NO(3) Enhances the Kinase Activity for Phosphorylation of Phosphoenolpyruvate Carboxylase and Sucrose Phosphate Synthase Proteins in Wheat Leaves: Evidence from the Effects of Mannose and Okadaic Acid

The aim of this work was to determine which of the two reactions (i.e. phosphorylation or dephosphorylation) involved in the establishment of the phosphorylated status of the wheat leaf phosphoenolpyruvate carboxylase and sucrose phosphate synthase protein responds in vivo to NO₃⁻ uptake and assimilation. Detached mature leaves of wheat (Triticum aestivum L. cv Fidel) were fed with N-free (low-NO₃⁻ leaves) or 40 mm NO₃⁻ solution (high-NO₃⁻ leaves). The specific inhibition of the enzyme-protein kinase or phosphatase activities was obtained in vivo by addition of mannose or okadaic acid, respectively, in the uptake solution. Mannose at 50 mm, by blocking the kinase reaction, inhibited the processes of NO₃⁻-dependent phosphoenolpyruvate carboxylase activation and sucrose phosphate synthase deactivation. Following the addition of mannose, the deactivation of phosphoenolpyruvate carboxylase and the activation of sucrose phosphate synthase, both due to the enzyme-protein dephosphorylation, were at the same rate in low-NO₃⁻ and high-NO₃⁻ leaves, indicating that NO₃⁻ had no effect per se on the enzyme-protein phosphatase activity. Upon treatment with okadaic acid, the higher increase of phosphoenolpyruvate carboxylase and decrease of sucrose phosphate synthase activities observed in high NO₃⁻ compared with low NO₃⁻ leaves showed evidence that NO₃⁻ enhanced the protein kinase activity. These results support the concept that NO₃⁻, or a product of its metabolism, favors the activation of phosphoenolpyruvate carboxylase and deactivation of sucrose phosphate synthase in wheat leaves by promoting the light activation of the enzyme-protein kinase(s) without affecting the phosphatase(s).     

Dependency of Nitrate Reduction on Soluble Carbohydrates in Primary Leaves of Barley under Aerobic Conditions

Nitrate reduction was studied as a function of carbohydrate concentration in detached primary leaves of barley (Hordeum vulgare L. cv Numar) seedlings under aerobic conditions in light and darkness. Seedlings were grown either in continuous light for 8 days or under a regimen of 16-hour light and 8-hour dark for 8 to 15 days. Leaves of 8-day-old seedlings grown in continuous light accumulated 4 times more carbohydrates than leaves of plants grown under a light and dark regimen. When detached leaves from these seedlings were supplied with NO₃⁻ in darkness, those with the higher levels of carbohydrates reduced a greater proportion of the NO₃⁻ that was taken up. In darkness, added glucose increased the percentage of NO₃⁻ reduced up to 2.6-fold depending on the endogenous carbohydrate status of the leaves. Both NO₃⁻ reduction and carbohydrate content of the leaves increased with age. Fructose and sucrose also increased NO₃⁻ reduction in darkness to the same extent as glucose. Krebs cycle intermediates, citrate and succinate, did not increase NO₃⁻ reduction, whereas malate slightly stimulated it in darkness.

In light, 73 to 90% of the NO₃⁻ taken up was reduced by the detached leaves; therefore, an exogenous supply of glucose had little additional effect on NO₃⁻ reduction. The results indicate that in darkness the rate of NO₃⁻ reduction in primary leaves of barley depends upon the availability of carbohydrates.

     

Endogenous NO(3) in the Root as a Source of Substrate for Reduction in the Light

An experiment was conducted to investigate the reduction of endogenous NO₃⁻, which had been taken up by plants in darkness, during the course of the subsequent light period. Vegetative, nonnodulated soybean plants (Glycine max [L]. Merrill, `Ransom') were exposed to 1.0 millimolar <sup>15</sup>NO<sub>3</sub><sup>−</sup> for 12 hours in darkness and then returned to a solution containing 1.0 millimolar <sup>14</sup>NO<sub>3</sub><sup>−</sup> for the 12 hours `chase' period in the light. Another set of plants was exposed to ¹⁵NO₃⁻ during the light period to allow a direct comparison of contributions of substrate from the endogenous and exogenous sources. At the end of the ¹⁵NO₃⁻ exposure in the dark, 70% of the absorbed ¹⁵NO₃⁻ remained unreduced, and 83% of this unreduced NO₃⁻ was retained in roots. The pool of endogenous ¹⁵NO₃⁻ in roots was depleted at a steady rate during the initial 9 hours of light and was utilized almost exclusively in the formation of insoluble reduced-N in leaves. Unlabeled endogenous NO₃⁻, which had accumulated in the root prior to the previous dark period, also was depleted in the light. When exogenous ¹⁵NO₃⁻ was supplied during the light period, the rate of assimilation progressively increased, reflecting an increased rate of uptake and decreased accumulation of NO₃⁻ in the root tissue. The dark-absorbed endogenous NO₃⁻ in the root was the primary source of substrate for whole-plant NO₃⁻ reduction in the first 6 hours of the light period, and exogenous NO₃⁻ was the primary source of substrate thereafter. It is concluded that retention of NO₃⁻ in roots in darkness and its release in the following light period is an important whole-plant regulatory mechanism which serves to coordinate delivery of substrate with the maximal potential for NO₃⁻ assimilation in photosynthetic tissues.     

Regulation of NO(3) Assimilation by Anion Availability in Excised Soybean Leaves

The regulation of NO₃⁻ assimilation by xylem flux of NO₃⁻ was studied in illuminated excised leaves of soybean (Glycine max L. Merr. cv Kingsoy). The supply of exogenous NO₃⁻ at various concentrations via the transpiration stream indicated that the xylem flux of NO₃⁻ was generally rate-limiting for NO₃⁻ reduction. However, NO₃⁻ assimilation rate was maintained within narrow limits as compared with the variations of the xylem flux of NO₃⁻. This was due to considerable remobilization and assimilation of previously stored endogenous NO₃⁻ at low exogenous NO₃⁻ delivery, and limitation of NO₃⁻ reduction at high xylem flux of NO₃⁻, leading to a significant accumulation of exogenous NO₃⁻. The supply of ¹⁵NO₃⁻ to the leaves via the xylem confirmed the labile nature of the NO₃⁻ storage pool, since its half-time for exchange was close to 10 hours under steady state conditions. When the xylem flux of ¹⁵NO₃⁻ increased, the proportion of the available NO₃⁻ which was reduced decreased similarly from nearly 100% to less than 50% for both endogenous ¹⁴NO₃⁻ and exogenous ¹⁵NO₃⁻. This supports the hypothesis that the assimilatory system does not distinguish between endogenous and exogenous NO₃⁻ and that the limitation of NO₃⁻ reduction affected equally the utilization of NO₃⁻ from both sources. It is proposed that, in the soybean leaf, the NO₃⁻ storage pool is particularly involved in the short-term control of NO₃⁻ reduction. The dynamics of this pool results in a buffering of NO₃⁻ reduction against the variations of the exogenous NO₃⁻ delivery.     

Effect of Phloem-Translocated Malate on NO(3) Uptake by Roots of Intact Soybean Plants

In soybean (Glycine max L. Merr. cv Kingsoy), NO₃⁻ assimilation in leaves resulted in production and transport of malate to roots (B Touraine, N Grignon, C Grignon [1988] Plant Physiol 88: 605-612). This paper examines the significance of this phenomenon for the control of NO₃⁻ uptake by roots. The net NO₃⁻ uptake rate by roots of soybean plants was stimulated by the addition of K-malate to the external solution. It was decreased when phloem translocation was interrupted by hypocotyl girdling, and partially restored by malate addition to the medium, whereas glucose was ineffective. Introduction of K-malate into the transpiration stream using a split root system resulted in an enrichment of the phloem sap translocated back to the roots. This treatment resulted in an increase in both NO₃⁻ uptake and C excretion rates by roots. These results suggest that NO₃⁻ uptake by roots is dependent on the availability of shoot-borne, phloem-translocated malate. Shoot-to-root transport of malate stimulated NO₃⁻ uptake, and excretion of HCO₃⁻ ions was probably released by malate decarboxylation. NO₃⁻ uptake rate increased when the supply of NO₃⁻ to the shoot was increased, and decreased when the activity of nitrate reductase in the shoot was inhibited by WO₄²⁻. We conclude that in situ, NO₃⁻ reduction rate in the shoot may control NO₃⁻ uptake rate in the roots via the translocation rate of malate in the phloem.     

In Vivo Nitrate Reduction in Roots and Shoots of Barley (Hordeum vulgare L.) Seedlings in Light and Darkness

In vivo NO₃⁻ reduction in roots and shoots of intact barley (Hordeum vulgare L. var Numar) seedlings was estimated in light and darkness. Seedlings were placed in darkness for 24 hours to make them carbohydrate-deficient. During darkness, the leaves lost 75% of their soluble carbohydrates, whereas the roots lost only 15%. Detached leaves from these plants reduced only 7% of the NO₃⁻ absorbed in darkness. By contrast, detached roots from the seedlings reduced the same proportion of absorbed NO₃⁻, as did roots from normal light-grown plants. The rate of NO₃⁻ reduction in the roots accounted for that found in the intact dark-treated carbohydrate-deficient seedlings. The rates of NO₃⁻ reduction in roots of intact plants were the same for approximately 12 hours, both in light and darkness, after which the NO₃⁻ reduction rate in roots of plants placed in darkness slowly declined. In the dark, approximately 40% of the NO₃⁻ reduction occurred in the roots, whereas in light only 20% of the total NO₃⁻ reduction occurred in roots. A lesser proportion was reduced in roots because the leaves reduced more nitrate in light than in darkness.     

Effect of photosynthetic inhibitors and uncouplers of oxidative phosphorylation on nitrate and nitrite reduction in barley leaves

The effects of several photosynthetic inhibitors and uncouplers of oxidative phosphorylation on NO₃⁻ and NO₂⁻ assimilation were studied using detached barley (Hordeum vulgare L. cv Numar) leaves in which only endogenous NO₃⁻ or NO₂⁻ were available for reduction. Uncouplers of oxidative phosphorylation greatly increased NO₃⁻ reduction in both light and darkness, while photosynthetic inhibitors did not.

The NO₂⁻ concentration in the control leaves was very low in both light and darkness; 98% or more of the NO₂⁻ formed from NO₃⁻ was further assimilated in control leaves. More NO₂⁻ accumulated in the leaves in light and darkness in the presence of photosynthetic inhibitors. Of this NO₂⁻, 94% or more was further assimilated. It appears that metabolites, either external or internal to the chloroplast, capable of reducing NADP (which, in turn, could reduce ferredoxin via NADP reductase) might support NO₂⁻ reduction in darkness and light when photosynthetic electron flow is inhibited by photosynthetic inhibitors.

Nitrite assimilation was much more sensitive to uncouplers in darkness than in light: in darkness, 74% or more of NO₂⁻ formed from NO₃⁻ was further assimilated, whereas in light, 95% or more of the NO₂⁻ was further assimilated.

     

Studies of the Regulation of Nitrate Influx by Barley Seedlings Using NO(3)

Using ¹³NO₃⁻, effects of various NO₃⁻ pretreatments upon NO₃⁻ influx were studied in intact roots of barley (Hordeum vulgare L. cv Klondike). Prior exposure of roots to NO₃⁻ increased NO₃⁻ influx and net NO₃⁻ uptake. This `induction' of NO<sub>3</sub><sup>−</sup> uptake was dependent both on time and external NO<sub>3</sub><sup>−</sup> concentration ([NO<sub>3</sub><sup>−</sup>]). During induction influx was positively correlated with root [NO<sub>3</sub><sup>−</sup>]. In the postinduction period, however, NO<sub>3</sub><sup>−</sup> influx declined as root [NO<sub>3</sub><sup>−</sup>] increased. It is suggested that induction and negative feedback regulation are independent processes: Induction appears to depend upon some critical cytoplasmic [NO<sub>3</sub><sup>−</sup>]; removal of external NO<sub>3</sub><sup>−</sup> caused a reduction of <sup>13</sup>NO<sub>3</sub><sup>−</sup> influx even though mean root [NO<sub>3</sub><sup>−</sup>] remained high. It is proposed that cytoplasmic [NO<sub>3</sub><sup>−</sup>] is depleted rapidly under these conditions resulting in `deinduction' of the NO₃⁻ transport system. Beyond 50 micromoles per gram [NO₃⁻], ¹³NO₃⁻ influx was negatively correlated with root [NO₃⁻]. However, it is unclear whether root [NO₃⁻] per se or some product(s) of NO₃⁻ assimilation are responsible for the negative feedback effects.     

Assimilation of NO(3) Taken Up by Plants in the Light and in the Dark

An experiment was conducted to determine the extent that NO₃⁻ taken up in the dark was assimilated and utilized differently by plants than NO₃⁻ taken up in the light. Vegetative, nonnodulated soybean plants (Glycine max L. Merrill, `Ransom') were exposed to ¹⁵NO₃⁻ throughout light (9 hours) or dark (15 hours) phases of the photoperiod and then returned to solutions containing ¹⁴NO₃⁻, with plants sampled subsequently at each light/dark transition over 3 days. The rates of ¹⁵NO₃⁻ absorption were nearly equal in the light and dark (8.42 and 7.93 micromoles per hour, respectively); however, the whole-plant rate of ¹⁵NO₃⁻ reduction during the dark uptake period (2.58 micromoles per hour) was 46% of that in the light (5.63 micromoles per hour). The lower rate of reduction in the dark was associated with both substantial retention of absorbed ¹⁵NO₃⁻ in roots and decreased efficiency of reduction of ¹⁵NO₃⁻ in the shoot. The rate of incorporation of ¹⁵N into the insoluble reduced-N fraction of roots in darkness (1.10 micromoles per hour) was somewhat greater than that in the light (0.92 micromoles per hour), despite the lower rate of whole-plant ¹⁵NO₃⁻ reduction in darkness.

A large portion of the ¹⁵NO₃⁻ retained in the root in darkness was translocated and incorporated into insoluble reduced-N in the shoot in the following light period, at a rate which was similar to the rate of whole-plant reduction of ¹⁵NO₃⁻ acquired during the light period. Taking into account reduction of NO₃⁻ from all endogenous pools, it was apparent that plant reduction in a given light period (~13.21 micromoles per hour) exceeded considerably the rate of acquisition of exogenous NO₃⁻ (8.42 micromoles per hour) during that period. The primary source of substrate for NO₃⁻ reduction in the dark was exogenous NO₃⁻ being concurrently absorbed. In general, these data support the view that a relatively small portion (<20%) of the whole-plant reduction of NO₃⁻ in the light occurred in the root system.

     

Comparison between NO(x) Evolution Mechanisms of Wild-Type and nr(1) Mutant Soybean Leaves

The nr₁ soybean (Glycine max [L.] Merr.) mutant does not contain the two constitutive nitrate reductases, one of which is responsible for enzymic conversion of nitrite to NO_x (NO + NO₂). It was tested for possible nonenzymic NO_x formation and evolution because of known chemical reactions between NO₂⁻ and plant metabolites and the instability of nitrous acid. It did not evolve NO_x during the in vivo NR assay, but intact leaves did evolve small amounts of NO_x under dark, anaerobic conditions. Experiments were conducted to compare NO₃⁻ reduction, NO₂⁻ accumulation, and the NO_x evolution processes of the wild type (cv Williams) and the nr₁ mutant. In vivo NR assays showed that wild-type leaves had three times more NO₃⁻ reducing capacity than the nr₁ mutant. NO_x evolution from intact, anerobic nr₁ leaves was approximately 10 to 20% that from wild-type leaves. Nitrite content of the nr₁ mutant leaves was usually higher than wild type due to low NO_x evolution. Lag times and threshold NO₂⁻ concentrations for NO_x evolution were similar for the two genotypes. While only 1 to 2% of NO_x from wild type is NO₂, the nr₁ mutant evolved 15 to 30% NO₂. The kinetic patterns of NO_x evolution with time weré completely different for the mutant and wild type. Comparisons of light and heat treatments also gave very different results. It is generally accepted that the NO_x evolution by wild type is primarily an enzymic conversion of NO₂⁻ to NO. However, this report concludes that NO_x evolution by the nr₁ mutant was due to nonenzymic, chemical reactions between plant metabolites and accumulated NO₂⁻ and/or decomposition of nitrous acid. Nonenzymic NO_x evolution probably also occurs in wild type to a degree but could be easily masked by high rates of the enzymic process.     

Effects of Altered Carbohydrate Availability on Whole-Plant Assimilation of NO(3)

An experiment was conducted to investigate the relative changes in NO₃⁻ assimilatory processes which occurred in response to decreasing carbohydrate availability. Young tobacco plants (Nicotiana tabacum [L.], cv NC 2326) growing in solution culture were exposed to 1.0 millimolar ¹⁵NO₃⁻ for 6 hour intervals during a normal 12 hour light period and a subsequent period of darkness lasting 42 hours. Uptake of ¹⁵NO₃⁻ decreased to 71 to 83% of the uptake rate in the light during the initial 18 hours of darkness; uptake then decreased sharply over the next 12 hours of darkness to 11 to 17% of the light rate, coincident with depletion of tissue carbohydrate reserves and a marked decline in root respiration. Changes also occurred in endogenous ¹⁵NO₃⁻ assimilation processes, which were distinctly different than those in ¹⁵NO₃⁻ uptake. During the extended dark period, translocation of absorbed ¹⁵N out of the root to the shoot varied rhythmically. The adjustments were independent of ¹⁵NO₃⁻ uptake rate and carbohydrate status, but were reciprocally related to rhythmic adjustments in stomatal resistance and, presumably, water movement through the root system. Whole plant reduction of ¹⁵NO₃⁻ always was limited more than uptake. The assimilation of ¹⁵N into insoluble reduced-N in roots remained a constant proportion of uptake throughout, while assimilation in the shoot declined markedly in the first 18 hours of darkness before stabilizing at a low level. The plants clearly retained a capacity for ¹⁵NO₃⁻ reduction and synthesis of insoluble reduced-¹⁵N even when ¹⁵NO₃⁻ uptake was severely restricted and minimal carbohydrate reserves remained in the tissue.     

Studies of the Uptake of Nitrate in Barley: I. Kinetics of NO(3) Influx

¹³NO₃⁻ was used to investigate patterns of NO₃⁻ influx into roots of barley plants (Hordeum vulgare L. cv Klondike) previously grown with (`induced') or without (`uninduced') a source of external NO₃⁻ ([NO₃⁻]₀). In both induced and uninduced plants, ¹³NO₃⁻ influx was biphasic in the range from 0.005 to 50 moles per cubic meter [NO₃⁻]₀. In the low concentration range (<1 mole per cubic meter for induced plants and <0.3 mole per cubic meter for uninduced plants), influx was saturable and V_max and K_m values for influx either increased or decreased according to NO₃⁻ pretreatment. By contrast, ¹³NO₃⁻ influx in the high concentration range revealed a strictly linear concentration dependence. These fluxes appeared to be mediated by a constitutive, rather than an inducible, transport system.     

Photosynthesis and photosynthate partitioning in n(2)-fixing soybeans

Leaf area, chlorophyll content, net CO₂ photoassimilation, and the partitioning of fixed carbon between leaf sucrose and starch and soluble protein were examined in Glycine max (L) Merr. cv Williams grown under three different nitrogen regimes. One group (Nod+/+) was inoculated with Bradyrhizobium and watered daily with a nutrient solution containing 6 millimolar NH₄NO₃. A second set (Nod+/−) was inoculated and had N₂ fixation as its sole source of nitrogen. A third group (Nod⁻) was not inoculated and was watered daily with a nutrient solution containing 6 millimolar NH₄NO₃. The mean net micromole CO₂ uptake per square decimeter per hour of the most recently matured source leaves was similar among the three groups of plants, being about 310. Mean leaf area of the source leaves, monitored for net photosynthesis was also similar. However, the mean milligram of chlorophyll per square decimeter of Nod+/− test leaves was about 50% lower than the other groups' leaves and indicated nitrogen deficiency. Thus, Nod+/− utilized their chlorophyll more efficiently for photosynthetic CO₂ uptake than the plants of the other treatments. The ratio of foliar carbohydrate:protein content was high in Nod+/− but low in the plants from the other two treatments. This inverse relationship between foliar protein and carbohydrate content suggests that more fixed carbon is diverted to the synthesis of protein when nitrogen availability is high. It was also found that Nod+/− sequestered more storage protein in their paraveinal mesophyll than plants of the other treatments. This study indicates that when inorganic nitrogen regimes are used to control photosynthate partitioning, then both leaf carbohydrate and leaf protein must be considered as end products of carbon assimilate allocation.     

Mitochondrial Respiration Can Support NO(3) and NO(2) Reduction during Photosynthesis : Interactions between Photosynthesis, Respiration, and N Assimilation in the N-Limited Green Alga Selenastrum minutum

Mass spectrometric analysis shows that assimilation of inorganic nitrogen (NH₄⁺, NO₂⁻, NO₃⁻) by N-limited cells of Selenastrum minutum (Naeg.) Collins results in a stimulation of tricarboxylic acid cycle (TCA cycle) CO₂ release in both the light and dark. In a previous study we have shown that TCA cycle reductant generated during NH₄⁺ assimilation is oxidized via the cytochrome electron transport chain, resulting in an increase in respiratory O₂ consumption during photosynthesis (HG Weger, DG Birch, IR Elrifi, DH Turpin [1988] Plant Physiol 86: 688-692). NO₃⁻ and NO₂⁻ assimilation resulted in a larger stimulation of TCA cycle CO₂ release than did NH₄⁺, but a much smaller stimulation of mitochondrial O₂ consumption. NH₄⁺ assimilation was the same in the light and dark and insensitive to DCMU, but was 82% inhibited by anaerobiosis in both the light and dark. NO₃⁻ and NO₂⁻ assimilation rates were maximal in the light, but assimilation could proceed at substantial rates in the light in the presence of DCMU and in the dark. Unlike NH₄⁺, NO₃⁻ and NO₂⁻ assimilation were relatively insensitive to anaerobiosis. These results indicated that operation of the mitochondrial electron transport chain was not required to maintain TCA cycle activity during NO₃⁻ and NO₂⁻ assimilation, suggesting an alternative sink for TCA cycle generated reductant. Evaluation of changes in gross O₂ consumption during NO₃⁻ and NO₂⁻ assimilation suggest that TCA cycle reductant was exported to the chloroplast during photosynthesis and used to support NO₃⁻ and NO₂⁻ reduction.     

Characterization of a NO(3)-Sensitive H-ATPase from Corn Roots

When assayed in the presence of azide, NO₃⁻ was shown to be a specific inhibitor of a proton-translocating ATPase present in corn (Zea mays L. cv WF9 × M017) root microsomal membranes. The distribution of the NO₃⁻-sensitive ATPase on sucrose gradients and its general characteristics are similar to those previously reported for the anion-stimulated H⁺-ATPase of corn roots believed to be of tonoplast origin. An ATPase inhibited by 20 μm vanadate and insensitive to molybdate was also identified in corn root microsomal membranes which could be largely separated from the NO₃⁻-sensitive ATPase on sucrose gradients and is believed to be of plasma membrane origin. Inasmuch as both ATPase most likely catalyze the efflux of H⁺ from the cytoplasm, our objective was to characterize and compare the properties of both ATPases under identical experimental conditions. The vanadate-sensitive ATPase was stimulated by cations (K⁺ > NH₄⁺ > Rb⁺ > Cs⁺ > Li⁺ > Na⁺ > choline⁺) whereas the NO₃⁻-sensitive ATPase was stimulated by anions (Cl⁻ > Br⁻ > C₂H₃O₂⁻ > SO₄²⁻ > I⁻ > HCO₃⁻ > SCN⁻). Both ATPases required divalent cations. However, the order of preference for the NO₃⁻-sensitive ATPase (Mn²⁺ > Mg²⁺ > Co²⁺ > Ca²⁺ > Zn²⁺) differed from that of the vanadate-sensitive ATPase (Co²⁺ > Mg²⁺ > Mn²⁺ > Zn²⁺ > Ca²⁺). The vanadate-sensitive ATPase required higher concentrations of Mg:ATP for full activity than did the NO₃⁻-sensitive ATPase. The kinetics for Mg:ATP were complex for the vanadate-sensitive ATPase, indicating positive cooperativity, but were simple for the NO₃⁻-sensitive ATPase. Both ATPases exhibited similar temperature and pH optima (pH 6.5). The NO₃⁻-sensitive ATPase was stimulated by gramicidin and was associated with NO₃⁻-inhibitable H⁺ transport measured as quenching of quinacrine fluorescence. It was insensitive to molybdate, azide, and vanadate, but exhibited slight sensitivity to ethyl-3-(3-dimethylaminopropyl carbodiimide) and mersalyl. Overall, these results indicate several properties which distinguish these two ATPases and suggest that under defined conditions NO₃⁻-sensitive ATPase activity may be used as a quantitative marker for those membranes identified tentatively as tonoplast in mixed or nonpurified membrane fractions. We feel that NO₃⁻ sensitivity is a better criterion by which to identify this ATPase than either Cl⁻ stimulation or H⁺ transport because it is less ambiguous. It is also useful in identifying the enzyme following solubilization.     

Role of Nitrate and Nitrite in the Induction of Nitrite Reductase in Leaves of Barley Seedlings

The role of NO₃⁻ and NO₂⁻ in the induction of nitrite reductase (NiR) activity in detached leaves of 8-day-old barley (Hordeum vulgare L.) seedlings was investigated. Barley leaves contained 6 to 8 micromoles NO₂⁻/gram fresh weight × hour of endogenous NiR activity when grown in N-free solutions. Supply of both NO₂⁻ and NO₃⁻ induced the enzyme activity above the endogenous levels (5 and 10 times, respectively at 10 millimolar NO₂⁻ and NO₃⁻ over a 24 hour period). In NO₃⁻-supplied leaves, NiR induction occurred at an ambient NO₃⁻ concentration of as low as 0.05 millimolar; however, no NiR induction was found in leaves supplied with NO₂⁻ until the ambient NO₂⁻ concentration was 0.5 millimolar. Nitrate accumulated in NO₂⁻-fed leaves. The amount of NO₃⁻ accumulating in NO₂⁻-fed leaves induced similar levels of NiR as did equivalent amounts of NO₃⁻ accumulating in NO₃⁻-fed leaves. Induction of NiR in NO₂⁻-fed leaves was not seen until NO₃⁻ was detectable (30 nanomoles/gram fresh weight) in the leaves. The internal concentrations of NO₃⁻, irrespective of N source, were highly correlated with the levels of NiR induced. When the reduction of NO₃⁻ to NO₂⁻ was inhibited by WO₄²⁻, the induction of NiR was inhibited only partially. The results indicate that in barley leaves NiR is induced by NO₃⁻ directly, i.e. without being reduced to NO₂⁻, and that absorbed NO₂⁻ induces the enzyme activity indirectly after being oxidized to NO₃⁻ within the leaf.     

Relative Content of NO(3) and Reduced N in Xylem Exudate as an Indicator of Root Reduction of Concurrently Absorbed NO(3)

It is unclear if the relative content of NO₃⁻ and reduced N in xylem exudate provides an accurate estimate of the percentage reduction of concurrently absorbed NO₃⁻ in the root. Experiments were conducted to determine whether NO₃⁻ and reduced N in xylem exudate of vegetative, nonnodulated soybean plants (Glycine max [L.] Merr., `Ransom') originated from exogenous recently absorbed ¹⁵NO₃⁻ or from endogenous ¹⁴N pools. Plants either were decapitated and exposed to ¹⁵NO₃⁻ solutions for 2 hours or were decapitated for the final 20 minutes of a 50-minute exposure to ¹⁵NO₃⁻ in the dark and in the light. Considerable amounts of ¹⁴NO₃⁻ and reduced ¹⁴N were transported into the xylem, but almost all of the ¹⁵N was present as ¹⁵NO₃⁻. Dissimilar changes in transport of ¹⁴NO₃⁻, reduced ¹⁴N and ¹⁵NO₃⁻ during the 2 hours of sap collection resulted in large variability over time in the percentage of total N in the exudate which was reduced N. Over a 20-minute period the rate of ¹⁵N transport into the xylem of decapitated plants was only 21 to 36% of the ¹⁵N delivered to the shoot of intact plants. Based on the proportion of total ¹⁵N which was found as reduced ¹⁵N in exudate and in intact plants in the dark, it was estimated that 5 to 17% of concurrently absorbed ¹⁵NO₃⁻ was reduced in the root. This was much less than the 38 to 59% which would have been predicted from the relative content of total NO₃⁻ and total reduced N in the xylem exudate.     

Comparative Induction of Nitrate Reductase by Nitrate and Nitrite in Barley Leaves

The comparative induction of nitrate reductase (NR) by ambient NO₃⁻ and NO₂⁻ as a function of influx, reduction (as NR was induced) and accumulation in detached leaves of 8-day-old barley (Hordeum valgare L.) seedlings was determined. The dynamic interaction of NO₃⁻ influx, reduction and accumulation on NR induction was shown. The activity of NR, as it was induced, influenced its further induction by affecting the internal concentration of NO₃⁻. As the ambient concentration of NO₃⁻ increased, the relative influences imposed by influx and reduction on NO₃⁻ accumulation changed with influx becoming a more predominant regulant. Significant levels of NO₃⁻ accumulated in NO₂⁻-fed leaves. When the leaves were supplied cycloheximide or tungstate along with NO₂⁻, about 60% more NO₃⁻ accumulated in the leaves than in the absence of the inhibitors. In NO₃⁻-supplied leaves NR induction was observed at an ambient concentration of as low as 0.02 mm. No NR induction occurred in leaves supplied with NO₂⁻ until the ambient NO₂⁻ concentration was 0.5 mm. In fact, NR induction from NO₂⁻ solutions was not seen until NO₃⁻ was detected in the leaves. The amount of NO₃⁻ accumulating in NO₂⁻-fed leaves induced similar levels of NR as did equivalent amounts of NO₃⁻ accumulating from NO₃⁻-fed leaves. In all cases the internal concentration of NO₃⁻, but not NO₂⁻, was highly correlated with the amount of NR induced. The evidence indicated that NO₃⁻ was a more likely inducer of NR than was NO₂⁻.     

Regulation of NO(3) Influx in Barley : Studies Using NO(3)

Short-term (10 minutes) measurements of plasmalemma NO₃⁻ influx (_oc) into roots of intact barley plants were obtained using ¹³NO₃⁻. In plants grown for 4 days at various NO₃⁻ levels (0.1, 0.2, 0.5 millimolar), _oc was found to be independent of the level of NO₃⁻ pretreatment. Similarly, pretreatment with Cl⁻ had no effect upon plasmalemma ¹³NO₃⁻ influx. Plants grown in the complete absence of ¹³NO₃⁻ (in CaSO₄ solutions) subsequently revealed influx values which were more than 50% lower than for plants grown in NO₃⁻. Based upon the documented effects of NO₃⁻ or Cl⁻ pretreatments on net uptake of NO₃⁻, these observations suggest that negative feedback from vacuolar NO₃⁻ and/or Cl⁻ acts at the tonoplast but not at the plasmalemma. When included in the influx medium, 0.5 millimolar Cl⁻ was without effect upon ¹³NO₃⁻ influx, but NH₄⁺ caused approximately 50% reduction of influx at this concentration.     

Short Term Studies of Nitrate Uptake into Barley Plants Using Ion-Specific Electrodes and ClO(3): II. Regulation of NO(3) Efflux by NH(4)

The influence of NH₄⁺, in the external medium, on fluxes of NO₃⁻ and K⁺ were investigated using barley (Hordeum vulgare cv Betzes) plants. NH₄⁺ was without effect on NO₃⁻ (³⁶ClO₃⁻) influx whereas inhibition of net uptake appeared to be a function of previous NO₃⁻ provision. Plants grown at 10 micromolar NO₃⁻ were sensitive to external NH₄⁺ when uptake was measured in 100 micromolar NO₃⁻. By contrast, NO₃⁻ uptake (from 100 micromolar NO₃⁻) by plants previously grown at this concentration was not reduced by NH₄⁺ treatment. Plants pretreated for 2 days with 5 millimolar NO₃⁻ showed net efflux of NO₃⁻ when roots were transferred to 100 micromolar NO₃⁻. This efflux was stimulated in the presence of NH₄⁺. NH₄⁺ also stimulated NO₃⁻ efflux from plants pretreated with relatively low nitrate concentrations. It is proposed that short term effects on net uptake of NO₃⁻ occur via effects upon efflux. By contrast to the situation for NO₃⁻, net K⁺ uptake and influx of ³⁶Rb⁺-labeled K⁺ was inhibited by NH₄⁺ regardless of the nutrient history of the plants. Inhibition of net K⁺ uptake reached its maximum value within 2 minutes of NH₄⁺ addition. It is concluded that the latter ion exerts a direct effect upon K⁺ influx.