The ferritin Fe2 site at the diiron catalytic center controls the reaction with O 2 in the rapid mineralization pathway
- 25 November 2008
- journal article
- research article
- Published by Proceedings of the National Academy of Sciences in Proceedings of the National Academy of Sciences
- Vol. 105 (47) , 18182-18187
- https://doi.org/10.1073/pnas.0805083105
Abstract
Oxidoreduction in ferritin protein nanocages occurs at sites that bind two Fe(II) substrate ions and O 2 , releasing Fe(III) 2 –O products, the biomineral precursors. Diferric peroxo intermediates form in ferritins and in the related diiron cofactor oxygenases. Cofactor iron is retained at diiron sites throughout catalysis, contrasting with ferritin. Four of the 6 active site residues are the same in ferritins and diiron oxygenases; ferritin-specific Gln 137 and variable Asp/Ser/Ala 140 substitute for Glu and His, respectively, in diiron cofactor active sites. To understand the selective functions of diiron substrate and diiron cofactor active site residues, we compared oxidoreductase activity in ferritin with diiron cofactor residues, Gln 137 → Glu and Asp 140 → His, to ferritin with natural diiron substrate site variations, Asp 140 , Ser 140 , or Ala 140 . In Gln 137 → Glu ferritin, diferric peroxo intermediates were undetectable; an altered Fe(III)–O product formed, Δ A 350 = 50% of wild type. In Asp 140 → His ferritin, diferric peroxo intermediates were also undetectable, and Fe(II) oxidation rates decreased 40-fold. Ferritin with Asp 140 , Ser 140 , or Ala 140 formed diferric peroxo intermediates with variable kinetic stabilities and rates: t 1/2 varied 1- to 10-fold; k cat varied approximately 2- to 3-fold. Thus, relatively small differences in diiron protein catalytic sites determine whether, and for how long, diferric peroxo intermediates form, and whether the Fe–active site bonds persist throughout the reaction cycle (diiron cofactors) or break to release Fe(III) 2 –O products (diiron substrates). The results and the coding similarities for cofactor and substrate site residues—e.g., Glu/Gln and His/Asp pairs share 2 of 3 nucleotides—illustrate the potential simplicity of evolving active sites for diiron cofactors or diiron substrates.Keywords
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