- Research article
- Open Access
Elevated CO2 can modify the response to a water status gradient in a steppe grass: from cell organelles to photosynthetic capacity to plant growth
© The Author(s). 2016
Received: 31 May 2016
Accepted: 6 July 2016
Published: 12 July 2016
The atmospheric CO2 concentration is rising continuously, and abnormal precipitation may occur more frequently in the future. Although the effects of elevated CO2 and drought on plants have been well reported individually, little is known about their interaction, particularly over a water status gradient. Here, we aimed to characterize the effects of elevated CO2 and a water status gradient on the growth, photosynthetic capacity, and mesophyll cell ultrastructure of a dominant grass from a degraded grassland.
Elevated CO2 stimulated plant biomass to a greater extent under moderate changes in water status than under either extreme drought or over-watering conditions. Photosynthetic capacity and stomatal conductance were also enhanced by elevated CO2 under moderate drought, but inhibited with over-watering. Severe drought distorted mesophyll cell organelles, but CO2 enrichment partly alleviated this effect. Intrinsic water use efficiency (WUEi) and total biomass water use efficiency (WUEt) were increased by elevated CO2, regardless of water status. Plant structural traits were also found to be tightly associated with photosynthetic potentials.
The results indicated that CO2 enrichment alleviated severe and moderate drought stress, and highlighted that CO2 fertilization’s dependency on water status should be considered when projecting key species’ responses to climate change in dry ecosystems.
The IPCC’s Fifth Assessment Report (AR5) showed that atmospheric carbon dioxide concentration had increased by 40 % since the pre-industrial era, reaching ~390 μmol mol−1 in 2011. It is predicted to rise to 500 μmol mol−1, perhaps even above 900 μmol mol−1, by the end of this century. Continued emissions of greenhouse gases will cause further warming and precipitation changes . The effects of elevated CO2 concentration (elevated CO2) and climatic change on plants—from the molecular basis to physiological processes, individual growth, and vegetation productivity aspects—have attracted considerable attention for several decades (e.g., [2–6]).
Many studies have reported the biological responses of plants to CO2 enrichment and its interactions with other environmental factors (e.g., [3, 4, 6]). The effects of elevated CO2 include enhanced net photosynthesis rate (A net), down-regulated stomatal conductance (g s) [3, 7–9], dilution of chemical elements , imbalance of sink–source relationships [11, 12], increased plant growth and vegetation productivity [2, 13], changes in species competition interactions and community structure [13–15], and lengthened growing seasons . However, these elevated CO2-induced changes might be mediated by other environmental factors, particularly changes of water availabilities. Severe drought adversely affects plant growth, gas exchange, and photosynthetic activity , but elevated CO2 might partly alleviate the harmful impact of water deficit stress on these biological processes, and even survival [18–21]. Elevated CO2 can enhance plant resistance to water deficit stress by mitigating oxidative damage, maintaining A net and decreasing g s, and improving the plant water status, thereby raising the water use efficiency (WUE) [4, 21–24]. Under moderate water stress, a marked stimulation occurs due to elevated CO2 [22–26]. However, over-watering can reduce, or even reverse this stimulation [27–30]. Nevertheless, few studies on the combined effects of elevated CO2 and a water status gradient have been conducted, particularly on multiple scales.
Agropyron cristatum (L.) Gaertn, or crested wheatgrass, a C3 species, is a dominant species in the steppe regions of Central Asia, and is also widespread in western North America [31, 32]. It is a perennial herb native to North China with good palatability and high forage value. Moreover, its prosperity is recognized as an indicator of degradation of the steppe ecosystem in the context of overgrazing and adverse climate change. For instance, degradation might initially occur if crested wheatgrass thrives relative to other dominant species such as Leymus chinensis and Stipa grandis . Thus, this species is crucial for assessing the vulnerability and restorative capacity of the semiarid region, as well as forage resource management. These temperate grasslands, which are dominated by several major grasses including A. cristatum, have been severely degraded during recent decades because of adverse climatic change and improper land use [34–37]. Although this arid region is projected to become drier and hotter, excessive precipitation events may occur more frequently [38, 39]. This would further threaten the ecosystem function including dominant species growth and survival [36, 37, 40]. The leaf-level instantaneous responses of A net, g s, and WUE to elevated CO2 have been quite well investigated [4, 6, 8]. To our knowledge, however, few prior efforts have been made to examine the effects of elevated CO2 under a wide-ranging water status gradient (seven watering treatments from extremely severe deficit to relative over-watering) (but see Manea and Leishman, ), particularly integrating multiple variables from organelle structure to physiological processes, individual morphology and structure, biomass allocation, and plant growth aspects. In this experiment, structural and physiological traits were examined to find sensitive indicators, and to summarize the adaptive strategy of A. cristatum to climatic changes. The objective of the current study was to test the hypotheses: (1) elevated CO2 modifies the effects of soil water status on the dominant species, with stimulation in a moderate range of water status changes, no positive response with over-watering, but an alleviation of damage from severe water deficit; and (2) associated responses co-occur at the mesophyll cell ultrastructure, photosynthetic physiological activity, plant growth and structure levels under elevated CO2 and different water conditions.
Each PVC plastic pot (9.7 cm in diameter, 9.5 cm in height, 0.70 L) was filled with 0.68 ± 0.01 (±SE, n = 60) kg of dry soil, and planted with four plants per pot. The soil was retrieved from the local soil surface (0–30 cm), and A. cristatum seeds were collected the year before the experiment from the local steppe—a typical grassland ecosystem in Xilinhot (43°38′N, 116°42′E, 1100 m a.s.l.), Inner Mongolia, China. The soil was a castanozem type, with a medium texture containing 29.0 %, 31.2 %, and 39.8 % clay (<5 μm particle diameter), silt (5–50 μm), and sand (>50 μm), respectively. The soil organic carbon, total nitrogen, and available nitrogen concentrations were 12.31 ± 0.19 g kg−1, 1.45 ± 0.02 g kg−1, and 81.61 ± 0.71 mg kg−1, respectively. The soil water field capacity (FC) and permanent wilting point were 25.8 and 6.0 % (w/w), respectively, and the gravimetric bulk density was 1.21 g cm−3. With a mean annual temperature of 2.95 °C and mean annual precipitation (MAP) of 266 mm over the past 30 years, this region is characterized by a continental temperate climate with a dry, frigid winter (−18.6 °C lowest mean month temperature in Jan), and a wet, hot summer (21.4 °C maximal mean month temperature in Jul). Most precipitation (88 %) occurs in the growth season from May to Sep. To obtain uniform seedlings [26, 41], all pots were initially placed in a naturally illuminated glasshouse (day/night temperatures of 26–28/18–20 °C) until the third leaf emerged (27 days after sowing), and then transferred into two open-top chambers (OTCs) to subject the plants to two-month watering and increased CO2 concentration treatments. Water was provided by a sprayer at around 17:00 every 3 days according to previous similar experiments [26, 35].
The OTCs were established in a regular hexahedron shape (each side 85 cm wide, 150 cm high) with a top-opening rain shelter on the top and a space below for free exchange of gases between the OTC and ambient atmosphere. Pure CO2 gas (99.999 %) was supplied from a cylinder (Chao Hong Ping Gas Co. Ltd, Beijing, China), and a CO2 gas sensor (eSENSE-D, SenseAir, Delsbo, Sweden) was used to continuously monitor and control the CO2 concentration over 24 h with a data logger (DAM-3058RTU, Altai Sci Tech Dev Co. Ltd., Shang Hai, China). The CO2 concentrations had a ±30 μmol mol−1 change relative to the set points. The air temperature and relative humidity (RH) were monitored using thermocouples (HOBO S-TMB-M006, Onset Computer Co., Bourne, MA, USA) and humidity transducers (HOBO S-SMA-M005) installed at 75 cm height in and out of the chambers, respectively. Climatic data were automatically recorded and collected by a logger (HOBO H21-002) every 30 min during the experiments; day/night temperatures were 28.3 ± 5.7/22.7 ± 4.2 °C and RH was 62.4 ± 4.0 % in the OTCs, which were 1.3/0.5 °C greater and 3.5 ± 2.3 % lower than outside the OTCs. The OTC system has been proven to have acceptable effectiveness, relative availability, and data comparability for assessing the effects of elevated CO2 with climatic change at low cost [42, 43], although data interpretation needs to be cautious in various environmental contexts [44, 45].
The experiment was designed with two factors, two CO2 concentrations (ambient CO2, ~390; elevated CO2, 550 μmol mol−1) and a seven-level precipitation gradient: W−60 (−60 % relative to mean precipitation in the local site over 30 years, as an extreme drought treatment), W−30 (−30 % relative to local mean precipitation), W−15 (−15 % relative to local mean precipitation), W0 (local mean precipitation, the control watering treatment), W15 (+15 % relative to local mean precipitation), W30 (+30 % relative to local mean precipitation, an over-watering treatment relative to the normal local precipitation), and W60 (+60 % relative to local mean precipitation), roughly equaling 147.0, 257.3, 312.5, 367.6, 422.7, 477.9, and 588.1 mm of precipitation during the growth season, respectively. Two OTCs were used, with separate irrigation treatments within each one as a split plot and 3–5 replicates (pots/treatment). A total of 80 plots were included initially; some pots were kept in reserve in case of experimental or plant growth problems. Plants were randomly placed within each OTC initially, replaced every 3 days, and transferred between the two chambers weekly (CO2 target points were switched simultaneously) to minimize any differences between growth chambers except for the desired treatments—CO2 concentration and water status [26, 46, 47].
Soil water status and water use
The soil water content (SWC, g water g−1 dry soil) during the experiment was determined by weighing pots. The soil dry weight (SDW) at sowing was calculated as (TW − PW) × (1- SWC0) at sowing (the SWC0 was determined before sowing by oven-drying soil samples; there was no water drainage because the pots used had no holes, and plant weight was neglected). The SWC during the experiment was expressed as (TW − SDW − PW)/SDW, and the soil relative water content (SRWC) was expressed as SWC/FC × 100. Water use, i.e., actual evapotranspiration during the entire experiment, was derived from a water balance equation; water use = TW at harvest − TW at initial time + applied water amount. Thus, total biomass water use efficiency (WUEt) could be estimated as total plant biomass/water use . TW is the total weight of the pot plus soil at each measurement time; PW is the net pot weight determined before filling with soil; FC is the SWC measured 24 h after fully wetting the soil.
Plant biomass and leaf area
Each plant was separated into four parts, the stem, root, green leaves, and dead leaves, at both the start and end of the experiment, dried at 75 °C to a constant weight, and then weighed to get the biomass. Before drying, plant height, tiller and green leaf numbers were recorded; and green leaf area per plant, and the leaf parts used to determine gas exchange parameters were measured with a WinFOLIA system for root/leaf analysis (WinRhizo, Régent Instruments, Quebec, Canada).
Plant growth analysis
Plant growth analysis was performed following Poorter . The relative growth rate of each individual (RGR, mg g−1 day−1) was expressed as (ln w 2 − ln w 1)/(t 2 − t 1), where w 2 and w 1 are the biomass at final and initial harvest dates, respectively, and t 2 and t 1 indicate the two harvest times. The leaf mass ratio of total plant mass (LMR), stem mass ratio (SMR), and root mass ratio (RMR), as biomass allocation indicators, were expressed as percentages of leaf, stem, and root mass in the total plant mass, respectively. The plant/leaf morphological and structural indicators leaf area ratio (LAR, m2 kg−1; an indicator of the canopy size), leaf area and root mass ratio (LARMR, m2 kg−1; a proxy of the biomass balance between light-intercepting organs and resource element uptake organs), specific stem length (SSL, cm mg−1; a marker of the investment of stem carbon into plant height), and specific leaf area (SLA, m2 kg−1; an indicator of leaf thickness and compactness) were expressed as ratios of leaf area to whole plant mass, leaf area to root mass, stem length to mass, and leaf area to mass, respectively .
Photosynthesis and chlorophyll a fluorescence
Leaf gas exchange and chlorophyll fluorescence were measured simultaneously using an open gas exchange system (LI-6400 F, LI-COR, Inc., Lincoln, NE, USA) combined with a leaf chamber fluorometer (LI-6400-40, LI-COR). Illumination was supplied to the leaves from a red-blue LED light source and the data were initially analyzed with data acquisition software (OPEN 6.1.4, LI-COR). Before measurement, the leaves were acclimated in the chamber for at least 10 min at 26–28 °C with a CO2 concentration of 390 μmol mol−1 and a photosynthetic photon flux density of 1500 μmol m−2 s−1, under which photosynthesis is nearly saturated, to obtain gas exchange parameters such as net light-saturated maximum photosynthetic rate (A sat), g s, transpiration rate (E), and intrinsic water use efficiency (WUEi, A sat/E). We measured at least three each of the youngest and fully expanded leaves from different individuals (one plant per pot) for all replicates, from 9:00 to 16:30 h daily. The vapor pressure deficit (VPD) in the cuvette was maintained at 1.7–2.7 kPa (2.39 ± 0.04, n = 492), possibly reflecting the actual conditions within the OTCs [26, 50]. The steady-state value of fluorescence (F s) was determined, and a second saturating pulse at 8000 μmol m−2 s−1 was imposed to determine the maximal light-adapted fluorescence (F' m). The actinic light was removed and the minimal fluorescence in the light-adapted state (F' 0) was determined after 3 s of far-red illumination. The maximum photochemical efficiency of photosystem II (F v/F m) was determined midnight–predawn in completely dark-adapted leaves with a leaf fluorometer (LI-6400-40) linked to a LI-6400 F gas exchange system. The minimal fluorescence yield (F 0) was determined under low modulated light of 1.0 μmol m−2 s−1, and the maximal fluorescence yield (F m) was obtained with a 0.8 s saturating pulse at ~8000 μmol m−2 s−1. The fluorescence parameters were calculated from the following formulae [51, 52]; the maximal efficiency of photosystem II (PSII) photochemistry is F v/F m = (F m − F 0)/F m, and the efficiency of excitation energy captured by open PSII reaction centers is F' v/F' m = (F' m − F' 0)/F' m.
Estimation of A/C i response curves
To analyze the A/C i response curve to obtain key photosynthetic capacity parameters, a stepwise CO2 concentration gradient was implemented (390, 300, 200, 100, 50, 390, 390, 550, 800, and 1000 μmol m−2 s−1). Note, the third 390 value is not an error, but a trick to easily recover the ambient CO2 level from the lowest point of 50 μmol m−2 s−1. At each CO2 level, the leaves needed 2–3 min to equilibrate, and a match was also run to balance the CO2 and water vapor concentrations between the reference and leaf chambers. Furthermore, to estimate maximum rate of carboxylation (V c,max), maximum rate of electron transport (J max), and rate of thiose phosphate utilization (TPU), a curve-fitting software tool by Sharkey et al.  based on the method of Farquhar et al.  was run to analyze the A/C i response data.
For transmission electron microscopy, 2-mm2 pieces from the middle sections of the youngest and fully expanded leaves were dissected and immediately fixed in 2.5 % (v/v) glutaraldehyde in 0.1 M phosphate buffer (pH 7.0) overnight at 4 °C. The samples were then washed three times with the same buffer and post-fixed in 1 % osmium tetroxide overnight at 4 °C. After being washed in the same buffer, the leaf tissues were passed through an ethanol dehydration series, and then infiltrated and embedded in Spurr’s resin (Agar Scientific, Essex, UK). Sections were cut using an Ultracut R ultramicrotome (Leica, Wetzlar, Germany). The thin sections were stained with 2 % uranyl acetate and lead citrate , and then observed and photographed under a transmission electron microscope (JEM-1230, JEOL Ltd, Tokyo, Japan). For each treatment, three leaf samples were examined, and approximately 130 mesophyll cells were randomly chosen for the observations.
A principal component analysis (PCA) was first conducted to test the relationships among the traits including the plant growth, structural, morphological, biomass allocation, and photosynthetic parameters, and the multivariate patterns of the effects of CO2 concentration and watering treatments alone and in combination [26, 56, 57]. Thereafter, we conducted an analysis of variance (ANOVA) for the plant growth, structural, morphological, biomass allocation, and photosynthetic traits, and the anatomical changes in mesophyll cells and their organelles with GLM Full Factorial Mode to test the main effects of watering, elevated CO2, and their interactions. Where watering treatments had a significant effect based on ANOVA, a multiple comparison was done with Duncan’s multiple range test. A one-way ANOVA was also conducted to test the differences between the two CO2 levels within the same watering treatment. The multiple factorial ANOVA model can be used for unequal variances and data near a normal distribution. All statistical analyses were made using the SPSS 20.0 software (SPSS Inc., Chicago, IL, USA). Unless otherwise noted, P < 0.05 was considered statistically significant.
Soil water status
The watering treatments produced a wide-ranging soil water gradient combined with either ambient or elevated CO2 during the entire experimental period; when measured before watering at 17:00 every 3 days (the irrigation day) during a consecutive 10-day period, the SRWCs were 26.7 %, 39.4 %, 42.7 %, 45.6 %, 50.8 %, 53.3 %, and 61.7 % in the W−60, W−30, W−15, W0, W+15, W+30, W+60 watering treatments at ambient CO2, and 25.4 %, 36.1 %, 38.4 %, 44.0 %, 45.5 %, 50.9 %, and 51.5 % at elevated CO2, respectively (Additional file 1: Figure S1), indicating that elevated CO2 reduced the SRWC under every watering treatment (on average from 45.7 to 41.7 %, decreasing by 8.9 %). Watering and elevated CO2 exerted significant effects almost every day over the continuous 10-day period except for elevated CO2 concentration on the 57th and 62nd days after sowing according to a GLM ANOVA (Additional file 2: Table S1).
Multiple plant traits and environmental effects
Plant growth analysis
From W−60 to W0, an increase in LAR with improving water status was observed under the ambient CO2 level; however, this increase trend seemed to be partly offset by elevated CO2 (Fig. 2c,). LARMR had a similar response to the water status gradient, and CO2 enrichment-induced attenuation of the response to water status change was also observed (Fig. 2d). Both watering and CO2 concentration had significant effects on these two parameters (P < 0.05, Additional file 3: Table S2).
Photosynthetic capacity, stomatal conductance, and intrinsic WUE
The two chlorophyll a fluorescence parameters—F v/F m and F' v/F' m—were only significantly decreased by severe water deficit. Elevated CO2 did not have a significant effect on either parameter, except a slight stimulation under relative water deficit. F v/F m was unchanged but F' v/F' m was decreased by elevated CO2 under relatively sufficient water conditions (Fig. 4d, h). Watering alone had significant effects on F v/F m and F' v/F' m, while CO2 concentration and the interaction of CO2 and water had no effect (Additional file 3: Table S2).
Mesophyll cell ultrastructure
No significant changes in mesophyll cell length were observed under changes in the two treatment factors (Additional file 4: Table S3). Cell width increased with elevated CO2, but decreased with reducing water except in the W30 and W60 treatments. There was a linear increase in cell area with increasing water under ambient CO2; under elevated CO2, cell area was often increased with improving water status, but decreased with excess water. Cell wall thickness (CWT) was decreased only under extreme drought (W−60), but was drastically increased by CO2 enrichment by 22.2 % across all watering treatments. The chloroplast number per cell was decreased by extreme drought, but markedly increased by CO2 enrichment in all watering treatments. Although the three chloroplast size parameters (length, width, and profile area) showed no systematic responses to the water status gradient, they were decreased under elevated CO2 in plants subjected to extreme and severe drought (W−60 and W−30) and increased in the excess water treatments (W30 and W60). The number of grana thylakoid membranes (TMN) was unaffected by watering treatment, but was decreased by elevated CO2 by an average of 22.9 % across all watering treatments. Water deficit and relative water surplus caused declines in the starch grain number per chloroplast profile (SGN), and no intact starch grains were found at W−60 with ambient CO2. Elevated CO2 led to decreases in SGN in the W−15 and W−30 treatments, but increases in the other water treatments, indicating that the effect of elevated CO2 strongly depended on water status. The plastoglobuli number per chloroplast (PGN) tended to decrease under ample watering at ambient CO2; elevated CO2 seemed to decrease PGN under severe drought (W−30 and W−60), but increase it under excess water treatments. Based on ANOVA, CO2 concentration, watering, and their interaction all significantly affected CWT and PGN. Elevated CO2 and watering both had significant effects on the chloroplast number, but their interaction did not. Cell width, cell area, and SGN was significantly affected only by watering, and TMN only by elevated CO2. Finally, watering, and its interaction with CO2 concentration significantly affected the chloroplast length (Additional file 4: Table S3).
Total water use and biomass water use efficiency
Our experiment on the effects of elevated CO2 on plants under various watering regimes showed that plant growth and photosynthetic capacity were stimulated by elevated CO2 under moderate water changes relative to normal precipitation; however, over-watering or extreme water deficit diminished or even eliminated this stimulation. The damage from severe drought, i.e., chloroplast and grana thylakoid damage, was partially ameliorated under the high CO2 level. This mostly confirmed our first hypothesis. This response to water status gradient at a high CO2 concentration was reflected by combined changes in plant architecture, biomass allocation, stomatal behavior, CO2 assimilation, PSII photochemical process, cell organelle structure, and water use efficiency (WUE), demonstrating highly synergistic changes at multiple scales. This coordinated response pattern may partly support our second hypothesis. Our results provide a deeper insight into the effects of varying water status on the response to CO2 enrichment, from cell ultrastructure to in vivo photosynthetic physiology and whole plant growth, highlighting that various aspects of the comprehensive responses of the dominant species need to be considered when assessing and projecting terrestrial ecosystem responses to climatic change, particularly in arid regions.
A reduction in g s under enhanced CO2 can improve plant water status, thereby ameliorating the adverse effects of soil water deficiency on plant growth and physiological activity [8, 58]. As reported by Easlon et al. , a low g s coupled with high photosynthetic capacity in A. thaliana plants growing under elevated CO2 might result from more conservative N investment in the photosynthetic apparatus. In the present experiment, the marked g s decline due to water deficit seemed to be alleviated by elevated CO2, implying that increased CO2 has a protective role in drought-stressed leaves (Fig. 4f). In Liquidambar styraciflua plants, however, severe drought can lead to excessive stomatal closure and accelerated leaf senescence that may offset the benefits of CO2 enrichment for saving water . The lack of benefit from increased CO2 to drought-stricken plants may be attributable to a lack of stomatal regulation . Thus, the effect of elevated CO2 on the stomatal response to water change may depend on the species and extent of water deficit , but this needs to be explored further.
A marked decline in g s under severe water deficit in close parallel with photosynthetic capacity may reflect the coexistence of stomatal and mesophyll limitations on photosynthesis (Fig. 4), in agreement with Flexas and Medrano . Their results indicated that non-stomatal limitations including decreased photochemistry and Rubisco activity corresponded with decreases in g s, particularly below 100 mmol m−2 s−1. Photosynthetic mesophyll limitations, such as decreases in both photosynthetic activity and cell size, may play a major role in photosynthetic depression , which is almost in agreement with the present results. A recent report showed that Ramonda nathaliae plants with smaller stomata had higher resistance to drought than R. serbica , in line with the reductions in mesophyll cell size and g s under severe drought in the present experiment (Additional file 4: Table S3). Thus, an associated change in cell size and stomatal behavior might confer a highly adaptive response to climate change.
In vivo physiological capacity
Photosynthetic capacity parameters such as A sat, V cmax J max, and TPU are inhibited under extreme and severe drought, but elevated CO2 can partly alleviate this inhibition [4, 24, 26, 65, 66]. However, in the present results, although elevated CO2 increased the photosynthetic capacity under severe and moderate drought and control treatments, it had no significant effect, or caused a decrease, under surplus watering conditions (Fig. 4). As reported previously, the photosynthetic capacity was decreased under elevated CO2 in Eucalyptus seedlings grown under well-watered but not water-stressed conditions . Thus, the positive effects of elevated CO2 on photosynthesis may favor plants exposed to a moderate range of water statuses—from severe to moderate water deficit stress.
The effect of elevated CO2 on in vivo chlorophyll a fluorescence is also uncertain. For example, the maximal photochemical efficiency of PSII (F v/F m) was increased by elevated CO2 in poplar seedlings . However, chlorophyll fluorescence showed no changes under elevated CO2 in Scots pine needles  and some grasses . Roden and Ball  showed that elevated CO2 led to a reduction of F v/F m in amply watered Eucalyptus seedlings, but no effect was found under drought. No significant differences in F v/F m were found in control and water-deprived Phaseolus vulgaris plants, although plant fresh weight decreased approximately 30 % in water-stressed conditions , suggesting that other metabolic processes related to growth, rather than PSII photochemical activity, might play a critical role in the response to water deficit stress. Our findings indicated that CO2 enrichment had no effect on F v/F m, and even inhibited the photochemical efficiency of open reaction centers of PSII (F′v/F′m) in relatively well-watered plants, but had a stimulatory effect under relative water deficit (Fig. 4h). Moreover, we found that accelerated accumulation in starch grains might damage the chloroplast structure under well-watered conditions, which might partly explain the depression of PSII activity.
In Rakić et al. , a reduction in F v/F m occurred only in severely drought-stressed resurrection plants, consistent with our results in which a dramatic decline in F v/F m and F′v/F′m appeared only under extreme water deficit. Therefore, a drastic decline occurs only in plants subjected to extreme environmental stress, suggesting that these two parameters might not be good indicators of moderate water status changes. Elevated CO2 might not affect or might decrease these parameters, possibly because of decreased leaf thickness (greater SLA) or down-regulation of photosynthetic potential .
Organelle structure changes
The chloroplast, a compulsory light-harvesting organelle, can be easily and seriously affected by elevated CO2 [70, 71]. Many previous studies have shown that elevated CO2 could increase the number of chloroplasts in mesophyll cells [47, 70, 72, 73], which was also confirmed by the current study (Additional file 4: Table S3, Fig. 5). However, the mechanism by which elevated CO2 positively regulates chloroplast numbers still remains unclear [47, 72]. Some reports have suggested it results from stimulation of chloroplast biogenesis processes [47, 74]. Additionally, there is other evidence for this abnormal change induced by increased CO2: a drastic increase in the amount of chloroplast stroma thylakoid membranes has been found relative to those in lower CO2 levels . Damage to chloroplast ultrastructure can also occur under elevated CO2, partly as a result of increased starch grain size and numbers through accelerated starch accumulation in chloroplasts . Enhanced accumulation of starch grains within chloroplasts by elevated CO2 can induce distortion of grana thylakoids, with plants exposed to a high CO2 level often having a low A net . In our current results, the increase in photosynthetic capacity was in agreement with the more numerous and larger starch grains in the chloroplasts of well-watered plants under the high CO2 level. It could be reasoned that starch accumulation might not be enough to limit the increase in photosynthesis induced by CO2 enrichment. However, this phenomenon would disappear under water deficit stress. Moreover, extremely severe water deficit can damage mesophyll cells, resulting in abnormal and disorganized cell organelles including chloroplasts and their grana , which was confirmed by the current experiment. However, this damage was partly ameliorated by elevated CO2, implying that plants have a strong dependence on the combination of CO2 concentration and water status.
Plant structural traits and associations with physiological activities
Interestingly, LARMR increased with increasing water supply but decreased at the high CO2 level (Fig. 2d), reflecting different effects on the biomass investment balance between the light trapping organs and resource element-deriving organs from the two climatic factors [49, 76]. This indicates that elevated CO2 might negate the enhanced investment in light-intercepting organs under an over-watering regime in this species, in line with our earlier study . PCA can not only unveil the extent and directions of correlations among plant structural and functional traits, but also distinguish the effects of treatment factors or their combinations from the projections, highlighting the importance of this useful analysis tool [23, 26, 57]. Here, for example, RMR and SMR had opposite distributions in the PC loadings (Fig. 1a), possibly reflecting the carbon allocation trade-off between root and stem organs . Moreover, we found positive close relationships between plant structural traits and functional traits such as photosynthetic activities and g s; they were all positively related with PC1, which might highlight their coordinated changes under different climatic change factors (Fig. 1a). Close associations between morphological/structural and functional traits have been widely reported, depending on the species and environment [26, 77–79]. Our results again highlight that multiple variables at different scales might together play a critical role in the adaptive response to global change by balancing or offsetting each other.
Water use efficiency
Elevated CO2 can improve plant water status by reducing g s and thereby increasing WUE to ameliorate the adverse effects on plant growth and physiological processes from stress factors alone and in combination [4, 8, 58]. Water status also mediated the effectiveness of rising CO2 by coupling the processes of gas exchange and leaf enlargement. Nevertheless, the pros and cons of acclimation to changes in water conditions might coexist in plant responses to elevated CO2; leaf area enlargement induced by CO2 might exaggerate water use, while decreased g s would promote WUEi [15, 58]. However, WUEi might decline under severe drought in some relict plant species exposed to elevated CO2 . In the present experiment, both WUEi and WUEt were increased by elevated CO2, implying that the promotion of A net and plant biomass by elevated CO2 might play a dominant role.
In the same steppe, conflicting results can occur because of different data types. For example, field rain use efficiency (RUE) increased with increasing MAP across different vegetation types, but decreased across different years in a given site, particularly in drier areas [40, 80]. Decreased RUE with increasing precipitation can be due to low productivity or other resource limitations such as N deficit . WUEt and RMR increased significantly with decreasing precipitation, but decreased with elevated CO2 . In the present experiment, however, we found that the increase of WUEt with increases in both water use and plant biomass (Fig. 6), particularly at a high CO2 level, might explain the resource limitation to WUE; both a water use increase and CO2 enrichment, as increases in available resources, might promote WUE by stimulating photosynthetic capacity and plant growth. Furthermore, our results indicated that although WUEt and WUEi showed a similar response to elevated CO2, the former was more sensitive, implying that WUEt might be a better indicator than WUEi for assessing responses to climate change .
Elevated CO2 mitigation of severe drought
Elevated CO2 can ameliorate the negative effects of environmental stresses including severe water deficit in many different plant functional types or species such as the desert shrubs Caragana intermedia and Caragana microphylla [26, 82], the C3 perennial grasses L. chinensis and Stipa grandis [26, 27], and the C4 grass species Cleistogenes squarrosa . The current experiment confirmed this amelioration due to CO2 enrichment in a C3 perennial grass from the same steppe as earlier experiments [26, 27, 82]. However, this amelioration was not observed in other reports on species such as some relict species , Populus deltoides , L. styraciflua , and Eucalyptus radiata . Moreover, CO2 enrichment had a negligible effect on the response of E. radiata seedlings to drought, and did not alleviate the deleterious effects of drought due to rising temperature . Thus, high CO2 may protect against or exacerbate stress effects, depending on different plant functional types and species.
A previous report showed that the growth of a dominant perennial shrub in a Mojave Desert ecosystem was doubled by a 50 % increase in CO2 only in a drier year . In the present study, although elevated CO2 stimulated plant growth and photosynthetic activity in water deficit-treated plants, it had an inhibitory effect on the amply watered plants. This again indicates that CO2 enrichment may be more beneficial in drought conditions, implying that elevated CO2 may eliminate drought-induced negative plant responses. Thus, the allocation response to rising CO2 may also depend on water status. However, in a recent report, elevated CO2 productivity did no significantly modify the effects from soil water status in mesic grassland, semi-arid grassland, and xeric shrubland . Taken together, these results suggest the integrated effects of elevated CO2 and water status on plants may be highly species- and habitat-specific.
Elevated CO2 can improve plant water status and therefore stimulate various physiological and ecological processes from the organelle to cell, organ and plant individual level. However, this stimulation is strongly dependent on water status. Elevated CO2 generally increased the growth and photosynthetic physiological parameters of A. cristatum such as V cmax, A sat, J max, gs, TPU, and F v/F m at severe to moderate water status, but had no effect on or even decreased these parameters in over-watering conditions. This indicates that CO2 enrichment can often ameliorate deleterious drought effects under moderate water deficit, but not extreme drought or over-watering conditions, and that plant morphological and structural alterations, and carbon allocation may be involved in this adaptive regulation. Our results for a dominant species from a degraded steppe suggest that water status changes such as severe drought or over-watering events might fundamentally contribute to the effects of CO2 enrichment on key physiological activities, cell structure, plant growth and even survival in a future climatic context, even completely reversing the direction of the effect. Our results highlight that CO2 fertilization’s dependency on water status should be considered when projecting plant responses to climate change. These findings contribute to our understanding of plant responses to global climate change, and may be useful in vulnerable ecosystem management.
A sat, light-saturated maximum photosynthetic rate; F′ v/F′ m, photochemical efficiency of open reaction centers of PSII; F v/F m, maximal PSII photochemical efficiency; g s, stomatal conductance; J max, maximum rate of electron transport; LAR, leaf area and plant total mass ratio; LARMR, leaf area and root mass ratio; LMR, leaf mass ratio; PCA, principal component analysis; RGR, relative growth rate; RMR, root mass ratio; SLA, specific leaf area; SMR, stem mass ratio; SSL, specific stem length; TPU, rate of thiose phosphate utilization; V c,max, maximum rate of carboxylation; WUEi, intrinsic water use efficiency; WUEt, total biomass water use efficiency.
We are grateful to Hui Wang, Yaohui Shi, Xiaomin lv, Zhixiang Yang, and Jian Song for their assistant works during the current experiment. We also greatly appreciate the anonymous reviewers and Dr. Giles Johnson for their constructive comments and suggestions.
This research was jointly funded by National Natural Science Foundation of China (31170456), and China Special Fund for Meteorological Research in the Public Interest (Major projects) (GYHY201506001-3).
Availability of data and materials
The data sets supporting the results of this article are included within the article and its additional files.
JY, XZ and ZG conceived and designed the study; JY, XZ and LT conducted the experiment and performed the data analysis; JY and XZ drafted the manuscript. All authors approved the final manuscript.
The authors declare that they have no competing interests.
Consent to publish
Ethics approval and consent to participate
The soil and seed collections from the field in our experiments are conducted in and permitted by Inner Mongolia Grassland Ecosystem Research Station, Institute of Botany, Chinese Academy of Sciences, Beijing. No species are involved at risk of extinction in the present experiment. Others are not applicable.
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