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Author(s): Rashmi Upadhyay*

Email(s): rashmiupadhyay123@gmail.com

Address: Indira Gandhi Krishi Vishwavidyalaya, Raipur, C.G, India
*Corresponding Author: rashmiupadhyay123@gmail.com

Published In:   Volume - 32,      Issue - 1,     Year - 2019


Cite this article:
Upadhyay (2019). Identification of QTLS for NH4+ and NO3- use efficiency under water stress and non-stress conditions and expression analysis of glutamine synthetase and nitrate reductase in rice (Oryza Sativa L.). Journal of Ravishankar University (Part-B: Science), 32 (1), pp. 43-60.



Journal of Ravishankar University –B, 32 (1), 43-60 (2019)

 
 

Identification of QTLS for NH4+ and NO3- use efficiency under water stress and non-stress conditions and expression analysis of glutamine synthetase and nitrate reductase in rice (Oryza Sativa L.)

                         Rashmi Upadhyay*

                         Indira Gandhi Krishi Vishwavidyalaya, Raipur, C.G, India.

 *Corresponding Author: rashmiupadhyay123@gmail.com

                [Received: 31 January 2019; Revised version: 27 April 2019; Accepted: 28 April 2019]

Abstract. Nitrogen (N) is one of the most critical inputs and the current average nitrogen use efficiency (NUE) in the rice field is approximately 33%, poorest among cereals. Predominant form of N in aerobic soils is nitrate (NO3-) while ammonium (NH4+) exists in anaerobic soils. Development of cultivars with improved NH4+ or NO3- use efficiency by harnessing inherent significant variability for NUE can be an important approach. Considering these facts, the present study was established with one hundred twenty two and selected thirty two recombinant inbred lines (RILs) of two indica genotypes, Danteshwari × Dagad deshi under three nitrogen forms and three environments. The trend analysis of NH4+-N & NO3--N dynamics revealed that NH4+-N concentration persisted more under anaerobic condition and NO3--N concentration under aerobic conditions. Three way-ANOVA showed high level of significance for variance components (G, N, E) and their interactions effects (GXN, GXE, NXE, EXNXG) for yield & NUE and their component traits. Mean performance of genotypes depicted higher values for agronomically important traits i.e. yield and NUE under NH4+ as compared to NO3--N and N0. The phenotypic and genotypic data was statistically analyzed for QTLs identification for yield & NUE traits. A total of 58 QTLs conferring the corresponding five traits were detected under three N forms and two environments. We also investigated the different members of AMT (Ammonium transporters), NRT (Nitrate transporters), GS (Glutamine Synthetase) & GOGAT (Glutamate Synthase) genes, involved in NUE and analyzed the expression pattern of each gene using gene-specific primer in young rice seedlings. Collectively, OsGln1;1, OsGln1;2, OsGln1;3, OsGln2, OsGlt1 and OsGlt2 manifested different and reciprocal responses to nitrate and ammonium supply. The activity of enzymes NR, NiR, GS & GOGAT was significantly affected by NH4+and NO3- treatment. These results assist us to identify NH4+ & NO3- responsive cultivars which could be used for cultivation and/or used as parent’s in future breeding program to produce better nitrogen use efficiency varieties under water stress and non-stress conditions.

Key words: ammonium transporters; nitrate transporters; NUE; glutamine synthetase.

Introduction

The main driver for crop improvement over the years has been yield. Over the period, the rate of yield improvement has accelerated primarily not only due to the introduction of an increasingly scientific approach, but also through external use of fertilizers. Among these fertilizers in spite of being the most abundant element in the atmosphere (78 %), N is one of the most limiting nutrients in natural and agricultural ecosystems. The majority of plant-useable N is consumed as nitrate (NO3-) from well-aerated soils and as ammonium (NH4+) from poorly aerated, submerged soils. Since rice is capable of assimilating both forms of N it is adapted to aerobic as well as anaerobic growth conditions (Kronzucker et al. 1998).

Furthermore, scarcity of water is a severe environmental constraint to plant productivity. Drought-induced loss in crop yield probably exceeds losses from all other causes, since both the severity and duration of the stress are critical. Influence of drought on plant nutrition may also be related to limited availability of energy for assimilation of NO3-/NH4+, PO43-and SO24 - they must be converted in energy-dependent processes before these ions can be used for growth and development of plants (Grossman and Takahashi, 2001).

Nitrogen use efficiency (NUE) of a plant defines its ability to utilize available nitrogen (N) resources to optimize its productivity. Nitrogen uptake, assimilation and redistribution within cell along with balance between storage and current use at cellular and whole plant level are included in this (Abdin et al., 2005). NUE is a matter of great concern. Burgeoning population of world needs crop genotypes showing direct relationship with yield and are highly nitrogen responsive. NUE is a complex trait which is governed by activities of ammonium and nitrate transporters that are regulated by N form and concentration affects the N acquisition by roots (Garnett et al., 2009). Intrinsic aspects of N utilization includes many gene families, including NO3- and NH4+ transporters genes and primary assimilatory genes that have been identified by different approaches. To cope with varying NO3- & NH4+ concentrations in soils, N uptake in roots is mainly regulated by a high affinity transport system (HATs) that regulates uptake at N levels <1mM, and a low affinity transport system (LATs) that functions at high N concentrations >1mM (Glass et al., 2001). Nitrate transporter system along with nitrate reductase (NR) and nitrite reductase (NiR) enzymes subsequently facilitate reduction of NO3- in to NH4+. Expression of the NRTs is highly regulated (Feng et al., 2011). NH4+ from both the nitrate reduction pathway and direct absorption are subsequently incorporated into amino acids through the synthesis of glutamine and glutamate (Campbell, 2002) primarily in the chloroplasts and plastids via the glutamine synthetase (GS)/glutamate synthase (GOGAT) cycle (Andrews et al., 2004).

Nitrogen utilization within rice plants followed by NH4+ uptake and assimilation in the roots is a complex process that depends on many factors during the growth and development of plants. Reverse genetics is a powerful approach to obtain conclusive evidence on the function of the corresponding gene products, also enzymes involved in metabolic of nitrogen assimilation pathway can be characterized by reverse genetics. But now it is very difficult to identify target genes that are involved in regulation, unlike enzymes in metabolic pathway, so an approach of quantitative trait loci (QTLs) analysis could be one way to isolate regulatory genes. Many gene families, including NO3- and NH4+ transporters and primary assimilation genes, amino acid transporters, as well as transcription factors and other regulatory genes, have been identified by different approaches. With the identification of orthologous genes from rice, opportunities are now emerging for utilizing these genes in marker-assisted breeding for N efficiency (Kant et al. 2011). So in rice, the effect of QTLs would be potential research to confirmed target genes controlling uptake, assimilation, and metabolism of nitrogen, as well as nitrogen use efficiency. The highly complex objective requires comprehensive knowledge and deep understanding of the physiological, biochemical and molecular responses of rice genotypes under different nitrogen regimes. In the present investigation, attempts has been made to identify efficient lines in mapping population derived from Indica parents that shows differential expression of transporter systems and key assimilatory enzymes along with biochemical characterization of these enzymes & morphological characterization of their root system.

Experimental

Plant material and experimental site

The plant material used in present study includes two parent viz., Danteshwari and Dagad deshi and their recombinant inbred lines (RILs) population. Phenotypic data was generated on Vertisol of Research cum Instructional farm, College of Agriculture, Indira Gandhi Krishi Vishwavidyalaya, Raipur. Molecular Marker Laboratory, Department of Plant Molecular Biology and Biotechnology, IGKV, Raipur was used as platform to generate the genotypic data for identifying QTLs for agronomically complex trait i.e. NUE, study NH4+ and NO3- dynamics in soil and carry out enzyme assay and expression analysis of key known genes.

Methods

Field Studies

The RIL lines derived from a cross between Danteshwari×Dagad deshi were evaluated in the field during wet season 2014, 2015 and summer 2015-16 at research cum instructional farm of College of Agriculture, IGKV, Raipur. The rainfed and TSD fields selected for the study were upland in topology with good drainage and percolation rate. In case of terminal drought trials to reduce the chance of rainfall interfering with drought development in the wet season, trials were planted later and water was drained from the field so that the crop has a better chance of being exposed to drought. Good bunds were a prerequisite for this experiment to limit seepage and treatment flow. The entire experiment was laid out in factorial randomized block design with two replication of different forms of nitrogen under varied sets of conditions. The field view of experiment is presented in Fig.1.

Evaluating NH4+-N and NO3- -N dynamics in soil

On-farm experiment conducted during wet season of 2014, 2015 was subjected to analysis of soil nitrogen inorganic fraction in each treatment under all environments.

Nitrogen inorganic fractions

The fractionation of soil nitrogen was carried out by the procedure given by Bremner and Keeney (1965), described by Keeney and Nelson (1982). Steps involved in the process are elaborated as such:

Extraction of NO3--N and NH4--N with 2.0 M KCl

Soil moisture determination

Clean and dry tin + lid were weigh to 0.01 g (W1). 30g of representative moist soil was selected and sample was placed in the weighing tin and lid was replaced. Tin and contents was weigh to 0.01g (W2). Lid was removed and tin was placed with contents in the oven and dry to constant weight between 105 °C and 110 °C Tin with contents was removed from oven and placed as whole in the desiccator to cool. Tin and content was weighed finally.

The soil moisture was calculated in percent  by formula:

                                                                            

Where: SMC = Soil moisture content (%), W1 = Weight of tin (g), W2 = Weight of moist soil + tin (g), W3 = Weight of dried soil + tin (g)

Preparation of equilibrium extract

Principle

Ammonium in held in exchangeable form in soils in the same manner as exchangeable metal cations. Fixed or non exchangeable NH4+ can make up a significant portion of soil N; however fixed NH4+ is defined as the NH4+ in soil that cannot be replaced by the neutral K salt solution. Exchangeable NH4+ is extracted by shaking with 2.0 M KCl. Nitrite is water soluble and hence can also be extracted by the 2.0 M KCl.

Figure 1. A view of experimental field

 

Steps involved

30 g of soil sample was taken in a polyethylene bottle. 150 ml of 2.0 M KCl solution was added (If the sample is limited, it can be reduced to a minimum of 1.0 g and 5 ml 2.0 M KCl to keep 1 : 5 ratio which is mandatory). Bottle was capped and kept in mechanical shaker for 30 min. Soil-KCl suspension was allowed to settle until the supernatant liquid is clear (usually about 30 minutes). This supernatant is filtered into Erlenmeyer flasks gravimetrically through filter paper fixed in funnels. Analyses of NO3--N and NH4+-N elements was performed on aliquots of this liquid (If the KCl extract cannot be analyzed within 24 hours after its preparation store the filtrate in a refrigerator until analyses can be performed).

Determination of NH4+-N and NO3--N in 2.0 M KCL extract using KEL plus distillation apparatus

Material

Distillation apparatus consisting of 500 or 800 mL Kjeldahl flasks, Connecting bulbs, Vertical condenser, Hot plates, 300 mL receiving beakers or Erlenmeyer flasks, Microburette.

Procedure

10 ml of boric acid-indicator solution was added to 125 ml Erlenmeyer flask marked to indicate a volume of 75 ml and flask was placed under the condenser of the steam-distillation apparatus so that the end of the condenser is in the boric acid. An aliquot (usually 20-50 ml) of the soil extract was transferred into a distillation flask and add 0.4 g of MgO was added. Commence distillation by placing plug in the steam bypass tube of the distillation apparatus and 75 ml of distillate was collected. End of the condenser was rinsed and ammonium-N in the distillate was determined by titration with .005N sulphamic acid using a microburette graduated at 0.02-ml intervals. The colour change at the endpoint is from green or blue to a permanent pink. Blank titration value is obtained before running representative samples.After removal of NH4+-N from the sample as described above. The sample in the distillation flask was treated with 1 ml of (1%) Sulphamic acid solution and the flask was swirled for a few seconds to destroy nitrite (NO2-). 0.2-0.4 g of Devardas alloy was added to the distillation flask and the distillation was continued. The amount of NO3- -N was determined same as described above for exchangeable ammonical nitrogen omitting the 2 step. Brief view is given in Fig 2.2.

 

Analyses of soil testing results

Calculation

                           NH4+-N / NO3---N (ppm) = (V-B’) X N X R X 14.01 X 1000

                 W - Θ

 

Where, V= Volume of sulphamic acid required for titrating sample (ml) B’= Blank titration value (ml), N = Normality of sulphamic acid, R = ratio between volume of extract obtained and volume used for titration, W = Weight of oven-dried sample, Θ = Weight of water (g) per 30g oven-dried sample.

Extraction and assay of nitrogen uptake and ammonium assimilation enzymes

The three enzymes, namely, NR, NiR, GS and GOGAT were assayed in freshly harvested leaf at seedling stage of rice genotypes. The protein was determined from all of the enzyme extracts. All the assays were done with three replications. Specific activity of an enzyme has been defined as µmol of product formed per mg protein.

Nitrate Reductase (NR)

The nitrate reductase (NR) activity was estimated by using the method described by (Hageman and Hucklesby, 1971). 500mg of freshly harvested leaf tissue were cut into small pieces and were transferred into test tubes containing 3mL of each 0.2M potassium phosphate buer (pH 7.5), and 0.4M potassium nitrate which were then incubated in dark at 33◦C for 30 min. Add 0.2mL of above extract after incubation in separate test tube containing 1mL distilled water. Add 1.2mL (1:1 v/v) mixture of NED (0.1% w/v) and sulphanilamide (1% (w/v) in 3N HCl) and keep in darkness for 15min for pink colour development. The absorbance was measured at 540 nm with the help of spectrophotometer using distilled water as blank, and the amount of nitrite present was found out by comparing with the standard curve.

Glutamine Synthetase (GS)

The assays were carried out by continuous spectrophotometric rated determination method. The extraction buer included, 10mM-Tris HCl (pH 7.6), 1mM-MgCl2, 1mMEDTA, and 1mM-2 mercaptoethanol. Leaves (2g) were grinded using liquid N2 in the presence of cover slips followed by centrifugation at 12,000xg for 30min at 4◦C. Supernatant was collected and stored at−20◦C (Pateman, 1969).

Glutamate Synthase (GOGAT)

Standard assay mixture contained 40mM potassium phosphate buer (pH 7.5), 10mM L-glutamine, 10mM 2oxoglutarate, 0.14mM NADH, and crude enzyme (final volume 3m 1). Increase in absorbance at 340nm for 34min at room temperature (25◦C) was recorded. Absorbance (340nm/min) was calculated from initial linear portion of the curve (Grot and Vance, 1981).

Stover and grain nitrogen analysis

Stover and grain nitrogen concentrations were estimated by digestion methods using MicroKjeldahl’s apparatus (Humphries, 1956) along with H2SO4 containing digestion mixture (10 parts potassium sulphate and 1 part copper sulphate), 1 g working sample from each treatment from submitted ground sample were put in a Kjeldhal’s flask and digested. The blank was run and determined periodically, using all the ingredients except the sample. The percentage of protein in the grain was calculated by multiplying the grain N content with a constant factor of 6.25 and results were expressed on dry weight basis.

Temporal expression analysis of transporter system and assimilatory enzymes by Quantitative Real Time -PCR analysis (qPCR) In the present investigation qPCR was performed with selected gene specific primers with actin and tubulin as internal controls or housekeeping genes. qPCR was accomplished on Mx3000P® QPCR System (Stratagene, USA) using gene specific primers. qPCR was performed using SYBR green qPCR mix (Applied biosystems and Thermo Fisher make) using approximately 700-1000 ng total cDNA in a 20 ul reaction mixture containing final composition of 1X qPCR mix and 0.5-0.8 uM of each forward and reverse primers. Reaction was set as per manufacturer’s instructions. Blank was always set for each primer during every PCR setup. The relative quantification of expression was done by using the mathematical model given by Livak and Schmittgen (2001).

R = 2 -∆∆Ct

∆∆Ct= [ΔCt treatment – ΔCt control]

                      ΔCt treatment= Ct with primer-Ct with endogenous control (treatment)

                          ΔCt control= Ct with primer-Ct with endogenous control (Control)

QTL analysis

The linkage map was constructed with QTL Cartographer 2.5. Graphical genotyping of these molecular data was done using GGT 2.0 (Van Berloo, 1999). The phenotypic and genotypic data was analyzed using QTL cartographer 2.5 (Composite Interval Mapping) with a threshold value of 3.0 LOD (Wang et al., 2005) and QTL IciMapping 3.2 where a LOD score of 2.5 was used for declaring the presence of a suggestive QTL (Li et al., 2007).

Statistical methods

A complete factorial arrangement of treatments was used (genotype x treatment) as a complete randomized design with three replications All data was analyzed by analysis of variance, and F-test was used to determine treatment significance. Duncan’s multiple range test (DMRT) was used to compare treatment means at 5% probability level using M-STAT-C 14.2 software. Mean ± standard error mean (SEM) values were calculated for statistical analysis. Appropriate regression equations and correlation analysis were also used for further analysis of relations between different parameters.

Observation and results

Growth parameters

Number of effective tillers

5 plants from the row of 10 plants were randomly selected and number of tillers per plants bearing panicle was counted.

Days to 50% flowering

The time taken (days) from sowing to flowering period was recorded on plot basis by visual means.

Plant height

Plant height was measured in centimetre (cm) from soil surface to tip of the tallest panicle at maturity.

Panicle length

Single panicle length of 5 randomly selected plants was measured in centimetres from base to tip of panicle and averaged it.

Biological yield

The biological yield was recorded as actual weight in gram of total biomass of shoot portion per line.

Grain yield

The actual yield of grain in gram per line was recorded.

Harvest index

Harvest index was worked out by using the formula as given below:

 

Chlorophyll content

SPAD-502 was used to measure chlorophyll content of leaves in SPAD units. Readings were taken of young fully expanded leaves of five representative plants from each genotype and average reading was recorded.

Results and Discussion

Seasonal NH4+-N and NO3--N dynamics in soil (kg ha-1)

The trend analysis of NH4+-N and dynamics during kharif 2014 and kharif 2015 revealed that NH4+-N concentration persisted more under anaerobic condition as compared to aerobic condition as compared to aerobic condition while trend analysis of NO3--N dynamics during kharif 2014 and kharif 2015 showed that maximum values of NO3--N concentrations under aerobic conditions as compared to anaerobic conditions under all treatments and soil environments. The trend analysis can be seen in fig. 3.1 and 3.2.

Yield and NUE related traits

Figure 2. Periodic changes in ammonical nitrogen status under different levels of nitrogenous fertilizer and soil moisture regime during kharif 2014 and 2015

Yield and yield related traits were evaluated in 122 and 32 RILs during wet season 2014 and 2015. Three way-ANOVA showed high level of significance for variance components (G, N, E) and their interactions effects (GXN, GXE, NXE, EXNXG). Nitrogen and environment was the main consideration of present study and they significantly affected investigated traits which allow us to conclude that it is possible to manipulate these plant parameters in favour of higher grain yield by using appropriate nitrogen form and environment. During wet season 2014, mean performance of genotypes depicted higher values for agronomically important traits i.e. grain yield, biological yield, plant height and total tillers under NH4+ treatment (317.1 g/m2, 998.6 g/m2, 117.1 cm & 361.6 g/m2) followed by NO3- (311.3 g/m2, 827.7 g/m2, 117.1 cm & 303.6 g/m2) and N0 (352 g/m2 , 850 g/m2 , 170 cm, 108 g/m2 ) treatment under irrigated condition . Furthermore, under rainfed condition high mean phenotypic values were observed under grain yield, biological yield, plant height and total tillers in NH4+ treatment (241.1 g/m2, 933 g/m2, 86 cm, 450 g/m2) followed by NO3--treatment (179 g/m2, 651 g/m2, 86 cm, 401 g/m2) and N0 treatment (57 g/m2, 274 g/m2, 71 cm, 272 g/m2). Moreover, during wet season 2015, NH4+ form showed highest values for all evaluated traits then NO3- and N0 forms. High phenotypic coefficient of variability and genotypic coefficient of variability was obtained for grain yield (>25.6%), biological yield (>19.9%), harvest index (>20.1%), seedling biomass (>17.9%) and spikelet sterility (>27.3%) under all sets of conditions during wet season 2014 and 2015 and broad sense heritability estimates for the estimated 19 traits during wet season 2014 ranged from 8.2% to 84.1 % and during wet season 2015 ranged from 24% to 98.4 % under differential N and water regimes. NUE and NUE component traits ANOVA revealed that genotypic effects and genotype x nitrogen interaction effects were significantly different for investigated N use efficiency and its component traits (p<0.05, p<0.01).

During wet season 2015, mean performance of genotypes depicted higher values for agronomically complex traits i.e. straw nitrogen content (SNC), grain protein content (GPC), grain nitrogen content (GNC), straw nitrogen yield (SNY), grain nitrogen yield (GNY), biological nitrogen yield (BNY), nitrogen harvest index (NHI), N uptake (NUE), N-utilization (NUtE) and N-use efficiency (NUE) was highest in NH4+ treatment (1.23%, 7.3%, 0.5%, 3.5 g/m2, 2.7 g/m2, 6.3 g/m2, 57%, 0.20 gg-1, 45.2 gg-1, 9.8 gg-1) followed by NO3- treatment (1.1%, 6.8%, 0.47%, 2.6 g/m2, 2.1 g/m2, 4.7 g/m2, 56%, 0.18 gg-1, 49.4 gg-1, 9.3 gg-1) and N0 treatment (1.1%, 6.6%, 0.4%, 2.4 g/m2, 1.7 g/m2, 4.2 g/m2, 56.7%, 0.15 gg-1, 51.6 gg-1, 8.8 gg-1). Similarly, under rainfed condition, maximum values of mean performance of genotypes was obtained in NH4+ treatment (1.5%, 8.9%, 0.9%, 2.0 g/m2, 4.1 g/m2, 6.1 g/m2, 5%, 0.22 gg-1, 21.8 gg-1, 5.0 gg-1) followed by NO3-  treatment (1.3%, 8.2%, 0.8%, 1.7 g/m2, 3.1 g/m2, 4.7 g/m2, 34.7%, 0.17 gg-1, 25.1 gg-1, 4.7 gg-1) and N0 treatment (1.2%, 6.9%, 6%, 1.1 g/m2, 1.7 g/m2, 2.8 g/m2, 32.5%, 0.10 gg-1, 30.5 gg-1, 3.3 gg-1). Results is shown in table 1, 2 and 3.

 

Figure 3. Periodic changes in nitrate nitrogen (NO3--N) status under different levels of nitrogenous fertilizer and soil moisture regime during kharif 2014 & 2015

Enzymatic activities and its relationship with Nitrogen use efficiency

Table 1. Effect of NH4+, NO3- & N0 treatments on activities of NR, NiR, GS and GOGAT

Treatment

NR b

NiRc

GSd

GOGATe

Leaves

 

 

 

 

NH4+

0.053 ± 0.004

0.023 ± 0.001

0.099 ± 0.006

0.196 ± 0.014

NO3-

1.49 ± 0.197

0.031± 0.002

0.123 ± 0.007

0.280± 0.032

N0

0.019 ± 0.001

0.016 ± 0.001

0.155 ± 0.012

0.290 ± 0.050

Roots

 

 

 

 

NH4+

0.002 ± 0.001

0.001 ± 0.000

0.023 ± 0.001

0.051± 0.003

NO3-

0.006 ± 0.001

0.017 ± 0.001

0.034 ± 0.001

0.056± 0.003

N0

0.001 ± 0.008

0.001 ± 0.000

0.038 ± 0.003

0.68    0.002

NR activity expressed in µmol NO2 formed mg−1 proteins min−1. NiR activity expressed in µmol NO2 reduced mg−1 proteins min−1. GS activity expressed in µmol Pi formed mg−1 proteins min−1.bGOGAT activity expressed in µmol NADH oxidized mg−1 proteins min−1

In a set of 122 RILs, 32 selected genotypes were evaluated for NUE & related traits and cluster analysis was further performed to classify these genotypes as high NUE, medium NUE and low NUE. Frequency distribution of leaf colour was also recorded to categorize RILs into four different classes’ viz., dark green, green, light green, yellow. Investigation of leaf colour trait accompanied by evaluation of NUE, yield and yield related parameters provided us with the 10 distinct genotypes. The differences observed in the leaf colour and NUE parameters under different N forms in these genotypes possibly may be due to genotypic variation in the activity of enzymes involved in assimilation of nitrogen. Our experiment aimed to investigate the activity of key assimilatory enzymes namely, Glutamine Synthetase (GS), Glutamate Synthase (GOGAT), Nitrate Reductase (NR) and Nitrite Reductase (NiR) at seedling stage in 10 selected rice genotypes. The results showed that N forms greatly influenced the measured traits and substantial differences among rice genotypes were recorded in the activities of the enzymes. Results are shown in Table2and3.


Table 2. Mean phenotypic performance, range, standard deviation (SD), Coefficient of variance (CV %) of investigated yield and yield related traits of 122 RILs and their parents under differential N regimes and environments during wet season 2014

 

 

Wet Season 2014

Traits

N

IRRIGATED (I)

RILs

                                          RAINFEED (Ds)

RILs

 

 

D

DD

Mean±SEm

Range

CV%

D

DD

Mean±SEm

Range

CV%

GY

NH4+

625.52

499.0

352.1± 14

37.3-844

48

100

256

241.1±7

47- 486

37

 

NO3-

375

323

338.3±10

55-842

36

96

212

179.1±8

15-447

55

 

N0

320

242

312.1±11

30-673

37

41

79

57.2±2

14-165

48

BY

NH4+

1266

923

1065.6±20

415-1644

24

543

826

933.1±16

447-1755

21

 

NO3-

796

695

908.5±20

392-2561

28

500

810

651.6±15

185-1231

29

 

N0

752

560

905.6±13

492-1496

17

225

324

274.41±7

118-515

30

HI

NH4+

49

46

37.4±1

6.4-56.1

34

20

30

27.1±0.6

7.3-56.3

30

 

NO3-

47

46

34.7±0.7

11.4-59.6

21

19

26

26.0±0.7

3.1-42.6

32

 

N0

42

43

32.6±0.8

4.9-54.3

26

17

24

20.1±0.4

8.6-36.1

27

TT/m2

NH4+

392

242

361.6±4

238-568

16

483

281

450.8±6

262-636

17

 

NO3-

358

206

303.6±5

123-495

20

393

393

401±7

168-984

23

 

N0

190

105

170.2±2

104-271

16

197

258

272±4

124-464

20

TT/P

NH4+

8.5

5.5

7±0.1

13.1-5.0

20

 

 

 

 

 

 

NO3-

7.8

4.3

6±0.1

11.2-4.0

21

 

 

 

 

 

 

N0

5.9

3.5

5.7±0.1

8.8-2.2

2

 

 

 

 

 

ET/P

NH4+

8

5

6.4±0.1

2.4-10

22

 

 

 

 

 

 

NO3-

7

3

5.3±0.1

2.4-8.2

22

 

 

 

 

 

 

N0

6

4

5.7±0.1

2.2-8.2

18

 

 

 

 

 

DTF

NH4+

79

76

80.9±0.6

62.5-107

9

83

72

80.5±0.5

65.1-104.5

8

 

NO3-

80

76

82.7±0.6

66-130

9

87

88

87±0.4

74.3-98.1

6

 

N0

77

75

79.5±0.6

58-102

9

77

75

79.6±0.6

58.1-104.2

9

PH

NH4+

104

147

117.1±1.6

73.6-170.4

16

79

98

102.6±1

61.2-146.1

17

 

NO3-

91

136

108.1±1.3

72.4-157.9

14

87

88

86.2±1

57.2-122.7

16

 

N0

92

139

111.3±1.5

63.2-220.8

17

61

77

71.6±0.9

47.3-99.7

15

PL

NH4+

25

26

23.8±0.1

17.5-27.6

7

19

26

21.7±0.2

16.3-30.1

10

 

NO3-

24

26

23.2±.1

19.85-27.2

6

17

22

19.7±0.8

15.3-32.3

10

 

N0

24

25

23.4±0.1

18.5-26.5

7

18

18

18.1±0.1

14.2-26

10

FLL

NH4+

30

37

30.8±.04

21.8-44.5

15

26

28

29.4±0.5

20.5-55.5

18

 

NO3-

28

38

28.6±0.3

21.2-39.5

13

22

35

26.2±0.4

17.4-43.7

19

 

N0

27

36

28.2±0.3

20.1-38.4

14

14

17

17.9±0.3

8.25-28.1

17

FLW

NH4+

1.1

1.4

1.4±0.02

0.98-2

12.9

1.3

1.5

1.3±0.1

1.02-2

21

 

NO3-

1.2

1.8

1.3±.02

0.97-1.92

14.2

1.2

1.5

1.1±0.1

0.7-1.1

18

 

N0

1.2

1.2

1.2±0.01

1-2.6

16

0.8

1.1

1.00±0.02

0.7-2.3

20

FLA

NH4+

24

40

32.2±0.6

18.8-52.0

20

26

33

29.9±0.7

17.4-83.2

28

 

NO3-

25

50

27.2±0.5

16.1=50.4

21

20

38

22.7±0.6

9.1-62.7

32

 

N0

23

33

26.2±0.5

17.2-52.2

20

8

14

13.4±0.3

2.6-33.7

30

PLL

NH4+

37

51

44.3±0.6

30.2-62.3

15

40

43

42.5±0.6

29.2-65.6

18

 

NO3-

36

47

40.1±0.5

29.4-56.5

13

30

49

38.3±0.6

23.2-61.8

20

 

N0

36

41

40.2±0.5

28.7-56.9

13

22

29

28.4±0.4

20-40.4

17

PLW

NH4+

1

1.1

1.2±0.01

0.8-1.6

12

1.1

1.2

1.1±0.02

0.69-2.2

17

 

NO3-

1

1.2

1.0±0.01

0.7-1.3

12

0.9

1.1

0.9±0.02

0.57-1.9

22

 

N0

0.9

1.2

1.0±0.01

0.7-1.3

11

0.6

0.7

0.7±0.01

0.49-1.3

18

SL

NH4+

9

9

9.1±.04

7.5-10.2

6

9

8

9.2±0.05

7.7-10.6

6

 

NO3-

9

9

9.2±0.05

7.5-11.2

6

9

9

9.1±0.04

7.65-10.7

6

 

N0

10

8

9.1±0.04

7.4-10.3

6

10

8

9.1±0.04

7.4-10.3

6

SB

NH4+

2

3

2.5±.01

2-2.95

7

2

3

2.4±0.01

2.1-2.9

11

 

NO3-

2

3

2.6±0.01

2.1-3.1

7

2

3

3.5±0.01

2.1-3.2

7

 

N0

2

3

2.6±0.01

2.1-3.2

7

2

3

2.6±0.01

2.1-3.2

7

SLB

NH4+

4

3

3.7±.02

2.6-4.4

9

4

3

3.6±0.03

2.39-4.84

11

 

NO3-

4

3

3.6±.04

1.3-4.7

11

4

4

3.6±0.1

2.85-4.60

10

 

N0

4

3

3.6±0.03

2.5-6.1

12

4

3

3.5±0.1

2.58-4.62

10

SF

NH4+

71

52

74.8±1

49-89.1

18

85

86

80.9±0.7

55.2-96.3

11

 

NO3-

60

73

74.7±0.7

48.8-88.8

11

59

98

79.6±0.8

50.3-97.6

11

 

N0

72

80

71.1±1

17.2-90.1

18

65

78

79.6±1.1

30.2-95.4

17

SS

NH4+

29

48

31.3±1

7.0-86.8

40

15

14

19.1±0.8

3.7-44.7

47

 

NO3-

40

27

25.1±0.7

10.1-41.1

32

41

5

20.4±0.8

55.2-96.3

45

 

N0

28

20

28.1±1.07

9.8-82.7

45

35

22

20.4±1.1

4.6-69.8

66

GY=grain yield, BG= biological yield, HI= harvest index, TT= total tillers, DTF= days to 50 % flowering, TT= total tiller, ET= effective tiller, SB= seedling biomass, PH= plant height, PL=panicle length, FLL=flag leaf length, FLW=flag leaf width, FLA=flag leaf area, PLL= penultimate leaf length, FLW=flag leaf width, FLA=flag leaf area, PLL= penultimate leaf length, PLW= penultimate leaf width, SL= seed length, SB= seed breadth, SLB= seed length and breadth ratio, SF=Spikelet fertility.

 


 

 

Table 3. Mean phenotypic performance, range, standard deviation (SD), Coefficient of variance (CV %) of investigated yield and yield related traits of 32 selected RILs and their parents under differential N regimes and environments during wet season 2015

 

 

Traits

N

IRRIGATED (I)

RILs

RAINFEED (R)

RILs

TERMINAL STAGE DROUGHT (TSD)

RILs

 

 

 

 

D

DD

Mean±SEm

Range

CV%

D

DD

Mean±SEm

Range

CV%

D

DD

Mean±SEm

Range

CV%

 

 

 

NH4+

316

224

284±17.1

117-522

34.1

80

321

136±8

48-261

36

113

135

130±8.6

20-260

37

 

 

GY

NO3-

292

241

233.3±8.9

135-381

22

71

239

125±10

29-248

46

62

103

90±4.6

37-177

29

 

 

 

N0

223

106

221.3±12.9

90.6-383

33

52

162

88±6

20-162

39

70

115

89±4.5

50-179

32

 

 

 

NH4+

640

594

849.9±41.0

372-1410

27.3

291

962

588±27

317-1042

26

439

497

528±11

398-665

12

 

 

BY

NO3-

631

494

674±31.3

427-1388

26

362

724

505±23

247-740

26

257

396

365±8.2

257-432

13

 

 

 

N0

514

221

613±26.1

310.4-921

24

208

518

375±15

151-546

23

271

279

327±8.3

255-424

15

 

 

 

NH4+

49

37

37±1.2

11.4-46.7

19.7

27

33

23±0.9

9.4-36.3

23

26

27

27±1.4

4-49

34

 

 

HI

NO3-

43

40

35.2±0.8

25.2-43.3

13

19

32

22±1.0

11.9-35

23

24

26

24±1.0

9.6-40

24

 

 

 

N0

42

36

35.5±1.2

19.2-40.3

19

25

30

21±1.0

13-33

25

26

36

23±1.3

5-38

22

 

 

 

NH4+

 

 

 

 

 

429

357

440±13

295-617

17

 

 

 

 

 

 

 

TT/m2

NO3-

 

 

 

 

 

362

724

394±7.7

139-301

19

 

 

 

 

 

 

 

 

N0

 

 

 

 

 

488

323

226±13

275-569

20

 

 

 

 

 

 

 

 

NH4+

9

5.3

8.1±0.28

5.0-12.0

19

 

 

 

 

 

12

6

9±0.2

6.3-12

14

 

 

TT/P

NO3-

7.5

3.6

6.76±0.2

3.6-9.5

19

 

 

 

 

 

10

5.8

8.6±0.1

5.8-11

13

 

 

 

N0

6.7

3.4

6.5±0.2

3.4-9.4

19

 

 

 

 

 

8.3

5.5

7.8±0.1

5.5-10

12

 

 

 

NH4+

8.5

5

6.9±0.3

3-9.9

25

 

 

 

 

 

12

6

8±0.2

5.6-11

16

 

 

ET/P

NO3-

7.3

3.6

6.2±0.2

3.6-9.3

19

 

 

 

 

 

8.5

6

7.8±0.1

5.9-9.7

13

 

 

 

N0

6.1

3.4

6.2±0.2

3.4-8.5

19

 

 

 

 

 

8

5.1

7.2±0.1

5.1-9.2

15

 

 

 

NH4+

2.2

4.2

3.85±0.28

2.0-9.3

33

5.8

6.5

5.0±0.2

2.4-7.9

26

 

 

 

 

 

 

 

SB

NO3-

1.3

3.5

2.9±0.10

1.3-3.5

28

2.9

5

3.4±0.1

2.0-6.1

31

 

 

 

 

 

 

 

 

N0

2.3 8

2.5 3

3.1±0.1

1.9-4.8

24

1.5

2.2

2.2±0.1

1.2-3.3

24

 

 

 

 

 

 

 

 

NH4+

80

70

76.4±1.4

66-102.5

11

79

67

76±1.6

62.5- 102.5

17

75

80

80±1.5

71-102

11

 

 

DTF

NO3-

79

70

78.4±1.5

67.5-104

10

79

67

76±1.6

65-104

11

77

78

81±1.4

71-103

10

 

 

 

N0

76

68

80.4±1.5

66.5-103

11

83

68

78±1.4

68-100

11

77

79

81±1.4

71-102

10

 

 

 

NH4+

79

128

106±3.7

74-147

20

81

130

99±3.2

73.6-135

12

76

128

101±3.3

73-141

18

 

 

PH

NO3-

75

116

97.7±3.3

64.6-132

19

77

122

92±3.1

64-125

19

70

128

90±2.9

66-129

19

 

 

 

N0

81

117

96.1±2.9

64.4-132

17

72

103

82±2.6

63-116

18

65

122

89±2.8

63-123

19

 

 

 

NH4+

22

23

23.4±0.4

20.3-32.6

10

20

25. 5

22±0.4

18.7-27.4

10

21

26

22±0.3

17.5-26

8

 

 

PL

NO3-

22

24

22.5±0.3

19.1-30.3

9

18

24

21±0.4

18-26.4

10

19

21

20±0.3

18-25

9

 

 

 

N0

21

22

21.6±0.3

18.3-25.8

7

17

20

19±0.3

14-34

9

20

19

20±0.4

16-26

10

 

 

 

NH4+

26

33

30.5±0.9

21.1-44.2

17

24

37

39±1.0

19-45

19

22

31

27±0.5

21-35

11

 

 

FLL

NO3-

24

30

26.6±0.6

20.1-35.3

14

28

45

32±1.2

22-52

20

19

25

24±0.5

19-36

14

 

 

 

N0

20

29

24.5±0.7

17.8-35.3

16

18

30

21±0.8

14.5-34

21

21

23

24±0.5

19-31

13

 

 

 

NH4+

1.1

1.5

1.3±0.1

1.06-1.72

13

1.4

2

1.4±0.1

1.2-2

14

1.2

1.7

1.4±0.03

0.8-1.7

13

 

 

FLW

NO3-

1.2

1.4

1.2±0.1

0.9-1.5

13

1.4

1.8

1.3±0.03

22.6-51.9

12

1.1

1.5

1.3±0.03

0.9-1.9

14

 

 

 

N0

0.9 4

1.4

0.9±0.1

0.6-1.3

19

1

1.6

1.2±0.1

0.8-2.1

11

1

1.6

1.3±0.03

0.8-1.7

12

 

 

 

NH4+

23

40

30.4±1.4

18.9-54.3

26

27

55

35.6-1.6

22-60

27

20

39

28.1±0.9

17-39

19

 

 

FLA

NO3-

22

33

23.8±0.8

16.9-36.7

20

31

63

34.5±1.9

21.1-67.6

31

16

28

24.9±0.8

16-39

19

 

 

 

N0

14.5

28.8

17.6±0.9

9.3-29.9

28

13

38

20.8±1.3

20.8-40.9

32

16

29

23±0.7

16-33

20

 

 

 

NH4+

33

48

38.8±1.2

29-60.2

18

38

58

41-1.1

31-58

16

32

40

37.6±0.7

28.9-47.9

11

 

 

PLL

NO3-

32

44

36.5±1.1

26.6-51.2

17

32

52

38.3±1.2

28-56

18

30

45

36.4±0.4

29.4-47.1

10

 

 

 

N0

27

43

34.5±1.2

25.3-51.2

19

26

47

32.5±1.1

23.2-47.4

19

35

43

36±0.7

28-46

12

 

 

 

NH4+

0.8

1.4

1.07±0.1

0.51-1.44

16

1.1

1.6

1.2±0.1

0.9-3.1

17

0.9

1.3

1.1±0.03

0.6-1.4

17

 

 

PLW

NO3-

1.07

1.1

1.0±0.1

0.7-1.3

14

1.1

1.5

1.1±0.02

0.8-1.6

14

0.7

1.3

0.9±0.03

0.4-1.5

22

 

 

 

N0

0.94

1.49

1.0±0.1

0.6-1.5

19

0.9

1.2

0.97±0.1

0.6-1.3

17

0.6

1.2

0.9±0.03

0.63-1.36

21

 

 

 

NH4+

9.3

9.6

9.1±0.1

7.2-10

7

8.9

8.7

8.8±0.1

7.2-10.2

7

 

 

 

 

 

 

 

SL

NO3-

8.7

9.7

9.0±0.1

7.3-9.9

6

8.8

8.9

8.7±0.01

7.8-9.2

3

 

 

 

 

 

 

 

 

N0

8.1

8.6

8.9±0.1

7.4-10.1

7

9

8.7

8.5±0.1

7.4-9.8

7

 

 

 

 

 

 

 

 

NH4+

2.6

2.7

2.6±0.1

2.3-2.9

6

2.4

2.5

2.5±0.02

2.2-2.7

5

 

 

 

 

 

 

 

SB

NO3-

2.4

2.5

2.5±0.1

2.3-2.8

5

2.3

2.4

2.5±0.02

2.2-2.6

5

 

 

 

 

 

 

 

 

N0

2.5

2.7

2.6±0.1

2.3-2.8

4

2.4

2.7

2.5±0.03

2.1-2.9

7

 

 

 

 

 

 

 

 

NH4+

3.6

3.5

3.4±0.1

3.1-4.1

7

3.6

3.4

3.5±0.0

3.1-4.1

7

 

 

 

 

 

 

 

SLB

NO3-

3.5

3.8

3.5±0.1

2.9-4.1

8

3.7

3.6

3.5±0.03

3.2-4.0

5

 

 

 

 

 

 

 

 

N0

3.2

3.1

3.5±0.1

3.1-4.1

7

3.7

3.1

3.4±0.05

2.5-4.0

10

 

 

 

 

 

 

 

 

NH4+

2.3

2.8

2.6±0.1

1.8-3.1

11

2

2.5

2.3±0.05

1.7-3

12

 

 

 

 

 

 

 

1000W

NO3-

2.3

2.6

2.6±0.5

1.7-3.0

13

1.8

2.5

2.4±0.01

1.6-3

13

 

 

 

 

 

 

 

 

N0

2.3

2.4

2.5±0.1

1.7-3.0

12

2.1

3

2.4±0.1

1.7-3.1

14

 

 

 

 

 

 

 

GY=grain yield, BG= biological yield, HI= harvest index, TT= total tillers, DTF= days to 50 % flowering, TT= total tiller, ET= effective tiller, SB= seedling biomass, CGR= crop growth rate, PH= plant height, PL=panicle length, FLL=flag leaf length, FLW=flag leaf width, FLA=flag leaf area, PLL= penultimate leaf length, , FLW=flag leaf width, FLA=flag leaf area, PLL= penultimate leaf length, , PLW= penultimate leaf width, SL= seed length, SB= seed breadth, SLB= seed length and breadth ratio, TT/P= total tiller per plant, ETP= Effective tillers per plant, SB= Seedling biomass.

 

 

 

 

Table 4. Mean phenotypic performance, range, standard deviation (SD), Coefficient of variance (CV %) of investigated chlorophyll parameters, NUE and its component traits of 32 selected RILs and their parents under differential N regimes and environments during wet season, 2015.

 

 

Source of variation

IRRIGATED (I)

RILs

RAINFED (R)

RILs

Traits

N

G TMSS DF=31

N TMSS DF=2

E TMSS DF=1

EXG TMSS DF=31

NXG

TMSS DF=62

EXN

TMSS DF=2

EXNXG

TMSS DF=62

D

DD

Mean±SEm

Range

CV%

D

DD

Mean±SEm

Range

CV%

 

NH4+

 

 

 

 

 

 

 

35

32

32±0.3

29-38

6

35

31

32±0.4

29-38

6

SPAD till

NO3-

49.2**

186**

NS

NS

5.3 *

NS

NS

33

30

31±0.4

26-37

7

33

30

31±0.4

26-36

7

 

N0

 

 

 

 

 

 

 

31

31

30±0.4

26-35

7

32

30

30±0.4

26-34

7

 

NH4+

 

 

 

 

 

 

 

37

35

36±0.4

30-42

6

38

40

37±0.6

28-43

8

SPAD now

NO3-

50.2**

190**

NS

NS

6.6*

NS

NS

36

32

35±1.3

28-41

6

34

37

35±0.1

29-41

8

 

N0

 

 

 

 

 

 

 

32

29

32±0.5

24-37

7

31

28

28±0.5

22-33

10

 

NH4+

 

 

 

 

 

 

 

1.4

1.2

1.2±0.1

1-1.4

10

1.7

1.6

1.5±0.1

1.1-2

12

GNC

NO3-

0.05**

1.6**

3.1**

0.04**

0.03**

0.4**

0.29 *

1.1

1.2

1.1±0.3

0.9-1

8

1.2

1.1

1.3±0.2

1.1-2

11

 

N0

 

 

 

 

 

 

 

1.0

1.2

1.1±0.2

0.7-1

7

1.2

1.1

1.2±0.1

1.0-2

8

 

NH4+

 

 

 

 

 

 

 

8.2

6.9

7.3±0.1

6.1-8.7

10

10

9.6

8.9±0.2

6.9-11

13

GPC

NO3-

1.8**

59**

114 **

1.6**

1.0**

15.4 **

1.0**

6.5

7.4

6.8± 0.1

5.8-8.1

8

7.5

6.9

8.2±0.2

6.8-10

12

 

N0

 

 

 

 

 

 

 

5.8

7.0

6.6±0.1

4.6-7.8

8

7.6

6.9

6.9±0.1

6.1-8

8

 

NH4+

 

 

 

 

 

 

 

0.6

0.5

0.5±0.1

0.3-0.6

18

1.1

0.7

0.9±0.1

0.6-2

21

SNC

NO3-

0.09**

0.89**

9.3**

0.04**

0.02**

0.47**

0.01**

0.5

0.5

0.47±0.1

0.3-0.6

12

0.9

0.5

0.8±0.1

0.5-1

19

 

N0

 

 

 

 

 

 

 

0.5

0.5

0.45±0.0

0.2-0.6

14

0.7

0.5

0.6±0.1

0.4-1

21

 

NH4+

 

 

 

 

 

 

 

2.4

3.0

3.5±0.2

1.4-6.9

35

1.4

3.6

2.0±0.1

0.8-3

37

GNY

NO3-

3.0**

35**

158**

2.1**

0.73**

2.73**

0.61**

2.8

2.9

2.6±0.1

1.6-4.8

23

0.9

2.7

1.7±0.1

0.5-3

44

 

N0

 

 

 

 

 

 

 

2.6

2.4

2.4±0.1

0.9-4.1

22

0.8

1.9

1.0±0.1

0.2-2

21

 

NH4+

1.6**

84**

53**

1.6**

0.9**

13**

0.7**

1.5

2.1

2.7±0.2

1.4-4.8

33

2.6

6.1

4.0±0.1

2.5-7

23

SNY

NO3-

 

 

 

 

 

 

 

2.0

1.9

2.1±0.2

1.1-5.3

35

2.8

2.6

3.0±0.1

1.9-5

21

 

N0

 

 

 

 

 

 

 

1.9

1.5

1.7±0.1

0.5-3.0

32

1.4

1.8

1.7±0.1

0.8-3

41

 

NH4+

6.3**

22**

27**

5.6**

2.3**

17.7**

1.7**

3.9

5.1

6.3±0.3

2.9-11

28

4.0

9.6

6.1±0.2

3.9-10

23

BNY

NO3-

 

 

 

 

 

 

 

4.7

4.8

4.7±0.1

2.8-10

26

3.7

5.4

4.7±0.2

2.6-7

25

 

N0

 

 

 

 

 

 

 

4.5

3.9

4.2±0.2

2.0-6.3

24

2.2

3.7

2.8±0.1

1.1-4.3

27

 

NH4+

381**

121*

45,655**

183**

84**

20**

84**

58

58

57±1.6

25-69

17

35

36

35±1.2

17-45

21

NHI

NO3-

 

 

 

 

 

 

 

57

60

56±1.0

45-66

10

24

50

34±1.7

16-50

27

 

N0

 

 

 

 

 

 

 

57

61

56.7±1.6

36 ±74

11

36

49

32±1.7

20-52

24

 

NH4+

0.25**

0.17**

0.01**

0.01**

0.003**

0.11**

0.003*

0.1

0.2

0.20±0.1

0.1-0.3

28

0.1

0.4

0.22±0.1

0.1-0.3

24

NUpE

NO3-

 

 

 

 

 

 

 

0.2

0.2

0.18±0.0

0.1-0.3

26

0.1

0.2

0.17±0.1

0.1-0.2

25

 

N0

 

 

 

 

 

 

 

0.2

0.2

0.15±0.0

0.1-0.3

23

0.09

0.1

0.10±0.2

0.04-0.2

28

 

NH4+

343**

1,753**

47,295**

166**

100**

NS

104**

42.8

50.3

45±1.4

18-59

18

20

22

21.8±0.8

9.4-33

22

NUtE

NO3-

 

 

 

 

 

 

 

53.3

48.9

49±1.1

34-60

13

19

43

25.1±1.4

9.5-43

31

 

N0

 

 

 

 

 

 

 

60.3

52.6

51±1.7

28-66

12

28

42

30.5±1.5

18-45

27

 

NH4+

 

 

 

 

 

 

 

5.6

8.5

9.8±0.5

3.8-17

34

3.1

8.4

5.0±0.3

1.8-9

35

NUE

NO3-

29.5**

33**

2,003**

16.5**

6.5**

99**

4.8 **

8.5

7.8

9.3±0.3

4.5-12

21

2.7

9.0

4.7±0.4

1.1-9.9

46

 

N0

 

 

 

 

 

 

 

12.0

9.0

8.8±0.5

4.0-17

20

2.4

6.1

3.3±0.2

0.7-6.1

39

 ** significance at .05, .01 levels respectively, SPADtill = SPAD at tillering , SPADflow = SPAD at flowering, GNC= grain nitrogen content (%), GPC= grain protein content (%),SNC= straw N content (SNC), GNY = grain N yield (g/m2), SNY = straw nitrogen yield (g/m2), BNY= biological N yield (g/m2), NHI = nitrogen harvest index (%), NUpE= nitrogen uptake efficiency (gg-1 N), NUtE= nitrogen utilization efficiency ((gg-1 N) , NUE= nitrogen use efficiency ((gg-1 N).

 


QTL analysis

A total of 58 QTLs conferring the corresponding five traits were detected under three N forms and two environments (table 4); that as a matter of fact included 14, 15 & 11 QTLs under NH4+, NO3- and N0 level of irrigated condition and 5, 10 & 1 QTLs under NH4+, NO3- and N0 level of rainfed conditions respectively. These QTLs were mapped to different genomic regions of all rice chromosomes and most of them were on chromosomes 1 and 9.

Expression of GS and GOGAT gene families under different N forms

Plant GS and GOGAT genes are very important in N assimilation, but the systematic expression patterns of the GS and GOGAT genes families have not yet been clearly established. Thus, we examined the level of expression of each member of the GS and GOGAT gene families under NH4+ and N03- treatment using quantitative real time PCR.

Actin Vs GS gene family

GS1 and GS2 are two major isoforms of Glutamine Synthetase (GS). GS gene family comprises of three cytosolic GS1 gene (OsGln1; 1, OsGln1;2 and OsGln1;3) and a single plastidic OsGln2 gene. Distinct roles for this enzyme have been suggested by a number of studies on organ, tissue and development (Harrison et al., 2000; Weber and Harrison, 2002).

In the present qPCR experiment for GS genes, the levels of transcripts in organs under study were calculated relative to the Actin gene. The relative expression values more than one shows the increased expression or up regulation while values less than one shows the decreased expression or down regulation as compared to control. Under both NH4+ and NO3- treatment, two of the genes, OsGln1;1 & OsGln1;2 showed a markedly preferential expression pattern in roots whereas OsGln1;2 was mainly expressed in shoot. OsGln2 showed the differential expression level both in root and shoot tissues among all selected genotypes. Furthermore, significant effect of NO3- and NH4+ treatment was observed on GS expression. Overall, in root tissue, OsGln1;1 gene seems to be upregulated in root under both NH4+ and NO3 - treatment with line no.10 (14.82) manifesting significantly strong expression while in shoot line no. 4 (55.13) and line no. 3 (6.16) showed strong expression under NH4+ and NO3- treatment. OsGln1;2 in root showed significant down-regulation by NH4+ treatment except for line no. 10 (8.1)and up-regulation by NO3-  with strong expression harbouring in line no.4 (13.08) while in shoot, excluding line no. 9 (3.27) a significant down regulation and weak expression was observed by NH4+ treatment while NO3- treatment resulted in up regulation as well as down regulation in 10 selected rice genotypes. OsGln1;3 gene in root exhibited strong expression in line no. 4 (10.12) & 5 (7.54) while in shoot most of the genes were up-regulated as a result of NH4+ treatment. Additionally, most of the genotypes showed significant up regulation of OsGln1;3 by NO3- treatment in both root and shoot with line no.3 (11.91) manifesting strong expression. NH4+ treatment revealed strong expression of OsGln2 gene in shoot of line no. 4 (125.8) and in root of line no. 1 (30.59) while in NO3-treatment strong expression in shoot is visible in line no. 4 (186.7) and line no. 10 (63.11) in root. This study suggest that OsGln1; 1, OsGln1;2 and OsGln1;3 shows reciprocal responses to NH4+ and NO3- supply as oppose to proposed mechanism. Collectively, among all isoforms, OsGln2 which predominantly functions in green tissue and is indispensable for assimilation of photo respiratory ammonia in high NUE genotypes revealed shoot preferential expression pattern. OsGln2 was highly upregulated in line no. 4 among all isoforms under both the N supply. This line is high yielding and falls in dark green spectrum of colour classes which denotes the relationship of GS in green tissues with grain yield.

Actin Vs GOGAT gene family

GOGAT catalyzes reductive transfer of the amide group of Gln to 2-oxogluarate to form two Glu molecules. In rice plants, NADH-GOGAT is coded by two genes, OsNADH-GOGAT1 (OsGlt1) and OsNADH-GOGAT2 (OsGlt2) (Tabuchi et al., 2007b).

In the present qPCR experiment for GS genes, the levels of transcripts in organs under study were calculated relative to the Actin gene. The relative expression values more than one shows the increased expression or up regulation while values less than one shows the decreased expression or down regulation as compared to control. Expression of OsGlt1 and OsGlt2 genes was strongly repressed by NH4+ and NO3- treatment for most of the genotypes. Exceptionally, OsGlt1 gene in root tissue of line no. 7 (7.31) of green colour and line no. 10 (1.17) of yellow colour was upregulated by NH4+ treatment while line no.4 (2.74) and line no.5 (2.50) which falls in dark green and yellow colour in colour class was upregulated by NO3- treatment. OsGlt1 gene in shoot tissue of line no. 4 (1.46) showed increased expression in NH4+ treatment and line no. 9(2.71) of dark green colour class and line no. 10 (2.35) of yellow colour class in NO3- treatment. OsGlt2 gene


Table 5. Results of QTLs for five traits under three N levels under two environments

 

Trait

 

 

Left marker

Right marker

LOD

Add.

R2  (%)

Grain Yield (GY)

1

 

1

RM3825

          RM302

2.8

          43.6

        9.8

 

NH4+ I

7

HvSSR7-53

RM-2

3.05

-72.12

18.28

 

 

11

HvSSR11-2

HvSSR11-3

2.82

46.53

8.81

 

 

12

RM277

RM260

3.13

29.31

8.10

 

 

9

RM434

RM410

3.11

31.84

10.97

 

NO3- I

1

RM410

RM108

3.03

33.75

9.17

 

 

11

HvSSR11-2

HvSSR11-3

3.19

30.51

9.47

 

N0 I

1

RM449

RM-5

2.51

35.4

7.20

 

 

9

RM434

RM410

2.55

38.77

8.48

 

NH4+ R

1

RM449

RM5

3.42

-32.73

12.42

 

 

1

RM572

RM24

2.91

-38.10

14.31

 

 

1

HvSSR1-34

HvSSR1-49

2.56

-28.92

3.68

 

NO3- R

9

HvSSR9-25

HvSSR9-27

5.54

-35.88

11.70

 

 

9

RM434

RM410

3.97

-35.63

11.75

 

 

11

RM21

RM26334

3.38

-38.13

7.32

Biological Yield (BY)

 

 

 

 

 

 

 

 

NH +

12

HvSSR12-36

HvSSR12-40

3.85

-103.52

12.3

 

 

12

RM260

RM519

4.89

132.91

17.92

 

NO3- I

1

RM243

RM572

3.34

65.14

15.65

 

 

1

RM449

RM5

3.31

51.86

9.63

 

N0 I

6

RM136

RM340

3.78

-65.42

13.29

 

 

9

RM434

RM410

2.54

46.20

7.64

 

NO3- R

9

HvSSR9-25

HvSSR9-27

2.89

-58.03

8.02

 

 

9

HvSSR9-37

HvSSR9-57

3.88

-67.75

11.86

 

Harvest index (HI)

N0 R

7

RM2

RM11

2.57

31.22

9.15

 

 

1

HvSSR1-87

HvSSR1-89

2.7

3.39

8.02

 

NH4+ I

2

HvSSR2-27

HvSSR2-78

2.59

-3.77

7.91

 

 

4

HvSSR4-26

HvSSR4-35

3.12

3.64

9.1

 

 

1

RM1

HvSSR1-80

2.58

3.42

14.53

 

 

1

HvSSR1-89

RM259

3.21

3.23

11.52

 

NO3- I

9

RM434

RM410

2.73

3.03

12.1

 

 

9

RM410

RM108

2.81

2.72

9.98

 

 

11

HvSSR11-2

HvSSR11-3

3.93

3.27

13.44

 

 

12

RM20

HvSSR11-35

3.56

3.89

19.02

 

N0 I

1

RM486

RM14

5.13

5.71

31.5

 

 

3

HvSSR3-6

HvSSR3-9

3.92

4.46

17.05

 

 

9

RM434

RM410

3.22

2.94

8.68

 

 

11

RM206

RM254

2.57

3.54

10.49

 

NH4+ R

1

RM449

RM5

4.68

-3.57

19.83

 

 

12

RM270

RM17

2.53

-2.57

9.3

 

NO3- R

1

RM449

RM5

3.43

-2.89

12.85

Chlorophyll content (CC)

 

 

 

 

 

 

 

 

NH4+ I

1

HvSSR1-87

HvSSR1-89

8.48

2.14

25.56

 

NO3- I

1

HvSSR1-87

HvSSR1-89

2.83

1.3

8.27

 

 

1

RM572

RM24

4.27

-1.37

15.31

 

N0 I

1

HvSSR1-87

HvSSR1-89

8.8

1.89

27.34

 

 

9

RM288

RM253

2.58

0.98

6.73

Grain yield response (GYR)

 

 

 

 

 

 

 

 

NH4+ I

8

HvSSR8-29

RM310

3.05

-41.28

15.57

 

 

8

RM72

RM515

3.27

-44.14

18.71

 

NO3- I

11

RM202

RM229

2.89

-31.05

13.19

 

NO3- R

1

HvSSR1-34

HvSSR1-49

2.64

-23.71

5.07

 

 

9

HvSSR9-25

HvSSR9-27

7.35

-34.98

16.34

Biological yield response

 

 

 

 

 

 

 

(BYR)

NH4+ I

3

RM135

RM55

2.83

66.06

10.99

 

 

5

HvSSR5-66

RM163

2.51

-116.23

35.61

 

NO3- I

8

RM230

RM433

2.85

41.26

7.97

 

 

10

RM222

HvSSR10-34

2.76

-46.01

9.46

 

NH4+ R

6

       HvSSR6-35

HvSSR6-44

3.41

-91.51

18.51


in root tissue of line no. 10 (3.81) and in shoot tissue of line no. 4 (8.63) was upregulated by NH4+ treatment whereas line no. 3 (5.83) showed significant upregulation in shoot tissue and line no. 9 (4.12) showed significant upregulation in root tissue by NO3- treatment.

The expression of these genes encoding NADH-GOGAT remarkably reduced by external N forms and conditions. Our results also showed that transcription of OsGlt1 is decreased in root and shoot by N concentration while transcription of OsGlt2 is relatively increased in root and shoot by N concentration. When N level is relatively high in soil, expression of OsGlt1 and OsGlt2 can be decreased in order to limit N acquisition but in the opposite side, expression of OsGlt1 and OsGlt2 can be enhanced in order to increase N acquisition. This may be kind of buffering effects in higher plants.

Expression of AMT and NRT transporters under different N forms

Actin Vs AMT gene family

Although functionally not well characterized, twelve putative AMT proteins have been identified located on different chromosome and grouped in to five subfamilies (AMT1-AMT5) with one to three gene members (Deng et al., 2007b; Lie et al., 2009b). So far, studies on expressions and regulations of AMT genes in rice have been focused on the three genes of OsAMT1 family, which displayed different spatio-temporal expression patterns in response to changes in N levels. OsAMT1;1, OsAMT1;2, OsAMT1;3 have been identified as members of AMT1, each showing a distinct expression pattern: OsAMT1;1 shows constitutive expression in both shoots and roots (Ding et al., 2011b). In the present study, similar results were obtained influx of NH4+ ion resulted in up regulation and significant strong expression of OsAMT 1.1 in both root and shoot tissue of line no. 5 (1.11, 10.52), 7 (1.82, 6.36) and line no. 9 (3.95, 4.00) whereas NO3- influx resulted in strong expression in shoot tissue of line no. 3 (28.54). OsAMT1; 2 shows root-specific and ammonium-inducible expression (Ding et al., 2011c). This is in contrary with present results in which up regulation of OsAMT1;2 was obtained in both root and shoot by NH4+ and NO3 - treatment of some genotypes with exceptionally high and strong expression by NH4+ in shoot of line no. 4 (133.43) and in shoot of line no. 3 (99.04) &5 (86.82) by NO3-. Furthermore, NH4+ and NO3-treatment resulted in up regulation of OsAMT1; 3 in both root and shoot of genotypes under study with comparatively strongest expression in root and shoot tissue of line no. 9 (42.23) and line no. 4 (11.39) by NH4+ treatment and root & shoot tissues of line no. 8 (11.63) and line no. 3 (11.55) by NO3- treatment. In, contrary, Sonoda et al. (2003b) reported that OsAMT1; 3 shows root-specific and nitrogen-suppressible expression.

Our results dictates that OsAMT1;2 shows maximum mRNA accumulation in line no. 4 which also pertains high GS2 activity thus OsAMT1;2 expression increases with increase in endogenous glutamine. It also seems that OsAMT1;2 functions in ammonium uptake in ammonium enriched soils as its expression was highest in NH4+ treatment. These findings collaborate with Sonoda et al. (2003c) who studied feedback regulation.

Actin Vs NRT gene family

When breeding crops that utilize nitrogen efficiently, it is important to reveal the regulation of nitrate uptake at molecular level. We focussed on expression of two nitrate uptake related genes, OsNRT2.4 and OsNRT7.8, who are nitrate inducible and is mainly expressed in parenchyma cells around the xylem. OsNRT2.4 and OsNRT7.8 mainly participate in unloading nitrate from the xylem and maintains root-to-shoot nitrate transport and vascular development (Xia et al., 2015). In the present study, (Fig.3& table 5) significant upregulation of OsNRT2.4 was observed in shoot tissue of line no. 4 (6.10) and root tissue of line no. 5 (1.39) by NH4+ treatment while in shoot tissue of line no. 3 (10.26) and root tissue of line no. 5 (3.4) by NO3- treatment. OsNRT7.8 revealed significant strong upregulation in root tissues of line no. 10 under NH4+ (19.35) and NO3- (6.96) treatment.

Since rice roots are exposed to NO3- nutrition under aerobic or water deficit condition and the importance of NO3- nutrition can be dictated and the regulation & function of nitrate transporter genes in rice are worthy of investigation. Strong upregulation of OsNRT7.8 in line no. 10 which is actually of pale-yellow colour allow us to select this line for breeding and production purposes for efficient nitrate uptake under drought and water limited condition where major form of available nitrogen is NO3-

Discussion

Zia et al. (2001) on nitrogen dynamics under aerobic and anaerobic soil conditions observed the maximum drop in NH4+ concentration under aerobic environment while high increase in NO3- concentration was registered under aerobic condition. Chaturvedi et al. (2005) reported earlier that more number of tillers in experiment might be due to the more availability of nitrogen, which played a vital role in cell division. Similarly, it was reported that the maximum number of tillers were at N200 level and the minimum at N0 level by Meena et al. (2003). Also, Fageria and Baligar (2001) reported a quadratic relationship between rice grain yield and dry matter yield of shoot. Woldeyessus et al. (2004) dictated the importance of NUE varieties in future breeding program. Earlier reports by Tabuchi et al., 2007; Martin et al., 2006 etc illustrates variation in enzyme activity in genotypes and their role in enhancing NUE of a genotypes. In the present study, the QTLs for grain yield, biological yield, harvest index, chlorophyll content, grain yield response and biological yield response under different nitrogen and water regimes have been speculated and identified. These results are consistent with previous studies. Cho et al. (2007) found that QTLs detected under high and low N levels are widely different. However, the study of Tong et al. (2006) showed the presence of the same and specially expressed QTLs under low and high N levels. Hu et al. (2012) detected QTLs for N content and NUE in adjacent regions, respectively. Wei et al. (2012) detected QTLs for nitrogen deficiency and nitrogen use efficiency traits. For NDT and NUE traits, seven and eight QTLs were identified in 2006 and 2007, respectively. Tong et al. (2011) analyzed the QTLs for rice yield and its components under high, middle and low N levels, and detected 15, 23 and 19 QTLs at three N levels, respectively, thereby indicating the occurrence of obvious interactions between QTLs for yield traits and N levels. QTL for chlorophyll content (CC) was rarely reported previously. The genomic region RZ599-RM53 on chromosome 2, where grain yield and biological response QTL was located, was reported to have QTLs for grain yield under low nitrogen and normal nitrogen by Wei et al. (2011). Rice plant have developed intrinsic mechanism for uneven N distribution thus assimilate N efficiently in roots by this kind of flexible and reciprocal regulatory mechanism, and control rice growth and development. Similar results for OsGln1; 1, OsGln1;2, OsGln1;3 and OsGln2 was earlier reported by Ishimaya et al. (2004). Previous studies by Watanabe et al., (1996) show similar responses and contradict previous report showing ammonium inducibility (Tobin et al., 2001). Aaraki and Hasegawa (2006) revealed the importance of nitrate uptake and nitrate transporters studies in rice. Systemic expression pattern for nitrate transporters is not studied in past thus we open new insight for nitrate-nitrogen studies.

Acknowledgment

I would like to extend my appreciation to Proff. Dr. S.B. Verulkar for his guidance during the course of my research work. Without his valuable assistance, this work would have not been completed. I thankfully acknowledge the Department of Plant Molecular Biology and Biotechnology, IGKV, Raipur for providing all necessary assistance and inputs required to implement this research ideas. Finally, I am deeply indebted to Department of Science and Technology, Government of India, for their cooperation and financial support in form of Inspire fellowship.

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