Physiologically active chloroplasts contain pools of unassembled extrinsic proteins of the photosynthetic oxygen-evolving enzyme complex in the thylakoid lumen

The oxygen-evolving complex (OEC) of photosystem II (PS II) consists of at least three extrinsic membrane-associated protein subunits, OE33, OE23, and OE17, with associated Mn2+, Ca2+, and Cl- ions. These subunits are bound to the lumen side of PS II core proteins embedded in the thylakoid membrane. Our experiments reveal that a significant fraction of each subunit is normally present in unassembled pools within the thylakoid lumen. This conclusion was supported by immunological detection of free subunits after freshly isolated pea thylakoids were fractionated with low levels of Triton X-100. Plastocyanin, a soluble lumen protein, was completely released from the lumen by 0.04% Triton X-100. This gentle detergent treatment also caused the release from the thylakoids of between 10 and 20%, 40 and 60%, and 15 and 50% of OE33, OE23, and OE17, respectively. Measurements of the rates of oxygen evolution from Triton-treated thylakoids, both in the presence and absence of Ca2+, and before and after incubation with hydroquinone, demonstrated that the OEC was not dissociated by the detergent treatment. Thylakoids isolated from spinach released similar amounts of extrinsic proteins after Triton treatment. These data demonstrate that physiologically active chloroplasts contain significant pools of unassembled extrinsic OEC polypeptide subunits free in the lumen of the thylakoids.     

Distribution of the extrinsic proteins as a potential marker for the evolution of photosynthetic oxygen-evolving photosystem II

Distribution of photosystem II (PSII) extrinsic proteins was examined using antibodies raised against various extrinsic proteins from different sources. The results showed that a glaucophyte (Cyanophora paradoxa) having the most primitive plastids contained the cyanobacterial-type extrinsic proteins (PsbO, PsbV, PsbU), and the primitive red algae (Cyanidium caldarium) contained the red algal-type extrinsic proteins (PsO, PsbQ', PsbV, PsbU), whereas a prasinophyte (Pyraminonas parkeae), which is one of the most primitive green algae, contained the green algal-type ones (PsbO, PsbP, PsbQ). These suggest that the extrinsic proteins had been diverged into cyanobacterial-, red algal- and green algal-types during early phases of evolution after a primary endosymbiosis. This study also showed that a haptophyte, diatoms and brown algae, which resulted from red algal secondary endosymbiosis, contained the red algal-type, whereas Euglena gracilis resulted from green algal secondary endosymbiosis contained the green algal-type extrinsic proteins, suggesting that the red algal- and green algal-type extrinsic proteins have been retained unchanged in the different lines of organisms following the secondary endosymbiosis. Based on these immunological analyses, together with the current genome data, the evolution of photosynthetic oxygen-evolving PSII was discussed from a view of distribution of the extrinsic proteins, and a new model for the evolution of the PSII extrinsic proteins was proposed.     

Manganese-binding proteins of the oxygen-evolving complex

The extrinsic 33-kDa protein (P33) was cross-linked covalently to the binding site on P33-depleted PSII preparations which is responsible for reconstitution of photosynthetic water oxidation after PSII preparations have been washed with 1 M CaCl2. Conditions were found in which more than half of the cross-linked protein complexes formed in the PSII preparations retained the ability to catalyze the oxidation of water. The complex is composed of the P33 cross-linked to the D1 and D2 proteins and a 34-kDa protein, which is present in lower abundance than the other three proteins. After solubilization of the membranes with SDS and purification by preparative SDS-PAGE, the complex retains bound manganese and can catalyze the conversion of H2O2 to O2. Calcium and chloride increased the catalase activity of the purified cross-linked complex while lanthanum or hydroxylamine abolished the activity. By use of the specific activity of the H2O2-dependent reaction to follow the extent of purification of the cross-linked complex, the most highly purified complex was determined to contain 0.34 microgram of manganese/180 micrograms of protein. The mole ratio of Mn/protein was calculated to range from 3.6 to 4.5 depending on the assumed stoichiometry of the protein subunits. The results presented here provide direct evidence that one or more of the three proteins that have cross-linked to the P33 are responsible for binding the manganese of the oxygen-evolving complex.     

Structure and evolution of the extrinsic proteins that stabilize the oxygen-evolving engine.

PsbO, PsbP and PsbQ are the extrinsic proteins associated with the oxygen-evolving (OE) engine of all known higher plants. However their presence is not constant throughout all known oxy-photosynthetic organisms. For this reason, comparative analyses of the sequence and the structure of these proteins in different species from prokaryotes to eukaryotes may allow unravelling of the evolutionary track that they have followed and infer new hints about their function in the OE complex. The results show that PsbP and PsbQ present different evolutionary profiles, and that PsbQ is more closely associated to PsbO and probably to the manganese stabilizing role assigned to this protein.     

Effects of Photosystem II extrinsic proteins on microstructure of the oxygen-evolving complex and its reactivity to water analogs

We used Triton-prepared PS II membranes in studies of the inactivation of O₂ evolution and solubilization of Mn and specific PS II polypeptides by NH₂OH, N- and O-substituted NH₂OH derivatives, NH₂NH₂ and NH₄Cl. The inactivation of O₂-evolution, solubilization of Mn and the solubilization of the extrinsic PS II polypeptides (17, 23 and 33 kDa) proved closely correlated, half-maximal effects occurring with only 100 μM NH₂OH. NH₂OH (2 mM) and NaCl (1 M) extractions solubilized about one-half the amount of protein solubilized by 0.8 M Tris-HCl (pH 8.0). The inactivation of the Mn-S-state complex proceeded by apparent first-order kinetics, the rate constant dependent on NH₂OH (CH₃NHON) concentration and pH. In the range of micromolar concentrations of NH₂OH, this inactivation did not occur via a cooperative type mechanism. Depletion of the 17 and 23 kDa proteins modified the pH dependency of inactivation (from pH 7.8 to 6.5) and also resulted in an approx. 2-fold maximum increase in the inactivation rate constant. Significantly, reconstitution of such NaCl-TMF-2 membranes with the 17 and 23 kDa proteins reverted both the pH dependency and the inactivation rate constant to that of TMF-2. A hierarchy of effectivity for solubilization of Mn and protein, which was highly correlated with inactivation of the Mn-S-state enzyme, was observed among NH₂OH and its derivatives. This same hierarchy was observed irrespective of prior depletion of the 17 and 23 or the 17, 23 and 33 kDa proteins from TMF-2. The hierarchy of effectivity among derivatives was: NH₂OH > CH₃NHOH > NH₂NH₂, NH₂OSO₃ > NH₂OCH₃ ⪢ CH₃NHOCH₃, NH₄Cl. The function(s) of the extrinsic PS II proteins as determinants of the reactivity of the Mn-S-state complex with polar amine vs other type compounds is discussed.     

Stoichiometric association of extrinsic cytochrome c550 and 12 kDa protein with a highly purified oxygen-evolving photosystem II core complex from Synechococcus vulcanus.

A highly purified, native photosystem II (PS II) core complex was isolated from thylakoids of Synechococcus vulcanus, a thermophilic cyanobacterium by lauryldimethylamine N-oxide (LDAO) and dodecyl beta-D-maltoside solubilization. This native PS II core complex contained, in addition to the proteins that have been well characterized in the core complex previously purified by LDAO and Triton X-100, two more extrinsic proteins with apparent molecular weights of 17 and 12 kDa. These two proteins were associated with the core complex in stoichiometric amounts and could be released by treatment with 1 M CaCl2 or 1 M alkaline Tris but not by 2 M NaCl or low-glycerol treatment, indicating that they are the real components of PS II of this cyanobacterium. N-Terminal sequencing revealed that the 17 and 12 kDa proteins correspond to the apoprotein of cytochrome c550, a low potential c-type cytochrome, and the 9 kDa extrinsic protein previously found in a partially purified PS II preparation from Phormidium laminosum, respectively. In spite of retention of these two extrinsic proteins, no homologues of higher plant 23 and 17 kDa extrinsic proteins could be detected in this cyanobacterial PS II core complex.     

Comparison of photosynthetic performances of marine picocyanobacteria with different configurations of the oxygen-evolving complex

The extrinsic PsbU and PsbV proteins are known to play a critical role in stabilizing the Mn₄CaO₅ cluster of the PSII oxygen-evolving complex (OEC). However, most isolates of the marine cyanobacterium Prochlorococcus naturally miss these proteins, even though they have kept the main OEC protein, PsbO. A structural homology model of the PSII of such a natural deletion mutant strain (P. marinus MED4) did not reveal any obvious compensation mechanism for this lack. To assess the physiological consequences of this unusual OEC, we compared oxygen evolution between Prochlorococcus strains missing psbU and psbV (PCC 9511 and SS120) and two marine strains possessing these genes (Prochlorococcus sp. MIT9313 and Synechococcus sp. WH7803). While the low light-adapted strain SS120 exhibited the lowest maximal O₂ evolution rates (P_max per divinyl-chlorophyll a, per cell or per photosystem II) of all four strains, the high light-adapted strain PCC 9511 displayed even higher P^Chl_max and P^PSII_max at high irradiance than Synechococcus sp. WH7803. Furthermore, thermoluminescence glow curves did not show any alteration in the B-band shape or peak position that could be related to the lack of these extrinsic proteins. This suggests an efficient functional adaptation of the OEC in these natural deletion mutants, in which PsbO alone is seemingly sufficient to ensure proper oxygen evolution. Our study also showed that Prochlorococcus strains exhibit negative net O₂ evolution rates at the low irradiances encountered in minimum oxygen zones, possibly explaining the very low O₂ concentrations measured in these environments, where Prochlorococcus is the dominant oxyphototroph.     

Structural characterization of photosystem II complex from red alga Porphyridium cruentum retaining extrinsic subunits of the oxygen-evolving complex.

The structure of photosystem II (PSII) complex isolated from thylakoid membranes of the red alga Porphyridium cruentum was investigated using electron microscopy followed by single particle image analysis. The dimeric complexes observed contain all major PSII subunits (CP47, CP43, D1 and D2 proteins) as well as the extrinsic proteins (33 kDa, 12 kDa and the cytochrome c(550)) of the oxygen-evolving complex (OEC) of PSII, encoded by the psbO, psbU and psbV genes, respectively. The single particle analysis of the top-view projections revealed the PSII complex to have maximal dimensions of 22 x 15 nm. The analysis of the side-view projections shows a maximal thickness of the PSII complex of about 9 nm including the densities on the lumenal surface that has been attributed to the proteins of the OEC complex. These results clearly demonstrate that the red algal PSII complex is structurally very similar to that of cyanobacteria and to the PSII core complex of higher plants. In addition, the arrangement of the OEC proteins on the lumenal surface of the PSII complex is consistent to that obtained by X-ray crystallography of cyanobacterial PSII.     

The interaction of ammonia with the photosynthetic oxygen-evolving system

The reaction of ammonia with the oxygen-evolving system was investigated using EPR. Two sites with distinct binding properties were found. One site, previously known to be responsible for the modification by ammonia of the multiline EPR signal from the S₂ state and believed to be accessible in this state only, was found to bind ammonia also in the S₁ state although weaker. The second binding site, identified by the effect of bound ammonia on the shape and position of the g = 4.1 EPR signal, was also found to be accessible in both the S₁ and S₂ states. The apparent dissociation constants for ammonia at the two sites in the S₁ and S₂ states were determined. In neither state did the binding the ammonia account for the observed inhibition of oxygen evolution, suggesting that binding to other S states plays an important role in the inhibition. Chloride, which is known to interfere with ammonia-induced inhibition of oxygen evolution, was found to compete with ammonia at the site associated with the modification of the g = 4.1 EPR signal. The broadening of the hyperfine lines of the multiline EPR signal, seen in the presence of ¹⁷O-labeled water, was still observed after the modification of the signal by ammonia. This indicates that ammonia has not completely displaced water bound to the catalytic site in the S₂ state. The results of the binding studies are interpreted in terms of a two state — two site model, where the two states are identified by their EPR signals, the multiline and the g = 4.1 signal, respectively, and the two sites identified by the effects of ammonia on these signals and where the equilibrium between the two states is regulated by the binding of ligands to the sites.     

Inhibition of the oxygen-evolving complex of photosystem II and depletion of extrinsic polypeptides by nickel

The toxic effect of Ni²⁺ on photosynthetic electron transport was studied in a photosystem II submembrane fraction. It was shown that Ni²⁺ strongly inhibits oxygen evolution in the millimolar range of concentration. The inhibition was insensitive to NaCl but significantly decreased in the presence of CaCl₂. Maximal chlorophyll fluorescence, together with variable fluorescence, maximal quantum yield of photosystem II, and flash-induced fluorescence decays were all significantly declined by Ni²⁺. Further, the extrinsic polypeptides of 16 and 24 kDa associated with the oxygen-evolving complex of photosystem II were depleted following Ni²⁺ treatment. It was deduced that interaction of Ni²⁺ with these polypeptides caused a conformational change that induced their release together with Ca²⁺ from the oxygen-evolving complex of photosystem II with consequent inhibition of the electron transport activity.     

Transport of proteins into chloroplasts. Import and maturation of precursors to the 33-, 23-, and 16-kDa proteins of the photosynthetic oxygen-evolving complex

The 33-, 23-, and 16-kDa proteins of the photosynthetic oxygen-evolving complex are synthesized as precursors in the cytoplasm and transported into the thylakoid lumen of higher plant chloroplasts. In this report we have analyzed the import and maturation of these precursors, using reconstituted protein import assays and partially purified preparations of the processing peptidases involved. Precursors of the 33- and 23-kDa proteins from Spinacia and Triticum aestivum are processed by a stromal peptidase to intermediate forms; polypeptides of similar size are observed during the transport of these precursors and possibly that of the 16-kDa protein, into isolated chloroplasts. Complete maturation of the 33- and 23-kDa proteins is carried out by a thylakoidal peptidase shown previously to be involved in plastocyanin biogenesis. The data support an import mechanism involving successive cleavages by the stromal and thylakoidal processing peptidases.     

The extreme halophyte Salicornia veneta is depleted of the extrinsic PsbQ and PsbP proteins of the oxygen-evolving complex without loss of functional activity

Background and Aims

Photosystem II of oxygenic organisms is a multi-subunit protein complex made up of at least 20 subunits and requires Ca²⁺ and Cl⁻ as essential co-factors. While most subunits form the catalytic core responsible for water oxidation, PsbO, PsbP and PsbQ form an extrinsic domain exposed to the luminal side of the membrane. In vitro studies have shown that these subunits have a role in modulating the function of Cl⁻ and Ca²⁺, but their role(s) in vivo remains to be elucidated, as the relationships between ion concentrations and extrinsic polypeptides are not clear. With the aim of understanding these relationships, the photosynthetic apparatus of the extreme halophyte Salicornia veneta has been compared with that of spinach. Compared to glycophytes, halophytes have a different ionic composition, which could be expected to modulate the role of extrinsic polypeptides.

Methods

Structure and function of in vivo and in vitro PSII in S. veneta were investigated and compared to spinach. Light and electron microscopy, oxygen evolution, gel electrophoresis, immunoblotting, DNA sequencing, RT–PCR and time-resolved chlorophyll fluorescence were used.

Key Results

Thylakoids of S. veneta did not contain PsbQ protein and its mRNA was absent. When compared to spinach, PsbP was partly depleted (30 %), as was its mRNA. All other thylakoid subunits were present in similar amounts in both species. PSII electron transfer was not affected. Fluorescence was strongly quenched upon irradiation of plants with high light, and relaxed only after prolonged dark incubation. Quenching of fluorescence was not linked to degradation of D1 protein.

Conclusions

In S. veneta the PsbQ protein is not necessary for photosynthesis in vivo. As the amount of PsbP is sub-stoichiometric with other PSII subunits, this protein too is largely dispensable from a catalytic standpoint. One possibility is that PsbP acts as an assembly factor for PSII.Key words: Photosystem II, PsbQ, PsbP, halophytes, Salicornia veneta     

Chloride cofactor in the photosynthetic oxygen-evolving complex studied by fourier transform infrared spectroscopy

Fourier transform infrared (FTIR) spectroscopy, using midfrequency S2/S1 FTIR difference spectra, has been applied to studies of chloride cofactor in the photosynthetic oxygen-evolving complex (OEC) to determine the effects of Cl(-) depletion and monovalent anion substitution. Cl(-) depletion resulted in the disappearance of a large part of the amide I and II vibrational modes, and induced characteristic modification in the features of the stretching modes of the carboxylate ligands of the Mn cluster. The normal spectral features were largely restored by replenishment of Cl(-) except for some changes in amide bands. The overall features of Br(-) -, I(-) -, or NO3(-) -substituted spectra were similar to those of the Cl(-) -reconstituted spectrum, consistent with their ability to support oxygen evolution. In contrast, the spectrum was significantly altered by the replacement of Cl(-) with F- or CH3COO(-), which resulted in marked suppression and distortion of both the carboxylate and amide bands. The activity of oxygen evolution restored by NO3(-) was as high as that by Cl(-) when measured under limited light conditions, indicating that the NO3(-) -substituted OEC is fully active in oxygen evolution, although with a slow turnover rate. The double-difference spectrum between the 14NO3(-) -substituted and 15NO3- -substituted S2/S1 difference spectrum showed isotopic bands for asymmetric NO stretching mode in the region of 1400-1300 cm(-1) due to NO3(-) bound to the Cl(-) site. This demonstrated structural coupling between the Cl(-) site and the Mn cluster. A proposed model for the isotopic bands suggested that Cl(-) as well as NO3(-) is not directly associated with the Mn cluster and exists in a more symmetric configuration and weaker binding state in the S2 state than in the S1 state. These results also suggest that Cl(-) is required for changes in the structure of the specific carboxylate ligand of the Mn cluster as well as the peptide backbone of protein matrixes upon the transition from S1 to S2.     

Mechanism of photosynthetic water oxidation in the dimeric oxygen-evolving complex of chloroplast photosystem II

Based on the analysis of the molecular organization and properties of an isolated oxygen-evolving complex of photosystem II of plant chloroplasts, a mechanism of water oxidation and oxygen release during photosynthesis was proposed. It is suggested that the photolysis of water occurs in a dimeric oxygen-evolving complex consisting of two core complexes. In the region of contact of these complexes, a hydrophobic "boiler" is formed where the conditions for screening and stabilization of Z-linanded manganese cations accumulating positive charges for the oxidation of water molecules are created. A prerequisite to the photolysis of water is the formation of a binuclear [Mn(3+)-OH ... HO-Mn3+] hydroxyl-manganese associate, which appears in the dimeric oxygen-evolving complex after the first two light flashes as a result of photohydrolysis of photochemically oxidized Z-liganded manganese cations. The process is accompanied by the release of the first water protons to the medium. The photosynthetic oxidation of water hydroxyls occurs at the next stage and is considered as synchronous detachment of four electrons from two bound OH-groups of the associate upon photooxidation of Mn3+ cations to Mn4+ cations after two subsequent light flashes. This process is accompanied by the disproportionation of electron density and the formation of a bond between oxygen atoms of hydroxyls followed by the evolution of molecular oxygen and protons, and regeneration of two starting Mn2+ cations and the primary state of the system.     

Coordination sphere and structure of the Mn cluster of the oxygen-evolving complex in photosynthetic organisms

The great similarity between the binding of Fe(II) and the high-affinity Mn-binding site in the Mn-depleted PSII membranes (Semin et al. (1996) FEBS Lett. 375, 223–226) suggests that the coordination sphere of Mn in PSII is also suitable for iron. A comparison is performed between the primary amino acid sequences of D1 and D2 and diiron-oxo enzymes with the function of oxygen activation. All conservative motifs (EXXH) and residues binding and stabilizing the diiron cluster in diiron-oxo enzymes have been found in the C-terminal domains of D1 and D2 polypeptides. On the basis of these sequence similarities we suggest a structural model for the manganese cluster in the oxygen-evolving complex.     

Glycerol binding at the narrow channel of photosystem II stabilizes the low-spin S2 state of the oxygen-evolving complex

Photosynthesis Research - The oxygen-evolving complex (OEC) of photosystem II (PSII) cycles through redox intermediate states Si (i?=?0–4) during the photochemical oxidation of...     

Formation and flash-dependent oscillation of the S2-state multiline EPR signal in an oxygen-evolving Photosystem-II preparation lacking the three extrinsic proteins in the oxygen-evolving system

In PS-II-enriched membranes lacking the three extrinsic water-soluble proteins in the oxygen-evolving system (18, 24 and 33 kDa), but still evolving oxygen to some extent, the formation of the multiline EPR signal originating from the S₂-state is dependent on the concentration of Cl⁻. In 200 mM Cl⁻ the multiline signal was observed after the first flash and oscillated with the flash number with a period of four. At 20 mM Cl⁻ no signal could be observed in this material. These results suggest that the extrinsic proteins are not necessary for multiline signal formation and that complete advancement through the S-states can occur in their absence when sufficient Cl⁻ is present.