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