Altered cell wall properties are responsible for ammonium‐reduced aluminium accumulation in rice roots

The phytotoxicity of aluminium (Al) ions can be alleviated by ammonium (NH₄⁺) in rice and this effect has been attributed to the decreased Al accumulation in the roots. Here, the effects of different nitrogen forms on cell wall properties were compared in two rice cultivars differing in Al tolerance. An in vitro Al‐binding assay revealed that neither NH₄⁺ nor NO₃^? altered the Al‐binding capacity of cell walls, which were extracted from plants not previously exposed to N sources. However, cell walls extracted from NH₄⁺‐supplied roots displayed lower Al‐binding capacity than those from NO₃^?‐supplied roots when grown in non‐buffered solutions. Fourier‐transform infrared microspectroscopy analysis revealed that, compared with NO₃^?‐supplied roots, NH₄⁺‐supplied roots possessed fewer Al‐binding groups (‐OH and COO‐) and lower contents of pectin and hemicellulose. However, when grown in pH‐buffered solutions, these differences in the cell wall properties were not observed. Further analysis showed that the Al‐binding capacity and properties of cell walls were also altered by pHs alone. Taken together, our results indicate that the NH₄⁺‐reduced Al accumulation was attributed to the altered cell wall properties triggered by pH decrease due to NH₄⁺ uptake rather than direct competition for the cell wall binding sites between Al³⁺ and NH₄⁺.     

Gas and ion exchanges in wheat roots after nitrogen supply

Wheat (Triticum aestivum L. cv. Sicco) was grown for 10 days on CaSO₄ (0.5 mmol dm^?3) and then exposed for 2 days to various nitrogenous salts in an apparatus designed to measure the exchange of O₂ and CO₂, at constant pH and pNO₃. Nitrate salts (KNO₃ at 0.5 and Ca(NO₃)₂ at 0.25 and 1 mmol dm^?3) caused a transient increase (40–50%) in both O₂uptake and CO₂ release by the roots. The rate of gas exchange was nearly doubled by (NH₄)₂SO₄ (0.25 mmol dm^?3). Respiration was constant in roots kept on CaSO₄ or given KCl. In CaSO₄ the content of water-soluble sugars in roots fell by about 15% day^?1. The pletion of soluble sugars was higher with NO₃^? and NH₄⁺(40 and 30% day^?1, respectively). At most 10 to 20% of the released CO₂ is involved in HCO₃N^?NO₃^? exchange and this fraction represents at most 10% of the total carbon imported or 30% of the net carbon gain by the roots. The contribution of the non-phosphorylating “alternative” route to total root respiration was 15% in CaSO₄and over 40% with NH₄⁺ In NO₃^? the roots respired exclusively via the cytochrome route. Increased respiration at decreased efficiency in roots of NH₄⁺plants may be due to an overproduction of NADH. Our data support the contention that excess NADH as a “by-product” of the formation of carboxylates in the citrate cycle can be disposed of in an alternative respiratory pathway during NH₄⁺nutrition.     

The Influence of Nitrogen Nutrition on the Carbohydrate and Nitrogen Status of Emergent Macrophyte Acorus calamus L.

Carbon and nitrogen balance in Acorus calamus, a wetland species colonising littoral zones with a high trophic status, was studied under experimental conditions using water or sand culture with a defined composition of the nutrient solution. Influence of graded level of N (1.86, 7.5 and 18.6 mM) and/or forms of N (NH₄⁺ versus NO ₃^–) on the content of non-structural carbohydrates, free amino acids, total C, and total N was studied in Acorus rhizomes and roots to find possible connection with a reduced growth of Acorus plants under high N and NH₄⁺–N nutrition described in our previous study [Vojtíšková et al., 2004. Hydrobiologia 518: 9–22]. High N availability and pure NH₄⁺–N nutrition affected the C/N balance of rhizome and root systems of Acorus in a similar way. NH₄⁺–N was the only form of N elevated under the high N treatment. The major proportion of the total non-structural carbohydrates (TNC) was starch (91–93% and 51–64% in rhizomes and roots, respectively). The content of starch was significantly and and negatively affected by high N availability (P = 0.001), as well as by NH₄⁺–N nutrition (P=0.001). Amounts of simple soluble carbohydrates (sucrose, glucose, and fructose) were negligible in comparison to starch in rhizomes and branched roots (up to 5% of TNC), while roots without developed lateral roots (unbranched) contained up to 33% of TNC in the form of simple soluble sugars. Moreover, high hexoses/sucrose ratio, low starch/soluble sugars ratio, high content of N, and low C/N ratio support the notion that unbranched roots are metabolically active young roots with tissue differentiation in progress. A high content of free amino acids, typically with dominance of N-rich amino acids (Arg-46%, Gln-8%, Asn-7%), was found simultaneously with a low carbohydrate content under high N supply, which indicates that NH₄⁺ received is effectively incorporated into the organic form by this species. Since the decrease in carbohydrate content was not accompanied by luxurious growth, other possible carbon consuming processes were discussed in relation to NH₄⁺ nutrition. More dramatic changes in total N than C were found under high N availability resulting a shift in C/N ratio in favour of N. Although the shift towards N metabolism was obvious, no serious carbohydrate depletion occurred, which could explain the reduced growth of Acorus plants under high N and sole NH₄⁺–N nutrition described previously.     

Fish gill water boundary layer: a site of linkage between carbon dioxide and ammonia excretion

Summary Carbon dioxide excreted across fish gills is hydrated catalytically to form HCO ₃ ^– and H⁺ ions in water near the gill surface. We tested the possibility that CO₂ excretion is functionally linked to ammonia excretion through chemical reactions in the gill-water boundary layer. A bloodperfused trout head preparation was utilized in which the convective and diffusive components of branchial gas transfer were controlled. Pre-incubation of blood perfusate with the carbonic anhydrase inhibitor, acetazolamide, reduced both carbon dioxide and ammonia excretion in the blood-perfused preparation. Increasing the buffering capacity of inspired ventilatory water significantly reduced ammonia excretion, but carbon dioxide excretion was unaffected. Each of these experimental treatments significantly reduced the acidification of ventilatory water flowing over the gills. It is proposed that the catalysed conversion of excreted CO₂ to form HCO ₃ ^– and H⁺ ions provides a continual supply of H⁺ ions need for the removal of NH₃ as NH ₄ ⁺ . We suggest, therefore, that acidification of boundary layer water by CO₂ enhances blood-to-water NH₃ diffusion gradients and facilitates ammonia excretion.     

Transport and Distribution of 14CO2 Assimilate in Lolium perenne in Response to Varying Nitrogen Supply to Halves of a Divided Root System

The movement of ¹⁴C assimilate from shoots to roots and its subsequent metabolism in the root of Lolium perenne L. was studied using variable N nutrition supplied to halves of a divided root system. Half of the N-deficient root system was supplied with either high NO₃-N or high NH₄-N for 16 hours or 6 days before ¹⁴CO₂ labeling of the shoots. The distribution of ¹⁴C in sugars, ethanol-soluble nitrogen and organic acids in roots appeared to be related to the N content of the tissue. Supply of high NO₃-N for 6 days resulted in significant internal translocation of N into the low N supplied root half. Both root halves also had similar patterns of ¹⁴C distribution among soluble and insoluble metabolites. However, NH₄-N supply for 6 days did not result in a significant increase of N in the low N supplied roots, thus only the high NH₄-N supplied roots displayed stimulated sugar metabolism, similar to that in both root halves in the high NO₃-N supply treatment. Percent transport of ₁₄C assimilates from shoot to root was influenced by form and level of N supplied to root halves. Root halves supplied with either high N source for 6 days accumulated greater amounts of ¹⁴C assimilate than the corresponding low N root half. However NH₄-N supply appeared to make roots stronger sinks since NH₄ supply resulted in significantly greater ¹⁴C accumulation in both the high NH₄ supplied and the low N root halves than did NO₃-N supply in corresponding root halves. The data suggest that factors other than root metabolism, such as N mediated metabolism in the shoot, may also influence the percent transport of assimilates to the root. Internal distribution of the incoming assimilate within the root system could be regulated by the metabolic activity or assimilate demand of the roots.     

Nitrogen Acquisition from Atmospheric NH3 by Lolium perenne

Ammonia (NH₃) is the third most abundant N species in the atmosphere and, due to various natural and anthropogenic sources, can reach high concentrations in some areas. While some plants show effects of toxicity, others are capable of using this N-form and grow well without any utilization of soil-N. Acquisition of atmospheric NH₃ will affect the acid-base balance of the plants as absorption and dissolution causes an alkalinisation (production of OH^?) and assimilation of NH₃ results in an acidification (generation of H⁺). As there is only a limited capacity for biochemical disposal of excess H⁺ in shoots, pH regulation may involve H⁺/OH^? extrusion into the media via roots and transport of (in)organic ions between roots and above-ground parts of the plant. Our aim therefore was to assess NH₃ acquisition by Lolium perenne and to study the effects of gas phase NH₃ on growth, acid-base balance and mineral composition of the plants. The experiments therefore included application of a range of ¹⁴NH₃ to the shoots and of ¹⁵N as NO₃^?, NH₄⁺ or NH₄NO₃ to the roots, from which the amount of gas phase NH₃ acquisition could be quantified. Analysis of the mineral composition provided data for calculation of acid-base balance as well as for water use efficiencies of the plants. The results indicate that over the range of NH₃ supplied, plants from all treatments could utilize gas-phase NH₃ as demonstrated by increases in growth and in N and C use efficiencies. Plants receiving NO₃^? via their roots had a higher capacity to use gaseous NH₃ than those growing with NH₄⁺. NH₃ assimilation in shoots reduced both the acid load with NH₄⁺ nutrition and the alkaline load with NO₃^? supply to the roots. The results of the experiments are discussed in relation to possible acid-base regulation mechanisms of the whole plant.     

Cell type distinct accumulations of mRNA and protein for NADH-dependent glutamate synthase in rice roots in response to the supply of NH4+

Transient and NH₄⁺-inducible accumulation of the mRNA for NADH-dependent glutamate synthase (NADH-GOGAT; EC 1.4.1.14) in the roots of rice seedlings was analyzed in situ to identify the cell types responsible for the induction. The mRNA was detected specifically in sclerenchyma cells (the third cell-layer from the root surface), and the maximal accumulation was seen at 3–6 h following the supply of NH₄⁺ ions. Expression of the NADH-GOGAT gene in sclerenchyma cells was also confirmed using transgenic rice plants expressing GUS reporter gene under the control of rice NADH-GOGAT promoter. On the other hand, clear signals for the NADH-GOGAT protein were detected in epidermial cells and exodermal cells (the first and second cell layers from the root surface) at 12 h, following the supply of NH₄⁺ ions. The distinct localization of mRNA and protein for NADH-GOGAT suggests that either the mRNA or the translated protein in the sclerenchyma cells is migrated to the root surface. In contrast to NADH-GOGAT protein, Fd-GOGAT (EC 1.4.7.1) protein was detected in sclerenchyma cells, cortex cells, and stele in the rice roots. The distinct localization of the two GOGAT species indicates that they have different roles in the nitrogen metabolism in rice roots.     

The effect of some ammonium salts on nitrate reductase level,onin vivo nitrate reduction and on nitrate content in excisedpisum sativum roots

The effect of some ammonium salts on nitrate reductase (NR) level, onin vivo nitrate reduction and on nitrate content was followed in the presence of nitrate in the medium, under changing experimental conditions, in excisedPisum sativum roots, and their effect was compared with that of KNO₃, Ca(NO₃)₂ and NaNO₃ at 15 mM NO₃ ^- concentration, i.e. at a concentration which considerably exceeded the level of saturation with nitrate with respect to nitrate reductase. The effect of ammonium salts on NR level is indirect and changes from a positive one to a strongly negative one which is dependent on the time of action of the salt, on the presence of other cations, on pH of the solution of the ammonium salt and on the nature of the anion of the ammonium salt. A positive effect on the enzyme level can be observed in the presence of other cations than NH₄ ⁺ at suitable concentrations of those ammonium salts, the solutions of which have their pH values in the acid region (i.e. NH₄H₂PO₄, (NH₄)₂SO₄ and NH₄NO₃). However their positive effect is independent of the presence of NH₄ ⁺ ions, and it is obviously the result of an increased concentration of H⁺ ions. A clear-cut negative effect on NR level can be observed after 24 h in one-salt NH₄NO₃ solution where NH₄ ⁺ is not balanced with other cations and thus certainly can adversely influence many metabolic processes, and in the solutions containing neutral (pH 6.2) and dibasic ammonium phosphates in which dissolved undissociated ammonia [(NH₃). (H₂O) which can also affect many metabolic processes incl. proteosynthesis] probably has a toxic influence. Thein vivo nitrate reduction is always depressed in excised pea roots in the presence of ammonium salts in the medium, regardless of the level of nitrate reductase. Under the described conditions, no relationship could be established between the enzyme level and the so-called metabolic NO₃ ^- pool (i.e. NO₂ ^- production under anaerobic conditions), nor between NR level and the total nitrate content in the roots. One-salt solutions of NaNO₃, Ca(NO₃)₂ and KNO₃ exert different effects on the level of nitrate reductase and on the content of NO₃ ^- in the roots, but the in vivo NO₃ ^- reduction shows the same trend as NR level in the roots influenced by these salts. Cl^- ions, supplied in NH₄C1, depress both NR level and NO₃ ^- content in the roots at higher concentrations, but they do not significantly affect the in vivo nitrate reduction in comparison with other ammonium salts. These results indicate that NR level,in vivo nitrate reduction, and nitrate uptake can be regulated in pea roots independently of each other.     

Uptake and Assimilation of NO(3) and NH(4) by Nitrogen-Deficient Perennial Ryegrass Turf

Assimilation of NO₃⁻ and NH₄⁺ by perennial ryegrass (Lolium perenne L.) turf, previously deprived of N for 7 days, was examined. Nitrogen uptake rate was increased up to four- to five-fold for both forms of N by N-deprivation as compared to N-sufficient controls, with the deficiency-enhanced N absorption persisting through a 48 hour uptake period. Nitrate, but not NH₄⁺, accumulated in the roots and to a lesser degree in shoots. By 48 hours, 53% of the absorbed NO₃⁻ had been reduced, whereas 97% of the NH₄⁺ had been assimilated. During the early stages (0 to 8 hours) of NO₃⁻ uptake by N-deficient turf, reduction occurred primarily in the roots. Between 8 and 16 hours, however, the site of reduction shifted to the shoots. Nitrogen form did not affect partitioning of the absorbed N between roots (40%) and shoots (60%) but did affect growth. Compared to NO₃⁻, NH₄⁺ uptake inhibited root, but not shoot, growth. Total soluble carbohydrates decreased in both roots and shoots during the uptake period, principally the result of fructan metabolism. Ammonium uptake resulted in greater total depletion of soluble carbohydrates in the root compared to NO₃⁻ uptake. The data indicate that N assimilation by ryegrass turf utilizes stored sugars but is also dependent on current photosynthate.     

Net fluxes of ammonium and nitrate in association with H+ fluxes in fine roots of Populus popularis

Poplar plants are cultivated as woody crops, which are often fertilized by addition of ammonium (NH₄ ⁺) and/or nitrate (NO₃ ^?) to improve yields. However, little is known about net NH₄ ⁺/NO₃ ^? fluxes and their relation with H⁺ fluxes in poplar roots. In this study, net NH₄ ⁺/NO₃ ^? fluxes in association with H⁺ fluxes were measured non-invasively using scanning ion-selective electrode technique in fine roots of Populus popularis. Spatial variability of NH₄ ⁺ and NO₃ ^? fluxes was found along root tips of P. popularis. The maximal net uptake of NH₄ ⁺ and NO₃ ^? occurred, respectively, at 10 and 15 mm from poplar root tips. Net NH₄ ⁺ uptake was induced by ca. 48 % with provision of NO₃ ^? together, but net NO₃ ^? uptake was inhibited by ca. 39 % with the presence of NH₄ ⁺ in poplar roots. Furthermore, inactivation of plasma membrane (PM) H⁺-ATPases by orthovanadate markedly inhibited net NH₄ ⁺/NO₃ ^? uptake and even led to net NH₄ ⁺ release with NO₃ ^? co-provision. Linear correlations were observed between net NH₄ ⁺/NO₃ ^? and H⁺ fluxes in poplar roots except that no correlation was found between net NH₄ ⁺ and H⁺ fluxes in roots exposed to NH₄Cl and 0 mM vanadate. These results indicate that root tips play a key role in NH₄ ⁺/NO₃ ^? uptake and that net NH₄ ⁺/NO₃ ^? fluxes and the interaction of net fluxes of both ions are tightly associated with H⁺ fluxes in poplar roots.     

Measurement of Net Fluxes of Ammonium and Nitrate at the Surface of Barley Roots Using Ion-Selective Microelectrodes : II. Patterns of Uptake Along the Root Axis and Evaluation of the Microelectrode Flux Estimation Technique

Net fluxes of NH₄⁺ and NO₃⁻ into roots of 7-day-old barley (Hordeum vulgare L. cv Prato) seedlings varied both with position along the root axis and with time. These variations were not consistent between replicate plants; different roots showed unique temporal and spatial patterns of uptake. Axial scans of NH₄⁺ and NO₃⁻ net fluxes were conducted along the apical 7 centimeters of seminal roots of intact barley seedlings in solution culture using ion-selective microelectrodes in the unstirred layer immediately external to the root surface. Theoretically derived relationships between uptake and concentration gradients, combined with experimental observations of the conditions existing in our experimental system, permitted evaluation of the contribution of bulk water flow to ion movement in the unstirred layer, as well as a measure of the spatial resolution of the microelectrode flux estimation technique. Finally, a method was adopted to assess the accuracy of this technique.     

Influence of inorganic nitrogen sources on K+/Na+ homeostasis and salt tolerance in sorghum plants

This work aimed to study the regulation of K⁺/Na⁺ homeostasis and the physiological responses of salt-treated sorghum plants [Sorghum bicolor (L.) Moench] grown with different inorganic nitrogen (N) sources. Four days after sowing (DAS), the plants were transferred to complete nutrient solutions containing 0.75 mM K⁺ and 5 mM N, supplied as either NO₃ ^? or NH₄ ⁺. Twelve DAS, the plants were subjected to salt stress with 75 mM NaCl, which was applied in two doses of 37.5 mM. The plants were harvested on the third and seventh days after the exposure to NaCl. Under the salt stress conditions, the reduction of K⁺ concentrations in the shoot and roots was higher in the culture with NO₃ ^? than with NH₄ ⁺. However, the more conspicuous effect of N was on the Na⁺ accumulation, which was severely limited in the presence of NH₄ ⁺. This ionic regulation had a positive influence on the K⁺/Na⁺ ratio and the selective absorption and transport of K⁺ in the plants grown with NH₄ ⁺. Under control and salt stress conditions, higher accumulation of free amino acids and soluble proteins was promoted in NH₄ ⁺ grown roots than NO₃ ^? grown roots at both harvesting time, whereas higher accumulation of soluble sugars was observed only at 7 days of salt stress exposure. Unlike the NH₄ ⁺ grown plants, the gas exchanges of the NO₃ ^? grown plants were reduced after 7 days of salt stress. These results suggest that external NH₄ ⁺ may limit Na⁺ accumulation in sorghum, which could contribute to improving its physiological and metabolic responses to salt stress.     

Activity of myrosinase from Sinapis alba seeds immobilized into Ca-polygalacturonate as a simplified model of soil-root interface mucigel

Ca-polygalacturonate is a demethoxylated component of pectins which are constitutive of plant root mucigel. In order to define the role of root mucigel in myrosinase immobilization and activity at root level, a myrosinase enzyme which had been isolated from Sinapis alba seeds was immobilized into Ca-polygalacturonate. The activity profile for the immobilized and free enzyme was evaluated using the pH-Stat method as a function of time, temperature, and pH. The Michaelis-Menten kinetic parameters change between the immobilized (V _max ?=?127?±?13 U mg^?1 protein; K _M ?=?6.28?±?0.09?mM) and free (V _max ?=?17?±?1 U mg^?1 protein; K _M ?=?0.96?±?0.01?mM) forms of myrosinase, probably due to conformational changes involving the active site as a consequence of enzyme immobilization. Immobilized enzyme activity evaluated as a function of different substrates gave the highest value with nasturtin, the glucosinolate that is typical of several brassicaceae plant roots containing the glucosinolate-myrosinase defensive system. No feedback regulation mechanism was found in the presence of an excess of enzymatic reaction products (i.e. allyl isothiocyanate or sulphate). The high enzyme immobilization yield into Ca-polygalacturonate and its activity preservation under different conditions suggest that the enzyme released by plants at root level could be entrapped in root mucigel in order to preserve its activity.     

The distribution of ammonium ion from a localized source into the soil

The distribution of ammoniun ions from a concentrated source in the soil is calculated with a computed model based on chromatographic theory. The analytical solution for the chromatographic equation with convective transport in a pistonlike flow, for a non linear adsorption isotherm, is compared with computer simulation model results and actual experimental data from soil solumns.Adsorption isotherms for the exchange of Ca⁺⁺ by NH₄ ⁺ ions in the range of 0.01 to 6 eq NH₄/I were obtained. The isotherm are described by a modification of Freundlich's isotherm.Ammonium displacement is a frontal movement. The resulting concentration profile is a uniform zone of influence within which ammonium concentration is close to 2/3 of the soil C.E.C. A relatively narrow transition zone exists between the zone of influence and the bulk soil.Good correlation was obtained between experimental and computed ammonium concentration distribution along the soil profile after leaching.The results presented in this work indicate that a quantitative estimation of the extent to which ammonium ions are transported from application site, and the processes following this transport, can be obtained.Present address of the first author: Universidad Catolica de Chile, Dept. of Soils, Chile.     

Different sensitivity of Phragmites australis and Glyceria maxima to high availability of ammonium-N

The ability to cope with NH₄⁺-N was studied in the littoral helophytes Phragmites australis and Glyceria maxima, species commonly occupying fertile habitats rich in NH₄⁺ and often used in artificial wetlands. In the present study, Glyceria growth rate was reduced by 16% at 179 μM NH₄⁺-N, and the biomass production was reduced by 47% at 3700 μM NH₄⁺-N compared to NO₃⁻-N. Similar responses were not found in Phragmites. The amounts (mg g⁻¹ dry wt) of starch and total non-structural carbohydrates (TNC) in rhizomes were significantly lower in NH₄⁺ (8.9; 12.2 starch; 20.1; 41.9 TNC) compared to NO₃⁻ treated plants (28.0; 15.6 starch; 58.5; 56.3 TNC) in Phragmites and Glyceria, respectively. In addition, Glyceria showed lower amounts (mg g⁻¹ dry wt) of soluble sugars, TNC, K⁺, and Mg²⁺ in roots under NH₄⁺ (5.6; 14.3; 20.6; 1.9) compared to NO₃⁻ nutrition (11.6; 19.9; 37.9; 2.9, for soluble sugars, TNC, K⁺, and Mg²⁺, respectively), while root internal levels of NH₄⁺ and Ca²⁺ (0.29; 4.6 mg g⁻¹ dry wt, mean of both treatments) were only slightly affected. In Phragmites, no changes in soluble sugars, TNC, Ca²⁺, K⁺, and Mg²⁺ contents of roots (7.3; 14.9; 5.1; 17.3; 2.6 mg g⁻¹ dry wt, means of both treatments) were found in response to treatments. The results, therefore, indicate a more pronounced tolerance towards high NH₄⁺ supply in Phragmites compared to Glyceria, although the former may be susceptible to starch exhaustion in NH₄⁺-N nutrition. In contrast, Glyceria's ability to colonize fertile habitats rich in NH₄⁺ is probably related to the avoidance strategy due to shallow rooting or to the previously described ability to cope with high NH₄⁺ levels when P availability is high and NO₃⁻ is also provided.     

A comparative study of ammonium toxicity at different constatn pH of the nutrient solution

Seedlings of 14 species were grown for 14–28 days on nutrient solution with 6 mmol.l⁻¹ NH₄ as the sole nitrogen source. Solutions acidity was were kept constant at pH 4.0, 5.0, 6.0 and 7.0 by continuous titration with diluted KOH. The following species were used: barley, maize, oats sorghum, yellow and white lupin, pea, soybean, carrot, flax, castor-oil, spinach, sugarbeet and sunflower. Most plant species grew optimally at pH 6.0 with slight reductions at pH 5.0. Growth of many species was severely inhibited at pH 4.0, but this inhibition was not observed with the legume and cereal species. Yield depressions at pH 4.0 relative to pH 6.0 were well correlated with the respective relative decreases of the K concentration in their roots (P<0.002). In the roots of two species (sunflower and flax) total N concentrations were also strongly reduced at pH 4.0. apparently, the interactions between uptake of K, NH₄ and H ions become the prevalent problem at suboptimal pH. At pH 7.0, yields were also considerably decreased, with the exception of the lupines. At this pH, the roots of the growth inhibited plants were characterized by increased levels of total N and free NH₄. It is thought that the binding capacity of the roots for NH₄ is an important factor in preventing NH₄/NH₃ toxicity at supraoptimal pH.     

Induction of adventitious roots and analysis of ginsenoside content and the genes involved in triterpene biosynthesis inPanax ginseng

Adventitious roots were produced directly from root segments ofPanax ginseng seedlings when cultured on an MS solid medium containing 3.0 mg L^-1 IBA. Omitting NH₄NO₃ from this medium greatly enhanced both the frequency of adventitious root formation and the number of roots per expiants. This frequency declined markedly with the age of the root, but could be increased through repeated sub-culturing events. A two-step procedure that included NH₄NO₃ free media for the first two weeks of culture, followed by transfer onto media containing NH₄NO₃ for another four weeks, greatly improved total fresh weights of these adventitious roots compared with a method of continuous culture over six weeks in media that always contained NH₄NO₃. Expression of the genes involved in triterpene biosynthesis was analyzed by RT-PCR. Ginsenoside contents were enhanced by the omission of NH₄NO₃ and were also greatly increased by treatment with methyl jasmonate.     

Ammonia Assimilation in Alnus glutinosa and Glycine max: SHORT-TERM STUDIES USING [N]AMMONIUM

The pattern of assimilation of NH₄⁺ by Alnus glutinosa, a N₂-fixing, nonleguminous angiosperm, was examined. Detached nodules, roots, and nodulated roots of intact plants were exposed to ¹³NH₄⁺ for up to 15 minutes. Glutamine was the most highly labeled compound at all times; the only other compound labeled significantly was glutamate. Similar results were obtained after incubating soybean (L. merr) nodules and roots with ¹³NH₄⁺. These observations and the results of pulse-labeling and inhibitor studies with nodules of Alnus were distinctly different from those predicted for the assimilation of NH₄⁺ via glutamine synthetase and glutamate synthase and suggest that glutamate dehydrogenase may play a major role in the assimilation of exogenously supplied NH₄⁺.     

A possible mechanism of ammonium ion regulation of photosynthetic carbon flow in higher plants

Addition of NH₄⁺ to the photosynthesizing leaf cells of Dolichos lab lab L. var. Lignosis Prain and leaf discs of Vigna sinensis L. savi ex Hassk caused a significant increase in the flow of photosynthetic carbon toward amino acids with a concomitant decrease toward sugars without affecting the over-all photosynthetic rate. Similar diversion of photosynthetic carbon away from sugars was also observed in the photosynthesizing isolated chloroplasts of V. sinensis, but the latter differed in that they accumulated organic acids rather than amino acids. In an effort to understand the mechanism of NH₄⁺-mediated regulation, the specific and total activities of NAD(P)-glutamate dehydrogenase, glutamine synthetase, pyruvate kinase, alkaline fructose 1,6-bisphosphatase, and NAD(P)-glyceraldehyde-3-phosphate dehydrogenase of the cells of D. lab lab were checked but none was affected by the added ammonium salts even after prolonged incubation. At certain concentrations, ammonium ions abolished the light activation of NADP-glyceraldehyde-3-phosphate dehydrogenase and alkaline fructose 1,6-bisphosphatase in isolated chloroplasts from dark-adapted Vigna leaves without interfering with the basal dark activity of these enzymes. Based on these observations, a possible mechanism of action of NH₄⁺ in regulating the photosynthetic carbon flow is postulated.     

Differential effect of ammonium on the induction of nitrate and nitrite reductase activities in roots of barley (Hordeum vulgare) seedlings

The effect of exogenous NH₄⁺ on the induction of nitrate reductase activity (NRA; EC 1.6.6.1) and nitrite reductase activity (NiRA; EC 1.7.7.1) in roots of 8-day-old intact barley (Hordeum vulgare L.) seedlings was studied. Enzyme activities were induced with 0.1, 1 or 10 mM NO₃⁺ in the presence of 0, 1 or 10 mM NH₄⁺, Exogenous NH₄⁺ partially inhibited the induction of NRA when roots were exposed to 0.1 mM, but not to 1 or 10 mM NO₃⁺, In contrast, the induction of NiRA was inhibited by NH₄⁺ at all NO₃⁺ levels. Maximum inhibition of the enzyme activities occurred at 1.0 mM NH₄⁺ Pre-treatment with NH₄⁺ had no effect on the subsequent induction of NRA in the absence of additional NH₄⁺ whereas the induction of NiRA in NH₄⁺-pretreated roots was inhibited in the absence of NH₄⁺ At 10 mM NO₃⁺ L-methionine sulfoximine stimulated the induction of NRA whether or not exogenous NH₄⁺ was present. In contrast, the induction of NiRA was inhibited by L-methionine sulfoximine irrespective of NH₄⁺ supply. During the postinduction phase, exogenous NH₄⁺ decreased NRA in roots supplied with 0.1 mM but not with 1mM NH₃⁺ whereas, NiRA was unaffected by NH₄⁺ at either substrate concentration. The results indicate that exogenous NH₄⁺ regulates the induction of NRA in roots by limiting the availability of NO₃⁺. Conversely, it has a direct effect, independent of the availability of NO₃⁺, on the induction of NiRA. The lack of an NH₄⁺ effect on NiRA during the postinduction phase is apparently due to a slower turnover rate of that enzyme.