X-ray absorption spectroscopy has provided important insights into the structure and function of the Mn 4 Ca cluster in the oxygenevolving complex of Photosystem II (PS II). The range of manganese extended x-ray absorption fine structure data collected from PS II until now has been, however, limited by the presence of iron in PS II. Using a crystal spectrometer with high energy resolution to detect solely the manganese K␣ fluorescence, we are able to extend the extended x-ray absorption fine structure range beyond the onset of the iron absorption edge. This results in improvement in resolution of the manganese-backscatterer distances in PS II from 0.14 to 0.09 Å . The high resolution data obtained from oriented spinach PS II membranes in the S 1 state show that there are three di--oxo-bridged manganese-manganese distances of ϳ2.7 and ϳ2.8 Å in a 2:1 ratio and that these three manganese-manganese vectors are aligned at an average orientation of ϳ60°relative to the membrane normal. Furthermore, we are able to observe the separation of the Fourier peaks corresponding to the ϳ3.2 Å manganese-manganese and the ϳ3.4 Å manganese-calcium interactions in oriented PS II samples and determine their orientation relative to the membrane normal. The average of the manganese-calcium vectors at ϳ3.4 Å is aligned along the membrane normal, while the ϳ3.2 Å manganese-manganese vector is oriented near the membrane plane. A comparison of this structural information with the proposed Mn 4 Ca cluster models based on spectroscopic and diffraction data provides input for refining and selecting among these models.Photosynthesis by green plants, algae, and cyanobacteria provides essentially all of the dioxygen in the biosphere as a byproduct of the electron transfer processes utilizing water as the ultimate electron source:Water oxidation is a light-driven reaction that is catalyzed by an oxygen-evolving complex (OEC) 4 of Photosystem II (PS II) (1-4). The active site of the OEC is known to be a proteinbound complex containing four manganese and one calcium atom. This complex cycles through a series of five intermediate redox states that are referred to as S states (S 0 to S 4 ) (5). The S state transitions are driven by successive light-induced oneelectron oxidations of the PS II reaction center. In each step the complex accumulates oxidizing equivalents until dioxygen is released during the spontaneous return from S 4 to S 0 .Many of the proposed mechanisms of water oxidation depend critically on knowledge of the Mn 4 Ca cluster structure. To date, structural models of the OEC complex have been suggested based on EPR techniques (6 -9), x-ray absorption spectroscopy (XAS) (10 -14), x-ray diffraction (XRD) (15-17), and infrared spectroscopy (Fourier transform infrared) (18). The XRD studies (3.0 -3.8 Å resolution) have located the Mn 4 Ca cluster in the density map (16,17) and confirmed the presence of calcium in the OEC cluster, as had been shown previously by and by extended x-ray absorption fine structure (EXAFS) spectroscopy (22,23)...