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.

     

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.

     

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.     

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.

     

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.     

Comparative Kinetics and Reciprocal Inhibition of Nitrate and Nitrite Uptake in Roots of Uninduced and Induced Barley (Hordeum vulgare L.) Seedlings

Nitrate and NO₂⁻ transport by roots of 8-day-old uninduced and induced intact barley (Hordeum vulgare L. var CM 72) seedlings were compared to kinetic patterns, reciprocal inhibition of the transport systems, and the effect of the inhibitor, p-hydroxymercuribenzoate. Net uptake of NO₃⁻ and NO₂⁻ was measured by following the depletion of the ions from the uptake solutions. The roots of uninduced seedlings possessed a low concentration, saturable, low K_m, possibly a constitutive uptake system, and a linear system for both NO₃⁻ and NO₂⁻. The low K_m system followed Michaelis-Menten kinetics and approached saturation between 40 and 100 micromolar, whereas the linear system was detected between 100 and 500 micromolar. In roots of induced seedlings, rates for both NO₃⁻ and NO₂⁻ uptake followed Michaelis-Menten kinetics and approached saturation at about 200 micromolar. In induced roots, two kinetically identifiable transport systems were resolved for each anion. At the lower substrate concentrations, less than 10 micromolar, the apparent low K_ms of NO₃⁻ and NO₂⁻ uptake were 7 and 9 micromolar, respectively, and were similar to those of the low K_m system in uninduced roots. At substrate concentrations between 10 and 200 micromolar, the apparent high K_m values of NO₃⁻ uptake ranged from 34 to 36 micromolar and of NO₂⁻ uptake ranged from 41 to 49 micromolar. A linear system was also found in induced seedlings at concentrations above 500 micromolar. Double reciprocal plots indicated that NO₃⁻ and NO₂⁻ inhibited the uptake of each other competitively in both uninduced and induced seedlings; however, K_i values showed that NO₃⁻ was a more effective inhibitor than NO₂⁻. Nitrate and NO₂⁻ transport by both the low and high K_m systems were greatly inhibited by p-hydroxymercuribenzoate, whereas the linear system was only slightly inhibited.     

Nitrate Reductase Activity in Shoots and Roots of Maize Seedlings as Affected by the Form of Nitrogen Nutrition and the pH of the Nutrient Solution

The effect of nitrogen form (NH₄-N, NH₄-N + NO₃⁻, NO₃⁻) on nitrate reductase activity in roots and shoots of maize (Zea mays L. cv INRA 508) seedlings was studied. Nitrate reductase activity in leaves was consistent with the well known fact that NO₃⁻ increases, and NH₄⁺ and amide-N decrease, nitrate reductase activity. Nitrate reductase activity in the roots, however, could not be explained by the root content of NO₃⁻, NH₄-N, and amide-N. In roots, nitrate reductase activity in vitro was correlated with the rate of nitrate reduction in vivo. Inasmuch as nitrate reduction results in the production of OH⁻ and stimulates the synthesis of organic anions, it was postulated that nitrate reductase activity of roots is stimulated by the released OH⁻ or by the synthesized organic anions rather than by nitrate itself. Addition of HCO₃⁻ to nutrient solution of maize seedlings resulted in a significant increase of the nitrate reductase activity in the roots. As HCO₃⁻, like OH⁻, increases pH and promotes the synthesis of organic anions, this provides circumstantial evidence that alkaline conditions and/or organic anions have a more direct impact on nitrate reductase activity than do NO₃⁻, NH₄-N, and amide-N.     

Differential light induction of nitrate reductases in greening and photobleached soybean seedlings

Soybean (Glycine max [L.] Merr.) seeds were imbibed and germinated with or without NO₃⁻, tungstate, and norflurazon (San 9789). Norflurazon is a herbicide which causes photobleaching of chlorophyll by inhibiting carotenoid synthesis and which impairs normal chloroplast development. After 3 days in the dark, seedlings were placed in white light to induce extractable nitrate reductase activity. The induction of maximal nitrate reductase activity in greening cotyledons did not require NO₃⁻ and was not inhibited by tungstate. Induction of nitrate reductase activity in norflurazon-treated cotyledons had an absolute requirement for NO₃⁻ and was completely inhibited by tungstate. Nitrate was not detected in seeds or seedlings which had not been treated with NO₃⁻. The optimum pH for cotyledon nitrate reductase activity from norflurazon-treated seedlings was at pH 7.5, and near that for root nitrate reductase activity, whereas the optimum pH for nitrate reductase activity from greening cotyledons was pH 6.5. Induction of root nitrate reductase activity was also inhibited by tungstate and was dependent on the presence of NO₃⁻, further indicating that the isoform of nitrate reductase induced in norflurazon-treated cotyledons is the same or similar to that found in roots. Nitrate reductases with and without a NO₃⁻ requirement for light induction appear to be present in developing leaves. In vivo kinetics (light induction and dark decay rates) and in vitro kinetics (Arrhenius energies of activation and NADH:NADPH specificities) of nitrate reductases with and without a NO₃⁻ requirement for induction were quite different. K_m values for NO₃⁻ were identical for both nitrate reductases.     

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.     

Soybean mutants lacking constitutive nitrate reductase activity : I. Selection and initial plant characterization

The objectives of this study were to select and initially characterize mutants of soybean (Glycine max L. Merr. cv Williams) with decreased ability to reduce nitrate. Selection involved a chlorate screen of approximately 12,000 seedlings (progeny of mutagenized seed) and subsequent analyses for low nitrate reductase (LNR) activity. Three lines, designated LNR-2, LNR-3, and LNR-4, were selected by this procedure.

In growth chamber studies, the fully expanded first trifoliolate leaf from NO₃⁻-grown LNR-2, LNR-3, and LNR-4 plants had approximately 50% of the wild-type NR activity. Leaves from urea-grown LNR-2, LNR-3, and LNR-4 plants had no NR activity while leaves from comparable wild-type plants had considerable activity; the latter activity does not require the presence of NO₃⁻ in the nutrient solution for induction and on this basis is tentatively considered as a constitutive enzyme. Summation of constitutive (urea-grown wild-type plants) and inducible (NO₃⁻-grown LNR-2, LNR-3, or LNR-4 plants) leaf NR activities approximated activity in leaves of NO₃⁻-grown wild-type plants. Root NR activities were comparable in wild-type and mutant plants grown on NO₃⁻, and roots of both plant types lacked constitutive NR activity when grown on urea. In both growth chamber- and field-grown plants, oxides of nitrogen [NO_(x)] were evolved from young leaves of wild-type plants, but not from leaves of LNR-2 plants, during in vivo NR assays. Analysis of leaves from different canopy locations showed that constitutive NR activity was confined to the youngest three fully expanded leaves of the wild-type plant and, therefore, on a total plant canopy basis, the NR activity of LNR-2 plants was approximately 75% that of wild-type plants. It is concluded that: (a) the NR activity in leaves of NO₃⁻-grown wild-type plants includes both constitutive and inducible activity; (b) the missing NR activity in LNR-2, LNR-3, and LNR-4 leaves is the constitutive component; and (c) the constitutive NR activity is associated with NO_(x) evolution and occurs only in physiologically young leaves.

     

Influence of Nitrate and Ammonium Nutrition on the Uptake, Assimilation, and Distribution of Nutrients in Ricinus communis

Ricinus communis L. plants were grown in nutrient solutions in which N was supplied as NO₃⁻ or NH₄⁺, the solutions being maintained at pH 5.5. In NO₃⁻-fed plants excess nutrient anion over cation uptake was equivalent to net OH⁻ efflux, and the total charge from NO₃⁻ and SO₄²⁻ reduction equated to the sum of organic anion accumulation plus net OH⁻ efflux. In NH₄⁺-fed plants a large H⁺ efflux was recorded in close agreement with excess cation over anion uptake. This H⁺ efflux equated to the sum of net cation (NH₄⁺ minus SO₄²⁻) assimilation plus organic anion accumulation. In vivo nitrate reductase assays revealed that the roots may have the capacity to reduce just under half of the total NO₃⁻ that is taken up and reduced in NO₃⁻-fed plants. Organic anion concentration in these plants was much higher in the shoots than in the roots. In NH₄⁺-fed plants absorbed NH₄⁺ was almost exclusively assimilated in the roots. These plants were considerably lower in organic anions than NO₃⁻-fed plants, but had equal concentrations in shoots and roots. Xylem and phloem saps were collected from plants exposed to both N sources and analyzed for all major contributing ionic and nitrogenous compounds. The results obtained were used to assist in interpreting the ion uptake, assimilation, and accumulation data in terms of shoot/root pH regulation and cycling of nutrients.     

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⁻.     

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.     

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.     

The role of nitrate and ammonium ions and light on the induction of nitrate reductase in maize leaves

Corn seedlings (Zea mays cv W64A × W182E) were grown hydroponically, in the presence or absence of NO₃⁻, with or without light and with NH₄Cl as the only N source. In agreement with earlier results nitrate reductase (NR) activity was found only in plants treated with both light and NO₃⁻. Sodium dodecyl sulfate-polyacrylamide gel electrophoresis followed by transfer of the proteins to nitrocellulose paper and reaction with antibodies prepared against a pure NR showed that crude extracts prepared from light-grown plants had a polypeptide of approximately 116 kilodaltons (the subunit size for NR) when NO₃⁻ was present in the growth medium. Crude extracts from plants grown in the dark did not have the 116 kilodalton polypeptide, although smaller polypeptides, which reacted with NR-immunoglobulin G, were sometimes found at the gel front. When seedlings were grown on Kimpack paper or well washed sand, NR activity was again found only when the seedlings were exposed to light and NO₃⁻. Under these conditions, however, a protein of about 116 kilodaltons, which reacted with the NR antibody was present in light-grown plants whether NO₃⁻ was added to the system or not. The NR antibody cross-reacting protein was also seen in hydroponically grown plants when NH₄Cl⁻ was the only added form of nitrogen. These results indicate that the induction of an inactive NR-protein precursor in corn is mediated either by extremely low levels of NO₃⁻ or by some other unidentified factor, and that higher levels of NO₃⁻ are necessary for converting the inactive NR cross-reacting protein to a form of the enzyme capable of reducing NO₃⁻ to NO₂⁻.     

Nitrogen metabolism of soybeans: I. Effect of tungstate on nitrate utilization, nodulation, and growth

The effects of N source (6 mm nitrogen as NO₃⁻ or urea) and tungstate (0, 100, 200, 300, and 400 μm Na₂ WO₄) on nitrate metabolism, nodulation, and growth of soybean (Glycine max [L.] Merr.) plants were evaluated. Nitrate reductase activity and, to a lesser extent, NO₃⁻ content of leaf tissue decreased with the addition of tungstate to the nutrient growth medium. Concomitantly, nodule mass and acetylene reduction activity of NO₃⁻-grown plants increased with addition of tungstate to the nutrient solution. In contrast, nodule mass and acetylene reduction activity of urea-grown plants decreased with increased nutrient tungstate levels. The acetylene reduction activity of nodulated roots of NO₃⁻-grown plants was less than 10% of the activity of nodulated roots of urea-grown plants when no tungstate was added. At 300 and 400 μm tungstate levels, acetylene reduction activity of nodulated roots of NO₃⁻-grown plants exceeded the activity of comparable urea-grown plants.     

Spinach Leaf Chloroplast CO(2) and NO(2) Photoassimilations Do Not Compete for Photogenerated Reductant: Manipulation of Reductant Levels by Quantum Flux Density Titrations

Potential competition between CO₂ and NO₂⁻ photoassimilation for photogenerated reductant (e.g. reduced ferredoxin and NADPH) was examined employing isolates of mesophyll cells and intact chloroplasts derived from mature `source' spinach leaves. Variations in the magnitude of incident light energy were used to manipulate the supply of reductant in situ within chloroplasts. Leaf cell and plastid isolates were fed with saturating CO₂ and/or NO₂⁻ to produce the highest demand for reductant by CO₂ and/or NO₂⁻ assimilatory processes (enzymes). Even in the presence of CO₂ fixation, NO₂⁻ reduction in intact leaf cell isolates as well as plastid isolates was maximal at light energies as low as 50 to 200 microeinsteins per second per square meter. Simultaneously, 500 to 800 microeinsteins per second per square meter were required to support maximal CO₂ assimilation. Regardless of the magnitude of the incident light energy, CO₂ assimilation did not repress NO₂⁻ reduction, nor were these two processes mutually repressed. These observations have been interpreted to mean that reduced ferredoxin levels in situ in the plastids of mature source leaf mesophyll cells were adequate to supply the concurrent maximal demands exerted by enzymes associated with CO₂ as well as with inorganic nitrogen photoassimilation.     

Cation pretreatment effects on nitrate uptake, xylem exudate, and malate levels in wheat seedlings

Week-old wheat seedlings absorbed at least 40% NO₃⁻ from NaNO₃ when preloaded with K⁺ than when preloaded with Na⁺ or Ca²⁺. Cultures of Triticum vulgare L. cv. Arthur were grown for 5 days on 0.2 mm CaSO₄, pretreated for 48 hours with either 1 mm CaSO₄, K₂SO₄, or Na₂SO₄, and then transferred to 1 mm NaNO₃. All solutions contained 0.2 mm CaSO₄. Shoots of K⁺-preloaded plants accumulated three times more NO₃⁻ than shoots of the other two treatments. Initially, the K⁺-preloaded plants contained 10-fold more malate than either Na⁺- or Ca²⁺-preloaded seedlings. During the 48-hour treatment with NaNO₃, malate in both roots and shoots of the K⁺-preloaded seedlings decreased. Seedlings preloaded with K⁺ reduced 25% more NO₃⁻ than those preloaded with either Na⁺ or Ca²⁺. These experiments indicate that K⁺ enhanced NO₃⁻ uptake and reduction even though the absorption of K⁺ and NO₃⁻ were separated in time. Xylem exudate of K⁺-pretreated plants contained roughly equivalent concentrations of K⁺ and NO₃⁻, but exudate from Na⁺ and Ca²⁺-pretreated plants contained two to four times more NO₃⁻ than K⁺. Therefore K⁺ is not an obligatory counterion for NO₃⁻ transport in xylem.     

Studies on molybdenum absorption and transport in bean and rice

The patterns of molybdenum (MoO₄²⁻) absorption and transport were investigated in intact bean (Phaseolus vulgaris L.) and rice (Oryza sativa L. cv. I.R.8) plants. The mobility of MoO₄²⁻ absorbed by roots and by leaves was compared with that of a freely mobile element, Rb⁺. Although MoO₄²⁻ absorption by bean roots was nearly as high as that of Rb⁺, its transport to the shoot was considerably less. When MoO₄²⁻ was fed to one of the primary leaves, most of it was transported to the stem and root. Evidence obtained here showed that MoO₄²⁻ was mobile. Experiments with intact rice seedlings revealed large differences in the absorption and transport of MoO₄²⁻ between the plants grown in CaSO₄ and those in Hoagland solution. Molybdate uptake by excised rice roots was suggested to be an active process since it was greatly inhibited by a metabolic inhibitor. The presence of Mn²⁺, Zn²⁺, Cu²⁺, CI⁻, or SO₄²⁻ in the absorption medium reduced MoO₄²⁻ uptake which was markedly enhanced by the presence of Fe²⁺.     

Early effects of salinity on nitrate assimilation in barley seedlings

The effect of NaCl and Na₂SO₄ salinity on NO₃⁻ assimilation in young barley (Hordeum vulgare L. var Numar) seedlings was studied. The induction of the NO₃⁻ transporter was affected very little; the major effect of the salts was on its activity. Both Cl⁻ and SO₄²⁻ salts severely inhibited uptake of NO₃⁻. When compared on the basis of osmolality of the uptake solutions, Cl⁻ salts were more inhibitory (15-30%) than SO₄²⁻ salts. At equal concentrations, SO₄²⁻ salts inhibited NO₃⁻ uptake 30 to 40% more than did Cl⁻ salts. The absolute concentrations of each ion seemed more important as inhibitors of NO₃⁻ uptake than did the osmolality of the uptake solutions. Both K⁺ and Na⁺ salts inhibited NO₃⁻ uptake similarly; hence, the process seemed more sensitive to anionic salinity than to cationic salinity.

Unlike NO₃⁻ uptake, NO₃⁻ reduction was not affected by salinity in short-term studies (12 hours). The rate of reduction of endogenous NO₃⁻ in leaves of seedlings grown on NaCl for 8 days decreased only 25%. Nitrate reductase activity in the salt-treated leaves also decreased 20% but its activity, determined either in vitro or by the `anaerobic' in vivo assay, was always greater than the actual in situ rate of NO₃⁻ reduction. When salts were added to the assay medium, the in vitro enzymic activity was severely inhibited; whereas the anaerobic in vivo nitrate reductase activity was affected only slightly. These results indicate that in situ nitrate reductase activity is protected from salt injury. The susceptibility to injury of the NO₃⁻ transporter, rather than that of the NO₃⁻ reduction system, may be a critical factor to plant survival during salt stress.