Kinetic and spectroscopic properties of the YZ* radical in Ca2+- and Cl--depleted photosystem II preparations

Depletion of Ca2+ and/or Cl- ions from PSII membranes blocks the electron-transfer reactions that precede O2 evolution on the oxidizing side of the enzyme. Illumination of these inhibited preparations at 273 K generates a paramagnetic species that is detectable by low-temperature (T < 20 K) EPR as a signal in the g = 2 region, 90-230 G wide, depending on the treatment that PSII has undergone. This signal has recently been assigned to YZ* in magnetic interaction with the manganese cluster in its S2 state [Gilchrist et al. (1995) Proc. Natl. Acad. Sci. U.S.A. 92, 9545-9549]. This view, however, is not universal, owing, in part, to the fact that its spectroscopic properties depend on the preparation and the experimental conditions used for its study and, in part, to uncertainties as to the room temperature behavior of YZ* in inhibited preparations. Here, we report time-resolved and conventional EPR data showing that, at room temperature and at 273 K, YZ* can be accumulated in its 20 G form in high yields in both Ca2+-depleted and acetate-inhibited preparations, and that the kinetics of its decay match the decay kinetics of the low-temperature signal generated in corresponding samples. The properties of the YZ* signal, however, are shown to depend on the polypeptide content, the temperature, and the electron donors and acceptors present in the sample under examination. Our results support assignment of the EPR signal in inhibited preparations to S2 YZ* and demonstrate a protective role of the 17 and 23 kDa extrinsic polypeptides for the manganese cluster against externally added reductants.     

Vibrational spectrum associated with the reduction of tyrosyl radical D* in photosystem II: a comparative biochemical and kinetic study

Photosystem II (PSII) contains a redox-active tyrosine, D. Difference FT-IR spectroscopy can be used to obtain structural information about this species, which is a neutral radical, D*, in the photooxidized form. Previously, we have used isotopic labeling, site-directed mutagenesis, and kinetics to assign a vibrational line at 1477 cm-1 to D*; these studies were performed on highly resolved PSII preparations at pH 7.5 ?Kim et al. (1998) Biochim. Biophys. Acta 1364, 337-360; publisher's correction, Biochim. Biophys. Acta 1366, 330-354?. Here, we use kinetics to assign vibrational features to tyrosyl radical, D*, in PSII membranes. EPR and fluorescence controls identify a time regime in which D* decay occurs independently of redox changes involving the PSII quinone acceptors. Difference FT-IR spectra, acquired over this time regime, exhibit decreases in the amplitude of a 1477 cm-1 line; quantitative comparison with EPR transients supports the assignment to D*. Conditions, requiring the use of phosphate/formate, have been described for observation of a dissimilar FT-IR spectrum, which has been assigned to tyrosyl radical D*; this spectrum lacks a 1477 cm-1 line ?Hienerwadel et al. (1997) Biochemistry 36, 14712-14723?. Under these conditions, we have observed (1) an acceleration in the rate of D* decay and a decrease in D* yield attributable to the presence of formate, (2) a proportional decrease in the amplitude of FT-IR spectra acquired over the time regime in which D* decays, (3) frequency shifts in the D* - D FT-IR spectrum, (4) large-scale structural changes, as assessed by the amide I line shape, and (5) contributions to the FT-IR spectrum from the phosphate/formate buffer in the absence of PSII. We conclude that changes in the FT-IR spectrum, observed in the presence of phosphate/formate, are caused by alterations in the environment of D* and by direct phosphate/formate contributions to the spectrum.     

Biochemical and functional properties of photosystem II in agranal membranes from maize mesophyll and bundle sheath chloroplasts

We have studied the occurrence and organization of photosystem II (PSII) in bundle sheath thylakoids and stroma lamellae from maize. As shown by non-denaturing lauryl beta-D- iminopropionidate (Deriphat)/PAGE, PSII exists in a dimeric form in grana membranes. In bundle sheath and stroma lamellae, however, only a monomeric form was found. Based on immunotitration data, we estimated the stoichiometry of the individual components of the PSII core complex and antenna systems. In stroma lamellae, all PSII antenna complexes had a stoichiometry similar to that in grana membranes, with the exception of light-harvesting complex II (LHCII) that was somewhat over-represented, while the minor antenna complexes CP26 and CP29 were under-represented. In bundle sheath, the amount of LHCII was approximately eight times higher than expected with respect to D1. The 33-kDa protein of the oxygen-evolving enhancer polypeptides was not detectable nor was the ferredoxin-NADP+ reductase, thus strongly suggesting that no significant linear electron transport occurs in bundle sheath thylakoids. Fluorescence induction data suggest that most of the PSII reaction centers in bundle sheath and stroma lamellae sustain electron transport towards a secondary acceptor pool. Stromal PSII centers are only weakly inhibited by 3-(3,4-dichlorophenyl)-1,1-dimethylurea (diuron), whereas, unexpectedly, dichlorobenzoquinone and methyl viologen had a pronounced inhibitory effect of the QA- reoxidation. An additional specificity of these centers is the slow rate (50-ms range) of the QA to QB electron transfer. The amplitude of variable fluorescence found in stroma lamellae can only account for a small fraction (1-2%) of the variable fluorescence of whole thylakoids. This suggests that stromal PSII cannot be solely responsible for the slow beta-phase of the induction kinetics.     

Characterization of the interaction between manganese and tyrosine Z in acetate-inhibited photosystem II

When acetate-inhibited photosystem II (PSII) membranes are illuminated at temperatures above 250 K and quickly cooled to 77 K, a 240 G-wide electron paramagnetic resonance (EPR) signal is observed at 10 K. This EPR signal arises from a reciprocal interaction between the spin 1/2 ground state of the S2 state of the Mn4 cluster, for which a multiline EPR signal with shifted 55Mn hyperfine peaks is observed, and the oxidized tyrosine residue, YZ*, for which a broadened YZ* EPR spectrum is observed. The S2YZ* EPR signal in acetate-inhibited PSII is the first in which characteristic spectral features from both paramagnets can be observed. The observation of distinct EPR signals from each of the paramagnets together with the lack of a half-field EPR transition indicates that the exchange and dipolar couplings are weak. Below 20 K, the S2YZ* EPR signal in acetate-inhibited PSII is in the static limit. Above 20 K, the line width narrows dramatically as the broad low-temperature S2YZ* EPR signal is converted to a narrow YZ* EPR signal at room temperature. The line width narrowing is interpreted to be due to averaging of the exchange and dipolar interactions between YZ* and the S2 state of the Mn4 cluster by rapid spin-lattice relaxation of the Mn4 cluster as the temperature is increased. Decay of the S2YZ* intermediate at 200 K shows that the g = 4.1 form of the S2 state is formed and that a noninteracting S2-state multiline EPR signal is not observed as an intermediate in the decay. This result shows that a change in the redox state of YZ induces a spin-state change in the Mn4 cluster in acetate-inhibited PSII. The interconversion between spin states of the Mn4 cluster in acetate-inhibited PSII supports the idea that YZ oxidation or YZ* reduction is communicated to the Mn4 cluster through a direct hydrogen-bonding pathway, possibly involving a ligand bound to the Mn4 cluster.     

Chloride-depletion of photosynthetic water oxidase. No proton release during the second oxidation step, S2*==>S3*, and a transmembrane radical pair recombination from the third on

Chloride depletion blocks the normal four-step progress of photosynthetic water oxidation. We studied proton release in chloride-depleted thylakoids which were dark-adapted and excited by flashing light. Proton release was blocked from the second flash on, possibly leaving an uncompensated positive charge in the catalytic centre. The reduction of P+680 by Tyrz was still very rapid (< 10 microseconds). From the third flash on, P+680 was reduced more slowly (70 microseconds/200 microseconds), and by an electrogenic back-reaction. The uncompensated positive charge may be the reason why the rapid reduction of P+680 by Tyrz is prevented and the transmembrane charge-pair recombination is facilitated.     

Catalase-free photosystem II: the O2-evolving complex does not dismutate hydrogen peroxide

A photosystem II (PSII) membrane-associated heme catalase has been identified as a major source of the dark H2O2-dismutation reaction in PSII membrane samples [Sheptovitsky, Y. G., and Brudvig, G. W. (1996) Biochemistry 35, 16255-16263]. Based on this finding, a catalase-free PSII membrane sample was prepared by using mild heat treatment to deplete most of the PSII membrane-associated heme catalase followed by inhibition of the residual catalase with 50 mM 3-amino-1,2,4-triazole, a specific heme catalase inhibitor that binds covalently to compound I. After these treatments, the PSII membrane sample exhibited only 0.02% of the original H2O2-dismutation activity when assayed in the presence of 20 mM 3-amino-1,2,4-triazole. This small residual H2O2-dismutation activity is attributed to adventitious metal ions or the non-heme iron in PSII because the activity was still present in a Mn-depleted PSII sample but was completely suppressed by adding 5 mM ferricyanide to the assay buffer; the effect of ferricyanide is attributed to oxidation of H2O2-dismutating cations. Although the H2O2-dismutation activity was completely eliminated by these treatments, the light-induced O2-evolution activity was retained. A single saturating flash given to catalase-free PSII membranes did not induce any H2O2-dismutation activity. These results demonstrate that the S1/S-1 and S2/S0 cycles of the O2-evolving complex of PSII do not occur in the presence of H2O2, as proposed by Velthuys, B., and Kok, B. [(1978) Biochim. Biophys. Acta 502, 211-221]. The light-induced O2-evolution activity in catalase-free PSII was found to be irreversibly impaired by micromolar concentrations of H2O2. Thus, it is possible that the PSII membrane-associated heme catalase plays an important role in protection of the O2-evolving complex from damage by H2O2.     

Model for the fluorescence induction curve of photoinhibited thylakoids

The fluorescence induction curve of photoinhibited thylakoids measured in the presence of 3-(3,4-dichlorophenyl)-1,1-dimethyl urea was modeled using an extension of the model of Lavergne and Trissl (Biophys. J. 68:2474-2492), which takes into account the reversible exciton trapping by photosystem II (PSII) reaction centers and exciton exchange between PSII units. The model of Trissl and Lavergne was modified by assuming that PSII consists of photosynthetically active and photoinhibited (inactive in oxygen evolution) units and that the inactive PSII units can efficiently dissipate energy even if they still retain the capacity for the charge separation reaction. Comparison of theoretical and experimental fluorescence induction curves of thylakoids, which had been subjected to strong light in the presence of the uncoupler nigericin, suggests connectivity between the photoinhibited and active PSII units. The model predicts that photoinhibition lowers the yield of radical pair formation in the remaining active PSII centers. However, the kinetics of PSII inactivation in nigericin-treated thylakoids upon exposure to photoinhibitory light ranging from 185 to 2650 micromol photons m-2 s-1 was strictly exponential. This may suggest that photoinhibition occurs independently of the primary electron transfer reactions of PSII or that increased production of harmful substances by photoinhibited PSII units compensates for the protection afforded by the quenching of excitation energy in photoinhibited centers.     

The 23 and 17 kDa extrinsic proteins of photosystem II modulate the magnetic properties of the S1-state manganese cluster

An S1-state parallel polarization "multiline" EPR signal arising from the oxygen-evolving complex has been detected in spinach (PSII) membrane and core preparations depleted of the 23 and 17 kDa extrinsic polypeptides, but retaining the 33 kDa extrinsic protein. This S1-state multiline signal, with an effective g value of 12 and at least 18 hyperfine lines, has previously been detected only in PSII preparations from the cyanobacterium sp. Synechocystis sp. PCC6803 [Campbell, K. A., Peloquin, J. M., Pham, D. P., Debus, R. J., and Britt, R. D. (1998) J. Am. Chem. Soc. 120, 447-448]. It is absent in PSII spinach membrane and core preparations that either fully retain or completely lack the 33, 23, and 17 kDa extrinsic proteins. The S1-state multiline signal detected in spinach PSII cores and membranes has the same effective g value and hyperfine spacing as the signal detected in Synechocystis PSII particles. This signal provides direct evidence for the influence of the extrinsic PSII proteins on the magnetic properties of the Mn cluster.     

Correlation between structure and magnetic spin state of the manganese cluster in the oxygen-evolving complex of photosystem II in the S2 state: determination by X-ray absorption spectroscopy

The structure of the manganese cluster in the S2 state with the g approximately 4 EPR signal (S2-g4 state) generated by 130 K illumination of photosystem II (PSII) membranes prepared from spinach has been investigated by X-ray absorption spectroscopy. The Mn X-ray absorption K-edge spectra of the S2-g4 state not only show a shift of the inflection point to higher energy from the S1 state but also reveal a different edge shape from that of the S2 state with the multiline signal (S2-MLS state). Extended X-ray absorption fine structure (EXAFS) studies of the Mn K-edge show that the structure of the Mn cluster in the S2-g4 state is distinctly different from those in the S2-MLS or S1 states. In the S2-g4 state, the second shell of back-scatters from the Mn absorber is found to contain two Mn-Mn distances of 2.73 and 2.85 A. We interpret this to indicate the presence of two nonequivalent di-mu-oxo-bridged Mn binuclear structures in the Mn cluster of the S2-g4 state. The third shell of the S2-g4 state at about 3.3 A also contains increased heterogeneity. By contrast, very little distance disorder was found to exist in the second shell of the S1 or S2-MLS states. A mechanism is proposed to explain these results in the context of our model for the Mn cluster and the EPR properties of the Mn complex in the S2 state.     

Mechanism of carbon monoxide oxidation by the carbon monoxide dehydrogenase/acetyl-CoA synthase from Clostridium thermoaceticum: kinetic characterization of the intermediates

Carbon monoxide dehydrogenase/acetyl-CoA synthase (CODH/ACS) from Clostridium thermoaceticum catalyzes (i) the synthesis of acetyl-CoA from a methylated corrinoid protein, CO, and coenzyme A and (ii) the oxidation of CO to CO2. CO oxidation occurs at a Ni- and FeS-containing center known as cluster C. Electrons are transferred from cluster C to a separate metal center, cluster B, to external acceptors like ferredoxin. In the work described here, we performed reductive titrations of CODH/ACS with CO and sodium dithionite and monitored the reaction by electron paramagnetic resonance (EPR) spectroscopy. We also performed pre-steady-state kinetic studies by rapid freeze-quench EPR spectroscopy (FQ-EPR) and stopped-flow kinetics. Redox titrations of CODH/ACS revealed the existence of a UV-visible and EPR-silent electron acceptor denoted center S that does not appear to be associated with any of the other metal centers in the protein. Our results support the previous proposals [Anderson, M. E., & Lindahl, P. A. (1994) Biochemistry 33, 8702-8711; Anderson, M. E., & Lindahl, P. A. (1996) Biochemistry 35, 8371-8380] that the Cred2 form of cluster C is two electrons more reduced than the Cred1 form. The combined results from titrations and pre-steady-state studies were used to formulate a mechanism for CO oxidation, composed of the following steps: (i) CO binding to the [Cred1,Box, Xox] state to yield a Cred1-CO complex; (ii) two-electron reduction of Cred1 to Cred2 concerted with CO2 release; (iii) binding of a second CO molecule to the [Cred2,Box,Xox] state to form a Cred2-CO complex; (iv) electron transfer from Cred2-CO to cluster B to form [Cred2,Bred,Xred] with concerted release of the second CO2. Step iii competes with internal electron transfer from Cred2 to Box and Xox. At high CO concentrations, step iii is favored, whereas at low concentrations, only one CO molecule per turnover binds and undergoes oxidation. Closure of the catalytic cycle involves electron transfer from reduced enzyme to an electron acceptor protein, like ferredoxin. Xox is a yet-uncharacterized electron acceptor that may be an intermediate in the reduction of center S. The Cred2 state appears to be the predominant state of cluster C during steady-state turnover. The rate-determining step for the first half-reaction is step iv, while during steady-state turnover, it appears to be electron transfer to external electron acceptors.     

Analysis of the reaction coordinate of photosynthetic water oxidation by kinetic measurements of 355 nm absorption changes at different temperatures in photosystem II preparations suspended in either H2O or D2O

Flash-induced absorption changes at 355 nm were measured at different temperatures within the range of 2 degrees C S2) = 14 kJ/mol, EA(S2-->S3) = 35 kJ/mol, and EA(S3-->-->S0 + O2) = 21 kJ/mol for theta > 11 degrees C, 67 kJ/mol for theta < 11 degrees C in PS II core complexes dissolved in H2O; (b) replacement of exchangeable protons by deuterons causes only minor changes ( S2, S2 --> S3, and S3 -->--> S0 + O2, respectively. The corresponding values of PS II membrane fragments are 1.3, 1.3, and 1. 4. Based on these results and corresponding EA data reported in the literature for PS II membrane fragments from spinach [Renger, G., & Hanssum, B. (1992) FEBS Lett. 299, 28-32] and PS II particles from the thermophilic cyanobacterium Synechococcus vulcanus Copeland [Koike, H., Hanssum, B., Inoue, Y., & Renger, G. (1987) Biochim. Biophys. Acta 893, 524-533], the reaction coordinate of the redox sequence in the WOC is inferred to be almost invariant to the evolutionary development from cyanobacteria to higher plants. Furthermore, the rather high activation energy of the S2 --> S3 transition provides evidence for a significant structural change coupled with this reaction. Implications for the mechanism of photosynthetic water oxidation are discussed.     

Effects of photoinhibition on the QA-Fe2+ complex of photosystem II studied by EPR and M?ssbauer spectroscopy

Effects of photoinhibition on the iron-quinone electron acceptor complex of oxygen-evolving photosystem II have been studied using low-temperature EPR and M?ssbauer spectroscopy. Photoinhibition of spinach photosystem II membrane particles at 4 degrees C decreases the EPR signal arising from the interaction of QA- with Fe2+ to 30% in 90 min under our conditions. The free radical EPR signal from QA- induced by cyanide treatment of the iron [Sanakis, Y., et al. (1994) Biochemistry 33, 9922-9928] declines with the same kinetics as the QA-Fe2+ EPR signal. In contrast, Fe2+ is present in about 70% of the centers after 90 min of photoinhibition, as shown by its EPR-detected interaction with NO and by its M?ssbauer absorption. Complete oxidation of this Fe2+ population to Fe3+ by ferricyanide is possible only in the presence of glycolate, which lowers the redox potential of the Fe3+/Fe2+ couple. In a fraction of PSII centers, which reach 30% after 90 min of photoinhibition, the iron cannot be detected. It is concluded that photoinhibition of oxygen-evolving photosystem II affects both QA and Fe2+. However, the photoinhibitory impairment of the QA redox functioning precedes the modification of the non-heme iron. In a considerable portion of the photoinhibited centers, which do not have functional QA, the non-heme iron is still present and redox active, but its redox potential is increased relative to that in the normal centers. This is probably due to a minor modification of the bicarbonate ligation site.(ABSTRACT TRUNCATED AT 250 WORDS)     

Kinetic determination of the fast exchanging substrate water molecule in the S3 state of photosystem II

In a previous communication we showed from rapid isotopic exchange measurements that the exchangeability of the substrate water at the water oxidation catalytic site in the S3 state undergoes biphasic kinetics although the fast phase could not be fully resolved at that time [Messinger, J., Badger, M., and Wydrzynski, T. (1995) Proc. Natl. Acad. Sci. U.S.A. 92, 3209-3213]. We have since improved the time resolution for these measurements by a further factor of 3 and report here the first detailed kinetics for the fast phase of exchange. First-order exchange kinetics were determined from mass spectrometric measurements of photogenerated O2 as a function of time after injection of H218O into spinach thylakoid samples preset in the S3 state at 10 degreesC. For measurements made at m/e = 34 (i. e., for the mixed labeled 16,18O2 product), the two kinetic components are observed: a slow component with k1 = 2.2 +/- 0.1 s-1 (t1/2 approximately 315 ms) and a fast component with k2 = 38 +/- 4 s-1 (t1/2 approximately 18 ms). When the isotopic exchange is measured at m/e = 36 (i.e., for the double labeled 18,18O2 product), only the slow component (k1) is observed, clearly indicating that the substrate water undergoing slow isotopic exchange provides the rate-limiting step in the formation of the double labeled 18,18O2 product. When the isotopic exchange is measured as a function of temperature, the two kinetic components reveal different temperature dependencies in which k1 increases by a factor of 10 over the range 0-20 degreesC while k2 increases by only a factor of 3. Assuming simple Arrhenius behavior, the activation energies are estimated to be 78 +/- 10 kJ mol-1 for the slow component and 39 +/- 5 kJ mol-1 for the fast component. The different kinetic components in the 18O isotopic exchange provide firm evidence that the two substrate water molecules undergo separate exchange processes at two different chemical sites in the S3 state, prior to the O2 release step (t1/2 approximately 1 ms at 20 degreesC). The results are discussed in terms of how the substrate water may be bound at two separate metal sites.     

Spin-lattice relaxation of the pheophytin, Pheo-, radical of photosystem II

The spin-lattice relaxation times (T1) of the pheophytin anion radical, Pheo-, of the PSII reaction center, were measured between 5 and 80 K by electron spin-echo spectroscopy. The Pheo- was studied in Mn-depleted PSII reaction centers in which the primary quinone, QA, was doubly reduced. The selective conversion of the non-heme Fe2+ into its low-spin (S = O) state, in CN-treated PSII, allowed the measurement of the intrinsic T1 of the Pheo- radical. The temperature dependence of the intrinsic (T1)-1 was found to be approximately T1.3 +/- 0.1. In Mn-depleted PSII membranes the high-spin (S = 2) non-heme iron, enhances the spin-lattice relaxation of Pheo-. By analyzing the data with a dipolar model, the dipolar interaction (k1d) between the Pheo and the Fe2+ (S = 2) is estimated over the temperature range 5-80 K. Comparison with the dipolar coupling between the iron and the tyrosine, YD+, shows that the Pheo is much closer to the iron than the YD+ in the PSII reaction center. By scaling the reported Fe(2+)-YD+ distance by the ratio [k1dPheo-]/[k1dYD+], we estimate the Fe(2+)-Pheo- distance in PSII to be 20 +/- 4.2 A. This distance is close to the Fe(2+)-BPheo- distance in the bacterial reaction center, and this result provides further evidence that the acceptor sides of the reaction centers in PSII and bacteria are homologous.     

Role of beta87 Thr in the beta6 Val acceptor site during deoxy Hb S polymerization

Three new Hb S variants containing beta87 Leu, Trp, or Asp instead of Thr were expressed in yeast in order to further define the role of the beta87 position in stability and polymerization of deoxy Hb S. Previous studies showed that hydrophobicity at beta85 Phe and beta88 Leu is critical for stabilization of hemoglobin. Results with the three Hb S beta87 variants, however, showed minimal differences in stability, suggesting that beta87 amino acid hydrophobicity is not critical for stabilization of hemoglobin. Polymerization properties of the variants in the deoxy form, however, were affected by the beta87 amino acid. Polymerization of Hb S beta87 Thr --> Leu and Hb S beta87 Thr --> Trp was preceded by a delay time like Hb S, while Hb S beta87 Thr --> Asp did not show a delay time. In addition, changes in time required for half polymer formation (T1/2) as a function of hemoglobin concentration for Hb S beta87 Thr --> Asp were similar to that for beta87 Thr --> Gln. Hb S beta87 Thr --> Leu polymerized at a lower hemoglobin concentration than Hb S while beta87 Thr --> Trp and Hb S beta87 Thr --> Asp required much higher hemoglobin concentrations for polymer formation. Critical concentration required for deoxy Hb S beta87 Thr --> Asp polymerization was 6- and 2.3-fold greater than that for Hb S beta85 Phe --> Glu and Hb S beta88 Leu --> Glu, respectively. These results suggest that even though beta87 Thr is not a direct interaction site for beta6 Val in deoxy Hb S polymers, it does play a critical role in formation of the hydrophobic acceptor pocket which then promotes protein-protein interactions facilitating formation of stable nuclei and polymers of deoxy Hb S.     

Comparison of simultaneous esophageal pH monitoring and scintigraphy in infants with gastroesophageal reflux

1. Analysis of the Soret spectra of hemoglobins A, S and F has been used to determine the extent of heme exposure and release from these hemoglobins in the presence of several solvent perturbants. 2. Oxyhemoglobin S unfolding in the presence of either urea or propyl urea resulted in greater heme exposure and release than either oxyhemoglobins A or F. 3. Methemoglobin formation resulted in lower denaturation midpoints for each hemoglobin compared to the reduced oxyhemoglobin state; methemoglobin F had the lowest denaturation midpoint under isothermal denaturing conditions. 4. Rate of heme exposure was greater for oxyhemoglobin S than oxyhemoglobin A in the presence of 200 microM the anionic detergent sodium dodecyl sulfate. 5. Evidence for increased levels of heme release in hemoglobin S may be related to the greater tendency of sickled red cell membranes to undergo lipid oxidation.     

Quantitative kinetic model for photoassembly of the photosynthetic water oxidase from its inorganic constituents: requirements for manganese and calcium in the kinetically resolved steps,

The process of photoactivation, the assembly of a functional water-oxidizing complex (WOC) from the apoproteins of photosystem II of higher plants and inorganic cofactors (Mn2+, Ca2+, and Cl-), was known from earlier works to be a two-step kinetic process, requiring two light-induced processes separated by a slower dark period. However, these steps had not been directly resolved in any kinetic experiment, until development of an ultrasensitive polarographic O2 electrode and synthesis of an improved chelator for cofactor removal allowed direct kinetic resolution of the first pre-steady state intermediate [Ananyev, G. M. & Dismukes, G. C. (1996a) Biochemistry 35, 4102-4109]. Herein, the dependence of the rates of each of the first two light steps and the dark step of photoactivation was directly determined in spinach PSII membranes over a range of calcium and manganese concentrations at least 10-fold lower than those possible using commercial O2 electrodes. The following results were obtained. (1) One Mn2+ ion binds and is photooxidized to Mn3+ at a high-affinity site, forming the first light-induced intermediate, IM1. Formation of IM1 is coupled to the dissociation of a bound Ca2+ ion either located in the Mn site or coupled to it. (2) The inhibition constant for Ca2+ dissociation from this site is equal to 1.5 mM. (3) The dissociation constant of Mn2+ at this high-affinity site is equal to 8 microM at the optimum calcium concentration for O2-evolving activity of 8 mM, in agreement with the high-affinity site for electron donation to PSII. (4) Prior to the next photolytic step, one Ca2+ ion must bind at its effector site so that stable photooxidation of a second Mn2+ ion can occur, forming the second light-induced intermediate, IM2. This dark process is the rate-determining step. (5) The Michaelis constant for recovery of O2 evolution by Ca2+ binding at this effector site (Km) is equal to 1.4 mM, a value that is the same as that measured for the calcium requirement for O2 evolution in intact PSII. (6) The low quantum yield for the formation of IM2 from IM1 increases linearly with the duration of the dark period up to the longest period we could examine (10 s). Accordingly, the rate limitation in the second photolytic step originates from a slow calcium-induced dark rearrangement of the first intermediate, IM1, which we propose to be a protein conformational change that allows stable binding of the next Mn2+ ion. We further propose that the single Ca2+ ion which is required for assembly of the Mn4 cluster is equivalent to the Ca2+ ion which functions at the "gatekeeper" site in intact O2-evolving centers, where it plays a role in limiting substrate access to the Mn4 cluster [Sivaraja, M., et al. (1989) Biochemistry 28, 9459-9464; Tso, J., et al., (1991) Biochemistry 30, 4734-4739]. A molecular model for photoactivation is proposed and discussed.     

Room-temperature vibrational difference spectrum for S2QB-/S1QB of photosystem II determined by time-resolved Fourier transform infrared spectroscopy

Time-resolved FTIR spectroscopy has been used to kinetically characterize the vibrational properties of intact photosystem II-enriched membrane samples undergoing the S1QB-to-S2QB- transition at room temperature. To optimize the experimental conditions for the FTIR measurements, oxygen polarographic and variable chlorophyll a fluorescence measurements were used to define the decay of S2 and QA-, respectively. The flash-induced S2QB-/S1QB difference spectra were measured at a temporal resolution of 4.44 s and a spectral resolution of 4 cm-1. An intense positive band is observed at 1480 cm-1 in the difference spectrum and shows a slow decay with a half time of approximately 13 s. Based on its decay kinetics and analogy to the infrared absorption of QA- of photosystem II and QB- in bacterial reaction centers, we conclude that the 1480 cm-1 band arises from QB- of PSII and tentatively assign it to the upsilon(CO) mode of the semiquinone anion QB-. The infrared spectral features attributed to the S1-to-S2 transition of the Mn cluster at room temperature show striking similarity to the S2/S1 difference spectrum measured at cryogenic temperatures (Noguchi, T., Ono, T.-A., and Inoue, Y. (1995) Biochim. Biophys. Acta 1228, 189-200).     

Smoking and female infertility: a systematic review and meta-analysis

The identification of Ca2+ as a cofactor in photosynthetic O2 evolution has encouraged research into the role of Ca2+ in photosystem II (PSII). Previous methods used to identify the number of binding sites and their affinities were not able to measure Ca2+ binding at thermodynamic equilibrium. We introduce the use of a Ca2(+)-selective electrode to study equilibrium binding of Ca2+ to PSII. The number and affinities of binding sites were determined via Scatchard analysis on a series of PSII membrane preparations progressively depleted of the extrinsic polypeptides and Mn. Untreated PSII membranes bound approximately 4 Ca2+ per PSII with high affinity (K = 1.8 microM) and a larger number of Ca2+ with lower affinity. The high-affinity sites are assigned to divalent cation-binding sites on the light-harvesting complex II that are involved in membrane stacking, and the lower-affinity sites are attributed to nonspecific surface-binding sites. These sites were also observed in all of the extrinsic polypeptide- and Mn-depleted preparations. Depletion of the extrinsic polypeptides and/or Mn exposed additional very high-affinity Ca2(+)-binding sites which were not in equilibrium with free Ca2+ in untreated PSII, owing to the diffusion barrier created by the extrinsic polypeptides. Ca2(+)-depleted PSII membranes lacking the 23 and 17 kDa extrinsic proteins bound an additional 2.5 Ca2+ per PSII with K = 0.15 microM. This number of very high-affinity Ca2(+)-binding sites agrees with the previous work of Cheniae and co-workers [Kalosaka, K., et al. (1990) in Current Research in Photosynthesis (Baltscheffsky, M., Ed.) pp 721-724, Kluwer, Dordrecht, The Netherlands] whose procedure for Ca2+ depletion was used. Further depletion of the 33 kDa extrinsic protein yielded a sample that bound only 0.7 very high-affinity Ca2+ per PSII with K = 0.19 microM. The loss of 2 very high-affinity Ca2(+)-binding sites upon depletion of the 33 kDa extrinsic protein could be due to a structural change of the O2-evolving complex which lost 2-3 of the 4 Mn ions in this sample. Finally, PSII membranes depleted of Mn and the 33, 23, and 17 kDa extrinsic proteins bound approximately 4 very high-affinity Ca2+ per PSII with K = 0.08 microM. These sites are assigned to Ca2+ binding to the vacant Mn sites.     

The effect of phosphor persistence on image quality in digital x-ray scanning systems

A digital x-ray scanning system offers several advantages over conventional film-screen systems. However, there are sources of image degradation resulting from the scanning motion, such as motion blur due to the temporal response of the phosphor. This mechanism produces an asymmetrical blur, requiring the use of the complex optical transfer function (OTF) rather than the normal modulation transfer function (MTF) for correct characterization of image resolution. The luminescence response of eight phosphors was measured under pulsed x-ray excitation. A weighted exponential model was used to represent the primary luminescence. The dominant luminescence life-times ranged from 2.7 microseconds for Gd2O2S:Pr to 558 microseconds for Gd2O2S:Tb. The long term response was also measured, monitoring significant increases in a slow form of luminescence known as afterglow. Afterglow was modeled by an inverse power law equation. Afterglow was found to be strong in two of the phosphors studied (ZnCdS:Ag and YTaO4). In selecting a phosphor for a scanning system, it must satisfy several criteria, including a fast temporal response. Thus, a phosphor like Gd2O2S:Tb, which has a slow luminescence, but otherwise excellent imaging properties, may not be as useful as a more rapid phosphor like CsI:Tl.