Moving Iron through ferritin protein nanocages depends on residues throughout each four α-helix bundle subunit.

ABSTRACT: Eukaryotic H ferritins move iron through protein cages to form biologically required, iron mineral concentrates. The biominerals are synthesized during protein-based Fe²⁺/O₂ oxidoreduction and formation of [Fe³⁺O](n) multimers within the protein cage, en route to the cavity, at sites distributed over ~50 Å. Recent NMR and Co²⁺-protein x-ray diffraction (XRD) studies identified the entire iron path and new metal-protein interactions: (i) lines of metal ions in 8 Fe²⁺ ion entry channels with three-way metal distribution points at channel exits and (ii) interior Fe³⁺O nucleation channels. To obtain functional information on the newly identified metal-protein interactions, we analyzed effects of amino acid substitution on formation of the earliest catalytic intermediate (diferric peroxo-A(650

SUBMITTER: Haldar S 

PROVIDER: S-EPMC3138320 | biostudies-literature | 2011 Jul

REPOSITORIES: biostudies-literature