The acceptor quinone complex of Rhodopseudomonas viridis reaction centers

The acceptor complex of isolated reaction centers from Rhodopseudomonas viridis contains both menaquinone and ubiquinone. In a series of flashes the ubiquinone was observed to undergo binary oscillations in the formation and disappearance of a semiquinone, indicative of secondary acceptor (QB) activity. The oscillating signal, Q-B, was typical of a ubisemiquinone anion with a peak at 450 nm (delta epsilon = 6 mM-1 X cm-1) and a shoulder at 430 nm. Weak electrochromic bandshifts in the infrared were also evident. The spectrum of the reduced primary acceptor (Q-A) exhibited a major peak at 412 nm (delta epsilon = 10 mM-1 X cm-1) consistent with the assignment of menaquinone as QA. The Q-A spectrum also had minor peaks at 385 and 455 nm in the blue region. The same spectrum was recorded after quantitative removal of the secondary acceptor, when only menaquinone was present in the reaction centers. Spectral features in the near-infrared due to Q-A were attributed to electrochromic effects on bacteriochlorophyll (BChl) b and bacteriopheophytin (BPh) b pigments resulting in a distinctive split peak at 810 and 830 nm (delta epsilon = 8 mM-1 X cm-1). The menaquinone was identified as 2-methyl-3-nonylisoprenyl-1,4-naphthoquinone (menaquinone-9). The native QA activity was uniquely provided by this menaquinone and ubiquinone was not involved. QB activity, on the other hand, displayed at least a 40-fold preference for ubiquinone (Q-10) as compared to menaquinone. Thus, both quinone-binding sites display remarkable specificity for their respective quinones. In the absence of donors to P+, charge recombination of the P+Q-A and P+Q-B pairs had half-times of 1.1 +/- 0.2 and 110 +/- 20 ms, respectively, at pH 9.0, indicating an electron-transfer equilibrium constant (Kapp2) of at least 100 for Q-AQB in equilibrium QAQ-B. Also observed was a slow recombination of the cytochrome c-558+ Q-A pair, with t 1/2 = 2 +/- 0.5 s at pH 6.     

MHC class II invariant chains in antigen processing and presentation

Most protein antigens cannot elicit a T-cell response unless they are processed to peptides, which are then presented to T lymphocytes by surface MHC class II molecules. Recent evidence supports an essential role of the invariant chain associated with class II MHC polypeptides in antigen processing.     

Inhibition and labelling of isolated reaction centers from Rhodobacter sphaeroides by dicyclohexylcarbodiimide

The effect of dicyclohexylcarbodiimide (DCCD) on electron transfer in the acceptor quinone complex of reaction centers (RC) from Rhodobacter sphaeroides is reported. DCCD covalently labelled the RC over a wide concentration range. At low concentrations (<10 M) the binding was specific for the L subunit. At relatively high concentrations (>100 M) DCCD accelerated the rate of charge recombination of the P⁺Q_B ^- state, consistent with a decrease in the equilibrium constant between Q_A ^-Q_B and Q_AQ_B ^-. At similar concentrations, in the presence of cytochrome c as exogenous donor, turnover of the RC was inhibited such that only three cytochromes were oxidized in a train of flashes. Both these inhibitory effects were fully reversed by dialysis, indicating that stable covalent binding was not involved. Possible mechanisms of action are discussed in terms of the putative role of specific residues in proton transfer and protonation and release of quinol from the RC.     

A major difference between the divergence patterns within the lines-1 families in mice and voles

L1 retroposons are represented in mice by subfamilies of interspersed sequences of varied abundance. Previous analyses have indicated that subfamilies are generated by duplicative transposition of a small number of members of the L1 family, the progeny of which then become a major component of the murine L1 population, and are not due to any active processes generating homology within preexisting groups of elements in a particular species. In mice, more than a third of the L1 elements belong to a clade that became active approximately 5 Mya and whose elements are > or = 95% identical. We have collected sequence information from 13 L1 elements isolated from two species of voles (Rodentia: Microtinae: Microtus and Arvicola) and have found that divergence within the vole L1 population is quite different from that in mice, in that there is no abundant subfamily of homologous elements. Individual L1 elements from voles are very divergent from one another and belong to a clade that began a period of elevated duplicative transposition approximately 13 Mya. Sequence analyses of portions of these divergent L1 elements (approximately 250 bp each) gave no evidence for concerted evolution having acted on the vole L1 elements since the split of the two vole lineages approximately 3.5 Mya; that is, the observed interspecific divergence (6.7%-24.7%) is not larger than the intraspecific divergence (7.9%-27.2%), and phylogenetic analyses showed no clustering into Arvicola and Microtus clades.      

Molecular phylogeny and divergence times of drosophilid species

The phylogenetic relationships and divergence times of 39 drosophilid species were studied by using the coding region of the Adh gene. Four genera--Scaptodrosophila, Zaprionus, Drosophila, and Scaptomyza (from Hawaii)--and three Drosophila subgenera--Drosophila, Engiscaptomyza, and Sophophora--were included. After conducting statistical analyses of the nucleotide sequences of the Adh, Adhr (Adh-related gene), and nuclear rRNA genes and a 905-bp segment of mitochondrial DNA, we used Scaptodrosophila as the outgroup. The phylogenetic tree obtained showed that the first major division of drosophilid species occurs between subgenus Sophophora (genus Drosophila) and the group including subgenera Drosophila and Engiscaptomyza plus the genera Zaprionus and Scaptomyza. Subgenus Sophophora is then divided into D. willistoni and the clade of D. obscura and D. melanogaster species groups. In the other major drosophilid group, Zaprionus first separates from the other species, and then D. immigrans leaves the remaining group of species. This remaining group then splits into the D. repleta group and the Hawaiian drosophilid cluster (Hawaiian Drosophila, Engiscaptomyza, and Scaptomyza). Engiscaptomyza and Scaptomyza are tightly clustered. Each of the D. repleta, D. obscura, and D. melanogaster groups is monophyletic. The splitting of subgenera Drosophila and Sophophora apparently occurred about 40 Mya, whereas the D. repleta group and the Hawaiian drosophilid cluster separated about 32 Mya. By contrast, the splitting of Engiscaptomyza and Scaptomyza occurred only about 11 Mya, suggesting that Scaptomyza experienced a rapid morphological evolution. The D. obscura and D. melanogaster groups apparently diverged about 25 Mya. Many of the D. repleta group species studied here have two functional Adh genes (Adh-1 and Adh-2), and these duplicated genes can be explained by two duplication events.      

Sulfate reduction and S-oxidation in a moorland pool sediment

In an oligotrophic moorland pool in The Netherlands, S cycling near the sediment/water boundary was investigated by measuring (1) SO₄ ^2– reduction rates in the sediment, (2) depletion of SO₄ ^2– in the overlying water column and (3) release of³⁵S from the sediment into the water column. Two locations differing in sediment type (highly organic and sandy) were compared, with respect to reduction rates and depletion of SO₄ ^2– in the overlying water.Sulfate reduction rates in sediments of an oligotrophic moorland pool were estimated by diagenetic modelling and whole core³⁵SO₄ ^2– injection. Rates of SO₄ ^2– consumption in the overlying water were estimated by changes in SO₄ ^2– concentration over time in in situ enclosures. Reduction rates ranged from 0.27–11.2 mmol m^–2 d^–1. Rates of SO₄ ^2– uptake from the enclosed water column varied from –0.5, –0.3 mmol m^–2 d^–1 (November) to 0.43–1.81 mmol m^–2 d^–1 (July, August and April). Maximum rates of oxidation to SO₄ ^2– in July 1990 estimated by combination of SO₄ ^2– reduction rates and rates of in situ SO₄ ^2– uptake in the enclosed water column were 10.3 and 10.5 mmol m^–2 d^–1 at an organic rich and at a sandy site respectively.Experiments with³⁵S^2– and³⁵SO₄ ^2– tracer suggested (1) a rapid formation of organically bound S from dissimilatory reduced SO₄ ^2– and (2) the presence of mainly non SO₄ ^2–-S derived from reduced S transported from the sediment into the overlying water. A³⁵S^2– tracer experiment showed that about 7% of³⁵S^2– injected at 1 cm depth in a sediment core was recovered in the overlying water column.Sulfate reduction rates in sediments with higher volumetric mass fraction of organic matter did not significantly differ from those in sediments with a lower mass fraction of organic matter.Corresponding author     

Investigations on the influence of headgroup substitution and isoprene side-chain length in the function of primary and secondary quinones of bacterial reaction centers

The contributions of headgroup and side-chain in the binding and function of the primary (QA) and secondary (QB) quinones of isolated reaction centers (RCs) from Rhodobacter sphaeroides were investigated. Various ubiquinones and structurally similar quinones were reconstituted into RCs depleted of one (1Q-RCs) or both (0Q-RCs) quinones. The influence of partition coefficients on the apparent binding affinities was minimized by expressing dissociation constants in terms of the mole fraction of quinone partitioned into the detergent. It was then apparent that the size of the isoprenyl side-chain was of little consequence in determining the binding affinity or the functional competence of either QA or QB, although an alkyl chain of equivalent size was a poor substitute. The degree of substitution of the headgroup, however, was a sensitive determinant of binding. For both quinone sites, the trisubstituted plastoquinones bond more weakly than the fully substituted ubiquinones. Similarly, for binding to the QA site, duroquinone (tetramethylbenzoquinone) bound much more strongly than trimethylbenzoquinone. The affinity of the QA site for ubiquinones was about 20-times stronger than the QB site, but the QB site is probably not more specific than the QA site. However, QB function depends on a suitable redox free-energy drop from QA as well as binding, and of all the quinones tested only the ubiquinones simultaneously supported full QA and QB activity. Even plastoquinone-A, which fills both roles in Photosystem II, was unable to do so in bacterial RCs, although it did bind. The unique ability of ubiquinones to both bind and provide the appropriate redox span is discussed. The temperature dependence of binding of the isoprenyl ubiquinones at the QA site changed markedly with chain length. For Q-10-Q-7, the binding enthalpy was positive and net binding was entirely driven by entropic factors. For the shorter-chain ubiquinones, Q-6-Q-1, both entropy and enthalpy of binding were favorable. This strong entropy-enthalpy compensation is suggested to arise from antagonistic interactions (anticooperativity) between headgroup and tail binding. For QB function by hydrophobic quinones, the temperature dependence of the micelle properties prevented easy access to thermodynamic parameters. However, for water-soluble Q-0, binding to the QB site was determined to be enthalpically driven.(ABSTRACT TRUNCATED AT 400 WORDS)     

Electron acceptors of bacterial photosynthetic reaction centers. II. H+ binding coupled to secondary electron transfer in the quinone acceptor complex.

The photoreduction of ubiquinone in the electron acceptor complex (QIQII) of photosynthetic reaction centers from Rhodopseudomonas sphaeroides, R26, was studied in a series of short, saturating flashes. The specific involvement of H+ in the reduction was revealed by the pH dependence of the electron transfer events and by net H+ binding during the formation of ubiquinol, which requires two turnovers of the photochemical act. On the first flash QII receives an electron via QI to form a stable ubisemiquinone anion (QII-); the second flash generates QI-. At low pH the two semiquinones rapidly disproportionate with the uptake of 2 H+, to produce QIIH2. This yields out-of-phase binary oscillations for the formation of anionic semiquinone and for H+ uptake. Above pH 6 there is a progressive increase in H+ binding on the first flash and an equivalent decrease in binding on the second flash until, at about pH 9.5, the extent of H+ binding is the same on all flashes. The semiquinone oscillations, however, are undiminished up to pH 9. It is suggested that a non-chromophoric, acid-base group undergoes a pK shift in response to the appearance of the anionic semiquinone and that this group is the site of protonation on the first flash. The acid-base group, which may be in the reaction center protein, appears to be subsequently involved in the protonation events leading to fully reduced ubiquinol. The other proton in the two electron reduction of ubiquinone is always taken up on the second flash and is bound directly to QII-. At pH values above 8.0, it is rate limiting for the disproportionation and the kinetics, which are diffusion controlled, are properly responsive to the prevailing pH. Below pH 8, however, a further step in the reaction mechanism was shown to be rate limiting for both H+ binding electron transfer following the second flash.