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Original Research ARTICLE

Front. Plant Sci., 24 February 2017 |

Growth, Morphological, and Physiological Responses to Drought Stress in Bothriochloa ischaemum

Ying Liu1,2, Peng Li1,2*, Guo Ce Xu1,2, Lie Xiao1,2, Zong Ping Ren1 and Zhan Bin Li2
  • 1Institute of Water Resources and Hydro–electric Engineering, Xi'an University of Technology, Xi'an, China
  • 2State Key Laboratory Base of Eco-Hydraulic Engineering in Arid Area, Xi'an University of Technology, Xi'an, China

Water shortage in the arid-semiarid regions of China seriously hampers ecosystem construction. Therefore, elucidation of the mechanisms by which vegetation in that area responds to drought stress may enable us to improve utilization of limited water resources and thus contend with the problem of drought and water shortage. We studied Bothriochloa ischaemum, a native grass species, conducted potting control tests to compare several indicators of B. ischaemum grown under three different moisture conditions (80%, 60%, 40% Field capacity represent sufficient water supply, mild water stress, and serious water stress, respectively). Plant response parameters measured included biomass accumulation, root morphology, transient water use efficiency (WUE), stable carbon isotope ratio (δ13C), and stable carbon isotope discrimination (Δ13C) of various plant organs and their interrelationships. B. ischaemum had the greatest WUE under mild drought stress. However, serious drought stress resulted in considerable decline in overall biomass but substantial increase in root-to-shoot ratio and fine-root biomass. Coarse-root biomass dropped appreciably, indicating that serious drought stress leads to allocation non-uniformity of the carbon “sink.” δ13C and Δ13C of stem correlated considerably with root morphology, suggesting the feasibility of characterizing WUE, biomass, and root morphology of B. ischaemum via the stable carbon isotope approach. Our evaluation of 21 drought resistance indicators of B. ischaemum showed that under a given moisture treatment gradient one can isolate an optimal indicator to express growth, morphology, and physiology, to improve the accuracy of depicting plant drought resistance and simplify the drought resistance indicator system. This study elucidates the response mechanism of B. ischaemum to drought stress and provides theoretical support to screening of drought-resistant plants across the arid-semiarid regions of China.


Water resources are scarce in arid-semiarid regions of China, which is not only the main limiting factor of ecological system in this area, but also the key factor to control ecosystem structure (Zou et al., 2016). Rainfall is a major means of recharging the vegetation ecosystem (Shan, 2002), but scant precipitation and non-uniform annual and quarterly allocation often become the limiting factors of local plant growth and vegetation restoration (Xu et al., 1997; Wei et al., 2004). Since the Chinese government implemented the “Grain for Green” policy in 1999, cropland area in western China has decreased dramatically while vegetation area has increased (Lu et al., 2012); this transformation has led to increased public focus on vegetation utilization of limited soil water resources. Related studies show that, plants can only absorb and utilize a small share of soil moisture (Huang et al., 2004; Wang et al., 2006), these studies suggest that identifying the anti-drought mechanism(s) of local plants can address the water shortage in this area and thus further improve crop utilization of the soil water resource.

Plant water-use efficiency (WUE) reflects water consumption and drought adaptability of a plant (Martin et al., 1999; Ray et al., 1999); high WUE is a mechanism of plant adaptation to water deficit and an important characteristic of plant response to an arid environment (Jaleel et al., 2008; Sun et al., 2008). Moreover, several studies indicate that plant root systems play an important role in plant adaptation to a drought stress habitat (Toorchi et al., 2002; Pu et al., 2010; Zhang et al., 2012). Traditional wisdom holds that a plant subjected to drought stress in the Loess Plateau area would show constant or increased WUE (Xu et al., 2003, 2010), increased root system biomass, and a morphology approaching deep and dense roots (Passioura, 1983; O'Toole and Bland, 1987; Blum and Sullivan, 1997). Nonetheless, other scholars have argued that if the root system is too large, the WUE would instead decline (Mu et al., 2005). Therefore, conflicting opinions suggest the need for further study of the adaptation strategy of plant morphology and physiology to drought in the arid-semiarid regions of China.

Recent studies of WUE for the Qinghai-Tibetan Plateau, Northeast China grassland, and tropical and subtropical plants in China have utilized stable carbon isotope analysis. These studies demonstrate that stable carbon isotope discrimination (Δ13C) and stable carbon isotope ratio (δ13C) of plant leaves correlate strongly with transient or prolonged WUE and can indicate plant adaptation to drought (Su et al., 2000; Qu et al., 2001; Chen et al., 2013; Zhou et al., 2013; Qiu et al., 2014). The related studies also mention that stable carbon isotope fractionation occurred to different organs of C3 and C4 plants (Zhao et al., 2004; Zhang et al., 2009; Ghashghaie et al., 2016), and the role of stable carbon isotope characteristics of each organ in defining plant WUE was supported to some extent. However, studies have not yet been reported on the possibility that stable carbon isotope characteristics can characterize root system anti-drought properties. Summarizing the studies of other researchers, we proposed to test the hypothesis that, compared with all other organs of a plant, one organ of the plant has a stable carbon isotope eigenvalue more relevant to WUE, biomass, and root system morphological properties; stable carbon isotope characteristics of this organ should allow us to characterize plant WUE, growth, and root system morphological features.

The above studies also demonstrate that plant drought resistance is an overall reflection of multiple factors; therefore, to understand plant drought resistance, it is important to reveal the anti-drought mechanisms of herbaceous plants in the arid Loess Plateau area by analyzing differences in given plant growth indicators (e.g., biomass allocation to the aboveground and underground portions), morphological indicators (e.g., root system morphology), and physiological indicators (WUE, Δ13C, and δ13C). However, to our knowledge there are few studies that utilize the stable carbon isotope technique to comprehensively evaluate and screen drought resistance indicators of herbaceous plants in the arid-semiarid regions of China. Therefore, we put forward the hypothesis: among plant growth, morphological, and physiological indicators, there is a best indicator which is more relevant to drought resistance, and its use can reflect plant drought resistance more concisely and accurately.

Bothriochloa ischaemum, a major grass species for creating grassland in the arid-semiarid regions farmland-to-grassland conversion project, is also an important species for restoration and carbon storage of degraded grassland (Xu et al., 2007; Cheng et al., 2010). Characterized by its superior regenerative capacity, quick reproduction, drought and trampling resistance, notable regional adaptability, and high productivity, it constitutes a high-quality natural forage in the arid-semiarid regions of China. Its root system is well developed and forms a network that can intercept rainfall and conserve soil and water. We carried out moisture-controlled potting tests to study biomass accumulation and allocation of B. ischaemum under different soil moisture conditions. Our observations included root system morphological characteristics and the relationship of transient WUE vs. δ13C and Δ13C values of natural abundance of each organ, so as to elucidate the response mechanism of B. ischaemum to drought stress and provide theoretical support to construction and management of man-made grassland in the arid-semiarid regions.

Materials and Methods

Experimental Materials and Design

The experiment was carried out at Xi'an University of Technology in June 2014 using self-made transparent cuboid Plexiglas containers (19 × 4 × 27 cm). The test soil was collected from the B. ischaemum-dominated grassland at Wangmao gully in Suide, North Shaanxi; after superficial humus and litter were cleared away, a 0- to 30-cm layer of soil was removed, mixed well, bagged, and air-dried naturally. Thereafter, the soil was passed through a 2-mm sieve and its bulk density measured. Each Plexiglas pot was packed with 2.5 kg of soil, and the soil bulk density was 1.2 g cm−3, identical to that of the soil sampling plot in North Shaanxi. The test soil total nitrogen was 0.69 g kg−1 and its field capacity (FC) was 22%. The soil is classified as Calcic Cambisol (FAO-UNESCO, 1977) and is mainly a wind-deposited loess soil that is highly erosive.

Seeds of B. ischaemum for the test were harvested in October 2013 from natural grassland in Ansai, North Shaanxi; harvested seeds were stored in paper bags under natural conditions in the laboratory. On 01-May-2014 five bunches of seeds were sown by scattering in each container; the individual seedling growing most vigorously in each bunch was retained after seedling emergence. Seed holes lacking seedling emergence were replanted. The same seeds which for replanting were sown in the same soil conditions at the same time during the experiment. After seedling thinning, moisture control treatment was begun on 01-Jul-2014, using three soil moisture gradients: sufficient water supply (80% FC as control, CK), mild stress (60% FC, mild water stress, MS), and serious stress (40% FC, serious water stress, SS); nine replicate pots were prepared for each moisture gradient, for a total of 27 pots of samples. In the absence of stable carbon, hydrogen, and oxygen isotope labeling, stable carbon isotope ratios of all test samples were of natural abundance.

Potting soil moisture was controlled by means of weighing: first of all, the pots with the biomass of B. ischaemum was weighted and recorded of all the moisture control treatment as the background weight. The background weight of CK, WS and SS is 3,875, 3,765, and 3,655 g/pot. Then the pots were weighed at 18:00 every day, and watered if the weight was lower than the background weight until the experiment ended on 11-Nov-2014. The biomass of each pot of B. ischaemum was included in the background weight before the moisture control treatment. Because the difference between the initial biomass of seedling (0.867 g) and the maximum wet biomass of each pot of B. ischaemum (5.812 g) following the test was only 0.1% of the total weight of the overall moisture-controlled pot (3880 g), and the moisture control duration is short, the effects of B. ischaemum growth weight gain on moisture treatment control were neglected.

Experimental Methods and Determinations

Determination of Photosynthetic Characteristics and Transient WUE of B. ischaemum

The experiment was carried out during the period from 09:00 am to 11:00 am on 03-Aug-2014, 10-Aug-2014, and 13-Aug-2014, when the weather was sunny and cloudless (during the early-flowering phase of the B. ischaemum growing period). The 2- by 3-cm transparent leaf chamber of an Li-6400 portable photosynthesis system (LI-COR, Inc., Lincoln, NE) was used to determine photosynthetic characteristic indicators of B. ischaemum and environmental parameters under natural conditions (natural light source; uncontrolled CO2 concentration and humidity): net photosynthetic rate of leaf (Pn), transpiration rate (Tr), stomatal conductance (Gs), and intercellular CO2 concentration (Ci). Sufficiently spread leaves were selected for determination, and every point was stabilized for 2 min before reading. Based on the above determination parameters, leaf WUE was calculated as follows: WUE = Pn/Tr.

Determination and Calculation of Root System Morphological Indicators and Seedling Biomass of B. ischaemum

On 11-Nov-2014 the aboveground portion of all B. ischaemum plants of each pot was mowed, numbered, and stored separately as new leaves, old leaves, and stems. The soil in each pot along with the root system was poured onto a plastic cloth, and the root system was immediately hand-picked from the soil while distinguishing between the taproot (coarse root) and the lateral roots (fine roots), separately (the taproots were kept separate from lateral roots), then placed in a deionized water flume (2–3°C) and washed clean; both root system samples (i.e., taproot and fine roots) were placed in a deionized ice water flume and immediately scanned (Expression 4490, Epson China Co., Ltd., Beijing, China) to acquire root system morphological images. Root length, diameter, and surface area were statistically analyzed using a WinRHIZO 2013 image analysis system (Regent Instruments Inc., Quebec City, PQ). Thereafter, all scanned root system and aboveground portion samples were dried at 65°C until a constant weight was reached as confirmed by weighing with a balance (to the nearest 0.001 g). Specific root length and surface area were calculated from the ratio of root length of the corresponding root system to biomass and that of root surface area to biomass, respectively.

The above biomass ratios of various plant organs were calculated in grams, representing dry material masses of new leaves, old leaves, stem, fine root, and coarse root of B. ischaemum.

Determination of Stable Carbon Isotope Ratio and Calculation of Carbon Isotope Discrimination

The dry material of every organ of B. ischaemum was ground in a mortar and passed through an 80-mesh sieve for later use; the soil sample was passed through a 0.149-mm sieve for later use. A 0.005–0.006 g of plant sample was taken and burned in the solid combustion chamber of a MultiN/C3100 total carbon/total nitrogen analyzer (Analytik Jena AG, Germany) at 1050°C sufficiently to generate CO2 (while recording sample total carbon content value in g kg−1); the CO2 was then introduced into a CCIA-36d-EPCO2 isotope mass spectrometer (Los Gatos Research, San Jose, CA) to detect δ13C value of sample natural abundance. δ13C values of plant and soil were determined with PeeDee Belemnite (PDB) as the standard using the following formula (Farquhar et al., 1982):


where (13C/12C)PDB is 13C/12C of PDB standard, and δ13C denotes the per millage of deviation between 13C/12C of the sample and that of standard sample.

Carbon isotope discrimination Δ13C was calculated using the following formula:


where δ13Ca denotes carbon isotope ratio of CO2 in air, assumed to be −8%0 (Farquhar et al., 1989; Voltas et al., 2006); δ13Cp denotes carbon isotope ratio of CO2 in plant or soil sample.

Evaluation and Overall Ranking of Drought Resistance of Various Indicators

For root system morphological characteristic indicators (root length, root surface area, specific root length, and specific root surface area), physiological characteristic indicators (WUE, δ13C, and Δ13C), and growth characteristic indicators (biomass and biomass ratio of each organ) of B. ischaemum under different moisture conditions in this study, drought resistance was judged by means of membership function values. The calculation formula of membership function (Equation 1) is

If an indicator is positively correlated with drought resistance:


If an indicator is negatively correlated with drought resistance:

μ(Xi)=1XiXminXmaxXmin,i=1,2,3......n    (1)

where μ(Xi) is the membership function value, Xi is the measured value of an indicator, and Xmax and Xmin are the maximum and minimum of an indicator of all varieties tested.

For the above anti-drought physiological, ecological, and morphological indicators of B. ischaemum, principal component analysis (PCA) was used to extract a common factor with cumulative variance contribution rate ≥80%; common factor scores of different drought resistance indicators were then calculated and with the variance contribution rate of the principal component as the weight, weighted summations of the extracted scores were carried out to obtain the coefficient of each indicator in a composite drought resistance score model. Finally, the coefficients of the composite score model were normalized to obtain the factor weight ω(Xi) of each indicator. Based on factor weight ω(Xi) and membership function value μ(Xi), the drought resistance measure D(Xi) of each indicator was calculated using the following formula (Equation 2):

D(Xi)=ω(Xi)×μ(Xi),i=1,2,3......n    (2)

Data Analysis Method

All test data were plotted using SigmaPlot10.0 (IBM Corporation, Chicago, IL, USA) and processed using SPSS21.0 (IBM Corporation, Chicago, IL, USA) statistical analysis software. Correlation analysis was conducted on transient WUE, root system morphological characteristics (root length, root surface area, specific root length, and specific root surface area), organ biomass ratio, and stable carbon isotope characteristics. Significance was determined for the above indicators, and one-way ANOVA and Duncan method were used to compare significance level of the differences between the above indicators and ratios (α = 0.05). The principal component analysis was used to extract a common factor with cumulative variance contribution rate and conducted on the weight of different drought resistance indicators.


Photosynthetic Characteristics, Transient WUE, and Stable Carbon Isotope Characteristics of B. ischaemum under Drought Stress

All photosynthetic characteristic parameters decreased with decreasing soil moisture, among which net photosynthetic rate (Pn), transpiration rate (Tr), and stomatal conductance (Gs) under sufficient water supply (CK) were significantly higher than those under the MS and SS moisture stress conditions (Table 1). The WUEs under MS were 2.3 μmol mol−1, significantly higher than those under SS (2.0 μmol mol−1) but not significantly different from those under CK treatment (2.2 μmol mol−1). Although both Pn and Tr under MS treatment were significantly lower than those under CK, the stomatal conductance (Gs) under MS was only 0.073 mmol m−2 s−1, suggesting that the plant stomata closed under MS, so photosynthetic rate declined; however, the stomatal closure also lowered Tr, and eventually WUEs under MS were significantly higher than those under CK treatment. Under SS conditions, Pn of B. ischaemum declined, suggesting lower WUEs.


Table 1. Changes in B. ischaemum gas exchange parameters under different moisture conditions.

The changes in δ13C and isotope discrimination of each organ of B. ischaemum under drought stress are summarized in Figure 3. As drought stress was exacerbated, δ13C of each organ exhibited a rising trend. The δ13C values of new leaves (δ13CNL) under MS and SS treatment were −11.8 and −11.9%0, respectively, which were significantly greater than those under CK treatment. The δ13C values of the stem (δ13CS) under CK treatment was the lowest, which was −14.3%0, 1.6%0lower than SS treatment. The δ13C values of the stem under MS treatment was −13.6%0, which was significantly higher than SS treatment (P < 0.05). From the perspective of δ13C values of various organs, the δ13C values of fine root under SS treatment was the lowest, which was −11.7%0. While δ13COL was the highest, the δ13C values of organs under SS treatment showed no significant difference. The δ13C means of organs under MS treatment were manifested as follows (where δ13CFR is δ13C of fine roots, δ13COL is δ13C of old leaves, and δ13CCR is δ13C of coarse roots): δ13CFR > δ13CNL > δ13COL > δ13CCR > δ13CS. In contrast, δ13C means of organs under CK treatment were significantly different between δ13CFR, δ13CNL, and δ13CS.

Δ13C values of B. ischaemum under different moisture treatment conditions declined with increasing drought stress. The Δ13C values of new leaves under CK treatment was 4.8%0, which was significantly higher than MS and SS treatments, respectively. Upon comparing Δ13C values of organs under the various treatment regimens, we found that Δ13C values generally showed the following trend: Δ13CFR < Δ13CCR < Δ13COL < Δ13CS. Δ13C values of organs under SS treatment were significantly different between regimens, and significant difference existed in Δ13CR13CFR and Δ13CCR) vs. Δ13CNL and Δ13CR vs. Δ13CS for root system under CK and MS treatment. However, the difference between Δ13CNL and Δ13CS was insignificant.

Effects of Drought Stress on Biomass and Root System Morphology of B. ischaemum

Total root length and total root surface area of B. ischaemum under SS treatment increased significantly; total root length was 2.86 times that under CK and 2.60 times that under MS, and total root surface area was about 2.7–3.0 times those under CK and MS treatments (Table 2). Comparison of specific root length and specific root surface area of B. ischaemum under the three moisture treatment gradients shows that specific root length under MS treatment was significantly greater than specific root lengths under the two other treatment gradients, but specific root surface area showed no significant difference.


Table 2. Changes in B. ischaemum root morphology parameters under different moisture conditions.

Total biomass of B. ischaemum declined significantly with decreasing soil moisture, and its influence on the aboveground portion was significantly greater than that on the underground portion (Figure 1A). As to the aboveground portion, drought stress had no significant impact on new leaf biomass, but the old leaf biomass of B. ischaemum decreased significantly, and stem biomass under SS treatment was 0.049 g, significantly lower than that under CK treatment (0.071 g). As to the underground portion, although overall root system biomass did not differ significantly under the three moisture treatment gradients, further discrimination of the response to soil moisture between the taproot (coarse root) and lateral root (fine root) showed totally different manifestations. The coarse-root biomass was 0.024 g under sufficient moisture (CK), greater than the fine-root biomass (i.e., 0.014 g), and as soil moisture gradually decreased, the coarse-root biomass decreased while the fine root biomass increased. Under SS moisture condition, the coarse-root biomass was only 0.009 g, and the fine-root biomass was 0.049 g, 5.444 times the coarse-root biomass.


Figure 1. The biomass and ratio of different parts under different water conditions Bothriochloa ischaemum biomass (A) the biomass of different parts, (B) the biomass ratios of different parts. CK (adequate moisture), black bars with white crosshatching; MS (moderate water stress), white with black diagonal lines; SS, (severe water stress), white with black dots. Lowercase letters above each bar indicate significant difference (P < 0.05); vertical lines, mean ± SE.

The root-to-leaf ratio under SS treatment was 0.386, significantly greater than those under the other two treatment conditions; the ratio of fine roots to coarse roots was 6.123 under SS treatment, 5.649 times that under MS treatment, and 8.056 times under CK treatment (Figure 1B). The leaf-to-stem ratio under SS treatment decreased significantly, and consequentially the root-to-shoot ratio under SS treatment was significantly greater than the same ratios under the other treatment conditions; in other words, the significant rise in root-to-shoot ratio under SS treatment was due to synergy of significantly increased fine roots and significantly decreased leaves.

Correlation among Stable Carbon Isotope Characteristics, WUE, Biomass, and Root Morphological Characteristics of B. ischaemum

Correlation analysis of stable carbon isotope values, discriminations, and transient WUEs of various organs (new leaves, old leaves, stem, fine root, and coarse root) of B. ischaemum showed that δ13C and Δ13C of each organ exhibited very significant negative correlation (all correlation coefficients exceeded −0.989; Table 3). δ13CNL, δ13COL, and δ13CS exhibited significant positive correlation with WUE; Δ13CNL, Δ13COL, Δ13CS, and Δ13CFR exhibited significant negative correlation (P < 0.05) with WUE, in which the correlation coefficient (0.614) between δ13CNL of new leaves and WUE was the maximum, followed by that of δ13COL (0.460), whereas the negative correlation coefficient between Δ13CNL of new leaves and WUE was the maximum (i.e., −0.531).


Table 3. Correlation analysis for carbon isotope ratio (δ13C), carbon isotope discrimination (Δ13C), and water use efficiency (WUE) in B. ischaemum organs.

Correlation analysis of B. ischaemum biomass, root system morphological characteristics, and WUE (Table 4) showed that, disregarding the effects of soil moisture, WUE was very significantly correlated with root-to-shoot ratio, ratio of fine roots to coarse roots, root-to-leaf ratio, and root-to-stem ratio, and was the most correlated with the root-to-shoot ratio. Regarding the drought stress condition, the fine-root to coarse-root biomass ratio under CK treatment was the most correlated with WUE; under MS and SS treatment, the correlation between root system morphological characteristics and WUE was greater than that between biomass and WUE, and root length and WUE exhibited very significant correlation.


Table 4. Correlation analysis for root morphology, biomass accumulation, and WUE in B. ischaemum.

Correlation analyses of stable carbon isotope characteristics of each organ of B. ischaemum versus biomass and root system eigenvalue, respectively, revealed that the biomass of B. ischaemum was significantly correlated with the stable carbon isotope characteristic of new leaves only (P < 0.05; n = 9), in which the root-to-shoot and root-to-leaf ratios exhibited significant negative correlation with δ13CNL (Table 5). Each of the root system morphological indicators exhibited significant negative correlation with δ13CS and significant positive correlation with Δ13CS. Moreover, total root length and total root surface area were significantly correlated with Δ13CFR (P < 0.05; n = 9), whereas specific root surface area exhibited significant negative correlation with δ13COL and significant positive correlation with Δ13COL, respectively.


Table 5. Correlation analysis for carbon isotope ratio (δ13C), carbon isotope discrimination (Δ13C), Biomass and Root traits in B. ischaemum.

Principal Component Analysis of Growth, Morphological, and Physiological Characteristic Indicators of B. ischaemum

Principal component analysis was carried out over a total of 21 indicators of B. ischaemum under three moisture treatment conditions, including growth indicators (biomass and ratios), physiological indicators (WUE, carbon isotope value δ13C, and carbon isotope discrimination Δ13C), and morphological indicators (root morphology), to obtain eigenvectors, factor loading, and contribution rates (Table 6). The results show that, for the first two factors out of CK and MS factor eigenvalues, their cumulative contribution rates had reached 80%, and their characteristic roots (λ) were >4.71 and >3.50, respectively; the first two factors were extracted, and variables of the same nature were classified as one type, so as to get two new composite indicators independent of each other (i.e., common factors, denoted by F1 and F2, respectively). Under SS treatment, three common factors were extracted, denoted by F1, F2, and F3, respectively. From absolute load factors of common factor loading matrix, it can be seen that, in the case of CK treatment, F1 had higher loading on root length and root surface area and F2 had higher loading on fine-root to coarse-root biomass ratio and root-to-leaf biomass ratio. In the case of MS treatment, F1 had higher loading on stable isotope ratios and isotope discriminations of new leaves and fine root, WUE, and root length; F2 had higher loading on root-to-shoot ratio and root-to-leaf ratio. In the case of SS treatment, F1 had higher loading on WUE and on stable isotope ratios and isotope discriminations of new leaves and old leaves; F2 had higher loading on leaf-to-stem ratio, stable isotope ratio, and isotope discrimination of stem; F3 had higher loading on mass ratio of new leaves to old leaves. Based on common-factor eigenvectors and contribution rates acquired, a composite score was calculated; thereby we determined the weight coefficient ω of each factor, which was used to weight a membership function value.


Table 6. Changes in B. ischaemum principal component factor load matrix, characteristic root, synthesis score, and factor weight under different moisture conditions.

Membership Function Analysis and Drought Resistance Evaluation of B. ischaemum Drought Indicators

A fuzzy membership function approach was applied to the above drought resistance indicators. Membership function value μ of each factor was calculated using Equation 1, to which a corresponding weight coefficient ω was assigned. A weighted membership function value was calculated using Equation 2 and served as composite drought resistance measure D, thereby allowing more accurate evaluation of drought resistance indicators; the greater the D-value, the stronger the drought resistance (Table 7). Depending on the D-value, drought resistance varied with soil moisture. In the case of CK treatment, the first three indicators capable of expressing drought resistance of B. ischaemum were root-to-stem ratio, stable isotope ratio of coarse roots (δ13CCR), and specific root length, respectively; in the case of MS treatment the first three indicators were isotope ratio of new leaves (δ13CNL), isotope ratio of coarse root (δ13CCR), and root length, respectively; as to SS treatment, the first three indicators were isotope discrimination of new leaves (Δ13CNL), mass ratio of new leaves to old leaves, and root-to-shoot ratio, respectively. This also suggests that there is an optimal indicator expressing drought resistance of B. ischaemum, and the optimal indicator varies with moisture treatment.


Table 7. Changes in B. ischaemum membership function analysis and performance evaluation of drought resistance indexes under different moisture conditions.


Drought Stress Adaptation Strategy of B. ischaemum Morphological and Physiological Characteristics

A plant adapts to prolonged drought stress via changes in the root system morphological conformation, photosynthetic product allocation to aboveground, and underground portions, and more efficient utilization of the limited soil water. First to perceive soil moisture variation is the plant's root system, which adapts by regulating its own morphological, physiological, and biochemical characteristics. This plasticity of root system morphology in relation to its soil environment in turn influences a plant's absorption and utilization of soil moisture and nutrients and further affects growth of and biomass allocation to the aboveground portion of the plant (Sun and Zhang, 2002; Chen et al., 2012). Other scholars have proposed a “source-sink” relation in plant photosynthetic product allocation, wherein leaves are the “source” and roots are the “sink” of plant photosynthetic products; the source organ acquires the assimilation product (carbohydrate) through photosynthesis and delivers it to the sink organ via the stem, so that the individual plant grows in proportion. Such “source-sink” relationships vary with species, with CO2 concentration, as well as with drought stress intensity and duration (Fernández et al., 2002; Xu et al., 2005); for example, when the root system grows to reach a water source, the root and shoot compete for carbohydrates and most assimilation products are allocated to the root system, resulting in a higher root-to-shoot ratio (Xu et al., 2003; Wei et al., 2005). In this study we found that under serious drought stress, total root length, total root surface area, and root-to-shoot ratio of B. ischaemum increased significantly, and fine-root biomass was significantly greater than coarse-root biomass (Table 2). These results suggest that B. ischaemum adapts to drought stress by developing the organ (root) that allows its growth and reproduction and correspondingly reduces photosynthetic product allocation to other organs (stem and leaves), in support of the “source-sink” balance proposal. Root-to-shoot ratio increased significantly under SS treatment (Figure 1), suggesting that the plant intensifies transport of photosynthetic products from the “source” organ to the “sink” organ, thus amplifying the sink organ's share of photosynthetic product so as to adapt to the arid environment.

Marcelis and Heuvelink (2007) held that soil nutrients and moisture might change the pattern of photosynthetic product allocation by influencing organ morphological growth, and the mechanism of functional balance among organs is very complex. The current study showed that B. ischaemum responded to serious drought stress by allocating carbon flowing from the leaf “source” into the root system “sink” but utilized the carbon primarily to grow fine (lateral) roots and not coarse (taproot) root. A likely explanation is that the sensitivity of fine roots to nutrients and moisture is greater than that of taproot; indeed, the chief physiological function of fine roots is to absorb nutrients and moisture, whereas the taproot's main role consists of transport and support (Mei et al., 2006). Such non-uniformity of “sink” carbon allocation follows the principle of individual plant allocation optimization (Niklas, 2006); as a result, fine-root biomass increased while coarse-root biomass decreased.

A plant's root system also influences its WUE by varying morphological characteristics and biomass, so as to adapt to an arid environment (de Dorlodot et al., 2007; Jia and Zhang, 2008). It is commonly observed that, size, depth, and density of root system are positively correlated with drought resistance (Passioura, 1983; O'Toole and Bland, 1987; Blum and Sullivan, 1997); however, recent studies of the relationship between crop root systems and WUE show that an excessively large root system correlates negatively with aboveground yield, in that the oversized root system competes with fruit-bearing organs for photosynthetic product, consequentially leading to reduction in crop yield. This study analyzed the correlation between the morphological characteristics of the B. ischaemum root system and WUE; we found that all morphological characteristics of the B. ischaemum root system correlated significantly with WUE, and regression curves had basically similar trends and exhibited a quadratic relation (Figure 2). However, correlation levels differed and can be ranked as follows, in descending order: specific root length (R2 = 0.9514, P < 0.01) > total root length (R2 = 0.9041, P < 0.01) > total root surface area (R2 = 0.5277, P < 0.01) > specific root surface area (R2 = 0.4288, P < 0.01). Here, total root length and total root surface area had similar changing trends; the changing trend of specific root length and specific root surface area was opposite that of root length and root surface area, but each of the root system properties relative to WUE showed a peak. When a morphological indicator of root system properties exceeded the peak, WUE fell conversely; hence it is incorrect to assume that a larger and denser root system always promises better drought resistance. From the perspective of optimizing yield and moisture utilization, a plant subjected to limited water resource must have an appropriately sized root system. Furthermore, under serious drought stress, the correlation between WUE and root system morphological characteristics (i.e., root length and surface area, specific length, and specific surface area) of B. ischaemum was better than that between WUE and biomass, also indicating that, compared with root system biomass alone, root system morphological conformation and contribution rates of biomass allocated to fine root and coarse root appear to make more sense for maintenance of a high WUE.


Figure 2. The relation between root traits and WUE. Relationship between four root traits and water use efficiency in B. ischaemum. (A) Root length; (B) root area; (C) specific root length; (D) specific root area. The line in each panel is the best- fit function of root traits and WUE.

Correlation of B. ischaemum Drought Resistance Indicators and Screening of Drought Resistance Expression

First, as to WUE and stable carbon isotope characteristics of B. ischaemum, WUE is expressed here as a ratio of the photosynthetic rate of leaves to its transpiration rate. To make full use of moisture, a plant often responds to exacerbated drought stress by closing its stomata, reducing stomatal conductance, and lowering transpiration rate; the ensuing decline in intercellular CO2 concentration results in less availability of CO2 for selective absorption by the plant, with the consequence that the δ13C value increases and Δ13C value decreases (Chaves et al., 2002; Wingate et al., 2010). Yao et al. (2015) found that the δ13C value of Quercus liaotungensis increases with increasing drought stress; Zhang et al. (2014) concluded from a study of Ipomoea batatas (sweet potatoes) that the Δ13C value falls with decreasing soil moisture; Chen et al. (2014) demonstrated that, with increasing water deficit under drought conditions, δ13C values of Isatis indigotica and Semen cassia obtusifolia increase significantly and Δ13C values of both plants decrease significantly. For B. ischaemum, which is a C4 plant, the relation of Δ13C versus WUE in photosynthesis engineering is:

WUE=Ca(b1+ϕb2Δ13C)1.6ν(b1+ϕb2a)    (3)

where Δ13C is carbon isotope discrimination of each organ of B. ischaemum, a is carbon isotope discrimination value arising out of the CO2 diffusion process, b1 is the discrimination generated by gaseous CO2 through phosphoenolpyruvate carboxylase fixation, b2 is the discrimination of ribulose-bisphosphate carboxylase with respect to 13C, ψ denotes the proportion of CO2 released from a bundle sheath to mesophyll cells, Ca is concentration of CO2 in air (Ci is intercellular CO2 concentration of B. ischaemum leaf), ν is vapor pressure deficit (where ν = μ(1–RH), μ is vapor pressure of air, RH is relative humidity of air), and 1.6 is the conversion coefficient between stomatal conductance to air and that to CO2.

In theory, WUE is negatively correlated with Δ13C, and this study shows that the correlation coefficient between WUE of B. ischaemum and Δ13C of leaves was −0.531 (Table 3), exhibiting a highly significant negative correlation (P < 0.01). Meanwhile, WUE and δ13C of leaves exhibited a highly significant positive correlation—-a finding that is consistent with those of other studies showing that leaf Δ13C is more appropriately used to study a plants' relation to WUE, and is corroborated by other studies of C4 plants (Zhang et al., 2009; Wingate et al., 2010). Therefore, by determining δ13C or Δ13C value of C4 plant leaves, it is likewise feasible to judge moisture utilization of B. ischaemum under drought conditions.

Second, biomass usually serves as an indicator reflecting plant growth, and previous studies on growth and WUE demonstrate that WUE for a plant under an arid environment correlates positively with root-to-shoot ratio and negatively with both aboveground and total biomass (Saraswathi and Paliwal, 2011; Chen et al., 2014). We found in this study that WUE indeed correlated positively with root-to-shoot ratio under MS treatment (Table 4), in agreement with the results of previous studies; however, under SS and CK treatment, WUE of B. ischaemum correlated negatively with root-to-shoot ratio, reflecting the result of the quadratic curves we created of WUE vs. root system morphological characteristics under different drought stress treatment conditions; that is, root system morphological characteristics relative to WUE had a peak, and WUE would decline when root system growth became redundant. Under serious drought stress, the root-to-stem ratio of B. ischaemum increased significantly; this suggests that a plant improves WUE of the whole plant by reducing biomass allocation to stem and increasing root system growth, so as to adapt to the arid environment. We also found that, δ13CNL and Δ13CNL of B. ischaemum correlated very significantly with root-to-shoot ratio and root-to-leaf ratio, with respective correlation coefficients of −0.61 and 0.54 (P < 0.01), suggesting that it is likewise feasible to use δ13CNL and Δ13CNL to study their relations with growth indicators such as root-to-shoot and root-to-leaf ratios.

Third, unlike with use of δ13CNL and Δ13CNL to express plant WUE and biomass, δ13CS and Δ13CS of B. ischaemum were most correlated with root system morphology (P < 0.05), and only under the drought stress treatments (the MS and SS treatments) could root system morphology be significantly correlated with WUE. According to the hypothesis of “source-sink” relations in photosynthetic product allocation, during the plant germination phase the root system is the main sink, and after the plant receives illumination, leaves become the main carbon source; thereafter, the root system loses its dominant role and the stem portion becomes the main sink. During different phases of plant growth, the intensity of each sink differs, so that the allocation pattern of plant photosynthetic products also changes (Marcelis and Heuvelink, 2007). Sampling time in this study was the flowering phase of B. ischaemum, and during that growth phase sink intensity gradually migrated from root system to the stem; thus, it is also feasible to represent root system morphology via stable isotope value and isotope discrimination of the stem.

In general, δ13CNL and Δ13CNL could be used to characterize plant WUE and biomass, while 13CS and Δ13CS could express root system morphological characteristics. This corroborates our proposal in the introduction: The stable isotope approach can provide a quick and easy method to selectively breed plants with good growth, high WUE, and reasonably structured root system in the Loess Plateau under limited moisture conditions. However, breeders using the stable isotope approach must consider the influence on the final result of carbon fractionation among the sampling organ and various organs.

Finally, we found from the above analysis that mechanisms of plant drought resistance are complex and variable, and the influential indicators also mutually interacted, so reasonable selection of indicators is a key to drought resistance identification (Li et al., 2014). Previous researchers have used this method mostly to compare differences in drought resistance between crop varieties, between clonal varieties of the same plant, or between shrub species (Dai et al., 2016; Liu et al., 2016; Qiu et al., 2014). Based on this information, we selected 21 drought-related indicators (growth, morphology, and physiology) of B. ischaemum under different drought stress conditions and used the membership function approach and PCA to obtain measures of drought resistance (D-value). This method not only integrated relations among indicators but also considered the importance of each indicator; by comparing D-values, we screened for the optimal indicator that expresses drought resistance of B. ischaemum under different drought stress conditions.

Our study found that (Tables 6, 7), when moisture supply was sufficient, the growth, morphological, and physiological indicators most indicative of B. ischaemum drought resistance were root-to-stem ratio, specific root length, and δ13CCR; when moisture stress was mild, the morphological and physiological indicators most indicative of drought resistance were the root length, δ13CNL, and δ13CCR; when moisture stress was serious, the physiological and growth indicators most indicative of drought resistance were δ13CNL, root-to-shoot ratio, and ratio of new leaves to old leaves. These results only partially support our original proposal that we could identify an optimal indicator expressing drought resistance of B. ischaemum. Under each of the three moisture treatment conditions we found different optimal indicators expressing growth, morphology, and physiology of B. ischaemum; therefore, we provide here a theoretical reference for screening plant drought resistance indicators under different moisture conditions in the Loess Plateau. However, the difficulty we experienced in finding a single optimal indicator indicating plant drought resistance suggests that plant anti-drought mechanisms differ under various moisture conditions. In light of this difficulty, further in-depth study will be required to determine the specific plant and environmental characteristics that trigger the physiological, morphological, and growth changes we measured herein under varying conditions of B. ischaemum drought stress.

Difference in Carbon Isotope Composition of Each Organ of B. ischaemum

Many researchers have performed carbon isotope fractionation analysis of different organs of C4 plants such as corn (Zhang et al., 2009), C3 plants such as sweet potatoes (Zhang et al., 2014), and aerobic rice (Zhao et al., 2004), finding that δ13C values of all organs of C3 plants differed significantly, whereas δ13C differences between leaf and stem in C4 plants were insignificant; both seeds and root systems of C3 and C4 plants were more prone to 13C enrichment than their leaves and stems. ANOVA of the current study (Figure 3) showed that differences in δ13C and Δ13C values among organs under CK and MS conditions reached significant levels, whereas the differences among organs under SS treatment were insignificant, probably because different moisture treatment conditions influenced 13C fractionation of B. ischaemum. To summarize the differences among organs, the differences in Δ13C values among stem, new leaves, and old leaves were insignificant (Table 2); 13C fractionation did not occur between leaves and stem of B. ischaemum, but Δ13C values of both stem and leaves were significantly greater than those of root, suggesting that 13C fractionation had occurred between root and foliage. The root system is the “sink” organ of a plant, and its carbon undergoes the combined effects of environmental and metabolic factors during accumulation. Brugnoli and Farquhar (1998) and Leavitt and Long (1986) proposed three causes for 13C fractionation of a plant: First, variation in chemical composition of each organ leads to 13C fractionation, in that every chemical component has its own stable δ13C value; a higher cellulose content in an organ is more prone to 13C enrichment, and the higher the lignin and fat content, the lower the 13C content. Second, the physiological and ecological characteristics of plant organs differ extensively. Therefore, secondary fractionation of 13C might occur during carbohydrate synthesis; during carbohydrate export, loading, and unloading via phloem; and during transport of photosynthetic product from the “source” to the “sink.” Third, respiration characteristics of different organs differ greatly; because plant organs tend to utilize 12C in respiration, 13C is enriched in tissue. Therefore, comparisons of δ13C and Δ13C values between plants will require specific analysis of results from different organs of each individual plant.


Figure 3. Carbon isotope ratio and carbon isotope discrimination of various plant organs under different water treatments (A) Mean carbon isotope ratio of various plant organs; (B) Mean carbon isotope ratio of different water treatments; (C) Mean carbon isotope discrimination of various plant organs; (D) Mean carbon isotope discrimination of different water treatments. Lowercase letters indicate significant difference between different water treatments at the 0.05 level. Capital letters represent significant difference among different organs at 0.05 level.

Author Contributions

PL and YL conceived and designed the experiments. GX, LX performed the experiments. ZR and ZL analyzed the data. YL wrote the manuscript.


This research was funded by the National Natural Science Foundation of China (No. 41471226, No. 41271290, and No. 41330858), National key research and development program (No. 2016YFC0402404) and the School foundation of Xi'an University of Technology (310-252071506).

Conflict of Interest Statement

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.


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Keywords: Bothriochloa ischaemum, stable carbon isotope, root morphology, water use efficiency, drought stress

Citation: Liu Y, Li P, Xu GC, Xiao L, Ren ZP and Li ZB (2017) Growth, Morphological, and Physiological Responses to Drought Stress in Bothriochloa ischaemum. Front. Plant Sci. 8:230. doi: 10.3389/fpls.2017.00230

Received: 18 October 2016; Accepted: 06 February 2017;
Published: 24 February 2017.

Edited by:

Patrick H. Masson, University of Wisconsin-Madison, USA

Reviewed by:

Michael Vincent Mickelbart, Purdue University, USA
Guoliang Wang, Institute of Soil and Water Conservation (CAS), China

Copyright © 2017 Liu, Li, Xu, Xiao, Ren and Li. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Peng Li,