Coordination between manganese and nitrogen within the ligands in the manganese complexes facilitates the reconstitution of the water-oxidizing complex in manganese-depleted photosystem II preparations

The water-oxidizing complex (WOC) within photosystem II (PSII) can be reconstituted with synthetic manganese complexes by a process called photoactivation; however, the key factors affecting the efficiency of synthetic manganese complexes in reconstitution of electron transport and oxygen evolution activity in manganese-depleted PSII remain unclear. In the present study, four complexes with different manganese coordination environments were used to reconstitute the WOC, and an interesting relationship was found between the coordination environment of the manganese atom in the complexes and their efficiency in restoring electron transport and oxygen evolution. If Mn(II) is coordinated to nitrogen atoms within the ligand, it can restore significant rates of electron transport and oxygen evolution; however, if the manganese atom is coordinated only to oxygen atoms instead of nitrogen atoms, it has no capability to restore electron transport and oxygen evolution. So, our results demonstrate that the capability of manganese complexes to reconstitute the WOC is mainly determined by the coordination between nitrogen atoms from ligands and the manganese atom. It is suggested from our results that the ligation between the nitrogen atom and the manganese atom within the manganese complex facilitates the photoligation of the manganese atom to histidyl residues on the apo-protein in manganese-depleted PSII during photoactivation.     

Involvement of Carboxyl Groups of the PSII Reaction Center Proteins in Photoactivation of the Apo-Water-Oxidizing Complex

Involvement of residues of acidic amino acids in photo-ligationof manganese into the apo-water-oxidizing complex was investigatedby use of l-ethyl-3-[3-(dimethylami-no)propyl]carbodiimide (EDC),a water-soluble carboxyl modifier. Treatment of Mn-depletedPSII membranes by EDC in the presence of nucleophiles induceda loss of photoactivation capability in the Mn complex and partialloss of capability of photooxidation of Mn²⁺, but little decreasein the DCIP photoreduction supported by diphen-ylcarbazide.The inhibition of diphenylcarbazide-photo-oxidation by submicromolarMn²⁺, indicative of the intactness of high-affinity Mn-bindingsites, was apparently abolished by EDC treatment. From aminoacid quantitation analysis of Dl and D2 proteins and CP47 ofthe chemically-modified membranes, approximately three carboxylgroups of the D1 protein were found to be chemically-modifiedwith EDC after removal of the functional Mn. These results suggestthat acidic amino acids on the D1 protein are involved in photoactivationof the apo-water-oxidizing complex and probably in ligationof Mn to the water-oxidizing complex. (Received October 21, 1996; Accepted March 3, 1997)     

Requirements for the photoligation of Mn2+ in PS II membranes and the expression of water-oxidizing activity of the polynuclear Mn-catalyst

Ligation of Mn²⁺ into the polynuclear Mn-catalyst of water oxidation was shown using PS II membranes depleted of their Mn and the 17, 23 and 33 kDa extrinsic proteins. This process specifically required light and Ca²⁺ concentrations of 5̃0 mM. Evidence was obtained indicating Mn²⁺/Ca²⁺ competition for Ca²⁺ and Mn²⁺ binding sites essential for the photoligation of Mn. Photoligation of Mn did not result in an increase of water oxidation capacity; however, water oxidation capacity was expressed following dark reconstitution minimally with the 33 kDa protein. The results represent the first observation of photoactivation of water oxidation in a system that excludes simple light-driven Mn²⁺ transport across membrane(s).     

Manganese and calcium requirements for reconstitution of oxygen-evolution activity in manganese-depleted photosystem II membranes

The Mn complex of photosystem II and O2-evolution activity are reconstituted in Mn-depleted photosystem II membranes in a light-dependent process called photoactivation. Recovery of O2-evolution activity requires both Mn2+ and Ca2+ in the photoactivation medium. The Mn2+ and Ca2+ dependences of both the effective rate constant and yield of photoactivation have been determined. A comparison of these data with the predictions of mathematical models for photoactivation leads to the conclusion that photoactivation occurs in two stages. The first stage, photoligation of Mn, requires light and depends primarily on Mn2+. The second stage, binding of Ca2+, is required for expression of O2-evolution activity. This two-stage model affords an excellent fit to the data and provides dissociation constants and binding stoichiometries for Ca2+ and Mn2+. We conclude that one Mn2+ ion is bound and photooxidized in the rate-determining step(s) of photoactivation. On the basis of these results and data already in the literature, the molecular details of the elementary steps in photoactivation are discussed and a mechanism of photoactivation is proposed.     

Photoassembly of the manganese cluster in mutants perturbed in the high affinity Mn-binding site of the H2O-oxidation complex of photosystem II

The light-driven, oxidative assembly of Mn2+ ions into the H2O-oxidation complex (WOC) of the photosystem II (PSII) reaction center is termed photoactivation and culminates in the formation of the oxygen-evolving (Mn4-Ca) center of the WOC. Initial binding and photooxidation of Mn2+ to the apoprotein is critically dependent upon aspartate 170 of the D1 protein (D1-D170) of the high affinity Mn site [Nixon and Diner (1992) Biochemistry 31, 942-948]. Three O2-evolving mutant strains of Synechocystis, D1-D170E, D1-D170H, and D1-D170V, were studied in terms of the kinetics of photoactivation under both continuous and flashing light. Photoactivation using single turnover flashes revealed D1-D170H and D1-D170V, but not D1-D170E, were prone to form substantial amounts ( approximately 40-50%) of inactive centers ascribed to photoligation of aberrant nonfunctional Mn based upon the reversibility of the inactivation and similarity to previous in vitro results [Chen, C., Kazimir, J., and Cheniae, G. M. (1995) Biochemistry 34, 13511-13526]. On the other hand, D1-D170E lowers the quantum efficiency of photoactivation compared to the wild-type by the largest amount (80% decrease) versus D1-D170H and D1-D170V, which do not produce measurable decreases in quantum efficiency. The low quantum efficiency of photoactivation in D1-D170E is due to the destabilization of photoactivation intermediates. Numerical analysis indicates that the PSII centers in D1-D170E are heterogeneous with respect to photoactivation kinetics and that the majority of centers are characterized by intermediates that decay approximately 10-fold more rapidly than the wild-type control. Additionally, the kinetics of O2 release during the S3-S0 transition was markedly retarded in D1-D170E, in contrast to D1-D170H and D1-D170V, which did not exhibit a discernible slow-down compared to the wild-type.     

Bicarbonate requirement for the water-oxidizing complex of photosystem II

It is well established that bicarbonate stimulates electron transfer between the primary and secondary electron acceptors, Q(A) and Q(B), in formate-inhibited photosystem II; the non-heme Fe between Q(A) and Q(B) plays an essential role in the bicarbonate binding. Strong evidence of a bicarbonate requirement for the water-oxidizing complex (WOC), both O2 evolving and assembling from apo-WOC and Mn2+, of photosystem II (PSII) preparations has been presented in a number of publications during the last 5 years. The following explanations for the involvement of bicarbonate in the events on the donor side of PSII are considered: (1) bicarbonate serves as an electron donor (alternative to water or as a way of involvement of water molecules in the oxidative reactions) to the Mn-containing O2 center; (2) bicarbonate facilitates reassembly of the WOC from apo-WOC and Mn2+ due to formation of the complexes MnHCO3+ and Mn(HCO3)2 leading to an easier oxidation of Mn2+ with PSII; (3) bicarbonate is an integral component of the WOC essential for its function and stability; it may be considered a direct ligand to the Mn cluster; (4) the WOC is stabilized by bicarbonate through its binding to other components of PSII.     

Possible relationship of mechanisms of Mn2+ oxidation and formation of plant photosystem II manganese cluster.

The mechanisms of Mn2+ cation oxidation in alkaline, neutral and slightly acidic media were studied. In all cases, the Mn2+ oxidation resulted in the formation of the structure[see text]. The formal resemblance and differences in the Mn2O3 structure and Klein's model of the Mn cluster of PS II were noted. The necessity of the primary ligation of Mn2+ cations was discussed for both the decrease in the Mn2+ oxidation potential and the stability of the Mn2O3 structure. It was supposed that Mn2O3 is an initial block for the assembly of the inorganic core of the photosynthetic water-oxidizing complex.     

Mutagenesis of CP43-arginine-357 to serine reveals new evidence for (bi)carbonate functioning in the water oxidizing complex of Photosystem II.

The chlorophyll-binding protein CP43 is an inner subunit of the Photosystem II (PSII) reaction center core complex of all oxygenic photoautotrophs. X-Ray structural evidence places the guanidinium cation of the conserved arginine 357 residue of CP43 within a few Angstroms to the Mn(4)Ca cluster of the water-oxidizing complex (WOC) and has been implicated as a possible carbonate binding site. To test the hypothesis, the serine mutant, CP43-R357S, from Synechocystis PCC 6803 was investigated by PSII variable fluorescence (F(v)/F(m)) and simultaneous flash O(2) yield measurements in cells and thylakoid membranes. The R357S mutant assembles PSII-WOC centers, but is unable to grow photoautotrophically. Reconstitution of O(2) evolution by photoactivation and the occurrence of period-four oscillations of F(v)/F(m) establishes that the R357S mutant contains an assembled Mn(4)Ca cluster, but turnover is impaired as seen by an 11-fold larger Kok double miss parameter and faster decay of upper S states. Using pulsed light to avoid photoinactivation, wild-type cells and thylakoid membranes exhibit a 2-4-fold loss in O(2) evolution rate upon partial bicarbonate depletion under multiple turnover conditions, while the R357S mutant is unaffected by bicarbonate. Arginine R357 appears to function in binding a (bi)carbonate ion essential to normal catalytic turnover of the WOC. The quantum yield of electron donation from the WOC into PSII increases with decreasing turnover rate in R357S mutant cells and involves an aborted two-flash pathway that is distinct from the classical four-flash pattern. We speculate that an altered photochemical mechanism for O(2) production occurs via formation of hydrogen peroxide, by analogy to other treatments that retard the kinetics of proton release into the lumen.     

Photoactivation of Oxygen-Evolving Enzyme in Dark-Grown Pine Cotyledons: Relationship between Assembly of Photosystem II Proteins and Integration of Manganese and Calcium

Dark-grown cotyledons of pine (Pinus thunbergit) did not exhibitO₂ evolution, but this capability was rapidly activated by illuminationfor a short period (photoactivation). To examine the biochemicalchanges which accompany the process of photoactivation in gymnosperms,a method enabling the preparation of highly active O₂-evolvingphotosystem II (PS II) membranes was applied to light-grown,dark-grown, and photoactivated cotyledons. PS II membranes preparedfrom light-grown cotyledons exhibited high O₂-evolving activity,and contained all the intrinsic proteins as well as the threeextrinsic proteins (32, 23 and 17 kDa) associated with PS II.These membranes were also found to contain 4.4 Mn and 0.83 Ca/PSII reaction center. PS II membranes from dark-grown cotyledonscontained all the intrinsic proteins, but preserved only 32kDa extrinsic protein, and zero Mn and 0.85 Ca/PS II reactioncenter. The two extrinsic proteins (23 and 17 kDa) absent inthe PS II membranes from dark-grown cotyledons were, however,present as mature forms in whole thylakoid membranes from thecorresponding sample. The PS II membranes isolated from photoactivatedcotyledons showed a high activity of O₂ evolution and retainedthe three extrinsic proteins, 5.3 Mn and 1.1 Ca/PS II reactioncenter, respectively. The results indicated that Mn and thetwo extrinsic proteins were tightly integrated in the O₂-evolvingapparatusduring the process of photoactivation but integration of Capreceded the integration of Mn by photoactivation. (Received December 9, 1991; Accepted February 1, 1992)     

Photoactivation of the latent water-oxidizing complex in photosystem II membranes isolated from dark-grown spruce seedlings

Photosystem II membranes (D-PSII) were isolated from dark-grown spruce seedlings. All major PSII proteins except the 17- and 23-kDa extrinsic proteins were present in D-PSII. O₂ evolution and Mn content in D-PSII were negligible, while PSII-donor activity showed a value comparable to that of NH₂OH-treated PSII membranes (NH₂OH-L-PSII) from light-grown seedlings. Light incubation of D-PSII with 1 m M MnCl₂, 50 m M CaCl₂ and 100 μ M DCIP at pH 5.3 resulted in activation of the latent water-oxidizing complex. Accomplishment of photoactivation of PSII membranes from dark-grown spruce seedlings clearly indicates that only ligation of Mn²⁺ to the apo-water oxidizing complex is required for expression of O₂ evolution, and that protein synthesis is not involved in the photoactivation process. There was no essential difference between 'photoactivation' of naturally Mn-free PSII membranes and 'photoreactivation' of artificially Mn-depleted PSII membranes on kinetics, pH dependence, Mn²⁺-concentration dependence. However, kinetics and pH dependence of photoactivation were appreciably different in spruce PSII membranes and in PSII membranes of angiosperms such as wheat and spinach.     

Pigment and protein composition of reconstituted light-harvesting complexes and effects of some protein modifications

The structure and heterogeneity of LHC II were studied by in vitro reconstitution of apoproteins with pigments (Plumley and Schmidt 1987, Proc Natl Acad Sci 84: 146–150). Reconstituted CP 2 complexes purified by LDS-PAGE were subsequently characterized and shown to have spectroscopic properties and pigment-protein compositions and stoichiometries similar to those of authentic complexes. Heterologous reconstitutions utilizing pigments and light-harvesting proteins from spinach, pea and Chlamydomonas reinhardtii reveal no evidence of specialized binding sites for the unique C. reinhardtii xanthophyll loroxanthin: lutein and loroxanthin are interchangeable for in vitro reconstitution. Proteins modified by the presence of a transit peptide, phosphorylation, or proteolytic removal of the NH₂-terminus could be reconstituted. Evidence suggests that post-translational modification are not responsible for the presence of six electrophoretic variants of C. reinhardtii CP 2. Reconstitution is blocked by iodoacetamide pre-treatment of the apoproteins suggesting a role for cysteine in pigment ligation and/or proper folding of the pigment-protein complex. Finally, no effect of divalent cations on pigment reassembly could be detected.Abbreviations cab chlorophyll a/b-binding protein genes - Chl chlorophyll - CP2 light-harvesting chlorophyll A+b-protein complex fractionated by mildly denaturing LDS-PAGE from Photosystem II in thylakoids - CP 43 and CP 47 chlorophyll a-antenna complexes fractionated from Photosystem II in thylakoids by mildly denaturing LDS-PAGE at 4°C - IgG gamma immunoglobulin - LDS lithium dodecyl sulfate - LDS-PAGE lithium dodecyl sulfate polyacrylamide gel electrophoresis at 4°C - LHC I and LHC II thylakoid light-harvesting chlorophyll a+b-protein holocomplexes associated with Photosystems I and II, respectively - PS II Photosystem II - TX100 Triton X-100 - TX100-derived LHC light-harvesting complexes enriched in LHC II following fractionation of thylakoids by TX100     

Bicarbonate accelerates assembly of the inorganic core of the water-oxidizing complex in manganese-depleted photosystem II: a proposed biogeochemical role for atmospheric carbon dioxide in oxygenic photosynthesis

The proposed role for bicarbonate (HCO(3)(-)) as an intrinsic cofactor within the water-oxidizing complex (WOC) of photosystem II (PSII) [Klimov et al. (1997) Biochemistry 36, 16277-16281] was tested by investigation of its influence on the kinetics and yield of photoactivation, the light-induced assembly of the functional inorganic core (Mn(4)O(y)Ca(1)Cl(x)) starting from the cofactor-depleted apo-WOC-PSII center and free Mn(2+), Ca(2+), and Cl(-). Two binding sites for bicarbonate were found that stimulate photoactivation by accelerating the formation and suppressing the decay, respectively, of the first light-induced assembly intermediate, IM(1) [apo-WOC-Mn(OH)(2)(+)]. A high-affinity bicarbonate site (K(D) 相似文献   

Water cleavage by solar radiation—an inspiring challenge of photosynthesis research

Solar energy exploitation by photosynthetic water cleavage is of central relevance for the development and sustenance of all higher forms of living matter in the biosphere. The key steps of this process take place within an integral protein complex referred to as Photosystem II (PS II) which is anisotropically incorporated into the thylakoid membrane. This minireview concentrates on mechanistic questions related to i) the generation of strongly oxidizing equivalents (holes) at a special chlorophyll a complex (designated as P680) and ii) the cooperative reaction of four holes with two water molecules at a manganese containing unit WOC (water oxidizing complex) resulting in the release of molecular oxygen and four protons. The classical work of Pierre Joliot and Bessel Kok and their coworkers revealed that water oxidation occurs via a sequence of univalent oxidation steps including intermediary redox states S_i (i = number of accumulated holes within the WOC). Based on our current stage of knowledge, an attempt is made a) to identify the nature of the redox states S_i, b) to describe the structural arrangement of the (four) manganese centers and their presumed coordination and ligation within the protein matrix, and c) to propose a mechanism of photosynthetic water oxidation with special emphasis on the key step, i.e. oxygen-oxygen bond formation. It is assumed that there exists a dynamic equilibrium in S₃ with one state attaining the nuclear geometry and electronic configuration of a complexed peroxide. This state is postulated to undergo direct oxidation to complexed dioxygen by univalent electron abstraction with Y_Z ^ox and simultaneous internal ligand to metal charge transfer.Key questions on the mechanism will be raised. The still fragmentary answers to these questions not only reflect our limited knowledge but also illustrate the challenges for future research.Abbreviations b559 cytochrome b559 - BChl bacteriochlorophyll - Chl chlorophyll - CP47 Chl a containing a 47 kDa polypeptide - D1/D2 polypeptides of the PS II reaction center - ENDOR electron nuclear double resonance - EPR electron paramagnetic resonance - ESEEM electron spin echo envelope modulation - EXAFS extended X-ray absorption fine structure - FTIR Fourier transform infrared - NMR nuclear magnetic resonance - P680, P700 photoactive Chl a of PS II and PS I, respectively - PS II Photosystem II - Q_A special plastoquinone of PS II - S_i redox states of WOC - WOC water oxidizing complex - WOS water oxidizing site - UV/VIS ultraviolet/visible - Y_D, Y_Z redox active tyrosines of polypeptides D2 and D1, respectively     

What Are the Oxidation States of Manganese Required To Catalyze Photosynthetic Water Oxidation?

Photosynthetic O(2) production from water is catalyzed by a cluster of four manganese ions and a tyrosine residue that comprise the redox-active components of the water-oxidizing complex (WOC) of photosystem II (PSII) in all known oxygenic phototrophs. Knowledge of the oxidation states is indispensable for understanding the fundamental principles of catalysis by PSII and the catalytic mechanism of the WOC. Previous spectroscopic studies and redox titrations predicted the net oxidation state of the S(0) state to be (Mn(III))(3)Mn(IV). We have refined a previously developed photoassembly procedure that directly determines the number of oxidizing equivalents needed to assemble the Mn(4)Ca core of WOC during photoassembly, starting from free Mn(II) and the Mn-depleted apo-WOC complex. This experiment entails counting the number of light flashes required to produce the first O(2) molecules during photoassembly. Unlike spectroscopic methods, this process does not require reference to synthetic model complexes. We find the number of photoassembly intermediates required to reach the lowest oxidation state of the WOC, S(0), to be three, indicating a net oxidation state three equivalents above four Mn(II), formally (Mn(III))(3)Mn(II), whereas the O(2) releasing state, S(4), corresponds formally to (Mn(IV))(3)Mn(III). The results from this study have major implications for proposed mechanisms of photosynthetic water oxidation.     

Assembly and disassembly of the photosystem II manganese cluster reversibly alters the coupling of the reaction center with the light-harvesting phycobilisome

The light-driven oxidative assembly of Mn (2+) ions into the H 2O oxidation complex (WOC) of the photosystem II (PSII) reaction center is termed photoactivation. The fluorescence yield characteristics of Synechocystis sp. PCC6803 cells undergoing photoactivation showed that basal fluorescence, F 0, exhibited a characteristic decline when red, but not blue, measuring light was employed. This result was traced to a progressive increase in the coupling of the phycobilisome (PBS) to the PSII reaction center as determined by observing the changes in room temperature and 77 K fluorescence emission spectra that accompany photoactivation. The results support the hypothesis that strong energetic coupling of the PBS to the PSII reaction center depends upon the formation of an active WOC, which presumably diminishes the likelihood of photodamage to reaction centers that have either lost an intact Mn cluster or are in the process of assembling an active WOC.     

Remarkable affinity and selectivity for Cs+ and uranyl (UO22+) binding to the manganese site of the apo-water oxidation complex of photosystem II.

The size and charge density requirements for metal ion binding to the high-affinity Mn2+ site of the apo-water oxidizing complex (WOC) of spinach photosystem II (PSII) were studied by comparing the relative binding affinities of alkali metal cations, divalent metals (Mg2+, Ca2+, Mn2+, Sr2+), and the oxo-cation UO22+. Cation binding to the apo-WOC-PSII protein was measured by: (1) inhibition of the rate and yield of photoactivation, the light-induced recovery of O2 evolution by assembly of the functional Mn4Ca1Clx, core from its constituent inorganic cofactors (Mn2+, Ca2+, and Cl-); and by (2) inhibition of the PSII-mediated light-induced electron transfer from Mn2+ to an electron acceptor (DCIP). Together, these methods enable discrimination between inhibition at the high- and low-affinity Mn2+ sites and the Ca2+ site of the apo-WOC-PSII. Unexpectedly strong binding of large alkali cations (Cs+ > Rb+ > K+ > Na+ > Li+) was found to smoothly correlate with decreasing cation charge density, exhibiting one of the largest Cs+/Li+ selectivities (>/=5000) for any known chelator. Both photoactivation and electron-transfer measurements at selected Mn2+ and Ca2+ concentrations reveal that Cs+ binds to the high-affinity Mn2+ site with a slightly greater affinity (2-3-fold at pH 6.0) than Mn2+, while binding about 10(4)-fold more weakly to the Ca2+-specific site required for reassembly of functional O2 evolving centers. In contrast to Cs+, divalent cations larger than Mn2+ bind considerably more weakly to the high-affinity Mn2+ site (Mn2+ > Ca2+ > Sr2+). Their affinities correlate with the hydrolysis constant for formation of the metal hydroxide by hydrolysis of water: Me2+aq --> [MeOH]+aq + H+aq. Along with the strong stimulation of the rate of photoactivation by alkaline pH, these metal cation trends support the interpretation that [MnOH]+ is the active species that forms upon binding of Mn2+aq to apo-WOC. Further support for this interpretation is found by the unusually strong inhibition of Mn2+ photooxidation by the linear uranyl cation (UO22+). The intrinsic binding constant for [MnOH]+ to apo-WOC was determined using a thermodynamic cycle to be K = 4.0 x 10(15) M-1 (at pH 6.0), consistent with a high-affinity, preorganized, multidentate coordination site. We propose that the selectivity for binding [MnOH]+, a linear low charge-density monocation, vs symmetrical Me2+ dications is functionally important for assembly of the WOC by enabling: (1) discrimination against higher charge density alkaline earth cations (Mg2+ and Ca2+) and smaller alkali metal cations (Na+ and K+) that are present in considerably greater abundance in vivo, and thus would suppress photoactivation; and (2) higher affinity binding of the one Ca2+ ion or the remaining three Mn2+ ions via coordination to form mu-hydroxo-bridged intermediates, apo-WOC-[Mn(mu-OH)2Mn]3+ or apo-WOC-[Mn(mu-OH)Ca]3+, during subsequent assembly steps of the native Mn4Ca1Clx core. In contrast to more acidic Me2+ divalent ion inhibitors of the high-affinity Mn2+ site, like Ca2+ and Sr2+, Cs+ does not accelerate the decay of the first light-induced intermediate, IM1, formed during photoactivation (attributed to apo-WOC-[Mn(OH)2]+). The inability of Cs+ to promote decay of IM1, despite having comparable affinity as Mn2+, is consistent with its considerably weaker Lewis acidity, resulting in the reprotonation of IM1 by water becoming the rate-limiting step for decay prior to displacement of Mn2+. All four different lines of evidence provide a self-consistent picture indicating that the initial step in assembly of the WOC involves high-affinity binding of [MnOH]+.     

Nano-sized manganese-calcium cluster in photosystem II

Cyanobacteria, algae, and plants are the manufacturers that release O₂ via water oxidation during photosynthesis. Since fossil resources are running out, researchers are now actively trying to use the natural catalytic center of water oxidation found in the photosystem II (PS II) reaction center of oxygenic photosynthetic organisms to synthesize a biomimetic supercatalyst for water oxidation. Success in this area of research will transcend the current bottleneck for the development of energy-conversion schemes based on sunlight. In this review, we go over the structure and function of the water-oxidizing complex (WOC) found in Nature by focusing on the recent advances made by the international research community dedicated to achieve the goal of artificial water splitting based on the WOC of PS II.     

Unique binding site for Mn2+ ion responsible for reducing an oxidized YZ tyrosine in manganese-depleted photosystem II membranes.

Binding of Mn2+ to manganese-depleted photosystem II and electron donation from the bound Mn2+ to an oxidized YZ tyrosine were studied under the same equilibrium conditions. Mn2+ associated with the depleted membranes in a nonsaturating manner when added alone, but only one Mn2+ ion per photosystem II (PS II) was bound to the membranes in the presence of other divalent cations including Ca2+ and Mg2+. Mn2+-dependent electron donation to photosystem II studied by monitoring the decay kinetics of chlorophyll fluorescence and the electron paramagnetic resonance (EPR) signal of an oxidized YZ tyrosine (YZ+) after a single-turnover flash indicated that the binding of only one Mn2+ ion to the manganese-depleted PS II is sufficient for the complete reduction of YZ+ induced by flash excitation. The results indicate that the manganese-depleted membranes have only one unique binding site, which has higher affinity and higher specificity for Mn2+ compared with Mg2+ and Ca2+, and that Mn2+ bound to this unique site can deliver an electron to YZ+ with high efficiency. The dissociation constant for Mn2+ of this site largely depended on pH, suggesting that a single amino acid residue with a pKa value around neutral pH is implicated in the binding of Mn2+. The results are discussed in relation to the photoactivation mechanism that forms the active manganese cluster.     

Isolation of PS II reaction centre and its relationship to the minor chlorophyll-protein complexes

Evidence is presented for the identification of the chlorophyll- protein complex CPa-1 (CP 47) as the reaction centre of photosystem II (PS II). We have developed a simple, rapid method using octyl glucoside solubilization to obtain preparations from spinach and barley that are highly enriched in PS II reaction centre activity (measured as the light-driven reduction of diphenylcarbazide by 2,6-dichlorophenolindophenol). These preparations contain only the two minor chlorophyll-protein complexes CPa-1 and CPa-2. During centrifugation on a sucrose density gradient, there is a partial separation of the two CPa complexes from each other, and a complete separation from other chlorophyll-protein complexes. The PS II activity comigrates with CPa-1 but not CPa-2, strongly suggesting that the former is the reaction centre complex of PS II. Reaction centre preparations are sensitive to the herbicide 3(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU), but only at much higher concentrations than those required to inhibit intact thylakoid membranes. A model of PS II incorporating our current knowledge of the chlorophyll-protein complexes is presented. It is proposed that CPa-2 and the chlorophyll a + b complex CP 29 may function as internal antenna complexes surrounding the reaction centre, with the addition of variable amounts of the major chlorophyll a + b light-harvesting complex.     

Long-lived primary radical pair state detected by time-resolved fluorescence and absorption spectroscopy in an isolated Photosystem two core

A Photosystem two (PS II) core preparation containing the chlorophyll a binding proteins CP 47, CP 43, D1 and D2, and the non-chlorophyll binding cytochrome-b559 and 33 kDA polypeptides, has been isolated from PS II-enriched membranes of peas using the non-ionic detergent heptylthioglucopyranoside and elevated ionic strengths. The primary radical pair state, P680⁺Pheo^-, was studied by time-resolved absorption and fluorescence spectroscopy, under conditions where quinone reduction and water-splitting activities were inhibited. Charge recombination of the primary radical pair in PS II cores was found to have lifetimes of 17.5 ns measured by fluorescence and 21 ns measured by transient decay kinetics under anaerobic conditions. Transient absorption spectroscopy demonstrated that the activity of the particles, based on primary radical pair formation, was in excess of 70% (depending on the choice of kinetic model), while time-resolved fluorescence spectroscopy indicated that the particles were 91% active. These estimates of activity were further supported by steady-state measurements which quantified the amount of photoreducible pheophytin. It is concluded that the PS II core preparation we have isolated is ideal for studying primary radical pair formation and recombination as demonstrated by the correlation of our absorption and fluorescence transient data, which is the first of its kind to be reported in the literature for isolated PS II core complexes from higher plants.Abbreviations CP 43 and CP 47 chlorophyll binding proteins of PS II having apparent molecular weights on SDS-PAGE of 43 kDa and 47 kDa, respectively - D1 and D2 polypeptides PS II reaction centre polypeptides encoded by the psbA and psbD genes, respectively - HPLC high performance liquid chromatography - PS II Photosystem two - SDS-PAGE sodium dodecyl sulphate-polyacrylamide gel electrophoresis - P680 primary electron donor of PS II - Pheo phenophytin a - SPC single photon counting - PBQ phenyl-p-benzoquinone - DPC 1,5-diphenylcarbazide AFRC Photosynthesis Research Group, Department of Biochemistry