O2 Evolution from the Manganese−Oxo Cubane Core Mn4O46+: A Molecular Mimic of the Photosynthetic Water Oxidation Enzyme?

Abstract

Photosynthesis produces molecular oxygen from water catalyzed by an enzyme whose active site contains a tetramanganese−oxo core of incompletely established structure. The first functional mimic of this core has been synthesized containing a cubical [Mn 4 O 4 ] n + core, surrounded by six facially bridging bidentate chelates to the manganese ions ((dpp) 6 Mn 4 O 4 ( 1 ); dpp - = diphenylphosphinate anion). Bond enthalpy data predict that the Mn 4 O 4 6+ core is thermodynamically capable of releasing molecular O 2, but is kinetically prevented from doing so by an activation barrier. UV light absorption into a Mn−O charge-transfer excited state (but not excitation of a Mn ligand-field excited state) efficiently releases an O 2 molecule if performed in the gas phase and concomitantly releases a bridging dpp - anion and the cationic species (dpp) 5 Mn 4 O 2 + (presumed Mn 4 O 2 -butterfly core type). All species were identified by high resolution mass spectrometry. This reaction proceeds with high quantum efficiency (>50%) and is the only observable reaction channel. The O 2 product derived exclusively from the corner oxo's of the cube based on photochemistry of the 18 O-isotopomer, ((dpp) 6 Mn 4 ( 18 O) 4 . Neither O 2 release nor dpp - dissociation are observed individually to occur in the excited state, indicating that O−O bond formation and O 2 release require dissociation of one of the six dpp - chelates (“Jack-in-the-Box” mechanism for O 2 formation). By contrast, neither O 2 production nor chelate photodissociation are observed in condensed phases, presumably due to either quenching of the photoexcited state or rapid recombination of dpp - and (dpp) 5 Mn 4 O 4 + in the solvent cage. Previous results show that chemical reduction of ( 1 ) in solution using hydrogen atom donors produces the deoxygenated (dpp) 6 Mn 4 O 2 core and releases two water molecules as the only products. Thus the [Mn 4 O 4 ] n + cubane core is an intrinsically reactive core topology that facilitates both the selective chemical reduction of two of the four oxygen atom bridges to water molecules and their photorearrangement to an O 2 molecule under the control of chelation of the manganese ions by dpp - . These results may offer insight into the possible nature of the photosynthetic O 2 -evolving mechanism.