Versatility of cryo-electron microscopy as a structural technique informs iron mineral nucleation and growth in a mini-ferritin

Abstract

Iron is an enigmatic element. While necessary for life, it also contributes to the generation of reactive oxygen species via the Fenton reaction. To mitigate this, cellular life has evolved the ferritin family of proteins, including the 24 subunit ferritins and bacterioferritins, and the 12 subunit DPSL "mini-ferritins". Each of these catalyze the controlled oxidation and sequestration of iron as a hydrous ferric oxyhydroxide within their hollow protein cores. While there is a wealth of structural information on the unmineralized ferritins, little is known about the structures of the biomineralized forms, and the mechanism of ferric oxyhydroxide nucleation and growth. Here we report structural and biochemical characterization of a DPS-Like protein from Pyrococcus furiosus. This "thioferritin" utilizes a bacterioferritin-like ferroxidase center, but adopts the mini-ferritin quaternary structure, and is thus thought to sit at the evolutionary boundary between mini- and maxi-ferritins. In addition to the unmineralized structure, we report the 1.91 angstrom structure of P. furiosus thioferritin as it nucleates iron-oxyhydroxide distal to the ferroxidase site. In this very low iron form, a pair of conserved glutamate residues and unsaturated carbonyls at the 3-fold axis serve to template initial nucleation. We also determine structures of higher iron forms with a biomineralized ferrihydrite core, where C-terminal residues 170-176 interact directly with the initial mineral surface, which then grows towards the particle center. These studies provide important new insight into biological mechanisms for the controlled nucleation, growth and storage of ferric oxyhydroxide in this thioferritin specifically, and the ferritin superfamily as a whole.