- Research article
- Open Access
Tomato root transcriptome response to a nitrogen-enriched soil patch
© Ruzicka et al; licensee BioMed Central Ltd. 2010
Received: 3 February 2010
Accepted: 27 April 2010
Published: 27 April 2010
Nitrogen (N), the primary limiting factor for plant growth and yield in agriculture, has a patchy distribution in soils due to fertilizer application or decomposing organic matter. Studies in solution culture over-simplify the complex soil environment where microbial competition and spatial and temporal heterogeneity challenge roots' ability to acquire adequate amounts of nutrients required for plant growth. In this study, various ammonium treatments (as 15N) were applied to a discrete volume of soil containing tomato (Solanum lycopersicum) roots to simulate encounters with a localized enriched patch of soil. Transcriptome analysis was used to identify genes differentially expressed in roots 53 hrs after treatment.
The ammonium treatments resulted in significantly higher concentrations of both ammonium and nitrate in the patch soil. The plant roots and shoots exhibited increased levels of 15N over time, indicating a sustained response to the enriched environment. Root transcriptome analysis identified 585 genes differentially regulated 53 hrs after the treatments. Nitrogen metabolism and cell growth genes were induced by the high ammonium (65 μg NH4+-N g-1 soil), while stress response genes were repressed. The complex regulation of specific transporters following the ammonium pulse reflects a simultaneous and synergistic response to rapidly changing concentrations of both forms of inorganic N in the soil patch. Transcriptional analysis of the phosphate transporters demonstrates cross-talk between N and phosphate uptake pathways and suggests that roots increase phosphate uptake via the arbuscular mycorrhizal symbiosis in response to N.
This work enhances our understanding of root function by providing a snapshot of the response of the tomato root transcriptome to a pulse of ammonium in a complex soil environment. This response includes an important role for the mycorrhizal symbiosis in the utilization of an N patch.
Nitrogen (N) is often a primary limiting factor for plant growth and yield in agriculture. Applications of N in conventional agriculture include fertilizer banding to the side of the plants, broadcasting on the surface of soil, and anhydrous ammonia injections. These N application methods as well as localized microbial turnover of organic N can result in spatial and temporal heterogeneity (patchiness) of soil N resulting in non-uniform availability to plant roots. Furthermore, the rapid immobilization and nitrification of N additions by soil microbes can quickly alter N availability to the root [1–3]. Roots respond to localized nutrient patches by up-regulating ion transporters and by the proliferation of new roots into the patch to capture the additional N [4–6]. Mycorrhizal fungi provide plants with an additional mechanism to explore the soil and capture nutrients from enriched regions, increasing nutrient uptake potential [7, 8].
Plant roots predominantly acquire N from the rhizosphere as inorganic ammonium (NH4+) or nitrate (NO3-), and subsequently assimilate intracellular NH4+ into amino acids [9, 10]. Roots sense and respond to changes in internal and external N status, which includes the regulation of gene expression, metabolism, and further N uptake and assimilation [11, 12]. High and low affinity N transport systems in roots allow plants to maximize uptake depending on soil N availability. High affinity transport systems are induced or activated under conditions where soil N availability is reduced (1 μM to 0.5 mM), while low affinity transport systems (active above ~0.5 mM N) may be constitutively expressed and transport N into the plant when soil N concentrations are high . Members of the NH4+ transporter (AMT) gene family  transport NH4+ across the plasma membrane of root epidermal cells where it may be locally assimilated . Intracellular NH4+ is assimilated into glutamine and glutamate via the N-regulated glutamine synthetase (GS) and glutamate synthase (GOGAT) enzymes . The NO3- transporters (NRT) are also encoded by a large gene family . The NO3- taken up by roots can be translocated to the shoot or reduced in roots to nitrite (NO2-) and then NH4+ via N-regulated NO3- reductase and NO2- reductase [13, 16]. Both AMTs and NRTs exhibit complex gene regulation patterns in response to various forms and concentrations of N. These transporters are regulated by internal and external N and provide roots with a mechanism to mount a coordinated response that may serve to increase N acquisition and metabolism [11, 18, 19].
Recent studies have moved beyond examining expression changes of single genes or gene families to studying global changes in plant gene regulation by nutrients [19–22]. Microarray analyses of Arabidopsis and tomato roots subjected to increased NO3- identified hundreds of differentially regulated genes whose functions included N metabolism, cell growth, and transcription [19, 21]. However, most genomics studies on plant nutrient metabolism have utilized hydroponic-grown non-mycorrhizal plants, potentially limiting their translatability to our understanding of roots response in soil where nutrients are not distributed uniformly and inorganic N is being transformed. In this report we used molecular tools to study root response to the application of known concentrations of NH4+ in a well defined region of the soil. Our aim was to characterize how roots respond to a nutrient patch in natural soils where complex ecological processes are occurring including mycorrhizal colonization and the microbial transformation of NH4+ to NO3-. This approach is in contrast to previous studies [19–22] that have used hydroponics to study responses to NH4+ or NO3- singly rather than a dynamic situation which is more relevant to agriculture or natural ecosystems where NH4+ is rapidly transformed to NO3-. We report on 15N uptake and translocation and the coordinated changes in gene expression patterns in mycorrhizal roots following a localized pulse of NH4+ as NO3- gradually became more available.
Soil N, plant status, and plant N uptake
The NH4+ treatments increased the soil inorganic N concentrations in the patch soil, simulating heterogeneous soil patches. In the high NH4+ treatment group, the highest soil NH4+ concentration (39.7 μg NH4+-N g-1 dry soil) was measured at the time of the first sampling which was 5 hrs after injection. At 53 hrs after treatment it remained significantly higher than controls (25.3 μg NH4+-N g-1 dry soil) (Fig 1b), and by 96 hrs, decreased to 3.5 μg NH4+-N g-1 dry soil due to microbial transformations and/or plant uptake of the added NH4+. In the high NH4+ treatment rings, soil NO3- concentrations were above ambient levels within 29 hours, indicating nitrification of NH4+ (Figure 1c). Patch soil NO3- concentrations increased over the first 53 hrs after injection of the high NH4+ treatment. In the low NH4+ treatment, soil NH4+ and NO3- concentrations were similar to the water controls.
Over the course of the experiment, plant shoot growth was unaffected by treatment (P = 0.78). Percent total N (mean ± SE) in the shoots was 2.29% ± 0.08 at the time of treatment and unaffected by the N treatments (P = 0.85). Percent phosphate (P) (mean ± SE) in the shoots was 0.18% ± 0.002 and was unaffected by the N treatments. Roots were significantly colonized by arbuscular mycorrhizal fungi as measured by microscopic counting (33.5% ± 8.4, mean ± SE) and fungal transcript analysis (data not shown).
To test whether the NH4+ treatments resulted in measurable 15N uptake and translocation, atom percent 15N was assayed in roots and leaves (Figure 1d and 1e). Within 29 hrs, patch roots and leaves from high NH4+ plants contained increased amounts of 15N compared to naturally occurring 15N levels in the water control. The amount of 15N in these tissues continued to increase over time. In the patch roots from the low NH4+ treatment, atom % 15N was not higher compared to the water controls until 53 hrs after injection, and there was no significant enrichment detected in leaves of the low NH4+ treatments at any time point. There were significantly higher concentrations of 15N in the high NH4+ treatment roots and leaves compared to the low NH4+ treatment samples at multiple time points, further confirming a physiological difference between these treatments.
Microarray analysis of patch root transcription
We annotated and categorized nearly 80% of the 585 differentially regulated genes into putative functional classes. The NH4+ treatments resulted in the differential regulation of genes in a wide range of functional categories (Figure 2b). In every functional category, the high NH4+ vs. water comparison contained a significantly higher number of genes compared to the low NH4+ vs. water comparison, further indicating that the high NH4+ treatment resulted in a larger scale transcriptional response. Fisher's exact test was used to determine whether the gene lists from the [high NH4+ vs. water] or [low NH4+ vs. water] comparisons were enriched for different functional categories compared to one another, indicating a unique type of response to the two NH4+ treatments. Significantly more cell growth and division genes were identified in the high NH4+ vs. water comparison (29 out of 535, 5.4%) than the low NH4+ vs. water comparison (0 out of 89, 0%) (P = 0.0245). Conversely, significantly more signal transduction genes were identified in the low NH4+ vs. water comparison (15 out of 89, 16.9%) than the high NH4+ vs. water comparison (45 out of 535, 8.4%) (P = 0.0187).
A significant proportion (39 out of 89, 43.8%) of the genes in the low NH4+ vs. water comparison were similarly regulated in the high NH4+ vs. water comparison (Additional file 2), and included N assimilation and metabolism genes such as glutamine synthetase and tryptophan synthase. Eight of the remaining 50 (16%) genes uniquely identified only in the low NH4+ vs. water comparison function in sugar metabolism including glucosyl hydrolase, trehalose 6-phosphate synthase, low affinity sucrose transporter SUT4, isocitrate lyase, and glucose 6-phosphate translocator.
Identification of genes regulated among the N treatments
Differentially regulated nitrogen assimilation and metabolism genes.
Probe Set ID
(High N vs. water)
(Low N vs. water)
nitrate transporter 2.1
NADH-dependent glutamate synthase
chorismate synthase 2
peptide transporter 1
ammonium tranporter 1
g-aminobutyrate transaminase subunit precursor
homogentisate 1,2-dioxygenase HGO
cystathionine beta-synthase domain protein
alpha-aminoadipic semialdehyde synthase
ANR1-like MADS-box transcription factor
Differentially regulated cell growth and division genes.
Probe Set ID
(High N vs. water)
cdc20 cell cycle regulator
B2-type cyclin dependent kinase
replicon protein A
mitotic arrest deficient-like
histone H4 replacement isoform
minichromosome maintenance protein
nucleosome chromatin assembly factor
histone H4 replacement isoform
nucleosome chromatin assembly factor
microtubule associated protein
ER auxin binding protein 1
Differentially regulated cell wall metabolism genes.
Probe Set ID
(High N vs. water)
(Low N vs. water)
cell wall-plasma membrane linker
cellulose synthase isomer
cobra-like4 phytocheletin synthase
chitinase class IV
endo-xyloglucan transferase A2-like
Differentially regulated stress and defense response genes.
Probe Set ID
(High N vs. water)
(Low N vs. water)
TAS14 peptide dehydrin
type I small heat shock protein
pathogen responsive alpha-dioxygenase 2
pathogenesis-related chitin-binding protein
pathogenesis related PR5-like protein
early responsive to dehydration 7-like
responsive to dehydration 22-like
pathogenesis-related protein 1 like
universal stress protein
pathogenesis related protein 1-like
stress enhanced protein 2-like
rare cold inducible protein-like
universal stress protein
responsive to dehydration 22-like
thaumatin-like pathogenesis-related PR-5 like protein
early responsive to dehydration 3-like
heat shock factor binding protein 1
heat shock protein
dnaJ related molecular chaperone
dnaJ homologue 3
heat shock protein
dnaJ heat shock protein
cold-regulated plasma membrane 1 protein
dehydration response element B1A
response to desiccation 26-like transcription factor
The NH4+ treatments caused various transcriptional responses in multiple stress and defense-response genes, and genes in this functional category were some of the most differentially regulated genes of the experiment (Table 4). Genes in certain stress and defense response subcategories exhibited similar transcriptional responses including glutathione metabolism genes (6 out of 7 higher expression in water samples), pathogen response factors (5 out of 6 higher expression in water samples), and heat shock proteins (6 out of 7 higher expression in high NH4+ samples).
Previous studies have reported the transcriptional regulation of genes in diverse functional groups including metabolism, energy, cell growth, and transcription/translation in response to N nutrition as NO3- or NH4+ [19–22]. However, these have utilized hydroponics systems that do not necessarily reflect the rhizosphere environment encountered by plant roots in agricultural and natural ecosystems. Roots grown in solution culture systems do not compete with soil microbes for nutrients, and the concentrations of nutrients in solution are more uniform both spatially and temporally. Fertilizer application and soil processes in conventional and organic farming result in the formation of heterogeneous soil nutrient patches , and plant utilization of N patches depends on roots rapidly sensing and response to the local enrichment of nutrients where they are in competition with soil microbial N assimilation and nitrification, leaching, and denitrification [2, 3, 27, 28].
To better understand plant root response to a localized and dynamic inorganic N soil patch, we utilized an experimental design that simulated a more realistic patch environment. The buried ring created the spatial attributes of an N patch by ensuring that harvested roots were localized to the NH4+ treatment patch. Measurements of soil NH4+ and NO3- levels confirmed dynamic soil transformations of available N by 53 hrs when we sampled the roots for microarray analysis. After 96 hrs, we observed a trend of decreasing NH4+ and NO3- soil levels, indicating plant and microbial uptake of both NH4+ and NO3- [1, 9]. Furthermore, estimates of the % recovery of applied 15N in shoots from high and low NH4+ treatment groups after 96 hrs (22% and 21%, respectively) support the assertion that roots faced significant competition for N in the soil environment.
The rapid N uptake observed in this study demonstrates the ability of tomato roots to quickly capture fertilizer in soil patches [29, 30]. The roots that encountered the high NH4+ treatment took up and translocated significantly more 15N from the patch than the low NH4+ treatment roots. This observation is in agreement with the larger transcriptional response to the high NH4+ treatment including multiple nitrogen transport, assimilation, and metabolism genes. However, the relatively low % recovery suggests that actual uptake and assimilation are only a small fraction of what was initially available despite the rapid root responses.
The genes coordinately regulated in both high and low treatments may represent a conserved physiological response to different ranges of N patch conditions. The co-regulated list of genes did not include the NH4+ or NO3- transporters AMT1, AMT2, or NRT2.1 identified in the high NH4+ vs. water control comparison. We speculate that roots in the high NH4+ patch needed additional transporters to effectively capture the higher soil N levels, while constitutively expressed transporters were sufficient in the low NH4+ patch. Of equal interest, however, is the set of 50 genes regulated by the low NH4+ treatment that were not similarly regulated by the high NH4+ treatment. This group of genes included a significant number of sugar metabolism genes for which we have no clear explanation as to the functional significance for the change in regulation. One possibility is that sugar metabolism may have been required for the production of root exudates, which can increase plant growth promoting rhizobacteria, or stimulate N cycling by microbial populations in the rhizosphere . While the total number of genes regulated by the two treatments suggests that the high NH4+ treatment caused a larger response, the responses were in part unique, and may reflect different strategies to effectively utilize the N patch. Increased N availability stimulates highly regulated root development and growth in order to efficiently scavenge and assimilate the additional soil N [32, 33]. The induction of multiple histone gene family members such as histones H4, H3 and H2AX in the high NH4+ treatment suggests an increase in DNA replication [34, 35], while the increased expression of a mitotic spindle checkpoint gene, replicon protein A, multiple cyclin genes, and a putative cdc20 suggest an increase in cell division processes [36, 37]. Furthermore, the induction of cell wall genes including expansins, pectinesterases, and cellulose synthase suggests an increase in cell wall biosynthesis that would be required during root growth . In Arabidopsis, multiple expansins and other cell wall modification enzymes were up-regulated by NO3- 3 hrs post-treatment , and gene expression profiling of maize roots in early response to a NO3- treatment identified multiple genes involved in cell growth and lateral root elongation including alpha-expansin, kinesin, and cellulose synthase . These experiments imply that similar N developmental response mechanisms are conserved across maize, Arabidopsis, and tomato roots, and that the root response to an N nutrient patch includes coordinated root growth.
In this study, diverse stress response genes encoding heat-shock proteins, glutathione transferases, thioredoxin, pathogenesis-related proteins, and dehydration/desiccation responsive proteins were found to be differentially expressed among the NH4+ treatment groups. Limiting nutrient conditions cause various stress-related responses including the up-regulation of reactive oxygen species metabolism . Chronic N stress induces a range of plant stress responses which include the transcriptional regulation of numerous stress responsive genes. In Arabidopsis ~35% of the genes upregulated by a severe chronic N limitation stress were classified as response to abiotic stimulus, general stress, or oxidative stress . Studies of N effects on the expression of stress response genes in rice also indicate that N limiting conditions cause the differential regulation of biotic and abiotic stress genes . From their studies, Lian et al. postulate that this could be due to the perception of N limitation as a biotic or abiotic stress that requires a conserved set of regulated genes that play protective roles . Our results suggest that the conditions in the water control samples may have initiated a stress response in roots due to an N limitation, and that the high and low NH4+ treatments alleviated this coordinated stress response.
The complex regulation of specific NH4+ and NO3- transporters following the NH4+ pulse may reflect a simultaneous and synergistic response to both NH4+ and NO3- in the soil patch. Both Arabidopsis AtAMT1.1 and tomato LeAMT1 exhibit increased transcript levels during N deprivation and are repressed by NO3- and NH4+ [43–45]. The higher expression of LeAMT1 under control conditions and its repression by high NH4+ in the present study further support the idea that LeAMT1 is a high affinity ammonium transporter whose expression is regulated by N-limiting conditions to increase NH4+ uptake. In two hydroponics studies, LeAMT2 was induced by increased concentrations of NH4+ over the course of 24 hrs but repressed by increased concentrations of NO3- after 24 hrs [19, 44]. The higher expression of LeAMT2 in response to the soil N patch 53 hrs after treatment in this current study suggests that the positive effects of NH4+ may be stronger than the long-term repressive effects of NO3- exposure. Arabidopsis, barley and tomato NO3- transporters AtNRT2.1, HvNRT2, and LeNRT2.1 were induced by NO3- in hydroponic culture, and NH4+ repressed HvNRT2 expression [13, 19]. We report that LeNRT2.1 was induced in the high NH4+ treatment where we measured increased NO3- concentrations. The increased NO3- in the patch may have induced LeNRT2.1, although the effects of NH4+ alone in the absence of NO3- on LeNRT2.1 remain to be tested. The complex regulation of the NH4+ and NO3- transporters in this study indicate that tomato roots are able to quickly sense and respond to changing concentrations of NH4+ and NO3- simultaneously in a localized N patch, enhancing N uptake and utilization. Moreover, growth is known to increase with co-provision of NH4+ and NO3- . Recent studies have also reported root responses to soil glutamate that may have been available to patch roots . This study highlights the ability of plant roots to simultaneously regulate multiple transporters for uptake of both forms of inorganic N as part of a plastic response strategy to quickly exploit the N pulse.
Numerous transcription factors were identified in the microarray study that may function as key regulators of a secondary response to the N enrichment. The tomato MADS-box transcription factor BT013126 shares 67% amino acid sequence similarity with Arabidopsis ANR1 and is expressed 3.26-fold higher in the water control compared to the high NH4+ treatment (Table 1). Arabidopsis ANR1 is a key regulator of the developmental response to N in roots and is induced by N starvation and repressed by NO3- re-supply [47, 48]. Prior to the N additions, the plants were most likely N-limited as the shoot N concentration was below sufficiency levels (mean = 1.94% for water control) . The expression pattern of this tomato ANR1-like gene in N patch roots corresponds to what was found in Arabidopsis, suggesting that its functional role to regulate root development in response to N is conserved across species and in diverse root environments.
Root responses to macronutrients N, P, potassium (K), and sulfur (S) are interconnected and may be due to the increased availability of one causing an imbalance in another. Previous studies have shown N addition to increase the expression level of S metabolism genes [21, 50], which could account for the changes in S metabolism genes reported here (Additional file 1). Alternatively, these genes may have been affected by sulfate in the NH4+ treatment, although soil S concentrations were likely sufficient for the plant. Cross talk between K and N has also been shown where K deficiency alters the transcriptional and post-transcriptional activity of various N uptake, assimilation, and metabolism genes including three nitrate transporters [51, 52]. Nitrogen and phosphate metabolism have been shown to be closely linked where N uptake results in coordinated P uptake [53, 54]. However, in response to a 3 hr nitrate pulse, phosphate transporter expression levels in hydroponics-grown Arabidopsis did not change . In soils, mineral availability and acquisition is additionally affected by the mycorrhizal symbiosis, and previous work has linked the up-regulation of the fungal phosphate transporter GiPT to the presence of N . In this current study, multiple phosphate transporters were regulated by the NH4+ treatments, in contrast to the Arabidopsis findings . We observed that mycorrhizal-induced PT3 and mycorrhizal-specific PT4 were more highly expressed when more NH4+ was present in the soil. The PT3 and PT4 expression patterns suggest that arbuscular mycorrhizal Pi uptake may be enhanced by NH4+ soil enrichment. Phosphate transporters PT1 and PT2 are found in both mycorrhizal and nonmycorrhizal root tissues, but are repressed in mycorrhizal roots [56–58]. The repression of PT1 and PT2 in the NH4+ treatments in the present study further supports the conclusion that the NH4+ treatments promoted the symbiotic Pi uptake pathway. In fact, Wang et al. reported that tomato PT2 was induced by NO3- in hydroponic-grown non-mycorrhizal roots , and thus it appears that PT2 regulation in the current study was in response to up-regulation of the mycorrhizal Pi uptake pathway rather than soil NO3- directly. We can speculate that the NH4+ soil enrichment induced root growth in the nutrient patch, resulting in a localized P deficiency that promoted the mycorrhizal Pi uptake pathway. Importantly, the lower expression level of phosphate-starvation induced TPSI1 in the low and high NH4+ treatment plants suggests that these roots were receiving more Pi than the water control samples , although this was not measured directly. This shift towards the mycorrhizal Pi uptake pathway may have resulted in increased Pi uptake, possibly as a mechanism to support N-induced growth. Our results detail a novel and complex interaction between inorganic N, the arbuscular mycorrhizal symbiosis, and the tomato phosphate transporter gene family, and suggest an important role for the symbiosis in the utilization of an N patch to increase P uptake and maintain N-induced growth.
Spatially discrete NH4+ is quickly transformed in the soil and taken up by plants, and the tomato root transcriptome reflects levels of N availability and transformations of N that occur in the soil. The dynamic regulation of both NH4+ and NO3- transporters in N-patch roots demonstrates that roots are able to simultaneously sense and respond to both forms of inorganic N, in ways that are likely to increase root competition with microbial immobilization, nitrification, and denitrification, and conserve N within cropping systems. The arbuscular mycorrhizal symbiosis may further increase the effective recovery of other nutrients such as P in an N patch. The strong and diverse transcriptional response to the soil N patch illustrates the utility of applying transcriptomic studies to plants growing in realistic soil environments and the key genes co-regulated under high and low N conditions in this study may serve as molecular tools for monitoring plant N status in agricultural sites for finer tuning of fertilizer application, soil microbial N processes, and ultimately, to develop more efficient agriculture methods.
Soil and plant material
Seeds of Solanum lycopersicum L. Cv. 76R  were surface sterilized, germinated with mist irrigation and then watered with one-tenth strength Long Ashton's solution containing N as (NH4)2SO4 (4 mM) and NaNO3 (8 mM). Plants were maintained under day/night length of 16/8 hr in UC Davis glasshouses. Seven week old seedlings were transplanted into 12-L pots containing buried rings with field-collected soil (Zamora loam, a fine silty, mixed thermic, Mollic Haploxeralfs) collected on an organically managed farm (Jim and Deborah Durst Farming in Esparto, Yolo County, California) . The buried soil root in-growth cores (rings) were 7.3 cm in diameter and 4.2 cm tall (total volume 176 cm3) and were filled with 210 g of field soil to a final bulk density equal to that of the surrounding soil (1.2 g cm-3). The broad ends of the ring were covered with 1 mm plastic mesh to easily allow roots to grow up and down into the ring. The soil was passed through a 1 cm sieve before packing into pots at a bulk density of 1.2 g cm-3. Extractable inorganic N (mean ± standard error) was 0.20 ± 0.02 μg NH4+-N g-1 dry soil and 9.7 ± 1.09 μg NO3-N g-1 dry soil at the time the rings were prepared. An application of one tenth strength Long Ashton's solution was applied two weeks after transplanting. Soil moisture was maintained gravimetrically at 19% before and after treatment injection by weighing the pots daily, and watering to compensate for evapotranspiration water loss.
We applied the nutrient treatments five weeks after transplantation by injecting 9 aliquots of 2 mL solution inside the buried ring using a template placed on the soil surface to assure an even distribution of nutrients and minimal loss of the solution. We added 6.5 μg and 65 μg 15NH4+-N (99 atom percent) g-1 dry soil in the ring for the low and high NH4+ treatments, respectively (1.35 mg 15NH4+-N per ring and 13.5 mg 15NH4+-N per ring, respectively). Water was used as a control. Each treatment consisted of three biological replicates, and plants were destructively harvested at 5, 29, 53, and 96 hrs after 15NH4+-N addition, for a total number of 36 plants in an unreplicated block design. The transcriptome analyses were performed on roots harvested at 53 hrs post-treatment.
Harvest and sample analysis
At harvest, shoots were severed at the soil surface, dried at 60°C, weighed, and ground to a fine powder for isotope analyses. Immediately following the harvest of the aboveground biomass, the root in-growth rings were carefully exposed, and the roots growing into and out of the ring were severed. Patch roots for transcriptome analysis were rinsed and immediately frozen in liquid nitrogen. A homogenous sub-sample of the patch soil and the surrounding pot soil was immediately removed for gravimetric water content and soil inorganic N concentrations. Soil NH4+ and NO3- were analyzed after KCl extractions and colorimetric determination using modifications of Miranda et al.,  and Foster et al.,  respectively. A small subsample of ring roots was scored for arbuscular mycorrhizal fungi at 200× . The remaining patch roots were washed by wet sieving, dried at 60°C, weighed, and ground to a fine powder for isotope analyses. All dried plant material was analyzed for δ15N on a PDZ Europa ANCA-GSL elemental analyzer and a PDZ Europa 20-20 isotope ratio mass spectrometer (Sercon Ltd., Cheshire, UK) at the UC Davis Stable Isotope Facility, USA. Background 15N was calculated as the average atom percent 15N in the water samples (mean atom percent 15N ± SD in shoots: 0.369% ± 0.0003). Leaf total P was analyzed by microwave digestion with nitric acid/hydrogen peroxide  followed by atomic absorption spectrometry and inductively coupled plasma atomic emission spectrometry at the UC Davis Division of Agriculture and Natural Resource Laboratory.
Soil nutrient and plant isotope data were analyzed with a two-way analysis of variance (ANOVA) with harvest time, nutrient addition, and block as fixed main effects. All two-way interactions were tested. The three way interaction was not tested because of insufficient degrees of freedom. Data was checked to assure that the ANOVA assumptions were met and was transformed as necessary. Tukey-Kramer Honestly Significant Difference test was used to determine differences between means at P < 0.05. All data were analyzed using R (R Core Development Team 2007).
Root RNA samples were extracted using the RNeasy Plant Mini Kit (Qiagen Sciences, Germantown, MD, USA) following the manufactures guidelines plus a third wash step before elution. RNA concentrations and quality were assessed using the Agilent Nanodrop and the RNA 6000 Nano Assay (Bioanalyzer 2100, Agilent, Santa Clara CA). RNA samples had RNA integrity numbers (RIN) of at least 7.0. DNase digestion was performed on 20 ug total RNA using RQ1 RNase-free DNase (Promega, Madison WI). These RNA were used for both microarray analysis and cDNA synthesis for qRT-PCR analysis.
Transcriptome profiling of each 53h-post injection RNA sample was performed using the Tomato Genome Array Chip (Affymetrix, Santa Clara, CA, USA). RNA samples were prepared for microarray analysis using the MessageAmp Premier RNA Amplification Kit (Ambion, Foster City CA) with 200 ng total RNA as input. Fragmented cRNA samples were then sent to the University of Missouri's DNA Core Facility for Array hybridization and scanning. Each array's CEL file was summarized in Affymetrix Expression Console software using the MAS5 algorithm. The signal intensities were log transformed, and quality control analysis performed. This array data has been made available on the Gene Expression Omnibus (GEO; http://www.ncbi.nlm.nih.gov/projects/geo/) accession #GSE21020. The data were filtered to remove probesets whose log signal intensity was below 4.605 in all 9 arrays. For each probeset, which represents the combined expression data from all relevant probe pairs on the chip, the generalized linear model Yij = μ + Ti + εij was fit. In each ANOVA, Yij is the log normalized transcript level for the ith treatment and the jth replicate, μ is the overall mean expression for the probeset and Ti represents the ith treatment (water, low nutrient, and high nutrient). The null hypothesis t1 = t0 (i.e., mean expression not different between a pair of treatments) was tested using an F-test. We examined the model for conformation to the assumption of normality of the residuals testing the null hypothesis that the residuals for each gene were normally distributed using the Shapiro-Wilk Test. All analyses were performed in JMP Genomics 3.0 (SAS Institute, Cary NC). An FDR level of 10% was used for declaring findings significant, and a stringent rate of 5% was also examined [65, 66]. ANOVA analysis of all differentially expressed genes can be found in Additional file 1. The list of statistically significant transcripts was initially annotated using the Affymetrix NetAffyx annotation file to match a representative Genbank public ID and Unigene to each probeset. The functional annotations of the Unigenes were grouped into functional categories as described in Bevan et al. . In cases where the tomato gene did not have a matching Unigene or had not been functionally annotated, the tomato sequence was used to identify Arabidopsis orthologues by WU-BLAST searches at TAIR . To test for enrichment of specific functional categories between the high vs water and low vs. water pairwise comparisons, Fisher's exact test was performed using GraphPad Prism 5.0, San Diego CA). Within specific categories, binomial distribution probability tests were performed to test for enrichment in the up/down regulation patterns of functionally related genes (expectation = 0.5).
Quantitative real-time RT-PCR
cDNA was synthesized from 1.5 ug DNase-treated total RNA using the Superscript III kit (Invitrogen Carlesbad CA). Gene-specific primer sets were designed using IDT's primerquest software program (Additional file 3), and their sequence uniqueness confirmed with a nucleotide BLAST search against the tomato genome database. Primer pairs were tested for specificity and efficiency with serial dilution reactions and dissociation curve analysis post-amplification. Real-time PCR reactions were run on the Stratagene MX3000 PCR machine using Sybr Green chemistry (Invitrogen Platinum Sybr Green II master mix, 400 nM primer concentration, ROX reference dye, and 1:150 diluted cDNA). Multiple reference control genes were tested against all samples to identify control genes whose expression was not affected by the NH4+ treatments. LeACT and LeUBI were similarly expressed across the samples while LeTubulin was differentially expressed. LeACT was subsequently used as the reference control gene, and the relative expression of the various target genes was analyzed according to the ΔΔCT method . Standard error was computed from the average of the ΔCT values for each biological sample .
We thank Lauren McIntyre for her insights and contributions to the microarray analysis, Julie Chou, Kimberly Jacobs, Julien Linares, Walter Lopez, and Annie Young-Matthews for their help in the execution of the experiment and subsequent sample processing, the University of Missouri DNA Core Facility for hybridization and scanning of the Affymetrix GeneChips, and the National Science Foundation for funding support (#0723775 to DPS and LEJ).
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