EPR and M?ssbauer studies of nucleotide-bound nitrogenase iron protein from Azotobacter vinelandii

We have recently shown (Lindahl, P. A., Day, E. P., Kent, T. A., Orme-Johnson, W. H., and Münck, E. (1985) J. Biol. Chem. 260, 11160-11173) that the [4Fe-4S]1+ cluster of the native Fe protein can exist in two forms characterized by different cluster spin: an S = 1/2 state exhibiting a g = 1.94 type EPR signal and an S = 3/2 state yielding signals at g approximately 5.8 and 5.1. We have now extended our study of the Fe protein to include the MgATP- and MgADP-bound forms. The [4Fe-4S]1+ cluster of the nucleotide-bound Fe protein exists in a similar S = 1/2, S = 3/2 spin mixture. The S = 3/2 cluster exhibits a broad EPR signal at g approximately 4.8. In spectra of the MgATP-bound protein, we have also observed a g = 4.3 signal from an S = 5/2 state (D = 1 - 3 cm-1, E/D approximately 0.32). Various experiments strongly suggest that this signal does not originate from adventitiously bound Fe3+. The g = 4.3 signal may arise from approximately 2% of the [4Fe-4S]1+ clusters when MgATP is protein-bound. We have also discovered substoichiometric amounts of what appears to be ADP in some nominally nucleotide-free Fe protein samples. MgATP binds to Fe protein in the presence of perturbing solvents, resulting in EPR spectra similar to those of MgATP-bound samples in aqueous solutions; MgADP binding, on the other hand, results in signals more typical of the solvent state. Spectra of samples frozen during turnover of the nitrogenase system exhibit a mixture of spin states. Characterization of the Fe protein EPR signature described here should aid future mechanistic and nucleotide-binding studies.     

The Fe-only nitrogenase and the Mo nitrogenase from Rhodobacter capsulatus: a comparative study on the redox properties of the metal clusters present in the dinitrogenase components.

The dinitrogenase component proteins of the conventional Mo nitrogenase (MoFe protein) and of the alternative Fe-only nitrogenase (FeFe protein) were both isolated and purified from Rhodobacter capsulatus, redox-titrated according to the same procedures and subjected to an EPR spectroscopic comparison. In the course of an oxidative titration of the MoFe protein (Rc1Mo) three significant S = 1/2 EPR signals deriving from oxidized states of the P-cluster were detected: (1) a rhombic signal (g = 2.07, 1.96 and 1.83), which showed a bell-shaped redox curve with midpoint potentials (Em) of -195 mV (appearance) and -30 mV (disappearance), (2) an axial signal (g(parallel) = 2.00, g perpendicular = 1.90) with almost identical redox properties and (3) a second rhombic signal (g = 2.03, 2.00, 1.90) at higher redox potentials (> 100 mV). While the 'low-potential' rhombic signal and the axial signal have been both attributed to the one-electron-oxidized P-cluster (P1+) present in two conformationally different proteins, the 'high-potential' rhombic signal has been suggested rather to derive from the P3+ state. Upon oxidation, the FeFe protein (Rc1Fe) exhibited three significant S = 1/2 EPR signals as well. However, the Rc1Fe signals strongly deviated from the MoFe protein signals, suggesting that they cannot simply be assigned to different P-cluster states. (a) The most prominent feature is an unusually broad signal at g = 2.27 and 2.06, which proved to be fully reversible and to correlate with catalytic activity. The cluster giving rise to this signal appears to be involved in the transfer of two electrons. The midpoint potentials determined were: -80 mV (appearance) and 70 mV (disappearance). (b) Under weakly acidic conditions (pH 6.4) a slightly altered EPR signal occurred. It was characterized by a shift of the g values to 2.22 and 2.05 and by the appearance of an additional negative absorption-shaped peak at g = 1.86. (c) A very narrow rhombic EPR signal at g = 2.00, 1.98 and 1.96 appeared at positive redox potentials (Em = 80 mV, intensity maximum at 160 mV). Another novel S = 1/2 signal at g = 1.96, 1.92 and 1.77 was observed on further, enzymatic reduction of the dithionite-reduced state of Rc1Fe with the dinitrogenase reductase component (Rc2Fe) of the same enzyme system (turnover conditions in the presence of N2 and ATP). When the Rc1Mo protein was treated analogously, neither this 'turnover signal' nor any other S = 1/2 signal were detectable. All Rc1Fe-specific EPR signals detected are discussed and tentatively assigned with special consideration of the reference spectra obtained from Rc1Mo preparations.     

Characterization of a tungsten-substituted nitrogenase isolated from Rhodobacter capsulatus

In the phototrophic non-sulfur bacterium Rhodobacter capsulatus, the biosynthesis of the conventional Mo-nitrogenase is strictly Mo-regulated. Significant amounts of both dinitrogenase and dinitrogenase reductase were only formed when the growth medium was supplemented with molybdate (1 microM). During cell growth under Mo-deficient conditions, tungstate, at high concentrations (1 mM), was capable of partially (approximately 25%) substituting for molybdate in the induction of nitrogenase synthesis. On the basis of such conditions, a tungsten-substituted nitrogenase was isolated from R. capsulatus with the aid of anfA (Fe-only nitrogenase defective) mutant cells and partially purified by Q-sepharose chromatography. Metal analyses revealed the protein to contain an average of 1 W-, 16 Fe-, and less than 0.01 Mo atoms per alpha(2)beta(2)-tetramer. The tungsten-substituted (WFe) protein was inactive in reducing N(2) and marginally active in acetylene reduction, but it was found to show considerable activity with respect to the generation of H(2) from protons. The EPR spectrum of the WFe protein, recorded at 4 K, exhibited three distinct signals: (i) an S = 3/2 signal, which dominates the low-field region of the spectrum (g = 4.19, 3.93) and is indicative of a tungsten-substituted cofactor (termed FeWco), (ii) a marginal S = 3/2 signal (g = 4.29, 3.67) that can be attributed to residual amounts of FeMoco present in the protein, and (iii) a broad S = 1/2 signal (g = 2.09, 1.95, 1.86) arising from at least two paramagnetic species. Redox titrational analysis of the WFe protein revealed the midpoint potential of the FeWco (E(m) < -200 mV) to be shifted to distinctly lower potentials as compared to that of the FeMoco (E(m) approximately -50 mV) present in the native enzyme. The P clusters of both the WFe and the MoFe protein appear indistinguishable with respect to their midpoint potentials. EPR spectra recorded with the WFe protein under turnover conditions exhibited a 20% decrease in the intensity of the FeWco signal, indicating that the cofactor can be enzymatically reduced only to a small extent. The data presented in the current study demonstrate the pivotal role of molybdenum in optimal N(2) fixation and provides direct evidence that the inability of a tungsten-substituted nitrogenase to reduce N(2) is due to the difficulty to effectively reduce the FeW cofactor beyond its semi-reduced state.     

A novel S = 3/2 EPR signal associated with native Fe-proteins of nitrogenase

In addition to their g = 1.94 EPR signal, nitrogenase Fe-proteins from Azotobacter vinelandii, Azotobacter chroococcum and Klebsiella pneumoniae exhibit a weak EPR signal with g approximately equal to 5. Temperature dependence of the signal was consistent with an S = 3/2 system with negative zero-field splitting, D = -5 +/- 0.7 cm-1. The ms = +/- 3/2 ground state doublet gives rise to a transition with geff = 5.90 and the transition within the excited ms = +/- 1/2 doublet has a split geff = 4.8, 3.4. Quantitation gave 0.6 to 0.8 spin . mol-1 which summed with the spin intensity of the S = 1/2 g = 1.94 line to roughly 1 spin/mol. MgATP and MgADP decreased the intensity of the S = 3/2 signal with no concomitant changes in intensity of the S = 1/2 signal.     

Quantitative EPR of an S = 7/2 system in thionine-oxidized MoFe proteins of nitrogenase. A redefinition of the P-cluster concept

Thionine-oxidized nitrogenase MoFe proteins from Azotobacter vinelandii. Azotobacter chroococcum and Klebsiella pneumoniae exhibit excited-state EPR signals with g = 10.4, 5.8 and 5.5 with a maximal amplitude in the temperature range of 20-50 K. The magnitude of these effective g values, combined with the temperature dependence of the peak area at g = 10.4 from 12 K to 86 K, are consistent with an S = 7/2 system with spin Hamiltonian parameters D = -3.7 +/- 0.7 cm-1, [E] = 0.16 +/- 0.01 cm-1 and g = 2.00. This interpretation predicts nine additional effective g values some of which have been detected as broad features of low intensity at g approximately 10, approximately 2.5 and approximately 1.8. The S = 7/2 EPR is ascribed to the multi-iron exchange-coupled entities known as the P clusters. Quantification relative to the S = 3/2 EPR signal from dithionite-reduced MoFe protein indicates a stoichiometry of one P cluster per FeMo cofactor. Two possible interpretations for these observations, together with data from the literature, are proposed. In the first model there are two P clusters per tetrameric MoFe protein. Each P cluster encompasses approximately 8Fe ions and releases a total of three electrons on oxidation with excess thionine. In the second model the conventional view of four P clusters, each containing approximately 4Fe, is retained. This alternative requires that following one-electron oxidation, the P clusters factorize into two populations, Pa and Pb, only one of which is further oxidized with thionine resulting in the S = 7/2 system. Both models require eight-electron oxidation of tetrameric MoFe protein to reach the S = 7/2 state.     

EPR characterization of a high-spin system in carbon monoxide dehydrogenase from Methanothrix soehngenii.

Carbon monoxide dehydrogenase and methyl-coenzyme M reductase were purified from 61Ni-enriched and natural-abundance nickel-grown cells of the methanogenic archae Methanothrix soehngenii. The nickel-EPR signal from cofactor F-430 in methyl-CoM reductase was of substoichiometric intensity and exhibited near-axial symmetry with g = 2.153, 2.221 and resolved porphinoid nitrogen superhyperfine splittings of approximately 1 mT. In the spectrum from 61Ni-enriched enzyme a well-resolved parallel I = 3/2 nickel hyperfine splitting was observed, A parallel = 4.4 mT. From a computer simulation of this spectrum the final enrichment in 61Ni was estimated to be 69%, while the original enrichment of the nickel metal was 87%. Carbon monoxide dehydrogenase isolated from the same batch exhibited four different EPR spectra. However, in none of these signals could any splitting or broadening from 61Ni be detected. Also, the characteristic g = 2.08 EPR signal found in some other carbon monoxide dehydrogenases and ascribed to a Ni-Fe-C complex, was never observed by us under any conditions of detection (4 to 100 K) and incubation in the presence of ferricyanide, dithionite, CO, coenzyme A, or acetyl-coenzyme A. Novel, high-spin EPR was found in the oxidized enzyme with effective g-values at g = 14.5, 9.6, 5.5, 4.6, 4.2, 3.8. The lines at g = 14.5 and 5.5 were tentatively ascribed to an S = 9/2 system (approximately 0.3 spins/alpha beta) with rhombicity E/D = 0.047 and D less than 0. The other signals were assigned to an S = 5/2 system (0.1 spins/alpha beta) with E/D = 0.27. Both sets of signals disappear upon reduction with Em,7.5 = - 280 mV. With a very similar reduction potential, Em,7.5 = - 261 mV, an S = 1/2 signal (0.1 spins/alpha beta) appears with the unusual g-tensor 2.005, 1.894, 1.733. Upon further lowering of the potential the putative double cubane signal also appears. At a potential E approximately - 320 mV the double cubane is only reduced by a few percent and this allows the detection of individual cubane EPR not subjected to dipolar interaction; a single spectral component is observed with g-tensor 2.048, 1.943, 1.894.     

Fe-S centers in lactyl-CoA dehydratase

Lactyl-CoA dehydratase consists of two enzymes, E1 and E2, and requires catalytic quantities of ATP for activity [Kuchta, R. D., & Abeles, R. H. (1985) J. Biol. Chem. 260, 13181-13189]. In contrast to E1, which contains no Fe, E2 contains 8.20 +/- 0.04 mol of Fe/mol of E2, one of which can be removed by 1,10-phenanthroline. E2 also contains 7.33 +/- 0.68 mol of inorganic sulfur/mol of E2, indicating that at least seven of the Fe atoms are present as Fe-S clusters. E1 and E2 contain less than 0.14 mol of Cu, Co, Zn, Mn, and Ni/mol of E1 or E2. Both reduced and oxidized E1 are EPR silent over a 10,000-G scan range at 4 K, while two signals in E2 are observable at 4 K. Identical spectra were obtained with E2 containing either seven or eight Fe atoms, and both signals were only observable at T less than 30 K. Signal 1 has axial symmetry with g = 2.0232 and g = 2.0006. Signal 2 is orthorhombic with g1 = 1.982, g2 = 1.995, and g3 = 2.019. Computer simulation of these spectra with a S = 1/2 spin Hamiltonian was used to extract the g matrices. The intensity of both signals decreases when E2 is reduced with Na2S2O4. We propose that signal 1 is due to an unusual [4Fe-4S] cluster and signal 2 to a [3Fe-3/4S] cluster. Addition of either acrylyl-CoA or lactyl-CoA dramatically alters signal 2.(ABSTRACT TRUNCATED AT 250 WORDS)     

Multifrequency EPR investigations into the origin of the S2-state signal at g = 4 of the O2-evolving complex.

The low-temperature S2-state EPR signal at g = 4 from the oxygen-evolving complex (OEC) of spinach Photosystem-II-enriched membranes is examined at three frequencies, 4 GHz (S-band), 9 GHz (X-band) and 16 GHz (P-band). While no hyperfine structure is observed at 4 GHz, the signal shows little narrowing and may mask underlying hyperfine structure. At 16 GHz, the signal shows g-anisotropy and a shift in g-components. The middle Kramers doublet of a near rhombic S = 5/2 system is found to be the only possible origin consistent with the frequency dependence of the signal. Computer simulations incorporating underlying hyperfine structure from an Mn monomer or dimer are employed to characterize the system. The low zero field splitting (ZFS) of D = 0.43 cm-1 and near rhombicity of E/D = 0.25 lead to the observed X-band g value of 4.1. Treatment with F- or NH3, which compete with Cl- for a binding site, increases the ZFS and rhombicity of the signal. These results indicate that the origin of the OEC signal at g = 4 is either an Mn(II) monomer or a coupled Mn multimer. The likelihood of a multimer is favored over that of a monomer.     

The iron-sulfur clusters in 2-hydroxyglutaryl-CoA dehydratase from Acidaminococcus fermentans. Biochemical and spectroscopic investigations.

The reversible dehydration of (R)-2-hydroxyglutaryl-CoA to (E)-glutaconyl-CoA is catalysed by the combined action of two oxygen-sensitive enzymes from Acidaminococcus fermentans, the homodimeric component A (2 x 27 kDa) and the heterodimeric component D (45 and 50 kDa). Component A was purified to homogeneity (specific activity 25-30 s-1) using streptavidin-tag affinity chromatography. In the presence of 5 mM MgCl2 and 1 mM ADP or ATP, component A could be stabilized and stored for 4-5 days at 4 degrees C without loss of activity. The purification of component D from A. fermentans was also improved as indicated by the 1.5-fold higher specific activity (15 s-1). The content of 1.0 riboflavin 5'-phosphate (FMN) per heterodimer could be confirmed, whereas in contrast to an earlier report only trace amounts of riboflavin (< 0.1) could be detected. Each active component contains an oxygen sensitive diamagnetic [4Fe-4S]2+ cluster as revealed by UV-visible, EPR and M?ssbauer spectroscopy. Reduction of the [4Fe-4S]2+ cluster in component A with dithionite yields a paramagnetic [4Fe-4S]1+ cluster with the unusual electron spin ground state S = 3/2 as indicated by strong absorption type EPR signals at high g values, g = 4-6. Spin-Hamiltonian simulations of the EPR spectra and of magnetic M?ssbauer spectra were performed to determine the zero field splitting (ZFS) parameters of the cluster and the 57Fe hyperfine interaction parameters. The electronic properties of the [4Fe-4S]2+, 1+ clusters of component A are similar to those of the nitrogenase iron protein in which a [4Fe-4S]2+ cluster bridges the two subunits of the homodimeric protein. Under air component A looses its activity within seconds due to irreversible degradation of its [4Fe-4S]2+ cluster to a [2Fe-2S]2+ cluster. The [4Fe-4S]2+ cluster of component D could not be reduced to a [4Fe-4S]1+ cluster, even with excess of Ti(III)citrate or dithionite. Exposure to oxic conditions slowly converts the diamagnetic [4Fe-4S]2+ cluster of component D to a paramagnetic [3Fe-4S]+ cluster concomitant with loss of activity (30% within 24 h at 4 degrees C).     

Nitrogenase from Klebsiella pneumoniae. An e.p.r. signal observed during enzyme turnover under ethylene is associated with the iron-molybdenum cofactor.

During turnover at 10 degrees C at pH 7.4 in the presence of ethylene, the MoFe protein of Klebsiella pneumoniae nitrogenase (Kp 1) exhibited an electron-paramagnetic-resonance signal with g-values at 2.12, 1.998 and 1.987. 57Fe isotopic substitution demonstrated that this signal arose from the Kp 1 FeMo-cofactor in an S = 1/2 spin state.     

The vanadium nitrogenase of Azotobacter chroococcum. Purification and properties of the VFe protein.

1. Nitrogenase activity of a strain of Azotobacter chroococcum lacking the structural genes for conventional nitrogenase (nifHDK) was separated into two components: an Fe-containing protein and a vanadoprotein. 2. The larger protein was purified to homogeneity by the criterion of electrophoresis of 10% (w/v) acrylamide gels in the presence of SDS. Two types of subunit, of Mr 50,000 and 55,000, were present in equal amounts. 3. The protein had an Mr of 210,000 and contained 2 V atoms, 23 Fe atoms and 20 acid-labile sulphide groups per molecule. The Mo content was less than 0.06 g-atom/mol. All the common amino acids were present, with a predominance of acidic residues. Ultracentrifugal analysis gave a maximum sedimentation coefficient of 9.7 S and a symmetrical boundary at 5 mg of protein X ml-1; dissociation occurred at lower concentrations. The specific activities (nmol of product/min per mg of protein), when assayed under optimum conditions with the complementary Fe protein from this strain, were 1348 for H2 evolution, 350 for NH3 formation and 608 for acetylene reduction. Activity was O2-labile, with a t1/2 of 40 s in air. At low temperatures the dithionite-reduced protein showed e.p.r. signals at g = 5.6, 4.35, 3.77 and 1.93, consistent with an S = 3/2 ground state with an additional S = 1/2 centre giving rise to the feature at g = 1.93. The u.v. spectra of dithionite-reduced and thionine-oxidized protein were very similar. Oxidation resulted in a general increase in absorbance in the visible region. The shoulder at 380 nm in the spectrum of reduced protein was replaced with shoulders near 330 nm and 420 nm on oxidation.     

Single-crystal electron paramagnetic resonance studies of photolyzed oxy- and nitric oxide-cobalt myoglobins

Low-temperature photodissociation of oxygen from oxy-cobalt myoglobin was studied by single-crystal electron paramagnetic resonance (EPR) spectroscopy at 5 K. The photolyzed oxy-cobalt myoglobin exhibited an EPR spectrum consisting of two nonequivalent sets (species I and II) of the principal values and eigenvectors of the g tensors: g1I = 3.55, g2I = 3.47, and g3I = 2.26 for species I, and g1II = 2.04, g2II = 1.93, and g3II = 1.86 for species II, which resembled neither the deoxy nor the oxy form. Possible models of the photodissociated state of oxy-cobalt myoglobin are proposed by comparison with cobalt porphyrin complexes. The photolyzed product of nitric oxide-cobalt myoglobin exhibited new EPR signals at g = 4.3 and a very broad signal at around g = 2. The principal g values have been determined from the single-crystal EPR measurements: g1 = 4.39, g2 = 4.27, and g3 = 4.00. Analysis of another EPR signal around g = 2 was difficult due to its broadness. Magnetic interactions were observed. An isotropic EPR signal at g = 4.3 suggested a weakly spin-coupled system between cobaltous spin (S = 1/2 or 3/2) and nitric oxide spin (S = 1/2).     

M?ssbauer, EPR, and magnetization studies of the Azotobacter vinelandii Fe protein. Evidence for a [4Fe-4S]1+ cluster with spin S = 3/2

We have studied the Fe protein (Av2) of the Azotobacter vinelandii nitrogenase system with M?ssbauer and EPR spectroscopies and magnetic susceptometry. In the oxidized state the protein exhibits M?ssbauer spectra typical of diamagnetic [4Fe-4S]2+ clusters. Addition of Mg.ATP or Mg.ADP causes a pronounced decline in the quadrupole splitting of the M?ssbauer spectra of the oxidized protein. Our studies show that reduced Av2 in the native state is heterogeneous. Approximately half of the molecules contain a [4Fe-4S]1+ cluster with electronic spin S = 1/2 and half contain a [4Fe-4S]1+ cluster with spin S = 3/2. The former yields the characteristic g = 1.94 EPR signal whereas the latter exhibits signals around g = 5. The magnetization of reduced Av2 is dominated by the spin S = 3/2 form of its [4Fe-4S]1+ clusters. These results explain a long standing puzzle, namely why the integrated spin intensity of the g = 1.94 EPR signal is substantially less than 1 spin/4 Fe atoms. In 50% ethylene glycol, 90% of the clusters are in the spin S = 1/2 form whereas, in 0.4 M urea, 85% are in the S = 3/2 form. In 0.4 M urea, the EPR spectrum of reduced Av2 exhibits well defined resonances at g = 5.8 and 5.15, which we assign to the S = 3/2 system. The EPR and M?ssbauer studies yield a zero-field splitting of 2D approximately equal to -5 cm-1 for this S = 3/2 state.     

Q-band EPR of the S2 state of photosystem II confirms an S = 5/2 origin of the X-band g = 4.1 signal

Disagreement has remained about the spin state origin of the g = 4.1 EPR signal observed at X-band (9 GHz) from the S2 oxidation state of the Mn cluster of Photosystem II. In this study, the S2 state of PSII-enriched membrane fragments was examined at Q-band (34 GHz), with special interest in low-field signals. Light-induced signals at g = 3.1 and g = 4.6 were observed. The intensity of the signal at g = 3.1 was enhanced by the presence of F- and suppressed by the presence of 5% ethanol, indicating that it was from the same spin system as the X-band signal at g = 4.1. The Q-band signal at g = 4.6 was also enhanced by F-, but not suppressed by 5% ethanol, making its identity less clear. Although it can be accounted for by the same spin system, other sources for the signal are considered. The observation of the signal at g = 3.1 agrees well with a previous study at 15.5 GHz, in which the X-band g = 4.1 signal was proposed to arise from the middle Kramers doublet of a near rhombic S = 5/2 system. Zero-field splitting values of D = 0.455 cm(-1) and E/D = 0.25 are used to simulate the spectra.     

The manganese site of the photosynthetic oxygen-evolving complex probed by EPR spectroscopy of oriented photosystem II membranes: the g = 4 and g = 2 multiline signals.

The g = 4 and g = 2 multiline EPR signals arising from the Mn cluster of the photosynthetic oxygen-evolving complex (OEC) in the S2 state were studied in preparations of oriented photosystem II (PSII) membranes. The ammonia-modified forms of these two signals were also examined. The g = 4 signal obtained in oriented PSII membranes treated with NH4Cl at pH 7.5 displays at least 16 partially resolved Mn hyperfine transitions with a regular spacing of 36 G [Kim, D.H., Britt, R.D., Klein, M.P., & Sauer, K. (1990) J. Am. Chem. Soc. 112, 9389-9391]. The observation of this g = 4 "multiline signal" provides strong spectral evidence for a tetranuclear Mn origin for the g = 4 signal and is strongly suggestive of a model in which different spin state configurations of a single exchange-coupled Mn cluster give rise to the g = 4 and g = 2 multiline signals. A simulation shows the observed spectrum to be consistent with an S = 3/2 or S = 5/2 state of a tetranuclear Mn complex. The resolution of hyperfine structure on the NH3-modified g = 4 signal is strongly dependent on sample orientation, with no resolved hyperfine structure when the membrane normal is oriented perpendicular to the applied magnetic field. The dramatic NH3-induced changes in the g = 4 signal resolved in the spectra of oriented samples are suggestive that NH3 binding at the Cl- site of the OEC may represent direct coordination of NH3 to the Mn cluster.(ABSTRACT TRUNCATED AT 250 WORDS)     

Purification of a second alternative nitrogenase from a nifHDK deletion strain of Azotobacter vinelandii.

A second alternative nitrogenase complex (nitrogenase 3) was purified from a nifHDK deletion strain of Azotobacter vinelandii. The active complex is made up of two components, dinitrogenase 3 and dinitrogenase reductase 3. Dinitrogenase 3 contains two protein subunits (alpha, Mr 58,000, and beta, Mr 50,000) which assemble into at least two active configurations: alpha 2 beta 2 (dinitrogenase 3s) and alpha 1 beta 2 (dinitrogenase 3F). Dinitrogenase 3s contains 24 Fe and 18 acid-labile S2-ions per Mr 216,000, and dinitrogenase 3F contains 11 Fe and 9 acid-labile S2-ions per Mr 158,000. Dinitrogenase reductase 3 is composed of two protein subunits of identical Mr (32,500) and contains four Fe and four acid-labile S2- ions per Mr 65,000. On two-dimensional gels, the protein subunits of the nitrogenase 3 complex comigrated with the four Mo-, V-, and NH4+-repressible proteins originally designated as N2ase B: the nitrogenase hypothesized to exist in the alternative N2 fixation system first described in 1980 (P.E. Bishop, D. M. L. Jarlenski, and D. R. Hetherington, Proc. Natl. Acad. Sci. USA 77:7342-7346, 1980). Neutron activation analysis indicated that the nitrogenase 3 complex lacked significant amounts of Mo, V, Cr, Re, and W. Some Zn, however, was found in the dinitrogenase 3S and dinitrogenase 3F preparations. The pattern of substrate reduction efficiency was H+ greater than N2 greater than C2H2. The maximum specific activity found for N2 reduction was 38 nmol of NH3 per min per mg of protein (dinitrogenase 3S). Nitrogenase 3 was found to be extremely sensitive to O2, and activities could not be reproducibly maintained during freezing and thawing.     

Nitrogenase proteins from Gluconacetobacter diazotrophicus, a sugarcane-colonizing bacterium

Gluconacetobacter diazotrophicus Pal-5 grew well and expressed nitrogenase activity in the absence of NH4+ and at initial O2 concentrations greater than 5% in the culture atmosphere. G. diazotrophicus nitrogenase consisted of two components, Gd1 and Gd2, which were difficult to separate but were purified individually to homogeneity. Their compositions were very similar to those of Azotobacter vinelandii nitrogenase, however, all subunits were slightly smaller in size. The purified Gd1 protein contained a 12:1 Fe/Mo ratio as compared to 14:1 found for Av1 purified in parallel. Both Gd2 and Av2 contained 3.9 Fe atoms per molecule. Dithionite-reduced Gd1 exhibited EPR features at g=3.69, 3.96, and 4.16 compared with 3.64 and 4.27 for Av1. Gd2 gave an S=1/2 EPR signal identical to that of Av2. A Gd1 maximum specific activity of 1600 nmol H2 (min mg of protein)(-1) was obtained when complemented with either Gd2 or Av2, however, more Av2 was required. Gd2 had specific activities of 600 and 1100 nmol H2 (min mg protein)(-1) when complemented with Av1 and Gd1, respectively. The purified G. diazotrophicus nitrogenase exhibited a narrowed pH range for effective catalysis compared to the A. vinelandii nitrogenase, however, both exhibited maximum specific activity at about pH 7. The Gd-nitrogenase was more sensitive to ionic strength than the Av-nitrogenase.     

Electron-paramagnetic-resonance studies on nitrogenase of Klebsiella pneumoniae. Evidence for acetylene- and ethylene-nitrogenase transient complexes.

Klebsiella pneumoniae nitrogenase exhibited four new electron-paramagnetic-resonance signals during turnover at 10 degrees C, pH7.4, which were assigned to intermediates present in low concentrations in the steady state. 57Fe-substituted Mo--Fe protein showed that they arose from Fe--S clusters in the Mo--Fe protein of nitrogenase. The new signals are designated: Ic, g values at 4.67, 3.37 and approx. 2.0; VI, g values at 2.125, 2.000 and 2.000; VII, g values at 5.7 and 5.4; VIII, g values at 2.092, 1.974 and 1.933. The sharp axial signal VI arises from a Fe4S4 cluster at the --1 oxidation level. This signal was only detected in the presence of ethylene and provides the first evidence of an enzyme--product complex for nitrogenase. [13C]Acetylene and [13C]ethylene provided no evidence for direct binding of this substrate and product to the Fe--S clusters giving rise to these signals. The dependence of signal intensities on acetylene concentration indicated two types of binding site, with apparent dissociation constants K less than 16 micron and K approximately 13mM. A single binding site for ethylene (K=1.5mM) was detected. A scheme is proposed for the mechanism of reduction of acetylene to ethylene and inhibition of this reaction by CO.     

Dual-mode EPR study of new signals from the S3-state of oxygen-evolving complex in photosystem II

The light-induced new EPR signals at g = 12 and 8 were observed in photosystem II (PS II) membranes by parallel polarization EPR. The signals were generated after two flashes of illumination at room temperature, and the signal intensity had four flashes period oscillation, indicating that the signal origin could be ascribed to the S3-state. Successful simulations were obtained assuming S = 1 spin for the values of the zero-field parameters, D = +/-0.435 +/- 0. 005 cm-1 and E/D = -0.317 +/- 0.002. Orientation dependence of the g =12 and 8 signal intensities shows that the axial direction of the zero-field interaction of the manganese cluster is nearly parallel to the membrane normal.     

Diazene (HN=NH) is a substrate for nitrogenase: insights into the pathway of N2 reduction

Nitrogenase catalyzes the sequential addition of six electrons and six protons to a N2 that is bound to the active site metal cluster FeMo-cofactor, yielding two ammonia molecules. The nature of the intermediates bound to FeMo-cofactor along this reduction pathway remains unknown, although it has been suggested that there are intermediates at the level of reduction of diazene (HN=NH, also called diimide) and hydrazine (H2N-NH2). Through in situ generation of diazene during nitrogenase turnover, we show that diazene is a substrate for the wild-type nitrogenase and is reduced to NH3. Diazene reduction, like N2 reduction, is inhibited by H2. This contrasts with the absence of H2 inhibition when nitrogenase reduces hydrazine. These results support the existence of an intermediate early in the N2 reduction pathway at the level of reduction of diazene. Freeze-quenching a MoFe protein variant with alpha-195His substituted by Gln and alpha-70Val substituted by Ala during steady-state turnover with diazene resulted in conversion of the S = 3/2 resting state FeMo-cofactor to a novel S = 1/2 state with g1 = 2.09, g2 = 2.01, and g3 approximately 1.98. 15N- and 1H-ENDOR establish that this state consists of a diazene-derived [-NHx] moiety bound to FeMo-cofactor. This moiety is indistinguishable from the hydrazine-derived [-NHx] moiety bound to FeMo-cofactor when the same MoFe protein is trapped during turnover with hydrazine. These observations suggest that diazene joins the normal N2-reduction pathway, and that the diazene- and hydrazine-trapped turnover states represent the same intermediate in the normal reduction of N2 by nitrogenase. Implications of these findings for the mechanism of N2 reduction by nitrogenase are discussed.