Kinetics of iron passage through subcellular compartments of rabbit reticulocytes

Summary The kinetics of the separate processes of Fe₂(III)-transferrin binding to the transferrin receptor, transferrin-receptor internalization, iron dissociation from transferrin, iron passage through the membrane, and iron mobilization into the cytoplasm were studied by pulse-chase experiments using rabbit reticulocytes and⁵⁹Fe,¹²⁵I-labeled rabbit transferrin. The binding of⁵⁹Fe-transferrin to transferrin receptors was rapid with an apparent rate constant of 2×10⁵ m ^–1 sec^–1. The rate of internalization of⁵⁹Fe-transferrin was directly measured at 520±100 molecules of Fe₂(III)-transferrin internalized/sec/cell with 250±43 sec needed to internalize the entire complement of reticulocyte transferrin receptors. Subsequent to Fe₂(III)-transferrin internalization the flux of⁵⁹Fe was followed through three compartments: internalized transferrin, membrane, and cytosol.A process preceding iron dissociation from transferrin and a reaction involving membrane-associated iron required 17±2 sec and 34±5 sec, respectively. Apparent rate constants of 0.0075±0.002 sec^–1 and 0.0343±0.0118 sec^–1 were obtained for iron dissociation from transferrin and iron mobilization into the cytosol, respectively. Iron dissociation from transferrin is the rate-limiting step. An apparent rate constant of 0.0112±0.0025 sec^–1 was obtained for processes involving iron transport through the membrane although at least two reactions are likely to be involved. Based on mechanistic considerations, iron transport through the membrane may be attributed to an iron reduction step followed by a translocation step. These data indicate that the uptake of iron in reticulocytes is a sequential process, with steps after the internalization of Fe₂(III)-transferrin that are distinct from the handling of transferrin.     

Dynamic equilibria in iron uptake and release by ferritin

The function of ferritins is to store and release ferrous iron. During oxidative iron uptake, ferritin tends to lower Fe²⁺ concentration, thus competing with Fenton reactions and limiting hydroxy radical generation. When ferritin functions as a releasing iron agent, the oxidative damage is stimulated. The antioxidant versus pro-oxidant functions of ferritin are studied here in the presence of Fe²⁺, oxygen and reducing agents. The Fe²⁺-dependent radical damage is measured using supercoiled DNA as a target molecule. The relaxation of supercoiled DNA is quantitatively correlated to the concentration of exogenous Fe²⁺, providing an indirect assay for free Fe²⁺. After addition of ferrous iron to ferritin, Fe²⁺ is actively taken up and asymptotically reaches a stable concentration of 1–5 m. Comparable equilibrium concentrations are found with plant or horse spleen ferritins, or their apoferritins. After addition of ascorbate, iron release is observed using ferrozine as an iron scavenger. Rates of iron release are dependent on ascorbate concentration. They are about 10 times larger with pea ferritin than with horse ferritin. In the absence of ferrozine, the reaction of ascorbate with ferritins produces a wave of radical damage; its amplitude increases with increased ascorbate concentrations with plant ferritin; the damage is weaker with horse ferritin and less dependent on ascorbate concentrations.     

The ferroxidase center is essential for ferritin iron loading in the presence of phosphate and minimizes side reactions that form Fe(III)-phosphate colloids

Ferritin iron loading was studied in the presence of physiological serum phosphate concentrations (1 mM), elevated serum concentrations (2–5 mM), and intracellular phosphate concentrations (10 mM). Experiments compared iron loading into homopolymers of H and L ferritin with horse spleen ferritin. Prior to studying the reactions with ferritin, a series of control reactions were performed to study the solution chemistry of Fe²⁺ and phosphate. In the absence of ferritin, phosphate catalyzed Fe²⁺ oxidation and formed soluble polymeric Fe(III)-phosphate complexes. The Fe(III)-phosphate complexes were characterized by electron microscopy and atomic force microscopy, which revealed spherical nanoparticles with diameters of 10–20 nm. The soluble Fe(III)-phosphate complexes also formed as competing reactions during iron loading into ferritin. Elemental analysis on ferritin samples separated from the Fe(III)-phosphate complexes showed that as the phosphate concentration increased, the iron loading into horse ferritin decreased. The composition of the mineral that does form inside horse ferritin has a higher iron/phosphate ratio (~1:1) than ferritin purified from tissue (~10:1). Phosphate significantly inhibited iron loading into L ferritin, due to the lack of the ferroxidase center in this homopolymer. Spectrophotometric assays of iron loading into H ferritin showed identical iron loading curves in the presence of phosphate, indicating that the ferroxidase center of H ferritin efficiently competes with phosphate for the binding and oxidation of Fe²⁺. Additional studies demonstrated that H ferritin ferroxidase activity could be used to oxidize Fe²⁺ and facilitate the transfer of the Fe³⁺ into apo transferrin in the presence of phosphate.     

Purification of fusion ferritin from recombinant E. coli using two-step sonications

Fusion ferritin, combined by heavy chain ferritin (21 kDa) and light chain ferritin (19 kDa), was expressed in recombinant E. coli. The fusion ferritin was easily purified by two-step sonications as well as gel filtration chromatography. SDS-gel electrophoresis showed a single band of 38 kDa with heavy and light chains. MALDI-TOF MS gave a molecular weight of fusion ferritin was 38 kDa. The specific activity and yield of purified fusion ferritin are 0.41 Fe³⁺ mg mg^–1 of protein and 66%. Those values are larger than the previous ones of 0.2 Fe³⁺ mg mg^–1 (Kim et al. 2001).     

Implications for in vitro studies of the autoxidation of ferrous ion and the iron-catalyzed autoxidation of dithiothreitol

The influences of buffers and iron chelators on the rate of autoxidation of Fe²⁺ were examined in the pH range 6.0–7.4. The catalysis by Fe²⁺ and Fe³⁺ of the autoxidation of dithiothreitol was also investigated. In buffers which are non- or poor chelators of iron, 0.25 mM Fe²⁺, and 0.3 mM dithiothreitol when present with iron, oxidize within minutes at pH 7.4 and 30°C. The stability of each increases as the pH is decreased and more than 90% of each remains after 1 h at pH 6.0. In the presence of buffers or oxy-ligands which preferentially and strongly chelate Fe³⁺ over Fe²⁺, Fe²⁺ autoxidizes rapidly in the pH range 6.0–7.4 while dithiothreitol is protected. Ligands which preferentially bind strongly to Fe²⁺ stabilize both Fe²⁺ and dithiothreitol at pH 7.4. Dithiothreitol readily reduces Fe³⁺ in non-chelating buffers or in the presence of strong chelators of Fe²⁺, however, the ferrous ions produced are prone to reoxidation at higher pH values. These results show that Fe²⁺ and dithiothreitol are very susceptible to autoxidation in the neutral pH range, and that the rates are strongly influenced by the presence of chelators of Fe²⁺ and Fe³⁺. The rapid autoxidations of these species need to be taken into account when designing and interpreting experiments involving Fe²⁺ or both dithiothreitol and iron.     

Molecular aspects of the removal of ferritin-bound iron bydl-dihydrolipoate

The removal of ferritin-bound iron by the physiologic dithioldl-dihydrolipoate was studied over the pH range 5.5–9.0. A novel method was devised for the determination of iron removal, making it possible to study the actual release of iron from ferritin, regardless of the oxidation state or complexation form. The overall iron-removal process appears to depend upon a balance between the deprotonation of the dithiol and the protolytic dissolution of the iron core inside the ferritin molecule. The amount of iron removed at equilibrium increases with the pH, at any of the dihydrolipoate/ferritin iron ratios tested. The formation of the binuclear iron-dithiol complex [Fe₂-dihydrolipoate)₃]⁻³ is not strictly required for iron mobilization, but it seems to affect the efficiency of the dithiol in iron mobilization by providing a stable complexation form for the released iron outside the ferritin protein shell. Comparison of the release of ferritin-bound iron by free and immobilized dihydrolipoate indicates that mobility of the dithiol is mandatory for the removal process to take place.     

A paradox: Fe2+-containing agents decreased ROS and apoptosis induced by CoNPs in vascular endothelial cells by inhibiting HIF-1α

Cobalt nanoparticles (CoNPs) released from hip joint implants are known to have a toxic effect on several organs probably through increasing reactive oxygen species (ROS). Ferrous ion (Fe²⁺) is well-known to enhance oxidative stress by catalysing the production of ROS. However, in our pilot study, we found that Fe²⁺ conversely inhibited the ROS production induced by CoNPs. To elucidate the underlying mechanism, the present study treated vascular endothelial HUVEC and HMEC-1 cells with CoNPs alone or in combination with ferrous lactate [Fe(CH₃CHOHCOO)₂], ferrous succinate [Fe(CH₂COO)₂], and ferrous chloride (FeCl₂). CoNP toxicity was evaluated by measuring cell viability, rate of apoptosis and lactose dehydrogenase (LDH) release, and intracellular ROS levels. Treatment with CoNPs decreased cell viability, LDH release, and ROS production and increased apoptosis. CoNPs increased hypoxia-inducible factor-1α (HIF-1α) protein level and mRNA levels of vascular endothelial growth factor (VEGF) and glucose transporter 1 (GLUT1) downstream of HIF-1α signalling. Silencing HIF-1α attenuated CoNP toxicity, as seen by recovery of cell viability, LDH release, and ROS levels and reduced apoptosis. CoNPs caused a pronounced reduction of Fe²⁺ in cells, but supplementation with Fe(CH₃CHOHCOO)₂, Fe(CH₂COO)₂, and FeCl₂ restored Fe²⁺ levels and inhibited HIF-1α activation. Moreover, all three Fe²⁺-containing agents conferred protection from CoNPs; Fe(CH₃CHOHCOO)₂ and Fe(CH₂COO)₂ more effectively than FeCl₂. In summary, the present study revealed that CoNPs exert their toxicity on human vascular endothelial cells by depleting intracellular Fe²⁺ level, which causes activation of HIF-1α signalling. Supplements of Fe²⁺, especially in the form of Fe(CH3CHOHCOO)₂ and Fe(CH₂COO)₂, mitigated CoNP toxicity.     

Effects of acidity on the growth of two Euglena species

Our study separates the effects of elevated protons (at pH <3) and elevated metals (Al, Cd, Cu, Fe, Ni, Zn) on the growth of E. mutabilis Schmitz, a pioneering phototroph in acid mine drainage (AMD) and E. gracilis Klebs, a closely-related species rarely found in severely AMD-impacted sites. Both species were acid tolerant, growing optimally at pH 2.5–7. At pH values typical of AMD (pH 2.5–4) in the absence of elevated metals, E. gracilis outcompeted E. mutabilis (growth rates of 1.0 and 0.8 div d^–1, respectively). Relative metal toxicities were evaluated based on the Effective Exposure causing 50% growth reduction (= EE50). With total metal additions similar to AMD levels, E. mutabilis demonstrated significantly greater tolerance to all metals, except Cu. E. gracilis showed two-fold higher tolerance to Cu²⁺ than E. mutabilis (EE50 of 91.6 vs. 45.7 pmol cell^–1). The EE50 for Zn²⁺ was similar for both species (368 pmol cell^–1 for E. gracilis and 423 pmol cell^–1 for E. mutabilis). With Cd and Ni, E. mutabilis tolerated an order of magnitude higher exposure than E. gracilis(EE50 of 1.6 vs. 0.2 pmol Cd²⁺ cell^–1; EE50 of 942 vs. 87 pmol Ni²⁺ cell^–1). Al and Fe were tolerated at high total metal concentrations (up to 100 mM) by E. mutabilis, but toxicity was evident with E. gracilisat much lower levels. E. mutabilis grew at double the Al³⁺ exposure tolerated by E. gracilis (EE50 of 398 vs. 188 pmol Al³⁺ cell^–1). There was an 18-fold difference in Fe tolerance levels between E. mutabilis and E. gracilis with EE50s of 8773 and 502 pmol Fe²⁺ cell^–1, respectively. We conclude that differential metal tolerance, particularly to Fe²⁺, accounts for the mutually exclusive distribution of E. gracilis and E. mutabilis in AMD-impacted habitats.     

Effects of aluminum,iron, oxygen and nitrate additions on phosphorus release from the sediment of a Danish softwater lake

The effects of oxygen, aluminum, iron and nitrate additions on phosphate release from the sediment were evaluated in the softwater Lake Vedsted, Denmark, by a 34-day experiment with undisturbed sediment cores. Six treatments were applied: (1) Control - O₂ (0–20% saturation), (2) O₂ (100% saturation) (3) Al³⁺ – O₂, (4) Fe³⁺ + O₂, (5) Fe³⁺ – O₂, and (6) NO₃ ^– – O₂. Al₂(SO₄)₃*18 H₂O and FeCl₃*4H₂O were added in amounts that theoretically should immobilize the exchangeable P-pool in the top 5 cm of the sediment, while sodium nitrate concentrations were increased to 5 mg N l^–1. The four treatments with metals or NO₃ ^– reduced the P efflux from the sediment significantly as compared to the suboxic control treatment. Mean accumulated P-release rates for suboxic treatments with Al³⁺, Fe³⁺, and NO₃ ^– were: –0.27 mmol m^–2 (st. dev = 0.02 mmol m^–2, N = 5), 0.58 mmol m^–2 (st. dev = 0.30 mmol m^–2, N = 5) and 1.40 mmol m^–2 (st. dev = 0.14 mmol m^–2, N = 5), respectively. The oxic treatment with Fe³⁺ had a P efflux of 0.36 mmol m^–2 (st. dev = 0.08 mmol m^–2, N = 5). The two highest P-release rates were observed in the control treatment and the treatment with O₂ (14.50 mmol m^–2 (st. dev = 3.90 mmol m^–2, N = 5) and 2.31 mmol m^–2 (st. dev = 0.80 mmol m^–2, N = 5), respectively). In order to identify changes in the P and Fe binding sites in the sediment as caused by the treatments, a sequential P extraction procedure was applied on the sediment before and after the efflux experiment. Addition of O₂, Fe³⁺ and NO₃ ^– to the sediment increased the amounts of oxidized Fe³⁺ and P_BD. Al³⁺ addition resulted in a lower fraction of P_BD but a correspondingly higher fraction of Al-bound P. Addition of Al³⁺ decreased the Fe-efflux from the suboxic sediment as well as the amount of oxidized Fe³⁺ in the sediment. This questions the use of Al compounds that contain sulfate because of the possible formation of FeS, which will restrict upward migration of Fe²⁺ and the formation of new Fe-oxides in the surface sediment. Instead, we suggest the use of AlCl₃ for lake restoration purposes.     

The photocycle and the structure of iron containing bacteriorhodopsin —a kinetic and Mössbauer spectroscopy investigation

Bacteriorhodopsin (bR), converted by deionization to the blue form was reconstituted to the active purple membrane by the addition of Fe²⁺ or Fe³⁺ ions. ⁵⁷Fe Mossbauer spectra of these samples were measured at different pH values (pH 3.9, pH 5.0 and pH 7.0) and at temperatures ranging from 4 K to 300 K. The hyperfine parameters reveal two iron environments with oxygen atoms in the neighbourhood of iron. Iron type 1 is in the 3⁺ high spin state. It is bound to acid side chains of the protein and/or the phosphate groups of the lipids. Iron type 2 is in the 2⁺ high spin state and is linked to carboxy groups of the protein in a rather unspecific way. Dynamics as measured by Mossbauer spectroscopy show that the purple membrane becomes flexible only above 220 K. At the interface between membrane and bulk water the mobility is comparable to that of proteins with hydrophilic surfaces. The photocycle of Fe ³⁺-bR is slowed down compared to native bR. 3–5 Fe³⁺/bR are sufficient to inhibit the photocycle turnover by one order of magnitude. This specific effect is also found with Cr³⁺, though it is less pronounced. Mössbauer spectra of Fe³⁺-bR at 4 K reveal that iron nuclei are spin-coupled, indicating their close spatial proximity. It is proposed that iron trinuclear clusters interact with the proton uptake site of bR. Offprint requests to: M. Engelhard     

Methacryloylamidohistidine in affinity ligands for immobilized metal-ion affinity chromatography of ferritin

A new metal-chelate adsorbent utilizing 2-methacryloylamidohistidine (MAH) was prepared as a metalchelating ligand. MAH was synthesized using methacryloly chloride and histidine. Monosize nanospheres with an average diameter of 450 nm were produced by emulsion polymerization of 2-hydroxyetylmethacrylate (HEMA) and MAH. Then, Fe³⁺ ions were chelated directly onto the monosize nanospheres. Mon-poly(HEMA-MAH) nanospheres were characterized by Fourier transform infrared spectroscopy, scanning electron microscopy, and elemental analysis. Fe³⁺ chelated monosize nanospheres were used in ferritin adsorption from an aqueous solution. The maximum ferritin adsorption capacity of Fe³⁺-chelated mon-poly(HEMAMAH) nanospheres was 202 mg/g at pH 4.0 in acetate buffer. The non-specific ferritin adsorption on the monpoly( HEMA-MAH) nanospheres was 20 mg/g. The adsorption behavior of ferritin could be modeled using both Langmuir and Freundlich isotherms. The adsorption capacity decreased with increasing ionic strength of the binding buffer. High desorption ratios (> 95% of the adsorbed ferritin) were achieved with 1.0 M NaCl at pH 7.0. Ferritin could be repeatedly adsorbed and desorbed with the Fe³⁺-chelated mon-poly(HEMA-MAH) nanospheres without significant loss of adsorption capacity.     

Process for biological oxidation and control of dissolved iron in bioleach liquors

Iron has a central role in bioleaching and biooxidation processes. Fe²⁺ produced in the dissolution of sulfidic minerals is re-oxidized to Fe³⁺ mostly by biological action in acid bioleaching processes. To control the concentration of iron in solution, it is important to precipitate the excess as part of the process circuit. In this study, a bioprocess was developed based on a fluidized-bed reactor (FBR) for Fe²⁺ oxidation coupled with a gravity settler for precipitative removal of ferric iron. Biological iron oxidation and partial removal of iron by precipitation from a barren heap leaching solution was optimized in relation to the performance and retention time (τ_FBR) of the FBR. The biofilm in the FBR was dominated by Leptospirillum ferriphilum and “Ferromicrobium acidiphilum.” The FBR was operated at pH 2.0 ± 0.2 and at 37 °C. The feed was a barren leach solution following metal recovery, with all iron in the ferrous form. 98–99% of the Fe²⁺ in the barren heap leaching solution was oxidized in the FBR at loading rates below 10 g Fe²⁺/L h (τ_FBR of 1 h). The optimal performance with the oxidation rate of 8.2 g Fe²⁺/L h was achieved at τ_FBR of 1 h. Below the τ_FBR of 1 h the oxygen mass transfer from air to liquid limited the iron oxidation rate. The precipitation of ferric iron ranged from 5% to 40%. The concurrent Fe²⁺ oxidation and partial precipitative iron removal was maximized at τ_FBR of 1.5 h, with Fe²⁺ oxidation rate of 5.1 g Fe²⁺/L h and Fe³⁺ precipitation rate of 25 mg Fe³⁺/L h, which corresponded to 37% iron removal. The precipitates had good settling properties as indicated by the sludge volume indices of 3–15 mL/g but this step needs additional characterization of the properties of the solids and optimization to maximize the precipitation and to manage sludge disposal.     

Biosorption of uranium(VI) by Aspergillus fumigatus

Aspergillus fumigatus removed uranium(VI) very rapidly and reached equilibrium within 1 h of contact of biomass with the aqueous metal solution. Biosorption data fitted to Langmuir model of isotherm and a maximum loading capacity of 423 mg U g^–1 dry wt was obtained. Distribution coefficient as high as 10,000 (mg U g^–1)/(mg U ml^–1) at a residual metal ion concentration of 19 mg l^–1 indicates its usefulness in removal of uranium(VI) from dilute waste streams. Optimum biosorption was seen at pH 5.0 and was independent of temperature (5–50°C ). Initial metal ion concentration significantly influenced uptake capacity which brought down % (w/w) uranium(VI) removal from 90 at 200 mg U l^–1 to 35 at 1000 mg U l^–1. Presence of 0.84 mmol Fe²⁺, Fe³⁺, Ca²⁺ and Zn²⁺ had no effect on uranium(VI) biosorption unlike Al³⁺ (0.84 mM) which was inhibitory.     

Chemical modification of lipase with ferromagnetic modifier — A ferromagnetic-modified lipase

Summary A ferromagnetic modifier was prepared by reacting ferrous(Fe²⁺)- and ferric(Fe³⁺)-ions with polyethylene glycol having two carboxyl groups (MW:2000) at pH 8.0–8.5. Lipase fromPseudomonas fragi 22–39B was coupled with the modifier using water-soluble carbodiimide. The modified lipase, which was dispersed into buffered solutions in the size range of 30–70 nm, exerted the hydrolytic activity of 8.0 U/mg. In a magnetic field of 250 Oe, the ferromagnetic-modified lipase was readily recovered from the colloidal solution.     

Succinylated bovine heart mitochondrial cytochromec oxidase

Cytochromec oxidase was prepared by sequential extraction of bovine heart muscle submitochondrial particles with sodium deoxycholate, followed by fractional precipitation with ammonium sulfate and chromatography on Sephadex G-75. The resulting preparation had typical absorption spectra, an activity of 1.28 sec^–1 (mg protein)^–1 (3 ml)^–1 in deoxycholate or 4.13 sec^–1 (mg protein)^–1 (3 ml)^–1 in 0.5% Tween 80, and a minimum molecular weight of 120,000 daltons as calculated from the heme content and the total protein. Amino acid analyses of nine preparations yielded a molecular weight per heme of 86,500 daltons. The net charge was calculated to be +8.7 at pH 7.0. Succinylation of cytochromec oxidase in the presence of 500 molar excess of succinic anhydride produced a soluble preparation having a negative charge at neutral pH. The modified enzyme was highly autoxidizable and had little or no activity toward ferrocytochromec as a substrate. Its averageS _20,w was 5.8 and its apparentD was 4.0 × 10^–7 cm² sec^–1, from which a molecular weight of 126,000 daltons was calculated. This size of enzyme is considered to be that of the monomer, because the value is practically the same as the minimum molecular weight reported herein, and since it is approximately onehalf the value obtained in our laboratory (and in others) for the unmodified enzyme.     

Potentiometric assessment of iron release during ferritin reduction by exogenous agents

This work studied the possibilities for quantitative determination of iron mobilization in connection with ferritin reduction by ascorbic acid (vitamin C) and sodium dithionite in vitro. The iron storage protein was incubated with an excess of reductant in aerobic conditions in the absence of complexing agents in the medium. The release of Fe²⁺ was let to go to completion, and the overall content of Fe²⁺ in the solution was evaluated with the aid of potentiometric titration using Ce⁴⁺ as an oxidizing titrant. Results suggest a moderate iron efflux under the influence of the chosen reducing agents. Although such a reduction of the protein mineral core by dihydroxyfumarate contributes greatly to the iron mobilization, ferritin behavior with vitamin C and dithionite seems to be different. Although redox properties of dihydroxyfumarate are determined by hydroxyl groups similar to those of ascorbic acid, the two compounds differ significantly in structure, and this could be the basis for an explanation of the specificities in their interaction with ferritin. As revealed by the study, potentiometric titration promises to be a reliable tool for evaluation of the amount of Fe²⁺ present in the solution as a result of the reduction of the ferritin’s mineral core.     

H2-Uptake Activity, Spectra, Reduction Potentials, and Kinetics of Iron Release on the Surface of Iron Core from Azotobacter vinelandii Bacterial Ferritin

Bacterial ferritin from Azotobacter vinelandii (AvBF_o has a function in H₂ uptake. The Fe³⁺ reduction on the surface of the iron core from AvBF_o is accompanied simultaneously by H₂ uptake, with a maximum activity of H₂ uptake of 450 H₂/AvBF_o. A reduction potential of –402 mV for iron reduction on the surface of the core is found. A shift to the red the protein absorbance peaks ranging from 280 to 290 nm is observed between pH5 and 9 under 100% H₂ reduction. The reduction potential for iron release becomes negative at a rate of 0.025 mV/Fe²⁺ released. The kinetics of iron release on the surface of the core is a first-order reaction.     

Soil Iron Content as a Predictor of Carbon and Nutrient Mobilization in Rewetted Fens

Rewetted, previously drained fens often remain sources rather than sinks for carbon and nutrients. To date, it is poorly understood which soil characteristics stimulate carbon and nutrient mobilization upon rewetting. Here, we assess the hypothesis that a large pool of iron in the soil negatively affects fen restoration success, as flooding-induced iron reduction (Fe³⁺ to Fe²⁺) causes a disproportionate breakdown of organic matter that is coupled with a release of inorganic compounds. We collected intact soil cores in two iron-poor and two iron-rich drained fens, half of which were subjected to a rewetting treatment while the other half was kept drained. Prolonged drainage led to the mobilization of nitrate (NO₃^-, > 1 mmol L^-1) in all cores, regardless of soil iron content. In the rewetted iron-rich cores, a sharp increase in pore water iron (Fe) concentrations correlated with concentrations of inorganic carbon (TIC, > 13 mmol L^-1) and dissolved organic carbon (DOC, > 16 mmol L^-1). Additionally, ammonium (NH₄⁺) accumulated up to phytotoxic concentrations of 1 mmol L^-1 in the pore water of the rewetted iron-rich cores. Disproportionate mobilization of Fe, TIC, DOC and NH₄⁺ was absent in the rewetted iron-poor cores, indicating a strong interaction between waterlogging and iron-mediated breakdown of organic matter. Concentrations of dissolved phosphorus (P) rose slightly in all cores upon rewetting, but remained low throughout the experiment. Our results suggest that large pools of iron in the top soil of drained fens can hamper the restoration of the fen’s sink-service for ammonium and carbon upon rewetting. We argue that negative effects of iron should be most apparent in fens with fluctuating water levels, as temporary oxygenation allows frequent regeneration of Fe³⁺. We conclude that rewetting of iron-poor fens may be more feasible for restoration.     

Free metal activity and total metal concentrations as indices of micronutrient availability to barley [Hordeum vulgare (L.) ‘Klages’]

The form in which a micronutrient is found in the rhizosphere affects its availability to plants. We compared the availability to barley of the free hydrated cation form of Fe³⁺, Cu²⁺, Zn²⁺, and Mn²⁺ versus their total metal concentrations (free ion plus complexes) in chelator-buffered solutions. Free metal ion activities were estimated using the chemical equilibrium program GEOCHEM-PC with the corrected database. In experiment 1, barley was grown in nutrient solutions with different Fe³⁺ activities using chelators to control Fe levels. Chlorosis occurred at Fe³⁺ activities of 10^–18 and 10^–19 M for barley grown in HEDTA and EDTA solutions, respectively. In experiment 2, barley was grown in nutrient solutions with the same calculated Fe³⁺ activity and the same chelator, but different total Fe concentrations. Leaf, root and shoot Fe concentrations were higher from CDTA buffered solutions which had the higher total Fe concentration indicating the importance of the total Fe concentration on Fe uptake. Results from treatments using EDTA or HEDTA, with one exception, were similar to the results from the CDTA treatment. This suggests differences in critical Fe³⁺ activities found in experiment 1 were due to differences in the total Fe concentration and not errors in chelate formation constants used to estimate the critical activities. Results for Cu, Zn, and Mn were similar to Fe; despite solutions with equal free Cu²⁺, Zn²⁺ and Mn²⁺ activities, plant concentrations of these metals were generally greater when grown in the solutions with the greater total amount of Cu, Zn, or Mn. When the free Zn²⁺ activity was kept constant while the total amount of Zn was increased from 4.4 to 49 M, leaf Zn concentration increased from 77 to 146 g g^-1. In order to predict metal availability to barley and other species in chelator-buffered nutrient solutions, both free and total metal concentrations in solution must be considered. The critical Fe³⁺ activities required by barley in this study are much higher than those from tomato and soybean, 10^-28 M, which strongly supports the Strategy 2 model of Fe uptake for Poaceae. This is related to the importance of the Fe³⁺ (barley) and the Fe²⁺ (tomato and soybean) ions in Fe uptake. Fe-stressed barley is known to release phytosiderophores which compete for Fe³⁺ in the nutrient solution, while tomato and soybean reduce Fe³⁺ to Fe²⁺ at the epidermal cell membranes to allow uptake of Fe²⁺ from Fe³⁺ chelates in solution.Abbreviations CDTA trans-1,2-diaminocyclohexane-N,N,N,N-tetracetic acid - DTPA diethylenetriaminepentacetic acid - EDTA ethylenediaminetetracetic acid - EDDHA ethylenediamine-di(o-hydroxyphenylacetic acid) - HBED-N,N di(2-hydroxybenzoyl)-ethylenediamine-N,N-diacetic acid - HEDTA-N hydroxyethylenediaminetriacetic acid - MES-2 (N-morpholino)ethanesulfonic acid - NTA nitrilotriacetic acid     

Transfer cell formation in sugar beet roots induced by latent Fe deficiency

Leaves of Fe deficient sugar beets precultured in complete nutrient solution with Fe(III)EDTA remained green during the first 6 days of –Fe treatment when grown in a small nutrient solution volume (0.5 L/plant). After 3 days of –Fe treatment, roots placed in agar showed enhanced H⁺ release and ferric reduction at the tips of young laterals where short root hairs and transfer cells had developed. However, the H⁺ release was too weak to cause a pH decrease of the bulk nutrient solution. Nevertheless, the Fe stress response reactions probably lead to mobilization of Fe from the apoplasmic pool so that chlorosis development was prevented. Slight chlorosis symptoms appeared only after 4 more days of Fe deficiency and the pH of the bulk nutrient solution decreased to pH 4.5 simultaneously with renewed transfer cell formation and subsequent rapid regreening. In the 10 times higher volume of 5 L-Fe solution/plant, laterals with root hairs and transfer cells also showed localized acidification of the agar system. However, the protons released were so diluted that no pH decrease of the bulk solution was measurable. Instead, the leaves showed continuously increasing chlorosis with degenerated chloroplast ultrastructure. It is concluded that root hairs and transfer cells are not only formed under severe chlorosis but, instead, they seem to be an integral part of the adaptive response to latent Fe deficiency.