Iron and activated oxygen species in biology: The basic chemistry

This paper briefly presents a critical review concerning the chemical reactions involved when superoxide or hydrogen peroxide meet iron complexes. The data commented on are required for a correct interpretation of the chemical processes which play a paramount role in the biological activation of dioxygen and arise in normal metabolism as well as in pathological processes.     

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).     

Iron and the heart: A paradigm shift from systemic to cardiomyocyte abnormalities

Iron is a key micronutrient for the human body and participates in biological processes, such as oxygen transport, storage, and utilization. Iron homeostasis plays a crucial role in the function of the heart and both iron deficiency and iron overload are harmful to the heart, which is partly mediated by increased oxidative stress. Iron enters the cardiomyocyte through the classic pathway, by binding to the transferrin 1 receptor (TfR1), but also through other routes: T-type calcium channel (TTCC), divalent metal transporter 1 (DMT1), L-type calcium channel (LTCC), Zrt-, Irt-like Proteins (ZIP) 8 and 14. Only one protein, ferroportin (FPN), extrudes iron from cardiomyocytes. Intracellular iron is utilized, stored bound to cytoplasmic ferritin or imported by mitochondria. This cardiomyocyte iron homeostasis is controlled by iron regulatory proteins (IRP). When the cellular iron level is low, expression of IRPs increases and they reduce expression of FPN, inhibiting iron efflux, reduce ferritin expression, inhibiting iron storage and augment expression of TfR1, increasing cellular iron availability. Such cellular iron homeostasis explains why the heart is very susceptible to iron overload: while cardiomyocytes possess redundant iron importing mechanisms, they are equipped with only one iron exporting protein, ferroportin. Furthermore, abnormalities of iron homeostasis have been found in heart failure and coronary artery disease, however, no clear picture is emerging yet in this area. If we better understand iron homeostasis in the cardiomyocyte, we may be able to develop better therapies for a variety of heart diseases to which abnormalities of iron homeostasis may contribute.     

Some aspects of iron cycling in maritime antarctic lakes

Iron occurs in extremely high concentrations in certain maritime Antarctic freshwater lakes which seasonally develop an anoxic zone. In oligotrophic Sombre Lake the data show that Fe(II) precipitates as Fe(III) oxyhydroxides which bind phosphorus and return it to the sediments. In nutrient-enriched Amos lake, significant quantities of sulphide are also produced and this binds a proportion of the released Fe(II) so reducing the ratio of total iron to phosphorus at the redox boundary where the oxyhydroxides are formed. A proportion of the sediment-released phosphorus therefore reaches the upper waters of this lake (unlike in Sombre Lake) and provides the initial nutrient source for under-ice phytoplankton development in spring. Iron-reducing bacteria have been isolated, from Sombre Lake sediments, which apparently utilise the abundant Fe(III) oxyhydroxides. From thermodynamic considerations (assuming Fe(III) is not limiting) these should outcompete sulphate reducers and methanogens (both previously reported from Sombre and Amos Lakes) and could therefore constitute an important component of the anaerobic mineralisation of organic carbon in such lakes.     

水稻土中铁氧化物对产甲烷古菌群落结构的影响

产甲烷菌广泛分布在淹水水稻土等各种厌氧环境中,在全球气候变化、碳循环和能源等领域都发挥着重要的作用。研究发现,厌氧条件下,水稻土中铁氧化物的生物还原会抑制产甲烷菌的甲烷合成作用。然而,目前关于铁氧化物对产甲烷菌群落结构的影响报道较少。通过泥浆厌氧培养实验,向采集的水稻土中添加甲酸盐作为甲烷合成的底物(Control,CK处理),并设置添加水铁矿作为体系中唯一电子受体的处理组(Ferrihydrite,Fh处理)。培养结束后,与CK相比,添加水铁矿显著降低了古菌在总微生物群落中的占比,但对古菌群落的物种多样性和均一度没有显著影响;且两组处理中优势种均为操作分类单元(Operational taxonomic unit,OTU)2056和OTU 911(76%—80%)。这说明碳源相同时,产甲烷菌的群落结构不受铁氧化物的影响。本研究为探索土壤中微生物铁还原与碳循环耦合的分子机制奠定基础。     

Candida albicans iron acquisition within the host

As a commensal and opportunistic pathogen, Candida albicans possesses a range of determinants that contribute to survival, persistence and virulence. Among this repertoire of fitness and virulence attributes are iron acquisition factors and pathways, which allow fungal cells to gain this essential mineral in the iron-poor environment of the host. The aim of this review is to present the strategies used by C. albicans to exploit host iron reservoirs and their impact on C. albicans pathogenicity. Because iron in the human host is mostly linked to host proteins, pathogens such as C. albicans must possess mechanisms to gain iron from these proteins. Here, we introduce the most important groups of human proteins, including haemoglobin, transferrin, lactoferrin and ferritin, which contain iron and that are potential iron sources for invading microorganisms. We then summarize and discuss the known and proposed strategies by which C. albicans exploits or may exploit iron from host proteins and compare these with strategies from other pathogenic microorganisms.     

Iron Binding and Autoreduction by Citrate: Are These Involved in Signalling by Iron Regulatory Protein-l?

Ferric ions bind to citrate and undergo an autoreduction to form a ferrous-citrate complex, greatly increasing the redox activity of the iron complex. Ferrous ions and citrate are also essential for the enzymic activity of aconitase. Aconitase, with its iron-sulphur cluster has a versatile structure which allows it to act as an iron regulatory protein (IW-1). The purpose of this study was to see whether iron binding, and its autoreduction by citrate, could play a physiological signalling role in iron regulation. Significant amounts of ferrous ions were associated with citrate, when measured using ferrozine, however, these did not appear to activate iron-requiring aconitase.     

Chemistry for an essential biological process: the reduction of ferric iron

In biological systems, the predominant form of iron is the trivalent Fe(III) form, which is potentially not readily bioavailable because of its hydrolysis and polymerization to insoluble forms. It is also the easiest of the two predominant forms of iron to chelate selectively. In a short overview of iron chemistry, we point out some of the pitfalls using standard redox potentials, comment on the interaction of ferric complexes with hydrogen peroxide to give hydroxyl radicals and address the release of iron from ferrisiderophores. In biological systems there are two classes of ferric reductases, the soluble flavin reductases found in prokaryotes, and the membrane-bound cytochrome b-like reductases found in eukaryotes. Finally the role of dissimilatory ferric reduction in microbial respiration and biomineralization is discussed.     

补铁剂研究进展

缺铁性贫血是全球最常见的一种营养素缺乏疾病,患者由于血氧不足,易引起疲劳、烦躁、记忆力减退等系列症状,严重影响身 体健康,降低了生活质量。补铁剂是目前最广谱有效的预防和治疗缺铁性贫血的药物。综述补铁剂的发展历程,在铁吸收代谢机制的基础上, 归纳总结传统铁剂的特点和类别,同时对高分子铁剂的结构信息、理化性质、给药途径和剂量、吸收机制等进行系统整理,介绍3 种即 将进入我国市场的新型静脉铁剂的使用和临床试验情况,为补铁剂的研究提供参考。     

海帕西啶铁调节和血色素沉着

血色素沉着是一种血浆铁沉积过多而导致的器官损伤性疾病,多种铁调节基因如HFE、HJV、HAMP和TfR2等的突变均可导致该病的发生,其中HAMP是最为重要的一种。HAMP基因编码一种名为海帕西啶的小肽,是小肠铁重吸收和巨噬细胞铁释放的负调节因子。海帕西啶含量的减少将导致血清铁过负荷和血色素沉着的发生,HFE、HJV和TfR2等基因可影响海帕西啶的表达,从而使海帕西啶成为血色素沉着的中央调节者。这些研究对血色素沉着发生机制的理解及其诊断和治疗具有重要意义。     

Co-occurrence of nicotianamine and avenic acids in Avena sativa and Oryza sativa

An amino acid derivative isolated from seedlings of Avena sativa and Oryza sativa, along with avenic acid A and its derivatives which possess a chelating ability with iron ions, has been shown to be nicotianamine. The co-occurrence of nicotianamine and avenic acids in the same plant, as well as their structural similarity, reveals their close biosynthetic relationship.     

The determination of ferric iron in plants by HPLC using the microbial iron chelator desferrioxamine E

Common methods for plant iron determination are based on atomic absorption spectroscopy, radioactive measurements or extraction with subsequent spectrophotometry. However, accuracy is often a problem due to background, contamination and interfering compounds. We here describe a novel method for the easy determination of ferric iron in plants by chelation with a highly effective microbial siderophore and separation by high performance liquid chromatography (HPLC). After addition of colourless desferrioxamine E (DFE) to plant fluids, the soluble iron is trapped as a brown-red ferrioxamine E (FoxE) complex which is subsequently separated by HPLC on a reversed phase column. The formed FoxE complex can be identified due to its ligand-to-metal charge transfer band at 435 nm. Alternatively, elution of both, DFE and FoxE can be followed as separate peaks at 220 nm wavelength with characteristic retention times. The extraordinarily high stability constant of DFE with ferric iron of K=10³² enables extraction of iron from a variety of ferrous and ferric iron compounds and allows quantitation after separation by HPLC without interference by coloured by-products. Thus, iron bound to protein, amino acids, citrate and other organic acid ligands and even insoluble ferric hydroxides and phosphates can be solubilized in the presence desferrioxamine E. The “Ferrioxamine E method” can be applied to all kinds of plant fluids (apoplasmic, xylem, phloem, intracellular) either at physiological pH or even at acid pH values. The FoxE complex is stable down to pH 1 allowing protein removal by perchloric acid treatment and HPLC separation in the presence of trifluoroacetic acid containing eluents. Published online December 2004     

哺乳动物铁稳态分子机制研究进展

铁是机体必需微量元素,参与机体合成血红蛋白、肌红蛋白及多种酶的组成和功能发挥,对维持生命和健康至关重要。近四分之一的世界人口遭受铁缺乏或缺铁性贫血的威胁。此外,部分人群还存在铁过载问题,以脏器铁离子蓄积为主要病理改变的遗传性血色病,其在欧美发病率高达1/200,在中国也有报道。血色病后期多诱发肝脏、胰腺及心脏的功能衰退。铁过少或过多对健康都会造成严重危害,机体需要复杂而精密的调控体系维持铁稳态平衡。铁代谢主要包括小肠吸收、肝脏储存、血液转运、巨噬细胞再循环以及周身细胞利用。过去十多年是铁代谢研究的黄金时期,先后发现众多铁稳态代谢相关基因。该文综述了近年来哺乳动物铁代谢领域的研究进展,并对铁稳态代谢中存在的问题进行了初步讨论,为理解和进一步深入研究铁代谢分子机制提供参考。     

Two pathways of iron uptake in bovine spleen apoferritin dependent on iron concentration

Iron incorporation by bovine spleen apoferritin either with ferrous ammonium sulfate in different buffers or with ferrous ammonium sulfate and phosphate was studied. Iron uptake and iron autoxidation were recorded spectrophotomerically. The buffers [4-(2-hydroxyethyl)-1-piperazinyl]ethanesulphonic acid (Hepes) and tris(hydroxymethyl)aminoethane (Tris) exhibited pH-dependent iron autoxidation, with Tris showing less iron autoxidation than Hepes. An Eadie-Scatchard plot (v/[s] versus v) of the iron uptake rate in Hepes was a curved rather than a straight line, suggesting that there are two iron uptake pathways. On the other hand, the Eadie-Scatchard plots of Tris and of Hepes after the addition of phosphate showed a straight line. Phosphate accelerated the iron uptake rate. The iron loading kinetics of apoferritin in Hepes was dependent on apoferritin concentration. The K_m value obtained from iron uptake kinetics was 4.5 M, corresponding to the physiological iron concentration. These results demonstrate that iron loading of apoferritin was accomplished at physiological iron concentrations, which is essential for iron uptake, via two uptake pathways of dependent on iron concentration.     

Partition coefficients of the iron(III) complexes of pyridoxal isonicotinoyl hydrazone and its analogs and the correlation to iron chelation efficacy

Pyridoxal isonicotinoyl hydrazone and its analogs are orally effective Fe(III) chelators which show potential as drugs to treat iron overload disease. The present investigation describes the measurement of the partition coefficient of the apochelator and Fe(III) complex of 20 of these ligands. These measurements have been done to investigate the relationship between lipophilicity and the efficacy of iron chelation in rabbit reticulocytes loaded with non-heme ⁵⁹Fe. The results demonstrate a linear relationship between the partition coefficient (P) of the apochelator and its Fe(III) complex, and a simple equation has been derived relating these two parameters. Experimental data in the literature are in agreement with the equation. The relationship of the partition coefficients of the iron chelators and of their Fe(III) complexes to the effectiveness of the ligands in mobilizing iron in vitro and in vivo is also discussed.     

Juncus bulbosus as a pioneer species in acidic lignite mining lakes: interactions, mechanism and survival strategies

Bulbous rush ( Juncus bulbosus ) initiates plant colonization in extremely acid lakes resulting from coal mining operations. Various analytical techniques (methylene blue/agar method, Ti³⁺-citrate solution) X-ray diffraction (XRD), scanning electron microscopy (SEM), and Energy-dispersive X-ray (EDX) were used to assess the mechanisms and strategies employed by J. bulbosus to overcome the extreme conditions. The plant releases oxygen into the rhizosphere in turn increasing the redox potential and inducing iron oxide plaque formation. XRD showed that the iron oxide of the plaque is mainly goethite that has been developed in the presence of CO₂; SEM showed that there is a micro-space between the roots and sand grains which is inhabited by microorganisms. Furthermore, SEM-EDX studies on internal iron distribution demonstrate that iron toxicity is delayed by the physiological and biochemical structure of the plant. It is suggested that J. bulbosus uses a variety of mechanisms and strategies (morphological, physiological and biochemical adaptation) which are mainly complementary and which interact with each other to help J. bulbosus to manage its growth and survival in an extreme environment.     

植物铁代谢及植物铁蛋白结构与功能研究进展

铁在生命过程中起着很重要的作用,植物缺铁后叶绿素合成受阻而导致的黄化症状已成为世界性植物营养失调问题。与之相随,人类铁营养的缺乏也极为严重,因此研究植物铁代谢并且开发安全、天然、高效的补铁因子具有重要的意义。到目前为止,在已经发现的植物中,只有豆科类植物是将其种子中～90％的铁储藏在铁蛋白中,所以来源于豆科类植物的铁蛋白是一个理想的补铁资源。与动物铁蛋白相比,植物铁蛋白具有两个显著的特点：首先,植物铁蛋白在其N端具有一个独特的EP肽段;其次,植物铁蛋白只含有H型亚基,且有两种不同的H型亚基组成。主要阐述有关植物铁代谢及铁蛋白的结构、功能的最新研究进展。     

Fine structure of the mineralized teeth of the chiton Acanthopleura echinata (Mollusca: Polyplacophora)

The major lateral teeth of the chiton Acanthopleura echinata are composite structures composed of three distinct mineral zones: a posterior layer of magnetite; a thin band of lepidocrocite just anterior to this; and apatite throughout the core and anterior regions of the cusp. Biomineralization in these teeth is a matrix-mediated process, in which the minerals are deposited around fibers, with the different biominerals described as occupying architecturally discrete compartments. In this study, a range of scanning electron microscopes was utilized to undertake a detailed in situ investigation of the fine structure of the major lateral teeth. The arrangement of the organic and biomineral components of the tooth is similar throughout the three zones, having no discrete borders between them, and with crystallites of each mineral phase extending into the adjacent mineral zone. Along the posterior surface of the tooth, the organic fibers are arranged in a series of fine parallel lines, but just within the periphery their appearance takes on a "fish scale"-like pattern, reflective of the cross section of a series of units that are overlaid, and offset from each other, in adjacent rows. The units are approximately 2 microm wide and 0.6 microm thick and comprise biomineral plates separated by organic fibers. Two types of subunits make up each "fish scale": one is elongate and curved and forms a trough, in which the other, rod-like unit, is nestled. Adjacent rod and trough units are aligned into large sheets that define the fracture plane of the tooth. The alignment of the plates of rod-trough units is complex and exhibits extreme spatial variation within the tooth cusp. Close to the posterior surface the plates are essentially horizontal and lie in a lateromedial plane, while anteriorly they are almost vertical and lie in the posteroanterior plane. An understanding of the fine structure of the mineralized teeth of chitons, and of the relationship between the organic and mineral components, provides a new insight into biomineralization mechanisms and controls.