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O 2 Activation by Non-Heme Thiolate-Based Dinuclear Fe Complexes

Iron centers featuring thiolates in their metal coordination sphere (as ligands or substrates) are well-known to activate dioxygen. Both heme and non-heme centers that contain iron-thiolate bonds are found in nature. Investigating the ability of iron-thiolate model complexes to activate O is expecte...

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Bibliographic Details
Published in:Inorganic chemistry 2020-03, Vol.59 (5), p.3249-3259
Main Authors: Wang, Lianke, Gennari, Marcello, Cantú Reinhard, Fabián G, Padamati, Sandeep K, Philouze, Christian, Flot, David, Demeshko, Serhiy, Browne, Wesley R, Meyer, Franc, de Visser, Sam P, Duboc, Carole
Format: Article
Language:English
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Summary:Iron centers featuring thiolates in their metal coordination sphere (as ligands or substrates) are well-known to activate dioxygen. Both heme and non-heme centers that contain iron-thiolate bonds are found in nature. Investigating the ability of iron-thiolate model complexes to activate O is expected to improve the understanding of the key factors that direct reactivity to either iron or sulfur. We report here the structural and redox properties of a thiolate-based dinuclear Fe complex, [Fe (LS) ] (LS = 2,2'-(2,2'-bipyridine-6,6'-iyl)bis(1,1-diphenylethanethiolate)), and its reactivity with dioxygen, in comparison with its previously reported protonated counterpart, [Fe (LS)(LSH)] . When reaction with O occurs in the absence of protons or in the presence of 1 equiv of proton (i.e., from [Fe (LS)(LSH)] ), unsupported μ-oxo or μ-hydroxo Fe dinuclear complexes ([Fe (LS) O] and [Fe (LS) (OH)] , respectively) are generated. [Fe (LS) O], reported previously but isolated here for the first time from O activation, is characterized by single crystal X-ray diffraction and Mössbauer, resonance Raman, and NMR spectroscopies. The addition of protons leads to the release of water and the generation of a mixture of two Fe-based "oxygen-free" species. Density functional theory calculations provide insight into the formation of the μ-oxo or μ-hydroxo Fe dimers, suggesting that a dinuclear μ-peroxo Fe intermediate is key to reactivity, and the structure of which changes as a function of protonation state. Compared to previously reported Mn-thiolate analogues, the evolution of the peroxo intermediates to the final products is different and involves a comproportionation vs a dismutation process for the Mn and Fe derivate, respectively.
ISSN:0020-1669
1520-510X
DOI:10.1021/acs.inorgchem.9b03633