A key question for the understanding of photosynthetic water oxidation is whether the four oxidizing equivalents necessary to oxidize water to dioxygen are accumulated on the four Mn ions of the oxygen-evolving complex (OEC), or whether some ligand-centered oxidations take place before the formation and release of dioxygen during the S₃ → [S₄] → S₀ transition. Progress in instrumentation and flash sample preparation allowed us to apply Mn Kβ X-ray emission spectroscopy (Kβ XES) to this problem for the first time. The Kβ XES results, in combination with Mn X-ray absorption near-edge structure (XANES) and electron paramagnetic resonance (EPR) data obtained from the same set of samples, show that the S₂ → S₃ transition, in contrast to the S₀ → S₁ and S₁ → S₂ transitions, does not involve a Mn-centered oxidation. On the basis of new structural data from the S₃-state, manganese μ-oxo bridge radical formation is proposed for the S₂ → S₃ transition, and three possible mechanisms for the O−O bond formation are presented.