Bromide does not bind to the Mn4Ca complex in its S1 state in Cl(-)-depleted and Br(-)-reconstituted oxygen-evolving photosystem II: evidence from X-ray absorption spectroscopy at the Br K-edge.

Chloride is an important cofactor in photosynthetic water oxidation. It can be replaced by bromide with retention of the oxygen-evolving activity of photosystem II (PSII). Binding of bromide to the Mn(4)Ca complex of PSII in its dark-stable S(1) state was studied by X-ray absorption spectroscopy (XAS) at the Br K-edge in Cl(-)-depleted and Br(-)-substituted PSII membrane particles from spinach. The XAS spectra exclude the presence of metal ions in the first and second coordination spheres of Br(-). EXAFS analysis provided tentative evidence of at least one metal ion, which may be manganese or calcium, at a distance of approximately 5 A to Br(-). The native Cl(-) ion may bind at a similar distance. Accordingly, water oxidation may not require binding of a halide directly to the metal ions of the Mn complex in its S(1) state.

Conformational regulation of charge recombination reactions in a photosynthetic bacterial reaction center.

In bright light the photosynthetic reaction center (RC) of Rhodobacter sphaeroides stabilizes the P(+)(870).Q(-)(A) charge-separated state and thereby minimizes the potentially harmful effects of light saturation. Using X-ray diffraction we report a conformational change that occurs within the cytoplasmic domain of this RC in response to prolonged illumination with bright light. Our observations suggest a novel structural mechanism for the regulation of electron transfer reactions in photosynthesis.

Spectroscopic characterization of a semi-stable, charge-separated state in Cu(2+)-substituted reaction centers from Rhodobacter sphaeroides.

In reaction centers from Rhodobacter sphaeroides exposed to continuous illumination in the presence of an inhibitor of the Q(A)(-) to Q(B) electron transfer, a semi-stable, charge-separated state was formed with halftimes of formation and decay of several minutes. When the non-heme iron was replaced by Cu(2+), the decay of the semi-stable, charge-separated state became much slower than in centers with bound Fe(2+) with about the same rate constant for formation. In Cu(2+)-substituted reaction centers, the semi-stable state was associated with an EPR signal, significantly different from that observed after chemical reduction of the acceptor-side quinone or after illumination at low temperature, but similar to that of an isolated Cu(2+) in the absence of magnetic interaction. The EPR results, obtained with Cu(2+)-substituted reaction centers, suggest that the slow kinetics of formation and decay of the charge-separated, semi-stable state is associated with a structural rearrangement of the acceptor side and the immediate environment of the metal-binding site.

Lipidic cubic phase crystal structure of the photosynthetic reaction centre from Rhodobacter sphaeroides at 2.35A resolution.

Well-ordered crystals of the bacterial photosynthetic reaction centre from Rhodobacter sphaeroides were grown from a lipidic cubic phase. Here, we report the type I crystal packing that results from this crystallisation medium, for which 3D crystals grow as stacked 2D crystals, and the reaction centre X-ray structure is refined to 2.35A resolution. In this crystal form, the location of the membrane bilayer could be assigned with confidence. A cardiolipin-binding site is found at the protein-protein interface within the membrane-spanning region, shedding light on the formation of crystal contacts within the membrane. A chloride-binding site was identified in the membrane-spanning region, which suggests a putative site for interaction with the light-harvesting complex I, the cytochrome bc(1) complex or PufX. Comparisons with the X-ray structures of this reaction centre deriving from detergent-based crystals are drawn, indicating that a slight compression occurs in this lipid-rich environment.

The function of the chloride ion in photosynthetic oxygen evolution.

The involvement of Cl(-) and several other monovalent anions in photosynthetic oxygen evolution was studied using photosystem II membranes depleted of Cl(-) by dialysis. The results of these studies differ significantly from results obtained using other depletion methods. Binding studies with glycerol as a cryoprotectant confirm our previous observations with sucrose of two interconvertible binding states of photosystem II with similar activities and with slow or fast exchange, respectively, of the bound ion. With glycerol, Cl(-) depletion decreased the oxygen evolution rate to 55% of that with Cl(-) present without decreasing the quantum efficiency of the reaction, supporting our previous conclusion that oxygen evolution can proceed at high rates in the absence of Cl(-). Further, after Cl(-) depletion the S(2) state multiline signal displayed the same periodic appearance with the same signal yield after consecutive laser flashes as with Cl(-) present. Br(-), I(-), and NO(3)(-), although with different capacities to reactivate oxygen evolution, also showed two binding modes. I(-) inhibited when bound in the low-affinity, fast-exchange mode but activated in the high-affinity mode. A comparison of the EPR properties of the S(2) state with these anions suggests that the nature of the ion or the binding mode only has a minor influence on the environment of the manganese. In contrast, F(-) completely inhibited oxygen evolution by preventing the S(2) to S(3) transition and shifted the equilibrium between the g = 4.1 and multiline S(2) forms toward the former, which suggests a considerable perturbation of the manganese cluster. To explain these and earlier observations, we propose that the role of chloride in the water-splitting mechanism is to participate together with charged amino acid side chains in a proton-relay network, which facilitates proton transfer from the manganese cluster to the medium. The structural requirements likely to be involved may explain the sensitivity of oxygen evolution to Cl(-) depletion or other perturbations.

Characterization of a semi-stable, charge-separated state in reaction centers from Rhodobacter sphaeroides.

In reaction centers from Rhodobacter sphaeroides, subjected to continuous illumination in the presence of an inhibitor of the Q(A) to Q(B) electron transfer, the oxidation of P870 consisted of several kinetic phases with a fast initial reaction followed by very slow accumulation of P870(+) with a halftime of several minutes. When the light was turned off, a phase of fast charge recombination was followed by an equally slow reduction of P870(+). In reaction centers depleted of Q(B), where forward electron transfer from Q(A) is also prevented, the slow reactions were also observed but with different kinetic properties. The kinetic traces of accumulation and decay of P870(+) could be fitted to a simple three-state model where the initial, fast charge separation is followed by a slow reversible conversion to a long-lived, charge-stabilized state. Spectroscopic examination of the charge-separated, semi-stable state, using optical absorbance and EPR spectroscopy, suggests that the unpaired electron on the acceptor side is located in an environment significantly different from normal. The activation parameters and enthalpy and entropy changes, determined from the temperature dependence of the slow conversion reaction, suggest that this might be coupled to changes in the protein structure of the reaction centers, supporting the spectroscopic results. One model that is consistent with the present observations is that reaction centers, after the primary charge separation, undergo a slow, light-induced change in conformation affecting the acceptor side.