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.     

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.     

UV-B radiation-induced donor- and acceptor-side modifications of photosystem II in the cyanobacterium Synechocystis sp. PCC 6803.

We studied the effect of UV-B radiation (280-320 nm) on the donor- and acceptor-side components of photosystem II in the cyanobacterium Synechocystis sp. PCC 6803 by measuring the relaxation of flash-induced variable chlorophyll fluorescence. UV-B irradiation increases the t(1/2) of the decay components assigned to reoxidation of Q(A)(-) by Q(B) from 220 to 330 micros in centers which have the Q(B) site occupied, and from 3 to 6 ms in centers with the Q(B) site empty. In contrast, the t(1/2) of the slow component arising from recombination of the Q(A)Q(B)(-) state with the S(2) state of the water-oxidizing complex decreases from 13 to 1-2 s. In the presence of DCMU, fluorescence relaxation in nonirradiated cells is dominated by a 0.5-0.6 s component, which reflects Q(A)(-) recombination with the S(2) state. After UV-B irradiation, this is partially replaced by much faster components (t(1/2) approximately 800-900 micros and 8-10 ms) arising from recombination of Q(A)(-) with stabilized intermediate photosystem II donors, P680(+) and Tyr-Z(+). Measurement of fluorescence relaxation in the presence of different concentrations of DCMU revealed a 4-6-fold increase in the half-inhibitory concentration for electron transfer from Q(A) to Q(B). UV-B irradiation in the presence of DCMU reduces Q(A) in the majority (60%) of centers, but does not enhance the extent of UV-B damage beyond the level seen in the absence of DCMU, when Q(A) is mostly oxidized. Illumination with white light during UV-B treatment retards the inactivation of PSII. However, this ameliorating effect is not observed if de novo protein synthesis is blocked by lincomycin. We conclude that in intact cyanobacterium cells UV-B light impairs electron transfer from the Mn cluster of water oxidation to Tyr-Z(+) and P680(+) in the same way that has been observed in isolated systems. The donor-side damage of PSII is accompanied by a modification of the Q(B) site, which affects the binding of plastoquinone and electron transport inhibitors, but is not related to the presence of Q(A)(-). White light, at the intensity applied for culturing the cells, provides protection against UV-B-induced damage by enhancing protein synthesis-dependent repair of PSII.     

Nonlineal relationship between g=2 doublet and multiline signals in Ca(2+)-depleted Photosystem II

Illuminating of the Ca(2+)-depleted PS II in the S(2) state for a short period induced the doublet signal at g=2 with concomitant diminution of the multiline signal, both in the presence and absence of 3-(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU). In the absence of DCMU, the doublet signal decayed (t(1/2) approximately 7 min) during subsequent dark incubation at 273 K and the multiline signal was regenerated to the original amplitude with the same kinetics of the doublet decay. In the presence of DCMU, the doublet signal decayed much faster (t(1/2) approximately 1 min) by charge recombination with Q(A)(-), while the time course of the multiline recovery was inherently identical with that observed in the absence of DCMU. A simple theoretical consideration indicates the direct conversion from the doublet-signal state to the multiline state with no intermediate state between them. Lengthy dark storage at 77 K led to disappearance of the DCMU-affected doublet signal and a Fe(2+)/Q(A)(-) electron spin resonance (ESR) signal, but no recovery of the multiline signal. Notably, the multiline signal was restored by subsequent dark incubation at 273 K. The charge recombination between Q(A)(-) and the doublet signal species led to a thermoluminescence band at 7 degrees C in a medium at pH 5.5. The peak position shifted to 17 degrees C at pH 7.0, presumably due to a pH-dependent change in the redox property of a donor-side radical species responsible for the doublet signal. Based on these results, redox events in the Ca(2+)-depleted PS II are discussed in contradistinction with the normal processes in oxygen-evolving PS II.     

Insights into the function of PsbR protein in Arabidopsis thaliana

The functional state of the Photosystem (PS) II complex in Arabidopsis psbR T-DNA insertion mutant was studied. The DeltaPsbR thylakoids showed about 34% less oxygen evolution than WT, which correlates with the amounts of PSII estimated from Y(D)(ox) radical EPR signal. The increased time constant of the slow phase of flash fluorescence (FF)-relaxation and upshift in the peak position of the main TL-bands, both in the presence and in the absence of DCMU, confirmed that the S(2)Q(A)(-) and S(2)Q(B)(-) charge recombinations were stabilized in DeltaPsbR thylakoids. Furthermore, the higher amount of dark oxidized Cyt-b559 and the increased proportion of fluorescence, which did not decay during the 100s time span of the measurement thus indicating higher amount of Y(D)(+)Q(A)(-) recombination, pointed to the donor side modifications in DeltaPsbR. EPR measurements revealed that S(1)-to-S(2)-transition and S(2)-state multiline signal were not affected by mutation. The fast phase of the FF-relaxation in the absence of DCMU was significantly slowed down with concomitant decrease in the relative amplitude of this phase, indicating a modification in Q(A) to Q(B) electron transfer in DeltaPsbR thylakoids. It is concluded that the lack of the PsbR protein modifies both the donor and the acceptor side of the PSII complex.     

Probing subtle coordination changes in the iron-quinone complex of photosystem II during charge separation,by the use of NO

The terminal electron acceptor of Photosystem II, PSII, is a linear complex consisting of a primary quinone, a non-heme iron(II), and a secondary quinone, Q(A)Fe(2+)Q(B). The complex is a sensitive site of PSII, where electron transfer is modulated by environmental factors and notably by bicarbonate. Earlier studies showed that NO and other small molecules (CN(-), F(-), carboxylate anions) bind reversibly on the non-heme iron in competition with bicarbonate. In the present study, we report on an unusual new mode of transient binding of NO, which is favored in the light-reduced state (Q(A)(-)Fe(2+)Q(B)) of the complex. The related observations are summarized as follows: (i) Incubation with NO at -30 degrees C, following light-induced charge separation, results in the evolution of a new EPR signal at g = 2.016. The signal correlates with the reduced state Q(A)(-)Fe(2+) of the iron-quinone complex. (ii) Cyanide, at low concentrations, converts the signal to a more rhombic form with g values at 2.027 (peak) and 1.976 (valley), while at high concentrations it inhibits formation of the signals. (iii) Electron spin-echo envelope modulation (ESEEM) experiments show the existence of two protein (14)N nuclei coupled to electron spin. These two nitrogens have been detected consistently in the environment of the semiquinone Q(A)(-) in a number of PSII preparations. (iv) NO does not directly contribute to the signals, as indicated by the absence of a detectable isotopic effect ((15)NO vs (14)NO) in cw EPR. (v) A third signal with g values (2.05, 2.03, 2.01) identical to those of an Fe(NO)(2)(imidazole) synthetic complex develops slowly in the dark, or faster following illumination. (vi) In comparison with the untreated Q(A)(-)Fe(2+) complex, the present signals not only are confined to a narrow spectral region but also saturate at low microwave power. At 11 K the g = 2.016 signal saturates with a P(1/2) of 110 microW and the g = 2.027/1.976 signal with a P(1/2) of 10 microW. (vii) The spectral shape and spin concentration of these signals is successfully reproduced, assuming a weak magnetic interaction (J values in the range 0.025-0.05 cm(-)(1)) between an iron-NO complex with total spin of (1)/(2) and the spin, (1)/(2), of the semiquinone, Q(A)(-). The different modes of binding of NO to the non-heme iron are examined in the context of a molecular model. An important aspect of the model is a trans influence of Q(A) reduction on the bicarbonate ligation to the iron, transmitted via H-bonding of Q(A) with an imidazole ligand to the iron.     

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.     

Nitric oxide-induced formation of the S-2 state in the oxygen-evolving complex of photosystem II from Synechococcus elongatus

In spinach photosystem II (PSII) membranes, the tetranuclear manganese cluster of the oxygen-evolving complex (OEC) can be reduced by incubation with nitric oxide at -30 degrees C to a state which is characterized by an Mn(2)(II, III) EPR multiline signal [Sarrou, J., Ioannidis, N., Deligiannakis, Y., and Petrouleas, V. (1998) Biochemistry 37, 3581-3587]. This state was recently assigned to the S(-)(2) state of the OEC [Schansker, G., Goussias, C., Petrouleas, V., and Rutherford, A. W. (2002) Biochemistry 41, 3057-3064]. On the basis of EPR spectroscopy and flash-induced oxygen evolution patterns, we show that a similar reduction process takes place in PSII samples of the thermophilic cyanobacterium Synechococcus elongatus at both -30 and 0 degrees C. An EPR multiline signal, very similar but not identical to that of the S(-)(2) state in spinach, was obtained with monomeric and dimeric PSII core complexes from S. elongatus only after incubation at -30 degrees C. The assignment of this EPR multiline signal to the S(-)(2) state is corroborated by measurements of flash-induced oxygen evolution patterns and detailed fits using extended Kok models. The small reproducible shifts of several low-field peak positions of the S(-)(2) EPR multiline signal in S. elongatus compared to spinach suggest that slight differences in the coordination geometry and/or the ligands of the manganese cluster exist between thermophilic cyanobacteria and higher plants.     

An EPR study of the pH dependence of formate effects on Photosystem II.

Effects of formate on rates of O(2) evolution and electron paramagnetic resonance (EPR) signals were observed in the oxygen evolving PS II membranes as a function of pH. In formate treated PS II membranes, decrease in pH value resulted in the inhibition of the O(2) evolving activity, a decrease in the intensity of S(2) state multiline signal but an increase in the intensity of the Q(A)(-)Fe(2+) EPR signal. Time-resolved EPR study of the Y(Z)(*) decay kinetics showed that the light-induced intensity of Y(Z)(*) EPR signal was proportional to the formate concentration. The change in the pH affected both the light-induced intensities and the decay rates of Y(Z)(*), which was found to be faster at lower pH. At 253 K, t(1/e) value of Y(Z)(*) decay kinetics was found to be 8-10 s at pH 6.0 and 18-21 s at pH 5.0. The results presented here indicate that the extent of inhibition at the donor and the acceptor side of PS II due to formate is pH dependent, being more effective at lower pH.     

Oxidation of the non-heme iron complex in photosystem II

In photosystem II (PSII), the redox properties of the non-heme iron complex (Fe complex) are sensitive to the redox state of quinones (Q(A/)(B)), which may relate to the electron/proton transfer. We calculated the redox potentials for one-electron oxidation of the Fe complex in PSII [E(m)(Fe)] based on the reference value E(m)(Fe) = +400 mV at pH 7 in the Q(A)(0)Q(B)(0) state, considering the protein environment in atomic detail and the associated changes in protonation pattern. Our model yields the pH dependence of E(m)(Fe) with -60 mV/pH as observed in experimental redox titration. We observed significant deprotonation at D1-Glu244 in the hydrophilic loop region upon Fe complex oxidation. The calculated pK(a) value for D1-Glu244 depends on the Fe complex redox state, yielding a pK(a) of 7.5 and 5.5 for Fe(2+) and Fe(3+), respectively. To account for the pH dependence of E(m)(Fe), a model involving not only D1-Glu244 but also the other titratable residues (five Glu in the D-de loops and six basic residues near the Fe complex) seems to be needed, implying the existence of a network of residues serving as an internal proton reservoir. Reduction of Q(A/B) yields +302 mV and +268 mV for E(m)(Fe) in the Q(A)(-)Q(B)(0) and Q(A)(0)Q(B)(-) states, respectively. Upon formation of the Q(A)(0)Q(B)(-) state, D1-His252 becomes protonated. Forming Fe(3+)Q(B)H(2) by a proton-coupled electron transfer process from the initial state Fe(2+)Q(B)(-) results in deprotonation of D1-His252. The two EPR signals observed at g = 1.82 and g = 1.9 in the Fe(2+)Q(A)(-) state of PSII may be attributed to D1-His252 with variable and fixed protonation, respectively.     

Semiquinone-iron complex of photosystem II: EPR signals assigned to the low-field edge of the ground state doublet of QA•-Fe2+ and QB•-Fe2+

The quinone-iron complex of the electron acceptor complex of Photosystem II was studied by EPR spectroscopy in Thermosynechococcus elongatus. New g ～ 2 features belonging to the EPR signal of the semiquinone forms of the primary and secondary quinone, i.e., Q(A)(?-)Fe(2+) and Q(B)(?-)Fe(2+), respectively, are reported. In previous studies, these signals were missed because they were obscured by the EPR signal arising from the stable tyrosyl radical, TyrD(?). When the TyrD(?) signal was removed, either by chemical reduction or by the use of a mutant lacking TyrD, the new signals dominated the spectrum. For Q(A)(?-)Fe(2+), the signal was formed by illumination at 77 K or by sodium dithionite reduction in the dark. For Q(B)(?-)Fe(2+), the signal showed the characteristic period-of-two variations in its intensity when generated by a series of laser flashes. The new features showed relaxation characteristics comparable to those of the well-known features of the semiquinone-iron complexes and showed a temperature dependence consistent with an assignment to the low-field edge of the ground state doublet of the spin system. Spectral simulations are consistent with this assignment and with the current model of the spin system. The signal was also present in Q(B)(?-)Fe(2+) in plant Photosystem II, but in plants, the signal was not detected in the Q(A)(?-)Fe(2+) state.     

Thermoluminescence studies on the function of Photosystem II in the desiccation tolerant lichen Cladonia convoluta

The effect of desiccation and rehydration on the function of Photosystem II has been studied in the desiccation tolerant lichen Cladonia convoluta by thermoluminescence. We have shown that in functional fully hydrated thalli thermoluminescence signals can be observed from the recombination of the S₂₍₃₎Q_B ^– (B band), S₂Q_A ^– (Q band), Tyr-D⁺Q_A ^– (C band) and Tyr-Z⁺(His⁺)Q_A ^– (A band) charge stabilization states. These thermoluminescence signals are completely absent in desiccated thalli, but rapidly reappear on rehydration. Flash-induced oscillation in the amplitude of the thermoluminescence band from the S₂₍₃₎Q_B ^– recombination shows the usual pattern with maxima after 2 and 6 flashes when rehydration takes place in light. However, after rehydration in complete darkness, there is no thermoluminescence emission after the 1 st flash, and the maxima of the subsequent oscillation are shifted to the 3rd and 7th flashes. It is concluded that desiccation of Cladonia convoluta converts PS II into a nonfunctional state. This state is characterized by the lack of stable charge separation and recombination, as well as by a one-electron reduction of the water-oxidizing complex. Restoration of PS II function during rehydration can proceed both in the light and in darkness. After rehydration in the dark, the first charge separation act is utilized in restoring the usual oxidation state of the water-oxidizing comples.Abbreviations Chl chlorophyll - DCMU 3-(3,4-dichlorophenyl)-1,1-dimethylurea - DT desiccation tolerant - PS II Photosystem II - TL thermoluminescence - P₆₈₀ reaction center Chl of PS II - Q_A and Q_B puinone electron acceptors of PS II - S₀,...,S₄ the redox states of the water-oxidizing complex - Tyr-Z and Tyr-D redox-active tyrosine electron donors of PS II     

Proton equilibria in the manganese cluster of photosystem II control the intensities of the S(0) and S(2) state g approximately 2 electron paramagnetic resonance signals

We have studied the pH effect on the S(0) and S(2) multiline electron paramagnetic resonance (EPR) signals from the water-oxidizing complex of photosystem II. Around pH 6, the maximum signal intensities were detected. On both the acidic and alkaline sides of pH 6, the intensities of the EPR signals decreased. Two pKs were determined for the S(0) multiline signal; pK(1) = 4.2 +/- 0.2 and pK(2) = 8.0 +/- 0.1, and for the S(2) multiline signal the pKs were pK(1) = 4.5 +/- 0.1 and pK(2) = 7.6 +/- 0.1. The intensity of the S(0)-state EPR signal was partly restored when the pH was changed from acidic or alkaline pH back to pH approximately 6. In the S(2) state we observed partial recovery of the multiline signal when going from alkaline pH back to pH approximately 6, whereas no significant recovery of the S(2) multiline signal was observed when the pH was changed from acidic pH back to pH approximately 6. Several possible explanations for the intensity changes as a function of pH are discussed. Some are ruled out, such as disintegration of the Mn cluster or decay of the S states and formal Cl(-) and Ca(2+) depletion. The altered EPR signal intensities probably reflect the protonation/deprotonation of ligands to the Mn cluster or the oxo bridges between the Mn ions. Also, the possibility of decreased multiline signal intensities at alkaline pH as an effect of changed redox potential of Y(Z) is put forward.     

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.     

Decay products of the S(3) state of the oxygen-evolving complex of photosystem II at cryogenic temperatures. Pathways to the formation of the S = 7/2 S(2) state configuration

The water-oxidizing complex of photosystem II cycles through five oxidation states, denoted S(i)() (i = 0-4), during water oxidation to molecular oxygen, which appears at the (transient) S(4) state. The recent detection of bimodal EPR signals from the S(3) state [Matsukawa, T., Mino, H., Yoneda, D., Kawamori, A. (1999) Biochemistry 38, 4072-4077] has drawn significant attention to this critical state. An interesting property of the S(3) state is the sensitivity to near-IR (NIR) light excitation. Excitation of the S(3) state by near-IR light at cryogenic temperatures induces among other signals a derivative-shaped EPR signal at g= 5 [Ioannidis, N., and Petrouleas, V. (2000) Biochemistry 39, 5246-5254]. The signal bears unexpected similarities to a signal observed earlier in samples that had undergone multiple turnovers and subsequently had been stored at 77 K for a week or longer [Nugent, J. H. A., Turconi, S., and Evans, M. C. W. (1997) Biochemistry 36, 7086-7096]. Recently, both signals were assigned to an S = 7/2 configuration of the Mn cluster [Sanakis, Y., Ioannidis, N., Sioros, G., and Petrouleas, V. (2001) J. Am. Chem. Soc. 123, 10766-10767]. In the present study, we employ bimodal EPR spectroscopy to investigate the pathways of formation of this unusual state. The following observations are made: (i) The g = 5 signal evolves in apparent correlation with the diminution of the S(3) state signals during the slow (tens of hours to several days range) charge recombination of S(3) with Q(A)(-) at 77 K. The tyrosyl radical D* competes with S(3) for recombination with Q(A)(-), the functional redox couple at cryogenic temperatures inferred to be D*/D(-). Transfer to -50 degrees C and above results in the relaxation of the g = 5 to the multiline and g = 4.1 signals of the normal S(2) state. (ii) The transition of S(3) to the state responsible for the g = 5 signal can be reversed by visible light illumination directly at -30 degrees C or by illumination at 4.2 K followed by brief (2 min) transfer to -50 degrees C in the dark. The latter step is required in order to overcome an apparent thermal activation barrier (charge recombination appears to be faster than forward electron transfer at 4.2 K). (iii) The "g = 5" state can be reached in a few tens of minutes at 4.2 K by near-IR light excitation of the S(3) state. This effect is attributed to the transfer of the positive hole from the Mn cluster to a radical (probably tyr Z), which recombines much faster than the Mn cluster with Q(A)(-). (iv) The above properties strongly support the assignment of the configuration responsible for the g = 5 signal to a modified S(2) state, denoted S(2)'. Evidence supporting the assignment of the S(2)' to a proton-deficient S(2) configuration is provided by the observation that the spectrum of S(2) at pH 8.1 (obtained by illumination of the S(1) state at -30 degrees C) contains a g = 5 contribution.     

Effects of copper and zinc ions on photosystem II studied by EPR spectroscopy.

The effect of Zn(2+) or Cu(2+) ions on Mn-depleted photosystem II (PS II) has been investigated using EPR spectroscopy. In Zn(2+)-treated and Cu(2+)-treated PS II, chemical reduction with sodium dithionite gives rise to a signal attributed to the plastosemiquinone, Q(A)(*)(-), the usual interaction with the non-heme iron being lost. The signal was identified by Q-band EPR spectroscopy which partially resolves the typical g-anisotropy of the semiquinone anion radical. Illumination at 200 K of the unreduced samples gives rise to a single organic free radical in Cu(2+)-treated PS II, and this is assigned to a monomeric chlorophyll cation radical, Chl a(*)(+), based on its (1)H-ENDOR spectrum. The Zn(2+)-treated PS II under the same conditions gives rise to two radical signals present in equal amounts and attributed to the Chl a(*)(+) and the Q(A)(*)(-) formed by light-induced charge separation. When the Cu(2+)-treated PS II is reduced by sodium ascorbate, at >/=77 K electron donation eliminates the donor-side radical leaving the Q(A)(*)(-) EPR signal. The data are explained as follows: (1) Cu(2+) and Zn(2+) have similar effects on PS II (although higher concentrations of Zn(2+) are required) causing the displacement of the non-heme Fe(2+). (2) In both cases chlorophyll is the electron donor at 200 K. It is proposed that the lack of a light-induced Q(A)(*)(-) signal in the unreduced Cu(2+)-treated sample is due to Cu(2+) acting as an electron acceptor from Q(A)(*)(-) at low temperature, forming the Cu(+) state and leaving the electron donor radical Chl a(*)(+) detectable by EPR. (3) The Cu(2+) in PS II is chemically reducible by ascorbate prior to illumination, and the metal can therefore no longer act as an electron acceptor; thus Q(A)(*)(-) is generated by illumination in such samples. (4) With dithionite, both the Cu(2+) and the quinone are reduced resulting in the presence of Q(A)(*)(-) in the dark. The suggested high redox potential of Cu(2+) when in the Fe(2+) site in PS II is in contrast to the situation in the bacterial reaction center where it has been shown in earlier work that the Cu(2+) is unreduced by dithionite. It cannot be ruled out however that Q(A)-Cu(2+) is formed and a magnetic interaction is responsible for the lack of the Q(A)(-) signal when no exogenous reductant is present. With this alternative possibility, the effects of reductants would be explained as the loss of Cu(2+) (due to formation of Cu(+)) leading to loss of the Cu(2+) from the Fe(2+) site due to the binding equilibrium. The quite different binding and redox behavior of the metal in the iron site in PS II compared to that of the bacterial reaction center is presumably a further reflection of the differences in the coordination of the iron in the two systems.     

Inactivation of photosynthetic oxygen evolution by UV-B irradiation: A thermoluminescence study

The influence of UV-B irradiation on photosynthetic oxygen evolution by isolated spinach thylakoids has been investigated using thermoluminescence measurements. The thermoluminescence bands arising from the S₂Q_B ^- (B band) and S₂Q_A ^– (Q band) charge recombination disappeared with increasing UV-B irradiation time. In contrast, the C band at 50°C, arising from the recombination of Q_A ^- with an accessory donor of Photosystem II, was transiently enhanced by the UV-B irradiation. The efficiency of DCMU to block Q_A to Q_B electron transfer decreased after irradiation as detected by the incomplete suppression of the B band by DCMU. The flash-induced oscillatory pattern of the B band was modified in the UV-B irradiated samples, indicating a decrease in the number of centers with reduced Q_B. Based on the results of this study, UV-B irradiation is suggested to damage both the donor and acceptor sides of Photosystem II. The damage of the water-oxidizing complex does not affect a specific S-state transition. Instead, charge stabilization is enhanced on an accessory donor. The acceptor-side modifications decrease the affinity of DCMU binding. This effect is assumed to reflect a structural change in the Q_B/DCMU binding site. The preferential loss of dark stable Q_B ^- may be related to the same structural change or could be caused by the specific destruction of reduced quinones by the UV-B light.Abbreviations Chl chlorophyll - DCMU 3-(3,4,-dichlorophenyl)-1,1-dimethylurea - PS II Photosystem II - Q_A first quinone electron acceptor of PS II - Q_B second quinone electron acceptor of PS II - Tyr-D accessory electron donor of PS II - S₀-S₄ charge storage states of the water-oxidizing complex     

Ammonia-induced structural changes of the oxygen-evolving complex in photosystem II as revealed by light-induced FTIR difference spectroscopy

Light-induced Fourier transform infrared difference spectroscopy has been applied to studies of ammonia effects on the oxygen-evolving complex (OEC) of photosystem II (PSII). We found that NH(3) induced characteristic spectral changes in the region of the symmetric carboxylate stretching modes (1450-1300 cm(-1)) of the S(2)Q(A)(-)/S(1)Q(A) FTIR difference spectra of PSII. The S(2) state carboxylate mode at 1365 cm(-1) in the S(2)Q(A)(-)/S(1)Q(A) spectrum of the controlled samples was very likely upshifted to 1379 cm(-1) in that of NH(3)-treated samples; however, the frequency of the corresponding S(1) carboxylate mode at 1402 cm(-1) in the same spectrum was not significantly affected. These two carboxylate modes have been assigned to a Mn-ligating carboxylate whose coordination mode changes from bridging or chelating to unidentate ligation during the S(1) to S(2) transition [Noguchi, T., Ono, T., and Inoue, Y. (1995) Biochim. Biophys. Acta 1228, 189-200; Kimura, Y., and Ono, T.-A. (2001) Biochemistry 40, 14061-14068]. Therefore, our results show that NH(3) induced significant structural changes of the OEC in the S(2) state. In addition, our results also indicated that the NH(3)-induced spectral changes of the S(2)Q(A)(-)/S(1)Q(A) spectrum of PSII are dependent on the temperature of the FTIR measurement. Among the temperatures we measured, the strongest effect was seen at 250 K, a lesser effect was seen at 225 K, and little or no effect was seen at 200 K. Furthermore, our results also showed that the NH(3) effects on the S(2)Q(A)(-)/S(1)Q(A) spectrum of PSII are dependent on the concentrations of NH(4)Cl. The NH(3)-induced upshift of the 1365 cm(-1) mode is apparent at 5 mM NH(4)Cl and is completely saturated at 100 mM NH(4)Cl concentration. Finally, we found that CH(3)NH(2) has a small but clear effect on the spectral change of the S(2)Q(A)(-)/S(1)Q(A) FTIR difference spectrum of PSII. The effects of amines on the S(2)Q(A)(-)/S(1)Q(A) FTIR difference spectra (NH(3) > CH(3)NH(2) > AEPD and Tris) are inverse proportional to their size (Tris approximately AEPD > CH(3)NH(2) > NH(3)). Therefore, our results showed that the effects of amines on the S(2)Q(A)(-)/S(1)Q(A) spectrum of PSII are sterically selective for small amines. On the basis of the correlations between the conditions (dependences on the excitation temperature and NH(3) concentration and the steric requirement for the amine effects) that give rise to the NH(3)-induced upshift of the 1365 cm(-)(1) mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum of PSII and the conditions that give rise to the altered S(2) state multiline EPR signal, we propose that the NH(3)-induced upshift of the 1365 cm(-1) mode is caused by the binding of NH(3) to the site on the Mn cluster that gives rise to the altered S(2) state multiline EPR signal. In addition, we found no significant NH(3)-induced change in the S(2)Q(A)(-)/S(1)Q(A) FTIR difference spectrum at 200 K. Under this condition, the OEC gives rise to the NH(3)-stabilized g = 4.1 EPR signal and a suppressed g = 2 multiline EPR signal. Our results suggest that the structural difference of the OEC between the normal g = 2 multiline form and the NH(3)-stabilized g = 4.1 form is small.     

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.