Miwa Sugiura

X-ray crystallography identifies two chloride binding sites in the oxygen evolving centre of Photosystem II

Bromide anomalous X-ray diffraction analyses have been used to locate chloride binding sites in the vicinity of the water splitting/oxygen evolving centre (OEC) of Photosystem II. Three-dimensional crystals of PSII from Thermosynechococcus elongatus were grown from (i) isolated PSII crystals infiltrated with bromide or (ii) PSII obtained from cells cultured in a medium in which the chloride content was totally replaced by bromide. In either case, the anomalous diffraction yielded the same result, the existence of two bromide binding sites in the vicinity of the OEC. Neither are in the first coordination sphere of the Mn and Ca ions which form the catalytic centre of the OEC, being about 6 to 7 A from the metal-cluster. Site 1 is located close to the side chain nitrogen of D2-K317 and the backbone nitrogen of D1-Glu333 while Site 2 is adjacent to backbone nitrogens of CP43-Glu354 and D1-Asn338. Their positioning close to postulated hydrophilic channels may suggest a role in proton removal from, or substrate access to, the OEC.

Rapid formation of the stable tyrosyl radical in photosystem II.

Two symmetrically positioned redox active tyrosine residues are present in the photosystem II (PSII) reaction center. One of them, TyrZ, is oxidized in the ns–μs time scale by P680+ and reduced rapidly (μs to ms) by electrons from the Mn complex. The other one, TyrD, is stable in its oxidized form and seems to play no direct role in enzyme function. Here, we have studied electron donation from these tyrosines to the chlorophyll cation (P680+) in Mn-depleted PSII from plants and cyanobacteria. In particular, a mutant lacking TyrZ was used to investigate electron donation from TyrD. By using EPR and time-resolved absorption spectroscopy, we show that reduced TyrD is capable of donating an electron to P680+ with t1/2 ≈ 190 ns at pH 8.5 in approximately half of the centers. This rate is ≈105 times faster than was previously thought and similar to the TyrZ donation rate in Mn-depleted wild-type PSII (pH 8.5). Some earlier arguments put forward to rationalize the supposedly slow electron donation from TyrD (compared with that from TyrZ) can be reassessed. At pH 6.5, TyrZ (t1/2 = 2–10 μs) donates much faster to P680+ than does TyrD (t1/2 > 150 μs). These different rates may reflect the different fates of the proton released from the respective tyrosines upon oxidation. The rapid rate of electron donation from TyrD requires at least partial localization of P680+ on the chlorophyll (PD2) that is located on the D2 side of the reaction center.

Monitoring proton release during photosynthetic water oxidation in photosystem II by means of isotope-edited infrared spectroscopy.

In photosynthetic water oxidation performed in the water oxidizing center (WOC) of photosystem II (PSII), two water molecules are converted into one oxygen molecule and four protons through a light-driven cycle of intermediates called S states (S(0)-S(4)). To understand the molecular mechanism of water oxidation and the chemical nature of substrate intermediates, it is essential to determine the stoichiometry of proton release from substrate water at individual S-state transitions. In this study, we have monitored proton release during water oxidation by means of isotope-edited Fourier transform infrared (FTIR) spectroscopy. FTIR difference spectra upon successive flash illumination were measured using PSII core complexes from a thermophilic cyanobacterium Thermosynechococcus elongatus, which were suspended in a high concentration (200 mM) Mes buffer at pH 6.0. The spectra involved, in addition to protein bands, the bands of the Mes buffer that trapped virtually all protons from the WOC. Mes-only signals were extracted by subtracting the spectra measured in deuterated-Mes (Mes-d(12)). The flash-number dependence of the intensity increase of the isotope-edited Mes signal showed a clear period-four oscillation. By simulating the oscillation with different assumptions about miss factors, the proton release pattern was estimated to be 0.8-1.0:0.2-0.3:0.9-1.2:1.5-1.6 for the S(0)-->S(1)-->S(2)-->S(3)-->S(0) transitions. The effect of H/D exchange on the COOH region of proteins in FTIR difference spectra of the S-state cycle showed that protonation/deprotonation of carboxylic groups contributed little to the observed proton release pattern. Together with the present and previous FTIR results suggesting no involvement of also His and Cys side groups, it was concluded that proton release from substrate water takes place with a 1:0:1:2 stoichiometry, which is perturbed by partial protonation/deprotonation of side groups probably of Arg, Lys, or Tyr located nearby the WOC.

Spectroelectrochemical determination of the redox potential of pheophytin a, the primary electron acceptor in photosystem II

Thin-layer cell spectroelectrochemistry, featuring rigorous potential control and rapid redox equilibration within the cell, was used to measure the redox potential Em(Phe a/Phe a−) of pheophytin (Phe) a, the primary electron acceptor in an oxygen-evolving photosystem (PS) II core complex from a thermophilic cyanobacterium Thermosynechococcus elongatus. Interferences from dissolved O2 and water reductions were minimized by airtight sealing of the sample cell added with dithionite and mercury plating on the gold minigrid working electrode surface, respectively. The result obtained at a physiological pH of 6.5 was Em(Phe a/Phe a−) = −505 ± 6 mV vs. SHE, which is by ≈100 mV more positive than the values measured ≈30 years ago at nonphysiological pH and widely accepted thereafter in the field of photosynthesis research. Using the P680* − Phe a free energy difference, as estimated from kinetic analyses by previous authors, the present result would locate the Em(P680/P680+) value, which is one of the key parameters but still resists direct measurements, at approximately +1,210 mV. In view of these pieces of information, a renewed diagram is proposed for the energetics in PS II.

Redox Potential of the Primary Plastoquinone Electron Acceptor QA in Photosystem II from Thermosynechococcus elongatus Determined by Spectroelectrochemistry

The redox potential of the primary plastoquinone electron acceptor Q(A), E(m)(Q(A)/Q(A)(-)), in an oxygen-evolving photosystem (PS) II complex from a thermophilic cyanobacterium Thermosynechococcus elongatus was determined to be -140 +/- 2 mV vs. SHE by thin-layer cell spectroelectrochemistry for the first time. The E(m)(Q(A)/Q(A)(-)) value obtained here together with the recently determined redox potential of pheophytin (Phe) a [Kato et al. (2009) Proc. Natl. Acad. Sci. U.S.A. 106, 17365-17370] yields -330 to -370 mV for the free energy change by electron transfer from Phe a(-) to Q(A) and provides a renewed picture for the energetics on the electron acceptor side in PS II.

Biosynthetic Exchange of Bromide for Chloride and Strontium for Calcium in the Photosystem II Oxygen-evolving Enzymes

The active site for water oxidation in photosystem II goes through five sequential oxidation states (S0 to S4) before O2 is evolved. It consists of a Mn4Ca cluster close to a redox-active tyrosine residue (TyrZ). Cl- is also required for enzyme activity. To study the role of Ca2+ and Cl- in PSII, these ions were biosynthetically substituted by Sr2+ and Br-, respectively, in the thermophilic cyanobacterium Thermosynechococcus elongatus. Irrespective of the combination of the non-native ions used (Ca/Br, Sr/Cl, Sr/Br), the enzyme could be isolated in a state that was fully intact but kinetically limited. The electron transfer steps affected by the exchanges were identified and then investigated by using time-resolved UV-visible absorption spectroscopy, time-resolved O2 polarography, and thermoluminescence spectroscopy. The effect of the Ca2+/Sr2+ and Cl-/Br- exchanges was additive, and the magnitude of the effect varied in the following order: Ca/Cl < Ca/Br < Sr/Cl < Sr/Br. In all cases, the rate of O2 release was similar to that of the S3TyrZ. to S0TyrZ transition, with the slowest kinetics (i.e. the Sr/Br enzyme) being ≈6-7 slower than in the native Ca/Cl enzyme. This slowdown in the kinetics was reflected in a decrease in the free energy level of the S3 state as manifest by thermoluminescence. These observations indicate that Cl- is involved in the water oxidation mechanism. The possibility that Cl- is close to the active site is discussed in terms of recent structural models.

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.

Distribution of the Cationic State over the Chlorophyll Pair of the Photosystem II Reaction Center

The reaction center chlorophylls a (Chla) of photosystem II (PSII) are composed of six Chla molecules including the special pair Chla P(D1)/P(D2) harbored by the D1/D2 heterodimer. They serve as the ultimate electron abstractors for water oxidation in the oxygen-evolving Mn(4)CaO(5) cluster. Using the PSII crystal structure analyzed at 1.9 Å resolution, the redox potentials of P(D1)/P(D2) for one-electron oxidation (E(m)) were calculated by considering all PSII subunits and the protonation pattern of all titratable residues. The E(m)(Chla) values were calculated to be 1015-1132 mV for P(D1) and 1141-1201 mV for P(D2), depending on the protonation state of the Mn(4)CaO(5) cluster. The results showed that E(m)(P(D1)) was lower than E(m)(P(D2)), favoring localization of the charge of the cationic state more on P(D1). The P(D1)(•+)/P(D2)(•+) charge ratio determined by the large-scale QM/MM calculations with the explicit PSII protein environment yielded a P(D1)(•+)/P(D2)(•+) ratio of ~80/~20, which was found to be due to the asymmetry in electrostatic characters of several conserved D1/D2 residue pairs that cause the E(m)(P(D1))/E(m)(P(D2)) difference, e.g., D1-Asn181/D2-Arg180, D1-Asn298/D2-Arg294, D1-Asp61/D2-His61, D1-Glu189/D2-Phe188, and D1-Asp170/D2-Phe169. The larger P(D1)(•+) population than P(D2)(•+) appears to be an inevitable fate of the intact PSII that possesses water oxidation activity.

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.

Probing the coupling between proton and electron transfer in photosystem II core complexes containing a 3-fluorotyrosine.

The catalytic cycle of numerous enzymes involves the coupling between proton transfer and electron transfer. Yet, the understanding of this coordinated transfer in biological systems remains limited, likely because its characterization relies on the controlled but experimentally challenging modifications of the free energy changes associated with either the electron or proton transfer. We have performed such a study here in Photosystem II. The driving force for electron transfer from Tyr(Z) to P(680)(*+) has been decreased by approximately 80 meV by mutating the axial ligand of P(680), and that for proton transfer upon oxidation of Tyr(Z) by substituting a 3-fluorotyrosine (3F-Tyr(Z)) for Tyr(Z). In Mn-depleted Photosystem II, the dependence upon pH of the oxidation rates of Tyr(Z) and 3F-Tyr(Z) were found to be similar. However, in the pH range where the phenolic hydroxyl of Tyr(Z) is involved in a H-bond with a proton acceptor, the activation energy of the oxidation of 3F-Tyr(Z) is decreased by 110 meV, a value which correlates with the in vitro finding of a 90 meV stabilization energy to the phenolate form of 3F-Tyr when compared to Tyr (Seyedsayamdost et al. J. Am. Chem. Soc. 2006, 128,1569-1579). Thus, when the phenol of Y(Z) acts as a H-bond donor, its oxidation by P(680)(*+) is controlled by its prior deprotonation. This contrasts with the situation prevailing at lower pH, where the proton acceptor is protonated and therefore unavailable, in which the oxidation-induced proton transfer from the phenolic hydroxyl of Tyr(Z) has been proposed to occur concertedly with the electron transfer to P(680)(*+). This suggests a switch between a concerted proton/electron transfer at pHs < 7.5 to a sequential one at pHs > 7.5 and illustrates the roles of the H-bond and of the likely salt-bridge existing between the phenolate and the nearby proton acceptor in determining the coupling between proton and electron transfer.