Reversible Cleavage and Formation of the Dioxygen O-O Bond Within a Dicopper Complex

A key step in dioxygen evolution during photosynthesis is the oxidative generation of the O-O bond from water by a manganese cluster consisting of M$_2$(μ-O)$_2$ units (where M is manganese). The reverse reaction, reductive cleavage of the dioxygen O-O bond, is performed at a variety of dicoipper an...

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Published inScience (American Association for the Advancement of Science) Vol. 271; no. 5254; pp. 1397 - 1400
Main Authors Halfen, Jason A., Mahapatra, Samiran, Wilkinson, Elizabeth C., Kaderli, Susan, Young, Victor G., Que, Lawrence, Zuberbühler, Andreas D., Tolman, William B.
Format Journal Article
LanguageEnglish
Published Washington, DC American Society for the Advancement of Science 08.03.1996
American Association for the Advancement of Science
The American Association for the Advancement of Science
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Summary:A key step in dioxygen evolution during photosynthesis is the oxidative generation of the O-O bond from water by a manganese cluster consisting of M$_2$(μ-O)$_2$ units (where M is manganese). The reverse reaction, reductive cleavage of the dioxygen O-O bond, is performed at a variety of dicoipper and di-iron active sites in enzymes that catalyze important organic oxidations. Both processes can be envisioned to involve the interconversion of dimetal-dioxygen adducts, M$_2$(O$_2$), and isomers having M$_2$(μ-O)$_2$ cores. The viability of this notion has been demonstrated by the identification of an equilibrium between synthetic complexes having [Cu$_2$($\mu - \eta^2$: $\eta^2 -O_2$)]$^{2+}$ and [cu$_2$(μ-O)$_2$]$^{2+}$ cores through kinetic, spectroscopic, and crystallographic studies.
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ISSN:0036-8075
1095-9203
DOI:10.1126/science.271.5254.1397