Role of the 33-kDa polypeptide in preserving Mn in the photosynthetic oxygen-evolution system and its replacement by chloride ions

Treatment of Photosystem II particles from spinach chloroplasts with Triton X-100 with 2.6 M urea in the presence of 200 mM NaCl removed 3 polypeptides of 33 kDa, 24 kDa and 18 kDa, but left Mn bound to the particles. The (urea + NaCl)-treated particles could evolve oxygen in 200 mM, but not in 10 mM NaCl. Mn was gradually released with concomitant loss of oxygen-evolution activity in 10 mM NaCl but not in 200 mM Cl^?. The NaCl-treated particles, which contained Mn and the 33-kDa polypeptide but not the 24-kDa and 18-kDa polypeptides, did not lose Mn or oxygen-evolution activity in 10 mM NaCl. These observations suggest that the 33-kDa polypeptide maintains the binding of Mn to the oxygen-evolution system and can be functionally replaced by 200 mM Cl^?.     

Calcium ions can be substituted for the 24-kDa polypeptide in photosynthetic oxygen evolution

Photosystem II particles were prepared from spinach chloroplasts with Triton X-100, and treated with 1.0 M NaCl to remove polypeptides of 24 kDa and 18 kDa and to reduce the photosynthetic oxygen-evolution activity by about half. Oxygen-evolution activity was restored almost to the original level with 10 mM Ca²⁺, in a similar manner to the rebinding of 24-kDa polypeptide. Other cations such as magnesium, sodium and manganese ions could not restore any oxygen-evolution activity. These observations, together with a kinetic analysis, suggest that Ca²⁺ can be substituted for the 24-kDa polypeptide in photosynthetic oxygen evolution in Photosystem II particles.     

Partial degradation of the 18-kDa protein of the photosynthetic oxygen-evolving complex: A study of a binding site

When the NaCl extract from spinach Photosystem II particles was dialyzed against a low-salt medium, the 18-kDa protein slowly degraded to a fragment of 17 kDa. This observation suggests that a proteinase previously associated with the Photosystem II particles in a latent form was activated by dissociation with NaCl. The 18-kDa protein and the 17-kDa fragment were purified, and their N-terminal amino acid sequences and total amino acid compositions were determined. These results determined 44 amino acid residues at the N-terminal of the 18-kDa protein, and suggest that 12 amino acid residues (mostly hydrophobic) at the N-terminal were lost by the degradation. The 18-kDa protein could rebind to the NaCl-treated and 24-kDa protein-supplemented Photosystem II particles and sustain their oxygen-evolution activity in a low-Cl⁻ medium, whereas the 17-kDa fragment had lost these abilities. These observations suggest that the N-terminal region of the 18-kDa protein forms a domain which binds to Photosystem II particles.     

Partial reconstitution of the photosynthetic oxygen evolution system by rebinding of the 33-kDa polypeptide

Treatment with 2.6 M urea of the Photosystem II particles depleted of two polypeptides of 24 kDa and 18 kDa completely released a polypeptide of 33 kDa and eliminated the oxygen-evolution activity. The 33-kDa polypeptide rebound to the urea-treated particles and partially reactivated the oxygen evolution. A quantitative analysis of the rebinding suggests tha there is a specific binding site for the 33-kDa polypeptide on the membrane surface.     

Inhibition by ethylenediamine tetraacetate and restoration by Mn2+ and Ca2+ of oxygen-evolving activity in Photosystem II preparation from the thermophilic cyanobacterium,Synechococcus sp

The Photosystem II particles capable of evolving oxygen with ferricyanide as an electron acceptor were isolated from β-octylglucoside-solubilized thylakoid membranes of the thermophilic cyanobacterium Synechococcus sp. High and steady rates of oxygen evolution were observed only in the presence of 0.5% digitonin and 1 M sucrose. The activity was totally lost when the particles had been treated with 1 mM ethylenediamine tetraacetate for 1 min in a hypotonic medium. The treatment removed two out of four Mn atoms present per the Photosystem II reaction center in the particles. A significant rate of oxygen evolution was restored almost immediately after the addition of 5 mM MnCl₂ to the treated particles. The activity was also slowly and partially restored when the treated particles had been incubated with 5 mM CaCl₂. MgCl₂ was much less effective irrespective of the incubation time. The addition of MnCl₂ to the CaCl₂-restored particles increased the activity to a level which is significantly larger than the sum of the MnCl₂- and the CaCl₂-induced increases in the activity. The Mn- and Ca-effects were largely suppressed by the simultaneous addition of CaCl₂ and MnCl₂, respectively. It is concluded that both Mn²⁺ and Ca²⁺ are essential components of the water oxidation of photosynthesis, but the two cations support oxygen evolution through different mechanisms.     

Light-dependent inactivation of photosynthetic oxygen evolution during NaCl treatment of photosystem II particles: The role of the 24-kDa protein

Photosystem (PS) II particles prepared from spinach thylakoids with Triton X-100 were treated with 1.5 M NaCl either in the light or dark. Under both conditions, the 24-kDa and 18-kDa proteins were released from the particles, but rebound to them when the NaCl concentration was reduced to 34 mM by dilution. Oxygen evolution measured after the dilution was inactivated following NaCl treatment in the light, but not following treatment in the dark. The inactivation in the light was suppressed when 5 mM CaCl₂ was added during or after the NaCl treatment. Based on these observations, a scheme is proposed for the mechanism of light-dependent inactivation of oxygen evolution during NaCl treatment of PS II particles and for the function of the 24-kDa protein in regulating the conformation of a supposed Ca²⁺-binding intrinsic protein.Abbreviations Chl chlorophyll - EGTA ethyleneglycol-bis-(-aminoethyl ether)-N,N,N,N-tetraacetic acid - Mes 4-morpholineethanesulphonic acid - PS photosystem - SDS sodium dodecylsulphate     

Mn-preserving extraction of 33-, 24- and 16-kDa proteins from O2-evolving PS II particles by divalent salt-washing

Divalent salt-washing of O₂-evolving PS II particles caused total liberation of 33-, 24- and 16-kDa proteins, but the resulting PS II particles retained almost all amounts of Mn present in initial particles. The retained Mn was EPR-silent when the particles were kept in high concentrations of divalent salt. By divalent salt-washing, the activity of diphenylcarbazide (DPC) photooxidation was not affected at all, neither suppressed nor enhanced, while O₂ evolution was totally inactivated. These results indicate that Mn can be kept associated with PS II particles even after liberation of the 33-kDa protein, and suggest that the 33-kDa protein is probably not responsible for binding Mn onto membranes, but is possibly responsible for maintaining the function of Mn atoms in the O₂-evolving center.     

Effect of the 33-kDa protein on the S-state transitions in photosynthetic oxygen evolution

The effect of the extrinsic 33-kDa protein on the photosynthetic oxygen evolution was studied by comparing spinach Photosystem II particles depleted of the 33-kDa protein with those reconstituted with the protein. The light-intensity dependence of the oxygen-evolution activity under continuous illumination suggests that a dark step, but not a light step, in the oxygen-evolving reaction is accelerated by the 33-kDa protein. Consistently, the pattern of oxygen yield with a series of short saturating flashes, which showed a maximum on the third flash and a damped oscillation with a period of 4, was not much affected by the removal and rebinding of the 33-kDa protein, when the dark interval between the flashes was long enough, i.e., longer than 0.5 s. The millisecond kinetics of oxygen release after the third flash was retarded by the removal of the 33-kDa protein and stimulated by its rebinding, suggesting that the transition from S₃ to S₀ is accelerated by the 33-kDa protein. The stability of the S₂ and S₃ states in darkness was higher in the absence of the 33-kDa protein than its presence.     

Studies on the polypeptide composition of the cyanobacterial oxygen-evolving complex

Various approaches have been used to investigate the polypeptides required for oxygen evolution in cyanobacteria, in particular the thermophile Phormidium laminosum. Antibodies against the extrinsic 33 kDa protein from spinach Photosystem II cross-reacted clearly in immunoblotting experiments with a corresponding polypeptide in isolated thylakoids and Photosystem II particles from P. laminosum and with whole-cell homogenates of three species of cyanobacteria (Phormidium laminosum, Synechococcus leopoliensis and Anabaena variabilis). In contrast, no cyanobacterial proteins reacted with antibodies against the 23 and 16 kDa proteins of spinach Photosystem II. The lack of cross-reactivity and the absence of these polypeptides from highly active Photosystem II particles of Phormidium laminosum strongly suggest that cyanobacteria do not contain polypeptides corresponding to these two chloroplast proteins. Treatment of P. laminosum Photosystem II particles with 0.8 M alkaline Tris, 1 M NaCl, CaCl₂ or MgCl₂ inhibited O₂ evolution, and quantitatively removed a 9 kDa polypeptide from the particles. None of these treatments removed comparable amounts of the 33 kDa polypeptide, and only Tris treatment removed manganese. The release of the 9 kDa polypeptide upon NaCl treatment correlated well with the deactivation at the donor side of Photosystem II. A direct connection between the 33 kDa polypeptide and O₂ evolution was established by the finding that trypsin treatment digested this polypeptide and inhibited O₂ evolution in parallel.     

Evidence for an association between a 33 kDa extrinsic membrane protein,manganese and photosynthetic oxygen evolution. I. Correlation with the S2 multiline EPR signal

The removal of peripheral membrane proteins of a molecular mass of 17 and 23 kDa by washing of spinach Photosystem-II (PS II) membranes in 1 M salt between pH 4.5 and 6.5 produces a minimal loss of the S₁ → S₂ reaction, as seen by the multiline EPR signal for the S₂ state of the water-oxidizing complex, while reversibly inhibiting O₂ evolution. The multiline EPR signal simplifies from a ‘19-line’ spectrum to a ‘16-line’ spectrum, suggestive of partial uncoupling of a cluster of 3 or 4 to yield photo-oxidation of a binuclear Mn site. Alkaline salt washing progressively releases a 33 kDa peripheral protein between pH 6.5 and 9.5, in direct parallel with the loss of O₂ evolution and the S₂ multiline EPR signal. The 33 kDa protein can be partially removed (20%) at pH 8.0 prior to managanese release. Salt treatment releases four Mn ions between pH 8.0 and 9.5 with the first 2 or 3 Mn ions released cooperatively. A common binding site is thus suggested in agreement with earlier EPR spectroscopic data establishing a tetranuclear Mn site. At least two of these Mn ions bind directly at a site in the PS II complex for which photooxidation by the reaction center is controlled by the 33 kDa protein. The washing of PS II membranes with 1 M CaCl₂ to affect the release of the 33 kDa protein, while preserving Mn binding to the membrane (Ono, T.-A. and Inoue, Y. (1983) FEBS Lett. 164, 255–260), is found to leave some 33 kDa protein undissociated in proportion to the extent of O₂ evolution and S₂ multiline yield. These depleted membranes do not oxidize water or produce the normal S₂ state without the binding of the 33 kDa protein. A method for the accurate determination of relative concentrations of the peripheral membrane proteins using gel electrophoresis is presented.     

Isolation of an Mn-carrying 33-kDa protein from an oxygen-evolving photosystem-II preparation by phase partitioning with butanol

An Mn-containing 33-kDa protein was isolated by phase partitioning with 50% n-butanol from an O₂-evolving photosystem-II preparation. The Mn content in the 33-kDa protein increased when 1 mM potassium ferricyanide and 0.4 mM diaminodurene were present as oxidants during the butanol treatment and the following dialysis. Under these conditions, 0.1–0.25 atom Mn was detected in one 33-kDa protein molecule. EPR spectra of the Mn protein showed that the Mn atoms were bound to the protein.     

Stepwise Transition of the Tetra-Manganese Complex of Photosystem II to a Binuclear Mn2(μ-O)2 Complex in Response to a Temperature Jump: A Time-Resolved Structural Investigation Employing X-Ray Absorption Spectroscopy

In oxygenic photosynthesis, water is oxidized at a protein-cofactor complex comprising four Mn atoms and, presumably, one calcium. Using multilayers of Photosystem II membrane particles, we investigated the time course of the disassembly of the Mn complex initiated by a temperature jump from 25°C to 47°C and terminated by rapid cooling after distinct heating periods. We monitored polarographically the oxygen-evolution activity, the amount of the Y_D^ox radical and of released Mn²⁺ by EPR spectroscopy, and the structure of the Mn complex by x-ray absorption spectroscopy (XAS, EXAFS). Using a novel approach to analyze time-resolved EXAFS data, we identify three distinct phases of the disassembly process: (1) Loss of the oxygen-evolution activity and reduction of Y_D^ox occur simultaneously (k₁ = 1.0 min⁻¹). EXAFS spectra reveal the concomitant loss of an absorber-backscatterer interaction between heavy atoms separated by ~3.3 Å, possibly related to Ca release. (2) Subsequently, two Mn(III) or Mn(IV) ions seemingly separated by ~2.7 Å in the native complex are reduced to Mn(II) and released (k₂ = 0.18 min⁻¹). The x-ray absorption spectroscopy data is highly suggestive that the two unreleased Mn ions form a di-μ-oxo bridged Mn(III)₂ complex. (3) Finally, the tightly-bound Mn₂(μ-O)₂ unit is slowly reduced and released (k₃ = 0.014 min⁻¹).     

Properties of a peripheral 34 kDa protein in Synechococcus vulcanus Photosystem II particles. Its exchangeability with spinach 33 kDa protein in reconstitution of O2 evolution

Photosystem II (PS II) particles retaining a high rate of O₂ evolution were prepared from a thermophilic cyanobacterium, Synechococcus vulcanus Copeland, and the composition and properties of their peripheral proteins were investigated. The following results were obtained. (1) The O₂-evolving PS II particles of S. vulcanus contained only one peripheral protein with a molecular mass of 34000 which corresponded to the 33 kDa protein in higher plant PS II particles, but no other peripheral proteins corresponding to the 24 and 16 kDa proteins of higher plant PS II particles. (2) The cyanobacterial peripheral 34 kDa protein was removed from the particles by 1 M CaCl₂-washing concomitant with total inactivation of O₂ evolution, and the inactivated O₂ evolution was reconstituted to 75% of the original activity by rebinding of this protein back to the washed particles. (3) The cyanobacterial peripheral 34 kDa protein rebound to CaCl₂-washed spinach PS II particles and restored O₂ evolution to an appreciable extent (28%). (4) The spinach peripheral 33 kDa protein rebound to CaCl₂-washed PS II particles of S. vulcanus and partially restored O₂ evolution (60%). These results suggested that the peripheral 34 kDa protein of S. vulcanus possesses the determinants for both binding and activity reconstitution identical with those of the peripheral 33 kDa protein of spinach.     

Heat inactivation of oxygen evolution in Photosystem II particles and its acceleration by chloride depletion and exogenous manganese

Heat inactivation of oxygen evolution by isolated Photosystem II particles was accelerated by Cl⁻ depletion and exogenous Mn²⁺. Weak red light also accelerated heat inactivation. Heat treatment released the 33, 24 and 18 kDa proteins and Mn from the Photosystem II particles. The protein release was stimulated by Cl⁻ depletion and exogenous Mn²⁺, and the Mn release was also stimulated by Cl⁻ depletion. A 50% loss of Mn corresponded to full inactivation of oxygen evolution, whereas no direct correlation seemed to exist between the loss of any one protein and inactivation of oxygen evolution. Removal of the 24 and 18 kDa proteins from photosystem II particles only slightly decreased the heat stability of oxygen evolution.     

Manganese proteins isolated from spinach thylakoid membranes and their role in O2 evolution: II. A binuclear manganese-containing 34 kilodalton protein,a probable component of the water dehydrogenase enzyme

Extraction conditions have been found which result in the retention of managanese to the 33–34 kDa protein, first isolated as an apoprotein by Kuwabara and Murata (Kuwabara, T. and Murata, N. (1979) Biochim. Biophys Acta 581, 228–236). By maintaining an oxidizing-solution potential, with hydrophilic and lipophilic redox buffers during protein extraction of spinach grana-thylakoid membranes, the 33–34 kDa protein is observed to bind a maximum of 2 Mn/protein which are not released by extended dialysis versus buffer. This manganese is a part of the pool of 4 Mn/Photosystem II normally associated with the oxygen-evolving complex. The mechanism for retention of Mn to the protein during isolation appears to be by suppression of chemical reduction of natively bound, high-valent Mn to the labile Mn(II) oxidation state. This protein is also present in stoichiometric levels in highly active, O₂-evolving, detergent-extracted PS-II particles which contain 4–5 Mn/PS II. Conditions which result in the loss of Mn and O₂ evolution activity from functional membranes, such as incubation in 1.5 mM NH₂OH or in ascorbate plus dithionite, also release Mn from the protein. The protein exists as a monomer of 33 kDa by gel filtration and 34 kDa by gel electrophoresis, with an isoelectric point of 5.1 ± 0.1. The protein exhibits an EPR spectrum only below 12 K which extends over at least 2000 G centered at g = 2 consisting of non-uniformly separated hyperfine transitions with average splitting of 45–55 G. The magnitude of this splitting is nominally one-half the splitting observed in monomeric manganese complexes having O or N donor ligands. This is apparently due to electronic coupling of the two ⁵⁵Mn nuclei in a presumed binuclear site. Either a ferromagnetically coupled binuclear Mn₂(III,III) site or an antiferromagnetically coupled mixed-valence Mn₂(II,III) site are considered as possible oxidation states to account for the EPR spectrum. Qualitatively similar hyperfine structure splittings are observed in ferromagnetically coupled binuclear Mn complexes having even-spin ground states. The extreme temperature dependence suggests the population of low-lying excited spin states such as are present in weakly coupled dimers and higher clusters of Mn ions, or, possibly, from efficient spin relaxation such as occurs in the Mn(III) oxidation state. Either 1.5 mM NH₂OH or incubation with reducing agents abolishes the low temperature EPR signal and releases two Mn(II) ions to solution. This is consistent with the presence of Mn(III) in the isolated protein. The intrinsically unstable Mn₂(II,III) oxidation state observed in model compounds favors the assignment of the stable protein oxidation state to the Mn₂(III,III) formulation. This protein exhibits characteristics consistent with an identification with the long-sought Mn site for photosynthetic O₂ evolution. An EPR spectrum having qualitatively similar features is observable in dark-adapted intact, photosynthetic membranes (Dismukes, G.C., Abramowicz, D.A., Ferris, F.K., Mathur, P., Upadrashta, B. and Watnick, P. (1983) in The Oxygen-Evolving System of Plant Photosynthesis (Inoue, Y., ed.), pp. 145–158, Academic Press, Tokyo) and in detergent-extracted, O₂-evolving Photosystem-II particles (Abramowicz, D.A., Raab, T.K. and Dismukes, G.C. (1984) Proceedings of the Sixth International Congress on Photosynthesis (Sybesma, C., ed.), Vol. I, pp. 349–354, Martinus Nijhoff/Dr. W. Junk Publishers, The Hague, The Netherlands), thus establishing a direct link with the O₂ evolving complex.     

The Cl effect on photosynthetic oxygen evolution: interaction of Cl with 18-kDa, 24-kDa and 33-kDa proteins

The interaction of Cl⁻ with the extrinsic proteins of 18 kDa, 24 kDa and 33 kDa in the photosynthetic oxygen-evolution complex was studied by comparing spinach photosystem II particles of different protein compositions. The 33-kDa protein decreased the Cl⁻ concentration optimum for oxygen evolution from 150 to 30 mM, and the 24-kDa protein decreased it from 30 to 10 mM. The 18-kDa protein did not change the optimum Cl⁻ concentration, but sustained oxygen evolution at Cl⁻ concentrations lower than 3 mM. The presence of the 24-kDa and 18-kDa proteins, but not each protein alone, markedly suppressed inactivation of oxygen evolution at a very low Cl⁻ concentration and its restoration by readdition of Cl⁻.     

Reconstitution of photosynthetic charge accumulation and oxygen evolution in CaCl2-treated PS II particles: I: Establishment of a high recovery of O2 evolution and examination of the roles of the 17-, 23- and 34-kDa proteins,focusing on the effect of Cl− on O2 evolution

The reconstitution of high O₂ evolution in CaCl₂-treated PS II particles was achieved by the simultaneous addition of the 17-, 23- and 34-kDa proteins and total thylakoid lipids in the presence of 25% glycerol and 15 mM sodium cholate. The activity of the reconstituted membranes recovered to 85% of that of the non-depleted original PS II particles at the optimal condition. By means of this reconstitution method, evidence for the cooperation of the three proteins in the recovery of O₂ evolution in the CaCl₂-treated PS II particles was found by changing the concentration of NaCI in the assay medium, and the relationship between the amount of manganese retained in the water-splitting complex and the O₂ evolving activity was examined by using the partially solubilized PS II particles with n-octyl-β-D-glucoside.     

Reconstitution of photosynthetic charge accumulation and oxygen evolution in CaCl2-treated PS II particles: II: EPR evidence for reactivation of the S1 → S2 transition in CaCl2-treated PS II particles with the 17-, 23-, and 34-kDa proteins

Extraction of PS II particles with 1 M CaCl₂ caused complete disappearance of the light-induced signal of the possible Kok S₂ state of the water-splitting complex and total loss of the O₂, evolving activity, concomitant with perfect removal of the 17-, 23- and 34-kDa proteins from the particles. The recovery of the multiline signal in the CaCl₂-treated PS II was performed by reinserting the 34-kDa protein, when CI^? was present in the solution for the EPR measurement. However, in the absence of Cl^?, besides the 34-kDa protein, the 17- and 23-kDa proteins were required for the recovery of the signal. These results are compared with the results on the recovery of the O₂, evolution in the reconstituted PS II to examine the role of these three proteins on the water splitting.     

Cooperation of Photosynthetic Reaction Center of Photosystem II under Weak Light as Shown by Light Intensity-dependence of the Half-effective Dose of Atrazine

The binding constant (K) and number of binding sites (N) of atrazine to isolated photosystem (PS) II membranes were measured with an apparent correlation between N and the activity of oxygen evolution. Upon the addition of an electron acceptor, N became equal to the total number of the population of PS II reaction centers irrespective of having oxygen-evolving activity, about 4 mmol per mole of chlorophyll, with a concomitant decline of K from 1.32 (±0.34) × 10⁷ M^–1 to 4.09 (±0.40) × 10⁶ M^–1 . NH₂OH and NaCl treatments, which inactivate oxygen evolution, affected neither the binding to PS II membranes of the extrinsic 33-kDa protein or of atrazine. The atrazine binding sites that are latent in CaCl₂-treated PS II membranes was partially restored by the reconstitution of the membranes with isolated extrinsic 33-kDa protein. An oxidizing system involving the 33-kDa protein may provide a suitable structure of PS II reaction center complex for atrazine binding. The level of inhibition of oxygen-evolving activity by atrazine under the saturating intensity of light parallels the fraction of the photosystem (PS) II reaction center with the quinone-binding site blocked by atrazine. In contrast, under a rate-limiting intensity of light, percents of remaining oxygen-evolving activity after the addition of atrazine correlated with the 1.33th power of the fraction of atrazine-free binding sites. Inhibition of PS II complexes more than one that bound with atrazine suggests a cooperation between PS II complexes to evolve oxygen under weak light intensity.     

Purification and properties of an oxygen-evolving Photosystem II reaction-center complex from spinach

A chlorophyll-protein complex, capable of photochemical water oxidation and consisting of only one extrinsic protein of 33 kDa in addition to six intrinsic proteins of the Photosystem II reaction center, has been isolated from spinach thylakoids by digitonin extraction, performed at pH 6.0, followed by chromatographic separations using DEAE-Toyopearl 650S as described briefly (Tang, X.S. and Satoh, K. (1985) FEBS Lett. 179, 60–64). The protein complex contained approx. 3–4 manganese atoms, 2 mol plastoquinone-9 and 2 mol low-potential forms of cytochrome b-559 heme per mol of the photoactive primary acceptor, Q_A. The oxygen evolution of the complex was highly stimulated by the presence of CaCl₂ and stabilized by glycerol; the typical rate of 400–500 μmol O₂ per mg Chl per h was attained with 2,5-dichlorobenzoquinone and potassium ferricyanide as electron acceptors in the presence of 50 mM CaCl₂. The protein complex exhibited a dark-stable EPR Signal II; the microwave power saturation profile of the signal was almost identical with that of oxygen-evolving membrane preparations. The multiline EPR signal ascribable to Kok's S₂-state was elicited in this protein complex by illumination at 200 K, as in membrane preparations. These results indicate that the basic machinery of photosynthetic water oxidation is preserved in an almost intact state in the isolated chlorophyll-protein complex.