Characterization of the tyrosine-Z radical and its environment in the spin-coupled S2TyrZ* state of photosystem II from Thermosynechococcus elongatus

The Mn4Ca cluster of photosystem II (PSII) goes through five sequential oxidation states (S0-S4) in the water oxidation process that also involves a tyrosine radical intermediate (TyrZ*). An S2TyrZ* state in which the Mn4Ca cluster and TyrZ* are magnetically coupled to each other and which is characterized by a distinct "split-signal" EPR spectrum can be generated in acetate-treated PSII. This state was examined by high-field EPR (HFEPR) in PSII from Thermosynechococcus elongatus isolated from a D2-Tyr160Phe mutant to avoid spectral contributions from TyrD*. In contrast to the same state in plants, both antiferromagnetic and ferromagnetic spin-spin couplings were observed. The intrinsic g values of TyrZ* in the coupled state were directly measured from the microwave frequency dependence of the HFEPR spectrum. The TyrZ* gx value in the antiferromagnetic centers was 2.0083, indicating that the coupled radical was in a less electropositive environment than in Mn-depleted PSII. Two gx values were found in the ferromagnetically coupled centers, 2.0069 and 2.0079. To put these values in perspective, the second redox-active tyrosine, TyrD*, was examined in various electrostatic environments. The TyrD* gx value changed from 2.0076 in the wild type to 2.0095 when the hydrogen bond from histidine 189 to TyrD* was removed using the D2-His189Leu mutant, indicating a change to a significantly less electropositive environment. BLY3P/6-31+G** density functional calculations on the hydrogen-bonded p-ethylphenoxy radical-imidazole supermolecular model complex showed that the entire range of Tyr* gx values, from 2.0065 to 2.0095, could be explained by the combined effects of hydrogen bonding and the dielectric constant of the local protein environment.     

Low-temperature photochemistry in photosystem II from Thermosynechococcus elongatus induced by visible and near-infrared light

The active site for water oxidation in photosystem II (PSII) consists of a Mn4Ca cluster close to a redox-active tyrosine residue (TyrZ). The enzyme cycles through five sequential oxidation states (S0 to S4) in the water oxidation process. Earlier electron paramagnetic resonance (EPR) work showed that metalloradical states, probably arising from the Mn4 cluster interacting with TyrZ., can be trapped by illumination of the S0, S1 and S2 states at cryogenic temperatures. The EPR signals reported were attributed to S0TyrZ., S1TyrZ. and S2TyrZ., respectively. The equivalent states were examined here by EPR in PSII isolated from Thermosynechococcus elongatus with either Sr or Ca associated with the Mn4 cluster. In order to avoid spectral contributions from the second tyrosyl radical, TyrD., PSII was used in which Tyr160 of D2 was replaced by phenylalanine. We report that the metalloradical signals attributed to TyrZ. interacting with the Mn cluster in S0, S1, S2 and also probably the S3 states are all affected by the presence of Sr. Ca/Sr exchange also affects the non-haem iron which is situated approximately 44 A units away from the Ca site. This could relate to the earlier reported modulation of the potential of QA by the occupancy of the Ca site. It is also shown that in the S3 state both visible and near-infrared light are able to induce a similar Mn photochemistry.     

Inhibition of tyrosine Z photooxidation after formation of the S3 state in Ca(2+)-depleted and Cl(-)-depleted photosystem II.

Ca2+ and Cl- are obligatory cofactors in photosystem II (PS-II), the oxygen-evolving enzyme of plants. The sites of inhibition in both Ca(2+)- and Cl(-)-depleted PS-II were compared using EPR and flash absorption spectroscopies to follow the extent of the photooxidation of the redox-active tyrosine (TyrZ) and of the primary electron donor chlorophyll (P680) and their subsequent reduction in the dark. The inhibition occurred after formation of the S3 state in Ca(2+)-depleted PS-II. In Cl(-)-depleted photosystem II, the inhibition occurred after formation of the S3 state in about half of the centers and probably after S2TyrZ+ formation in the remaining centers. After the S3 state was formed in Ca(2+)- and Cl(-)-depleted photosystem II, electron transfer from TyrZ to P680 was inhibited. This inhibition is discussed in terms of electrostatic constraints resulting from S3 formation in the absence of Ca2+ and Cl-.     

Probing the functional role of Ca2+ in the oxygen-evolving complex of photosystem II by metal ion inhibition

Photosynthetic oxygen evolution in photosystem II (PSII) takes place in the oxygen-evolving complex (OEC) that is comprised of a tetranuclear manganese cluster (Mn4), a redox-active tyrosine residue (YZ), and Ca2+ and Cl- cofactors. The OEC is successively oxidized by the absorption of 4 quanta of light that results in the oxidation of water and the release of O2. Ca2+ is an essential cofactor in the water-oxidation reaction, as its depletion causes the loss of the oxygen-evolution activity in PSII. In recent X-ray crystal structures, Ca2+ has been revealed to be associated with the Mn4 cluster of PSII. Although several mechanisms have been proposed for the water-oxidation reaction of PSII, the role of Ca2+ in oxygen evolution remains unclear. In this study, we probe the role of Ca2+ in oxygen evolution by monitoring the S1 to S2 state transition in PSII membranes and PSII core complexes upon inhibition of oxygen evolution by Dy3+, Cu2+, and Cd2+ ions. By using a cation-exchange procedure in which Ca2+ is not removed prior to addition of the studied cations, we achieve a high degree of reversible inhibition of PSII membranes and PSII core complexes by Dy3+, Cu2+, and Cd2+ ions. EPR spectroscopy is used to quantitate the number of bound Dy3+ and Cu2+ ions per PSII center and to determine the proximity of Dy3+ to other paramagnetic centers in PSII. We observe, for the first time, the S2 state multiline electron paramagnetic resonance (EPR) signal in Dy3+- and Cd2+-inhibited PSII and conclude that the Ca2+ cofactor is not specifically required for the S1 to S2 state transition of PSII. This observation provides direct support for the proposal that Ca2+ plays a structural role in the early S-state transitions, which can be fulfilled by other cations of similar ionic radius, and that the functional role of Ca2+ to activate water in the O-O bond-forming reaction that occurs in the final step of the S state cycle can only be fulfilled by Ca2+ and Sr2+, which have similar Lewis acidities.     

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.     

Ca(2+) function in photosynthetic oxygen evolution studied by alkali metal cations substitution

Effects of adding monovalent alkali metal cations to Ca(2+)-depleted photosystem (PS)II membranes on the biochemical and spectroscopic properties of the oxygen-evolving complex were studied. The Ca(2+)-dependent oxygen evolution was competitively inhibited by K(+), Rb(+), and Cs(+), the ionic radii of which are larger than the radius of Ca(2+) but not inhibited significantly by Li(+) and Na(+), the ionic radii of which are smaller than that of Ca(2+). Ca(2+)-depleted membranes without metal cation supplementation showed normal S(2) multiline electron paramagnetic resonance (EPR) signal and an S(2)Q(A)(-) thermoluminescence (TL) band with a normal peak temperature after illumination under conditions for single turnover of PSII. Membranes supplemented with Li(+) or Na(+) showed properties similar to those of the Ca(2+)-depleted membranes, except for a small difference in the TL peak temperatures. The peak temperature of the TL band of membranes supplemented with K(+), Rb(+), or Cs(+) was elevated to approximately 38 degrees C which coincided with that of Y(D)(+)Q(A)(-) TL band, and no S(2) EPR signals were detected. The K(+)-induced high-temperature TL band and the S(2)Q(A)(-) TL band were interconvertible by the addition of K(+) or Ca(2+) in the dark. Both the Ca(2+)-depleted and the K(+)-substituted membranes showed the narrow EPR signal corresponding to the S(2)Y(Z)(+) state at g = 2 by illuminating the membranes under multiple turnover conditions. These results indicate that the ionic radii of the cations occupying Ca(2+)-binding site crucially affect the properties of the manganese cluster.     

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

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

Effect of the 17- and 23-kilodalton polypeptides, calcium, and chloride on electron transfer in photosystem II

Electron paramagnetic resonance (EPR) measurements were performed on photosystem II (PSII) membranes that were treated with 2 M NaCl to release the 17- and 23-kilodalton (kDa) polypeptides. By using 75 microM 3-(3,4-dichlorophenyl)-1,1-dimethylurea to limit the photosystem II samples to one stable charge separation in the temperature range of 77-273 K, we have quantitated the EPR signals of the several electron donors and acceptors of photosystem II. It was found that removal of the 17- and 23-kDa polypeptides caused low potential cytochrome b559 to become fully oxidized during the course of dark adaptation. Following illumination at 77-130 K, one chlorophyll molecule per reaction center was oxidized. Between 130 and 200 K, both a chlorophyll molecule and the S1 state were photooxidized and, together, accounted for one oxidation per reaction center. Above 200 K, the chlorophyll radical was unstable. Oxidation of the S1 state gave rise to the S2-state multiline EPR signal, which arises from the Mn site of the O2-evolving center. The yield of the S2-state multiline EPR signal in NaCl-washed PSII membranes was as high as 93% of the control, untreated PSII membranes, provided that both Ca2+ and Cl- were bound. Furthermore, the 55Mn nuclear hyperfine structure of the S2-state multiline EPR signal was unaltered upon depletion of the 17- and 23-kDa polypeptides. In NaCl-washed PSII samples where Ca2+ and/or Cl- were removed, however, the intensity of the S2-state multiline EPR signal decreased in parallel with the fraction of PSII lacking bound Ca2+ and Cl-.(ABSTRACT TRUNCATED AT 250 WORDS)     

The stable tyrosyl radical in photosystem II: why D?

Two redox-active tyrosines are present in Photosysytem II, the water-oxidizing enzyme. While the tyrosine that is kinetically competent in electron transfer, TyrZ, may also have a role in the enzyme mechanism, the second tyrosine, TyrD, has a stable radical and is not directly involved in the redox chemistry associated with enzyme function. Nevertheless, reasonable mechanistic roles for TyrD have been postulated that satisfy desires to rationalise the presence of this cofactor, or, in English, we think we know what it does. First, the TyrD radical acts an oxidant of the Mn cluster in the lowest state of the redox accumulation cycle (i.e., S(0)), providing potential benefits in maintaining the cluster in the more stable higher valence states. This redox role may also be important during Mn assembly and indeed overreduced forms of the Mn cluster appear to be oxidised by TyrD(*). Second, the proton generated by the TyrD radical is thought to remain in its vicinity having an electrostatic influence on the location and potential of the chlorophyll cation, P(+). This effect may be important for the kinetics of TyrZ oxidation and may provide a significant thermodynamic boost to the enzyme. In addition, through its electrostatic influence, TyrD(*)(H(+)) may confine the highly oxidising cation P(+) to the chlorophyll nearest to TyrZ, thereby accelerating TyrZ oxidation and restricting the potentially damaging redox chemistry to one side of the reaction centre: the disposable D1 side. This second role, evidence for which is beginning to emerge, constitutes a new role for a redox-active tyrosine in biology: as a positive charge generator in a hydrophobic environment. In this short review, we focus on work relevant to these two roles.     

Purification, crystallization and X-ray diffraction analyses of the T. elongatus PSII core dimer with strontium replacing calcium in the oxygen-evolving complex

The core complex of photosystem II (PSII) was purified from thermophilic cyanobacterium Thermosynechococcus elongatus grown in Sr(2+)-containing and Ca(2+)-free medium. Functional in vivo incorporation of Sr(2+) into the oxygen-evolving complex (OEC) was confirmed by EPR analysis of the isolated and highly purified SrPSII complex in agreement with the previous study of Boussac et al. [J. Biol. Chem. 279 (2004) 22809-22819]. Three-dimensional crystals of SrPSII complex were obtained which diffracted to 3.9 A and belonged to the orthorhombic space group P2(1)2(1)2(1) with unit cell dimensions of a=133.6 A, b=236.6 A, c=307.8 A. Anomalous diffraction data collected at the Sr K-X-ray absorption edge identified a novel Sr(2+)-binding site which, within the resolution of these data (6.5 A), is consistent with the positioning of Ca(2+) in the recent crystallographic models of PSII [Ferreira et al. Science 303 (2004) 1831-1838, Loll et al. Nature 438 (2005) 1040-1044]. Fluorescence measurements on SrPSII crystals confirmed that crystallized SrPSII was active in transferring electrons from the OEC to the acceptor site of the reaction centre. However, SrPSII showed altered functional properties of its modified OEC in comparison with that of the CaPSII counterpart: slowdown of the Q(A)-to-Q(B) electron transfer and stabilized S(2)Q(A)(-) charge recombination.     

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.     

The basic properties of the electronic structure of the oxygen-evolving complex of photosystem II are not perturbed by Ca2+ removal

Ca(2+) is an integral component of the Mn(4)O(5)Ca cluster of the oxygen-evolving complex in photosystem II (PS II). Its removal leads to the loss of the water oxidizing functionality. The S(2)' state of the Ca(2+)-depleted cluster from spinach is examined by X- and Q-band EPR and (55)Mn electron nuclear double resonance (ENDOR) spectroscopy. Spectral simulations demonstrate that upon Ca(2+) removal, its electronic structure remains essentially unaltered, i.e. that of a manganese tetramer. No redistribution of the manganese valence states and only minor perturbation of the exchange interactions between the manganese ions were found. Interestingly, the S(2)' state in spinach PS II is very similar to the native S(2) state of Thermosynechococcus elongatus in terms of spin state energies and insensitivity to methanol addition. These results assign the Ca(2+) a functional as opposed to a structural role in water splitting catalysis, such as (i) being essential for efficient proton-coupled electron transfer between Y(Z) and the manganese cluster and/or (ii) providing an initial binding site for substrate water. Additionally, a novel (55)Mn(2+) signal, detected by Q-band pulse EPR and ENDOR, was observed in Ca(2+)-depleted PS II. Mn(2+) titration, monitored by (55)Mn ENDOR, revealed a specific Mn(2+) binding site with a submicromolar K(D). Ca(2+) titration of Mn(2+)-loaded, Ca(2+)-depleted PS II demonstrated that the site is reversibly made accessible to Mn(2+) by Ca(2+) depletion and reconstitution. Mn(2+) is proposed to bind at one of the extrinsic subunits. This process is possibly relevant for the formation of the Mn(4)O(5)Ca cluster during photoassembly and/or D1 repair.     

Molecular interference of Cd(2+) with Photosystem II

Many heavy metals inhibit electron transfer reactions in Photosystem II (PSII). Cd(2+) is known to exchange, with high affinity in a slow reaction, for the Ca(2+) cofactor in the Ca/Mn cluster that constitutes the oxygen-evolving center. This results in inhibition of photosynthetic oxygen evolution. There are also indications that Cd(2+) binds to other sites in PSII, potentially to proton channels in analogy to heavy metal binding in photosynthetic reaction centers from purple bacteria. In search for the effects of Cd(2+)-binding to those sites, we have studied how Cd(2+) affects electron transfer reactions in PSII after short incubation times and in sites, which interact with Cd(2+) with low affinity. Overall electron transfer and partial electron transfer were studied by a combination of EPR spectroscopy of individual redox components, flash-induced variable fluorescence and steady state oxygen evolution measurements. Several effects of Cd(2+) were observed: (i) the amplitude of the flash-induced variable fluorescence was lost indicating that electron transfer from Y(Z) to P(680)(+) was inhibited; (ii) Q(A)(-) to Q(B) electron transfer was slowed down; (iii) the S(2) state multiline EPR signal was not observable; (iv) steady state oxygen evolution was inhibited in both a high-affinity and a low-affinity site; (v) the spectral shape of the EPR signal from Q(A)(-)Fe(2+) was modified but its amplitude was not sensitive to the presence of Cd(2+). In addition, the presence of both Ca(2+) and DCMU abolished Cd(2+)-induced effects partially and in different sites. The number of sites for Cd(2+) binding and the possible nature of these sites are discussed.     

The S3 state of photosystem II: differences between the structure of the manganese complex in the S2 and S3 states determined by X-ray absorption spectroscopy

O2-evolving photosystem II (PSII) membranes from spinach have been cryogenically stabilized in the S3 state of the oxygen-evolving complex. The cryogenic trapping of the S3 state was achieved using a double-turnover illumination of dark-adapted PSII preparations maintained at 240 K. A double turnover of PSII was accomplished using the high-potential acceptor, Q400, which is the high-spin iron of the iron-quinone acceptor complex. EPR spectroscopy was the principal tool establishing the S-state composition and defining the electron-transfer events associated with a double turnover of PSII. The inflection point energy of the Mn X-ray absorption K-edge of PSII preparations poised in the S3 state is the same as for those poised in the S2 state. This is surprising in light of the loss of the multiline EPR signal upon advancing to the S3 state. This indicates that the oxidative equivalent stored within the oxygen-evolving complex (OEC) during this transition resides on another intermediate donor which must be very close to the manganese complex. An analysis of the Mn extended X-ray absorption fine structure (EXAFS) of PSII preparations poised in the S2 and S3 states indicates that a small structural rearrangement occurs during this photoinduced transition. A detailed comparison of the Mn EXAFS of these two S states with the EXAFS of four multinuclear mu-oxo-bridged manganese compounds indicates that the photosynthetic manganese site most probably consists of a pair of binuclear di-mu-oxo-bridged manganese structures. However, we cannot rule out, on the basis of the EXAFS analysis alone, a complex containing a mononuclear center and a linear trinuclear complex. The subtle differences observed between the S states are best explained by an increase in the spread of Mn-Mn distances occurring during the S2----S3 state transition. This increased disorder in the manganese distances suggests the presence of two inequivalent di-mu-oxo-bridged binuclear structures in the S3 state.     

Tyrosine D oxidation at cryogenic temperature in photosystem II

Photosystem II (PSII) contains two redox-active tyrosines (TyrZ and TyrD) possessing very different properties. TyrD is stable in its oxidized form, while TyrZ is kinetically competent in the water oxidizing reaction. The temperature dependence of the formation of light-induced tyrosyl radical was studied as a function of pH in Mn-depleted PS II from cyanobacteria and plants. Tyrosyl radical formation was observed in the majority of the centers at pH 8.5 and 15 K. The use of two Synechocystis mutants where either TyrZ or TyrD was replaced by a phenylalanine residue allowed a clear demonstration that only TyrD and not TyrZ was oxidized under these conditions. By lowering the pH, the fraction of centers undergoing TyrD oxidation greatly diminished. This pH dependence could be fitted by assuming a single protonable group with a pK(a) of approximately 7.6. This pH dependence correlates with the unexpectedly rapid oxidation of TyrD at room temperature [Faller, P., Debus, R. J., Brettel, K., Sugiura, M., Rutherford, A. W., and Boussac, A. (2001) Proc. Nat. Acad. Sci. U.S.A. 98, 14368]. The equally unexpectedly ability to undergo oxidation at cryogenic temperatures reported here, puts limitations on the nature of the protonation reactions associated with electron transfer in this system, raising the possibility of proton tunneling along the hydrogen bond or alternatively the presence of deprotonated TyrD (tyrosinate) prior to oxidation.     

Influence of the PsbA1/PsbA3, Ca(2+)/Sr(2+) and Cl(-)/Br(-) exchanges on the redox potential of the primary quinone Q(A) in Photosystem II from Thermosynechococcus elongatus as revealed by spectroelectrochemistry

Ca(2+) and Cl(-) ions are essential elements for the oxygen evolution activity of photosystem II (PSII). It has been demonstrated that these ions can be exchanged with Sr(2+) and Br(-), respectively, and that these ion exchanges modify the kinetics of some electron transfer reactions at the Mn?Ca cluster level (Ishida et al., J. Biol. Chem. 283 (2008) 13330-13340). It has been proposed from thermoluminescence experiments that the kinetic effects arise, at least in part, from a decrease in the free energy level of the Mn(4)Ca cluster in the S? state though some changes on the acceptor side were also observed. Therefore, in the present work, by using thin-layer cell spectroelectrochemistry, the effects of the Ca(2+)/Sr(2+) and Cl(-)/Br(-) exchanges on the redox potential of the primary quinone electron acceptor Q(A), E(m)(Q(A)/Q(A)(-)), were investigated. Since the previous studies on the Ca(2+)/Sr(2+) and Cl(-)/Br(-) exchanges were performed in PsbA3-containing PSII purified from the thermophilic cyanobacterium Thermosynechococcus elongatus, we first investigated the influences of the PsbA1/PsbA3 exchange on E(m)(Q(A)/Q(A)(-)). Here we show that i) the E(m)(Q(A)/Q(A)(-)) was up-shifted by ca. +38mV in PsbA3-PSII when compared to PsbA1-PSII and ii) the Ca(2+)/Sr(2+) exchange up-shifted the E(m)(Q(A)/Q(A)(-)) by ca. +27mV, whereas the Cl(-)/Br(-) exchange hardly influenced E(m)(Q(A)/Q(A)(-)). On the basis of the results of E(m)(Q(A)/Q(A)(-)) together with previous thermoluminescence measurements, the ion-exchange effects on the energetics in PSII are discussed.     

Structural perturbation of the carboxylate ligands to the manganese cluster upon Ca2+/Sr2+ exchange in the S-state cycle of photosynthetic oxygen evolution as studied by flash-induced FTIR difference spectroscopy

A Ca(2+) ion is an indispensable element in the oxygen-evolving Mn cluster in photosystem II (PSII). To investigate the structural relevance of Ca(2+) to the Mn cluster, the effects of Sr(2+) substitution for Ca(2+) on the structures and reactions of ligands to the Mn cluster during the S-state cycle were investigated using flash-induced Fourier transform infrared (FTIR) difference spectroscopy. FTIR difference spectra representing the four S-state transitions, S(1) --> S(2), S(2) --> S(3), S(3) --> S(0), and S(0) --> S(1), were recorded by applying four consecutive flashes either to PSII core complexes from Thermosynechococcus elongatus or to PSII-enriched membranes from spinach. The spectra were also recorded using biosynthetically Sr(2+)-substituted PSII core complexes from T. elongatus and biochemically Sr(2+)-substituted PSII membranes from spinach. Several common spectral changes upon Sr(2+) substitution were observed in the COO(-) stretching region of the flash-induced spectra for both preparations, which were best expressed in Ca(2+)-minus-Sr(2+) double difference spectra. The significant intensity changes in the symmetric COO(-) peaks at approximately 1364 and approximately 1418 cm(-)(1) at the first flash were reversed as opposite intensity changes at the third flash, and the slight shift of the approximately 1446 cm(-)(1) peak at the second flash corresponded to the similar but opposite shift at the fourth flash. Analyses of these changes suggest that there are at least three carboxylate ligands whose structures are significantly perturbed by Ca(2+)/Sr(2+) exchange. They are (1) the carboxylate ligand having a bridging or unidentate structure in the S(2) and S(3) states and perturbed in the S(1) --> S(2) and S(3) --> S(0) transitions, (2) that with a chelating or bridging structure in the S(1) and S(0) states and perturbed also in the S(1) --> S(2) and S(3) --> S(0) transitions, and (3) that with a chelating structure in the S(3) and S(0) states and changes in the S(2) --> S(3) and S(0) --> S(1) transitions. Taking into account the recent FTIR studies using site-directed mutagenesis and/or isotope substitution [Chu et al. (2004) Biochemistry 43, 3152-3116; Kimura et al. (2005) J. Biol. Chem. 280, 2078-2083; Strickler et al. (2006) Biochemistry 45, 8801-8811], it was concluded that these carboxylate groups do not originate from either D1-Ala344 (C-terminus) or D1-Glu189, which are located near the Ca(2+) ion in the X-ray crystallographic model of the Mn cluster. It was thus proposed that if the X-ray model is correct, the above carboxylate groups sensitive to Sr(2+) substitution are ligands to the Mn ions strongly coupled to the Ca(2+) ion rather than direct ligands to Ca(2+).     

Quantifying the ion selectivity of the Ca2+ site in photosystem II: evidence for direct involvement of Ca2+ in O2 formation.

Calcium is an essential cofactor in the oxygen-evolving complex (OEC) of photosystem II (PSII). The removal of Ca2+ or its substitution by any metal ion except Sr2+ inhibits oxygen evolution. We used steady-state enzyme kinetics to measure the rate of O2 evolution in PSII samples treated with an extensive series of mono-, di-, and trivalent metal ions in order to determine the basis for the affinity of metal ions for the Ca2+-binding site. Our results show that the Ca2+-binding site in PSII behaves very similarly to the Ca2+-binding sites in other proteins, and we discuss the implications this has for the structure of the site in PSII. Activity measurements as a function of time show that the binding site achieves equilibrium in 4 h for all of the PSII samples investigated. The binding affinities of the metal ions are modulated by the 17 and 23 kDa extrinsic polypeptides; their removal decreases the free energy of binding of the metal ions by 2.5 kcal/mol, but does not significantly change the time required to reach equilibrium. Monovalent ions are effectively excluded from the Ca2+-binding site, exhibiting no inhibition of O2 evolution. Di- and trivalent metal ions with ionic radii similar to that of Ca2+ (0.99 A) bind competitively with Ca2+ and have the highest binding affinity, while smaller metal ions bind more weakly and much larger ones do not bind competitively. This is consistent with a size-selective Ca2+-binding site that has a rigid array of coordinating ligands. Despite the large number of metal ions that competitively replace Ca2+ in the OEC, only Sr2+ is capable of partially restoring activity. Comparing the physical characteristics of the metal ions studied, we identify the pK(a) of the aqua ion as the factor that determines the functional competence of the metal ion. This suggests that Ca2+ is directly involved in the chemistry of water oxidation and is not only a structural cofactor in the OEC. We propose that the role of Ca2+ is to act as a Lewis acid, binding a substrate water molecule and tuning its reactivity.     

The S0 state of photosystem II induced by hydroxylamine: differences between the structure of the manganese complex in the S0 and S1 states determined by X-ray absorption spectroscopy

Hydroxylamine at low concentrations causes a two-flash delay in the first maximum flash yield of oxygen evolved from spinach photosystem II (PSII) subchloroplast membranes that have been excited by a series of saturating flashes of light. Untreated PSII membrane preparations exhibit a multiline EPR signal assigned to a manganese cluster and associated with the S2 state when illuminated at 195 K, or at 273 K in the presence of 3-(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU). We used the extent of suppression of the multiline EPR signal observed in samples illuminated at 195 K to determine the fraction of PSII reaction centers set back to a hydroxylamine-induced S0-like state, which we designate S0*. The manganese K-edge X-ray absorption edges for dark-adapted PSII preparations with or without hydroxylamine are virtually identical. This indicates that, despite its high binding affinity to the oxygen-evolving complex (OEC) in the dark, hydroxylamine does not reduce chemically the manganese cluster within the OEC in the dark. After a single turnover of PSII, a shift to lower energy is observed in the inflection of the Mn K-edge of the manganese cluster. We conclude that, in the presence of hydroxylamine, illumination causes a reduction of the OEC, resulting in a state resembling S0. This lower Mn K-edge energy of S0*, relative to the edge of S1, implies the storage and stabilization of an oxidative equivalent within the manganese cluster during the S0----S1 state transition. An analysis of the extended X-ray absorption fine structure (EXAFS) of the S0* state indicates that a significant structural rearrangement occurs between the S0* and S1 states. The X-ray absorption edge position and the structure of the manganese cluster in the S0* state are indicative of a heterogeneous mixture of formal valences of manganese including one Mn(II) which is not present in the S1 state.