4XKT
E coli BFR variant Y149F
Summary for 4XKT
Entry DOI | 10.2210/pdb4xkt/pdb |
Descriptor | Bacterioferritin, SULFATE ION (3 entities in total) |
Functional Keywords | iron storage, diiron site, metal binding protein |
Biological source | Escherichia coli |
Total number of polymer chains | 12 |
Total formula weight | 223273.01 |
Authors | Bradley, J.M.,Hemmings, A.M.,Le Brun, N.E. (deposition date: 2015-01-12, release date: 2015-12-16, Last modification date: 2024-01-10) |
Primary citation | Bradley, J.M.,Svistunenko, D.A.,Lawson, T.L.,Hemmings, A.M.,Moore, G.R.,Le Brun, N.E. Three Aromatic Residues are Required for Electron Transfer during Iron Mineralization in Bacterioferritin. Angew.Chem.Int.Ed.Engl., 54:14763-14767, 2015 Cited by PubMed Abstract: Ferritins are iron storage proteins that overcome the problems of toxicity and poor bioavailability of iron by catalyzing iron oxidation and mineralization through the activity of a diiron ferroxidase site. Unlike in other ferritins, the oxidized di-Fe(3+) site of Escherichia coli bacterioferritin (EcBFR) is stable and therefore does not function as a conduit for the transfer of Fe(3+) into the storage cavity, but instead acts as a true catalytic cofactor that cycles its oxidation state while driving Fe(2+) oxidation in the cavity. Herein, we demonstrate that EcBFR mineralization depends on three aromatic residues near the diiron site, Tyr25, Tyr58, and Trp133, and that a transient radical is formed on Tyr25. The data indicate that the aromatic residues, together with a previously identified inner surface iron site, promote mineralization by ensuring the simultaneous delivery of two electrons, derived from Fe(2+) oxidation in the BFR cavity, to the di-ferric catalytic site for safe reduction of O2. PubMed: 26474305DOI: 10.1002/anie.201507486 PDB entries with the same primary citation |
Experimental method | X-RAY DIFFRACTION (1.82 Å) |
Structure validation
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