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Extrinsic 33-kilodalton protein of spinach oxygen-evolving complexes: kinetic studies of folding and disulfide reduction.

The 33-kDa protein is one of the three extrinsic proteins in the oxygen-evolving photosystem II complexes. The protein has one intrachain disulfide bond. On reduction of this disulfide bond, the protein was unfolded and lost its activity. On the basis of the unfolding equilibrium curve obtained by using guanidine hydrochloride, the free energy change of unfolding in the absence of guanidine hydrochloride was estimated to be 4.4 kcal/mol using the Tanford method [Tanford, C. (1970) Adv. Protein Chem. 24, 1-95] and 2.8 kcal/mol using the linear extrapolation method. The unfolding of the 33-kDa protein caused by reduction was explained in terms of the entropy change associated with reduction of the intrachain disulfide bond. The kinetics of the reduction of the disulfide bond using dithiothreitol were studied at various concentrations of guanidine hydrochloride at pH 7.5 and 25 degrees C. The disulfide bond was reduced even in the absence of guanidine hydrochloride. The unfolding and refolding kinetics of the 33-kDa protein using guanidine hydrochloride were also studied under the same conditions, and the results were compared with those for the reduction kinetics. It was shown that the reduction of the disulfide bond proceeds through a species in which the disulfide bond is exposed by local fluctuations.

Chemical Phenomena↗

The S(3) state of the oxygen-evolving complex in photosystem II is converted to the S(2)Y(Z)* state at alkaline pH.

Here we report an EPR signal that is induced by a pH jump to alkaline pH in the S(3) state of the oxygen-evolving complex in photosystem II. The S(3) state is first formed with two flashes at pH 6. Thereafter, the pH is changed in the dark prior to freezing of the sample. The EPR signal is 90-100 G wide and centered around g = 2. The signal is reversibly induced with a pK = 8.5 +/- 0.3 and is very stable with a decay half-time of 5-6 min. If the pH is changed in the dark from pH 8.6 to 6.0, the signal disappears although the S(3) state remains. We propose that the signal arises from the interaction between the Mn cluster and Y(Z), resulting in the spin-coupled S(2)Y(Z)(*) signal. Our data suggest that the potential of the Y(Z)(*)/Y(Z) redox couple is sensitive to the ambient pH in the S(3) state. The alkaline pH decreases the potential of the Y(Z)(*)/Y(Z) couple so that Y(Z) can give back an electron to the S(3) state, thereby obtaining the S(2)Y(Z)(*) EPR signal. The tyrosine oxidation also involves proton release from Y(Z), and the results support a mechanism where this proton is released to the bulk medium presumably via a close-lying base. Thus, the equilibrium is changed from S(3)Y(Z) to S(2)Y(Z)(*) by the alkaline pH. At normal pH (pH 5.5-7), this equilibrium is set strongly to the S(3)Y(Z) state. The results are discussed in relation to the present models of water oxidation. Consequences for the relative redox potentials of Y(Z)(*)/Y(Z) and S(3)/S(2) at different pH values are discussed. We also compare the pH-induced S(2)Y(Z)(*) signal with the S(2)Y(Z)(*) signal from Ca(2+)-depleted photosystem II.

Chlorophyll↗

The temperature dependence of P680(+) reduction in oxygen-evolving photosystem II.

The temperature dependence for the reduction of the oxidized primary electron donor P680(+) by the redox active tyrosine Y(Z) has been studied in oxygen-evolving photosystem II preparations from spinach. The observed temperature dependence is found to vary markedly with the S-state of the manganese cluster. In the higher oxidation states, S(2) and S(3), sub-microsecond P680(+) reduction exhibits activation energies of about 260 meV. In contrast, there is only a small temperature dependence for the sub-microsecond reaction in the S(0) and S(1) states (an activation energy of approximately 50 meV). Slower microsecond components of P680(+) reduction show an activation energy of about 250 meV which, within experimental error, is independent of the oxidation state of the Mn cluster. By combining these values with measurements of DeltaG for electron transfer, the reorganization energies for each component of P680(+) reduction have been calculated. High activation and reorganization energies are found for sub-microsecond P680(+) reduction in S(2) and S(3), demonstrating that these electron transfers are coupled to significant reorganization events which do not occur in the presence of the lower S-states. One interpretation of these results is that there is an increase in the net charge on the manganese cluster on the S(1) to S(2) transition which acts as a barrier to electron transfer in the higher S-states. This argues against the electroneutrality requirement for some models of the function of the manganese cluster and hence against a role for Y(Z) as a hydrogen abstractor on all S-state transitions. An alternative or additional possibility is that there are proton (or other ion) motions in the sub-microsecond phases in S(2) and S(3) which contribute to the large reorganization energies observed, these motions being absent in the S(0) and S(1) states. Indeed charge accumulation may directly cause the increased reorganization energy.

Electron Transport↗

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.

Cold Temperature↗

Characteristic changes of the S2/S1 difference FTIR spectrum induced by Ca2+ depletion and metal cation substitution in the photosynthetic oxygen-evolving complex.

Effects of Ca2+ depletion and substitution with other metal cations on the structure of the protein matrices of the oxygen-evolving complex (OEC) and their corresponding changes upon the S1 to S2 transition were examined using Fourier transform infrared (FTIR) spectroscopy. Ca2+ depletion and further supplementation with Li+, Na+, Mg2+, Ca2+, or Sr2+ did not significantly affect the typical vibrational features in the double difference S2/S1 spectrum, including the symmetric [1365(+)/1404(-) cm(-1)] and the asymmetric [1587(+)/1566(-) cm(-1)] stretching modes of the carboxylate ligand and the amide I and II modes of the backbone polypeptides. On the other hand, supplementation with K+, Rb+, Cs+, or Ba2+ significantly modified the S2/S1 spectrum, in which the carboxylate modes disappeared and the amide I and II modes were modified. Results indicate that the binding of metal cations that have ionic radii larger than that of Ca2+ to the Ca2+ site induces perturbations in the protein matrices in the vicinity of the Mn cluster to interrupt the characteristic structural and/or conformational changes upon the oxidation of the Mn cluster accompanied with the S1 to S2 transition. The spectrum was also altered by the supplementation of Cd2+, which has an ionic radius comparable to that of Ca2+. A single-pulse-induced S2/S1 difference spectrum revealed that bands that have been assigned to the vibrational modes for the Y(Z) tyrosine and the histidine ligand for the Mn cluster were not induced in the K+-supplemented membranes, although the histidine band is likely to be preserved in the Ca2+-depleted membranes. The Y(Z) band was considerably small in the double difference S2/S1 spectrum in the Ca2+-depleted and the cation-substituted membranes but distinctively present in the Sr2+- or Ca2+-replenished membranes. Furthermore, cation supplementation induced several new bands that disappeared following the Ca2+ replenishment. These results suggest that the proper organization of the hydrogen bond network within OEC for the water oxidation chemistry requires the Ca2+ ion and indicate that the role of Ca2+ is not purely structurally defined by the physical properties of the ion, such as valence and ionic radius. On the basis of these and other findings, we propose that Ca2+ is necessary for the formation of the hydrogen bond network that is involved in the reaction step of water oxidation.

Calcium↗

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

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

Binding Sites↗

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.

Cations↗

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

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

Calcium↗

Alterations of the oxygen-evolving apparatus induced by a 305Arg --> 305Ser mutation in the CP43 protein of photosystem II from Synechocystis sp. PCC 6803 under chloride-limiting conditions.

The psbC gene encodes CP43, a component of Photosystem II (PSII) in higher plants, algae, and cyanobacteria. Previous work demonstrated that alteration of an arginine residue occurring at position 305 to serine produced a strain (R305S) with altered PSII activity (Knoepfle, N., Bricker, T. M., and Putnam-Evans, C. (1999) Biochemistry 38, 1582-1588). This strain grew at wild-type rates in complete BG-11 media (480 microM chloride) and evolved oxygen at rates that were 60-70% of the observed wild-type rates. The R305S strain assembled approximately 70-80% of the functional PSII centers contained in the control strain, and these PSII centers were very sensitive to photoinactivation at high light intensities. We recently observed that the R305S mutant exhibited a pronounced chloride effect. When this mutant was grown in media depleted of chloride (30 microM chloride), it exhibited a severely reduced photoautotrophic growth rate. The effect of chloride depletion on the growth rate of the mutant was reversed by the addition of 480 microM bromide to the chloride-depleted BG-11 media. Oxygen evolution rates for the mutant were further depressed to about 22% of that observed in control cells under chloride-limiting conditions. Addition of bromide restored these rates to those observed under chloride-sufficient conditions. The mutant exhibited a significantly lower relative quantum yield for oxygen evolution than did the control strain, and this was exacerbated under chloride-limiting conditions. Fluorescence yield measurements indicated that both the mutant and the control strains assembled fewer PSII reaction centers under chloride-limiting conditions. The reaction centers assembled by the mutant exhibited an enhanced sensitivity to photoinactivation under chloride-limiting conditions, with a t(1/2) of photoinactivation of 2.6 min under chloride-limiting conditions as compared to a t(1/2) of 4.7 min under normal growth conditions. The mutant also exhibited an enhanced stability of its S(2) state and increased number of centers in the S(1) state following dark incubation. These results indicate that the mutant R305S exhibits a defect in its ability to utilize chloride in support of efficient oxygen evolution in PSII. This is the first mutant of this type described in the CP43 protein.

Arginine↗

(18)O isotope exchange measurements reveal that calcium is involved in the binding of one substrate-water molecule to the oxygen-evolving complex in photosystem II.

Direct evidence is presented to show that calcium is inherently involved in the binding of one of the two substrate-water molecules to the oxygen-evolving complex in photosystem II. Previous rapid (millisecond range) (18)O isotope exchange measurements between added H(2)(18)O and the photogenerated O(2) have shown that the two substrate-water molecules bind to separate sites throughout the S-state cycle, as revealed by their kinetically distinct rates of (18)O exchange [Hillier, W., and Wydrzynski, T. (2000) Biochemistry 39, 4399-4405]. Upon extraction of the functionally bound calcium using a either a low-pH/citrate treatment or a NaCl/A23187/EGTA treatment and subsequent reconstitution of activity with strontium, we show for the first time a specific increase in the slow rate of (18)O exchange by a factor of 3-4. This increase in the slow rate of exchange is consistently observed across the S(1), S(2), and S(3) states. In contrast, the fast phase of (18)O exchange in the S(3) state appears to be affected little upon strontium reconstitution, while the fast phases of exchange in the S(1) and S(2) states remain largely unresolvable, at the detectable limits of the current techniques. The results are discussed in terms of a possible substrate bridging structure between the functional calcium and a catalytic manganese ion that gives rise to the slowly exchanging component.

Binding Sites↗

Changes of low-frequency vibrational modes induced by universal 15N- and 13C-isotope labeling in S2/S1 FTIR difference spectrum of oxygen-evolving complex.

The effects of universal (15)N- and (13)C-isotope labeling on the low- (650-350 cm(-1)) and mid-frequency (1800-1200 cm(-1)) S(2)/S(1) Fourier transform infrared (FTIR) difference spectrum of the photosynthetic oxygen-evolving complex (OEC) were investigated in histidine-tagged photosystem (PS) II core particles from Synechocystis sp. PCC 6803. In the mid-frequency region, the amide II modes were predominantly affected by (15)N-labeling, whereas, in addition to the amide II, the amide I and carboxylate modes were markedly affected by (13)C-labeling. In the low-frequency region, by comparing a light-induced spectrum in the presence of ferricyanide as the electron acceptor, with the double difference S(2)/S(1) spectrum obtained by subtracting the Q(A)(-)/Q(A) from the S(2)Q(A)(-)/S(1)Q(A) spectrum, considerable numbers of bands found in the light-induced spectrum were assigned to the S(2)/S(1) vibrational modes in the unlabeled PS II core particles. Upon (13)C-labeling, changes were observed for most of the prominent bands in the S(2)/S(1) spectrum. Although (15)N-labeling also induced changes similar to those by (13)C-labeling, the bands at 616(-), 605(+), 561(+), 555(-), and 544(-) cm(-1) were scarcely affected by (15)N-labeling. These results indicated that most of the vibrational modes found in the low-frequency spectrum are derived from the coupling between the Mn-cluster and groups containing nitrogen and/or carbon atom(s) in a direct manner and/or through hydrogen bonding. Interestingly, an intensive band at 577(-) cm(-1) was not affected by (15)N- and (13)C-isotope labeling, indicating that this band arises from the mode that does not include either nitrogen or carbon atoms, such as the skeletal vibration of the Mn-cluster or stretching vibrational modes of the Mn-ligand.

Carbon Isotopes↗

Influence of the 33 kDa manganese-stabilizing protein on the structure and substrate accessibility of the oxygen-evolving complex of photosystem II.

The 33 kDa manganese-stabilizing extrinsic protein binds to the lumenal side of photosystem II (PS II) close to the Mn(4)Ca cluster of the oxygen-evolving complex, where it limits access of small molecules to the metal site. Our previous finding that the removal of this protein did not alter the magnetic coupling regime within the manganese cluster, measured by electron spin-echo envelope modulation [Gregor, W., and Britt, R. D. (2000) Photosynth. Res. 65, 175-185], prompted us to examine whether this accessibility control is also true for substrate water, using the same pulsed EPR technique. Comparing the deuteron modulation of the S(2)-state multiline signal of PS II membranes, equilibrated with deuterated water (D(2)O) after removal or retention of the 33 kDa protein, we observed no change in the number and the distance of deuterons magnetically coupled to manganese, indicating that the number and distance of water molecules bound to the manganese cluster are independent of bound 33 kDa protein in the S(1) state, in which the sample was poised prior to cryogenic illumination. A simple modulation depth analysis revealed a distance of 2.5-2.6 A between the closest deuteron and manganese. These results are in agreement with our refined X-ray absorption analysis. The manganese K-edge positions, reflecting their oxidation states, and the extended X-ray absorption fine structure amplitudes and distances between the manganese ions and their oxygen and nitrogen ligands (1.8, 2.7, and 3.3-3.4 A) were independent of bound 33 kDa protein.

Binding Sites↗

PsbU provides a stable architecture for the oxygen-evolving system in cyanobacterial photosystem II.

PsbU is a lumenal peripheral protein in the photosystem II (PS II) complex of cyanobacteria and red algae. It is thought that PsbU is replaced functionally by PsbP or PsbQ in plant chloroplasts. After the discovery of PsbP and PsbQ homologues in cyanobacterial PS II [Thornton et al. (2004) Plant Cell 16, 2164-2175], we investigated the function of PsbU using a psbU deletion mutant (DeltaPsbU) of Synechocystis 6803. In contrast to the wild type, DeltaPsbU did not grow when both Ca2+ and Cl- were eliminated from the growth medium. When only Ca2+ was eliminated, DeltaPsbU grew well, whereas when Cl- was eliminated, the growth rate was highly suppressed. Although DeltaPsbU grew normally in the presence of both ions under moderate light, PS II-related disorders were observed as follows. (1) The mutant cells were highly susceptible to photoinhibition. (2) Both the efficiency of light utilization under low irradiance and the chlorophyll-specific maximum rate of oxygen evolution in DeltaPsbU cells were 60% lower than those of the wild type. (3) The decay of the S2 state in DeltaPsbU cells was decelerated. (4) In isolated PS II complexes from DeltaPsbU cells, the amounts of the other three lumenal extrinsic proteins and the electron donation rate were drastically decreased, indicating that the water oxidation system became significantly labile without PsbU. Furthermore, oxygen-evolving activity in DeltaPsbU thylakoid membranes was highly suppressed in the absence of Cl-, and 60% of the activity was restored by NO3- but not by SO4(2-), indicating that PsbU had functions other than stabilizing Cl-. On the basis of these results, we conclude that PsbU is crucial for the stable architecture of the water-splitting system to optimize the efficiency of the oxygen evolution process.

Bacterial Proteins↗

pH dependence of the flash-induced S-state transitions in the oxygen-evolving center of photosystem II from Thermosynechoccocus elongatus as revealed by Fourier transform infrared spectroscopy.

pH dependence of the efficiencies of the flash-induced S-state transitions in the oxygen-evolving center (OEC) was studied by means of Fourier transform infrared (FTIR) difference spectroscopy using photosystem II (PSII) core complexes from the thermophilic cyanobacterium Thermosynechoccocus elongatus. The PSII core complexes dark-adapted at different pHs in the presence of ferricyanide as an electron acceptor were excited by four consecutive saturating laser flashes, and FTIR difference spectra induced by each flash were recorded in the region of 1800-1200 cm(-1). Each difference spectrum was fitted with a linear combination of standard spectra measured at pH 6.0, which represent the spectra upon individual S-state transitions, and the transition efficiencies were estimated from the fitting parameters. It was found that the S1 --> S2 transition probability is independent of pH throughout the pH region of 3.5-9.5, while the S2 --> S3, S3 --> S0, and S0 --> S1 transition probabilities decrease at acidic pH with pK values of 3.6 +/- 0.2, 4.2 +/- 0.3, and 4.7 +/- 0.5, respectively. These findings, i.e., the pH-independent S1 --> S2 transition probability and the pK values for the inhibition in the acidic range of the other three transitions, were in good agreement with recent results obtained by electron paramagnetic resonance measurements for PSII-enriched membranes of spinach [Bernát, G., Morvaridi, F., Feyziyev, Y., and Styring, S. (2002) Biochemistry 41, 5830-5843]. On the basis of this correspondence for quite different types of PSII preparations exhibiting marked difference in the pH dependence of the apparent proton release pattern, it is concluded that the inhibition of the S2 --> S3, S3 --> S0, and S0 --> S1 transitions in the acidic region is an inherent property of the OEC. This feature probably reflects proton release from substrate water in these three transitions. On the other hand, all of the S-state transitions remained generally efficient up to pH 9.5 in the alkaline region, except for a slight decrease of the S3 --> S0 transition probability above pH 8 (pK approximately 10). This observation partly differs from the tendency reported for spinach preparations, suggesting that a mechanism different from that in the acidic region is responsible for the transition efficiencies in the alkaline region.

Bacterial Proteins↗

Site-directed mutagenesis of Thermosynechococcus elongatus photosystem II: the O2-evolving enzyme lacking the redox-active tyrosine D.

Site-directed mutagenesis in the photosystem II (PSII) oxygen-evolving enzyme was achieved in the thermophilic cyanobacterium Thermosynechococcus elongatus. PSII from this species is the focus of attention because its robustness makes it suitable for enzymological and biophysical studies. PSII, which lacks the redox-active tyrosine Tyr(D), was engineered by substituting a phenylalanine for tyrosine 160 of the D2 protein. An aim of this work was to engineer a mutant for spectroscopy, in particular, for EPR, on the active enzyme. The Tyr(D)(*) EPR signal was monitored in whole cells (i) to control the expression level of the two genes (psbD(1) and psbD(2)) encoding D2 and (ii) to assess the success of the mutagenesis. Both psbD(1) and psbD(2) could be expressed, and recombination occurred between them. The D2-Y160F mutation was introduced into psbD(1) after psbD(2) was deleted and a His-tag was attached to the CP43 protein. The effects of the Y160F mutation were characterized in cells, thylakoids, and isolated PSII. The efficiency of enzyme function under the conditions tested was unaffected. The distribution and lifetime of the redox states (S(n)() states) of the enzyme cycle were modified, with more S(0) in the dark and no rapid decay phase of S(3). Although not previously reported, these effects were expected because Tyr(D)(*) is able to oxidize S(0) and Tyr(D) is able to reduce S(2) and S(3). Slight changes in the difference spectra in the visible and infrared recorded upon the formation and reduction of the chlorophyll cation P(680)(+) and kinetic measurements of P(680)(+) reduction indicated minor structural perturbations, perhaps in the hydrogen-bonding network linking Tyr(D) and P(680), rather than electrostatic changes associated with the loss of a charge from Tyr(D)(*)(H(+)). We show here that this fully active preparation can provide spectra from the Mn(4)CaO(4) complex and associated radical species uncontaminated by Tyr(D)(*).

Amino Acid Substitution↗

Narrowing substrate specificity in a directly evolved enzyme: the A293D mutant of aspartate aminotransferase.

Several mutant Escherichia coli aspartate aminotransferases (eAATases) have been characterized in the attempt to evolve or rationally redesign the substrate specificity of eAATase into that of E. coli tyrosine aminotransferase (eTATase). These include HEX (designed), HEX + A293D (design followed by directed evolution), and SRHEPT (directed evolution). The A293D mutation realized from directed evolution of HEX is here imported into the SRHEPT platform by site-directed mutagenesis, resulting in an enzyme (SRHEPT + A293D) with nearly the same ratio of k(cat)/K(m)(Phe) to k(cat)/K(m)(Asp) as that of wild-type eTATase. The A293D substitution is an important specificity determinant; it selectively disfavors interactions with dicarboxylic substrates and inhibitors compared to aromatic ones. Context dependence analysis is generalized to provide quantitative comparisons of a common substitution in two or more different protein scaffolds. High-resolution crystal structures of ligand complexes of HEX + A293D, SRHEPT, and SRHEPT + A293D were determined. We find that in both SRHEPT + A293D and HEX + A293D, the additional mutation holds the Arg 292 side chain away from the active site to allow increased specificity for phenylalanine over aspartate. The resulting movement of Arg 292 allows greater flexibility of the small domain in HEX + A293D. While HEX is always in the closed conformation, HEX + A293D is observed in both the closed and a novel open conformation, allowing for more rapid product release.

Alanine↗

Ammonia-induced structural changes of the oxygen-evolving complex in photosystem II as revealed by light-induced FTIR difference spectroscopy.

Light-induced Fourier transform infrared difference spectroscopy has been applied to studies of ammonia effects on the oxygen-evolving complex (OEC) of photosystem II (PSII). We found that NH(3) induced characteristic spectral changes in the region of the symmetric carboxylate stretching modes (1450-1300 cm(-1)) of the S(2)Q(A)(-)/S(1)Q(A) FTIR difference spectra of PSII. The S(2) state carboxylate mode at 1365 cm(-1) in the S(2)Q(A)(-)/S(1)Q(A) spectrum of the controlled samples was very likely upshifted to 1379 cm(-1) in that of NH(3)-treated samples; however, the frequency of the corresponding S(1) carboxylate mode at 1402 cm(-1) in the same spectrum was not significantly affected. These two carboxylate modes have been assigned to a Mn-ligating carboxylate whose coordination mode changes from bridging or chelating to unidentate ligation during the S(1) to S(2) transition [Noguchi, T., Ono, T., and Inoue, Y. (1995) Biochim. Biophys. Acta 1228, 189-200; Kimura, Y., and Ono, T.-A. (2001) Biochemistry 40, 14061-14068]. Therefore, our results show that NH(3) induced significant structural changes of the OEC in the S(2) state. In addition, our results also indicated that the NH(3)-induced spectral changes of the S(2)Q(A)(-)/S(1)Q(A) spectrum of PSII are dependent on the temperature of the FTIR measurement. Among the temperatures we measured, the strongest effect was seen at 250 K, a lesser effect was seen at 225 K, and little or no effect was seen at 200 K. Furthermore, our results also showed that the NH(3) effects on the S(2)Q(A)(-)/S(1)Q(A) spectrum of PSII are dependent on the concentrations of NH(4)Cl. The NH(3)-induced upshift of the 1365 cm(-1) mode is apparent at 5 mM NH(4)Cl and is completely saturated at 100 mM NH(4)Cl concentration. Finally, we found that CH(3)NH(2) has a small but clear effect on the spectral change of the S(2)Q(A)(-)/S(1)Q(A) FTIR difference spectrum of PSII. The effects of amines on the S(2)Q(A)(-)/S(1)Q(A) FTIR difference spectra (NH(3) > CH(3)NH(2) > AEPD and Tris) are inverse proportional to their size (Tris approximately AEPD > CH(3)NH(2) > NH(3)). Therefore, our results showed that the effects of amines on the S(2)Q(A)(-)/S(1)Q(A) spectrum of PSII are sterically selective for small amines. On the basis of the correlations between the conditions (dependences on the excitation temperature and NH(3) concentration and the steric requirement for the amine effects) that give rise to the NH(3)-induced upshift of the 1365 cm(-)(1) mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum of PSII and the conditions that give rise to the altered S(2) state multiline EPR signal, we propose that the NH(3)-induced upshift of the 1365 cm(-1) mode is caused by the binding of NH(3) to the site on the Mn cluster that gives rise to the altered S(2) state multiline EPR signal. In addition, we found no significant NH(3)-induced change in the S(2)Q(A)(-)/S(1)Q(A) FTIR difference spectrum at 200 K. Under this condition, the OEC gives rise to the NH(3)-stabilized g = 4.1 EPR signal and a suppressed g = 2 multiline EPR signal. Our results suggest that the structural difference of the OEC between the normal g = 2 multiline form and the NH(3)-stabilized g = 4.1 form is small.

Amines↗

Effects of ethylene glycol and methanol on ammonia-induced structural changes of the oxygen-evolving complex in photosystem II.

Ammonia is an inhibitor of water oxidation and a structural analogue for substrate water, making it a valuable probe for the structural properties of the possible substrate-binding site on the oxygen-evolving complex (OEC) in photosystem II (PSII). By using the NH(3)-induced upshift of the 1365 cm(-)(1) IR mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum and the NH(3)-modified S(2) state EPR signals of PSII as spectral probes, we found that ethylene glycol has clear effects on the binding properties of the NH(3)-specific site on the OEC. Our results show that in PSII samples containing 30% (v/v) ethylene glycol, the affinity of the NH(3)-specific binding site on the OEC is estimated to be more than 10 times lower than that in PSII samples containing 0.4 M sucrose. In addition, our results show that the NH(3)-induced upshift of the 1365 cm(-)(1) IR mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum is dependent on the concentration of ethylene glycol, but not dependent on the concentration of sucrose (up to 1.5 M) or methanol (up to 5.4 M). By comparing the concentration dependence of sucrose and ethylene glycol on NH(3)-induced spectral change and also by comparing the sucrose and ethylene glycol data at similar concentrations ( approximately 1 M), we conclude that ethylene glycol has a clear effect on the NH(3)-induced spectral changes. Furthermore, our results also show that ethylene glycol alters the steric requirement of the amine effect on the upshift of the 1365 cm(-)(1) mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum. In PSII samples containing 30% (v/v) ethylene glycol, only NH(3), not other bulkier amines (e.g., Tris, AEPD, and CH(3)NH(2)), has a clear effect on the upshift of the 1365 cm(-)(1) mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum; in contrast, in PSII samples containing 0.4 M sucrose, both NH(3) and CH(3)NH(2) have a clear effect. On the basis of the results mentioned above, we propose that ethylene glycol acts directly or indirectly to decrease the affinity or limit the accessibility of NH(3) and CH(3)NH(2) to the NH(3)-specific binding site on the OEC in PSII. Finally, we also applied the same approach to test whether methanol is able to compete with ammonia on its binding site on the OEC. We found that 4% (v/v) methanol does not have any significant effect on the NH(3)-induced upshift of the 1365 cm(-)(1) mode in the S(2)Q(A)(-)/S(1)Q(A) spectrum and the NH(3)-modified S(2) state g = 2 multiline EPR signal. Our results suggest that methanol is unable to compete with NH(3) upon binding to the Mn site of the OEC that gives rise to the altered S(2) state g = 2 multiline EPR signal.

Ammonia↗