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.     

The origin of the split S3 EPR signal in Ca(2+)-depleted photosystem II: histidine versus tyrosine.

The radical formed as the formal S3 charge storage state in Ca(2+)-depleted photosystem II and detected as a split EPR signal was previously assigned to an oxidized histidine radical on the basis of its UV spectrum. In a recent paper [Hallahan, B. J., Nugent, J. H. A., Warden, J. T., & Evans, M. C. W. (1992) Biochemistry 31, 4562-4573], this assignment was challenged, and it was suggested that the signal arises instead from the well-known tyrosine radical Tyrz., the electron carrier between the photooxidized chlorophyll and the Mn cluster. Here, we provide evidence that the measurements of the Tyr., on which the new interpretation was based, are artifactual due to the use of saturating microwave powers. Other than a relaxation-enhancement effect, the formation of the split S3 signal is accompanied by no change in the Tyr. signal. Although essentially unrelated to the origin of the S3 radical, several other experimental and interpretational problems in the work of Hallahan et al. (1992) are pointed out and rationalized. For example, the inability of Hallahan et al. (1992) to observe the split S3 signal in samples containing DCMU or without a chelator, in contrast to our observations, is attributed to a number of technical problems including the incomplete inhibition of the enzyme. We thus conclude that the assignment of the split S3 signal as His., although not proven, remains the most reasonable on the basis of current data.     

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.     

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.     

The g = 2 multiline EPR signal of the S2 state of the photosynthetic oxygen-evolving complex originates from a ground spin state.

The amplitude of the g = 2 Mn 'multiline' EPR signal of the S2 state of the photosynthetic oxygen-evolving complex varies inversely with temperature, indicating that this signal arises from a ground spin state. Electron spin echo experiments at temperatures of 4.2 K and 1.4 K show such Curie-law behavior of the g = 2 multiline EPR signal, as do continuous-wave EPR experiments performed at a non-saturating microwave power in the range from 15.0 K to 4.2 K.     

Factors influencing the formation of modified S2 EPR signal and the S3 EPR signal in Ca(2+)-depleted photosystem II

NaCl/EGTA-washing of photosystem II (PS-II) results in the removal of Ca2+ and the inhibition of oxygen evolution. Two new EPR signals were observed in such samples: a stable and modified S2 multiline signal and an S3 signal [(1989) Biochemistry 28, 8984-8989]. Here, we report what factors are responsible for the modifications of the S2 signal and the observation of the S3 signal. The following results were obtained. (i) The stable, modified, S2 multiline signal can be induced by the addition of high concentrations of EGTA or citrate to PS-II membranes which are already inhibited by Ca(2+)-depletion. (ii) The carboxylic acids act in the S3-state, are much less effective in S2 and have no effect in the S1-state. (iii) The extrinsic polypeptides (17- and 23-kDa) are not required to observe either the modified S2 signal or the S3 signal. However, they do influence the splitting and the lifetime of the S3 signal, and they seem to have a slight influence on the hyperfine pattern of the S2 signal. (iv) The S3 signal can be observed in Ca(2+)-depleted PS-II which does not exhibit the modified multiline signal. Then, it is proposed that formation of histidine radical during the S2 to S3 transition in Ca(2+)-depleted PS-II [(1990) Nature 347, 303-306] also occurs in functional PS-II.     

Probing tyrosine Z oxidation in photosystem II core complex isolated from spinach by EPR at liquid helium temperatures

Tyrosine Z (Tyr_Z) oxidation observed at liquid helium temperatures provides new insights into the structure and function of Tyr_Z in active Photosystem II (PSII). However, it has not been reported in PSII core complex from higher plants. Here, we report Tyr_Z oxidation in the S₁ and S₂ states in PSII core complex from spinach for the first time. Moreover, we identified a 500 G-wide symmetric EPR signal (peak position g = 2.18, trough position g = 1.85) together with the g = 2.03 signal induced by visible light at 10 K in the S₁ state in the PSII core complex. These two signals decay with a similar rate in the dark and both disappear in the presence of 6% methanol. We tentatively assign this new feature to the hyperfine structure of the S₁Tyr_Z ^• EPR signal. Furthermore, EPR signals of the S₂ state of the Mn-cluster, the oxidation of the non-heme iron, and the S₁Tyr_Z ^• in PSII core complexes and PSII-enriched membranes from spinach are compared, which clearly indicate that both the donor and acceptor sides of the reaction center are undisturbed after the removal of LHCII. These results suggest that the new spinach PSII core complex is suitable for the electron transfer study of PSII at cryogenic temperatures.     

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.     

Orientation of the tetranuclear manganese cluster and tyrosine Z in the O(2)-evolving complex of photosystem II: An EPR study of the S(2)Y(Z)(*) state in oriented acetate-inhibited photosystem II membranes.

Inhibitory treatment by acetate, followed by illumination and rapid freezing, is known to trap the S(2)Y(Z)(*) state of the O(2)-evolving complex (OEC) in photosystem II (PS II). An EPR spectrum of this state exhibits broad split signals due to the interaction of the tyrosyl radical, Y(Z)(*), with the S = 1/2 S(2) state of the Mn(4) cluster. We present a novel approach to analyze S(2)Y(Z)(*) spectra of one-dimensionally (1-D) oriented acetate-inhibited PS II membranes to determine the magnitude and relative orientation of the S(2)Y(Z)(*) dipolar vector within the membrane. Although there exists a vast body of EPR data on isolated spins in oriented membrane sheets, the present study is the first of its kind on dipolar-coupled electron spin pairs in such systems. We demonstrate the feasibility of the technique and establish a rigorous treatment to account for the disorder present in partially oriented 1-D membrane preparations. We find that (i) the point-dipole distance between Y(Z)(*) and the Mn(4) cluster is 7.9 +/- 0.2 A, (ii) the angle between the interspin vector and the thylakoid membrane normal is 75 degrees, (iii) the g(z)()-axis of the Mn(4) cluster is 70 degrees away from the membrane normal and 35 degrees away from the interspin vector, and (iv) the exchange interaction between the two spins is -275 x 10(-)(4) cm(-)(1), which is antiferromagnetic. Due to the sensitivity of EPR line shapes of oriented spin-coupled pairs to the interspin distance, the present study imposes a tighter constraint on the Y(Z)-Mn(4) point-dipole distance than obtained from randomly oriented samples. The geometric constraints obtained from the 1-D oriented sample are combined with published models of the structure of Mn-depleted PS II to propose a location of the Mn(4) cluster. A structure in which Y(Z) is hydrogen bonded to a manganese-bound hydroxide ligand is consistent with available data and favors maximal orbital overlap between the two redox center that would facilitate direct electron- and proton-transfer steps.     

Electron spin-lattice relaxation studies of different forms of the S2 state multiline EPR signal of the Photosystem II oxygen-evolving complex

The pulsed EPR inversion recovery sequence has been utilized to monitor the temperature dependence of the electron spin-lattice relaxation rate of the Mn cluster of the Photosystem II oxygen evolving complex poised in a variety of S ₂ state forms giving rise to g = 2 multiline EPR signals. A previous study (Lorigan and Britt (1994) Biochemistry 33: 12072–12076) showed that for PS II membranes treated with 5% ethanol, the S ₂ state Mn cluster relaxes via the Orbach spin-lattice relaxation mechanism, where the relaxation is enhanced via phonon scattering off an excited state spin manifold, in this case at an energy of Δ = 36.5 cm⁻¹ above the S = 1/2 ground state giving rise to the multiline EPR signal. Parallel experiments are reported for PS II membranes with 5% methanol, treated with ammonia, and following short and long term dark adaptation. In each case, the temperature dependence of the electron spin-lattice relaxation rate is consistent with Orbach relaxation, and the range of excited state energies is relatively narrow (33.8 cm⁻¹ ≤ Δ ≤ 39.7 cm⁻¹). In addition, short term dark adapted (6 min, ‘active state’) PS II membranes show biphasic recovery traces which indicate that a minority fraction of the oxygen evolving complexes are trapped in a form with greatly slowed spin-lattice relaxation. This revised version was published online in June 2006 with corrections to the Cover Date.     

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 S(3) state of the oxygen-evolving complex in photosystem II is converted to the S(2)Y(Z)* state at alkaline pH

Here we report an EPR signal that is induced by a pH jump to alkaline pH in the S(3) state of the oxygen-evolving complex in photosystem II. The S(3) state is first formed with two flashes at pH 6. Thereafter, the pH is changed in the dark prior to freezing of the sample. The EPR signal is 90-100 G wide and centered around g = 2. The signal is reversibly induced with a pK = 8.5 +/- 0.3 and is very stable with a decay half-time of 5-6 min. If the pH is changed in the dark from pH 8.6 to 6.0, the signal disappears although the S(3) state remains. We propose that the signal arises from the interaction between the Mn cluster and Y(Z), resulting in the spin-coupled S(2)Y(Z)(*) signal. Our data suggest that the potential of the Y(Z)(*)/Y(Z) redox couple is sensitive to the ambient pH in the S(3) state. The alkaline pH decreases the potential of the Y(Z)(*)/Y(Z) couple so that Y(Z) can give back an electron to the S(3) state, thereby obtaining the S(2)Y(Z)(*) EPR signal. The tyrosine oxidation also involves proton release from Y(Z), and the results support a mechanism where this proton is released to the bulk medium presumably via a close-lying base. Thus, the equilibrium is changed from S(3)Y(Z) to S(2)Y(Z)(*) by the alkaline pH. At normal pH (pH 5.5-7), this equilibrium is set strongly to the S(3)Y(Z) state. The results are discussed in relation to the present models of water oxidation. Consequences for the relative redox potentials of Y(Z)(*)/Y(Z) and S(3)/S(2) at different pH values are discussed. We also compare the pH-induced S(2)Y(Z)(*) signal with the S(2)Y(Z)(*) signal from Ca(2+)-depleted photosystem II.     

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.     

Q-band EPR of the S2 state of photosystem II confirms an S = 5/2 origin of the X-band g = 4.1 signal

Disagreement has remained about the spin state origin of the g = 4.1 EPR signal observed at X-band (9 GHz) from the S2 oxidation state of the Mn cluster of Photosystem II. In this study, the S2 state of PSII-enriched membrane fragments was examined at Q-band (34 GHz), with special interest in low-field signals. Light-induced signals at g = 3.1 and g = 4.6 were observed. The intensity of the signal at g = 3.1 was enhanced by the presence of F- and suppressed by the presence of 5% ethanol, indicating that it was from the same spin system as the X-band signal at g = 4.1. The Q-band signal at g = 4.6 was also enhanced by F-, but not suppressed by 5% ethanol, making its identity less clear. Although it can be accounted for by the same spin system, other sources for the signal are considered. The observation of the signal at g = 3.1 agrees well with a previous study at 15.5 GHz, in which the X-band g = 4.1 signal was proposed to arise from the middle Kramers doublet of a near rhombic S = 5/2 system. Zero-field splitting values of D = 0.455 cm(-1) and E/D = 0.25 are used to simulate the spectra.     

Theoretical study of the multiline EPR signal from the S2 state of the oxygen evolving complex of photosystem II: Evidence for a magnetic tetramer

The Oxygen evolving complex of plant photosystem II is made of a manganese cluster that gives rise to a low temperature EPR multiline signal in the S₂ oxidation state. The origin of this EPR signal has been addressed with respect to the question of the magnetic couplings between the electron and nuclear spins of the four possible Mn ions that make up this complex. Considering Mn(III) and Mn(IV) as the only possible oxidation states present in the S₂ state, and no large anisotropy of the magnetic tensors, the breadths of the EPR spectra calculated for dimers and trimers with S = ½ have been compared with that of the biological site. It is concluded that neither a dinuclear nor a trinuclear complex made of Mn(III) and Mn(IV) can be responsible for the multiline signal; but that, by contrast, a tetranuclear Mn complex can be the origin of this signal. The general shape of the experimental spectrum, its particular hyperfine pattern, the positions of most of the hyperfine lines and their relative intensities can be fit by a tetramer model described by the following six fitting parameters: g ≈ 1.987, A₁ ≈ 122.4 10^-4 cm^-1, A₂ ≈ 87.2 10^-4 cm^-1, A₃ ≈ 81.6 10^-4 cm^-1, A₄ ≈ 19.1 10^-4 cm^-1 and δH = 24.5 G. A second model described by parameters very close to those given above except for A₄ ≈ 77.5 10^-4 cm^-1 gives an equally good fit. However, no other set of parameters gives an EPR spectrum that reproduces the hyperfine pattern of the S₂ multiline signal. This demonstrates that in the S₂ state of the oxygen evolving complex, the four manganese ions are organized in a magnetic tetramer.     

Multifrequency EPR investigations into the origin of the S2-state signal at g = 4 of the O2-evolving complex.

The low-temperature S2-state EPR signal at g = 4 from the oxygen-evolving complex (OEC) of spinach Photosystem-II-enriched membranes is examined at three frequencies, 4 GHz (S-band), 9 GHz (X-band) and 16 GHz (P-band). While no hyperfine structure is observed at 4 GHz, the signal shows little narrowing and may mask underlying hyperfine structure. At 16 GHz, the signal shows g-anisotropy and a shift in g-components. The middle Kramers doublet of a near rhombic S = 5/2 system is found to be the only possible origin consistent with the frequency dependence of the signal. Computer simulations incorporating underlying hyperfine structure from an Mn monomer or dimer are employed to characterize the system. The low zero field splitting (ZFS) of D = 0.43 cm-1 and near rhombicity of E/D = 0.25 lead to the observed X-band g value of 4.1. Treatment with F- or NH3, which compete with Cl- for a binding site, increases the ZFS and rhombicity of the signal. These results indicate that the origin of the OEC signal at g = 4 is either an Mn(II) monomer or a coupled Mn multimer. The likelihood of a multimer is favored over that of a monomer.     

The EPR spectrum of tyrosine Z* and its decay kinetics in O2-evolving photosystem II preparations

The O2-evolving complex of photosystem II, Mn 4Ca, cycles through five oxidation states, S0,..., S4, during its catalytic function, which involves the gradual abstraction of four electrons and four protons from two bound water molecules. The direct oxidant of the complex is the tyrosine neutral radical, YZ(*), which is transiently produced by the highly oxidizing power of the photoexcited chlorophyll species P680. EPR characterization of YZ(*) has been limited, until recently, to inhibited (non-oxygen-evolving) preparations. A number of relatively recent papers have demonstrated the trapping of YZ(*) in O2-evolving preparations at liquid helium temperatures as an intermediate of the S0 to S1, S1 to S2, and S2 to S3 transitions. The respective EPR spectra are broadened and split at g approximately 2 by the magnetic interaction with the Mn cluster, but this interaction collapses at temperatures higher than about 100K [Zahariou et al. (2007) Biochemistry 46, 14335 -14341]. We have conducted a study of the Tyr Z(*) transient in the temperature range 77-240 K by employing rapid or slow EPR scans. The results reveal for the first time high-resolution X-band spectra of Tyr Z(*) in the functional system and at temperatures close to the onset of the S-state transitions. We have simulated the S 2Y Z(*) spectrum using the simulation algorithm of Svistunenko and Cooper [(2004) Biophys. J. 87, 582 -595]. The small g(x) = 2.00689 value inferred from the analysis suggests either a H-bonding of Tyr Z (*) (presumably with His190) that is stronger than what has been assumed from studies of Tyr D(*) or Tyr Z(*) in Mn-depleted preparations or a more electropositive environment around Tyr Z(*). The study has also yielded for the first time direct information on the temperature variation of the YZ(*)/QA(-) recombination reaction in the various S states. The reaction follows biphasic kinetics with the slow phase dominating at low temperatures and the fast phase dominating at high temperatures. It is tentatively proposed that the slow phase represents the action of the YZ(*)/YZ(-) redox couple while the fast phase represents that of the YZ(*)/YZH couple; it is inferred that Tyr Z at elevated temperatures is protonated at rest. It is also proposed that YZ(*)/YZH is the couple that oxidizes the Mn cluster during the S1-S2 and S2-S3 transitions. A simple mechanism ensuring a rapid (concerted) protonation of Tyr Z upon oxidation of the Mn cluster is discussed, and also, a structure-based molecular model suggesting the participation of His190 into two hydrogen bonds is proposed.     

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...     

Assignment of the g = 4.1 EPR signal to manganese in the S2 state of the photosynthetic oxygen-evolving complex: an X-ray absorption edge spectroscopy study

X-ray absorption spectroscopy at the Mn K-edge has been utilized to study the origin of the g = 4.1 EPR signal associated with the Mn-containing photosynthetic O2-evolving complex. Formation of the g = 4.1 signal by illumination of Photosystem II preparations at 140 K is associated with a shift of the Mn edge inflection point to higher energy. This shift is similar to that observed upon formation of the S2 multiline EPR signal by 190 K illumination. The g = 4.1 signal is assigned to the Mn complex in the S2 state.     

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.