The differences in microenvironments and functions of tyrosine radicals YZ and YD in photosystem II studied by EPR

Electron paramagnetic resonance (EPR) and electron nuclear double resonance (ENDOR) were performed to investigate the difference in microenvironments and functions between tyrosine Z (Y(Z)) and tyrosine D (Y(D)). Mn-depletion or Ca(2+)-depletion causes extension of the lifetime of tyrosine radical Y(Z)(*), which can be trapped by rapid freezing after illumination at about 250 K. Above pH 6.5, Y(Z)(*) radical in Mn-depleted PS II shows similar EPR and ENDOR spectra similar to that of Y(D)(*) radical, which are ascribed to a typical neutral tyrosine radical. Below pH 6.5, Y(Z)(*) radical shows quite different EPR and ENDOR spectra. ENDOR spectra show the spin density distribution of the low-pH form of Y(Z)(*) that has been quite different from the high-pH form of Y(Z)(*). The spin density distribution of the low-pH Y(Z)(*) can be explained by a cation radical or the neutral radical induced by strong electrostatic interaction. The pH dependence of the activation energy of the recombination rate between Y(Z)(*) and Q(A)(-) shows a gap of 4.4 kJ/mol at pH 6.0-6.5. In the Ca(2+)-depleted PS II, Y(Z)(*) signal was the mixture of the cation-like and normal neutral radicals, and the pH dependence of Y(Z)(*) spectrum in Ca(2+)-depleted PS II is considerably different from the neutral radical found in Mn-depleted PS II. Based on the recent structure data of cyanobacterial PS II, the pH dependence of Y(Z)(*) could be ascribed to the modification of the local structure and hydrogen-bonding network induced by the dissociation of ASP170 near Y(Z).     

Formate-induced inhibition of the water-oxidizing complex of photosystem II studied by EPR

The effects of various formate concentrations on both the donor and the acceptor sides in oxygen-evolving PS II membranes (BBY particles) were examined. EPR, oxygen evolution and variable chlorophyll fluorescence have been observed. It was found that formate inhibits the formation of the S(2) state multiline signal concomitant with stimulation of the Q(A)(-)Fe(2+) signal at g = 1.82. The decrease and the increase in intensities of the multiline and Q(A)(-)Fe(2+) signals, respectively, had a linear relation for formate concentrations between 5 and 500 mM. The g = 4.1 signal formation measured in the absence of methanol was not inhibited by formate up to 250 mM in the buffer. In the presence of 3% methanol the g = 4.1 signal evolved as formate concentration increased. The evolved signal could be ascribed to the inhibited centers. Oxygen evolution measured in the presence of an electron acceptor, phenyl-p-benzoquinone, was also inhibited by formate proportionally to the decrease in the multiline signal intensity. The inhibition seemed to be due to a retarded electron transfer from the water-oxidizing complex to Y(Z)(+), which was observed in the decay kinetics of the Y(Z)(+) signal induced by illumination above 250 K. These results show that formate induces inhibition of water oxidation reactions as well as electron transfer on the PS II acceptor side. The inhibition effects of formate in PS II were found to be reversible, indicating no destructive effect on the reaction center induced by formate.     

Iron-blocking the high-affinity Mn-binding site in photosystem II facilitates identification of the type of hydrogen bond participating in proton-coupled electron transport via YZ

Incubation of Mn-depleted PSII membranes [PSII(-Mn)] with Fe(II) is accompanied by the blocking of Y(Z)(*) at the high-affinity Mn-binding site to exogenous electron donors [Semin et al. (2002) Biochemistry 41, 5854-5864] and a shift of the pK(app) of the hydrogen bond partner for Y(Z) (base B) from 7.1 to 6.1 [Semin, B. K., and Seibert, M. (2004) Biochemistry 43, 6772-6782]. Here we calculate activation energies (E(a)) for Y(Z)(*) reduction in PSII(-Mn) and Fe-blocked PSII(-Mn) samples [PSII(-Mn, +Fe)] from temperature dependencies of the rate constants of the fast and slow components of the flash-probe fluorescence decay kinetics. At pH < pK(app) (e.g., 5.5), the decays are fit with one (fast) component in both types of samples, and E(a) is equal to 42.2 +/- 2.9 kJ/mol in PSII(-Mn) and 46.4 +/- 3.3 kJ/mol in PSII(-Mn, +Fe) membranes. At pH > pK(app), the decay kinetics exhibit an additional slow component in PSII(-Mn, +Fe) membranes (E(a) = 36.1 +/- 7.5 kJ/mol), which is much lower than the E(a) of the corresponding component observed for Y(Z)(*) reduction in PSII(-Mn) samples (48.1 +/- 1.7 kJ/mol). We suggest that the above difference results from the formation of a strong low barrier hydrogen bond (LBHB) between Y(Z) and base B in PSII(-Mn, +Fe) samples. To confirm this, Fe-blocking was performed in D(2)O to insert D(+), which has an energetic barrier distinct from H(+), into the LBHB. Measurement of the pH effects on the rates of Y(Z)(*) reduction in PSII(-Mn, +Fe) samples blocked in D(2)O shows a shift of the pK(app) from 6.1 to 7.6, and an increase in the E(a) of the slow component. This approach was also used to measure the stability of the Y(Z)(*) EPR signal at various temperatures in both kinds of membranes. In PSII(-Mn) membranes, the freeze-trapped Y(Z)(*) radical is stable below 190 K, but half of the Y(Z)(*) EPR signal disappears after a 1-min incubation when the sample is warmed to 253 K. In PSII(-Mn, +Fe) samples, the trapped Y(Z)(*) radical is unstable at a much lower temperature (77 K). However, the insertion of D(+) into the hydrogen bond between Y(Z) and base B during the blocking process increases the temperature stability of the Y(Z)(*) EPR signal at 77 K. Again, these results indicate that Fe-blocking involves Y(Z) in the formation of a LBHB, which in turn is consistent with the suggested existence of a LBHB between Y(Z) and base B in intact PSII membranes [Zhang, C., and Styring, S. (2003) Biochemistry 42, 8066-8076].     

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.     

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.     

The effect of mono- and divalent salts on the rise and decay kinetics of EPR signal II in Photosystem II preparations from spinach

The rise and decay kinetics of EPR signal II have been used to probe the organization of the donor side of Photosystem II (PS II) before and after extraction of PS II preparations with high concentrations of salt. 800 mM NaCl or 500-800 mM NaBr substantially depletes the preparations of the 16 and 24 kDa proteins and decreases the steady-state rate of O2-evolution by 70-80% from control rates. These treatments do not largely alter the decay kinetics of Signal II; the rise kinetics remain in the instrument limited time range (2 microseconds or less) during the first 8-12 flashes. Treating PS II preparations with 800 mM CaCl2 removes the 16, 24 and 33 kDa proteins with at least 95% inhibition of the steady-state rates of O2 evolution. The additional removal of the 33 kDa polypeptide decreases the rates of oxidation and rereduction of Z, the species responsible for Signal II. Preparations treated with either mono- or divalent salts show a steady-state light-induced increase in Signal II similar to that seen in Tris-washed samples. Such a steady-state increase indicates that the rate of electron transport from water to Z is greatly decreased or blocked. The data are interpreted within a model in which there is an intermediate electron carrier between the O2 evolving complex and Z.     

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.     

Iron bound to the high-affinity Mn-binding site of the oxygen-evolving complex shifts the pK of a component controlling electron transport via Y(Z)

Flash-probe fluorescence spectroscopy was used to compare the pH dependence of charge recombination between Y(Z)(*) and Q(a)(-) in Mn-depleted, photosystem II membranes [PSII(-Mn)] and in membranes with the high-affinity (HA(Z)) Mn-binding site blocked by iron [PSII(-Mn,+Fe); Semin, B. K., Ghirardi, M. L., and Seibert, M. (2002) Biochemistry 41, 5854-5864]. The apparent half-time for fluorescence decay (t(1/2)) in PSII(-Mn) increased from 9 ms at pH 4.4 to 75 ms at pH 9.0 [with an apparent pK (pK(app)) of 7.1]. The actual fluorescence decay kinetics can be fit to one exponential component at pH <6.0 (t(1/2) = 9.5 ms), but it requires an additional component at pH >6.0 (t(1/2) = 385 ms). Similar measurements with PSII(-Mn,+Fe) membranes show that iron binding has little effect on the maximum and minimum t(1/2) values measured at alkaline and acidic pHs but that it does shift the pK(app) from 7.1 to 6.1 toward the more acidic pK(app) value typical of intact membranes. Light-induced Fe(II) blocking of the PSII(-Mn) membrane is accompanied by a decrease in buffer Fe(II) concentration. This decrease was not the result of Fe(II) binding, but rather of its oxidation at two sites, the HA(Z) site and the low-affinity site. M?ssbauer spectroscopy at 80 K on PSII(-Mn,+Fe) samples, prepared under conditions providing the maximal blocking effect but minimizing the amount of nonspecifically bound iron cations, supports this conclusion since this method detected only Fe(III) cations bound to the membranes. Correlation of the kinetics of Fe(II) oxidation with the blocking parameters showed that blocking occurs after four to five Fe(II) cations were oxidized at the HA(Z) site. In summary, the blocking of the HA(Z) Mn-binding site by iron in PSII(-Mn) membranes not only prevents the access of exogenous donors to Y(Z) but also partially restores the properties of the hydrogen bond net found in intact PS(II), which in turn controls the rate of electron transport to Y(Z).     

Low-temperature electron transfer in photosystem II: a tyrosyl radical and semiquinone charge pair

The states induced by illumination at 7 K in the oxygen-evolving enzyme (PSII) from Thermosynechococcus elongatus were studied by EPR. In the S(0) and S(1) redox states, two g approximately 2 EPR signals, a split signal and a g = 2.03 signal, respectively, were generated by illumination with visible light. These signals were comparable to those already reported in plant PSII in terms of their g value, shape, and stability at low temperatures. We report that the formation and decay of these signals correlate with EPR signals from the semiquinone of the first quinone electron acceptor, Q(A)(-). The light-induced EPR signals from oxidized side-path electron donors (Cyt b(559), Car, and Chl(Z)) were also measured, and from these and the signals from Q(A)(-), estimates were made of the proportion of centers involved in the formation of the g approximately 2 signals (approximately 50% in S(0) and 40% in S(1)). Comparisons with the signals generated in plant PSII indicated approximately similar yields for the S(0) split signal. A single laser flash at 7 K induced more than 75% of the maximum split and g = 2.03 EPR signal observed by continuous illumination, with no detectable oxidation of side-path donors. The matching electron acceptor side reactions, the high quantum yield, and the relatively large proportion of centers involved support earlier suggestions that the state being monitored is Tyr(Z)(*)Q(A)(-), with the g approximately 2 EPR signals arising from Tyr(Z)(*) interacting magnetically with the Mn complex. The current picture of the photochemical reactions occurring in PSII at low temperatures is reassessed.     

Formation of split electron paramagnetic resonance signals in photosystem II suggests that tyrosine(Z) can be photooxidized at 5 K in the S0 and S1 states of the oxygen-evolving complex

The effect of illumination at 5 K of photosystem II in different S-states was investigated with EPR spectroscopy. Two split radical EPR signals around g approximately 2.0 were observed from samples given 0 and 3 flashes, respectively. The signal from the 0-flash sample was narrow, with a width of approximately 80 G, in which the low-field peak can be distinguished. This signal oscillated with the S(1) state in the sample. The signal from the 3-flash sample was broad, with a symmetric shape of approximately 160 G width from peak to trough. This signal varied with the concentration of the S(0) state in the sample. Both signals are assigned to arise from the donor side of PSII. Both signals relaxed fast, were formed within 10 ms after a flash, and decayed with half-times at 5 K of 3-4 min. The signal in the S(0) state closely resembles split radical signals, originating from magnetic interaction between Y(Z)(*) and the S(2) state, that were first observed in Ca(2+)-depleted photosystem II samples. Therefore, we assign this signal to Y(Z)(*) in magnetic interaction with the S(0) state, Y(Z)(*)S(0). The other signal is assigned to the magnetic interaction between Y(Z)(*) and the S(1) state, Y(Z)(*)S(1). An important implication is that Y(Z) can be oxidized at 5 K in the S(0) and S(1) states. Oxidation of Y(Z) involves deprotonation of the tyrosine. This is restricted at 5 K, and we therefore suggest that the phenolic proton of Y(Z) is involved in a low-barrier hydrogen bond. This is an unusually short hydrogen bond in which proton movement at very low temperatures can occur.     

pH-dependent characteristics of Y(Z) radical in Ca(2+)-depleted photosystem II studied by CW-EPR and pulsed ENDOR

The Y(Z)-tyrosine radical was trapped by freezing immediately after illumination in Ca(2+)-depleted Photosystem II (PS II) membranes and the pH-dependent characteristics of the radical were investigated using CW-EPR and pulsed ENDOR. The spectrum of the Y*(Z) radical trapped in the Y*(Z)S(1) state at pH 5.5 was cation-like as reported in Mn-depleted PS II (H. Mino et al., Spectrochim. Acta A 53 (1997) 1465-1483). By illuminating the PS II-retaining S(2) state, the Y*(Z) radical and a broad doublet signal formed in the g approximately 2 region were trapped concomitantly. The spectrum of the trapped Y*(Z) radical in the Y*(Z)S(2) state was cation-like at pH 5.5 but the pulsed ENDOR measurements reveals the involvement of the neutral Y*(Z) radical in the doublet signal. At pH 7.0, the resulting Y*(Z) signal was the mixture of the cation-like and neutral radical spectra, and considerably different from the neutral radical found in Mn-depleted PS II. pH-Dependent changes in the properties of the Y*(Z) radical are discussed in relation to the redox events occurring in Ca(2+)-depleted PS II.     

Elucidating the site of action of oxalate in photosynthetic electron transport chain in spinach thylakoid membranes

The effects of oxalate on PS II and PS I photochemistry were studied. The results suggested that in chloride-deficient thylakoid membranes, oxalate inhibited activity of PS II as well as PS I. To our knowledge, this is the only anion so far known which inhibits both the photosystems. Measurements of fluorescence induction kinetics, YZ* decay, and S2 state multiline EPR signal suggested that oxalate inhibited PS II at the donor side most likely on the oxygen evolving complex. Measurements of re-reduction of P700+ signal in isolated PS I particles in oxalate-treated samples suggested a binding site of oxalate on the donor, as well as the acceptor side of PS I.     

Stability of the S₃and S₂state intermediates in photosystem II directly probed by EPR spectroscopy

The stability of the S(3) and S(2) states of the oxygen evolving complex in photosystem II (PSII) was directly probed by EPR spectroscopy in PSII membrane preparations from spinach in the presence of the exogenous electron acceptor PpBQ at 1, 10, and 20 °C. The decay of the S(3) state was followed in samples exposed to two flashes by measuring the split S(3) EPR signal induced by near-infrared illumination at 5 K. The decay of the S(2) state was followed in samples exposed to one flash by measuring the S(2) state multiline EPR signal. During the decay of the S(3) state, the S(2) state multiline EPR signal first increased and then decreased in amplitude. This shows that the decay of the S(3) state to the S(1) state occurs via the S(2) state. The decay of the S(3) state was biexponential with a fast kinetic phase with a few seconds decay half-time. This occurred in 10-20% of the PSII centers. The slow kinetic phase ranged from a decay half-time of 700 s (at 1 °C) to ~100 s (at 20 °C) in the remaining 80-90% of the centers. The decay of the S(2) state was also biphasic and showed quite similar kinetics to the decay of the S(3) state. Our experiments show that the auxiliary electron donor Y(D) was oxidized during the entire experiment. Thus, the reduced form of Y(D) does not participate to the fast decay of the S(2) and S(3) states we describe here. Instead, we suggest that the decay of the S(3) and S(2) states reflects electron transfer from the acceptor side of PSII to the donor side of PSII starting in the corresponding S state. It is proposed that this exists in equilibrium with Y(Z) according to S(3)Y(Z) ? S(2)Y(Z)(?) in the case of the S(3) state decay and S(2)Y(Z) ? S(1)Y(Z)(?) in the case of the S(2) state decay. Two kinetic models are discussed, both developed with the assumption that the slow decay of the S(3) and S(2) states occurs in PSII centers where Y(Z) is also a fast donor to P(680)(+) working in the nanosecond time regime and that the fast decay of the S(3) and S(2) states occurs in centers where Y(Z) reduces P(680)(+) with slower microsecond kinetics. Our measurements also demonstrate that the split S(3) EPR signal can be used as a direct probe to the S(3) state and that it can provide important information about the redox properties of the S(3) state.     

EPR kinetic studies of the S-1 state in spinach thylakoids

The Y(Z)* decay kinetics in a formal S(-1) state, regarded as a reduced state of the oxygen evolving complex, was determined using time-resolved EPR spectroscopy. This S(-1) state was generated by biochemical treatment of thylakoid membranes with hydrazine. The steady-state oxygen evolution of the sample was used to optimize the biochemical procedure for performing EPR experiments. A high yield of the S(-1) state was generated as judged by the two-flash delay in the first maximum of oxygen evolution in Joliot flash-type experiments. We have shown that the Y(Z)* re-reduction rate by the S(-1) state is much slower than that of any other S-state transition in hydrazine-treated samples. This slow reduction rate in the S(-1) to S(0) transition, which is in the order of the S(3) to S(0) transition rate, suggests that this transition is accompanied by some structural rearrangements. Possible explanations of this unique, slow reduction rate in the S(-1) to S(0) transition are considered, in light of earlier observations by others on hydrazine/hydroxylamine reduced PS II samples.     

EPR studies of the water oxidizing complex in the S1 and the higher S states: the manganese cluster and Y(Z) radical

The parallel polarization electron paramagnetic resonance (EPR) method has been applied to investigate manganese EPR signals of native S1 and S3 states of the water oxidizing complex (WOC) in photosystem (PS) II. The EPR signals in both states were assigned to thermally excited states with S=1, from which zero-field interaction parameters D and E were derived. Three kinds of signals, the doublet signal, the singlet-like signal and g=11-15 signal, were detected in Ca2+-depleted PS II. The g=11-15 signal was observed by parallel and perpendicular modes and assigned to a higher oxidation state beyond S2 in Ca2+-depleted PS II. The singlet-like signal was associated with the g=11-15 signal but not with the Y(Z) (the tyrosine residue 161 of the D1 polypeptide in PS II) radical. The doublet signal was associated with the Y(Z) radical as proved by pulsed electron nuclear double resonance (ENDOR) and ENDOR-induced EPR. The electron transfer mechanism relevant to the role of Y(Z) radical was discussed.     

Histidine 332 of the D1 polypeptide modulates the magnetic and redox properties of the manganese cluster and tyrosine Y(Z) in photosystem II

An electron spin-echo envelope modulation study [Tang, X.-S., Diner, B. A., Larsen, B. S., Gilchrist, M. L., Jr., Lorigan, G. A., and Britt, R. D. (1994) Proc. Natl. Acad. Sci. U.S.A. 91, 704-708] and a recent Fourier transform infrared study [Noguchi, T., Inoue, Y., and Tang, X.-S. (1999) Biochemistry 38, 10187-10195], both conducted with [(15)N]histidine-labeled photosystem II particles, show that at least one histidine residue coordinates the O(2)-evolving Mn cluster in photosystem II. Evidence obtained from site-directed mutagenesis studies suggests that one of these residues may be His332 of the D1 polypeptide. The mutation D1-H332E is of particular interest because cells of the cyanobacterium Synechocystis sp. PCC 6803 that contain this mutation evolve no O(2) but appear to assemble Mn clusters in nearly all photosystem II reaction centers [Chu, H.-A., Nguyen, A. P. , and Debus, R. J. (1995) Biochemistry 34, 5859-5882]. Photosystem II particles isolated from the Synechocystis D1-H332E mutant are characterized in this study. Intact D1-H332E photosystem II particles exhibit an altered S(2) state multiline EPR signal that has more hyperfine lines and narrower splittings than the S(2) state multiline EPR signal observed in wild-type PSII particles. However, the quantum yield for oxidizing the S(1) state Mn cluster is very low, corresponding to an 8000-fold slowing of the rate of Mn oxidation by Y(Z)(*), and the temperature threshold for forming the S(2) state is approximately 100 K higher than in wild-type PSII preparations. Furthermore, the D1-H332E PSII particles are unable to advance beyond the Y(Z)(*)S(2) state, as shown by the accumulation of a narrow "split" EPR signal under multiple turnover conditions. In Mn-depleted photosystem II particles, charge recombination between Q(A)(*)(-) and Y(Z)(*) in D1-H332E is accelerated in comparison to wild-type, showing that the mutation alters the redox properties of Y(Z) in addition to those of the Mn cluster. These results are consistent with D1-His332 being located near the Mn-Y(Z) complex and perhaps ligating Mn.     

EPR characteristics of chloride-depleted photosystem II membranes in the presence of other anions.

Chloride is an essential cofactor for the oxidation of water to oxygen. Anion substitution (Br(-), I(-), NO(2)(-), F(-)) in Cl(-)-depleted PS II membranes brings out significant changes in the EPR signals arising from the S(2) state and from the iron-quinone complex of PS II. On the basis of the changes observed in the S(2) state multiline signal and the Q(A)Fe(3+) EPR signal in Cl(-)-depleted PS II membranes after substituting with various anions, we report a possible binding site of anions such as chloride and bromide at the PS II donor side as well as at the acceptor side.     

Interactions of Chloride and Formate at the Donor and the Acceptor Side of Photosystem II

Chloride is required for the maximum activity of the oxygen evolving complex (OEC) while formate inhibits the function of OEC. On the basis of the measurements of oxygen evolution rates and the S₂ state multiline EPR signal, an interaction between the action of chloride and formate at the donor side of PS II has been suggested. Moreover, the Fe₂+Q–A EPR signals were measured to investigate a common binding site of both these anions at the PS II acceptor side. Other monovalent anions like bromide, nitrate etc. could influence the effects of formate to a small extent at the donor side of PS II, but not significantly at the acceptor side of PS II. The results presented in this paper clearly suggest a competitive binding of formate and chloride at the PS II acceptor side.     

Pulsed EPR studies of doublet signal and singlet-like signal in oriented Ca2+-depleted PS II membranes: location of the doublet signal center in PS II

Doublet signal and singlet-like signal induced in Ca(2+)-depleted PS II were investigated by pulsed EPR in one-dimensionally oriented photosystem (PS) II membranes. The doublet signal showed marked angular dependent change in its spectrum in term of the applied magnetic field, indicating that the magnetic dipole-dipole interaction is mainly responsible for the doublet signal. The singlet-like signal also showed angular dependence, which was less pronounced than that of the doublet signal. The parameters of dipole and exchange interactions used to simulate the doublet signal indicate that the signal arises from a magnetically coupled organic radical pair. Angular dependence of the doublet signal indicates that the radius vector of the radical pair (r) and the normal of the thylakoid membrane is at an angle of 65 degrees. Pulsed ELDOR studies in the oriented membranes indicate that the vector (R) connecting the doublet-signal center with the Y(D)(*) radical and the plane of the thylakoid membrane are at an angle of 8 degrees. Furthermore, the angle between the projections of the R and r vectors on the plane of the thylakoid membrane was determined to be 64 degrees. The location of the doublet-signal species in PS II is discussed.     

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.