Oxidative Ionic Metabolites of L-Methyl-4-Phenyl-L, 2, 3, 6-Tetrahydropy-Ridine (MPTP): Correlation of Electro-Reduction with Physiological Behavior

Electrochemical studies (reduction potential and reversibility) were performed on 1 -methyl-4-pheny!pyridi-nium(MPP ⁺) and l-methyl-4-phenyl-2, 3-dihydropyridinium (MPDP ⁺) . MPP⁺ gave reduction potentials in the range of - 1.09 to - 1.11 V in organic solvents in a process which was reversible. The reduction potential of MPDP⁺ was -0.64 V (irreversible). Possible relationships involving the electrochemical properties, oxy radical formation, and biological activity of these and related iminium species are discussed.     

Plasmalemma Redox Chain and H Extrusion: II. Respiratory and Metabolic Changes Associated with Fusicoccin-Induced and with Ferricyanide-Induced H Extrusion

Ferricyanide reduction by Elodea densa leaves is associated with a release of protons in the cytoplasm, a fraction of the increase in protons being then extruded by the ATP-driven proton pump (20). The data presented here show that ferricyanide induces a marked increase in O₂ uptake, additive to that induced by fusicoccin plus K⁺, and here interpreted as depending on the utilization of ATP by the H⁺ pump. Glucose 6-phosphate and malate levels are markedly increased by fusicoccin plus K⁺. The simultaneous presence of ferricyanide reduces by about 50% the increase of malate, while it completely suppresses that of glucose 6-phosphate. The ferricyanide-induced decrease of malate is interpreted as due to the acidification of the cytosol associated with ferricyanide reduction, while the more marked decrease of glucose 6-phosphate might depend in part on the pH change and in part on a faster oxidation of this substrate. In fact, ferricyanide reduction is accompanied by a marked decrease of the incorporation into RNA ribose of C-1 as compared with C-2 of [¹⁴C]glucose. This suggests a stimulation of the release of C-1 as CO₂ at the level of the glucose 6-phosphate oxidation pathway, as expected if NADPH was the electron donor for ferricyanide reduction. These results are interpreted as confirming that the H⁺ efflux associated with ferricyanide reduction depends on the activation of the ATP-driven plasmalemma H⁺ pump. They also suggest that NADPH is used as an electron donor to some initial component of the plasmalemma redox system.     

Effects of cytochalasin B on water, Na+ and Cl? exchanges in the gill of seawater adapted mulletMugil capito

Summary Electron microscopy study shows that cytochalasin treatment of the mullet damages the microfilaments system in the apex of gill ionocytes: the microfilaments are reduced in number and shortened. Cytochalasin causes a reduction of transgill potential difference and an increase of the Na⁺ and Cl^– blood concentration, of the diffusional water permeability of the gill, of the Na⁺ branchial influx and of Cl^– efflux. The increase of the Na⁺ influx may result in a reduction of the Na⁺ net excretion flux compared to the control. The increased permeability in cytochalasin treated fish facilitates the Cl^– entry probably leading to a reduction of the net Cl^– excretion. The partial inhibition of the K⁺ dependent components of Na⁺ and Cl^– effluxes also contributes to the reduction of Na⁺ and Cl^– excretion. The role of microfilaments in the mechanisms of ionic excretion by the gill is discussed.     

Studies on the Redox Characteristics of Ferrioxamine E

Thermodynamic parameters for the reduction of ferrioxamine E as calculated from redox potentials determined at four different temperatures were found to be ΔH ^≠ =7.1±3.4 kJ mol^?1 and ΔS^≠=?146 J mol^?1 K^?1. The negative entropy value is large, because the decrease in the charge at the metal center and an increase in its ionic radius force the structure of the complex to become less rigid and resemble the desferrisiderophore. The hydrophilic groups of the system are now (relatively more) available for solvent interaction. Thus, a large negative entropy change accompanies the reduction of the complex. Kinetics of reduction of ferrioxamine by V^II, Cr^II, Eu^II, and dithionite were measured at different temperatures and by dithionite at different pH values. The Cr^II and Eu^II reactions proceed by an inner‐sphere mechanism and have second‐order rate constants at 25° of 1.37×10⁴ and 1.23×10⁵ M ^?1 s^?1, respectively. For the V^II reduction, the corresponding rate constant was 1.89×10³ M ^?1 s^?1. The activation parameters for the V^II reduction were ΔH^≠ = 8.3 kJ mol^?1; ΔS^≠ = ?154 J mol^?1 K^?1. These values are indicative of an outer‐sphere mechanism for V^II reduction. The reduction by dithionite is half order in dithionite concentration indicating that SO ^. is the sole reducing species. log of reduction rate constants of different trihydroxamates by this reductant were correlated with their respective redox potentials, and the variation was found to be in approximate correspondence with the expectations of Marcus relationship.     

Mechanism of iron uptake by peanut plants : I. Fe reduction, chelate splitting, and release of phenolics

Iron deficiency in peanuts (Arachis hypogeae L.) caused an increase in release of caffeic acid, a higher rate of Fe^III reduction, and increased rates of both Fe^III chelate splitting and iron uptake.

Experiments on Fe^III reduction by phenolics (in vitro experiments) and by roots of Fe-deficient peanuts exclude the direct involvement of released phenolics in Fe^III reduction by roots: Fe^III reduction by phenolics had a pH optimum higher than 8.0 and was strongly dependent on the concentration and the stability of the supplied Fe^III chelates. In contrast, Fe^III reduction by roots of Fe-deficient peanuts had a pH optimum of about 5.0 and was less dependent on the stability of the supplied Fe^III chelates. Furthermore, the observed release of phenolics into nutrient solution would have to be at least 200 times higher to attain the reduction rates of roots of Fe-deficient peanuts. The results of these experiments support the idea of an enzymic reduction of Fe^III on the plasmalemma of cortical cells of roots.

     

Localized Tetrazolium Reduction in Relation to N2 Fixation, CO2 Fixation, and H2 Uptake in Aquatic Filamentous Cyanobacteria

The aquatic filamentous cyanobacteria Anabaena oscillarioides and Trichodesmium sp. reveal specific cellular regions of tetrazolium salt reduction. The effects of localized reduction of five tetrazolium salts on N₂ fixation (acetylene reduction), ¹⁴CO₂ fixation, and ³H₂ utilization were examined. During short-term (within 30 min) exposures in A. oscillarioides, salt reduction in heterocysts occurred simultaneously with inhibition of acetylene reduction. Conversely, when salts failed to either penetrate or be reduced in heterocysts, no inhibition of acetylene reduction occurred. When salts were rapidly reduced in vegetative cells, ¹⁴CO₂ fixation and ³H₂ utilization rates decreased, whereas salts exclusively reduced in heterocysts were not linked to blockage of these processes. In the nonheterocystous genus Trichodesmium, the deposition of reduced 2,3,5-triphenyl-2-tetrazolium chloride (TTC) in the internal cores of trichomes occurs simultaneously with a lowering of acetylene reduction rates. Since TTC deposition in heterocysts of A. oscillarioides occurs contemporaneously with inhibition of acetylene reduction, we conclude that the cellular reduction of this salt is of use in locating potential N₂-fixing sites in cyanobacteria. The possible applications and problems associated with interpreting localized reduction of tetrazolium salts in cyanobacteria are presented.     

Microbial Manganese and Sulfate Reduction in Black Sea Shelf Sediments

The microbial ecology of anaerobic carbon oxidation processes was investigated in Black Sea shelf sediments from mid-shelf with well-oxygenated bottom water to the oxic-anoxic chemocline at the shelf-break. At all stations, organic carbon (C_org) oxidation rates were rapidly attenuated with depth in anoxically incubated sediment. Dissimilatory Mn reduction was the most important terminal electron-accepting process in the active surface layer to a depth of ~1 cm, while SO₄²⁻ reduction accounted for the entire C_org oxidation below. Manganese reduction was supported by moderately high Mn oxide concentrations. A contribution from microbial Fe reduction could not be discerned, and the process was not stimulated by addition of ferrihydrite. Manganese reduction resulted in carbonate precipitation, which complicated the quantification of C_org oxidation rates. The relative contribution of Mn reduction to C_org oxidation in the anaerobic incubations was 25 to 73% at the stations with oxic bottom water. In situ, where Mn reduction must compete with oxygen respiration, the contribution of the process will vary in response to fluctuations in bottom water oxygen concentrations. Total bacterial numbers as well as the detection frequency of bacteria with fluorescent in situ hybridization scaled to the mineralization rates. Most-probable-number enumerations yielded up to 10⁵ cells of acetate-oxidizing Mn-reducing bacteria (MnRB) cm⁻³, while counts of Fe reducers were <10² cm⁻³. At two stations, organisms affiliated with Arcobacter were the only types identified from 16S rRNA clone libraries from the highest positive MPN dilutions for MnRB. At the third station, a clone type affiliated with Pelobacter was also observed. Our results delineate a niche for dissimilatory Mn-reducing bacteria in sediments with Mn oxide concentrations greater than ~10 μmol cm⁻³ and indicate that bacteria that are specialized in Mn reduction, rather than known Mn and Fe reducers, are important in this niche.     

Isolation, Growth, and Metabolism of an Obligately Anaerobic, Selenate-Respiring Bacterium, Strain SES-3

A gram-negative, strictly anaerobic, motile vibrio was isolated from a selenate-respiring enrichment culture. The isolate, designated strain SES-3, grew by coupling the oxidation of lactate to acetate plus CO₂ with the concomitant reduction of selenate to selenite or of nitrate to ammonium. No growth was observed on sulfate or selenite, but cell suspensions readily reduced selenite to elemental selenium (Se⁰). Hence, SES-3 can carry out a complete reduction of selenate to Se⁰. Washed cell suspensions of selenate-grown cells did not reduce nitrate, and nitrate-grown cells did not reduce selenate, indicating that these reductions are achieved by separate inducible enzyme systems. However, both nitrate-grown and selenate-grown cells have a constitutive ability to reduce selenite or nitrite. The oxidation of [¹⁴C]lactate to ¹⁴CO₂ coupled to the reduction of selenate or nitrate by cell suspensions was inhibited by CCCP (carbonyl cyanide m-chlorophenylhydrazone), cyanide, and azide. High concentrations of selenite (5 mM) were readily reduced to Se⁰ by selenate-grown cells, but selenite appeared to block the synthesis of pyruvate dehydrogenase. Tracer experiments with [⁷⁵Se]selenite indicated that cell suspensions could achieve a rapid and quantitative reduction of selenite to Se⁰. This reduction was totally inhibited by sulfite, partially inhibited by selenate or nitrite, but unaffected by sulfate or nitrate. Cell suspensions could reduce thiosulfate, but not sulfite, to sulfide. These results suggest that reduction of selenite to Se⁰ may proceed, in part, by some of the components of a dissimilatory system for sulfur oxyanions.     

Surface Charges and Regulation of FMN to Heme Electron Transfer in Nitric-oxide Synthase

The nitric-oxide synthases (NOS, EC 1.14.13.39) are modular enzymes containing attached flavoprotein and heme (NOSoxy) domains. To generate nitric oxide (NO), the NOS FMN subdomain must interact with the NOSoxy domain to deliver electrons to the heme for O₂ activation during catalysis. The molecular basis and how the interaction is regulated is unclear. We explored the role of eight positively charged residues that create an electropositive patch on NOSoxy in enabling the electron transfer by incorporating mutations that neutralized or reversed their individual charges. Stopped-flow and steady-state experiments revealed that individual charges at Lys⁴²³, Lys⁶²⁰, and Lys⁶⁶⁰ were the most important in enabling heme reduction in nNOS. Charge reversal was more disruptive than neutralization in all cases, and the effects on heme reduction were not due to a weakening in the thermodynamic driving force for heme reduction. Mutant NO synthesis activities displayed a complex pattern that could be simulated by a global model for NOS catalysis. This analysis revealed that the mutations impact the NO synthesis activity only through their effects on heme reduction rates. We conclude that heme reduction and NO synthesis in nNOS is enabled by electrostatic interactions involving Lys⁴²³, Lys⁶²⁰, and Lys⁶⁶⁰, which form a triad of positive charges on the NOSoxy surface. A simulated docking study reveals how electrostatic interactions of this triad can enable an FMN-NOSoxy interaction that is productive for electron transfer.     

Barite in hydrothermal environments as a recorder of subseafloor processes: a multiple‐isotope study from the Loki's Castle vent field

Barite chimneys are known to form in hydrothermal systems where barium‐enriched fluids generated by leaching of the oceanic basement are discharged and react with seawater sulfate. They also form at cold seeps along continental margins, where marine (or pelagic) barite in the sediments is remobilized because of subseafloor microbial sulfate reduction. We test the possibility of using multiple sulfur isotopes (δ³⁴S, Δ³³S, ?³⁶S) of barite to identify microbial sulfate reduction in a hydrothermal system. In addition to multiple sulfur isotopes, we present oxygen (δ¹⁸O) and strontium (⁸⁷Sr/⁸⁶Sr) isotopes for one of numerous barite chimneys in a low‐temperature (~20 °C) venting area of the Loki's Castle black smoker field at the ultraslow‐spreading Arctic Mid‐Ocean Ridge (AMOR). The chemistry of the venting fluids in the barite field identifies a contribution of at least 10% of high‐temperature black smoker fluid, which is corroborated by ⁸⁷Sr/⁸⁶Sr ratios in the barite chimney that are less radiogenic than in seawater. In contrast, oxygen and multiple sulfur isotopes indicate that the fluid from which the barite precipitated contained residual sulfate that was affected by microbial sulfate reduction. A sulfate reduction zone at this site is further supported by the multiple sulfur isotopic composition of framboidal pyrite in the flow channel of the barite chimney and in the hydrothermal sediments in the barite field, as well as by low SO₄ and elevated H₂S concentrations in the venting fluids compared with conservative mixing values. We suggest that the mixing of ascending H₂‐ and CH₄‐rich high‐temperature fluids with percolating seawater fuels microbial sulfate reduction, which is subsequently recorded by barite formed at the seafloor in areas where the flow rate is sufficient. Thus, low‐temperature precipitates in hydrothermal systems are promising sites to explore the interactions between the geosphere and biosphere in order to evaluate the microbial impact on these systems.     

Redox properties of heme peroxidases

Peroxidases are heme enzymes found in bacteria, fungi, plants and animals, which exploit the reduction of hydrogen peroxide to catalyze a number of oxidative reactions, involving a wide variety of organic and inorganic substrates. The catalytic cycle of heme peroxidases is based on three consecutive redox steps, involving two high-valent intermediates (Compound I and Compound II), which perform the oxidation of the substrates. Therefore, the thermodynamics and the kinetics of the catalytic cycle are influenced by the reduction potentials of three redox couples, namely Compound I/Fe³⁺, Compound I/Compound II and Compound II/Fe³⁺. In particular, the oxidative power of heme peroxidases is controlled by the (high) reduction potential of the latter two couples. Moreover, the rapid H₂O₂-mediated two-electron oxidation of peroxidases to Compound I requires a stable ferric state in physiological conditions, which depends on the reduction potential of the Fe³⁺/Fe²⁺ couple. The understanding of the molecular determinants of the reduction potentials of the above redox couples is crucial for the comprehension of the molecular determinants of the catalytic properties of heme peroxidases.This review provides an overview of the data available on the redox properties of Fe³⁺/Fe²⁺, Compound I/Fe³⁺, Compound I/Compound II and Compound II/Fe³⁺ couples in native and mutated heme peroxidases. The influence of the electron donor properties of the axial histidine and of the polarity of the heme environment is analyzed and the correlation between the redox properties of the heme group with the catalytic activity of this important class of metallo-enzymes is discussed.     

Appropriate biotechnology for sustainable agriculture in developing countries

Many transnational organizations are investing heavily in biotechnological research¹. They are primarily interested in activities such as the sale of chemicals and/or food processing. Consequently, research leading to an expansion in the use of chemicals or a reduction of commodity prices is advantageous to those companies. An increase in the sale of chemicals can, for instance, be expected as a result of research on herbicide resistance², a further reduction of commodity prices can be stimulated by biotechnological research directed at cost reduction or finding cheaper substitutes³. Western governmental research institutes and universities contribute to these research directions by cooperating closely with these companies^4,5.In view of these developments, it can be expected that biotechnological research will contribute to a further decrease in commodity prices and further instability of the agricultural structure in many developing countries and, consequently, an acceleration of migration to the already overcrowded cities.The question is, can biotechnology also contribute to sustainable development in rural areas by assisting small-scale and semi-subsistence farmers? I suggest it can.     

The time-related subcellular distribution of chromium in the rat liver cell after intravenous administration of Na2 51CrO4

After intravenous administration of Na₂ ⁵¹CrO₄ to rats the subcellular distribution of⁵¹Cr was determined at different time intervals after dosage. A time-related compartment shift from the cytosol into the mitochondrial and nuclear fractions was demonstrated. Dialysis studies indicated a firmer binding of⁵¹Cr to the mitochondrial and nuclear fractions than to the cytosol. Indirect evidence is presented that reduction from CrVI to CrIII takes place primarily inside the mitochondria. The hypothesis is put forward that reduction from Cr^VI to Cr^III may take place at any intracellular site where electron donors are available. Electron donors in the different intracellular organelles are discussed.     

Differential responses of freshwater wetland soils to sulphate pollution

Sulphate (SO₄ ^2-)reduction rates are generally low in freshwaterwetlands and are regulated by the scarceavailability of the ion. Increasedconcentrations of this electron acceptor due tosulphur (S) pollution of groundwater andsurface water may, however, lead to highSO₄ ^2- reduction rates now regulatedby the availability of appropriate electrondonors. Due to variations in this availability,the response to S pollution (e.g. from surfacewater or groundwater) is expected to differbetween soils. This hypothesis was tested inlaboratory mesocosm experiments by comparingtwo wetland soil types with distinctlydifferent humus profiles: a Hydromoder and aRhizomull type. In the first type, expected tohave a higher availability of degradable soilorganic matter (SOM), SO₄ ^2-availability appeared to be rate limiting forSO₄ ^2- reduction. In the Rhizomullsoils, in contrast, the electron acceptor didnot limit SO₄ ^2- reduction rates athigher concentrations. These differences inresponse could not, however, be attributed todifferences in the various SOM fractions or inSOM densities. Eutrophication and free sulphideaccumulation, two major biogeochemical problemscaused by SO₄ ^2- pollution, occurredin both types. The absolute extent ofphosphorus mobilisation was determined by theconcentration of this element in the soil (C/Pratio), while the level of sulphideaccumulation was governed by the concentrationof dissolved iron in the pore water. It wastherefore concluded that neither the humusprofile nor the concentrations of different SOMfractions in the soils are reliable indicatorsfor the sensitivity of wetland types to Spollution.     

Oxido-reduction kinetics of Signal II slow in tris-washed chloroplasts

In this report, we characterize the relationship between species “Z” (giving rise to EPR Signal II fast) and “D” (EPR Signal II slow) in triswashed chloroplasts.At pH 8.5 an externally added donor phenylenediamine competes with D for Z⁺ reduction after its oxidation by a flash. The reduction of Z⁺ by D occurs within some milliseconds. In a subsequent dark period, D⁺ is reduced by PD, the reaction rate being independant of phenylenediamine concentration. These results are consistent with the hypothesis of an equilibrium between Z⁺D and ZD⁺, the reduction of D by phenylenediamine occuring via Z. At lower pH's, the connection between Z and D is looser: a high concentration of phenylenediamine which reduces rapidly Z⁺, is very slow in reducing D⁺ and the subsequent photooxidation of D is less efficient.     

Disruption of sulfur cycling and acid neutralization in lakes at low pH

Experimental acidification of a softwater lake to below pH 5 fundamentally changed the sulfur cycle and lowered internal alkalinity generation (IAG). Prior to reaching pH 4.5, the balance of sulfur reduction and oxidation reactions within the lake was in favour of reduction, and the lake was a net sink for sulfate. In the four years at pH 4.5 the balance of reduction and oxidation reactions was in favour of oxidation, and there was a net production of sulfate (SO₄ ^2–) within the lake. Evidence indicating a decrease in net SO₄ ^2– reduction at pH 4.5 was also obtained in an anthropogenically acidified lake that had been acidified for many decades. In both lakes, the decrease in net SO₄ ^2– reduction appeared to be linked not to a simple inhibition of SO₄ ^2– reduction but rather to changes in benthic ecosystem structure, especially the development of metaphytic filamentous green algae, which altered the balance between SO₄ ^2– reduction and sulfur oxidation.At pH's above 4.5, net SO₄ ^2– reduction was the major contributor to IAG in the experimental lake, as it is in many previously studied lakes at pH 5 and above. At pH 4.5, the change in net annual SO₄ ^2– reduction (a decrease of 110%) resulted in a 38% decrease in total IAG. Because of the important role of net SO₄ ^2– reduction in acid neutralization in softwater lakes, models for predicting acidification and recovery of lakes may need to be modified for lakes acidified to pH <5.     

Chemical and Biological Interactions during Nitrate and Goethite Reduction by Shewanella putrefaciens 200

Although previous research has demonstrated that NO₃⁻ inhibits microbial Fe(III) reduction in laboratory cultures and natural sediments, the mechanisms of this inhibition have not been fully studied in an environmentally relevant medium that utilizes solid-phase, iron oxide minerals as a Fe(III) source. To study the dynamics of Fe and NO₃⁻ biogeochemistry when ferric (hydr)oxides are used as the Fe(III) source, Shewanella putrefaciens 200 was incubated under anoxic conditions in a low-ionic-strength, artificial groundwater medium with various amounts of NO₃⁻ and synthetic, high-surface-area goethite. Results showed that the presence of NO₃⁻ inhibited microbial goethite reduction more severely than it inhibited microbial reduction of the aqueous or microcrystalline sources of Fe(III) used in other studies. More interestingly, the presence of goethite also resulted in a twofold decrease in the rate of NO₃⁻ reduction, a 10-fold decrease in the rate of NO₂⁻ reduction, and a 20-fold increase in the amounts of N₂O produced. Nitrogen stable isotope experiments that utilized δ¹⁵N values of N₂O to distinguish between chemical and biological reduction of NO₂⁻ revealed that the N₂O produced during NO₂⁻ or NO₃⁻ reduction in the presence of goethite was primarily of abiotic origin. These results indicate that concomitant microbial Fe(III) and NO₃⁻ reduction produces NO₂⁻ and Fe(II), which then abiotically react to reduce NO₂⁻ to N₂O with the subsequent oxidation of Fe(II) to Fe(III).     

A mechanistic study of ferrioxamine B reduction by the biological reducing agent ascorbate in the presence of an iron(II) chelator

The iron overload drug desferal (desferrioxamine B) forms the stable iron complex ferrioxamine B. The reduction potential of ferrioxamine B (E^o = −482 mV versus NHE pH 7) prohibits its reduction by biological reducing agents such as ascorbate, but it was found that the iron(II) chelator 2,2′-bipyridine (bipy) facilitates this reduction. Evidence is given to support the formation of a ternary complex between iron, bipy, and desferrioxamine B as the key step in facilitating the reduction. The equilibrium constant for the formation of the ternary complex was found to be 8.9 × 10⁷ and ternary complex formation is explained in terms of a three step mechanism. The mechanism for the reduction of ferrioxamine B is discussed in terms of rapidly established pre-equilibria which include ternary complex formation, ascorbic acid deprotonation, and encounter complex formation between ascorbate and the ternary complex. These equilibria are followed by rate limiting reduction of the ternary complex. Bipy was found to be a similar facilitator to sulfonated bathophenanthroline for the reduction of ferrioxamine B by ascorbate.     

Anaerobic filter treatment of fishery wastewater

Anaerobic treatment of wastewater from a selected seafood processing plant was conducted at organic loading rates (OLR) ranging from 0.3 to 1.8 kg chemical oxygen demand (COD)/m³.day and hydraulic retention times (HRT) ranging from 36 to 6 days. COD reduction decreased with increasing OLR. More than 75% COD reduction could be maintained up to an OLR of about 1 kg COD/m³.day with an HRT of 11 days. An OLR of 1.3 kg COD/m³.day corresponding to an HRT of 6.6 days gave maximal biogas productivity of 1.5 m³/m³.day or 1.3 m³ biogas/kg COD with a 65% COD reduction. If the HRT was kept constant at 11 days, an OLR of 1.3 kg COD/m³.day achieved maximal biogas productivity (1.1 m³/m³.day) and yield (0.75 m³/kg COD) and a 60% COD reduction for treatment of tuna condensate.P. Prasertsan and S. Jung are with the Department of Agro-Industry, Faculty of Natural Resources, Prince of Songkla University, Hatyai 90110, Thailand. K.A. Buckle is with the Department of Food Science and Technology, University of New South Wales, Kensington, NSW 2033, Australia.     

Nitrate Reduction in Roots and Shoots of Barley (Hordeum vulgare L.) and Corn (Zea mays L.) Seedlings: I. N Study

Nitrate reduction in roots and shoots of 7-day-old barley seedlings, and 9-day-old corn seedlings was investigated. The N-depleted seedlings were transferred for 24 h or 48 h of continuous light to a mixed nitrogen medium containing both nitrate and ammonium. Total nitrate reduction was determined by ¹⁵N incorporation from ¹⁵NO₃⁻, translocation of reduced ¹⁵N from the roots to the shoots was estimated with reduced ¹⁵N from ¹⁵NH₄⁺ assimilation as tracer, and the translocation from the shoots to the roots was measured on plants grown with a split root system. A model was proposed to calculate the nitrate reduction by roots from these data. For both species, the induction phase was characterized by a high contribution of the roots which accounted for 65% of the whole plant nitrate reduction in barley, and for 70% in corn. However, during the second period of the experiment, once this induction process was finished, roots only accounted for 20% of the whole plant nitrate reduction in barley seedlings, and for 27% in corn. This reversal in nitrate reduction localization was due to both increased shoot reduction and decreased root reduction. The pattern of N exchanges between the organs showed that the cycling of reduced N through the plant was important for both species. In particular, the downward transport of reduced N increased while nitrate assimilation in roots decreased. As a result, when induction was achieved, the N feeding of the roots appeared to be highly dependent on translocation from the leaves.