Inhibition of Azotobacter vinelandii ribonucleic acid polymerase by glutamyl, tyrosyl copolymers.
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The Mo-nitrogenase-catalyzed reduction of both cyanide and azide results in the production of excess NH3, which is an amount of NH3 over and above that expected to be formed from the well-recognized reactions. Several suggestions about the possible sources of excess NH3 have been made, but previous attempts to characterize these reactions have met with either limited (or no) success or controversy. Because V-nitrogenase has a propensity to release partially reduced intermediates, e.g., N2H4 during N2 reduction, it was selected to probe the reduction of cyanide and azide. Sensitive assay procedures were developed and employed to monitor the production of either HCHO or CH3OH (its further two-electron-reduced product) from HCN. Like Mo-nitrogenase, V-nitrogenase suffered electron-flux inhibition by CN- (but was much less sensitive than Mo-nitrogenase), but unlike the case for Mo-nitrogenase, MgATP hydrolysis was also inhibited by CN-. V-Nitrogenase also released more of the four-electron-reduced intermediate, CH3NH2, than did Mo-nitrogenase. At high NaCN concentrations, V-nitrogenase directed a significant percentage of electron flux into excess NH3, and under these conditions, substantial amounts of HCHO, but no CH3OH, were detected for the first time. With azide, in contrast to the case for Mo-nitrogenase, both total electron flux and MgATP hydrolysis with V-nitrogenase were inhibited. V-Nitrogenase, unlike Mo-nitrogenase, showed no preference between the two-electron reduction to N2-plus-NH3 and the six-electron reduction to N2H4-plus-NH3. V-Nitrogenase formed more excess NH3, but reduction of the N2 produced by the two-electron reduction of N3(-) was not its source. Rather, it was formed directly by the eight-electron reduction of N3(-). Unlike Mo-nitrogenase, CO could not completely eliminate either cyanide or azide reduction by V-nitrogenase. CO did, however, eliminate the inhibition of both electron flux and MgATP hydrolysis by CN-, but not that caused by azide. These different responses to CO suggest different sites or modes of interaction for these two substrates with V-nitrogenase.
Deletion of nifB results in the formation of a variant nitrogenase MoFe protein (DeltanifB MoFe protein) that appears to contain two normal [8Fe-7S] P clusters. This protein can be reactivated to form the holo MoFe protein upon addition of isolated FeMo cofactor. In contrast, deletion of nifH results in a variant protein (DeltanifH MoFe protein) that appears to contain FeS clusters different from the normal P cluster, presumably representing precursors of the normal P cluster. The DeltanifH MoFe protein is not reconstituted to the holo MoFe protein with isolated FeMo cofactor. The EPR and EXAFS spectroscopic properties of FeS clusters in the DeltanifH MoFe protein clearly differ from those of the normal P cluster found in the DeltanifB MoFe protein and suggest the presence of [4Fe-4S]-like clusters. To further characterize the metal cluster structures in the DeltanifH MoFe protein, a variable-temperature, variable-field magnetic circular dichroism (VTVH-MCD) spectroscopic study has been undertaken on both the DeltanifB MoFe protein and the DeltanifH MoFe protein in both the dithionite-reduced and oxidized states. This study clearly shows that each half of the dithionite-reduced DeltanifH MoFe protein contains a [4Fe-4S]+ cluster paired with a diamagnetic [4Fe-4S]-like cluster. Upon oxidation, the VTVH-MCD spectrum of the DeltanifH MoFe protein reveals a paramagnetic, albeit EPR-silent system, suggesting an integer spin state. These results suggest that the DeltanifH MoFe protein contains a pair of neighboring, unusual [4Fe-4S]-like clusters, which are paramagnetic in their oxidized state.
The arginine-277 residue of the alpha-subunit of the nitrogenase MoFe protein was targeted for substitution because it is (i) a close neighbor of alpha-cysteine-275, which is one of only two residues anchoring the FeMo cofactor to the polypeptide, and (ii) a component of a potential channel for entry/exit of substrates/products and for accepting FeMo cofactor during MoFe-protein maturation. Several of the eight mutant strains constructed were capable of good diazotrophic growth and also contained FeMo cofactor as indicated by its biologically unique S = 3/2 EPR spectrum. These observations indicate that the positively charged alpha-arginine-277 residue is not required for acceptance of the negatively charged FeMo cofactor by the separately synthesized, cofactor-deficient, apo-MoFe protein. The wide range of nitrogen-fixation phenotypes shown by these mutant strains generally correlated well with their C2H2- and proton-reduction activities, which range from 5 to 65% of wild-type activity. One notable exception is the histidine-substituted strain, DJ788 (alpha-277His). This strain, although unable to fix N2 and grow diazotrophically, elaborates an altered alpha-277His MoFe protein that catalyzes the reduction of the alternative substrates, C2H2, HCN, HN3, and protons. These observations are best explained if multiple redox levels are available to the MoFe protein but the alpha-277His MoFe protein is incapable of reaching the more-reduced redox levels required for nitrogen fixation. Under nonsaturating CO concentrations, the alpha-277His MoFe-protein-catalyzed reduction of C2H2 showed sigmoidal kinetics, which is consistent with inhibitor-induced cooperativity among two C2H4-evolving sites and indicates the presence of three sites, which can be simultaneously occupied, on the MoFe protein. Similar kinetics were not observed for alpha-277His MoFe-protein-catalyzed reduction of either HCN or HN3 with nonsaturating CO levels, indicating that these substrates are unlikely to share common binding sites with C2H2. Further, CN- did not induce cooperativity in C2H2 reduction and, therefore, CO and CN- are unlikely to share a common binding site. These changed substrate specificities, reinforced by changes in the FeMo-cofactor-derived S = 3/2 EPR spectrum, clearly indicate the importance of the alpha-277 residue in catalysis and the delicate control exerted on the properties of bound FeMo cofactor by its polypeptide environment.
Wild-type nitrogenase MoFe protein shows a deep 14N electron spin-echo envelope modulation (ESEEM) arising from a nitrogen nucleus (N1) coupled to the S = 3/2 spin system of the FeMo-cofactor of the MoFe protein. A previous ESEEM study on altered MoFe proteins generated by substitutions at the alpha-195-histidine position suggested that alpha-195-histidine provides a hydrogen bond to the FeMo-cofactor but is not the source of the 14N1 modulation [DeRose et al. (1995) Biochemistry 34, 2809-2814]. This study also raised the possibility of a correlation between ESEEM spectroscopic properties and the nitrogenase phenotype. We now report ESEEM studies on altered MoFe proteins with substitutions at residues alpha-96-arginine, alpha-359-arginine, and alpha-381-phenylalanine to (i) assign the first-shell hydrogen bonding as revealed by the 14N modulation; (ii) explore the mechanistic relevance of the ESEEM signatures to nitrogenase activity; and (iii) study microscopic changes within the polypeptide environment of the FeMo-cofactor. Present ESEEM data reveals that two kinds of 14N modulations are present in wild-type MoFe protein. A new 2-dimensional procedure for high-precision analysis of the ESEEM data of the MoFe proteins shows that the deep wild-type ESEEM modulation (denoted N1) has a hyperfine-coupling constant of Aiso = 1.05 MHz and nuclear quadrupole coupling parameters of e2qQ = 2.17 MHz, eta = 0.59; the other (denoted N2) has a smaller hyperfine coupling of Aiso = approximately 0.5 MHz and e2qQ = approximately 3.5 MHz, eta = approximately 0.4. The N2 ESEEM pattern is more obvious when unmasked by substitutions that result in the loss of the deep N1 modulation. Correlations of the ESEEM properties and catalytic activities of the altered MoFe proteins suggest that (i) the side chain of the alpha-359-arginine is the source of the deep ESEEM N1 modulation; (ii) one or both of the amide nitrogens of alpha-356-glycine/alpha-357-glycine are responsible for the weak N2 modulation; (iii) substitution of the nonpolar alpha-381-phenylalanine residue, as well as substitution of either the alpha-195-histidine or alpha-359-arginine residues, can eliminate the N1 interaction with FeMo-cofactor; and (iv) ESEEM can be used to detect slight reorientations of FeMo-cofactor within its polypeptide pocket, although the mechanistic relevance of the loss or perturbation of the hydrogen-bonding interactions between FeMo-cofactor and polypeptide environment has not yet been established.
Nitrogenase consists of two metalloproteins (Fe protein and MoFe protein) which are assumed to associate and dissociate to transfer a single electron to the substrates. This cycle, called the Fe protein cycle, is driven by MgATP hydrolysis and is repeated until the substrates are completely reduced. The rate-limiting step of the cycle, and substrate reduction, is suggested to be the dissociation of the Fe protein-MoFe protein complex which is obligatory for the reduction of the Fe protein [Thorneley, R. N. F., and Lowe, D. J. (1983) Biochem. J. 215, 393-403]. This hypothesis is based on experiments with dithionite as the reductant. We also tested besides dithionite flavodoxin hydroquinone, a physiological reductant. Two models could describe the experimental data of the reduction by dithionite. The first model, with no reduction of Fe protein bound to MoFe protein, predicts a rate of dissociation of the protein complex of 8.1 s-1. This rate is too high to be the rate-limiting step of the Fe protein cycle (kobs = 3.0 s-1). The second model, with reduction of the Fe protein in the nitrogenase complex, predicts a rate of dissociation of the protein complex of 2.3 s-1, which in combination with reduction of the nitrogenase complex can account for the observed turnover rate of the Fe protein cycle. When flavodoxin hydroquinone (155 microM) was the reductant, the rate of reduction of oxidized Fe protein in the nitrogenase complex (kobs approximately 400 s-1) was 100 times faster than the turnover rate of the cycle with flavodoxin as the reductant (4 s-1). Pre-steady-state electron uptake experiments from flavodoxin hydroquinone indicate that before and after reduction of the nitrogenase complex relative slow reactions take place, which limits the rate of the Fe protein cycle. These results are discussed in the context of the kinetic models of the Fe protein cycle of nitrogenase.
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