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.     

Effects of lanthanide substitution at Ca2+-site on the properties of the oxygen evolving center of photosystem II

Functional calcium present in a photosynthetic oxygen evolving center (OEC) was replaced by lanthanides. To this end, sample membranes depleted of Ca2+ as well as 16 and 24 kDa extrinsic proteins were prepared and the effects of lanthanides substitution on OEC were studied. The lanthanides inhibited Ca2+-dependent restoration of oxygen evolution but the presence of Ca2+ during the treatment protected OEC from this inhibition, which occurred within 1 min at 20 degrees C but required much longer time at 0 degrees C. Kinetic analysis suggests that lanthanides function as a mixed-type competitor for Ca2+. Lanthanides with ionic radii smaller than Ca2+ show higher affinity for the Ca2+ site than those with larger radii. A lanthanide-substituted OEC displayed a thermoluminescence (TL) band arising from S2Q(A)- charge recombination, indicating that the Mn cluster is oxidized to the S2 state. However, the peak temperature of the TL band varied depending on lanthanide species. The results indicate that the oxidation potential of the Mn cluster is modified in various ways in a substituted OEC. Furthermore, the threshold temperature for the S1 to S2 transition in the lanthanide-substituted OEC was markedly upshifted to the temperature coincident with that found in Ca2+-depleted but 24 kDa protein preserved OEC. Changes in the OEC induced by the binding of lanthanides to the Ca2+-site are discussed based on these results.     

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.     

The origin of split EPR signals in the Ca2+-depleted Photosystem II

A light-driven reaction model for the Ca²⁺-depleted Photosystem (PS) II is proposed to explain the split signal observed in electron paramagnetic resonance (EPR) spectra based on a comparison of EPR assignments with recent x-ray structural data. The split signal has a splitting linewidth of 160 G at around g = 2 and is seen upon illumination of the Ca²⁺-depleted PS II in the S₂ state associated with complete or partial disappearance of the S₂ state multiline signal. Another g=2 broad ESR signal with a 110 G linewidth was produced by 245 K illumination for a short period in the Ca²⁺-depleted PS II in S₁ state. At the same time a normal Y_Z^· radical signal was also efficiently trapped. The g=2 broad signal is attributed to an intermediate S₁X^· state in equilibrium with the trapped Y_Z^· radical. Comparison with x-ray structural data suggests that one of the split signals (doublet signal) is attributable to interaction between His 190 and the Y_Z^· radical, and other signals is attributable to interaction between His 337 and the manganese cluster, providing further clues as to the mechanism of water oxidation in photosynthetic oxygen evolution.     

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.     

Biosynthetic Ca2+/Sr2+ exchange in the photosystem II oxygen-evolving enzyme of Thermosynechococcus elongatus

The thermophilic cyanobacterium, Thermosynechococcus elongatus, has been grown in the presence of Sr2+ instead of Ca2+ with the aim of biosynthetically replacing the Ca2+ of the oxygen-evolving enzyme with Sr2+. Not only were the cells able to grow normally with Sr2+, they actively accumulated the ion to levels higher than those of Ca2+ in the normal cultures. A protocol was developed to purify a fully active Sr(2+)-containing photosystem II (PSII). The modified enzyme contained a normal polypeptide profile and 1 strontium/4 manganese, indicating that the normal enzyme contains 1 calcium/4 manganese. The Sr(2+)- and Ca(2+)-containing enzymes were compared using EPR spectroscopy, UV-visible absorption spectroscopy, and O2 polarography. The Ca2+/Sr2+ exchange resulted in the modification of the EPR spectrum of the manganese cluster and a slower turnover of the redox cycle (the so-called S-state cycle), resulting in diminished O2 evolution activity under continuous saturating light: all features reported previously by biochemical Ca2+/Sr2+ exchange in plant PSII. This allays doubts that these changes could be because of secondary effects induced by the biochemical treatments themselves. In addition, the Sr(2+)-containing PSII has other kinetics modifications: 1) it has an increased stability of the S3 redox state; 2) it shows an increase in the rate of electron donation from TyrD, the redox-active tyrosine of the D2 protein, to the oxygen-evolving complex in the S3-state forming S2; 3) the rate of oxidation of the S0-state to the S1-state by TyrD* is increased; and 4) the release of O2 is slowed down to an extent similar to that seen for the slowdown of the S3TyrZ* to S0TyrZ transition, consistent with the latter constituting the limiting step of the water oxidation mechanism in Sr(2+)-substituted enzyme as well as in the normal enzyme. The replacement of Ca2+ by Sr2+ appears to have multiple effects on kinetics properties of the enzyme that may be explained by S-state-dependent shifts in the redox properties of both the manganese complex and TyrZ as well as structural effects.     

Reconstitution of the photosystem II Ca2+ binding site

The roles of Ca(2+) in H(2)O oxidation may be as a site of substrate binding, and as a structural component of the photosystem II O(2)-evolving complex. One indication of this dual role of the metal is revealed by probing the Mn cluster in the Ca(2+) depleted O(2) evolving complex that retains extrinsic 23- and 17-kDa polypeptides with reductants (NH(2)OH and hydroquinone) [Biochemistry 41 (2002) 958]. Calcium appears to bind to photosystem II at a site where it could bind substrate H(2)O. Equilibration of Ca(2+) with this binding site is facilitated by increased ionic strength, and incubation of Ca(2+) reconstitution mixtures at 22 degrees C accelerates equilibration of Ca(2+) with the site. The Ca(2+) reconstituted enzyme system regains properties of unperturbed photosystem II: Sensitivity to NH(2)OH inhibition is decreased, and Cl(-) binding with increased affinity can be detected. The ability of ionic strength and temperature to facilitate rebinding of Ca(2+) to the intact O(2) evolving complex suggests that the structural environment of the oxidizing side of photosystem II may be flexible, rather than rigid.     

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.     

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.     

Relative stability of the S2 isomers of the oxygen evolving complex of photosystem II

Photosynthesis Research - The oxidation of water to O2 is catalyzed by the Oxygen Evolving Complex (OEC), a Mn4CaO5 complex in Photosystem II (PSII). The OEC is sequentially oxidized from state S0...     

Ca2+-controlled conformational states of the Ca2+ transport enzyme of sarcoplasmic reticulum.

The fluorescent reagent, S-mercuric N-dansyl-cysteine, reacts specifically with thiols of the purified Ca2+-ATPase of the sarcoplasmic reticulum, producing an increase of fluorescence of fluorescence intensity at 500 nm (lambda ex = 335 nm). The reaction is stoichiometric, and the increase of the fluorescence intensity is proportional to the number of blocked thiols. Twelve reactive thiols per 10(5) daltons of ATPase peptide fall into roughly three classes. Blocking of the most reactive thiol entails little inhibition of enzyme activity. Blocking of the five thiols reacting next (intermediate class) results in almost complete inhibition of both phosphorylated intermediate formation and ATP hydrolysis. The second order rate constants of the reaction of thiols have been determined by stopped flow studies. The most reactive thiol and the six least reactive thiols can each be treated as a single class with respect to the rate constant; five thiols of intermediate reactivity appear to have different rate constants (k2, k3, ..k6). Of these constants, k1, corresponding to the most reactive thiol, does not change with [Ca2+]. Upon increasing [Ca2+] from 10(-9) to 10(-5) M, k2 increase and k7-12 decreases; the changes roughly parallel the activation of ATPase activity and the Ca2+ binding to the high affinity alpha sites (Ikemoto, N. (1975) J. Biol. Chem. 250, 7219-7224). Upon further increase of [Ca2+] k2 decreases and k7-12 increase, in parallel with the inhibition of ATPase activity and with the Ca2+ binding to the low affinity gamma sites.     

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.     

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.     

pH dependence of the donor side reactions in Ca2+-depleted photosystem II

We have studied how low pH affects the water-oxidizing complex in Photosystem II when depleted of the essential Ca(2+) ion cofactor. For these samples, it was found that the EPR signal from the Y(Z)(*) radical decays faster at low pH than at high pH. At 20 degrees C, Y(Z)(*) decays with biphasic kinetics. At pH 6.5, the fast phase encompasses about 65% of the amplitude and has a lifetime of approximately 0.8 s, while the slow phase has a lifetime of approximately 22 s. At pH 3.9, the kinetics become totally dominated by the fast phase, with more than 90% of the signal intensity operating with a lifetime of approximately 0.3 s. The kinetic changes occurred with an approximate pK(a) of 4.5. Low pH also affected the induction of the so-called split radical EPR signal from the S(2)Y(Z)(*) state that is induced in Ca(2+)-depleted PSII membranes because of an inability of Y(Z)(*) to oxidize the S(2) state. At pH 4.5, about 50% of the split signal was induced, as compared to the amplitude of the signal that was induced at pH 6.5-7, using similar illumination conditions. Thus, the split-signal induction decreased with an apparent pK(a) of 4.5. In the same samples, the stable multiline signal from the S(2) state, which is modified by the removal of Ca(2+), was decreased by the illumination to the same extent at all pHs. It is proposed that decreased induction of the S(2)Y(Z)(*) state at lower pH was not due to inability to oxidize the modified S(2) state induced by the Ca(2+) depletion. Instead, we propose that the low pH makes Y(Z)(*) able to oxidize the S(2) state, making the S(2) --> S(3) transition available in Ca(2+)-depleted PSII. Implications of these results for the catalytic role of Ca(2+) and the role of proton transfer between the Mn cluster and Y(Z) during oxygen evolution is discussed.     

Effects of pH on the S(3) state of the oxygen evolving complex in photosystem II probed by EPR split signal induction

The electrons extracted from the CaMn(4) cluster during water oxidation in photosystem II are transferred to P(680)(+) via the redox-active tyrosine D1-Tyr161 (Y(Z)). Upon Y(Z) oxidation a proton moves in a hydrogen bond toward D1-His190 (His(Z)). The deprotonation and reprotonation mechanism of Y(Z)-OH/Y(Z)-O is of key importance for the catalytic turnover of photosystem II. By light illumination at liquid helium temperatures (～5 K) Y(Z) can be oxidized to its neutral radical, Y(Z)(?). This can be followed by the induction of a split EPR signal from Y(Z)(?) in a magnetic interaction with the CaMn(4) cluster, offering a way to probe for Y(Z) oxidation in active photosystem II. In the S(3) state, light in the near-infrared region induces the split S(3) EPR signal, S(2)'Y(Z)(?). Here we report on the pH dependence for the induction of S(2)'Y(Z)(?) between pH 4.0 and pH 8.7. At acidic pH the split S(3) EPR signal decreases with the apparent pK(a) (pK(app)) ～ 4.1. This can be correlated to a titration event that disrupts the essential H-bond in the Y(Z)-His(Z) motif. At alkaline pH, the split S(3) EPR signal decreases with the pK(app) ～ 7.5. The analysis of this pH dependence is complicated by the presence of an alkaline-induced split EPR signal (pK(app) ～ 8.3) promoted by a change in the redox potential of Y(Z). Our results allow dissection of the proton-coupled electron transfer reactions in the S(3) state and provide further evidence that the radical involved in the split EPR signals is indeed Y(Z)(?).     

Reactivation of oxygen accumulation function after complete removal of manganese from the photosystem II particles

Reactivation of 02 evolution function has been studied in PS-2 particles after complete removal of Mn and water soluble 10, 17, 24, 33 kDa proteins, It has been shown that 02 evolution function in such particles can be reactivated by adding 5 μM Mn2 and 20 mM Ca2(+). Preliminary illumination of the sample is necessary to exhibit the reactivation effect of 02 evolution. The maximum value of the reactivation of 02 evolution rate is about 60% of the control. Upon illumination of the reactivated particles with flashes of 1s duration and at a frequency of 0,1 Hz, 02 evolution occurs according to the mechanism analogous to that in the initial parties of PS 2. Thus the reactivation of water oxidation and 02 evolution after complete removal of Mn and water soluble 10, 17, 24, 33 kDa proteins resulting in the suppression of 02 evolution function has been shown for the first time and it can serve as a basic approach for profound investigation of the mechanism of photosynthetic water oxidation.     

Interaction and inhibitory effect of ammonium cation in the oxygen evolving center of photosystem II

Photosynthetic O(2) evolution takes place at the Mn cluster in photosystem II (PSII) by oxidation of water. It has been proposed that ammonia, one of water analogues, functions as an inhibitor of O(2) evolution at alkaline pH. However, the detailed mechanism of inhibition has not been understood yet. In this study, we investigated the mechanism of ammonia inhibition by examining the NH(4)Cl-induced inhibition of O(2) evolution in a wide pH range (pH 5.0-8.0) and by detecting the interaction site using Fourier transform infrared (FTIR) spectroscopy. In addition to intact PSII membranes from spinach, PSII membranes depleted of the PsbP and PsbQ extrinsic proteins were used as samples to avoid the effect of the release of these proteins by salt treatments. In both types of samples, oxygen evolution activity decreased by approximately 40% by addition of 100 mM NH(4)Cl in the range of pH 5.0-8.0. The presence of inhibition at acidic pH without significant pH dependence strongly suggests that NH(4)(+) cation functions as a major inhibitor in the acidic pH region, where neutral NH(3) scarcely exists in the buffer. The NH(4)Cl treatment at pH 6.5 and 5.5 induced prominent changes in the COO(-) stretching regions in FTIR difference spectra upon the S(1) → S(2) transition measured at 283 K. The NH(4)Cl concentration dependence of the amplitude of the spectral changes showed a good correlation with that of the inhibition of O(2) evolution. From this observation, it is proposed that NH(4)(+) cation interacts with carboxylate groups coupled to the Mn cluster as direct ligands or proton transfer mediators, causing inhibition of the O(2) evolving reaction.     

Split EPR signals from photosystem II are modified by methanol, reflecting S state-dependent binding and alterations in the magnetic coupling in the CaMn4 cluster

Methanol binds to the CaMn4 cluster in photosystem II (PSII). Here we report the methanol dependence of the split EPR signals originating from the magnetic interaction between the CaMn4 cluster and the Y(Z)* radical in PSII which are induced by illumination at 5 K. We found that the magnitudes of the "split S1" and "split S3" signals induced in the S1 and S3 states of PSII centers, respectively, are diminished with an increase in the methanol concentration. The methanol concentrations at which half of the respective spectral changes had occurred ([MeOH](1/2)) were 0.12 and 0.57%, respectively. By contrast, the "split S0" signal induced in the S0 state is broadened, and its amplitude is enhanced. [MeOH](1/2) for this change was found to be 0.54%. We discuss these observations with respect to the location and nature of the methanol binding site. Furthermore, by comparing this behavior with methanol effects reported for other EPR signals in the different S states, we propose that the observed methanol-dependent changes in the split S1 and split S0 EPR signals are caused by an increase in the extent of magnetic coupling within the cluster.     

The charge accumulation mechanism in NaCl-washed and in Ca2+-reactivated Photosystem-II particles

In this report we show that, under flashing light, NaCl-washed, Photosystem-II particles which do not evolve oxygen, are unable to go beyond the S₃Z⁺ state. Addition of Ca²⁺ alone restores the S₃Z⁺ → S₀ transition and oxygen evolution. These conclusions were reached by analysis of the oxygen and luminescence oscillations.     

S-state dependent Fourier transform infrared difference spectra for the photosystem II oxygen evolving complex

Vibrational spectroscopy provides a means to investigate molecular interactions within the active site of an enzyme. We have applied difference FTIR spectroscopy coupled with a flash turnover protocol of photosystem II (PSII) to study the oxygen evolving complex (OEC). Our data show two overlapping oscillatory patterns as the sample is flashed through the four-step S-state cycle that produces O(2) from two H(2)O molecules. The first oscillation pattern of the spectra shows a four-flash period four oscillation and reveals a number of new vibrational modes for each S-state transition, indicative of unique structural changes involved in the formation of each S-state. Importantly, the first and second flash difference spectra are reproduced in the 1800-1200 cm(-)(1) spectral region by the fifth and sixth flash difference spectra, respectively. The second oscillation pattern observed is a four-flash, period-two oscillation associated with changes primarily to the amide I and II modes and reports on changes in sign of these modes that alternate 0:0:1:1 during S-state advance. This four-flash, period-two oscillation undergoes sign inversion that alternates during the S(1)-to-S(2) and S(3)-to-S(0) transitions. Underlying this four-flash period two is a small-scale change in protein secondary structure in the PSII complex that is directly related to S-state advance. These oscillation patterns and their relationships with other PSII phenomena are discussed, and future work can initiate more detailed vibrational FTIR studies for the S-state transitions providing spectral assignments and further structural and mechanistic insight into the photosynthetic water oxidation reaction.