Inhomogeneity of the EPR multiline signal from the S2-state of the photosystem II oxygen-evolving enzyme

The manganese complex (Mn₄) which is responsible for water oxidation in photosystem II is EPR detectable in the S₂-state, one of the five redox states of the enzyme cycle. The S₂-state is observable at 10?K either as an EPR multiline signal (spin S?=?1/2) or as a signal at g?=?4.1 (spin S?=?3/2 or 5/2). It has recently been shown that the state responsible for the multiline signal is converted to that responsible for the g?=?4.1 signal upon the absorption of near-infrared light [Boussac A, Girerd J-J, Rutherford AW (1996) Biochemistry 35?:?6984–6989]. It is shown here that the yield of the spin interconversion may be variable and depends on the photosystem II (PSII) preparations. The EPR multiline signal detected after near-infrared illumination, and which originates from PSII centers not susceptible to the near-infrared light, is shown to be different from that which originates from infrared-susceptible PSII centers. The total S₂-multiline signal results from the superposition of the two multiline signals which originate from these two PSII populations. One S₂ population gives rise to a "narrow" multiline signal characterized by strong central lines and weak outer lines. The second population gives rise to a "broad" multiline signal in which the intensity of the outer lines, at low and high field, are proportionally larger than those in the narrow multiline signal. The larger the relative amplitude of the outer lines at low and high field, the higher is the proportion of the near-infrared-susceptible PSII centers and the yield of the multiline to g?=?4.1 signal conversion. This inhomogeneity of the EPR multiline signal is briefly discussed in terms of the structural properties of the Mn₄ complex.     

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.     

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.     

S1-state model of the O2-evolving complex of photosystem II

We introduce a quantum mechanics/molecular mechanics model of the oxygen-evolving complex of photosystem II in the S(1) Mn(4)(IV,III,IV,III) state, where Ca(2+) is bridged to manganese centers by the carboxylate moieties of D170 and A344 on the basis of the new X-ray diffraction (XRD) model recently reported at 1.9 ? resolution. The model is also consistent with high-resolution spectroscopic data, including polarized extended X-ray absorption fine structure data of oriented single crystals. Our results provide refined intermetallic distances within the Mn cluster and suggest that the XRD model most likely corresponds to a mixture of oxidation states, including species more reduced than those observed in the catalytic cycle of water splitting.     

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⁺.     

Recent pulsed EPR studies of the photosystem II oxygen-evolving complex: implications as to water oxidation mechanisms

The pulsed electron paramagnetic resonance (EPR) methods of electron spin echo envelope modulation (ESEEM) and electron spin echo-electron nuclear double resonance (ESE-ENDOR) are used to investigate the structure of the Photosystem II oxygen-evolving complex (OEC), including the paramagnetic manganese cluster and its immediate surroundings. Recent unpublished results from the pulsed EPR laboratory at UC-Davis are discussed, along with aspects of recent publications, with a focus on substrate and cofactor interactions. New data on the proximity of exchangeable deuterons around the Mn cluster poised in the S(0)-state are presented and interpreted. These pulsed EPR results are used in an evaluation of several recently proposed mechanisms for PSII water oxidation. We strongly favor mechanistic models where the substrate waters bind within the OEC early in the S-state cycle. Models in which the O-O bond is formed by a nucleophilic attack by a Ca(2+)-bound water on a strong S(4)-state electrophile provide a good match to the pulsed EPR data.     

EPR characterization of an oxygen-evolving photosystem II preparation from the transformable cyanobacterium Synechocystis 6803.

The transformable cyanobacterium Synechocystis 6803 has a photosynthetic apparatus that is similar to that of plants. Because of the ease with which this organism can be genetically manipulated and isotopically labeled, Synechocystis has been used extensively in recent studies of electron transfer in the water-splitting complex, photosystem II. Here, we present the first EPR characterization of a highly active oxygen-evolving preparation from this organism. This preparation shows oxygen-evolution activities in the range from 2400-2600 mumol of O2/(mg of chlorophyll.h). We show that this preparation is stable enough for room temperature EPR studies. We then use this assay to show that the lineshapes of the D+ and Z+ tyrosine radicals are identical in this preparation, as has been observed in photosystem II complexes from a wide variety of photosynthetic species. We also present the first multiline EPR spectrum that has been observed from the Synechocystis manganese cluster.     

The EPR signals from the S0 and S2 states of the Mn cluster in photosystem II relax differently

The oxygen evolving complex (OEC) of photosystem II (PSII) gives rise to manganese-derived electron paramagnetic resonance (EPR) signals in the S0 and S2 oxidation states. These signals exhibit different microwave power saturation behavior between 4 and 10 K. Below 8 K, the S0 state EPR signal is a faster relaxer than the S2 multiline signal, but above 8 K, the S0 signal is the slower relaxer of the two. The different temperature dependencies of the relaxation of the S0 and S2 ground-state Mn signals are due to differences in the spin-lattice relaxation process. The dominating spin-lattice relaxation mechanism is concluded to be a Raman mechanism in the S0 state, with a T(4.1) temperature dependence of the relaxation rate. It is proposed that the relaxation of the S2 state arises from a Raman mechanism as well, with a T(6.8) temperature dependence of the relaxation rate, although the data also fit an Orbach process. If both signals relax through a Raman mechanism, the different exponents are proposed to reflect structural differences in the proteins surrounding the Mn cluster between the S0 and S2 states. The saturation of SII(slow) from the Y(D)(ox) radical on the D2 protein was also studied, and found to vary between the S0 and the S2 states of the enzyme in a manner similar to the EPR signals from the OEC. Furthermore, we found that the S2 multiline signal in the second turnover of the enzyme is significantly more difficult to saturate than in the first turnover. This suggests differences in the OEC between the first and second cycles of the enzyme. The increased relaxation rate may be caused by the appearance of a relaxation enhancer, or it may be due to subtle structural changes as the OEC is brought into an active state.     

Comparative study of the g=4.1 EPR signals in the S(2) state of photosystem II

The Mn(4) complex which is involved in water oxidation in photosystem II is known to exhibit three types of EPR signals in the S(2) state, one of the five redox states of the enzyme cycle: a multiline signal (spin 1/2), signals at g5 (spin 5/2) and a signal at g=4.1 (or g=4.25). The g=4.1 signal could be generated under two distinct sets of conditions: either by illumination at room temperature or at 200 K in certain experimental conditions (g4(S) signal) or by near-infrared illumination between approximately 77 and approximately 160 K of the S(2)-multiline state (g4(IR) signal). The two g=4.1 signals arise from states which have quite different stability in terms of temperature. In the present work we have compared these two signals in order to test if they originate from the same or from different chemical origins. The microwave power saturation properties of the two signals measured at 4.2 K were found to be virtually identical. Their temperature dependencies measured at non-saturating powers were also identical. The presence of Curie law behavior for the g4(S) and g4(IR) signals indicates that the states responsible for both signals are ground states. The orientation dependence, anisotropy and resolved hyperfine structure of the two g4 signals were also found to be virtually indistinguishable. We have been unable to confirm the behavior reported earlier indicating that the g4(S) signal is an excited state, nor were we able to confirm the presence of signal from a higher excited state in samples containing the g4(S), nor a radical signal in samples containing the g4(IR). These findings are best interpreted assuming that the two signals have a common origin i.e. a spin 5/2 ground state arising from a magnetically coupled Mn-cluster of 4 Mn ions.     

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.     

Investigation of the origin of the "S3" EPR signal from the oxygen-evolving complex of photosystem 2: the role of tyrosine Z.

The origin of the "S3" EPR signal from calcium-depleted photosystem 2 samples has been investigated. This signal is observed after freezing samples under illumination and has been assigned to an interaction between the manganese cluster and an oxidized histidine radical [Boussac et al. (1990) Nature 347; 303-306]. In calcium-depleted samples prepared by three different methods, we observed the trapping of the tyrosine radical YZ+ under conditions which also formed the "S3" signal. An "S3"-type signal and YZ+ were also formed in PS2 samples treated with the water analogue ammonia. Following illumination at 277 K, the "S3" and YZ+ signals decayed at the same rate at 273 K in the dark. Both the YZ+ and "S3" signals decayed on storage at 77 K and could be subsequently regenerated by illumination at 8-77 K. No evidence to support histidine oxidation was found. The effects of DCMU, chelators, and alkaline pH on the dark-stable multiline S2 and the "S3" signals from calcium-depleted samples were determined. Both signals required the presence of EGTA or citrate for maximum yield. The addition of DCMU caused a reduction in the yield of "S3" generated by freezing under illumination. Incubation at pH 7.5 resulted in the loss of both signals. We propose that a variety of treatments which affect calcium and chloride binding cause a stabilization of the S2 state and slow the reduction of YZ+. This allows the trapping of YZ+, the interaction with the manganese cluster (probably in the S2 state) resulting in the "S3" signal. The data allow the position of the manganese cluster to be estimated as within 10 A of tyrosine Z (D1-161).     

EPR study of the oxygen evolving complex in His-tagged photosystem II from the cyanobacterium Synechococcus elongatus

The Mn(4)-cluster and the cytochrome c(550) in histidine-tagged photosystem II (PSII) from Synechococcus elongatus were studied using electron paramagnetic resonance (EPR) spectroscopy. The EPR signals associated with the S(0)-state (spin = 1/2) and the S(2)-state (spin = 1/2 and IR-induced spin = 5/2 state) were essentially identical to those detected in the non-His-tagged strain. The EPR signals from the S(3)-state, not previously reported in cyanobacteria, were detectable both using perpendicular (at g = 10) and parallel (at g = 14) polarization EPR, and these signals are similar to those found in plant PSII. In the S(3)-state, near-infrared illumination at 50 K induced a 176-G-wide split signal at g = 2 and signals at g = 5.20 and g = 1.51. These signals differ slightly from those reported in plant PSII [Ioannidis, N., and Petrouleas, V. (2000) Biochemistry 39, 5246-5254]. In accordance with the cited work, the split signal presumably reflects a radical interacting with the Mn(4)-cluster in a fraction of centers, while the g = 5.20 and g = 1.51 signals are tentatively attributed to a high-spin state of the Mn(4)-cluster with zero field splitting parameters different from those in plant PSII, reflecting minor changes in the environment of the Mn(4)-cluster. Biochemical modifications (Sr(2+)/Ca(2+) substitution, acetate and NH(3) treatments) were also investigated. In Sr(2+)-reconstituted PSII, in addition to the expected modified S(2) multiline signal, a signal at g = 5.2 was present instead of the g approximately 4 signal seen in plant PSII. In NH(3)-treated samples, in addition to the expected modified S(2)-multiline signal, a g approximately 4 signal was detected in a small proportion of the reaction centers. This is of note since g approximately 4 spectra arising from the Mn(4)-cluster in the S(2) state have not yet been published in cyanobacterial PSII. The detection of modified S(3)-signals in both perpendicular (at g = 7.5) and parallel (at g = 12) polarization EPR from NH(3)-treated PSII indicate that NH(3) is still bound in the S(3)-state. The acetate-treated PSII behaves essentially as in plant PSII. A study using oriented samples indicated that the heme plane of the oxidized low spin Cytc(550) was perpendicular to the plane of the membrane.     

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.     

Calcium EXAFS establishes the Mn-Ca cluster in the oxygen-evolving complex of photosystem II

The proximity of Ca to the Mn cluster of the photosynthetic water-oxidation complex is demonstrated by X-ray absorption spectroscopy. We have collected EXAFS data at the Ca K-edge using active PS II membrane samples that contain approximately 2 Ca per 4 Mn. These samples are much less perturbed than previously investigated Sr-substituted samples, which were prepared after Ca depletion. The new Ca EXAFS clearly shows backscattering from Mn at 3.4 A, a distance that agrees with that surmised from previously recorded Mn EXAFS. This result is also consistent with earlier related experiments at the Sr K-edge, using samples that contained functional Sr, that show Mn is approximately 3.5 A distant from Sr. The totality of the evidence clearly advances the notion that the catalytic center of oxygen evolution is a Mn-Ca heteronuclear 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.     

Spectral resolution of the split EPR signals induced by illumination at 5 K from the S1, S3, and S0 states in photosystem II

S-State-dependent split EPR signals that are induced by illumination at cryogenic temperatures (5 K) have been measured in spinach photosystem II without interference from the Y(D)* radical in the g approximately 2 region. This allows us to present the first decay-associated spectra for the split signals, which originate from the CaMn4 cluster in magnetic interaction with a nearby radical, presumably Y(Z)*. The three split EPR signals that were investigated, "Split S1", "Split S3", and Split S0", all exhibit spectral features at g approximately 2.0 together with surrounding characteristic peaks and troughs. From microwave relaxation studies we can reach conclusions about which parts of the complex spectra belong together. Our analysis strongly indicates that the wings and the middle part of the split spectrum are parts of the same signal, since their decay kinetics in the dark at 5 K and microwave relaxation behavior are indistinguishable. In addition, our decay-associated spectra indicate that the g approximately 2.0 part of the "Split S1" EPR spectrum contains a contribution from magnetically uncoupled Y(Z)* as judged from the g value and 22 G line width of the EPR signal. The g value, 2.0033-2.0040, suggests that the oxidation of Y(Z) at 5 K results in a partially protonated radical. Irrespective of the S state, a small amount of a carotenoid or chlorophyll radical was formed by the illumination. However, this had relaxation and decay characteristics that clearly distinguish this radical from the split signal spectra. In this paper, we present the "clean" spectra from the low-temperature illumination-induced split EPR signals from higher plants, which will provide the basis for further simulation studies.     

Formation and flash-dependent oscillation of the S2-state multiline EPR signal in an oxygen-evolving Photosystem-II preparation lacking the three extrinsic proteins in the oxygen-evolving system

In PS-II-enriched membranes lacking the three extrinsic water-soluble proteins in the oxygen-evolving system (18, 24 and 33 kDa), but still evolving oxygen to some extent, the formation of the multiline EPR signal originating from the S₂-state is dependent on the concentration of Cl⁻. In 200 mM Cl⁻ the multiline signal was observed after the first flash and oscillated with the flash number with a period of four. At 20 mM Cl⁻ no signal could be observed in this material. These results suggest that the extrinsic proteins are not necessary for multiline signal formation and that complete advancement through the S-states can occur in their absence when sufficient Cl⁻ is present.     

The two substrate-water molecules are already bound to the oxygen-evolving complex in the S2 state of photosystem II

The first direct evidence which shows that both substrate-water molecules are bound to the O(2)-evolving catalytic site in the S(2) state of photosystem II (PSII) is presented. Rapid (18)O isotope exchange measurements between H(2)(18)O incubated in the S(2) state of PSII-enriched membrane samples and the photogenerated O(2) reveal a fast and a slow phase of exchange at m/e 34 (which measures the level of the (16)O(18)O product). The rate constant for the slow phase of exchange ((34)k(1)) equals 1.9 +/- 0.3 s(-1) at 10 degrees C, while the fast phase of exchange is unresolved by our current experimental setup ((34)k(2) >or= 175 s(-1)). The unresolvable fast phase has left open the possibility that the second substrate-water molecule binds to the catalytic site only after the formation of the S(3) state [Hillier, W., and Wydrzynski, T. (2000) Biochemistry 39, 4399-4405]. However, for PSII samples depleted of the 17 and 23 kDa extrinsic proteins (Ex-depleted PSII), two completely resolvable phases of (18)O exchange are observed in the S(2) state of the residual activity, with the following rate constants: (34)k(1) = 2.6 +/- 0.3 s(-1) and (34)k(2) = 120 +/- 14 s(-1) at 10 degrees C. Upon addition of 15 mM CaCl(2) to Ex-depleted PSII, the O(2) evolution activity increases to approximately 80% of the control level, while the two resolvable phases of exchange remain the same. In measurements of Ex-depleted PSII at m/e 36 (which measures the level of the (18)O(18)O product), only a single phase of exchange is observed in the S(2) state, with a rate constant ((36)k(1) = 2.5 +/- 0.2 s(-1)) that is identical to the slow rate of exchange in the m/e 34 data. Taken together, these results show that the fast phase of (18)O exchange is specifically slowed by the removal of the 17 and 23 kDa extrinsic proteins and that the two substrate-water molecules must be bound to independent sites already in the S(2) state. In contrast, the (18)O exchange behavior in the S(1) state of Ex-depleted PSII is no different from what is observed for the control, with or without the addition of CaCl(2). Since the fast phase of exchange in the S(1) state is unresolved (i.e., (34)k(2) > 100 s(-1)), the possibility remains that the second substrate-water molecule binds to the catalytic site only after the formation of the S(2) state. The role of the 17 and 23 kDa extrinsic proteins in establishing an asymmetric dielectric environment around the substrate binding sites is discussed.     

Formation spectra of the EPR split signals from the S0, S1, and S3 states in photosystem II induced by monochromatic light at 5 K

The interaction EPR split signals from photosystem II (PSII) have been reported from the S0, S1, and S3 states. The signals are induced by illumination at cryogenic temperatures and are proposed to reflect the magnetic interaction between YZ* and the Mn4Ca cluster. We have investigated the formation spectra of these split EPR signals induced in PSII enriched membranes at 5 K using monochromatic laser light from 400 to 900 nm. We found that the formation spectra of the split S0, split S1, and split S3 EPR signals were quite similar, but not identical, between 400 and 690 nm, with maximum formation at 550 nm. The major deviations were found between 440 and 480 nm and between 580 and 680 nm. In the regions around 460 and 680 nm the amplitudes of the formation spectra were 25-50% of that at 550 nm. A similar formation spectrum was found for the S2-state multiline EPR signal induced at 0 degrees C. In general, the formation spectra of these signals in the visible region resemble the reciprocal of the absorption spectra of our PSII membranes. This reflects the high chlorophyll concentration necessary for the EPR measurements which mask the spectral properties of other absorbing species. No split signal formation was found by the application of infrared laser illumination between 730 and 900 nm from PSII in the S0 and S1 states. However, when such illumination was applied to PSII membranes poised in the S3 state, formation of the split S3 EPR signal was observed with maximum formation at 740 nm. The quantum yield was much less than in the visible region, but the application of intensive illumination at 830 nm resulted in accumulation of the signal to an amplitude comparable to that obtained with illumination with visible light. The split S3 EPR signal induced by NIR light was much more stable at 5 K (no observable decay within 60 min) than the split S3 signal induced by visible light (50% of the signal decayed within 30 min). The split S3 signals induced by each of these light regimes showed the same EPR spectral features and microwave power saturation properties, indicating that illumination of PSII in the S3 state by visible light or by NIR light produces a similar configuration of YZ* and the Mn4Ca cluster.     

Glycerol binding at the narrow channel of photosystem II stabilizes the low-spin S2 state of the oxygen-evolving complex

Photosynthesis Research - The oxygen-evolving complex (OEC) of photosystem II (PSII) cycles through redox intermediate states Si (i?=?0–4) during the photochemical oxidation of...