Role of D1-His190 in the proton-coupled oxidation of tyrosine YZ in manganese-depleted photosystem II.

To further characterize the role of D1-His190 in the oxidation of tyrosine Y(Z) in photosystem II, the pH dependence of P(680)(*)()(+) reduction was measured in H190A and Mn-depleted wild-type PSII particles isolated from the cyanobacterium, Synechocystis sp. PCC 6803. Measurements were conducted in the presence and absence of imidazole and other small organic bases. In H190A PSII particles, rapid reduction of P(680)(*)()(+) attributed to electron transfer from Y(Z) increased dramatically above pH 9, with an apparent pK(A) of approximately 10.3. In the presence of ethanolamine and imidazole, this dramatic increase occurred at lower pH values, with the efficiency of Y(Z) oxidation correlating with the solution pK(A) value of the added base. We conclude that the pK(A) of Y(Z) is approximately 10.3 in D1-H190A PSII particles. In Mn-depleted wild-type PSII particles, P(680)(*)()(+) reduction was accelerated by all exogenous bases examined (substituted imidazoles, histidine, Tris, and 1,4-diazabicyclo[2.2.2]octane). We conclude that Y(Z) is solvent accessible in Mn-depleted wild-type PSII particles and that its pK(A) is near that of tyrosine in solution. In Mn-depleted wild-type PSII particles, over 80% of the kinetics of P(680)(*)()(+) reduction after a flash could be described by three kinetic components. The individual rate constants of these components varied slightly with pH, but their relative proportions varied dramatically with pH, showing apparent pK(A) values of 7.5 and 6.25 (6.9 and 5.8 in the presence of Ca(2+) and Mg(2+) ions). An additional pK(A) value (pK(A) < 4.5) may also be present. To describe these data, we propose (1) the pK(A) of His190 is 6.9-7.5, depending on buffer ions, (2) the deprotonation of Y(Z) is facilitated by the transient formation of a either a hydrogen bond or a hydrogen-bonded water bridge between Y(Z) and D1-His190, and (3) when protonated, D1-His190 interacts with nearby residues having pK(A) values near 6 and 4. Because Y(Z) and D1-His190 are located near the Mn cluster, these residues may interact with the Mn cluster in the intact system.     

Electron-transfer reactions in manganese-depleted photosystem II

We have used flash-detection optical and electron paramagnetic resonance spectroscopy to measure the kinetics and yield per flash of the photooxidation of cytochrome b559 and the yield per flash of the photooxidation of the tyrosine residue YD in Mn-depleted photosystem II (PSII) membranes at room temperature. The initial charge separation forms YZ+ QA-. Following this, cytochrome b559 is oxidized on a time scale of the same order and with the same pH dependence as is observed for the decay of YZ+; under the conditions of our experiments, the decay of YZ+ is determined by the lifetime of YZ+ QA-. In order to explain this observation, we have constructed a model for electron donation in which YZ+ and P680+ are in redox equilibrium and cytochrome b559 and YD are oxidized via P680+. Using our results, together with data from earlier investigations of the kinetics of electron transfer from YZ to P680+ and charge recombination of YZ+ QA-, we have obtained the first global fit for electron donation in Mn-depleted PSII that accounts for the data over the pH range from 5 to 7.5. From these calculations, we have obtained the intrinsic rate constants of all the electron-donation reactions in Mn-depleted PSII. These rate constants allow us to calculate the free energy difference between YZ+ P680 and YZ P680+, which is found to increase by 47 +/- 4 mV/pH from pH 5 to 6 and is observed to increase more slowly per pH unit for pH greater than 6. An important conclusion of our experimental work is that the rates of photooxidation of cytochrome b559 and YD are determined by the lifetime of the oxidizing equivalent on YZ/P680. Extension of our model to oxygen-evolving PSII samples leads to the prediction that the kinetics and yields of electron donation from cytochrome b559 and YD to P680+ will depend on the S2- or S3-state lifetime.     

Unique binding site for Mn2+ ion responsible for reducing an oxidized YZ tyrosine in manganese-depleted photosystem II membranes.

Binding of Mn2+ to manganese-depleted photosystem II and electron donation from the bound Mn2+ to an oxidized YZ tyrosine were studied under the same equilibrium conditions. Mn2+ associated with the depleted membranes in a nonsaturating manner when added alone, but only one Mn2+ ion per photosystem II (PS II) was bound to the membranes in the presence of other divalent cations including Ca2+ and Mg2+. Mn2+-dependent electron donation to photosystem II studied by monitoring the decay kinetics of chlorophyll fluorescence and the electron paramagnetic resonance (EPR) signal of an oxidized YZ tyrosine (YZ+) after a single-turnover flash indicated that the binding of only one Mn2+ ion to the manganese-depleted PS II is sufficient for the complete reduction of YZ+ induced by flash excitation. The results indicate that the manganese-depleted membranes have only one unique binding site, which has higher affinity and higher specificity for Mn2+ compared with Mg2+ and Ca2+, and that Mn2+ bound to this unique site can deliver an electron to YZ+ with high efficiency. The dissociation constant for Mn2+ of this site largely depended on pH, suggesting that a single amino acid residue with a pKa value around neutral pH is implicated in the binding of Mn2+. The results are discussed in relation to the photoactivation mechanism that forms the active manganese cluster.     

On the molecular mechanism of light-induced D1 protein degradation in photosystem II core particles.

The mechanism of D1 protein degradation was investigated during photoinhibitory illumination of isolated photosystem II core preparations. The studies revealed that a proteolytic activity resides within the photosystem II core complex. A relationship between the inhibition of D1 protein degradation and the binding of the highly specific serine protease inhibitor diisopropyl fluorophosphate to isolated complexes of photosystem II was observed, evidence that this protease is of the serine type. Using radiolabeled inhibitor, it was shown that the binding site, representing the active serine of the catalytic site, is located on a 43-kDa polypeptide, probably the chlorophyll a protein CP43. The protease is apparently active in darkness, with the initiation of breakdown being dependent on high light-induced substrate activation. The proteolysis, which has an optimum at pH 7.5, gives rise to primary degradation fragments of 23 and 16 kDa. In addition, D1 protein fragments of 14, 13, and 10 kDa were identified. Experiments with phosphate-labeled D1 protein and sequence-specific antisera showed that the 23- and 16-kDa fragments originate from the N- and C-termini, respectively, suggesting a primary cleavage of the D1 protein at the outer thylakoid surface in the region between transmembrane helices D and E.     

Carotenoid oxidation in photosystem II.

The oxidation of carotenoid upon illumination at low temperature has been studied in Mn-depleted photosystem II (PSII) using EPR and electronic absorption spectroscopy. Illumination of PSII at 20 K results in carotenoid cation radical (Car+*) formation in essentially all of the centers. When a sample which was preilluminated at 20 K was warmed in darkness to 120 K, Car+* was replaced by a chlorophyll cation radical. This suggests that carotenoid functions as an electron carrier between P680, the photooxidizable chlorophyll in PSII, and ChlZ, the monomeric chlorophyll which acts as a secondary electron donor under some conditions. By correlating with the absorption spectra at different temperatures, specific EPR signals from Car+* and ChlZ+* are distinguished in terms of their g-values and widths. When cytochrome b559 (Cyt b559) is prereduced, illumination at 20 K results in the oxidation of Cyt b559 without the prior formation of a stable Car+*. Although these results can be reconciled with a linear pathway, they are more straightforwardly explained in terms of a branched electron-transfer pathway, where Car is a direct electron donor to P680(+), while Cyt b559 and ChlZ are both capable of donating electrons to Car+*, and where the ChlZ donates electrons when Cyt b559 is oxidized prior to illumination. These results have significant repercussions on the current thinking concerning the protective role of the Cyt b559/ChlZ electron-transfer pathways and on structural models of PSII.     

Manganese and calcium requirements for reconstitution of oxygen-evolution activity in manganese-depleted photosystem II membranes

The Mn complex of photosystem II and O2-evolution activity are reconstituted in Mn-depleted photosystem II membranes in a light-dependent process called photoactivation. Recovery of O2-evolution activity requires both Mn2+ and Ca2+ in the photoactivation medium. The Mn2+ and Ca2+ dependences of both the effective rate constant and yield of photoactivation have been determined. A comparison of these data with the predictions of mathematical models for photoactivation leads to the conclusion that photoactivation occurs in two stages. The first stage, photoligation of Mn, requires light and depends primarily on Mn2+. The second stage, binding of Ca2+, is required for expression of O2-evolution activity. This two-stage model affords an excellent fit to the data and provides dissociation constants and binding stoichiometries for Ca2+ and Mn2+. We conclude that one Mn2+ ion is bound and photooxidized in the rate-determining step(s) of photoactivation. On the basis of these results and data already in the literature, the molecular details of the elementary steps in photoactivation are discussed and a mechanism of photoactivation is proposed.     

Electron-transfer events leading to reconstitution of oxygen-evolution activity in manganese-depleted photosystem II membranes

O2-evolution activity and the Mn complex can be reconstituted in photosystem II by a process called photoactivation. We have studied the elementary steps in photoactivation by using electron paramagnetic resonance spectroscopy to probe electron transport in Mn-depleted photosystem II membranes. The electron donation reactions in Mn-depleted photosystem II were found to be identical with those in untreated photosystem II, except that electron donation from the Mn complex was absent and could be replaced by slower electron donation from exogenous Mn2+. Mn2+ photooxidation by Mn-depleted photosystem II membranes correlates with reconstitution of O2-evolution activity. However, photooxidation of Mn2+ occurs in competition with photooxidation of the tyrosine residue YD, and cytochrome b-559. Thus, these two species are excluded from direct participation in the initial steps in the assembly of the Mn complex. Because photooxidation of Mn2+ is slower than photooxidation of the competing electron donors, cytochrome b-559 and chlorophyll, as well as recombination of the charge-separated states chlorophyll+QA- or YZ+QA-, these other reactions dominate in a single photochemical turnover reaction. This provides a molecular basis for both the low yield and low quantum yield of photoactivation. The first photochemical step in the assembly of the Mn complex results in photooxidation of one Mn2+ ion. Therefore, the first intermediate in assembly of the Mn complex contains Mn3+. On the basis of these results and previous kinetic studies [Miller, A.-F., & Brudvig, G. W. (1989) Biochemistry 28, 8181], we conclude that the second intermediate of Mn complex assembly contains Mn2+Mn3+, which is photooxidized to Mn3+2.     

Water oxidation in photosystem II

Photosynthesis Research - Biological water oxidation, performed by a single enzyme, photosystem II, is a central research topic not only in understanding the photosynthetic apparatus but also for...     

Photoproduction of catalase-insensitive peroxides on the donor side of manganese-depleted photosystem II: evidence with a specific fluorescent probe

The photoproduction of organic peroxides (ROOH) in photosystem II (PSII) membranes was studied using the fluorescent probe Spy-HP. Two types of peroxide, highly lipophilic ones and relatively hydrophilic ones, were distinguished by the rate of reaction with Spy-HP; the former oxidized Spy-HP to the higher fluorescent form Spy-HPOx within 5 min, while the latter did so very slowly (the reaction was still not completed after 180 min). The level of photoproduction of these peroxides was significantly larger in the alkaline-treated, Mn-depleted PSII membranes than that in the untreated membranes, and it was suppressed by an artificial electron donor (diphenylcarbazide or ferrocyanide) and by the electron transport inhibitor diuron. Postillumination addition of Fe(2+) ions, which degrade peroxides by the Fenton mechanism, abolished the accumulation of Spy-HPOx, but catalase did not change the peroxide level, indicating that the detected species were organic peroxides, excluding H(2)O(2). These results agreed with our previous observation of an electron transport-dependent O(2) consumption on the PSII donor side and indicated that ROOH accumulated via a radical chain reaction that started with the formation of organic radicals on the donor side. Illumination (λ > 600 nm; 1500 μmol of photons m(-2) s(-1)) of the Mn-depleted PSII membranes for 3 min resulted in the formation of nearly 200 molecules of hydrophilic ROOH per reaction center, but only four molecules of highly lipophilic ROOH. The limited formation of the latter was due to the limited supply of its precursor to the reaction, suggesting that it represented structurally fixed peroxides, i.e., either protein peroxides or peroxides of the lipids tightly bound to the core complex. These ROOH forms, likely including several species derived from lipid peroxides, may mediate the donor side-induced photoinhibition of PSII via protein modification.     

Function of redox-active tyrosine in photosystem II

Water oxidation at photosystem II Mn-cluster is mediated by the redox-active tyrosine Y(Z). We calculated the redox potential (E(m)) of Y(Z) and its symmetrical counterpart Y(D), by solving the linearized Poisson-Boltzmann equation. The calculated E(m)(Y( )/Y(-)) were +926 mV/+694 mV for Y(Z)/Y(D) with the Mn-cluster in S2 state. Together with the asymmetric position of the Mn-cluster relative to Y(Z/D), differences in H-bond network between Y(Z) (Y(Z)/D1-His(190)/D1-Asn(298)) and Y(D) (Y(D)/D2-His(189)/D2-Arg(294)/CP47-Glu(364)) are crucial for E(m)(Y(Z/D)). When D1-His(190) is protonated, corresponding to a thermally activated state, the calculated E(m)(Y(Z)) was +1216 mV, which is as high as the E(m) for P(D1/D2). We observed deprotonation at CP43-Arg(357) upon S-state transition, which may suggest its involvement in the proton exit pathway. E(m)(Y(D)) was affected by formation of P(D2)(+) (but not P(D1)(+)) and sensitive to the protonation state of D2-Arg(180). This points to an electrostatic link between Y(D) and P(D2).     

Enhancement by chloride ions of photoactivation of oxygen evolution in manganese-depleted photosystem II membranes

The Mn cluster that catalyzes photosynthetic oxygen evolution was removed from the photosystem II (PSII) complex by treating PSII membranes with 1.0 mM NH2OH with concomitant inactivation of oxygen evolution. The cluster was reconstituted by incubating the treated membranes with 1.0 mM Mn2+, 20 mM Ca2+, 10 microM 2,6-dichlorophenolindophenol, and Cl- under illumination with continuous or flashing light to restore the oxygen-evolving capacity. This light-dependent activation (photoactivation) of oxygen evolution did not occur to a significant extent at 3 mM Cl-, but markedly accelerated at higher Cl- concentrations without showing a saturation phenomenon even at 1 M Cl-. At 10 mM Cl- only about 10% of the oxygen-evolving activity before NH2OH treatment was restored by 5-min illumination with continuous light, whereas at 600 mM Cl- about 60% of the original activity was recovered. This acceleration resulted from at least two different actions of Cl-: (1) stabilization of the intermediate state involved in the photoactivation process and (2) increase in the quantum yield of photoactivation. The stabilization of the intermediate was saturated at about 150 mM Cl-, whereas the increase in yield did not show saturation. The Cl(-)-induced increase in quantum yield did not involve any changes in the affinity of either Mn2+ binding or Ca2+ binding for photoactivation, but was rather ascribed to a protective effect of Cl- against inhibition of photoactivation by high concentrations of Mn2+. We also found that removal of the extrinsic 33-kDa protein from the PSII complex increased the Cl- requirement for photoactivation.     

Substitution of chloride by bromide modifies the low-temperature tyrosine Z oxidation in active photosystem II

Chloride is an essential cofactor for photosynthetic water oxidation. However, its location and functional roles in active photosystem II are still a matter of debate. We have investigated this issue by studying the effects of Cl⁻ replacement by Br⁻ in active PSII. In Br⁻ substituted samples, Cl⁻ is effectively replaced by Br⁻ in the presence of 1.2 M NaBr under room light with protection of anaerobic atmosphere followed by dialysis. The following results have been obtained. i) The oxygen-evolving activities of the Br⁻-PSII samples are significantly lower than that of the Cl⁻-PSII samples; ii) The same S₂ multiline EPR signals are observed in both Br⁻ and Cl⁻-PSII samples; iii) The amplitudes of the visible light induced S₁Tyr_Z^• and S₂Tyr_Z^• EPR signals are significantly decreased after Br⁻ substitution; the S₁Tyr_Z^• EPR signal is up-shifted about 8 G, whereas the S₂Tyr_Z^• signal is down-shifted about 12 G after Br⁻ substitution. These results imply that the redox properties of Tyr_Z and spin interactions between Tyr_Z^• and Mn-cluster could be significantly modified due to Br⁻ substitution. It is suggested that Cl⁻/Br⁻ probably coordinates to the Ca²⁺ ion of the Mn-cluster in active photosystem II.     

Water oxidation chemistry of photosystem II

Photosystem II (PSII) uses light energy to split water into protons, electrons and O2. In this reaction, nature has solved the difficult chemical problem of efficient four-electron oxidation of water to yield O2 without significant amounts of reactive intermediate species such as superoxide, hydrogen peroxide and hydroxyl radicals. In order to use nature's solution for the design of artificial catalysts that split water, it is important to understand the mechanism of the reaction. The recently published X-ray crystal structures of cyanobacterial PSII complexes provide information on the structure of the Mn and Ca ions, the redox-active tyrosine called YZ and the surrounding amino acids that comprise the O2-evolving complex (OEC). The emerging structure of the OEC provides constraints on the different hypothesized mechanisms for O2 evolution. The water oxidation mechanism of PSII is discussed in the light of biophysical and computational studies, inorganic chemistry and X-ray crystallographic information.     

Water oxidation chemistry of photosystem II

The O(2)-evolving complex of photosystem II catalyses the light-driven four-electron oxidation of water to dioxygen in photosynthesis. In this article, the steps leading to photosynthetic O(2) evolution are discussed. Emphasis is given to the proton-coupled electron-transfer steps involved in oxidation of the manganese cluster by oxidized tyrosine Z (Y(*)(Z)), the function of Ca(2+) and the mechanism by which water is activated for formation of an O-O bond. Based on a consideration of the biophysical studies of photosystem II and inorganic manganese model chemistry, a mechanism for photosynthetic O(2) evolution is presented in which the O-O bond-forming step occurs via nucleophilic attack on an electron-deficient Mn(V)=O species by a calcium-bound water molecule. The proposed mechanism includes specific roles for the tetranuclear manganese cluster, calcium, chloride, Y(Z) and His190 of the D1 polypeptide. Recent studies of the ion selectivity of the calcium site in the O(2)-evolving complex and of a functional inorganic manganese model system that test key aspects of this mechanism are also discussed.     

Molecular origin of the pH dependence of tyrosine D oxidation kinetics and radical stability in photosystem II

A role for redox-active tyrosines has been demonstrated in many important biological processes, including water oxidation carried out by photosystem II (PSII) of oxygenic photosynthesis. The rates of tyrosine oxidation and reduction and the Tyr/Tyr reduction potential are undoubtedly controlled by the immediate environment of the tyrosine, with the coupling of electron and proton transfer, a critical component of the kinetic and redox behavior. It has been demonstrated by Faller et al. that the rate of oxidation of tyrosine D (Tyr(D)) at room temperature and the extent of Tyr(D) oxidation at cryogenic temperatures, following flash excitation, dramatically increase as a function of pH with a pK(a) of approximately 7.6 [Faller et al. 2001 Proc. Natl. Acad. Sci. USA 98, 14368-14373; Faller et al. 2001 Biochemistry 41, 12914-12920]. In this work, we investigated, using FTIR difference spectroscopy, the mechanistic reasons behind this large pH dependence. These studies were carried out on Mn-depleted PSII core complexes isolated from Synechocystis sp. PCC 6803, WT unlabeled and labeled with (13)C(6)-, or (13)C(1)(4)-labeled tyrosine, as well as on the D2-Gln164Glu mutant. The main conclusions of this work are that the pH-induced changes involve the reduced Tyr(D) state and not the oxidized Tyr(D)() state and that Tyr(D) does not exist in the tyrosinate form between pH 6 and 10. We can also exclude a change in the protonation state of D2-His189 as being responsible for the large pH dependence of Tyr(D) oxidation. Indeed, our data are consistent with D2-His189 being neutral both in the Tyr(D) and Tyr(D)() states in the whole pH6-10 range. We show that the interactions between reduced Tyr(D) and D2-His189 are modulated by the pH. At pH greater than 7.5, the nu(CO) mode frequency of Tyr(D) indicates that Tyr(D) is involved in a strong hydrogen bond, as a hydrogen bond donor only, in a fraction of the PSII centers. At pH below 7.5, the hydrogen-bonding interaction formed by Tyr(D) is weaker and Tyr(D) could be also involved as a hydrogen bond acceptor, according to calculations performed by Takahashi and Noguchi [J. Phys. Chem. B 2007 111, 13833-13844]. The involvement of Tyr(D) in this strong hydrogen-bonding interaction correlates with the ability to oxidize Tyr(D) at cryogenic temperatures and rapidly at room temperature. A strong hydrogen-bonding interaction is also observed at pH 6 in the D2-Gln164Glu mutant, showing that the residue at position D2-164 regulates the properties of Tyr(D.) The IR data point to the role of a protonatable group(s) (with a pK(a) of approximately 7) other than D2-His189 and Tyr(D), in modifying the characteristics of the Tyr(D) hydrogen-bonding interactions, and hence its oxidation properties. It remains to be determined whether the strong hydrogen-bonding interaction involves D2-His189 and if Tyr(D) oxidation involves the same proton transfer route at low and at high pH.     

Molecular origin of the pH dependence of tyrosine D oxidation kinetics and radical stability in photosystem II

A role for redox-active tyrosines has been demonstrated in many important biological processes, including water oxidation carried out by photosystem II (PSII) of oxygenic photosynthesis. The rates of tyrosine oxidation and reduction and the Tyr/Tyr reduction potential are undoubtedly controlled by the immediate environment of the tyrosine, with the coupling of electron and proton transfer, a critical component of the kinetic and redox behavior. It has been demonstrated by Faller et al. that the rate of oxidation of tyrosine D (Tyr_D) at room temperature and the extent of Tyr_D oxidation at cryogenic temperatures, following flash excitation, dramatically increase as a function of pH with a pK_a of ≈ 7.6 [Faller et al. 2001 Proc. Natl. Acad. Sci. USA 98, 14368-14373; Faller et al. 2001 Biochemistry 41, 12914-12920]. In this work, we investigated, using FTIR difference spectroscopy, the mechanistic reasons behind this large pH dependence. These studies were carried out on Mn-depleted PSII core complexes isolated from Synechocystis sp. PCC 6803, WT unlabeled and labeled with ¹³C₆-, or ¹³C₁(4)-labeled tyrosine, as well as on the D2-Gln164Glu mutant. The main conclusions of this work are that the pH-induced changes involve the reduced Tyr_D state and not the oxidized Tyr_D state and that Tyr_D does not exist in the tyrosinate form between pH 6 and 10. We can also exclude a change in the protonation state of D2-His189 as being responsible for the large pH dependence of Tyr_D oxidation. Indeed, our data are consistent with D2-His189 being neutral both in the Tyr_D and Tyr_D states in the whole pH6-10 range. We show that the interactions between reduced Tyr_D and D2-His189 are modulated by the pH. At pH greater than 7.5, the ν(CO) mode frequency of Tyr_D indicates that Tyr_D is involved in a strong hydrogen bond, as a hydrogen bond donor only, in a fraction of the PSII centers. At pH below 7.5, the hydrogen-bonding interaction formed by Tyr_D is weaker and Tyr_D could be also involved as a hydrogen bond acceptor, according to calculations performed by Takahashi and Noguchi [J. Phys. Chem. B 2007 111, 13833-13844]. The involvement of Tyr_D in this strong hydrogen-bonding interaction correlates with the ability to oxidize Tyr_D at cryogenic temperatures and rapidly at room temperature. A strong hydrogen-bonding interaction is also observed at pH 6 in the D2-Gln164Glu mutant, showing that the residue at position D2-164 regulates the properties of Tyr_D. The IR data point to the role of a protonatable group(s) (with a pK_a of ≈ 7) other than D2-His189 and Tyr_D, in modifying the characteristics of the Tyr_D hydrogen-bonding interactions, and hence its oxidation properties. It remains to be determined whether the strong hydrogen-bonding interaction involves D2-His189 and if Tyr_D oxidation involves the same proton transfer route at low and at high pH.     

C-550 in photosystem II subchloroplast particles

The photoreactions mediated by Photosystem II at low temperatures were examined in subchloroplast particles enriched in Photosystem II to determine if the Photosystem II activity was independent of C-550 in such particle preparations. Two types of Photosystem II particle preparations were tested, one enriched in chlorophyll b and the other purified further to eliminate the chlorophyll b. The Photosystem II-mediated photoreactions at low temperature were the same in both of the Photosystem II particle preparations as they were in normal chloroplasts. C-550 acted as if it were the primary electron acceptor of Photosystem II in all of the experiments performed.     

Substrate water binding and oxidation in photosystem II

This mini review presents a general introduction to photosystem II with an emphasis on the oxygen evolving complex. An attempt is made to summarise what is currently known about substrate interaction in the oxygen evolving complex of photosystem II in terms of the nature of the substrate, the timing and the location of its binding. As the nature of substrate water binding has a direct bearing on the mechanism of O-O bond formation in PSII, a discussion of O-O bond formation follows the summary of current opinion in substrate interaction.     

Chemical and kinetic evidence for an essential histidine in horseradish peroxidase for iodide oxidation.

Horseradish peroxidase (HRP), when incubated with diethylpyrocarbonate (DEPC), shows a time-dependent loss of iodide oxidation activity. The inactivation follows pseudo-first order kinetics with a second order rate constant of 0.43 min-1 M-1 at 30 degrees C and is reversed by neutralized hydroxylamine. The difference absorption spectrum of the modified versus native enzyme shows a peak at 244 nm, characteristic of N-carbethoxyhistidine, which is diminished by treatment with hydroxylamine. Correlation between the stoichiometry of histidine modification and the extent of inactivation indicates that out of 2 histidine residues modified, one is responsible for inactivation. A plot of the log of the reciprocal half-time of inactivation against log DEPC concentration further suggests that only 1 histidine is involved in catalysis. The rate of inactivation shows a pH dependence with an inflection point at 6.2, indicating histidine derivatization by DEPC. Inactivation due to modification of tyrosine, lysine, or cysteine has been excluded. CD studies reveal no significant change in the protein or heme conformation following DEPC modification. We suggest that a unique histidine residue is required for maximal catalytic activity of HRP for iodide oxidation.