X-ray structures of homopolymerich uman L-ferritin andh orse spleen ferritin weres olved by freezing protein crystals at different time intervals after exposure to a ferric salt and revealed the growth of an octa-nuclear iron cluster on the inner surface of the protein cage with ak ey role played by some glutamate residues.A na tomic resolution view of how the clusterf ormation developss tarting from a( m 3 -oxo)tris[(m 2 -glutamato-kO:kO')](glutamato-kO)-(diaquo)triiron(III) seed is provided. The results support the idea that iron biomineralizationi nf erritin is ap rocess initiating at the level of the protein surface, capable of contributing coordinationb onds and electrostatic guidance.In animals, cytosolic ferritin is ah eteropolymer consisting of 24 subunits of H-and L-chains that self-assemble into ah ollow structure that hosts iron deposits. L-subunits lack the ferroxidase site for the catalytic oxidation of Fe 2 + ,w hich is the characteristic feature of H-subunits. [1,2] The H/L ratio in the heteropolymeri sd etermined by the different expression levels of these two components and is tissue and cell specific. [3,4] In humans,c ages rich in Hs ubunits are found in tissues requiring fast iron metabolism (e.g.,m uscles and heart), whereas cages rich in Ls ubunits are found in tissues involved in long-term iron storage (such as liver and spleen). In brain, neurons express mostly H-ferritin, microglia express mostly L-ferritin, oligodendrocytes express similar amounts of both Ha nd Ls ubunits. [5] The H/L ratio determines the rate of iron biomineralization, which occurs as the result of the formation of nanosized particles of iron oxidesw ithin the inner nanocage cavity. [6] From TEM, SAXS, XANES, EELS and SQUID data, [7][8][9][10] ap olypha-sic structure (ferrihydrite,m agnetite, hematite) of the bulk biomineral has been proposed,w ith af errihydrite enriched core and ap redominantly magnetite-like surface. [7] The amount of L-type subunits influences the morphology,a se videnced by STEM micrographs, giving rise to hollow structures with shapes defined by the number of nucleation sites in the protein shell. [8] Nevertheless, the atomic-levelm echanism of the mineral formationr emains elusive. Recently,b yu sing timelapse crystallographic techniques, we have observed biomineral seeds consistingo f( m 3 -oxo)tris[(m 2 -peroxo)] triiron(III) clusters at the protein-inner cavity interface, which form upon spontaneous oxidation of ferrous ions internalized by recombinant human homopolymeric L-ferritin as well as by natural horse spleen ferritin, which contains about 1-2Hsubunits/cage (Figures S1 Aa nd S2 A, Supporting Information). [11] In this work, we have modified our experimental setting to extendt he observation beyond the formation of these initial nucleation clusters. In the previouse xperiments, we could observe Fe 3 + clusterf ormation via free diffusion of Fe 2 + through L-ferritin crystalsf ollowed by spontaneous oxidation, and flash freezing. [11] Undert hose experimental conditions, in the homopolym...