Ethan A Hill1, Andrew C Weitz2, Elizabeth Onderko3, Adrian Romero-Rivera4, Yisong Guo2, Marcel Swart4,5, Emile L Bominaar2, Michael T Green1,3, Michael P Hendrich2, David C Lacy1, A S Borovik1. 1. Department of Chemistry, University of California , Irvine, California 92697, United States. 2. Department of Chemistry, Carnegie Mellon University , Pittsburgh, Pennsylvania 15213, United States. 3. Department of Chemistry, Pennsylvania State University , University Park, Pennsylvania 16802, United States. 4. Institut de Química Computacional i Catàlisi and Departament de Química, Universitat de Girona , 17003 Girona, Spain. 5. ICREA , Pg. Lluís Companys 23, 08010 Barcelona, Spain.
Abstract
High-valent Fe-OH species are often invoked as key intermediates but have only been observed in Compound II of cytochrome P450s. To further address the properties of non-heme FeIV-OH complexes, we demonstrate the reversible protonation of a synthetic FeIV-oxo species containing a tris-urea tripodal ligand. The same protonated FeIV-oxo species can be prepared via oxidation, suggesting that a putative FeV-oxo species was initially generated. Computational, Mössbauer, XAS, and NRVS studies indicate that protonation of the FeIV-oxo complex most likely occurs on the tripodal ligand, which undergoes a structural change that results in the formation of a new intramolecular H-bond with the oxido ligand that aids in stabilizing the protonated adduct. We suggest that similar protonated high-valent Fe-oxo species may occur in the active sites of proteins. This finding further argues for caution when assigning unverified high-valent Fe-OH species to mechanisms.
High-valent Fe-OH species are often invoked as key intermediates but have only been observed in Compound II of cytochrome P450s. To further address the properties of non-n class="Chemical">hemeFeIV-OH complexes, we demonstrate the reversible protonation of a synthetic FeIV-oxo species containing a tris-urea tripodal ligand. The same protonated FeIV-oxo species can be prepared via oxidation, suggesting that a putative FeV-oxo species was initially generated. Computational, Mössbauer, XAS, and NRVS studies indicate that protonation of the FeIV-oxo complex most likely occurs on the tripodal ligand, which undergoes a structural change that results in the formation of a new intramolecular H-bond with the oxido ligand that aids in stabilizing the protonated adduct. We suggest that similar protonated high-valent Fe-oxo species may occur in the active sites of proteins. This finding further argues for caution when assigning unverified high-valent Fe-OH species to mechanisms.
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