Ferritins are an ancient superfamily of protein nanocages that synthesize, reversibly, iron concentrates for cellular use, heme, FeS cluster, and Fe-protein synthesis and provide oxidant protection by consumption of dioxygen or hydrogen peroxide and ferrous iron during stress; the protein cavities containing the minerals are ϳ60% of the cage volume (1-4). Ferritins differ in cage size, location, and mechanism of catalytic sites, mineral size, and mineral crystallinity; the Fe 2ϩ /O 2 oxidoreductase sites are also called ferroxidase sites or FC (ferroxidase centers) sites (1-5). In eukaryotic H ferritins, Fe 2ϩ and dioxygen are substrates for oxidoreductase sites and are catalytically coupled at multiple protein sites to synthesize diferric oxo mineral precursors (Fig. 1). Consumption of both iron and oxygen by ferritins accounts for the antioxidant response and iron-controlled gene regulation of ferritins in eukaryotes (6). Many catalytic proteins use iron and oxygen to produce a variety of organic products. Such products include unsaturated fatty acids such as oleate stearoyl-CoA desaturase-1 (7), deoxyribose (ribonucleotide reductase), and prolyhydroxyl modification of oxygen-sensing DNA transcription factors, e.g. hypoxia-inducible factor-␣ (8). Only in ferritins are both substrates inorganic. The exclusive use of inorganic substrates may relate to the ancient origins of the ferritins, which are distributed in all kingdoms and in both anaerobes and aerobes; ferritin gene deletion is lethal early in mammalian embryogenesis (9).There are two types of protein channels that move iron into and through the 24 subunit cages during synthesis of [Fe 3ϩ O] n in eukaryotic ferritins. The two functional types of ferritin channels are: (i) ion entry channels around the 3-fold axes, for , where diferric oxo mineral precursors produced by oxidoreduction fuse to tetramers and larger multimers before exiting from the protein cage for mineral growth.Recent high resolution structural studies show that ferritin is a soluble ion channel protein with lines of multiple metal ions (10), much like K ϩ and other membrane ion channel proteins. The eight Fe 2ϩ entry channels (Fig. 1) suggest roles beyond just electrostatics for the conserved carboxylates, such as ion selectivity at the channel constriction or directing Fe 2ϩ substrate ions to active sites in three subunits that also form the entry channels (10). The Fe 3ϩ O nucleation channels were recently identified using 13 C-13 C solution NMR spectroscopy in the presence and absence of Fe 3ϩ , by the disappearance of resonances within 5 Å of Fe 3ϩ O moving away from the active sites (11). Nucleation channel exits into the cavity are clustered around the 4-fold axes of the cage, which facilitates ordered mineral growth. 4 The abbreviations used are: DFP, diferric peroxo; MCD, magnetic circular dichroism; bis-Tris, bis(2-hydroxyethyl)iminotris(hydroxymethyl)methane.