Interaction of the high-spin Fe atom in the photosystem II reaction center with the quinones QA and QB in purified oxygen-evolving PS II reaction center complex and in PS II particles

EPR signals in the high-spin region were studied at 10 K in photosystem II (PS II) particles and in a purified oxygen-evolving PS II reaction center complex under oxidizing conditions. PS II particles showed EPR peaks at g = 8.0 and 5.6, confirming the recent report by Petrouleas and Diner [(1986) Biochim. Biophys. Acta 849, 264-275]. Addition of 3-(3',4'-dichlorophenyl)-1,1-dimethylurea (DCMU) or o-phenanthroline shifted the peaks to be closer to g = 6.0 depending on the medium pH. On the other hand, the PS II reaction center complex showed peaks at g = 6.1 and 7.8, and at g = 6.1 and 6.4, in the absence and presence of o-phenanthroline, respectively. All these peaks were found to be decreased by the illumination at 10 K. These results suggest that the high-spin signals are due to Q₄₀₀, Fe(III) atom interacting with the PS II primary electron acceptor quinone Q_A as reported and that the Fe atom also interacts with the secondary acceptor quinone Q_B. This interaction seems to induce the highly asymmetric ligand coordination of the Fe atom and to be affected by DCMU and o-phenanthroline in a somewhat different manner.     

A new EPR signal attributed to the primary plastosemiquinone acceptor in Photosystem II

A study of signals, light-induced at 77 K in O₂-evolving Photosystem II (PS II) membranes showed that the EPR signal that has been attributed to the semiquinone-iron form of the primary quinone acceptor, Q^?_AFe, at g = 1.82 was usually accompanied by a broad signal at g = 1.90. In some preparations, the usual g = 1.82 signal was almost completely absent, while the intensity of the g = 1.90 signal was significantly increased. The g = 1.90 signal is attributed to a second EPR form of the primary semiquinone-iron acceptor of PS II on the basis of the following evidence. (1) The signal is chemically and photochemically induced under the same conditions as the usual g = 1.82 signal. (2) The extent of the signal induced by the addition of chemical reducing agents is the same as that photochemically induced by illumination at 77 K. (3) When the g = 1.82 signal is absent and instead the g = 1.90 signal is present, illumination at 200 K of a sample containing a reducing agent results in formation of the characteristic split pheophytin^? signal, which is thought to arise from an interaction between the photoreduced pheophytin acceptor and the semiquinone-iron complex. (4) Both the g = 1.82 and g = 1.90 signals disappear when illumination is given at room temperature in the presence of a reducing agent. This is thought to be due to a reduction of the semiquinone to the nonparamagnetic quinol form. (5) Both the g = 1.90 and g = 1.82 signals are affected by herbicides which block electron transfer between the primary and secondary quinone acceptors. It was found that increasing the pH results in an increase of the g = 1.90 form, while lowering the pH favours the g = 1.82 form. The change from the g = 1.82 form to the g = 1.90 form is accompanied by a splitting change in the split pheophytin^? signal from approx. 42 to approx. 50 G. Results using chloroplasts suggest that the g = 1.90 signal could represent the form present in vivo.     

The iron-quinone acceptor complex in Rhodospirillum rubrum chromatophores studied by EPR

A new EPR signal is reported in Rhodospirillum rubrum chromatophores. The signal is attributed to Q⁻_BFe²⁺, the semiquinone-iron complex of the secondary quinone electron acceptor, on the basis of the following observations. (1) It is induced by a single laser flash given a room temperature and is stable. (2) It is present after odd-numbered flashes and absent after even-numbered flashes when a series of flashes is given. (3) When it is already present, low-temperature illumination results in the disappearance of the signal due to formation of the Q⁻_AFe²⁺Q⁻_B state. (4) Its formation is inhibited by the presence of orthophenanthroline at normal values of pH. The Q⁻_BFe²⁺ signal has two main features, one at g = 1.93 and the other at g = 1.82. The two features have different microwave power and temperature dependences, with the g = 1.82 signal being more difficult to saturate and requiring lower temperatures to be observable. Raising the pH leads to an increase in the g = 1.82 feature, while the g = 1.93 signal decreases in amplitude. It is suggested that the two parts of the signal may represent two EPR forms due to structural heterogeneity. The low-field feature of the Q⁻_BFe²⁺ signal shifts to lower field as the pH is raised and a pK for this change seems to occur at pH 9.4. The Q⁻_AFe²⁺ signal at g = 1.88 also shifts as the pH is increased; however, the shift is less marked than that seen for Q⁻_BFe²⁺, the shift is to higher field and the range over which it occurs is wider and depends upon the temperature of Q⁻_AFe²⁺ formation. This effect may be due to a pK on a protein group being shifted to higher pH by the presence of Q⁻_A. ortho-Phenanthroline broadens and shifts the Q⁻_AFe²⁺ signal. The inhibition of electron transfer between Q⁻_A and Q_B by ortho-phenanthroline becomes less effective at high pH. The new Q⁻_BFe²⁺ signal is unlike other semiquinone-iron signals reported in the literature in bacteria; however, it is remarkably similar to the Q⁻_BFe²⁺ signal reported in Photosystem II.     

Peroxynitrite inhibits electron transport on the acceptor side of higher plant photosystem II

Peroxynitrite is a strong oxidant that has been proposed to form in chloroplasts. The interaction between peroxynitrite and photosystem II (PSII) has been investigated to determine whether this oxidant could be a hazard for PSII. Peroxynitrite is shown to inhibit oxygen evolution in PSII membranes in a dose-dependent manner. Analyses by PAM fluorimetry and EPR spectroscopy have demonstrated that the inhibition target of peroxynitrite is on the PSII acceptor side. In the presence of the herbicide DCMU, the chlorophyll (Chl) a fluorescence induction curve is inhibited by peroxynitrite, but the slow phase of the Chl a fluorescence decay does not change. EPR studies demonstrate that the Signal II_slow and Signal II_fast of peroxynitrite-treated Tris-washed PSII membranes are induced at room temperature, implying that the redox active tyrosines Y_Z and Y_D of PSII are not significantly nitrated. A featureless EPR signal with a g value of approximately 2.0043 ± 0.0003 and a line width of 10 ± 1 G is induced under continuous illumination in the presence of peroxynitrite. This new EPR signal corresponds with the semireduced plastoquinone Q_A in the absence of magnetic interaction with the non-heme Fe²⁺. We conclude that peroxynitrite impairs PSII electron transport in the Q_AFe²⁺ niche.     

Low-temperature electron transfer suggests two types of QA in intact photosystem II

The correlation between the reduction of Q_A and the oxidation of Tyr_Z or Car/Chl_Z/Cyt_b559 in spinach PSII enriched membranes induced by visible light at 10 K is studied by using electron paramagnetic resonance spectroscopy. Similar g = 1.95-1.86 Q_A^-•EPR signals are observed in both Mn-depleted and intact samples, and both signals are long lived at low temperatures. The presence of PPBQ significantly diminished the light induced EPR signals from Q_A^-•, Car^+•/Chl^+• and oxidized Cyt_b559, while enhancing the amplitude of the S₁Tyr_Z• EPR signal in the intact PSII sample. The quantification and stability of the g = 1.95-1.86 EPR signal and signals arising from the oxidized Tyr_Z and the side-path electron donors, respectively, indicate that the EPR-detectable g = 1.95-1.86 Q_A^-• signal is only correlated to reaction centers undergoing oxidation of the side-path electron donors (Car/Chl_Z/Cyt_b559), but not of Tyr_Z. These results imply that two types of Q_A^-• probably exist in the intact PSII sample. The structural difference and possible function of the two types of Q_A are discussed.     

Effects of trypsin upon EPR signals arising from components of the donor side of Photosystem II

EPR signals from components functioning on the electron donor side of Photosystem II (PS II) have been monitored in PS II membranes isolated from spinach chloroplasts after treatment with trypsin at pH 7.5 and pH 6.0. The following information has been obtained. (1) The multiline manganese signal, the g = 4.1 signal and Signal II_slow are lost with trypsin treatment at pH 7.5, but not at pH 6.0. (2) At pH 7.5 the multiline S₂ signal and the g = 4.1 signal are lost with approximately the same dependency on the incubation time with trypsin. At pH 6.0 trypsin treatment is known to block electron transfer between Q_A and Q_B (the first and the second quinone electron acceptors, respectively) allowing only a single turnover to occur. Under these conditions both the g = 4.1 signal and the multiline signal are induced by illumination at 200 K and their amplitudes are almost the same as in untreated samples. These results are interpreted as indicating that the g = 4.1 signal arises from a side path donor or from S₂ itself rather than a carrier functioning between the S states and the reaction center as previously suggested. (3) Cytochrome b-559 is converted to its oxidized low-potential form by trypsin treatment at both values of pH. At pH 6.0 the S-state turnover still occurs indicating that the presence of reduced high-potential cytochrome b-559 is not necessary for this process.     

EPR studies of the oxygen-evolving enzyme of Photosystem II

The light-induced EPR multiline signal is studied in O₂-evolving PS II membranes. The following results are reported: (1) Its amplitude is shown to oscillate with a period of 4, with respect to the number of flashes given at room temperature (maxima on the first and fifth flashes). (2) Glycerol enhances the signal intensity. This effect is shown to come from changes in relaxation properties rather than an increase in spin concentration. (3) Deactivation experiments clearly indicate an association with the S₂ state of the water-oxidizing enzyme. A signal at g = 4.1 with a linewidth of 360 G is also reported and it is suggested that this arises from an intermediate donor between the S states and the reaction centre. This suggestion is based on the following observations: (1) The g = 4.1 signal is formed by illumination at 200 K and not by flash excitation at room temperature, suggesting that it arises from an intermediate unstable under physiological conditions. (2) The formation of the g = 4.1 signal at 200 K does not occur in the presence of DCMU, indicating that more than one turnover is required for its maximum formation. (3) The g = 4.1 signal decreases in the dark at 220 K probably by recombination with Q^?_AFe. This recombination occurs before the multiline signal decreases, indicating that the g = 4.1 species is less stable than S₂. (4) At short times, the decay of the g = 4.1 signal corresponds with a slight increase in the multiline S₂ signal, suggesting that the loss of the g = 4.1 signal results in the disappearance of a magnetic interaction which diminishes the multiline signal intensity. (5) Tris-washed PS II membranes illuminated at 200 K do not exhibit the signal.     

Evidence for an anisotropic magnetic interaction between the (bacteriopheophytin) intermediary acceptor and the first quinone acceptor in bacterial photosynthesis

We have investigated electron spin polarization effects occurring in protonated and perdeuterated reaction centers of Rhodospirillum rubrum with electron spin resonance at 9 and 35 GHz (X- and Q-band). As for Rhodopseudomonas sphaeroides strains 2.4.1 and R-26 (Gast, P. and Hoff, A.J. (1979) Biochim. Biophys. Acta 548, 520–535; Gast, P., Mushlin, R.A. and Hoff, A.J. (1982) J. Phys. Chem. 86, 2886–2891), electron spin polarization effects of the prereduced first quinone acceptor Q^?_A in R. rubrum are strongly nonuniform. This nonuniformity is due to an anisotropic magnetic coupling between the intermediary bacteriopheophytin acceptor (I^?) and Q^?_A. It is argued that the anisotropy is too strong to arise solely from an anisotropy in the exchange interaction between I^? and Q^?_A and that dipolar contributions to the magnetic coupling between I^? and Q^?_A are important. The anisotropy in the magnetic coupling for reaction centers of Rps. sphaeroides strains 2.4.1 and R-26 is different from that of R. rubrum wild type. The combination of the 4-fold higher resolution at Q-band and the line narrowing upon deuteration has enabled us to obtain the principal g values and two hyperfine interaction constants of the reduced first quinone acceptor Q^?_A. The principal g values are g_x = 2.0067, g_y = 2.0056 and g_z = 2.0024; the hyperfine constant of the CH₂ group at position 1 is 1.6 G and that of the CH₃ group at position 2 is 2.1 G. These values are close to those found for ubisemiquinone in vitro (Okamura, M.Y., Debus, R.J., Isaacson, R.A. and Feher, G. (1980) Fed. Proc. 39, 1802; Hales, B.J. (1975) J. Am. Chem. Soc. 97, 5993–5997).     

Radical pair interactions in spinach chloroplasts

Time-resolved EPR studies were done on broken spinach chloroplasts under reducing conditions at low temperature (10 K). A dramatic dependence of signal dynamics and lineshape in the g 2.00 region on the reduction state of Photosystem I is demonstrated. Computer simulations of the spin-polarized lineshapes obtained in this work suggest that the primary electron acceptor in Photosystem I, a species known as A₁, could be a chlorophyll a dimer.     

Oxidation-reduction properties of the electron acceptors of Photosystem II. II. Redox titration at various pH values of the flash-induced formation of C550 in Chlamydomonas Photosystem II particles lacking the secondary quinone electron acceptor

Redox titrations of the flash-induced formation of C550 (a linear indicator of Q^?) were performed between pH 5.9 and 8.3 in Chlamydomonas Photosystem II particles lacking the secondary electron acceptor, B. One-third of the reaction centers show a pH-dependent midpoint potential (E_m,7.5) = ? 30 mV) for redox couple $\text{Q}\text{Q}{}^{\mathrm{?}}$, which varies by ?60 mV/pH unit. Two-thirds of the centers show a pH-independent midpoint potential (E_mm = + 10 mV) for this couple. The elevated pH-independent E_m suggests that in the latter centers the environment of Q has been modified such as to stabilize the semiquinone anion, Q^?. The midpoint potentials of the centers having a pH-dependent E_m are within 20 mV of those observed in chloroplasts having a secondary electron acceptor. It appears therefore that the secondary electron acceptor exerts little influence on the E_m of $\text{Q}\text{Q}{}^{\mathrm{?}}$. An EPR signal at g 1.82 has recently been attributed to a semiquinone-iron complex which comprises Q^?. The similar redox behavior reported here for C550 and reported by others (Evans, M.C.W., Nugent, J.H.A., Tilling, L.A. and Atkinson, Y.E. (1982) FEBS Lett. 145, 176–178) for the g 1.82 signal in similar Photosystem II particles confirm the assignment of this EPR signal to Q^?. At below ?200 mV, illumination of the Photosystem II particles produces an accumulation of reduced pheophytin (Ph^?). At ?420 mV Ph^? appears with a quantum yield of 0.006–0.01 which in this material implies a lifetime of 30–100 ns for the radical pair P-680⁺Ph^?.     

Comparison of the electron spin polarized spectrum found in plant photosystem I and in iron-depleted bacterial reaction centers with time-resolved K-band EPR; evidence that the photosystem I acceptor A1 is a quinone

The suggestion that the electron acceptor A₁ in plant photosystem I (PSI) is a quinone molecule is tested by comparisons with the bacterial photosystem. The electron spin polarized (ESP) EPR signal due to the oxidized donor and reduced quinone acceptor (P ₈₇₀ ⁺ Q^-) in iron-depleted bacterial reaction centers has similar spectral characteristics as the ESP EPR signal in PSI which is believed to be due to P ₇₀₀ ⁺ A ₁ ^- , the oxidized PSI donor and reduced A₁. This is also true for better resolved spectra obtained at K-band (24 GHz). These same spectral characteristics can be simulated using a powder spectrum based on the known g-anisotropy of reduced quinones and with the same parameter set for Q^- and A₁ ^-. The best resolution of the ESP EPR signal has been obtained for deuterated PSI particles at K-band. Simulation of the A₁ ^- contribution based on g-anisotropy yields the same parameters as for bacterial Q^- (except for an overall shift in the anisotropic g-factors, which have previously been determined for Q^-). These results provide evidence that A₁ is a quinone molecule. The electron spin polarized signal of P₇₀₀ ⁺ is part of the better resolved spectrum from the deuterated PSI particles. The nature of the P₇₀₀ ⁺ ESP is not clear; however, it appears that it does not exhibit the polarization pattern required by mechanisms which have been used so far to explain the ESP in PSI.Abbreviations hf hyperfine - A₀ A₀ acceptor of photosystem I - A₁ A₁ acceptor of photosystem I - Brij-58 polyoxyethylene 20 cetyl ether - CP1 photosystem I particles which lack ferridoxin acceptors - ESP electron spin polarized - EPR electron paramagnetic resonance - I intermediary electron acceptor, bacteriopheophytin - LDAO lauryldimethylamine - N-oxide, P₇₀₀ primary electron donor of photosystem I - PSI photosystem I - P₇₀₀ ^T triplet state of primary donor of photosystem I - P₈₇₀ primary donor in R. sphaeroides reaction center - Q quinore-acceptor in photosynthetic bacteria - RC reaction center     

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

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

Photosystem I charge separation in the absence of centers A and B. II. ESR spectral characterization of center ‘X’ and correlation with optical signal ‘A2’

The Photosystem I electron acceptor complex was characterized by optical flash photolysis and electron spin resonance (ESR) spectroscopy after treatment of a subchloroplast particle with lithium dodecyl sulfate (LDS). The following properties were observed after 60 s of incubation with 1% LDS followed by rapid freezing. (i) ESR centers A and B were not observed during or after illumination of the sample at 19 K, although the P-700⁺ radical at g = 2.0026 showed a large, reversible light-minus-dark difference signal. (ii) Center ‘X’, characterized by g factors of 2.08, 1.88 and 1.78, exhibited reversible photoreduction at 8 K in the absence of reduced centers A and B. (iii) The backreaction kinetics at 8 K between P-700, observed at g = 2.0026, and center X, observed at g = 1.78, was 0.30 s. (iv) The amplitudes of the reversible g = 2.0026 radical observed at 19 K and the 1.2 ms optical 698 nm transient observed at 298 K were diminished to the same extent when treated with 1% LDS at room temperature for periods of 1 and 45 min. We interpret the strict correlation between the properties and lifetimes of the optical P-700⁺ A⁻₂ reaction pair and the ESR P-700⁺ center X⁻ reaction pair to indicate that signal A₂ and center X represent the same iron-sulfur center in Photosystem I.     

Spectroscopic characterization of a semi-stable, charge-separated state in Cu-substituted reaction centers from Rhodobacter sphaeroides

In reaction centers from Rhodobacter sphaeroides exposed to continuous illumination in the presence of an inhibitor of the Q_A⁻ to Q_B electron transfer, a semi-stable, charge-separated state was formed with halftimes of formation and decay of several minutes. When the non-heme iron was replaced by Cu²⁺, the decay of the semi-stable, charge-separated state became much slower than in centers with bound Fe²⁺ with about the same rate constant for formation. In Cu²⁺-substituted reaction centers, the semi-stable state was associated with an EPR signal, significantly different from that observed after chemical reduction of the acceptor-side quinone or after illumination at low temperature, but similar to that of an isolated Cu²⁺ in the absence of magnetic interaction. The EPR results, obtained with Cu²⁺-substituted reaction centers, suggest that the slow kinetics of formation and decay of the charge-separated, semi-stable state is associated with a structural rearrangement of the acceptor side and the immediate environment of the metal-binding site.     

Comparative EPR and thermoluminescence study of anoxic photoinhibition in Photosystem II particles

Photosystem II particles were exposed to 800 W m^–2 white light at 20 °C under anoxic conditions. The F_o level of fluorescence was considerably enhanced indicating formation of stable-reduced forms of the primary quinone electron acceptor, Q_A. The F_m level of fluorescence declined only a little. The g=1.9 and g=1.82 EPR forms characteristic of the bicarbonate-bound and bicarbonate-depleted semiquinone-iron complex, Q_A ^–Fe²⁺, respectively, exhibited differential sensitivity against photoinhibition. The large g=1.9 signal was rapidly diminished but the small g=1.82 signal decreased more slowly. The S₂-state multiline signal, the oxygen evolution and photooxidation of the high potential form of cytochrome b-559 were inhibited approximately with the same kinetics as the g=1.9 signal. The low potential form of oxidized cytochrome b-559 and Signal II_slow arising from Tyr_D ⁺ decreased considerably slower than the g=1.9 semiquinone-iron signal. The high potential form of oxidized cytochrome b-559 was diminished faster than the low potential form. Photoinhibition of the g=1.9 and g=1.82 forms of Q_A was accompanied with the appearance and gradual saturation of the spin-polarized triplet signal of P 680. The amplitude of the radical signal from photoreducible pheophytin remained constant during the 3 hour illumination period. In the thermoluminescence glow curves of particles the Q band (S₂Q_A ^– charge recombination) was almost completely abolished. To the contrary, the C band (Tyr_D ⁺Q_A ^– charge recombination) increased a little upon illumination. The EPR and thermoluminescence observations suggest that the Photosystem II reaction centers can be classified into two groups with different susceptibility against photoinhibition.Abbreviations C band thermoluminescence band associated with Tyr-D⁺Q _a ^– charge recombination - Chl chlorophyll - DCMU 3-(3,4-dichlorophenyl)-1,1-dimethylurea - EPR electron paramagnetic resonance - F_o initial fluorescence - F_m maximum fluorescence - Q band thermoluminescence band originating from S₂Q _a -charge recombination - Q _a the primary quinone electron acceptor of PS II - P 680 the primary electron donor chlorophyll of PS II - S₂ oxidation state of the water-splitting system - Phe pheophytin - TL thermoluminescence - Tyr _d redox active tyrosine-160 of the D₂ protein     

A relationship between the midpoint potential of the primary acceptor and low temperature photochemistry in photosystem II

Redox titrations of the photo-induced pheophytin EPR signal in Photosystem II show two transitions which reflect the redox state of Q. The high potential wave (E_m ? ?50 mV) can be photo-induced at 5 K and 77 K. The low potential wave (E_m ? ?275 mV) required illumination at 200 K. This indicates the presence of two kinds of PS-II reaction centres differing in terms of the competence of their donors at low temperature and the E_m-values of their acceptors. Measurements of the semiquinone-iron acceptor also demonstrate functional heterogeneity at low temperature. This is the first observation of the semiquinone-iron acceptor in a non-mutant species.     

Hydroxylamine as an inhibitor between Z and P680 in photosystem II

Upon addition of hydroxylamine to chloroplasts or photosystem II preparations, the EPR signal of Z^? disappears and a new signal is observed. From its shape and g-value this signal is identified with the oxidized reaction center chlorophyll, P680⁺. The decay of P680⁺ occurs with a halftime of ? 200 μs and apparently is the result of a back reaction with the reduced form of the primary acceptor, Q_A. This mode of hydroxylamine inhibition is reversible. These observations indicate that hydroxylamine, in addition to its well known inhibitory action on the oxygen evolving complex, is also able to disrupt physiological electron flow to P680 itself.     

On the depletion and reconstitution of both QA and metal in reaction centers of the photosynthetic bacterium Rb. sphaeroides R-26

Four possible ways to prepare Q_A-depleted, Fe-depleted and Q_A-reconstituted RCs were studied: (1) first depleting the Fe, then depleting Q_A and finally reconstituting Q_A (D-Fe, D-Q, R-Q), (2) first depleting Q_A, then depleting the Fe and finally reconstituting Q_A (D-Q, D-Fe, R-Q), (3) first depleting Q_A, then reconstituting Q_A and finally depleting Fe (D-Q, R-Q, D-Fe), (4) first depleting Q_A, then depleting the Fe and reconstituting Q_A in the same step (D-Q, D-Fe-R-Q). Our results showed that: method (1) results in the irreversible loss of photochemical activity; method (2) and (3) result in low recovery of the photochemical activity and poor yield of Fe-depleted, Q_A-reconstituted RCs; method (4) gives surprisingly good results. This method allows for the first time to prepare the Q_A-depleted, Fe-depleted, Q_A-reconstituted RCs with high recovery of the photochemical activity and good yield. The sample has 98% of photochemical activity (yield of P⁺ Q_A ^-) compared with that of the native RCs and shows strong polarization of the EPR signal of Q_A ^- under continuous illumination at 5K. The decay halftime of I^- is slow (5 ns) compared with that of the native RCs, but it is the same as that measured for the RCs from which only iron is removed. These results indicate that the depletion of iron and the reconstitution of Q_A have been successful. Reconstitution of the Q_A-depleted, Fe-depleted and Q_A-reconstituted RCs with Zn²⁺ gives also the spin-polarized Q_A ^-, and yields the same decay of I^- (halftime 200 ps) as that of the native RCs.Abbreviations LDAO lauryldimethylamine N-oxide - EDTA ethylenediaminetetraacetic acid - BSA albumin bovine - TL buffer 10 mM Tris.HCl, 0.1% LDAO and 0.1 mM EDTA     

Biochemical and biophysical studies on cytochrome c oxidase. XVII. An epr study of the photodissociation of cytochrome a32+ · CO

1. The photodissociation reaction of the cytochrome c oxidase-CO compound was studied by EPR at 15 °K. Illumination with white light at both room and liquid N₂ temperatures of the partially reduced cytochrome c oxidase (2 electrons per 4 metals) in the presence of CO, causes the appearance of a rhombic (g_x = 6.60, g_y = 5.37) high-spin heme signal.This signal disappears completely upon darkening of the sample and reappears upon illumination at room temperature; accordingly the photolytic process is reversible. Under these conditions, no great changes in the intensities are observed, neither of the copper signal at g = 2, nor of the low-spin heme signal at g = 3, 2.2 and 1.5.2. In the presence of ferricyanide (2 mM) and CO, both the low-spin heme signal (g = 3.0, 2.2 and 1.5) and the copper signal of the partially reduced enzyme have intensities about equal to those of the completely oxidized enzyme in the absence of CO. Upon illumination of the carboxy-cytochrome c oxidase in the presence of ferricyanide, it was found that the rhombic high-spin heme signal appears without affecting appreciably the copper of low-spin heme signals. Thus, in the presence of ferricyanide the EPR-detectable paramagnetism of the illuminated carboxy-cytochrome c oxidase is higher than in the untreated oxidized enzyme.3. The membrane-bound cytochrome c oxidase reduced with NADH in the presence of CO and subsequently oxidized with ferricyanide shows a similar rhombic high-spin heme signal (g_x = 6.62, g_y = 5.29) upon illumination at room temperature. This signal disappears completely upon darkening and reappears upon illumination at room temperature.     

EPR detection of a cryogenically photogenerated intermediate in photosynthetic oxygen evolution

In Photosystem II preparations at low temperature we were able to generate and trap an intermediate state between the S₁ and S₂ states of the Kok scheme for photosynthetic oxygen evolution. Illumination of dark-adapted, oxygen-evolving Photosystem II preparations at 140 K produces a 320-G-wide EPR signal centered near g = 4.1 when observed at 10 K. This signal is superimposed on a 5-fold larger and somewhat narrower background signal; hence, it is best observed in difference spectra. Warming of illuminated samples to 190 K in the dark results in the disappearance of the light-induced g = 4.1 feature and the appearance of the multiline EPR signal associated with the S₂ state. Low-temperature illumination of samples prepared in the S₂ state does not produce the g = 4.1 signal. Inhibition of oxygen evolution by incubation of PS II preparations in 0.8 M NaCl buffer or by the addition of 400 μM NH₂OH prevents the formation of the g = 4.1 signal. Samples in which oxygen evolution is inhibited by replacement of Cl^? with F^? exhibit the g = 4.1 signal when illuminated at 140 K, but subsequent warming to 190 K neither depletes the amplitude of this signal nor produces the multiline signal. The broad signal at g = 4.1 is typical for a $\text{S =}\text{5}\text{2}$ spin system in a rhombic environment, suggesting the involvement of non-heme Fe in photosynthetic oxygen evolution.