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Mucosal iron-binding proteins in mice with X-linked anaemia.

The mouse with X-linked anaemia [sla] has a defect in iron absorption which can be temporarily reversee by feeding a low iron diet. Duodenal non-haem iron was significantly higher in the sla than in the normal mouse on an iron supplemented diet but non-haem iron was reduced to minute amounts when the mice were fed a low iron diet. Gel chromatography on Sephadex G-200 of th partial-free supernatant of pooled mucosal homogenates revealed the presence of three proteins binding 59Fe. Fraction I [mol wt 450 000] resembled ferritin and was present in both normal and sla mice fed an iron supplemented diet. Fraction II [mol wt 78 ooo] eluted in a similar position to transferrin and was evident in both normal and sla mice fed an iron deficient diet. Fraction III [mol wt less than 15 000] contained equivalent amounts of radioiron in normal and sla mice fed the iron deficient diet, whereas this fraction contained less radioactivity in sla animals in two of three experiments in which the animals were fed an iron supplemented diet. The iron transport defect in sla mice does not appear to reside in the iron-binding proteins in the supernatant fraction of the intestinal mucosa and the cause of the defect in iron absorption remains to be elucidated.

Anemia, Hypochromic↗

Liquid scintillation counting of 55Fe applied to air-filter samples.

A simple and rapid method has been improved for determination of low specific activity of 55Fe with a liquid scintillation counter. High counting efficiency was obtained for a sample containing up to 150 mg of iron using mixture of a colorless solution of phosphate iron complex and an emulsifier liquid scintillator. The detection limit was 0.31 Bq (8.4 pCi) per gram iron assuming the counting for 1000 minutes and 95% confidence level. This counting method was applied to determination of 55Fe in air-filter samples.

Air Pollutants↗

Iron metabolism of Escherichia coli studied by Mössbauer spectroscopy and biochemical methods.

To date it has barely been recognized that the nature of about 75% of the Escherichia coli iron pool is unknown. Here we report the isolation of two iron species representing major components of iron metabolism in various growth states of E. coli. In vivo Mössbauer spectroscopy was applied to obtain information on the intracellular distribution pattern of iron in E. coli K12 W3110. Only two types of iron could be detected in the cell spectra: hexacoordinated Fe2+ and Fe3+ high-spin complexes. Other iron-requiring compounds are at least one order of magnitude less abundant in E. coli. The Mössbauer parameters of these complexes fit neither cytochromes nor iron-sulfur proteins nor ferric holo-bacterioferritin. They are sensitive to metabolic changes and inhibitors. The ratio of Fe/subunit, Fe2+/Fe3+ interconversion, chromatographic and electrophoretic data exclude bacterioferritin as the main iron metabolite in E. coli. Bacterioferritin can be observed only at very high ferric ion concentrations in the medium. The 55Fe fluorograms of both cytoplasmic and membrane fractions exhibit two exclusive bands with apparent molecular masses of 17 and 15 kDa, respectively. The two bands comprised 70% of the applied radioactivity. In gel filtration the main iron peak elutes at 155 kDa yielding two bands with apparent molecular masses of 17 and 15 kDa on SDS/PAGE. We therefore conclude that the iron species form a protein with an apparent molecular mass of 155 kDa containing 17-kDa and 15-kDa subunits. The iron content of the protein is 44 micrograms Fe/mg protein which corresponds to approximately 13 iron ions/subunit. No iron protein exhibiting the observed features has been described so far. Additional Mössbauer experiments suggest that these novel iron proteins are not restricted to E. coli but that similar components are detectable in several bacterial and fungal systems, thus pointing to a general occurrence.

Bacterial Proteins↗

Effects of diet and development upon the uptake and distribution of cerebral iron.

In order to determine whether iron sequestered by the rat brain during the third week of postnatal life could be mobilized by subsequent dietary iron deficiency (ID), iron-59 (59Fe) was administered to rats at 2 weeks of age. The animals were placed on an ID or a control diet from age 4 through 8 weeks and killed by perfusion. Brain radioactivity was identical for both groups, and autoradiography revealed no differences in the distribution of radioactivity. Thus, neither the sequestration of cerebral iron acquired at age 2 weeks nor its subsequent redistribution was affected by ID. Since ID beginning after age 3 weeks reportedly produces a cerebral iron deficit that is in part reversible, an attempt was made to determine whether 59Fe administered after ID was preferentially delivered to any brain region. Rats were placed on an ID or a control diet from age 3 through 7 weeks and then injected with 59Fe, placed on a normal diet, and killed 2 weeks later. Thre was no difference between groups in amount or distribution of brain 59Fe, except in the choroid plexus, which was more radioactive in the ID rats than in the controls. This finding may represent a mechanism by which the choroid plexus buffers the brain against rapid rises in plasma iron content.

Animals↗

Influence of physicochemical characteristics of freshwater on artificial radioactivity content.

An intensive study was designed to determine the activity of different radionuclides in water, including strontium-90 (90Sr), cesium-134 (134Cs), cesium-137 (137Cs), plutonium-239-240 (239+240Pu), and tritium (3H). Activity levels detected were between 0.6 and 21.3 mBq/L for 90Sr; less than 0.5, 1.4, and 327 Bq/L for 134Cs, 137Cs, and 3H, respectively; and between 0.14 and 21 microBq/L for 239+240Pu. Other nonradioactive parameters were measured including pH; dry residue: conductivity; calcium concentration, [Ca++]; magnesium concentration, [Mg++]; potassium concentration, [K+]; iron(II) and (III) concentration, [Fe2+,3+]; and ammonium concentration [NH4+]. Only the aquifer corresponding to the refrigeration reservoir of the nuclear power plant of Almaraz (Extremadura, Spain) showed greater-than-average concentrations of 3H and 239+240Pu compared with those found in the remaining aquifers. The greater presence of dissolved Fe in the waters analyzed clearly indicated greater activity associated with 90Sr, 137Cs, and 239+240Pu in dissolution. In addition, the water samples that were highly mineralized aided the dissolution of 90Sr and (to a lesser extent) 137Cs and made dissolution of 239+240Pu more difficult.

Environmental Monitoring↗

Smectite clays in Mars soil: evidence for their presence and role in Viking biology experimental results.

Various chemical, physical and geological observations indicate that smectite clays are probably the major components of the Martian soil. Satisfactory ground-based chemical simulation of the Viking biology experimental results was obtained with the smectite clays nontronite and montmorillonite when they contained iron and hydrogen as adsorbed ions. Radioactive gas was released from the medium solution used in the Viking Labeled Release (LR) experiment when interacted with the clays, at rates and quantities similar to those measured by Viking on Mars. Heating of the active clay (mixed with soluble salts) to 160 degrees C in CO2 atmosphere reduced the decomposition activity considerably, again, as was observed on Mars. The decomposition reaction in LR experiment is postulated to be iron-catalyzed formate decomposition on the clay surface. The main features of the Viking Pyrolytic Release (PR) experiment were also simulated recently (Hubbard, 1979) which the iron clays, including a relatively low '1st peak' and significant '2nd peak'. The accumulated observations on various Martian soil properties and the results of simulation experiments, thus indicate that smectite clays are major and active components of the Martian soil. It now appears that many of the results of the Viking biology experiments can be explained on the basis of their surface activity in catalysis and adsorption.

Chemical Phenomena↗

Mucosal iron retention and plasma iron absorption in the duodenum and jejunum of dogs.

Two groups of non-anemic dogs, one with normal tissue iron stores and one with decreased tissue iron stores, underwent a surgical construction of two equal segments of duodenum and jejunum. A solution of 0.1 mg ferrous sulfate and 1 mg ascorbic acid was injected into the lumen of each segment. The solution for the duodenal segment contained 30 muc of iron59, for the jejunum segment 60 muc of iron55. The solutions were left in the segments for 2 1/2 hours before washout. On the 14th postoperative day, iron59 and iron55 radioactivity per ml/RBC was measured, and iron uptake by segments determined in two ways. Bone marrow, liver, and spleen were histologically assessed of iron stores. In dogs with normal iron stores, percent iron retained was slightly higher in jejunum that duodenum. In dogs with decreased iron stores percent retention was always higher in duodenum; in this group iron retained was about four times higher than in dogs with normal iron stores. This indicates that mucosal uptake of iron from lumen and mucosal transfer of iron from plasma vary inversely with body iron stores, but compared to mucosal uptake, mucosal transfer is more restricted to duodenum, more affected by body iron stores, more limited, and more crucial to regulation of iron absorption.

Animals↗

Experimental evidence that potassium is a substantial radioactive heat source in planetary cores.

The hypothesis that (40)K may be a significant radioactive heat source in the Earth's core was proposed on theoretical grounds over three decades ago, but experiments have provided only ambiguous and contradictory evidence for the solubility of potassium in iron-rich alloys. The existence of such radioactive heat in the core would have important implications for our understanding of the thermal evolution of the Earth and global processes such as the generation of the geomagnetic field, the core-mantle boundary heat flux and the time of formation of the inner core. Here we provide experimental evidence to show that the ambiguous results obtained from earlier experiments are probably due to previously unrecognized experimental and analytical difficulties. The high-pressure, high-temperature data presented here show conclusively that potassium enters iron sulphide melts in a strongly temperature-dependent fashion and that (40)K can serve as a substantial heat source in the cores of the Earth and Mars.

Journal Article↗

Specific photoaffinity labelling of a ferripyoverdin outer membrane receptor of Pseudomonas aeruginosa.

In order to identify and characterize the receptors involved in pyoverdin-mediated iron transport in Pseudomonas aeruginosa ATCC 15692, a photoactivatable siderophore has been synthesized. In the dark, this probe is stable and is able to promote iron transport at the same rate as the native pyoverdin. Under irradiation at 312 nm, the molecule is photodecomposed and a clear inhibition of the iron transport is observed. With the radioactive form of this photoactivatable probe, we were able to visualize on a SDS-PAGE gel a labelled protein of approximately 90 kDa molecular mass, which is very likely the FpvA receptor or a yet unknown pyoverdin receptor.

Affinity Labels↗

[Application of double focusing magnetic sector high resolution ICP-MS to the study of iron stable isotope trace].

Iron absorption efficiency study is one of the key steps to overcome iron deficiency anemia. Determination of iron isotope ratios is the base of iron absorption study. For this purpose radioactive isotope trace method, neutron activation, and thermal ionization mass spectrometry etc. have been used as accessory means. A double focusing inductively coupled plasma mass spectrometry (DF-ICP-MS) was used to determine isotope ratios of Fe in food and human faeces in this paper. Interferences of 40Ar16O to 56Fe and 40Ar14N to 54Fe were avoided by using higher resolution (3000). Longer times and fast electronic scanning were employed to decrease the influence of signal fluctuations from the plasma. Instrumental parameters of the mass spectrometer were optimized while keeping the total integral time under 27s. RSD values obtained for isotope ratios of 5Fe/56Fe, 57Fe/56Fe and 58 Fe/56Fe were 0.23%, 0.14%, 0.22%, respectively, for a natural standard solution of 5 microg x mL(-1). The method has been used to iron nutrition studies.

Iron↗

Effects of dietary protein, glycine, and tryptophan on iron metabolism in the growing chick.

Experiments were conducted to determine the effects of feeding diets low in protein, glycine, or tryptophan on iron metabolism in the growing chick. Three-day-old chicks, which were fed the experimental diets to 2 weeks of age, were given orally a solution of 59FeSO4 in order to determine the percentage of iron absorbed and excreted (determined by the fecal recovery method) and iron utilized and stored (determined by the radioactivity retained per unit liver, gastrocnemius muscle, and whole blood) 7 days post dose administration. The feeding of diets low in protein (5.4%, 8.5%, or 10.8%) or tryptophan (0.12%) but adequate in iron to growing chicks caused: a marked reduction in growth, rate of erthropoiesis, and percentage iron absorption; an excessive increase in iron deposited in the liver and muscle, and percentage iron collected in the excreta; and anemia which was attributed to the deficiency of protein or tryptophan respectively, in the diets fed. The feeding of diets low in glycine (0.33%) but adequate in iron caused: a marked reduction in growth and percentage iron, absorption, and a transitory increase in percentage of iron excreted without causing anemia or affecting the distribution of absorbed iron in liver, muscle and blood. The total plasma protein concentration was reduced in protein deficient chicks, but was not affected by a tryptophan or glycine deficiency.

Animals↗