Sec. Plant Nutrition
Elevated-CO2 Response of Stomata and Its Dependence on Environmental Factors
- 1State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China
- 2Chinese Academy of Meteorological Sciences, Beijing, China
Stomata control the flow of gases between plants and the atmosphere. This review is centered on stomatal responses to elevated CO2 concentration and considers other key environmental factors and underlying mechanisms at multiple levels. First, an outline of general responses in stomatal conductance under elevated CO2 is presented. Second, stomatal density response, its development, and the trade-off with leaf growth under elevated CO2 conditions are depicted. Third, the molecular mechanism regulating guard cell movement at elevated CO2 is suggested. Finally, the interactive effects of elevated CO2 with other factors critical to stomatal behavior are reviewed. It may be useful to better understand how stomata respond to elevated CO2 levels while considering other key environmental factors and mechanisms, including molecular mechanism, biochemical processes, and ecophysiological regulation. This understanding may provide profound new insights into how plants cope with climate change.
Elevated atmospheric carbon dioxide concentration (elevated CO2) is a major component of climate change. It has increased from the pre-industrial level of 280 μmol mol-1 in 1750 to c. 400 μmol mol-1 at present and is expected to increase to c. 900 μmol mol-1 by the end of the 21st century. The global surface temperature is projected to rise 2.6–4.8°C by the end of this century, according to RCP8.5 (IPCC, 2013), a more undisciplined management scenario. Climate change, including elevated CO2, rising temperatures, and altered precipitation patterns, have markedly affected terrestrial ecosystem structure and function, carbon and water balance, and crop productivity (Lobell et al., 2011; Peñuelas et al., 2013; Ruiz-Vera et al., 2013; Bagley et al., 2015; Lavania et al., 2015). Moreover, a profound interaction between climate change and other critical environmental factors, including limited nutrition and air pollution, as well as some biotic factors, such as herbivorous insects, may intensify the adverse impacts (Gillespie et al., 2012; Peñuelas et al., 2013; Xu et al., 2013; Zavala et al., 2013; Sun et al., 2015; Xu et al., 2016).
Many studies have reported the biological responses to CO2 enrichment and their interaction with environmental change at various levels (Ainsworth and Rogers, 2007; Medeiros et al., 2015; Xu et al., 2015; Rodrigues et al., 2016). Elevated CO2 generally can enhance CO2 fixation and consequently plant growth and production (Ainsworth and Rogers, 2007; Xu et al., 2013). On the other hand, the decrease in stomatal conductance (gs) under elevated CO2 conditions may limit the CO2 fixation rate but promote water use efficiency (WUE) to benefit plant growth, especially within a climate change context where water shortage periods are expected to increase (Leakey et al., 2009; Sreeharsha et al., 2015).
Of these responses, the stomata are pivotal doors that control the gas exchange between vegetation and the atmosphere, i.e., CO2 entering from the atmosphere and water vapor releasing from plants into the atmosphere (Woodward, 1987). Carbon dioxide can reach the fixed Rubisco site through CO2 gas diffusions from the boundary layer, stomata, and intercellular airspaces near the chloroplast (Ball et al., 1987; Woodward, 1987; Warren, 2008). The main factors controlling stomatal opening processes include Ca2+ level, guard cell turgor, and hormones (Assmann, 1999; Lawson et al., 2014). Stomatal behavior may be affected by environmental factors, such as water status (e.g., soil water deficit, vapor pressure deficit [VPD]), temperature, CO2 concentrations, and light either alone and/or in combination (e.g., Lee et al., 2008; Perez-Martin et al., 2009; Hubbart et al., 2013; Laanemets et al., 2013; Šigut et al., 2015). Furthermore, stomatal short-term behavior (e.g., stomatal closure) and a long-term developmental (e.g., stomatal size and its density) responses to environmental changes might occur together, depending on species and genotypes (Gray et al., 2000; Ainsworth and Rogers, 2007; Haworth et al., 2013; DaMatta et al., 2016).
Our review focuses on the stomatal responses to elevated CO2 conditions with climatic change as well as the relevant metabolic processes and underlying mechanisms. The future perspectives for this study and possible implications are briefly presented and discussed. The present report may advance our current knowledge of the stomatal response to climatic change. It may also provide a new vision of its interdisciplinary and systematic synthesis to promote further relevant research.
Stomatal Response to Elevated Co2
Elucidating the stomatal response to CO2 concentrations is important for understanding the stomatal physiology and gas exchanges between vegetation and the atmosphere. To adapt CO2 intake for photosynthesis and water release for transpiration, plants need to mediate stomatal development and behavior to balance CO2 and water exchange through the leaf epidermis in a changing environment (Gray et al., 2000; Haworth et al., 2013; Lawson et al., 2014). Elevated CO2 generally causes reductions in stomatal density (SD, e.g., Woodward, 1987; Lin et al., 2001; Teng et al., 2009), stomatal conductance (Medlyn et al., 2001; Ainsworth and Rogers, 2007; Gao et al., 2015), leaf transpiration (Teng et al., 2009; Katul et al., 2010), and canopy/ecosystem evapotranspiration (Medlyn et al., 2001; Bernacchi et al., 2007; Leakey et al., 2009; Bernacchi and VanLoocke, 2015). However, some studies have challenged this response because the reverse response might occur when elevated CO2 interacts with other climatic factors (see the sections below).
Stomatal Conductance Response
The decreased magnitude of gs by CO2 enrichment greatly depends on environmental variables and species (Medlyn et al., 2001; Ainsworth and Rogers, 2007; Haworth et al., 2013; Ward et al., 2013). In an earlier report, doubled ambient CO2 decreased gs by c. 40% in almost all enclosure experiments, such as greenhouse and chamber experiments (Kimball et al., 1993; Morison and Lawlor, 1999). A 50% gs decrease induced by elevated CO2 was found (Jackson et al., 1994), and a synthesis report showed a 21% gs decrease in trees (Medlyn et al., 2001). A model scaling from leaf-level to canopy indicated that elevated CO2 might reduce canopy gs by 16% (Baldocchi and Harley, 1995). According to a meta-analysis, the elevated CO2-induced gs reduction in free air CO2 enrichment (FACE) experiments was averaged 22% across all plant species (n = c. 580). A significant variation among plant functional types (PFTs) was obtained: a maximum decease for C3 grass (30–40%) and a minimum decrease for shrub species (c. 15%; Ainsworth and Rogers, 2007). However, in a few experiments, gs did not respond to CO2 concentrations in an obvious way (Ellsworth et al., 2011; Haworth et al., 2013; Ward et al., 2013; Bernacchi and VanLoocke, 2015; DaMatta et al., 2016). The gs increase was even observed (Uddling et al., 2009) with short-term CO2 fertilization, for instance, in A. thaliana (Zinta et al., 2014). A recent experiment also found 23 and 18% gs increases from elevated CO2 conditions in during vegetative and reproductive growth phases, respectively, of the Pigeon pea (Cajanus cajan L.; Sreeharsha et al., 2015). In a recent finding, the Arabidopsis Tetraploid, Me-0, with larger stomata, still had a comparatively high gs when exposed to increased CO2 concentrations, suggesting that taller plants with larger stomatal size can better deal with rising CO2 by improving their stomatal behavior (Monda et al., 2016). Thus, the decrease in gs due to elevated CO2 is a general rather than a universal response due to some unexpected factors’ effects. This difference is particularly found in dramatic ecotypes-, species-, PFTs-, and development stages. As such, the underlying mechanism remains to be clarified further.
Interaction of gs, A, and WUE
The decrease in gs generally leads to a decrease in net assimilation rate (A) and is recognized as one of the two major limitations of photosynthesis; the other is non-stomatal limitation (Noormets et al., 2001). There was no obvious evidence from FACE that gs independently acclimated to elevated CO2 levels despite exposure time (Nijs et al., 1997; Leakey et al., 2006a; Ainsworth and Rogers, 2007; Gao et al., 2015). An earlier model by Ball et al. (1987) predicted that gs may be restricted when down-regulation in A occurs in response to CO2 enrichment. Although stomatal limitation to photosynthesis may decrease with elevated CO2 levels (e.g., Noormets et al., 2001), the uncoupling of gs with A has been confirmed in a transgenic tobacco plant due to its reduced Rubisco content (von Caemmerer et al., 2004). However, an experiment has shown that a high A caused by increasing gs can be maintained in a rice mutant that has a deficient slow anion channel 1 (SLAC1), that is, a guard cell anion channel protein that does not respond to rising CO2 levels (Kusumi et al., 2012). Furthermore, a recent experiment indicated that, with elevated CO2, Cajanus cajan leaves had 7–18% higher leaf instantaneous WUE (WUEi) due to simultaneously maintaining both higher A and gs. However, the former was higher than the latter (Sreeharsha et al., 2015). It is also noteworthy that at a high CO2 levels, a significant gs decrease in C4 plants, such as maize, may occur only during drought, leading to WUE promotion rather than enhanced photosynthetic capacity as a result of the gs decrease (Leakey et al., 2006b, 2009). A recent report by Lawson and Blatt (2014) has indicated that although stomatal responses to environmental changes may be closely associated with CO2 assimilation and water transpiration, a better balance between CO2 uptake and water loss may be improved by manipulating guard cell physical, anatomical, and transport characteristics to promote WUE (Lawson and Blatt, 2014). This may need further testing under elevated CO2 conditions.
Stomatal Development and Its Density
Response Magnitude of Stomatal Density
A decrease in SD is considered a general response to elevated CO2. As reported by Woodward (1987), as CO2 levels from the pre-industrial level of 280 μmol mol-1 rose to the ambient level of 340 μmol mol-1 in 1987, a dramatic (67%) decrease in SD was found in the leaves of herbarium specimens and in experiments under controlled environmental conditions. Based on a paleobotanic analysis of fossil Buxus (3775–3640 BC) by Rivera et al. (2014), the SD and stomatal index (SI) had significantly greater values than the current Buxus balearica and B. sempervirens species (297.6 vs. 227.8 stomata mm-2, 12.7 vs. 8.0%, respectively). The dramatic declines are closely associated with a drastic increase in atmospheric CO2 concentration that has been occurring since the mid-Holocene era (Joos et al., 2004; Rivera et al., 2014). However, only a 5% SD decrease due to elevated CO2 was obtained from a meta-analysis on stomatal response (Ainsworth and Rogers, 2007). Relatively few studies reported an unchanged (Tricker et al., 2005) or even increased SD (Reid et al., 2003). A recent report by Field et al. (2015) showed that SD in non-vascular land plants, such as hornwort (Anthoceros punctatus, Phaeoceros laevis) and some moss sporophytes, did not respond to CO2 enrichment. It was even slightly increased in Funaria hygrometrica sporophytes at elevated CO2. A recent report showed the appearance of SD responses to elevated CO2 depends on tropic coffee genotypes (Rodrigues et al., 2016). These findings imply that the magnitude of SD response to CO2 enrichment might easily vary according to the experimental facility, experimental duration, species/genotypes, and other environmental variables (e.g., Ainsworth and Rogers, 2007; Haworth et al., 2013; Rodrigues et al., 2016). Thus, considerable caution is required when using SD as an indicator of a stomatal adaptive process in response to elevated atmospheric CO2 concentration.
Stomatal Development under Elevated CO2
The relevant genes may be involved in stomatal development under elevated CO2 conditions (Gray et al., 2000). The Arabidopsis gene hic (high carbon dioxide) encodes a negative regulator of stomatal development that responds to CO2 concentrations and can be adversely regulated by elevated CO2. A 42% increase in SD in the mutant hic plants was evidence of a doubled CO2 level (Gray et al., 2000). Arabidopsis plants with the GTL1 gene have higher transpiration and lower WUE due to regulation of SD via transrepression of SD and distribution 1 (SDD1; Yoo et al., 2010). As reported by Engineer et al. (2014), the extracellular pro-peptide-encoding gene epidermal patterning factor 2 (EPF2) in wild-type Arabidopsis can be induced by elevated CO2, possibly providing an essential role for CO2 control of stomatal development. Furthermore, in the β-carbonic anhydrase double mutants (ca1, ca4), a secreted protease CRSP may cleave the EPF2 and then repress stomatal development, demonstrating an inverse response of the wild-type plants to elevated CO2. This partly elucidates the key mechanisms of how the sensing and transduction CO2 signals are linked to stomatal development (Engineer et al., 2014). This finding also indicates that some transduction signals between stomata and nearby pavement cells (PCs) may be involved in abscisic acid (ABA)-mediated inhibition of PC enlargement and may ultimately affect stomatal distribution and its density (Tanaka et al., 2013a). It has been suggested that the signals are peptide hormones (Hunt et al., 2010; Sugano et al., 2010; Jewaria et al., 2013; Lee et al., 2015; see below). However, a clear role of the response of stomatal development to elevated CO2 remains largely unknown. A description on the genes regarding stomatal development in response to CO2 concentration are listed in Table 1.
Stomatal Density and A under Elevated CO2
Photosynthetic capacity is closely linked to SD (Xu and Zhou, 2008). Leaf A was negatively correlated with SD when plants were exposed to elevated CO2 (Woodward, 1987; Ainsworth and Rogers, 2007), whereas a positive correlation occurred when grass was subjected to a water status gradient (Xu and Zhou, 2008). Moreover, photosynthetic potential might be enhanced with increased SD in Arabidopsis by a modulating gas diffusion function, as was recently reported by Tanaka et al. (2013b). In this case, the A increase at elevated CO2 is tightly associated with increased SD. Here, the stomagen gene overexpression confers a positive response to stomatal development in A. thaliana (Hunt et al., 2010; Doheny-Adams et al., 2012; Tanaka et al., 2013b). As recently reported, an EP3 gene in rice may be responsible for guard cell development, which may determine SD. This is due to the ep3 mutant plants exhibiting a smaller GC with low SD, gs, and A compared with their wild-type controls (Yu et al., 2015).
Trade-off between Stomatal Density and Leaf Growth under Elevated CO2
The response and feedback of SD with leaf growth to elevated CO2 may be described generally in a linkage network (Figure 1). A general SD decrease in CO2 enrichment may have several possible coherent explanations. (1) The promotion of a leaf area may contribute to a lower SD. For instance, the leaf area in grass plants markedly increased under elevated CO2 (Xu et al., 2014), possibly reducing the SD (Xu and Zhou, 2008; Xu et al., 2009b). An 11–23% decrease in SD by in Scots pine (Pinus sylvestris) needles by high CO2 conditions might result from an increase in needle thickness and needle width, i.e., the surface area of the entire needle. Thus, this structural plasticity may often occur in short-term elevated CO2 fertilization. (2) With long-term elevated CO2, the relevant gene expression levels may contribute to the diminishment of stomatal development, leading to a reduction in SD (e.g., Gray et al., 2000; Engineer et al., 2014). (3) The coordination of other key environmental factors may together regulate changes in SD. For instance, a moderate water deficit may increase SD due to a potential acclimated response, whereas excessive watering or severe water deficit stress decreases SD by inhibiting GCs (Xu and Zhou, 2008; Xu et al., 2009b). This suggests that the former would encounter an SD decline due to rising CO2, and the latter would accelerate its reduction further (Woodward, 1987; Xu and Zhou, 2008; Xu et al., 2009b).
FIGURE 1. A representation of the response to elevated CO2 (eCO2) with abiotic factor stress on stomatal density (SD) under regulation by leaf growth. Elevated CO2 may lead to an acclimated reduction in SD by inhibition of guard cells, which involves the regulation of gene expression and adaptive evolution (1); meanwhile, eCO2 could promote leaf enlargement (2) consequently decreasing SD (3). A severe abiotic stress factor such as drought may diminish leaf enlargement (4), ultimately increasing SD (5); it may directly decrease SD due to inhibition of guard cell development (6). However, under moderate stress, SD may be increased possibly due to an acclimated response (7). In summary, this synergic increase (8) or trade-off interaction (9) may occur between the effects of both leaf growth and changes in SD toward the variations in eCO2 under abiotic stress, ultimately determining SD.
Similarly, a temperature higher than optimum may limit leaf enlargement, leading to increased SD, but moderate warming may do the opposite. In fact, both temperature and water status or their interaction might regulate stomatal development and distribution in response to CO2 enrichment. This would ultimately determine SD due to the trade-off, depending on environmental stresses or species-specific adaptation (Fraser et al., 2009; Xu et al., 2009b; Locosselli and Ceccantini, 2013; Figure 1), which still remains elusive to some extent. As reported by Pyakurel and Wang (2014), elevated CO2 can reduce the leaf area and increase the SD of birch plants, demonstrating high resistance to water deficit stress. Moreover, an interaction between elevated CO2 and light may also determine SD. For example, rice leaf SD was slightly decreased by elevated CO2 or by decreased light irradiance. However, the effect of light on SD may be diminished by elevated CO2 (Hubbart et al., 2013). Thus, multifaceted effects on SD responses to elevated CO2 need to be further clarified.
Molecular Mechanisms Controlling Guard Cell in Response to Elevated CO2
General Molecular Mechanism
Guard cell (GC) metabolism and the signal transduction network have been reviewed in several reports (e.g., Lawson et al., 2014; Negi et al., 2014). Here, we succinctly present the findings of these reports, particularly the explanations concerning the regulation of CO2 concentration (Figure 2). Generally, ion and organic solute concentration levels determine the turgor pressure of guard cells and subsequently affect stomatal aperture. Under elevated CO2, stomata tend to close because a greater depolarization seems to appear in GCs. The process may be controlled by (1) a decrease in K+ concentration, with enhanced activity in outward rectifying K+ channels and decreased inward activity, (2) decreased cytosolic Ca2+ in GCs, (3) decreased Cl- and malate (Mal2-) concentrations by stimulating the release of Cl- and Mal2- from GCs resulting from the activation of S-type anion channels, and (4) by decreases in the cytosolic zeaxanthin level and the pH value in GCs. Together, these factors lead to a decline in GC turgor, causing the GCs to shrink and the stomatal aperture to close (e.g., Webb et al., 1996; Zhu et al., 1998; Assmann, 1999; Schroeder et al., 2001; Fujita et al., 2013; Lawson et al., 2014). The potential messengers in the stomatal response to CO2 concentrations mainly include ion channel activity, cytosolic free calcium, ABA, malate levels, membrane potential, pH gradients, zeaxanthin content in chloroplasts, photosynthesis-derived ATP content, protein phosphorylation, and dephosphorylation processes (McAinsh et al., 1990; Schroeder et al., 2001; Ainsworth and Rogers, 2007; Kim et al., 2010; Wang et al., 2013; Lawson et al., 2014). For instance, the experiments have shown that elevated CO2 can enhance anion channel activity in GCs to induce stomatal closure. In this event, the SLAC1 protein provides or regulates a gate for anion transport (Raschke et al., 2003; Marten et al., 2008; Vahisalu et al., 2008; Negi et al., 2014; Yamamoto et al., 2016).
FIGURE 2. Possible stomatal response mechanisms controlling guard cells (GC) under elevated CO2. With rising CO2, a depolarization in GCs appears: the levels of K+, Ca2+, Cl-, and zeaxanthin (Zea) may decrease (1), whereas the H+ concentration may remain at a high level (2) leading to a lower pH value. The pH gradient (3), protein phosphorylation (4), and photosynthesis-derived ATP (5, 6) are involved in the regulation process by modifying channel activities; together, they promote osmotic regulation (7) and decrease GC turgor (8) consequently causing the GCs to drain water (9) leading to stomatal closure to some extent (10). Meanwhile, Calvin–Benson–Basshan (CBB) cycle and sugar metabolism in GC may produce less malate (Mal2-), (11) and sucrose (Suc) (12) with triose phosphate (triose-P) at eCO2, which also affects osmotic regulation. Furthermore, elevated CO2 may reduce Suc accumulation in the vicinity of the GC wall from the mesophyll due to the limitation of some apoplastic Suc in the transpiration stream toward GC (13) and enhance Mal2- transport from GCs into mesophyll cells by stimulating anion efflux through channels such as GCAG1 and the potential involvement of the AtABCB14 gene (14), also resulting in stomatal closure. Finally, hexokinase (HXK) involvement may limit sugar synthesis and its entrance into GCs from mesophyll cells (15) and then inducing stomatal closure (e.g., Webb et al., 1996; Assmann, 1999; Schroeder et al., 2001; Kang et al., 2007; Lee et al., 2008; Kim et al., 2010; Fujita et al., 2013; Kelly et al., 2013; Lawson et al., 2014; Negi et al., 2014).
Role of Sugar
In the guard cell itself, major reports have provided evidence that GCs may play only a trivial role in the regulation of the stomatal aperture, including osmotic adjustments. As such, GSs have a limited photosynthetic capacity, fewer chloroplasts, low electron transport, and relatively lower levels of relevant metabolites, such as those related to ATP and NADPH, sucrose (Suc), and malate (Outlaw, 1989; Reckmann et al., 1990; Lawson et al., 2003; Lawson et al., 2014). Some studies support that the apoplastic Suc, where occurs in some cell walls of GCs from mesophyll cells as an osmoticum, may be responsible for the stomatal opening (Lawson et al., 2003; Kang et al., 2007). An early starch-sugar hypothesis suggested sugars, such as Suc, which is the end product of photosynthesis, may be derived from starch degradation in mesophyll cells and may play an important role in linking mesophyll photosynthesis to GC function (Pallas, 1964; Tallman and Zeiger, 1988; Ni, 2012). However, this hypothesis is still not well tested. With the ambiguous role of sugars in stomatal regulation, the role of Suc as a major osmoticum driving stomatal movement has been debated. However, Suc may still play a critical role in interrelating mesophyll and stomatal behavior, possibly via apoplasts. Thus, Suc role is implicated in a feedback-inhibition mechanism with an expression of hexokinase (HXK) in GCs when the Suc production rate exceeds the efflux rate at which Suc is loaded into the phloem (Kelly et al., 2013) under elevated CO2 conditions (Cheng et al., 1998; Long et al., 2004; Ainsworth and Rogers, 2007). A HXK-induced expression of ABA-related genes leads to a decrease in the influx of apoplastic sugar entering the GCs from the mesophyll, which may coordinate photosynthesis with transpiration by coupling with a stomatal closure (Kang et al., 2007; Kelly et al., 2013). It highlights the pivotal role of HXK. Moreover, a limitation to a carbon sink or transportation of sugar from shoot to root via the phloem leads to the accumulation of sugar in shoots and/or leaves and results in stomatal closure. This strengthens the hypothesis of sugar-driven stomatal movement (Domec and Pruyn, 2008; Silber et al., 2013).
The negative regulation of elevated CO2-induced stomatal closure may be closely linked to an impaired Ca2+ priming sensor, a HT1 protein kinase, and an RHC1 MATE-type transporter in Arabidopsis plants (Hashimoto et al., 2006; Young et al., 2006; Negi et al., 2014; Tian et al., 2015) (Table 1). However, the underlying mechanism concerning the precise signal transduction molecular pathways that regulate the stomatal closure upstream still remains elusive. This needs to be explored further, particularly for different genetic types, species, and even PFTs. A repression of the ABC transporter AtABCB14 may play a considerable role in stomatal closure in response to elevated CO2 levels (Lee et al., 2003, 2008; Laanemets et al., 2013). This SLAC1 may also be involved in stomatal closure induced by elevated CO2 levels (Negi et al., 2008; Laanemets et al., 2013). A recent report indicated that SLAC1 perception of CO2 signals may be located in a transmembrane region by an ABA-independent pathway (Yamamoto et al., 2016). Phosphorylation of KAT1 on the C-terminal region, which is expressed primarily in GCs in A. thaliana plants, might modulate the activity of K+ channels involved in the signal transduction cascade (Sato et al., 2009), which might be negatively regulated by nitric oxide (NO)—an active signaling molecule in plants (Gayatri et al., 2013). ABA may trigger its generation (Neill et al., 2008; Shi et al., 2014; Xia et al., 2015) through the modulation of vitamin B6 homeostasis (Xia et al., 2014). Furthermore, because blue light photoreception may also be involved in light–CO2 interactions in GCs, the changes in zeaxanthin levels may correspond to changes in the CO2 level, which are linked to the pH sensitivity of the relevant enzymes (Zeiger and Zhu, 1998; Zhu et al., 1998). A recent report indicated that NADPH oxidases and respiratory burst oxidase homologs (RBOHs) were closely associated with the network of reactive oxygen species (ROS) production, which may regulate the stomatal aperture (Baxter et al., 2014).
Mesophyll-Derived Signal (MDS)
Malate generated in GCs, through the metabolite of triose phosphate (triose-P) from the Calvin–Benson–Basshan (CBB) cycle, may directly involve stomatal aperture regulation as an osmoticum and as a sink for the end products of GC electron transport involving phosphoenolpyruvate carboxylase (PEPC; Cousins et al., 2007; Lawson et al., 2014). A component of malate may also originate from mesophyll cells because when the tricarboxylic acid (TCA) cycle function has been limited, e.g., by the inhibition of fumarase (Nunes-Nesi et al., 2007), there is a decline in GC malate, as it is one of the metabolites derived from the TCA cycle in mesophyll cells (Fernie and Martinoia, 2009; Araújo et al., 2011). It might confirm that malate could be the mesophyll-derived signal (MDS) linking stomatal behavior. A negative correlation between the fumarate level in mesophyll and gs indicated that fumarate, as an MDS, may also be involved in stomatal closure, although its influence seems to be less than that of malate (Araújo et al., 2011; Medeiros et al., 2015). Moreover, high CO2 concentration-induced stomatal closure may be attributable to an increase in the concentrations of malate produced in the mesophyll stimulating anion efflux through, for example, the R-type channel (ALMT). This is a malate-sensitive anion channel operating as a CO2 sensor in GCs and is linked to mesophyll photosynthesis (Hedrich and Marten, 1993; Sasaki et al., 2010; De Angeli et al., 2013; Lawson et al., 2014; Medeiros et al., 2015).
However, whether mesophyll and/or guard cell photosynthesis is involved in the GC response to CO2 concentrations remains controversial (von Caemmerer et al., 2004; Messinger et al., 2006; Lawson et al., 2014). Early reports show that a specific blue light response involving H+-ATPase activation is independent of A, whereas the red light response may be associated with A, which might be induced by the intercellular CO2 concentration (Ci) reduction resulting from the mesophyll consumption of CO2 (Roelfsema et al., 2002; Messinger et al., 2006). A recent study showed that Arabidopsis plants with an overexpression of plasma membrane H+-ATPase under the control of a guard cell-specific promoter may facilitate the coordinative capacity between stomatal opening, A, and growth rate (Wang et al., 2014). Thus, the role of photosynthesis in regulating GC movement in response to elevated CO2 remains elusive (Roelfsema et al., 2002; Ainsworth and Rogers, 2007; Engineer et al., 2014). The relative role of photosynthesis in guard cells and the nearby related cells, such as mesophyll cells, in response to elevated CO2 may require further testing.
There is no clear evidence for or against the existence of MDS and the involved signals. Some potential signals, such as chloroplastic ATP, zeaxanthin, NADPH, RuBP, and stomatin, have been suggested (cf. Lawson et al., 2014). Support for the role of MDS has been found in some excellent experiments, such as those by epidermal peels vs. the intact leaves methods. These experiments yield strong evidence that MDS might occur (e.g., Roelfsema et al., 2002; Mott et al., 2008; Fujita et al., 2013). Some reports indicate the MDS may exist in modern seed plants rather than in ferns and lycophytes (e.g., McAdam and Brodribb, 2012). Additionally, MDS may need certain transduction medium conditions, such as a vapor phase (Sibbernsen and Mott, 2010) or aqueous phase (Fujita et al., 2013). With increasing evidence that Ci may play only a trivial role (von Caemmerer et al., 2004; Hanson et al., 2013), the biological activities closely related to MDS often refer to electron transport, the redox state, metabolites in the transpiration stream, vapor phase ion, and electrical signals (Lawson et al., 2014). A report indicated that stomatal opening linked to apoplast transfer from mesophyll signals is dependent on photosynthesis at lower levels of CO2 (Fujita et al., 2013). Moreover, the stomatal closure is relatively independent of photosynthesis at elevated CO2, i.e., without ATP involvement in mesophyll photosynthesis (Roelfsema et al., 2002; Fujita et al., 2013). The S-type anion channels activated at elevated CO2 may contribute to stomatal closure (Roelfsema et al., 2002; Fujita et al., 2013). A study using chlorophyll fluorescence imaging showed spatiotemporal decoupling of stomata and mesophyll in response to the cutting of leaf veins, which weakens further support for the appearance of MDS (Hanson et al., 2013).
Integrated Signaling Processes
The changes in stomatal development and its aperture induced by elevated CO2 and involving mesophyll conductance (gm; Mizokami et al., 2015; Youshi and Santrucek, 2015) might be mediated by ABA levels (Giday et al., 2014; Youshi and Santrucek, 2015). In a recent study, genetic analysis using mutants in the ABA signaling pathway on GC-specific transcriptional memory for the related genes indicated that SnRK2.6 is more important for overall stomatal control. The SnRK2.2 and SnRK2.3 are more important for implementing GC stress memory in the subsequent dehydration response (Virlouvet and Fromm, 2015). However, the involvement of SnRK2.2 and SnRK2.3 in elevated CO2 regulation on the stomatal response and feedback remains largely unclear. The long-distance signaling cascades (Lake et al., 2002), e.g., from mature leaves to immature leaves, may also contribute to the GC behavior response to CO2 levels. ABA, ethylene, salicylic acid (SA), jasmonic acid (JA), NO, some peptides, and sugar levels might be involved in the integrated signaling processes’ response to environmental changes (e.g., Neill et al., 2008; Poór et al., 2011; Silber et al., 2013; Xia et al., 2014, 2015; Grienenberger and Fletcher, 2015; Medeiros et al., 2015).
Interactions with Other Factors
Elevated CO2 with Drought
Soil water deficit and high VPD often reduce the stomatal opening, depending on the species (Warren, 2008; Perez-Martin et al., 2009; Peak and Mott, 2011). Generally, water status has a stronger impact on gs than changes in CO2 concentration. A relatively small effect of elevated CO2 on gs generally appears as water deficit stress occurs, possibly because the drought-induced reduction dramatically outweighs the reduction caused by elevated CO2 (Morgan et al., 2004; Leakey et al., 2006b). Flexas et al. (2004) indicated that decreases in gs and gm, but not biochemical activities, may limit the photosynthetic capacity in drought-stressed leaves, depending on the species (Bota et al., 2004; Flexas et al., 2014). Even for drought-severely stressed plants, the biochemical limitation can be negligible (Galmés et al., 2007). A non-stomatal limitation appears only when gs is below 250 mmol m-2s-1 in grass plants grown in drought conditions (Xu et al., 2009a). In tall fescue (Festuca arundinacea) plants exposed to elevated CO2, an increased A with a low gs but high Rubisco activity during both drought and rewatering may also indicate the alleviation of metabolic limitations caused by drought damages rather than stomatal limitations imposed by elevated CO2 (Chen et al., 2015). CO2 enrichment may relieve non-stomatal limitations by protecting the photosynthetic apparatus during severe drought (Xu et al., 2014). However, a recent report showed that Ramonda nathaliae plants with smaller stomata have higher resistance to drought than R. serbica, which have larger stomata (Rakić et al., 2015). This highlights the role of the stomatal size.
Elevated CO2 may improve plant water status by reducing gs and thereby raising WUE, ameliorating the adverse effects of stressful factors on plant growth and physiological processes (Ainsworth and Rogers, 2007; Xu et al., 2013, 2014). A decrease in soil water availability under elevated CO2 may be closely linked to an increase in leaf area, which offsets a decline in gs and promotes plant growth (Manea and Leishman, 2015). Studies have clearly shown that water status mediates rising CO2 effectiveness through the coupling of processes between gas exchange and leaf enlargement. Nevertheless, the pros and cons of acclimation to changes in water conditions may coexist in response to elevated CO2. Leaf area enlargement, i.e., canopy enhancement induced by CO2, may exaggerate water use, whereas decreased gs would promote WUE (e.g., Woodward, 1990; Ward et al., 2013; Manea and Leishman, 2015), depending on canopy density and its homogeneity (Bernacchi and VanLoocke, 2015). However, an intrinsic WUE decline might appear during severe drought in some relict species plants exposed to elevated CO2 (Linares et al., 2009). Thus, future research is necessary to focus on the linkage among leaf area, gs, and both WUEi and total plant biomass water use efficiency (WUEt) under climatic change. Furthermore, some results indicated that although WUEt and WUEi showed a similar response to elevated CO2, the former seemed to have a higher level of sensitivity, implying that WUEt may be a better indicator than WUEi of the response to climate change (Duan et al., 2014). WUE and the root: shoot biomass ratio increased significantly with decreased precipitation but decreased with elevated CO2 levels (Li et al., 2014). Thus, besides the regulation of leaf growth, root development may also involve stomatal movement behavior and WUE changes under climatic change. The possible primary stomatal closure induced by elevated CO2 may be offset by positive indirect effects on gs, possibly caused by root system promotion and hydraulic capacity under rising CO2 conditions (Uddling et al., 2009). Forest canopy evapotranspiration can be reduced under high CO2 concentration levels (Medlyn et al., 2001), possibly due to leaf gs slowdown. Thus, water loss is diminished. However, a lower response to elevated CO2 in the canopy evapotranspiration rate relative to leaf gs was found in a rice field (Shimono et al., 2013). Nevertheless, the canopy carbon fixation and its association with gs at the leaf and canopy scales during climatic change remains to be tested. A succinct description on the trade-off between gs, leaf enlargement, and WUE under elevated CO2 and drought conditions is summarized in Figure 3.
FIGURE 3. A representation of the response to elevated CO2 (eCO2) with drought on water use efficiency (WUE) under regulations by balancing stomatal conductance (gs) and leaf growth. Elevated CO2 may lead to an acclimated reduction in gs, which involves signaling sensing and transduction, biophysical and biochemical processes, and gene expression (1); meanwhile, eCO2 could promote leaf enlargement (2), possibly increasing transpiration (E) of the total leaf subsequently reducing WUE (3). A severe drought stress may shrink leaf growth (4), consequently decreasing E and finally increasing WUE (5); gs can directly be reduced by drought (6). However, a moderate drought may directly enhance WUE by some adaptive responses such as a relative increase in the root systems (7), which can be further improved by elevated CO2 (8). Root systems may be enhanced by eCO2, particularly under drought through alterations in carbon allocation between above- and belowground parts (9), which may lead to either decreased WUE at eCO2 (10), or increased WUE under drought conditions (11). Consequently, this trade-off interaction (12) or synergic increase (13) may occur with leaf growth and gs changes at eCO2 under drought, ultimately affecting WUE.
Moreover, most studies have confirmed that elevated CO2 may improve the water status of drought-stressed plants by reducing gs (e.g., Brodribb et al., 2009; Katul et al., 2010; Chen et al., 2015; Easlon et al., 2015), but these findings were species-dependent (Beerling et al., 1996; Bernacchi et al., 2007; Liu et al., 2016). However, this case may not occur under severe or extreme drought conditions, possibly due to the depression of stomatal regulatory ability (Xu and Zhou, 2008). Furthermore, plant size and root distribution may override the expected direct physiological effects of elevated CO2 (Duursma et al., 2011; Liu et al., 2016).
Elevated CO2 with Salinity
Generally, stomata may exert a similar response to salt stress relative to drought (Clough and Sim, 1989; Wang et al., 2003; Flexas et al., 2004; Chaves et al., 2009). Stomatal conductance often decreases remarkably with increased salinity and/or aridity, such as leaf to air VPD, depending on the species and its habits (e.g., Clough and Sim, 1989; Chaves et al., 2009; Ashraf and Harris, 2013; Nguyen et al., 2015; Sanoubar et al., 2016). Enhanced salt stress and elevated CO2 concentrations are projected to co-occur in the future (Chaves et al., 2009; Pérez-López et al., 2009; Hoque et al., 2016). Generally, stomatal conductance was decreased by severe salt stress and elevated CO2 alone or in combination (Pérez-López et al., 2012; Nguyen et al., 2015; Stavridou et al., 2016). For example, as barley (Hordeum vulgare) plants are grown in high salinity soil, the rate of CO2 diffusion to the carboxylating site and photochemical electron sink capacity increased under elevated CO2 conditions, despite stomatal and internal conductance being decreased (Pérez-López et al., 2012). Similar to the severe desiccation effect, high salinity stress may lead to oxidative damage in plant tissue (Shalata et al., 2001; Sanoubar et al., 2016). However, elevated CO2 may alleviate the oxidative stress-induced by salinity with lower ROS level and a higher A, thus improving plant growth under high salinity conditions (Nicolas et al., 1993; Pérez-López et al., 2009). Studies have indicated that the rising-CO2 protection from salt-inhibited plants alleviates the metabolic limitations rather than the stomatal limitations. Moreover, although there was a gs decrease of 1–2 factors by high soil salinity in wetland grass Phragmites australis plants, the salinity effect hardly occurred with the combination of elevated CO2 and temperature (plus 310 μmolmol-1 CO2, and plus 5°C relative to ambient variables; Eller et al., 2014). The non-species expansion into saline areas may be promoted because the salinity-caused non-stomatal limitations (i.e., carboxylation rates of Rubisco or electron transport rates) may be mitigated under the elevated climatic conditions (Eller et al., 2014). However, the alleviated effect of elevated CO2 on severe salt stress strongly depends on species and cultivars/ecotypes (Eller et al., 2014; Geissler et al., 2015). Nevertheless, the responses of stomatal characteristics to the combination of elevated CO2 on salt stress are scarcely reported and need to be explored further.
Elevated CO2 with High Temperatures
The combined effects of elevated CO2 and high temperatures have also been reported in some studies. While there are exceptional cases (e.g., Bernacchi et al., 2007), elevated CO2 decreases gs, thus increasing leaf temperature because lower transpiration releases less heat (Kim et al., 2006; Negi et al., 2014; Šigut et al., 2015). As a consequence, elevated CO2 with high temperatures may play an antagonistic role by exaggerating heat damage partly due to decreased gs (Warren et al., 2011). However, an elevated CO2-induced 13–30% decline in gs induced a 2°C increase in leaf temperature, leading to a 2.9–6.0°C increase in the temperature optima for the light-saturated rate of CO2 assimilation (Amax). Thus, this would enhance heat stress tolerance in beech and spruce saplings (Šigut et al., 2015). The increased adaptation to heat stress may be due to reduced photorespiration and the limitation of photosynthesis by RuBP regeneration under elevated CO2 (Šigut et al., 2015). A recent report also confirmed the heat-tolerance enhancement due to elevated CO2 for coffee crops (Rodrigues et al., 2016). Thus, the negative effect of elevated CO2 on heat stress due to reduced gs was not confirmed. In contrast, a beneficial adaptation may occur. Yet, this may depend on the species and the range of temperature variation.
Elevated CO2 with Nutrition Status and Air Pollution
Based on a recent report (Easlon et al., 2015), better plant growth and photosynthesis in the low gs in A. thaliana lines under N-limitation, rather than sufficient N supply under elevated CO2, may imply an adaptive coupling between lowered gs and improved N utilization. Increased conservative N investment in photosynthetic biochemistry in order to acclimate to CO2 fertilization highlights a positively synergistic relationship between stomatal regulation and nutrition status. However, a lower gs in elevated CO2 concentrations but a higher gs with an abundant N supply have been found in Liquidambar styraciflua plants (Ward et al., 2013), suggesting that these factors may play opposite roles in the gs response. A recent study has indicated that improved phosphorus (P) nutrition can enhance drought tolerance in the field pea due to the CO2-induced decrease in gs and the promotion of root systems (Jin et al., 2015). A general decline in gs by elevated CO2 and ozone (O3) alone or their combination has been extensively reported, suggesting that rising CO2 may alleviate the injury caused by high O3 pollution decreasing gs (Kellomäki and Wang, 1997; Mansfield, 1998; Warren et al., 2006; Hoshika et al., 2015). However, some species, such as aspen (Populus tremuloides Michx.) and birch (Betula papyrifera Marsh.), have a high gs under both high CO2 and high O3 concentrations (Uddling et al., 2009). This indicates that the interactive effects between elevated CO2 and O3 on stomatal behavior may depend on species, plant/leaf ages, and treatment regimens, such as time and sites (Uddling et al., 2009; Hoshika et al., 2015; Matyssek et al., 2015). Thus, it again highlights the complex/specific response.
Elevated CO2 with Biotic Factors
The stomatal response to elevated CO2 with biotic factors has received much attention (e.g., Casteel et al., 2012; Zavala et al., 2013). For instance, a greater gs reduction in cabbage with decreased aphid (one of the most destructive insect pests in crops) colonization rates and total plant volatile emissions, such as terpene emissions, occurred when plants were exposed to elevated CO2 over the long-term (6–10 weeks) rather than the short-term (2 weeks; Klaiber et al., 2013). This indicates that, as hosts, plants may acclimatize to future increases in elevated CO2 by modifying stomatal behavior. Under elevated CO2, a decrease in micronutrients, such as calcium, magnesium, or phosphorus, due to the gs reduction may lead to poor aphid performance (Myzus persicae; Dáder et al., 2016). Furthermore, a recent report (Sun et al., 2015) showed that aphid infestation may synergistically promote the effects of elevated CO2 on stomatal closure, possibly by triggering the ABA signaling pathway. Therefore, the water status of the host plants of Medicago truncatula was improved, ultimately enhancing feeding efficiency and abundance of aphid (Zavala et al., 2013; Sun et al., 2015). Taken together, plant–insect interactions might be modified by stomatal closure under high levels of CO2. The metabolism and emission of plant biogenic volatile organic compounds may also be involved (Klaiber et al., 2013; Zavala et al., 2013). It is suggested that an enhanced accumulation of JA and SA may also be involved in signal transduction in relation to stomatal movement as plants are subjected to CO2 enrichment and herbivore attack. This highlights an important role in stomatal regulation to cope with a combination of climate change and biotic factors (Poór et al., 2011; Casteel et al., 2012; Zavala et al., 2013; Sun et al., 2015). Thus, the herbivore’s adaptive capacity to its host might be promoted when exposed to elevated CO2, at least partly through stomatal regulation.
Conclusion and Perspectives
Under high CO2 conditions, both stomatal conductance and its density generally decreased with a few exceptions. The decline in SD may be the result of a long-term genetic variation or short-term structural plasticity under elevated CO2. Elevated CO2 may induce the excessive depolarization of guard cells to cause stomatal closure when mesophyll-driven signals, such as malate, ATP, zeaxanthin, and NADPH, may be involved in stomatal movement. Their photosynthesis in both guard cells and mesophyll cells and their link to the stomatal response in elevated CO2 conditions may play an important role. However, challenges remain in elucidating the underlying mechanism. The differences and linkage in stomatal responses to elevated CO2 levels across the molecular, cellular, biochemical, eco-physiological, canopy, and vegetation levels (Zhu et al., 2012; Peñuelas et al., 2013; Shimono et al., 2013; Armstrong et al., 2016) should raise concerns about ecological and climatic management.
Several crucial aspects of research into the stomatal response may need to be strengthened in the future. (1) The underlying mechanism of responses to CO2 enrichment for key biological processes, including stomatal behavior; the critical metabolic bioprocesses, such as hormone-involved regulation; and relevant biochemical signal cascades must be further elucidated. (2) The diverse responses from different species and PFTs to elevated CO2 or its combination with other abiotic and biotic factors must be compared and clarified. (3) Various spatial–temporal scales from the molecular, biochemical, physiological, individual, and canopy to vegetation levels must be integrated. Instantaneous to annual or longer time-scales (e.g., Zhu et al., 2012; Shimono et al., 2013; Armstrong et al., 2016) must also be integrated. We should elucidate the underlying mechanism of the stomatal responses associated with key biological processes across the multiple scales under different climatic factors, including elevated CO2, warming, drought, and air pollution. (4) We need to investigate whether improving stomatal response to elevated CO2 by manipulating guard cell performance may yield a better balance between CO2 uptake and water loss through transpiration to enhance photosynthetic capacity with high WUE (e.g., Engineer et al., 2014; Lawson and Blatt, 2014; Grienenberger and Fletcher, 2015). Enhanced expression of some related genes, such as patrol1, may drastically increase both gs and plant growth under higher CO2 levels (Hashimoto-Sugimoto et al., 2013). This task needs to be implemented urgently. Finally, understanding how to improve or combine earth system models (ESMs), general circulation models (GCMs), and land surface models (LSMs) may help to correctly interpret the gs response to climate change (Sato et al., 2015). The integration issue should be solved urgently to precisely assess the response and feedback of terrestrial ecosystem to global change.
YJ and BJ are co-first authors, ZX and GZ designed the study, ZX, YJ, and BJ collected and analyzed the data, all authors wrote and reviewed the manuscript.
Conflict of Interest Statement
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
The study was funded by the National Natural Science Foundation of China (41330531, 31170456), and China Special Fund for Meteorological Research in the Public Interest (GYHY201506019).
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Keywords: elevated CO2, drought, guard cell, global warming, mesophyll-driven signals, regulation mechanism, photosynthesis, stomatal behavior
Citation: Xu Z, Jiang Y, Jia B and Zhou G (2016) Elevated-CO2 Response of Stomata and Its Dependence on Environmental Factors. Front. Plant Sci. 7:657. doi: 10.3389/fpls.2016.00657
Received: 20 September 2015; Accepted: 29 April 2016;
Published: 13 May 2016.
Edited by:Jan Kofod Schjoerring, University of Copenhagen, Denmark
Reviewed by:Iker Aranjuelo, Agrobiotechnology Institute–Consejo Superior de Investigaciones Científicas–Universidad Pública de Navarra, Spain
Maite Lacuesta, Universidad del Pais Vasco – Euskal Herriko Unibertsitatea, Spain
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