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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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Bibliographic Details
Published in:Science (American Association for the Advancement of Science) 1996-03, Vol.271 (5254), p.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: Article
Language:English
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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.
ISSN:0036-8075
1095-9203
DOI:10.1126/science.271.5254.1397