Spectroscopic Evidence for and Characterization of a Trinuclear Ferroxidase Center in Bacterial Ferritin from Desulfovibrio vulgaris Hildenborough

• Authors: Alice S. Pereira, Universidade Nova de Lisboa; Cristina G. Timoteo, Universidade Nova de Lisboa; Marcia Guilherme, Universidade Nova de Lisboa; Filipe Folgosa, Universidade Nova de Lisboa; Sunil G. Naik, Emory University; Americo G. Duarte, Universidade Nova de Lisboa; B H Vincent Huynh, Emory University; Pedro Tavares, Universidade Nova de Lisboa
• Journal Title: Journal of the American Chemical Society
• Volume: Volume 134, Number 26
• Publisher: American Chemical Society | 2012-07-04, Pages 10822-10832
• Type of Work: Article | Post-print: After Peer Review
• Publisher DOI: http://doi.org/10.1021/ja211368u
• Subjects: Chemistry, General; Physics, General

Abstract

Ferritins are ubiquitous and can be found in practically all organisms that utilize Fe. They are composed of 24 subunits forming a hollow sphere with an inner cavity of ~80 Å in diameter. The main function of ferritin is to oxidize the cytotoxic Fe2+ ions and store the oxidized Fe in the inner cavity. It has been established that the initial step of rapid oxidation of Fe2+ (ferroxidation) by H-type ferritins, found in vertebrates, occurs at a diiron binding center, termed ferroxidase center. In bacterial ferritins, however, X-ray crystallographic evidence and amino-acid sequence analysis revealed a trinuclear Fe binding center comprising a binuclear Fe binding center (sites A and B), homologous to the ferroxidase center of H-type ferritin, and an adjacent mononuclear Fe binding site (site C). In an effort to obtain further evidence supporting the presence of a trinuclear Fe binding center in bacterial ferritins and to gain information on the states of the iron bound to the trinuclear center, bacterial ferritin from Desulfovibrio vulgaris (DvFtn) and its E130A variant were loaded with sub-stoichiometric amounts of Fe2+ and products were characterized by Mössbauer and EPR spectroscopy. Four distinct Fe species were identified: a paramagnetic diferrous species, a diamagnetic diferrous species, a mixed valence Fe2+Fe3+ species and a mononuclear Fe2+ species. The latter three species were detected in the wild-type DvFtn, while the paramagnetic diferrous species was detected in the E130A variant. These observations can be rationally explained by the presence of a trinuclear Fe binding center, and the four Fe species can be properly assigned to the three Fe binding sites. Further, our spectroscopic data suggest that (1) the fully occupied trinuclear center supports an all ferrous state, (2) site B and C are bridged by a μ-OH group forming a diiron sub-center within the trinuclear center, and (3) this sub-center can afford both a mixed valence Fe2+Fe3+ state and a diferrous state. Mechanistic insights provided by these new findings are discussed and a minimal mechanistic scheme involving O-O bond cleavage is proposed.