C O M M U N I C A T I O N S
2 was converted to 3 by addition of benzoyl chloride (data not
shown). It has been well-documented that the reactions of metal-
peroxo species, including Mn(III)-peroxo porphyrins, with benzoyl
chloride lead to formation of their corresponding high-valent metal-
oxo species.11 However, the O-O bond cleavage mechanism of
the putative Mn(IV)-OOH intermediate is not yet clear at this
moment (see Scheme 2 for O-O bond homolysis vs heterolysis).
Nevertheless, to our knowledge, this is the first demonstration of
the analogous conversion of a Mn-peroxo corrole to a Mn-oxo
corrole upon protonation.
Scheme 2. Proposed Mechanisms of O-O Bond Cleavage and
Formation between Mn-Peroxo and -Oxo Corroles
Figure 2. (a) ESI MS spectrum of 2. Inset shows isotope distribution
patterns for 2-16O (left) and 2-18O (right). The mass peaks at m/z 1017.1
and 1048.1 correspond to [Mn(TFMPC)(CH3O)]- and [Mn(TFMPC)-
(CH3O)2]-, respectively. (b) EPR spectrum of 2. Inset shows a parallel mode
X-Band CW-EPR spectrum of the starting MnIII(TFMPC) complex. Also,
see SI, Figure S4.
We then synthesized a Mn(V)-oxo corrole complex, 3, by
reacting 1 with 2.0 equiv of iodosylbenzene (PhIO) in CH3CN at
10 °C (Scheme 1, reaction B; Figure 1 and SI, Figure S5 for
UV-vis spectral changes).8 The ESI MS of 3 exhibited a prominent
ion peak at m/z 1002.1, whose mass and isotope distribution pattern
corresponds to Mn(TFMPC)(O) (calculated m/z 1002.1; Figure 3a).
When 3 was prepared with isotopically labeled PhI18O in the
presence of H218O, a mass peak corresponding to Mn(TFMPC)(18O)
appeared at m/z 1004.2 (calculated m/z 1004.1; Figure 3a, inset). 3
is EPR silent (SI, Figure S4), suggesting a diamagnetic d2 (S ) 0)
species as has been reported for other Mn(V)-oxo corrole and
corrolazine complexes.8,9 The resonance Raman spectrum of 3,
measured in CH3CN at -40 °C with 442-nm laser excitation,
displays an isotope sensitive band at 957 cm-1, which shifts to 920
cm-1 upon introduction of 18O (Figure 3b). The observed isotopic
shift of -37 cm-1 with 18O substitution is in close agreement with
the value calculated for a Mn-O diatomic oscillator (-42 cm-1).
The calculated force constant for the 957 cm-1 mode by a simple
Hook’s law is 6.7 mdyne/Å, which is consistent with triply bonded
Mn-O bonds in Mn(V)-oxo complexes.8c,9,10 Taken together, the
spectroscopic data demonstrate that 3 is a Mn(V)-oxo corrole with
a Mn-O triple bond, MnV(O)(TFMPC).
In the O-O bond formation reaction, addition of base to the
Mn(V)-oxo complex, 3, produced the Mn(IV)-peroxo complex, 2,
quantitatively (Scheme 1, reaction D; Figure 1). The formation of
2 was further confirmed by taking EPR and ESI MS of the resulting
solution; a broad signal at g ≈ 4 was observed in the EPR spectrum
(SI, Figure S4). In ESI MS experiments, 2 prepared in the reaction
of Mn(V)16O and 16OH- contained an 16O16O group (SI, Figure
S6). Similarly, 2 prepared in the reaction of Mn(V)18O and 16OH-
contained an 18O16O group (SI, Figure S6). These results demon-
strate that the peroxo ligand in 2 was generated by the O-O bond
formation between the Mn-oxo moiety in 3 and the hydroxide ion,
followed by a deprotonation of a hydroperoxo ligand by another
hydroxide ion (Scheme 2).4,12 However, there is an electron missing
in the proposed mechanism, and this is probably due to a greater
stability of a Mn(IV)-peroxo corrole species under the reaction
conditions.
Remarkably, a reversible conversion between the Mn(IV)-peroxo
and Mn(V)-oxo corroles was observed upon addition of acid and
base (Scheme 1, reactions C and D); this reversible cycle could be
repeated several times without showing a significant decrease of
the absorption bands corresponding to the products. First, the
Mn(IV)-peroxo complex, 2, was converted to the Mn(V)-oxo
complex, 3, upon addition of HClO4 (Scheme 1, reaction C); the
full formation of 3 was confirmed by the UV-vis and EPR spectra
of the resulting solution (Figure 1 and SI, Figure S4). In addition,
In conclusion, we have synthesized and characterized new
Mn(IV)-peroxo and Mn(V)-oxo corroles and used them in O-O
bond cleavage and formation reactions. We have also shown the
first example of reversible O-O bond cleavage and formation
between high-valent metal-oxo and metal-peroxo species. Future
studies will be focused on understanding mechanistic aspects
involved in the O-O bond cleavage and formation processes.
Acknowledgment. The research was supported by KOSEF/
MEST of Korea through the CRI, WCU (R31-2008-000-10010-
0), and GRL (2010-00353) Programs (to W.N. and J.S.V.), Grant-
in-Aid for scientific research (C) (No. 21570171) and Priority Area
(No. 477) (KAKENHI) and GCOE program (Picobiology) by
MEXT, Japan (to T.O.), and Polish Ministry of Science and Higher
Education (Contract 50611) (to D.T.G.).
Supporting Information Available: Experimental details and
Figures S1-S6. This material is available free of charge via the Internet
References
(1) Nam, W. Acc. Chem. Res. 2007, 40, 465. and review articles in the special
issue.
(2) (a) Groves, J. T. In Cytochrome P450: Structure, Mechanism, and
Biochemistry; Ortiz de Montellano, P. R., Ed.; Kluwer Academic/Plenum
Publishers: New York, 2005; pp 1-43. (b) Wertz, D. L.; Valentine, J. S.
Struct. Bonding (Berlin) 2000, 97, 37–60. (c) Shaik, S.; Kumar, D.; de
Figure 3. (a) ESI MS spectrum of the complex 3. Inset shows isotope
distribution patterns prepared with PhI16O (left) and PhI18O (right). (b)
Resonance Raman spectra of 3 prepared with PhI16O (black line) and PhI18O
(red line), and the difference spectrum of 3-16O-3-18O (blue line). The peaks
marked with * are from solvent.
9
J. AM. CHEM. SOC. VOL. 132, NO. 40, 2010 14031