Effects of genetic modification of nitrate reductase expression on 15NO3– uptake and reduction in Nicotiana plants

The physiological consequences for NO₃^– utilization by the plant of underexpression and overexpression of nitrate reductase (NR) were investigated in nine transformants of Nicotiana tabacum and Nicotiana plumbaginifolia. The in vitro NR activities (NRAs) in both roots and leaves of low- and high-NR tobacco transformants ranged from 5–10% to 150–200%, respectively, of those measured in wild-type plants. The level of NR expression markedly affected the NO₃^– reduction efficiency in detached leaves and intact plants. In both species, ¹⁵NO₃^– reduction ranged from 15–45% of ¹⁵NO₃^– uptake in the low-NR plants, to 40–80% in the wild-type, and up to 95% in high-NR plants. In the high-NR genotypes, however, total ¹⁵NO₃^– assimilation was not significantly increased when compared with that in wild-type plants, because the higher ¹⁵NO₃^– reduction efficiency was offset by lower ¹⁵NO₃^– uptake by the roots. The inhibition of NO₃^– uptake appeared to be the result of negative feedback regulation of NO₃^– influx, and is interpreted as an adjustment of NO₃^– uptake to prevent excessive amino acid synthesis. In genotypes underexpressing NR, the low ¹⁵NO₃^– reduction efficiency also was generally associated with a decrease in net ¹⁵NO₃^– uptake as compared with the wild type. Thus, underexpression of NR resulted in an inhibition of reduced ¹⁵N synthesis in the plant, although the effect was much less pronounced than that expected from the very low NRAs. The restricted NO₃^– uptake in low-NR plants emphasizes the point that the products of NO₃^– assimilation are not the only factors responsible for down-regulation of the NO₃^– uptake system.     

The nitrogen balance of Raphanus sativus x raphanistrum plants. II. Growth, nitrogen redistribution and photosynthesis under NO3− deprivation

Abstract. Wild radish plants deprived of, and continuously supplied with solution NO^?₃ for 7 d following 3 weeks growth at high NO^?₃ supply were compared in terms of changes in dry weight, leaf area, photosynthesis and the partitioning of carbon and nitrogen (NH₂-N and NO^?₃-N) among individual organs. Initial levels of NO^?₃-N accounted for 25% of total plant N. Following termination of NO^?₃ supply, whole plant dry weight growth was not significantly reduced for 3 d, during which time plant NH₂-N concentration declined by about 25% relative to NO^?₃-supplied plants, and endogenous NO^?₃-N content was reduced to nearly zero. Older leaves lost NO^?₃ and NH₂-N, and roots and young leaves gained NH₂-N in response to N stress. Relative growth rate declined due both to decreased net assimilation rate and a decrease in leaf area ratio. A rapid increase in specific leaf weight was indicative of a greater sensitivity to N stress of leaf expansion compared to carbon gain. In response to N stress, photosynthesis per unit leaf area was more severely inhibited in older leaves, whereas weight-based rates were equally inhibited among all leaf ages. Net photosynthesis was strongly correlated with leaf NH₂-N concentration, and the relationship was not significantly different for leaves of NO₃^?-supplied compared to NO^?₃-deprived plants. Simulations of the time course of NO^?₃ depletion for plants of various NH₂-N and NO^?₃ compositions and relative growth rates indicated that environmental conditions may influence the importance of NO^?₃ accumulation as a buffer against fluctuations in the N supply to demand ratio.     

Relations between uptake and utilization of NO−3 in Pisum growing exponentially under nitrogen limitation

The utilization and translocation of nitrogen was investigated in exponentially growing, nitrogen-limited Pisum sativum L. cv. Marma. The plants were given N daily at exponentially increasing, although suboptimal, relative nitrogen addition rates (R_N) calculated to yield a relative increment in N of 0.06 day^?1 and 0.12 day^?1. After 10 days of NO^?₃ additions (26 days after sowing), the relative growth rate more or less equaled R_N. Uptake of NO^?₃ was several-fold higher than the N requirement for the growth rate set by R_N. The daily addition of NO^?₃ was taken up after 7 to 8 h, resulting in a cyclic behaviour in the NO^?₃ utilization. During the phase of net NO^?₃ influx, the filling phase (0 to 8 h), in vitro nitrate reductase activity (NR activity) and intracellular levels of soluble N in the root increased. In the phase of no net influx of NO^?₃ the depletion phase (8 to 24 h), the plants were entirely dependent on stored N. During this phase both in vitro NR activity and intracellular levels of soluble N decreased. Also the calculated actual rate of NO^?₃ reduction was high in the filling phase, while it was close to zero in the depletion phase. The pattern of these fluctuations indicates that the regulation of NO^?₃ utilization involves an interplay between transmembrane fluxes of NO^?₃, the cytosolic NO^?₃ concentration and NR activity. Cyclic fluctuations in N-containing compounds were also found in the xylem. Nitrogen was mainly transported as amino acids. The pattern of NO^?₃ transport in the xylem and the fluctuations in the shoot of in vitro NR activity indicate that a reasoning similar to that for the regulation of NO^?₃ assimilation in the root also applies for the shoot. The results also indicate a substantial supply of amino acids to the xylem through recirculation from the shoot.     

Distribution of NO3− reduction between roots and shoots of peachtree seedlings as affected by NO3− uptake rate

The distribution of NO₃^? reduction between roots and shoots was studied in hydro-ponically-grown peach-tree seedlings (Prunus persica L.) during recovery from N starvation. Uptake, translocation and reduction of NO₃^?, together with transport through xylem and phloem of the newly reduced N were estimated, using ¹⁵N labellings, in intact plants supplied for 90 h with 0.5 mM NH₄⁺ and 0.5, 1.5 or 10 mM NO₃^?. Xylem transport of NO₃^? was further investigated by xylem sap analysis in a similar experiment. The roots were the main site of NO₃^? reduction at all 3 levels of NO₃^? nutrition. However, the contribution of the shoots to the whole plant NO₃^? reduction increased with increasing external NO₃^? availability. This contribution was estimated to be 20, 23 and 42% of the total assimilation at 0.5, 1.5 and 10 mM NO₃^?, respectively. Both ¹⁵N results and xylem sap analysis confirmed that this trend was due to an enhancement of NO₃^? translocation from roots to shoots. It is proposed that the lack of NO₃^? export to the shoots at low NO₃^? uptake rate resulted from a competition between NO₃^? reduction in the root epidermis/cortex and NO₃^? diffusion to the stele. On the other hand, net xylem transport of newly reduced N was very efficient since ca 70% of the amino acids synthesized in the roots were translocated to the shoots, regardless of the level of NO₃^? nutrition. This net xylem transport by far exceeded the net downward phloem transport of the reduced N assimilated in shoots. As a consequence, the reduced N resulting from NO₃^? assimilation, principally occurring in the roots, was mainly incorporated in the shoots.     

Effects of non-steady-state iron limitation on nitrogen assimilatory enzymes in the marine diatom thalassiosira weissflogii (BACILLARIOPHYCEAE)

Since the recognition of iron‐limited high nitrate (or nutrient) low chlorophyll (HNLC) regions of the ocean, low iron availability has been hypothesized to limit the assimilation of nitrate by diatoms. To determine the influence of non‐steady‐state iron availability on nitrogen assimilatory enzymes, cultures of Thalassiosira weissflogii (Grunow) Fryxell et Hasle were grown under iron‐limited and iron‐replete conditions using artificial seawater medium. Iron‐limited cultures suffered from decreased efficiency of PSII as indicated by the DCMU‐induced variable fluorescence signal (F_v/F_m). Under iron‐replete conditions, in vitro nitrate reductase (NR) activity was rate limiting to nitrogen assimilation and in vitro nitrite reductase (NiR) activity was 50‐fold higher. Under iron limitation, cultures excreted up to 100 fmol NO₂^?·cell^?1·d^?1 (about 10% of incorporated N) and NiR activities declined by 50‐fold while internal NO₂^? pools remained relatively constant. Activities of both NR and NiR remained in excess of nitrogen incorporation rates throughout iron‐limited growth. One possible explanation is that the supply of photosynthetically derived reductant to NiR may be responsible for the limitation of nitrogen assimilation at the NO₂^? reduction step. Urease activity showed no response to iron limitation. Carbon:nitrogen ratios were equivalent in both iron conditions, indicating that, relative to carbon, nitrogen was assimilated at similar rates whether iron was limiting growth or not. We hypothesize that, diatoms in HNLC regions are not deficient in their ability to assimilate nitrate when they are iron limited. Rather, it appears that diatoms are limited in their ability to process photons within the photosynthetic electron transport chain which results in nitrite reduction becoming the rate‐limiting step in nitrogenassimilation.     

Ammonium can stimulate nitrate and nitrite reductase in the absence of nitrate in Clematis vitalba

Nitrogen assimilation was studied in the deciduous, perennial climber Clematis vitalba. When solely supplied with NO₃^– in a hydroponic system, growth and N-assimilation characteristics were similar to those reported for a range of other species. When solely supplied with NH₄⁺, however, nitrate reductase (NR) activity dramatically increased in shoot tissue, and particularly leaf tissue, to up to three times the maximum level achieved in NO₃^– supplied plants. NO₃^– was not detected in plant material that had been solely supplied with NH₄⁺, there was no NO₃^– contamination of the hydroponic system, and the NH₄⁺-induced activity did not occur in tobacco or barley grown under similar conditions. Western Blot analysis revealed that the induction of NR activity, either by NO₃^– or NH₄⁺, was matched by NR and nitrite reductase protein synthesis, but this was not the case for the ammonium assimilation enzyme glutamine synthetase. Exposure of leaf disks to N revealed that NO₃^– assimilation was induced in leaves directly by NO₃^– and NH₄⁺ but not glutamine. Our results suggest that the NH₄⁺-induced potential for NO₃^– assimilation occurs when externally sourced NH₄⁺ is assimilated in the absence of any NO₃^– assimilation. These data show that the potential for nitrate assimilation in C. vitalba is induced by a nitrogenous compound in the absence of its substrate and suggest that NO₃^– assimilation in C. vitalba may have a significant role beyond the supply of reduced N for growth.     

Growth and Major Nutrient Concentrations in Brassica campestris Supplied with Different NH4^＋/NO3 Ratios

In the present study, we investigated whether growth and main nutrient ion concentrations of cabbage （Brassica campestris L.） could be increased when plants were subjected to different NH4^＋/NO3- ratios. Cabbage seedlings were grown in a greenhouse in nutrient solutions with five NH4^＋/NO3- ratios （1：0; 0.75：0.25; 0.5：0.5; 0.25：0.75; and 0：1）. The results showed that cabbage growth was reduced by 87% when the proportion of NH4^＋-N in the nutrient solution was more than 75% compared with a ratio NH4^＋/NO3- of 0.5：0.5 35 d after transplanting, suggesting a possible toxicity due to the accumulation of a large amount of free ammonia in the leaves. When the NH4＋/NO3- ratio was 0.5：0.5, fresh seedling weight, root length, and H2PO4- （P）, K^＋, Ca^2＋, and Mg^2＋ concentrations were all higher than those in plants grown under other NH4^＋/NO3- ratios. The nitrate concentration in the leaves was the lowest in plants grown at 0.5： 0.5 NH4^＋/NO3-. The present results indicate that an appropriate NH4^＋/NO3- ratio improves the absorption of other nutrients and maintains a suitable proportion of N assimilation and storage that should benefit plant growth and the quality of cabbage as a vegetable.     

Physiological effects of a long term exposure to low concentrations of NH3, NO2 and SO2 on Douglas fir (Pseudotsuga menziesii)

The above-ground parts of two years old seedlings of Douglas fir (Pseudotsuga menziesii) were exposed to filtered air, NH₃, NO₂₊, SO₂ (66, 96 and 95 μg m^?3, respectively), to a mixture of NO₂+NH₃ (55 + 82 μg m^?3) or SO₂+NO₂ (128 + 129 μg m^?3), for 8 months in fumigation chambers. Both chlorophyll fluorescence and gas exchange measurements were carried out on shoots which had sprouted at the beginning of the exposure period. The chlorophyll fluorescence measurements were performed after 3 and 5 months of exposure (average shoot age 70 and 140 days, respectively). Light response curves of electron transport rate (J) were determined, in which J was deduced from chlorophyll fluorescence. In addition, light response curves of net CO₂ assimilation were determined after 5 months of exposure. After 3 months of exposure (average shoot age 70 days) all exposure treatments showed a lower maximum electron transport rate (J_max) as compared to the control shoots (filtered air). A large reduction (45%) was observed for shoots exposed to SO₂+NO₂. During the exposure period between 3 and 5 months (average shoot age 70 and 140 days, respectively) a decrease of J_max was observed for all treatments. J_max had further declined some time after termination of the exposure, when average shoot age was 310 days. Shoots exposed to SO₂ and SO₂+NO₂ also showed a reduction in maximum net CO₂ assimilation (P_max) as compared to the control shoots. However, shoots exposed to NO₂ showed no reduction and even a higher P_max was observed for shoots exposed to NH₃ or NO₂+NH₃. Needles of these treatments also showed a higher chlorophyll content which might explain the contradictory results obtained for these treatments: the increased amount of photosynthetic units counteracts the reduction in J_max and consequently no reduction in P_max is measured. Shoots exposed to SO₂ and SO₂+NO₂ also showed a reduction in maximum stomatal conductance (g_s). However, the stomatal opening was larger than could be expected on basis of their (maximum) CO₂ assimilation rate. Consequently, water use efficiency of these shoots was lower than that of the control shoots. Also shoots exposed to NO₂ had a lower water use efficiency due to a significantly higher maximum g_s. Shoots exposed to NH₃ showed a high transpiration rate in the dark, indicating imperfect stomatal closure.     

Oxygen consumption during leaf nitrate assimilation in a C3 and C4 plant: the role of mitochondrial respiration

Measurements of net fluxes of CO₂ and O₂ from leaves and chlorophyll a fluorescence were used to determine the role of mitochondrial respiration during nitrate (NO₃^–) assimilation in both a C₃ (wheat) and a C₄ (maize) plant. Changes in the assimilatory quotient (net CO₂ consumed over net O₂ evolved) when the nitrogen source was shifted from NO₃^– to NH₄⁺ (ΔAQ) provided a measure of shoot NO₃^– assimilation. According to this measure, elevated CO₂ inhibited NO₃^– assimilation in wheat but not maize. Net O₂ exchange under ambient CO₂ concentrations increased in wheat plants receiving NO₃^– instead of NH₄⁺, but gross O₂ evolution from the photosynthetic apparatus (J_O2) was insensitive to nitrogen source. Therefore, O₂ consumption within wheat photosynthetic tissue (ΔΟ₂), the difference between J_O2 and net O₂ exchange, decreased during NO₃^– assimilation. In maize, NO₃^– assimilation was insensitive to changes in intercellular CO₂ concentration (C_i); nonetheless, ΔΟ₂ at low C_i values was significantly higher in NO₃^–‐fed than in NH₄⁺‐fed plants. Changes in O₂ consumption during NO₃^– assimilation may involve one or more of the following processes: (a) Mehler ascorbate peroxidase (MAP) reactions; (b) photorespiration; or (c) mitochondrial respiration. The data presented here indicates that in wheat, the last process, mitochondrial respiration, is decreased during NO₃^– assimilation. In maize, NO₃^– assimilation appears to stimulate mitochondrial respiration when photosynthetic rates are limiting.     

Implications of N acquisition from atmospheric NH3 for acid-bAse and cation-anion balance of Lolium perenne

In the atmosphere, ammonia (NH₃) is the third most abundant N species which, due to various natural and anthropogenic sources, can locally reach high concentrations. The acquisition of atmospheric NH₃ by plant shoots will lead to two opposing effects on acid-base balance. Absorption and dissolution of NH₃ will cause an alkalinisation, while the assimilation of NH₃ results in an acidification. Different rates of these processes would lead to an acid-base imbalance with consequences for the ionic balance of the plant. As there is only a limited capacity for biochemical disposal of excess H⁺ in shoots, pH regulation may involve a pattern of (in)organic ion flow between shoots and roots followed by H⁺/OH^? extrusion into the media via roots. The acquisition of NH₃ as additional N source should lead to a reduction in the ratio of mol H⁺/OH^? gained per mol N assimilated. We have recently investigated the NH₃ acquisition by Lolium perenne L. cv. Centurion and studied the effects of gas phase NH₃ on growth, acid-base balance and water-use efficiency. The experiments, therefore, included the application of a range of ¹⁴NH₃ to the shoots and of ¹⁵N as NO₃^?, NH₄⁺ or NH₄NO₃ to the roots. After a summary of the main conclusions from those experiments, we discuss the implications of the use of atmospheric NH₃ for the mineral composition of the plants. Over the range of NH₃ supplied, plants from all treatments could utilize gas-phase NH₃. 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 most significant effect of fumigation on the ion balance was an increase in K⁺ within all treatments, and this effect was highest in the NH₄⁺-fed plants. The results of the experiments support predictions of a combination of neutralizing biochemical reactions as well as transport of organic anion salts between shoots and roots as possible acid-base regulation mechanisms of the whole plant.     

Enriched rhizosphere CO2 concentrations can ameliorate the influence of salinity on hydroponically grown tomato plants

Our previous work indicated that salinity caused a shift in the predominant site of nitrate reduction and assimilation from the shoot to the root in tomato plants. In the present work we tested whether an enhanced supply of dissolved inorganic carbon (DIC, CO₂+ HCO₃) to the root solution could increase anaplerotic provision of carbon compounds for the increased nitrogen assimilation in the root of salinity-stressed Lycopersicon esculentum (L.) Mill. cv. F144. The seedlings were grown in hydroponic culture with 0 or 100mM NaCl and aeration of the root solution with either ambient or CO₂-enriched air (5000 μmol mol^?1). The salinity-treated plants accumulated more dry weight and higher total N when the roots were supplied with CO₂-enriched aeration than when aerated with ambient air. Plants grown with salinity and enriched DIC also had higher rates of NO^?₃ uptake and translocated more NO^?₃ and reduced N in the xylem sap than did equivalent plants grown with ambient DIC. Incorporation of DIC was measured by supplying a 1 -h pulse of H¹⁴CO^?₃ to the roots followed by extraction with 80% ethanol. Enriched DIC increased root incorporation of DIC 10-fold in both salinized and non-salinized plants. In salinity-stressed plants, the products of dissolved inorganic ¹⁴C were preferentially diverted into amino acid synthesis to a greater extent than in non-salinized plants in which label was accumulated in organic acids. It was concluded that enriched DIC can increase the supply of N and anaplerotic carbon for amino acid synthesis in roots of salinized plants. Thus enriched DIC could relieve the limitation of carbon supply for ammonium assimilation and thus ameliorate the influence of salinity on NO^?₃ uptake and assimilation as well as on plant growth.     

Influence of elevated CO2 and nitrogen nutrition on photosynthesis and nitrate photo-assimilation in maize (Zea mays L.)

Measurements of CO₂ and O₂ gas exchange and chlorophyll a fluorescence were used to test the hypothesis that elevated atmospheric CO₂ inhibits nitrate (NO₃ ^– ) photo‐assimilation in the C₄ plant, maize (Zea mays L.). The assimilatory quotient (AQ), the ratio of net CO₂ assimilation to net O₂ evolution, decreases as NO₃ ^– photo‐assimilation increases so that the difference in AQ between the ammonium‐ and nitrate‐fed plants (ΔAQ) provided an in planta estimate of NO₃ ^– photo‐assimilation. In fully expanded maize leaves, NO₃ ^– photo‐assimilation was detectable only under high light and was not affected by CO₂ treatments. Furthermore, CO₂ assimilation and O₂ evolution were higher under NO₃ ^– than ammonia (NH₄⁺) regardless of CO₂ levels. In conclusion, NO₃ ^– photo‐assimilation in maize primarily occurred at high light when reducing equivalents were presumably not limiting. Nitrate photo‐assimilation enhanced C₄ photosynthesis, and in contrast to C₃ plants, elevated CO₂ did not inhibit foliar NO₃^– photo‐assimilation.     

Investigating the in vivo calcium transport path to developing potato tuber using 45Ca: a new concept in potato tuber calcium nutrition

Calcium is believed to be transported with water in the xylem. Consistent with this proposal, low‐transpiring organs such as potato Solanum tuberosum tubers are known to suffer from calcium deficiency. Although roots on tubers and stolons have been shown to supply water to tubers, there is no direct evidence for the calcium transport pathway to tubers. Both a xylem and a phloem transport pathway have been suggested. We investigated in vivo calcium transport to developing potato, cv. Dark Red Norland and cv. Russet Burbank, tubers using ⁴⁵Ca in a controlled environment facility. Whole plant split pot experiments allowed the placement of ⁴⁵Ca either in the main (basal) root or the tuber and stolon areas of the pot. The results showed that ⁴⁵Ca was transported to the shoot with the transpiration stream from both areas but was not re‐translocated to tubers or the main (basal) root system even 57 days after ⁴⁵Ca application. Radioactivity could only be detected in the tuber when ⁴⁵Ca was fed to the stolon and tuber area. When ⁴⁵Ca was fed to specific tubers, radioactivity was detected in the aerial shoot; however, no activity was detected in other tubers or the main (basal) roots. In another set of experiments, roots on a stolon near a tuber were precisely fed ⁴⁵Ca and Safranin O. The radioactive signal exactly overlapped the water transport pathway in the tuber marked with Safranin O dye, suggesting that water and calcium can be simultaneously transported from stolon roots to the tuber. No transport of ⁴⁵Ca across the tuber periderm was detected 8 days after ⁴⁵Ca was applied to the tuber periderm. This indicated that no significant transport of calcium occurs from the soil across the periderm. Our results provide evidence that: (1) calcium is not re‐translocated via the phloem from the aerial shoot tubers and main (basal) roots; (2) the main root system does not supply calcium to the tuber; (3) calcium is not transported across the periderm to the interior tuber tissue; (4) calcium is transported to the tuber via the xylem along with water, and the roots on the stolon associated with the tuber supply water and calcium to the developing tuber; and (5) transpirational demand is a significant determinant of calcium distribution within the plant.     

Studies on nitrate reductase activity in Laminariadigitata (Huds.) Lamour. I. Longitudinal and transverse profiles of nitrate reductase activity within the thallus

The distribution of the enzyme nitrate reductase (NR) within the thallus of the brown alga Laminaria digitata (Huds.) Lamour is described for plants sampled from the east coast of Scotland in May and June when growth rates are at a maximum. Highest NR activities (≈ 0.2 μmol NO₃^? reduced·g^?1 wet wt·h^?1) occurred in the mature blade. NR activities declined towards the basal meristematic region of the blade. Activities in the stipe and holdfast were also low, being between 0.05 and 0.07 μmol NO₃^? reduced·g^?1 wet wt·h^?1. The activities of the enzyme glutamine synthetase (GS), which is important in the assimilation of NH₄⁺, showed a similar distribution within the blade to those of NR.The transverse profile of NR activity in the stipe exhibited a decline from the outer to the inner tissues. Maximum activities (0.13 μmol NO₃^? reduced·g^?1 wet wt·h^?1) occurred in the meristoderm, while those of the cortex and medulla were 0.04 and 0.01 μmol NO₃^? reduced·g^?1 wet wt·h^?1 respectively.These data indicate that most of the NO₃^? assimilation occurs in the mature blade rather than in the meristematic tissue where there is a high nitrogen demand for growth. The data are consistent with the maintenance of meristematic growth by the internal transport of organic nitrogen from the mature blade.     

Absorption of nitrate and ammonium ions by Lolium perenne from flowing solution cultures at low root temperatures

Lolium perenne L. cv. 23 (perennial ryegrass) plants were grown in flowing solution culture and acclimatized over 49 d to low root temperature (5°C) prior to treatment at root temperatures of 3, 5, 7 and 9°C for 41 d with common air temperature of 20/15°C day/night and solution pH 5·0. The effects of root temperature on growth, uptake and assimilation of N were compared with N supplied as either NH₄ or NO3 at 10 mmol m^?3. At any given temperature, the relative growth rate (RGR) of roots exceeded that of shoots, thus the root fraction (Rf) increased with time. These effects were found in plants grown with the two N sources. Plants grown at 3 and 5°C had very high dry matter contents as reflected by the fresh weight: freeze-dried weight ratio. This ratio increased sharply, especially in roots at 7 and 9°C. Expressed on a fresh weight basis, there was no major effect of root temperature on the [N] of plants receiving NHJ but at any given temperature, the [N] in plants grown with NHJ was significantly greater than in those grown with NO₃. The specific absorption rate (SAR) of NH⁺₄ was greater at all temperatures than SAR-NO₃. In plants grown with NH⁺, 3–5% of the total N was recovered as NH⁺₄, whereas in those grown with NO^?₃ the unassimilated NO^?₃ rose sharply between 7 and 9°C to become 14 and 28% of the total N in shoots and roots, respectively. The greater assimilation of NH⁺₄ lead to concentrations of insoluble reduced N (= protein) which were 125 and 20% greater, in roots and shoots, respectively, than in NO^?₃-grown plants. Plants grown with NH⁺₄ had very much greater glutamine and asparagine concentrations in both roots and shoots, although other amino acids were more similar in Concentration to those in NO^?₃ grown plants. It is concluded that slow growth at low root temperature is not caused by restriction of the absorption or assimilation of either NH⁺₄ or NO^?₃. The additional residual N (protein) in NH⁺₄ grown plants may serve as a labile store of N which could support growth when external N supply becomes deficient.     

Photosynthetic acclimation to elevated CO2 in Phaseolus vulgaris L. is altered by growth response to nitrogen supply

Abstract Long‐term exposure of plants to elevated CO₂ often leads to downward photosynthetic acclimation. Nitrogen (N) deficiency could potentially exacerbate this response by reducing growth rate and the sink for photosynthates, but this has not always been observed. Experimentally, the interpretation of N effects on CO₂ responses can be confounded by increasing severity of tissue N deficiency over time when N supply is not adjusted as demand increases. In this study, N supply ranged from sub‐ to supra‐optimal (20–540 kgN ha^–l equivalent), and relatively stable levels of tissue N concentration were obtained in all treatments by varying twice‐weekly application rates in proportion to plant growth. The effects of N on photosynthesis and growth of beans (Phaseolus vulgaris L.) raised at ambient (35 Pa) and three elevated (70, 105, 140 Pa) CO₂ partial pressures (pCO₂) were evaluated. Averaging across N treatments, leaf total non‐structural carbohydrates (TNC) were 2.5‐ to 3‐fold higher and leaf N concentrations were 31–35% lower at elevated compared to ambient pCO₂. Light‐saturated net CO₂ assimilation rates measured at growth pCO₂ (A_satg) were significantly higher (26–40% depending on N supply) in plants grown at elevated compared to ambient pCO₂. When measured at a common pCO₂ of 35 Pa, the A_sat of plants grown at elevated CO₂ was 15–29% less than that of plants grown at 35 Pa, indicative of downward photosynthetic acclimation. The magnitude of downward photosynthetic acclimation to elevated CO₂ was greater in plants grown at high (180 and 540 kgN ha^–l) compared to low (20 and 60 kgN ha^–l) N supply, and this was associated with a higher A_sat at growth pCO₂, higher leaf area ratio (leaf area/total biomass), and higher TNC in leaves of high‐N plants. Our results indicate that the effect of N on acclimation to CO₂ will depend on the balance between supply and demand for N during the growing period, and the effect this has on biomass allocation and source‐sink C balance at the whole‐plant level.     

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.     

Mode of action of chlorsulfuron in a sensitive wheat (Triticum aestivum) cultivar: primary and secondary effects on nitrogen assimilation

Chlorsulfuron (15 g a.i. ha^-1) inhibited growth of wheat (Triticurn aestivum L. cv. Rongotea) especially on high nitrate (NO₃) supply. Decreased growth at high NO^-₃ was associated with higher concentrations of reduced nitrogen (N) and NO^-₃ in the shoots. Seven days after spraying (DAS), shoot dry weight (dry wt) of sprayed plants was similar with NO^-₃ or branched chain amino acids as main N supply but 28 DAS, shoot dry wt was greater with the amino acid treatment. One DAS, chlorsulfuron caused substantial decreases in extension of the youngest leaf and acetolactate synthase activity and valine content of shoots of plants supplied with NO^-₃ or branched chain amino acids. Total amino acid content of shoots was greater in sprayed plants than in unsprayed plants 1 DAS. Acetolactate synthase activity of sprayed plants supplied low NO^-₃ returned to normal 14–21 DAS. For sprayed plants transferred from low to high NO^-₃ supply 7, 14 or 21 DAS, shoot dry wt 50 DAS increased with increased time of transfer to high NO^-₃ while shoot NO^-₃ content decreased. Shoot NO₃ content of sprayed plants transferred to high NO^-₃ supply 7 or 14 DAS was similar to that in unsprayed plants at applied NO^-₃ concentrations which inhibited growth. It is concluded that inhibition of acetolactate synthase is likely to be the primary mode of action of chlorsulfuron in this wheat cultivar; data are consistent with the proposal that subsequent NO^-₃ accumulation can also inhibit growth.     

The influence of enriched rhizosphere CO2 on N uptake and metabolism in wild-type and NR-deficient barley plants

Positive influences of high concentrations of dissolved inorganic carbon (DIC) in the growth medium of salinity-stressed plants are associated with carbon assimilation through phosphoenolpyruvate carboxylase (PEPc) activity in roots; and also in salinity-stressed tomato plants, enriched CO₂ in the rhizosphere increases NO^?₃uptake. In the present study, wild-type and nitrate reductase-deficient plants of barley (Hordeum vulgare L. cv. Steptoe) were used to determine whether the influence of enriched CO₂ on NO^?₃ uptake and metabolism is dependent on the activity of nitrate reductase (NR) in the plant. Plants grown in NH₄⁺and aerated with ambient air, were transferred to either NO₃^? or NH₄⁺ solutions and aerated with air containing between 0 and 6 500 μmol mol^?1 CO₂. Nitrogen uptake and tissue concentrations of NO₃^? and NH₄⁺ were measured as well as activities of NR and PEPc. The uptake of NO^?₃ by the wild-type was increased by increasing CO₂. This was associated with increased in vitro NR activity, but increased uptake of NO₃^? was found also in the NR-deficient genotype when exposed to high CO₂ concentrations; so that the influence of CO₂ on NO₃^? uptake was independent of the reduction of NO₃^? and assimilation into amino acids. The increase in uptake of NO₃^? in wild-type plants with enriched CO₂ was the same at pH 7 as at pH 5, indicating that the relative abundance of HCO₃^? or CO₂ in the medium did not influence NO₃^? uptake. Uptake of NH₄⁺ was decreased by enriched CO₂ in a pH (5 or 7) independent fashion. Thus NO₃^? and NH⁺₄ uptakes are influenced by the CO₂ component of DIC independently of anaplerotic carbon provision for amino acid synthesis, and CO₂ may directly affect the uptake of NO₃^? and NH₄⁺ in ways unrelated to the NR activity in the tissue.