Inhibition of Nitrate Assimilation in Roots in the Presence of Ammonium: The Moderating Influence of Potassium

Experiments were conducted to investigate the effect of concentrationof NH₄⁺ in nutrient solution on root assimilation of NO₃^–and to determine whether the NH₄⁺NO₃^– interaction wasmodified in the presence of K⁺. Dark-grown, detopped corn seedlings(cv. Pioneer 3369A) were exposed for 8 h to 0.15 mM Ca(NO₃)₂and varying concentrations of (NH₄)₂SO₄ in the absence or presenceof 0.15 mM K₂SO₄. The accelerated phase of NO₃^– uptakeappeared most sensitive to restriction by additions of 0.15mM (NH₄)₂SO₄. In the absence of K⁺, the restriction increasedonly slightly even when solution (NH₄)₂SO₄, was increased from0.15 mM to 12.5 mM which was accompanied by an increase of NH₄⁺in the tissue from about 7.0 to 35 µmol g^–1 fr.wt. of root. Increasing concentrations of solution NH₄⁺ progressivelyinhibited net K+ uptake. At the highest solution NH₄⁺ concentrations,there was an initial net efflux of K⁺ and no net influx occurredduring the treatment period. The severity of the NH₄)SO₄ restrictionof NO₃^– uptake was moderated considerably in the presenceof K⁺ as long as a net influx of K⁺ occurred. However, net influxof K⁺ was not associated with alteration of NH₄⁺ uptake, assimilation,or accumulation in the root tissue. The lack of correlationbetween the severity of restriction of NO₃^– uptake andendogenous NHJ suggested the restriction resulted from an effectexerted by exogenous NH₄⁺ which tended to saturate at lowersolution NHJ concentrations or by inhibitory factors generatedduring assimilation of NH₄⁺. Several mechanisms were postulatedto account for the moderating influence of K⁺. In all experiments,root NO₃^– reduction was restricted by the presence ofambient NH₄⁺. The quantitative decreases in reduction tendedto be less than decreases in NO₃^– uptake and therefore,could result from inhibition solely of uptake with subsequentlimitation in availability of substrate for the reduction process,but the possibility of a direct effect on reduction could notbe excluded.     

The Influence of Nitrate and Ammonium Nutrition on the Growth of Wheat (Triticum aestivum) and Maize (Zea mays) Plants

The effects of NO^-₃ and NH⁺₄ nutrition on hydroponically grownwheat (Triticum aestivum L.) and maize (Zea mays L.) were assessedfrom measurements of growth, gas exchange and xylem sap nitrogencontents. Biomass accumulation and shoot moisture contents ofwheat and maize were lower with NH⁺₄ than with NO^-₃ nutrition.The shoot:root ratios of wheat plants were increased with NH⁺₄compared to NO^-₃ nutrition, while those of maize were unaffectedby the nitrogen source. Differences between NO^-₃ and NH⁺₄-fedplant biomasses were apparent soon after introduction of thenitrogen into the root medium of both wheat and maize, and thesedifferences were compounded during growth. Photosynthetic rates of 4 mM N-fed wheat were unaffected bythe form of nitrogen supplied whereas those of 12 mM NH⁺₄-fedwheat plants were reduced to 85% of those 12 mM NO^-₃-fed wheatplants. In maize supplied with 4 and 12 mM NH⁺₄ the photosyntheticrates were 87 and 82% respectively of those of NO^-₃-fed plants.Reduced photosynthetic rates of NH⁺₄ compared to NO^-₃-fed wheatand maize plants may thus partially explain reduced biomassaccumulation in plants supplied with NH⁺₄ compared to NO^-₃ nutrition.Differences in the partitioning of biomass between the shootsand roots of NO^-₃-and NH⁺₄-fed plants may also, however, arisefrom xylem translocation of carbon from the root to the shootin the form of amino compounds. The organic nitrogen contentof xylem sap was found to be considerably higher in NH⁺₄- thanin NO^-₃-fed plants. This may result in depletion of root carbohydrateresources through translocation of amino compounds to the shootin NH⁺₄-fed wheat plants. The concentration of carbon associatedwith organic nitrogen in the xylem sap of maize was considerablyhigher than that in wheat. This may indicate that the shootand root components of maize share a common carbon pool andthus differences induced by different forms of inorganic nitrogenare manifested as altered overall growth rather than changesin the shoot:root ratios.Copyright 1993, 1999 Academic Press Triticum aestivum, wheat, Zea mays, maize, nitrogen, growth, photosynthesis, amino acids, xylem     

Photosynthetic Nitrogen Metabolism in High and Low CO2-adapted Scenedesmus: II. EFFECT OF AMMONIUM AND METHIONINE SULPHOXIMINE ON NITRATE UTILIZATION

Larsson, C.-M., Larsson, M. and Guerrero, M. G. 1985. Photosyntheticnitrogen metabolism in high and low CO²-adapted Scenedesmus.II. Effect of ammonium and methionine sulphoximine on nitrateutilization.—J. exp. Bot. 36: 1387–1395 In 3% CO²-grown Scenedesmus obtusiusculus Chod. utilizing NO₃^–J as the N source, NH₄⁺ addition caused a prompt inhibitionof NO₃^– utilization. Nitrate reductase (NR) activity declinedrapidly in response to the presence of NO₄⁺, but the cessationof NO₃^– utilization was too rapid to be accounted forby the loss in NR activity. The first site of NO₄⁺ inhibitionin these cells seems to be the entrance of NO₃^– into thecells. Upon exhaustion of NO₄⁺ from the medium, NO₃^– utilizationwas rapidly restored and NR activity increased. Air-grown cellswere much less sensitive to the effect of NO₄⁺, more than 30min being required for added NO₄⁺ to cause complete inhibitionof NO₃^– utilization. In these cells, NO₃^– uptakeand NR activity decreased in parallel in response to NO₄⁺ addition.In 3% CO²-grown cells simultaneously subjected to NO₄⁺ and air-levelof CO², NO₄⁺ initially inhibited NO₃^– utilization completely,but a slight recovery took place after approximately 20 min The glutamine synthetase (GS) inhibitor L-methionine D, L-sulphoximine(MSO) behaved as a potent inhibitor of NO₃^– uptake in3% CO²-grown cells, but had considerably less effect in air-growncells, although the time-course of the MSO-induced inhibitionof GS was the same in both cases Key words: Ammonium, nitrate utilization, Scenedesmus     

The Influence of NO-3 and NH+4 Nutrition on the Gas Exchange Characteristics of the Roots of Wheat (Triticum aestivum) and Maize (Zea mays) Plants

Respiratory oxygen consumption by roots was 1·4- and1·6-fold larger in NH⁺₄-fed than in NO^-₃-fed wheat (Triticumaestivum L.) and maize (Zea mays L.) plants respectively. Higherroot oxygen consumption in NH⁺₄-fed plants than in NO^-₃-fedplants was associated with higher total nitrogen contents inNH⁺4-fed plants. Root oxygen consumption was, however, not correlatedwith growth rates or shoot:root ratios. Carbon dioxide releasewas 1·4- and 1·2-fold larger in NO⁺3-fed thanin NH⁺₄-fed wheat and maize plants respectively. Differencesin oxygen and carbon dioxide gas exchange rates resulted inthe gas exchange quotients of NH^-₄-fed plants (wheat, 0·5;maize, 0·6) being greatly reduced compared with thoseof NO^-₃-fed plants (wheat, 1·0; maize, 1·1). Measuredrates of HCO^-₃ assimilation by PEPc in roots were considerablylarger in 4 mM NH⁺₄-fed than in 4 NO^-₃ plants (wheat, 2·6-fold;maize, 8·3-fold). These differences were, however, insufficientto account for the observed differences in root carbon dioxideflux and it is probable that HCO^-₃ uptake is also importantin determining carbon dioxide fluxes. Thus reduced root extension in NH⁺₄-fed compared with NO^-₃-fedwheat plants could not be ascribed to differences in carbondioxide losses from roots.Copyright 1993, 1999 Academic Press Triticum aestivum, wheat, Zea mays, maize assimilation, ammonium assimilation, root respiration     

Function and contribution of the root tip in the induction of NO3- uptake along the barley root axis

The seminal roots of N-free-grown barley seedlings were ableto take up NO₃^– immediately upon initial exposure; theuptake rate in the tip was half of that in the older root zones(middle and base). A lag of 60 min was required in all rootzones before the uptake rates started to increase during inductionwith external NO₃^–. This increase could be prevented bythe addition of pFPA; we thus assume that additional NO₃^–transport proteins were synthesized during NO₃^– induction.During the time-course of NO₃^– induction different uptakerates were measured in morphologically different regions ofthe tip (1 mm segments) indicating a regulation of NO₃^–induction on a narrow local scale. In NO₃^– grown plants, NO₃^– uptake as well as NO₃^–content increased basipetally along the root axis concomitantlywith increasing vacuolization of the cells. Although NO₃^–uptake into the tip was only half of that into the older rootzones, this NO₃^– uptake was very important for the entireroot. Firstly, it provided the substrate for protein biosynthesisin the meristematic region: nitrate reductase activity and totalsoluble protein were highest in the first apical mm of the tip.Secondly, 3% of the NO₃^– taken up by the tip was foundin the base where it induced NO₃^– uptake: NO₃^– wastranslocated almost exclusively basipetally and as little as20nmolg^–1 root fr. wt. translocated from the tip weresufficient for acceleration of NO₃^– induction in the rootbase of N-free-grown plants. This clearly shows that the inductionof NO₃^– uptake does not depend exclusively on the availabilityof external NO₃^–, but can be mediated also with internallytranslocated NO₃^–.The root tip, therefore, may be consideredthe NO₃^– sensing region of the root. Key words: Barley, Hordeum vulgare L, internal NO₃^–, NO₃^– uptake, root zones     

The Effect of Various Nitrogen Sources upon the Production of Extracellular Polysaccharide by the Blue-Green Alga Anabaena flos-aquae A-37

Anabaena flos-aquae A-37 was grown in bacteria-free cultureon a variety of nitrogen sources. Extracellular polysaccharideproduction was found to be a part of the normal metabolic processescausing the liberation of excess carbohydrates into the surroundingmedium rather than the result of cellular lysis. Non-adaptedcells supplied with NH₄Cl produced abundant polysaccharide.However, the population did not increase. Cells adapted to NH₄Clproduced smaller quantities of polysaccharide, but the populationdid increase. Polysaccharide production per cell was similaron Mg(NO₃)₂, KNO₃, NaN0₃, NH₄NO₃, and NH₄Cl. It was concludedthat an adequately utilized nitrogen source does not affectpolysaccharide production in A. flos-aquae A-37.     

Effect of Denitrification on Nitrogen Fixation in Light in a Photodenitrifier, Rhodopseudomonas sphaeroides forma sp. denitrificans

The effect of denitrification on N₂ fixation was studied ina denitrifying photosynthetic bacterium, Rhodopseudomonas sphaeroidesforma sp. denitrificans. KNO₃ inhibited diazotrophic growthin light, but NC₃–-dependent diazotrophic growth in darknesswas found. NO₃– inhibited C₂H₂ reduction activity in lightin cells grown with NO₃–. NO₃–-dependent C₂H₂ reductionactivity in darkness also was present in cells grown with N₂plus NO₃–, but not in cells grown on glutamate with NO₃–.NO₃– repressed the synthesis of nitrogenase in light.This repression was not overcome by the addition of methioninesulfoximine. The inhibitory and repressive effect of NO₃– was not mediatedby the NO₂– produced from NC₃– nor by the NH₄+ excretedinto the medium. But, as N₂ fixation is controlled by O₂ (redoxcontrol) it seems to be mediated through the denitrificationprocesses. Much of the glutamine synthetase was adenylylatedin cells grown with NO₃– and its adenylylation state closelyparallelled nitrogenase activity in the cells. (Received September 4, 1982; Accepted December 11, 1982)     

Nitrate transport in intact wheat roots:II. Long-term effects of NO3- concentration in the nutrient solution on NO3- unidirectional fluxes and distribution within the tissues5

We have examined the long-term effects of NO₃^– concentrationson NO₃^– (¹⁵NO₃^–) fluxes and cellular pool sizesin roots of intact 30-d-old wheat (Triticum aestivum cv. Courtot)grown hydroponically. Compartmental analysis was performed understeady-state conditions at five different levels of NO₃^–concentration (from 0.1 up to 5 mol m^–3 taking into accountmetabolism and secretion into the xylem (Devienne et al., 1994).Nitrate and reduced nitrogen levels in the tissues were largelyindependent of external NO₃^– concentration although below1.5 mol m^–3 NO₃^–; concentration limited plant growth.In the chamber, marked diurnal variations in net uptake occurredand, in the light, higher NO₃^– concentrations yieldedhigher NO₃^– uptake rates. After transfer of the plantsto the laboratory, the increase in net uptake linked to elevationof NO₃^–; concentrations was even larger (from 0.1 to 8.8µmolh^–1 g^–1 FW) as a result of a marked increase (x10–11) in the unidirectional influx at the plasmalemmawhile NO₃^– efflux was less enhanced (x 4–5). Underthese conditions, influx into the vacuole was also higher (x2–4) while efflux from the vacuole was little affected(x 1–3). NO₃^– concentrations within the cell compartmentswere estimated under the clas sical assumptions. The vacuolarconcentration was a little modified by NO₃^– availabilitywhereas that in the cytosol increased from about 10 mol m^–3to about 20 mol m^–3 indicating that (1) the absolute valuefor the cytosol was high and (2) it displayed only a small increasedespite very large changes in NO₃^– fluxes. NO₃^–distribution within the cells did not seem to involve an activeaccumulation of NO₃^– in the vacuole. Key words: Wheat, ion transport, nitrate, ¹⁵N, compartmentation     

Interactions of NH4+ and L-glutamate with NO3- transport processes of non-mycorrhizal Fagus sylvatica roots

The processes of NO₃^– uptake and transport and the effectsof NH₄⁺ or L-glutamate on these processes were investigatedwith excised non-mycorrhizal beech (Fagus sylvatica L.) roots.NO₃^– net uptake followed uniphasic Michaelis-Menten kineticsin a concentration range of 10µM to 1 mM with an apparentK_m of 9.2 µM and a V_max of 366 nmol g^–1 FW h^–1.NH₄⁺, when present in excess to NO₃^–, or 10 mM L-glutamateinhibited the net uptake of NO₃^– Apparently, part of NO₃^–taken up was loaded into the xylem. Relative xylem loading ofNO₃^– ranged from 3.21.6 to 6.45.1% of NO₃^– netuptake. It was not affected by treatment with NH₄⁺ or L-glutamate.¹⁶N/¹³N double labelling experiments showed that NO₃^–efflux from roots increased with increasing influx of NO₃^–and, therefore, declined if influx was reduced by NH₄⁺ or L-glutamateexposure. From these results it is concluded that NO₃^–net uptake by non-mycorrhizal beech roots is reduced by NH₄⁺or L-glutamate at the level of influx and not at the level ofefflux. Key words: Nitrate transport, net uptake, influx, efflux, ammonium, Fagus, Fagaceae     

Soil nitrogen form and plant nitrogen uptake along a boreal forest productivity gradient

We present results from a study of soil solution concentrations of ammonium (NH₄⁺), nitrate (NO₃^-), and amino acid N over one growing season along a local 90-m-long plant productivity gradient in a boreal forest. Three forest types are found along the gradient: an ericaceous dwarf-shrub type between 0 and 40 m, a low-herb type between 40 and 80 m, and a tall-herb type at 90 m. Soil sampling of the mor layer was performed in June, July, August and October in the three forest types. In addition, plant uptake of NH₄⁺, NO₃^- and the amino acid glycine was investigated. A mixture of the three N forms was injected into the soil; one N form at a time was labeled with ¹⁵N, and in the case of glycine also with ¹³C. In the dwarf-shrub forest, where plant productivity was low, the soil N pool was strongly dominated by amino acid N. There, plants took up more NH₄⁺ than NO₃^-. Glycine uptake did not differ significantly from either NH₄⁺ or NO₃^- uptake. Along the gradient, soil concentrations of NH₄⁺ and NO₃^- increased, as did plant productivity. In the low-herb forest NH₄⁺ comprised a major portion of the soil N pool, and plants took up more NH₄⁺ than NO₃^- or glycine. In the tall-herb forest, NO₃^- was as abundant as NH₄⁺, and together these two N forms dominated the soil N pool. Here, plants took up nearly equal amounts of NO₃^- and NH₄⁺, and this uptake exceeded that of glycine severalfold. Apart from the overall preference for NH₄⁺ that plants exhibited throughout the gradient, the results show a correlation between soil concentrations of amino acids and NO₃^- and plant preferences for these N forms.     

Determination of Levels of NO-3, NO-2 and NH+4 Ions in Leaves of Various Plants by Capillary Electrophoresis

Levels of NO^-₃, NO^-₂ and NH⁺₄ ions in leaves of six plant specieswere determined by capillary electrophoresis. Levels of NO^-₃ions differed by a factor of more than 350 in the six species.NO^-₂ and NH⁺₄ ions were detected in all species examined butat lower and more similar respective levels than NO^-₃ ions. (Received March 8, 1996; Accepted June 24, 1996)     

Influence of nitrate on uptake of ammonium by nitrogen-depleted soybean: is the effect located in roots or shoots?

In non-nodulated soybean [Glycine max (L.) Merrill cv. Ransom]plants that were subjected to 15 d of nitrogen deprivation inflowing hydroponic culture, concentrations of nitrogen declinedto 1.0 and 1.4mmol Ng^–1 dry weight in shoots and roots,respectively, and the concentration of soluble amino acids (determinedas primary amines) declined to 40µmol g^–1 dry weightin both shoots and roots. In one experiment, nitrogen was resuppliedfor 10 d to one set of nitrogen-depleted plants as 1.0 mol m^–3NH₄⁺ to the whole root system, to a second set as 0.5 mol m^–3NH₄⁺ plus 0.5 mol m^–3 NO₃^– to the whole root system,and to a third set as 1.0 mol m^–3 NH₄⁺ to one-half ofa split-root system and 1.0 mol m^–3 NO₃^– to theother half. In a second experiment, 1.0 mol m^–3 of nitrogenwas resupplied for 4 d to whole root systems in NH₄⁺ : NO₃^–ratios of 1:0, 9:1, and 1:1. Nutrient solutions were maintainedat pH 6.0. When NH₄⁺ was resupplied in combination with NO₃^– to thewhole root system in Experiment I, cumulative uptake of NH₄⁺for the 10 d of resupply was about twice as great as when NH₄⁺was resupplied alone. Also, about twice as much NH₄⁺ as NO₃^–was taken up when both ions were resupplied to the whole rootsystem. When NH₄⁺ and NO₃^– were resupplied to separatehalves of a split-root system, however, cumulative uptake ofNH₄⁺ was about half that of NO₃^–. The uptake of NH₄⁺,which is inhibited in nitrogen-depleted plants, thus is facilitatedby the presence of exogenous NO₃^–, and the stimulatingeffect of NO₃^– on uptake of NH₄⁺ appears to be confinedto processes within root tissues. In Experiment II, resupplyof nitrogen as both NH₄⁺ and NO₃^– in a ratio of either1:1 or 9:1 enhanced the uptake of NH₄⁺. The enhancement of NH₄⁺uptake was 1.8-fold greater when the NH₄⁺: NO₃^–-resupplyratio was 1:1 than when it was 9:1; however, only 1.3 timesas much NO₃^– was taken up by plants resupplied with the1 :1 exogenous ratio. The effect of NO₃^– on enhancementof uptake of NH₄⁺ apparently involves more than net uptake ofNO₃^– itself and perhaps entails an effect of NO₃^–uptake on maintenance of K⁺ availability within the plant. Theconcentration of K⁺ in plants declined slightly during nitrogendeprivation and continued to decline following resupply of nitrogen.The greatest decline in K⁺ concentration occurred when nitrogenwas resupplied as NH₄⁺ alone. It is proposed that decreasedavailability of K⁺ within the NH₄⁺-resup-plied plants inhibitedNH₄⁺ uptake through restricted transfer of amino acids fromthe root symplasm into the xylem. Key words: Ammonium, Glycine max, nitrate, nitrogen-nutrition, nitrogen stress, split-root cultures     

Nitrate Transport into Chara corallina Cells using 36C1O3 as an Analogue for Nitrate: II. COMPARISON WITH 14C METHYLAMINE FLUXES AT DIFFERENT pH0 AND NH+4sol;NO3 INTERACTIONS

³⁶C1O₃/NO₃ influx into Chara cells was found to be sensitiveto pH_o and a maximum was found at pH_o = 4.5. By contrast ¹⁴Cmethylamine influx into Chara showed a maximum at pH_o = 8.5,and at this pH_o influx rates were about 150 times higher thanrates of ³⁶C1O₃/NO₃ influx. However, at pH_o = 4.5, ³⁶C1O₃/NO₃influx rates were, in some cases, comparable with rates of ¹⁴Cmethylamine influx. ³⁶C1O₃/NO₃ influx into Chara cells was stimulatedby Rb ⁺, K⁺, Na ⁺, and NH₄⁺, but not by Cs⁺ or Li ⁺. NO₃ andCl reduced ¹⁴C methylamine influx into Chara by 30%. NH₄⁺ causedvery considerable inhibition of ¹⁴C methylamine influx intoChara, but had no effect on ³⁶C1O₃/NO₃ influx in the presenceof K ⁺. Net NO³ uptake into Chara was completely prevented byNH₄⁺ even at relatively low NH₄⁺ concentrations (25 mmol m ^–3).This latter effect was reversed by diethylstilbestrol (DES).Evidence is presented for the stimulation of NO₃ efflux by NH⁴⁺as the mechanism responsible for the immediate effects of NH₄⁺on net NO₃ uptake into Chara cells. Key words: Chara, ¹⁴C methylamine, ³⁶ClO^–₃, pH     

Cortical Cell Fluxes of Ammonium and Nitrate in Excised Root Segments ofAllium cepa L; Studies using15N

From compartmental analysis of ¹⁵N elution measurements, concentrationsand fluxes of NH⁺₄ and NO₃^– were estimated for corticalcells in excised root segments, when bathed in a complete nutrientsolution, in which 20 mol m^–3 NH₄⁺ or NO₃^– werethe single N sources. The results were compared with those fornutrient solution containing 20 mol m^–3 NH₄NO₃. No nitratereductase activity was detected in the roots but rapid assimilationof NH₄⁺ occurred, due to glutamine synthetase activity. Theefflux curves for NH₄⁺, on a 'µg ¹⁵N remaining againsttime' basis, deviated from the criteria determining conformityto first order kinetics, since the slowest rate constant wasan order of magnitude lower than that exhibited by the curvefor efflux versus time. The data were transformed to conformto the appropriate criteria, revealing a large slowly exchangingpool equated with assimilated NH₄⁺. The presence of NO₃^–had little effect on NH₄⁺ uptake and exchange, but NH₄⁺ suppressedNOj uptake and reduced exchange across plasmalemma and tonoplast.It was established that NH₄⁺ absorption was an active process.However, NH₄⁺ entering and leaving the vacuole was overestimated,since the flux equation used did not differentiate between total¹⁵NH₄ influx at the plasmalemma and that at the tonoplast, afterassimilation. The only active NO₃^– transfer was influxat the plasmalemma. The results were compared with those ofothers using¹³N and ³⁶C1O₃ analogues to measure NH₄⁺ and NO₃^–fluxes in cereal roots. Key words: Ammonium, nitrate, compartmental analysis, ¹⁵N, active transport     

Changes in the growth rates of saline-lake diatoms in response to variation in salinity, brine type and nitrogen form

The growth rates of four saline-lake diatom taxa were measuredunder varying conditions of salinity (5, 8 and 11), brine type(sulfate- versus bicarbonate-dominated) and nitrogen form (NH₄⁺versus NO₃^–), using a full factorial design. With NO₃^–as the nitrogen source, Cyclotella quillensis, Cymbella pusillaand Anomoeoneis costata exhibited lower growth rates in thesulfate versus bicarbonate media. The strain of Chaetoceroselmorei used in these experiments, isolated from a sulfate-dominatedlake, was unable to grow on NO₃^– alone. In the NH₄⁺ treatments,neither salinity nor brine type affected the growth rates ofC.quillensis or C.elmorei. When supplied with NH₄⁺, C.pusillaand A.costata had higher growth rates in the bicarbonate versussulfate media, although for C.pusilla the difference on NH₄⁺was not as great as on NO₃^–. The impact of brine typeon NO₃^– use is consistent with the theory that sulfateinhibits molybdate uptake, as molybdenum is required for NO₃^–use but not NH₄⁺. Cymbella pusilla was the only taxon affectedby changes in salinity. The four taxa used in these experimentsare frequently found in saline lakes and saline-lake sediments,hence they are used in paleoclimate reconstructions; the resultspresented here provide additional information that may enhancethese diatom-based reconstructions.     

Synchronization of Phosphorylation of a Chloroplast Protein with the Cell Division Cycle in Heterosigma akashiwo

Fumigation of plants of five species with NO₂ in darkness causedvisible injuries to leaves, with the most severe injuries inkidney bean plants and the least severe in spinach plants. Fumigationof these plants in the light caused virtually no visible injuries.NO₂-fumigated leaves accumulated nitrite in the darkness butnot in the light. The level of accumulated NO₂^– was decreasedby light much more rapidly in spinach leaves than in those ofkidney bean, with much less injury to spinach leaves than tothose of kidney bean. A larger amount of NO₂^– accumulatedin the trifoliate leaves of kidney bean plants cultivated withNO₃^– as a main source of nitrogen than in those of plantscultivated with NH₄⁺, and the former plants were more susceptibleto injury from NO₂ than the latter. Administration of NO₂^–to leaves of spinach and kidney bean plants induced the destructionof Chi in the light. The extent of the destruction of Chi wassmaller in spinach than in kidney bean, consistent with theirrespective responses to NO₂. The NO₂^–-induced destructionof Chi was inhibited to some extent by scavengers of free radicals.Activities of superoxide dismutase (SOD) were higher in leavesof spinach than in those of kidney bean. These results indicatethat NO₂^– is the toxic species generated by fumigationwith NO₂ and that spinach has a greater tolerance for NO₂ thankidney bean, probably as a result both of a higher capacityfor reduction of NO₂^– and a higher level of activity ofSOD. (Received October 4, 1991; Accepted January 31, 1992)     

Diurnal regulation of NO3- uptake in soybean plants III. Implication of the Dijkshoorn-Ben Zioni model in relation with the diurnal changes in NO3- assimilation

According to the Dijkshoorn-Ben Zioni model, NO₃^– uptakein the roots is stimulated by NO₃^– assimilation in theshoots, through downward phloem transport of malate synthesizedin response to reduction of NO₂^– to NH³. In this paper,one hypothesis resulting from this model was tested, i.e. thatthe diurnal changes in NO₃^– uptake are due to the lightdependence of NO₃^– reduction in the leaves. This dependencewas studied in detached leaves transferred to deionized wateror supplied via the transpiration stream with similar amountsof ¹⁵NO₃^– in light or darkness. In the dark, the reductionof previously stored NO₃^– or xylem-borne ¹⁵NO₃^–was generally about 40–50% of that measured in the light.Glucose supply to the detached leaves stimulated NO₃^–reduction in the dark, but not enough to increase it up to thesame rate as in the light. Nitrite reduction in detached leaveswas much less affected by darkness, and could be maintainedat a high level by exogenous supply of substrate. Advantagewas taken from this last observation to sustain NO₂^–reductionin attached darkened shoots at the same rate as in the light,by ensuring an appropriate delivery of NO₂^– from the xylem.Although this was assumed to restore the light level of theassociated synthesis of malate, it led to a marked inhibitionof NO₃^– uptake. In addition, the direct supply of malateto the shoots or to the roots failed to prevent the decreaseof NO₃^– uptake in darkness. Thus, our conclusion is thatthe mechanisms evoked in the Dijkshoorn-Ben Zioni model do notplay an important role in the diurnal variations of NO₃^–uptake in soybean plants. Key words: Glycine max, light/dark cycle, malate synthesis, NO₃^– reduction, NO₃^– uptake     

A comparison of nitrate transport in four different rice (Oryza sativa L.) cultivars

As rice can use both nitrate (NO₃^-) and ammonium (NH₄⁺), we have tested the hypothesis that the shift in the pattern of cultivars grown in Jiangsu Province reflects the ability of the plants to exploit NO₃^- as a nitrogen (N) source. Four rice cultivars were grown in solution culture for comparison of their growth on NO₃^- and NH₄⁺ nitrogen sources. All four types of rice, Xian You 63 (XY63), Yang Dao 6 (YD), Nong Keng 57 (NK) and Si You 917 (SY917), grew well and produced similar amounts of shoot biomass with 1 mmol/L NH₄⁺ as the only N source. However, the roots of NK were significantly smaller in comparison with the other cultivars. When supplied with 1 mmol/L NO₃^-, YD produced the greatest biomass; while NK achieved the lowest growth among the four cultivars. Electrophysiological measurements on root rhizodermal cells showed that the NO₃^--elicited changes in membrane potential (ΔE_m) of these four rice cultivars were significantly different when exposed to low external NO₃^- (<1 mmol/L); while they were very similar at high external NO₃^- (10 mmol/L). The root cell membrane potentials of YD and XY63 were more responsive to low external NO₃^- than those of NK and SY917. The ΔE_m values for YD and XY63 rhizodermal cells were almost the same at both 0.1 mmol/L and 1 mmol/L NO₃^-; while for the NK and SY917 the values became larger as the external NO₃^- increased. For YD cultivar, ΔE_m was measured over a range of NO₃^- concentrations and a Michaelis-Menten fit to the data gave a K_m value of 0.17 mmol/L. Net NO₃^- uptake depletion kinetics were also compared and for some cultivars (YD and XY63) a single-phase uptake system with first order kinetics best fitted the data; while other cultivars (ND and SY917) showed a better fit to two uptake systems. These uptake systems had two affinity ranges: one had a similar K_m in all the cultivars (0.2 mmol/L); the other much higher affinity system (0.03 mmol/L) was only present in NK and SY917. The expression pattern of twelve different NO₃^- transporter genes was tested using specific primers, but only OsNRT1.1 and OsNRT2.1 expression could be detected showing significant differences between the four rice cultivars. The results from both the physiological and molecular experiments do provide some support for the hypothesis that the more popular rice cultivars grown in Jiangsu Province may be better at using NO₃^- as an N source.     

Nodule Function in Symbiotic Bambara Groundnut (Vigna subterraneaL.) and Kersting's Bean (Macrotyloma geocarpumL.) is Tolerant of Nitrate in the Root Medium

Nitrogen-fixing activity in two nodulated African legumes, Bambaragroundnut (Vigna subterraneaL.) and Kersting's bean (MacrotylomageocarpumL.), was assessed in the presence of nitrate (NO₃^-)ions in the rooting medium. Nitrogenase activity was unimpairedby the supply of 5 mol m^-3NO₃to both species. Also, large concentrationsof ureides dominated the transpiration stream of NO₃-fed plants.Compared to other symbiotic legumes cultured with similar NO₃concentrations,nodule functioning in the tested landraces of Bambara groundnutand Kersting's bean is tolerant of NO₃ions in the rhizosphere.The potential benefits of such naturally occurring NO₃-tolerantsymbioses are substantial, as they would permit inorganic Nfertilizer application in intercropping systems without inhibitingN₂fixation in the associated legumes.Copyright 1998 Annals ofBotany Company NO₃tolerance, Bambara groundnut, Kersting's bean, nitrogenase activity, xylem ureides.     

Influence of the Form of Nitrogen Supply on Root Uptake and Translocation of Cations in the Xylem Exudate of Maize (Zea mays L)

Concentrations of inorganic cations are often lower in plantssupplied with NH₄⁺ as compared with NO₃^–. To examine whetherthis is attributable to impaired root uptake of cations or lowerinternal demand, the rates of uptake and translocation of K,Mg, and Ca were compared in maize plants (Zea mays L.) withdifferent growth-related nutrient demands. Plants were grownin nutrient solution with either 1·0 mol m^–3 NO₃^–or NH₄⁺ and the shoot growth rate per unit weight of roots wasmodified by varying the temperature of the shoot base (SBT)including the apical shoot meristem. The shoot growth rate per unit weight of roots, which was takenas the parameter for the nutrient demand imposed on the rootsystem, was markedly lower at 12°C than at 24°C SBT.As a consequence of the lower nutrient demand at 12°C SBT,uptake rates of NO₃^– and NH₄⁺ declined by more than 50%Compared with NO₃^– supply, NH₄⁺ nutrition depressed theconcentrations of K and particularly of Ca in the shoot, bothin plants with high and with low nutrient demand. This indicatesa control of cation concentration by internal demand ratherthan by uptake capacity of the roots. Translocation rates of K, Mg and Ca in the xylem exudate werelower in NH₄⁺- than in NO₃^–-fed plants. Net accumulationrates of Ca in the shoot were also decreased, whereas net accumulationrates of K in the shoot were even higher in NH₄⁺-fed plants.It is concluded that reduced cation concentrations in the xylemsap of plants supplied with NH₄⁺ are due to the lower demandof cations for charge balance. The lower K translocation tothe shoot is compensated by reduced retranslocation to the roots.For Ca, in contrast, decreased translocation rates in NH₄⁺-fedplants result in lower shoot concentration. Key words: Nitrogen form, cation nutrition, charge balance, xylem exudate, recirculation