EPR evidence for the primary water oxidation step upon the S2 → S3 transition in the Joliot-Kok cycle of plant photosystem II

Photosynthetic water oxidation: towards a mechanism

This mini-review outlines the current theories on the mechanism of electron transfer from water to P680, the location and structure of the water oxidising complex and the role of the manganese cluster. We discuss how our data fit in with current theories and put forward our ideas on the location and mechanism of water oxidation.

Simulation of S2-state multiline EPR signal in oriented photosystem II membranes: structural implications for the manganese cluster in an oxygen-evolving complex

High-quality angular-dependent spectra of multiline electron paramagnetic resonance (EPR) signals from the S2-state Mn cluster in a photosynthetic oxygen-evolving complex (OEC) were obtained for partially oriented photosystem (PS) II membranes, and the magnetic structure of the Mn cluster has been studied by simulation analysis. The angular-dependent multiline spectra were simulated by taking into account the anisotropic properties of both hyperfine tensors of intrinsic Mn ions and g-tensor of the cluster in a tetranuclear model. The best-fit parameters for the simulation indicate that (a) the oxidation state of the S2-state Mn cluster is Mn(III, IV, IV, IV), (b) the electronic orbital configuration of the Mn(III) ion is (dpi)3[dz2(sigma))]1, (c) the effective g-tensor of the Mn cluster and the hyperfine tensor of the Mn(III) ion are axially symmetric, and their principal z-axes are nearly collinear each other, and (d) the z-axis of the dz2 orbital of the Mn(III) ion and the normal of the thylakoid membrane are at an angle of 50.1 +/- 1.8 degrees. The results are compatible with those of the oriented XAFS study [Mukerji, I., et al. (1994) Biochemistry 33, 9712-9721], and indicate that the O-O vector of the putative di-mu-oxo bridged Mn(III)-Mn(IV) dimer unit in the Mn cluster tilts by 43-56 degrees with respect to the normal of thylakoid membrane. A model of the arrangement of the di-mu-oxo bridged Mn(III)-Mn(IV) unit with respect to the thylakoid membrane is proposed.

EPR investigation of water oxidizing photosystem II: detection of new EPR signals at cryogenic temperatures

Experiments are described which allow the detection and characterization of new EPR signals in photosystem II (PSII). PSII has been extensively studied with the water oxidising complex (WOC) poised in the S1 and S2 states. Other stages in the cycle of water oxidation lack characteristic EPR signals for use as probes. In this study, experiments use multiple turnovers of PSII from an initial S1 state to allow new states of PSII to be studied. The first EPR signal detected, centered at g = 4.85 and termed the g = 5 signal, is suggested to be a new form of S2 probably formed by decay of S3 at cryogenic temperatures, but a novel form of oxidized non-heme iron cannot be fully excluded at present. The second signal is split around g = 2 and shows characteristics of signals formed by spin-spin interaction between two paramagnetic species. The split g = 2 signal is reversibly formed by illumination at <30 K of a sample containing the g = 5 signal. The g = 2 signal may be a form of the "S3" EPR signal previously only found in a variety of PSII preparations where oxygen evolution has been inhibited. Those "S3" signals are thought to arise from the interaction of an oxidized amino acid radical and the S2 state, i.e., S2X+. Illumination at higher temperatures or illumination at <30 K, followed by dark-adaptation at 77 K, removes the g = 5 signal and prevents subsequent detection of the g = 2 signal on illumination at <30 K. The most likely explanation of our data is that illumination at <30 K of centers containing the g = 5 species allows accumulation of an oxidized intermediate and that at higher temperatures electron transfer proceeds to re-form an EPR-silent S state equivalent to that initially trapped during sample preparation. Study of these signals should provide an important new insight into the WOC and PSII.

Oxygenic photosynthesis. Electron transfer in photosystem I and photosystem II

Photosystems I and II drive oxygenic photosynthesis. This requires biochemical systems with remarkable properties, allowing these membrane-bound pigment-protein complexes to oxidise water and produce NAD(P)H. The protein environment provides a scaffold in the membrane on which cofactors are placed at optimum distance and orientation, ensuring a rapid, efficient trapping and conversion of light energy. The polypeptide core also tunes the redox potentials of cofactors and provides for unidirectional progress of various reaction steps. The electron transfer pathways use a variety of inorganic and organic cofactors, including amino acids. This review sets out some of the current ideas and data on the cofactors and polypeptides of photosystems I and II.