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.     

Reaction pattern and mechanism of light induced oxidative water splitting in photosynthesis

This mini review is an attempt to briefly summarize our current knowledge on light driven oxidative water splitting in photosynthesis. The reaction leading to molecular oxygen and four protons via photosynthesis comprises thermodynamic and kinetic constraints that require a balanced fine tuning of the reaction coordinates. The mode of coupling between electron (ET) and proton transfer (PT) reactions is shown to be of key mechanistic relevance for the redox turnover of Y_Z and the reactions within the WOC. The WOC is characterized by peculiar energetics of its oxidation steps in the WOC. In all oxygen evolving photosynthetic organisms the redox state S₁ is thermodynamically most stable and therefore this general feature is assumed to be of physiological relevance. Available information on the Gibbs energy differences between the individual redox states S_i+1 and S_i and on the activation energies of their oxidative transitions are used to construct a general reaction coordinate of oxidative water splitting in photosystem II (PS II). Finally, an attempt is presented to cast our current state of knowledge into a mechanism of oxidative water splitting with special emphasis on the formation of the essential O-O bond and the active role of the protein environment in tuning the local proton activity that depends on time and redox state S_i. The O-O linkage is assumed to take place within a multistate equilibrium at the redox level of S₃, comprising both redox isomerism and proton tautomerism. It is proposed that one state, S₃(P), attains an electronic configuration and nuclear geometry that corresponds with a hydrogen bonded peroxide which acts as the entatic state for the generation of complexed molecular oxygen through S₃(P) oxidation by Y_Z^ox.     

Water cleavage by solar radiation—an inspiring challenge of photosynthesis research

Solar energy exploitation by photosynthetic water cleavage is of central relevance for the development and sustenance of all higher forms of living matter in the biosphere. The key steps of this process take place within an integral protein complex referred to as Photosystem II (PS II) which is anisotropically incorporated into the thylakoid membrane. This minireview concentrates on mechanistic questions related to i) the generation of strongly oxidizing equivalents (holes) at a special chlorophyll a complex (designated as P680) and ii) the cooperative reaction of four holes with two water molecules at a manganese containing unit WOC (water oxidizing complex) resulting in the release of molecular oxygen and four protons. The classical work of Pierre Joliot and Bessel Kok and their coworkers revealed that water oxidation occurs via a sequence of univalent oxidation steps including intermediary redox states S_i (i = number of accumulated holes within the WOC). Based on our current stage of knowledge, an attempt is made a) to identify the nature of the redox states S_i, b) to describe the structural arrangement of the (four) manganese centers and their presumed coordination and ligation within the protein matrix, and c) to propose a mechanism of photosynthetic water oxidation with special emphasis on the key step, i.e. oxygen-oxygen bond formation. It is assumed that there exists a dynamic equilibrium in S₃ with one state attaining the nuclear geometry and electronic configuration of a complexed peroxide. This state is postulated to undergo direct oxidation to complexed dioxygen by univalent electron abstraction with Y_Z ^ox and simultaneous internal ligand to metal charge transfer.Key questions on the mechanism will be raised. The still fragmentary answers to these questions not only reflect our limited knowledge but also illustrate the challenges for future research.Abbreviations b559 cytochrome b559 - BChl bacteriochlorophyll - Chl chlorophyll - CP47 Chl a containing a 47 kDa polypeptide - D1/D2 polypeptides of the PS II reaction center - ENDOR electron nuclear double resonance - EPR electron paramagnetic resonance - ESEEM electron spin echo envelope modulation - EXAFS extended X-ray absorption fine structure - FTIR Fourier transform infrared - NMR nuclear magnetic resonance - P680, P700 photoactive Chl a of PS II and PS I, respectively - PS II Photosystem II - Q_A special plastoquinone of PS II - S_i redox states of WOC - WOC water oxidizing complex - WOS water oxidizing site - UV/VIS ultraviolet/visible - Y_D, Y_Z redox active tyrosines of polypeptides D2 and D1, respectively     

Oxidative photosynthetic water splitting: energetics,kinetics and mechanism

This minireview is an attempt to summarize our current knowledge on oxidative water splitting in photosynthesis. Based on the extended Kok model (Kok, Forbush, McGloin (1970) Photochem Photobiol 11:457–476) as a framework, the energetics and kinetics of two different types of reactions comprising the overall process are discussed: (i) P680^+• reduction by the redox active tyrosine Y_Z of polypeptide D1 and (ii) Y_z^ox induced oxidation of the four step sequence in the water oxidizing complex (WOC) leading to the formation of molecular oxygen. The mode of coupling between electron transport (ET) and proton transfer (PT) is of key mechanistic relevance for the redox turnover of Y_Z and the reactions within the WOC. The peculiar energetics of the oxidation steps in the WOC assure that redox state S₁ is thermodynamically most stable. This is a general feature in all oxygen evolving photosynthetic organisms and assumed to be of physiological relevance. The reaction coordinate of oxidative water splitting is discussed on the basis of the available information about the Gibbs energy differences between the individual redox states S _i+1 and S _i and the data reported for the activation energies of the individual oxidation steps in the WOC. Finally, an attempt is made to cast our current state of knowledge into a mechanism of oxidative water splitting with special emphasis on the formation of the essential O–O bond and on the active role of the protein in tuning the local proton activity that depends on time and redox state S _i . The O–O linkage is assumed to take place at the level of a complexed peroxide.     

Electron transfer from Cyt b 559 and tyrosine-D to the S2 and S3 states of the water oxidizing complex in photosystem II at cryogenic temperatures

The Mn₄CaO₅ cluster of photosystem II (PSII) catalyzes the oxidation of water to molecular oxygen through the light-driven redox S-cycle. The water oxidizing complex (WOC) forms a triad with Tyrosine_Z and P₆₈₀, which mediates electrons from water towards the acceptor side of PSII. Under certain conditions two other redox-active components, Tyrosine_D (Y_D) and Cytochrome b ₅₅₉ (Cyt b ₅₅₉) can also interact with the S-states. In the present work we investigate the electron transfer from Cyt b ₅₅₉ and Y_D to the S₂ and S₃ states at 195 K. First, Y_D ^? and Cyt b ₅₅₉ were chemically reduced. The S₂ and S₃ states were then achieved by application of one or two laser flashes, respectively, on samples stabilized in the S₁ state. EPR signals of the WOC (the S₂-state multiline signal, ML-S₂), Y_D ^? and oxidized Cyt b ₅₅₉ were simultaneously detected during a prolonged dark incubation at 195 K. During 163 days of incubation a large fraction of the S₂ population decayed to S₁ in the S₂ samples by following a single exponential decay. Differently, S₃ samples showed an initial increase in the ML-S₂ intensity (due to S₃ to S₂ conversion) and a subsequent slow decay due to S₂ to S₁ conversion. In both cases, only a minor oxidation of Y_D was observed. In contrast, the signal intensity of the oxidized Cyt b ₅₅₉ showed a two-fold increase in both the S₂ and S₃ samples. The electron donation from Cyt b ₅₅₉ was much more efficient to the S₂ state than to the S₃ state.     

EPR studies of the water oxidizing complex in the S1 and the higher S states: the manganese cluster and YZ radical

The parallel polarization electron paramagnetic resonance (EPR) method has been applied to investigate manganese EPR signals of native S₁ and S₃ states of the water oxidizing complex (WOC) in photosystem (PS) II. The EPR signals in both states were assigned to thermally excited states with S=1, from which zero-field interaction parameters D and E were derived. Three kinds of signals, the doublet signal, the singlet-like signal and g=11–15 signal, were detected in Ca²⁺-depleted PS II. The g=11–15 signal was observed by parallel and perpendicular modes and assigned to a higher oxidation state beyond S₂ in Ca²⁺-depleted PS II. The singlet-like signal was associated with the g=11–15 signal but not with the Y_Z (the tyrosine residue 161 of the D1 polypeptide in PS II) radical. The doublet signal was associated with the Y_Z radical as proved by pulsed electron nuclear double resonance (ENDOR) and ENDOR-induced EPR. The electron transfer mechanism relevant to the role of Y_Z radical was discussed.     

How chloride functions to enable proton conduction in photosynthetic water oxidation: Time-resolved kinetics of intermediates (S-states) in vivo and bromide substitution

Chloride (Cl⁻) is essential for O₂ evolution during photosynthetic water oxidation. Two chlorides near the water-oxidizing complex (WOC) in Photosystem II (PSII) structures from Thermosynechococcus elongatus (and T. vulcanus) have been postulated to transfer protons generated from water oxidation. We monitored four criteria: primary charge separation flash yield (P* → P⁺Q_A⁻), rates of water oxidation steps (S-states), rate of proton evolution, and flash O₂ yield oscillations by measuring chlorophyll variable fluorescence (P* quenching), pH-sensitive dye changes, and oximetry. Br-substitution slows and destabilizes cellular growth, resulting from lower light-saturated O₂ evolution rate (−20 %) and proton release (−36 % ΔpH gradient). The latter implies less ATP production. In Br- cultures, protonogenic S-state transitions (S₂ → S₃ → S₀’) slow with increasing light intensity and during O₂/water exchange (S₀’ → S₀ → S₁), while the non-protonogenic S₁ → S₂ transition is kinetically unaffected. As flash rate increases in Cl⁻ cultures, both rate and extent of acidification of the lumen increase, while charge recombination is suppressed relative to Br⁻. The Cl⁻ advantage in rapid proton escape from the WOC to lumen is attributed to correlated ion-pair movement of H₃O⁺Cl⁻ in dry water channels vs. separated Br⁻ and H⁺ ion movement through different regions (>200-fold difference in Bronsted acidities). By contrast, at low flash rates a previously unreported reversal occurs that favors Br⁻ cultures for both proton evolution and less PSII charge recombination. In Br⁻ cultures, slower proton transfer rate is attributed to stronger ion-pairing of Br⁻ with AA residues lining the water channels. Both anions charge-neutralize protons and shepherd them to the lumen using dry aqueous channels.     

Water exchange in manganese-based water-oxidizing catalysts in photosynthetic systems: From the water-oxidizing complex in photosystem II to nano-sized manganese oxides

The water-oxidizing complex (WOC), also known as the oxygen-evolving complex (OEC), of photosystem II in oxygenic photosynthetic organisms efficiently catalyzes water oxidation. It is, therefore, responsible for the presence of oxygen in the Earth's atmosphere. The WOC is a manganese–calcium (Mn₄CaO₅(H₂O)₄) cluster housed in a protein complex. In this review, we focus on water exchange chemistry of metal hydrates and discuss the mechanisms and factors affecting this chemical process. Further, water exchange rates for both the biological cofactor and synthetic manganese water splitting are discussed. The importance of fully unveiling the water exchange mechanism to understand the chemistry of water oxidation is also emphasized here. This article is part of a Special Issue entitled: Photosynthesis Research for Sustainability: Keys to Produce Clean Energy.     

Search for intermediates of photosynthetic water oxidation

Photosystem II of cyanobacteria and plants incorporates the catalytic centre of water oxidation. Powered and clocked by quanta of light the centre accumulates four oxidising equivalents before oxygen is released. The first three oxidising equivalents are stored on the Mn₄Ca-cluster, raising its formal oxidation state from S₀ to S₃ and the third on Y_Z, producing S₃ Y_Z^ox. From there on water oxidation proceeds in what appears as a single reaction step (S₃ Y_Z^ox(H₂O)₂O₂ + 4H⁺ + S₀. Intermediate oxidation products of bound water had not been detected, until our recent report on the stabilisation of such an intermediate by high oxygen pressure (NATURE 430, 2004, 480–483). Based on the oxygen titration (half-point 2.3 bar) the standard free-energy profile of a reaction sequence with a single intermediate was calculated. It revealed a rather small difference (−3 kJ mol⁻¹) between the starting state [S₃Y_Z^OX and the product state S₀Y_Z + O₂ + 4H⁺ . Here we describe the tests for side effects of exposing core particles to high oxygen pressure. We found the reduction of P₆₈₀^{+ ·} in ns and the reduction/dismutation of quinones at the acceptor side of PSII both unaffected, and the inhibition of the oxygen evolving reaction by exposure to high O₂-pressure was fully reversible by decompression to atmospheric conditions.     

Mn2+ reduces Yz + in manganese-depleted Photosystem II preparations

Manganese in the oxygen-evolving complex is a physiological electron donor to Photosystem II. PS II depleted of manganese may oxidize exogenous reductants including benzidine and Mn²⁺. Using flash photolysis with electron spin resonance detection, we examined the room-temperature reaction kinetics of these reductants with Y_z ⁺, the tyrosine radical formed in PS II membranes under illumination. Kinetics were measured with membranes that did or did not contain the 33 kDa extrinsic polypeptide of PS II, whose presence had no effect on the reaction kinetics with either reductant. The rate of Y_z ⁺ reduction by benzidine was a linear function of benzidine concentration. The rate of Y_z ⁺ reduction by Mn²⁺ at pH 6 increased linearly at low Mn²⁺ concentrations and reached a maximum at the Mn²⁺ concentrations equal to several times the reaction center concentration. The rate was inhibited by K⁺, Ca²⁺ and Mg²⁺. These data are described by a model in which negative charge on the membrane causes a local increase in the cation concentration. The rate of Y_z ⁺ reduction at pH 7.5 was biphasic with a fast 400 s phase that suggests binding of Mn²⁺ near Y_z ⁺ at a site that may be one of the native manganese binding sites.Abbreviations PS II Photosystem II - Y_D tyrosine residue in Photosystem II that gives rise to the stable Signal II EPR spectrum - Y_z tyrosine residue in Photosystem II that mediates electron transfer between the reaction center chlorophyll and the site of water oxidation - ESR electron spin resonance - DPC diphenylcarbazide - DCIP dichlorophenolindophenol     

Studies on the electron transfer from Tyr-161 of polypeptide D-1 to P680+ in PS II membrane fragments from spinach

The functional connection between redox component Y _z identified as Tyr-161 of polypeptide D-1 (Debus et al. 1988) and P680⁺ was analyzed by measurements of laser flash induced absorption changes at 830 nm in PS II membrane fragments from spinach. It was found that neither DCMU nor the ADRY agent 2-(3-chloro-4-trifluoromethyl) anilino-3,5-dinitrothiophene (ANT 2p) affects the rate of P680⁺ reduction by Y _z under conditions where the catalytic site of water oxidation stays in the redox state S₁. In contrast to that, a drastic retardation is observed after mild trypsin treatment at pH=6.0. This effect which is stimualted by flash illumination can be largely reversed by Ca²⁺. The above mentioned data lead to the following conclusions: (a) the segment of polypeptide D-1 containing Tyr-161 and coordination sites of P680 is not allosterically affected by structural changes due to DCMU binding at the Q_B-site which is also located in D-1. (b) ANT 2p as a strong protonophoric uncoupler and ADRY agent does not modify the reaction coordinate of P680⁺ reduction by Y _z , and (c) Ca²⁺ could play a functional role for the electronic and vibrational coupling between the redox groups Y _z and P680. The electron transport from Y _z to P680⁺ is discussed within the framework of a nonadiabatic process. Based on thermodynamic considerations the reorganization energy is estimated to be in the order of 0.5 V.Abbreviations ADRY acceleration of the deactivation reactions of the water splitting enzyme system Y - ANT 2p 2-(3-chloro-4-trifluoromethyl)anilino-3,5 dinitrothiophene - DCMU 3-(3,4-dichlorophenyl)-1,1-dimethylurea - MES 2[N-Morpholino]ethanesulfonic acid - PS II photosystem II - Q_A, Q_B primary and secondary plastoquinone acceptor of photosystem II - S _i redox states of the catalytic site of water oxidation - Y _z redox active Tyr-161 of polypeptide D-1     

Synthesis, characterization and redox reactivity of l-tartrato bridged dinuclear manganese complex with 2,2′-bipyridine

A new l-tartrato manganese(III) complex was synthesized and characterized as the dinuclear dimanganese(III) structure with a stereospefically formed [Λ-Λ] absolute configuration around Mn(III) ions. The thermal and photo decomposition gave the first example of dihydrogen gas evolution besides CO and CO₂ gas associated with cis-[Mn^II(ox)(bpy)(H₂O)₂]. A proposed redox reaction proceeds from Mn(III) to Mn(II) via intermediate Mn(IV) and Mn(II) with CO anion radical species followed by oxidation of tartrate ligands.     

EPR and ENDOR studies of the water oxidizing complex of Photosystem II

A comparative study of X-band EPR and ENDOR of the S₂ state of photosystem II membrane fragments and core complexes in the frozen state is presented. The S₂ state was generated either by continuous illumination at T=200 K or by a single turn-over light flash at T=273 K yielding entirely the same S₂ state EPR signals at 10 K. In membrane fragments and core complex preparations both the multiline and the g=4.1 signals were detected with comparable relative intensity. The absence of the 17 and 23 kDa proteins in the core complex preparation has no effect on the appearance of the EPR signals. ¹H-ENDOR experiments performed at two different field positions of the S₂ state multiline signal of core complexes permitted the resolution of four hyperfine (hf) splittings. The hf coupling constants obtained are 4.0, 2.3, 1.1 and 0.6 MHz, in good agreement with results that were previously reported (Tang et al. (1993) J Am Chem Soc 115: 2382–2389). The intensities of all four line pairs belonging to these hf couplings are diminished in D₂O. A novel model is presented and on the basis of the two largest hfc's distances between the manganese ions and the exchangeable protons are deduced. The interpretation of the ENDOR data indicates that these hf couplings might arise from water which is directly ligated to the manganese of the water oxidizing complex in redox state S₂.Abbreviations cw continuous wave - ENDOR electron nuclear double resonance - EPR electron paramagnetic resonance - hf hyperfine - hfc hyperfine coupling - MLS multiline signal - PS II Photosystem II - rf radio frequency - WOC water oxidizing complex     

Spectroscopic studies of the manganese complex of Photosystem II

Our recent EPR and EXAFS experiments investigating the structure of the oxygen-evolving complex of PS II are discussed. PS II treatments which affect the cofactors calcium and chloride have been used to poise samples in modified forms of the S-states, S₁, S₂ and S₃. X-ray absorption studies indicate a similar overall structure for the manganese complex between treated and native samples although the influence of the treatments and cofactors is observed. Manganese oxidation (or oxidation of a ligand to the manganese cluster) is indicated to occur on each of the transitions S₁ S₂ and S₂ S₃ in these modified samples. The cluster appears to contain at least two inequivalent Mn-Mn pairs. In the native samples the Mn-Mn distance is 2.7 Å, but in samples where the calcium site is affected, one of the pairs has a 3.0 Å Mn-Mn distance. The intensity of the 3.3/3.6 Å interaction is reduced on sodium chloride treatment (calcium depletion) perhaps indicating calcium binding close to the manganese cluster. From EPR data we also propose that treatments which affect calcium and chloride binding cause a modification of the native S₂ state, slow the reduction of Y_z and allow an S3 EPR signal to be observed following illumination. The origin of the S3 EPR signal, a modified S₃ or S₂ X where X is an organic radical of unknown charge, is discussed in relation to the results from the EXAFS studies.Abbreviations EPR electron paramagnetic resonance spectroscopy - EXAFS extended X-ray absorption fine structure - HTG n-heptyl -d-thioglucoside - MES 2(N-morpholino)ethanesulfonic acid - OEC oxygen evolving complex - PPBQ phenyl-1,4-benzoquinone - PS II Photosystem II - Y_z redox active tyrosine     

The origin of split EPR signals in the Ca2+-depleted Photosystem II

A light-driven reaction model for the Ca²⁺-depleted Photosystem (PS) II is proposed to explain the split signal observed in electron paramagnetic resonance (EPR) spectra based on a comparison of EPR assignments with recent x-ray structural data. The split signal has a splitting linewidth of 160 G at around g = 2 and is seen upon illumination of the Ca²⁺-depleted PS II in the S₂ state associated with complete or partial disappearance of the S₂ state multiline signal. Another g=2 broad ESR signal with a 110 G linewidth was produced by 245 K illumination for a short period in the Ca²⁺-depleted PS II in S₁ state. At the same time a normal Y_Z^· radical signal was also efficiently trapped. The g=2 broad signal is attributed to an intermediate S₁X^· state in equilibrium with the trapped Y_Z^· radical. Comparison with x-ray structural data suggests that one of the split signals (doublet signal) is attributable to interaction between His 190 and the Y_Z^· radical, and other signals is attributable to interaction between His 337 and the manganese cluster, providing further clues as to the mechanism of water oxidation in photosynthetic oxygen evolution.     

Electron exchange coupling in a naturally occurring tetramangano cluster in the mineral helvite, (Mn4S)(SiBeO4)3

The mineral helvite, (Mn₄S)(BeSiO₄)₃, contains discrete tetrahedral Mn₄S⁺⁶ clusters in which the S^?2 is tetrahedrally coordinated and each Mn(II) is in a distorted tetrahedron of one S^?2 and three oxygens; the cluster is situated within an encompassing lattice of SiO₄^?4 and BeO₄^?6 tetrahedra. Mn₄S⁺⁶ centers provide an interesting model for comparison to the polynuclear manganese center that is associated with photosynthetic water oxidation. Magnetic susceptibility data between 77 and 298 K have been measured for a natural helvite sample containing principally Mn₄S⁺⁶ centers but with significant contamination from Mn₃FeS⁺⁶ and Mn₃CaS⁺⁶. The data exhibited Curie-Weiss behavior with μ_eff = 5.969 B.M. and θ = 178.3 K. An analysis of the magnetic susceptibility, based on Van Vleck's formalism, demonstrated the presence of antiferromagnetic coupling, with a coupling constant J = ?5.83 cm^?1. Mössbauer spectra of Mn₃FeS centers in helvite and of Fe₄S centers in the related mineral danalite have also been recorded. Isomer shifts show little temperature dependence and lie in the range 1.23–1.43 $\text{mm}\text{sec.}$. This range is typical of tetrahedrally coordinated Fe(II) in several ionic crystals but is significantly above that of Fe(II) in ferredoxins and below that in the [quinone-Fe(II)-quinone] complex of the photosynthetic bacterium,Rhodopseudomonas sphaeroides. Quadrupole splittings are highly temperature dependent, ranging from 2.4 $\text{mm}\text{sec}$ at 4.2 K to less than 0.5 $\text{mm}\text{sec}$ at 248 K.     

Photo-catalytic oxidation of a di-nuclear manganese centre in an engineered bacterioferritin ‘reaction centre’

Photosynthesis involves the conversion of light into chemical energy through a series of electron transfer reactions within membrane-bound pigment/protein complexes. The Photosystem II (PSII) complex in plants, algae and cyanobacteria catalyse the oxidation of water to molecular O₂. The complexity of PSII has thus far limited attempts to chemically replicate its function. Here we introduce a reverse engineering approach to build a simple, light-driven photo-catalyst based on the organization and function of the donor side of the PSII reaction centre. We have used bacterioferritin (BFR) (cytochrome b1) from Escherichia coli as the protein scaffold since it has several, inherently useful design features for engineering light-driven electron transport. Among these are: (i.) a di-iron binding site; (ii.) a potentially redox-active tyrosine residue; and (iii.) the ability to dimerise and form an inter-protein heme binding pocket within electron tunnelling distance of the di-iron binding site. Upon replacing the heme with the photoactive zinc-chlorin e₆ (ZnCe₆) molecule and the di-iron binding site with two manganese ions, we show that the two Mn ions bind as a weakly coupled di-nuclear Mn₂^II,II centre, and that ZnCe₆ binds in stoichiometric amounts of 1:2 with respect to the dimeric form of BFR. Upon illumination the bound ZnCe₆ initiates electron transfer, followed by oxidation of the di-nuclear Mn centre possibly via one of the inherent tyrosine residues in the vicinity of the Mn cluster. The light dependent loss of the Mn^II EPR signals and the formation of low field parallel mode Mn EPR signals are attributed to the formation of Mn^III species. The formation of the Mn^III is concomitant with consumption of oxygen. Our model is the first artificial reaction centre developed for the photo-catalytic oxidation of a di-metal site within a protein matrix which potentially mimics water oxidation centre (WOC) photo-assembly.     

Synthesis, characterization, electrochemical and magnetic studies on manganese(III) complexes involving bridging carboxylates

A series of carboxylate-bridged manganese(III) complexes derived from Schiff bases obtained by the condensation of salicylaldehyde or 5-bromo-salicylaldehyde and different types of diamine have been synthesized and characterized and, in the case of [Mn₂(L1)₂(μ-ClCH₂COO)](ClO₄) (1), the structure has been obtained by X-ray crystallography. The structure of 1 consists of two manganese atoms separated by 5.487(3) Å and bridged by a carboxylate anion. This dinuclear structural unit is linked by bridging phenoxy oxygens to adjacent dinuclear units to produce a one-dimensional chain. Cyclic voltammograms of all the compounds exhibit grossly similar features consisting of a reversible or quasi-reversible Mn^III/Mn^II reduction and a Mn^III/Mn^IV oxidation. It has been observed that bromo-substitution stabilizes the lower oxidation state in the Mn^III/Mn^II couple and destabilizes the higher oxidation state in the Mn^III/Mn^IV couple. Variable temperature magnetic susceptibility measurements of 1 show a weak antiferromagnetic interaction. The magnetic behavior is satisfactorily modeled by inclusion of zero-field splitting and an intermolecular interaction component.     

The tetranuclear manganese complex of Photosystem II

A polynuclear manganese complex functions in Photosystem II both to accumulate oxidizing equivalents and to bind water and catalyze its four-electron oxidation. Recent electron paramagnetic resonance (EPR) spectroscopic studies of the manganese complex show that four manganese ions are required to account for its magnetic properties. The exchange couplings between manganese ions in the S₂ state are characteristic of a Mn₄O₄ cubane-like structure. Based on this structure for the manganese complex in the S₂ state, as well as a consideration of the known properties of the manganese complex in Photosystem II and the coordination chemistry of manganese, structures are proposed for the five intermediate oxidation states of the manganese complex. A molecular mechanism for the formation of an O-O bond and the displacement of O₂ from the S₄ state is suggested.     

Amorphous Manganese-Calcium Oxides as a Possible Evolutionary Origin for the CaMn<Subscript>4</Subscript> Cluster in Photosystem II

In this paper a few calcium-manganese oxides and calcium-manganese minerals are studied as catalysts for water oxidation. The natural mineral marokite is also studied as a catalyst for water oxidation for the first time. Marokite is made up of edge-sharing Mn³⁺ in a distorted octahedral environment and eight-coordinate Ca²⁺ centered polyhedral layers. The structure is similar to recent models of the oxygen evolving complex in photosystem II. Thus, the oxygen evolving complex in photosystem II does not have an unusual structure and could be synthesized hydrothermally. Also in this paper, oxygen evolution is studied with marokite (CaMn₂O₄), pyrolusite (MnO₂) and compared with hollandite (Ba_0.2Ca_0.15K_0.3Mn_6.9Al_0.2Si_0.3O₁₆), hausmannite (Mn₃O₄), Mn₂O₃.H₂O, CaMn₃O₆.H₂O, CaMn₄O₈.H₂O, CaMn₂O₄.H₂O and synthetic marokite (CaMn₂O₄). I propose that the origin of the oxygen evolving complex in photosystem II resulted from absorption of calcium and manganese ions that were precipitated together in the archean oceans by protocyanobacteria because of changing pH from ~5 to ~8-10. As reported in this paper, amorphous calcium-manganese oxides with different ratios of manganese and calcium are effective catalysts for water oxidation. The bond types and lengths of the calcium and manganese ions in the calcium-manganese oxides are directly comparable to those in the OEC. This primitive structure of these amorphous calcium-manganese compounds could be changed and modified by environmental groups (amino acids) to form the oxygen evolving complex in photosystem II.