Sana
Karbalaei
a,
Alicja
Franke
b,
Julian
Oppelt
b,
Tarfi
Aziz
a,
Aubree
Jordan
a,
P. Raj
Pokkuluri
a,
Dean D.
Schwartz
c,
Ivana
Ivanović-Burmazović
*b and
Christian R.
Goldsmith
*a
aDepartment of Chemistry and Biochemistry, Auburn University, Auburn, AL 36849, USA. E-mail: crgoldsmith@auburn.edu
bDepartment of Chemistry, Ludwig-Maximilians-Universität München, 81377 München, Germany. E-mail: ivana.ivanovic-burmazovic@cup.uni-muenchen.de
cDepartment of Anatomy, Physiology, and Pharmacology, College of Veterinary Medicine, Auburn University, Auburn, AL 36849, USA
First published on 5th September 2023
Previously, we found that linear quinol-containing ligands could allow manganese complexes to act as functional mimics of superoxide dismutase (SOD). The redox activity of the quinol enables even Zn(II) complexes with these ligands to catalyze superoxide degradation. As we were investigating the abilities of manganese and iron complexes with 1,8-bis(2,5-dihydroxybenzyl)-1,4,8,11-tetraazacyclotetradecane (H4qp4) to act as redox-responsive contrast agents for magnetic resonance imaging (MRI), we found evidence that they could also catalyze the dismutation of H2O2. Here, we investigate the antioxidant behavior of Mn(II), Fe(II), and Zn(II) complexes with H4qp4. Although the H4qp4 complexes are relatively poor mimetics of SOD, with only the manganese complex displaying above-baseline catalysis, all three display extremely potent catalase activity. The ability of the Zn(II) complex to catalyze the degradation of H2O2 demonstrates that the use of a redox-active ligand can enable redox-inactive metals to catalyze the decomposition of reactive oxygen species (ROS) besides superoxide. The results also demonstrate that the ligand framework can tune antioxidant activity towards specific ROS.
In previous work from our laboratories, we found that linear polydentate ligands with 1,4-hydroquinone (quinol) groups could be used as the organic components in a variety of SOD mimics (Scheme 1).6–10 A manganese complex with H2qp1 displayed activity that was comparable to those of the most effective SOD mimetics reported to date: manganese complexes with pentaazamacrocycle and cationic porphyrin ligands.11–14 The redox activity of the quinol group enables it to act as the redox partner for O2˙− and can allow SOD mimicry even without a redox-active metal. Although the ligands by themselves are inactive, the Zn(II) complexes with H2qp1 and H4qp2 are functional SOD mimics, with the latter ligand resulting in higher activity.9,10
More recent work has focused on the macrocyclic ligand 1,8-bis(2,5-dihydroxybenzyl)-1,4,8,11-tetraazacyclotetradecane (H4qp4, Scheme 2).15,16 Our initial interest in this molecule was as a component in highly water-stable magnetic resonance imaging (MRI) contrast agent sensors for H2O2. When the quinols are oxidized to para-quinones, water molecules displace these groups, increasing the T1-weighted relaxivity (r1) of its Mn(II) complex, [MnII(H3qp4)](OTf) (1).15 Although quinol oxidation and an accompanying enhancement in r1 also occur when the Fe(II) complex, [FeII(H3qp4)](OTf) (2), reacts with H2O2, it is instead metal oxidation that is primarily responsible for the increase in relaxivity.16 For both 1 and 2, we found that the oxidation of the quinols and the accompanying activation of the sensor occur more slowly in higher concentrations of H2O2.15,16 This led us to speculate that the initial reactions with H2O2 may be generating a higher-valent metal species that can either react intramolecularly to oxidize the ligand or intermolecularly with a second equiv. of H2O2 (Scheme 3).15 The intermolecular activity depletes H2O2, thereby mimicking catalase. The intramolecular reaction was proposed to be inherently slower, only proceeding to a noticeable extent after the [H2O2] decreases enough to make the intermolecular reaction less competitive.
Scheme 3 Previously proposed mechanism for competing H2O2 degradation (blue) and quinol oxidation (red). The above graphic was slightly modified from one that originally appeared in ref. 15. |
Replicating the activity of catalase enzymes has proven to be challenging, and the best small molecule mimics reported thus far have displayed modest reactivity with H2O2. Two metrics are commonly used to assess catalysis: the rate constant for the reaction between H2O2 and the antioxidant and the turnover number (TON).17–27 Comparisons are often difficult to make since the reaction conditions and protocols can vary considerably. The highest rate constant for H2O2 degradation corresponded to a second-order reaction with an Fe(III) complex with a fluorinated corrole (k2 = 4300 M−1 s−1 in 37 °C pH 7.4 phosphate buffer).27 The highest TON corresponded to a manganese porphyrin complex (TON = 12.54 in 25 °C pH 7.8 Tris buffer).22
In the present manuscript, we thoroughly investigate the abilities of the Mn(II) and Fe(II) complexes with H4qp4 to mimic both SOD and catalase. We also prepare and evaluate the antioxidant properties of a Zn(II) complex with H4qp4: [ZnII(H3qp4)](OTf) (3). We find that although the SOD activities are severely attenuated relative to those of complexes with linear quinol-containing ligands, all three H4qp4 complexes act as highly potent catalase mimics, with activities that greatly exceed those exhibited by most other reported small molecule mimics of these enzymes.17–27 The Zn(II) complex is further notable in that it represents the first instance, to the best of our knowledge, where a coordination complex with a redox-inactive metal ion successfully catalyzed the degradation of H2O2.
(1) |
The catalase activity was more stringently quantitated by polarographically following O2 production using a Clark-type O2 sensitive electrode (Hansatech Pentney, Norfolk, England). We first calibrated the system using a N2 saturated solution to establish a zero O2 level within the reaction chamber prior to experimental measurements. The initial series of reactions contained 1 nM of the tested antioxidant and were carried out at RT in solutions containing 50 mM tris(hydroxymethyl)aminomethane (Tris) buffered to pH 7.2. The buffer and solution containing the coordination complex were initially mixed in the reaction chamber for 20 s to establish a baseline, after which H2O2 was injected to initiate the evolution of O2.34 Subsequently, we measured the initial rates of reactions between 10 mM H2O2 and 1.0–100 nM of the catalysts to calculate k2 rate constants. The data were corrected to account for uncatalyzed H2O2 decomposition.
Peroxidase activity can also contribute to the degradation of H2O2, representing a means to consume H2O2 without generating O2. This potential reactivity was evaluated by monitoring the abilities of the antioxidants to promote the reaction between H2O2 and 2,2′-azinobis(3-ethylbenzothiazoline-6-sulfonate) (ABTS); this reaction generates the radical cation ABTS+ (ε417 = 34.7 mM−1 cm−1).35 One series of reactions were run in RT 50 mM acetate solution buffered to pH 5.0, with reaction concentrations of 10 mM ABTS, 0.1 mM coordination complex, and 1–500 mM H2O2. Another series of reactions were run in RT 50 mM acetate solution buffered to pH 5.0, with reaction concentrations of 10 mM H2O2, 0.1 mM coordination complex, and 1–500 mM ABTS. The conversion of ABTS to its radical cation was followed using a Shimadzu UV-1601 spectrophotometer (Columbia, MD). The following equation is used to convert the absorbance data into initial rates (vo/[M]T):
The redox capabilities of 3 were initially assessed using cyclic voltammetry (CV, Fig. S6†). In phosphate solution buffered to pH 7.2, we observe one irreversible redox event with an Epa = 225 mV and an Epc = −11 mV (vs. Ag/AgCl). This resembles irreversible CV features seen for both 1 and 2. The redox event for the Mn(II) complex has an Epa = 240 mV and an Epc = −20 mV;15 whereas, that for the Fe(II) compound has an Epa = 240 mV and an Epc = −60 mV. A smaller feature is observed with Epc = 5 mV; this may be attributable to acid/base behavior for either the quinol or the semiquinone. A similar feature was observed for 2.16
We crystallized 3 from MeOH/ether and structurally characterized the complex through single crystal X-ray diffraction (Fig. 1 and Table S1†). The H3qp3− ligand coordinates to the Zn(II) through five out of its six possible donor atoms, with the neutral quinol not directly binding to the metal center. The coordination geometry of the N4O donors around the Zn(II) is best described as a distorted trigonal bipyramidal, with a τ5 value of 0.70.36 The pendent quinol may hydrogen bond to the outer-sphere triflate; the distance between O(3) and O(6) is 2.72 Å.
Fig. 1 ORTEP representation of the structure of [ZnII(H3qp4)]+. The triflate counteranion and all H atoms are omitted for clarity. All ellipsoids are drawn at 50% probability. Full crystallographic data are provided in the ESI and in the Cambridge Structural Database (number 2173563†). |
The aforementioned assay is somewhat notorious for providing misleading results due to possible side reactions between its components.31,37–43 In the case of 4 and 5, the assay predicted similar activities, but later stopped-flow kinetics analysis of the direct reactions between the Mn(II) compounds and KO2 indicated that the H2qp1 complex was much more active than the H4qp2 complex in HEPES solutions.8 Further, both compounds had kcat values that were much lower than those predicted by the assay. Complexes 1, 2, and 3 were studied in 60 mM MOPS buffered to either pH 7.4 or pH 7.8 and 50 mM phosphate buffered to pH 7.4 (Table 1). The stopped-flow kinetics data indicate that 1 is significantly less active than either 4 or 5 in either a sulfonate-containing buffer or phosphate (Fig. S8†). As with 4 and many other manganese-containing SOD mimics studied by ourselves,8,31,44 complex 1 is less catalytically active in phosphate buffer. The iron and zinc complexes, 2 and 3, have no noticeable impact on the rate of decomposition of O2˙− when analyzed by stopped-flow kinetics. The free H4qp4 ligand is likewise inactive as a catalyst.
Buffer, pH | 1 | 2 | 3 | 4 | 5 |
---|---|---|---|---|---|
a Data from ref. 8; the first-row data for 4 and 5 were collected in HEPES, rather than MOPS. | |||||
60 mM MOPS/HEPES, 7.4 | 6.0 × 106 | N.A. | N.A. | 9.7 × 107 | 1.2 × 107 |
60 mM MOPS, 7.8 | 4.5 × 106 | N.A. | N.A. | N.D. | N.D. |
50 mM phosphate, 7.4 | 2.9 × 106 | N.A. | N.A. | 8.0 × 106 | 1.0 × 107 |
The obtained results further demonstrate that indirect assays often cannot even qualitatively distinguish between SOD active and inactive compounds. Instead of being more active than the SOD used as the positive control, 2 does not display any catalytic SOD activity at all and that for 1 is rather low (Table 1).
Although 3 is not an effective SOD mimic, it does react with KO2, as assessed by EPR, UV/vis, and MS analysis (Fig. S9–S11†). The EPR data show a weak signal at g = 2 at 30 s that completely disappears within 15 min. We do not believe that the EPR feature corresponds to residual O2˙− since the oxidant should be consumed to levels below the limit of EPR detection within 1 s, even in the absence of a catalyst.9 The g value of the signal and its short lifetime are consistent with organic radicals similar to what we observed for previous Zn(II)-quinoxyl radical species.9,10 A Zn(II)-semiquinone species observed with the H4qp2 ligand, for instance, persists to detectable levels for over 45 min.10 The UV/vis data indicate that the complex is initially deprotonated by KO2, which is a base as well as an oxidant, and then slowly oxidized to Zn(II)-para-quinone species over 90 s. The MS data indicate that the reaction with O2˙− degrades the complex (Fig. S11†). Although 3 does react with O2˙−, this activity is not enough to noticeably accelerate superoxide degradation beyond the rate observed for the uncatalyzed reaction.
The metal-free H4qp4 ligand was unable to catalyze the degradation of H2O2. Each coordination complex, conversely, catalyzes the decomposition of H2O2. In all three cases, the reactivity is consistent with Michaelis–Menten kinetics with clear saturation behavior observed at high concentrations of H2O2 (Fig. 3). Oxygraphic measurements confirm that O2 is being evolved; these data were fitted to the re-arranged Michaelis–Menten equation, which has parameters kcat and kcat/KM (Tables 2 and S3†). The iron complex 2 appears to be slightly more active than the other two, but the individual rate constants do not vary much within this series.
Fig. 3 Plots of vo/[M] vs. the concentration of H2O2, where [M] is the concentration of the tested H4qp4 complex: 1 (black), 2 (pink), 3 (green). The vo corresponds to the formation of O2, which was measured through oxygraphy. All reactions were performed in 25 °C 50 mM Tris buffered to pH 7.2. 1 nM of each coordination complex was present as a catalyst. Each shown data point is the average of at least five independent runs. Further details regarding the models used to fit the data can be found in Table S3.† |
Complex | k cat (s−1) | k cat/KM (M−1 s−1) | K M (M) | k 2 (M−1 s−1) | TON |
---|---|---|---|---|---|
1 (Mn) | 1.4 × 103 | 3.2 × 104 | 4.6 × 10−2 | 1.5 (±0.1) × 103 | 80 (±3) |
2 (Fe) | 2.2 × 103 | 5.2 × 104 | 4.2 × 10−2 | 2.2 (±0.1) × 103 | 130 (±1) |
3 (Zn) | 1.3 × 103 | 1.1 × 104 | 1.2 × 10−1 | 1.2 (±0.1) × 103 | 51 (±1) |
Full details regarding the models used to fit the data for the three compounds are provided in Table S3 in the ESI.† The listed errors represent one standard deviation.
Second-order rate constants (k2) were calculated by measuring the initial rates of O2 production via oxygraphy with catalyst concentrations ranging from 1.0 to 100 nM (Fig. 4). The k2 values are much lower than the kcat/KM values obtained from the Michaelis–Menten models but more accurately represent the activities of the catalysts.22 We also measured turnover numbers (TON) by quantifying the total O2 made over time (Fig. S12†). This parameter depends on both the robustness and activity of the catalyst and is arguably the most accurate measure of the practicality of a catalase mimic. Due to the high activity of the three complexes, we needed to perform these measurements with lower concentrations of the coordination complexes; otherwise, the O2 evolution is too fast to monitor via oxygraphy. Mahammed and Gross encountered similar issues in their studies of the Fe(III) complex with the fluorinated corrole.27 Although the conversions of H2O2 to O2 are relatively low for these measurements, the amount of generated O2 (A) still greatly exceeds that of the uncatalyzed reaction and (B) is highly replicable between experiments. We obtained similar TON and 10-fold greater conversions when the initial concentration of H2O2 was 1.0 mM rather than 10 mM (Fig. S12†). As assessed by both the initial rates analysis and the overall O2 production, 2 clearly outperforms its manganese and zinc analogs.
Fig. 4 Determination of k2 from plots of the initial rates (vo) vs. concentration of catalyst. All reactions were run at 25 °C in 50 mM Tris buffered to pH 7.2. The initial concentration of H2O2 was 10.0 mM for all reactions. The reaction was run at least three times at each catalyst concentration. The k2 values on Table 2 were calculated by dividing the slopes of the shown linear fits by the concentration of H2O2 (0.010 M) and multiplying by two to account for the reaction stoichiometry (2 equiv. of H2O2 are consumed per equiv. of O2 produced). (A) Data for 1. (B) Data for 2. (C) Data for 3. |
The activity was qualitatively confirmed with parallel experiments that monitored the disappearance of H2O2 (Fig. S13 and Table S4†). The rate constants from these experiments are much less reliable than those calculated from O2 production since all three complexes absorb strongly at the monitored 240 nm wavelength, and this technique generally tends to overestimate the activities of catalase mimics.22 Nonetheless, the activities of the complexes follow the same general order, with 2 and 3 being the most and least effective catalase mimics, respectively.
We further analyzed the reactions between H2O2 and the three H4qp4 complexes by EPR, with an emphasis on collecting data at an earlier time point that would coincide with higher catalase activity. EPR analysis suggests that some of the Mn(II) and Fe(II) in 1 and 2 has been oxidized 30 s after the reactions begin (Fig. S15†). With 1, the signal intensity for the Mn(II) decreases by approximately 10%. When 2 is oxidized by H2O2, a weak signal develops with g = 2.04, 1.99. Relative to the intensity of the Fe(III) end-products,16 approximately 25% of the iron has been oxidized to Fe(III) by 30 s. The Fe(III) feature is distinct from the high-spin Fe(III) product that was previously observed as the major end-product of the reaction16 and is instead consistent with a low-spin Fe(III) species. With 3, we observe a weak signal with g = 2. The intensity of the signal is barely above the noise level, however, and it is ambiguous whether this can be attributed to a species on the main catalytic cycle.
UV/vis analysis suggests that the quinols are oxidized during the reaction between 3 and H2O2 (Fig. 5). With an initial concentration of 0.6 mM H2O2, the 299 nm band attributable to the quinols almost completely vanishes by 15 min. The rate of quinol oxidation is approximately as fast as that observed for 1, which likewise lacks obfuscating charge transfer bands, under the same conditions.15 When the initial concentration of H2O2 is 10 mM, the rate of quinol oxidation slows relative to that seen at 0.6 mM H2O2, as was previously seen with 1 and 2.15,16 Such behavior is in agreement with the catalase activity of these complexes. An initially generated catalytically active species can either oxidize H2O2 or undergo self-oxidation (e.g. oxidation of the quinols, which is monitored in Fig. 5). Therefore, the more H2O2 that is initially present in the solution, the longer catalytic H2O2 decomposition proceeds and the longer the quinol groups of the ligand remain in their original reduced states. This explains why the quinols are oxidized more slowly with 10 mM H2O2. When there is a lower concentration of H2O2, the initially generated active species does not have enough substrate (H2O2) with which to react and more readily attacks the quinol moieties of the ligand, thereby resulting in faster ligand oxidation shown in Fig. 5.
With an initial concentration of 10 mM H2O2, however, the quinols in 3 oxidize much more quickly than those in 1 under the same conditions. The quinols in 3 appear to be almost entirely consumed by 30 min; whereas, ligand oxidation does not occur to a noticeable extent for 1 by 30 min. The results suggest that the redox-active ligand is more heavily involved in H2O2 degradation for 3 than it is for 1. Since 3 has lower catalase activity than 1, it is more susceptible to degradation than the more active 1 in the presence of the same concentration of H2O2.
We reacted each H4qp4 complex with equimolar amounts of H2O2 in attempts to identify intermediates that might precede quinol oxidation by UV/vis (e.g. M–OOH species). In each case, however, the quinol oxidation occurs immediately, and no new features were observed (Fig. S16†). The final spectra for 1 and 2 resemble those observed for the end-products of previous reactions with large excesses of the terminal oxidant.15,16
MS studies of reactions between 10 mM H2O2 and the H4qp4 complexes in MeCN further suggest that ligand-derived redox is more prevalent for 3 than it is for the two H4qp4 complexes with redox-active metals. The data for 1 and 2 at 30 s look identical to those in solutions that lack H2O2;15,16 the major m/z peaks are consistent with [MnIII(H2qp4)]+ and [FeIII(H2qp4)]+, respectively (Fig. S17 and S18†). Without H2O2, the Mn(II) and Fe(II) appear to oxidize spontaneously under MS ionizing conditions. The data are inconsistent with M(II) or M(III) complexes with oxidized forms of the ligand, leading us to conclude that the ligand exists as the doubly deprotonated H2qp42− rather than the monoquinol/mono-para-quinone H2qp4. When we react 3 and 10 mM H2O2, however, we observe a much different set of m/z peaks that are consistent with ligand oxidation (Fig. S19 and S20†). Specifically, we detect a m/z peak at 505.1790 at 30 s that is consistent with a Zn(II) complex with the monoquinolate/mono-para-quinone form of the ligand (calculated m/z = 505.1794). Further, we observe peaks that are consistent with the addition of one oxygen atom to the mono-para-quinone complex ([Zn(Hqp4 + O)]+) with m/z = 521.1736 (calculated m/z = 521.1743) and with the addition of two oxygen atoms to the diquinol complex ([Zn(H3qp4 + 2O)]+) with m/z = 539.1395 (calculated m/z = 539.1848). After 60 s, oxygenated products appear to become more prominent (Fig. S21†). We analyzed longer-term reactions between 1 and 2 with larger excess of H2O2 and likewise found evidence of ligand oxidation beyond the quinol-to-para-quinone conversion. With 1, we detect m/z peaks consistent with the loss of quinol groups (Fig. S22†). With 2, new m/z peaks are observed, but these are more difficult to assign to specific oxidation products (Fig. S23†).
Given that other quinol-containing ligands had been found to allow the redox-inactive metal ion Zn(II) to catalyze the dismutation of superoxide,9,10 we also prepared and tested the reactivity of a Zn(II) complex with H4qp4, [ZnII(H3qp4)](OTf) (3). The synthesis of the Zn(II) complex was identical in most aspects to those used to prepare both 1 and 2, and as with these syntheses, a complex with singly deprotonated ligand (H3qp4−) was the isolated product.15,16 Unlike the manganese and iron systems, we were able to obtain a crystal structure for the divalent metal. The H3qp4− ligand does not fully coordinate to the metal center (Fig. 1), which may suggest that the Zn(II) is too small to be fully accommodated by the ligand pocket. Only one of the quinols is coordinated in the crystal structure, and it appears that it remains unassociated with the metal center in aqueous solution since the second measured pKa of 9.71 is only slightly lower than the value of ∼10 expected for a non-coordinated quinol. Nonetheless, the Zn(II) complex with the H3qp4− form of the ligand is highly stable in water like 1 and 2; the analogous logKML values for Mn(II) and Fe(II) are 18.22 and 27.16, respectively.15,16
Given that manganese and zinc complexes with other quinol-containing ligands were found to act as functional mimics of superoxide dismutase (SOD),8–10 we initially assessed the abilities of the three complexes to catalyze the degradation of O2˙−. We screened 1, 2, and 3 using the xanthine oxidase/hypoxanthine/lucigenin assay (Fig. 2).28,29 Although the assay suggests that 1 and 2 are potent antioxidants, subsequent stopped-flow analysis of the direct reactions between KO2 and the complexes found that only the manganese complex 1 had a noticeable effect on O2˙− decomposition. The activity of 1 was generally inferior to those displayed by two manganese complexes that were previously reported by our lab groups: [MnII(H2qp1)(MeCN)](OTf)2 (4) and [MnII(H4qp2)Br2] (5, Scheme 1).8 As with many other manganese-containing SOD mimics studied by our groups, 1 is most effective as a catalyst in pH 7.4 solutions with sulfonate-based buffers (HEPES/MOPS) and becomes less active as the solution becomes more basic or the buffer switches to phosphate.31,45–51 In the presence of phosphate ions that can coordinate to the metal center, the reaction step involving O2˙− binding will compete with the rate-determining step that would be observed without phosphate. Superoxide coordination becomes the rate-determining step once the phosphate concentration exceeds a specific concentration.31
We determined that 1, 2, and 3 are all highly active catalase mimics using a Clark-type O2 sensitive electrode to follow O2 production polarographically (Fig. 3). This technique provides a more reliable measure of catalase activity than spectrophotometrically following H2O2 depletion. We measured second-order rate constants by assessing the initial rates of O2 production (Fig. 4) and determined overall turnover numbers (TON) by monitoring the reactions until completion. Of the three complexes, the iron-containing 2 is the most active, followed by 1, then 3. Given the magnitudes of these constants, care must be taken to ensure that these are calculated properly.19,25 Inspection of the plots from Fig. 3 shows that the rates per M of catalyst do indeed plateau at the kcat values. The k2 values of the three H4qp4 complexes might be exceeded only by an Fe(III) complex with a fluorinated corrole prepared by Mahammed and Gross.27 The reactivity between this compound and H2O2 follows second-order kinetics with a k2 = 4300 M−1 s−1 in 37 °C pH 7.4 phosphate buffer. The Fe(III)–corrole has a tendency to condense into a less active binuclear Fe(III) species; this process can be hindered by adding imidazole to the solution, increasing the k2 to 6400 M−1 s−1. Comparisons between Mahammed and Gross's results and ours, however, are obfuscated by the higher temperature at which they studied their catalase activity and by the fact that they had to follow the kinetics by UV/vis rather than oxygraphy. The TON of the H4qp4 complexes range from 51 (3) to 130 (2). These compare extremely well to TON values reported for other catalase mimics. In a recent review of catalase mimics, the best listed TON was 12.54, and we were unable to locate a higher value.22 Mahammed and Gross did not report a TON for their Fe(III)–corrole complex, but the overall O2 production appears to be severely limited by the formation of the binuclear ferric side-product, even when imidazole is present to hinder that particular reaction.27 Although the three reported metal complexes with H4qp4 are active CAT mimics, the free ligand is not; the coordinated metal ion is essential to the reactivity.
The high stabilities of the H4qp4 complexes in aqueous solutions contribute to their abilities to act as effective catalysts in water. In this, they resemble other CAT mimics with macrocyclic ligands, such as porphyrins and corroles.22,27 The activities of non-porphyrinic manganese-containing catalase mimics, conversely, are instead determined in MeCN.17–23
The activity of the Zn(II) complex is particularly notable in that all previously characterized systems capable of such catalysis contain a redox-active metal ion. Catalases themselves use either dinuclear manganese or heme groups in their active sites to degrade H2O2, and most small molecule functional mimics of these enzymes likewise contain either manganese or iron.17–23,26,27 Our results demonstrate that quinol complexes with redox-inactive metal ions can be used to catalyze the degradation of reactive oxygen species (ROS) other than O2˙−. The inability of 3 to act as an SOD mimic, however, shows that one cannot simply assume that SOD and catalase activities scale with each other for this class of antioxidants. In other words, one cannot expect that a strategy that leads to SOD mimicry will invariably also lead to catalase activity.
We also analyzed the capabilities of the complexes to act as peroxidase mimics using 2,2′-azinobis(3-ethylbenzothiazoline-6-sulfonate) (ABTS) as the substrate. We found that 1 and 2, but not 3, can catalyze the oxidation of ABTS to ABTS+ by H2O2. Enzymes that can perform both catalase and peroxidase activity have been proposed to go through a common intermediate, and the same could conceivably hold for 1 and 2. The reactivity of 3, however, is less straightforward, but it appears that whatever intermediates are generated from the reaction between the Zn(II) complex and H2O2 cannot be directed towards other substrates. With 1 and 2, the peroxidase activity is much slower than the catalase activity. This reaction selectivity is an attractive quality for a catalase mimic since competing in vivo peroxidase activity could potentially oxidize essential biomolecules as well as the catalysts themselves.
The relative lack of peroxidase activity should protect the three H4qp4 complexes from oxidative ligand degradation and may also contribute to their high catalase activity. Iron porphyrin and corrole mimics of catalase, conversely, more readily commonly undergo oxidative degradation,26 and the remarkable catalase activity exhibited by Mahammad and Gross's complex has been attributed to its ability to temporarily resist such decomposition.27 As mentioned above, the three H4qp4 complexes are also all highly water-stable, and metal ion dissociation from the ligand is negligible even under highly acidic conditions.15,16 This represents a substantial advantage over most manganese-containing catalase mimics.17–23 With these compounds, the aqueous stabilities have not been rigorously established, and the catalysis is studied in organic solvents instead of water.21,23–25 The abilities of the H4qp4 complexes to function in water would facilitate the application of either these complexes or more highly performing derivatives towards the clinical treatment of oxidative stress.
Despite the lesser peroxidase activities, complexes 1–3 do eventually degrade when exposed to exceedingly high concentrations of H2O2 (Fig. S21–S23†). This limits the TON, as evidenced by the low conversions (0.10–0.22%) observed in Fig. S12;† in these experiments, 0.1 μM of each complex reacts with 10 mM H2O2. In light of this result, we reviewed the conditions used to study the MRI properties of 1 and 2 and determined that the 0.1–1.0 mM concentrations for the MRI studies were sufficient to completely degrade the 10 mM of H2O2 used to activate the sensors.15,16 We will also note that we did not observe any ligand oxidation beyond the quinol-to-para-quinone conversion in these prior studies.
That 1, 2, and 3 catalyze H2O2 dismutation at similar rates led us to initially hypothesize that the three catalysts mainly rely on a common mechanistic cycle that does not feature redox at the metal center. EPR analysis of the reactions between H2O2 and 1 and 2 at 30 s, however, reveals that the metals in these complexes do noticeably oxidize, with the Mn(II) signal diminishing and a novel low-spin Fe(III) signal appearing, respectively. The low-spin Fe(III) signal seen for 2 could potentially correspond to an Fe(III)–OOH species,52 but other species could give rise to a similar signal. We attempted to determine whether any Fe(III)–OOH species were present using resonance Raman spectroscopy but were regrettably unable to locate any diagnostic O–O or Fe–O stretches. Our prior analysis of the reactions between H2O2 and 1 and 2 suggested that the quinols in the H4qp4 ligand do not start to convert to para-quinones until most of the H2O2 has been depleted.15,16 With a stoichiometric amount of H2O2, ligand oxidation occurs immediately for both 1 and 2 (Fig. S16†).
UV/vis and MS analysis of the reactions between 3 and H2O2, conversely, demonstrate that one of the quinols oxidizes to a para-quinone early in its reaction with a large excess of H2O2 (Fig. 5 and S19†). Additionally, we observe a m/z feature at 539.1396; the mass and charge are consistent with a Zn(II)–OOH complex with the mono-para-quinone form of the H4qp4 ligand, H2qp4. We caution that the data could also correspond to other species, such as a Zn(II)–OH complex with an oxygenated ligand and that we were likewise unsuccessful in our attempts to visualize a Zn(II)–OOH species with resonance Raman spectroscopy. The ambiguity in the MS data would not be resolvable by 18O-labeling studies. We do not observe any MS data consistent with a diquinone (qp4) species. Based on these results, we tentatively propose that the H2O2 dismutation for 3 proceeds through the cycle shown in Scheme 4. H2O2 reacts with [Zn(H3qp4)]+ to yield a M(II)–OOH species (B), with subsequent intramolecular oxidation of one of the quinols to a para-quinone (C). The coordination of H2O2 to Zn(II) has been previously observed,53 leading us to believe that Zn(II)–OOH species are indeed plausible intermediates. A second equiv. of H2O2 then coordinates the metal center as HOO−, generating [Zn(H2qp4)(OOH)]+ (D), which we may be detecting by MS. The para-quinone can then oxidize this second equiv. of H2O2. Since D appears to accumulate, this may be the rate-limiting step in the catalase activity. A previous report found that acids could catalyze the reduction of para-quinone to quinol,54 and the Zn(II) in 3 may do likewise in its capacity as a Lewis acid. The Zn(II) could either coordinate water and facilitate the delivery of protons to the para-quinone, or it could promote the reduction portion of the PCET by coordinating the para-quinone.
Redox-inactive metal ions, such as Al(III) and Ga(III), are capable of activating H2O2; in this chemistry, hydroxyl and hydroperoxyl radicals are released upon the coordination of multiple equiv. of the oxidant to the metal center.55–57 Given the observed Michaelis–Menten kinetics and lack of a second-order dependence of the rate on [H2O2], we do not believe that the simultaneous coordination of two equiv. of H2O2 is required for catalase activity to proceed. Further, the inability of 3 to oxidize external substrates such as ABTS is inconsistent with the release of highly oxidizing hydroxyl and hydroperoxyl radicals.
Since extensive ligand oxidation is not observed in the early stages of catalase activity, we propose that 1 and 2 mostly catalyze H2O2 dismutation through a fundamentally different mechanism (Scheme 5). The initial step corresponding to the coordination of H2O2 to the divalent metal ion remains the same, but once B is generated, the O–O bond may break heterolytically to yield a M(IV) species (C′). Such a high-valent species would stabilized by two factors: the presence of the anionic quinolate and the ability of the quinolate to donate an electron to the metal center to yield an isoelectronic M(III)-ligand radical. Species C′ can either react with a second equiv. of H2O2, removing two net hydrogen atoms to yield O2 and a M(II)–OH2 species (D′), or it can further oxidize the ligand to a para-quinone species (E). Although E is shown as a hydroxyl complex in Scheme 5, the OH group is basic enough to abstract a proton from the buffered medium, yielding the aquated species observed in our prior report on 1.15 The Fe(II) in 2 eventually is oxidized to Fe(III),16 and this may occur through a side reaction between Fe(II) species and 0.5 equiv. H2O2.
That 1 and 2 have higher TON than 3 likely results from improvements to both the speed and durability of the catalyst. The k2 rate constants for 1 and 2 are both higher than that of 3 (Table 2); this is consistent with the redox-active metals opening new pathways for H2O2 dismutation (Scheme 5). Catalysts 1 and 2 also appear to better resist over-oxidation. If external oxidants are initially channeled towards converting quinols to para-quinones, one would anticipate that catalysts that can avoid the full oxidation of the quinols (Scheme 5) would be less susceptible to alternative oxidation reactions, such as benzylic C–H activation, than catalysts that rely exclusively on the quinol/para-quinone redox couple (Scheme 4).
Footnote |
† Electronic supplementary information (ESI) available. CCDC 2173563. For ESI and crystallographic data in CIF or other electronic format see DOI: https://doi.org/10.1039/d3sc02398b |
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