Hyperfine evidence of strong double exchange in multimetallic {[Fe4S4]-Fe} active center of Escherichia coli sulfite reductase

 The spin-coupling model of the {[Fe₄S₄]-Fe} center of the active site of sulfite reductase, which includes the Heisenberg exchange and double-exchange interactions, explains the peculiarities of the induced paramagnetism. The effective hyperfine constants of the SiR^–1-NO complex are explained in the model with maximal pair spins S₁₂=S₃₄=9/2 in the ground state formed by strong double exchange. Received: 12 January 1996 / Accepted: 23 January 1996     

The N-terminal Domain of Escherichia coli Assimilatory NADPH-Sulfite Reductase Hemoprotein Is an Oligomerization Domain That Mediates Holoenzyme Assembly

Assimilatory NADPH-sulfite reductase (SiR) from Escherichia coli is a structurally complex oxidoreductase that catalyzes the six-electron reduction of sulfite to sulfide. Two subunits, one a flavin-binding flavoprotein (SiRFP, the α subunit) and the other an iron-containing hemoprotein (SiRHP, the β subunit), assemble to make a holoenzyme of about 800 kDa. How the two subunits assemble is not known. The iron-rich cofactors in SiRHP are unique because they are a covalent arrangement of a Fe₄S₄ cluster attached through a cysteine ligand to an iron-containing porphyrinoid called siroheme. The link between cofactor biogenesis and SiR stability is also ill-defined. By use of hydrogen/deuterium exchange and biochemical analysis, we show that the α₈β₄ SiR holoenzyme assembles through the N terminus of SiRHP and the NADPH binding domain of SiRFP. By use of small angle x-ray scattering, we explore the structure of the SiRHP N-terminal oligomerization domain. We also report a novel form of the hemoprotein that occurs in the absence of its cofactors. Apo-SiRHP forms a homotetramer, also dependent on its N terminus, that is unable to assemble with SiRFP. From these results, we propose that homotetramerization of apo-SiRHP serves as a quality control mechanism to prevent formation of inactive holoenzyme in the case of limiting cellular siroheme.     

Heterometallic [AgFe3S4] ferredoxin variants: synthesis, characterization, and the first crystal structure of an engineered heterometallic iron–sulfur protein

Heterometallic [AgFe₃S₄] iron–sulfur clusters assembled in wild-type Pyrococcus furiosus ferredoxin and two variants, D14C and D14H, are characterized. The crystal structure of the [AgFe₃S₄] D14C variant shows that the silver(I) ion is indeed part of the cluster and is coordinated to the thiolate group of residue 14. Cyclic voltammetry shows one redox pair with a reduction potential of +220 mV versus the standard hydrogen electrode which is assigned to the [AgFe₃S₄]^2+/+ couple. The oxidized form of the [AgFe₃S₄] D14C variant is stable in the presence of dioxygen, whereas the oxidized forms of the [AgFe₃S₄] wild type and D14H variants convert to the [Fe₃S₄] ferredoxin form. The monovalent d ¹⁰ silver(I) ion stabilizes the [Fe₃S₄]^+/0 cluster fragment, as opposed to divalent d ¹⁰ metal ions, resulting in more than 0.4 V difference in reduction potentials between the silver(I) and, e.g., zinc(II) heterometallic [MFe₃S₄] ferredoxins. The trend in reduction potentials for the variants containing the [AgFe₃S₄] cluster is wild type ≤ D14C < D14H and shows the same trend as reported for the variants containing the [Fe₃S₄] cluster, but is different from the D14C < D14H < wild type trend reported for the [Fe₄S₄] ferredoxin. The similarity in the reduction potential trend for the variants containing the heterometallic [AgFe₃S₄] cluster and the [Fe₃S₄] cluster can be rationalized in terms of the electrostatic influence of the residue 14 side chains, rather than the dissociation constant of this residue, as is the case for [Fe₄S₄] ferredoxins. The trends in reduction potentials are in line with there being no electronic coupling between the silver(I) ion and the Fe₃S₄ fragment.     

1H NMR studies of the Fe7S8 ferredoxin from Bacillus schlegelii: a further attempt to understand Fe3S4 clusters

 The oxidized Fe₇S₈ ferredoxin from Bacillus schlegelii, containing both [Fe₃S₄]⁺ and [Fe₄S₄]²⁺ clusters, has been investigated by ¹H NMR spectroscopy. An extensive sequence-specific assignment of the hyperfine-shifted resonances has been obtained by making use of a computer-generated structural model. The pattern and the temperature dependence of the hyperfine shifts of the β-CH₂ protons of the cysteines coordinating the [Fe₃S₄]⁺ cluster are rationalized in terms of magnetic interactions between the iron ions. The same approach holds for the hyperfine coupling with ⁵⁷Fe. It is shown that the magnetic interactions are more asymmetric in Fe₇S₈ ferredoxins than in Fe₃S₄ ferredoxins. The NMR non-observability of the β-CH₂ protons of coordinated cysteines in the one-electron-reduced form has been discussed. Received: 19 June 1996 / Accepted: 2 August 1996     

Simultaneous interpretation of Mössbauer, EPR and 57Fe ENDOR spectra of the [Fe4S4] cluster in the high-potential iron protein I Ectothiorhodospira halophila

4 S₄]^3 + and the reduced [Fe₄S₄]^2 + clusters in the high-potential iron protein I from Ectothiorhodospira halophila were measured in a temperature range from 5 K to 240 K. EPR measurements and ⁵⁷Fe electron-nuclear double resonance (ENDOR) experiments were carried out with the oxidized protein. In the oxidized state the cluster has a net spin S = 1/2 and is paramagnetic. As common in [Fe₄S₄]^3 + clusters, the M?ssbauer spectrum was simulated with two species contributing equally to the absorption area: two Fe^3 + atoms couple to the “ferric-ferric” pair, and one Fe^2 + and one Fe^3 + atom give the “ferric-ferrous pair”. For the simulation of the M?ssbauer spectrum, g-values were taken from EPR measurements. A-tensor components were determined by ⁵⁷Fe ENDOR experiments that turned out to be a necessary source of estimating parameters independently. In order to obtain a detailed agreement of M?ssbauer and ENDOR data, electronic relaxation has to be taken into account. Relaxing the symmetry condition in a way that the electric field gradient tensor does not coincide with g- and A-tensors yielded an even better agreement of experimental and theoretical M?ssbauer spectra. Spin-spin and spin-lattice relaxation times were estimated by pulsed EPR; the former turned out to be the dominating mechanism at T = 5 K. Relaxation times measured by pulsed EPR and obtained from the M?ssbauer fit were compared and yield nearly identical values. The reduced cluster has one additional electron and has a diamagnetic (S = 0) ground state. All the four irons are indistinguishable in the M?ssbauer spectrum, indicating a mixed-valence state of Fe^2.5 + for each. Received: 15 February 1999 / Accepted: 31 August 1999     

The relationship between structure and function for the sulfite reductases

The six-electron reductions of sulfite to sulfide and nitrite to ammonia, fundamental to early and contemporary life, are catalyzed by diverse sulfite and nitrite reductases that share an unusual prosthetic assembly in their active centers, namely siroheme covalently linked to an Fe₄S₄ cluster. The recently determined crystallographic structure of the sulfite reductase hemoprotein from Escherichia coli complements extensive biochemical and spectroscopic studies in revealing structural features that are key for the catalytic mechanism and in suggesting a common symmetric structural unit for this diverse family of enzymes.     

Probing the structural, electronic and magnetic properties of multicenter Fe2S2 0/−, Fe3S4 0/− and Fe4S4 0/− clusters

The structural, electronic and magnetic properties of neutral and anion Fe₂S₂, Fe₃S₄ and Fe₄S₄ have been investigated with the aid of previous photoelectron spectroscopy and density functional theory calculations. Theoretical electron detachment energies (both vertical and adiabatic) of anion clusters for the lowest energy structure were computed and compared with the experimental results to verify the ground states. The optimized structures show that the ground state structures of Fe₂S₂ ^0/?, Fe₃S₄ ^0/? and Fe₄S₄ ^0/? favor high spin state and are similar to their structures in proteins. The electron delocalization pattern for all the clusters and the nature of bonding between Fe and S atoms were studied by analyzing molecular orbitals. Natural population analysis demonstrates that Fe atoms act as an electron donor in all clusters, and the electron density difference map clearly shows the direction of the electron flow over the whole complex. Furthermore, the investigated magnetism shows that the Fe atoms carried most of the magnetic moments, which is due mainly to the 3d state, while only very small magnetic moments are found on S atoms.     

Expression,purification and characterization of an iron-sulfur cluster assembly protein,IscU, from <Emphasis Type="Italic">Acidithiobacillus ferrooxidans</Emphasis>

An iron-sulfur cluster assembly protein, IscU, is encoded by the operon iscSUA in Acidithiobacillus ferrooxidans. The gene of IscU was cloned and expressed in Escherichia coli. The protein was purified by one-step affinity chromatography to homogeneity. The protein was in apo-form, the [Fe₂S₂] cluster could be assembled in apoIscU with Fe²⁺ and sulfide in vitro, and in the presence of IscA and IscS, the IscU could utilize l-cysteine and Fe²⁺ to synthesize [Fe₂S₂] cluster in the protein. Site-directed mutagenesis for the protein revealed that Cys37, Asp39, Cys63 and Cys106 were involved in ligating with the [Fe₂S₂] cluster.     

Magnetic circular dichroism studies on monomeric and dimeric iron—sulfur complexes

Magnetic Circular dichroism (MCD) spectra were obtained for bis(o-xylyl-dithiolato)ferrate(III) ([Fe(S₂-o-xylyl)₂]⁻) and bis[o-xylyl-dithiolato-μ₂-sulfidoferrate(III)] ([Fe₂S^*₂(S₂-o-xylyl)₂]²⁻) ions. The MCD magnitude of the dimeric [Fe₂S^*₂(S₂-o-xylyl)₂]²⁻ ion was found to be only one half of that for the monomeric [Fe(S₂-o-xylyl)₂]⁻ ion. The difference in MCD magnitudes was attributed to the change in the thermal populations of ground state sublevels derived from the magnetic exchange interaction.     

An Intertwined Evolutionary History of Methanogenic Archaea and Sulfate Reduction

Hydrogenotrophic methanogenesis and dissimilatory sulfate reduction, two of the oldest energy conserving respiratory systems on Earth, apparently could not have evolved in the same host, as sulfite, an intermediate of sulfate reduction, inhibits methanogenesis. However, certain methanogenic archaea metabolize sulfite employing a deazaflavin cofactor (F₄₂₀)-dependent sulfite reductase (Fsr) where N- and C-terminal halves (Fsr-N and Fsr-C) are homologs of F₄₂₀H₂ dehydrogenase and dissimilatory sulfite reductase (Dsr), respectively. From genome analysis we found that Fsr was likely assembled from freestanding Fsr-N homologs and Dsr-like proteins (Dsr-LP), both being abundant in methanogens. Dsr-LPs fell into two groups defined by following sequence features: Group I (simplest), carrying a coupled siroheme-[Fe₄-S₄] cluster and sulfite-binding Arg/Lys residues; Group III (most complex), with group I features, a Dsr-type peripheral [Fe₄-S₄] cluster and an additional [Fe₄-S₄] cluster. Group II Dsr-LPs with group I features and a Dsr-type peripheral [Fe₄-S₄] cluster were proposed as evolutionary intermediates. Group III is the precursor of Fsr-C. The freestanding Fsr-N homologs serve as F₄₂₀H₂ dehydrogenase unit of a putative novel glutamate synthase, previously described membrane-bound electron transport system in methanogens and of assimilatory type sulfite reductases in certain haloarchaea. Among archaea, only methanogens carried Dsr-LPs. They also possessed homologs of sulfate activation and reduction enzymes. This suggested a shared evolutionary history for methanogenesis and sulfate reduction, and Dsr-LPs could have been the source of the oldest (3.47-Gyr ago) biologically produced sulfide deposit.     

De novo design of a non-natural fold for an iron-sulfur protein: Alpha-helical coiled-coil with a four-iron four-sulfur cluster binding site in its central core

Using a ‘metal-first’ approach, we computationally designed, prepared, and characterized a four-iron four-sulfur (Fe₄S₄) cluster protein with a non-natural α-helical coiled-coil fold. The novelty of this fold lies in the placement of a Fe₄S₄ cluster within the hydrophobic core of a four-helix bundle, making it unique among previous iron-sulfur (FeS) protein designs, and different from known natural FeS proteins. The apoprotein, recombinantly expressed and purified from E. coli, readily self-assembles with Fe₄S₄ clusters in vitro. UV-Vis absorption and CD spectroscopy, elemental analysis, gel filtration, and analytical ultracentrifugation confirm that the protein is folded and assembled as designed, namely, α-helical coiled-coil binding a single Fe₄S₄ cluster. Dithionite-reduced holoprotein samples have characteristic rhombic EPR spectra, typical of low-potential, [Fe₄S₄]⁺ (S = 1/2), with g values of g_z,y = (1.970, 1.975), and g_x = 2.053. The temperature, and power dependence of the signal intensity were also characteristic of [Fe₄S₄]⁺ clusters with very efficient spin relaxation, but almost without any interaction between adjacent clusters. The new design is very promising although optimization is required, particularly for preventing aggregation, and adding second shell interactions to stabilize the reduced state. Its main advantage is its extendibility into a multi-FeS cluster protein by simply duplicating and translating the binding site along the coiled-coil axis. This opens new possibilities for designing protein-embedded redox chains that may be used as “wires” for coupling any given set of redox enzymes.     

Electron exchange coupling in a naturally occurring tetramangano cluster in the mineral helvite, (Mn4S)(SiBeO4)3

The mineral helvite, (Mn₄S)(BeSiO₄)₃, contains discrete tetrahedral Mn₄S⁺⁶ clusters in which the S^?2 is tetrahedrally coordinated and each Mn(II) is in a distorted tetrahedron of one S^?2 and three oxygens; the cluster is situated within an encompassing lattice of SiO₄^?4 and BeO₄^?6 tetrahedra. Mn₄S⁺⁶ centers provide an interesting model for comparison to the polynuclear manganese center that is associated with photosynthetic water oxidation. Magnetic susceptibility data between 77 and 298 K have been measured for a natural helvite sample containing principally Mn₄S⁺⁶ centers but with significant contamination from Mn₃FeS⁺⁶ and Mn₃CaS⁺⁶. The data exhibited Curie-Weiss behavior with μ_eff = 5.969 B.M. and θ = 178.3 K. An analysis of the magnetic susceptibility, based on Van Vleck's formalism, demonstrated the presence of antiferromagnetic coupling, with a coupling constant J = ?5.83 cm^?1. Mössbauer spectra of Mn₃FeS centers in helvite and of Fe₄S centers in the related mineral danalite have also been recorded. Isomer shifts show little temperature dependence and lie in the range 1.23–1.43 $\text{mm}\text{sec.}$. This range is typical of tetrahedrally coordinated Fe(II) in several ionic crystals but is significantly above that of Fe(II) in ferredoxins and below that in the [quinone-Fe(II)-quinone] complex of the photosynthetic bacterium,Rhodopseudomonas sphaeroides. Quadrupole splittings are highly temperature dependent, ranging from 2.4 $\text{mm}\text{sec}$ at 4.2 K to less than 0.5 $\text{mm}\text{sec}$ at 248 K.     

Dissimilatory sulfite reductase from Archaeoglobus profundus and Desulfotomaculum thermocisternum: phylogenetic and structural implications from gene sequences

The genes encoding the α- and β-subunits of dissimilatory sulfite reductase, dsrAB, from the hyper-thermophilic archaeon Archaeoglobus profundus and the thermophilic gram-positive bacterium Desulfotomaculum thermocisternum were cloned and sequenced. The dsrAB genes are contiguous, and most probably comprise an operon also including a dsrD homolog, a conserved gene of unknown function located downstream of dsrAB in all four sulfate reducers so far sequenced. Sequence comparison confirms that dissimilatory sulfite reductase, Dsr, is a highly conserved enzyme. A phylogenetic analysis using the available Dsr sequences, including Dsr-like proteins from nonsulfate reducers, suggests a paralogous origin of the α- and β-subunits. Furthermore, the Dsr from sulfate reducers forms a separate cluster, with Dsr from the bacterial sulfate reducers Desulfotomaculum thermocisternum and Desulfovibrio vulgaris branching together, next to Dsr from Archaeoglobus profundus and Archaeoglobus fulgidus. Based on an alignment with the assimilatory sulfite reductase from Escherichia coli, the amino acid residues involved in binding of sulfite, siroheme, and [Fe₄S₄]-clusters have been tentatively identified, which is consistent with the binding of two sirohemes and four [Fe₄S₄]-clusters per α₂β₂ structure. The evolution of Dsr and the structural basis for the binding of substrate and cofactors are discussed. Received: May 1, 1998 / Accepted: August 10, 1998     

M?ssbauer spectroscopy of the nitrogenase proteins from Klebsiella pneumoniae. Structural assignments and mechanistic conclusions

The Mo–Fe protein and the Fe protein which together constitute the nitrogenase of Klebsiella pneumoniae were prepared from bacteria grown in ⁵⁷Fe-enriched medium. The Mössbauer spectrum of the Mo–Fe protein, as isolated in the presence of Na₂S₂O₄, showed that the protein contained three iron species, called M4, M5 and M6. The area of the spectrum associated with species M4, with δ=0.65mm/s and ΔE=3.05mm/s at 4.2°K, corresponded to two iron atoms/molecule of protein and it is interpreted as being due to a high-spin ferrous, spin-coupled pair of iron atoms. The iron atoms of species M4 may be involved in the quaternary structure of the protein. Species M5, with δ=0.61mm/s and ΔE=0.83mm/s at 77°K, corresponded to eight iron atoms/molecule of protein and is interpreted as being due to Fe₄S₄ or Fe₂S₂ low-spin ferrous iron clusters. Species M6, with δ=0.37mm/s and ΔE=0.71mm/s at 77°K, also corresponded to eight iron atoms/molecule of protein and, at 4.2°K, became a broad shallow absorption, characteristic of magnetic hyperfine interaction. Oxidation of the Mo–Fe protein with the redox dye Lauth''s Violet did not affect the activity of the protein but changed species M4, M5 and M6 into the species M1 (δ=0.37mm/s, ΔE=0.75mm/s at 77°K, broad magnetic component at 4.2°K) and M2 (δ=0.35mm/s, ΔE=0.9mm/s at 4.2°K). In the presence of the Fe protein, Na₂S₂O₄, ATP and Mg²⁺, the M6 component of the Mo–Fe protein was replaced by species M7 with δ=0.46mm/s, ΔE=1.04mm/s at 4.2°K. The change in Mössbauer parameters associated with the M6 → M7 transformation was very similar to the change observed on reduction of the high-potential Fe protein from Chromatium vinosum. In contrast, Na₂S₂O₄-reduced Fe protein contained only one type of iron cluster (F4). Species F4 had δ=0.50mm/s, ΔE=0.9mm/s at 195°K, and at 4.2°K broadened in a manner characteristic of a magnetic hyperfine interaction, associated with half-integral spin, equally distributed over all four atoms of the Fe protein. The Mössbauer spectra of the Mo–Fe and the Fe protein under argon were unaffected by the reducible substrates N₂ and C₂H₂ and the inhibitor CO in the presence of ATP, Mg²⁺ and Na₂S₂O₄. A number of Mössbauer spectral species associated with inactivated Mo–Fe and Fe proteins are described and discussed.     

Parsing redox potentials of five ferredoxins found within Thermotoga maritima

Most organisms contain multiple soluble protein‐based redox carriers such as members of the ferredoxin (Fd) family, that contain one or more iron–sulfur clusters. The potential redundancy of Fd proteins is poorly understood, particularly in connection to the ability of Fd proteins to deliver reducing equivalents to members of the “radical SAM,” or S‐adenosylmethionine radical enzyme (ARE) superfamily, where the activity of all known AREs requires that an essential iron–sulfur cluster bound by the enzyme be reduced to the catalytically relevant [Fe₄S₄]¹⁺ oxidation state. As it is still unclear whether a single Fd in a given organism is specific to individual redox partners, we have examined the five Fd proteins found within Thermotoga maritima via direct electrochemistry, to compare them in a side‐by‐side fashion for the first time. While a single [Fe₄S₄]‐cluster bearing Fd (TM0927) has a potential of ?420 mV, the other four 2x[Fe₄S₄]‐bearing Fds (TM1175, TM1289, TM1533, and TM1815) have potentials that vary significantly, including cases where the two clusters of the same Fd are essentially coincident (e.g., TM1175) and those where the potentials are well separate (TM1815).     

Electron paramagnetic resonance and Mössbauer spectroscopy of intact mitochondria from respiring <Emphasis Type="Italic">Saccharomyces cerevisiae</Emphasis>

Mitochondria from respiring cells were isolated under anaerobic conditions. Microscopic images were largely devoid of contaminants, and samples consumed O₂ in an NADH-dependent manner. Protein and metal concentrations of packed mitochondria were determined, as was the percentage of external void volume. Samples were similarly packed into electron paramagnetic resonance tubes, either in the as-isolated state or after exposure to various reagents. Analyses revealed two signals originating from species that could be removed by chelation, including rhombic Fe³⁺ (g = 4.3) and aqueous Mn²⁺ ions (g = 2.00 with Mn-based hyperfine). Three S = 5/2 signals from Fe³⁺ hemes were observed, probably arising from cytochrome c peroxidase and the a₃:Cu_b site of cytochrome c oxidase. Three Fe/S-based signals were observed, with averaged g values of 1.94, 1.90 and 2.01. These probably arise, respectively, from the [Fe₂S₂]⁺ cluster of succinate dehydrogenase, the [Fe₂S₂]⁺ cluster of the Rieske protein of cytochrome bc ₁, and the [Fe₃S₄]⁺ cluster of aconitase, homoaconitase or succinate dehydrogenase. Also observed was a low-intensity isotropic g = 2.00 signal arising from organic-based radicals, and a broad signal with g _ave = 2.02. Mössbauer spectra of intact mitochondria were dominated by signals from Fe₄S₄ clusters (60–85% of Fe). The major feature in as-isolated samples, and in samples treated with ethylenebis(oxyethylenenitrilo)tetraacetic acid, dithionite or O₂, was a quadrupole doublet with ΔE _Q = 1.15 mm/s and δ = 0.45 mm/s, assigned to [Fe₄S₄]²⁺ clusters. Substantial high-spin non-heme Fe²⁺ (up to 20%) and Fe³⁺ (up to 15%) species were observed. The distribution of Fe was qualitatively similar to that suggested by the mitochondrial proteome.     

The "prismane" protein resolved: X-ray structure at 1.7 Å and multiple spectroscopy of two novel 4Fe clusters

The three-dimensional structure of the native "putative prismane" protein from Desulfovibrio vulgaris (Hildenborough) has been solved by X-ray crystallography to a resolution of 1.72?Å. The molecule does not contain a [6Fe-6S] prismane cluster, but rather two 4Fe clusters some 12?Å apart and situated close to the interfaces formed by the three domains of the protein. Cluster 1 is a conventional [4Fe-4S] cubane bound, however, near the N-terminus by an unusual, sequential arrangement of four cysteine residues (Cys 3, 6, 15, 21). Cluster 2 is a novel 4Fe structure with two μ₂-sulfido bridges, two μ₂-oxo bridges, and a partially occupied, unidentified μ₂ bridge X. The protein ligands of cluster 2 are widely scattered through the second half of the sequence and include three cysteine residues (Cys 312, 434, 459), one persulfido-cysteine (Cys 406), two glutamates (Glu 268, 494), and one histidine (His 244). With this unusual mixture of bridging and external type of ligands, cluster 2 is named the "hybrid" cluster, and its asymmetric, open structure suggests that it could be the site of a catalytic activity. X-ray absorption spectroscopy at the Fe K-edge is readily interpretable in terms of the crystallographic model when allowance is made for volume contraction at 10?K; no Fe··Fe distances beyond 3.1?Å could be identified. EPR, Mössbauer and MCD spectroscopy have been used to define the oxidation states and the magnetism of the clusters in relation to the crystallographic structure. Reduced cluster 1 is a [4Fe-4S]¹⁺ cubane with S?=?3/2; it is the first biological example of a "spin-admixed" iron-sulfur cluster. The hybrid cluster 2 has four oxidation states from (formally) all Fe^III to three Fe^II plus one Fe^III. The four iron ions are exchange coupled resulting in the system spins S?=?0, 9/2, 0 (and 4), 1/2, respectively, for the four redox states. Resonance Raman spectroscopy suggests that the bridging ligand X which could not be identified unambiguously in the crystal structure is a solvent-exchangeable oxygen.     

Effects of phenoxide ligation: Synthesis and characterization of the [Mo2Fe6S8(SEt)3(OPh)6]3− ion

Reaction of phenol with an alkylthiolate-ligated double cubane complex effects phenolate substitution at the terminal positions; the product can be isolated as its benzyltriethylammonium salt. The phenolate cluster possesses unaltered magnetic properties and blue shifted optical spectra, and undergoes ligand exchange reactions with electrophiles as expected for terminal phenolate substitution. Increased isotropic proton NMR shifts and large negative shifts in corresponding first and second reduction potentials are consistent with increased donation of electron density to the [MoFe₃S₄]³⁺ cores for phenolate versus thiophenolate terminal ligands to iron. Similar behavior has been observed for Fe₄S₄, Fe₂S₂ and MoS₂Fe systems.