Monitoring water reactions during the S-state cycle of the photosynthetic water-oxidizing center: detection of the DOD bending vibrations by means of Fourier transform infrared spectroscopy

Photosynthetic water oxidation takes place in the water-oxidizing center (WOC) of photosystem II (PSII). To clarify the mechanism of water oxidation, detecting water molecules in the WOC and monitoring their reactions at the molecular level are essential. In this study, we have for the first time detected the DOD bending vibrations of functional D 2O molecules during the S-state cycle of the WOC by means of Fourier transform infrared (FTIR) difference spectroscopy. Flash-induced FTIR difference spectra upon S-state transitions were measured using the PSII core complexes from Thermosynechococcus elongatus moderately deuterated with D 2 (16)O and D 2 (18)O. D 2 (16)O-minus-D 2 (18)O double difference spectra at individual S-state transitions exhibited six to eight peaks arising from the D (16)OD/D (18)OD bending vibrations in the 1250-1150 cm (-1) region. This observation indicates that at least two water molecules, not in any deprotonated forms, participate in the reaction at each S-state transition throughout the cycle. Most of the peaks exhibited clear counter peaks with opposite signs at different transitions, reflecting a series of reactions of water molecules at the catalytic site. In contrast, negative bands at approximately 1240 cm (-1) in the S 2 --> S 3, S 3 --> S 0, and possibly S 0 --> S 1 transitions, for which no clear counter peaks were found in other transitions, can be interpreted as insertion of substrate water into the WOC from a water cluster in the proteins. The characteristics of the weakly D-bonded OD stretching bands were consistent with the insertion of substrate from internal water molecules in the S 2 --> S 3 and S 3 --> S 0 transitions. The results of this study show that FTIR detection of the DOD bending vibrations is a powerful method for investigating the molecular mechanism of photosynthetic water oxidation as well as other enzymatic reactions involving functional water molecules.     

Mutation of arginine 357 of the CP43 protein of photosystem II severely impairs the catalytic S-state cycle of the H2O oxidation complex

Basic amino acid side chains situated in active sites may mediate critical proton transfers during an enzymatic catalytic cycle. In the case of photosynthetic water oxidation, a strong base is postulated to facilitate the deprotonation of the active site Mn4-Ca cluster, thereby allowing the otherwise thermodynamically constrained transfer of an electron away from the Mn4-Ca cluster to the oxidized redox active tyrosine radical, YZ*, generated by photosynthetic charge separation. Arginine 357 of the CP43 polypeptide may be located in the second coordination shell of the O2-evolving Mn4-Ca cluster of photosystem II (PSII) according to current structural models. An ostensibly conservative substitution mutation, CP43-357K, was investigated using polarographic and fluorescence techniques in evaluating its potential impact on S-state cycling. Cells containing the CP43-357K mutation lost their capacity for autotrophic growth and exhibited a drastic reduction in O2 evolving activity ( approximately 15% of that of the wild type) despite the fact that mutant cells contained more than 80% of the concentration of charge-separating PSII reaction centers and more than half of these contained photooxidizable Mn. Fluorescence kinetics indicated that acceptor side electron transfer, dominated by the transfer of electrons from QA- to QB, was unaffected, but the fraction of centers containing Mn clusters capable of forming the S2 state was reduced to approximately 40% of that of the wild type. Analysis of O2 yields using a bare platinum electrode indicated a severe defect in the S-state cycling properties of the mutant H2O oxidation complexes. Although O2 evolution was delayed to the third flash during a train of single-turnover saturating flashes, the pattern of O2 emission did not exhibit a discernible periodicity indicating a very high miss factor, which was estimated to be approximately 45% compared to the wild-type value of approximately 10%. On the other hand, the multiflash fluorescence measurements indicate that the yield of formation of the S2 state from S1 is diminished by approximately 20%, although this latter estimate is complicated by the presence of damaged PSII centers. Taken together, the experiments indicate that the high miss factor observed during S-state cycling is likely due to a defect in the higher S-state transitions. These results are discussed in relation to the idea that CP43-R357 may serve as a ligand to bicarbonate or as the catalytic base proposed to mediate proton-coupled electron transfer (PCET) in the higher S states of the catalytic cycle of H2O oxidation.     

FTIR detection of water reactions during the flash-induced S-state cycle of the photosynthetic water-oxidizing complex

Photosynthetic water oxidation is performed via the light-driven S-state cycle in the water-oxidizing complex (WOC) of photosystem II (PS II). To understand its molecular mechanism, monitoring the reaction of substrate water in each S-state transition is essential. We have for the first time detected the reactions of water molecules in WOC throughout the S-state cycle by observing the OH vibrations of water using flash-induced Fourier transform infrared (FTIR) difference spectroscopy. Moderately hydrated (or deuterated) PS II core films from Synechococcus elongatus were used to obtain the FTIR difference spectra upon the first, second, third, and fourth flash illumination, representing the structural changes in the S(1) --> S(2), S(2) --> S(3), S(3) --> S(0), and S(0) --> S(1) transitions, respectively. In the weakly H-bonded OH region, bands appeared at 3617/3588 cm(-1) as a differential signal in the first-flash spectrum and at 3634, 3621, and 3612 cm(-1) with negative intensities in the second-, third-, and fourth-flash spectra, respectively. These bands shifted down by approximately 940 cm(-1) upon deuteration and by approximately 10 cm(-1) upon H(18)O substitution, indicating that they arise from the OH stretches of water including the substrate and its intermediates. Strongly D-bonded OD bands of water were also identified as broad features in the range of 2600-2200 cm(-1) by taking the double difference between the spectra of D(2)(16)O- and D(2)(18)O-deuterated films. In addition, broad continuum features that probably arise from the large proton polarizability of H-bonds were observed around 3000, 2700, 2550, and 2600 cm(-1) in the first-, second-, third-, and fourth-flash spectra, respectively, of the hydrated PS II film, revealing changes in the H-bond network of the protein. The negative OH intensities upon the second to fourth flashes might be related to proton release from substrate water. The results presented here showed that FTIR detection of water OH(D) bands can be a powerful method for investigating the mechanism of photosynthetic water oxidation.     

Mono-manganese mechanism of the photosystem II water splitting reaction by a unique Mn4Ca cluster

The molecular mechanism of the water oxidation reaction in photosystem II (PSII) of green plants remains a great mystery in life science. This reaction is known to take place in the oxygen evolving complex (OEC) incorporating four manganese, one calcium and one chloride cofactors, that is light-driven to cycle four intermediates, designated S(0) through S(4), to produce four protons, five electrons and lastly one molecular oxygen, for indispensable resources in biosphere. Recent advancements of X-ray crystallography models established the existence of a catalytic Mn(4)Ca cluster ligated by seven protein amino acids, but its functional structure is not yet resolved. The (18)O exchange rates of two substrate water molecules were recently measured for four S(i)-state samples (i=0-3) leading to (34)O(2) and (36)O(2) formations, revealing asymmetric substrate binding sites significantly depending on the S(i)-state. In this paper, we present a chemically complete model for the Mn(4)Ca cluster and its surrounding enzyme field, which we found out from some possible models by using the hybrid density functional theoretic geometry optimization method to confirm good agreements with the 3.0 A resolution PSII model [B. Loll, J. Kern, W. Saenger, A. Zouni , J. Biesiadka, Nature 438 (2005) 1040-1044] and the S-state dependence of (18)O exchange rates [W. Hillier and T. Wydrzynski, Phys. Chem. Chem. Phys. 6 (2004) 4882-4889]. Furthermore, we have verified that two substrate water molecules are bound to asymmetric cis-positions on the terminal Mn ion being triply bridged (mu-oxo, mu-carboxylato, and a hydrogen bond) to the Mn(3)CaO(3)(OH) core, by developing a generalized theory of (18)O exchange kinetics in OEC to obtain an experimental evidence for the cross exchange pathway from the slow to the fast exchange process. Some important experimental data will be discussed in terms of this model and its possible tautomers, to suggest that a cofactor, Cl(-) ion, may be bound to CP43-Arg357 nearby Ca(2+) ion and that D1-His337 may be used to trap a released proton only in the S(2)-state.     

FTIR detection of water reactions in the oxygen-evolving centre of photosystem II

Flash-induced Fourier transform infrared (FTIR) difference spectroscopy has been used to study the water-oxidizing reactions in the oxygen-evolving centre of photosystem II. Reactions of water molecules were directly monitored by detecting the OH stretching bands of weakly H-bonded OH of water in the 3700-3500 cm(-1) region in FTIR difference spectra during S-state cycling. In the S1-->S2 transition, a band shift from 3588 to 3617 cm(-1) was observed, indicative of a weakened H-bond. Decoupling experiments using D2O:H2O (1:1) showed that this OH arose from a water molecule with an asymmetric H-bonding structure and this asymmetry became more significant upon S2 formation. In the S2-->S3, S3-->S0 and S0-->S1 transitions, negative bands were observed at 3634, 3621 and 3612 cm(-1), respectively, representing formation of a strong H-bond or a proton release reaction. In addition, using complex spectral features in the carboxylate stretching region (1600-1300 cm-(1)) as 'fingerprints' of individual S-state transitions, pH dependency of the transition efficiencies and the effect of dehydration were examined to obtain the information of proton release and water insertion steps in the S-state cycle. Low-pH inhibition of the S2-->S3, S3-->S0 and S0-->S1 transitions was consistent with a view that protons are released in the three transitions other than S1-->S2, while relatively high susceptibility to dehydration in the S2-->S3 and S3-->S0 transitions suggested the insertion of substrate water into the system during these transitions. Thus, a possible mechanism of water oxidation to explain the FTIR data is proposed.     

Structure of an active water molecule in the water-oxidizing complex of photosystem II as studied by FTIR spectroscopy

The vibrations of a water molecule in the water-oxidizing complex (WOC) of photosystem II were detected for the first time using Fourier transform infrared (FTIR) spectroscopy. In a flash-induced FTIR difference spectrum upon the S(1)-to-S(2) transition, a pair of positive and negative bands was observed at 3618 and 3585 cm(-1), respectively, and both bands exhibited downshifts by 12 cm(-1) upon replacement of H(2)(16)O by H(2)(18)O. Upon D(2)O substitution, the bands largely shifted down to 2681 and 2652 cm(-1). These observations indicate that the bands at 3618 and 3585 cm(-1) arise from the O-H stretching vibrations of a water molecule, probably substrate water, coupled to the Mn cluster in the S(2) and S(1) states, respectively. The band frequencies indicate that the O-H group forms a weak H-bond and this H-bonding becomes weaker upon S(2) formation. Intramolecular coupling with the other O-H vibration of this water molecule was studied by a decoupling experiment using a H(2)O/D(2)O (1:1) mixture. The downshifts by decoupling were estimated to be 4 and 12 cm(-1) for the 3618 (S(2)) and 3585 cm(-1) (S(1)) bands, both of which were much smaller than 52 cm(-1) of water in vapor, indicating that the observed water has a considerably asymmetric structure; i.e., one of the O-H groups is weakly and the other is strongly H-bonded. The smaller coupling in the S(2) than the S(1) state means that this H-bonding asymmetry becomes more prominent upon S(2) formation. Such a structural change may facilitate the proton release reaction that takes place in the later step by lowering the potential barrier. The present study showed that FTIR detection of the O-H vibrations is a useful and promising method to directly monitor the chemical reactions of substrate water and clarify the molecular mechanism of photosynthetic water oxidation.     

Time-resolved infrared detection of the proton and protein dynamics during photosynthetic oxygen evolution

Photosynthetic oxygen evolution by plants and cyanobacteria is performed by water oxidation at the Mn(4)CaO(5) cluster in photosystem II. The reaction is known to proceed via a light-driven cycle of five intermediates called S(i) states (i = 0-4). However, the detailed reaction processes during the intermediate transitions remain unresolved. In this study, we have directly detected the proton and protein dynamics during the oxygen-evolving reactions using time-resolved infrared spectroscopy. The time courses of the absorption changes at 1400 and 2500 cm(-1), which represent the reactions and/or interaction changes of carboxylate groups and the changes in proton polarizability of strong hydrogen bonds, respectively, were monitored upon flash illumination. The results provided experimental evidence that during the S(3) → S(0) transition, drastic proton rearrangement, most likely reflecting the release of a proton from the catalytic site, takes place to form a transient state before the oxidation of the Mn(4)CaO(5) cluster that leads to O(2) formation. Early proton movement was also detected during the S(2) → S(3) transition. These observations reveal the common mechanism in which proton release facilitates the transfer of an electron from the Mn(4)CaO(5) cluster in the S(2) and S(3) states that already accumulate oxidizing equivalents. In addition, relatively slow rearrangement of carboxylate groups was detected in the S(0) → S(1) transition, which could contribute to the stabilization of the S(1) state. This study demonstrates that time-resolved infrared detection is a powerful method for elucidating the detailed molecular mechanism of photosynthetic oxygen evolution by pursuing the reactions of substrate and amino acid residues during the S-state transitions.     

FTIR detection of structural changes in a histidine ligand during S-state cycling of photosynthetic oxygen-evolving complex

Changes in structural coupling between the Mn cluster and a putative histidine ligand during the S-state cycling of the oxygen-evolving complex (OEC) have been detected directly by Fourier transform infrared (FTIR) spectroscopy in photosystem (PS) II core particles from the cyanobacterium Synechocystis sp. PCC6803, in which histidine residues were selectively labeled with l-[(15)N(3)]histidine. The bands sensitive to the histidine-specific isotope labeling appeared at 1120-1090 cm(-)(1) in the spectra induced upon the first-, second-, and fourth-flash illumination, for the S(2)/S(1), S(3)/S(2), and S(1)/S(0) differences, at similar frequencies with different sign and/or intensity depending on the respective S-state transitions. However, no distinctive band was observed in the third-flash induced spectrum for the S(0)/S(3) difference. The results indicate that a single histidine residue coupled with the structural changes of the OEC during the S-state cycling is responsible for the observed histidine bands, in which the histidine modes changed during the S(0)-to-S(1) transition are reversed upon the S(1)-to-S(2) and S(2)-to-S(3) transitions. The 1186(+)/1178(-) cm(-)(1) bands affected by l-[(15)N(3)]histidine labeling were observed only for the S(2)/S(1) difference, but those affected by universal (15)N labeling appeared prominently showing a clear S-state dependency. Possible origins of these bands and changes in the histidine modes during the S-state cycling are discussed.     

Flash-induced FTIR difference spectroscopy shows no evidence for the structural coupling of bicarbonate to the oxygen-evolving Mn cluster in photosystem II

Bicarbonate is known to be required for the maximum activity of photosystem II. Although it is well established that bicarbonate is bound to the nonheme iron to regulate the quinone reactions, the effect of bicarbonate on oxygen evolution is still controversial, and its binding site and exact physiological roles remain to be clarified. In this study, the structural coupling of bicarbonate to the oxygen-evolving center (OEC) was studied using Fourier transform infrared (FTIR) difference spectroscopy. Flash-induced FTIR difference spectra during the S-state cycle of OEC were recorded using the PSII core complexes from Thermosynechococcus elongatus in the presence of either unlabeled bicarbonate or (13)C-bicarbonate. The H (12)CO 3 (-)-minus-H (13)CO 3 (-) double difference spectra showed prominent bicarbonate bands at the first flash, whereas no appreciable bands were detected at the second to fourth flashes. The bicarbonate bands at the first flash were virtually identical to those from the nonheme iron, which was preoxidized by ferricyanide and photoreduced by a single flash, recorded using Mn-depleted PSII complexes. Using the bicarbonate bands of the nonheme iron as an internal standard, it was concluded that no bicarbonate band arising from OEC exists in the S-state FTIR spectra. This conclusion indicates that bicarbonate is not affected by the structural changes in OEC upon the four S-state transitions. It is thus strongly suggested that bicarbonate is neither a ligand to the Mn cluster nor a cofactor closely coupled to OEC, although the possibility cannot be fully excluded that nonexchangeable bicarbonate exists in OEC as a constituent of the Mn-cluster core. The data also provide strong evidence that bicarbonate does not function as a substrate or a catalytic intermediate. Bicarbonate may play major roles in the photoassembly process of the Mn cluster and in the stabilization of OEC by a rather indirect interaction.     

Resonance Raman characterization of biotin sulfoxide reductase. Comparing oxomolybdenum enzymes in the ME(2)SO reductase family

Resonance Raman spectroscopy has been used to define active site structures for oxidized Mo(VI) and reduced Mo(IV) forms of recombinant Rhodobacter sphaeroides biotin sulfoxide reductase expressed in Escherichia coli. On the basis of (18)O/(16)O labeling studies involving water and the alternative substrate dimethyl sulfoxide and the close correspondence to the resonance Raman spectra previously reported for dimethyl sulfoxide reductase (Garton, S. D., Hilton, J., Oku, H., Crouse, B. R., Rajagopalan, K. V., and Johnson, M. K. (1997) J. Am. Chem. Soc. 119, 12906-12916), vibrational modes associated with a terminal oxo ligand and the two molybdopterin dithiolene ligands have been assigned. The results indicate that the enzyme cycles between mono-oxo-Mo(VI) and des-oxo-Mo(IV) forms with both molybdopterin dithiolene ligands remaining coordinated in both redox states. Direct evidence for an oxygen atom transfer mechanism is provided by (18)O/(16)O labeling studies, which show that the terminal oxo group at the molybdenum center is exchangeable with water during redox cycling and originates from the substrate in substrate-oxidized samples. Biotin sulfoxide reductase is not reduced by biotin or the nonphysiological products, dimethyl sulfide and trimethylamine. However, product-induced changes in the Mo=O stretching frequency provide direct evidence for a product-associated mono-oxo-Mo(VI) catalytic intermediate. The results indicate that biotin sulfoxide reductase is thermodynamically tuned to catalyze the reductase reaction, and a detailed catalytic mechanism is proposed.     

Botanical and geographical origin identification of industrial ethanol by stable isotope analyses of C, H, and O

The isotope ratios of carbon, hydrogen, and oxygen of rectified alcohols were determined to distinguish their botanical and geographical origins by continuous flow-isotope ratio mass spectrometry (CF-IRMS). The (13)C/(12)C and (18)O/(16)O ratios of 27 fermented alcohols with known origins showed clusters derived from each botanical origin, viz. corn, sugarcane, wheat, and tapioca. C3 and C4 plants were easily distinguishable by the (13)C/(12)C ratio. Sugarcane and corn are both C4 plants, and they showed small differences in isotope ratios. The combination plots of the D/H and (18)O/(16)O ratios enabled us to designate the geographical origins of alcohol derived from the same kind of crop, such as Chinese or American corn. The chemically synthetic and fermented alcohols were clearly distinguished by D/H and (18)O/(16)O ratios. Isotope ratios were useful for origin identification of alcohol. We plan to construct a database of alcohol isotope ratios to determine the origins of raw materials in alcohol.     

Mid- to low-frequency Fourier transform infrared spectra of S-state cycle for photosynthetic water oxidation in Synechocystis sp. PCC 6803

Flash-induced Fourier transform infrared (FTIR) difference spectra for the four-step S-state cycle and the effects of global (15)N- and (13)C-isotope labeling on the difference spectra were examined for the first time in the mid- to low-frequency (1200-800 cm(-1)) as well as the mid-frequency (1700-1200 cm(-1)) regions using photosystem (PS) II core particles from cyanobacterium Synechocystis sp. PCC 6803. The difference spectra clearly exhibited the characteristic vibrational features for each transition during the S-state cycling. It is likely that the bands that change their sign and intensity with the S-state advances reflect the changes of the amino acid residues and protein matrices that have functional and/or structural roles within the oxygen-evolving complex (OEC). Except for some minor differences, the trends of S-state dependence in the 1700-1200 cm(-1) frequency spectra of the PS II cores from Synechocystis were comparable to that of spinach, indicating that the structural changes of the polypeptide backbones and amino acid side chains that occur during the oxygen evolution are inherently identical between cyanobacteria and higher plants. Upon (13)C-labeling, most of the bands, including amide I and II modes and carboxylate stretching modes, showed downward shifts; in contrast, (15)N-labeling induced isotopic shifts that were predominantly observed in the amide II region. In the mid- to low-frequency region, several bands in the 1200-1140 cm(-1) region were attributable to the nitrogen- and/or carbon-containing group(s) that are closely related to the oxygen evolution process. Specifically, the putative histidine ligand exhibited a band at 1113 cm(-1) which was affected by both (15)N- and (13)C-labeling and showed distinct S-state dependency. The light-induced bands in the 900-800 cm(-1) region were downshifted only by (13)C-labeling, whereas the bands in the 1000-900 cm(-1) region were affected by both (15)N- and (13)C-labeling. Several modes in the mid- to low-frequency spectra were induced by the change in protonation state of the buffer molecules accompanied by S-state transitions. Our studies on the light-induced spectrum showed that contributions from the redox changes of Q(A) and the non-heme iron at the acceptor side and Y(D) were minimal. It was, therefore, suggested that the observed bands in the 1000-800 cm(-1) region include the modes of the amino acid side chains that are coupled to the oxidation of the Mn cluster. S-state-dependent changes were observed in some of the bands.     

Investigation of substrate water interactions at the high-affinity Mn site in the photosystem II oxygen-evolving complex

18 O isotope exchange measurements of photosystem II (PSII) in thylakoids from wild-type and mutant Synechocystis have been performed to investigate binding of substrate water to the high-affinity Mn4 site in the oxygen-evolving complex (OEC). The mutants investigated were D1-D170H, a mutation of a direct ligand to the Mn4 ion, and D1-D61N, a mutation in the second coordination sphere. The substrate water 18 O exchange rates for D61N were found to be 0.16+/-0.02 s(-1) and 3.03+/-0.32 s(-1) for the slow and fast phases of exchange, respectively, compared with 0.47+/-0.04 s(-1) and 19.7+/-1.3 s(-1) for the wild-type. The D1-D170H rates were found to be 0.70+/-0.16 s(-1) and 24.4+/-4.6 s(-1) and thus are almost within the error limits for the wild-type rates. The results from the D1-D170H mutant indicate that the high-affinity Mn4 site does not directly bind to the substrate water molecule in slow exchange, but the binding of non-substrate water to this Mn ion cannot be excluded. The results from the D61N mutation show an interaction with both substrate water molecules, which could be an indication that D61 is involved in a hydrogen bonding network with the substrate water. Our results provide limitations as to where the two substrate water molecules bind in the OEC of PSII.     

Oxygen ligand exchange at metal sites - implications for the O2 evolving mechanism of photosystem II

The mechanism for photosynthetic O2 evolution by photosystem II is currently a topic of intense debate. Important questions remain as to what is the nature of the binding sites for the substrate water and how does the O-O bond form. Recent measurements of the 18O exchange between the solvent water and the photogenerated O2 as a function of the S-state cycle have provided some surprising insights to these questions (W. Hillier, T. Wydrzynski, Biochemistry 39 (2000) 4399-4405). The results show that one substrate water molecule is bound at the beginning of the catalytic sequence, in the S0 state, while the second substrate water molecule binds in the S3 state or possibly earlier. It may be that the second substrate water molecule only enters the catalytic sequence following the formation of the S3 state. Most importantly, comparison of the observed exchange rates with oxygen ligand exchange in various metal complexes reveal that the two substrate water molecules are most likely bound to separate Mn(III) ions, which do not undergo metal-centered oxidations through to the S3 state. The implication of this analysis is that in the S1 state, all four Mn ions are in the +3 oxidation state. This minireview summarizes the arguments for this proposal.     

No evidence from FTIR difference spectroscopy that aspartate-170 of the D1 polypeptide ligates a manganese ion that undergoes oxidation during the S0 to S1, S1 to S2, or S2 to S3 transitions in photosystem II

On the basis of mutagenesis and X-ray crystallographic studies, Asp170 of the D1 polypeptide is widely believed to ligate the (Mn)4 cluster that is located at the catalytic site of water oxidation in photosystem II. Recent proposals for the mechanism of water oxidation postulate that D1-Asp170 ligates a Mn ion that undergoes oxidation during one or more of the S0 --> S1, S1 --> S2, and S2 --> S3 transitions. To test these hypotheses, we have compared the FTIR difference spectra of the individual S state transitions in wild-type* PSII particles from the cyanobacterium Synechocystis sp. PCC 6803 with those in D1-D170H mutant PSII particles. Remarkably, our data show that the D1-D170H mutation does not significantly alter the mid-frequency regions (1800-1000 cm(-1)) of any of the FTIR difference spectra. Therefore, we conclude that the oxidation of the (Mn)4 cluster does not alter the frequencies of the carboxylate stretching modes of D1-Asp170 during the S0 --> S1, S1 --> S2, or S2 --> S3 transitions. The simplest explanation for these data is that the Mn ion that is ligated by D1-Asp170 does not increase its charge or oxidation state during any of these S state transitions. These data have profound implications for the mechanism of water oxidation. Either (1) the oxidation of the Mn ion that is ligated by D1-Asp170 occurs only during the transitory S3 --> S4 transition and serves as the critical step in the ultimate formation of the O-O bond or (2) the oxidation increments and O2 formation chemistry that occur during the catalytic cycle involve only the remaining Mn3Ca portion of the Mn4Ca cluster. Our data also show that, if the increased positive charge on the (Mn)4 cluster that is produced during the S1 --> S2 transition is delocalized over the (Mn)4 cluster, it is not delocalized onto the Mn ion that is ligated by D1-Asp170.     

Oxidation of the Mn cluster induces structural changes of NO3- functionally bound to the Cl- site in the oxygen-evolving complex of photosystem II

Cl(-) is an indispensable cofactor for photosynthetic O(2) evolution and is functionally replaced by NO(3)(-). Structural changes of an isotopically labeled NO(3)(-) ion, induced by the oxidation of the Mn cluster (S(1)-to-S(2)), were detected by FTIR spectroscopy. NO(3)(-)-substituted photosystem II core particles showed (14)N(16)O(3)(-)/(15)N(16)O(3)(-) and (14)N(16)O(3)(-)/(14)N(18)O(3)(-) isotopic bands in the S(2)/S(1) spectra with markedly high signal/noise ratio. These bands appeared only in the region from 1415 to 1284 cm(-1), indicating that the bands do not arise from a metal-bound NO(3)(-) but from an ionic NO(3)(-). The intensity of the bands exhibited a quantitatively proportional relationship with the O(2) activity. These results demonstrate that the NO(3)(-) functionally bound to the Cl(-) site couples to the Mn cluster structurally, but is not associated with the cluster as a direct ligand. Comparison of the bands for two isotopes ((15)N and (18)O) and their simulations enable us to assign each band to the S(1) and S(2) states. The results indicate that the NO(3)(-) ion bound to the Cl(-) site is highly asymmetric in S(1) but rather symmetric in S(2). Since NO(3)(-) functionally replaces Cl(-), most of the conclusions drawn from this study will be also applicable to Cl(-).     

Cooperative binding of oxygen to the water-splitting enzyme in the filamentous cyanobacterium Oscillatoria chalybea

In the filamentous cyanobacterium Oscillatoria chalybea photolysis of water does not take place in the complete absence of oxygen. A catalytic oxygen partial pressure of 15x10(-6) Torr has to be present for effective water splitting to occur. By means of mass spectrometry we measured the photosynthetic oxygen evolution in the presence of H(2)(18)O in dependence on the oxygen partial pressure of the atmosphere and analysed the liberations of (16)O(2), (16)O(18)O and (18)O(2) simultaneously. The observed dependences of the light-induced oxygen evolution on bound oxygen yield sigmoidal curves. Hill coefficient values of 3.0, 3.1 and 3.2, respectively, suggest that the binding is cooperative and that four molecules of oxygen have to be bound per chain to the oxygen evolving complex. Oxygen seems to prime the water-splitting reaction by redox steering of the S-state system, putting it in the dark into the condition from which water splitting can start. It appears that in O. chalybea an interaction of oxygen with S(0) and S(1) leads to S(2) and S(3), thus yielding the typical oxygen evolution pattern in which even after extensive dark adaptation substantial amounts of Y(1) and Y(2) are found. The interacting oxygen is apparently reduced to hydrogen peroxide. Mass spectrometry permits to distinguish this highly specific oxygen requirement from the interaction of bulk atmospheric oxygen with the oxygen evolving complex of the cyanobacterium. This interaction leads to the formation H(2)O(2) which is decomposed under O(2) evolution in the light. The dependence on oxygen-partial pressure and temperature is analysed. Structural peculiarities of the cyanobacterial reaction centre of photosystem II referring to the extrinsic peptides might play a role.     

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

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

Water oxidation in PSII-H atom abstraction revisited

A model for the water oxidation reaction in Photosystem II (PSII) is presented, based on an H atom abstraction mechanism. The model rationalises the S-state dependence of observed substrate water exchange kinetics [Biochim. Biophys. Acta 1503 (2001) 197] and assumes that H transfer occurs to an oxidised micro-oxo bridge oxygen on the S(3)-->S(4)-->S(0) transition. The model requires that only one Mn-pair and a Ca ion be directly involved in the substrate binding and catalytic function. The multiline signal observed in the S(0) state is shown to plausibly arise from such a system. A detailed molecular model of the three-metal site, assuming ligation by those residues identified by mutagenesis as Ca/Mn ligands is presented. This bears a resemblance to the dinuclear Mn site in Mn catalase and is generally consistent with the electron density map of cyanobacterial PSII recently presented [Proc. Natl. Acad. Sci. U. S. A. 100 (2003) 98].     

No evidence from FTIR difference spectroscopy that glutamate-189 of the D1 polypeptide ligates a Mn ion that undergoes oxidation during the S0 to S1, S1 to S2, or S2 to S3 transitions in photosystem II

In the recent X-ray crystallographic structural models of photosystem II, Glu189 of the D1 polypeptide is assigned as a ligand of the oxygen-evolving Mn(4) cluster. To determine if D1-Glu189 ligates a Mn ion that undergoes oxidation during one or more of the S(0) --> S(1), S(1) --> S(2), and S(2) --> S(3) transitions, the FTIR difference spectra of the individual S-state transitions in D1-E189Q and D1-E189R mutant PSII particles from the cyanobacterium Synechocystis sp. PCC 6803 were compared with those in wild-type PSII particles. Remarkably, the data show that neither mutation significantly alters the mid-frequency regions (1800-1200 cm(-)(1)) of any of the FTIR difference spectra. Importantly, neither mutation eliminates any specific symmetric or asymmetric carboxylate stretching mode that might have been assigned to D1-Glu189. The small spectral alterations that are observed are similar in amplitude to those that are observed in wild-type PSII particles that have been exchanged into FTIR analysis buffer by different methods or those that are observed in D2-H189Q mutant PSII particles (the residue D2-His189 is located >25 A from the Mn(4) cluster and accepts a hydrogen bond from Tyr Y(D)). The absence of significant mutation-induced spectral alterations in the D1-Glu189 mutants shows that the oxidation of the Mn(4) cluster does not alter the frequencies of the carboxylate stretching modes of D1-Glu189 during the S(0) --> S(1), S(1) --> S(2), or S(2) --> S(3) transitions. One explanation of these data is that D1-Glu189 ligates a Mn ion that does not increase its charge or oxidation state during any of these S-state transitions. However, because the same conclusion was reached previously for D1-Asp170, and because the recent X-ray crystallographic structural models assign D1-Asp170 and D1-Glu189 as ligating different Mn ions, this explanation requires that (1) the extra positive charge that develops on the Mn(4) cluster during the S(1) --> S(2) transition be localized on the Mn ion that is ligated by the alpha-COO(-) group of D1-Ala344 and (2) any increase in positive charge that develops on the Mn(4) cluster during the S(0) --> S(1) and S(2) --> S(3) transitions be localized on the one Mn ion that is not ligated by D1-Asp170, D1-Glu189, or D1-Ala344. An alternative explanation of the FTIR data is that D1-Glu189 does not ligate the Mn(4) cluster. This conclusion would be consistent with earlier spectroscopic analyses of D1-Glu189 mutants, but would require that the proximity of D1-Glu189 to manganese in the X-ray crystallographic structural models be an artifact of the radiation-induced reduction of the Mn(4) cluster that occurred during the collection of the X-ray diffraction data.