期刊
BIOCHEMISTRY
卷 40, 期 36, 页码 10832-10838出版社
AMER CHEMICAL SOC
DOI: 10.1021/bi011052j
关键词
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资金
- NIGMS NIH HHS [R37 GM20194] Funding Source: Medline
The ferritins are a class of iron storage and detoxification proteins that play a central role in the biological management of iron. These proteins have 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 during the past 10 years on a number of vertebrate ferritins have provided evidence that H2O2 is produced at this diiron ferroxidase site. Recently reported experiments using three different analytical methods with horse spleen ferritin (HoSF) have failed to detect H2O2 production in this protein [Lindsay, 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]. Here a sensitive fluorescence assay and an assay based on O-2 evolution in the presence of catalase were used to demonstrate that H2O2 is produced in HoSF as previously reported. However, because of the relatively few H-chain ferroxidase sites in HoSF and the reaction of H2O2 with the protein, H2O2 is more difficult to detect in this ferritin than in recombinant human H-chain ferritin (EuHF). The proper sequence of addition of reagents is important for measurement of the total amount of H2O2 produced during the ferroxidation reaction.
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