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      Catalysis of iron core formation in Pyrococcus furiosus ferritin

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          Abstract

          The hollow sphere-shaped 24-meric ferritin can store large amounts of iron as a ferrihydrite-like mineral core. In all subunits of homomeric ferritins and in catalytically active subunits of heteromeric ferritins a diiron binding site is found that is commonly addressed as the ferroxidase center (FC). The FC is involved in the catalytic Fe(II) oxidation by the protein; however, structural differences among different ferritins may be linked to different mechanisms of iron oxidation. Non-heme ferritins are generally believed to operate by the so-called substrate FC model in which the FC cycles by filling with Fe(II), oxidizing the iron, and donating labile Fe(III)–O–Fe(III) units to the cavity. In contrast, the heme-containing bacterial ferritin from Escherichia coli has been proposed to carry a stable FC that indirectly catalyzes Fe(II) oxidation by electron transfer from a core that oxidizes Fe(II). Here, we put forth yet another mechanism for the non-heme archaeal 24-meric ferritin from Pyrococcus furiosus in which a stable iron-containing FC acts as a catalytic center for the oxidation of Fe(II), which is subsequently transferred to a core that is not involved in Fe(II)-oxidation catalysis. The proposal is based on optical spectroscopy and steady-state kinetic measurements of iron oxidation and dioxygen consumption by apoferritin and by ferritin preloaded with different amounts of iron. Oxidation of the first 48 Fe(II) added to apoferritin is spectrally and kinetically different from subsequent iron oxidation and this is interpreted to reflect FC building followed by FC-catalyzed core formation.

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          The online version of this article (doi:10.1007/s00775-009-0571-z) contains supplementary material, which is available to authorized users.

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          Most cited references41

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          Mineralization in ferritin: an efficient means of iron storage.

          Ferritins are a class of iron storage and mineralization proteins found throughout the animal, plant, and microbial kingdoms. Iron is stored within the protein shell of ferritin as a hydrous ferric oxide nanoparticle with a structure similar to that of the mineral "ferrihydrite." The eight hydrophilic channels that traverse the protein shell are thought to be the primary avenues by which iron gains entry to the interior of eukaryotic ferritins. Twenty-four subunits constitute the protein shell and, in mammalian ferritins, are of two types, H and L, which have complementary functions in iron uptake. The H chain contains a dinuclear ferroxidase site that is located within the four-helix bundle of the subunit; it catalyzes the oxidation of ferrous iron by O(2), producing H(2)O(2). The L subunit lacks this site but contains additional glutamate residues on the interior surface of the protein shell which produce a microenvironment that facilitates mineralization and the turnover of iron(III) at the H subunit ferroxidase site. Recent spectroscopic studies have shown that a di-Fe(III) peroxo intermediate is produced at the ferroxidase site followed by formation of a mu-oxobridged dimer, which then fragments and migrates to the nucleation sites to form incipient mineral core species. Once sufficient core has developed, iron oxidation and mineralization occur primarily on the surface of the growing crystallite, thus minimizing the production of potentially harmful H(2)O(2). Copyright 1999 Academic Press.
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            Ferritins: dynamic management of biological iron and oxygen chemistry.

            Ferritins are spherical, cage-like proteins with nanocavities formed by multiple polypeptide subunits (four-helix bundles) that manage iron/oxygen chemistry. Catalytic coupling yields diferric oxo/hydroxo complexes at ferroxidase sites in maxi-ferritin subunits (24 subunits, 480 kDa; plants, animals, microorganisms). Oxidation occurs at the cavity surface of mini-ferritins/Dps proteins (12 subunits, 240 kDa; bacteria). Oxidation products are concentrated as minerals in the nanocavity for iron-protein cofactor synthesis (maxi-ferritins) or DNA protection (mini-ferritins). The protein cage and nanocavity characterize all ferritins, although amino acid sequences diverge, especially in bacteria. Catalytic oxidation/di-iron coupling in the protein cage (maxi-ferritins, 480 kDa; plants, bacteria and animal cell-specific isoforms) or on the cavity surface (mini-ferritins/Dps proteins, 280 kDa; bacteria) initiates mineralization. Gated pores (eight or four), symmetrically arranged, control iron flow. The multiple ferritin functions combine pore, channel, and catalytic functions in compact protein structures required for life and disease response.
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              Structure, function, and mechanism of ribonucleotide reductases.

              Ribonucleotide reductase (RNR) is the enzyme responsible for the conversion of ribonucleotides to 2'-deoxyribonucleotides and thereby provides the precursors needed for both synthesis and repair of DNA. In the recent years, many new crystal structures have been obtained of the protein subunits of all three classes of RNR. This review will focus upon recent structural and spectroscopic studies, which have offered deeper insight to the mechanistic properties as well as evolutionary relationship and diversity among the different classes of RNR. Although the three different classes of RNR enzymes depend on different metal cofactors for the catalytic activity, all three classes have a conserved cysteine residue at the active site located on the tip of a protein loop in the centre of an alpha/beta-barrel structural motif. This cysteine residue is believed to be converted into a thiyl radical that initiates the substrate turnover in all three classes of RNR. The functional and structural similarities suggest that the present-day RNRs have all evolved from a common ancestral reductase. Nevertheless, the different cofactors found in the three classes of RNR make the RNR proteins into interesting model systems for quite diverse protein families, such as diiron-oxygen proteins, cobalamin-dependent proteins, and SAM-dependent iron-sulfur proteins. There are also significant variations within each of the three classes of RNR. With new structures available of the R2 protein of class I RNR, we have made a comparison of the diiron centres in R2 from mouse and Escherichia coli. The R2 protein shows dynamic carboxylate, radical, and water shifts in different redox forms, and new radical forms are different from non-radical forms. In mouse R2, the binding of iron(II) or cobalt(II) to the four metal sites shows high cooperativity. A unique situation is found in RNR from baker's yeast, which is made up of heterodimers, in contrast to homodimers, which is the normal case for class I RNR. Since the reduction of ribonucleotides is the rate-limiting step of DNA synthesis, RNR is an important target for cell growth control, and the recent finding of a p53-induced isoform of the R2 protein in mammalian cells has increased the interest for the role of RNR during the different phases of the cell cycle.
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                Author and article information

                Contributors
                w.r.hagen@tudelft.nl
                Journal
                J Biol Inorg Chem
                Journal of Biological Inorganic Chemistry
                Springer-Verlag (Berlin/Heidelberg )
                0949-8257
                1432-1327
                22 July 2009
                November 2009
                : 14
                : 8
                : 1265-1274
                Affiliations
                Department of Biotechnology, Delft University of Technology, Julianalaan 67, 2628 BC Delft, The Netherlands
                Article
                571
                10.1007/s00775-009-0571-z
                2771142
                19623480
                ad007692-a390-4ef5-8aa3-53ae25894c85
                © The Author(s) 2009
                History
                : 18 March 2009
                : 9 July 2009
                Categories
                Original Paper
                Custom metadata
                © SBIC 2009

                Inorganic & Bioinorganic chemistry
                kinetics,ferritin,ferroxidase,uv–vis spectroscopy,pyrococcus furiosus

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