Spectroscopic and Theoretical Investigation of a Complex with an [O═FeIV–O–FeIV═O] Core Related to Methane Monooxygenase Intermediate Q
Author:
Affiliation:
1. Department of Chemistry, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States
2. Department of Chemistry and Center for Metals in Biocatalysis, University of Minnesota, Minneapolis, Minnesota 55455, United States
Funder
National Science Foundation
National Institutes of Health
Publisher
American Chemical Society (ACS)
Subject
Colloid and Surface Chemistry,Biochemistry,General Chemistry,Catalysis
Link
https://pubs.acs.org/doi/pdf/10.1021/ja411376u
Reference58 articles.
1. A transient intermediate of the methane monooxygenase catalytic cycle containing an FeIVFeIV cluster
2. Kinetic and spectroscopic characterization of intermediates and component interactions in reactions of methane monooxygenase from Methylococcus capsulatus (Bath)
3. An Fe 2 IV O 2 Diamond Core Structure for the Key Intermediate Q of Methane Monooxygenase
4. Reconsideration of X, the Diiron Intermediate Formed during Cofactor Assembly in E. coli Ribonucleotide Reductase
5. The First Direct Characterization of a High-Valent Iron Intermediate in the Reaction of an α-Ketoglutarate-Dependent Dioxygenase: A High-Spin Fe(IV) Complex in Taurine/α-Ketoglutarate Dioxygenase (TauD) from Escherichia coli
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