Thermal unfolding of Apo and Holo Desulfovibrio desulfuricans flavodoxin: cofactor stabilizes folded and intermediate states

We here compare thermal unfolding of the apo and holo forms of Desulfovibrio desulfuricans flavodoxin, which noncovalently binds a flavin mononucleotide (FMN) cofactor. In the case of the apo form, fluorescence and far-UV circular dichroism (CD) detected transitions are reversible but do not overlap (T(m) of 50 and 60 degrees C, respectively, pH 7). The thermal transitions for the holo form follow the same pattern but occur at higher temperatures (T(m) of 60 and 67 degrees C for fluorescence and CD transitions, respectively, pH 7). The holoprotein transitions are also reversible and exhibit no protein concentration dependence (above 10 microM), indicating that the FMN remains bound to the polypeptide throughout. Global analysis shows that the thermal reactions for both apo and holo forms proceed via an equilibrium intermediate that has approximately 90% nativelike secondary structure and significant enthalpic stabilization relative to the unfolded states. Incubation of unfolded holoflavodoxin at high temperatures results in FMN dissociation. Rebinding of FMN at these conditions is nominal, and therefore, cooling of holoprotein heated to 95 degrees C follows the refolding pathway of the apo form. However, FMN readily rebinds to the apoprotein at lower temperatures. We conclude that (1) a three-state thermal unfolding behavior appears to be conserved among long- and short-chain, as well as apo and holo forms of, flavodoxins and (2) flavodoxin's thermal stability (in both native and intermediate states) is augmented by the presence of the FMN cofactor.     

Folding of Desulfovibrio desulfuricans flavodoxin is accelerated by cofactor fly-casting

Folding of cofactor-binding proteins involves ligand binding in addition to polypeptide folding. We here assess the kinetic folding/binding landscape for Desulfovibrio desulfuricans flavodoxin that coordinates an FMN cofactor. The apo-form folds in a two-step process involving a burst-phase intermediate. Studies on Tyr98Ala and Trp60Ala variants reveal that these aromatics-that stack with the FMN in the holo-form-are not participating in the apo-protein folding pathway. However, these residues are essential for FMN interactions with the unfolded protein during refolding of holo-flavodoxin. Unfolding of wild-type holo-flavodoxin is coupled to FMN dissociation whereas for Tyr98Ala and Trp60Ala holo-variants, FMN dissociates before polypeptide unfolding. Both variants refold as apo-proteins before FMN rebinds. In sharp contrast, refolding of unfolded wild-type holo-flavodoxin is over an order of magnitude faster than that of the apo-form, the pathway does not include a burst-phase intermediate, and the speed is independent of FMN excess ratio. These observations demonstrate that FMN binds rapidly to the unfolded polypeptide and guides folding straight to the native state. As this path to functional D. desulfuricans holo-flavodoxin is faster than if the cofactor binds to pre-folded apo-protein, this is one of few examples where molecular recognition via a "fly-casting" mechanism is kinetically favored.     

FMN binding and unfolding of Desulfovibrio desulfuricans flavodoxin: "hidden" intermediates at low denaturant concentrations

The flavin mononucleotide (FMN) cofactor in Desulfovibrio desulfuricans flavodoxin stays associated with the polypeptide upon guanidine hydrochloride (GuHCl) induced unfolding. Using isothermal titration calorimetry (ITC), we determined the affinity of FMN for the flavodoxin polypeptide as a function of both urea and GuHCl concentrations (pH 7, 25 degrees C). The FMN affinity for folded and GuHCl-unfolded flavodoxin differs 10-fold, which is in agreement with the difference in thermodynamic stability between the apo- and holo-forms. In contrast, the urea-unfolded protein does not interact with FMN and equilibrium unfolding of holo-flavodoxin in urea results in FMN dissociation prior to polypeptide unfolding. ANS-binding, near-UV circular dichroism (CD), acrylamide quenching and FMN-emission experiments reveal the presence of native-like intermediates, not detected by far-UV CD and aromatic fluorescence detection methods, in low concentrations of both denaturants. Time-resolved experiments show that FMN binding is fastest at GuHCl concentrations where the native-like intermediate species is populated.     

Cloning and characterization of the flavodoxin gene from Desulfovibrio desulfuricans

The gene coding for the flavodoxin protein from Desulfovibrio desulfuricans [Essex 6] (ATCC 29577) has been cloned and sequenced. The gene was identified on Southern blots of HindIII-digested genomic DNA by hybridization to the coding region for the flavodoxin from Desulfovibrio vulgaris [Hildenborough] (Krey, G.D., Vanin, E.F. and Swenson, R.P. (1988) J. Biol. Chem. 263, 15436-15443). Ultimately, a 1.8 kb TaqI fragment was cloned which contains an open reading frame of 447 nucleotides coding for an acidic protein of 148 amino acids and calculated molecular weight of 15,726. The derived amino acid sequence of this protein is 47% identical to the flavodoxin from D. vulgaris. Regions of the polypeptide which form the flavin mononucleotide binding site are largely homologous; however, some perhaps significant differences are noted. The aromatic amino acid residues that flank the flavin isoalloxazine ring in the D. vulgaris structure, i.e., tryptophan-60 and tyrosine-98, are conserved in this flavodoxin.     

A comparison of the urea-induced unfolding of apoflavodoxin and flavodoxin from Desulfovibrio vulgaris.

The kinetics and thermodynamics of the urea-induced unfolding of flavodoxin and apoflavodoxin from Desulfovibrio vulgaris were investigated by measuring changes in flavin and protein fluorescence. The reaction of urea with flavodoxin is up to 5000 times slower than the reaction with the apoprotein (0.67 s(-1) in 3 m urea in 25 mm sodium phosphate at 25 degrees C), and it results in the dissociation of FMN. The rate of unfolding of apoflavodoxin depends on the urea concentration, while the reaction with the holoprotein is independent of urea. The rates decrease in high salt with the greater effect occurring with apoprotein. The fluorescence changes fit two-state models for unfolding, but they do not exclude the possibility of intermediates. Calculation suggests that 21% and 30% of the amino-acid side chains become exposed to solvent during unfolding of flavodoxin and apoflavodoxin, respectively. The equilibrium unfolding curves move to greater concentrations of urea with increase of ionic strength. This effect is larger with phosphate than with chloride, and with apoflavodoxin than with flavodoxin. In low salt the conformational stability of the holoprotein is greater than that of apoflavodoxin, but in high salt the relative stabilities are reversed. It is calculated that two ions are released during unfolding of the apoprotein. It is concluded that the urea-dependent unfolding of flavodoxin from D. vulgaris occurs because apoprotein in equilibrium with FMN and holoprotein unfolds and shifts the equilibrium so that flavodoxin dissociates. Small changes in flavin fluorescence occur at low concentrations of urea and these may reflect binding of urea to the holoprotein.     

1H and 15N NMR resonance assignments and solution secondary structure of oxidized Desulfovibrio desulfuricans flavodoxin

Summary Sequence-specific ¹H and ¹⁵N resonance assignments have been made for 137 of the 146 nonprolyl residues in oxidized Desulfovibrio desulfuricans [Essex 6] flavodoxin. Assignments were obtained by a concerted analysis of the heteronuclear three-dimensional ¹H-¹⁵N NOESY-HMQC and TOCSY-HMQC data sets, recorded on uniformly ¹⁵N-enriched protein at 300 K. Numerous side-chain resonances have been partially or fully assigned. Residues with overlapping ¹H^N chemical shifts were resolved by a three-dimensional ¹H-¹⁵N HMQC-NOESY-HMQC spectrum. Medium-and long-range NOEs, ³J_NH coupling constants, and ¹H^N exchange data indicate a secondary structure consisting of five parallel -strands and four -helices with a topology similar to that of Desulfovibrio vulgaris [Hidenborough] flavodoxin. Prolines at positions 106 and 134, which are not conserved in D. vulgaris flavodoxin, contort the two C-terminal -helices.Abbreviations CSI chemical shift index - DQF-COSY double-quantum-filtered correlation spectroscopy - DIPSI decoupling in the presence of scalar interactions - FMN flavin mononucleotide - GARP globally optimized alternating phase rectangular pulse - HMQC heteronuclear multiple-quantum coherence - HSQC heteronuclear single-quantum coherence - NOE nuclear Overhauser effect - NOESY nuclear Overhauser enhancement spectroscopy - TOCSY total correlation spectroscopy - TPPI time-proportional phase increments - TSP 3-(trimethylsilyl)propionic-2,2,3,3-d ₄ acid, sodium salt     

Toxicity of Al to Desulfovibrio desulfuricans

The toxicity of Al to Desulfovibrio desulfuricans G20 was assessed over a period of 8 weeks in a modified lactate C medium buffered at four initial pHs (5.0, 6.5, 7.2, and 8.3) and treated with five levels of added Al (0, 0.01, 0.1, 1.0, and 10 mM). At pH 5, cell population densities decreased significantly and any effect of Al was negligible compared to that of the pH. At pHs 6.5 and 7.2, the cell population densities increased by 30-fold during the first few days and then remained stable for soluble-Al concentrations of <5 × 10⁻⁵ M. In treatments having total-Al concentrations of ≥1 mM, soluble-Al concentrations exceeded 5 × 10⁻⁵ M and limited cell population growth substantially and proportionally. At pH 8.3, soluble-Al concentrations were below the 5 × 10⁻⁵ M toxicity threshold and cell population density increases of 20- to 40-fold were observed. An apparent cell population response to added Al at pH 8.3 was attributed to the presence of large, spirilloidal bacteria (accounting for as much as 80% of the cells at the 10 mM added Al level). Calculations of soluble-Al speciation for the pH 6.5 and 7.2 treatments that showed Al toxicity suggested the possible presence of the Al₁₃O₄(OH)₂₄(H₂O)₁₂⁷⁺ “tridecamer” cation and an inverse correlation of the tridecamer concentration and the cell population density. Analysis by ²⁷Al nuclear magnetic resonance spectroscopy, however, yielded no evidence of this species in freshly prepared samples or those taken 800 days after inoculation. Exclusion of the tridecamer species from the aqueous speciation calculations at pHs 6.5 and 7.2 yielded inverse correlations of the neutral Al(OH)₃ and anionic Al(OH)₄⁻ monomeric species with cell population density, suggesting that one or both of these ions bear primary responsibility for the toxicity observed.     

Toxicity of Al to Desulfovibrio desulfuricans

The toxicity of Al to Desulfovibrio desulfuricans G20 was assessed over a period of 8 weeks in a modified lactate C medium buffered at four initial pHs (5.0, 6.5, 7.2, and 8.3) and treated with five levels of added Al (0, 0.01, 0.1, 1.0, and 10 mM). At pH 5, cell population densities decreased significantly and any effect of Al was negligible compared to that of the pH. At pHs 6.5 and 7.2, the cell population densities increased by 30-fold during the first few days and then remained stable for soluble-Al concentrations of <5 x 10(-5) M. In treatments having total-Al concentrations of > or =1 mM, soluble-Al concentrations exceeded 5 x 10(-5) M and limited cell population growth substantially and proportionally. At pH 8.3, soluble-Al concentrations were below the 5 x 10(-5) M toxicity threshold and cell population density increases of 20- to 40-fold were observed. An apparent cell population response to added Al at pH 8.3 was attributed to the presence of large, spirilloidal bacteria (accounting for as much as 80% of the cells at the 10 mM added Al level). Calculations of soluble-Al speciation for the pH 6.5 and 7.2 treatments that showed Al toxicity suggested the possible presence of the Al(13)O(4)(OH)(24)(H(2)O)(12)(7+) "tridecamer" cation and an inverse correlation of the tridecamer concentration and the cell population density. Analysis by (27)Al nuclear magnetic resonance spectroscopy, however, yielded no evidence of this species in freshly prepared samples or those taken 800 days after inoculation. Exclusion of the tridecamer species from the aqueous speciation calculations at pHs 6.5 and 7.2 yielded inverse correlations of the neutral Al(OH)(3) and anionic Al(OH)(4)(-) monomeric species with cell population density, suggesting that one or both of these ions bear primary responsibility for the toxicity observed.     

Reduction of uranium by Desulfovibrio desulfuricans.

The possibility that sulfate-reducing microorganisms contribute to U(VI) reduction in sedimentary environments was investigated. U(VI) was reduced to U(IV) when washed cells of sulfate-grown Desulfovibrio desulfuricans were suspended in a bicarbonate buffer with lactate or H2 as the electron donor. There was no U(VI) reduction in the absence of an electron donor or when the cells were killed by heat prior to the incubation. The rates of U(VI) reduction were comparable to those in respiratory Fe(III)-reducing microorganisms. Azide or prior exposure of the cells to air did not affect the ability of D. desulfuricans to reduce U(VI). Attempts to grow D. desulfuricans with U(VI) as the electron acceptor were unsuccessful. U(VI) reduction resulted in the extracellular precipitation of the U(IV) mineral uraninite. The presence of sulfate had no effect on the rate of U(VI) reduction. Sulfate and U(VI) were reduced simultaneously. Enzymatic reduction of U(VI) by D. desulfuricans was much faster than nonenzymatic reduction of U(VI) by sulfide, even when cells of D. desulfuricans were added to provide a potential catalytic surface for the nonenzymatic reaction. The results indicate that enzymatic U(VI) reduction by sulfate-reducing microorganisms may be responsible for the accumulation of U(IV) in sulfidogenic environments. Furthermore, since the reduction of U(VI) to U(IV) precipitates uranium from solution, D. desulfuricans might be a useful organism for recovering uranium from contaminated waters and waste streams.     

Pyruvate-carbon dioxide exchange reaction of Desulfovibrio desulfuricans

Suh, Byungse (University of Kansas, Lawrence), and J. M. Akagi. Pyruvate-carbon dioxide exchange reaction of Desulfovibrio desulfuricans. J. Bacteriol. 91:2281-2285. 1966.-The pyruvate-CO(2) exchange reaction, catalyzed by Desulfovibrio desulfuricans, required the presence of phosphate and coenzyme A. However, the requirement for phosphate disappeared when the concentration of coenzyme A was increased to a level of 3.8 x 10(-3)m. Passing crude extracts through a diethylaminoethyl-cellulose column and an Amberlite CG-50 ion-exchange column, to remove ferredoxin and cytochrome c(3), resulted in a marked decrease in exchange activity; full activity was restored by the addition of ferredoxin or cytochrome c(3). Fe(++) or Co(++) stimulated the exchange of CO(2) into pyruvate.     

Reduction of uranium by Desulfovibrio desulfuricans.

The possibility that sulfate-reducing microorganisms contribute to U(VI) reduction in sedimentary environments was investigated. U(VI) was reduced to U(IV) when washed cells of sulfate-grown Desulfovibrio desulfuricans were suspended in a bicarbonate buffer with lactate or H2 as the electron donor. There was no U(VI) reduction in the absence of an electron donor or when the cells were killed by heat prior to the incubation. The rates of U(VI) reduction were comparable to those in respiratory Fe(III)-reducing microorganisms. Azide or prior exposure of the cells to air did not affect the ability of D. desulfuricans to reduce U(VI). Attempts to grow D. desulfuricans with U(VI) as the electron acceptor were unsuccessful. U(VI) reduction resulted in the extracellular precipitation of the U(IV) mineral uraninite. The presence of sulfate had no effect on the rate of U(VI) reduction. Sulfate and U(VI) were reduced simultaneously. Enzymatic reduction of U(VI) by D. desulfuricans was much faster than nonenzymatic reduction of U(VI) by sulfide, even when cells of D. desulfuricans were added to provide a potential catalytic surface for the nonenzymatic reaction. The results indicate that enzymatic U(VI) reduction by sulfate-reducing microorganisms may be responsible for the accumulation of U(IV) in sulfidogenic environments. Furthermore, since the reduction of U(VI) to U(IV) precipitates uranium from solution, D. desulfuricans might be a useful organism for recovering uranium from contaminated waters and waste streams.     

Cytochrome c3 Mutants of Desulfovibrio desulfuricans

To explore the physiological role of tetraheme cytochrome c₃ in the sulfate-reducing bacterium Desulfovibrio desulfuricans G20, the gene encoding the preapoprotein was cloned, sequenced, and mutated by plasmid insertion. The physical analysis of the DNA from the strain carrying the integrated plasmid showed that the insertion was successful. The growth rate of the mutant on lactate with sulfate was comparable to that of the wild type; however, mutant cultures did not achieve the same cell densities. Pyruvate, the oxidation product of lactate, served as a poor electron source for the mutant. Unexpectedly, the mutant was able to grow on hydrogen-sulfate medium. These data support a role for tetraheme cytochrome c₃ in the electron transport pathway from pyruvate to sulfate or sulfite in D. desulfuricans G20.     

Characterization of sulfate transport in Desulfovibrio desulfuricans

Uptake of ³⁵S-labelled sulfate was studied with a new isolate of Desulfovibrio desulfuricans, strain CSN. Micromolar additions of sulfate (1–10 M or nmol/mg protein) to cell suspensions incubated in 150 mM KCl at-1°C were almost completely taken up and accumulated about 5,000-fold. Accumulation was not influenced by incubation in NaCl instead of KCl, by acidic pH (5.5) or by incubation under air for 10 min. In alkaline milieu (pH 8.5), after prolonged contact with air (2 h), or after growth with excess sulfate or thiosulfate as electron acceptor, the amount taken up was diminished approximately by half. Pasteurization inhibited sulfate uptake completely. With increasing concentrations of added sulfate (0.1 to 2.5 mM) the intracellular concentration increased only slowly up to 25 mM, and the accumulation factor decreased down to 8. Sulfate transport was reversible. Accumulated sulfate was rapidly lost from the cells after addition of excess non-labelled sulfate or after addition of the uncoupler carbonyl cyanide m-chlorophenylhydrazone (CCCP). The ATPase inhibitor dicyclohexylcarbodiimide (DCCD) specifically inhibited sulfate reduction but had no immediate influence on sulfate accumulation. Addition of the phosphate analogue arsenate (5 mM) was without effect. These results were not in favour of an ATP-dependent transport system. The K⁺-H⁺-antiporter nigericin (in 150 mM KCl) and the Na⁺-H⁺-antiporter monensin (in 150 mM NaCl) caused partial inhibition of sulfate accumulation, whereas the K⁺-transporter valinomycin (in 150 mM KCl) and the Na⁺-H⁺ exchange inhibitor amiloride (2 mM) were without effect. The permeant thiocyanate anion (150 mM) inhibited sulfate uptake by 60% at pH 7, and completely at pH 8.5. Although the effects of the different ionophores on the chemiosmotic gradients have not been studied so far, the results indicated that probably both, pH and drive sulfate accumulation and that sulfate is taken up electrogenically in symport with more than 2 protons. The structural sulfate analogues tungstate and molybdate (0.1 mM, each) did not affect sulfate accumulation, although molybdate inhibited sulfate reduction. Chromate completely blocked both of these activities. Sulfite and selenite caused little or no decrease of sulfate accumulation, whereas with thiosulfate and selenate significant inhibition was observed.Abbreviations CCCP carbonyl cyanide m-chlorophenylhydrazone - DCCD dicyclohexylcarbodiimide     

The preferred electron acceptor of Desulfovibrio desulfuricans CSN

Abstract: The sulfate-reducing bacterium Desulfovibrio desulfuricans strain CSN (DSM 104) oxidized H₂ with thiosulfate, sulfate, sulfite, nitrite, nitrate and oxygen with rates increasing (in the order listed) from 20 to 525 nmol H₂ min⁻¹ mg⁻¹ protein. Nitrate reduction was induced by nitrate or limiting concentrations of sulfate during growth, while all other activities were constitutive. Oxygen prevented reduction of all other electron acceptors, while nitrate and nitrite blocked the reduction of the sulfur compounds. In the presence of H₂ and reduced sulfur compounds, H₂ was the preferred electron donor. The cells oxidized thiosulfate or sulfite coupled to the reduction of nitrate to ammonia. This represents a novel type of metabolism connecting the sulfur and nitrogen cycles. It is concluded that oxygen is the preferred electron acceptor of D. desulfuricans . Sulfate reduction in oxic environments must be due to different organisms or mechanisms.     

Amino acid sequence of Desulfovibrio vulgaris flavodoxin.

The complete amino acid sequence for the 148-amino acid flavodoxin from Desulfovibrio vulgaris was determined to be: H3N+-Met-Pro-Lys-Ala-Leu-Ile-Val-Tyr-Gly-Ser-Thr-Thr-Gly-Asn-Thr-Glu-Tyr-Thr-Ala-Glu-Thr-Ile-Ala-Arg-Glu-Leu-Ala-Asn-Ala-Gly-Tyr-Glu-Val-Asp-Ser-Arg-Asp-Ala-Ala-Ser-Val-Glu-Ala-Gly-Gly-Leu-Phe-Glu-Gly-Phe-Asp-Leu-Val-Leu-Leu-Gly-Cys-Ser-Thr-Trp-Gly-Asp-Asp-Ser-Ile-Glu-Leu-Gln-Asp-Asp-Phe-Ile-Pro-Leu-Phe-Asp-Ser-Leu-Glu-Glu-Thr-Gly-Ala-Gln-Gly-Arg-Lys-Val-Ala-Cys-Phe-Gly-Cys-Gly-Asp-Ser-Ser-Tyr-Glu-Tyr-Phe-Cys-Gly-Ala-Val-Asp-Ala-IleGlu-Glu-Lys-Leu-Lys-Asn-Leu-Gly-Ala-Glu-Ile-Val-Gln-Asp-Gly-Leu-Arg-Ile-Asp-Gly-Asp-Pro-Arg-Ala-Ala-Arg-Asp-Asp-Ile-Val-Gly-Try-Ala-His-Asp-Val-Arg-Gly-Ala-Ile-COO. This protein is of interest as it was the first flavoenzyme for which high resolution x-ray diffraction studies were published (Watenpaugh, K.D., Sieker, L.C., and Jensen, L.H. (1973) Proc. NAtl. Acad. Sci. U.S.A. 70, 3857-3860). Ser(10), Thr(12), Asn(14), and Thr(15) were shown to bind the phosphate of the FMN while the isoalloxazine ring is positioned between Trp(60) and Tyr(98).     

A study on electron transport-driven proton translocation in Desulfovibrio desulfuricans

Proton translocation by washed cells of the sulfate-reducing bacterium Desulfovibrio desulfuricans strain Essex 6 was studied by means of pH and sulfide electrodes. Reversible extrusion of protons could be induced either by addition of electron acceptors to cells incubated under hydrogen, or by addition of hydrogen to cells incubated in the presence of an appropriate electron acceptor. Proton translocation was increased in the presence of ionophores that dissipate the membrane potential (thiocyanate, methyl triphenylphosphonium cation, but not valinomycin) and was sensitive to the uncoupler carbonylcyanide m-chlorophenylhydrazone (CCCP). Upon micromolar additions of H₂, usually sulfide was formed in stoichiometric amounts, and extrapolated H⁺/H₂ ratios were 1.8±0.5 with sulfate, 2.3±0.3 with sulfite and 0.5±0.1 with thiosulfate. In several experiments hydrogen pulses caused increased proton extrusion not associated with sulfide production. This was a hint that sulfite might be reduced via intermediates. In the absence of H₂S formation, extrapolated H⁺/H₂ ratios were 3.1±0.8 with sulfate, 3.4±1.1 with sulfite, 4.4±0.8 with thiosulfate and 6.3±1.2 with oxygen. Micromolar pulses of electron acceptors to cells incubated under H₂ caused less proton translocation than H₂ pulses in presence of excess of electron acceptor; extrapolated H⁺/H₂ ratios were 1.3±0.4 with sulfite, 3.3±0.9 with nitrite and 4.2±0.5 with oxygen. No proton translocation was observed after micromolar pulses of sulfate, thiosulfate or nitrate to cells incubated under hydrogen in the presence of thiocyanate. Inhibition experiments with CO and CuCl₂ revealed that the hydrogenase activity was localized in the intracellular space, and that no periplasmic hydrogenase was present. The results indicate that D. desulfuricans can generate a proton gradient by pumping protons across the cytoplasmic membrane.Abbreviations APS adenosine 5-phosphosulfate - CCCP carbonyl cyanide m-chlorophenylhydrazone - MTTP⁺ methyl triphenylphosphonium cation