Moving Fe from Ferritin Ion Channels to Catalytic OH Centers
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+ Moving Fe2 from ferritin ion channels to catalytic OH centers depends on conserved protein cage carboxylates Rabindra K. Beheraa,1 and Elizabeth C. Theila,b,2 aChildren’s Hospital Oakland Research Institute, Oakland, CA 94609; and bDepartment of Molecular and Structural Biochemistry, North Carolina State University, Raleigh, NC 27695-7622 Edited by Harry B. Gray, California Institute of Technology, Pasadena, CA, and approved April 15, 2014 (received for review September 30, 2013) Ferritin biominerals are protein-caged metabolic iron concentrates Ferritin protein ion channels are 15 Å long, analogous to short used for iron–protein cofactors and oxidant protection (Fe2+ and ion channels in biological membranes (3). Positioned around the 2+ O2 sequestration). Fe passage through ion channels in the pro- threefold symmetry axes of the cage (Fig. 1), ferritin protein ion tein cages, like membrane ion channels, required for ferritin biomin- channels form during cage self-assembly from three proximal + eral synthesis, is followed by Fe2 substrate movement to ferritin subunits; ion channel amino acids are highly conserved (Table 1) 2+ enzyme (Fox)sites.Fe and O2 substrates are coupled via a diferric (14). Both external and internal ferritin ion channel pores are 3+ peroxo (DFP) intermediate, λmax 650 nm, which decays to [Fe –O– 4–5 Å in diameter with a midchannel constriction, 2.3 Å in di- + Fe3 ] precursors of caged ferritin biominerals. Structural studies show ameter, created by the carboxylate side chains from the three multiple conformations for conserved, carboxylate residues E136 and glutamate residues at position 130. In protein crystals, ferritin B E57, which are between ferritin ion channel exits and enzymatic sites, ion channels bind a variety of divalent metal ions (Fig. S2 and suggesting functional connections. Here we show that E136 and E57 Table S1). Because hydrated ions have diameters of 6.4–6.9 Å, are required for ferritin enzyme activity and thus are functional links partial dehydration must occur for ion passage through the E130 between ferritin ion channels and enzymatic sites. DFP formation (Kcat constriction (2.3-Å diameter). Only single metal atoms are ob- and kcat/Km), DFP decay, and protein-caged hydrated ferric oxide ac- served in protein–metal crystal structures at the ring of three cumulation decreased in ferritin E57A and E136A; saturation required E130 residues, contrasting with the multiple metal atoms accu- + higher Fe2 concentrations. Divalent cations (both ion channel and mulated near the channel exits around the ring of three D127 intracage binding) selectively inhibit ferritin enzyme activity (block residues with shorter carboxylate side chains (Fig. 1 B and C); Fe2+ access), Mn2+ << Co2+ < Cu2+ < Zn2+, reflecting metal ion– + multiple ordered water molecules also accumulate near D127. protein binding stabilities. Fe2 –Cys126 binding in ferritin ion chan- Here we report functional studies that trace the movement of 2+ + nels, observed as Cu –S–Cys126 charge-transfer bands in ferritin Fe2 from ferritin ion channel exits to ferritin enzyme sites (Fig. 1). 2+ E130D UV-vis spectra and resistance to Cu inhibition in ferritin The strategy is to compare enzymatic reactions among variant 2+ CHEMISTRY C126S, was unpredicted. Identifying E57 and E136 links in Fe move- ferritins E57A, E136A, and E57A/E136A to WT and to an ion ment from ferritin ion channels to ferritin enzyme sites completes channel variant, E130D, which has detectable enzymatic activity; 2+ a bucket brigade that moves external Fe into ferritin enzymatic sites. in protein crystal structures, ferritin cage residues E57 and E136 2+ The results clarify Fe transport within ferritin and model molecular have multiple conformations and bind metal ions. Enzymatically + links between membrane ion channels and cytoplasmic destinations. active ferritin subunits (type H) in eukaryotic ferritin couple Fe2 iron traffic | oxidoreductase enzyme activity | antioxidant | ferrihydrite | Significance BioIron BIOCHEMISTRY How ions move between ion channel exits and final desti- iological and synthetic ion channels transport metal ions nations is poorly understood. Fe2+ substrate enters ferritin Bthrough barriers, including those in ferritin protein cages protein nanocages through cage-penetrating ion channels – + (1 8). How ions reach specific destinations, after exiting ion chan- analogous to membrane ion channels. Fe2 then moves to nels, remains unknown. Ion channels embedded in soluble fer- ferritin cage enzyme (Fox) sites, reacting with oxygen substrate ritin protein cages are more accessible to study than membrane + to produce diferric oxy complexes, the precursors of ferritin ion channels embedded in lipid-rich membranes. Fe2 substrate minerals (Fe2O3·H2O). Ferritin iron is used in heme and iron– is transported into ferritin protein cages through multiple ion sulfur cofactors. Monitoring rapid (ms) diferric peroxo forma- A–D channels that penetrate the cages (Fig. 1 ) and is delivered tion in WT ferritin and E57 and E136 variants showed that to multiple ferritin enzyme (Fox) sites. Each ferritin enzyme site 2+ these conserved residues are required for enzyme activity. binds 2 Fe substrate ions which, in eukaroytic ferritins, react Combining the results with older structural studies identifies + with O2 substrate; the intermediate of enzyme activity is diferric ferritin E57 and E136 links in the Fe2 bucket brigade con- peroxo (DFP) that decays to diferric oxy, the precursors of necting ferritin ion channels and destinations. By analogy, key · protein-caged ferritin biominerals (Fe2O3 H2O). Ferritin bio- carboxylates in ion transporters link ion channels to cytoplas- minerals vary in size, depending on iron availability, up to 4,500 mic destinations. Fe/cage. Rapid (ms) formation of blue color DFP (λmax: 650 nm) 2+ (9, 10) requires cooperative binding of 2 Fe /active site (Hill Author contributions: R.K.B. and E.C.T. designed research; R.K.B. performed research; R.K.B. 2+ coefficient = 3) (11) and indicates correct Fe delivery to the and E.C.T. analyzed data; and R.K.B. and E.C.T. wrote the paper. multiple ferritin enzymatic centers. Ferritin protein-caged iron The authors declare no conflict of interest. biominerals, slow to dissolve in solution (Fig. S1), are metabolic This article is a PNAS Direct Submission. iron concentrates for cofactor biosynthesis such as heme or iron- 1Present address: Department of Chemistry, National Institute of Technology, Rourkela 2+ sulfur clusters. The conversion of Fe and O2 into protein- 769008, Odisha, India. coated solids inside ferritin cages is an antioxidant activity, and 2To whom correspondence should be addressed. E-mail: [email protected]. ferritin genes are regulated with other antioxidant response This article contains supporting information at www.pnas.org/lookup/suppl/doi:10.1073/ proteins (4, 12, 13). pnas.1318417111/-/DCSupplemental. www.pnas.org/cgi/doi/10.1073/pnas.1318417111 PNAS | June 3, 2014 | vol. 111 | no. 22 | 7925–7930 Downloaded by guest on September 23, 2021 2+ Fig. 1. Ion channels in soluble ferritin protein nanocages transport Fe to multiple catalytic centers (Fox or oxidoreductase sites). (A) The 24-subunit ferritin + + protein cage. Red helices, Fe2 channels. (B) A ferritin Fe2 ion channel (side view). Green spheres, metal ions. Conserved residues E57 and E136 are putative 2+ carboxylate links in Fe transit between ferritin ion channel carboxylate (E130 and D127) and ferritin enzyme (Fox) sites based on phylogenetic structural location and conformational flexibility in protein crystals (16, 18). (C) A single ferritin protein cage subunit (side view). Tan, channel helix segments. (D)Ion channel (viewed from inside the protein cage). Green spheres, metal ions. Prepared from PDB 3KA3 using PyMol. and O2 substrates in an oxidoreductase reaction that may be Results written as Conserved Carboxylates E57 and E136 Are Required for Rapid Reactions + Â Ã ÂÀ ÁÃ of Fe2 at Ferritin Enzyme Centers. Ferritin variants E57A and 2+• + → • 3+‐ ‐ ‐ 3+• 2 Fe H2O O2 H2O Fe O O Fe H2O E136A (Fig. 1C) (16, 17) were constructed for the following rea- + i ii → Fe2O3 • H2O + 4H : sons: ( ) E57 and E136 are highly conserved, ( ) E57 and E136 lie between internal exits and diiron catalytic centers (Table S1) A blue diferric peroxo intermediate forms in ms and decays quickly (<1 s) (4, 12, 13). Diferric oxy enzymatic reaction prod- 2+ ucts in ferritin are released inside the protein cage and coalesce Table 1. Conservation of ferritin amino acids in Fe cage into ferric-oxo multimers within nucleation channels between the transfer residues and ion channel walls enzyme sites and the central mineral growth cavity (Fig. 1); stoi- + Transfer carboxylates: E136 chiometric amounts of hydrogen peroxide and Fe3 are detected at + Organism and E57 Ion channel: helix 4 subsaturating amounts of Fe2 (<36 Fe/cage). Sets of four prox- imal nucleation channel exits surround the inner surface of the Eukaryotes fourfold cage axes, which can facilitate ordered interactions Frog M HSHEEREHAE–EEQVKDIK DPHLCDFLESEYL among the emerging biomineral precursors (8). Engineered ferritin Frog H QSHEEREHAE–EEQVKSIK DPHLCDFLETEYL variants E57A and E136A lack the conserved carboxylate residues Human H QSHEEREHAE–NEQVKAIK DPHLCDFIETHYL that lie between the ion channel exits and the diiron enzymatic sites. Human L LAEEKREGYE–DEEVKLIK DPHLCDFLETHFL Ferritin E130D ion channels were designed to compare an enzy- Human Mt-H QSREETEHAE–NEQVKSIK DPHLCDFLETYYL