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Nitrate and Ammonium Contribute to the Distinct Nitrogen Metabolism of Populus simonii during Moderate Salt Stress

Soil salinity is a major abiotic stressor affecting plant growth. Salinity affects nitrification and ammonification in the soil, however, limited information is available on the influence of different N sources on N metabolism during salt stress. To understand the N metabolism changes in response to different N sources during moderate salt stress, we investigated N uptake, assimilation and the transcript abundance of associated genes in Populus simonii seedlings treated with moderate salt stress (75mM NaCl) under hydroponic culture conditions with nitrate (NO3-) or ammonium (NH4+). Salt stress negatively affected plant growth in both NH4+-fed and NO3--fed plants. Both NH4+ uptake and the total N concentration were significantly increased in the roots of the NH4+-fed plants during salt stress. However, the NO3- uptake and nitrate reductase (NR) and nitrite reductase (NiR) activity primarily depended on the NO3- supply and was not influenced by salt stress. Salt stress decreased glutamine synthetase (GS) and glutamate synthase (GOGAT) activity in the roots and leaves. Most genes associated with NO3-uptake, reduction and N metabolism were down-regulated or remained unchanged; while two NH4+ transporter genes closely associated with NH4+ uptake (AMT1;2 and AMT1;6) were up-regulated in response to salt stress in the NH4+-fed plants. The accumulation of different amino acid compounds was observed in the NH4+- and NO3-- fed plants during salt treatment. The results suggested that N metabolism in P. simonii plants exposed to salt enhanced salt resistance in the plants that were fed with NO3- instead of NH4+ as the sole N source.

) or ammonium (NH 4 + ). Salt stress negatively affected plant growth in both NH 4 + -fed and NO 3 --fed plants. Both NH 4 + uptake and the total N concentration were significantly increased in the roots of the NH 4 + -fed plants during salt stress. However, the NO 3 uptake and nitrate reductase (NR) and nitrite reductase (NiR) activity primarily depended on the NO 3 supply and was not influenced by salt stress. Salt stress decreased glutamine synthetase (GS) and glutamate synthase (GOGAT) activity in the roots and leaves. Most genes associated with NO 3 uptake, reduction and N metabolism were downregulated or remained unchanged; while two NH 4 + transporter genes closely associated with NH 4 + uptake (AMT1;2 and AMT1;6) were up-regulated in response to salt stress in the NH 4 + -fed plants. The accumulation of different amino acid compounds was observed in the NH 4 + -and NO 3

Introduction
Salinity is a major abiotic stressor that affects plant growth and productivity [1]. Salt stress constitutes an agricultural and environmental problem worldwide, and salinity is expected to cause serious salinization problems for more than 50% of all arable lands until 2050 [2,3]. NaCl stress leads to various deleterious effects at morphological, physiological, biochemical and molecular levels. Salinity affects nitrification and ammonification in the soil [4], thus, the deleterious effect of NaCl stress on plant growth might relate to changes of nitrogen (N) uptake and metabolism [5] since N is one of the key mineral nutrients for plant growth and development. Different N metabolism has been reported in different species in response to N nutrition and salinity [6,7]. The salt stress tolerance of some durum wheat cultivars (Triticum turgidum subsp.durum) was dependent on nitrogen availability [7]. Earlier studies also demonstrated that salt stress led to altered ion balance and nitrogen metabolism in rice (Oryza sativa L.) [8]. A sufficient N supply compensates and corrects nutritional imbalances in salt-stressed plants. For instance, NH 4 + application could lower the uptake of cations in maize (Zea mays L.) [9].
Previous studies have focused on the influence of the N supply on plant growth and antioxidant enzyme activity during salt stress. For example, the growth inhibition of Catharanthus roseus under salt stress could largely be ameliorated by fertilization with both ammonium (NH 4 + ) and nitrate (NO 3 -) [10]. NH 4 + -fed plants of the halophyte Spartina alterniflora exhibited enhanced growth compared to NO 3 --fed plants in high salinity conditions, reflecting the high antioxidant enzyme activity in NH 4 + -fed plants [11]. However, different results were obtained in Pisum sativum [12] and Triticum aestivum [13], suggesting that NH 4 + might increase sensitivity to NaCl treatment. These results suggest that either ammonium or nitrate could improve salt tolerance, depending on the characteristics of the species and its specific ecological conditions. N metabolism involves the uptake, transport, assimilation and utilization of N for amino acid biosynthesis and ultimately growth [14]. NH 4 + and NO 3 -in soil solution are the two major inorganic N forms for plant. NO 3 is converted to NH 4 + by NR and NiR. After direct uptake or conversion from NO 3 -, NH 4 + is assimilated to glutamine and glutamate via glutamine synthetase (GS) and glutamate synthase (GOGAT), and the products of the GS/GOGAT pathway are required for the biosynthesis of other nitrogenous compounds [14]. Each of these steps might be differently regulated by the N source, leading to differences in N metabolism and the performance of plants during salt stress. N source availability may be an important determinant of species distribution in ecosystems and these differences in the patterns of Nutilization may be a factor in niche separation among species [15][16][17][18]. However, limited information is available on the influence of different N sources, such as NO 3 - [19]. In pea plants with NH 4 + or NO 3 under salt stress, the root growth and belowground total N concentration were reduced, and the amino acid concentration increased at the expense of the protein content [12]. NH 4 + might also increase sensitivity to NaCl treatment in P. canescens; It appears that the reduction of N uptake in plants grown in the solutions containing ammonium as sole N source can be attributed to an increased Na: NH 4 + ratio and competitive inhibition of Na + and NH 4 + [19]. These results suggest that during salt stress, the N source influences N metabolism, including N uptake, assimilation and accumulation (total N, proteins and amino acids), and these effects varied in different species. P. simonii is widely distributed in the northern areas of China, and this plant has been recognized as an important afforestation species. In some areas, particularly the Loess Plateau, the soil typically suffers from salt stress [20]. In the present study, to understand the growth and N metabolism of P. simonii in response to different N sources (NO 3 or NH 4 + ) during moderate salt stress, we examined several morphological (root characteristics), physiological (e.g., photosynthesis, N metabolism enzyme activities, total N concentration and amino acid compounds) and molecular (transcript levels of representative genes involved in N metabolism) changes relevant for N metabolism in response to the N source under salt stress. Based on our previous study [5] and the ecological conditions of P. simonii, we proposed that NH 4 + -fed P. simonii is more susceptible to salt treatment compared to NO 3 --fed plants.

Materials and Methods
Plant growth conditions and treatments P. simonii cuttings (ca. 15 cm in length, 2 cm in diameter) were obtained from 2-year-old stems and rooted in pots (10 L) filled with fine sand. The cuttings were provided by a tree nursery (Yang Ling, Shannxi, China) and the P. simonii seedlings were collected within a privately owned forest area with permission given by local forest owners in March 2012. , with and without salt), six plants were cultivated. The plants were harvested at 13:00h at three time points (time point 0 was before the salt application and time points 2 and 3 were 1 and 2 weeks after the start of the salt treatment, respectively).

Measurement of growth parameters
The gas exchange of three mature leaves (leaf plastochron index = 8-10) was determined for each plant. The net photosynthetic rate was measured from 9:00 to 11:00 h using a portable photosynthesis system (Li-Cor-6400; Li-Cor, Inc., Lincoln, NE) with an attached LED light source (1000 μmol photon m -2 s -1 ). The CO 2 concentration in the chambers was 400 μmol mol -1 and the air flow was 500 μmol s -1 . The chlorophyll content of each plant selected was measured using a portable meter (Minolta SPAD 502 Meter). In addition, the height of the main shoot of each plant was measured using a ruler.
The harvested roots and leaves were wrapped in tinfoil and immediately frozen in liquid N. Subsequently, the samples were ground into a fine powder in liquid N using a mortar and pestle and stored at -80°C. The total root lengh, root surface and root volume of each plant were scanned and analyzed using a WinRHIZO root analyzer system (WinRHIZO version 2007b, Regent Instruments Canada, Montreal, Canada).
Determination of N uptake using the 15

N tracer method
Prior to harvesting, 3 seedlings of each treatment were treated in a solution containing either 15 15 N recovered in the roots could not be determined when both forms of inorganic N were present in the solution). The roots were rinsed for 10 min in solutions of 1 mM KCl to remove the enriched 15 N tracer solution that had adsorbed onto the surface of the roots. The roots were subsequently dried for 72 h at 80°C in an oven and homogenized using a mortar and pestle.
The samples were analyzed for 15 N using a Europa ANCA-SL elemental analyzer coupled to a GVI IsoPrime isotope ratio mass spectrometer (IRMS) at the Chinese Academy of Forestry. Continuous flow analysis was also used to determine the N content of each sample.

Determination of enzyme activities involved in N assimilation
The nitrate reductase (NR) activity in the tissues was assayed according to the method of Hogberg and Susan [22]. Approximately 0.5 g of the frozen material was ground into a fine powder in an ice bath. The powder was extracted in 4 ml of ice-cold extraction buffer containing 25 mM phosphate buffer (pH 7.5, a mixture of K 2 HPO 4 and KH 2 PO 4 ), 5 mM cysteine and 5 mM EDTA-Na 2 . The extract was centrifuged at 4,000 rpm for 15 min at 4°C, and 0.4 ml of enzyme extract was added to 1.6 ml of the assay mixture (1. remaining in the reaction mixture was determined at 540 nm after reaction with SA and NEDD as described above using a standard curve of known NaNO 2 concentrations. One unit of NiR activity is defined as 1 mM NO 2 reduced mg -1 protein h −1 . For the glutamine synthetase (GS) activity assay, the frozen tissues (approximately 1 g) were ground into 3 ml of 100 mM Tris-HCI (pH 7.6) extraction buffer containing 1 mM EDTA, 1 mM MgCl 2 Á6H 2 O and 10 mM 2-mercaptoethanol using an ice-cold mortar and pestle. The homogenate was clarified by centrifugation at 13,000 rpm for 25 min, and 1.2 ml of the crude enzyme extract was added to 1.6 ml of assay mixture containing 0.6 ml of imidazole-muriatic acid buffer (0.25 M, pH 7. 0), 0.4 ml of glutamic acid-Na (0.30 M, pH 7.0), 0.4 ml of ATP-Na (30 M, pH 7.0) and 0.2 ml of MgSO 4 (0.5 M). The mixture was incubated for 5 min at 25°C. Subsequently, 0.2 ml of hydroxylamine hydrochloride (a 1:1 mixture of 1 M hydroxylamine hydrochloride and 1 M HCl) was added, and the reaction was incubated for 15 min. The reaction was stopped after adding 0.8 ml of acidic FeCl 3 (2% (W/V) in TCA and 3.5% (W/V) FeCl 3 in 2% HCl). The samples were centrifuged at 4,000 rpm for 15 min, and the absorbance of the supernatant was measured at 540 nm. The amount of γglutamylhydroxamate formed was determined through a comparison with a standard curve that was generated after measuring authentic glutamylhydroxamate in the presence of all assay components. One unit of GS activity was determined as the amount of enzyme required to catalyze the formation of l μM γ-glutamylhydroxamate/min under the present conditions.
Glutamate synthase (GOGAT) activity was measured according to the methods of Singh and Srivastava [23]. The control and treated root and shoot samples (100 mg) were homogenized in 0.2 M sodium phosphate buffer (pH 7.5) containing 2 mM EDTA, 50 mM KCl, 0.1% (v/v) mercaptoethanol and 0.5% (v/v) Triton X-100. The homogenate was centrifuged (at 6,000 g) for 15 min at 4°C. The obtained supernatant was used to estimate the GOGAT activity. The reaction mixture (3 ml) included 25 mM sodium phosphate buffer (pH 7.3), which contained 1 mM EDTA, 20 mM l-glutamine, 5 mM 2-oxoglutarate, 100 mM KCl, 1 mM NADH and 0.3 ml of enzyme extract. The absorbance was read at 340 nm for 5 min.

Analysis of the transcript levels of representative genes involved in N assimilation
Based on previous studies [2,19,24,25], essential members of transporter families for NH 4 + (AMT1;2 and AMT1;6) and NO 3 -(NRT1;1, NRT2;4a) and genes encoding N assimilation (NR, NiR, GS1;3, GS2, Fd-GOGAT and NADH-GOGAT) were selected for the transcript analysis by quantitative RT-PCR (qPCR). Total RNA was isolated from the tissues and purified using a plant RNA extraction kit (R6827, Omega Bio-Tek, GA, USA), and trace genomic DNA was digested with DNase I (E1091, Omega Bio-Tek). Aliquots of 1 μg of total RNA were used for first-strand cDNA synthesis using the PrimeScript RT reagent kit (DRR037S, Takara, Dalian, China) in a 20-μl reaction according to the manufacturer's instructions. PCR was performed in a 20-μl reaction including 10 μl 2× SYBR Green Premix Ex Taq II, 2 μl of cDNA and 1 μl of 20 mM primers (S1 Table) using a LightCycler 96 System (Roche). Actin2/7 was used as a reference gene [26]. Three biological replicates, each with three technical replicates, were assayed for each sample. The reference gene was included on each plate. The efficiencies of all of the PCR reactions were between 95 and 105% (S1 Table).

Analysis of the amino acid compounds
Soluble amino acid compounds were extracted and analyzed as previously described [2,27]. Approximately 100 mg of the homogenized samples (fine roots, leaves) were incubated in 1 ml of methanol:chloroform (7:3, v/v) and 0.2 ml of HEPES buffer [5 mM ethylene glycol tetraacetic acid (EGTA), 20 mM HEPES, 10 mM NaF, pH 7.0]. The homogenates were incubated on ice for 30 min and subsequently extracted twice with 0.6 ml of distilled water. The aqueous phases were freeze-dried and dissolved in 1 ml of 0.2 M lithium citrate buffer (pH 2.2). The amino compounds were detected using an automated amino acid analyzer (L-8900, Hitachi High-Technologies Corporation, Japan).

Data processing and statistical analysis
All of the statistical tests were performed using SPSS software (version 20.0, SPSS Inc., Chicago, IL, USA). A three-way ANOVA was used to examine the effects of salt, N treatment and time on the experimental variables. The data were tested for normality prior to further analyses. Differences between the means were determined on the basis of least significant differences (P = 0.05).

Growth parameters
After 2 weeks of exposure to 75 mM NaCl, the plants exhibited growth inhibition (Table 1). Total root length and stem height were significantly reduced after salt treatment, but no effect of N nutrition was observed (Table 1). Total surface area, chlorophyll content and photosynthesis were also significantly reduced after salt treatment (from T0 until T2 in Table 1). The reductions of chlorophyll content and photosynthesis were much more affected by salt treatment in the NH 4 + -fed plants compared to the NO 3 --fed plants (Table 1).

Total N concentration and 15 N content in the roots and leaves
Salt treatment significantly increased the total N concentration in the roots of NH 4 + -fed plants, particularly after 2 weeks of salt application (Fig 1). In leaves, the increase in total N concentration after salt exposure was significant in the NH 4 + -fed plants but not in the NO 3 --fed plants after two weeks (Fig 1).The increase in total N concentration because of salt exposure in the leaves was significantly dependent on N nutrition. Similar to the total N concentration, the 15 N content in the roots and leaves was significantly increased by salt stress in the NH 4 + -fed plants but not in the NO 3 --fed plants (Fig 2). After 2 weeks of salt application, the 15 N content in roots was greater with NH 4 + compared to NO 3 - (Fig 2).

Enzymes for NO 3 utilization
Significantly higher NR activity was detected in both the roots and leaves of the NO 3 --fed plants compared to the plants that were fed with NH 4 + after two weeks of salt treatment (Fig 3). After 2  weeks of salt application, the average NR activity in the roots was 0.9 ± 0.1 μM NO 3 g -1 FW h -1 (in the control plants) and 0.94 ± 0.17 μM NO 3 g -1 FW h -1 (in the salt-treated plants) for the NH 4 + fed plants, and it was 1.53 ± 0.12μM NO 3 g -1 FW h -1 (in the control plants) and 1.33 ± 0.23 μM NO 3 g -1 FW h -1 (in the salt-treatment plants) for the NO 3 --fed plants (Fig 3). Salt treatment did not significantly decrease NR activity in the roots (Fig 3). Consistent differences in root NR activity were observed as a result of different N sources (NO 3 versus NH 4 + ); After 2 weeks of salt application, the average NR activity in the leaves was 0.99 ± 0.12 μM NO 3 g -1 FW h -1 (in the control plants) and 0.89 ± 0.10 μM NO 3 g -1 FW h -1 (in the salt-treatment plants) for the NH 4 + -fed plants, and it was 1.76 ± 0.12 μM NO 3 g -1 FW h -1 (in the control plants) and 1.54 ± 0.11 μM NO 3 g -1 FW h -1 (in the salt-treated plants) for the NO 3 --fed plants (Fig 3). The decrease in foliar NR activity because of salt stress was significant in the NO 3 --fed plants but not in the NH 4 + -fed plants after 2 weeks (Fig 3).
Similar to the NR activity, the NiR activity in the roots and leaves was significantly higher in the NO 3 --fed plants than in the NH 4 + -fed plants (Fig 3). Salt stress had no effect on the NiR activity in the roots and leaves (Fig 3). Enzymes for NH 4 + utilization The GS activity was significantly decreased upon salt stress in both the roots and leaves, and the amplitude of this effect was dependent on N nutrition (Fig 4). Two weeks of salt treatment resulted in a 75% (in roots) and 65% (in leaves) reduction in GS activity in the NH 4 + -fed plants, whereas a 52% (in roots) and 46% (in leaves) reduction was observed in the NO 3 --fed plants (Fig 4). Salt stress led to a continuous decrease in GOGAT activity in the roots of both the NH 4 + and NO 3 --fed plants during the 2 weeks of salt exposure (Fig 4). This reduction was higher in the NH 4 + -fed plants than in the NO 3 --fed plants (Fig 4). However, no changes in GOGAT activity were observed in the leaves after salt exposure (Fig 4).

Transcriptional regulation of the genes involved in N uptake and metabolism
In the NH 4 + -fed plants, the AMT1;2 and AMT1;6 transcripts were higher in both the roots and leaves (with the exception of AMT1;2 in leaves which was specifically expressed in roots) under salt exposure compared to the controls that were not exposed to salt (Fig 5). However, the AMT1;2 and AMT1;6 transcript levels did not change as a result of salt treatment when NO 3 was supplied as the N source (Fig 5). The NRT1;1 and NRT2;4a transcripts in the roots and leaves were higher in the NH 4 + -fed plants than in the NO 3 --fed plants (Fig 5). In both the roots and leaves, salt stress suppressed the transcript levels of NRT2;4a, whereas no effects on NRT1;1 expression were observed (Fig 5).
Higher NR and NiR transcript levels were detected in the roots and leaves of the plants fed with NO 3 than in the plants fed with NH 4 + (Fig 5). Salt stress did not affect the NR and NiR transcript levels in the NO 3 and NH 4 + -fed plants (Fig 5).
Substantially lower GS1;3 and GS2transcript levels in the roots and leaves were observed in the salt-treated plants compared to the controls that were not exposed to salt (except in the leaves of the NO 3 --fed plants) (Fig 5). Similarly, salt stress resulted in a significant decrease of the Fd-GOGAT and NADH-GOGAT transcript levels in both the NO 3 --and NH 4 + -fed plants ( Fig 5). The genes involved in NH 4 + assimilation (GS1;3, GS2, Fd-GOGAT and NADH-GO-GAT) were generally not affected by the N source (except GS2 in both the roots and leaves of the control plants).

Analysis of the amino compounds in the fine roots and leaves
The salt treatment also changed the composition of the amino compounds depending on the N source (Fig 6 and S2 Table). In the roots of the salt-stressed plants grown with NH 4 + , the increment of total amino compounds primarily reflected an increase in aspartate-, glutamateand valine-derived amino compounds (Fig 6A). The main components of the aspartate, glutamate and valine groups were asparagine, glutamine and valine, respectively. Changes in the distribution of the amino compounds were different from the changes in the absolute amounts of amino compound groups. In the roots of the plants grown with NH 4 + , the proportions of aspartate (from 24 to 26%), glutamate (from 36 to 39%) and valine (from 13 to 16%) did not significantly change under salt stress (Fig 6A). In the roots of the salt-stressed plants grown with NO 3 -, the increase in total amino compounds primarily reflected an increase in aspartateand glutamate-derived amino compounds (Fig 6A). In the roots of the plants grown with NO 3 -, the proportion of the glutamate group increased under salt stress (from 37 to 45%), but the proportion of the serine group decreased (from 21 to 12%), whereas the proportions of the other groups did not change (Fig 6A).
In the leaves of the salt-stressed plants, all groups of amino compounds increased upon salt stress, independent of the N source. The amino acids derived from serine were increased in the NH 4 + -(six-fold) and NO 3 --fed plants (four-fold), resulting in an increased contribution to total amino compounds (21 to 41% in the NH 4 + -fed plants and from 22 to 35% in the NO 3 -fed plants) (Fig 6B). The main component of the serine group was serine. Amino acids derived from glutamate in both the NH 4 + -and NO 3 --fed plants also significantly increased (approximately 2.5-fold) as a result of the salt stress, and the relative proportion of this group of amino Nitrogen Metabolism of Populus simonii under Salt Stress compounds slightly decreased (from 45 to 36% in NH 4 + -fed plants and from 48 to 44% in NO 3 --fed plants) (Fig 6B). Glutamate was the most abundant amino compound in this group.
The absolute amount of glutamate in the leaves of both the NH 4 + and NO 3 --fed plants increased 2-fold upon salt stress. The absolute amount of proline, which also belongs to the glutamate group, increased in the NH 4 + -fed plants but did not change in the NO 3 --fed plants in response to salt stress (Fig 6B). The total amount of the aspartate group increased in response to salt stress, but the relative proportion of this group of amino compounds decreased (from 20 to 12% in both the NH 4 + -and NO 3 --fed plants) (Fig 6B). The amino compounds of the tyrosine and valine groups increased two-to three-fold as a result of salt stress, independent of the N source, whereas the relative proportions of the two groups did not change (Fig 6B).

Discussion
Salinity has detrimental effects on plant growth and development, such as reduced root length and changed leaf substructure [28,29]. The effects of salt stress on plant growth in P. simonii included decreased total root surface area, total volume and photosynthesis inhibition; these effects were dependent on the N source (Table 1). In the present study, the application of salt stress reduced chlorophyll content and net photosynthetic rate more intensively in the NH 4 + -fed plants. These results indicate that P. simonii performs better under salt stress when fed with NO 3 -.  The 15 N uptake and soluble protein in plant materials increased in both the roots and leaves of the NH 4 + -fed plants in response to salt stress. However, increases in N uptake and soluble protein were not observed in the NO 3 fed plants. These results indicate enhanced NH 4 + uptake during salt treatment; similar results were also reported in the roots of Picea glauca [5,30]. These changes might reflect cation exchange because NH 4 + application could lower the uptake of cations in plant tissues compared to NO 3 --treated plants [9]. In addition, NH 4 + uptake has a lower energy requirement for assimilation in the roots, and the increased NH 4 + concentration could enhance osmotic resistance in rice plants because of aquaporin expression [31]. The accumulation of soluble protein under osmotic resistance has been reported in many species [32][33][34]. The increased soluble protein might reflect a decrease in amino export [35], the mobilization of storage proteins in tissues [36] and the decomposition and/or the synthesis inhibition of non-soluble proteins. These hypotheses were not investigated in the present study and require further examination. During assimilation, NO 3 is converted to NH 4 + by NR and NiR [37]. NH 4 + can be assimilated to glutamine by GS and GOGAT [38,39]. Distinct NO 3 assimilation has been reported in different species or genotypes in response to salt stress. For instance, previous studies have demonstrated that salt stress decreased NR activity in Brugueira parviflora [1], rice (Oryza sativa L.) [40] and maize (Zea mays L.) [41], whereas in gray poplar (Populus tremula× alba), NO 3 assimilation was not influenced [2]. In the present study, salt stress had only minor effects on NR and NiR activity while the substrate concentration (NO 3 supply) influences NR and NiR activity in P. simonii. GS and GOGAT activitywas much lower in the salt-treated plants (except foliar GOGAT activity) compared to the control plants. We suspect that this effect might have two potential explanations: salt stress causes a direct reduction of NH 4 + uptake in the roots in response to the salt stress; and salt stress causes a reduction of NH 4 + production from photorespiration. Na + and Claccumulation to toxic levels in rice harmed the chloroplast, influenced photorespiration process, and reduced NH 4 + production from photorespiration, which immediately down-regulated the OsGS2 and OsFd-GOGAT and weakened the GS/GOGAT pathway [8]. However, NH 4 + uptake was not reduced by salt stress. Our results support the second hypothesis. As an indicator of N uptake and assimilation, the transcript levels of representative genes involved in N uptake and assimilation were analyzed. Several studies have shown that the transcripts of some NH 4 + 3 transport and also functions as a NO 3 sensor to activate the expression of NO 3 --related genes in plants [24,44]. NRT2;4a also plays an important role in NO 3 --uptake, particularly under low N conditions. The high levels of NRT1;1 and NRT2;4a transporters in the NH 4 + -fed plants suggest that P. simonii might be sensitive to NO 3 --deficiency. The mRNA level of the NR and NiR transcripts was not affected under salt stress and was primarily regulated by the substrate concentration (NO 3 -), consistent with NR and NiR enzyme activities. However, the transcripts of the genes involved in NH 4 + assimilation were generally decreased in response to salt stress. The down-regulation of the genes involved in NH 4 + assimilation (GS1.3, GS2, NADH-GOGAT and Fd-GOGAT) might be a harmful response to NaCl toxicity. P. simonii might accumulate Na + and Clto toxic levels under salt stress, and this effect might reduce NH 4 + production from photorespiration, which immediately down-regulates the genes involved in NH 4 + assimilation.
The accumulation of amino acid compounds playing an important role in osmoregulation in response to salt stress has been reported in many plants [24,[32][33][34]45]. The amino compounds were more reactive to salt stress in the NH 4 + -fed plants compared to the NO 3 --fed plants. Significant increases in response to salt stress were observed in the serine and glutamate biosynthesis groups. Cysteine (its precursor is serine), glutamate and glycine are important for the synthesis of glutathione (GSH). GSH is important for the stress resistance of plants through the elimination of free radicals. Thus, significant increases of the serine and glutamate biosynthetic groups in response to salt stress might be associated with GSH synthesis. Additionally, aspartate and glutamine were used for the storage and/or transport of N from source to sink tissue [2], indicating intensive N allocation in salt-treated plants.
In summary, salt stress decreased the root development and photosynthesis of P. simonii, depending on the N source. NH 4 + uptake was enhanced, whereas NH 4 + assimilation was decreased in response to salt stress. NO 3 metabolism was less affected under salt treatment.
The accumulation of amino acid compounds indicates an adaption in response to salt stress. Soils on the Loess Plateau in Northwest China are alkaline, and low levels of N are available. NH 4 + levels are particularly low, making NO 3 the most available form of N in this region.
Thus, P. simonii growing in these regions exhibits different N uptake and assimilation strategies during salt stress, depending on the N source.
Supporting Information S1 Table. Specific primers for key genes involved in N uptake and assimilationin P.simonii. (XLSX) S2 Table. 17 Amino compounds in roots and leaves of P.simonii as affected by salt treatment and nitrogen nutrition.
(XLSX) S3 Table. Total N concentration, activities of nitrate reductase, nitrite reductase, glutamine synthetase and glutamate synthase in roots and leaves of P.simonii as affected by salt treatment and nitrogen nutrition.
S4 Table. Transcriptional fold-changes of key genes involved in N uptake and assimilation in roots and leaves of P.simonii as affected by salt treatment and nitrogen nutrition. (XLSX)