We produce strong evidence of the interaction of ozone with a series o
f Manganese (III) porphyrinato complexes to form a well defined reacti
ve intermediate. In the latter species, the Manganese atom which is fo
rmally in a tetravalent (IV) state, is (at least) hexacoordinated with
the metal unambiguously lying in the basal plane of the four pyrrolic
nitrogens of the porphyrin macrocycle. Substitution of Bromine or Chl
orine axial ligands by ozonids is most likely to happen. This conclusi
on is also supported by XANES and EXAFS spectra recorded at the Chlori
ne K-edge which suggest that ozone may even form with chlorine a compl
ex anion.