The binding site of the non-heme iron of photosystem II (PS II) is investigated by light-induced Fourier tranform infrared (FTIR) difference spectroscopy on Tris-washed membranes. The non-heme iron is oxidized (Fe3+) in the dark with ferricyanide and reduced (Fe2+) after light-induced charge separation by electron transfer from the semiquinone anion QA-. EPR experiments and IR modes of ferri- and ferrocyanide show that the electron donor side of PS II is reduced in less than 2 s after a flash and that ferricyanide reoxidizes the non-heme iron with a half-time of approximately 20 s. Recording FTIR spectra before and 2 s after flash illumination thus results in the Fe2+/Fe3+ difference spectrum. This spectrum shows band shifts and intensity changes of IR modes from ligands and neighboring residues of the non-heme iron. The IR modes of bicarbonate are revealed by comparison of Fe2+/Fe3+ spectra obtained on PS II membranes with 12C or 13C isotope labeled bicarbonate in H2O and in 2H2O. The nu as(CO) and nu s(CO) modes of bicarbonate in the Fe2+ state are assigned at 1530 +/- 10 and 1338 cm-1, respectively. The low frequency of the nu as(CO) mode is taken as experimental evidence that bicarbonate is a ligand of the non-heme iron. Furthermore, the small frequency difference (192 cm-1) between the nu as(CO) and nu s(CO) modes as compared to even hydrogen-bonded ionic bicarbonate strongly indicates that bicarbonate is a bidentate ligand of the non-heme iron in PS II. Upon iron oxidation, the bicarbonate modes are largely affected. The nu s(CO) mode is assigned at 1228 cm-1, while the nu as(CO) mode is tentatively assigned at 1658 +/- 20 cm-1. The strong up- and downshifts of the nu as and nu s(CO) modes of bicarbonate upon iron oxidation results in a frequency difference of 430 +/- 20 cm-1 that is not only explained by the increased charge on the iron but indicates that bicarbonate is a monodentate ligand of the oxidized iron. The sensitivity of the nu s(CO) mode of bicarbonate to 1H/2H exchange in both the Fe2+ and Fe3+ states and the presence in the Fe2+ state of a delta (COH) mode at 1258 cm-1 confirm that bicarbonate and not carbonate is the iron ligand and further exhibits hydrogen bond(s) with the protein. The 13C isotope-sensitive modes of bicarbonate are not affected by 15N labeling of the PS II membranes. 15N sensitive signals at 1111/1102 and 1094 cm-1 are assigned to side chain modes from histidine ligands of the iron. The latter signal is proposed to account for a histidine ligand that deprotonates upon iron oxidation. The involvement of protein peptide groups and side chains in the hydrogen-bond network around the iron is also discussed.

In order to investigate the changes of protonation or environment of carboxylic residues occurring upon photoreduction of the secondary quinone acceptor (QB) in the reaction center (RC) of the photosynthetic bacteria Rhodobacter sphaeroides 2.4.1., we have performed light-induced Fourier transform infrared (FTIR) spectroscopy on RCs from wild-type (Wt) and several site-directed mutants. The FTIR QB-/QB spectra have been obtained at pH 7 upon single-saturating flash excitation for native RCs and RC mutants containing either a single-site mutation, with Gln at L212 (EQ L212), Asn at L213 (DN L213), or Asn at L210 (DN L210), or a double-site mutation with both Gln at L212 and Asn at L213 (EQ L212 + DN L213). The assignment of an IR band to the protonation/deprotonation of a particular carboxylic side chain was analyzed by combining the effects of site-directed mutagenesis and 1H/2H isotope exchange. A positive band at 1728 cm-1 in the QB-/QB spectra was observed in Wt, DN L213, and DN L210 and was absent in the mutants EQ L212 and EQ L212 + DN L213. The intensity of the 1728 cm-1 band was significantly reduced in 2H2O, and a new feature appears at 1717 +/- 1 cm-1. Furthermore, the amplitude of the 1728 cm-1 band was similar in native and DN L210 RCs but was increased in DN L213. This band is attributed to partial proton uptake by Glu L212 estimated to be 0.3-0.4 H+/QB- in native and DN L210 RCs and O.5-0.6 H+/QB- in DN L213 RCs. In contrast, the FTIR QB-/QB spectra show no evidence for change of protonation or environment of Asp L213 upon QB- formation. The increased protonation of Glu L212 in DN L213 RCs is explained by a decreased Glu L212 pKa value due to the loss of a negatively charged Asp L213. Part of a small differential signal at 1732 (+)/1740 (-) cm-1 that is affected by 1H/2H exchange is tentatively assigned to an environmental shift of the protonated Asp L210. A negative signal at 1685 cm-1 is propose to arise from the absorption change of the amide I carbonyl mode of Glu L212.(ABSTRACT TRUNCATED AT 400 WORDS)

Tyrosine D (TyrD), a side path electron carrier of photosystem II (PS II), has been studied by light-induced Fourier transform infrared (FTIR) difference spectroscopy in PS II core complexes of Synechocystis sp. PCC 6803 using the experimental conditions previously optimized to generate the pure TyrD./TyrD FTIR difference spectrum in PS II-enriched membranes of spinach [Hienerwadel, R., Boussac, A., Breton, J., and Berthomieu, C. (1996) Biochemistry 35, 115447-115460]. IR modes of TyrD and TyrD. have been identified by specific 2H- or 13C-labeling of the tyrosine side chains. The v8a(CC) and v19(CC) IR modes of TyrD are identified at 1615 and 1513-1510 cm-1, respectively. These frequencies show that TyrD is protonated. Comparison of isotope-sensitive signals in situ with those of the model compound p-methylphenol dissolved in different solvents leads to the assignment of the v7'a(CO) and delta(COH) modes of TyrD at 1275 and 1250 cm-1, respectively. It is shown that these modes and in particular the delta(COH) IR mode are very sensitive to the formation of hydrogen-bonded complexes with amide C=O or with imidazole nitrogen atoms. The frequencies observed in situ show that TyrD is hydrogen-bonded to the imidazole ring of a neutral histidine. For the radical TyrD., isotope-sensitive IR modes are identified at 1532 and 1503 cm-1. The signal at 1503 cm-1 is assigned to the v(CO) mode of TyrD. since it is sensitive to 13C-labeling at the ring carbon involved in the C4-O bond. The perturbation of TyrD and TyrD. IR modes upon site-directed replacement of D2-His189 by Gln confirms that a hydrogen bond exists between both TyrD and TyrD. and D2-His189. In the D2-His189Gln mutant, the v7'a(CO) mode of TyrD at 1267 cm-1 and the delta(COH) mode at approximately 1228 cm-1 show that a hydrogen bond is formed between TyrD and an amide carbonyl, probably that of the D2-Gln189 side chain. Electron nuclear double resonance (ENDOR) measurements have shown that TyrD. is hydrogen-bonded in the wild type but not in the mutant [Tang, X.-S., Chrisholm, D. A., Dismukes, G. C., Brudwig, G. W., and Diner, B. A. (1993) Biochemistry 32, 13742-13748]. The v(CO) mode of TyrD. at 1497 cm-1 is downshifted by 6 cm-1 compared to WT PS II, indicating that hydrogen bonding induces a frequency upshift of the v(CO) IR mode of Tyr.. IR signals from the Gln side chain v(C=O) mode are proposed to contribute at 1659 and 1692 cm-1 in the TyrD and TyrD. states, respectively. These frequencies are consistent with the rupture of a hydrogen bond upon TyrD. formation in the mutant. The frequency of the v(CO) mode of TyrD., observed at 1503 cm-1 for WT PS II, is intermediate between that observed at 1497 cm-1 in the D2-His189Gln mutant and at 1513 cm-1 for Tyr. formed by UV irradiation in borate buffer, suggesting weaker or fewer hydrogen bonds for TyrD. in PS II than in solution. The role of D2-His189 in proton uptake upon TyrD. formation is also investigated.

Fourier transform infrared (FTIR) spectroscopy probes the vibrational properties of amino acids and cofactors, which are sensitive to minute structural changes. The lack of specificity of this technique, on the one hand, permits us to probe directly the vibrational properties of almost all the cofactors, amino acid side chains, and of water molecules. On the other hand, we can use reaction-induced FTIR difference spectroscopy to select vibrations corresponding to single chemical groups involved in a specific reaction. Various strategies are used to identify the IR signatures of each residue of interest in the resulting reaction-induced FTIR difference spectra. (Specific) Isotope labeling, site-directed mutagenesis, hydrogen/deuterium exchange are often used to identify the chemical groups. Studies on model compounds and the increasing use of theoretical chemistry for normal modes calculations allow us to interpret the IR frequencies in terms of specific structural characteristics of the chemical group or molecule of interest. This review presents basics of FTIR spectroscopy technique and provides specific important structural and functional information obtained from the analysis of the data from the photosystems, using this method.

The TyrZ./TyrZ FTIR difference spectrum is reported for the first time in Mn-depleted photosystem II (PS II)-enriched membranes of spinach, in PS II core complexes of Synechocystis sp. PCC 6803 WT, and in the mutant lacking TyrD (D2-Tyr160Phe). In Synechocystis, the v7'a(CO) and delta(COH) infrared modes of TyrZ are proposed to account at 1279 and 1255 cm-1. The frequency of these modes indicate that TyrZ is protonated at pH 6 and involved in a strong hydrogen bond to the side chain of a histidine, probably D1-His190. A positive signal at 1512 cm-1 is assigned to the v(CO) mode of TyrZ. on the basis of the 27 cm-1 downshift observed upon 13C-Tyr labeling at the Tyr ring C4 carbon. A second IR signal, at 1532 cm-1, is tentatively assigned to the v8a(CC) mode of TyrZ.. The frequency of the v(CO) mode of TyrZ. at 1512 cm-1 is comparable to that observed at 1513 cm-1 for the Tyr. obtained by UV photochemistry of tyrosinate in solution, while it is higher than that of TyrD. in WT PS II at 1503 cm-1 and that of non-hydrogen-bonded TyrD. in the D2-His189Gln mutant at 1497 cm-1 [Hienerwadel, R., Boussac, A., Breton, J., Diner, B. A., and Berthomieu, C. (1997) Biochemistry 36, 14712-14723]. This latter work and the present FTIR study suggest that hydrogen bonding induces an upshift of the v(CO) IR mode of tyrosyl radicals and that TyrZ. forms (a) stronger hydrogen bond(s) than TyrD. in WT PS II. Alternatively, the frequency difference between TyrZ. and TyrD. v(CO) modes could be explained by a more localized positive charge near the tyrosyl radical oxygen of TyrD. than TyrZ.. The TyrZ./TyrZ spectrum obtained in Mn-depleted PS II membranes of spinach shows large similarities with the S3'/S2' spectrum characteristic of radical formation in Mn-containing but Ca(2+)-depleted PS II, in support of the assignment using ESEEM of TyrZ. as being responsible for the split EPR signal observed upon illumination in these conditions [Tang, X.-S., Randall, D. W., Force, D. A., Diner, B. A., and Britt, R. D. (1996) J. Am. Chem. Soc. 118, 7638-7639]. The peak at 1514 cm-1 is assigned to the v(CO) mode of TyrZ. in these preparations, which indicates that Mn depletion only very slightly perturbs the immediate environment of TyrZ. phenoxyl.

Fatty acid photodecarboxylase (FAP) is a photoenzyme with potential green chemistry applications. By combining static, time-resolved, and cryotrapping spectroscopy and crystallography as well as computation, we characterized Chlorella variabilis FAP reaction intermediates on time scales from subpicoseconds to milliseconds. High-resolution crystal structures from synchrotron and free electron laser x-ray sources highlighted an unusual bent shape of the oxidized flavin chromophore. We demonstrate that decarboxylation occurs directly upon reduction of the excited flavin by the fatty acid substrate. Along with flavin reoxidation by the alkyl radical intermediate, a major fraction of the cleaved carbon dioxide unexpectedly transformed in 100 nanoseconds, most likely into bicarbonate. This reaction is orders of magnitude faster than in solution. Two strictly conserved residues, R451 and C432, are essential for substrate stabilization and functional charge transfer.

The protonation events that occur upon QA-QB-->QAQB- electron transfer in photosynthetic reaction centers from Rhodobacter sphaeroides were investigated by time-resolved infrared spectroscopy using tunable diode lasers as previously described [Mäntele, W., Hienerwadel, R., Lenz, F., Riedel, E. J., Grisar, R., & Tacke, M. (1990) Spectrosc. Int. 2, 29-35; Hienerwadel, R., Thibodeau, D. L., Lenz, F., Nabedryk, E., Breton, J., Kreutz, W., & Mäntele, W. (1992) Biochemistry 31, 5799-5808]. In the mid-infrared region between 1695 and 1780 cm-1, transient signals associated with QA-QB-->QAQB- electron transfer were observed and characterized. The dominant transient absorbance changes are three positive signals at 1732, 1725, and 1706 cm-1 and two negative signals at 1716 and at 1698 cm-1. The 1725 cm-1-signal disappears upon 1H-->2H exchange as expected for an accessible COOH group and is absent in Glu L212 Gln mutant reaction centers. On this basis, we propose an assignment of this signal to the COOH group of Glu L212. The other signals could correspond to intensity changes and/or shifts of other carboxylic residues, although contributions from ester C = O groups of bacteriopheophytins cannot be ruled out. In native reaction centers at pH 7 and at 4 degrees C, biphasic kinetics of the transient components were observed at most frequencies. The major signal at 1725 cm-1 exhibits a fast kinetic component of t 1/2 = 0.18 ms (25% of the total amplitude) and a slow one of t1/2 = 1 ms (75% of the total amplitude). A global fit analysis of the signals between 1695 and 1780 cm-1 revealed that the spectral distributions of the fast and the slow components are different. Biphasic kinetics with comparable half-times were also observed for the Glu L212 to Gln mutant. The simplest model to explain these results is that the fast phase represents electron transfer and the slow phase represents proton transfer and/or conformational changes coupled to electron transfer. The difference spectra of the slow component from native reaction centers show that the 1725 cm-1 band corresponds to an absorbance increase and not to a shift of an existing band. The signal is therefore proposed to arise from the protonation of Glu L212. The amplitude of the 1725 cm-1 signal varies distinctly with pH as expected for protonation of a COO- group. With increasing pH, the amplitude of the slow component increases while that of the fast component decreases slightly.(ABSTRACT TRUNCATED AT 400 WORDS)

The non heme iron environment of photosystem II is studied by light-induced infrared spectroscopy. A conclusion of previous work [Hienerwadel, R., and Berthomieu, C. (1995) Biochemistry 34, 16288-16297] is that bicarbonate is a bidendate ligand of the reduced iron and a monodentate ligand in the Fe(3+) state. In this work, the effects of bicarbonate replacement with lactate, glycolate, and glyoxylate, and of o-phenanthroline binding are investigated to determine the specific interactions of bicarbonate with the protein. Fe(2+)/Fe(3+) FTIR spectra recorded with (12)C- and (13)C(1)-labeled lactate indicate that lactate displaces bicarbonate by direct binding to the iron through one carboxylate oxygen and the hydroxyl group in both the Fe(2+) and Fe(3+) states. This different binding mode with respect to bicarbonate could explain the lower midpoint of the iron couple observed in the presence of this anion [Deligiannakis, Y., Petrouleas, V., and Diner, B. A. (1994) Biochim. Biophys. Acta 1188, 260-270]. In agreement with the -60 mV/pH unit dependence of the iron midpoint potential in the presence of bicarbonate, the proton release upon iron oxidation by photosystem II is directly measured to 0.95 +/- 0.05 by the comparison of infrared signals of phosphate buffer and ferrocyanide modes. This accurate method may be applied to the study of other redox reactions in proteins. The pH dependence of the iron couple is proposed to reflect the deprotonation of D1His215, a putative iron ligand located at the Q(B) pocket, since the signal at 1094 cm(-1) assigned to the nu(C-N) mode of a histidinate ligand in the Fe(3+) state is not observed in the presence of o-phenanthroline. Specific regulation of the pK(a) of D1His215 by bicarbonate is inferred from the absence of the band at 1094 cm(-1) in Fe(2+)/Fe(3+) spectra recorded with glycolate, glyoxylate, or lactate. A broad positive continuum, maximum at approximately 2550 cm(-1), observed in the presence of bicarbonate, but absent with o-phenanthroline or lactate, glycolate, and glyoxylate, indicates a hydrogen bond network from the non heme iron toward the Q(B) pocket involving bicarbonate and His D1-215. Proton release of about 1, measured upon iron oxidation at pH 6 with the latter anions, points to a proton release mechanism different from that involved in the presence of bicarbonate.