the thylakoid membrane, remains permanently active and essentially inaccessible to chemicals other than analogs of H/sub 2/O (e.g., NH/sub 3/, NH/sub 2/OH). Thismore » O/sub 2/ evolving catalyst can be deactivated by a variety of treatments that do not alter the system II reaction center. Anions such as chloride seem to participate rather directly in the O/sub 2/ evolution process via unknown mechanism(s).« less