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Foliar δ13C response patterns along a moisture gradient arising from genetic variation and phenotypic plasticity in grassland species of Inner Mongolia

Authors


Correspondence

Haishan Niu, College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, 100049, China. Tel: +86 10 88256371; Fax: +86 10 88256415; E-mail: niuhs@ucas.ac.cn

Abstract

Plants depend upon both genetic differences and phenotypic plasticity to cope with environmental variation over different timescales. The spatial variation in foliar δ13C levels along a moisture gradient represents an overlay of genetic and plastic responses. We hypothesized that such a spatial variation would be more obvious than the variation arising purely from a plastic response to moisture change. Leymus chinensis and Stipa spp. were sampled from Inner Mongolia along a dry-wet transect, and some of these species were transplanted to an area with a moisture gradient. For Stipa spp., the slope of foliar δ13C and mean annual precipitation along the transect was significantly steeper than that of foliar δ13C and mean annual precipitation after the watering treatment. For L. chinensis, there was a general decreasing trend in foliar δ13C under the different (increasing) watering levels; however, its populations showed an irregular relationship between foliar δ13C and moisture origin. Therefore, support for our hypothesis was obtained from Stipa spp., but not from L. chinensis.

Introduction

Foliar δ13C is a well-documented surrogate of long-term water-use-efficiency (WUE), which is determined by both photosynthesis and transpiration. Since factors that affect either of these two processes also have effects on WUE, WUE is considered an integrated measure of physiological status and environmental conditions (Farquhar et al. 1989). Extensive evidence indicates a geographic pattern, particularly at large spatial scales, of decreasing δ13C with increasing moisture in plants, although the explanation for this pattern varies across studies (Schulze et al. 2006; Wittmer et al. 2008; Luo et al. 2009; Diefendorf et al. 2010).

Both genetic factores and plasticity could contribute to the above-mentioned spatial pattern (Kohorn et al. 1994; Lauteri et al. 2004; Corcuera et al. 2010). Several studies have suggested the existence of a plastic response in many plants that show a decrease in δ13C with an increase in moisture (for example, as a result of irrigation or rainfall) (Brock and Galen 2005; Hausmann et al. 2005). In addition, there are reports on genetic determination for the observed patterns of δ13C increase with climatic aridity (Comstock and Ehleringer 1992). Being a quantitative trait that is subjected to continuous genetic variation, WUE (and its long-term surrogate, δ13C) is under the influence of both genetic and environmental factors (Chen et al. 2011). WUE, or δ13C, reflects the balance between the photosynthesis rate and stomatal conductance. With an increase in water availability, the reduction in the number of stomata, which are the limiting factors for photosynthesis, results in decreased levels of δ13C (Diefendorf et al. 2010), and this mechanism is expected to hold true across all timescales.

If the above-mentioned genetic pattern holds true, xeric-adapted populations might be able to genetically maintain a higher level of foliar δ13C than mesic-adapted populations, even under the same moisture conditions. However, if the plastic response holds true, lower/higher foliar δ13C might be observed when moisture is below/above the average. It might be speculated that, if both the genetic and plastic patterns hold true, the variation in foliar δ13C observed along a spatial moisture gradient would be more obvious than the variation arising purely from a plastic response to moisture change.

Materials and Methods

Studied species

The species studied were Leymus chinensis and Stipa grandis. L. chinensis has long been identified as an euryhydric species, which occupies large areas as a dominant or co-dominant species in eastern parts of the Eurasian Steppes (Siberia, Mongolia, far-east Russia, Northern China and Korea) and thrives in a diverse range of habitats (Liu et al. 2007) (The Integrated Investigation Team in Inner Mongolia and Ningxia, CAS 1985). Throughout its geographic range, L. chinensis coexists with Stipa spp., alternately dominating communities, from the drier (western) “desert steppe” to the wetter (eastern) “meadow steppe”. In contrast to L. chinensis, however, each species of the Stipa genus has a limited distribution. In the middle part of the geographic range of L. chinensis, the most abundant species of Stipa is S. grandis, and the communities dominated or co-dominated by S. grandis are often named “typical steppe” (The Integrated Investigation Team in Inner Mongolia and Ningxia, CAS 1985; CAS).

Field investigation

In 2009, 12 sites were selected from west to east along a precipitation gradient in Inner Mongolia (Fig. 1 and Table S1). At each site, a baseline was first specified (by observation) along the direction presumed to represent maximum environmental variance. Next, mature leaves of L. chinensis and Stipa spp. were collected at six points (replications) along the line. The distance between two neighboring points was 10 m. Leaves were killed by subjecting them to microwaves immediately after collection and air-dried until an oven was available.

Figure 1.

Locations of the transplantation sites along the transect in Inner Mongolia in 2009. Sites are shown as closed black circles and are numbered I to XII along the transect. The five transplantation sites are labeled as follows: Mandulatu (MDLT); Xilinhaote (XLHT); Maodeng Grassland Ecological Research Station (MGERS); Xiwuqi (XWQ); and Huihe (HH).

Mean annual precipitation (MAP) at each site was established by linear interpolation of 40 weather stations distributed along the transect. MAP was computed for each station between 1950 and 2002.

Common garden experiment

In all five sites were chosen along the transect: Mandulatu (MDLT: 43°43.212′N, 113°31.640′E); Xilinhaote (XLHT: 44°01.313′N, 116°12.433′E); Xiwuqi (XWQ: 44°28.759′N, 117°15.977′E); Huihe (HH: 48°46.792′N, 119°27.825′E), and Maodeng Grassland Ecological Research Station (MGERS: 44°10.711′N, 116°27.467′E). MDLT is located in the desert steppes; XLHT, XWQ, and MGERS in the “typical” steppes; and HH in the meadow steppes. A total of 120 ramets of L. chinensis were transplanted to our field experimental site at MGERS, located in the middle part of Inner Mongolia, China, from the other four sites within a maximum of 3 days. A total of 108 bunches of S. grandis were collected from XWQ alone, because these plants were not found at MDLT, XLHT, and HH. These bunches of S. grandis were immediately transplanted to our field experimental site at MGERS.

For the common garden experiment, 12 plots (2 m × 2 m) were set up, and 49 holes (diameter: 15 cm; depth: 40 cm; layout: 7 × 7 matrix) were evenly dug in each plot by using a soil corer. Ten ramets of L. chinensis and nine bunches of S. grandis from each transplantation site were randomly selected and inserted into the holes.

Up until the end of the growing season in late September 2009, all the transplanted ramets (for L. chinensis) or bunches (for S. grandis) were watered to ensure their survival. In 2010, four levels of watering treatments (0, 100, 200 and 300 mm) were randomly assigned to the 12 plots, with three replications for each level. The amount of water for each level was evenly applied 10 times during the growing season, from June 13 to September 3. No treatment was applied if natural rainfall occurred during the growing season.

After the treatment for one season, mature leaves were collected in late September 2010. The local L. chinensis and S. grandis plants growing in each plot were also harvested. L. chinensis samples collected from MDLT, XLHT, MGERS, XWQ, and HH were defined as L-1, L-2, L-3, L-4, and L-5, respectively. S-3 and S-4 denote the S. grandis samples from MGERS and XWQ.

Carbon isotope measurement

All plant materials were dried at 65°C and ball-milled (MM200, Fa. Retsch, Haan, Germany) for δ13C measurement by using an IsoPrime100 Stable Isotope Ratio Mass Spectrometer (Isoprime Ltd, U.K). Stable isotope abundances are reported as:

display math

where R is the 13C/12C ratio of either the sample or the standard (Pee Dee belemnite, PDB). The standard deviation of repeated measurements of laboratory standards was ±0.15‰.

Data analyses

All statistical analyses were performed using R 2.10.0 (R Development Core Team 2009). Correlation between foliar δ13C and precipitation was tested by linear regression. Differences among regression slopes were determined using Standardised Major Axis Tests & Routines (SMATR), a freely available program (Falster et al. 2006). In the field investigation, two-way analysis of variance (ANOVA) was used to test the species and sites on foliar δ13C values. The effects of the transplanting site (origin) and watering level (environment) on foliar δ13C values in the common garden experiment were analyzed using the linear model VP = VO + VE + VO×E + Verr, where VP denotes the total variance in δ13C; VO is the origin variance; VE is the environmental variance (i.e., watering-induced variance); VO × E is the interaction between origin and environment; and Verr is the variance of residuals (Strand and Weisner 2004; Pigliucci 2005). Tukey's method was used for a multiple comparisons of the populations of L. chinensis.

Results

Foliar δ13C of L. chinensis and Stipa spp. along the transect

The slope of the regression between δ13C and MAP was extremely significant for Stipa spp. (= 1.219E−5), whereas it was almost significant for L. chinensis (= 0.068; Fig. 2). L. chinensis had a lower (more negative) foliar δ13C level than Stipa spp. (paired t-test, P = 0.012). The two-way ANOVA results for the transect experiment indicated an extremely significant species×site interaction (= 2.998E−7), where Stipa spp. were considered to be a “species”.

Figure 2.

Response of foliar δ13C to mean annual precipitation for Leymus chinensis (open circles) and Stipa spp. (crosses) from middle to eastern Inner Mongolia, China. The three asterisks (***) denote a statistically significant regression slope at the α = 0.001 level, whereas “ns” means “not significant at the α = 0.05 level”. The dotted line represents Stipa spp. and the solid line one represents L. chinensis.

Intra-species responses of foliar δ13C to watering

As shown in Fig. 3, foliar δ13C level generally decreased under the different (increasing) watering levels for L. chinensis samples of different origins. The P-values of the slope tests for L-1, L-2, L-3, L-4, and L-5 were calculated as 0.005, 0.118, 0.000, 0.110 and 0.238, respectively (Fig. 3).

Figure 3.

Response pattern of foliar δ13C to different precipitation conditions for Leymus chinensis from different origins. L-1, L-2, L-3, L4, and L-5 denote L. chinensis transplanted from MDLT, XLHT, MGERS, XWQ, and HH, respectively. Each point is the mean foliar δ13C ± 1SE.

Since origin was found to be a significant factor according to the two-way ANOVA results for both the species (L. chinensis,= 0.012; S. grandis,= 0.011), multiple comparisons were conducted using Tukey's method. L-1, which originated from the desert steppes, had significantly lower foliar δ13C level than those in L-2, L-3 and L-4. Although the P-value was lower, the difference in foliar δ13C level between L-1 and L-5 was not statistically significant (= 0.113). Despite origin having a significant effect on foliar δ13C in L. chinensis, the effect was not linear. L-1 had the lowest foliar δ13C value in three out of the four watering levels (Fig. 4a).

Figure 4.

Effects of origin on foliar δ13C for (a) Leymus chinensis and (b) Stipa grandis along the moisture gradient. L-1, L-2, L-3, L4, and L-5 denote L. chinensis transplanted from MDLT, XLHT, MGERS, XWQ, and HH, respectively, with the number increasing relative to a decrease in aridity of the habitat. S-3 and S-4 denote S. grandis transplanted from the same habitats like L-3 and L-4, respectively. Error bars are ±1SE.

It is worth noting that origin had a consistent effect across species, if only L-3, L-4, S-3 and S-4 were considered. The habitat of S-3 was drier than that of S-4, and δ13C values for S-3 were higher than those for S-4 under all watering levels (Fig. 4b). Similar results were noted for L. chinensis species, L-3 and L-4 (Fig. 4a).

Comparison of the response pattern between the transect and watering experiments

The P-values of the slope tests for watering ewperiments on S-3 and S-4 were not significant (= 0.049 and 0.005, respectively) and hence they were combined to form one slope for S. grandis. The combined slope was calculated as −0.006952‰·mm−1, which differs significantly from zero (= 0.008). The slope between δ13C and MAP for Stipa spp. in the transect experiment was −0.019319‰·mm−1, which also differed significantly from zero (= 0.000, Fig. 2). The two slopes, the combined slope obtained from the watering experiment and the other slope based on the transect sampling, differed significantly (= 0.001; Fig. 5).

Figure 5.

Response pattern of foliar δ13C to the different precipitations for Stipa grandis from different origins. S-3 and S-4 denote S. grandis transplanted from MGERS and XWQ, respectively. Each point is the mean foliar δ13C ± 1SE.

Discussion

Stipa spp. is generally more conservative than L. chinensis across the transect along which they coexist (Fig. 2). The combined slope of foliar δ13C and MAP for Stipa spp. along the transect (−0.0193) was very close to the “universal” slope for all C3 species reported by Prentice et al. (2011): −0.014. After converting δ13C to 13Δ, the combined slope for Stipa spp. (0.0193) was also close to the value of 0.0100‰/mm, or 0.0105 (13Δ/MAP), as reported by Wittmer et al. (2008). The slightly greater value of our slope might be attributed to the selection of the sampling area in our study that extended further toward the east, including the wet-adapted S. baicalensis.

The slope of foliar δ13C and MAP for Stipa spp. across the transect represents the effects of both genetic and phenotypic plasticity (Fig. 2), whereas the slope of δ13C and watering in the common garden experiment represents only the plastic response (Fig. 5), the former is significantly steeper than the latter. A plausible explanation for this is that, in addition to the plasticity pattern that has arisen (as seen in Fig. 5), there was a genetically determined pattern of foliar δ13C. Similar to other species reported in previous research (Comstock and Ehleringer 1992; Zhang et al. 1993; Dudley 1996), Stipa populations have a tendency to show increased foliar δ13C with aridity of their original environment, even under common conditions. Since under natural conditions, xeric-adapted populations are generally exposed to less moisture than mesic-adapted populations, a plastic response would further increase the foliar δ13C levels.

On the other hand, the genetic and plastic patterns differed in L. chinensis. The plasticity response pattern showed a linearly negative relationship between foliar δ13C and water availability (Fig. 3), which was similar to that noted in S. grandis (Fig. 5). However, the genetically determined response pattern was unique to L. chinensis. Populations derived from a moderately arid environment (sites with average MAP) were thought to show the highest foliar δ13C, whereas those (L-1) derived from the dryer end of the transect (site with the lowest MAP) maintained consistently lower δ13C values (Fig. 4). Although a significant relationship between δ13C and moisture availability was observed in L. chinensis, the particular (irregular) pattern in intrinsic δ13C among populations reduced the significance of the spatial relationship between δ13C and MAP (Fig. 2).

The nonlinear response pattern underlying the genetic variation of L. chinensis could explain the lack of agreement among previously published results. Chen et al. (2002) reported a negative relationship between δ13C and soil moisture for L. chinensis, this assessement was performed in plants sampled along an environmental gradient in the Xilin river basin. A similar relationship between δ13C and MAP for L. chinensis was observed by Su et al. (2000) along the North-East China Transect (NECT). On the basis of the results obtained from 171 species sampled along the NECT, Prentice et al. (2011) proposed a universal scaling relationship between δ13C and aridity, which persists both within and across species. Although most species in their study followed this universal pattern, L. chinensis was one of the two exceptions that showed a reverse relationship to that shown in Fig. 8 in Prentice et al. (2011). This exception could be explained by the unique genetic pattern of L. chinensis. Su et al. (2000) and Chen et al. (2002) sampled L. chinensis from the middle to eastern region of the NECT, while Prentice et al. (2011) sampled this species from the western region of the NECT.

In conclusion, in spite of the evidence for a genetic response pattern unique to L. chinensis, the underlying mechanism remains unknown and warrants further research.

Acknowledgements

This work was supported by the National Natural Science Foundation of China (40871032) and the Bureau of Science and Technology for Resources and Environment, Chinese Academy of Sciences (KZCX2-EW-QN604). We thank the Board of the Maodeng Grassland Ecological Research Station for providing the experimental field site and accommodation.

Conflict of Interest

None declared.

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