Dioxygen Activation in Soluble Methane Monooxygenase

• Published in: Accounts of chemical research 2011-04, Vol.44 (4), p.280-288
• Main Authors: Tinberg, Christine E, Lippard, Stephen J
• Format: Article
• Language: English
• Subjects: Humans; Iron - chemistry; Iron - metabolism; Oxygen - metabolism; Oxygenases - chemistry; Oxygenases - metabolism; Protons; Solubility
• ISSN: 0001-4842; 1520-4898
• DOI: 10.1021/ar1001473

The controlled oxidation of methane to methanol is a chemical transformation of great value, particularly in the pursuit of alternative fuels, but the reaction remains underutilized industrially because of inefficient and costly synthetic procedures. In contrast, methane monooxygenase enzymes (MMOs) from methanotrophic bacteria achieve this chemistry efficiently under ambient conditions. In this Account, we discuss the first observable step in the oxidation of methane at the carboxylate-bridged diiron active site of the soluble MMO (sMMO), namely, the reductive activation of atmospheric O2. The results provide benchmarks against which the dioxygen activation mechanisms of other bacterial multicomponent monooxygenases can be measured. Molecular oxygen reacts rapidly with the reduced diiron(II) cen-ter of the hydroxylase component of sMMO (MMOH). The first spectroscopically characterized intermediate that results from this process is a peroxodiiron(III) species, P*, in which the iron atoms have identical environments. P* converts to a second peroxodiiron(III) unit, Hperoxo, in a process accompanied by the transfer of a proton, probably with the assistance of a residue near the active site. Proton-promoted O−O bond scission and rearrangement of the diiron core then leads to a diiron(IV) unit, termed Q, that is directly responsible for the oxidation of methane to methanol. In one section of this Account, we provide a detailed discussion of these processes, with particular emphasis on possible structures of the intermediates. The geometries of P* and Hperoxo are currently unknown, and recent synthetic modeling chemistry has highlighted the need for further structural characterization of Q, currently assigned as a di(μ-oxo)diiron(IV) “diamond core.” In another section of the Account, we discuss in detail proton transfer during the O2 activation events. The role of protons in promoting O−O bond cleavage, thereby initiating the conversion of Hperoxo to Q, was previously a controversial topic. Recent studies of the mechanism, covering a range of pH values and in D2O instead of H2O, confirmed conclusively that the transfer of protons, possibly at or near the active site, is necessary for both P*-to-Hperoxo and Hperoxo-to-Q conversions. Specific mechanistic insights into these processes are provided. In the final section of the Account, we present our view of experiments that need to be done to further define crucial aspects of sMMO chemistry. Here our goal is to det