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Science 24 January 1997:
Vol. 275. no. 5299, pp. 515 - 518
DOI: 10.1126/science.275.5299.515

Reports

An Fe2IVO2 Diamond Core Structure for the Key Intermediate Q of Methane Monooxygenase

Lijin Shu, Jeremy C. Nesheim, Karl Kauffmann, Eckard Münck, John D. Lipscomb, Lawrence Que Jr. *

A new paradigm for oxygen activation is required for enzymes such as methane monooxygenase (MMO), for which catalysis depends on a nonheme diiron center instead of the more familiar Fe-porphyrin cofactor. On the basis of precedents from synthetic diiron complexes, a high-valent Fe2(µ-O)2 diamond core has been proposed as the key oxidizing species for MMO and other nonheme diiron enzymes such as ribonucleotide reductase and fatty acid desaturase. The presence of a single short Fe-O bond (1.77 angstroms) per Fe atom and an Fe-Fe distance of 2.46 angstroms in MMO reaction intermediate Q, obtained from extended x-ray absorption fine structure and Mössbauer analysis, provides spectroscopic evidence that the diiron center in Q has an Fe2IVO2 diamond core.

L. Shu and L. Que Jr., Department of Chemistry and Center for Metals in Biocatalysis, University of Minnesota, Minneapolis, MN 55455, USA.
J. C. Nesheim and J. D. Lipscomb, Department of Biochemistry, Medical School, and Center for Metals in Biocatalysis, University of Minnesota, Minneapolis, MN 55455, USA.
K. Kauffmann and E. Münck, Department of Chemistry, Carnegie Mellon University, Pittsburgh, PA 15213, USA.
*   To whom correspondence should be addressed. E-mail: QUE{at}chem.umn.edu


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