The basic properties of the electronic structure of the oxygen-evolving complex of photosystem II are not perturbed by Ca2+ removal

Ca(2+) is an integral component of the Mn(4)O(5)Ca cluster of the oxygen-evolving complex in photosystem II (PS II). Its removal leads to the loss of the water oxidizing functionality. The S(2)' state of the Ca(2+)-depleted cluster from spinach is examined by X- and Q-band EPR and (55)Mn electron nuclear double resonance (ENDOR) spectroscopy. Spectral simulations demonstrate that upon Ca(2+) removal, its electronic structure remains essentially unaltered, i.e. that of a manganese tetramer. No redistribution of the manganese valence states and only minor perturbation of the exchange interactions between the manganese ions were found. Interestingly, the S(2)' state in spinach PS II is very similar to the native S(2) state of Thermosynechococcus elongatus in terms of spin state energies and insensitivity to methanol addition. These results assign the Ca(2+) a functional as opposed to a structural role in water splitting catalysis, such as (i) being essential for efficient proton-coupled electron transfer between Y(Z) and the manganese cluster and/or (ii) providing an initial binding site for substrate water. Additionally, a novel (55)Mn(2+) signal, detected by Q-band pulse EPR and ENDOR, was observed in Ca(2+)-depleted PS II. Mn(2+) titration, monitored by (55)Mn ENDOR, revealed a specific Mn(2+) binding site with a submicromolar K(D). Ca(2+) titration of Mn(2+)-loaded, Ca(2+)-depleted PS II demonstrated that the site is reversibly made accessible to Mn(2+) by Ca(2+) depletion and reconstitution. Mn(2+) is proposed to bind at one of the extrinsic subunits. This process is possibly relevant for the formation of the Mn(4)O(5)Ca cluster during photoassembly and/or D1 repair.     

Investigation of the origin of the "S3" EPR signal from the oxygen-evolving complex of photosystem 2: the role of tyrosine Z.

The origin of the "S3" EPR signal from calcium-depleted photosystem 2 samples has been investigated. This signal is observed after freezing samples under illumination and has been assigned to an interaction between the manganese cluster and an oxidized histidine radical [Boussac et al. (1990) Nature 347; 303-306]. In calcium-depleted samples prepared by three different methods, we observed the trapping of the tyrosine radical YZ+ under conditions which also formed the "S3" signal. An "S3"-type signal and YZ+ were also formed in PS2 samples treated with the water analogue ammonia. Following illumination at 277 K, the "S3" and YZ+ signals decayed at the same rate at 273 K in the dark. Both the YZ+ and "S3" signals decayed on storage at 77 K and could be subsequently regenerated by illumination at 8-77 K. No evidence to support histidine oxidation was found. The effects of DCMU, chelators, and alkaline pH on the dark-stable multiline S2 and the "S3" signals from calcium-depleted samples were determined. Both signals required the presence of EGTA or citrate for maximum yield. The addition of DCMU caused a reduction in the yield of "S3" generated by freezing under illumination. Incubation at pH 7.5 resulted in the loss of both signals. We propose that a variety of treatments which affect calcium and chloride binding cause a stabilization of the S2 state and slow the reduction of YZ+. This allows the trapping of YZ+, the interaction with the manganese cluster (probably in the S2 state) resulting in the "S3" signal. The data allow the position of the manganese cluster to be estimated as within 10 A of tyrosine Z (D1-161).     

The S0 state of photosystem II induced by hydroxylamine: differences between the structure of the manganese complex in the S0 and S1 states determined by X-ray absorption spectroscopy

Hydroxylamine at low concentrations causes a two-flash delay in the first maximum flash yield of oxygen evolved from spinach photosystem II (PSII) subchloroplast membranes that have been excited by a series of saturating flashes of light. Untreated PSII membrane preparations exhibit a multiline EPR signal assigned to a manganese cluster and associated with the S2 state when illuminated at 195 K, or at 273 K in the presence of 3-(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU). We used the extent of suppression of the multiline EPR signal observed in samples illuminated at 195 K to determine the fraction of PSII reaction centers set back to a hydroxylamine-induced S0-like state, which we designate S0*. The manganese K-edge X-ray absorption edges for dark-adapted PSII preparations with or without hydroxylamine are virtually identical. This indicates that, despite its high binding affinity to the oxygen-evolving complex (OEC) in the dark, hydroxylamine does not reduce chemically the manganese cluster within the OEC in the dark. After a single turnover of PSII, a shift to lower energy is observed in the inflection of the Mn K-edge of the manganese cluster. We conclude that, in the presence of hydroxylamine, illumination causes a reduction of the OEC, resulting in a state resembling S0. This lower Mn K-edge energy of S0*, relative to the edge of S1, implies the storage and stabilization of an oxidative equivalent within the manganese cluster during the S0----S1 state transition. An analysis of the extended X-ray absorption fine structure (EXAFS) of the S0* state indicates that a significant structural rearrangement occurs between the S0* and S1 states. The X-ray absorption edge position and the structure of the manganese cluster in the S0* state are indicative of a heterogeneous mixture of formal valences of manganese including one Mn(II) which is not present in the S1 state.     

pH dependent competition between Y(Z) and Y(D) in photosystem II probed by illumination at 5 K

The photosystem II (PSII) reaction center contains two redox active tyrosines, YZ and YD, situated on the D1 and D2 proteins, respectively. By illumination at 5 K, oxidation of YZ in oxygen-evolving PSII can be observed as induction of the Split S1 EPR signal from YZ* in magnetic interaction with the CaMn4 cluster, whereas oxidation of YD can be observed as the formation of the free radical EPR signal from YD*. We have followed the light induced induction at 5 K of the Split S1 signal between pH 4-8.5. The formation of the signal, that is, the oxidation of YZ, is pH independent and efficient between pH 5.5 and 8.5. At low pH, the split signal formation decreases with pKa approximately 4.7-4.9. In samples with chemically pre-reduced YD, the pH dependent competition between YZ and YD was studied. Only YZ was oxidized below pH 7.2, but at pH above 7.2, the oxidation of YD became possible, and the formation of the Split S1 signal diminished. The onset of YD oxidation occurred with pKa approximately 8.0, while the Split S1 signal decreased with pKa approximately 7.9 demonstrating that the two tyrosines compete in this pH interval. The results reflect the formation and breaking of hydrogen bonds between YZ and D1-His190 (HisZ) and YD and D2-His190 (HisD), respectively. The oxidation of respective tyrosine at 5 K demands that the hydrogen bond is well-defined; otherwise, the low-temperature oxidation is not possible. The results are discussed in the framework of recent literature data and with respect to the different oxidation kinetics of YZ and YD.     

Nitric oxide-induced formation of the S-2 state in the oxygen-evolving complex of photosystem II from Synechococcus elongatus

In spinach photosystem II (PSII) membranes, the tetranuclear manganese cluster of the oxygen-evolving complex (OEC) can be reduced by incubation with nitric oxide at -30 degrees C to a state which is characterized by an Mn(2)(II, III) EPR multiline signal [Sarrou, J., Ioannidis, N., Deligiannakis, Y., and Petrouleas, V. (1998) Biochemistry 37, 3581-3587]. This state was recently assigned to the S(-)(2) state of the OEC [Schansker, G., Goussias, C., Petrouleas, V., and Rutherford, A. W. (2002) Biochemistry 41, 3057-3064]. On the basis of EPR spectroscopy and flash-induced oxygen evolution patterns, we show that a similar reduction process takes place in PSII samples of the thermophilic cyanobacterium Synechococcus elongatus at both -30 and 0 degrees C. An EPR multiline signal, very similar but not identical to that of the S(-)(2) state in spinach, was obtained with monomeric and dimeric PSII core complexes from S. elongatus only after incubation at -30 degrees C. The assignment of this EPR multiline signal to the S(-)(2) state is corroborated by measurements of flash-induced oxygen evolution patterns and detailed fits using extended Kok models. The small reproducible shifts of several low-field peak positions of the S(-)(2) EPR multiline signal in S. elongatus compared to spinach suggest that slight differences in the coordination geometry and/or the ligands of the manganese cluster exist between thermophilic cyanobacteria and higher plants.     

Mechanism of photoinhibition of photosynthetic water oxidation by Cl- depletion and F- substitution: oxidation of a protein residue

New evidence on the chloride requirement for photosynthetic O2 evolution has indicated that Cl- facilitates oxidation of the manganese cluster by the photosystem II (PSII) Tyr-Z+ radical. Illumination above 250 K of spinach PSII centers which are inhibited in O2 evolution by either Cl- depletion or F- substitution produces a new EPR signal which has magnetic characteristics similar to one recently discovered in samples inhibited by depletion of Ca2+ only [Boussac et al. (1989) Biochemistry 28, 8984; Sivaraja et al. (1989) Biochemistry 28, 9459]. The physiological roles of Cl- and Ca2+ in water oxidation are thus linked. The characteristics include a nearly isotropic g = 2.00 +/- 0.005, a symmetric line shape with line width = 16 +/- 2 mT, almost stoichiometric spin concentration relative to Try-D+ = 0.6 +/- 0.3 spin/PSII, very rapid spin relaxation at all temperatures measured down to 6 K, and an undetectable change in magnetic susceptibility upon formation (less than 1 mu B2). The signal appears to originate from a spin doublet (radical) in magnetic dipolar contact with a transition-metal ion, most probably a photooxidized protein residue within 10 A of the Mn cluster (Mn-proximal radical). It is distinct from the three other protein-bound radical-type electron donors found in the PSII reaction center: Tyr-D+, Tyr-Z+, and C+. This signal photoaccumulates to a stable level under continuous illumination at 270 K and decays only after illumination stops.(ABSTRACT TRUNCATED AT 250 WORDS)     

Reduction of the Mn cluster of the water-oxidizing enzyme by nitric oxide: formation of an S(-2) state

The manganese cluster of the oxygen-evolving enzyme of photosystem II is chemically reduced upon interaction with nitric oxide at -30 degrees C. The state formed gives rise to an S = 1/2 multiline EPR signal [Goussias, Ch., Ioannidis, N., and Petrouleas, V. (1997) Biochemistry 36, 9261] that is attributed to a Mn(II)- Mn(III) dimer [Sarrou, J., Ioannidis, N., Deligiannakis, Y., and Petrouleas, V. (1998) Biochemistry 37, 3581]. In this work, we sought to establish whether the state could be assigned to a specific, reduced S state by using flash oxymetry, chlorophyll a fluorescence, and electron paramagnetic resonance spectroscopy. With the Joliot-type O(2) electrode, the first maximum of oxygen evolution was observed on the sixth or seventh flash. Three saturating pre-flashes were required to convert the flash pattern characteristic of NO-reduced samples to that of the untreated control (i.e., O(2) evolution maximum on the third flash). Measurements of the S state-dependent level of chlorophyll fluorescence in NO-treated PSII showed a three-flash downshift compared to untreated controls. In the EPR study, the maximum S(2) multi-line EPR signal was observed after the fourth flash. The results from all three methods are consistent with the Mn cluster being in a redox state corresponding to an S(-2) state in a majority of centers after treatment with NO. We were unable to generate the Mn(II)-Mn(III) multi-line signal using hydrazine as a reductant; it appears that the valence distribution and possibly the structure of the Mn cluster in the S(-2) state are dependent on the nature of the reductant that is used.     

Ca2+ depletion from the photosynthetic water-oxidizing complex reveals photooxidation of a protein residue.

A new intermediate in the water-oxidizing reaction has been observed in spinach photosystem II (PSII) membranes that are depleted of Ca2+ from the site which is conformationally coupled to the manganese cluster comprising the water-oxidizing complex (WOC). It gives rise to a recently identified EPR signal (symmetric line shape with width 163 +/- 5 G, g = 2.004 +/- 0.005), which forms in samples inhibited either by depletion of Ca2+ [Boussac, A., Zimmerman, J.-L., & 28, 8984-8989; Sivaraja, M., Tso, J., & Dismukes, G.C. (1989) Biochemistry 28 9459-9464] or by substitution of Cl- by F- (Baumgarten, Philo, and Dismukes, submitted for publication). Further characterization of this EPR signal has revealed the following: (1) it forms independently of the local structure of the PSII acceptors; (2) it arises from photooxidation of a PSII species that donates an electron to Tyr-Z+ or to the Mn cluster in competition with an exogenous donor (DPC); (3) the Curie temperature dependence of the intensity suggests an isolated doublet ground state, attributable to a spin S = 1/2 radical; (4) the electron spin orientation relaxes 1000-fold more rapidly than typical for a free radical, exhibiting a strong temperature dependence of P1/2 (half-saturation power approximately T3.4) and a broad inhomogeneous line width; (5) it yields an undetectable change in the magnetic susceptibility upon formation by a laser flash; (6) it disappears in parallel with release of Mn during reduction with NH2OH, indicating that it forms only in the presence of the modified Mn cluster. (ABSTRACT TRUNCATED AT 250 WORDS)     

Characterization of the manganese O2-evolving complex and the iron-quinone acceptor complex in photosystem II from a thermophilic cyanobacterium by electron paramagnetic resonance and X-ray absorption spectroscopy

The Mn donor complex in the S1 and S2 states and the iron-quinone acceptor complex (Fe2+-Q) in O2-evolving photosystem II (PS II) preparations from a thermophilic cyanobacterium, Synechococcus sp., have been studied with X-ray absorption spectroscopy and electron paramagnetic resonance (EPR). Illumination of these preparations at 220-240 K results in formation of a multiline EPR signal very similar to that assigned to a Mn S2 species observed in spinach PS II, together with g = 1.8 and 1.9 EPR signals similar to the Fe2+-QA- acceptor signals seen in spinach PS II. Illumination at 110-160 K does not produce the g = 1.8 or 1.9 EPR signals, nor the multiline or g = 4.1 EPR signals associated with the S2 state of PS II in spinach; however, a signal which peaks at g = 1.6 appears. The most probable assignment of this signal is an altered configuration of the Fe2+-QA- complex. In addition, no donor signal was seen upon warming the 140 K illuminated sample to 215 K. Following continuous illumination at temperatures between 140 and 215 K, the average X-ray absorption Mn K-edge inflection energy changes from 6550 eV for a dark-adapted (S1) sample to 6551 eV for the illuminated (S2) sample. The shift in edge inflection energy indicates an oxidation of Mn, and the absolute edge inflection energies indicate an average Mn oxidation state higher than Mn(II). Upon illumination a significant change was observed in the shape of the features associated with 1s to 3d transitions. The S1 spectrum resembles those of Mn(III) complexes, and the S2 spectrum resembles those of Mn(IV) complexes. The extended X-ray absorption fine structure (EXAFS) spectrum of the Mn complex is similar in the S1 and S2 states. Simulations indicate O or N ligands at 1.75 +/- 0.05 A, transition metal neighbor(s) at 2.73 +/- 0.05 A, which are assumed to be Mn, and terminal ligands which are probably N and O at a range of distances around 2.2 A. The Mn-O bond length of 1.75 A and the transition metal at 2.7 A indicate the presence of a di-mu-oxo-bridged Mn structure. Simulations indicate that a symmetric tetranuclear cluster is unlikely to be present, while binuclear, trinuclear, or highly distorted tetranuclear structures are possible. The striking similarity of these results to those from spinach PS II suggests that the structure of the Mn complex is largely conserved across evolutionarily diverse O2-evolving photosynthetic species.     

Comparison of the structure of the manganese complex in the S1 and S2 states of the photosynthetic O2-evolving complex: an x-ray absorption spectroscopy study

A Mn-containing enzyme complex is involved in the oxidation of H2O to O2 in algae and higher plants. X-ray absorption spectroscopy is well suited for studying the structure and function of Mn in this enzyme complex. Results of X-ray K-edge and extended X-ray absorption fine structure (EXAFS) studies of Mn in the S1 and S2 states of the photosynthetic O2-evolving complex in photosystem II preparations from spinach are presented in this paper. The S2 state was prepared by illumination at 190 K or by illumination at 277 K in the presence of 3-(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU); these are protocols that limit the photosystem II reaction center to one turnover. Both methods produce an S2 state characterized by a multiline electron paramagnetic resonance (EPR) signal. An additional protocol, illumination at 140 K, produces as a state characterized by the g = 4.1 EPR signal. We have previously observed a shift to higher energy in the X-ray absorption K-edge energy of Mn upon advancement from the dark-adapted S1 state to the S2 state produced by illumination at 190 K [Goodin, D. B., Yachandra, V. K., Britt, R. D., Sauer, K., & Klein, M. P. (1984) Biochim. Biophys. Acta 767, 209-216]. The Mn K-edge spectrum of the 277 K illuminated sample is similar to that produced at 190 K, indicating that the S2 state is similar when produced at 190 or 277 K.(ABSTRACT TRUNCATED AT 250 WORDS)     

The first spectroscopic model for the S1 state multiline signal of the OEC

The parallel-mode electron paramagnetic resonance (EPR) spectrum of the S(1) state of the oxygen-evolving complex (OEC) shows a multiline signal centered around g=12, indicating an integer spin system. The series of [Mn(2)(2-OHsalpn)(2)] complexes were structurally characterized in four oxidation levels (Mn(II)(2), Mn(II)Mn(III), Mn(III)(2), and Mn(III)Mn(IV)). By using bulk electrolysis, the [Mn(III)Mn(IV)(2-OHsalpn)(2)(OH)] is oxidized to a species that contains Mn(IV) oxidation state as detected by X-ray absorption near edge spectroscopy (XANES) and that can be formulated as Mn(IV)(4) tetramer. The parallel-mode EPR spectrum of this multinuclear Mn(IV)(4) complex shows 18 well-resolved hyperfine lines center around g=11 with an average hyperfine splitting of 36 G. This EPR spectrum is very similar to that found in the S(1) state of the OEC. This is the first synthetic manganese model complex that shows an S(1)-like multiline spectrum in parallel-mode EPR.     

An evaluation of structural models for the photosynthetic water-oxidizing complex derived from spectroscopic and X-ray diffraction signatures

Four of the five intermediate oxidation states (S-states) in the catalytic cycle of water oxidation used by O2-evolving photoautotrophs have been previously characterized by EPR and/or ENDOR spectroscopy, with the first reports for the S0, S1, and S3 states available in just the last three years. The first electron density map of the Mn cluster derived from X-ray diffraction measurements of single crystals of photosystem II at 3.8-4.2 A resolution has also appeared this year. This wealth of new information has provided significant insight into the structure of the inorganic core (Mn4OxCa1Cl1-2), the Mn oxidation states, and the location and function of the essential Ca2+ cofactor within the water-oxidizing complex (WOC). We summarize these advances and provide a unified interpretation of debated structural proposals and Mn oxidation states, based on an integrated analysis of the published data, particularly from Mn X-ray absorption spectroscopy (XAS) and EPR/ENDOR data. Only three magnetic spin-exchange models for the inter-manganese interactions are possible from consideration of the EPR data for the S0, S1, S2 and S(-N) (NO-reduced) states. These models fall into one of three types denoted butterfly, funnel, or tetrahedron. A revised set of eight allowed chemical structures for the Mn4Ox core can be deduced that are shown to be consistent with both EPR and XAS. The popular "dimer-of-dimers" structural model is not compatible with the possible structural candidates. EPR data have identified two inter-manganese couplings that are sensitive to the S-state, suggesting two possible bridging sites for substrate water molecules. Spin densities derived from 55Mn hyperfine data together with Mn K-edge energies from Ca-depleted samples provide an internally consistent assignment for the Mn oxidation states of Mn4(3III,IV) for the S2 state. EPR and XAS data also provide a consistent picture, locating Ca2+ as an integral part of the inorganic core, probably via shared bridging ligands with Mn (aqua/hydroxo/carboxylato/chloro). XAS data reveal that the Ca2+ cofactor increases the Mn(1s-->4p) transition energy by 0.6-1 eV with minimal structural perturbation versus the Ca-depleted WOC. Thus, calcium binding appears to increase the Mn-ligand covalency by increasing electron transfer from shared ligands to Mn, suggesting a direct role for Ca2+ in substrate water oxidation. Consideration of both the XAS and the EPR data, together with reactivity studies on two model complexes that evolve O2, suggest two favored structure types as feasible models for the reactive S4 state that is precursor to the O2 evolution step. These are a calcium-capped "cuboidal" core and a calcium-capped "funnel" core.     

Proton equilibria in the manganese cluster of photosystem II control the intensities of the S(0) and S(2) state g approximately 2 electron paramagnetic resonance signals

We have studied the pH effect on the S(0) and S(2) multiline electron paramagnetic resonance (EPR) signals from the water-oxidizing complex of photosystem II. Around pH 6, the maximum signal intensities were detected. On both the acidic and alkaline sides of pH 6, the intensities of the EPR signals decreased. Two pKs were determined for the S(0) multiline signal; pK(1) = 4.2 +/- 0.2 and pK(2) = 8.0 +/- 0.1, and for the S(2) multiline signal the pKs were pK(1) = 4.5 +/- 0.1 and pK(2) = 7.6 +/- 0.1. The intensity of the S(0)-state EPR signal was partly restored when the pH was changed from acidic or alkaline pH back to pH approximately 6. In the S(2) state we observed partial recovery of the multiline signal when going from alkaline pH back to pH approximately 6, whereas no significant recovery of the S(2) multiline signal was observed when the pH was changed from acidic pH back to pH approximately 6. Several possible explanations for the intensity changes as a function of pH are discussed. Some are ruled out, such as disintegration of the Mn cluster or decay of the S states and formal Cl(-) and Ca(2+) depletion. The altered EPR signal intensities probably reflect the protonation/deprotonation of ligands to the Mn cluster or the oxo bridges between the Mn ions. Also, the possibility of decreased multiline signal intensities at alkaline pH as an effect of changed redox potential of Y(Z) is put forward.     

Decay products of the S(3) state of the oxygen-evolving complex of photosystem II at cryogenic temperatures. Pathways to the formation of the S = 7/2 S(2) state configuration

The water-oxidizing complex of photosystem II cycles through five oxidation states, denoted S(i)() (i = 0-4), during water oxidation to molecular oxygen, which appears at the (transient) S(4) state. The recent detection of bimodal EPR signals from the S(3) state [Matsukawa, T., Mino, H., Yoneda, D., Kawamori, A. (1999) Biochemistry 38, 4072-4077] has drawn significant attention to this critical state. An interesting property of the S(3) state is the sensitivity to near-IR (NIR) light excitation. Excitation of the S(3) state by near-IR light at cryogenic temperatures induces among other signals a derivative-shaped EPR signal at g= 5 [Ioannidis, N., and Petrouleas, V. (2000) Biochemistry 39, 5246-5254]. The signal bears unexpected similarities to a signal observed earlier in samples that had undergone multiple turnovers and subsequently had been stored at 77 K for a week or longer [Nugent, J. H. A., Turconi, S., and Evans, M. C. W. (1997) Biochemistry 36, 7086-7096]. Recently, both signals were assigned to an S = 7/2 configuration of the Mn cluster [Sanakis, Y., Ioannidis, N., Sioros, G., and Petrouleas, V. (2001) J. Am. Chem. Soc. 123, 10766-10767]. In the present study, we employ bimodal EPR spectroscopy to investigate the pathways of formation of this unusual state. The following observations are made: (i) The g = 5 signal evolves in apparent correlation with the diminution of the S(3) state signals during the slow (tens of hours to several days range) charge recombination of S(3) with Q(A)(-) at 77 K. The tyrosyl radical D* competes with S(3) for recombination with Q(A)(-), the functional redox couple at cryogenic temperatures inferred to be D*/D(-). Transfer to -50 degrees C and above results in the relaxation of the g = 5 to the multiline and g = 4.1 signals of the normal S(2) state. (ii) The transition of S(3) to the state responsible for the g = 5 signal can be reversed by visible light illumination directly at -30 degrees C or by illumination at 4.2 K followed by brief (2 min) transfer to -50 degrees C in the dark. The latter step is required in order to overcome an apparent thermal activation barrier (charge recombination appears to be faster than forward electron transfer at 4.2 K). (iii) The "g = 5" state can be reached in a few tens of minutes at 4.2 K by near-IR light excitation of the S(3) state. This effect is attributed to the transfer of the positive hole from the Mn cluster to a radical (probably tyr Z), which recombines much faster than the Mn cluster with Q(A)(-). (iv) The above properties strongly support the assignment of the configuration responsible for the g = 5 signal to a modified S(2) state, denoted S(2)'. Evidence supporting the assignment of the S(2)' to a proton-deficient S(2) configuration is provided by the observation that the spectrum of S(2) at pH 8.1 (obtained by illumination of the S(1) state at -30 degrees C) contains a g = 5 contribution.     

Does histidine 332 of the D1 polypeptide ligate the manganese cluster in photosystem II? An electron spin echo envelope modulation study

The tetranuclear manganese cluster in photosystem II is ligated by one or more histidine residues, as shown by an electron spin echo envelope modulation (ESEEM) study conducted with [(15)N]histidine-labeled photosystem II particles isolated from the cyanobacterium Synechocystis sp. strain PCC 6803 [Tang, X.-S., Diner, B. A., Larsen, B. S., Gilchrist, M. L., Jr., Lorigan, G. A., and Britt, R. D. (1994) Proc. Natl. Acad. Sci. U.S.A. 91, 704-708]. One of these residues may be His332 of the D1 polypeptide. Photosystem II particles isolated from the Synechocystis mutant D1-H332E exhibit an altered S(2) state multiline EPR signal that has more hyperfine lines and narrower splittings than the corresponding signal in wild-type PSII particles [Debus, R. J., Campbell, K. A., Peloquin, J. M., Pham, D. P., and Britt, R. D. (2000) Biochemistry 39, 470-478]. These D1-H332E PSII particles are also unable to advance beyond an altered S(2)Y(Z)(*) state, and the quantum yield for forming the S(2) state is very low, corresponding to an 8000-fold slowing of the rate of Mn oxidation by Y(Z)(*). These observations are consistent with His332 being close to the Mn cluster and modulating the redox properties of both the Mn cluster and tyrosine Y(Z). To determine if D1-His332 ligates the Mn cluster, we have conducted an ESEEM study of D1-H332E PSII particles. The histidyl nitrogen modulation observed near 5 MHz in ESEEM spectra of the S(2) state multiline EPR signal of wild-type PSII particles is substantially diminished in D1-H332E PSII particles. This result is consistent with ligation of the Mn cluster by D1-His332. However, alternate explanations are possible. These are presented and discussed.     

Spectroscopic studies of the manganese complex of Photosystem II

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

Histidine 332 of the D1 polypeptide modulates the magnetic and redox properties of the manganese cluster and tyrosine Y(Z) in photosystem II

An electron spin-echo envelope modulation study [Tang, X.-S., Diner, B. A., Larsen, B. S., Gilchrist, M. L., Jr., Lorigan, G. A., and Britt, R. D. (1994) Proc. Natl. Acad. Sci. U.S.A. 91, 704-708] and a recent Fourier transform infrared study [Noguchi, T., Inoue, Y., and Tang, X.-S. (1999) Biochemistry 38, 10187-10195], both conducted with [(15)N]histidine-labeled photosystem II particles, show that at least one histidine residue coordinates the O(2)-evolving Mn cluster in photosystem II. Evidence obtained from site-directed mutagenesis studies suggests that one of these residues may be His332 of the D1 polypeptide. The mutation D1-H332E is of particular interest because cells of the cyanobacterium Synechocystis sp. PCC 6803 that contain this mutation evolve no O(2) but appear to assemble Mn clusters in nearly all photosystem II reaction centers [Chu, H.-A., Nguyen, A. P. , and Debus, R. J. (1995) Biochemistry 34, 5859-5882]. Photosystem II particles isolated from the Synechocystis D1-H332E mutant are characterized in this study. Intact D1-H332E photosystem II particles exhibit an altered S(2) state multiline EPR signal that has more hyperfine lines and narrower splittings than the S(2) state multiline EPR signal observed in wild-type PSII particles. However, the quantum yield for oxidizing the S(1) state Mn cluster is very low, corresponding to an 8000-fold slowing of the rate of Mn oxidation by Y(Z)(*), and the temperature threshold for forming the S(2) state is approximately 100 K higher than in wild-type PSII preparations. Furthermore, the D1-H332E PSII particles are unable to advance beyond the Y(Z)(*)S(2) state, as shown by the accumulation of a narrow "split" EPR signal under multiple turnover conditions. In Mn-depleted photosystem II particles, charge recombination between Q(A)(*)(-) and Y(Z)(*) in D1-H332E is accelerated in comparison to wild-type, showing that the mutation alters the redox properties of Y(Z) in addition to those of the Mn cluster. These results are consistent with D1-His332 being located near the Mn-Y(Z) complex and perhaps ligating Mn.     

pH-dependent charge equilibria between tyrosine-D and the S states in photosystem II. Estimation of relative midpoint redox potentials

The effect of protonation events on the charge equilibrium between tyrosine-D and the water-oxidizing complex in photosystem II has been studied by time-resolved measurements of the EPR signal IIslow at room temperature. The flash-induced oxidation of YD by the water-oxidizing complex in the S2 state is a monophasic process above pH 6.5 and biphasic at lower pHs, showing a slow and a fast phase. The half-time of the slow phase increases from about 1 s at pH 8.0 to about 20 s at pH 5.0, whereas the half-time of the fast phase is pH independent (0.4-1 s). The dark reduction of YD+ was followed by measuring the decay of signal IIslow at room temperature. YD+ decays in a biphasic way on the tens of minutes to hours time scale. The minutes phase is due to the electron transfer to YD+ from the S0 state of the water-oxidizing complex. The half-time of this process increases from about 5 min at pH 8.0 to 40 min at pH 4.5. The hours phase of YD+ has a constant half-time of about 500 min between pH 4.7 and 7.2, which abruptly decreases above pH 7.2 and below pH 4.7. This phase reflects the reduction of YD+ either from the medium or by an unidentified redox component of PSII in those centers that are in the S1 state. The titration curve of the half-times for the oxidation of YD reveals a proton binding with a pK around 7.3-7.5 that retards the electron transfer from YD to the water-oxidizing complex. We propose that this monoprotic event reflects the protonation of an amino acid residue, probably histidine-190 on the D2 protein, to which YD is hydrogen bonded. The titration curves for the oxidation of YD and for the reduction of YD+ show a second proton binding with pK approximately 5.8-6.0 that accelerates the electron transfer from YD to the water-oxidizing complex and retards the process in the opposite direction. This protonation most probably affects the water-oxidizing complex. From the measured kinetic parameters, the lowest limits for the equilibrium constants between the S0YD+ and the S1YD as well as between the S1YD+ and S2YD states were estimated to be 5 and 750-1000, respectively.(ABSTRACT TRUNCATED AT 400 WORDS)     

High and low reduction potential 4Fe-4S clusters in Azotobacter vinelandii (4Fe-4S) 2ferredoxin I. Influence of the polypeptide on the reduction potentials.

Azotobacter vinelandii (4Fe-4S)2 ferredoxin I (Fd I) is an electron transfer protein with Mr equals 14,500 and Eo equals -420 mv. It exhibits and EPR signal of g equals 2.01 in its isolated form. This resonance is almost identical with the signal that originates from a "super-oxidized" state of the 4Fe-4S cluster of potassium ferricyanide-treated Clostridium ferredoxin. A cluster that exhibits this EPR signal at g equals 2.01 is in the same formal oxidation state as the cluster in oxidized Chromatium High-Potential-Iron-Protein (HiPIP). On photoreduction of Fd I with spinach chloroplast fragments, the resonance at g equals 2.01 vanishes and no EPR signal is observed. This EPR behavior is analogous to that of reduced HiPIP, which also fails to exhibit an EPR spectrum. These characteristics suggest that a cluster in A. vinelandii Fd I functions between the same pair of states on reduction as does the cluster in HiPIP, but with a midpoint reduction potential of -420 mv in contrast to the value of +350 mv characteristic of HiPIP. Quantitative EPR and stoichoimetry studies showed that only one 4Fe-4S cluster in this (4Fe-4S)2 ferredoxin is reduced. Oxidation of Fd I with potassium ferricyanide results in the uptake of 1 electron/mol as determined by quantitative EPR spectroscopy. This indicates that a cluster in Fd I shows no electron paramagnetic resonance in the isolated form of the protein accepts an electron on oxidation, as indicated by the EPR spectrum, and becomes paramagnetic. The EPR behavior of this oxidizable cluster indicates that it also functions between the same pair of oxidation states as does the Fe-S cluster in HiPIP. The midpoint reduction potential of this cluster is approximately +340 mv. A. vinelandii Fd I is the first example of an iron-sulfur protein which contains both a high potential cluster (approximately +340 mv) and a low potential cluster (-420 mv). Both Fe-S clusters appear to function between the same pair of oxidation states as the single Fe-S cluster in Chromatium HiPIP, although the midpoint reduction potentials of the two clusters are approximately 760 mv different.