Skip to content
BY 4.0 license Open Access Published by De Gruyter Open Access December 21, 2020

Natural variation in stress response induced by low CO2 in Arabidopsis thaliana

  • Chunxia Wu EMAIL logo , Yulou Sun , Guang Yang , Li Li , Wei Sun , Zenglan Wang , Hui Zhang and Yuanyuan Li EMAIL logo
From the journal Open Life Sciences

Abstract

Variation in atmospheric carbon dioxide (CO2) concentration can dictate plant growth and development and shape plant evolution. For paired populations of 31 Arabidopsis accessions, respectively, grown under 100 or 380 ppm CO2, we compared phenotypic traits related to vegetative growth and flowering time. Four accessions showed the least variation in measured growth traits between 100 ppm CO2 and 380 ppm CO2 conditions, though all accessions exhibited a dwarf stature with reduced biomass under low CO2. Our comparison of accessions also incorporated the altitude (indicated in meters) above sea level at which they were originally collected. Notably, An-1 (50 m), Est (50 m), Ws-0 (150 m), and Ler-0 (600 m) showed the least differences (lower decrease or increase) between treatments in flowering time, rosette leaf number, specific leaf weight, stomatal density, and less negative δ13C values. When variations for all traits and seedset were considered together, Ws-0 exhibited the least change between treatments. Our results showed that physiological and phenotypic responses to low CO2 varied among these accessions and did not correlate linearly with altitude, thus suggesting that slower growth or smaller stature under ambient CO2 may potentially belie a fitness advantage for sustainable growth under low CO2 availability.

1 Introduction

Carbon dioxide (CO2) is a central and predominant environmental factor necessary for plant growth. As photosynthetic organisms, plants take up atmospheric CO2 by diffusion into the leaf through the stomata and subsequently convert it into organic compounds necessary for maintaining plant metabolism and sustained growth. Atmospheric CO2 concentration has varied tremendously throughout the history of plant life on Earth, ranging from as high as 3,000 ppm (parts per million) in the early Devonian (∼400 million years [myr] ago) [1] to as low as 180 ppm during the Pleistocene glacial (∼20 kilo-years [kyr] ago) [2]. Variation in CO2 has been proposed as a driver of plant evolution [3,4]. Substantial previous research has established that elevated concentrations of atmospheric CO2 can exert clear phenotypic effects on plants such as increased photosynthetic rates, which in turn lead to higher crop yields and reduced water loss by transpiration [5,6,7,8]. Falling global atmospheric CO2 potentially imposes a selective pressure on vascular plants that can drive evolutionary trajectories for increased stomatal density (SD), decreased individual stomatal size [9,10], higher vein density, and greater water-use efficiency [11,12]. Several studies have thus postulated that around 30 myr ago, an abrupt drop in atmospheric CO2 induced the emergence of C4 species [13,14,15,16,17].

Previous studies have proposed that modern C3 plants experience heightened stress under low CO2 and may respond by changing their reproductive or developmental timing or by changing their allocation of biomass to different tissues, resulting in measurable, phenotypic responses to low CO2 that may be potentially inherited if the environmental conditions persist [18]. For example, Billings et al. [19] observed adaptive variation in Oxyria digyna, in which high-altitude ecotypes were capable of higher photosynthetic rates and lower CO2 compensation points compared to low-altitude ecotypes across a range of CO2 concentrations, including low CO2.

Arabidopsis (Arabidopsis thaliana (L.) Heynh) is widely distributed throughout the Northern Hemisphere and adapts to a broad range of climatic conditions and selective pressures [20,21]. Sharma et al. [22] grew 33 Arabidopsis accessions below the compensation point (achieved by growing the C4-plant maize alongside Arabidopsis) and found a difference of over 1 week in survival time among accessions. Ward and Strain [23] showed that Arabidopsis accessions from different elevations had significant variation in seed yield when grown at low CO2 (200 ppm). Ward and Kelly [24] observed a high level of genetic variation in percentage survival, reproductive output, and total seed production among the Arabidopsis genotypes when grown at low CO2 (200 ppm). Taken together, these studies suggest that Arabidopsis has phenotypic plasticity in response to low CO2, and natural accessions of Arabidopsis can vary widely genetically and phenotypically for many traits [20,25].

In order to survive and successfully reproduce in a given environment, plants must fix carbon to produce biomass, then initiate and complete their reproductive stage, in which plants direct energy into flowering and seed production. Several traits related to C3 and C4 carbon metabolism are essential for developing sufficient biomass for the plant to adequately support the production of flowers and seeds. For example, the trait of flowering time is critically important for reproductive fitness since plants must find pollinators (i.e., flowers of the same species) for successful outcrossing [26]. Similarly, the timing of seedset is extremely important for ensuring that seed is dispersed into conducive environmental conditions among selfing species [26]. Furthermore, these traits are regulated by external, environmental signals as well as internal, physiological cues [26].

Low CO2 has been shown to induce molecular changes in addition to a variety of phenotypical trait changes in A. thaliana. Growth on petri dishes wrapped with Parafilm led to CO2 deprivation as soon as cotyledons emerged [27]. This CO2 deprivation resulted in a 35% difference in the expression of biochemical pathways, such as those for carbohydrate metabolism, chlorophyll biosynthesis, secondary metabolite biosynthesis, and stress response, compared with fully aerated plants [27]. Specifically, short-term CO2 limitation (an 8 h shift from 10,000 ppm CO2 to 380 ppm CO2) did not cause visible changes in phenotype but significantly induced transcriptional and metabolic responses in five genes related to photorespiration through glycerate, glycolate, serine, and glycine production [28]. Moreover, when 5-week-old Arabidopsis plants were transferred into 100 ppm CO2 conditions for 24 h, ornithine accumulated, which is an intermediate of the urea cycle and a central metabolite of arginine synthesis and degradation [29]. Long-term low CO2 stress was induced in Arabidopsis Col-0 by growth in 100 ppm CO2 for 6 weeks [30]. The genes upregulated at 100 ppm CO2 were remarkably enriched in stress response and the downregulated genes were only significantly enriched in cell wall and endomembrane system [31]. However, energy metabolism, lipid metabolism, and amino acid metabolism pathways showed significant decreases in flux under low CO2, whereas nucleotide metabolism showed increased flux [31].

For these reasons, in this study, we chose to focus on flowering time, seedset, and several marker traits at flowering time, including aboveground biomass, rosette leaf number, SD, specific leaf weight (SLW), and stable isotope carbon assimilation as metrics for the ability to adapt to low CO2 among different wild Arabidopsis accessions. We hypothesized that accessions capable of adaptation to growth under low CO2 would show the least variation in biomass production, carbon assimilation, and flowering time compared to their growth under ambient CO2, whereas plants lacking the genetic variation that allows adaptation to low CO2 cannot successfully grow or reproduce under carbon-limited conditions. We thus compared growth during the vegetative and reproductive development of 31 Arabidopsis accessions under low CO2 (100 ppm) and ambient CO2 (380 ppm), to better understand the contribution of natural, heritable variation to the plant response to low CO2. This work contributes to the findings of previous studies that explored the genetic variation underlying evolutionary adaptations such as C4 metabolism, while also providing meaningful context for observable changes in wild populations that are subject to current changes in climate and atmospheric CO2.

2 Materials and methods

2.1 Plant materials and growth conditions

Thirty-one A. thaliana accessions were used in this study (Table 1) to represent a wide range of geographically separated locations, elevations, and climates.

Table 1

Accessions used in this study and their locations of origin and altitudes in meters

AccessionsStock numberCountryLocationAltitude (m above sea level)
Col-0CS1092USAColumbia50
An-1CS6603BelgiumAntwerpen50
Ct-1CS6674ItalyCatania50
EstCS6173Germany50
Lc-0CS6769UKLoch Ness50
LitvaCS925Lithuania50
Lm-2CS6784FranceLe Mans50
Pa-1N1439ItalyPalermo50
Per-1CS1444RussiaPerm50
Ren-1CS22253FranceRennes42
Te-0CS6918FinlandTenela50
Ts-1A22647SpainTossa del Mar50
Tsu-1CS6926JapanTsushima50
Van-0CS6884CanadaUniversity of British Columbia50
Wt-5CS6896GermanyWietze50
Be-0CS6613GermanyBensheim/Bergstr.150
Ga-0CS1181GabelsteinGabelstein150
Mt-0CS6799LibyaMartuba/Cyrenaica150
Rsch-4CS1494RussiaRschew/Starize150
Stw-0CS6865RussiaStobowa/Orel150
Ws-0RussiaWassilewskija150
Kin-0CS1272USAKindalville, MI300
Bay-0CS6608GermanyBayreuth350
Bs-1CS6627SwitzerlandBasel350
Kil-0CS6754UKKillean450
Lip-0CS1336PolandLipowiec/Chrzanow500
Ler-0CS163Germany600
Mc-0CS1363UKMickle Fell700
Ka-0CS6752AustriaKarnten950
Kas-1CS903IndiaKashmir1,580
ShaTadjikistanPamiro-Alay3,400

Note: Stock number (N, NASC stock center (http://arabidopsis.info/); A, ABRC stock center (http://abrc.osu.edu/)).

Arabidopsis seeds were surface-sterilized by soaking in 75% (v/v) ethanol for 10 min and rinsed 5–6 times with 95% ethanol, then sown on solid media containing half-strength Murashige and Skoog mineral salts, 1% (w/v) sucrose, and 0.8% (w/v) agar, pH 5.7. Plates with seeds were incubated in the dark at 4°C for 2 days to break dormancy prior to germination in growth chambers. The 7-day-old seedlings were transferred to a mixture of perlite/vermiculite/peat (1:1:3) in a 8 cm square pot (512 cm3). For each CO2 condition, at least 50 seedlings for one accession were transferred into the pot. Plants were then grown in a Percival controlled environment (E-36L, USA) growth chamber either at low CO2 (100 ppm) or ambient CO2 (380 ppm) with a 16 h light (22°C)/8 h dark (18°C) photoperiod and a light intensity of 120 µmol m−2 s−1 and 70% humidity. The CO2 concentration was set the same as our previous study [30]. Four chambers, two for low CO2 and the other two for 380 ppm CO2, were used. The plants in the two (under the same condition) chambers were switched twice a week.

2.2 Growth parameters

Boyes et al. [32] defined 30 growth stages, which were divided into 9 principal stages for Arabidopsis, spanning development from seed imbibition through the completion of flowering and seed maturation. Based on the physiological growth stages of A. thaliana established by Boyes et al. [32], we chose stage 5.10 (first flower buds visible) and stage 6.00 (first flower open) to measure the growth parameters. At the beginning of stage 5.10, the transition from vegetative growth to reproductive growth, we recorded the number of days since germination until the first flower buds were visible, as well as the aboveground fresh weight (FW), number of rosette leaves, SLW, and the δ13C value in leaves. At the beginning of stage 6.00, we again recorded the number of days between germination and the opening of the first flower, as well as SD. Individual leaves were detached from each plant with forceps and imaged for subsequent analysis using a scanner (V900; Shanghai MICROTEK Technology Co. Ltd, Shanghai, China). Length and area were measured using IMAGE J (v1.8.0, https://imagej.nih.gov/ij/index.html) software.

2.3 Stable carbon isotope analysis

The fully expanded third true leaf of each plant that developed before stage 5.10 was used to quantify the stable carbon isotope ratio (13C/12C). All samples were oven-dried at 65°C for 48 h to a constant weight. The measurements of stable carbon isotope ratios were carried out at the Chinese Academy of Forestry’s Stable Isotope Laboratory (Beijing, China) using a Flash EA1112 HT elemental analyzer (Thermo Fisher Scientific, Waltham, MA, USA) coupled with a Delta V advantage isotope ratio mass spectrometer (Thermo Fisher Scientific). Stable carbon isotope ratios were expressed as δ13C (‰) and were calculated as follows:

δ13C()=Rsample/Rstandard1×1,000,

where Rsample and Rstandard are the ratios of 13C/12C in the samples and the standard (Pee Dee Belemnite), respectively. The precision of the repeated sample was 0.15‰.

2.4 SD measurement

The largest, fully expanded leaves were selected for SD measurement and prepared as follows: (1) leaves were fixed overnight or longer in FAA solution (5 mL of formaldehyde:5 mL of acetic acid:90 mL of 70% ethanol); (2) leaves were decolorized in 70% ethanol until white; (3) tissue samples were mounted abaxially on slides with Hoyer’s solution; and (4) stomata were visualized by differential interference contrast microscopy on a Zeiss Imager Z2 microscope (Carl Zeiss Microscopy, LLC, White Plains, NY, USA) (0.379 mm2 field of view). Ten images were collected from the middle of the abaxial side of each leaf sample, between the mid-vein and the edge. Stomata were manually counted for all pictures and all leaves using IMAGE J (v1.8.0, https://imagej.nih.gov/ij/index.html). Six leaves per accession were analyzed.

2.5 Statistical analysis

Statistical analyses for all experiments were performed using Excel 2010 (Los Angeles, CA, USA), SPSS 19.0 (SPSS Inc., Chicago, IL, USA), and SigmaPlot (SyStat Software, San Jose, CA, USA) software. After calculating averages, standard deviations and standard errors were also determined. Significant differences between low and ambient CO2 treatments for each trait and the interaction effect of CO2 and accessions were determined by one-way analysis of variance with p ≤ 0.05 for each experiment.

3 Results

3.1 Effect of treatment on traits

In this experiment, the low CO2 concentration was set to 100 ppm, which was shown to be a severe stress to Arabidopsis ecotype Columbia-0, and the ambient CO2 was set to 380 ppm the same as those in our previous study [30]. A collection of 31 accessions (Table 1) was selected to analyze the genetic diversity based on the whole set of measurable responses to low CO2. As expected, all tested accessions showed reduced growth when grown under low CO2 versus ambient CO2 (380 ppm) (Data not shown. Part results are shown in Figure A1).

As shown in Table 2, the effects of CO2 concentration and accession were strongly significant in the comparison of the number of days to stage 5.10, FW, number of rosette leaves, SLW, and SD. The interaction effect of CO2 and accession on these five traits was also highly significant.

Table 2

Effects of CO2, accession, and CO2 × accession interaction for days to stage 5.10, FW, number of rosette leaves, SLW, and SD (F values are shown)

Variation sourceDays to stage 5.10FWNo. of rosette leavesSLWSD
CO21,192***3,494***93***6,978***37***
Accession1,336***180***192***47***132***
CO2 × Accession388***139***83***49***34***

Note: the significance level: *p < 0.05; **p < 0.01; ***p < 0.001.

3.2 Variation in flowering time

The onset of flowering, which is the transition from vegetative to reproductive stages, is a major determinant of a plant’s reproductive success and may be hastened or delayed by variations in climate that act as environmental cues or stimuli for the plant [33]. We measured the time from germination to the appearance of the first visible flower bud (developmental stage 5.10 as described in [32]) and the time to the first flower opening (developmental stage 6.00; [32]) of 31 accessions grown under low CO2 and ambient CO2, and calculated the difference in flowering times between the two CO2 treatments. Two accessions, Mc-0 and Rsch-4, made the transition to flowering (stage 5.10) 4 days earlier under low CO2 than under ambient CO2 (Figure 1a and b). In 17 accessions, the low CO2 treatment delayed flowering (stage 5.10) for at least 1 day. Among these, Ts-1 took 54 days longer to reach stage 5.10 under low CO2 (Figure 1a and b). Te-0 and Kas-1 never flowered and died under low CO2, so the data from these two accessions were missing in the following analysis. Twelve accessions (Figure 1b, red arrows) showed no difference in the time to stage 5.10 under low CO2 and ambient CO2, including Est, Ws-0, and Ler-0.

Figure 1 Effect of low CO2 on flowering time. (a) Days from germination to stage 5.10. (b) The difference in time from germination to stage 5.10 or 6.00 for plants grown under low CO2 compared with those under ambient CO2. Values are mean ± SE (n = 3). Red arrows indicate the accessions with no difference in duration from germination to stage 5.10 between the two CO2 treatments. Blue arrows indicate the accessions exhibiting a shorter time in days to reach stage 6.00 between the two CO2 treatments. Arabidopsis accessions listed on the x-axis (left to right) are arranged by altitude, in the same order as in Table 1.
Figure 1

Effect of low CO2 on flowering time. (a) Days from germination to stage 5.10. (b) The difference in time from germination to stage 5.10 or 6.00 for plants grown under low CO2 compared with those under ambient CO2. Values are mean ± SE (n = 3). Red arrows indicate the accessions with no difference in duration from germination to stage 5.10 between the two CO2 treatments. Blue arrows indicate the accessions exhibiting a shorter time in days to reach stage 6.00 between the two CO2 treatments. Arabidopsis accessions listed on the x-axis (left to right) are arranged by altitude, in the same order as in Table 1.

The time to the appearance of an open flower (stage 6.00) was far more variable than the time to stage 5.10, even though the timing of flower opening was consistently delayed in all the accessions when grown under low CO2 (Figure 1b). This delay in the first flower opening ranged from 1 day (Rsch-4) to 63 days (Lip-0). Five accessions, including An-1, Pa-1, Mt-0, Ws-0, and Bay-0, showed less difference between the time to stage 6.00 under low CO2 and ambient CO2 (Figure 1b). Two accessions Est and Ga-0 died after reaching stage 6.00 in low CO2 conditions. Under low CO2, the first flower of Est opened partly but withered gradually and died, while a portion of the Ga-0 flower buds opened but had no seed in siliques and also subsequently died. The flower buds of Ts-1 failed to open under low CO2 condition (Figure A1). Given the importance of a consistent flowering time when all conditions are stable except CO2, we postulated that accessions that were able to maintain their time of flowering in spite of low CO2 exhibited higher adaptability than accessions with a greater difference in flowering time. Supporting this point, five accessions failed to flower successfully and died at stages 5.10 and 6.00, indicating that they were unable to pass this developmental stage under low CO2.

3.3 Aboveground biomass

Biomass is frequently used as a reliable estimate of plant fitness [34]. All the accessions tested in this study exhibited a reduction in plant size during low CO2 growth. We measured aboveground biomass at the time of flowering (stage 5.10) and found that the aboveground (shoot) FW of all accessions decreased significantly (p < 0.001) under low CO2 compared to biomass of plants grown under ambient CO2 (Figure 2a). Two accessions, Pa-1 and An-1, showed a 60% reduction and four accessions showed a 70–80% reduction in shoot FW. The percent decrease for 7 accessions was between 80 and 90%, and for 16 accessions, biomass decreased over 90% (Figure 2a).

Figure 2 Effect of low CO2 on shoot biomass. Relative FW, the ratio of FW under low CO2 to FW under ambient CO2. Red arrows indicate the accessions screened out by shoot biomass. Values are mean ± SE (n = 3). Stars denote significant differences between Col-0 and other accessions (*p < 0.05, ***p < 0.001).
Figure 2

Effect of low CO2 on shoot biomass. Relative FW, the ratio of FW under low CO2 to FW under ambient CO2. Red arrows indicate the accessions screened out by shoot biomass. Values are mean ± SE (n = 3). Stars denote significant differences between Col-0 and other accessions (*p < 0.05, ***p < 0.001).

We also calculated the variation in relative FWs between the two treatments by determining the ratio of shoot FW under low CO2 to normal CO2. We found that compared to Col-0, the accessions An-1, Est, Pa-1, Ws-0, Ler-0, and Sha all showed lower variation in relative FW when grown in CO2-limiting conditions (Figure 2b). As with flowering time, we considered lower variation in FW for plants grown under low CO2 compared to ambient CO2 to be an indicator of higher adaptability by these accessions.

3.4 Rosette leaf number

The leaf number is closely correlated with the time to flowering and can be used as an indicator of phenotypic variability among different Arabidopsis accessions [35]. We counted the number of leaves in the rosette (excluding cotyledons) at the time of the first visible flower bud. Under low CO2, most of the accessions bolted, resulting in fewer rosette leaves. For example, Be-0, Tsu-1, Mc-0, and Rsch-4 exhibited a greater than 50% reduction in leaves compared to those growth in ambient CO2. However, An-1, Est, Pa-1, Ws-0, Ler-0, and Sha showed only a slight difference in rosette leaf number between treatments. Specifically, the leaf number of An-1 in low CO2 was slightly greater than under ambient CO2, whereas the other five accessions had on average one leaf less when grown under low CO2 (Figure 3).

Figure 3 Effect of low CO2 on rosette leaf number. Red arrows indicate the accessions with the least difference in leaf number between the two CO2 treatments. Values are mean ± SE (n = 3).
Figure 3

Effect of low CO2 on rosette leaf number. Red arrows indicate the accessions with the least difference in leaf number between the two CO2 treatments. Values are mean ± SE (n = 3).

We also counted the number of cauline leaves present at the time of the first flower opening. The cauline leaf response to low CO2 was more variable among accessions than the rosette leaf response. On average, the number of cauline leaves was reduced under low CO2 (data not shown), although in contrast, Wt-5 and Lip-0 had more cauline leaves due to the longer developmental time prior to reaching stage 6.00 from stage 5.10 under low CO2. These two accessions also had more lateral branches.

Interestingly, there were four accessions for which the number of cauline leaves was less than 20% higher in low CO2, whereas An-1 increased by 60% in low CO2 compared to plants grown without CO2 limitation. In contrast, 12 accessions exhibited a reduction in cauline leaves of less than 20% under low CO2 and 9 accessions had 20–66% fewer leaves under CO2-limiting treatment. The An-1, Est, Pa-1, Bay-0, Sha, and Wt-5 accessions had less than two leaves under ambient CO2, resulting in percent difference of less than 20% except for An-1 and Wt-5. Since the role of cauline leaves in photosynthetic productivity is less certain than for rosette leaves given their typical variability under unmodified atmospheric CO2, the contribution of variability in production of these leaves is also less predictable than that of rosette leaves, though in either case, we hypothesize that low variability indicates higher adaptability to low CO2.

3.5 SD

Stomata are present on the leaf surface and control the entry of CO2 into the leaves of plants prior to assimilation via photosynthesis [36,37,38]. Previous studies have reported that in Arabidopsis ecotype Col-0, SD (the number of stomata per unit leaf area) increased in response to low CO2 concentration [30]. Here, we examined the SD of the abaxial (lower) leaf blade epidermis of the surviving Arabidopsis accessions grown under ambient and low CO2 conditions. Among these 29 Arabidopsis accessions, there were 14 whose SD was significantly higher under low CO2 compared to ambient CO2 (Figure 4). Lc-0, Lm-2. Rsch-4, Ws-0, Bs-1, and Kil-0 did not show any significant differences in SD compared with Col-0. However, the SD of several accessions, including An-1 and Ler-0, decreased in response to low CO2 (Figure 4). We are inclined to speculates, in light of these results, that accessions showing increased SD have higher fitness under low CO2, since the higher number of stomata can increase the rate of CO2 diffusion in leaves.

Figure 4 Effect of low CO2 on SD. Relative SD is the ratio of the SD under low CO2 to the SD under ambient CO2. Red arrows indicate the accessions with no significant difference in relative SD compared to Col-0. Values are mean ± SE (n = 3). Stars denote significant differences between Col-0 and other accessions (*p < 0.05, ***p < 0.001).
Figure 4

Effect of low CO2 on SD. Relative SD is the ratio of the SD under low CO2 to the SD under ambient CO2. Red arrows indicate the accessions with no significant difference in relative SD compared to Col-0. Values are mean ± SE (n = 3). Stars denote significant differences between Col-0 and other accessions (*p < 0.05, ***p < 0.001).

3.6 SLW

SLW is defined as unit weight per unit leaf area, and it is an indicator of plant photosynthetic capacity, with high SLW interpreted as a decrease in photosynthetic efficiency [39,40,41,42]. In general, at low CO2, SLW was lower than at ambient CO2 among the Arabidopsis accessions in this screen. Here, we used the relative SLW, or the ratio of SLW under low CO2/SLW under ambient CO2, to evaluate the photosynthetic adaptations in response to low CO2. Compared to Col-0, the accessions An-1, Est, Ws-0, and Ler-0 showed substantially lower variation between two treatments (Figure 5).

Figure 5 Effect of low CO2 on SLW of accessions. Relative SLW is the ratio of the SLW under low CO2 to the SLW under ambient CO2. Red line delineates the relative SLW of Col-0. Red arrows indicate the accessions with higher relative SLW compared to Col-0. Values are mean ± SE (n = 3). Stars denote significant differences between Col-0 and the other accession (*p < 0.05, ***p < 0.001).
Figure 5

Effect of low CO2 on SLW of accessions. Relative SLW is the ratio of the SLW under low CO2 to the SLW under ambient CO2. Red line delineates the relative SLW of Col-0. Red arrows indicate the accessions with higher relative SLW compared to Col-0. Values are mean ± SE (n = 3). Stars denote significant differences between Col-0 and the other accession (*p < 0.05, ***p < 0.001).

3.7 Stable carbon isotope ratio of leaf tissue (δ13C)

The stable carbon isotope ratio is used to distinguish the photosynthetic CO2-fixing pathway in plants [43,44]. The δ13C values of C3 plants are typically more negative than those of C4 plants (−23 to −32% vs −6 to −19%, respectively) [43,44]. However, Arabidopsis carries some genes that belong to the C4 pathway, leading us to hypothesize that under ambient CO2, this species may exhibit a less negative δ13C value under low CO2 than ambient CO2. To investigate the effect of low CO2 on the photosynthetic capability of Arabidopsis accessions, we measured δ13C values in the third true leaves of all accessions, in order to analyze the stable carbon isotope ratio during treatment with low CO2. Unexpectedly, the δ13C values of seven accessions at low CO2 were more negative compared to those at ambient CO2, whereas most of the other accessions had more positive δ13C values under low CO2 treatment (Table 3), including the accessions An-1, Est, Ws-0, and Ler-0, thus suggesting a potential role for C4 genes in future potential adaptations to low CO2.

Table 3

Mean δ13C value of Arabidopsis accessions (n = 3)

AccessionsAmbient (380 ppm) CO2 (‰)Low (100 ppm) CO2 (‰)L-A (‰)
Ga-0−32.95−35.8−2.86
Be-0−33.33−34.48−1.16
Tsu-1−33.16−33.82−0.66
Bs-1−34.37−34.77−0.41
Wt-5−33.26−33.47−0.2
Ct-1−36.96−37.13−0.17
Stw-0−33.99−34.04−0.06
Kin-0−36.25−35.910.34
Lip-0−33.01−32.650.36
Mt-0−38.14−37.640.5
Mc-0−33.93−33.250.68
Ren-1−33.39−32.610.78
Litva−33.25−32.231.03
Est−39.37−38.341.03
Kas-1−30.29−29.241.05
An-1−38.55−37.461.09
Bay-0−38.51−37.381.13
Kil-0−37.61−36.451.16
Per-1−34.51−33.261.25
Rsch-4−36.78−35.461.32
Te-0−30.39−29.031.37
Col-0−36.68−35.021.66
Ler-0−38.75−37.041.72
Pa-1−38.94−37.211.73
Lc-0−37.4−35.531.87
Ws-0−39.19−37.221.97
Ts-1−31.52−29.372.14
Van-0−34.61−31.583.04
Sha−37.68−34.473.21
Lm-2−38.7−34.873.83
Ka-0−38.71−33.645.07

3.8 Genetic background

From the aforementioned results, the four accessions An-1, Est, Ws-0, and Ler-0 showed less variation in flowering time, shoot biomass, rosette leaf number, and SLW between the two treatments than did Col-0 (Figures 1–3 and 5). Supporting these data, all four of these accessions exhibited smaller overall size compared to Col-0 under ambient CO2 (Figure 6A). Our previous research [30] showed that low-CO2 treatment upregulated some C4-cycle genes including PEPC [45] and PEPC-K in Arabidopsis accession Col-0. The 1001 Genomes Project (https://1001genomes.org) provided whole genome sequence data to interrogate for genetic differences between different accessions, thus allowing us to potentially decipher how phenotypic variation is related to underlying genetic variation. We used the tool POLYMORPH (http://tools.1001genomes.org/polymorph/) to examine if low-CO2-responsive genes carried specific sequence changes among the four accessions we screened with the most extreme responses to low CO2. We calculated all polymorphic variants, including single nucleotide polymorphisms (SNPs), insertions, and deletions in all C4-cycle genes and C4-related transporter genes in the An-1, Est, Ws-0, and Ler-0 four accessions. However, no clear pattern in genetic variation emerged to indicate the mechanisms driving these phenotypic responses (Figure A2). For example, although PEPC (At2g42600) showed a 2.10-fold higher transcript abundance in Col-0 in response to low CO2 [30], An-1, Est, and Ws-0 had no identifiable differences in PEPC sequence compared to that of Col-0 (Figure 6b). Responses to low CO2 stress involve a complex network of regulatory elements to participate in mitigating damage induced by the stress, and differences in genetic background may potentially trigger unique stress responses among different accessions. Using transcriptomics sequence data, Carlson et al. [46] determined that a significant number of SNPs were absent in two accessions of Arabidopsis suecica (a relatively recent allopolyploid species) in the 1,001 genome SNP collection. RNA-seq analysis can effectively identify the genetic variation among these four accessions and we will use this technique in further experiments to explore the genetic basis underpinning plant adaptation to low CO2.

Figure 6 Phenotype and genetic difference of the four accessions An-1, Est, Ws-0, and Ler-0. (a) Phenotype of An-1, Est, Ws-0, and Ler-0 grown in ambient CO2 or low CO2. Scale bar = 2 cm. (b) The number of polymorphic variants (deletions, insertions, and SNPs) of the C4-cycle PEPC gene in accessions An-1, Est, Ws-0, and Ler-0 when compared to the Col-0 reference genome. The calculation was performed using the tool POLYMORPH (http://tools.1001genomes.org/polymorph/).
Figure 6

Phenotype and genetic difference of the four accessions An-1, Est, Ws-0, and Ler-0. (a) Phenotype of An-1, Est, Ws-0, and Ler-0 grown in ambient CO2 or low CO2. Scale bar = 2 cm. (b) The number of polymorphic variants (deletions, insertions, and SNPs) of the C4-cycle PEPC gene in accessions An-1, Est, Ws-0, and Ler-0 when compared to the Col-0 reference genome. The calculation was performed using the tool POLYMORPH (http://tools.1001genomes.org/polymorph/).

4 Discussion

Over the evolutionary history of plants, a number of stress-responsive adaptations have arisen to ensure that plants can successfully cope with environmental stresses. In Arabidopsis, intraspecific variation has been reported in responses by different lineages to abiotic stresses and shifts in climate conditions [47]. Our objective for the current study was to investigate potentially heritable phenotypic variation in response to low CO2 stress in Arabidopsis. In this study, the 31 Arabidopsis accessions from different geographic regions (Table 1) were selected for comparison of traits related to reproductive fitness and carbon assimilation under low (100 ppm) CO2 and ambient (380 ppm) CO2, in order to identify the most adaptable accessions under low CO2.

4.1 Arabidopsis showed substantial natural phenotypic variation among wild accessions in response to low CO2

Flowering time is an important determinant of plant fitness and represents a discrete developmental transition in response to environmental conditions [26]. Shifts in flowering time in response to low CO2 availability have previously been observed for some Arabidopsis lines [23,30]. In this study, we observed significant variation in flowering time across accessions. Compared to ambient conditions, 12 accessions, including An-1, Est, Ws-0, and Ler-0, took the same amount of days to reach stage 5.10 under low CO2. Only two accessions, Mc-0 and Rsch-4, flowered earlier (by 4 days) under CO2 limitation, whereas among the 17 late-flowering Arabidopsis accessions, Ts-1 took 54 days more to reach stage 5.10, and Te-0 and Kas-1 died under low CO2 without ever flowering (Figure 1a and b). The delay in first flower opening thus ranged from 1 day (Rsch-4) to 63 days (Lip-0). Two other accessions, Est and Ga-0, died after stage 6.00 under low, but not ambient CO2.

Rosette leaf number is commonly used as a standard indicator of flowering time in Arabidopsis and with late flowering plants typically developing more rosette leaves. In our screen, six accessions An-1, Est, Pa-1, Ws-0, Ler-0, and Sha showed a slight difference in leaf number between treatments, whereas some accessions (Tsu-1, Be-0, Rsch-4, and Mc-0) showed a greater than 50% reduction in rosette leaf number (Figure 3). There is a very strong correlation between the time to flowering and the number of leaves at flowering in Arabidopsis [35], with previous study suggesting that these two traits may be genetically linked in wild accessions [48]. In our experiment, low CO2 treatment delayed flowering time but did not increase the rosette leaf number, although a logical expectation would be that leaf number continues to increase as the duration of vegetative growth prior to flowering is prolonged. This finding agrees with results reported by Salomé et al. [48] for an F2 population derived from natural accessions in which the traits of “days to flower” and “leaf number” were canalized in natural accessions, though the link between the two could be genetically uncoupled. Taken together, these results suggest that response to low CO2 entails a combination of physiological and morphological changes that maximize the efficiency of carbon assimilation in order to maintain consistent reproductive processes.

Changes in CO2 concentration can induce profound effects on plant growth because of the central necessity for CO2 in plant metabolism. Higher atmospheric CO2 concentrations often boost the growth and reproduction of C3 annuals, whereas low CO2 has the opposite effect and decreases plant growth [30,49]. Previous studies showed that low CO2 availability was a limiting factor in plant growth, leading to reduced production of plant biomass [18,23,30,50,51,52,53,54]. However, a delay of first flower opening was common among the 31 accessions under low CO2 stress, the biomass of all accessions in our study decreased. Though all plants in this study, regardless of accession, exhibited a dwarfed morphology and decreased biomass when grown under CO2-starvation conditions, we observed extensive variation in aboveground biomass, which ranged from 58% to greater than 95% lower biomass compared to their growth at full CO2 availability (Figure 2). Furthermore, the accessions that grew the fastest under full, ambient CO2 also showed the greatest reduction in biomass at low CO2, consistent with previous research [55].

In general, subjecting plants to growth at 100 ppm CO2 induced significant changes to vegetative growth and reproductive development across a range of phenotypic traits (Table 2), including later flowering, dwarf stature, reduced biomass, and reduced rosette leaf number, which varied among the Arabidopsis accessions. Thus, individual accessions may have developed an adaptive response to low CO2 that can be used to further determine the genetic variability responsible for this adaptation.

4.2 Altitude of origin did not relate to low-CO2 response

The partial pressure of atmospheric CO2 decreases with the increase in altitude. Arabidopsis accessions adapted to growth at higher altitudes have presumably undergone a stronger selection for growth in lower CO2 concentration than that of low altitude accessions. We hypothesized that adaptation to low CO2 increases along an altitudinal gradient. To test this hypothesis, we used 31 Arabidopsis accessions that were originally collected from a variety of altitudes ranging from 50 to 3,400 m above sea level (Table 1). In Figures 1–5, the Arabidopsis accessions listed on the x-axis (left to right) are arranged by altitude, in the same order as in Table 1. However, we found that the responses to low CO2 for all of the changes in measured traits in this study did not correlate linearly with altitude. For example, although all accessions had significantly lower aboveground biomass at low compared with ambient CO2, six accessions An-1 (50 m), Est (50 m), Pa-1 (50 m), Ws-0 (150 m), Ler-0 (600 m), and Sha (3,400 m) performed much better than Col-0 (50 m) (Figure 2), suggesting that there was no clear differentiation between low-altitude genotypes and high-altitude genotypes. Ward and Strain [23] examined the responses to 20 Pa (200 ppm) CO2 in eight accessions from seven different altitudes between sea level and 3,400 m and found that accessions exhibited limited heritable variation in the response of biomass production. Therefore, in this work, the altitude of origin did not significantly affect vegetative growth in response to low CO2 (100 ppm).

4.3 Ws-0 was least affected by low CO2

In this study, we found that the accessions An-1, Est, Ws-0, and Ler-0 showed less variation in flowering time, shoot biomass, rosette leaf number, and SLW between the two treatments compared to Col-0 (Figures 1–3 and 5). Compared to other accessions, their flowering time and rosette leaf number remained almost the same in the two CO2 treatments, and shoot biomass was significantly less affected than in other accessions. Furthermore, the SLW was less affected by low CO2, compared to accession Col-0. In light of the combined quantitative trait data, Est and Ws-0 were the least affected among these four accessions. As mentioned above, Est did not set seeds under low CO2 (Figure A1), therefore Ws-0 would be the most effective candidate for further quantitative genetics studies.

When we examined the phenotypes of these four accessions grown under low CO2, we found that they did not have a bigger plant size, whereas under ambient CO2, they showed a smaller stature compared to other accessions. Temme et al. [55] reported species with fast growth or largest biomass at ambient CO2 showed the strongest absolute reduction at low CO2. Nitrogen content and photosynthetic rate are strongly affected by low CO2 [18,56,57]. Previous studies have proposed that stress-tolerant plants have lower growth rates (reviewed in ref. [58]). One explanation of our observations is that their smaller stature and relatively slow growth under ambient CO2 is an advantage in response to low CO2. The small stature or slow growth among some plants may indicate low energy and low carbon demands, thus C–N cycle and photosynthesis may be less affected and these plants show less affect when grown under low CO2. If this hypothesis is correct, it can provide us with valuable insight into the mechanisms by which C4 metabolism arose and the reasons why it evolved independently in grasses (i.e., roughly half of the known C4 species are grasses) and also in a number of eudicots, for example, Amaranthaceae, Euphorbiaceae, Asteraceae, and Boraginaceae [59].

In this study, we compared the phenotypic variation in response to low (100 ppm) CO2 among 31 Arabidopsis accessions to assess their relative adaptability through sustained vegetative growth and reproductive development. We found that A. thaliana displays extensive variation in its ability to adapt to low CO2 and that this variation was correlated with their rate of growth under non-CO2-limited conditions, rather than the altitude of origin for individual accessions. In particular, accession Ws-0 showed the least variability between treatments, indicating that it was the best potential candidate for use in further quantitative genetics studies and for isolation of genes underlying low CO2 response. We also propose that a lower growth rate can attenuate the effects of low-CO2 stress, though further experimental evidence is needed to test this hypothesis. Our findings on the physiological effects of growth under low CO2 provide insight into the mechanisms by which individual plants and whole ecosystems may adapt to changes in atmospheric CO2. As atmospheric levels of CO2 rise, our increased understanding of these mechanisms governing carbon assimilation and flowering time during stress can improve our capability to predict the future of natural ecosystems subject to increasingly wide variations in climate.


These authors contributed equally to this work.


Acknowledgments

This work was supported by the Project of Shandong Province Higher Educational Science and Technology Program (J14LE03). The authors thank Prof. Zhaojun Ding from Shandong University and Prof. Zhonghai Ren from Shandong Agricultural University for providing seeds of accessions. The authors thank graduated and undergraduate students who contributed in this work.

Appendix

Figure A1 Three accessions died under low (100 ppm) CO2. Est and Ga-0 accessions died after stage 6.00 when grown in low CO2. The first flower of Est partly opened but withered gradually and died; a portion of the Ga-0 flower buds opened but had no seed in siliques and died under low CO2. The flower buds of Ts-1 failed to open under low CO2 conditions. The scale bars in images of flower buds grown in ambient CO2 indicate 5 cm and those in low CO2 indicate 1 cm.
Figure A1

Three accessions died under low (100 ppm) CO2. Est and Ga-0 accessions died after stage 6.00 when grown in low CO2. The first flower of Est partly opened but withered gradually and died; a portion of the Ga-0 flower buds opened but had no seed in siliques and died under low CO2. The flower buds of Ts-1 failed to open under low CO2 conditions. The scale bars in images of flower buds grown in ambient CO2 indicate 5 cm and those in low CO2 indicate 1 cm.

Figure A2 Genetic difference in C4-cycle genes and C4-related transporter. The number of polymorphic variants (deletions, insertions, and SNPs) of C4-cycle genes and C4-related transporters in accessions An-1, Est, Ler-0, and Ws-0 when compared to the Col-0 reference genome. The calculation was performed using the tool POLYMORPH (http://tools.1001genomes.org/polymorph/).
Figure A2

Genetic difference in C4-cycle genes and C4-related transporter. The number of polymorphic variants (deletions, insertions, and SNPs) of C4-cycle genes and C4-related transporters in accessions An-1, Est, Ler-0, and Ws-0 when compared to the Col-0 reference genome. The calculation was performed using the tool POLYMORPH (http://tools.1001genomes.org/polymorph/).

  1. Conflict of interest: The authors state no conflict of interest.

  2. Data availability statement: The datasets generated during and/or analyzed during the current study are available from the corresponding author on reasonable request.

References

[1] Royer DL. CO2-forced climate thresholds during the Phanerozoic. Geochim Cosmochim Acta. 2006;70(23):5665–75.10.1016/j.gca.2005.11.031Search in Google Scholar

[2] Petit JR, Jouzel J, Raynaud D, Barkov NI, Barnola JM, Basile I, et al. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature. 1999;399(6735):429–36.10.1038/20859Search in Google Scholar

[3] Beerling DJ. Atmospheric carbon dioxide: a driver of photosynthetic eukaryote evolution for over a billion years? Philos Trans R Soc B Biol Sci. 2012;367(1588):477–82.10.1098/rstb.2011.0276Search in Google Scholar

[4] Leakey ADB, Lau JA. Evolutionary context for understanding and manipulating plant responses to past, present and future atmospheric [CO2]. Philos Trans R Soc B Biol Sci. 2012;367(1588):613–29.10.1098/rstb.2011.0248Search in Google Scholar

[5] Terashima I, Yanagisawa S, Sakakibara H. Plant responses to CO2: background and perspectives. Plant Cell Physiol. 2014;55(2):237–40.10.1093/pcp/pcu022Search in Google Scholar

[6] van Rooijen R, Kruijer W, Boesten R, van Eeuwijk FA, Harbinson J, Aarts MGM. Natural variation of YELLOW SEEDLING1 affects photosynthetic acclimation of Arabidopsis thaliana. Nat Commun. 2017;8(1):1421.10.1038/s41467-017-01576-3Search in Google Scholar

[7] Thompson M, Gamage D, Hirotsu N, Martin A, Seneweera S. Effects of elevated carbon dioxide on photosynthesis and carbon partitioning: a perspective on root sugar sensing and hormonal crosstalk. Front Physiol. 2017;8:578.10.3389/fphys.2017.00578Search in Google Scholar

[8] Dong J, Gruda N, Lam SK, Li X, Duan Z. Effects of elevated CO2 on nutritional quality of vegetables: a review. Front Plant Sci. 2018;9:924.10.3389/fpls.2018.00924Search in Google Scholar

[9] Franks PJ, Beerling DJ. Maximum leaf conductance driven by CO2 effects on stomatal size and density over geologic time. Proc Nat Acad Sci U S A. 2009;106(25):10343–7.10.1073/pnas.0904209106Search in Google Scholar

[10] Royer DL. Stomatal density and stomatal index as indicators of paleoatmospheric CO2 concentration. Rev Palaeobot Palynol. 2001;114(1–2):1–28.10.1016/S0034-6667(00)00074-9Search in Google Scholar

[11] Boyce CK, Brodribb TJ, Feild TS, Zwieniecki MA. Angiosperm leaf vein evolution was physiologically and environmentally transformative. Pro R Soc B Biol Sci. 2009;276(1663):1771–6.10.1098/rspb.2008.1919Search in Google Scholar

[12] Brodribb TJ, Feild TS. Leaf hydraulic evolution led a surge in leaf photosynthetic capacity during early angiosperm diversification. Ecol Lett. 2010;13:175–83.10.1111/j.1461-0248.2009.01410.xSearch in Google Scholar

[13] Cerling TE, Harris JM, MacFadden BJ, Leakey MG, Quade J, Eisenmann V, et al. Global vegetation change through the Miocene/Pliocene boundary. Nature. 1997;389(389):153–8.10.1038/38229Search in Google Scholar

[14] Christin PA, Besnard G, Samaritani E, Duvall MR, Hodkinson TR, Savolainen V, et al. Oligocene CO2 decline promoted C4 photosynthesis in grasses. Curr Biol. 2008;18(1):37–43.10.1016/j.cub.2007.11.058Search in Google Scholar

[15] Edwards EJ, Osborne CP, Stromberg CAE, Smith SA, Bond WJ, Christin PA, et al. The origins of C4 grasslands: integrating evolutionary and ecosystem science. Science. 2010;328(5978):587–91.10.1126/science.1177216Search in Google Scholar

[16] Osborne CP, Beerling DJ. Nature’s green revolution: the remarkable evolutionary rise of C4 plants. Philos Trans R Soc B Biol Sci. 2006;361(1465):173–94.10.1098/rstb.2005.1737Search in Google Scholar

[17] Pagani M, Zachos JC, Freeman KH, Tipple B, Bohaty S. Marked decline in atmospheric carbon dioxide concentrations during the Paleogene. Science. 2005;309(5734):600–3.10.1126/science.1110063Search in Google Scholar

[18] Gerhart LM, Ward JK. Plant responses to low [CO2] of the past. N Phytol. 2010;188(3):674–95.10.1111/j.1469-8137.2010.03441.xSearch in Google Scholar

[19] Billings WD, Clebsch EEC, Mooney HA. Effect of low concentrations of carbon dioxide on photosynthesis rates of two races of Oxyria. Science. 1961;133(3467):1834.10.1126/science.133.3467.1834Search in Google Scholar

[20] Alonso-Blanco C, Koornneef M. Naturally occurring variation in arabidopsis: an underexploited resource for plant genetics. Trends Plant Sci. 2000;5(1):22–9.10.1016/S1360-1385(99)01510-1Search in Google Scholar

[21] Hoffmann MH. Biogeography of Arabidopsis thaliana (L.) Heynh. (Brassicaceae). J Biogeogr. 2002;29(1):125–34.10.1046/j.1365-2699.2002.00647.xSearch in Google Scholar

[22] Sharma RK, Griffing B, Scholl RL. Variations among races of Arabidopsis thaliana (L.) Heynh for survival in limited carbon dioxide. Theor Appl Genet. 1979;54(1):11–5.10.1007/BF00265702Search in Google Scholar

[23] Ward JK, Strain BR. Effects of low and elevated CO2 partial pressure on growth and reproduction of Arabidopsis thaliana from different elevations. Plant Cell Envion. 1997;20(2):254–60.10.1046/j.1365-3040.1997.d01-59.xSearch in Google Scholar

[24] Ward JK, Kelly JK. Scaling up evolutionary responses to elevated CO2: lessons from Arabidopsis. Ecol Lett. 2004;7(5):427–40.10.1111/j.1461-0248.2004.00589.xSearch in Google Scholar

[25] Weigel D. Natural variation in Arabidopsis: from molecular genetics to ecological genomics. Plant Physiol. 2012;158(1):2–22.10.1104/pp.111.189845Search in Google Scholar

[26] Engelmann K, Purugganan M. The molecular evolutionary ecology of plant development: flowering time in Arabidopsis thaliana. Adv Bot Res. 2006;44:507–26.10.1016/S0065-2296(06)44013-1Search in Google Scholar

[27] Banerjee S, Siemianowski O, Liu M, Lind KR, Tian X, Nettleton D, et al. Stress response to CO2 deprivation by Arabidopsis thaliana in plant cultures. PLoS One. 2019;14(3):e0212462.10.1371/journal.pone.0212462Search in Google Scholar PubMed PubMed Central

[28] Eisenhut M, Brautigam A, Timm S, Florian A, Tohge T, Fernie AR, et al. Photorespiration is crucial for dynamic response of photosynthetic metabolism and stomatal movement to altered CO2 availability. Mol Plant. 2017;10(1):47–61.10.1016/j.molp.2016.09.011Search in Google Scholar PubMed

[29] Blume C, Ost J, Mühlenbruch M, Peterhänsel C, Laxa M. Low CO2 induces urea cycle intermediate accumulation in Arabidopsis thaliana. PLoS One. 2019;14(1):e0210342.10.1371/journal.pone.0210342Search in Google Scholar PubMed PubMed Central

[30] Li Y, Xu J, Haq NU, Zhang H, Zhu XG. Was low CO2 a driving force of C4 evolution: Arabidopsis responses to long-term low CO2 stress. J Exp Bot. 2014;65(13):3657–67.10.1093/jxb/eru193Search in Google Scholar PubMed PubMed Central

[31] Liu L, Shen F, Xin C, Wang Z. Multi-scale modeling of Arabidopsis thaliana response to different CO2 conditions: From gene expression to metabolic flux. J. Int Plant Biol. 2016;58(1):2–11.10.1111/jipb.12370Search in Google Scholar PubMed

[32] Boyes DC, Zayed AM, Ascenzi R, McCaskill AJ, Hoffman NE, Davis KR, et al. Growth stage–based phenotypic analysis of Arabidopsis: a model for high throughput functional genomics in plants. Plant Cell. 2001;13(7):1499–510.10.1105/TPC.010011Search in Google Scholar

[33] Koornneef M, Alonso-Blanco C, Vreugdenhil D. Naturally occurring genetic variation in Arabidopsis thaliana. Annu Rev Plant Biol. 2004;55(1):141–72.10.1146/annurev.arplant.55.031903.141605Search in Google Scholar PubMed

[34] Younginger BS, Sirová D, Cruzan MB, Ballhorn DJ. Is biomass a reliable estimate of plant fitness? Appl Plant Sci. 2017;5(2):1600094.10.3732/apps.1600094Search in Google Scholar PubMed PubMed Central

[35] Koornneef M, Hanhart CJ, van der Veen JH. A genetic and physiological analysis of late flowering mutants in Arabidopsis thaliana. Mol Gen Genet. 1991;229(1):57–66.10.1007/BF00264213Search in Google Scholar PubMed

[36] Du Q-S, Fan X-W, Wang C-H, Huang R-B. A possible CO2 conducting and concentrating mechanism in plant stomata SLAC1 channel. PLoS One. 2011;6(9):e24264.10.1371/journal.pone.0024264Search in Google Scholar PubMed PubMed Central

[37] Jakobson L, Vaahtera L, Tõldsepp K, Nuhkat M, Wang C, Wang YS, et al. Natural variation in Arabidopsis Cvi-0 accession reveals an important role of MPK12 in guard cell CO2 signaling. PLoS Biol. 2016;14(12):e2000322.10.1371/journal.pbio.2000322Search in Google Scholar PubMed PubMed Central

[38] Drake PL, de Boer HJ, Schymanski SJ, Veneklaas EJ. Two sides to every leaf: water and CO2 transport in hypostomatous and amphistomatous leaves. N Phytol. 2019;222(3):1179–87.10.1111/nph.15652Search in Google Scholar PubMed

[39] Hassiotou F, Ludwig M, Renton M, Veneklaas EJ, Evans JR. Influence of leaf dry mass per area, CO2, and irradiance on mesophyll conductance in sclerophylls. J Exp Bot. 2009;60(8):2303–14.10.1093/jxb/erp021Search in Google Scholar PubMed

[40] Niinemets Ü. Research review. Components of leaf dry mass per area – thickness and density – alter leaf photosynthetic capacity in reverse directions in woody plants. N Phytol. 1999;144(1):35–47.10.1046/j.1469-8137.1999.00466.xSearch in Google Scholar

[41] Niinemets Ü, Portsmuth A, Tena D, Tobias M, Matesanz S, Valladares F. Do we underestimate the importance of leaf size in plant economics? Disproportional scaling of support costs within the spectrum of leaf physiognomy. Ann Bot. 2007;100(2):283–303.10.1093/aob/mcm107Search in Google Scholar PubMed PubMed Central

[42] Terashima I, Hanba YT, Tazoe Y, Vyas P, Yano S. Irradiance and phenotype: comparative eco-development of sun and shade leaves in relation to photosynthetic CO2 diffusion. J Exp Bot. 2006;57(2):343–54.10.1093/jxb/erj014Search in Google Scholar PubMed

[43] Monson RK, Teeri JA, Ku MS, Gurevitch J, Mets LJ, Dudley S. Carbon-isotope discrimination by leaves of Flaveria species exhibiting different amounts of C3-and C4-cycle co-function. Planta. 1988;174(2):145–51.10.1007/BF00394765Search in Google Scholar PubMed

[44] Farquhar GD, Ehleringer JR, Hubick KT. Carbon isotope discrimination and photosynthesis. Annu Rev Plant Physiol Plant Mol Biol. 1989;40:503–37.10.1146/annurev.pp.40.060189.002443Search in Google Scholar

[45] You L, Zhang J, Li L, Xiao C, Feng X, Chen S, et al. Involvement of abscisic acid, ABI5, and PPC2 in plant acclimation to low CO2. J Exp Bot. 2020 Jul 6;71(14):4093–108.10.1093/jxb/eraa148Search in Google Scholar PubMed PubMed Central

[46] Carlson KD, Fernandez-Pozo N, Bombarely A, Pisupati R, Mueller LA, Madlung A. Natural variation in stress response gene activity in the allopolyploid Arabidopsis suecica. BMC Genom. 2017;18(1):653.10.1186/s12864-017-4067-xSearch in Google Scholar PubMed PubMed Central

[47] Assmann SM. Natural variation in abiotic stress and climate change responses in Arabidopsis: implications for twenty-first-century agriculture. Int J Plant Sci. 2013;174(1):3–26.10.1086/667798Search in Google Scholar

[48] Salomé PA, Bomblies K, Laitinen RA, Yant L, Mott R, Weigel D. Genetic architecture of flowering-time variation in Arabidopsis thaliana. Genetics. 2011;188(2):421–33.10.1534/genetics.111.126607Search in Google Scholar PubMed PubMed Central

[49] Ward JK. Evolution and growth of plants in a low CO2 world. Ecol Stud. 2005;177:232–57.10.1007/0-387-27048-5_11Search in Google Scholar

[50] Polley HW, Johnson HB, Mayeux HS, Malone SR. Physiology and growth of wheat across a subambient carbon dioxide gradient. Ann Bot. 1993;71(4):347–56.10.1006/anbo.1993.1044Search in Google Scholar

[51] Polley HW, Johnson HB, Marino BD, Mayeux HS. Increase in C3 plant water-use efficiency and biomass over Glacial to present CO2 concentrations. Nature. 1993;361(6407):61–4.10.1038/361061a0Search in Google Scholar

[52] Dippery JK, Tissue DT, Thomas RB, Strain BR. Effects of low and elevated CO2 on C3 and C4 annuals. I. Growth and biomass allocation. Oecologia. 1995;101(1):15–20.Search in Google Scholar

[53] Sage RF. Was low atmospheric CO2 during the Pleistocene a limiting factor for the origin of agriculture? Glob Change Biol. 1995;1(2):93–106.10.1111/j.1365-2486.1995.tb00009.xSearch in Google Scholar

[54] Sage RF, Coleman JR. Effects of low atmospheric CO2 on plants more than a thing of the past. Trends Plant Sci. 2001;6(1):18–24.10.1016/S1360-1385(00)01813-6Search in Google Scholar

[55] Temme AA, Liu JC, Cornwell WK, Cornelissen JH, Aerts R. Winners always win: growth of a wide range of plant species from low to future high CO2. Ecol Evol. 2015;5(21):4949–61.10.1002/ece3.1687Search in Google Scholar PubMed PubMed Central

[56] Temme AA, Cornwell WK, Cornelissen JH, Aerts R. Meta-analysis reveals profound responses of plant traits to glacial CO2 levels. Ecol Evol. 2013;3(13):4525–35.10.1002/ece3.836Search in Google Scholar PubMed PubMed Central

[57] Becklin K, Medeiros J, Sale K, Ward J. Evolutionary history underlies plant physiological responses to global change since the last glacial maximum. Ecol Lett. 2014;17(6):691–9.10.1111/ele.12271Search in Google Scholar PubMed PubMed Central

[58] Chapin FS. Integrated responses of plants to stress: a centralized system of physiological responses. BioSci. 1991;41(1):29–36.10.2307/1311538Search in Google Scholar

[59] Sage RF, Stata M. Photosynthetic diversity meets biodiversity: the C4 plant example. J Plant Physiol. 2015;172:104–19.10.1016/j.jplph.2014.07.024Search in Google Scholar PubMed

Received: 2020-05-08
Revised: 2020-08-19
Accepted: 2020-08-29
Published Online: 2020-12-21

© 2020 Chunxia Wu et al., published by De Gruyter

This work is licensed under the Creative Commons Attribution 4.0 International License.

Downloaded on 20.4.2024 from https://www.degruyter.com/document/doi/10.1515/biol-2020-0095/html
Scroll to top button