Rapid Assay for Microbially Reducible Ferric Iron in Aquatic Sediments

The availability of ferric iron for microbial reduction as directly determined by the activity of iron-reducing organisms was compared with its availability as determined by a newly developed chemical assay for microbially reducible iron. The chemical assay was based on the reduction of poorly crystalline ferric iron by hydroxylamine under acidic conditions. There was a strong correlation between the extent to which hydroxylamine could reduce various synthetic ferric iron forms and the susceptibility of the iron to microbial reduction in an enrichment culture of iron-reducing organisms. When sediments that contained hydroxylamine-reducible ferric iron were incubated under anaerobic conditions, ferrous iron accumulated as the concentration of hydroxylamine-reducible ferric iron declined over time. Ferrous iron production stopped as soon as the hydroxylamine-reducible ferric iron was depleted. In anaerobic incubations of reduced sediments that did not contain hydroxylamine-reducible ferric iron, there was no microbial iron reduction, even though the sediments contained high concentrations of oxalate-extractable ferric iron. A correspondence between the presence of hydroxylamine-reducible ferric iron and the extent of ferric iron reduction in anaerobic incubations was observed in sediments from an aquifer and in fresh- and brackish-water sediments from the Potomac River estuary. The assay is a significant improvement over previously described procedures for the determination of hydroxylamine-reducible ferric iron because it provides a correction for the high concentrations of solid ferrous iron which may also be extracted from sediments with acid. This is a rapid, simple technique to determine whether ferric iron is available for microbial reduction.     

Lipid peroxidation and associated hepatic organelle dysfunction in iron overload

Iron overload can have serious health consequences. Since humans lack an effective means to excrete excess iron, overload can result from an increased absorption of dietary iron or from parenteral administration of iron. When the iron burden exceeds the body's capacity for safe storage, the result is widespread damage to the liver, heart and joints, and the pancreas and other endocrine organs. Clear evidence is now available that iron overload leads to lipid peroxidation in experimental animals, if sufficiently high levels of iron are achieved. In contrast, there is a paucity of data regarding lipid peroxidation in patients with iron overload. Data from experiments using an animal model of dietary iron overload support the concept that iron overload results in an increase in an hepatic cytosolic pool of low molecular weight iron which is catalytically active in stimulating lipid peroxidation. Lipid peroxidation is associated with hepatic mitochondrial and microsomal dysfunction in experimental iron overload, and lipid peroxidation may underlie the increased lysosomal fragility that has been detected in homogenates of liver samples from both iron-loaded human subjects and experimental animals. Some current hypotheses focus on the possibility that the demonstrated functional abnormalities in organelles of the iron-loaded liver may play a pathogenic role in hepatocellular injury and eventual fibrosis. The recent demonstration that hepatic fibrosis is produced in animals with long-term dietary iron overload will allow this model to be used to further investigate the relationship between lipid peroxidation and hepatic injury in iron overload.     

OPT3 Is a Phloem-Specific Iron Transporter That Is Essential for Systemic Iron Signaling and Redistribution of Iron and Cadmium in Arabidopsis

Iron is essential for both plant growth and human health and nutrition. Knowledge of the signaling mechanisms that communicate iron demand from shoots to roots to regulate iron uptake as well as the transport systems mediating iron partitioning into edible plant tissues is critical for the development of crop biofortification strategies. Here, we report that OPT3, previously classified as an oligopeptide transporter, is a plasma membrane transporter capable of transporting transition ions in vitro. Studies in Arabidopsis thaliana show that OPT3 loads iron into the phloem, facilitates iron recirculation from the xylem to the phloem, and regulates both shoot-to-root iron signaling and iron redistribution from mature to developing tissues. We also uncovered an aspect of crosstalk between iron homeostasis and cadmium partitioning that is mediated by OPT3. Together, these discoveries provide promising avenues for targeted strategies directed at increasing iron while decreasing cadmium density in the edible portions of crops and improving agricultural productivity in iron deficient soils.     

Anion-independent iron coordination by the Campylobacter jejuni ferric binding protein

Campylobacter jejuni, the leading cause of human gastroenteritis, expresses a ferric binding protein (cFbpA) that in many pathogenic bacteria functions to acquire iron as part of their virulence repertoire. Recombinant cFbpA is isolated with ferric iron bound from Escherichia coli. The crystal structure of cFbpA reveals unprecedented iron coordination by only five protein ligands. The histidine and one tyrosine are derived from the N-terminal domain, whereas the three remaining tyrosine ligands are from the C-terminal domain. Surprisingly, a synergistic anion present in all other characterized ferric transport proteins is not observed in the cFbpA iron-binding site, suggesting a novel role for this protein in iron uptake. Furthermore, cFbpA is shown to bind iron with high affinity similar to Neisserial FbpA and exhibits an unusual preference for ferrous iron (oxidized subsequently to the ferric form) or ferric iron chelated by oxalate. Sequence and structure analyses reveal that cFbpA is a member of a new class of ferric binding proteins that includes homologs from invasive and intracellular bacteria as well as cyanobacteria. Overall, six classes are defined based on clustering within the tree and by their putative iron coordination. The absence of a synergistic anion in the iron coordination sphere of cFbpA also suggests an alternative model of evolution for FbpA homologs involving an early iron-binding ancestor instead of a requirement for a preexisting anion-binding ancestor.     

Iron uptake with ferripyochelin and ferric citrate by Pseudomonas aeruginosa.

Pyochelin is an iron-binding compound produced by Pseudomonas aeruginosa and demonstrates siderophore activity by its involvement in iron transport. During the transport process, an energy-independent association of [55Fe]ferripyochelin with bacteria occurred within the initial 30 s of reaction, followed by an energy-dependent accumulation of iron. The energy-independent association with iron appeared to be at the surface of the bacteria because the iron could be washed from the cells with thioglycolate, whereas accumulated iron was not washed from the bacteria. Energy-independent association of iron with bacteria and energy-dependent accumulation of iron in the presence of ferripyochelin varied concomitantly in cells grown under various conditions, but pyochelin synthesis appeared to be controlled separately. 55Fe complexed with citrate was also taken up by P. aeruginosa with a lower level of initial cell association. Bacterial mechanisms for iron uptake from ferric citrate were present in cells grown in a variety of media and were in lowest levels in cells grown in citrate. The synthesis of bacterial components for iron uptake from ferric citrate and from ferripyochelin was inhibited by high concentrations of iron supplied in growth media.     

Role of ceruloplasmin in macrophage iron efflux during hypoxia

The reticuloendothelial system has a central role in erythropoiesis and iron homeostasis. An important function of reticuloendothelial macrophages is phagocytosis of senescent red blood cells. The iron liberated from heme is recycled for delivery to erythrocyte precursors for a new round of hemoglobin synthesis. The molecular mechanism by which recycled iron is released from macrophages remains unresolved. We have investigated the mechanism of macrophage iron efflux, focusing on the role of ceruloplasmin (Cp), a copper protein with a potent ferroxidase activity that converts Fe2+ to Fe3+ in the presence of molecular oxygen. As shown by others, Cp markedly increased iron binding to apotransferrin at acidic pH; however, the physiological significance of this finding is uncertain because little stimulation was observed at neutral pH. Introduction of a hypoxic atmosphere resulted in marked Cp-stimulated binding of iron to apotransferrin at physiological pH. The role of Cp in cellular iron release was examined in U937 monocytic cells induced to differentiate to the macrophage lineage. Cp added at its normal plasma concentration increased the rate of 55Fe release from U937 cells by about 250%. The stimulation was absolutely dependent on the presence of apotransferrin and hypoxia. Cp-stimulated iron release was confirmed in mouse peritoneal macrophages. Stimulation of iron release required an intracellular "labile iron pool" that was rapidly depleted in the presence of Cp and apotransferrin. Ferroxidase-mediated loading of iron into apotransferrin was critical for iron release because ferroxidase-deficient Cp was inactive and because holotransferrin could not substitute for apotransferrin. The extracellular iron concentration was critical as shown by inhibition of iron release by exogenous free iron, and marked enhancement of release by an iron chelator. Together these data show that Cp stimulates iron release from macrophages under hypoxic conditions by a ferroxidase-dependent mechanism, possibly involving generation of a negative iron gradient.     

Iron and siderophores in fungal–host interactions

Most fungi and bacteria express specific mechanisms for the acquisition of iron from the hosts they infect for their own survival. This is primarily because iron plays a key catalytic role in various vital cellular reactions in conjunction with the fact that iron is not freely available in these environments due to host sequestration. High-affinity iron uptake systems, such as siderophore-mediated iron uptake and reductive iron assimilation, enable fungi to acquire limited iron from animal or plant hosts. Regulating iron uptake is crucial to maintain iron homeostasis, a state necessary to avoid iron-induced toxicity from iron abundance, while simultaneously supplying iron required for biochemical demand. Siderophores play diverse roles in fungal–host interactions, many of which have been principally delineated from gene deletions in non-ribosomal peptide synthetases, enzymes required for siderophore biosynthesis. These analyses have demonstrated that siderophores are required for virulence, resistance to oxidative stress, asexual/sexual development, iron storage, and protection against iron-induced toxicity in some fungal organisms. In this review, the strategies fungi employ to obtain iron, siderophore biosynthesis, and the regulatory mechanisms governing iron homeostasis will be discussed with an emphasis on siderophore function and relevance for fungal organisms in their interactions with their hosts.     

Rhodanese-iron protein association in bovine liver extracts

In semi-crude liver extracts, rhodanese is associated with iron protein. A component purified from mitochondrial extracts exhibits the properties of a rhodanese-apoprotein complex. It can be converted to a rhodanese-iron protein complex by incubation with iron ions, mercaptoethanol, and the sulfur-donor substrate, thiosulfate ion. The protein complex evidences an extinction coefficient close to 5000 per mole of bound iron near 400 nm. Estimates of labile sulfide for these preparations range from 0.6–0.9 mole per mole of bound iron. Furthermore, in the rhodanese-catalyzed thiosulfate-cyanide reaction, iron ion is an inhibitor competitive with cyanide suggesting that iron ion serves as a physiological sulfur-acceptor substrate for the enzyme.     

The Effect of Calcium on Non-heme Iron Uptake,Efflux, and Transport in Intestinal-like Epithelial Cells (Caco-2 Cells)

It has been suggested that calcium inhibits the absorption of dietary iron by directly affecting enterocytes. However, it is not clear if this effect is due to a decreased uptake of iron or its efflux from enterocytes. We studied the effect of calcium on the uptake, efflux, and net absorption of non-heme iron using the intestinal-like epithelial cell line Caco-2 as an in vitro model. Caco-2 cells were incubated for 60 min in a buffer supplemented with non-heme iron (as sulfate) and calcium to achieve calcium to iron molar ratios ranging from 50:1 to 1,000:1. The uptake, efflux, and net absorption of non-heme iron were calculated by following a radioisotope tracer of ⁵⁵Fe that had been added to the buffer. Administration of calcium and iron at molar ratios between 500 and 1,000:1 increased the uptake of non-heme iron and decreased efflux. Calcium did not have an effect on the net absorption of non-heme iron. At typical supplementary doses for calcium and non-heme iron, calcium may not have an effect on the absorption of non-heme iron. The effect of higher calcium to iron molar ratios on the efflux of non-heme iron may be large enough to explain results from human studies.     

Mechanisms of mammalian iron homeostasis

Iron is vital for almost all organisms because of its ability to donate and accept electrons with relative ease. It serves as a cofactor for many proteins and enzymes necessary for oxygen and energy metabolism, as well as for several other essential processes. Mammalian cells utilize multiple mechanisms to acquire iron. Disruption of iron homeostasis is associated with various human diseases: iron deficiency resulting from defects in the acquisition or distribution of the metal causes anemia, whereas iron surfeit resulting from excessive iron absorption or defective utilization causes abnormal tissue iron deposition, leading to oxidative damage. Mammals utilize distinct mechanisms to regulate iron homeostasis at the systemic and cellular levels. These involve the hormone hepcidin and iron regulatory proteins, which collectively ensure iron balance. This review outlines recent advances in iron regulatory pathways as well as in mechanisms underlying intracellular iron trafficking, an important but less studied area of mammalian iron homeostasis.     

The many faces of the octahedral ferritin protein

Iron is an essential trace nutrient required for the active sites of many enzymes, electron transfer and oxygen transport proteins. In contrast, to its important biological roles, iron is a catalyst for reactive oxygen species (ROS). Organisms must acquire iron but must protect against oxidative damage. Biology has evolved siderophores, hormones, membrane transporters, and iron transport and storage proteins to acquire sufficient iron but maintain iron levels at safe concentrations that prevent iron from catalyzing the formation of ROS. Ferritin is an important hub for iron metabolism because it sequesters iron during times of iron excess and releases iron during iron paucity. Ferritin is expressed in response to oxidative stress and is secreted into the extracellular matrix and into the serum. The iron sequestering ability of ferritin is believed to be the source of the anti-oxidant properties of ferritin. In fact, ferritin has been used as a biomarker for disease because it is synthesized in response to oxidative damage and inflammation. The function of serum ferritin is poorly understood, however serum ferritin concentrations seem to correlate with total iron stores. Under certain conditions, ferritin is also associated with pro-oxidant activity. The source of this switch from anti-oxidant to pro-oxidant has not been established but may be associated with unregulated iron release from ferritin. Recent reports demonstrate that ferritin is involved in other aspects of biology such as cell activation, development, immunity and angiogenesis. This review examines ferritin expression and secretion in correlation with anti-oxidant activity and with respect to these new functions. In addition, conditions that lead to pro-oxidant conditions are considered.     

Iron in bone marrow

In the bone-marrow, non-haemoglobin iron can predominantly be found in the reticulum. Slight granules containing iron can also be observed in parts of erythroblasts by means of the Berlin blue reaction. These cells are called sideroblasts. In chemical respect, non-haemoglobin iron consists of ferritin soluble in water and haemosiderin insoluble in water. Erythroblasts will only take their iron from plasma transferrin. For the most part, this iron uptake is being regulated by erythropoietin adapting erythropoiesis to the oxygen requirements of the tissue. The iron contained in erythroblasts is predominantly utilized for haemoglobin synthesis in these cells. A slight part is being taken up by ferritin. The bone-marrow reticulum will phagocytise aged erythrocytes and store liberated iron as ferritin and haemosiderin. Part of the iron is being delivered again to plasma transferrin. With constant serum iron level the liberation of iron from the reticulo-endothelial tissue must correspond to the iron uptake by erythropoiesis. The absence of iron capable of being coloured in the bone-marrow reticulum is considered to be a reliable parameter of iron deficiency. It enables the diagnosis of iron deficiency anaemia to be made even in those patients with serum iron level and a total iron binding capacity lying within the normal range and no hypochromia of erythrocytes being present. It enables iron deficiency anaemia to be separated from sideropenic anaemia with reticulo-endothelial siderosis in differential-diagnostic manner. Even in patients with sideroblastic anaemia, iron colouring of bone-marrow smears is required for ensuring the diagnosis. Recently, a separation has also been made for idiopathic anaemia with abnormal sideroblasts. In these patients there is an increased risk for acute leukemia to develop.     

希瓦氏菌铁稳态及调控的研究进展

铁元素通常以蛋白辅因子的形式参与一系列重要的生命过程,是绝大多数生命必需的营养物质。在细菌生命过程中,一方面铁短缺是必须克服的严峻挑战,另一方面铁过量又会危及生命。铁的这种二元性质要求细菌必须严格保持体内的铁稳态。当前革兰氏阴性菌铁稳态的作用模式及理解主要基于肠道细菌大肠杆菌的长期探索成果。近年来,在环境细菌中开展的相关研究揭示了革兰氏阴性菌的铁稳态机制存在出乎意料的多样性:细菌中铁稳态相关的生物途径及组成蛋白、关键调控系统的生理影响以及铁稳态与其他生物过程的相互影响等方面都显示不同菌种的生存和进化特征。本综述以希瓦氏菌中的相关发现为基础,分析总结革兰氏阴性菌铁稳态重要途径及其组成的多样性、不同途径的相互影响以及调控因子的生理影响和调控机理等方面的研究进展和未解决的问题,以期为革兰氏阴性菌铁稳态的研究提供参考。     

Iron absorption in the iron-deficient rat

Iron absorption in the iron-deficient rat was compared with that in the normal rat to better understand the regulation of this dynamic process. It was found that: Iron uptake by the iron-deficient intestinal mucosa was prolonged as a result of slower gastric release, particularly when larger doses of iron were employed. The increased mucosal uptake of ionized iron was not the result of increased adsorption, but instead appeared related to a metabolically active uptake process, whereas the increased mucosal uptake of transferrin iron was associated with increased numbers of mucosal cell membrane transferrin receptors. Mucosal ferritin acted as an iron storage protein, but its iron uptake did not explain the lower iron absorption in the normal rat. Iron loading the mucosal cell (by presenting a large iron dose to the intestinal lumen) decreased absorption for 3 to 4 days. Iron loading of the mucosal cell from circulating plasma transferrin was proportionate to the plasma iron concentration. Mucosal iron content was the composite of iron loading from the lumen and loading from plasma transferrin versus release of iron into the body. These studies imply that an enhanced uptake-throughout mechanism causes the increased iron absorption in the iron-deficient rat. Results were consistent with the existence of a regulating mechanism for iron absorption that responds to change in mucosal cell iron, which is best reflected by mucosal ferritin.     

A new role for heme, facilitating release of iron from the bacterioferritin iron biomineral

Bacterioferritin (BFR) from Escherichia coli is a member of the ferritin family of iron storage proteins and has the capacity to store very large amounts of iron as an Fe(3+) mineral inside its central cavity. The ability of organisms to tap into their cellular stores in times of iron deprivation requires that iron must be released from ferritin mineral stores. Currently, relatively little is known about the mechanisms by which this occurs, particularly in prokaryotic ferritins. Here we show that the bis-Met-coordinated heme groups of E. coli BFR, which are not found in other members of the ferritin family, play an important role in iron release from the BFR iron biomineral: kinetic iron release experiments revealed that the transfer of electrons into the internal cavity is the rate-limiting step of the release reaction and that the rate and extent of iron release were significantly increased in the presence of heme. Despite previous reports that a high affinity Fe(2+) chelator is required for iron release, we show that a large proportion of BFR core iron is released in the absence of such a chelator and further that chelators are not passive participants in iron release reactions. Finally, we show that the catalytic ferroxidase center, which is central to the mechanism of mineralization, is not involved in iron release; thus, core mineralization and release processes utilize distinct pathways.     

Lack of Plasma Protein Hemopexin Results in Increased Duodenal Iron Uptake

Purpose

The body concentration of iron is regulated by a fine equilibrium between absorption and losses of iron. Iron can be absorbed from diet as inorganic iron or as heme. Hemopexin is an acute phase protein that limits iron access to microorganisms. Moreover, it is the plasma protein with the highest binding affinity for heme and thus it mediates heme-iron recycling. Considering its involvement in iron homeostasis, it was postulated that hemopexin may play a role in the physiological absorption of inorganic iron.

Methods and Results

Hemopexin-null mice showed elevated iron deposits in enterocytes, associated with higher duodenal H-Ferritin levels and a significant increase in duodenal expression and activity of heme oxygenase. The expression of heme-iron and inorganic iron transporters was normal. The rate of iron absorption was assessed by measuring the amount of ⁵⁷Fe retained in tissues from hemopexin-null and wild-type animals after administration of an oral dose of ⁵⁷FeSO₄ or of ⁵⁷Fe-labelled heme. Higher iron retention in the duodenum of hemopexin-null mice was observed as compared with normal mice. Conversely, iron transfer from enterocytes to liver and bone marrow was unaffected in hemopexin-null mice.

Conclusions

The increased iron level in hemopexin-null duodenum can be accounted for by an increased iron uptake by enterocytes and storage in ferritins. These data indicate that the lack of hemopexin under physiological conditions leads to an enhanced duodenal iron uptake thus providing new insights to our understanding of body iron homeostasis.     

Sulfide is an efficient iron releasing agent for mammalian ferritins

The most prominent role of mammalian ferritins is to provide an extensive iron-buffering capacity to cells. The large ferritin iron stores can be mobilized in vitro, but the functional relevance of the most efficient iron releasing agents remains elusive. Sulfide is a strongly reducing chemical generated by a series of enzymes. In the presence of limited amounts of sulfide a continuous rate of iron release from ferritin was observed and a majority of the protein iron core was recovered in solution. The rate constants for iron efflux triggered by several reducing or chelating compounds have been measured and compared. Although not as efficient as reduced flavins, sulfide displayed kinetic parameters which suggest a potential physiological role for the chalcogenide in converting the iron storage protein into apoferritin. To further probe the relevance of sulfide in the mobilization of iron, several enzymes, such as NifS, rhodanese, or sulfite reductase generating reduced forms of sulfur by different mechanisms, have been assayed for their ability to catalyze the release of iron from ferritin. The results show that full reduction of sulfur into sulfide is needed to deplete iron from ferritin. These reactions suggest links between sulfur metabolism and intracellular iron homeostasis.