Orientation of calcium in the Mn4Ca cluster of the oxygen-evolving complex determined using polarized strontium EXAFS of photosystem II membranes

The oxygen-evolving complex of photosystem II (PS II) in green plants and algae contains a cluster of four Mn atoms in the active site, which catalyzes the photoinduced oxidation of water to dioxygen. Along with Mn, calcium and chloride ions are necessary cofactors for proper functioning of the complex. The current study using polarized Sr EXAFS on oriented Sr-reactivated samples shows that Fourier peak II, which fits best to Mn at 3.5 A rather than lighter atoms (C, N, O, or Cl), is dichroic, with a larger magnitude at 10 degrees (angle between the PS II membrane normal and the X-ray electric field vector) and a smaller magnitude at 80 degrees . Analysis of the dichroism of the Sr EXAFS yields a lower and upper limit of 0 degrees and 23 degrees for the average angle between the Sr-Mn vectors and the membrane normal and an isotropic coordination number (number of Mn neighbors to Sr) of 1 or 2 for these layered PS II samples. The results confirm the contention that Ca (Sr) is proximal to the Mn cluster and lead to refined working models of the heteronuclear Mn(4)Ca cluster of the oxygen-evolving complex in PS II.     

Kinetics of the oxygen-evolving complex in salt-washed photosystem II preparations

The kinetics of flash-induced electron transport were investigated in oxygen-evolving Photosystem II preparations, depleted of the 23 and 17 kDa polypeptides by washing with 2 M NaCl. After dark-adaptation and addition of the electron acceptor 2,5-dichloro-p-benzoquinone, in such preparations approx. 75% of the reaction centers still exhibited a period 4 oscillation in the absorbance changes of the oxygen-evolving complex at 350 nm. In comparison to the control preparations, three main effects of NaCl-washing could be observed: the half-time of the oxygen-evolving reaction was slowed down to about 5 ms, the misses and double hits parameters of the period 4 oscillation had changed, and the two-electron gating mechanism of the acceptor side could not be detected anymore. EPR-measurements on the oxidized secondary donor Z⁺ confirmed the slower kinetics of the oxygen-releasing reaction. These phenomena could not be restored by readdition of the released polypeptides nor by the addition of CaCl₂, and are ascribed to deleterious action of the highly concentrated NaCl. Otherwise, the functional coupling of Photosystem II and the oxygen-evolving complex was intact in the majority of the reaction centers. Repetitive flash measurements, however, revealed P⁺Q⁻ recombination and a slow Z⁺ decay in a considerable fraction of the centers. The flash-number dependency of the recombination indicated that this reaction only appeared after prolonged illumination, and disappeared again after the addition of 20 mM CaCl₂. These results are interpreted as a light-induced release of strongly bound Ca²⁺ in the salt-washed preparations, resulting in uncoupling of the oxygen-evolving system and the Photosystem II reaction center, which can be reversed by the addition of a relatively high concentration of Ca²⁺.     

Identification of a Mn-O-Mn cluster vibrational mode of the oxygen-evolving complex in photosystem II by low-frequency FTIR spectroscopy

We have developed conditions for recording the low-frequency S(2)/S(1) Fourier transform infrared difference spectrum of hydrated PSII samples. By exchanging PSII samples with buffered (18)O water, we found that a positive band at 606 cm(-)(1) in the S(2)/S(1) spectrum in (16)O water is clearly downshifted to 596 cm(-)(1) in (18)O water. By taking double-difference (S(2)/S(1) and (16)O minus (18)O) spectra, we assign the 606 cm(-)(1) mode to an S(2) mode and also identify a corresponding S(1) mode at about 625 cm(-)(1). In addition, by Sr and (44)Ca substitution experiments, we found that the 606 cm(-)(1) mode is upshifted to about 618 cm(-)(1) by Sr(2+) substitution but that this mode is not affected by substitution with the (44)Ca isotope. On the basis of these results and also on the basis of studies of Mn model compounds, we assign the 625 cm(-)(1) mode in the S(1) state and the 606 cm(-)(1) mode in the S(2) state to a Mn-O-Mn cluster vibration of the oxygen-evolving complex (OEC) in PSII. This structure may include additional bridge(s), which could be another oxo, carboxylato(s), or atoms derived from an amino acid side chain. Our results indicate that the bridged oxygen atom shown in this Mn-O-Mn cluster is exchangeable and accessible by water. The downshift in the Mn-O-Mn cluster vibration as manganese is oxidized during the S(1) --> S(2) transition is counterintuitive; we discuss possible origins of this behavior. Our results also indicate that Sr(2+) substitution in PSII causes a small structural perturbation that affects the bond strength of the Mn-O-Mn cluster in the PSII OEC. This suggests that Sr(2+), and by inference, Ca(2+), communicates with, but is not integral to, the manganese core.     

Digalactosyldiacylglycerol is required for stabilization of the oxygen-evolving complex in photosystem II

The galactolipid digalactosyldiacylglycerol (DGDG) is present in the thylakoid membranes of oxygenic photosynthetic organisms such as higher plants and cyanobacteria. Recent x-ray crystallographic analysis of protein-cofactor supercomplexes in thylakoid membranes revealed that DGDG molecules are present in the photosystem II (PSII) complex (four molecules per monomer), suggesting that DGDG molecules play important roles in folding and assembly of subunits in the PSII complex. However, the specific role of DGDG in PSII has not been fully clarified. In this study, we identified the dgdA gene (slr1508, a ycf82 homolog) of Synechocystis sp. PCC6803 that presumably encodes a DGDG synthase involved in the biosynthesis of DGDG by comparison of genomic sequence data. Disruption of the dgdA gene resulted in a mutant defective in DGDG synthesis. Despite the lack of DGDG, the mutant cells grew as rapidly as the wild-type cells, indicating that DGDG is not essential for growth in Synechocystis. However, we found that oxygen-evolving activity of PSII was significantly decreased in the mutant. Analyses of the PSII complex purified from the mutant cells indicated that the extrinsic proteins PsbU, PsbV, and PsbO, which stabilize the oxygen-evolving complex, were substantially dissociated from the PSII complex. In addition, we found that heat susceptibility but not dark-induced inactivation of oxygen-evolving activity was notably increased in the mutant cells in comparison to the wild-type cells, suggesting that the PsbU subunit is dissociated from the PSII complex even in vivo. These results demonstrate that DGDG plays important roles in PSII through the binding of extrinsic proteins required for stabilization of the oxygen-evolving complex.     

Altered structure of the Mn4Ca cluster in the oxygen-evolving complex of photosystem II by a histidine ligand mutation

The effect of replacing a histidine ligand on the properties of the oxygen-evolving complex (OEC) and the structure of the Mn₄Ca cluster in Photosystem II (PSII) is studied by x-ray absorption spectroscopy using PSII core complexes from the Synechocystis sp. PCC 6803 D1 polypeptide mutant H332E. In the x-ray crystallographic structures of PSII, D1-His³³² has been assigned as a direct ligand of a manganese ion, and the mutation of this histidine ligand to glutamate has been reported to prevent the advancement of the OEC beyond the S₂Yz^• intermediate state. The manganese K-edge (1s core electron to 4p) absorption spectrum of D1-H332E shifts to a lower energy compared with that of the native WT samples, suggesting that the electronic structure of the manganese cluster is affected by the presence of the additional negative charge on the OEC of the mutant. The extended x-ray absorption spectrum shows that the geometric structure of the cluster is altered substantially from that of the native WT state, resulting in an elongation of manganese-ligand and manganese-manganese interactions in the mutant. The strontium-H332E mutant, in which calcium is substituted by strontium, confirms that strontium (calcium) is a part of the altered cluster. The structural perturbations caused by the D1-H332E mutation are much larger than those produced by any biochemical treatment or mutation examined previously with x-ray absorption spectroscopy. The substantial structural changes provide an explanation not only for the altered properties of the D1-H332E mutant but also the importance of the histidine ligand for proper assembly of the Mn₄Ca cluster.     

Polypeptides of the oxygen-evolving photosystem II complex. Immunological detection and biogenesis

Oxygen-evolving photosystem II complex was isolated from spinach chloroplasts. The individual polypeptides of the complex were isolated from sodium dodecyl sulfate (SDS)-polyacrylamide gels and antibodies were raised in rabbits against these polypeptides. After washing of the isolation complex by 0.8 M Tris to release the extrinsic proteins, a distinct diffused protein band was revealed at the position of 33 kDa in SDS gels containing 4 M urea. When this band was electroeluted from the gel and subsequently electrophoresed on SDS gels, three distinct protein bands became apparent. Antibodies raised against each one of these polypeptides cross-reacted with the other two polypeptides to varying degrees but not with the other subunits of the complex. The three polypeptides were denoted as "34," "33," and "32" kDa and the 33 being the herbicide-binding protein. Using the antibodies, the relative amounts of the photosystem II polypeptides were followed during greening of etiolated spinach seedlings. While all three extrinsic polypeptides were present in etiolated leaves at relatively high amounts, the other polypeptides could not be detected prior to an approximate 6-h illumination period. Further illumination induced the appearance of all of the rest of the subunits in a relatively similar rate. The oxygen evolution activity was developed parallel to the increase in the amounts of these polypeptides. Therefore, the assembly of the active photosystem II during greening is a two-step process in contrast with the photosystem I reaction center, which is assembled step by step, and the rest of the chloroplast protein complexes, which are assembled by a concerted mechanism.     

Isolation and characterization of oxygen-evolving photosystem II particles and photosystem II core complex from the filamentous cyanobacterium Spirulina platensis

Photosystem (PS) II particles retaining a high rate of O₂ evolution were isolated from the mesophilic filamentous cyanobacterium, Spirulina platensis. To achieve high production of PSII complexes in the cells, irradiance from halogen incandescent lamps was used. Disruption of cells by vibration of glass beads proved to be the most suitable procedure for isolation of thylakoid membranes. The selectivity of detergents for PSII particle preparation rose in the order of Triton X-100 < decyl-β-D-glucopyranoside < dodecyldimethyl-aminooxide < n-heptyl-β-D-thioglucoside < N-dodecyl-N,N-dimethylammonio-3-propane sulphonate < n-octyl-β-thioglycoside < octylglucoside < n-dodecyl-β-D-maltoside. The last four detergents yielded extracts, from which pure PSII particles not contaminated by PSI complexes could be obtained by sucrose-gradient centrifugation (20–45%) at the 43% sucrose level. We assumed both the acceptor and donor sides of the isolated n-dodecyl-β-D-maltoside (DM) particles to be intact due to high oxygen production by DM particles [1,500 meq(e^?) mol^?1 (Chl) s^?1] achieved in the presence of all artificial acceptors tested. The PSII particle fraction from the sucrose gradient was used with immobilized metal (Cu²⁺) affinity chromatography (IMAC) for the preparation of the PSII core complex. By washing the column with a MES buffer containing MgCl₂ and CaCl₂, the phycobiliproteins were stripped off. The PSII core complex was eluted in a buffer containing 1% DM, mannitol, MgCl₂, NaCl, CaCl₂, and ?-aminocaproic acid. SDS-PAGE of the core complex provided pure bands of D1 and D2 proteins and PsbO protein from thylakoid membrane, which were used to raise polyclonal antibodies in rabbits. These antibodies recognized D1 and D2 not only as monomers of 31 and 32 kDa proteins, but also as heterodimers of D1, D2 corresponding to the band of 66 kDa on SDS-PAGE. This was in contrast to antibodies of synthetic determinants, which reacted only with the monomers of D1 and D2 proteins. These negative reactions against heterodimers of D1, D2 supported the hypothesis that dimeric forms of PSII reaction centre proteins have a C-terminal sequence sterically protected against a reaction with specific antibodies.     

Mechanism of photosynthetic water oxidation in the dimeric oxygen-evolving complex of chloroplast photosystem II

Based on the analysis of the molecular organization and properties of an isolated oxygen-evolving complex of photosystem II of plant chloroplasts, a mechanism of water oxidation and oxygen release during photosynthesis was proposed. It is suggested that the photolysis of water occurs in a dimeric oxygen-evolving complex consisting of two core complexes. In the region of contact of these complexes, a hydrophobic "boiler" is formed where the conditions for screening and stabilization of Z-linanded manganese cations accumulating positive charges for the oxidation of water molecules are created. A prerequisite to the photolysis of water is the formation of a binuclear [Mn(3+)-OH ... HO-Mn3+] hydroxyl-manganese associate, which appears in the dimeric oxygen-evolving complex after the first two light flashes as a result of photohydrolysis of photochemically oxidized Z-liganded manganese cations. The process is accompanied by the release of the first water protons to the medium. The photosynthetic oxidation of water hydroxyls occurs at the next stage and is considered as synchronous detachment of four electrons from two bound OH-groups of the associate upon photooxidation of Mn3+ cations to Mn4+ cations after two subsequent light flashes. This process is accompanied by the disproportionation of electron density and the formation of a bond between oxygen atoms of hydroxyls followed by the evolution of molecular oxygen and protons, and regeneration of two starting Mn2+ cations and the primary state of the system.     

Quantum mechanics/molecular mechanics structural models of the oxygen-evolving complex of photosystem II

The annual production of 260 Gtonnes of oxygen, during the process of photosynthesis, sustains life on earth. Oxygen is produced in the thylakoid membranes of green-plant chloroplasts and the internal membranes of cyanobacteria by photocatalytic water oxidation at the oxygen-evolving complex (OEC) of photosystem II (PSII). Recent breakthroughs in X-ray crystallography and advances in quantum mechanics/molecular mechanics (QM/MM) hybrid methods have enabled the construction of chemically sensible models of the OEC of PSII. The resulting computational structural models suggest the complete ligation of the catalytic center by amino acid residues, water, hydroxide and chloride, as determined from the intrinsic electronic properties of the oxomanganese core and the perturbational influence of the surrounding protein environment. These structures are found to be consistent with available mechanistic data, and are also compatible with X-ray diffraction models and extended X-ray absorption fine structure measurements. It is therefore conjectured that these OEC models are particularly relevant for the elucidation of the catalytic mechanism of water oxidation.     

Mechanism and energy diagram for O-O bond formation in the oxygen-evolving complex in photosystem II

The recent finding of a transition state with a significantly lower barrier than previously found, has made the mechanism for O-O bond formation in photosystem II much clearer. The full mechanism can be described in the following way. Electrons and protons are ejected from the oxygen-evolving complex (OEC) in an alternating fashion, avoiding unnecessary build-up of charge. The S0-S1 and S1-S2 transitions are quite exergonic, while the S2-S3 transition is only weakly exergonic. The strong endergonic S3-S4 transition is a key step in the mechanism in which an oxygen radical is produced, held by the dangling manganese outside the Mn3Ca cube. The O-O bond formation in the S4-state occurs by an attack of the oxygen radical on a bridging oxo ligand in the cube. The mechanism explains the presence of both a cube with bridging oxo ligands and a dangling manganese. Optimal orbital overlap puts further constraints on the structure of the OEC. An alternating spin alignment is necessary for a low barrier. The computed rate-limiting barrier of 14.7 kcal mol(-1) is in good agreement with experiments.     

Intermediates of the S(3) state of the oxygen-evolving complex of photosystem II

The S(3) state of the water-oxidizing complex (WOC) of photosystem II (PSII) is the last state that can be trapped before oxygen evolution occurs at the transient S(4) state. A number of EPR-detectable intermediates are associated with this critical state. The preceding paper examined mainly the decay of S(3) at cryogenic temperatures leading to the formation of a proton-deficient configuration of S(2) termed S(2)'. This second paper examines all intermediates formed by the near-IR light (NIR) excitation of the S(3) state and compares these with the light-excitation products of the S(2)' state. The rather complex set of observations is organized in a comprehensive flowchart, the central part of which is the S(3)...Q(A)(-) state. This state can be converted to various intermediates via two main pathways: (A) Excitation of S(3) by NIR light at temperatures below 77 K results presumably in the formation of an excited S(3) state, S(3), which decays via either of two pathways. Slowly at liquid helium temperatures but much faster at 77 K, S(3) decays to an EPR-silent state, denoted S(3)' ', which by raising the temperature to ca. 190 K converts to a spin configuration of the Mn cluster, characterized by g = 21, 3.7 in perpendicular and g = 23 in parallel mode EPR, denoted S(3)'. Upon further warming to 220 K, S(3)' relaxes to the untreated S(3) state. Below about 77 K and more favorably at liquid helium temperatures, an alternative pathway of S(3) decay via the metallo-radical intermediate S(2)'Z*...Q(A)(-) can be traced. This leads to the metastable state S(2)'Z...Q(A) via charge recombination. S(2)'Z* is characterized by a split-radical signal at g = 2, while all S(2)' transients are characterized by the same g = 5/2.9 (S = (7)/(2)) configuration of the Mn cluster with small modifications, reflecting an influence of the tyr Z oxidation state on the crystal-field symmetry at the Mn cluster. (B) S(2)'...Q(A) can be reached alternatively by the slow charge recombination of S(3) and Q(A)(-) at 77 K. White-light illumination of S(2)'.Q(A) below about 20 K results in charge separation, reforming the intermediate S(2)'Z*...Q(A)(-). Thermally activated branches to the main pathways are also described, e.g., at elevated temperatures tyr Z* reoxidizes S(2)' to the S(3) state. The above observations are discussed in terms of a molecular model of the S(3) state of the OEC. Main aspects of the model are the following. Intermediates, isoelectronic to S(3), are attributed to the NIR-induced translocation of the positive hole to different Mn ligands, or to tyr Z. On the basis of a comparison of the electron-donating efficiency of tyr Z and tyr D at cryogenic temperatures, it is inferred that the Mn cluster acts as the main proton acceptor from tyr Z. Water associated with the Mn cluster is assumed to be in hydrogen-bonding equilibrium with tyr Z, and an array comprising this water and adjacent water (or OH or O) ligands to Mn followed by a sequence of proton acceptors is proposed to act as an efficient proton translocation pathway. Oxidation of the tyrosine by P(680)(+) repels protons to and out from the Mn cluster. This proposed role of tyr Z in the water-splitting process is described as a proton repeller/electron abstractor.     

S-state dependence of the calcium requirement and binding characteristics in the oxygen-evolving complex of photosystem II

The functional role of the Ca (2+) ion in the oxygen-evolving complex of photosystem II is not yet clear. Current models explain why the redox cycle of the complex would be interrupted after the S 3 state without Ca (2+), but the literature shows that it is interrupted after the S 2 state. Reinterpretation of the literature on methods of Ca (2+) depletion [Miqyass, M., van Gorkom, H. J., and Yocum, C. F. (2007) Photosynth. Res. 92, 275-287] led us to propose that all S-state transitions require Ca (2+). Here we confirm that interpretation by measurements of flash-induced S-state transitions in UV absorbance. The results are explained by a cation exchange at the Ca (2+) binding site that, in the absence of the extrinsic PsbP and PsbQ polypeptides, can occur in minutes in low S-states and in seconds in high S-states, depending on the concentration of the substituting cation. In the S 2(K (+)) or S 2(Na (+)) state a slow conformational change occurs that prevents recovery of the slow-exchange situation on return to a lower S-state but does not inhibit the S-state cycle in the presence of Ca (2+). The ratio of binding affinities for monovalent vs divalent cations increases dramatically in the higher S-states. With the possible exception of S 0 to S 1, all S-state transitions specifically require Ca (2+), suggesting that Ca (2+)-bound H 2O plays an essential role in a H (+) transfer network required for H (+)-coupled electron transfer from the Mn cluster to tyrosine Z.     

Investigation of substrate water interactions at the high-affinity Mn site in the photosystem II oxygen-evolving complex

18 O isotope exchange measurements of photosystem II (PSII) in thylakoids from wild-type and mutant Synechocystis have been performed to investigate binding of substrate water to the high-affinity Mn4 site in the oxygen-evolving complex (OEC). The mutants investigated were D1-D170H, a mutation of a direct ligand to the Mn4 ion, and D1-D61N, a mutation in the second coordination sphere. The substrate water 18 O exchange rates for D61N were found to be 0.16+/-0.02 s(-1) and 3.03+/-0.32 s(-1) for the slow and fast phases of exchange, respectively, compared with 0.47+/-0.04 s(-1) and 19.7+/-1.3 s(-1) for the wild-type. The D1-D170H rates were found to be 0.70+/-0.16 s(-1) and 24.4+/-4.6 s(-1) and thus are almost within the error limits for the wild-type rates. The results from the D1-D170H mutant indicate that the high-affinity Mn4 site does not directly bind to the substrate water molecule in slow exchange, but the binding of non-substrate water to this Mn ion cannot be excluded. The results from the D61N mutation show an interaction with both substrate water molecules, which could be an indication that D61 is involved in a hydrogen bonding network with the substrate water. Our results provide limitations as to where the two substrate water molecules bind in the OEC of PSII.     

Inhibition of the oxygen-evolving complex of photosystem II and depletion of extrinsic polypeptides by nickel

The toxic effect of Ni²⁺ on photosynthetic electron transport was studied in a photosystem II submembrane fraction. It was shown that Ni²⁺ strongly inhibits oxygen evolution in the millimolar range of concentration. The inhibition was insensitive to NaCl but significantly decreased in the presence of CaCl₂. Maximal chlorophyll fluorescence, together with variable fluorescence, maximal quantum yield of photosystem II, and flash-induced fluorescence decays were all significantly declined by Ni²⁺. Further, the extrinsic polypeptides of 16 and 24 kDa associated with the oxygen-evolving complex of photosystem II were depleted following Ni²⁺ treatment. It was deduced that interaction of Ni²⁺ with these polypeptides caused a conformational change that induced their release together with Ca²⁺ from the oxygen-evolving complex of photosystem II with consequent inhibition of the electron transport activity.     

Molecular evolutionary analysis of the psbP gene family of the photosystem II oxygen-evolving complex in Nicotiana.

Photosystem II psbP protein of the oxygen-evolving complex is involved in the photosynthetic oxygen evolution in plants. Four psbP polypeptides were detected in Nicotiana tabacum on a two-dimensional gel by immunostaining the proteins with antiserum against the pea psbP Comparison of the protein patterns of psbP from N. tabacum and its ancestral parents, N. sylvestris and N. tomentosiformis, indicated that each of the ancestral parents has contributed a pair of psbP proteins. This was supported by Southern hybridization results, which suggested that psbP in Nicotiana is encoded by a gene family consisting of four members in N. tabacum and two members each in N. glauca, N. langsdorffii, N. sylvestris, and N. tomentosiformis. A scheme of molecular evolution of the psbP genes in Nicotiana is also proposed.     

Oxidation of the Mn cluster induces structural changes of NO3- functionally bound to the Cl- site in the oxygen-evolving complex of photosystem II

Cl(-) is an indispensable cofactor for photosynthetic O(2) evolution and is functionally replaced by NO(3)(-). Structural changes of an isotopically labeled NO(3)(-) ion, induced by the oxidation of the Mn cluster (S(1)-to-S(2)), were detected by FTIR spectroscopy. NO(3)(-)-substituted photosystem II core particles showed (14)N(16)O(3)(-)/(15)N(16)O(3)(-) and (14)N(16)O(3)(-)/(14)N(18)O(3)(-) isotopic bands in the S(2)/S(1) spectra with markedly high signal/noise ratio. These bands appeared only in the region from 1415 to 1284 cm(-1), indicating that the bands do not arise from a metal-bound NO(3)(-) but from an ionic NO(3)(-). The intensity of the bands exhibited a quantitatively proportional relationship with the O(2) activity. These results demonstrate that the NO(3)(-) functionally bound to the Cl(-) site couples to the Mn cluster structurally, but is not associated with the cluster as a direct ligand. Comparison of the bands for two isotopes ((15)N and (18)O) and their simulations enable us to assign each band to the S(1) and S(2) states. The results indicate that the NO(3)(-) ion bound to the Cl(-) site is highly asymmetric in S(1) but rather symmetric in S(2). Since NO(3)(-) functionally replaces Cl(-), most of the conclusions drawn from this study will be also applicable to Cl(-).     

Dual-mode EPR study of new signals from the S3-state of oxygen-evolving complex in photosystem II

The light-induced new EPR signals at g = 12 and 8 were observed in photosystem II (PS II) membranes by parallel polarization EPR. The signals were generated after two flashes of illumination at room temperature, and the signal intensity had four flashes period oscillation, indicating that the signal origin could be ascribed to the S3-state. Successful simulations were obtained assuming S = 1 spin for the values of the zero-field parameters, D = +/-0.435 +/- 0. 005 cm-1 and E/D = -0.317 +/- 0.002. Orientation dependence of the g =12 and 8 signal intensities shows that the axial direction of the zero-field interaction of the manganese cluster is nearly parallel to the membrane normal.     

Effects of ethylene glycol and methanol on ammonia-induced structural changes of the oxygen-evolving complex in photosystem II

Ammonia is an inhibitor of water oxidation and a structural analogue for substrate water, making it a valuable probe for the structural properties of the possible substrate-binding site on the oxygen-evolving complex (OEC) in photosystem II (PSII). By using the NH(3)-induced upshift of the 1365 cm(-)(1) IR mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum and the NH(3)-modified S(2) state EPR signals of PSII as spectral probes, we found that ethylene glycol has clear effects on the binding properties of the NH(3)-specific site on the OEC. Our results show that in PSII samples containing 30% (v/v) ethylene glycol, the affinity of the NH(3)-specific binding site on the OEC is estimated to be more than 10 times lower than that in PSII samples containing 0.4 M sucrose. In addition, our results show that the NH(3)-induced upshift of the 1365 cm(-)(1) IR mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum is dependent on the concentration of ethylene glycol, but not dependent on the concentration of sucrose (up to 1.5 M) or methanol (up to 5.4 M). By comparing the concentration dependence of sucrose and ethylene glycol on NH(3)-induced spectral change and also by comparing the sucrose and ethylene glycol data at similar concentrations ( approximately 1 M), we conclude that ethylene glycol has a clear effect on the NH(3)-induced spectral changes. Furthermore, our results also show that ethylene glycol alters the steric requirement of the amine effect on the upshift of the 1365 cm(-)(1) mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum. In PSII samples containing 30% (v/v) ethylene glycol, only NH(3), not other bulkier amines (e.g., Tris, AEPD, and CH(3)NH(2)), has a clear effect on the upshift of the 1365 cm(-)(1) mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum; in contrast, in PSII samples containing 0.4 M sucrose, both NH(3) and CH(3)NH(2) have a clear effect. On the basis of the results mentioned above, we propose that ethylene glycol acts directly or indirectly to decrease the affinity or limit the accessibility of NH(3) and CH(3)NH(2) to the NH(3)-specific binding site on the OEC in PSII. Finally, we also applied the same approach to test whether methanol is able to compete with ammonia on its binding site on the OEC. We found that 4% (v/v) methanol does not have any significant effect on the NH(3)-induced upshift of the 1365 cm(-)(1) mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum and the NH(3)-modified S(2) state g = 2 multiline EPR signal. Our results suggest that methanol is unable to compete with NH(3) upon binding to the Mn site of the OEC that gives rise to the altered S(2) state g = 2 multiline EPR signal.     

Trapping of the S2 to S3 state intermediate of the oxygen-evolving complex of photosystem II

Photosystem II preparations poised in the S(2)...Q(A) state produce no detectable intermediate during straightforward illumination at liquid helium temperatures. However, upon flash illumination in the range of 77-190 K, they produce a transient state which at -10 degrees C advances to S(3) or after rapid cooling to 10 K gives rise to a 116 G wide metalloradical EPR signal. The latter decays with half-times on the order of a few minutes, presumably by charge recombination, and can be regenerated repeatedly by illumination at 10 K. The constraints for Tyr Z oxidation are attributed to the presence of excess positive charge in S(2). Elevated temperatures are required presumably to overcome a thermal barrier in the deprotonation of Tyr Z(+) or most likely to allow secondary proton transfer away from the base partner of Tyr Z. Treatment with 5% (v/v) MeOH appears to remove the constraints for Tyr Z oxidation, and a 160 G wide metalloradical EPR signal is produced by illumination at 10 K, which decays with a half-time of ca. 80 s. Formation of the metalloradical signals is accompanied by reversible changes in the Mn multiline signal. The intermediates are assigned to Tyr Z(*) magnetically interacting with the Mn cluster in S(2), S(2)Y(Z)(*). A molecular model which extends an earlier suggestion and provides a plausible explanation of a number of observations, including the binding of small molecules to the Mn cluster, is presented.