Isolation and characterization of oxygen-evolving photosystem II complexes retaining the PsbO, P and Q proteins from Euglena gracilis

Oxygen-evolving photosystem II (PSII) complexes of Euglena gracilis were isolated and characterized. (1) The PSII complexes contained three extrinsic proteins of 33 kDa (PsbO), 23 kDa (PsbP) and 17 kDa (PsbQ), and showed oxygen-evolving activity of around 700 micromol O2 (mg Chl)(-1) h(-1) even in the absence of Cl- and Ca2+ ions. (2) NaCl-treatment removed not only PsbP and PsbQ but also a part of PsbO from Euglena PSII, indicating that PsbO binds to Euglena PSII more loosely than those of other organisms. Treatments by urea/NaCl, alkaline Tris or CaCl2 completely removed the three extrinsic proteins from Euglena PSII. (3) Each of the Euglena extrinsic proteins bound directly to PSII independent of the other extrinsic proteins, which is similar to the binding properties of the extrinsic proteins in a green alga, Chlamydomonas reinhardtii. (4) One of the significant features of Euglena PSII is that the oxygen evolution was not enhanced by Ca2+. When CaCl2-treated Euglena PSII was reconstituted with PsbO, the oxygen-evolving activity was stimulated by the addition of NaCl, but no further stimulation was observed by CaCl2. (5) Oxygen evolution of Euglena PSII reconstituted with PsbO from C. reinhardtii or spinach instead of that from Euglena also showed no enhancement by Ca2+, whereas a significant enhancement of oxygen evolution was observed by Ca2+ when the green algal or higher plant PSII was reconstituted with Euglena PsbO instead of their own PsbO. These results indicate that the PSII intrinsic proteins instead of the extrinsic PsbO protein, are responsible for the stimulation of oxygen evolution by Ca2+. Sequence comparison of major PSII intrinsic proteins revealed that PsbI of Euglena PSII is remarkably different from other organisms in that Euglena PsbI possesses extra 16-17 residues exposed to the luminal side. This may be related to the loss of enhancement of oxygen evolution by Ca2+ ion.     

Characterization of O2 evolution by a wheat photosystem II reaction center complex isolated by a simplified method: disjunction of secondary acceptor quinone and enhanced Ca2+ demand

An O2-evolving photosystem II (PSII) reaction center complex was prepared from wheat by a simple method consisting of octylglucoside solubilization of Triton PSII particles followed by one-step sucrose density gradient centrifugation. The complex contained six species of proteins including the 33-kDa extrinsic protein with the same relative abundance as in the original PSII particles, one cytochrome b559, 4 Mn, and about 40 chlorophyll (Chl) per O2-evolving unit, and evolved O2 at a high rate of 1400-1700 mumol O2/mg Chl/h. O2 evolution by the complex was dependent on acceptor species, showing a hierarchy, ferricyanide greater than dichlorobenzoquinone greater than phenylbenzoquinone greater than dimethylbenzoquinone greater than duroquinone, and insensitive to DCMU, indicative of disjunction of the secondary quinone acceptor of PSII from the electron transport pathway. O2 evolution also showed a marked dependence on Cl- and Ca2+: about 10-fold acceleration by Cl- and an additional 2- to 3-fold by Ca2+. Comparison of the dissociation constants for Cl- and Ca2+ between the complex and NaCl-washed PSII particles revealed that octylglucoside treatment gives rise to a new Ca2+-sensitive site by removal of some unknown factor(s) other than the extrinsic 22- and 16-kDa proteins, while it preserves the Cl(-)-sensitive site as native as in NaCl-washed PSII particles. Analysis of the relationship between Cl- demand and Ca2+ demand revealed that Ca2+ absence noncompetitively inhibits the Cl(-)-supported O2 evolution, indicative of the independence of the binding site of these two factors.     

Highly purified thermo-stable oxygen-evolving photosystem II core complex from the thermophilic cyanobacterium Synechococcus elongatus having His-tagged CP43

The carboxyl terminus of the CP43 subunit of photosystem II (PSII) in the thermophilic cyanobacterium, Synechococcus elongatus, was genetically tagged with six consecutive histidine residues to create a metal binding site on the PSII supramolecular complex. The histidine-tagging enabled rapid isolation of an intact cyanobacterial PSII core complex from dodecyl maltoside-solubilized thylakoids by a simple one-step Ni(2+)-affinity column chromatography. The isolated core complex was in a dimeric form with a molecular mass of about 580 kDa, consisting of five major intrinsic membrane proteins (CP47, CP43, D1, D2 and cytochrome b-559), three extrinsic proteins (33 kDa, 12 kDa, and cytochrome c-550), and a few low molecular mass membrane proteins, and evolved oxygen at a rate as high as 3,400 mumol (mg Chl)-1 h-1 at 45 degrees C with ferricyanide as an electron acceptor. The core complex emitted thermoluminescence B2-, B1- and Q-bands arising from S2QB-, S3QB- and S2QA- charge recombinations at respective emission temperatures of 45, 38 and 20 degrees C, all of which were higher by about 15 degrees C as compared with those in mesophilic spinach BBY membranes. These results indicated that the isolated core complex well retained the intact properties of thermoluminescence of thermophilic cyanobacterial cells, the deeper stabilization of PSII charge pairs. The isolated complex was extremely stable in terms of both protein composition and function, exhibiting no release of extrinsic proteins, no proteolytic degradation in any of its subunits, accompanied by only a slight (less than 10%) loss in oxygen evolution, after dark-incubation at 20 degrees C for 8 d. These properties of the thermophilic PSII core complex are highly useful for various types of studies on PSII.     

Isolation and characterization of oxygen-evolving thylakoid membranes and photosystem II particles from a marine diatom Chaetoceros gracilis

Thylakoid membranes retaining high oxygen-evolving activity (about 250 micromol O(2)/mg Chl/h) were prepared from a marine centric diatom, Chaetoceros gracilis, after disruption of the cells by freeze-thawing. We also succeeded in purification of Photosystem II (PSII) particles by differential centrifugation of the thylakoid membranes after treatment with 1% Triton X-100. The diatom PSII particles showed an oxygen-evolving activity of 850 and 1045 micromol O(2)/mg Chl/h in the absence and presence of CaCl(2), respectively. The PSII particles contained fucoxanthin chlorophyll a/c-binding proteins in addition to main intrinsic proteins of CP47, CP43, D2, D1, cytochrome b559, and the antenna size was estimated to be 229 Chl a per 2 molecules of pheophytin. Five extrinsic proteins were stoichiometrically released from the diatom PSII particles by alkaline Tris-treatment. Among these five extrinsic proteins, four proteins were red algal-type extrinsic proteins, namely, PsbO, PsbQ', PsbV and PsbU, whereas the other one was a novel, hypothetical protein. This is the first report on isolation and characterization of diatom PSII particles that are highly active in oxygen evolution and retain the full set of extrinsic proteins including an unknown protein.     

Influence of the PsbA1/PsbA3, Ca(2+)/Sr(2+) and Cl(-)/Br(-) exchanges on the redox potential of the primary quinone Q(A) in Photosystem II from Thermosynechococcus elongatus as revealed by spectroelectrochemistry

Ca(2+) and Cl(-) ions are essential elements for the oxygen evolution activity of photosystem II (PSII). It has been demonstrated that these ions can be exchanged with Sr(2+) and Br(-), respectively, and that these ion exchanges modify the kinetics of some electron transfer reactions at the Mn?Ca cluster level (Ishida et al., J. Biol. Chem. 283 (2008) 13330-13340). It has been proposed from thermoluminescence experiments that the kinetic effects arise, at least in part, from a decrease in the free energy level of the Mn(4)Ca cluster in the S? state though some changes on the acceptor side were also observed. Therefore, in the present work, by using thin-layer cell spectroelectrochemistry, the effects of the Ca(2+)/Sr(2+) and Cl(-)/Br(-) exchanges on the redox potential of the primary quinone electron acceptor Q(A), E(m)(Q(A)/Q(A)(-)), were investigated. Since the previous studies on the Ca(2+)/Sr(2+) and Cl(-)/Br(-) exchanges were performed in PsbA3-containing PSII purified from the thermophilic cyanobacterium Thermosynechococcus elongatus, we first investigated the influences of the PsbA1/PsbA3 exchange on E(m)(Q(A)/Q(A)(-)). Here we show that i) the E(m)(Q(A)/Q(A)(-)) was up-shifted by ca. +38mV in PsbA3-PSII when compared to PsbA1-PSII and ii) the Ca(2+)/Sr(2+) exchange up-shifted the E(m)(Q(A)/Q(A)(-)) by ca. +27mV, whereas the Cl(-)/Br(-) exchange hardly influenced E(m)(Q(A)/Q(A)(-)). On the basis of the results of E(m)(Q(A)/Q(A)(-)) together with previous thermoluminescence measurements, the ion-exchange effects on the energetics in PSII are discussed.     

Calcium depletion modifies the structure of the photosystem II O(2)-evolving complex.

A 5 min exposure of photosystem II to a pH 3 citric acid solution is a simple method for selective removal of Ca(2+) from the O(2)-evolving complex. The resulting preparation retains the 23 and 17 kDa extrinsic polypeptides, but the activity of this material is only 10-20% of that of an untreated control sample. Biochemical characterization of citrate-treated photosystem II reveals that some reaction centers lose the extrinsic proteins during citrate treatment. Furthermore, a comparison of photosystem II preparations treated with citrate, or depleted of 23 and 17 kDa extrinsic polypeptides by high-salt treatment, shows that low concentrations of a small reductant, NH(2)OH, which has little effect on the activity of intact photosystem II, can reduce and inhibit the Mn cluster in both types of preparations. In contrast, a large reductant, hydroquinone, cannot access the majority of O(2)-evolving centers in citrate-treated preparations, while 23 and 17 kDa-depleted material is rapidly inactivated by the reductant. Incubation of the citrate-treated samples in high ( approximately 60 mM) concentrations of CaCl(2) restores 50% of the lost activity; this Ca(2+)-reconstituted activity is chelator-insensitive, indicating that rebinding of Ca(2+) restores the structural integrity of the O(2)-evolving complex. A characterization of Ca(2+) and Cl(-) affinities in steady-state activity assays shows that citrate-treated preparations exhibit a Cl(-) requirement similar to that of polypeptide-depleted photosystem II, while Ca(2+) reactivation of O(2) evolution appears to occur at two structurally distinct sites. One site exhibits a high Ca(2+) affinity, similar to that found in polypeptide-depleted samples, but a second, lower-affinity site also exists, with a K(M) that is approximately 10 times greater than that of the high-affinity site, which is associated with centers that retain the extrinsic polypeptides. These data indicate that citrate-induced Ca(2+) depletion causes release of the 23 and 17 kDa extrinsic polypeptides from some photosystem II reaction centers, and also modifies the structure of the polypeptide-retaining O(2)-evolving centers so that the Mn cluster is exposed to small, but not large, reductants. This change may be due to subtle modifications to the structure of the photosystem II extrinsic proteins that produces a new pathway between the solvent and the Mn cluster or, alternatively, to the opening of an existing channel in the intrinsic lumenal polypeptide domain, between the solvent and the Mn cluster, that is normally occluded by a bound Ca(2+) atom.     

Isolation and characterization of oxygen-evolving thylakoid membranes and Photosystem II particles from a marine diatom Chaetoceros gracilis

Thylakoid membranes retaining high oxygen-evolving activity (about 250 μmol O₂/mg Chl/h) were prepared from a marine centric diatom, Chaetoceros gracilis, after disruption of the cells by freeze-thawing. We also succeeded in purification of Photosystem II (PSII) particles by differential centrifugation of the thylakoid membranes after treatment with 1% Triton X-100. The diatom PSII particles showed an oxygen-evolving activity of 850 and 1045 μmol O₂/mg Chl/h in the absence and presence of CaCl₂, respectively. The PSII particles contained fucoxanthin chlorophyll a/c-binding proteins in addition to main intrinsic proteins of CP47, CP43, D2, D1, cytochrome b559, and the antenna size was estimated to be 229 Chl a per 2 molecules of pheophytin. Five extrinsic proteins were stoichiometrically released from the diatom PSII particles by alkaline Tris-treatment. Among these five extrinsic proteins, four proteins were red algal-type extrinsic proteins, namely, PsbO, PsbQ', PsbV and PsbU, whereas the other one was a novel, hypothetical protein. This is the first report on isolation and characterization of diatom PSII particles that are highly active in oxygen evolution and retain the full set of extrinsic proteins including an unknown protein.     

The two substrate-water molecules are already bound to the oxygen-evolving complex in the S2 state of photosystem II

The first direct evidence which shows that both substrate-water molecules are bound to the O(2)-evolving catalytic site in the S(2) state of photosystem II (PSII) is presented. Rapid (18)O isotope exchange measurements between H(2)(18)O incubated in the S(2) state of PSII-enriched membrane samples and the photogenerated O(2) reveal a fast and a slow phase of exchange at m/e 34 (which measures the level of the (16)O(18)O product). The rate constant for the slow phase of exchange ((34)k(1)) equals 1.9 +/- 0.3 s(-1) at 10 degrees C, while the fast phase of exchange is unresolved by our current experimental setup ((34)k(2) >or= 175 s(-1)). The unresolvable fast phase has left open the possibility that the second substrate-water molecule binds to the catalytic site only after the formation of the S(3) state [Hillier, W., and Wydrzynski, T. (2000) Biochemistry 39, 4399-4405]. However, for PSII samples depleted of the 17 and 23 kDa extrinsic proteins (Ex-depleted PSII), two completely resolvable phases of (18)O exchange are observed in the S(2) state of the residual activity, with the following rate constants: (34)k(1) = 2.6 +/- 0.3 s(-1) and (34)k(2) = 120 +/- 14 s(-1) at 10 degrees C. Upon addition of 15 mM CaCl(2) to Ex-depleted PSII, the O(2) evolution activity increases to approximately 80% of the control level, while the two resolvable phases of exchange remain the same. In measurements of Ex-depleted PSII at m/e 36 (which measures the level of the (18)O(18)O product), only a single phase of exchange is observed in the S(2) state, with a rate constant ((36)k(1) = 2.5 +/- 0.2 s(-1)) that is identical to the slow rate of exchange in the m/e 34 data. Taken together, these results show that the fast phase of (18)O exchange is specifically slowed by the removal of the 17 and 23 kDa extrinsic proteins and that the two substrate-water molecules must be bound to independent sites already in the S(2) state. In contrast, the (18)O exchange behavior in the S(1) state of Ex-depleted PSII is no different from what is observed for the control, with or without the addition of CaCl(2). Since the fast phase of exchange in the S(1) state is unresolved (i.e., (34)k(2) > 100 s(-1)), the possibility remains that the second substrate-water molecule binds to the catalytic site only after the formation of the S(2) state. The role of the 17 and 23 kDa extrinsic proteins in establishing an asymmetric dielectric environment around the substrate binding sites is discussed.     

Mutations of arginine 64 within the putative Ca(2+)-binding lumenal interhelical a-b loop of the photosystem II D1 protein disrupt binding of the manganese stabilizing protein and cytochrome c(550) in Synechocystis sp. PCC6803

Mutations D1-R64E, D1-R64Q, and D1-R64V in the putative calcium-binding lumenal interhelical a-b loop of the photosystem II (PSII) D1 protein were characterized in terms of impact on growth, extrinsic protein binding, photoactivation, and properties of the H(2)O-oxidation complex. The D1-R64E charge reversal mutation greatly weakened the binding of the extrinsic manganese-stabilizing protein (MSP) and, to a considerably lesser extent, weakened the binding of cytochrome c(550) (c550). Both D1-R64Q and D1-R64E exhibited an increased requirement for Ca(2+) in the cell growth medium. Bare platinum electrode measurements of O(2)-evolving membranes showed a retarded appearance of O(2) following single turn-over flashes, especially in the case of the D1-R64E mutant. The D1-R64E mutant also had a pronounced tendency to lose O(2) evolution activity in the dark and exhibited an increased relative quantum yield of photoactivation, which are characteristics shared by mutants that lack extrinsic proteins. S(2) and S(3) decay measurements in the isolated membranes indicate that D1-R64E and D1-R64Q have faster decays of these higher S-states as compared to the wild-type. However, fluorescence decay in the presence of DCMU, which monitors primarily Q(A)(-) charge recombination with PSII donors, showed somewhat slower decays. Taken together, the fluorescence and S-state decay indicate that the midpoint of either Q(B)(-) has been modified to be more negative in the mutants or that a recombination path presumably involving either Q(B)(-) or Y(D) has become kinetically more accessible.     

Cross-reconstitution of various extrinsic proteins and photosystem II complexes from cyanobacteria, red algae and higher plants

Photosystem II (PSII) contains different extrinsic proteins required for oxygen evolution among different organisms. Cyanobacterial PSII contains the 33 kDa, 12 kDa proteins and cytochrome (cyt) c-550; red algal PSII contains a 20 kDa protein in addition to the three homologous cyanobacterial proteins; whereas higher plant PSII contains the 33 kDa, 23 kDa and 17 kDa proteins. In order to understand the binding and functional properties of these proteins, we performed cross-reconstitution experiments with combinations of PSII and extrinsic proteins from three different sources: higher plant (spinach), red alga (Cyanidium caldarium) and cyanobacterium (Synechococcus vulcanus). Among all of the extrinsic proteins, the 33 kDa protein is common to all of the organisms and is totally exchangeable in binding to PSII from any of the three organisms. Oxygen evolution of higher plant and red algal PSII was restored to a more or less similar level by binding of any one of the three 33 kDa proteins, whereas oxygen evolution of cyanobacterial PSII was restored to a larger extent with its own 33 kDa protein than with the 33 kDa protein from other sources. In addition to the 33 kDa protein, the red algal 20 kDa, 12 kDa proteins and cyt c-550 were able to bind to cyanobacterial and higher plant PSII, leading to a partial restoration of oxygen evolution in both organisms. The cyanobacterial 12 kDa protein and cyt c-550 partially bound to the red algal PSII, but this binding did not restore oxygen evolution. The higher plant 23 kDa and 17 kDa proteins bound to the cyanobacterial and red algal PSII only through non-specific interactions. Thus, only the red algal extrinsic proteins are partially functional in both the cyanobacterial and higher plant PSII, which implies a possible intermediate position of the red algal PSII during its evolution from cyanobacteria to higher plants.     

Dual role of triplet localization on the accessory chlorophyll in the photosystem II reaction center: photoprotection and photodamage of the D1 protein

Infrared absorption and electron spin resonance studies have shown that the excited triplet state of chlorophyll formed by radical pair recombination in the PSII reaction center is mainly localized on the accessory chlorophyll, which is most probably located in the D1 protein (Chl(1)). This triplet localization plays two contrasting roles, depending on the redox state of Q(A), in the process of acceptor-side photoinhibition of PSII. In the early stage of photoinhibition, in which singly reduced Q(A) is reversibly stabilized, the triplet state of Chl(1) ((3)Chl(1)*) is rapidly quenched (t(1/2) = 2-20 micro s) by the interaction with Q(A)(-), preventing formation of harmful singlet oxygen. In the next inhibitory stage, in which Q(A) is doubly reduced and then irreversibly released from the Q(A) pocket, the lifetime of (3)Chl(1)* becomes longer by more than two orders of magnitude (t(1/2) = 1-3 ms). As a result, singlet oxygen is produced around Chl(1) in the D1 protein, causing damage preferably to the D1 protein, which induces subsequent proteolytic degradation. Thus, (3)Chl(1)* functions as a switch to change from the protective to the degradative phase of the PSII reaction center by sensing either reversible or irreversible inhibited state at the Q(A) site.     

Photoactivation of Oxygen-Evolving Enzyme in Dark-Grown Pine Cotyledons: Relationship between Assembly of Photosystem II Proteins and Integration of Manganese and Calcium

Dark-grown cotyledons of pine (Pinus thunbergit) did not exhibitO₂ evolution, but this capability was rapidly activated by illuminationfor a short period (photoactivation). To examine the biochemicalchanges which accompany the process of photoactivation in gymnosperms,a method enabling the preparation of highly active O₂-evolvingphotosystem II (PS II) membranes was applied to light-grown,dark-grown, and photoactivated cotyledons. PS II membranes preparedfrom light-grown cotyledons exhibited high O₂-evolving activity,and contained all the intrinsic proteins as well as the threeextrinsic proteins (32, 23 and 17 kDa) associated with PS II.These membranes were also found to contain 4.4 Mn and 0.83 Ca/PSII reaction center. PS II membranes from dark-grown cotyledonscontained all the intrinsic proteins, but preserved only 32kDa extrinsic protein, and zero Mn and 0.85 Ca/PS II reactioncenter. The two extrinsic proteins (23 and 17 kDa) absent inthe PS II membranes from dark-grown cotyledons were, however,present as mature forms in whole thylakoid membranes from thecorresponding sample. The PS II membranes isolated from photoactivatedcotyledons showed a high activity of O₂ evolution and retainedthe three extrinsic proteins, 5.3 Mn and 1.1 Ca/PS II reactioncenter, respectively. The results indicated that Mn and thetwo extrinsic proteins were tightly integrated in the O₂-evolvingapparatusduring the process of photoactivation but integration of Capreceded the integration of Mn by photoactivation. (Received December 9, 1991; Accepted February 1, 1992)     

Extrinsic photosystem II carbonic anhydrase in maize mesophyll chloroplasts

One form of carbonic anhydrase (CA) has been observed in maize (Zea mays) thylakoids and photosystem II (PSII)-enriched membranes. Here, we show that an antibody produced against a thylakoid lumen-targeted CA found in Chlamydomonas reinhardtii reacts with a single 33-kD polypeptide in maize thylakoids. With immunoblot analysis, we found that this single polypeptide could be identified only in mesophyll thylakoids and derived PSII membranes, but not in bundle sheath thylakoids. Likewise, a CA activity assay confirmed a large amount of activity in mesophyll, but not in bundle sheath membranes. Immunoblot analysis and CA activity assay showed that the maximum CA can be obtained in the supernatant of the PSII-enriched membranes washed with 1 M CaCl(2), the same procedure used to remove all extrinsic lumenal proteins from PSII. Because this CA reacts with an antibody to lumen-directed CA in C. reinhardtii, and because it can be removed with 1 M CaCl(2) wash, we refer to it tentatively as extrinsic CA. This is to distinguish it from another form of CA activity tightly bound to PSII membranes that remains after CaCl(2) wash, which has been described previously. The function of extrinsic CA is not clear. It is unlikely to have the same function as the cytoplasmic CA, which has been proposed to increase the HCO(-)(3) concentration for phosphoenolpyruvate carboxylase and the C(4) pathway. We suggest that because the extrinsic CA is associated only with thylakoids doing linear electron flow, it could function to produce the CO(2) or HCO(-)(3) needed for PSII activity.     

Isolation and characterization of the oxygen-evolving photosystem II complex from the economical red alga <Emphasis Type="Italic">Bangia fusco-purpurea</Emphasis>

The highly pure and active photosystem II (PSII) complex was isolated from Bangia fusco-purpurea (Dillw) Lyngb., an important economic red alga in China, through two steps of sucrose density gradient ultracentrifugation and characterized by the room absorption and fluorescence emission spectra, DCIP (2,6-dichloroindophenol) reduction, and oxygen evolution rates. The PSII complex from B. fusco-purpurea had the characteristic absorption peaks of chlorophyll (Chl) a (436 and 676 nm) and typical fluorescence emission peak at 685 nm (Ex = 436 nm). Moreover, the acquired PSII complex displayed high oxygen evolution (139 μmol O₂/(mg Chl h) in the presence of 2.5 mM 2,6-dimethybenzoqinone as an artificial acceptor and was active in photoreduction of DCIP (2,6-dichloroindophenol) by DPC (1,5-diphenylcarbazide) at 163 U/(mg Chl a h). SDS-PAGE also suggested that the purified PSII complex contained four intrinsic proteins (D1, D2, CP43, and CP47) and four extrinsic proteins (33-kD protein, 20-kD protein, cyt c-550, and 14-kD protein).     

Multiflash experiments reveal a new kinetic phase of photosystem II manganese cluster assembly in Synechocystis sp. PCC6803 in vivo

The assembly of Mn(2+) ions into the H(2)O oxidation complex (WOC) of the photosystem II (PSII) reaction center is a light-driven process, termed photoactivation. According to the "two-quantum" model, photoactivation involves two light-driven charge separations coupled to the photooxidation of Mn(2+) in order to form the first stable intermediate in a process that culminates in the oxidative assembly of four Mn(2+) ions and one Ca(2+) ion to form the active, higher valence (Mn(4)-Ca) center of the WOC. To better define the kinetics of the dark rearrangement and to gain some understanding of the basis for the very low quantum yield of the overall process, photoactivation experiments, involving different flash patterns, were conducted with Synechocystis sp. PCC6803. It was found that even the so-called first stable intermediate is readily lost during protracted (1-10 s) dark periods during photoactivation of Synechocystis cells. Low concentrations of the electron acceptor, DCBQ, improved the stability of the dark intermediates. The unstable photoactivation intermediates formed early in the photoactivation process were not, however, stabilized by the addition of Ca(2+), although the overall yield of photoactivation is enhanced by the additional Ca(2+). Measurements of the kinetics of fluorescence yield verify that Q(A)(-) to Q(B) electron transfer rates change during the course of photoactivation as the high potential form of Q(A)(-) is converted to the low potential form and show that DCBQ acts as an efficient electron acceptor from Q(A)(-) even while in its high potential form. In addition the approximately 150 ms phase corresponding to the originally described dark rearrangement of photoactivation, repetitive, double flash experiments, with a 10 s intervening dark period, reveals a faster, 15 ms phase that is accentuated by DCBQ.     

Purification, crystallization and X-ray diffraction analyses of the T. elongatus PSII core dimer with strontium replacing calcium in the oxygen-evolving complex

The core complex of photosystem II (PSII) was purified from thermophilic cyanobacterium Thermosynechococcus elongatus grown in Sr(2+)-containing and Ca(2+)-free medium. Functional in vivo incorporation of Sr(2+) into the oxygen-evolving complex (OEC) was confirmed by EPR analysis of the isolated and highly purified SrPSII complex in agreement with the previous study of Boussac et al. [J. Biol. Chem. 279 (2004) 22809-22819]. Three-dimensional crystals of SrPSII complex were obtained which diffracted to 3.9 A and belonged to the orthorhombic space group P2(1)2(1)2(1) with unit cell dimensions of a=133.6 A, b=236.6 A, c=307.8 A. Anomalous diffraction data collected at the Sr K-X-ray absorption edge identified a novel Sr(2+)-binding site which, within the resolution of these data (6.5 A), is consistent with the positioning of Ca(2+) in the recent crystallographic models of PSII [Ferreira et al. Science 303 (2004) 1831-1838, Loll et al. Nature 438 (2005) 1040-1044]. Fluorescence measurements on SrPSII crystals confirmed that crystallized SrPSII was active in transferring electrons from the OEC to the acceptor site of the reaction centre. However, SrPSII showed altered functional properties of its modified OEC in comparison with that of the CaPSII counterpart: slowdown of the Q(A)-to-Q(B) electron transfer and stabilized S(2)Q(A)(-) charge recombination.     

Accessibility of tyrosine Y(.)(Z) to exogenous reductants and Mn(2+) in various Photosystem II preparations

The reduction of tyrosine Y(.)(Z) by benzidine and exogenous Mn(2+) was studied by kinetic EPR experiments in various Photosystem II (PSII) preparations. Using lanthanide treated PSII membranes it was demonstrated that neither the extrinsic polypeptides (17, 23 and 33 kDa) nor the Mn complex block the accessibility of Y(.)(Z) to exogenous reductants, such as benzidine. In addition, it was shown that in the presence of the native Mn complex exogenous Mn(2+) does not reduce Y(.)(Z).     

Structural localization of the O2-evolving apparatus to multimeric (tetrameric) particles on the lumenal surface of freeze-etched photosynthetic membranes

Isolated appressed chloroplast membranes, highly enriched in photosystem II (PSII) activity, were examined by freeze-etch electron microscopy. The exposed surfaces of these Triton X-100 solubilized membrane fragments correspond to the lumenal or ESs surface of intact stacked thylakoid membrane regions (Dunahay, T. G., L. A. Staehelin, M. Seibert, P. D. Ogilvie, and S. P. Berg. 1984. Biochim. Biophys. Acta. 764:179-193). The sequential removal from this sample of three extrinsic proteins (17, 23, and 33 kD) associated with the O2-evolving apparatus and the concomitant loss of O2 evolution, was related to subtle changes in the height and substructure of characteristic multimeric (often tetrameric) particles that protrude from the ESs membrane surface. After removal of these proteins, the multimeric particles disappeared and dimeric particles of similar diameter but of lesser height (6.1 vs. 8.2 nm in the controls) were observed. Reconstitution of the depleted membrane fragments with the extrinsic proteins led to rebinding of the three proteins, to a 63% recovery of the control rates of O2 evolution, and to the reappearance of the larger multimeric particles. Analysis of the structural changes associated with the loss and rebinding of the extrinsic proteins is consistent with a stoichiometry of one PSII complex for either one or two copies of the 17-, 23-, and 33-kD proteins, and these are symmetrically arranged on the lumenal surface of the complex. These results demonstrate that the multimeric ESs particles correspond to part of the intact O2-evolving apparatus of PSII, thus confirming previous indirect studies relating these particles to PSII. The dimeric particles probably contain the rest of the O2-evolving complex.     

Identification of functional domains of the extrinsic 12 kDa protein in red algal PSII by limited rroteolysis and directed mutagenesis.

The extrinsic 12 kDa protein in red algal photosystem II (PSII) functions to minimize the chloride and calcium requirement of oxygen-evolving activity [Enami et al. (1998) Biochemistry 37: 2787]. In order to identify functional domains of the 12 kDa protein, we prepared the 12 kDa protein lacking N-terminal peptides or C-terminal peptides or both by limited proteolysis and directed mutagenesis. The resulting 12 kDa protein fragments were examined for their binding and functional properties by reconstitution experiments. (1) A peptide fragment from Gly-6 to C-terminus of the 12 kDa protein was prepared by V8 protease. This fragment rebound to PSII completely, and it reactivated oxygen evolution partially in the absence of Cl(-) and Ca(2+) ions but significantly in the presence of Cl(-) ion. (2) A peptide from Leu-10 to Phe-83 was obtained by chymotrypsin treatment. This peptide rebound to PSII effectively, but the rebinding did not restore oxygen evolution in both the absence and presence of Cl(-) and Ca(2+) ions. (3) Two mutant proteins, one lacking five residues and the other lacking nine residues of the N-terminus, were able to bind to PSII effectively. Recovery of oxygen evolution by their binding was almost the same as that reconstituted with the V8 protease-treated peptide. (4) Three mutant proteins lacking ten, seven or three residues of the C-terminus effectively rebound to PSII, but their binding did not result in recovery of the oxygen evolution. In contrast, reconstitution with a mutant protein lacking one residue of the C-terminus showed the same high restoration of oxygen evolution as reconstitution with the full-length 12 kDa protein. (5) These results indicate that two residues from lysine of the C-terminus of the 12 kDa protein constitute an important domain for minimizing the chloride and calcium requirement of oxygen evolution. In addition, the N-terminus of the protein, at least five residues, has a secondary function for the chloride requirement.     

Acceptor side effects on the electron transfer at cryogenic temperatures in intact photosystem II

In intact PSII, both the secondary electron donor (Tyr(Z)) and side-path electron donors (Car/Chl(Z)/Cyt(b)(559)) can be oxidized by P(680)(+) at cryogenic temperatures. In this paper, the effects of acceptor side, especially the redox state of the non-heme iron, on the donor side electron transfer induced by visible light at cryogenic temperatures were studied by EPR spectroscopy. We found that the formation and decay of the S(1)Tyr(Z) EPR signal were independent of the treatment of K(3)Fe(CN)(6), whereas formation and decay of the Car(+)/Chl(Z)(+) EPR signal correlated with the reduction and recovery of the Fe(3+) EPR signal of the non-heme iron in K(3)Fe(CN)(6) pre-treated PSII, respectively. Based on the observed correlation between Car/Chl(Z) oxidation and Fe(3+) reduction, the oxidation of non-heme iron by K(3)Fe(CN)(6) at 0 degrees C was quantified, which showed that around 50-60% fractions of the reaction centers gave rise to the Fe(3+) EPR signal. In addition, we found that the presence of phenyl-p-benzoquinone significantly enhanced the yield of Tyr(Z) oxidation. These results indicate that the electron transfer at the donor side can be significantly modified by changes at the acceptor side, and indicate that two types of reaction centers are present in intact PSII, namely, one contains unoxidizable non-heme iron and another one contains oxidizable non-heme iron. Tyr(Z) oxidation and side-path reaction occur separately in these two types of reaction centers, instead of competition with each other in the same reaction centers. In addition, our results show that the non-heme iron has different properties in active and inactive PSII. The oxidation of non-heme iron by K(3)Fe(CN)(6) takes place only in inactive PSII, which implies that the Fe(3+) state is probably not the intermediate species for the turnover of quinone reduction.