Effect of Ca2+ and Mg2+ on the uptake of Fe3+ by mouse intestinal mucosa

Initial Fe3+ uptake rates by mouse intestinal fragments were determined in vitro. Uptake was dependent primarily on the Fe3+-nitrilotriacetate complex concentration. Addition of Ca2+ and Mg2+ to the incubation medium had only small effects on the Fe3+ uptake rate. Duodenal fragments from hypoxic animals showed enhanced uptake of Fe3+; this increase was more pronounced with a divalent cation-free medium. Ca2+ markedly diminished the Fe3+ uptake by mucosa from hypoxic mice; Mg2+ had no appreciable effect. Distal ileal fragments exhibited lower uptake rates compared to the duodenum, but were more sensitive to the effects of added Ca2+. The ileal fragments did not show an adaptive response of Fe3+ uptake to hypoxia. These results suggest the existence of more than one pathway for mucosal Fe3+ uptake. One pathway, sensitive to Ca2+ and not stimulated by hypoxia, may be present in the duodenum and ileum. A second pathway, inhibited by Ca2+ and exhibiting an adaptive response to hypoxia, occurs only in the duodenum. This latter pathway is more sensitive to the effects of metabolic inhibitors.     

Comparison of 59Fe3+ uptake in vitro and in vivo by mouse duodenum

Initial rates of 59Fe3+ uptake by mouse duodenal fragments (in vitro) and tied-off duodenal segments (in vivo) have been characterised for control and hypoxic animals. 59Fe3+ uptake by duodenal fragments was rapid, selective and dependent on medium Fe3+-nitrilotriacetate concentration. Most of the 59Fe3+ uptake (70-75%) occurred via the mucosal route and was dependent on the metabolic state of the tissue. Mucosal uptake showed an adaptive increase following exposure of animals to 3 days hypoxia; the enhancement was due to a 2-3-fold increase in Vmax app, without any significant changes in the Km app. Studies of upper small intestine transit times showed a mean residence time of 4-5 min for 59Fe-labelled mouse chow, emphasising the importance of initial uptake measurements. Time courses for in vivo total mucosal uptake exhibited linearity over a wide variety of absorption rates after correction for the permeation by intact metal-chelate complex. The corrected uptake showed a hyperbolic dependence on medium Fe3+-nitrilotriacetate concentration. Kinetic studies revealed a 2-3-fold increase in total mucosal uptake in hypoxia. Mucosa-to-carcass transfer of 59Fe was also markedly increased by chronic hypoxia. The in vitro system exhibits similar qualitative and quantitative kinetics for Fe3+ transport via the mucosal membrane to those obtained in vivo. The results observed in vitro are thus valid and provide a convenient method for further studies on Fe3+ transport in animals and in man.     

Mouse intestinal Fe3+ uptake kinetics in vivo. The significance of brush-border membrane vesicle transport in the mechanism of mucosal Fe3+ uptake

Initial rates of mucosal uptake of Fe3+ from luminal Fe3+-nitrilotriacetate solutions by tied segments of mouse intestine in vivo have been measured. Duodenal uptake showed an approximately hyperbolic dependence of uptake on Fe3+ complex concentration (Km(app) 66 microM, Vmax 6.2 pmol/min per mg intestine) with little dependence on nitrilotriacetate:Fe3+ ratio or on added Ca2+. Duodenal uptake was greatly stimulated by hypoxic treatment of mice. Uptake rates by distal ileum were lower than by duodenum and more sensitive to added Ca2+. These results show that isolated duodenal brush-border membrane Fe3+ transport characteristics (Simpson, R.J. and Peters, T.J. (1984) Biochim. Biophys. Acta 772, 220-226) are inadequate to explain duodenal Fe3+ uptake in vivo. However, ileal uptake can be explained by the properties of isolated ileal brush-border membrane (Simpson, R.J., Raja, K.B. and Peters, T.J. (1985) Biochim. Biophys. Acta 814, 8-12).     

Membrane potential dependence of Fe(III) uptake by mouse duodenum

Intestinal iron uptake by mouse duodenal fragments is inhibited in the absence of oxygen and glucose from the incubation medium and by a variety of metabolic inhibitors. The mechanism of energy coupling to iron uptake is, however, unclear. In vitro experiments using duodenal fragments showed Fe3+ uptake to be markedly inhibited, in a reversible fashion, by the replacement of incubation medium Na+ by K+. Addition of phloridzin to the medium failed to affect iron uptake, suggesting that the above effect was not a consequence of reduced glucose uptake. Substitution of Na+ by Rb+ also potently reduced duodenal iron uptake. Replacement of medium NaCl by either mannitol or choline chloride had no significant effect on Fe3+ uptake, thus excluding the possibility of the Fe3+ uptake process being Na+-dependent. Similar observations were made with duodenal fragments from animals with enhanced Fe3+ absorption, due to chronic hypoxia. Valinomycin (1-5 microM) increased the uptake of both glucose and Fe3+. Higher concentrations (22.5 microM) of the ionophore were inhibitory. In vivo studies (tied-off segments) using Rb+-containing medium confirmed the inhibitory effects of univalent cations on Fe3+ absorption. Enhanced absorption of Fe3+ was also demonstrable in vivo, with low concentrations of valinomycin and nigericin added to the luminal medium. These observations suggest that the Fe3+ uptake process may be dependent on the brush-border membrane potential.     

Fe3+ transport by brush-border membrane vesicles isolated from normal and hypoxic mouse duodenum and ileum

Studies of 59Fe3+ uptake by brush-border membrane vesicles prepared from mouse duodenum have indicated that uptake represents transport across the brush-border membrane which is rate-limited by the membrane-transfer step (Simpson, R.J. and Peters, T.J. (1984) Biochim. Biophys. Acta 772, 220-226). Further studies presented here reveal that the uptake rate represents the net influx rate for Fe3+ and is independent of Na+ in the medium and of the method of vesicle preparation. Uptake by brush-border membrane vesicles prepared from mouse distal ileum also represents predominantly transport and is higher than that observed with duodenal brush-border membrane vesicles. Studies of the initial uptake rate by vesicles prepared from normal and hypoxic mouse intestine demonstrated an increase in Fe3+ transport in duodenal vesicles only.     

Mucosal surface ferricyanide reductase activity in mouse duodenum

Mouse duodenum possesses mucosal surface ferricyanide reductase activity. The reducing activity, determined in vitro by measuring ferrocyanide production from ferricyanide, was found to be greater in duodenal fragments when compared with ileal fragments. Experiments with right-side out tied-off duodenal sacs show that reduction occurs mainly on the mucosal side and indicates that the reducing activity is associated with the brush border membrane. Experiments using mice with increased levels of iron absorption (hypoxic, iron-deficient) showed corresponding increases in reducing activity. The increase was present in duodenal but not ileal fragments. Inhibitor studies showed no effect of several compounds which inhibit other, more characterized, transplasma membrane reductases. In particular, doxorubicin (10 m) and quinacrine (1 mm) were without effect on duodenal mucosal transplasma membrane reducing activity. Depolarization of the membrane potential with high medium K ⁺ inhibited reducing activity. N-ethyl malemide (1 mm) was a potent inhibitor, but iodoacetate was found to be less inhibitory. Comparision with inhibitory effects on glyceraldehyde-3-phosphate dehydrogenase (GAPDH) demonstrated that the effect of N-ethyl malemide on reducing activity was not secondary to GAPDH. Collectively these results indicate that mouse duodenum possesses mucosal surface transplasma membrane ferricyanide reductase activity and that the activity is correlated with the process of intestinal iron absorption. Furthermore, the reducing activity appears to be distinct from other reported transplasma membrane reductases.     

Iron absorption and hepatic iron uptake are increased in a transferrin receptor 2 (Y245X) mutant mouse model of hemochromatosis type 3

Hereditary hemochromatosis type 3 is an iron (Fe)-overload disorder caused by mutations in transferrin receptor 2 (TfR2). TfR2 is expressed highly in the liver and regulates Fe metabolism. The aim of this study was to investigate duodenal Fe absorption and hepatic Fe uptake in a TfR2 (Y245X) mutant mouse model of hereditary hemochromatosis type 3. Duodenal Fe absorption and hepatic Fe uptake were measured in vivo by 59Fe-labeled ascorbate in TfR2 mutant mice, wild-type mice, and Fe-loaded wild-type mice (2% dietary carbonyl Fe). Gene expression was measured by real-time RT-PCR. Liver nonheme Fe concentration increased progressively with age in TfR2 mutant mice compared with wild-type mice. Fe absorption (both duodenal Fe uptake and transfer) was increased in TfR2 mutant mice compared with wild-type mice. Likewise, expression of genes participating in duodenal Fe uptake (Dcytb, DMT1) and transfer (ferroportin) were increased in TfR2 mutant mice. Nearly all of the absorbed Fe was taken up rapidly by the liver. Despite hepatic Fe loading, hepcidin expression was decreased in TfR2 mutant mice compared with wild-type mice. Even when compared with Fe-loaded wild-type mice, TfR2 mutant mice had increased Fe absorption, increased duodenal Fe transport gene expression, increased liver Fe uptake, and decreased liver hepcidin expression. In conclusion, despite systemic Fe loading, Fe absorption and liver Fe uptake were increased in TfR2 mutant mice in association with decreased expression of hepcidin. These findings support a model in which TfR2 is a sensor of Fe status and regulates duodenal Fe absorption and liver Fe uptake.     

Subcellular localization of recently-absorbed iron in mouse duodenal enterocytes: identification of a basolateral membrane iron-binding site

The subcellular distribution of newly absorbed iron in isolated mouse duodenal enterocytes was investigated by analytical subcellular fractionation using sucrose density gradient centifugation. Two major peaks of mucosal 59Fe activity were observed: one soluble and one particulate (density 1.18-1.20 g ml-1). The latter was increased following prior exposure of animals to chronic hypoxia. The particulate 59Fe was localized to the basolateral membranes using the marker enzyme Na+, K+ activated, Mg2+ dependent, ATPase and by washing intact enterocytes with the selective plasma membrane perturbant digitonin. The basolateral membrane can be selectively labelled by in vitro incubation of intact enterocytes at 0 degrees C with 59Fe(III)-nitrilotriacetate complex, confirming the presence of a 59Fe binding site on this membrane. No significant difference in in vitro iron binding to this site was observed between normal and chronically hypoxic animals. Iron binding to the basolateral membrane was significantly higher in disrupted, compared to intact enterocytes, indicating that this site is present on both sides of the basolateral membrane. It is therefore suggested that the increased labelling of this site in hypoxia, in vivo, is a consequence of an increase in a mucosal Fe pool which is available for binding to a membrane receptor.     

Iron homeostasis is maintained in the brain, but not the liver, following mild hypoxia

Alterations in iron metabolism or oxidative damage in response to hypoxic incidents have been examined following re-oxygenation of the hypoxic tissue. To understand the consequences of decreased tissue oxygen on iron load, metal-catalyzed redox activity and oxidative modifications in isolation from re-oxygenation, the present study exposed mice to either normoxia, or mild hypoxia (380 Torr; approximately 10% normobaric oxygen) where the tissue was not allowed to re-oxygenate prior to examination. Brain, liver and skeletal muscle were examined for Fe3+ load, metal-catalyzed redox activity and oxidative modifications to proteins (N(epsilon)-(carboxymethyl)lysine), lipids (4-hydroxynonenal pyrrole) and nucleic acids (8-hydroxyguanosine). Hypoxia induced a 43% increase in the iron content of the liver (P < 0.001) as determined by ICP-MS and a 3.8-fold increase in Fe3+ load (P < 0.001) as determined by Perl's stain. There was a corresponding 2-fold increase in metal-catalyzed redox activity (P < 0.01) in the liver, but no change in the expression of oxidative markers. In contrast, non-significant increases in Fe3+ and metal-catalyzed redox activity were observed in the cerebral cortex, and molecular and granular layers of the hippocampus and cerebellum. Interestingly, hypoxia significantly decreased oxidative modifications to proteins and lipids, but not nucleic acids in most brain regions examined. In addition, hypoxia did not alter the Fe content of skeletal muscle, or the contents of Zn, Cu, Ni or Mn in liver, skeletal muscle, cerebral cortex or hippocampus. Together, these results indicate that there is a tighter regulation of iron metabolism in the brain than the liver, which limits the redistribution of Fe3+ following hypoxia.     

Studies of Fe3+ transport across isolated intestinal brush-border membrane of the mouse

Mouse intestinal brush-border membrane vesicles take up iron from media containing 59Fe3 +-nitrilotriacetic acid. The iron uptake by the vesicles represents accumulation of iron which relates to an osmotically active space. Uptake is linearly related to vesicle protein concentration and is inhibited by low incubation temperature and low medium free Fe3+ concentrations. Experiments with the lipid soluble iron ligand 8-hydroxyquinoline and with Triton X-100 imply that the uptake is rate limited by membrane transport.     

Iron and cadmium uptake by duodenum of hypotransferrinaemic mice

Absorption from food is an important route for entry of the toxic metal, cadmium, into the body. Both cadmium and iron are believed to be taken up by duodenal enterocytes via the iron regulated, proton-coupled transporter, DMT1. This means that cadmium uptake could be enhanced in conditions where iron absorption is increased. We measured pH dependent uptake of ¹⁰⁹Cd and ⁵⁹Fe by duodenum from mice with an in vitro method. Mice with experimental (hypoxia, iron deficiency) or hereditary (hypotransferrinaemia) increased iron absorption were studied. All three groups of mice showed increased ⁵⁹Fe uptake (p<0.05) compared to their respective controls. Hypotransferrinaemic and iron deficient mice exhibited an increase in ¹⁰⁹Cd uptake (p<0.05). Cadmium uptake was not, however, increased by lowering the medium pH from 7.4 to 6. In contrast, ⁵⁹Fe uptake (from ⁵⁹FeNTA₂) and ferric reductase activity was increased by lowering medium pH in control and iron deficient mice (p<0.05). The data show that duodenal cadmium uptake can be increased by hereditary iron overload conditions. The uptake is not, however, altered by lowering medium pH suggesting that DMT1-independent uptake pathways may operate.     

High-fat diet causes iron deficiency via hepcidin-independent reduction of duodenal iron absorption

Obesity is often associated with disorders of iron homeostasis; however, the underlying mechanisms are not fully understood. Hepcidin is a key regulator of iron metabolism and may be responsible for obesity-driven iron deficiency. Herein, we used an animal model of diet-induced obesity to study high-fat-diet-induced changes in iron homeostasis. C57BL/6 mice were fed a standard (SD) or high-fat diet (HFD) for 8 weeks, and in addition, half of the mice received high dietary iron (Fe+) for the last 2 weeks. Surprisingly, HFD led to systemic iron deficiency which was traced back to reduced duodenal iron absorption. The mRNA and protein expressions of the duodenal iron transporters Dmt1 and Tfr1 were significantly higher in HFD- than in SD-fed mice, indicating enterocyte iron deficiency, whereas the mRNA levels of the duodenal iron oxidoreductases Dcytb and hephaestin were lower in HFD-fed mice. Neither hepatic and adipose tissue nor serum hepcidin concentrations differed significantly between SD- and HFD-fed mice, whereas dietary iron supplementation resulted in increased hepatic hepcidin mRNA expression and serum hepcidin levels in SD as compared to HFD mice. Our study suggests that HFD results in iron deficiency which is neither due to intake of energy-dense nutrient poor food nor due to increased sequestration in the reticulo-endothelial system but is the consequence of diminished intestinal iron uptake. We found that impaired iron absorption is independent of hepcidin but rather results from reduced metal uptake into the mucosa and discordant oxidoreductases expressions despite enterocyte iron deficiency.     

Fe2+ uptake by mouse intestinal mucosa in vivo and by isolated intestinal brush-border membrane vesicles

In vivo kinetics of mucosal uptake of luminal ⁵⁹Fe²⁺ by tied segments of normal mouse duodenum are characterised by a K_m of approx. 100 μM and a V_max of approx. 9 pmol/min per mg wet weight of intestine. These values were determined at pH 7.25 in the presence of excess sodium ascorbate. Studies with luminal Fe²⁺ concentrations of 100 μM reveal: (1) uptake is relatively independent of ascorbate: Fe ratio and luminal pH and (2) uptake is potently inhibited by 1 mM Co²⁺ or Mn²⁺ and large luminal NaCl concentrations but not by Ca²⁺. 3 days of hypoxia (0.5 atmospheres) yields no significant increase in subsequent total mucosal uptake by in vivo tied segments while uptake is significantly reduced by semi-starvation. Quantitative comparison of in vivo mucosal uptake with subsequent determination of isolated brush-border membrane ⁵⁹Fe²⁺ transport in individual mice reveals a positive correlation (P < 0.01) between the two parameters. These results, in conjunction with studies of isolated mouse duodenal brush-border membrane (Simpson, R.J. and Peters, T.J. (1985) Biochim. Biophys. Acta, 814, 381–388 and (1986) Biochim. Biophys. Acta 856, 109–114) suggest that the Fe²⁺ transport properties of isolated brush-border membrane are quantitatively adequate to explain in vivo mucosal uptake in normal and hypoxic mice at Fe²⁺ concentrations up to 100 μM.     

Comparison of changes in uptake and mucosal processing of iron in short and long-term iron depletion

Thirty minutes following an intragastric dose of [59]Fe, rats subjected to short-term and long-term iron depletion showed a similar increase in [59]Fe in plasma and a similar decrease in the retention of [59]Fe in mucosal cytosol compared to controls. With both low-iron groups, a two-fold increase in [59]Fe uptake by brush-border membrane vesicles and a six-fold reduction in the [59]Fe incorporated into the ferritin of the mucosal cytosol were observed. These studies indicate that short-term exposure to a low-iron diet triggers changes in both the uptake of iron by the brush-border membrane and the processing of iron within the mucosal cell prior to major changes in body iron status.     

Intestinal absorption of cobalt and iron: mode of interaction and subcellular distribution.

1. The absorption kinetic of 59Fe-(FeCl3) and 60CO-(CoCl2) 10 min after administration of increasing doses (0.5--1,000 nmoles metal) into tied-off duodenal segments of normal and iron-deficient rats shows saturation characteristic for both metals; in iron-deficient rats the absorption of both metals was enhanced. 2. The addition of increasing amounts of cobalt to the 59Fe-containing test solutions caused a decrease of the absorption of iron. 3. The study of the time dependence of this interaction in iron-deficient rats revealed, that cobalt inhibits the release of iron from mucosal cells into the blood, whereas the uptake of iron from the lumen into the mucosal cells did not differ from the controls without administration of cobalt. 4. The subcellular distribution of 59Fe and 60 Co in mucosal cell homogenates of iron-deficient rats after ultracentrifugation on a polyvinylpyrrolidone-CsCl solution shows a similar pattern for both metals; in the presence of cobalt the subcellular distribution of 59Fe is not changed. 5. From these results the conclusion is drawn that cobalt inhibits iron absorption not by an interference with iron binding sites on or in the luminal membranes of the mucosal cells but by an interaction with the releasing process at the contraluminal side.     

Rhythmic iron stress reactions in sunflower at suboptimal iron supply

Uptake and translocation of labelled iron were studied in sunflower ( Helianthus annuus L. cv. Sobrid) grown in nutrient solution with low FeEDDHA concentrations during preculture. In contrast to conditions for plants adequately supplied with iron, suboptimal iron supply leads to temporary Fe stress with rhythmic rates of uptake and translocation of iron (period 2–4 days). This rhythmic behaviour of iron uptake is associated with corresponding changes in morphology (thickening of root tips) and physiology (increase in reducing capacity) of the roots. Iron stress is alleviated within less than one day if sufficient iron is available. This is indicated by normalisation of root morphology, reducing capacity and rate of iron uptake and translocation. This rhythm in iron uptake stresses the importance of rhythmic patterns of biochemical behaviour in complex biological systems. It is suggested that phytohormones are involved in the transformation of the iron nutritional status of the shoot apex into a "signal" for the uptake sites of iron in the roots. Preliminary experiments with sunflower in calcareous soil indicate an ecological importance of this fine regulation mechanism for plants on soil with a low iron availability, manifested in rhythmic iron stress reactions.     

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.     

Significance of non-esterified fatty acids in iron uptake by intestinal brush-border membrane vesicles

Iron uptake from Fe/ascorbate by mouse brush-border membrane vesicles is not greatly inhibited by prior treatment with a variety of protein-modification reagents or heat. Non-esterified fatty acid levels in mouse proximal small intestine brush-border membrane vesicles show a close positive correlation with initial Fe uptake rates. Loading of rabbit duodenal brush-border membrane vesicles with oleic acid increases Fe uptake. Depletion of mouse brush-border membrane vesicle fatty acids by incubation with bovine serum albumin reduces Fe uptake. Iron uptake by vesicles from Fe/ascorbate is enhanced in an O2-free atmosphere. Iron uptake from Fe/ascorbate and Fe3+-nitrilotriacetate (Fe3+-NTA) were closely correlated. Incorporation of oleic acid into phosphatidylcholine/cholesterol (4:1) liposomes leads to greatly increased permeability to Yb3+, Tb3+, Fe2+/Fe3+ and Co2+. Ca2+ and Mg2+ are also transported by oleic acid-containing liposomes, but at much lower rates than transition and lanthanide metal ions. Fe3+ transport by various non-esterified fatty acids was highest with unsaturated acids. The maximal transport rate by saturated fatty acids was noted with chain length C14-16. It is suggested that Fe transport can be mediated by formation of Fe3+ (fatty acid)3 complexes.     

Iron assimilation in Chlamydomonas reinhardtii involves ferric reduction and is similar to Strategy I in higher plants

The mechanism of adaptation to Fe-deficiency stress was investigated in the unicellular green alga, Chlamydomonas reinhardtii. Upon removal of nutritional Fe, the activity of a cell surface Fe(III)-chelate reductase was increased by at least 15-fold within 24 h. This increase was negatively corelated with the Fe concentration in the growth media. Incubation of cells in the presence of the Fe²⁺-specific chelator, bathophenanthrolinedisulphonic acid, led to an increased Fe³⁺ reductase activity, even when sufficient Fe was present. Growth of cells in Cu-free media for 48 h led to no statistically significant increase in Fe³⁺ reductase activity. The Fe(III)-chelate reductase activity in Fe-starved cells was saturable with an apparent Km of 31 M and was inhibited by uncouplers of the transmembrane proton gradient but not by SH-specific reagents.Fe uptake was only observed in Fe-deficient cells. Uptake was specific for Fe in that at 100-fold excess of a number of metal ions in the transport assay did not inhibit uptake activity. However, a 100-fold excess of Cu resulted in a 87% inhibition of Fe uptake. The Vmax for Fe³⁺ reduction activity was 250-fold greater than for Fe uptake; although the Km values for both processes differed by only 10-fold. Thus, the rate limiting step in Fe assimilation was transport and not reduction. These results indicate that Fe assimilation in C. reinhardtii involves a reductive step and thus resembles the mechanism of Fe uptake in Strategy I higher plants.Keywords: Ferric chelate reduction, iron assimilation, iron uptake, unicellular green algae, Chlamydomonas.      

Effect of orally-administered epidermal growth factor on intestinal iron absorption and mucosal permeability

A progressive increase in intestinal 59Fe3+ absorption was observed on oral feeding of mice with physiological doses of EGF/UGO. Maximal changes were apparent after 3d and appeared to be dose-dependent. In addition to a small increase in intestinal cell proliferation, as reflected by increased ornithine decarboxylase activity, EGF/UGO-feeding increased mucosal permeability (evaluated with [51Cr]-EDTA): the latter could account for the increase in iron absorption. Sialoadenectomy, to remove the major source of endogenous EGF/UGO, had no appreciable effect on the intestinal absorption of iron.