The ferritins are a class of iron storage and detoxification proteins that
play a central role in the biological management of iron. These proteins ha
ve a catalytic site, "the ferroxidase site", located on the H-type subunit
that facilitates the oxidation of Fe(II) to Fe(III) by O-2. Measurements du
ring the past 10 years on a number of vertebrate ferritins have provided ev
idence that H2O2 is produced at this diiron ferroxidase site. Recently repo
rted experiments using three different analytical methods with horse spleen
ferritin (HoSF) have failed to detect H2O2 production in this protein [Lin
dsay, S., Brosnahan, D., and Watt, G.D. (2001) Biochemistry 40, 3340-3347].
These findings contrast with earlier results reporting H2O2 production in
HoSF [Xu, B., and Chasteen, N.D. (1991) J. Biol. Chem. 266, 19965-19970]. H
ere a sensitive fluorescence assay and an assay based on O-2 evolution in t
he presence of catalase were used to demonstrate that H2O2 is produced in H
oSF as previously reported. However, because of the relatively few H-chain
ferroxidase sites in HoSF and the reaction of H2O2 with the protein, H2O2 i
s more difficult to detect in this ferritin than in recombinant human H-cha
in ferritin (EuHF). The proper sequence of addition of reagents is importan
t for measurement of the total amount of H2O2 produced during the ferroxida
tion reaction.