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Nature Communications logoLink to Nature Communications
. 2026 May 5;17:6101. doi: 10.1038/s41467-026-72599-y

A mononuclear nonheme iron complex with higher affinity for O2 than CO via hydrogen bonding

Matthias Jux 1, Stefan Mebs 2, Michael Haumann 2, Sagie Katz 3, Ricardo Garcia-Serres 4, Peter Hildebrandt 3, Yong Wang 5, Wonwoo Nam 6,✉, Kallol Ray 1,✉
PMCID: PMC13358151  PMID: 42086585

Abstract

Dioxygen activation at iron centers is central to many biological and synthetic oxidation processes. In proteins, the reactivity and stability of iron–dioxygen intermediates are often controlled by secondary-sphere interactions such as hydrogen bonding. For example, hemoglobin stabilizes a Fe−O2 adduct through distal hydrogen bonding, while hemerythrin employs hydrogen bonding to stabilize reduced oxygen species within a diiron active site, enabling reversible O2 binding. Here we show that a mononuclear nonheme iron complex, [FeII(DIG3tren)]2+ (DIG3tren = tris(N’,N”-diisopropylguanidinyl-2-ethyl)amine), reversibly reduces O2 by two electrons to generate an iron(IV)-peroxido species. Strong hydrogen bonds from N − H groups of the ligand stabilize the O22− ligand, while the electron-rich guanidine donors promote the unusual FeII-mediated two-electron reduction of O2. As a result, the complex exhibits higher affinity for O2 than for CO due to preferential hydrogen-bond stabilization of the peroxido intermediate. These results demonstrate how secondary-sphere design can control both O2 activation and ligand selectivity at iron centers.

Subject terms: Ligands, Catalyst synthesis, Chemical bonding


A challenge in designing a synthetic system that can reversibly bind O2 is to prevent irreversible oxidation to oxo-bridged dimers. Here, the authors report a mononuclear nonheme iron(II) complex where the second coordination sphere is engineered to ensure a reversible two-electron reduction of dioxygen to form an iron(IV)-peroxido species through the inclusion of hydrogen bonding substituents.

Introduction

The binding of dioxygen at a ferrous site in proteins is an indispensable step in a variety of physiologically important reactions involved in dioxygen metabolism1–7. A common mechanistic hypothesis for dioxygen activation has been established based on intense research in this field over the past several decades8–33. The one-electron reduction of dioxygen to form an iron(III)-superoxido species34–39, which is energetically endergonic, is invariably the first step proposed during dioxygen activation. It is followed by fast proton-coupled electron-transfer steps that drive O–O bond cleavage to afford high-valent iron-oxido species, which are typically considered as the reactive intermediates responsible for mono- or dioxygenation of substrates. For reversible binding of dioxygen, in contrast, it is warranted that the high-energy iron(III)-superoxido intermediate is stabilized and prevented from further reduction. In hemoglobin (Hb) and myoglobin (Mb)40,41, for example, the protein structure surrounding the heme active site may play a significant role in enhancing superoxido stability. X-ray crystallographic studies suggest a role for H-bonding between the “distal histidine” site and the bound superoxido anion (Fig. 1a)42. Notably, the distal histidine in Hb/Mb is ideally situated to H-bond with bound oxygen, but out of place for optimal interaction with a bound CO, which is believed to be crucial for increasing its affinity for dioxygen compared to carbon monoxide.

Fig. 1. Oxygen binding at iron centers.

Fig. 1

Oxygen binding at the iron center in a hemoglobin, b picket fence porphyrin, c hemerythrin and d [Fe(DIG3tren)](OTf)2. Dashed lines represent H-bonding.

In the absence of any protective protein scaffold, one of the most difficult aspects of creating a synthetic system capable of reversibly binding O2 is preventing irreversible oxidation to oxo-bridged dimers, which act as thermodynamic sink in these reactions43,44. Collman and coworkers19,45,46 addressed this challenge synthetically by constructing a protective fence around one face of the corresponding iron-porphyrin complex using an atropisomer of an ortho-substituted meso-tetraphenylporphyrin (Fig. 1b). Additionally, by employing a sterically encumbered imidazole, this fence limited the coordination of any axial ligand to the unhindered side of the iron center, without hindering the binding of small molecules, such as dioxygen, within the cavity of the hindered face. Furthermore, the coordinated O₂ unit was protected from further reacting with a second iron center, thereby preventing the bimolecular decay pathway. These properties made the iron-dioxygen adduct stable enough to be characterized by single-crystal X-ray crystallography, which provided structural insight into the coordination mode of dioxygen in Hb and Mb47–50. However, although the amide linkages that form the fence could potentially act as H-bond donors to the Fe(III)-superoxido unit in a similar manner as the histidine residue in Hb/Mb, these groups are too far removed from the Fe(III)-superoxido unit (a distance of over 5 Å; Fig. 1b) to form intramolecular H-bonds. Accordingly, it is found to be much poorer at binding O2, relative to Hb.

In addition to heme-based respiratory proteins, the necessity for intramolecular H-bonds in enabling reversible O2 binding is also proposed in hemerythrin (Hr), which involves a nonheme diiron (FeII-FeII) active site51. Here, a proton-coupled electron-transfer process (Fig. 1c), which effects a superoxido-to-hydroperoxido conversion with the distal FeII center being the electron donor, has been put forward to rationalize reversible O2 binding in hemerythrin. Furthermore, the hydroperoxide species is proposed to be stabilized against irreversible O–O bond cleavage through a H-bond with the resulting µ-oxo bridge (Fig. 1c)2,51–54. Incorporation of these non-covalent interactions has therefore been a goal for synthetic chemists who desire to replicate the reactivity of metalloproteins. However, this proved to be challenging, as in addition to incorporating H-bond donors/acceptors, it also required their proper positioning that would allow their interaction with small molecules coordinated to the metal center(s). Although Collman’s porphyrin picket fence was unable to participate in H-bonding with the coordinated O2 unit45,46, this system established the feasibility of positioning functional groups within a molecule to facilitate H-bonding through incorporation into a rigid scaffold. Other groups have also extended this concept in nonheme ligand systems in the design of rigid ligand frameworks that establish local C3 symmetry around a metal center34,36,55–68. However, the Fe-O2 adducts in these complexes are mostly unstable against irreversible O−O cleavage to yield Fe–O moieties, which are stabilized by H-bonding interactions. Herein, we report a ligand system, referred to as DIG3tren (tris(N’,N”-diisopropylguanidinyl-2-ethyl)amine), which simultaneously provides three neutral diisopropyl guanidine (DIG) donors to enforce a trigonal pyramidal coordination environment at a metal ion and positions three NH groups proximal to a metal center in the secondary coordination sphere. This ligand design allowed us to prepare an Fe(II) complex that performs a unique H-bond mediated two-electron transfer between FeII and end-on bound O2 to form a rare example of an iron(IV)-peroxido complex in a reversible manner (Fig. 1d). The steric shielding and H-bond donors of the second coordination sphere in [FeIIDIG3tren] also enabled reversible CO binding. With an M value (Keq(CO)/Keq(O2)) of 0.6, which is an index of the discrimination between oxygen and carbon monoxide bindings46, [FeIIDIG3tren] has a higher affinity for O2 than for CO. [FeIIDIG3tren], therefore, represents a suitable Hb/Mb and Hr model complex (for Hb, M = 234; for Hr, M = 0; Hr does not bind carbon monoxide)69, which, mediated by intramolecular H-bonds in the secondary coordination sphere, reversibly binds O2 in an end-on fashion with a high tolerance for CO.

Results and discussion

Synthesis and characterization of iron(II) complexes

Combination of equimolar amounts of the reported ligand DIG3tren70 and [Fe(MeCN)2(OTf)2] (OTf=CF3SO3−) yields the complex [FeII(DIG3tren)](OTf)2 (1, Supplementary Figs. 1–7), which shows a four coordinate trigonal pyramidal geometry (τ4 = 0.86)71 with the OTf groups involved in intra- and intermolecular H-bonding interactions with the guandine NH moieties (Fig. 2). Each triflate anion forms H-bonds with three complex molecules via the NH groups, creating a network of H-bonds (Supplementary Fig. 8). The zero-field Mössbauer spectrum (Supplementary Fig. 9) of solid 1 at 14 K reveals two quadrupole doublets with isomer shifts (δ), quadrupole splittings (ΔEQ) of 1.01, 2.98 mm/s and 0.97, 1.67 mm/s, respectively, consistent with the presence of two Fe(II) high-spin (S = 2) centers. Based on the Mössbauer parameters (δ = 1.00 mm/s; ΔEQ = 1.66 mm/s, Supplementary Fig. 10) of the related [FeII(TMG3tren)(OTf)](OTf) (TMG3tren = 1,1,1-tris{2-[N2-(1,1,3,3-tetramethylguanidino)]ethyl}amine) complex, we attribute the doublet with δ = 0.97 mm/s and ΔEQ = 1.67 mm/s to [FeII(DIG3tren)(OTf)](OTf) (1-OTf) with an axial OTf ligand. The doublet with δ = 1.01 mm/s and ΔEQ = 2.98 mm/s then corresponds to the four-coordinate Fe(II) center observed in the X-ray structure of 1, which is also confirmed by Mössbauer measurements on the separated crystals of 1 (Supplementary Fig. 11). The four-coordinate iron center with vacant axial coordination site evident in the solid-state structure presumably contributes to the increased ΔEQ value in 1. Expectedly, in the presence of a non-coordinating BF4− anion, the four-coordinate species 1 is solely formed (because of strong H-bonding interaction), as evident from Mössbauer spectroscopy, which reveals a single quadrupole doublet with δ = 1.28 mm/s, and ΔEQ = 3.01 mm/s (Supplementary Figs. 12 and 13). A four-coordinate iron site was also evident from the EXAFS analysis of powder samples of 1 (Supplementary Figs. 14 and 15, Supplementary Table 9). Although, single crystals suitable for X-ray diffraction studies could not be obtained for 1-OTf, the structure of the corresponding [ZnII(DIG3tren)(Br)]Br (Zn-Br) complex (Fig. 2) established the ability of the tetradentate DIG3tren ligand to enforce a trigonal bipyramidal coordination environment at a metal ion and position three guanidine NH groups for H-bonding interaction with an axially bound small molecule (Br− in Zn-Br).

Fig. 2. SC-XRD structures 1 and Zn-Br with schematic representations.

Fig. 2

Top: molecular structures of 1 (left) and Zn-Br (right) obtained by XRD. Atoms are displayed as thermal ellipsoids at 50% probability level; H atoms are omitted for clarity except nitrogen-bound H atoms. Structural parameters are summarized in Supplementary Table 1. Dashed lines represent H-bonding. (Atom types: Fe: orange; N: blue; C: gray; O: red; S: yellow; F: green; H: white; Zn: violet; Br: brown). Bottom: schematic representations of 1, 1-OTf and Zn-Br.

Dioxygen reactivity and characterization of Fe-O2 adduct

While the four coordinate iron(II) center of 1 would appear to be well set up to bind O2, the stabilization of the bound OTf ligand by H-bonding interaction in 1-OTf (as also observed recently by Szymczak et al.63) may obstruct access of O2 to the Fe-site, thereby impacting its binding ability. The 19F-NMR spectrum (Supplementary Fig. 3) of a solution of 1/1-OTf in acetone, however, displayed a single resonance at −76.0 ppm, which confirmed that OTf is not bound to the Fe-center. Thus, in solution the Fe-center stays either four-coordinate with vacant axial coordinate site or five-coordinate with an axial acetone ligand (Supplementary Fig. 16). The Mössbauer spectrum of a frozen acetone solution of 1/1-OTf (Fig. 3a, top) reveals in addition to the quadruple doublet with δ = 1.01 mm/s, and ΔEQ = 2.98 mm/s, corresponding to 1 (29%), two additional doublets (1’, δ = 0.99 mm/s, and ΔEQ = 2.42 mm/s (30%) and 1”, δ = 0.83 mm/s, and ΔEQ = 1.10 mm/s (41%)), which are also assigned to Fe(II) high-spin (S = 2) centers associated with the different conformational isomers of 1. The formation of different species in solution is attributed to the intrinsic flexibility of the DIG3tren ligand, where, as demonstrated previously70, the isopropylamino group from each DIG moiety acts as a flap that can either close (closed conformation) over iron or rotate away from iron (open conformation) to open up a site for auxiliary ligand binding (Fig. 4). Based on their similar Mössbauer parameters, the structure of complex 1’ can be considered identical to 1 with a four-coordinate Fe(II) center and containing all the DIG moieties in a closed conformation (Supplementary Fig. 16); the slight differences in δ and ΔEQ values may presumably be attributed to the differences in the secondary coordination sphere, involving H-bonding interactions with acetone and OTf anion. In contrast, the Mössbauer parameters of 1” with lower ΔEQ values represent a more symmetric Fe(II) center, similar to that observed for 1-OTf. Accordingly, a five-coordinate trigonal bipyramidal structure similar to Zn-Br (Fig. 2) is proposed for 1” ( Supplementary Fig. 16) with an axial acetone ligand; it is presumably a conformational isomer, where one or more DIG moieties exist in the open conformation, thus enabling the binding of solvent.

Fig. 3. Mössbauer and UV/vis characterizations.

Fig. 3

a Top: zero-field Mössbauer spectrum of frozen acetone solution of 1 at 14 K (gray line: experimental spectrum; black line: simulated spectrum; red line: 1 with δ = 1.01 mm/s, ΔEQ = 2.98 mm/s, 29%; brown line: 1’ with δ = 0.99 mm/s, ΔEQ = 2.42 mm/s, 30%; blue line: 1” with δ = 0.83 mm/s, ΔEQ = 1.10 mm/s, 41%); Middle: zero-field Mössbauer spectrum of an oxygenated acetone solution of 57Fe enriched 1/1-OTf at 14 K (gray line: experimental spectrum; black line: simulated spectrum; blue lines: Fe(III) decay products with δ = 0.65 mm/s, ΔEQ = 1.35 mm/s, 20% and δ = 0.63 mm/s, ΔEQ = 0.68 mm/s, 25%; pink line: 2 with δ = 0.01 mm/s, ΔEQ = 2.94 mm/s, 46%; red line: residual 1, 9%). Bottom: zero-field Mössbauer spectrum of a CO flushed acetone solution of 57Fe enriched 1/1-OTf at 14 K (gray line: experimental spectrum; black line: simulated spectrum; purple line: 1-CO with δ = 0.34 mm/s, ΔEQ = 1.00 mm/s, Γ = 0.33 mm/s, 88%; red line: 1, Γ = 0.50 mm/s, 12%). b UV/vis spectra showing the reversible formation of 2 by oxygen and argon flushing of 1/1-OTf in acetone at −80 °C, with time trace of the band at 700 nm shown as an inset. c UV/vis spectra of the temperature-dependent binding of CO to 1/1-OTf to form 1-CO, with the time trace of the band at 604 nm shown as an inset.

Fig. 4. Scheme of proposed ligand-framework motion prior to O2 binding in 1.

Fig. 4

Preorganization of the N–H groups in 1 enables hydrogen-bond-assisted stabilization of the peroxido intermediate 2 upon O2 binding, whereas altered hydrogen-bonding environments in acetone prevent productive O2 reduction and instead leads to Fe(III) decay products.

Interestingly, Mössbauer studies (Fig. 3a top and middle) reveal that upon bubbling of O2 through an acetone solution of a mixture of 1, 1’ and 1” at −95 °C, the five-coordinate Fe(II) species 1” with ΔEQ < 2.0 mm/s that corresponds to 41% of Fe(II) in solution perform fast irreversible electron transfer process to yield two high-spin iron(III) decay products (Fig. 3a middle, green traces, 45%) with δ = 0.65 mm/s, ΔEQ = 1.35 mm/s and δ = 0.63 mm/s, ΔEQ = 0.68 mm/s. We propose that the Fe(II) centers with at least one of the DIG groups in open conformation react rapidly with O2 to form a transient superoxido species that undergoes oxidative decomposition via a ligand-centered hydrogen-atom abstraction process (Supplementary Fig. 17). This assignment is supported by ESI-MS analysis, which reveals three signals that are sensitive to 16/18O isotope-labeling (Supplementary Fig. 18). Of these, two signals at m/z = 744.4 and 297.7 are assigned to [Fe(O)(DIG3tren-H)(OTf)]⁺ and [Fe(O)(DIG3tren-H)]²⁺ (calcd. m/z = 744.37 and 297.71) ions, consistent with the formation of an alkoxoiron(III) species. A third signal at m/z = 594.4 corresponds to the dehydrogenated product [Fe(O)(DIG3tren-2H)]⁺ (calcd. m/z = 594.41). Together, these Fe(III) products indicate ligand-based hydrogen-atom abstraction coupled to O–O bond cleavage, accounting for the rapid oxidative decomposition observed for Fe(II) species derived from 1” in solution.

The four coordinate complexes 1 or 1’, with large ΔEQ values of 2.98 and 2.42 mm/s, respectively, represent 59% of Fe(II) in solution and contain all three DIG moieties in closed conformation, as evident from the crystal structure of 1 (Fig. 2). They are converted slowly (t = 4200 s) to an equilibrium mixture of a red intermediate 2 (Fig. 3a middle, pink trace, 46%; Fig. 3b; λmax = 700 nm; ε = 0.20 mM−1 cm−1; half-life at −70 °C = 100 s) with δ = 0.01 mm/s and ΔEQ = 2.94 mm/s and residual 1 (9%). The low δ value of 2 is strongly indicative of an iron(IV) complex, as it is similar to that of the FeIV site of [FeIV(O)(6-Me3tpa)(μ-O)FeIII(6-Me3tpa)(H2O)] (0.10 mm/s)72 and [FeIV(O)(TMG3tren)]2+ (0.09 mm/s)73, reflecting the nitrogen-rich ligand environment of 2. Remarkably, bubbling of Ar through the acetone solution of 2 for 2 min at −95 °C regenerates 1, showing that 2 is a reversible Fe−O2 adduct; several cycles of alternating Ar/O2 purges can be achieved (Fig. 3b and Supplementary Fig. 19).

The samples were analyzed by applied-field Mössbauer spectroscopy (Fig. 5c), with the precursor complex being measured separately in acetone and subtracted from the spectrum obtained after reaction of the mixture with O2 (Fig. 3a, top). After subtraction of the minor amount of the remaining precursor, the spectra were simulated with two species: an integer-spin (S = 1) species corresponding to 2 that yields a doublet in the low-field spectra, and a half-integer spin (S = 5/2) corresponding to the high-spin FeIII decay product that yields a six-line pattern. The splitting of the six-line pattern matches to what is expected for an S = 5/2 Fe(III) center. The 80 K spectrum was simulated with two doublets with parameters δ = 0.01 mm/s, ΔEQ = +2.94 mm/s (2, red line) and δ = 0.51 mm/s, ΔEQ = 0.94 mm/s (green line), consistent with Fe(IV) and high-spin Fe(III), respectively. The faint, broad absorptions under the baseline indicate that all the paramagnets of the S = 5/2 species have not switched to fast relaxation at 80 K, pointing to the formation of aggregates. The fitted value of the hyperfine coupling constant for 2 (FeIV) falls well within the expected range, which confirms the S = 1 ground state3,74–77. The large value for the zero-field splitting (D = +20.8 cm−1) is consistent with other S = 1 FeIV=O complexes, and implies a relatively well isolated Ms = 0 ground state within the S = 1 multiplet. This brings up the question of the possibility of an S = 0 ground state. A fit with an S = 0 spin Hamiltonian, however, fails to accurately reproduce the positions of the absorptions in the high-field spectra. We can therefore confidently assign the ground spin state as S = 1 for 2.

Fig. 5. rRaman and Mössbauer characterizations of 2.

Fig. 5

a rRaman spectra (−90 °C, λexc = 568 nm) of acetone-d6 (black) and 2 prepared at −90 °C in acetone-d6, generated by using 16O2 (red) and 18O2 (purple). b Band fitting analysis of the spectral region between 785 and 840 cm−1 of 2, prepared at −90 °C in acetone-d6 using a mixture of 16O2, 18O2, 16O–18O. The weak band of the solvent at 817 cm−1 was subtracted from the experimental spectrum (black trace). Four Lorentzian functions were fitted to the experimental spectrum, representing the complexes with 16O2 (orange), 16/18O2 and 18/16O2 (blue), and 18O2 (dark yellow). The red trace shows the cumulative fit. Details of the fitting procedure are given in the SI. c Mössbauer spectra of 2 (red component) recorded at 80 K without applied magnetic field or at 5.8 K in a magnetic field of 0.06, 4, or 7 T applied parallel to the direction of the γ-rays. Dark blue lines correspond to the FeIII decay products formed during the reaction. Spin-Hamiltonian simulation parameters in Supplementary Table 2.

The presence of a peroxido moiety in 2 is fully consistent with resonance-Raman (rRaman) measurements, as shown in Fig. 5a. A vibrational mode at 823 cm−1 is observed that shifts to 792 cm−1 upon 18O isotopic labeling. The frequency of 823 cm−1 is in line with the values expected for an O–O stretching of an iron-peroxido in side-on or end-on binding modes or the Fe=O stretching of an iron-oxido species10,13,15,17,44,78–81. To evaluate these possibilities, complex 2 was generated with mixed isotope O2 (16,18O2), corresponding to a mixture of 16O2, 16/18O2, and 18O2. If the 823 cm−1 band is an O–O stretching mode, one will expect, in addition to the bands at 792 (18O2) and 823 cm−1 (16O2), one or two further bands around 810 cm−182,83. While for the symmetrical side-on binding mode, 16O18O and 18O16O stretches are expected to appear at identical energies (one band), they will be different for the end-on mode (two bands). For an Fe=O vibration, the 16,18O2 spectrum will lack any band at ca. 810 cm−1. Figure 5b shows the rRaman spectrum of the active species prepared with 16,18O2. The region of the oxygen-sensitive modes between 785 and 840 cm−1 clearly involves at least three bands, such that an assignment to a Fe=O species can be ruled out. Thus, O2 must be bound to the Fe in the complex. Although three Lorentzian functions provide a mathematically good fit, it does not reproduce the bands of the 16O2- and 18O2-bound species (further details of the band fitting analysis are given in the SI; Supplementary Fig. 20). Thus, a side-on complex can be discarded as well. A similar good fit is achieved on the basis of four Lorentzians (Fig. 5b). Here, the bands of the 16O2- and 18O2-bound species are very well reproduced and also the two additional bands have the expected frequencies at 804.8 and 818.0 cm−1 of the Fe(16O–18O) and Fe(18O–16O) vibrational modes of an end-on [FeIV(η1-O2)(DIG3tren)]2+ moiety in 2.

Additional evidence for the end-on binding mode is demonstrated by extended X-ray absorption fine structure (EXAFS) data (Supplementary Figs. 14 and 15), which for 2 are compatible with the presence of iron-oxygen distances of about 1.83 and 2.76 Å due to an end-on peroxido species, respectively (Supplementary Table 9). The K-edge energy of 2 is in between the energies of the Fe(II) (1) and Fe(IV) (see below) containing complexes, which may reflect the presence of Fe(III) decay products, as seen in the Mössbauer spectrum.

To additionally verify the presence of the two oxygen atoms in 2, the reaction of 2 with 30 equivalents of triphenylphosphane (PPh3) was investigated at −90 °C in acetone (Fig. 6), leading to the quantitative formation of an iron(IV)-oxido intermediate 3 and triphenylphoshane oxide (O=PPh3) (Supplementary Fig. 21). To verify the nature of 3, we synthesized it directly from 1/1-OTf using artificial oxygen atom donor reagents and characterized it spectroscopically (see below).

Fig. 6. Oxygen atom transfer reactivity of 2.

Fig. 6

Reaction of 2 with triphenylphosphine in acetone at −90 °C, forming complex 3 and triphenylphosphine oxide.

Density functional theoretical (DFT) calculations were performed to investigate the electronic and geometric structures of the [FeIV(O2)(DIG3tren)]2+ moiety in 2 in the presence (Fig. 7a) and absence (Fig. 7b) of H-bonding (HB) interaction. The ground spin state is a triplet state (S = 1), which is consistent with the experimental results. All side-on isomers lie higher in energy than the end-on isomer. The H-bonding interaction reduces the energy gap of the end-on and the side-on isomers from 13.9 to 2.4 kcal mol−1. With the three H-bondings (a strong one with a (N)H-Odistal distance of 1.74 Ă and two weak ones with (N)H-Oproximal distances of 2.02 and 1.92 Å; Supplementary Figs. 22 and 23), the end-on isomer lies 3.2 kcal mol−1 lower than the side-on isomer. It is important to note that H-bonding to the distal oxygen atom is necessary to stabilize the experimentally determined end-on structure; when only the proximal oxygen atom takes part in H-bonding, a side-on binding mode of O22− is stabilized (Supplementary Fig. 24). The calculated Fe–O (1.802 Å) and O–O (2.391 and 1.391 Å) distances of the end-on peroxido complexes are in good agreement with the experiment. The spins of the iron and the dioxygen moieties are 1.42 and 0.33, respectively. Without the H-bonding interaction, altered spin densities of 2.45 and −0.78 are observed at iron and oxygen, respectively. The increase of approximately one spin on iron and the location of nearly one spin on the dioxygen moiety demonstrates that H-bonding interaction causes the modification of the electronic structure of the iron-dioxygen intermediate from an iron(III)-superoxido species to an iron(IV)-peroxido structure. Thus, a second electron transfer from Fe(III) to O2̄ ®⦁ is coupled to the H-bonding stabilization of the resultant O22− moiety (Fig. 1c). Notably, a similar proton coupled electron-transfer process is reported in Hr (Fig. 1b) and model Cu and Mn complexes, which effects a superoxo-to-hydroperoxo conversion51,53,54,84–86.

Fig. 7. DFT calculated structure of 2.

Fig. 7

a Optimized structures of [Fe(O2)DIG3tren]2+ in the presence of H-bonding. b Optimized structures of [Fe(O2)DIG3tren]2+ in the absence of H-bonding. Calculations were done at the UBP86-D3(BJ)/def2-TZVPP level in solvent. Hydrogen atoms of the ligand are omitted for clarity, except nitrogen-bound H atoms. Lengths are in Å units. Values in parentheses are Gibbs free energies.

Spectroscopic characterization of 3

Reaction of 1/1-OTf with 2-(tert-butylsulfonyl)iodosobenzene (sPhIO) or tetrabutylammonium periodate (Bu4NIO4) in acetone at −70 °C also yielded the temperature sensitive orange species 3 (half-time at −20 °C = 270 s) with absorption maxima at λmax = 395 nm (ε = 8.92 mM−1 cm−1) and λmax = 805 nm (ε = 0.25 mM−1 cm−1) with no apparent intensity changes observed within 30 min at −70 °C. The 19F-NMR spectrum of 3 at 203 K (Supplementary Fig. 25) shows only one singlet at δ = −77.73 ppm, which is typical of free triflate. In conjunction with the fact that the UV/vis spectra of 3 in both acetone (typically non-coordinating) and acetonitrile (coordinating) are identical (Supplementary Fig. 26) in the relevant range (350 to 1000 nm), it is confirmed that no other exogenous ligands are bound at the iron center. This indicates a five-coordinate geometry for 3, leading to the formulation as [FeIV(O)(DIG3tren)]2+. It is worth noting that at −70 °C, 3 shows no reaction with PPh3, allowing its isolation in the reaction of 2 and PPh3 by UV–vis (Fig. 8a) and Mössbauer (Fig. 8b) spectroscopic methods. The latter reaction, when followed by Mössbauer spectroscopy (Fig. 8b) reveals the formation of a new doublet (δ = 0.09 mm/s; ΔEQ = 0.17 mm/s, 50%) with the concomitant disappearance of the doublet corresponding to 2. The low isomer shift of 3 suggests another iron(IV) species formed, and the low quadrupole splitting is consistent with other trigonal bipyramidal iron(IV)-oxido complexes in the S = 2 spin state16. The greatly reduced reactivity of 3 towards OAT is plausibly attributed to the steric shielding and H-bond stabilization of the FeIV=O core by the secondary coordination sphere in [FeIV(O)DIG3tren]. This is also supported by the calculated DFT structure of 3 that shows three short N−H···O distances of approximately 1.7 Å, indicative of strong hydrogen-bonding interactions (Supplementary Fig. 27).

Fig. 8. UV/vis, NRVS, and Mössbauer characterizations of 3.

Fig. 8

a UV/vis spectrum of the reaction of 2 with 30 equivalents of PPh3 in acetone at −90 °C with time traces as inset. b Zero-field Mössbauer spectrum of the reaction of 2 with 30 equivalents of PPh3 in acetone at −90 °C (gray line: experimental spectrum; black line: simulated spectrum; blue line: 3 with δ = 0.09 mm/s; ΔEQ = 0.17 mm/s, Γ = 0.45 mm/s, 50%; green line: decay product with δ = 0.45 mm/s, ΔEQ = 1.24 mm/s, Γ = 0.60 mm/s, 50%). c Experimental (left) and calculated (right) NRVS spectra of 3 (16O H), 18O labelled 3 (18O H), 3-d6 (16O D) and 18O labelled 3-d6 (18O D) generated by reacting 1 or 1-d6 with sPhI16O and sPhI18O (spectra are vertically stacked for clarity; insets: magnified Fe=O vibration bands). Calculated NRVS spectra corresp to a general structure with 4 equatorial N-ligands at Fe(IV) and an axial Fe=O bond opposite to a vacant axial site.

The zero-field Mössbauer spectrum of 3 (Supplementary Fig. 28) generated in the reaction of 1/1-OTf with sPhIO reveals a major species (δ = 0.09 mm/s; ΔEQ = 0.17 mm/s) with the same parameters as that obtained in the OAT reaction of 2 and PPh3 (Fig. 8b). High magnetic field Mössbauer spectra (Supplementary Fig. 29) confirm the assignment of the S = 2 ground state of 3 with a typical small zero field splitting (D = +5.17 cm−1). The minor doublet is best simulated with S = 0. The magnetic measurements also reveal a third species with similar features to the S = 5/2 component of 2. It is therefore also assigned to high spin Fe(III). The Mössbauer parameters of the S = 0 component are similar to the latter. An assignment as dimeric high spin Fe(III) would explain both the Mössbauer parameters and the S = 0 spin multiplicity.

The trigonal-bipyramidal geometry for 3 is also supported by XAS analysis (Supplementary Figs. 14 and 15), where a short iron-oxygen bond length of ca. 1.64 Å was obtained, typical of an iron(IV)-oxido double bond and in good agreement with the DFT value (1.69 Å; Supplementary Tables 9 and 10). The difference in Fe–O bond lengths between 2 and 3 highlights the distinction between the iron peroxido and iron oxido units in 2 and 3, respectively. The average Fe–N distances in both complexes (2.00–2.02 Å), which belong to the N donors of DIG3tren, are likewise consistent between experiment and theory. The Fe K-edge X-ray absorption spectrum (Supplementary Fig. 14) of 3 shows an edge energy of 7123.1 eV (vs. 7120.4 eV for 1 and 7122.4 for 2), which supports an FeIV oxidation state. Nuclear resonance vibrational spectroscopy (NRVS) shows an Fe=O vibration mode for 3 (Fig. 8c) at 845 cm−1 that shifts to 803 cm−1 by 18O isotopic labeling, thereby clearly confirming the presence of an iron-oxido unit.

In order to experimentally verify the H-bonding interaction of the FeIV=O moiety in 3 with the DIG3tren ligand, the deuterated complex [Fe(DIG3tren-d6)](OTf)2 (1-d6) was synthesized with the -NH groups of the DIG3tren ligand being deuterated (N−D). Subsequently, 3-d6 was synthesized in acetone-d6 by following a procedure analogous to that of the synthesis of 3. A comparison of the self-decay kinetics of 3 at −20 °C in acetone (t1/2 = 270 s), in acetone-d6 (t1/2 = 381 s) and 3-d6 in acetone-d6 (t1/2 = 558 s) shows a significant increase in the stability of 3 upon deuteration of the ligand and the use of deuterated solvent (Supplementary Fig. 30) with a two-step kinetic profile. This reveals that the decay of 3 occurs via hydrogen atom abstraction (HAA) of one of the amine groups, providing evidence for close proximity of the N−H moieties to the oxido unit due to H-bonding. Electrospray ionization mass spectrometry recorded after completion of the decay shows signals at m/z = 744.3 and 297.7, assigned to [Fe(O)(DIG3tren-H)(OTf)]⁺ and [Fe(O)(DIG3tren-H)]²⁺, respectively (calcd. m/z = 744.37 and 297.71). Both species are lighter by one hydrogen atom relative to 3 and shift accordingly upon use of sPhI¹⁸O, confirming retention of the oxido ligand (Supplementary Fig. 31). The formation of −1 H products is consistent with intramolecular hydrogen-atom abstraction by the oxido unit, as reported for the related iron(IV)–oxido complex [FeIV(O)(TMG3tren)]2+. Although an N–H group is involved in initiating the decay, the final product reflects oxygenation at a carbon site within the secondary coordination sphere, yielding an alkoxylated ligand framework (Supplementary Fig. 32).

The presence of H-bonds to the oxido ligand was also confirmed by NRVS data (Fig. 8c). The iron oxido vibration was shown to down-shift by about 4 cm−1 upon deuteration of the -NH groups of 3 in 3-d6, both in the 16O and 18O complexes (Fig. 8c), similar to the DFT predicted shifts of ca. 2 cm−1. This small shift may be expected since the iron-oxido vibration is likely only slightly influenced by the presence of H-bonds.

Although 1-d6 could be converted to 3-d6 in the presence of sPhIO, its reaction with O2 in acetone-d6 led to the formation of 2 in significantly reduced yields (5%; Supplementary Fig. 33). Notably, H/D kinetic isotope effects (KIEs) are expected to be pronounced when quantum tunneling is of importance87,88, such as in the case of low-temperature binding of O2 to 1 involving the motion of hydrogen/deuterium atoms (from a position where the N–H/D groups point away from the O2 binding site in 1 (closed conformation) to that in 2 where N–H/D points towards the O2 binding site (open conformation); see Fig. 4). In addition to affecting the kinetics of O2 binding, deuteration of a hydrogen bond by replacing protium (H) with deuterium (D) can cause geometric changes in the hydrogen bond, known as the geometric H/D isotope effect (GIE)89,90. Upon deuteration, the donor acceptor distances in the N–H---O22− hydrogen bonds in 2 is expected to increase (“normal” Ubbelohde effect)91,92, which may also contribute to the mitigated access of O2 to the FeII center in 1.

Binding of carbon monoxide

We also examined the reaction of 1 with CO to detect any iron−carbonyl intermediate similar to carboxyhemoglobin40,46,93,94. An acetone solution of 1, when treated with CO at −90 °C, results in the formation of a blue intermediate 1-CO (λmax = 604 nm; ε = 2.05 mM−1 cm−1). CO coordination to the metal center occurs without a change in oxidation state, but induces a spin-state transition from high-spin (S = 2) to low-spin (S = 1)95–97 as evident from the zero-field Mössbauer spectroscopy (Fig. 3a bottom). The Mössbauer spectrum reveals one major doublet (δ = 0.34 mm/s; ΔEQ = 1.00 mm/s, 88%) corresponding to 1-CO and some residual 1 (12%). 1H-NMR spectrum of 1-CO (Supplementary Fig. 34) shows paramagnetically shifted bands confirming the presence of a S = 1 Fe(II) low-spin center in a TBP geometry. The resonance Raman spectrum (in acetone at −90 °C upon excitation at 568 nm) shows the CO vibration at 1975 cm−1, which disappears when the sample is warmed to room temperature (Supplementary Fig. 35); it reappears again upon exposure to CO at −90 °C. Notably, the νCO stretching frequency of 1-CO is slightly higher than that of carboxyhemoglobin (1951 cm−1)98. DFT calculations on the Fe(II)−CO adduct show that CO binds in a linear fashion with the presence of three hydrogen bonds from N–H donors in the secondary coordination sphere. The calculated N−H···O(CO) distances (ca. 2.3–2.4 Å) indicate weak hydrogen-bonding interactions that do not significantly perturb the Fe–C–O geometry (Supplementary Fig. 36). The calculated νCO vibration at 1896 cm−1 is in good agreement with the experiment. As the temperature is increased, the absorption band at 604 nm due to 1-CO decreased (Fig. 3c). This process is reversible in the temperature range −90 to −20 °C. The equilibrium constant (Keq(CO)) was determined (Supplementary Figs. 37 and 38) to be 0.09 mM−1 at −60 °C. Interestingly, under similar conditions, 1 binds O2 with a Keq(O2) of 0.15 mM−1. This gives a M value of 0.6, which is an index of the discrimination between oxygen and carbon monoxide bindings. Thus, the secondary coordination sphere provided by the DIG3tren ligand functions similarly as the distal histidine in Hb/Mb; it provides an ideal environment for strong H-bonds (N−H···O distances of 1.73, 1.95, and 2.00 Å; Fig. 7) with bound oxygen in [Fe(η1-O2)(DIG3tren)]2+, but out of place for optimal interaction with a linear bound CO (very weak N−H···O(CO) H-bonding interactions with 2.37, 2.36, and 2.40 Å; Supplementary Fig. 36a for 31-CO) in [Fe(CO)(DIG3tren)]2+. This is believed to be crucial for increasing the dioxygen affinity for [FeIIDIG3tren] compared to carbon monoxide.

This study establishes a new milestone in connecting H-bonding with reversible oxygen and carbon monoxide bindings in a mononuclear nonheme system, demonstrating an unusual iron mediated two-electron reduction of oxygen. Peroxide dianion is known to form strong hydrogen bonds to N–H groups from the hexacarboxamide cryptand99 or a zinc tripod65, which has led to two-electron reduction of dioxygen in the presence of an external reductant like cobaltocene. Closely related hydrogen-bond-assisted two-electron O2/H2O2 interconversion has also been demonstrated in saddle-distorted porphyrin/isophlorin redox couples100. In this report, we have now extended this effect to iron-dioxygen chemistry. DFT studies suggest that three H-bonding interactions between the O22− dianion and N–H groups from the DIG3tren ligand sufficiently reduce the barrier for the two-electron reduction of O2 by Fe(II) to form a rare nonheme Fe(IV)-peroxido intermediate (S = 1) in the reaction of 1 with dioxygen. The two-electron transfer from FeII to O2 is further facilitated by the electron-rich nature of [Fe(DIG3tren)]2+. This is evident from the low FeIII/II potential of +0.17 V vs. Fc+/o for 1 and a FeIV/III reductive wave for 3 at a large negative potential with Ep,c of −1.63 V vs. Fc+/o (determined by cyclic voltammetry; Supplementary Figs. 39 and 40), and can be attributed to the excellent donor quality of DIG3tren containing the superbasic guanidine moieties101. In the presence of none or weak H-bonding interaction, one-electron chemistry would prevail, as has been previously observed in the stabilization of the iron(III)-O2−• complexes in the Fe(II) and O2 reactions34–36,38,66. Notably, the ability to reversibly bind O2 is unique for four coordinate 1 in the presence of OTf anion, where all the DIG arms exist in the closed conformation (Fig. 2). The stabilization of the Fe(IV)-peroxido intermediate, however, warrants the conversion of the DIG arms into the open conformation (Figs. 4 and 7). Accordingly, O2 binding to the Fe(II) center and the isomerization of the DIG arms must occur at comparable rates, so that the transient Fe(III)-superoxido intermediate is converted to the more stable Fe(IV)-peroxido form via a H-bonding mediated electron-transfer process. Significant increase in the O2 binding rate relative to the ligand reorganization rate (for example, in the open conformation of one or more DIG units of the DIG3tren ligand), will allow the oxidative decomposition of ligand by the transient Fe(III)-superoxido intermediate, and complex 2 will be inaccessible. To further probe the role of the counterion, we examined complexes bearing weakly coordinating anions. While the solid-state Mössbauer spectrum of 1-BF4 shows a single Fe(II) species closely resembling 1, this complex does not form intermediate 2 upon exposure to O2, as evidenced by UV/vis spectroscopy (Supplementary Fig. 41). This behavior is attributed to stronger hydrogen-bonding interactions between BF4− and the DIG3tren ligand, which disrupt the secondary-sphere preorganization required for peroxido stabilization (Fig. 4). In contrast, complexes containing truly non-coordinating anions (1-BPh4 and 1-NTf2) display multiple Fe(II) environments in the solid state, consistent with the increased conformational flexibility of the ligand scaffold, and likewise fail to form 2 (Supplementary Figs. 42–45). Collectively, these results highlight the unique role of the triflate anion: it is sufficiently weakly coordinating to leave the axial site accessible for O2, yet capable of preorganizing the hydrogen-bonding network in a manner that selectively stabilizes the iron(IV)-peroxido intermediate (Fig. 4). Deuteration of the N–H group in the DIG moiety led to the formation of 2 in a reduced yield of 5%, giving an N–D/N–H kinetic isotope effect of 0.11. This may further corroborate the motion of hydrogen/deuterium atoms during the formation of 2; the rate of DIG3tren-d6 rearrangement involving heavier N–D moieties becomes slower relative to O2 binding, yielding 2 in significantly reduced yields. Thermodynamic parameters for O2 binding were obtained from a van’t Hoff analysis. Owing to the limited thermal stability of intermediate 2 above −80 °C, equilibrium constants could only be determined over a narrow temperature range (−95 to −80 °C in acetone). The resulting van’t Hoff plot (Supplementary Fig. 46) yields ΔH° = −10.66 ± 0.37 kJ mol−1 and ΔS° = −16.5 ± 2.0 J mol⁻¹ K⁻¹. The negative values of ΔH° and ΔS° are consistent with the binding of O2 only at low temperature. Furthermore, a significantly negative ΔS° term may corroborate an associative mechanism characterized by a well-ordered transition state (TS).

The reversibility of the dioxygen binding is a remarkable property of 2, typically observed in mononuclear heme or dinuclear nonheme systems. The low M value of 0.6 further shows the importance of H-bonds in relation to the preference for oxygen bonding vs. carbon monoxide bonding. As has been proposed in hemoproteins102–106, the presence of weak secondary H-bond donors does not affect significantly the energy of the linear Fe-CO unit, concomitantly increasing the O2 affinity of the intrinsically bent Fe-O2 group. Nevertheless, the near-quantitative formation of a single Fe(II)–CO adduct upon exposure to CO demonstrates that all Fe(II) centers in acetone solution (corresponding to 1, 1’, and 1”; Supplementary Fig. 16) are accessible for O2/CO binding. The CO coordination proceeds without electron transfer, preserving the Fe(II) oxidation state and preventing ligand oxidation; consequently, all conformers converge cleanly to 1-CO (Fig. 3a, bottom). In contrast, the productive two-electron reduction of O2 occurs only for a specific isomer in which all N–H hydrogen-bond donors stabilize the bound O22− species, thereby enabling formation of intermediate 2. For other isomers lacking this preorganized hydrogen-bonding environment, O2 binding instead results in a highly reactive Fe(III)-superoxido species, which rapidly induces ligand oxidation, resulting in reduced yields for 2. Complex 2 reacts with PPh3, leading to O–O bond cleavage and subsequent formation of a high-valent Fe(IV)-oxido species 3 (S = 2), which can also directly be synthesized from 1 using common oxygen atom transfer reagents. Thus, by elucidating the interplay between H-bonding and iron-based oxygen activation, our work expands the fundamental understanding of oxygen activation in biological and bioinspired systems, paving the way for novel catalyst design and biomimetic applications.

Methods

Chemicals and handling

Chemicals employed were purchased from the companies ABCR, ACROS, SIGMA-ALDRICH, MERCK, BLDpharm, and TCI, and used without further purification. Anhydrous solvents (acetonitrile, diethyl ether, dichloromethane and acetone) were purchased from CARL-ROTH GmbH under the tradename ROTIDRY (>99.5%, <50 ppm H2O), degassed by freeze-pump-thaw methods prior to use and stored over activated molecular sieves (except acetone). Deuterated solvents were purchased from EURISO-TOP. Preparation and handling of air or water sensitive compounds were performed under an inert atmosphere using either Schlenk techniques or a GS MEGA glovebox from GS GLOVEBOX Systemtechnik GmbH filled with N2. Nitrogen and Argon of quality 5.0 were used for this purpose and were purchased from AIR LIQUIDE. Commercially available O2 from AIR LIQUIDE (99.99% pure) and 18O2 (97.2% pure) from Euriso-Top were purchased and used as received.

Elemental analysis

All elemental analyses were performed by the analytical service of the Institut für Chemie of the Humboldt-Universität zu Berlin. The percentages of carbon, hydrogen, nitrogen and sulphur were determined using an HEKAtech EURO EA 3000 analyzer.

Nuclear magnetic resonance spectroscopy

All NMR spectra were recorded using a BRUKER AVANCE DPX 300 MHz or BRUKER AVANCE III 500 MHz spectrometer. Those of 1H, 13C, and 19F nuclei were recorded in deuterated solvents, and chemical shifts (ppm) referenced against residual protic solvent peaks. Unless otherwise stated, all spectra were recorded at room temperature.

Electrospray ionization mass spectrometry

ESI-MS spectra of organic molecules and inorganic complexes in solution were recorded by using an ADVION EXPRESSION CMS spectrometer (under typical ionization conditions), and spectra in positive and negative mode were collected in parallel; acetonitrile was used as an eluent. For thermally unstable complexes, the freshly thawed solutions were directly injected into the instrument while the ionization source temperature was decreased to 50 °C. The analysis of the data was carried out with the ADVION DATA EXPRESS version 6.0.11.3.

Gas chromatography

GC analysis was carried out by using an AGILENT 7890B gas chromatograph (HP5 25 column, 30 m) with a flame-ionization detector. GC-MS was performed on an AGILENT 5977B spectrometer with a triple-axis detector.

Single crystal X-ray structure determinations

For the determination of the X-ray crystal structure of the complex, data collection was performed at 100 K on a BRUKER D8 VENTURE diffractometer by using Mo Kα radiation (λ = 0.71073 Å). Multi-scan absorption corrections implemented in SADABS107 were applied to the data. The structure was solved by the intrinsic phasing method (SHELXT 2014/5)108 and refined by full matrix least square procedures based on F2 with all measured reflections (SHELXL-2018/3)109 in the graphical user interface SHELXle110) with anisotropic temperature factors for all non-hydrogen atoms. All hydrogen atoms were added geometrically and refined by using a riding model.

Mössbauer spectroscopy

Mössbauer spectra in the absence of magnetic field were recorded on a SEECO MS6 spectrometer that comprises the following instruments: a JANIS CCS-850 cryostat, including a CTI-CRYOGENICS closed cycle 10 K refrigerator, and a CTI-CRYOGENICS 8200 helium compressor. The cold head and sample mount are equipped with calibrated DT-670-Cu-1.4 L silicon diode temperature probes and heaters. Temperature is controlled by a LAKESHORE 335 temperature controller. Spectra are recorded using a LND-45431 Kr gas proportional counter with beryllium window connected to the SEECO W204 γ-ray spectrometer that includes a high voltage supply, a 10 bit and 5 μs ADC and two single channel analyzers. Motor control and recording of spectra is taken care of by the W304 resonant γ-ray spectrometer. For the reported spectra a RIVERTEC MCO7.114 source (57Co in Rh matrix) with an activity of about 1 GBq was used. All spectra were recorded in a plastic sample holder with a solid or frozen solution sample at 14 K, and data were accumulated for about 12–24 h. Spectra were simulated using the software WMOSS4111. Applied-field Mössbauer spectra were measured on an OXFORD INSTRUMENTS Spectromag 4000 cryostat containing an 8 T split-pair superconducting magnet. The spectrometer was operated in constant acceleration mode in transmission geometry, with the magnetic field applied parallel to the direction of the gamma rays. The isomer shifts are referenced against a room temperature metallic iron foil. Analysis of the data was performed using the in-house developed Python package easyMoss112. All spectra were modeled with slow relaxation.

Resonance Raman (rRaman) spectroscopy

Resonance Raman spectra were measured in acetone-d6 at −90 °C (Bruker cryostat) with 568 nm excitation (Coherent cw Kr+-laser, 8 mW) using a Horiba Jobin-Yvon LabRAM HR800 confocal Raman spectrometer. The sample concentrations employed were 10–20 mM.

Attenuated total reflection Fourier-transform infrared spectroscopy (ATR-FTIR)

IR spectra were measured at a Bruker ALPHA II FTIR spectrometer using the platinum ATR module (diamond crystal). Spectra were collected with a resolution of 4 cm−1 in the range of 350–4000 cm−1 and using 24 scans.

UV–vis spectroscopy

The UV–vis absorption spectra were recorded with an 8453 UV–visible spectroscopy system from Agilent. The measurements were carried out in 10 mm precision cuvettes made of SUPRASIL® quartz glass, the closures of which were equipped with a septum. The measurements at low temperatures were carried out by cooling the cuvette holder using a cooling thermostat USP-203-A from Unisoku Scientific Instruments. The analysis of the spectra was carried out with the software UV–Visible Chemstation from Agilent.

X-ray absorption spectroscopy

XAS at the Fe K-edge was performed at beamline KMC-3 at the BESSY-II synchrotron (Helmholtz Center Berlin, Germany) using a set-up including a Si[111] double-crystal monochromator, a 13-element energy resolving Si-drift detector (RaySpec) for X-ray fluorescence monitoring, and DXP-XMAP pulse-processing electronics (XIA). Samples were held at 20 K in a liquid-helium cryostat (Oxford). The energy axis of the monochromator was calibrated (accuracy ±0.1 eV) using the K-edge spectrum of an iron metal foil (fitted reference energy of 7112 eV in the first derivative spectrum). The spot size on the samples was ca. 1.5 × 3.0 mm (vertical × horizontal) as set by a focusing mirror and slits. X-ray fluorescence spectra were collected using a continuous scan mode of the monochromator (scan duration ca. 10 min). Up to 6 scans were averaged (1–2 scans per sample spot) for signal-to-noise ratio improvement. XAS data were processed (dead-time correction, background subtraction, normalization) to yield XANES and EXAFS spectra using our earlier described procedures and in-house software113. k3-weighted EXAFS spectra were simulated with in-house software and phase functions from FEFF9 (S02 = 0.8)114.

Nuclear resonance vibrational (X-ray) spectroscopy (NRVS)

NRVS data were collected at undulator beamline ID18 at the European Synchrotron Radiation Facility (ESRF, Grenoble, France) using the previously described set-up115,116 including a heat-load monochromator, a high-resolution monochromator (FWHM ~ 0.7 meV), gated APD detectors (~1 cm2 active area) for prompt and delayed inelastic and forward scattering detection, and a cold-finger liquid-helium cryostat. The storage ring was operated in 16-bunch mode (~90 mA). A sample temperature during the measurements of 30 ± 10 K was estimated from the ratio of NRVS counts in ±2.5–5 meV windows around the resonance. NRVS counts were detected with an APD at 90° to the incident X-ray beam and at ~4 mm distance from the sample. The energy axis of the high-resolution monochromator was calibrated using the CN− vibrational band at 74.0 meV of a (NH4)2Mg57Fe(CN)6 powder sample as a reference. NRVS spectra were collected in a −10 meV to 120 meV energy region around the resonance (0.2 meV steps, 2.5 s per data point, spot size on sample ~1.5 × 0.5 mm2) and up to 20 scans were averaged for signal-to-noise ratio improvement (5 scans of ~30 min per sample spot). NRVS data were processed, and the normalized partial vibrational density of states (PDOS) was calculated with the software package available at ID18. Energy to frequency axis conversion was done (1 meV = 8.06554 cm−1) before comparison of NRVS spectra. For theoretical NRVS spectra from DFT calculations, NRVS vibrational frequencies were derived from normal mode analysis of geometry-optimized, relaxed structures from Gaussian calculations. NRVS and normalized (spectral area = 1) PDOS spectra were calculated using NISspec117. Calculated (stick) NRVS spectra were broadened by Lorentzians (FWHM 14 cm−1) for comparison with experimental spectra. In-house software and functionalized EXCEL-sheets were used to process Gaussian and NISspec output files. NRVS vibrational modes were visualized with ChemCraft.

Cyclovoltammetry (CV)

Cyclic Voltammetry was carried out with a CHI 600E potentiostat using a 3 mm diameter glassy carbon disk electrode (ALS Co Ltd.) as working and a platinum wire (length 5 cm, diameter 0.5 mm; ALS Co Ltd.) as counter electrode. Prior to use, electrodes were polished with 0.05 μm alumina suspensions. Ag/AgNO3 (10 mM AgNO3 and 0.1 M [N(n-Bu)4]PF6 in MeCN) was used as the reference electrode for room temperature measurements and an Ag wire quasi-reference electrode for low temperature measurements. CV measurements were performed in a three-necked glass cell under an Ar atmosphere. Two milliliters of 1.5 mM compound solution in acetonitrile or acetone was taken in the presence of 100 mM TBAF as the supporting electrolyte. Unless noted otherwise, a scan rate of 100 mV/s was applied. Ferrocene (Fc) was used as an internal reference, and the potential scale is normalized with respect to the potential of the Fc+/0 couple.

Computational methodology

Density functional theory (DFT) calculations were carried out using the Gaussian 16 suite of programs118. The spin-unrestricted BP86 functional corrected with Grimme 10’s dispersion119 using the Becke–Johnson damping scheme120 was employed with two series of basis sets: (a) the TZVP basis set for the iron core and the atoms of the first coordination sphere, and 6–31 G** for the rest atoms. This basis set is denoted as B1 and was used to optimize transition states (TS) and minima; (b) The basis def2-tzvpp basis set for all atoms. This basis set is denoted as B2, which was used for single point energy (SPE) corrections. Solvent effects (acetone, e = 20.493) were included in all calculations using the conductor-like polarizable continuum model (CPCM) as implemented in Gaussian 16. An experimental temperature of −90 °C was adopted for the Gibbs free energy calculations.

Sample preparation

Complex 2 was usually formed by bubbling excess of dioxygen to 2 ml of a 1 mM solution of complex 1 in acetone at −90 °C under inert conditions in a UV–vis quartz cuvette (10 mm pathlength). The formation of 2 was monitored by UV–vis following the bands at 550 and 700 nm. Complex 1-CO was formed by purging an acetone solution with CO in an airtight UV/vis cuvette for 2 min. The solution was then cooled to −90 °C, and 0.05 ml of a 20 mM solution of 1 in acetone was added. The formation of 1-CO occurs immediately, as can be observed from the formation of the band at 604 nm. Complex 3 was usually formed by adding three equivalents of SPhIO dissolved in 0.05 ml DCM (or three equivalents of Bu4NIO4 dissolved in 0.05 ml acetone) to 2 ml of a 1 mM solution of complex 1 in acetone at −70 °C under inert conditions in a UV–vis quartz cuvette (10 mm pathlength). The same procedure was followed with 3-d6 using acetone-d6 as solvent. The formation of 3 was monitored by UV–vis following the bands at 525 and 810 nm. The samples were transferred into precooled sample holders as soon as the formation was complete. For the preparation of GC samples, five equivalents of substrate were added. After the 2000 s, the reaction solution was quenched with NaHSO3 and biphenyl was added as an internal standard. The solution was filtered with a small column filled with silica and MgSO4, rinsing with EtOAc. From the obtained solutions, 1 ml of each was used for GC-analysis.

Generation of 16/18O2

In a 500 ml Young Schlenk flask, 100 mbar of 16O2 and 18O2 were added by using a 3-way stopcock. The pressure was then reduced to approx. 70 mbar by carefully applying vacuum (note that low pressure is necessary, otherwise the applied energy in the next step will not lead to the breaking of the oxygen–oxygen bonds, but mainly to kinetic collisions). Then a High Frequency Generator (model BD-10ASV from Electro-Technic Products 4642 N Ravenswood Ave Chicago, IL 60640 USA) was used to apply high voltage (45 kV at a frequency of approx. 500 kHz with a current output about 1 mA) to the Schlenk flask (4 × 10 min with 20-min breaks in between to avoid overheating the generator), causing sparks to be observed. The gas mixture was then condensed into a 10 ml Young Schlenk flask containing a degassed, frozen solution of complex 1/1-OTf in acetone-d6 for intermediate formation. Intermediate formation took place at −90 °C using a cooling bath.

Band fitting analysis of the rRaman spectra

The band fitting analysis was carried out on the basis of Lorentzian functions. First, a weak solvent band at 818.7 cm−1 (half width 24.2 cm−1), determined from the spectrum of the neat solvent, was subtracted from the spectral region of interest (785-840 cm−1) of the complexes. Subsequently, the spectrum of complex 2 generated with 16O2, was analyzed to yield a band at 823.4 cm−1 (half width 12.4 cm−1). The spectrum of the complex generated by the 16O2/18O2 gas mixture was then simulated by four Lorentzians. Here we fixed the band widths to 12.4 cm−1 as determined for the 16O2-complex (Supplementary Fig. 20A). The fit provides an excellent reproduction of the bands of 16O2- and 18O2-complexes and also yields two band components at positions expected for the mixed 16O–18O-complexes. The residuals (Supplementary Fig. 20B) correspond to the noise level underlining the high quality of the fit. Note that the experimental set up does not ensure a gas supply at 1:1 ratio of 16O2 and 18O2, which accounts for deviations from the corresponding intensity ratio of 1:1:1:1. The alternative fit using three Lorentzian functions (Supplementary Fig. 20C) yielded similar residuals (Supplementary Fig. 20D) and thus a mathematically equally good fit. However, it does not reproduce the bands positions of 16O2- and 18O2-complexes, such that the side-on configuration can be ruled out.

Synthesis of tert-butylphenylsulfide

The compound has been previously reported121,122, and was independently synthesized as described below. A large excess of isobutene was condensed into a rapidly stirred suspension of Amberlyst H-15 (3 g) in thiophenol (11 g, 0.1 mol) and diethylether (80 mL) at –78 °C. The suspension was stirred overnight at –78 °C (dry ice bath). Upon completion, the mixture was allowed to warm to room temperature and subsequently filtered. The solvent was removed under reduced pressure to yield tert-butylphenylsulfide as colorless liquid (16.3 g, 95%) with a strong odor. 1H-NMR (300 MHz; CDCl3): δ = 7.47 (m, 2H), 7.28 (m, 2H), 7.20 (m, 1H), 1.22 (s, 9H) ppm.

Synthesis of tert-butylphenylsulfone

The compound has been previously reported121,122, and was independently synthesized as described below. Sodium perborate tetrahydrate (20.8 g, 120 mmol) was added to a solution of tert-butylphenylsulfide (5 g, 30 mmol) in acetic acid (60 mL). The cloudy suspension was stirred at 50 °C for 3 h, cooled, poured into water (200 mL), and extracted with dichloromethane (4 × 50 mL). The combined extracts were washed repeatedly with aqueous sodium hydrogen carbonate and water until the acid had been neutralized, and then dried (MgSO4) and evaporated under reduced pressure. The residue was washed with pentane to yield tert-butylphenylsulfone (2.26 g, 38%) as a colorless solid. 1H-NMR (300 MHz; CDCl3): δ = 7.94–7.86 (m, 2H), 7.68–7.53 (m, 3H), and 1.34 (s, 9H) ppm.

Synthesis of tert-butylsulfonyliodobenzene

The compound has been previously reported121,123, and was independently synthesized as described below. To tert-butylphenylsulfone (8.74 g, 44 mmol) in 100 mL THF at –78 °C was added 21.12 mL of n-BuLi in hexane (2.5 M, 52.8 mmol) over 5 min via syringe. After stirring for 40 min, a solution of I2 (17.5 g, 52.8 mmol) in 50 mL THF was added by cannula to the orange solution. The reaction mixture was stirred vigorously and allowed to warm up to room temperature. The excess iodine was quenched with aqueous sodium sulfite (Na2SO3). The organic layer was then separated and combined with another extraction of the aqueous layer with diethylether. The combined organic extracts were dried (MgSO4) and evaporated under vacuum to give tert-butylsulfonyliodobenzene (10.80 g, 75%) as a yellow solid. 1H-NMR (CDCl3, 300 MHz) δ = 8.21–8.14 (m, 1H), 8.12–8.06 (m, 1H), 7.60–7.52 (m, 1H), 7.24–7.18 (m, 1H), 1.42 (s, 9H) ppm.

Synthesis of 2-(tert-butylsulfonyl)(diacetoxyiodo)benzene

The compound has been previously reported121,123, and was independently synthesized as described below. A mixture of hydrogen peroxide (5 ml, 30%) and acetic anhydride (21 ml, 222 mmol) was stirred at 40 °C for 4 h. The solution was cooled to room temperature. To this solution was added tert-butylsulfonyliodobenzene (5 g, 15.4 mmol). The resulting pale-yellow solution was stirred for 24 h at 25–30 °C (if temperature is allowed to increase above this range PhSO2tBu is formed). The solvent was removed under reduced pressure to yield 2-(tert-butylsulfonyl)(diacetoxyiodo)benzene as a white solid (2.07 g, 33%). The product is best used directly for the synthesis of SPhIO, but can be further purified, albeit in greatly reduced yields, by recrystallization from a cyclohexane/acetic acid mixture. 1H NMR (CDCl3, 300 MHz): δ = 8.58–8.55 (m, 1H), 8.29–8.26 (m, 1H), 7.87–7.82 (m, 1H), 7.72–7.67 (m, 1H), 1.95 (s, 6H), 1.42 (s, 9H) ppm.

Synthesis of 2-(tert-butylsulfonyl)iodosylbenzene (SPhIO)

The compound has been previously reported121,123, and was independently synthesized as described below. To solid 2-(tert-butylsulfonyl)(diacetoxyiodo)benzene (2.4 g, 5.42 mmol) was added an aqueous solution of sodium hydroxide (20 ml, 3 M) dropwise with vigorous stirring. The resulting yellow suspension was stirred for another 25 min. The yellow solid was collected by filtration, washed with water and diethyl ether, and then dried under reduced pressure to give 2-(tert-butylsulfonyl)iodosylbenzene (300 mg, 16%) as a yellow powder. 1H-NMR (CDCl3, 300 MHz): δ = 8.14–8.06 (m, 1H), 7.94–7.83 (m, 2H), 7.69–7.60 (m, 1H), 1.42 (s, 9H) ppm. SPhI18O was synthesized analogously using Na18OH, prepared from NaH and H218O.

Synthesis of Fe(MeCN)2(OTf)2

In a Schlenk flask, 6 ml of concentrated hydrochloric acid (37%) was degassed by bubbling argon through the solution (note: do not use a metal cannula for this step). Elemental iron (100 mg) was weighed using a nonmagnetic spatula, then collected with a magnetic stir bar and added to the acid solution under an inert atmosphere. Immediate gas evolution is observed. The closed reaction mixture was heated to 60 °C and stirred until a clear, colorless solution was obtained. To prevent overpressure from building up, the pressure was occasionally reduced slightly. Drying at 60 °C under vacuum yielded FeCl2·4H2O as a white solid, which was then suspended in dry acetonitrile (10 ml). An excess of (CH3)3SiOTf (4 g) was added slowly in a glovebox. The solution was stirred for 18 h, and the solvent was removed by vacuum. The remaining yellow solid was dissolved in a minimum amount of acetonitrile, and an excess of dry diethyl ether was added. The mixture was shaken vigorously during which time white precipitate was formed. The solvent was then removed by decantation. The remaining solid was washed five times with dry diethyl ether and dried, yielding [Fe(MeCN)2(OTf)2] as a white solid (700 mg, 90%). Mössbauer spectroscopy revealed a single iron species with δ = 1.36 mm/s and ΔEQ = 3.30 mm/s. 57Fe(MeCN)2(OTf)2 was synthesized analogously using elemental 57Fe.

Synthesis of [Fe(TMG3tren)(OTf)]OTf

A solution of TMG3tren (120 mg, 0.27 mmol) in 1 ml acetonitrile was added dropwise to a solution of Fe(MeCN)2(OTf)2 (110 mg, 0.25 mmol) in 1.5 ml acetonitrile. After stirring for 24 h at room temperature, the solution was dropped into 20 ml of diethyl ether, resulting in the precipitation of a white solid. The solvent was then removed, the solid was washed twice with diethyl ether and dried to yield [Fe(TMG3tren)(OTf)](OTf) as a white solid (145 mg, 72%). Mössbauer spectroscopy revealed a single iron species with δ = 1.00 mm/s and ΔEQ = 1.66 mm/s.

Synthesis of Fe(THF)5(NTf2)2

In a Schlenk flask, HNTf2 (1 g, 3.55 mmol) was dissolved in dry benzene (6 ml), cooled to 0 °C, and PhSiMe3 (0.51 ml, 3 mmol) was added dropwise. The reaction mixture was stirred for 1 h while warming to room temperature. The resulting solution was then transferred to a suspension of FeCl2 (172 mg, 1.36 mmol) in THF (6 ml), which turned yellow upon addition. After stirring for 16 h, the supernatant was removed by pipette, and the precipitate washed five times with THF and twice with hexane. Subsequent drying yielded Fe(THF)5(NTf2)2 (1.10 g, 83%) as a white solid. Mössbauer spectroscopy revealed a single iron species with δ = 1.39 mm/s and ΔEQ = 3.01 mm/s.

Synthesis of tris(N’,N”-diisopropylguanidinyl-2-ethyl)amine (DIG3tren)

The synthesis is based on a literature procedure70. A mixture of tris(2-aminoethyl)amine (0.3 ml, 2 mmol) and diisopropylcarbodiimide (DIC, 1 ml, 6.46 mmol) was heated under argon to 100 °C for 3 h The excess of DIC was removed under vacuum, yielding DIG3tren as a viscous, pale yellow oil (997 mg, 95%). 1H-NMR (500 MHz, CDCl3) δ = 3.53 (br, 6H), 3.10 (t, J = 6.48 Hz, 6H), 2.69 (t, J = 6.48 Hz, 6H), 1.11 (d, J = 6.33 Hz, 36H) ppm. ESI-MS (pos. mode): m/z 525.4 [(DIG3tren+H)+].

Synthesis of [Fe(DIG3tren)](OTf)2 (1/1-OTf)

A solution of DIG3tren (255 mg, 0.48 mmol) in 1.5 ml acetonitrile was added dropwise to a solution of Fe(MeCN)2(OTf)2 (159 mg, 0.36 mmol) in 1.5 ml acetonitrile. After stirring for 20 h at room temperature, the yellow solution was dropped into 20 ml of diethyl ether, resulting in the precipitation of a light-yellow solid. The solvent was then removed, the solid was washed twice with diethyl ether and dried to yield [Fe(DIG3tren)](OTf)2 as a light-yellow solid (172 mg, 55%). Colorless crystals suitable for X-ray crystallography were obtained from an acetone/diethyl ether solution in the ratio (1:1). For Mössbauer and NRVS samples, [57Fe(DIG3tren)](OTf)2 was synthesized starting from 57Fe(MeCN)2(OTf)2. 19F-NMR (282 MHz, acetone-d6) δ = −78.86 (s) ppm. ESI-MS (pos. mode): m/z 729.3 [Fe(DIG3tren)(OTf)]+, 290.2 [Fe(DIG3tren)]2+. Elemental analysis calc. for C29H60F6FeN10O6S2: C 39.63, H 6.88, N 15.94, S 7.30; found: C 39.82, H 6.98, N 15.92, S 7.07.

Synthesis of [Fe(MeCN)6](BPh4)2

A solution of NaBPh4 (706 mg, 2.06 mmol) in 5 ml acetonitrile was added dropwise to a solution of Fe(MeCN)2(OTf)2 (300 mg, 0.69 mmol) in 5 ml acetonitrile. A white solid precipitated immediately. After stirring for 2 h, the solid was filtered off, washed twice with acetonitrile and diethyl ether and dried to yield [Fe(MeCN)6](BPh4)2 as a white solid (380 mg, 58%). Mössbauer spectroscopy revealed a single iron species with δ = 1.28 mm/s and ΔEQ = 0.78 mm/s.

Synthesis of [Fe(DIG3tren)](BPh4)2 (1-BPh4)

A solution of DIG3tren (150 mg, 0.28 mmol) in 2 ml acetonitrile was added dropwise to a solution of [Fe(MeCN)6](BPh4)2 (220 mg, 0.23 mmol) in 1.5 ml acetonitrile. After stirring for 24 h at room temperature, the yellow solution was dropped into 20 ml of diethyl ether, resulting in the precipitation of a pale yellow solid. The solvent was then removed, the solid was washed twice with diethyl ether and dried to yield [Fe(DIG3tren)](BPh4)2 as a pale yellow solid (160 mg, 57%). Mössbauer spectroscopy revealed two iron species with δ = 1.00 mm/s and ΔEQ = 2.62 mm/s and δ = 0.85 mm/s and ΔEQ = 1.39 mm/s. Elemental analysis calc. for C75H100B2FeN10: C 73.89, H 8.27, N 11.49; found: C 74.18, H 8.29, N 11.45.

Synthesis of [Fe(DIG3tren)](BF4)2 (1-BF4)

A solution of DIG3tren (500 mg, 0.95 mmol) in 1.5 mL MeCN was added dropwise to a suspension of Fe(BF4)2·6H2O (290 mg, 0.86 mmol) in 2 mL MeCN. The reaction mixture was stirred for 20 h at room temperature. The resulting dark green mixture was precipitated in 20 mL diethyl ether. The solvent was removed, and the precipitate was washed two times with diethyl ether and dried to yield [Fe(DIG3tren)](BF4)2 as a dark green solid (350 mg, 55%). Mössbauer spectroscopy revealed a single iron species with δ = 1.28 mm/s and ΔEQ = 3.01 mm/s. Elemental analysis calc. for C27H60B2F8FeN10: C 42.99, H 8.02, N 18.57; found: C 43.12, H 8.04, N 18.51.

Synthesis of [Fe(DIG3tren)](NTf2)2 (1-NTf2)

A solution of DIG3tren (140 mg, 0.26 mmol) in 1 ml acetonitrile was added dropwise to a solution of [Fe(THF)5](NTf2)2 (235 mg, 0.24 mmol) in 1.5 ml acetonitrile. After stirring for 24 h at room temperature, the yellow solution was dropped into 20 ml of diethyl ether, resulting in the precipitation of a pale yellow solid. The solvent was then removed, the solid was washed twice with diethyl ether and dried to yield [Fe(DIG3tren)](NTf2)2 as a pale yellow solid (190 mg, 69%). Mössbauer spectroscopy revealed three iron species with δ = 1.03 mm/s and ΔEQ = 2.68 mm/s, δ = 0.89 mm/s and ΔEQ = 1.92, δ = 0.84 mm/s and ΔEQ = 1.06 mm/s, mm/s. Elemental analysis calc. for C31H60F12FeN12O8S4: C 32.63, H 5.30, N 14.73, S 11.24; found: C 32.75, H 5.32, N 14.69, S 11.28.

Synthesis of [Zn(DIG3tren)(Br)]Br (Zn-Br)

A solution of DIG3tren (730 mg, 1.39 mmol) in 1.5 mL MeCN was added dropwise to a suspension of ZnBr2 (280 mg, 1.25 mmol) in 2 mL MeCN. The reaction mixture was stirred for 20 h at room temperature. The resulting white suspension was precipitated in 20 mL diethyl ether. To ensure complete precipitation, the solution was stored at −40 °C for 20 h. The solvent was removed, and the precipitate was washed two times with diethyl ether and dried to yield [Zn(DIG3tren)Br]Br as a white solid (580 mg, 60%). Colorless crystals suitable for X-ray crystallography were obtained by vapor diffusion from a MeCN solution with diethyl ether. Elemental analysis calc. for C27H60Br2N10Zn: C 43.24, H 8.06, N 18.68; found: C 43.40, H 8.09, N 18.62.

Synthesis of tren-d6, DIG3tren-d6 and [Fe(DIG3tren-d6)](OTf)2 (1-d6)

Tris(2-aminoethyl)amine (0.6 ml, 4 mmol) was mixed with 1.3 ml D2O, stirred for 24 h, and then dried. This step was repeated to ensure complete deuteration to form tris(2-aminoethyl)amine-d6. 1H-NMR (300 MHz, CDCl3) δ = 2.66 (t, J = 6.12 Hz, 6H), 2.42 (t, J = 6.12 Hz, 6H) ppm. Subsequently, a mixture of tris(2-aminoethyl)amine-d6 (0.3 ml, 2 mmol) and diisopropylcarbodiimide (DIC, 0.93 ml, 6 mmol) was heated under argon to 100 °C for 3 h. Drying under vacuum yielded DIG3tren-d6 as a viscous, pale yellow oil. 1-d6 was synthesized by replacing DIG3tren and acetonitrile with DIG3tren-d6 and acetonitrile-d3 following the procedure for 1.

Supplementary information

Source data

Source Data (69.9KB, xlsx)

Acknowledgements

We thank Martin Clémancey for magnetic Mössbauer measurements and Katrin Warm for SC-XRD measurements. Beamtime at the station XAS@KMC-3 at the BESST-II Synchrotron (Helmholtz Center Berlin) is greatly acknowledged. M.J. discloses support for the research of this work from Germany’s Excellence Strategy UniSysCat. Y.W. discloses support for the research of this work from the National Natural Science Foundation of China [nos. 22373053 and 42388101]. R.G.S. discloses support for the research of this work from Labex ARCANE [ANR-17-EURE-0003]. W.N. discloses support for the research and publication of this work from NRF of Korea [RS-2021-NR059914, RS-2023-NR121124 and RS-2025-02382972], Henan Center for Outstanding Overseas Scientists [GZS2024020], Einstein Foundation Berlin (EVF-NAM) and Alexander von Humboldt (AvH) foundation. K.R. thanks the Einstein Foundation Berlin for the Einstein Professorship. S.M., M.H., S.K., P.H., declare no relevant funding. We acknowledge support by the Open Access Publication Fund of Humboldt-Universität zu Berlin.

Author contributions

M.J. designed and performed the majority of the experiments, analyzed the data and wrote the original manuscript draft. K.R., W.N. conceived and supervised the project. S.M., M.H. performed and analyzed the XANES, EXAFS, and NRVS experiments. S.K., P.H. assisted with resonance Raman data analysis. R.G.S. carried out the magnetic Mössbauer data analysis. Y.W. performed the computational studies. M.J., K.R., W.N., P.H., M.H., R.G.S., and Y.W. contributed to writing and editing the manuscript. All authors contributed to data analysis and discussion of the results.

Peer review

Peer review information

Nature Communications thanks Takahiko Kojima and the other anonymous reviewer(s) for their contribution to the peer review of this work. A peer review file is available.

Funding

Open Access funding enabled and organized by Projekt DEAL.

Data availability

The authors declare that the data supporting the findings of this study are available within the paper and its Supplementary Information files. Should any raw data files be needed in another format, they are available from the corresponding author upon request. The optimized Cartesian coordinates generated in this study are provided in the Source data file. The X-ray crystallographic coordinates for structures reported in this study have been deposited at the Cambridge Crystallographic Data Centre (CCDC), under deposition numbers 2477483 (1) and 2477484 (Zn-Br). These data can be obtained free of charge from The Cambridge Crystallographic Data Centre via www.ccdc.cam.ac.uk/data_request/cif. Source data are provided with this paper.

Competing interests

The authors declare no competing interests.

Footnotes

Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Contributor Information

Wonwoo Nam, Email: wwnam@ewha.ac.kr.

Kallol Ray, Email: kallol.ray@chemie.hu-berlin.de.

Supplementary information

The online version contains Supplementary material available at 10.1038/s41467-026-72599-y.

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Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Supplementary Materials

Source Data (69.9KB, xlsx)

Data Availability Statement

The authors declare that the data supporting the findings of this study are available within the paper and its Supplementary Information files. Should any raw data files be needed in another format, they are available from the corresponding author upon request. The optimized Cartesian coordinates generated in this study are provided in the Source data file. The X-ray crystallographic coordinates for structures reported in this study have been deposited at the Cambridge Crystallographic Data Centre (CCDC), under deposition numbers 2477483 (1) and 2477484 (Zn-Br). These data can be obtained free of charge from The Cambridge Crystallographic Data Centre via www.ccdc.cam.ac.uk/data_request/cif. Source data are provided with this paper.


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