Iron deposition in apoferritin. Evidence for the formation of a mixed valence binuclear iron complex.
A preliminary EPR investigation of iron accumulation in apoferritin has identified paramagnetic species generated during the early stage of iron deposition within the apoprotein shell. A featureless resonance at g' = 4.3, attributable to solitary high spin Fe3+ ions bound to the protein, is generated when Fe(II) is added to apoferritin at a level of 0.5 Fe/subunit (12 Fe/molecule) followed by air oxidation. This resonance accounts for 36% of the added iron. The remainder is EPR-silent and is probably present as oligomeric Fe3+ species. The intensity of the g' = 4.3 signal is reduced 3-fold upon anaerobic addition of 5 Fe(II)/subunit as a new iron resonance with g' values of 1.94, 1.87, and 1.80 is generated. This signal is observable only at temperatures near that of liquid helium and resists saturation at power levels of 100 milliwatts. Its distinctive g-factors, temperature dependence, and saturation characteristics suggest that it arises from a spin-coupled Fe(II)-Fe(III) dimer having a net electron spin of 1/2. In accord with this idea, the signal disappears when air is admitted, presumably because of oxidation of the Fe(II). The proposed mixed valence dimer may be an important intermediate formed during the initiation of core formation within the protein shell.
Chasteen
N D
ND
Antanaitis
B C
BC
Aisen
P
P
D000818:Animals; D001052:Apoferritins / Q000032:analysis*; D004578:Electron Spin Resonance Spectroscopy; D005293:Ferritins / Q000031:analogs & derivatives*; D006736:Horses; D007501:Iron / Q000032:analysis*; D010100:Oxygen; D013154:Spleen / Q000032:analysis
D005293:Ferritins; D001052:Apoferritins; D007501:Iron; D010100:Oxygen