J. Hwang et al., A short Fe-Fe distance in peroxodiferric ferritin: Control of Fe substrateversus cofactor decay?, SCIENCE, 287(5450), 2000, pp. 122-125
The reaction of oxygen with protein diiron sites is important in bioorganic
syntheses and biomineralization. An unusually short Fe-Fe distance of 2.53
angstroms was found in the diiron (mu-1,2 peroxodiferric) intermediate tha
t forms in the early steps of ferritin biomineralization. This distance sug
gests the presence of a unique triply bridged structure. The Fe-Fe distance
s in the mu-1,2 peroxodiferric complexes that were characterized previously
are much longer (3.1 to 4.0 angstroms). The 2.53 angstrom Fe-Fe distance r
equires a small Fe-O-O angle (similar to 106 degrees to 107 degrees). This
geometry should favor decay of the peroxodiferric complex by the release of
H2O2 and mu-oxo or mu-hydroxo diferric biomineral precursors rather than b
y oxidation of the organic substrate. Geometrical differences may thus expl
ain how diiron sites can function either as a substrate (in ferritin biomin
eralization) or as a cofactor (in O-2 activation).