Drastic changes in the ligand structure of the oxygen-evolving Mn cluster upon Ca2+ depletion as revealed by FTIR difference spectroscopy

A Fourier transform infrared (FTIR) difference spectrum of the oxygen-evolving Mn cluster upon the S(1)-to-S(2) transition was obtained with Ca(2+)-depleted photosystem II (PSII) membranes to investigate the structural relevance of Ca(2+) to the Mn cluster. Previously, Noguchi et al. [Biochim. Biophys. Acta 1228 (1995) 189] observed drastic changes in the carboxylate stretching region of the S(2)/S(1) FTIR spectrum upon Ca(2+) depletion, whereas Kimura and co-workers [Biochemistry 40 (2001) 14061; ibid. 41 (2002) 5844] later claimed that these changes were not ascribed to Ca(2+) depletion itself but caused by the interaction of EDTA to the Mn cluster and/or binding of K(+) at the Ca(2+) site. In the present study, the preparation of the Ca(2+)-depleted PSII sample and its FTIR measurement were performed in the absence of EDTA and K(+). The obtained S(2)/S(1) spectrum exhibited the loss of carboxylate bands at 1587/1562 and 1364/1403 cm(-1) and diminished amide I intensities, which were identical to the previous observations in the presence of EDTA and K(+). This result indicates that the drastic FTIR changes are a pure effect of Ca(2+) depletion, and provides solid evidence for the general view that Ca(2+) is strongly coupled with the Mn cluster.     

Low-frequency fourier transform infrared spectroscopy of the oxygen-evolving and quinone acceptor complexes in photosystem II

The low-frequency (<1000 cm-1) region of the IR spectrum has the potential to provide detailed structural and mechanistic insight into the photosystem II/oxygen evolving complex (PSII/OEC). A cluster of four manganese ions forms the core of the OEC and diagnostic manganese-ligand and manganese-substrate modes are expected to occur in the 200-900 cm-1 range. However, water also absorbs IR strongly in this region, which has limited previous Fourier transform infrared (FTIR) spectroscopic studies of the OEC to higher frequencies (>1000 cm-1). We have overcome the technical obstacles that have blocked FTIR access to low-frequency substrate, cofactor, and protein vibrational modes by using partially dehydrated samples, appropriate window materials, a wide-range MCT detector, a novel band-pass filter, and a closely regulated temperature control system. With this design, we studied PSII/OEC samples that were prepared by brief illumination of O2 evolving and Tris-washed preparations at 200 K or by a single saturating laser flash applied to O2 evolving and inhibited samples at 250 K. These protocols allowed us to isolate low-frequency modes that are specific to the QA-/QA and S2/S1 states. The high-frequency FTIR spectra recorded for these samples and parallel EPR experiments confirmed the states accessed by the trapping procedures we used. In the S2/S1 spectrum, we detect positive bands at 631 and 602 cm-1 and negative bands at 850, 679, 664, and 650 cm-1 that are specifically associated with these two S states. The possible origins of these IR bands are discussed. For the low-frequency QA-/QA difference spectrum, several modes can be assigned to ring stretching and bending modes from the neutral and anion radical states of the quinone acceptor. These results provide insight into the PSII/OEC and demonstrate the utility of FTIR techniques in accessing low-frequency modes in proteins.     

Steady-state FTIR spectra of the photoreduction of QA and QB in Rhodobacter sphaeroides reaction centers provide evidence against the presence of a proposed transient electron acceptor X between the two quinones

In the reaction center (RC) of the photosynthetic bacterium Rhodobacter sphaeroides, two ubiquinone molecules, QA and QB, play a pivotal role in the conversion of light energy into chemical free energy by coupling electron transfer to proton uptake. In native RCs, the transfer of an electron from QA to QB takes place in the time range of 5-200 micros. On the basis of time-resolved FTIR step-scan measurements in native RCs, a new and unconventional mechanism has been proposed in which QB- formation precedes QA- oxidation [Remy, A., and Gerwert, K. (2003) Nat. Struct. Biol. 10, 637-644]. The IR signature of the proposed transient intermediary electron acceptor (denoted X) operating between QA and QB has been recently measured by the rapid-scan technique in the DN(L210) mutant RCs, in which the QA to QB electron transfer is slowed 8-fold compared to that in native RCs. This IR signature has been reported as a difference spectrum involving states X+, X, QA, and QA- [Hermes, S., et al. (2006) Biochemistry 45, 13741-13749]. Here, we report the steady-state FTIR difference spectra of the photoreduction of either QA or QB measured in both native and DN(L210) mutant RCs in the presence of potassium ferrocyanide. In these spectra, the CN stretching marker modes of ferrocyanide and ferricyanide allow the extent of the redox reactions to be quantitatively compared and are used for a precise normalization of the QA-/QA and QB-/QB difference spectra. The calculated QA- QB/QA QB- double-difference spectrum in DN(L210) mutant RCs is closely equivalent to the reported QA- X+/QA X spectrum in the rapid-scan measurement. We therefore conclude that species X+ and X are spectrally indistinguishable from QB and QB-, respectively. Further comparison of the QA- QB/QA QB- double-difference spectra in native and DN(L210) RCs also allows the possibility that QB- formation precedes QA- reoxidation to be ruled out for native RCs.     

The unusually strong hydrogen bond between the carbonyl of Q(A) and His M219 in the Rhodobacter sphaeroides reaction center is not essential for efficient electron transfer from Q(A)(-) to Q(B)

In native reaction centers (RCs) from photosynthetic purple bacteria the primary quinone (QA) and the secondary quinone (QB) are interconnected via a specific His-Fe-His bridge. In Rhodobacter sphaeroides RCs the C4=O carbonyl of QA forms a very strong hydrogen bond with the protonated Npi of His M219, and the Ntau of this residue is in turn coordinated to the non-heme iron atom. The second carbonyl of QA is engaged in a much weaker hydrogen bond with the backbone N-H of Ala M260. In previous work, a Trp side chain was introduced by site-directed mutagenesis at the M260 position in the RC of Rb. sphaeroides, resulting in a complex that is completely devoid of QA and therefore nonfunctional. A photochemically competent derivative of the AM260W mutant was isolated that contains a Cys side chain at the M260 position (denoted AM260(W-->C)). In the present work, the interactions between the carbonyl groups of QA and the protein in the AM260(W-->C) suppressor mutant have been characterized by light-induced FTIR difference spectroscopy of the photoreduction of QA. The QA-/QA difference spectrum demonstrates that the strong interaction between the C4=O carbonyl of QA and His M219 is lost in the mutant, and the coupled CO and CC modes of the QA- semiquinone are also strongly perturbed. In parallel, a band assigned to the perturbation of the C5-Ntau mode of His M219 upon QA- formation in the native RC is lacking in the spectrum of the mutant. Furthermore, a positive band between 2900 and 2400 cm-1 that is related to protons fluctuating within a network of highly polarizable hydrogen bonds in the native RC is reduced in amplitude in the mutant. On the other hand, the QB-/QB FTIR difference spectrum is essentially the same as for the native RC. The kinetics of electron transfer from QA- to QB were measured by the flash-induced absorption changes at 780 nm. Compared to native RCs the absorption transients are slowed by a factor of about 2 for both the slow phase (in the hundreds of microseconds range) and fast phase (microseconds to tens of microseconds range) in AM260(W-->C) RCs. We conclude that the unusually strong hydrogen bond between the carbonyl of QA and His M219 in the Rb. sphaeroides RC is not obligatory for efficient electron transfer from QA- to QB.     

Specific isotopic labeling and photooxidation-linked structural changes in the manganese-stabilizing subunit of photosystem II

Photosystem II (PSII) oxidizes water to molecular oxygen; the catalytic site is a cluster of four manganese ions. The catalytic site undergoes four sequential light-driven oxidation steps to form oxygen; these sequentially oxidized states are referred to as the Sn states, where n refers to the number of oxidizing equivalents stored. The extrinsic manganese stabilizing protein (MSP) of PSII influences the efficiency and stability of the manganese cluster, as well as the rates of the S state transitions. To understand how MSP influences photosynthetic water oxidation, we have employed isotope editing and difference Fourier transform infrared spectroscopy. MSP was expressed in Escherichia coli under conditions in which MSP aspartic and glutamic acid residues label at yields of 65 and 41%, respectively. Asparagine and glutamine were also labeled by this approach. GC/MS analysis was consistent with minimal scrambling of label into other amino acid residues and with no significant scrambling into the peptide bond. Selectively labeled MSP was then reconstituted to PSII, which had been stripped of native MSP. Difference Fourier transform infrared spectroscopy was used to probe the S1QA to S2QA- transition at 200 K, as well as the S1QB to S2QB- transition at 277 K. These experiments show that aspargine, glutamine, and glutamate residues in MSP are perturbed by photooxidation of manganese during the S1 to S2 transition.     

Energetics of primary and secondary electron transfer in Photosystem II membrane particles of spinach revisited on basis of recombination-fluorescence measurements

Photon absorption by one of the roughly 200 chlorophylls of the plant Photosystem II (PSII) results in formation of an equilibrated excited state (Chl200*) and is followed by chlorophyll oxidation (formation of P680+) coupled to reduction of a specific pheophytin (Phe), then electron transfer from Phe- to a firmly bound quinone (QA), and subsequently reduction of P680+ by a redox-active tyrosine residue denoted as Z. The involved free-energy differences (DeltaG) and redox potentials are of prime interest. Oxygen-evolving PSII membrane particles of spinach were studied at 5 degrees C. By analyzing the delayed and prompt Chl fluorescence, we determined the equilibrium constant and thus free-energy difference between Chl200* and the [Z+,QA-] radical pair to be -0.43+/-0.025 eV, at 10 mus after the photon absorption event for PSII in its S(3)-state. On basis of this value and previously published results, the free-energy difference between P680* and [P680+,QA-] is calculated to be -0.50+/-0.04 eV; the free-energy loss associated with electron transfer from Phe to QA is found to be 0.34+/-0.04 eV. The given uncertainty ranges do not represent a standard deviation or likely error, but an estimate of the maximal error. Assuming a QA-/QA redox potential of -0.08 V, the following redox-potential estimates are obtained: +1.25 V for P680/P680+; +1.21 V for Z/Z+ (at 10 mus); -0.42 V for Phe-/Phe; -0.58 V for P680*/P680+.     

Conformational heterogeneity of the bacteriopheophytin electron acceptor HA in reaction centers from Rhodopseudomonas viridis revealed by Fourier transform infrared spectroscopy and site-directed mutagenesis.

The light-induced Fourier transform infrared (FTIR) difference spectra corresponding to the photoreduction of either the HA bacteriopheophytin electron acceptor (HA-/HA spectrum) or the QA primary quinone (QA-/QA spectrum) in photosynthetic reaction centers (RCs) of Rhodopseudomonas viridis are reported. These spectra have been compared for wild-type (WT) RCs and for two site-directed mutants in which the proposed interactions between the carbonyls on ring V of HA and the RC protein have been altered. In the mutant EQ(L104), the putative hydrogen bond between the protein and the 9-keto C=O of HA should be affected by changing Glu L104 to a Gln. In the mutant WF(M250), the van der Waals interactions between Trp M250 and the 10a-ester C=O of HA should be modified. The characteristic effects of both mutations on the FTIR spectra support the proposed interactions and allow the IR modes of the 9-keto and 10a-ester C=O of HA and HA- to be assigned. Comparison of the HA-/HA and QA-/QA spectra leads us to conclude that the QA-/QA IR signals in the spectral range above 1700 cm-1 are largely dominated by contributions from the electrostatic response of the 10a-ester C=O mode of HA upon QA photoreduction. A heterogeneity in the conformation of the 10a-ester C=O mode of HA in WT RCs, leading to three distinct populations of HA, appears to be related to differences in the hydrogen-bonding interactions between the carbonyls of ring V of HA and the RC protein. The possibility that this structural heterogeneity is related to the observed multiexponential kinetics of electron transfer and the implications for primary processes are discussed. The effect of 1H/2H exchange on the QA-/QA spectra of the WT and mutant RCs shows that neither Glu L104 nor any other exchangeable carboxylic residue changes appreciably its protonation state upon QA reduction.     

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.     

Glutamate-354 of the CP43 polypeptide interacts with the oxygen-evolving Mn4Ca cluster of photosystem II: a preliminary characterization of the Glu354Gln mutant

In the recent X-ray crystallographic structural models of photosystem II, Glu354 of the CP43 polypeptide is assigned as a ligand of the O2-evolving Mn4Ca cluster. In this communication, a preliminary characterization of the CP43-Glu354Gln mutant of the cyanobacterium Synechocystis sp. PCC 6803 is presented. The steady-state rate of O2 evolution in the mutant cells is only approximately 20% compared with the wild-type, but the kinetics of O2 release are essentially unchanged and the O2-flash yields show normal period-four oscillations, albeit with lower overall intensity. Purified PSII particles exhibit an essentially normal S2 state multiline electron paramagnetic resonance (EPR) signal, but exhibit a substantially altered S2-minus-S1 Fourier transform infrared (FTIR) difference spectrum. The intensities of the mutant EPR and FTIR difference spectra (above 75% compared with wild-type) are much greater than the O2 signals and suggest that CP43-Glu354Gln PSII reaction centres are heterogeneous, with a minority fraction able to evolve O2 with normal O2 release kinetics and a majority fraction unable to advance beyond the S2 or S3 states. The S2-minus-S1 FTIR difference spectrum of CP43-Glu354Gln PSII particles is altered in both the symmetric and asymmetric carboxylate stretching regions, implying either that CP43-Glu354 is exquisitely sensitive to the increased charge that develops on the Mn4Ca cluster during the S1-->S2 transition or that the CP43-Glu354Gln mutation changes the distribution of Mn(III) and Mn(IV) oxidation states within the Mn4Ca cluster in the S1 and/or S2 states.     

Drastic changes in the ligand structure of the oxygen-evolving Mn cluster upon Ca depletion as revealed by FTIR difference spectroscopy

A Fourier transform infrared (FTIR) difference spectrum of the oxygen-evolving Mn cluster upon the S₁-to-S₂ transition was obtained with Ca²⁺-depleted photosystem II (PSII) membranes to investigate the structural relevance of Ca²⁺ to the Mn cluster. Previously, Noguchi et al. [Biochim. Biophys. Acta 1228 (1995) 189] observed drastic changes in the carboxylate stretching region of the S₂/S₁ FTIR spectrum upon Ca²⁺ depletion, whereas Kimura and co-workers [Biochemistry 40 (2001) 14061; ibid. 41 (2002) 5844] later claimed that these changes were not ascribed to Ca²⁺ depletion itself but caused by the interaction of EDTA to the Mn cluster and/or binding of K⁺ at the Ca²⁺ site. In the present study, the preparation of the Ca²⁺-depleted PSII sample and its FTIR measurement were performed in the absence of EDTA and K⁺. The obtained S₂/S₁ spectrum exhibited the loss of carboxylate bands at 1587/1562 and 1364/1403 cm^− 1 and diminished amide I intensities, which were identical to the previous observations in the presence of EDTA and K⁺. This result indicates that the drastic FTIR changes are a pure effect of Ca²⁺ depletion, and provides solid evidence for the general view that Ca²⁺ is strongly coupled with the Mn cluster.     

D1-Asp170 is structurally coupled to the oxygen evolving complex in photosystem II as revealed by light-induced Fourier transform infrared difference spectroscopy

We report both mid-frequency (1800-1200 cm(-)(1)) and low-frequency (670-350 cm(-)(1)) S(2)/S(1) FTIR difference spectra of photosystem II (PSII) particles isolated from wild-type and D1-D170H mutant cells of the cyanobacterium Synechocystis sp. PCC 6803. Both mid- and low-frequency S(2)/S(1) spectra of the Synechocystis wild-type PSII particles closely resemble those from spinach PSII samples, which confirms an earlier result by Noguchi and co-workers [Noguchi, T., Inoue, Y., and Tang, X.-S. (1997) Biochemistry 36, 14705-14711] and indicates that the coordination environment of the oxygen evolving complex (OEC) in Synechocystis is very similar to that in spinach. We also found that there is no appreciable difference between the mid-frequency S(2)/S(1) spectra of wild-type and of D1-D170H mutant PSII particles, from which we conclude that D1-Asp170 does not undergo a significant structural change during the S(1) to S(2) transition. This result also suggests that, if D1-Asp170 ligates Mn, it does not ligate the Mn ion that is oxidized during the S(1) to S(2) state transition. Finally, we found that a mode at 606 cm(-)(1) in the low-frequency wild-type S(2)/S(1) spectrum shifts to 612 cm(-)(1) in the D1-D170H mutant spectrum. Because this 606 cm(-)(1) mode has been previously assigned to an Mn-O-Mn cluster mode of the OEC [Chu, H.-A., Sackett, H., and Babcock, G. T. (2000) Biochemistry 39, 14371-14376], we conclude that D1-Asp170 is structurally coupled to the Mn-O-Mn cluster structure that gives rise to this band. Our results suggest that D1-Asp170 either directly ligates Mn or Ca(2+) or participates in a hydrogen bond to the Mn(4)Ca(2+) cluster. Our results demonstrate that combining FTIR difference spectroscopy with site-directed mutagenesis has the potential to provide insights into structural changes in Mn and Ca(2+) coordination environments in the different S states of the OEC.     

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+).     

Modulation of flash-induced photosystem II fluorescence by events occurring at the water oxidizing complex.

The mechanism of flash-induced changes with a periodicity of four in photosystem II (PSII) fluorescence was investigated with the aim of further using fluorescence measurements as an approach to studying the structural and functional organization of the water-oxidizing complex (WOC). The decay of the flash-induced high fluorescence state of PSII was measured with pulse amplitude modulated fluorometry in thylakoids and PSII enriched membrane fragments. Calculated QA- decay was well described by three exponential decay components, reflecting QA- reoxidation with halftimes of 450 and 860 micros, 2 and 7.6 ms, and 111 and 135 ms in thylakoids and PSII membranes, respectively. The effect of modification of the PSII donor side by changing pH or by removal of the extrinsic 17 and 24 kDa proteins on period four oscillations in both maximum fluorescence yield and the relative contribution of QA- reoxidation reactions was compared to flash-induced oxygen yield. The four-step oxidation of the manganese cluster of the WOC was found to be necessary but not sufficient to produce modulation of PSII fluorescence. The capacity of the WOC to generate molecular oxygen was also required to observe a period four in the fluorescence; however, direct quenching by oxygen was not responsible for the modulation. Potential mechanisms responsible for the periodicity of four in both maximum fluorescence yield pattern and flash-dependent changes in proportion of centers with different QA- reoxidation rates are discussed with respect to intrinsic deprotonation events occurring at the WOC.     

Chloride cofactor in the photosynthetic oxygen-evolving complex studied by fourier transform infrared spectroscopy

Fourier transform infrared (FTIR) spectroscopy, using midfrequency S2/S1 FTIR difference spectra, has been applied to studies of chloride cofactor in the photosynthetic oxygen-evolving complex (OEC) to determine the effects of Cl(-) depletion and monovalent anion substitution. Cl(-) depletion resulted in the disappearance of a large part of the amide I and II vibrational modes, and induced characteristic modification in the features of the stretching modes of the carboxylate ligands of the Mn cluster. The normal spectral features were largely restored by replenishment of Cl(-) except for some changes in amide bands. The overall features of Br(-) -, I(-) -, or NO3(-) -substituted spectra were similar to those of the Cl(-) -reconstituted spectrum, consistent with their ability to support oxygen evolution. In contrast, the spectrum was significantly altered by the replacement of Cl(-) with F- or CH3COO(-), which resulted in marked suppression and distortion of both the carboxylate and amide bands. The activity of oxygen evolution restored by NO3(-) was as high as that by Cl(-) when measured under limited light conditions, indicating that the NO3(-) -substituted OEC is fully active in oxygen evolution, although with a slow turnover rate. The double-difference spectrum between the 14NO3(-) -substituted and 15NO3- -substituted S2/S1 difference spectrum showed isotopic bands for asymmetric NO stretching mode in the region of 1400-1300 cm(-1) due to NO3(-) bound to the Cl(-) site. This demonstrated structural coupling between the Cl(-) site and the Mn cluster. A proposed model for the isotopic bands suggested that Cl(-) as well as NO3(-) is not directly associated with the Mn cluster and exists in a more symmetric configuration and weaker binding state in the S2 state than in the S1 state. These results also suggest that Cl(-) is required for changes in the structure of the specific carboxylate ligand of the Mn cluster as well as the peptide backbone of protein matrixes upon the transition from S1 to S2.     

Participation of glutamate-354 of the CP43 polypeptide in the ligation of manganese and the binding of substrate water in photosystem II

In the current X-ray crystallographic structural models of photosystem II, Glu354 of the CP43 polypeptide is the only amino acid ligand of the oxygen-evolving Mn(4)Ca cluster that is not provided by the D1 polypeptide. To further explore the influence of this structurally unique residue on the properties of the Mn(4)Ca cluster, the CP43-E354Q mutant of the cyanobacterium Synechocystis sp. PCC 6803 was characterized with a variety of biophysical and spectroscopic methods, including polarography, EPR, X-ray absorption, FTIR, and mass spectrometry. The kinetics of oxygen release in the mutant were essentially unchanged from those in wild type. In addition, the oxygen flash yields exhibited normal period four oscillations having normal S state parameters, although the yields were lower, correlating with the mutant's lower steady-state rate (approximately 20% compared to wild type). Experiments conducted with H(2)(18)O showed that the fast and slow phases of substrate water exchange in CP43-E354Q thylakoid membranes were accelerated 8.5- and 1.8-fold, respectively, in the S(3) state compared to wild type. Purified oxygen-evolving CP43-E354Q PSII core complexes exhibited a slightly altered S(1) state Mn-EXAFS spectrum, a slightly altered S(2) state multiline EPR signal, a substantially altered S(2)-minus-S(1) FTIR difference spectrum, and an unusually long lifetime for the S(2) state (>10 h) in a substantial fraction of reaction centers. In contrast, the S(2) state Mn-EXAFS spectrum was nearly indistinguishable from that of wild type. The S(2)-minus-S(1) FTIR difference spectrum showed alterations throughout the amide and carboxylate stretching regions. Global labeling with (15)N and specific labeling with l-[1-(13)C]alanine revealed that the mutation perturbs both amide II and carboxylate stretching modes and shifts the symmetric carboxylate stretching modes of the α-COO(-) group of D1-Ala344 (the C-terminus of the D1 polypeptide) to higher frequencies by 3-4 cm(-1) in both the S(1) and S(2) states. The EPR and FTIR data implied that 76-82% of CP43-E354Q PSII centers can achieve the S(2) state and that most of these can achieve the S(3) state, but no evidence for advancement beyond the S(3) state was observed in the FTIR data, at least not in a majority of PSII centers. Although the X-ray absorption and EPR data showed that the CP43-E354Q mutation only subtly perturbs the structure and spin state of the Mn(4)Ca cluster in the S(2) state, the FTIR and H(2)(18)O exchange data show that the mutation strongly influences other properties of the Mn(4)Ca cluster, altering the response of numerous carboxylate and amide groups to the increased positive charge that develops on the cluster during the S(1) to S(2) transition and weakening the binding of both substrate water molecules (or water-derived ligands), especially the one that exchanges rapidly in the S(3) state. The FTIR data provide evidence that CP43-Glu354 coordinates to the Mn(4)Ca cluster in the S(1) state as a bridging ligand between two metal ions but provide no compelling evidence that this residue changes its coordination mode during the S(1) to S(2) transition. The H(2)(18)O exchange data provide evidence that CP43-Glu354 interacts with the Mn ion that ligates the substrate water molecule (or water-derived ligand) that is in rapid exchange in the S(3) state.     

Improvement by benzoquinones of the quantum yield of photoactivation of photosynthetic oxygen evolution: direct evidence for the two-quantum mechanism.

Effects of eight differently substituted 1,4-benzoquinones (BQs) on the quantum yield of photoactivation of oxygen evolution (reconstitution of the Mn cluster) were examined with wheat photosystem II (PSII) membranes depleted of the Mn cluster by treatment with 1.0 mM NH2OH. Illumination with 10 flashes at 0.25-s intervals of the PSII membranes in the presence of 2.0 mM Mn2+, 20 mM Ca2+, and 1.2 M Cl- restored 14% of oxygen-evolving activity destroyed by the NH2OH treatment. Among the benzoquinones tested, DBMIB (2,5-dibromo-3-methyl-6-isopropyl-BQ) and tetramethyl-BQ did not enhance the activity recovery, but all the others doubled the recovery when present at their optimal concentrations during illumination. The order of effectiveness was tetrabromo-, phenyl-, and 2,6-dichloro-BQs greater than or equal to 2,5-dichloro-BQ greater than tetrachloro-BQ greater than 2,5-dimethyl-BQ, though the differences were small. This order reflects their efficiencies as electron acceptors of PSII. This finding, together with others, suggests that the enhancement of activity recovery results from rapid oxidation by the benzoquinones of the reduced form of the quinone acceptors in PSII, QA- and QB-, which cause loss of an oxidized intermediate through charge-recombination reaction with Mn3+. The flash-number dependence of the recovery of oxygen-evolving activity indicated that the activity was not restored after one flash but recovered significantly after illumination with two flashes and then further increased upon additional flashes. This provides direct evidence that the minimum quantum requirement for photoactivation is two.     

Evidence for delocalized anticooperative flash induced proton binding as revealed by mutants at the M266His iron ligand in bacterial reaction centers

Bacterial reaction centers (RCs) convert light energy into chemical free energy via the double reduction and protonation of the secondary quinone electron acceptor, QB, to the dihydroquinone QBH2. Two RC mutants (M266His --> Leu and M266His --> Ala) with a modified ligand of the non-heme iron have been studied by flash-induced absorbance change spectroscopy. No important changes were observed for the rate constants of the first and second electron transfers between the first quinone electron acceptor, QA, and QB. However, in the M266HL mutant a destabilization of approximately 40 meV of the free energy level of QA- was observed, at variance with the M266HA mutant. The superposition of the three-dimensional X-ray structures of the three proteins in the QA region provides no obvious explanation for the energy modification in the M266HL mutant. The shift of the midpoint redox potential of QA/QA- in M266HL caused accelerated recombination of the charges in the P+ QA- state of the RCs where the native QA was replaced by a low potential anthraquinone (AQA). As previously reported for the native RCs, in the M266HL we observed a biphasicity of the P+ AQA- --> P AQA charge recombination. Interestingly, both phases present a similar acceleration in the M266HL mutant with respect to the wild type. The pH dependencies of the proton uptake upon QA- and QB- formations are superimposable in both mutants but very different from those of native RCs. The data measured in mutants are similar to those that we previously obtained on strains modified at various sites of the cytoplasmic region. The similarity of the response to these different mutations is puzzling, and we propose that it arises from a collective behavior of multiple acidic residues resulting in strongly anticooperative proton binding. The unspecific disappearance of the high pH band of proton uptake observed in all these mutants appears as the natural consequence of removing any member of an interactive proton cluster. This long range interaction also accounts for the similar responses to mutations of the proton uptake pattern induced by either QA- or QB-. We surmise that the presence of an extended protonated water H-bond network providing protons to QB is responsible for these effects.     

Light-induced FTIR difference spectroscopy of the S(2)-to-S(3) state transition of the oxygen-evolving complex in Photosystem II

We have applied flash-induced FTIR spectroscopy to study structural changes upon the S(2)-to-S(3) state transition of the oxygen-evolving complex (OEC) in Photosystem II (PSII). We found that several modes in the difference IR spectrum are associated with bond rearrangements induced by the second laser flash. Most of these IR modes are absent in spectra of S(2)/S(1), of the acceptor-side non-heme ion, of Yradical(D)/Y(D) and of S(3)'/S(2)' from Ca-depleted PSII preparations. Our results suggest that these IR modes most likely originate from structural changes in the oxygen-evolving complex itself upon the S(2)-to-S(3) state transition in PSII.     

Flash-induced FTIR difference spectra of the water oxidizing complex in moderately hydrated photosystem II core films: effect of hydration extent on S-state transitions

Differently hydrated films of photosystem II (PSII) core complexes from Synechococcus elongatus were prepared in a humidity-controlled infrared cell. The relative humidity was changed by a simple method of placing a different ratio of glycerol/water solution in the sealed cell. The extent of hydration of the PSII film was lowered as the glycerol ratio increased. FTIR difference spectra of the water oxidizing complex upon the first to sixth flashes were measured at 10 degrees C using these hydrated PSII films. The FTIR spectra (1800-1200 cm(-1)) of the PSII films hydrated using 20% and 40% glycerol/water showed basically the same features as those of the core sample in solution [Noguchi, T., and Sugiura, M. (2001) Biochemistry 40, 1497-1502], and the prominent peaks exhibited clear period four oscillation patterns. These observations indicate that the S-state cycle properly functions in these hydrated samples. In the PSII films less hydrated, however, the efficiencies of S-state transitions decreased as the extent of hydration was lowered. This tendency was more significant in the S2 --> S3 and S3 --> S0 transitions than in the S1 --> S2 and S0 --> S1 transitions, indicating that the reactions or movements of water molecules are more strongly coupled with the former two transitions than the latter two. The implication of this observation was discussed in light of the water oxidizing mechanism especially in respect to the steps of substrate incorporation and proton release. Furthermore, in the OH stretching region (3800-3000 cm(-1)) of the first-flash spectrum, a differential signal was observed at 3618/3585 cm(-1), which was previously found in the S2/S1 spectrum of a frozen sample at 250 K and assigned to the water vibrations [Noguchi, T., and Sugiura, M. (2000) Biochemistry 39, 10943-10949]. The fact that the signal appeared even in rather dehydrated PSII films at a physiological temperature (10 degrees C) supported the idea that this water is located in the close vicinity of the Mn cluster and directly involved in the water oxidizing reaction. The results also showed that moderate hydration of the PSII sample made the whole OH region measurable, escaping from absorption saturation by bulk water, and thus will be a useful technique to monitor the water reactions during the S-state cycle using FTIR spectroscopy.