The function of 33-kDa protein in the photosynthetic oxygen-evolution system studied by reconstitution experiments

Treatment of Photosystem II particles with 1.2 M CaCl₂ released three proteins of 33, 24 and 18 kDa of the photosynthetic oxygen evolution system, but left Mn bound to the particles as demonstrated by Ono and Inoue (Ono, T. and Inoue, Y. (1983) FEBS Lett. 164, 252–260). Oxygen-evolution activity of the CaCl₂-treated particles was very low in a medium containing 10 mM NaCl as a salt, but could be restored by the 33-kDa protein. When the particles were incubated in 10 mM NaCl at 0°C, two of the four Mn atoms per oxygen-evolution system were released with concomitant loss of oxygen-evolution activity. The 33-kDa protein suppressed the release of Mn and the inactivation during the incubation. These findings from reconstitution experiments suggest that the 33-kDa protein acts to preserve Mn atoms in the oxygen-evolution system. The 33-kDa protein could be partially substituted by 100 or 150 mM Cl⁻ for the preservation of the Mn and oxygen-evolution activity. The Mn in Photosystem II particles enhanced rebinding of the 33-kDa protein to the particles.     

Specific loss of the extrinsic 18 KDa protein from Photosystem II upon heating to 47 °C causes inactivation of oxygen evolution likely due to Ca release from the Mn-complex

Exposure of Photosystem II (PS II) membrane particles from spinach to a temperature of 47 °C caused the rapid release of the 18 kDa protein in parallel to inactivation of oxygen evolution. Previously, it has been suggested that the first heat-jump response involves rapid Ca release from the Mn complex of O₂-evolution, followed by the slower release of (2 + 2) Mn^II ions [Pospisil P et al. (2003) Biophys J 84: 1370–1386]. Here, the predicted biphasic Mn^II release to the bulk was verified by atomic absorption spectroscopy (AAS). Analysis of laser flash-induced delayed fluorescence transients suggests that the loss of the essential Ca ion from the Mn₄Ca complex in the dark is due to the loss of the 18 kDa protein. The S₂-state multiline EPR signal of the Mn complex was still generated in heat-treated PS II presumably lacking Ca, but retaining four Mn ions.Dedicated to Professor Norio Murata on the occasion of his retirement     

The high-affinity binding site for manganese on the oxidizing side of Photosystem II

Electron donation to Photosystem II (PS II) by diphenylcarbazide (DPC) is interrupted by the presence of endogenous Mn in PS II particles. Removal of this Mn by Tris treatment greatly stimulates the electron transport with DPC as donor. Binding of low concentration of exogenous Mn(II) to Tris-treated PS II particles inhibits DPC photooxidation competitively with DPC. This phenomenon was used to locate a highly specific Mn(II) binding site on the oxidizing side of Photosystem II with dissociation constant about 0.15 μM. The binding of Mn(II) is electrostatic in nature. Its affinity depends not only on the ionic strength, but also on the anion species of the salt in the medium. The effectiveness in decreasing the affinity follows the order F⁻ > SO²⁻₄ > CH₃COO⁻ > CI⁻ > Br⁻ > NO₃⁻. This observation is interpreted as follows: smaller ions, like F⁻, CH₃COO⁻, and larger ions, like SO²⁻₄, have inhibitory effects on Mn(II) binding, whereas ions with optimal size, like Cl⁻, Br⁻ and NO₃⁻, can stabilize the binding, resembling the anion requirement for reactivation of Cl⁻-depleted chloroplasts. We suggest that the binding site for Mn(II) we observed is the site for the endogenous Mn in the O₂-evolving complex of PS II. This site remains after Tris treatment, which removes all the endogenous Mn as well as the three extrinsic proteins, indicating that it is on the intrinsic component(s) of PS II reaction centers. Furthermore, the Cl⁻ requirement for O₂ evolution may be attributed, at least partly to its stabilizing effect on Mn binding.     

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^?.     

The state of manganese in the photosynthetic apparatus: 5. The chloride effect in photosynthetic oxygen evolution. Is halide coordinated to the EPR-active manganese in the O2-evolving complex? Studies of the substructure of the low-temperature multiline EPR signal

The role of chloride in the manganese-containing oxygen-evolving complex of Photosystem II has been studied by observing the amplitude of the multiline EPR signal as a function of Cl⁻ concentration or when Cl⁻ is replaced by Br⁻ or F⁻. The correlation of the multiline EPR signal intensity and O₂ activity with the concentration of Cl⁻ shows that chloride is involved in oxygen evolution at the S₂ or earlier S states, and that it is necessary for the production of an EPR-detectable S₂ state. We have developed a new method for the preparation of subchloroplast PS II particles containing Br⁻ and F⁻) and have used these particles for studying the EPR fine structure at high resolution. The fine structure shows a multiplet of 4–6 lines with 10–15 G spacing; at the resolution of our experiment there are no significant differences between the Cl⁻-and Br⁻-containing samples, suggesting that the halide is not a ligand of the EPR-active Mn. Various structural possibilities for the Mn complex, which would account for the observed fine structure of the multiline EPR spectrum are discussed.     

The association of functional anions with the oxygen-evolving center of chloroplasts

The association of the site of photosynthetic water oxidation with Cl⁻ and other activating anions was analyzed with Photosystem II-enriched thylakoid particles prepared by Triton X-100 treatment. On the basis of the experimental evidence it is proposed that, regardless of the presence of the extrinsic 18 and 23 kDa polypeptides, the reactivation of Cl⁻-depleted particles by added anions is contingent upon the protonation of membrane-bound buffering groups with an apparent pK_a of approx. 6. The rate of dissociation of the anion from the site of water oxidation followed the order NO₃⁻ . ClO₄⁻ . Br⁻ ≈ Cl⁻. A model is developed that takes into account the known requirement of more than 1 anion/center for maximum activity. It assumes a finite and anion-dependent capacity of the water-oxidizing site for the activating anions, and that the rate of photosynthetic oxygen evolution is proportional to the number of anions at the water-oxidizing enzyme. In accord with suggestions made earlier, and in agreement with their further elaboration by Coleman and Govindjee (Proc. 16th FEBS Congress, Moscow, VNU Science Press, Utrecht), it is proposed that the Cl⁻ requirement of Photosystem II is linked to protonation-deprotonation events associated with photosynthetic water oxidation.     

The effect of chloride on the thermal inactivation of oxygen evolution

The effect of Cl depletion on the sensitivity of the oxygen-evolving complex of Photosystem II (PS II) to heat treatment was examined by a parallel study of the Hill activity (H₂O2,6-dichlorophenolindophenol), Cl^- binding (by ³⁵Cl-NMR) and Mn release (by EPR). The extent of thermal inactivation in spinach thylakoids was found to depend on the degree of Cl^- depletion in the sample. In partially Cl^--depleted thylakoids, mild heating (38°C, 3 min) was found to eliminate inflections in plots of both Hill activity versus [Cl^-] (at low light intensity) and excess ³⁵Cl-NMR linewidth versus [Cl^-] (in the dark). In PS II membranes, the same treatment reduced the differences between the linewidth maxima and minima, particularly in the region of 0.3 mM and 7.0 mM Cl^-, as compared to unheated membranes. These results indicate that mild heating affects the Cl^--binding domains within the oxygen-evolving complex, OEC, EPR measurements of the temperature dependence of Mn release from heated thylakoids show that Mn release begins to correlate with the loss of Hill activity only at higher temperatures, where the OEC is already substantially inactivated. We conclude from these studies that the Cl^--binding domains of the OEC constitute a principal site of damage by heat treatment.     

Stability and oscillation properties of thermoluminescent charge pairs in the O2-evolving system depleted of Cl− or the 33 kDa extrinsic protein

The effects of Cl⁻ depletion and removal of the 33 kDa extrinsic protein on the charge stabilization in O₂-evolving Photosystem II (PS II) particles were studied by curve fitting and deconvolution of thermoluminescence bands. The following results were obtained. (1) Cl⁻ depletion reversibly decreases the redox potential of the S₂ state by 60–80 mV, and thereby elevates the recombination temperature of both S₂Q⁻_B and S₂Q⁻_A charge pairs. (2) Removal of the 33 kDa extrinsic protein specifically elevates the recombination temperature of the S₂Q⁻_A charge pair, with practically no effect on the S₂Q⁻_B pair. This was tentatively interpreted as showing that the protein removal decreases the redox potential of both S₂ and Q⁻_B, but not of Q⁻_A, and, thus, the effects are mutually cancelled for the S₂Q⁻_B pair, but are manifested for the S₂Q⁻_A pair. (3) Deconvolution of glow curves demonstrated that S₃ is not formed in Cl⁻-depleted PS II, but is formed in 33 kDa protein-depleted PS II even at a low (20 mM) Cl⁻ concentration. Analysis of thermoluminescence oscillations confirmed that Cl⁻ depletion interrupts S₂-S₃ transition, whereas the protein removal interrupts S₃-(S₄)-S₀ transition at mM Cl⁻. (4) Cl⁻ depletion by SO²⁻₄ replacement in the absence of 33 kDa protein affected thermoluminescence in a different way from that in the presence of the protein. Based on these findings, the properties of charge pairs in the Cl⁻-depleted PS II particles were discussed in relation to the role of the 33 kDa extrinsic protein.     

Characterization of inhibitory effects of NH2OH and its N-methyl derivatives on the O2-evolving complex of Photosystem II

Inorganic cofactors (Mn, Ca²⁺ and Cl^-) are essential for oxidation of H₂O to O₂ by Photosystem II. The Mn reductants NH₂OH and its N-methyl derivatives have been employed as probes to further examine the interactions between these species and Mn at the active site of H₂O oxidation. Results of these studies show that the size of a hydroxylamine derivative regulates its ability to inactivate O₂ evolution activity, and that this size-dependent inhibition behavior arises from the protein structure of Photosystem II. A set of anions (Cl^-, F^- and SO₄ ^2-) is able to slow NH₂OH and CH₃NHOH inactivation of intact Photosystem II membranes by exerting a stabilizing influence on the extrinsic 23 and 17 kDa polypeptides. In contrast to this non-specific anion effect, only Cl^- is capable of attenuating CH₃NHOH and (CH₃)₂NOH inhibition in salt-washed preparations lacking the 23 and 17 kDa polypeptides. However, Cl^- fails to protect against NH₂OH inhibition in salt-washed membranes. These results indicate that the attack by NH₂OH and its N-methyl derivatives on Mn occurs at different sites in the O₂-evolving complex. The small reductant NH₂OH acts at a Cl^--insensitive site whereas the inhibitions by CH₃NHOH and (CH₃)₂NOH involve a site that is Cl^- sensitive. These findings are consistent with earlier studies showing that the size of primary amines controls the Cl^- sensitivity of their binding to Mn in the O₂-evolving complex.Abbreviation MES 4-morpholinoethanesulfonic acid - PS II Photosystem II     

The 16 and 23 kDa extrinsic polypeptides and the associated Ca2+ and Cl- modify atrazine interaction with the photosystem II core complex

The oxygen evolving complex of photosystem II (PS II) contains three extrinsic polypeptides of approximate molecular weights 16, 23 and 33 kDa. These polypeptides are associated with the roles of Cl^-, Ca²⁺ and Mn²⁺ in oxygen evolution. We have shown that selective removal of 16 and 23 kDa polypeptides from the above complex by NaCl washing of PS II enriched membrane fragments renders the PS II core complex more susceptible to the herbicide atrazine. On the other hand, when both native and depleted preparations were resupplied with exogenous Ca²⁺ and Cl^-, we obtained a reduction of atrazine inhibition which was much stronger in the depleted preparations than in the native ones. It is concluded that removal of 16 and 23 kDa polypeptides in general, and disorganization of associated Ca²⁺ and Cl^- in particular, enhances atrazine penetration to its sites of action in the vicinity of the PS II complex. The above could be interpreted if we assume a reduced plastoquinone affinity at the Q_B (secondary plastoquinone electron acceptor) pocket of D1 polypeptide following transmembranous modifications caused by the depletion of these polypeptides.Abbreviations CCCP carbonylcyanide-m-chlorophenylhydrazone - Chl chlorophyll - DCIP 2,6-dichlorophenolindophenol - MES 2-(N-morpholino)ethanesulfonic acid - PMSF phenylmethylsul-phonyfluoride - PS II photosystem II - PAGE polyacrilamide gel electrophoresis     

Differential response of chloride binding sites to elevated temperature: a comparative study in spinach thylakoids and PSII-enriched membranes

A study of heat effects was performed in thylakoids and photosystem II (PSII)-enriched membranes isolated from spinach in relation to Cl⁻-induced activation of PSII catalyzed oxygen evolution and the retention of Cl⁻ in the PSII complex. For this, Cl⁻-sufficient membranes and low-Cl⁻ membranes were used. The presence of Cl⁻ in the reaction medium did accelerate oxygen evolution, which remained unaffected by heat treatment up to 40°C in PSII membranes and up to 42.5°C in thylakoids. Heat resistance of Cl⁻-induced activation of oxygen evolution was found to be independent of the presence of ‘bound Cl⁻’ in the preparations. However, the functional stability of the PSII complex during heat treatment showed a marked dependence on the presence of bound Cl⁻ in PSII. Electron paramagnetic resonance study of manganese (Mn) release per reaction center/Y_D⁺ showed that there was little loss of Mn²⁺ up to 42°C in our preparations, although the PSII activity was significantly lowered. These observations together with data from steady state chlorophyll a fluorescence imply that the site of action of Cl⁻ causing direct activation of oxygen evolution was different from the site of primary heat damage. A differential response of chloride binding sites to heat stress was observed. The high-affinity (tightly bound, slow exchanging) site of chloride is affected earlier (∼37°C) while low-affinity (loosely bound, fast exchanging) site gets affected at higher temperatures (42.5°C in thylakoids and 40°C in the case of PSII-enriched membranes). Prasanna Mohanty is an INSA Honorary Scientist and Professor on Courtesy, DAVV, Indore.     

The release of polypeptides and manganese from oxygen-evolving photosystem II preparations following zinc-treatment

Inhibition of oxygen evolution in photosystem II membrane fragments from pea chloroplasts by washing with Zn₂₊ causes appearance of the EPR signal of Mn(H₂O)₆²⁺. This Mn²⁺ remains associated with the membrane fraction. Release of Mn²⁺ into the medium was correlated with the amount of the 23 kDa protein removed from the membrane. This suggests that this protein may function as a ‘gate’ to an aqueous compartment into which Mn²⁺ is released. Inhibition by Zn²⁺ correlated with the release of 1 Mn²⁺ per reaction centre, out of a total stoichiometry of 4 Mn atoms per reaction centre. By comparing the release of Mn following Zn-treatment of NaCI or CaC1₂ washed membranes, it is concluded that the 33 kDa protein is involved in binding of 2 Mn.     

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.     

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.     

Reactivation of oxygen evolution of NaCl-washed Photosystem-II particles by Ca2+ and/or the 24 kDa protein

We have studied the conditions required to reactivate oxygen evolution in NaCl-washed Photosystem-II particles. Restoration of oxygen evolution by Ca²⁺ revealed an heterogeneity in these Photosystem-II particles: 30% possess a low affinity site for Ca²⁺ (1–2 mM), 70% a high affinity site for Ca²⁺ (50–100 μM), even in the absence of the 24 kDa protein. The sole effect of the 24 kDa protein added back to Photosystem-II particles shortly before illumination was to stabilize oxygen evolution. Added back more than half an hour before, to Photosystem II particles at a high chlorophyll concentration, it increased oxygen evolution from approx. 40% of the control to 60–70% of the control. After reconstitution, an appreciable fraction of the low-affinity site for Ca²⁺ was still present.     

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.     

Molecular organization of oxygen-evolution system in chloroplast

The main function of Photosystem II in chloroplast is to oxidize water molecules to produce oxygen. Strong oxidant produced by photoreaction at Photosystem II reaction center derives electrons from water and the electrons are transferred via Photosystem I to NADP⁺. The components required for water oxidation in Photosystem II were identified and their molecular properties as well as their roles in the oxygen evolution process were elucidated. The entity of the oxygen evolution system is a supramolecular complex of Photosystem II in the thylakoid membrane where reaction center binding polypeptides, three extrinsic polypeptides, managenese atoms, Ca²⁺ and Cl⁻ ions are the essential components, and they constitute a specific catalytic domain for water oxidation. Recipient of the Botanical Society Award for Young Scientists, 1988.     

Disorganization of the Mn4Ca complex of photosystem II by ruthenium red: a thermoluminescence study

Ruthenium red (RR) is known to be an inhibitor that binds to Ca²⁺ sites. It releases Ca²⁺ and Cl^? together with the extrinsic polypeptide of 17 kDa associated with the oxygen evolving complex of photosystem II. In this work we used thermoluminescence to study S_2/3Q_B^? and S₂Q_A^? charge recombination. It is shown that RR produced a deeper inhibition of oxygen evolution compared with the effect of extrinsic polypeptide or Ca²⁺/Cl^? depletion. Even though Mn is not released, the Mn cluster is disorganized by RR and the S₁ → S₂ transition is inhibited. Copyright © 2008 John Wiley & Sons, Ltd.     

Studies of the slowly exchanging chloride in Photosystem II of higher plants

³⁶Cl^- was used to study the slow exchange of chloride at a binding site associated with Photosystem II (PS II). When PS II membranes were labeled with different concentrations of ³⁶Cl^-, saturation of binding at about I chloride/PS II was observed. The rate of binding showed a clear dependence on the concentration of chloride approaching a limiting value of about 3·10^-4 s^-1 at high concentrations, similar to the rate of release of chloride from labeled membranes. These rates were close to that found earlier for the release of chloride from PS II membranes isolated from spinach grown on ³⁶Cl^-, which suggests that we are observing the same site for chloride binding. The similarity between the limiting rate of binding and the rate of release of chloride suggests that the exchange of chloride with the surrounding medium is controlled by an intramolecular process. The binding of chloride showed a pH-dependence with an apparent pK_a of 7.5 and was very sensitive to the presence of the extrinsic polypeptides at the PS II donor side. The binding of chloride was competitively inhibited by a few other anions, notably Br^- and NO₃ ^-. The slowly exchanging Cl^- did not show any significant correlation with oxygen evolution rate or yield of EPR signals from the S₂ state. Our studies indicate that removal of the slowly exchanging chloride lowers the stability of PS II as indicated by the loss of oxygen evolution activity and S₂ state EPR signals.Abbreviations Chl chlorophyll - EPR electron paramagnetic resonance - Hepes 4-(2-hydroxyethyl)-1-piperazineethanesulfonic acid - Mes 4-morpholineethanesulfonic acid - MWCO molecular weight cut off - PPBQ phenyl-p-benzoquinone - PS II Photosystem II     

Ca2+ and Mg2+-binding and a putative calmodulin type Ca2+-binding site in Synechococcus Photosystem II

Thylakoids and Photosystem II particles prepared from the cyanobacterium Synechococcus PCC 7942 washed with a HEPES/glycerol buffer exhibited low rates of light-induced oxygen evolution. Addition of either Ca²⁺ or Mg²⁺ to both thylakoids and Photosystem II particles increased oxygen evolution independently, maximal rates being obtained by addition of both ions. If either preparation was washed with NaCl, light induced O₂ evolution was completely inhibited, but re-activated in the same manner by Ca²⁺ and Mg²⁺ but to a lower level. In the presence of Mg²⁺, the reactivation of O₂ evolution by Ca²⁺ allowed sigmoid kinetics, implying co-operative binding. The results are interpreted as indicating that not only Ca²⁺, but also Mg²⁺, is essential for light-induced oxygen evolution in thylakoids and Photosystem II particles from Synechococcus PC 7942. The significance of the reactivation kinetics is discussed. Reactivation by Ca²⁺ was inhibited by antibodies to mammalian calmodulin, indicating that the binding site in Photosystem II may be analogous to that of this protein.Abbreviation HEPES n-2-Hydroxyethylpiperazine--2-ethane sulphonic acid