Most of the dioxygen on earth is generated by the oxidation of water by photosystem II (PS II) using light from the sun. This lightdriven, four-photon reaction is catalyzed by the Mn 4 CaO 5 cluster located at the lumenal side of PS II. Various X-ray studies have been carried out at cryogenic temperatures to understand the intermediate steps involved in the water oxidation mechanism. However, the necessity for collecting data at room temperature, especially for studying the transient steps during the O-O bond formation, requires the development of new methodologies. In this paper we report room temperature X-ray diffraction data of PS II microcrystals obtained using ultrashort (<50 fs) 9 keV X-ray pulses from a hard X-ray free electron laser, namely the Linac Coherent Light Source. The results presented here demonstrate that the "probe before destroy" approach using an X-ray free electron laser works even for the highly-sensitive Mn 4 CaO 5 cluster in PS II at room temperature. We show that these data are comparable to those obtained in synchrotron radiation studies as seen by the similarities in the overall structure of the helices, the protein subunits and the location of the various cofactors. This work is, therefore, an important step toward future studies for resolving the structure of the Mn 4 CaO 5 cluster without any damage at room temperature, and of the reaction intermediates of PS II during O-O bond formation.manganese | oxygen-evolving complex P hotosystem II (PS II) is the only known biological system that has the unique capability of utilizing visible light for the oxidation of water into molecular oxygen (reaction 1) (1-4).PS II is a large protein complex embedded in the thylakoid membranes of cyanobacteria, algae, and plants (5). It is composed of at least 20 protein subunits and about 100 cofactor molecules, including the antenna and reaction center chlorophylls (Chl), pheophytins, cytochromes, carotenoids, quinones, lipids, and the Mn 4 CaO 5 cluster. Light absorption and excitation of the P 680 reaction center of PS II leads to charge separation across the thylakoid membrane, resulting in the formation of the positively charged Chl-based radical cation P 680 •þ and the negatively charged quinone radical anion Q B•− . P 680 •þ oxidizes the Mn 4 CaO 5 cluster of the oxygen-evolving complex (OEC) via a tyrosine residue, Y Z . The Mn 4 CaO 5 cluster is thus driven successively through a five-step catalytic cycle (with the intermediate S i states, i ¼ 0 to 4), coupling the isoenergetic one-electron photochemistry occurring at the PS II reaction center with the four-electron redox chemistry of water at the OEC. Many recent studies have shown that the oxidation or electron transfer processes are tightly coupled to proton-transfer reactions (6, 7). Although the S 0 through S 3 states are stable over a timescale of seconds, the S 4 state is highly reactive and has not yet been experimentally characterized in a conclusive manner (3,(8)(9)(10)(11). It is almost generally agreed that O-O bond formation oc...