Zhi-Yong
Yang
*a,
Emilio
Jimenez-Vicente
b,
Hayden
Kallas
a,
Dmitriy A.
Lukoyanov
c,
Hao
Yang
c,
Julia S.
Martin del Campo
b,
Dennis R.
Dean
*b,
Brian M.
Hoffman
*c and
Lance C.
Seefeldt
*a
aDepartment of Chemistry and Biochemistry, Utah State University, Logan UT 84322, USA. E-mail: nkyzy@hotmail.com; lance.seefeldt@usu.edu; Tel: +1-435-797-3964
bDepartment of Biochemistry, Virginia Tech, Blacksburg, VA 24061, USA. E-mail: deandr@vt.edu; Tel: +1-540-231-5895
cDepartment of Chemistry, Northwestern University, Evanston, IL 60208, USA. E-mail: bmh@northwestern.edu; Tel: +1-847-491-3104
First published on 29th March 2021
The electronic structure of the active-site metal cofactor (FeV-cofactor) of resting-state V-dependent nitrogenase has been an open question, with earlier studies indicating that it exhibits a broad S = 3/2 EPR signal (Kramers state) having g values of ∼4.3 and 3.8, along with suggestions that it contains metal-ions with valencies [1V3+, 3Fe3+, 4Fe2+]. In the present work, genetic, biochemical, and spectroscopic approaches were combined to reveal that the EPR signals previously assigned to FeV-cofactor do not correlate with active VFe-protein, and thus cannot arise from the resting-state of catalytically relevant FeV-cofactor. It, instead, appears resting-state FeV-cofactor is either diamagnetic, S = 0, or non-Kramers, integer-spin (S = 1, 2 etc.). When VFe-protein is freeze-trapped during high-flux turnover with its natural electron-donating partner Fe protein, conditions which populate reduced states of the FeV-cofactor, a new rhombic S = 1/2 EPR signal from such a reduced state is observed, with g = [2.18, 2.12, 2.09] and showing well-defined 51V (I = 7/2) hyperfine splitting, aiso = 110 MHz. These findings indicate a different assignment for the electronic structure of the resting state of FeV-cofactor: S = 0 (or integer-spin non-Kramers state) with metal-ion valencies, [1V3+, 4Fe3+, 3Fe2+]. Our findings suggest that the V3+ does not change valency throughout the catalytic cycle.
All three nitrogenase systems are united by common mechanistic features. Namely, electrons are sequentially transferred through a proposed ‘deficit-spending’ process, with electrons passing from the [4Fe–4S]1+ cluster in reduced Fe protein, through the P-cluster, and ultimately accumulated at the active site cofactor. Coupled hydrolysis of a minimum of 2ATP molecules to 2ADP/2Pi occurs for each electron transferred from Fe protein to the corresponding catalytic component.20,21 This cycle is repeated until sufficient electrons are accumulated on the active-site cofactor to enable binding and subsequent reduction of substrate. Reduction of different substrates (H+, N2, C2H2, CO) varies among the three isozymes.5,11,22–24 A recent comparative steady-state kinetic study revealed that all three isozymes follow the same fundamental eight-electron/proton mechanism for N2 reduction, with each step involving a cycle of association/dissociation of the two component proteins.4,20,21,23 In this scheme, the states of the corresponding catalytic component (MoFe, VFe, or FeFe protein) are denoted by En, where n represents the number of electrons/protons accumulated on the corresponding active site cofactor (Scheme 1). N2 binds at the E4 stage after the accumulation of four [e−/H+], and the reduction of N2 is driven by the mechanistically-coupled reductive elimination of two hydrides with the release of H2.23,25 It was further found that the three isozymes show different ratios of rate constants for this reductive elimination step versus the competing hydride protonolysis reaction that only releases H2.4,23 A determination of the electronic structures and redox properties of the metalloclusters, especially for the corresponding active-site cofactors, is a critical cornerstone in understanding the causes for differences in catalytic properties, as well deciphering common mechanistic features.4,6 In the present work, features of FeV-cofactor contained within the VFe protein, in both its resting and turnover states, are explored and compared to known features of FeMo-cofactor and FeFe-cofactor.
Among the three isozymes, Mo-dependent nitrogenase has been the best studied, with details of the mechanism being revealed by a combination of genetic, biochemical, spectroscopic and crystallographic studies.4,6,8,9,13,20,21,26 The atomic structure of the active site FeMo-cofactor in the dithionite-reduced (resting state, E0) MoFe protein is [7Fe–9S–Mo–C–(R)–homocitrate] with an S = 3/2 spin state (Fig. 1).27,28 Recent X-ray based spectroscopic studies supported the assignment of Mo3+ with a non-Hund d3 electronic configuration,29,30 leading to a preferred charge distribution of the cluster of [Mo3+4Fe3+3Fe2+9S2−–C4−]1− (Fig. 1).6,31,32 Earlier EXAFS and Mӧssbauer studies of resting-state VFe33–37 protein and FeFe14,38 protein indicated that: (i) both FeV-cofactor and FeFe-cofactor have similar atomic architecture and electronic properties of the 7Fe-subcluster to those of the FeMo-cofactor (Fig. 1);6 and (ii) the P-clusters in VFe and FeFe proteins are diamagnetic (S = 0), similar to that of their Mo counterpart.14,37,38 Recently, a crystal structure of VFe protein has been solved and the modeled structure resembles that for FeMo-cofactor, but with an unusual bidentate four light atomic ligand (assigned as CO32−, Fig. 1) replacing one of the belt sulfide (S2−) atoms.13,39
A Mӧssbauer study suggested that FeFe-cofactor has an even number of ferrous and ferric iron atoms ([4Fe3+4Fe2+]) with a diamagnetic ground state (S = 0), in agreement with the EPR-silence of the resting state FeFe protein.14,38 However, there is little consensus on the electronic structure of FeV-cofactor, in part because of contradictory observations of EPR spectra of different preparations of the VFe protein.5,6,11,13,19 To date, the FeV-cofactor in the resting state of the enzyme is most typically taken to have S = 3/2, and to exhibit a rhombic EPR signal with g ≈ 4.3 and 3.8, with the third g feature likely hidden under other high field EPR signals.5,6,13,19,40 However, the intensity of this signal compared to the S = 3/2 signal for resting-state FeMo-cofactor is too low to account for FeV-cofactor in all of the VFe protein present.41 Given the suggested S = 3/2 spin of the resting state FeV-cofactor, a recent study combining X-ray absorption (XAS) and X-ray emission (XES) spectroscopy and density functional theory (DFT) calculations of resting state MoFe and VFe protein and related synthetic clusters proposed an assignment of V3+ with an S = 1 d2 electronic configuration.35,42 Combined with the assignment of FeV-cofactor as EPR-active in the resting state, this implies there must be one more ferrous (Fe2+) ion in the Fe7 subcluster of FeV-cofactor (Fig. 1) compared to FeMo-cofactor.6,42,43
Considering the uncertainties in assigning the origins of the resting-state EPR signal for VFe protein, the electronic structures derived from these spectroscopic and theoretical studies, as summarized in Fig. 1, remained likewise uncertain. Moreover, a proposed assignment of the low spin (S = 1/2) EPR signal for resting-state VFe protein to the oxidized P-cluster has been debated.5,6,13 The present work is focused on the electronic structures of the FeV-cofactor in both the resting and turnover state of V-nitrogenase. It is revealed that none of the EPR signals previously assigned to FeV-cofactor are consistent with those species representing the dominant active species in the resting state, leading to the conclusion that the resting state FeV-cofactor (E0) does not exhibit a half-integer (Kramers) spin state. Rather, freeze-trapping a reduced intermediate formed during turnover reveals an S = 1/2 EPR signal showing defined 51V hyperfine coupling splitting, leading to the conclusion that this EPR-active partially reduced state of FeV-cofactor (E1 or E3) has V3+ (S = 1), and the proposal that this electronic state of vanadium persists throughout the catalytic cycle. These findings lead to a different assignment of iron-ion valencies for FeV-cofactor compared to prior work.
Affinity purification of VFe-protein produced by a nifB-deletion strain results in loss of the δ-subunit, encoded by vnfG, and sub-stochiometric co-purification with VnfY. VnfY has a similar primary structure when compared to NifY/NafY from the Mo-dependent system. Similar to the situation found here, NifY/NafY, which are proposed to be FeMo-cofactor trafficking proteins,10 co-purifies with MoFe protein produced by the nifB-deletion strain.46,52 It, therefore, appears that VnfY has a role related to FeV-cofactor trafficking/insertion during maturation of the VFe protein, which is also consistent with prior biochemical phenotype of a strain deleted for vnfY.53 Another feature of VFe-protein produced by the nifB-deletion strain is that it apparently accumulates as a mixture of α2β2 and α1β2 species based on the differential intensity of bands corresponding to the α- and β-subunits shown in lane 2 of Fig. 2, which, again, is consistent with previous reports.5,12,44,54
A comparison of the specific activities of the VFe proteins used in the present work for reduction of the physiological substrates, N2 and protons, is shown in Table 1. The VFeStr protein shows specific activities for N2 and proton reduction consistent with the highest reported values from prior studies,5 whereas, the VFeStrΔnifB protein, which does not contain FeV-cofactor, has no N2 or proton reduction capacity. For reasons described in a following section, VFe protein produced by a strain having nifE deleted (VFeStrΔnifE) was also isolated. NifE is specifically required for formation of the active site FeMo-cofactor associated with the Mo-dependent nitrogenase. The VFeStrΔnifE protein sample exhibited lower activities relative to the VFeStr protein for reduction of N2 and protons, but well within the variability we have routinely observed and others have reported5,40 for VFe protein preparations.
VFe protein | Substrates | ||
---|---|---|---|
Protons (1 atm Ar) | N2 (1 atm) and protons | ||
nmol of H2 min−1mg−1 | nmol of H2 min−1mg−1 | nmol of NH3 min−1mg−1 | |
a All assays were performed at 30 °C for 8 min at a molar ratio of VFe protein to VnfH of 1:40 (1:30 for VFeStrΔnifB), and the specific activities are expressed as nmol of product per min per mg of VFe protein as an average with standard deviation. b ND = not detected. | |||
VFeStr | 1980 ± 50 | 960 ± 25 | 310 ± 7 |
VFeStrΔnifB | NDb | ND | ND |
VFeStrΔnifE | 1110 ± 1 | 690 ± 3 | 160 ± 5 |
In vitro incubated VFeStrΔnifE | 1240 ± 27 | 700 ± 8 | 200 ± 9 |
Fig. 3 X-band EPR spectra of resting state strep-tagged VFe proteins. The EPR spectra for 50 μM of VFeStr protein (VFeStr, black trace), for 52 μM of VFeStr protein from a nifE-deleted genetic background (VFeStrΔnifE, red trace), for 48 μM of in vitro incubated Strep-tagged VFe protein from an nifE-deleted genetic background (in vitro incubated VFeStrΔnifE, blue trace), and for 50 μM VFeStr protein from an nifB-deleted genetic background (VFeStrΔnifB, magenta trace) are presented. The details for creation of the different strains with different genotypes and the in vitro incubation experiment are found in the ESI.† All samples were made in a 100 mM MOPS buffer, pH 7.3, with ca. 20 mM sodium dithionite and 150 mM NaCl. Inset shows an expansion of the low field region. EPR conditions: temperature, 12 K; microwave frequency, 9.38 GHz; microwave power, 20 mW; modulation amplitude, 8.14 G; time constant 20.48 ms. Each trace is the sum of five scans. |
The low intensity of the S = 3/2 signals raises doubts about their assignment to resting state FeV-cofactor. We, therefore, explored the possibility that these signals could arise from mis-incorporation of FeMo-cofactor into the VFe protein, given the similarities of g values to those arising from FeMo-cofactor in MoFe protein. To test this possibility, a VFe protein was isolated from A. vinelandii cells having the nifE gene deleted (VFeStrΔnifE). Deletion of nifE disables formation of FeMo-cofactor, removing any possibility of its misincorporation into VFe protein. The VFeStrΔnifE protein exhibits essentially the same EPR features in the S = 3/2 and S = 1/2 regions as VFeStr protein, although having a more prominent S = 1/2 signal compared to the S = 3/2 signal (Fig. 3). This observation rules out the possibility that the S = 3/2 signal might originate from FeMo-cofactor.
Expressing the VFeStr protein in a background having nifB deleted results in formation of VFeStrΔnifB protein that does not contain any FeV-cofactor. The EPR spectrum of this protein shows the persistence of the S = 1/2 signal, but loss of the S = 3/2, g 5.54 and g 4.35 and 3.78 signals (Fig. 3). As already described, this finding is consistent with assignment of the S = 1/2 signal to P-cluster, or a species associated with either P-cluster precursor or damaged P-cluster. Disappearance of the S = 3/2 features in isolated VFeStrΔnifB protein indicates that the low field EPR signals must originate either from FeV-cofactor or one of its intermediate assembly species.
To test whether the S = 3/2 signals might be associated with a VFeStr protein species that contains an immature form of FeV-cofactor, crude extract prepared from the strain producing VFeStrΔnifE was supplemented with V and α-ketoglutarate and incubated for 4 h under turnover conditions prior to isolation of VFeStrΔnifE. Extracts prepared from a strain deleted for nifE was used for this experiment to ensure there was no possibility for adventitious incorporation of FeMo-cofactor into VFe protein during the incubation. Such incubation resulted in only a slight increment in specific activity of the isolated protein (Table 1), but also a loss in the g 4.35 and 3.78 EPR signals (Fig. 3). The g 4.35 and 3.78 signals are thus not correlated with active protein, evidence against the assignment of these signals as the resting state of the active form of FeV-cofactor.5 Even though the chemistry behind the loss in the g 4.35 and 3.78 EPR signals is not yet understood, the result suggests these signals are not associated with the active form of FeV-cofactor.
The feature at g = 5.54 might originate from the overlap of the two signals with g ≈ 5.7 and 5.4 arising from the ground and excited state of an inverted S = 3/2 system.40 The assignment of this signal was probed by redox cycling of the VFe protein. Methylene blue (MB) is able to oxidize the resting state FeMo-cofactor (MN) and P-cluster (PN) in MoFe protein to a diamagnetic EPR silent Mox state and a paramagnetic Pox state, respectively.55 After a 15 min treatment of VFeStr with MB, the high spin S = 3/2 (g = 5.54) and low spin S = 1/2 (g = 2.04, 1.93, and 1.90) signals disappear in the EPR spectrum (Fig. 4). However, the S = 3/2 (g 4.35) signal remained after oxidation, accompanied by the appearance of an adventitious S = 5/2 Fe(III) species with a signal at g ≈ 4.3 (Fig. 4). Re-reduction of the oxidized VFeStr protein by 20 mM dithionite resulted in an unchanged S = 3/2 (g = 4.35) signal, and the recovery of the S = 1/2 signal, but not the S = 3/2 (g = 5.54) signal (Fig. 4). A broad but weak feature, different from the line-shape of the aforementioned S = 3/2 (g = 5.54) signal, appears in the EPR spectrum after the re-reduction by dithionite (Fig. 4). This broad feature ranges from g ∼ 5.8 to g ∼ 5.1. Careful examination of the line-shape revealed that this feature is quite similar to that for the S = 3/2 spin state of the [4Fe4S]1+ cluster Fe protein produced by the Mo-dependent system, which can be reversibly converted to the S = 1/2 spin state of the [4Fe4S]1+ cluster of Fe protein.6,56 The origin of this S = 3/2 signal is not yet clear. Because the appearance of this signal (g ∼ 5.8 to g ∼ 5.1) accompanies the recovery of the S = 1/2 signal after the dithionite re-reduction of MB-oxidized VFeStr, it is reasonable to propose that this new signal originates from the high spin form of the metal cluster displaying the S = 1/2 signal (g = 2.04, 1.93, and 1.90). VFeStr protein that was MB oxidized and then reduced by dithionite maintained about half of substrate reducing activities of that for non-oxidized VFeStr protein (see Table S1†) yet it lost the g = 5.54 EPR signal. Thus, it can be concluded that this signal does not arise from the catalytically active FeV-cofactor.
Fig. 4 X-band EPR spectra of oxidized VFe proteins. Shown is the resting state VFeStr in MOPS buffer with 20 mM DT (black trace), methylene blue (MB)-oxidized VFeStr after 15 min incubation at room temperature in MOPS buffer without DT (blue trace), and 20 mM DT re-reduced VFeStr after being oxidized by MB for 15 min (red trace). The MOPS buffer was 100 mM, pH 7.3, with ca. 150 mM NaCl. The final VFeStr concentration was 50 μM in all samples. The inset in the left bottom corner presents an overlay of the low field region of the spectra from three spectra and the spectra difference (magenta trace) between the MB-oxidized sample and DT re-reduced sample after MB oxidation. EPR conditions are the same as those in Fig. 3. |
The two S = 3/2 signals, from the g = 5.54 and g = 4.35 and 3.78 species, long seen in VFe preparations and ascribed to resting-state FeV-cofactor can be ruled out as arising from catalytically relevant FeV-cofactor based on the results presented here. Even though contradictory results for these signals have been reported, the intensity of the S = 3/2, g = 4.35 and 3.78 signals were still used as an indicator to distinguish the dithionite-reduced, ‘resting’ state from a ‘turnover’ state in the crystallographic study of VFe protein.13,50
Fig. 5 g-2 region X-band EPR spectra of V-nitrogenase proteins. (A) 12 K spectra of resting states (black trace for VFeStr and magenta trace for Fe protein) and Fe protein-VFeStr freeze-trapped during turnover under Ar (red trace) and N2 (blue trace) (B) 5.5 K (green trace) spectra of Ar-turnover Fe protein–VFeStr along with simulation of turnover intermediate (cyan trace) with 51V hyperfine coupling, aiso = 110 MHz, g = [2.18, 2.12, 2.09], and isotropic EPR linewidth of 75 MHz. Samples: all samples contain 5 μM of VFeStr protein except the Fe protein resting state sample, and 40 μM of Fe protein except the VFeStr resting state sample. All samples made in buffer with 200 mM MOPS at pH 7.3 and an ATP-regeneration system (20 mM ATP, 20 mM MgCl2, 1 mg mL−1 BSA, and 0.4 mg mL−1 creatine phosphokinase) with a final dithionite concentration at ∼20 mM. EPR conditions: as in Fig. 3 except each spectrum is the sum of 10 scans. |
Given the observation of 51V-hyperfine splitting, it can be concluded that the newly observed S = 1/2 signal arises from FeV-cofactor. The increase in intensity with increasing electron flux indicates that the signal is from a reduced intermediate. Confirmation that this signal is indeed associated with a catalytic En intermediate (Scheme 1) was provided by using EDTA to quench electron delivery from the Fe protein, which resulted in decay of the turnover dependent EPR signal (Fig. S5†). Confidence that EDTA quenching does not affect cluster composition is provided by the observation the EPR signature of the most sensitive cluster in the system, the Fe protein [4Fe–4S] cluster, is unaffected by the quenching procedure. An earlier report showed no appearance of a new S = 1/2 signal under turnover, much less one that exhibited 51V hyperfine structure.45 In that study, the turnover experiment was performed using low-flux conditions,45 whereas the turnover experiment reported here was performed using high-flux conditions. Although low-flux turnover experiments with MoFe protein have proven useful in the capture of the E1 state,59,60 they were not able to populate more highly reduced states of the enzyme.4,9
Careful inspection of the EPR spectrum of the intermediate shows the two 51V hyperfine lines at lowest field have the ‘absorption’ shape characteristic of components in a 51V (I = 7/2) octet associated with the g1 feature for an S = 1/2 center having a rhombic g-tensor, while the remaining 51V hyperfine lines have the derivative shape of the octet from the g2 feature. This pattern fixes both [g1, A1] and [g2, A2], but the strong Fe protein signal at 12 K precludes any insights into the values of [g3, A3]. However, as the temperature is lowered, the Fe protein signal saturates and decreases in amplitude, while that of the intermediate does not (Fig. 5B and S4†). At the base temperature of 5.5–6 K, at fields directly above the g2 octet, two additional negative going 51V hyperfine lines are observed, the shape expected for g3 features, with no indication of additional 51V lines to still higher field. With this guidance, the observed intermediate spectra can be simulated quite well with g-tensor, g = [2.18, 2.12, 2.09], and an isotropic 51V hyperfine tensor, A = aiso = 110 MHz, Fig. 5B and S6.† Together, the absence of this S = 1/2 signal with 51V hyperfine splitting in the EPR spectrum of resting state VFeStr and its appearance under turnover conditions indicate that this signal arises from FeV-cofactor of a turnover trapped state.
To estimate the degree of accumulation of this newly identified EPR-active intermediate, it is found that the simulated sum of the hyperfine-split signal (HSS) and Fe protein signal is achieved by adding them in the intensity ratio, HSS/Fe protein ∼1/17 (Fig. S6†). Given that the turnover conditions include high reductant concentration (20 mM dithionite) and high Fe protein concentration, it is reasonable to infer that Fe protein is overwhelmingly present in its EPR-active reduced state, and this is confirmed by direct integration of the signal to 0.48 spin per Fe protein. In the case FeV-cofactor, the relative contributions to the simulation imply that roughly 10% of that present (total, 5 μM VFe protein, 10 μM FeV-cofactor) has been trapped as the newly identified EPR active intermediate.
This effort begins with the recognition that the experimentally observed hyperfine coupling tensor for the nucleus of metal-ion site i, Ai, within the multinuclear spin-coupled FeV-cofactor cluster is proportional to the intrinsic hyperfine coupling tensor for the uncoupled (isolated) metal ion, Auni, as scaled by the projection of the metal ion's local spin onto the total cluster spin. This dimensionless constant, denoted the vector-coupling coefficient, Ki, is subject to a normalization condition on the sum over the Ki for the coupled metal ions;
Ai = KiAuni ; ΣKi = 1 | (1) |
According to eqn (1), spin coupling within a cluster alters the magnitude of the nuclear hyperfine interaction, not its ‘symmetry’: isotropic; axial; rhombic. The V3+ (d2, S = 1) valence state, which is relatively rare, has been found to exhibit an isotropic coupling (auniso(III) ≅ 300 MHz).61 The V4+ (d1, S = 1/2) state is quite common, and is well-known to show an extremely anisotropic (roughly axial) hyperfine tensor (component values that range around median values of, A‖∼500 MHz, A⊥ ∼200 MHz, auniso ∼300 MHz).62 The finding that 51V hyperfine coupling of E1,3(1,3H) is fully isotropic then identifies the vanadium of E1,3(1,3H) as V3+ (d2, S = 1).35,42,43
The isotropic 51V hyperfine coupling observed in the E1,3(1,3H) intermediate, aiso = 110 MHz, is much smaller than that of an isolated V3+, aunV ∼300 MHz, and furthermore, the intermediate signal is from an S = 1/2 (Kramers) center, not that of an isolated V3+ (non-Kramers) S = 1 center. These observations together confirm that the observed signal comes not from an isolated V3+ (d2, S = 1) complex produced by cofactor degradation, but from a spin-coupled multi-metallic cluster, a state of spin-coupled FeV-cofactor itself, and thus indeed from a VFe intermediate. Taking eqn (1) and using AunV = auniso ∼300 MHz for an isolated V3+ (d2, S = 1), then aiso = 110 MHz for the intermediate yields a vector-coupling coefficient for the V3+ of E1,3(1,3H): |KV(III)|∼0.3. ENDOR measurements of the sign of the 51V hyperfine coupling will establish the sign of this coefficient.
As an instructive exercise designed to illuminate the spin properties of this intermediate, we examine two alternative limiting models for spin coupling within a FeV-cofactor with cluster spin, S = 1/2 and containing V3+ (S = 1): simple antiferromagnetic coupling between a V3+ (S = 1) and a Fe7 subcluster would yield the observed S = 1/2 cluster spin if the subcluster had a net spin of either S(Fe7) = 1/2 or 3/2. It is straightforward to show that such coupling to a subcluster-spin S(Fe7) = 1/2 would give a vanadium spin-projection coefficient greater than unity, KV = 4/3, and thus a V3+ hyperfine coupling greater than that of an uncoupled ion, contrary to observation. In contrast, antiferromagnetic coupling to a subcluster spin S(Fe7) = 3/2 would give |KV| = 2/3 < 1 (actually, KV < 0), and thus a V3+ hyperfine coupling less than that of an uncoupled ion, a result that qualitatively, even though not quantitatively, reflects experiment. This exercise shows how the observed hyperfine coupling can be used to gain a qualitative understanding of how the V3+ (S = 1) in E1,3(1,3H) is anti-ferromagnetically coupled to an Fe7 sub-cluster of FeV-cofactor with an overall spin S = 3/2. A full treatment of spin coupling within FeV-cofactor, which is not at present accessible, would be needed to precisely discuss all the metal-ion hyperfine couplings and the E1,3(1,3H) g-tensor. Such a more complex scheme would explicitly incorporate contributions to its magnetic properties from zero-field splittings on both Fe and V.
It has been shown that E0 of FeMo-cofactor contains a d3 Mo3+ (Fig. 1),29,30,63 which is odd-electron, that in forming the MoFe E1(H) the molybdenum remains Mo3+,60,64 and further, it has been proposed that this valency persists throughout the catalytic cycle.65 Turning to FeV-cofactor, it is shown here the odd-electron (S = 1/2) E1,3(1,3H) state contains an even-electron V3+ (S = 1). It is proposed, in part by analogy to MoFe protein, that the V3+ valency likewise persists throughout the catalytic cycle, in which case the difference in spin states and EPR behavior observed for the En states of FeMo-cofactor and FeV-cofactor arise because the two cofactors exhibit the same, unchanging trivalent state for the heterometal throughout the cycle. Simply put, it is suggested that the difference between the overall cluster spin states for the En states of FeMo-cofactor and FeV-cofactor arises merely because Mo3+ is an odd-electron Kramers ion (half-integer spin), whereas V3+ is an even-electron, non-Kramers (integer-spin) ion, while the overall valencies of the Fe7 sub-cluster are the same in the corresponding En states of the two cofactors. Taken together, the results in this work suggest that the dithionite-reduced resting state (E0) FeV-cofactor is diamagnetic (S = 0) or paramagnetic with integer-spin (S = 1, 2…), with a high spin V3+ (d2, S = 1) ion, and four ferric (Fe3+) and three ferrous (Fe2+) ions in the Fe7 sub-cluster (Fig. 6).31,32 These findings are consistent with the electronic similarities suggested by iron-selective Mӧssbauer study of V-dependent nitrogenase,37 but contradict the suggestion of electronic structure differences of the Fe7 subclusters in FeMo-cofactor and FeV-cofactor based on XAS and DFT studies.6,42,43
Under turnover conditions, an S = 1/2 spin state intermediate (g = [2.18, 2.12, 2.09]) that forms prior to N2 binding (Scheme 1) has been trapped and is assigned to a state reduced by an odd number of electron: En, n = 1 or 3. The well-defined 51V hyperfine coupling seen for this intermediate show it to have a V3+ (d2, S = 1) valence. It further shows that the V(III) ion is antiferromagnetically spin-coupled to Fe ions of the Fe7 subcluster of FeV-cofactor, with the Fe ions themselves instructively discussed as being coupled into what is in effect a spin of S = 3/2. Given that the resting state of FeMo-cofactor is persuasively assigned valences of [Mo3+, 4Fe3+, 3Fe2+], the most plausible assumption is that the resting-state FeV-cofactor instead has metal-ion valences: [V3+, 4Fe3+, 3Fe2+].
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/d0sc06561g |
This journal is © The Royal Society of Chemistry 2021 |