Proton release during the four steps of photosynthetic water oxidation: induction of 1:1:1:1 pattern due to lack of chlorophyll a/b binding proteins.

In photosynthesis of green plants water is oxidized to dioxygen. This four-step process is accompanied by the release of four protons (per molecule of dioxygen) into the lumen of thylakoids. In dark-adapted thylakoids which are excited with a series of short flashes of light, the extent of proton release oscillates with period four as a function of flash number. Noninteger and pH-dependent proton/electron ratios (e.g., 1.1, 0.25, 1.0, and 1.65 at pH 7) have been attributed to a superposition of two reactions: chemical production of protons and transient electrostatic response of peripheral amino acid side chains. Aiming at the true pattern of proton production, we investigated the relative contribution of peripheral proteins. Thylakoids with and without chlorophyll a/b binding proteins were compared. Thylakoids lacking chlorophyll a/b binding proteins were prepared from pea seedlings grown under intermittent light [Jahns, P., & Junge, W. (1992) Biochemistry (preceding paper in this issue)]. We found no oscillation of proton release in the pH range from 6 to 7.5. These and other results showed that chlorophyll a/b binding proteins, which primarily serve as light-harvesting antennas, modulate proton release by water oxidation. A nonoscillating pattern of proton release, with proton/electron ratios of 1:1:1:1 more closely represents the events in the catalytic center proper. This implies hydrogen abstraction rather than electron abstraction from water during the oxygen-evolving step S3----S0.     

Proton and hydrogen currents in photosynthetic water oxidation

The photosynthetic processes that lead to water oxidation involve an evolution in time from photon dynamics to photochemically-driven electron transfer to coupled electron/proton chemistry. The redox-active tyrosine, Y(Z), is the component at which the proton currents necessary for water oxidation are switched on. The thermodynamic and kinetic implications of this function for Y(Z) are discussed. These considerations also provide insight into the related roles of Y(Z) in preserving the high photochemical quantum efficiency in Photosystem II (PSII) and of conserving the highly oxidizing conditions generated by the photochemistry in the PSII reaction center. The oxidation of Y(Z) by P(680)(+) can be described well by a treatment that invokes proton coupling within the context of non-adiabatic electron transfer. The reduction of Y(.)(Z), however, appears to proceed by an adiabatic process that may have hydrogen-atom transfer character.     

Proton release from water oxidation by photosystem II: similar stoichiometries are stabilized in thylakoids and PSII core particles by glycerol

During the four-stepped catalytic cycle of water oxidation by photosystem II (PSII) molecular oxygen is released in only one of the four reaction steps whereas the release of four protons is distributed over all steps. In principle, the pattern of proton production could be taken as indicative of the partial reactions with bound water. In thylakoids the extent and rate of proton release varies as function of the redox transition and of the pH without concomitant variations of the redox pattern. The variation has allowed to discriminate between deprotonation events of peripheral amino acids (Bohr effects) as opposed to the chemical deprotonation of a particular redox cofactor, and of water. In contrast, in thylakoids grown under intermittent light, as well as in PSII core particles the pattern of proton release is flat and independent of the pH. This has been attributed to the lack in these materials of the chlorophyll a,b-binding (CAB) proteins. We now found that a thylakoid-like, oscillatory pattern of proton release was restored simply by the addition of glycerol which modifies the protein–protein interaction. Being a further proof for the electrostatic origin of the greater portion of proton release, this effect will serve as an important tool in further studies of water oxidation.     

The terminal reaction cascade of water oxidation: Proton and oxygen release

In cyanobacteria, algae and plants Photosystem II produces the oxygen we breathe. Driven and clocked by light quanta, the catalytic Mn₄Ca-tyrosine centre accumulates four oxidising equivalents before it abstracts four electrons from water, liberating dioxygen and protons. Aiming at intermediates of the terminal four-electron cascade, we previously have suppressed this reaction by elevating the oxygen pressure, thereby stabilising one redox intermediate. Here, we established a similar suppression by increasing the proton concentration. Data were analysed in terms of only one (peroxy) redox intermediate between the fourfold oxidised Mn₄Ca-tyrosine centre and oxygen release. The surprising result was that the release into the bulk of one proton per dioxygen is linked to the first and rate-limiting electron transfer in the cascade rather than to the second which produces free oxygen. The penultimate intermediate might thus be conceived as a fully deprotonated peroxy-moiety.     

Proton release during the redox cycle of the water oxidase

Old and very recent experiments on the extent and the rate of proton release during the four reaction steps of photosynthetic water oxidation are reviewed. Proton release is discussed in terms of three main sources, namely the chemical production upon electron abstraction from water, protolytic reactions of Mn-ligands (e.g. oxo-bridges), and electrostatic response of neighboring amino acids. The extent of proton release differs between the four oxidation steps and greatly varies as a function of pH both, but differently, in thylakoids and PS II-membranes. Contrastingly, it is about constant in PS II-core particles. In any preparation, and on most if not all reaction steps, a large portion of proton transfer can occur very rapidly (<20 s) and before the oxidation of the Mn-cluster by Y_z ⁺ is completed. By these electrostatically driven reactions the catalytic center accumulates bases. An additional slow phase is observed during the oxygen evolving step, S₃S₄S₀. Depending on pH, this phase consists of a release or an uptake of protons which accounts for the balance between the number of preformed bases and the four chemically produced protons. These data are compatible with the hypothesis of concerted electron/proton-transfer to overcome the kinetic and energetic constraints of water oxidation.Abbreviations BBY-membranes Photosystem II-enriched membrane fragments prepared after Berthold, Babcock and Yocum (1981) - BSA bovine serum albumin - Chl chlorophyll - CAB-protein chlorophyll a/b-binding protein - core particles oxygen evolving reaction center core particles of Photosystem II - Cyt cytochrome - DCBQ 2,5-dichloro-p-benzoquinone - IML intermittent light - P-680 primary electron donor of Photosystem II - PS II Photosystem II - Y_z tyrosine residue on the D1 polypeptide, electron carrier between manganese and P-680 - photochemical reaction      

Discontinuous release of heat at successive steps of oxygenation in human and bovine hemoglobin at pH 9.0

We have measured the temperature dependence of the oxygen-binding isotherms of human and bovine hemoglobin at pH 9.0 in 0.1 M borate buffer. In both hemoglobins the ionization of the Bohr protons is finished at this pH; therefore, their heat does not interfere with the measurements. Two sets of curves have been obtained, which have been analyzed by either singular or global procedures for estimating the enthalpy changes of subsequent steps of oxygenation. The data indicate that in human hemoglobin the reaction with oxygen is enthalpy driven for steps 1, 2, and 4 while it is entropy driven for step 3. In bovine hemoglobin this phenomenon is even more evident: steps 2 and 4 are enthalpy driven while steps 1 and 3 are entropy driven. The discontinuous distribution of heat at subsequent steps of oxygenation suggests that the T to R transition in hemoglobin is not a monotonic process and involves conformations with novel characteristics.     

Proton stoichiometric imbalance during algae photosynthetic growth on various nitrogen sources: toward metabolic pH control

The use of algae as a potential platform for fuels or biochemical production requires process design and control that can be implemented at agronomic scales. Toward achieving pH control in large unmixed systems, we present a rigorous set of direct measurements of non-buffered proton uptake and efflux during growth on ammonium and nitrate, observing nearly unit molar proton imbalance H⁺/OH^? respectively for these nitrogen sources. This proton imbalance can be shown to be consistent with the initial assimilation steps of nitrogen from glutamate to peptide bonds which indicates that the remainder of metabolism is largely net proton balanced. These results are refined by demonstrating pH balance for growth with incrementally fed nitric acid and ammonium hydroxide. In contrast to the typical assumption of simple charge balance, each displays a slight proton uptake (around 10 % excess) that is considerably lower than urea, which displayed a molar H⁺ uptake per N assimilated of up to 33 %. This work illustrates details of proton imbalance that have been largely obscured in laboratory work due to use of elevated CO₂ and its associated carbonate equilibrium. Combined with the recent demonstration of preferential, mutually exclusive assimilation of ammonium over nitrate in Chlorella and Chlamydomonas, these results provide the stoichiometry and dynamics of photosynthetic algae growth needed to implement large-scale pH control in the absence of buffering.     

pH dependence of the four individual transitions in the catalytic S-cycle during photosynthetic oxygen evolution

We have investigated the pH dependence for each individual redox transition in the S-cycle of the oxygen evolving complex (OEC) of photosystem II by electron paramagnetic resonance (EPR) spectroscopy. In the experiments, OEC is advanced to the appropriate S-state at normal pH. Then, the pH is rapidly changed, and a new flash is given. The ability to advance to the next S-state in the cycle at different pHs is determined by measurements of the decrease or increase of characteristic EPR signals from the OEC in different S-states. In some cases the measured EPR signals are very small (this holds especially for the S0 ML signal at pH >7.5 and pH <4.8). Therefore, we refrain from providing error limits for the determined pK's. Our results indicate that the S1 --> S2 transition is independent of pH between 4.1 and 8.4. All other S-transitions are blocked at low pH. In the acidic region, the pK's for the inhibition of the S2 --> S3, the S3 --> [S4] --> S0, and the S0 --> S1 transitions are about 4.0, 4.5, and 4.7, respectively. The similarity of these pK values indicates that the inhibition of the steady-state oxygen evolution in the acidic range, which occurs with pK approximately 4.8, is a consequence of similar pH blocks in three of the redox steps involved in the oxygen evolution. In the alkaline region, we report a clear pH block in the S3 --> [S4] --> S0 transition with a pK of about 8.0. Our study also indicates the existence of a pH block at very high pH (pK approximately 9.4) in the S2 --> S3 transition. The S0 --> S1 transition is not affected, at least up to pH 9.0. This suggests that the inhibition of the steady-state oxygen evolution, which occurs with a pK of 8.0, is dominated by the inhibition of the S3 --> [S4] --> S0 transition. Our results are obtained in the presence of 5% methanol (v/v). However, it is unlikely that the determined pK's are affected by the presence of methanol since our results also show that the pH dependence of the steady-state oxygen evolution is not affected by methanol. The results in the alkaline region are in good agreement with a model, which suggests that the redox potential of Y(Z*)/Y(Z) is directly affected by high pH. At high pH the Y(Z*)/Y(Z) potential becomes lower than that of S2/S1 and S3/S2. The acidic block, with a pK of 4-5 in three S-transitions, implies that the inhibition mechanism is similar, and we suggest that it reflects protonation of a carboxylic side chain in the proton relay that expels protons from the OEC.     

Photosystem II and photosynthetic oxidation of water: an overview

Conceptually, photosystem II, the oxygen-evolving enzyme, can be divided into two parts: the photochemical part and the catalytic part. The photochemical part contains the ultra-fast and ultra-efficient light-induced charge separation and stabilization steps that occur when light is absorbed by chlorophyll. The catalytic part, where water is oxidized, involves a cluster of Mn ions close to a redox-active tyrosine residue. Our current understanding of the catalytic mechanism is mainly based on spectroscopic studies. Here, we present an overview of the current state of knowledge of photosystem II, attempting to delineate the open questions and the directions of current research.     

Mechanistic and structural aspects of photosynthetic water oxidation

Conclusions on the functional and structural organisation of photosynthetic water oxidation are gathered from a critical survey of the wealth of data reported in the literature and author's own experimental research: (1) the water oxidising complex (WOC) contains a tetranuclear manganese cluster of dimer of dimers' structure and functional heterogeneity of the metal centers, (2) the four step univalent oxidative pathway leading to water oxidation into molecular oxygen and four protons comprises only manganese, tyrosine Y_Z of polypeptide Dl and the substrate as redox active species, (3) the redox transitions S₀→ S₁ and S₁→ S₂ are manganese centered whereas S₂→ S₃ is most likely a ligand-centered reaction, (4) there exist several lines of evidence for a marked structural change that accompanies the redox transition S₂→ S₃, (5) one Ca²⁺ is an indispensible constituent of a functionally competent WOC while the role of Cl is much less clear and a direct participation disputable, (6) substrate water is most likely bound in all redox states S₀,…,S₃ and exchangeable with the bulk phase. The protonation state is determined by the redox state S₁ and the protein microenvironment. A mechanism is proposed for water oxidation in the WOC that is based on three key postulates: (1) water oxidation takes place in the first coordination sphere of one manganese dimer [Mn_aMn_b]; (2) the essential O-O bond is preformed in S₃ as part of a rapid redox isomerism S₃(I)→S₃(II) where in S₃(II) a nuclear geometry and electronic configuration is attained that corresponds to a peroxidic-type species; and (3) S₃(II) is an ‘entatic state’ for the formation of complexed dioxygen triggered by Y_Z^OX induced electron abstraction from the WOC and electronic redistribution to S₀(O₂).     

Application of the Marcus theory for analysis of the temperature dependence of the reactions leading to photosynthetic water oxidation: results and implications

The temperature dependence of donor side reactions was analysed within the framework of the Marcus theory of nonadiabatic electron transfer. The following results were obtained for PS II membrane fragments from spinach: (1) the reorganisation energy of P680^+? reduction by Y_Z is of the order of 0.5?eV in samples with a functionally fully competent water oxidising complex (WOC); (2) destruction of the WOC by Tris-washing gives rise to a drastic increase of λ to values of the order of 1.6?eV; (3) the reorganisation energies of the oxidation steps in the WOC are dependent, on the redox states S _i with values of about 0.6?eV for the reactions Y_Z ^OX S ₀→Y_Z S ₁ and Y_Z ^OX S ₁→Y_Z S ₂, 1.6?eV for the reaction Y_Z ^OX S ₂→Y_Z S ₃ and 1.1?eV (above a characteristic temperature u_c of about 6??°C) for the reaction Y_Z ^OX S ₃→→Y_Z S ₀+O₂. Using an empirical rate constant-distance relationship, the van der Waals distance between Y_Z and P680 was found to be about 10?Å, independent of the presence or absence of the WOC, whereas the distance between Y_Z and the manganese cluster in the WOC was ≥15?Å. Based on the calculated activation energies the environment of Y_Z is inferred to be almost "dry" and hydrophobic when the WOC is intact but becomes enriched with water molecules after WOC destruction. Furthermore, it is concluded that the transition S ₂→S ₃ is an electron transfer reaction gated by a conformational change, i.e. it comprises significant structural changes of functional relevance. Measurements of kinetic H/D isotope exchange effects support the idea that none of these reactions is gated by the break of a covalent O-H bond. The implications of these findings for the mechanism of water oxidation are discussed.     

Water-sensitive low-frequency vibrations of reaction intermediates during S-state cycling in photosynthetic water oxidation

In photosynthetic water oxidation, two water molecules are converted to an oxygen molecule through five reaction intermediates, designated S(n) (n = 0-4), at the catalytic Mn cluster of photosystem II. To understand the mechanism of water oxidation, changes in the chemical nature of the substrate water as well as the Mn cluster need to be defined during S-state cycling. Here, we report for the first time a complete set of Fourier transform infrared difference spectra during S-state cycling in the low-frequency (670-350 cm(-1)) region, in which interactions between the Mn cluster and its ligands can be detected directly, in PS II core particles from Thermosynechococcus elongatus. Furthermore, vibrations from oxygen and/or hydrogen derived from the substrate water and changes in them during S-state cycling were identified using multiplex isotope-labeled water, including H2(18)O, D2(16)O, and D2(18)O. Each water isotope affected the low-frequency S-state cycling spectra, characteristically. The bands sensitive only to (16)O/(18)O exchange were assigned to the modes from structures involving Mn and oxygen having no interactions with hydrogen, while the bands sensitive only to H/D exchange were assigned to modes from amino acid side chains and/or polypeptide backbones that associate with water hydrogen. The bands sensitive to both (16)O/(18)O and H/D exchanges were attributed to the structure involving Mn and oxygen structurally coupled with hydrogen in a direct or an indirect manner through hydrogen bonds. These bands include the changes of intermediate species derived from substrate water during the process of photosynthetic water oxidation.     

A new mechanism-based inhibitor of photosynthetic water oxidation: acetone hydrazone. 1. Equilibrium reactions

The process of photosynthetic water oxidation has been investigated by using a new type of water oxidation inhibitor, the alkyl hydrazones. Acetone hydrazone (AceH), (CH3)2CNNH2, inhibits water oxidation by a mechanism that is analogous to that of NH2OH. This involves binding to the water-oxidizing complex (WOC), followed by photoreversible reduction of manganese (loss of the S1----S2 reaction). At higher AceH concentrations the S1 state is reduced in the dark and Mn is released, albeit to a lesser extent than with NH2OH. Following extraction of Mn, AceH is able to donate electrons rapidly to the reaction center tyrosine radical Z+ (161Tyr-D1 protein), more slowly to a reaction center radical C+, and not at all to the dark-stable tyrosine radical D+ (160Tyr-D2 protein) which must be sequestered in an inaccessible site. Manganese, Z+, and C+ thus appear to be located in a common protein domain, with Mn being the first accessible donor, followed by Z+ and then C+. Photooxidation of Cyt b-559 is suppressed by AceH, indicating either reduction or competition for donation to P680+. Unexpectedly, Cl- was found not to interfere or compete with AceH for binding to the WOC in the S1 state, in contrast to the reported rate of binding of N,N-dimethylhydroxylamine, (CH3)2NOH [Beck, W., & Brudvig, G. (1988) J. Am. Chem. Soc. 110, 1517-1523]. We interpret the latter behavior as due to ionic screening of the thylakoid membrane, rather than a specific Cl- site involved in water oxidation.(ABSTRACT TRUNCATED AT 250 WORDS)     

A new mechanism-based inhibitor of photosynthetic water oxidation: acetone hydrazone. 2. Kinetic probes

The mechanism of photosynthetic water oxidation in spinach was investigated with a newly developed inhibitor of the water-oxidizing complex, acetone hydrazone (AceH), (CH3)2CNNH2 [Tso, J., Petrouleas, V., & Dismukes, G.C. (1990) Biochemistry (preceding paper in this issue)], by using fluorescence induction and single-turnover flashes to monitor O2 yield and thermoluminescence intensity. AceH binds slowly (1-3 min) in the dark to the S1 (resting) oxidation state of the water-oxidizing complex in thylakoids and PSII membranes. Once bound, it causes a two-flash delay in the pattern of O2 release seen in a train of flashes. This is initiated by reduction of manganese in the S2 oxidation state of the complex in a fast reaction (less than 0.5 s). In thylakoid membranes which have been partially inhibited at low AceH concentrations (less than 2 mM) the inhibition can be reversed by a single flash and a subsequent dark period. This behavior can be explained by two sequential one-electron oxidation steps: S1.AceHhv----S2.AceH in equilibrium S1.AceH+hv----S2.AceH+----S1 + AceH2+ Dissociation of the unobserved radical intermediate, AceH+, from S1 is proposed to account for the recovery from inhibition after one flash. In contrast, recovery from inhibition after a single flash is not observed in detergent-isolated PSII membranes or in intact thylakoid membranes at higher AceH concentrations (greater than 2 mM), where the two-flash delay in O2 release is seen. This suggests either a concerted two-electron process, S2----S0, or tight binding of AceH+ to S1.(ABSTRACT TRUNCATED AT 250 WORDS)     

Mechanistic implications of variable stoichiometries of oxygen consumption during tyrosinase catalyzed oxidation of monophenols and o-diphenols

The stoichiometry of oxygen consumption during tyrosinase-catalyzed oxidation of an o-diphenol (4-tert-butylcatechol, TBC) and a monophenol (4-tert-butylphenol, TBP) has been determined. At high [substrate]/[enzyme] ratios, in the case of o-diphenols, the stoichiometry of the enzyme-catalyzed reaction was always 1 O(2)/2 o-diphenols, although if the o-quinone product was unstable, the apparent stoichiometry could tend to 1 O(2)/1 o-diphenol due to regeneration of an o-diphenol in a side reaction. In the case of monophenols, the stoichiometry could be 1 O(2)/1 monophenol or 1.5 O(2)/1 monophenol depending if the o-quinone product was stable or unstable, respectively. However, at low [substrate]/[enzyme] ratios, the oxygen/substrate stoichiometry could, even in the case where stable products are formed, be lower than 1 O(2)/2 substrates for o-diphenols or higher than 1 O(2)/1 substrate for monophenols. These data supported the mechanism proposed by Rodríguez-López et al. [J. Biol. Chem. 267 (1992) 3801-3810], in which, during hydroxylation of monophenols, tyrosinase first transformed monophenol to o-diphenol and then either catalyzed a further oxidation to form o-quinone or released it into the reaction medium. In this second case, subsequent oxidation of the o-diphenol resulted in additional oxygen consumption.     

Studies on the mechanism of chloride action on photosynthetic water oxidation

In this paper, we describe experiments which were designed to probe the mechanism through which Cl^? anions exert their influence on electron transport on the oxidizing side of Photosystem II (PS II). We asked whether photosynthetically active Mn was released from and reinserted into the water-splitting enzyme upon Cl^? removal and subsequent repletion, and obtained evidence suggesting that it was not. To locate the site of the Cl^?-dependent lesion, we counted the number of electrons that were still available in Cl^?-free chloroplasts for rapid reduction of P-680⁺ following a flash, and compared our results with other, previously characterized methods of inhibition. Using both delayed and prompt fluorescence as measures of the lifetime of P-680⁺, we found that Cl^?-depleted thylakoids could deliver two electrons to the oxidized PS II reaction center. This is interpreted as indicating that two oxidizing equivalents can be generated and transiently stored by PS II after Cl^? removal. Two alternative schemes which describe the functional location of electron carriers in this portion of the electron transport chain are proposed to account for our data. An experiment designed to distinguish between them is discussed. We also investigated the stability of oxidants produced by the Cl^?-depleted PS II. The apparently contradictory results obtained by prompt fluorescence and luminescence measurements are tentatively resolved by postulating the existence of two pathways through which closed reaction centers reopen, only one of which proceeds via a luminescence-producing recombination mechanism. It is suggested that deactivation of the PS-II oxidizing equivalents through both pathways is accelerated by Cl^? removal.     

Aging of the photosynthetic apparatus VI. Changes in pH dependence of {Delta}pH, thylakoid internal pH and proton uptake and relationships to electron transport

The pH difference generated across the chloroplast membraneupon illumination (pH) and the internal pH (pHi) were analyzedin aged spinach chloroplasts and in fresh chloroplasts supplementedwith linolenate. In electron-flow conditions where both photosystemsor either photosystem alone were functional, the pH droppedand their optima shifted toward more acidic external pH (pHo)with a simultaneous increase in pHi. Upon aging or additionof linolenate, a decrease of pHo was therefore required to maintainthe pHi in the range of 5–5.5 for maximum electron-flowactivity. Moreover, aging like linolenate, diminished the protonpump activity and shifted its optimum (pH 6.7 in the controls)toward higher pHo. Although pH and pHi changes were similarin all electron-flow conditions, the sensitivity of pH towardaging and linolenate was eventually higher under photosystemII than photosystem I conditions. In conclusion, the electron-flow activity seems to be delicatelycontrolled by the proton pump, pH, pHi and pHo. Unsaturatedfatty acids which are released during chloroplast aging damagethe membrane integrity in such a way that the subtle equilibriumbetween these factors is disturbed. (Received April 19, 1977; )