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M L Paddock

Publications and source records attributed to M L Paddock.

28 records · Page 2Linked to original sources

Light-induced electrogenic events associated with proton uptake upon forming QB- in bacterial wild-type and mutant reaction centers.

Light-induced voltage changes (electrogenic events) were measured in wild-type and site-directed mutants of reaction centers (RCs) from Rhodobacter sphaeroides oriented in a lipid monolayer adsorbed to a Teflon film. A rapid increase in voltage associated with charge separation was followed by a slower increase attributed to proton transfer from solution to protonatable amino-acid residues in the vicinity of the QB site. In native reaction centers the proton-transfer voltage had a pH-dependent amplitude with two peaks at pH 4.5 and pH 9.7, respectively. In the Glu-L212-->Gln RCs the high-pH peak was absent, whereas in the Asp-L213-->Asn RCs the low-pH peak was absent and the high-pH peak was shifted to lower pH by about 1.3 pH units. The amplitudes of the electrogenic phases as a function of pH follow approximately the measured proton uptake from solution (P.H. McPherson, M.Y. Okamura, G. Feher, Biochim. Biophys. Acta, vol. 934, 1988, pp. 348-368) and are ascribed to proton transfer to amino acid residues upon QB- formation. The peak around pH 9.7 is ascribed to proton uptake predominantly by Glu-L212 and the peak around pH 4.5 to proton uptake predominantly by Asp-L213 or a residue strongly interacting with Asp-L213.

Hydrogen-Ion Concentration↗

Pathway of proton transfer in bacterial reaction centers: further investigations on the role of Ser-L223 studied by site-directed mutagenesis.

The role of Ser-L223 in proton transfer to reduced QB in the reaction center (RC) from Rhodobacter sphaeroides was studied by site-directed replacement of Ser with residues having different proton donor properties, e.g., the aliphatic residues Ala and Gly, the hydroxyl residue Thr, the amide residue Asn, the sulhydryl residue Cys, the imidazole residue His, and the carboxylic acid residue Asp. Compared to native reaction centers, RCs with Ala or Asn at L223 had greatly reduced (approximately 300-fold) proton-coupled electron transfer rates, kAB(2), associated with the second electron reduction of QB (QA(-)QB(-) + H+ --> QAQBH-). In contrast, RCs containing Thr, Asp, or Gly at L223 retained fast proton-coupled electron transfer rates. RCs with His or Cys at L223 did not bind the secondary quinone QB. These results show that kAB(2) is larger when a good proton transfer group, e.g., a hydroxyl residue (Ser, Thr) or a carboxylic acid (Asp), occupies the L223 site, supporting the proposal that Ser-L223 is a component of a proton transfer chain [Paddock, M. L., McPherson, P. H., Feher, G., & Okamura, M. Y. (1990) Proc. Natl. Acad. Sci. U.S.A. 87, 6803--6807]. The surprising result that kAB(2) is not significantly reduced in RCs with Gly at L223 suggests that a water molecule functionally replaces the missing Ser hydroxyl group in the mutant RCs. The importance of Ser-L223 in internal proton transfer reactions within the RC is discussed.

Base Sequence↗

Fourier transforms infrared difference spectroscopy of secondary quinone acceptor photoreduction in proton transfer mutants of Rhodobacter sphaeroides.

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)

Electron Transport↗

Protonation of Glu L212 following QB- formation in the photosynthetic reaction center of Rhodobacter sphaeroides: evidence from time-resolved infrared spectroscopy.

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)

Binding Sites↗

Crystallographic analyses of site-directed mutants of the photosynthetic reaction center from Rhodobacter sphaeroides.

Seven site-directed mutants of the bacterial photosynthetic reaction center (RC) from the 2.4.1 and WS 231 wild-type strains of Rhodobacter sphaeroides have been crystallized and their X-ray diffraction analyzed to resolutions between 3.0 and 4.0 A. The mutations can be divided into four distinct categories: (1) mutations altering cofactor composition that affect electron transfer and quantum yield, His M202-->Leu (M202HL), His L173-->Leu (L173HL), and Leu M214-->His (M214LH); (2) a mutation in the proposed pathway of electron transfer altering electron-transfer kinetics, Tyr M210-->Phe (M210YF); (3) a mutation around the non-heme iron resulting in an iron-less reaction center, His M219-->Cys (M219HC); and (4) mutations around the secondary electron acceptor, a ubiquinone, affecting proton transfer and quinone turnover, Glu L212-->Gln (L212EQ) and Asp L213-->Asn (L213DN). Residues L173 and M202 are within bonding distance of the respective magnesiums of the two bacteriochlorophylls of the BChl special pair, while M214 is close to the bacteriopheophytin on the active A branch of the RC. The L173HL and M202HL crystal structures show that the respective bacteriochlorophylls are replaced with bacteriopheophytins (i.e., loss of magnesium) without significant structural perturbations to the surrounding main-chain or side-chain atoms. In the M214LH mutant, the bacteriopheophytin has been replaced by a bacteriochlorophyll, and the side chain of His M214 is within ligand distance of the magnesium. The M210YF, L212EQ, and L213DN mutants show no significant tertiary structure changes near the mutation sites. The M219HC diffraction data indicate that the overall tertiary structure of the reaction center is maintained in the absence of the non-heme iron.

Chemical Phenomena↗

Protonation and free energy changes associated with formation of QBH2 in native and Glu-L212-->Gln mutant reaction centers from Rhodobacter sphaeroides.

Formation of the quinol QBH2 in Glu-L212-->Gln mutant [EQ(L212)] reaction centers (RCs) from Rhodobacter sphaeroides was investigated by measuring the proton uptake (using dyes), UV absorption changes, and free energy changes associated with the two-electron reduction of QB. The advantage of using the EQ(L212) RCs for these studies is that the individual protonation steps can be kinetically resolved and analyzed; conclusions reached regarding the mechanism of formation of QBH2 are expected to apply also to native RCs. The proton uptake by EQ(L212) RCs was strongly biphasic: the fast phase was essentially concomitant with the second electron transfer to QB- (approximately 1 ms at pH 7.5); the slow phase was approximately 2000-fold slower. The rate constant of the slow phase depended on the redox state of the primary quinone QA; for QA- the rate constant was larger (i.e., 8-fold at pH 6.0) than for QA. The electron and proton transfers to QB- in EQ(L212) RCs were modeled with a two-step scheme as follows: (1) fast, QA-QB- + H+(1)-->QA(QBH)-; (2) slow, QA(QBH)- + H+(2)-->QAQBH2, where reaction 1 involves concomitant electron transfer and proton uptake [Paddock, M. L., McPherson, P. H., Feher, G., & Okamura, M. Y. (1990) Proc. Natl. Acad. Sci. U.S.A. 87, 6803-6807]. The stoichiometry of the fast proton uptake associated with the two-electron reduction of QB varied from 1.1 to 1.4 H+/2e- at pH 6.5-8.5, consistent with the uptake of H+(1) plus an additional fractional proton uptake due to amino acid residues whose pKa values are shifted by interactions with the charge of (QBH)-. The total steady-state proton uptake stoichiometry was 2.0 H+/2e- at pH < or = 7.5, consistent with the formation of the quinol QBH2 (reactions 1 and 2). At pH 8.5, the steady-state proton uptake was 1.6 +/- 0.1 H+/2e-, which is consistent with an apparent pKa for H+(2) of approximately 8.5 [McPherson, P. H., Okamura, M. Y., & Feher, G. (1993) Biochim. Biophys. Acta 1144, 309-324]. The proton uptake kinetics indicate that Glu-L212 is a component of the proton transfer chain for H+(2) that connects reduced QB (buried in the RC protein) to the aqueous solvent as proposed previously [Paddock, M. L., Rongey, S. H., Feher, G., & Okamura, M. Y. (1989) Proc. Natl. Acad. Sci. U.S.A. 86, 6602-6606].(ABSTRACT TRUNCATED AT 400 WORDS)

Glutamine↗

Pathway of proton transfer in bacterial reaction centers: role of aspartate-L213 in proton transfers associated with reduction of quinoneto dihydroquinone.

The role of Asp-L213 in proton transfer to reduced quinone QB in the reaction center (RC) from Rhodobacter sphaeroides was studied by site-directed replacement of Asp with residues having different proton donor properties. Reaction centers (RCs) with Asn, Leu, Thr, and Ser at L213 had greatly reduced (approximately 6000-fold) proton-coupled electron transfer [kAB(2)] and proton uptake rates associated with the second electron reduction of QB (QA- QB- + 2H(+)-->QAQBH2) compared to native RCs. RCs containing Glu at L213 showed faster (approximately 90-fold) electron and proton transfer rates than the other mutant RCs but were still reduced (approximately 70-fold) compared with native RCs. These results show that kAB(2) is larger when a carboxylic acid occupies the L213 site, consistent with the proposal that Asp-L213 is a component of a proton transfer chain. The reduced kAB(2) observed with Glu versus Asp at L213 suggests that Asp at L213 is important for proton transfer for some other reason in addition to its proton transfer capabilities. Glu-L213 is estimated to have a higher apparent pKa (pKa > or = 7) than Asp-L213 (pKa < or = 4), as indicated by the slower rate of charge recombination (D+QAQB(-)-->DQAQB) in the mutant RCs. The importance of the pKa and charge of the residue at L213 for proton transfer are discussed. Based on these studies, a model for proton transfer is proposed in which Asp-L213 contributes to proton transfer in native RCs in two ways: (1) it is a component of a proton transfer chain connecting the buried QB molecule with the solvent and/or (2) it provides a negative charge that stabilizes a proton on or near QB.

Aspartic Acid↗

Pathway of proton transfer in bacterial reaction centers: second-site mutation Asn-M44-->Asp restores electron and proton transfer in reaction centers from the photosynthetically deficient Asp-L213-->Asn mutant of Rhodobacter sphaeroides.

Site-directed mutagenesis of the photosynthetic reaction center (RC) from Rhodobacter sphaeroides has shown Asp-213 of the L subunit (Asp-L213) to be important for photosynthetic viability. Replacement of Asp-L213 with Asn resulted in a photosynthetically deficient mutant, due to the 10(4)-fold slower rate for the proton-coupled electron transfer reaction QA-QB- + 2H+-->QAQBH2 (k(2)AB). The detrimental effect of Asn-L213 is surprising since RCs from Rhodopseudomonas viridis, Rhodospirillum rubrum, and Chloroflexus aurantiacus have Asn at the homologous position. However, RCs from these bacteria have an Asp located near QB (the secondary quinone acceptor) at the position homologous to Asn-M44 in Rb. sphaeroides which might function in place of Asp-L213. To test this conjecture a "viridis-like" structure was introduced into Rb. sphaeroides by replacing Asp-L213 with Asn and Asn-M44 with Asp. The RCs from this double mutant displayed near-native rates for the electron transfer reaction k(2)AB and restored photosynthetic competence. The rates for the first electron transfer reaction QA-QB-->QAQB- (k(1)AB) and charge recombination D+QAQB--->DQAQB (kBD) were also restored to near-native values. These results indicate that Asp at either the L213 or the M44 site near QB can provide a pathway for rapid proton transfer and explain why Asp-L213 need not be conserved in different photosynthetic bacteria. To test further the effect of Asp at M44 on electron and proton transfer to QB a mutant containing Asp at both L213 and M44 was constructed. The RCs from this mutant (Asn-M44-->Asp) exhibited faster proton-coupled electron transfer to QB-. The increased rate of proton-coupled electron transfer (k(2)AB) in the presence of negatively charged Asp residues near QB suggests the role of an Asp near QB as (i) a proton donor group in the proton transfer chain and/or (ii) a negatively charged residue stabilizing proton transfer to reduced QB.

Amino Acid Sequence↗

Pathway of proton transfer in bacterial reaction centers: replacement of serine-L223 by alanine inhibits electron and proton transfers associated with reduction of quinone to dihydroquinone.

The pathway of proton transfer in the reaction center (RC) from Rhodobacter sphaeroides was investigated by site-directed mutagenesis. Ser-L223, a putative proton donor that forms a hydrogen bond with the secondary quinone acceptor QB, was replaced with Ala and Thr. RCs with Ala-L223 displayed reduced electron transfer and proton uptake rates in the reaction QA-QB- + 2H+----QAQBH2. The rate constant for this reaction, k(2)AB, was found to be reduced approximately 350-fold to 4.0 +/- 0.2 s-1. Proton uptake measurements using a pH indicator dye showed a rapid uptake of 1 H+ per RC followed by a slower uptake of 1 H+ per RC at a rate of 4.1 +/- 0.1 s-1; native RCs showed a rapid uptake of 2H+ per RC. Evidence is provided that these changes were not due to gross structural changes in the binding site of QB. RCs with Thr-L223 showed little reduction in the rates of electron and proton transfer. These results indicate that proton transfer from the hydroxyl group of Ser-L223 or Thr-L223 is required for fast electron and proton transfer associated with the formation of the dihydroquinone QH2. In contrast, previous work showed that replacing Glu-L212, another putative proton donor to QB, with Gln slowed proton uptake from solution without significantly altering electron transfer. We propose a model that involves two distinct proton transfer steps. The first step occurs prior to transfer of the second electron to QB and involves proton transfer from Ser-L223. The second step occurs after this electron transfer through a pathway involving Glu-L212.

Alanine↗

Pathway of proton transfer in bacterial reaction centers: replacement of glutamic acid 212 in the L subunit by glutamine inhibits quinone (secondary acceptor) turnover.

The mechanism of proton transfer in the reaction centers (RCs) from Rhodobacter sphaeroides was investigated by site-directed mutagenesis. Replacement of Glu-212 of the L subunit, a protonatable residue located near the secondary acceptor (QB) binding site, by glutamine reduced the in vitro electron turnover from cytochrome c to 2,3-dimethoxy-5-methylbenzoquinone (UQ0) by a factor of 25. The electron transfer rate to QB remained essentially unimpaired. Consequently, it is postulated that the reduced turnover in the mutant is due to a reduced rate of proton transfer to QB2-. The lack of pH dependence of the forward electron transfer rate DQA-QB----DQAQB- and the back reaction rate D+QAQB- ----DQAQB (where D = primary donor and QA = primary acceptor) in the mutant RC indicate that the observed pH dependence in the native RC is due to Glu-212, which has an anomalously high pKa value of 9.5 +/- 0.3. These results support the involvement of Glu-212 as a proton donor to reduced QB.

Bacterial Proteins↗