Growth habit and leaf economics determine gas exchange responses to high elevation in an evergreen tree, a deciduous shrub and a herbaceous annual

Elevational changes in temperature and carbon dioxide can be used to predict the likely responses of plants to climate change. However, plant species often exhibit contrasting photosynthetic and morphological responses to altitude. We investigated the photosynthetic responses of plants with different leaf morphologies and growth habits to increased elevation. At high elevations, plants with schlerophyllous leaves that represent a large structural investment are more likely to be positively affected by rising carbon dioxide than species with a lower investment in foliage.


Introduction
The adaptational responses of plants to alterations in temperature and the partial pressure of carbon dioxide ( pCO 2 ) along elevational gradients have been used to infer the likely responses of vegetation to climatic changes in the past and future (e.g. Kö rner 2007;Kouwenberg et al. 2007;Bai et al. 2015). The partial pressure of all atmospheric gases declines with elevation, reducing the availability of CO 2 for photosynthesis and oxygen for respiration, while lower temperatures and higher levels of radiation may decrease the activity of photosynthetic and metabolic enzymes (Gale 1972a;Miroslavov and Kravkina 1991;Allen and Ort 2001). Growth at high elevation, therefore, necessitates physiological and morphological adaptations to enable photosynthesis (e.g. Woodward 1986;Williams and Black 1993;Terashima et al. 1995;Cordell et al. 1998;Körner 2007;Feng et al. 2013). High-elevation ecosystems are often more sensitive to climatic change than those at sea level, as the influence of rising atmospheric temperature and carbon dioxide concentration ([CO 2 ]) on photosynthesis becomes more pronounced with elevation (Gale 1972a(Gale , b, 1973Terashima et al. 1995). Nonetheless, not all plant species respond in the same manner along elevational gradients, and comparatively little is known regarding the physiological and morphological adaptation of plants growing at high elevations .2500 m above sea level (a.s.l.). An understanding of the physiological and morphological processes that underpin photosynthesis and leaf gas exchange at high elevations may assist in our understanding of the likely impacts of future climate change on these high-elevation ecosystems.
In addition to physical changes to pCO 2 and temperature, an increase in elevation may also be associated with fluctuations in soil type, wind speed, water availability and the quality/quantity of incident radiation (Kö rner 2007). These factors will all influence plant growth and photosynthesis (e.g. Körner and Cochrane 1985;Woodward 1986). The photosynthetic performance of a plant is determined by its capacity for the uptake and assimilation of CO 2 (Farquhar et al. 1980); this is controlled by stomatal (G s ) and mesophyll conductance (G m ) to CO 2 , the carboxylation capacity of ribulose-1,5-bisphosphate (RuBP) carboxylase/oxygenase (RubisCO) (V cmax ) and the maximum rate of electron transport for RuBP regeneration (J max ) (e.g. Shi et al. 2006;Centritto et al. 2009;Haworth et al. 2011;Feng et al. 2013). Stomatal conductance frequently increases with elevation, possibly as a result of the lower availability of CO 2 in the atmosphere necessitating increased rates of conductance to sustain adequate CO 2 uptake (Kö rner et al. 1986;Woodward 1986). This enhanced G s with elevation is often accompanied by increased stomatal density values and higher rates of transpirative water loss (Kö rner and Cochrane 1985;Woodward and Bazzaz 1988;Kouwenberg et al. 2007;Wang et al. 2014). The lower partial pressures of gases at high elevations will not only result in more rapid diffusion through the stomatal pore of CO 2 but also water vapour, which when combined with the generally higher irradiances and drier atmosphere at high elevations will enhance the transpirative costs of growth at high elevation (Gale 1972a(Gale , b, 1973. However, these patterns of increased G s are not universal, with species such as Quercus aquifolioides (Li et al. 2006;Feng et al. 2013), Q. guyavifolia (Hu et al. 2015) and Typha orientalis (Bai et al. 2015) exhibiting reduced G s and stomatal density with elevation. Species with reduced G s at high elevation may exploit the more rapid diffusion of CO 2 at low partial pressures (Gale 1972a) by increasing rates of carboxylation of CO 2 to maintain the diffusion gradient between the internal leaf and external atmosphere (Cordell et al. 1998;Shi et al. 2006) without incurring the additional transpirative costs associated with increased G s and stomatal density (Haworth et al. 2015). However, lower temperatures at high elevation may also minimize the effect of increased diffusion of CO 2 at lower partial pressures during the gaseous phase of CO 2 transport (Körner 2007).
The concentration of CO 2 inside the chloroplast envelope is directly related to stomatal and mesophyll conductance to the transport of CO 2 (Loreto et al. 2009;Flexas et al. 2013). As a result, G s and G m often operate synchronously to determine photosynthesis (A) as a function of the total conductance to CO 2 (G tot ) (Centritto et al. 2003;Hu et al. 2010;Lauteri et al. 2014). More rapid diffusion of CO 2 at lower partial pressures may counteract the effect of reduced availability on gaseous transport of CO 2 through the stomata to the spongy mesophyll (Gale 1972a), but this will not influence the transport of CO 2 through the aqueous phase to the chloroplast (Loreto et al. 1994;Flexas et al. 2013). As such, the lower partial pressure of CO 2 will have a significant impact on A, and G m will play a significant role in determining the response of a plant species to growth at high elevation. It may be expected that an increase in elevation would induce a rise in G m to ensure CO 2 uptake at lower partial pressures; however, G m is determined by a number of physical and biochemical factors (Warren 2007;Niinemets et al. 2009) that are also affected by elevation (Kö rner et al. 1979(Kö rner et al. , 1986Kogami et al. 2001;Feng et al. 2013). The specific leaf area (SLA) of temperate species tends to decrease with elevation, resulting in leaves with more closely packed cells (Friend and Pomeroy 1970;Friend et al. 1989;Li et al. 2013;Pan et al. 2013;Haworth and Raschi 2014) and lower G m values (Kogami et al. 2001;Niinemets et al. 2009;Feng et al. 2013). For example, Polygonum cuspidatum exhibited a reduction in SLA and G m over an elevation range of 10 -2500 m (Kogami et al. 2001). This reduction in SLA with elevation is likely a result of increased incident radiation inducing a more compact leaf morphology (Niinemets 2001;Poorter et al. 2009). Increased elevation also resulted in a decrease of SLA and G m values, but no change in G s , in the tropical Hawaiian tree species Meterosideros polymorpha (Cordell et al. 1998). In contrast, the highland species Buddleja davidii that grows from 1200 to 3500 m a.s.l. exhibited no alteration of SLA, but a reduction in G s alongside an increase in G m with elevation that corresponded to enhanced V cmax (Shi et al. 2006). This indicates the importance of the temperature to which a species is adapted and leaf economic strategy in determining the response to elevation (Hovenden and Vander Schoor 2004).
Photosynthesis rates decline with elevation due to lower partial pressures reducing the availability of CO 2 (Gale 1972a;Kö rner and Diemer 1987) and diminished temperatures resulting in lower activity of photosynthetic enzymes (Fryer et al. 1998). The selective pressures exerted by lower temperatures and pCO 2 may induce increased photosynthetic capacity (i.e. enhanced V cmax and J max ) at high elevation to enable sufficient CO 2 uptake (Cordell et al. 1998;Shi et al. 2006;Feng et al. 2013). At higher elevations, greater V cmax and J max are associated with increased leaf nitrogen and chlorophyll concentrations, but lower photosynthetic nitrogen use efficiency (PNUE) (Cordell et al. 1998;Kogami et al. 2001;Feng et al. 2013). Increased leaf nitrogen levels at higher elevations also commonly correspond to reduced SLA (Feng et al. 2013); conversely at sea level, SLA is often positively related to nitrogen concentration (Poorter et al. 1990). At high elevations, many species exhibit a reduction in leaf area (Kouwenberg et al. 2007), possibly as a response to increased levels of incident radiation that would increase leaf temperatures and transpiration rates through increased leaf to air vapour pressure deficit (Kö rner and Cochrane 1985). This shift in leaf area would affect the calculation of SLA (Poorter et al. 2009), and suggests that the temperature lapse rate and decline in pCO 2 with elevation, and the selective pressures they exert induce differential adaptational responses to those observed at low elevation, and may therefore have different effects on plants with contrasting growth habits and leaf economic strategies.
Plants growing at high elevations of 2500-3500 m a.s.l. experience relatively low pCO 2 in the range of 27.7-24.6 Pa in comparison with pCO 2 of 38 Pa at sea level. The temperature lapse rate equates to an average decline in temperature of 5.5 8C with every 1000 m gained in elevation (Barry 2013). In this study, we aimed to characterize the physiological and morphological adaptations of three plant species with different growth habits: an evergreen tree (Q. spinosa), a deciduous shrub (Salix atopantha) and a herbaceous annual (Rumex dentatus). The responses to growth at high elevation of the three study species were also compared with those of Q. aquifolioides from the same habitat in an earlier investigation by Feng et al. (2013). To assess the adaptational responses of these plants to high elevations in the range of 2500-3500 m a.s.l., we conducted leaf gas exchange measurements and sampled leaves in the field to (i) analyse photosynthetic physiology at high elevations, (ii) characterize leaf gas exchange through quantification of stomatal and mesophyll conductance responses to CO 2 and any diffusional limitation to photosynthesis, (iii) gauge the effect of reduced pCO 2 and temperature on leaf economics and nitrogen concentration and (iv) evaluate the likely effect of future climate change in terms of rising pCO 2 and temperature on mountainous species and ecosystems.

Plant material and study area
Three plant species with contrasting growth habits that grow at high elevations in north-western China were chosen for analysis. Quercus spinosa is a 6 -10 m tall evergreen tree occurring in mountain regions of South East Asia over an elevation range of 1000 -3500 m and over a range of 2000 -3500 m in south-western China (Wu et al. 2011). Salix atopantha is a deciduous shrub 1 -2 m in size, specific to western and south-western China occurring in mountainous regions at elevations of 2300-3500 m (Chen-Fu and Skvortsov 1998). Rumex dentatus is a 0.3 -0.7 m tall annual herb that grows on moist slopes from sea level to high elevations (.3500 m a.s.l.) in Asia, North Africa and Europe (Kumar et al. 2005). It grows in mountainous regions at elevations of 1200 -3600 m in south-western China (Shi and Ming 1987).
Populations of Q. spinosa, S. atopantha and R. dentatus at elevations of 2400 and 3500 m a.s.l. in the Wolong Reserve (south-eastern Tibetan-Qinghai area, Sichuan Province, China) (32825 ′ -32853 ′ N, 104820 ′ -104841 ′ E) were studied. The populations from the higher and lower elevations did not experience water stress and received full illumination with no shading. The leaves used for gas exchange measurements and collected for leaf economic traits, carbon isotope and nitrogen concentration analysis were at identical developmental stages (i.e. the youngest fully expanded leaf at the end of a branch). Field work was conducted from July to August 2010.

Gas exchange and fluorescence measurements
Leaf gas exchange and fluorescence parameters of the central leaf section were simultaneously measured using a LI-6400-40 leaf chamber fluorometer (LI-COR, Inc., Lincoln, NE, USA) equipped with a 2-cm 2 cuvette. One leaf was analysed from six plants for each species at each elevation. The concentration of atmospheric gases is constant with elevation; rather, it is the partial pressure of those gases that declines as elevation increases. All measurements were conducted at the same concentration of [CO 2 ] but at the respective partial pressures of 2500 and 3500 m a.s.l. The LiCor Li6400 contains a barometric pressure sensor that allows for compensation of the effects of AoB PLANTS www.aobplants.oxfordjournals.org changes in partial pressure on measurements over a range of 65 -115 kPa with an accuracy of and resolution of 0.002 kPa. Standard atmospheric pressure at sea level is 101.325 kPa, and at 3500 m a.s.l., atmospheric pressure is 70 kPa, indicating that our measurements were conducted within the operating range of the instrument. The measurements were made in situ between 9:00 and 15:00 at a saturating photosynthetic photon flux density (PPFD) of 1200 mmol m 22 s 21 for Q. spinosa, 1400 mmol m 22 s 21 for S. atopantha and 2000 mmol m 22 s 21 for R. dentatus at a CO 2 concentration of 380 mmol mol 21 . The saturating PPFD was determined by response curves of A to increasing PAR (Ö gren and Sundin 1996). Leaf temperature was set at 25 8C, and the relative humidity in the leaf cuvette ranged between 46 and 50 %. The chlorophyll fluorescence yield (i.e. the quantum yield of photosystem II (PSII) in the light, FPSII = DF/F ′ m ) was measured using a saturating pulse of white light (10 000 mmol m 22 s 21 ) (Genty et al. 1989). Mesophyll conductance to CO 2 diffusion was calculated using the variable J method (Harley et al. 1992). As this work was conducted in the field, it was not possible to calibrate electron transport rate under non-photorespiratory conditions; therefore, a standard calibration where a ¼ 0.85 and b ¼ 0.5 was used in the calculation of G m (Gilbert et al. 2012;Walker and Cousins 2013). The variable J method is sensitive to the estimation of the CO 2 compensation point to photorespiration (G*) and leaf respiration (Gilbert et al. 2012). While measurements of dark respiration (R n ) were also made at ambient CO 2 concentration in the dark on the same leaves, G* used in the gas exchange algorithm was calculated from the Rubisco-specific factors of Galmes et al. (2005) using the photosynthetic constants of Von Caemmerer (2000) and formulae of Brooks and Farquhar (1985) (Q. spinosa: G* ¼ 52.513 mmol 21 mol; S. atopantha: G* ¼ 54.145 mmol 21 mol and R. dentatus: G* ¼ 52.512 mmol 21 mol). As G* is a relatively conservative parameter (Harley et al. 1992), we assumed that the G* value used in the gas exchange algorithm did not affect the estimation of G m . To reduce diffusion leaks through the chamber gasket (Flexas et al. 2007), a supplementary external chamber gasket composed of the same polymer foam was added to create an interspace between the two gaskets (i.e. a double-gasket design with a 5-mm space separating the internal and external gaskets). Then the CO 2 and H 2 O gradients between the in-chamber air and pre-chamber air were minimized by feeding the infrared gas analyse exhaust air into the interspace between the chamber and the pre-chamber gaskets (Rodeghiero et al. 2007). Total conductance to CO 2 (G tot ) was calculated from mesophyll and stomatal conductance to CO 2 following Loreto et al. (1994) as: Light saturated A/P i response curves were measured at a leaf temperature of 25 8C and a relative humidity in the leaf cuvette of 50 % over a range of [CO 2 ] values on a minimum of five plants per species at each elevation. To remove the effect of stomatal limitation on A, the leaves were first pre-conditioned at a [CO 2 ] of 50 mmol mol 21 for 60 min to force stomatal opening as described by Centritto et al. (2003). The concentration of [CO 2 ] within the cuvette was then progressively increased to 2000 mmol mol 21 . The photosynthetic parameters A max (net CO 2 assimilation rate under conditions of PPFD and CO 2 saturation), V cmax (RuBPsaturated rate of Rubisco: estimate of the carboxylation efficiency of Rubisco determined from the slope of the A/P i curve at a [CO 2 ] of 40-200 mmol mol 21 ) and J max (maximum rate of electron transport) were estimated by fitting the mechanistic model of Farquhar et al. (1980).

Leaf sampling, carbon isotope discrimination and leaf nitrogen analysis
Immediately after the gas exchange measurements, two leaves per plant from six plants per species at each elevation were detached and stored in sealed plastic bags for the measurement of leaf area, leaf weight, leaf nitrogen concentration and foliar d 13 C. Leaf area was measured with a Li-3000 leaf area metre (LI-COR, Inc.). The leaves were then dried at 80 8C for 48 h, the dry mass recorded and then ground into a fine powder using a ceramic grinding container. Specific leaf area (cm 2 g 21 ) was determined as the leaf area to leaf dry mass ratio. Nitrogen concentration (N mass , mg g 21 ) was measured on 0.1 g of dried, ground tissue by using standard Kjeldahl technique and assayed for ammonium with an ultraviolet visible spectrophotometer (Tu1221, Beijing Purkinje General Instrument Company, Beijing, China). N area (nitrogen concentration on a leaf area basis, g m 22 ) and PNUE (mmol mol 21 s 21 ) (Hikosaka et al. 2002) were calculated using the following formulae: where 14 is the atomic mass of nitrogen. Carbon isotope composition (d 13 C) was measured on 0.001 g of ground dried tissue by using a continuous flow isotope ratio mass spectrometer. Samples were quantitatively combusted in an elemental analyser (Flash-EA 1112, Thermo Electron, Milano, Italy). The CO 2 obtained was injected into the helium stream of the mass spectrometer (DELTAplus XP, ThermoFinnigan, Bremen, Germany). The ratio of isotopes (R ¼ 13 C/ 12 C) was measured and used to calculate d 13 C referred to the Pee Dee Belemnite standard according to Farquhar and Richards (1984) as follows:

Statistical analysis
A one-way analysis of variance (ANOVA) was used to assess differences in the data collected from the plants growing at 2500 and 3500 m a.s.l. using the software package SPSS 13.5 (SPSS, Chicago, IL, USA), and graphs were prepared using SigmaPlot 11.0 software (Systat Software Inc., San Jose, CA, USA).

Ethics statement
The field study did not involve endangered or protected species. No specific permissions or permits were required for the analysis and collection of Q. spinosa, S. atopantha and R. dentatus leaves from the Wolong Reserve (32825 ′ -32853 ′ N, 104820 ′ -104841 ′ E; Tibetan-Qinghai area, Sichuan Province, China). The leaves were collected from public land with the consent of the responsible government agency (the Chinese Academy of Forestry).

Results
Photosynthesis was closely related to conductance to CO 2 in all of the species at high elevations ( Fig. 1). Total conductance (G t ) incorporating both G s and G m correlated most closely with A (Fig. 1C). However, the species analysed did not display identical responses to increased elevation; Q. spinosa and Q. aquifolioides showed reduced conductance to CO 2 with an increase in elevation, while S. atopantha and R. dentatus exhibited higher G s , G m and G tot values at higher elevations (Table 1). The annual herb R. dentatus and deciduous shrub S. atopantha exhibited generally higher values of conductance to CO 2 and A than the evergreen Quercus species (Fig. 1). Alterations in G s and G m with elevation did not significantly affect P i /P a or P c /P a ratios in any of the species analysed (Table 1), suggesting modification of the photosynthetic physiology alongside adjustment in conductance to CO 2 (Figs 1  and 2). Moreover, the similarity in the ratio of P i to P a indicates that any variation in or low values of C i was unlikely to be responsible for any of the observed patterns in G m reported in this study (Tholen et al. 2012). Respiration in the dark (R n ) was greater at the higher elevation in all of the species (Table 1). Leaves of Q. spinosa exhibited the lowest R n values of 21.21 mmol m 22 s 21 at 2500 m a.s.l., but following a 181.8 % increase showed the highest levels of R n at the greater elevation of 3500 m a.s.l., suggesting that the impact of increased elevation was greatest on the species with sclerophyllous evergreen foliage. The two species with leaf lifespans of ,9 months,  S. atopantha and R. dentatus, exhibited respective increases of 36.6 and 44.4 % in R n between 2500 and 3500 m a.s.l.
Photosynthetic response curves to increased [CO 2 ] (Fig. 2) Table 1. Leaf assimilation rate (A), stomatal conductance (G s ), mesophyll conductance (G m ), P i (CO 2 intercellular partial pressure)/P a (CO 2 ambient partial pressure), P c (CO 2 chloroplast partial pressure)/P a and R d (dark respiration) values of the three plants growing at higher and lower altitudes. Means of a parameter followed by the same letter were not statistically different using a one-way ANOVA (P . 0.05) with least significant difference (LSD) post hoc test.  in concert with shifts in G tot . Quercus spinosa exhibited 46.5 and 76.1 % reductions in V cmax and J max , respectively, that translated into 56 % reduction in the ratio of J max to V cmax (Table 2). In contrast, both S. atopantha and R. dentatus exhibited increased values of conductance to CO 2 (Table 1) and corresponding increases in the physiological capacity to assimilate CO 2 (Table 2). Salix atopantha and R. dentatus, respectively, showed 38.1 and 25.4 % increases in V cmax alongside 52.8 and 34.7 % rises in J max that did not significantly alter the J max to V cmax ratio of either species. The maximum rate of photosynthesis (A max ), V cmax and J max all correlated to G s , G m and G tot (Fig. 3). However, at higher G s , G m and G tot values, photosynthetic capacity stabilizes and no longer increases, possibly due to physiological limitations to the rate of photosynthesis. Individuals of the annual herb R. dentatus at the higher elevation displayed the greatest values of A max , V cmax and J max , while at the higher elevation, Quercus species exhibited the lowest levels of conductance and photosynthetic capacity to assimilate CO 2 (Fig. 3). The photosynthetic capacity of a leaf is generally related to the concentration of nitrogen within the foliage (Evans 1989). Both S. atopantha and R. dentatus showed increases in leaf nitrogen alongside A max , V cmax and J max with elevation (Fig. 4). Despite exhibiting reduced photosynthetic capacity and a 57 % increase in nitrogen concentration at higher elevations, Q. spinosa showed no significant relationship between leaf nitrogen and A max , V cmax and J max . The PNUE values of S. atopantha and R. dentatus increased by 79.4 and 16.7 % at the higher elevation, while Q. spinosa showed a 69.2 % reduction of PNUE at 3500 m a.s.l. All three species showed increased foliar nitrogen concentration at the higher elevation, but this did not correspond to an increase in SLA (Table 3). While the evergreen Q. spinosa and annual herb R. dentatus showed respective reductions of 13.0 and 31.5 % in SLA at higher elevation, the SLA of S. atopantha was relatively unchanged. Growth at the higher elevation of 3500 m resulted in significant increases of 5.3-10.2 % in the foliar d 13 C of all three species. The d 13 C values of the plants from 2500 m a.s.l. were significantly enriched in the heavier 13 C isotope relative to C3 plants growing at sea level (approximately +1-2‰) (Körner et al. 1988), and this enrichment in 13 C became more pronounced at 3500 m a.s.l. (approximately +3-4‰).
The results of this study have indicated the coordination of photosynthetic, gas exchange and morphological foliar responses to growth at high elevations of 2500 and 3500 m a.s.l. Nonetheless, two generally divergent responses to increased elevation become apparent from the study between the evergreen Quercus species with leaf lifespans of 1-3 years, and S. atopantha and R. dentatus that possess foliage with a leaf lifespan of ,9 months. To illustrate these contrasting leaf responses to increased elevation, the relative changes of the physiological, morphological and compositional responses were plotted in Fig. 5. These suggest that the sclerophyllous Quercus species generally reduce conductance to CO 2 and photosynthetic capacity with an increase in elevation from 2500 to 3500 m a.s.l., while the shorter-lived foliage of S. atopantha and R. dentatus showed the opposite response.  Table 2. Photosynthetic parameters of the three species growing at lower and higher elevations (detailed in Table 1). Values of A max , V cmax and J max were obtained by fitting the Farquhar et al. (1980) model of leaf photosynthesis to five A/P i response curves for each species at each elevation. Means of a parameter followed by the same letter were not statistically different using a one-way ANOVA (P . 0.05) with LSD post hoc test.

Discussion
The results of our study have demonstrated contrasting physiological and morphological plasticity responses to an increase in elevation from 2500 to 3500 m a.s.l. in three Chinese montane species. Quercus spinosa and Q. aquifolioides possess robust sclerophyllous evergreen foliage with an average leaf lifespan .1 year. These Quercus species generally showed reductions in leaf gas exchange and photosynthetic capacity at the higher elevation. In contrast, the shorter-lived mesophytic foliage of S. atopantha and R. dentatus exhibited increases in conductance to CO 2 and the capacity of photosynthetic physiology at the higher elevation (Fig. 5). This may suggest that the response of the plant species analysed to increased elevation was associated with growth habit and leaf economic traits (Milla and Reich 2011).
A rise in elevation confers a number of challenges to photosynthesis such as reduced pCO 2 and temperature (Kö rner 2007). Despite the contrasting responses in terms of conductance to CO 2 and photosynthetic physiology observed among different species in this study, increased elevation did result in more positive foliar d 13 C, greater nitrogen concentration, enhanced R n and reduced SLA in all species. At the same latitude, the d 13 C of CO 2 within the atmosphere is generally lower at high elevations (Trolier et al. 1996). The increased d 13 C observed in all four species growing at 3500 m reflects the lower availability of CO 2 reducing discrimination against 13 C (Farquhar et al. 1989), despite the heavier isotope forming a reduced proportion of CO 2 at the higher elevation (Trolier et al. 1996). The d 13 C of a leaf is frequently affected by G s and is indicative of the water use efficiency of a plant (Farquhar and Richards 1984;Figure 3. Relationship between photosynthetic physiological capacity to assimilate CO 2 (A max , V cmax and J max ) and conductance to CO 2 (G s , G m and G tot ) at high elevations of 2500 m (open symbols) and 3500 m (filled symbols) a.s.l. of Q. spinosa (upward triangles), S. atopantha (circles) and R. dentatus (squares) from this study and Q. aquifolioides (inverted triangles) from the study of Feng et al. (2013). (A) A max versus G s (regression R 2 ¼ 0.791, F 1,45 ¼ 147.009, P ¼ 1.272 × 10 215 ); (B) A max versus G m (regression R 2 ¼ 0.847, F 1,45 ¼ 227.498, P ¼ 3.250 × 10 219 ); (C) A max versus G tot (regression R 2 ¼ 0.872, F 1,45 ¼ 223.520, P ¼ 7.399 × 10 219 ); (D) V cmax versus G s (regression R 2 ¼ 0.788, F 1,45 ¼ 156.650, P ¼ 4.277 × 10 216 ); (E) V cmax versus G m (regression R 2 ¼ 0.794, F 1,45 ¼ 141.911, P ¼ 1.642 × 10 215 ); (F) V cmax versus G tot (regression R 2 ¼ 0.859, F 1,45 ¼ 181.645, P ¼ 3.186 × 10 217 ); (G) J max versus G s (regression R 2 ¼ 0.834, F 1,45 ¼ 149.711, P ¼ 9.323 × 10 216 ); (H) J max versus G m (regression R 2 ¼ 0.818, F 1,45 ¼ 136.184, P ¼ 3.323 × 10 215 ); (I) J max versus G tot (regression R 2 ¼ 0.883, F 1,45 ¼ 161.692, P ¼ 2.470 × 10 216 ). Farquhar et al. 1989). However, d 13 C increases in all three species, despite S. atopantha and R. dentatus exhibiting increased G s at the higher elevation (Fig. 1), suggest that at elevations .2500 m, factors other than G s may influence carbon isotope discrimination. The increase in d 13 C values of plants with elevation is commonly considered to reflect reduced P i /P a ratios. However, due to modification of G tot , V cmax and J max with elevation, none of the species analysed in this study exhibited reduced P i /P a ratios at the higher elevation (Table 1). Nonetheless, increased foliar d 13 C observed in this study may indicate longer-term reductions in the P i /P a ratio of the three species that was not apparent during the comparatively short duration of the gas exchange measurements. However, the d 13 C values of the species analysed in this study are at the lower end of the range of values exhibited by plant species adapted to growth at high elevations (i.e. .2500 m) (Kö rner et al. 1988), possibly indicating that the combination of reduced P i /P a ratios alongside the decreased availability of CO 2 may induce lower d 13 C values in other species.
The concentration of nitrogen per unit leaf area of the four species increased on average 29.4 % with a rise in elevation from 2500 to 3500 m a.s.l. (Fig. 5). Foliar nitrogen content and SLA are positively related to A (Poorter et al. 1990;Terashima et al. 2011). Point gas exchange measurements of A were taken under identical conditions of temperature, light and [CO 2 ] at both 2500 and 3500 m a.s.l. This showed increased A at the higher elevation in the two species with short-lived foliage and lower A in the evergreen Quercus leaves. The greater values of A at the higher elevation in the two species where G s and G m rose with elevation may suggest that temperature plays a major role in limiting photosynthesis, thus affecting d 13 C and determining the response of plants to elevation. In plants adapted to cool climates, leaves developed under low temperatures exhibited higher V cmax and J max values (Bunce 2000). However, despite exhibiting an increase in N area at the higher elevation, the two Quercus species showed reductions in A, V cmax and J max at the greater elevation; this suggests that the greater N area observed in Q. spinosa and Q. aquifolioides at the higher elevation was not associated with increased allocation of nitrogen to photosynthetic physiology (cf. Shi et al. 2006), or that diffusive limitations imposed by reduced G s and G m constrain any effect of increased allocation of nitrogen to RubisCO on A (e.g. Centritto et al. 2003;Loreto and Centritto 2008). The decrease in the J max to V cmax ratio observed in Q. spinosa is indicative of reduced allocation of nitrogen into light harvesting activities (Wullschleger . Table 3. Leaf carbon isotopic composition (d 13 C), SLA, leaf nitrogen concentration per unit mass (N mass ), leaf nitrogen concentration per unit area (N area ) and leaf PNUE of the three plants growing at lower and higher elevations (elevations detailed in Table 1). Means of a parameter followed by the same letter were not statistically different using a one-way ANOVA (P . 0.05) with LSD post hoc test.  Figure 5. Relative effect of an increase in elevation from 2500 to 3500 m a.s.l. on photosynthetic, morphological and compositional characteristics of Q. spinosa, S. atopantha and R. dentatus from this study and Q. aquifolioides from the study of Feng et al. (2013). Error bars indicate 1 SE. 1993), possibly due to increased levels of radiation at the higher elevation. The greater values of A evident at higher elevations from the point measurements of leaf gas exchange at identical light and temperature may reflect the enhanced photosynthetic capacity and G tot of S. atopantha and R. dentatus. This enhancement of A at higher elevations would likely not be evident under ambient growth conditions where temperatures and high incident radiation would not be conducive to photosynthesis (Fujimura et al. 2010). Woody species with thick sclerophyllous leaves generally have lower levels of G tot than deciduous species that exhibit higher SLA values (Centritto et al. 2011). This lower conductance to CO 2 reduces P c levels and as a result constrains photosynthetic rates (Flexas et al. 2013;Lauteri et al. 2014). Any increase in the availability of CO 2 will disproportionately affect evergreen species with low SLA values due to this limitation on transport of CO 2 to the chloroplast envelope (Centritto et al. 2011;Niinemets et al. 2011). Future rises in atmospheric [CO 2 ] would, therefore, most likely favour evergreen species growing at high elevations such as Q. spinosa rather than those plants with short leaf lifespans such as S. atopantha that exhibit increased G tot with elevation (Table 1). The divergent responses between the species may be due to the selective pressures associated with long-and short-lived foliage (Reich et al. 1991). Higher elevations experience factors such as increased incident radiation, drier air and stronger winds that increase the leaf to air vapour pressure deficit and the transpirative demand per unit leaf area (Kö rner and Diemer 1987;Kö rner 2007;Kouwenberg et al. 2007). Evergreen species such as Q. spinosa and Q. aquifolioides maintain leaves during periods that are not conducive to photosynthesis; this may necessitate a reduction in levels of G s to prevent desiccation. In contrast, at higher elevations, the species with short-lived foliage can more fully exploit episodes where conditions are favourable to photosynthesis through enhanced levels of G s and G m at higher elevations before dispensing with leaves when growth conditions deteriorate and excessive transpirative and carbon balance costs are incurred. This behaviour does, however, incur costs in terms of the replacement of foliage each year, accounting for the lower SLA values of S. atopantha and R. dentatus in comparison with the two species of Quercus (Table 3). However, the construction costs per leaf are lower as investment in robust foliage capable of tolerating physical abrasion in a high energy windy environment (Wilson 1984) or physiological protection from high levels of harmful radiation over long periods of time is not required for leaves with a short leaf lifespan (Venema et al. 2000).
The number of mitochondria per unit leaf area increases with elevation (Miroslavov and Kravkina 1991), accounting for the increased R n values at higher elevations observed in this (Table 2) and other studies (Ledig and Korbobo 1983;Shi et al. 2006;Feng et al. 2013). This increased R n may be associated with lower partial pressures reducing the availability of oxygen (Crawford 1992), the increased respiratory demand required to support an enhanced photosynthetic physiology (Shi et al. 2006) or reduced ambient growth temperatures that result in higher R n values when R n is determined at the same leaf temperature (Atkin and Tjoelker 2003). When grown in a common garden study, 11 plant species collected from high elevations exhibited enhanced respiration at high temperatures relative to individuals of the same species that originated at low elevations. However, when temperature was reduced, R n values were identical between individuals from low and high elevations (Larigauderie and Körner 1995). This may suggest that respiratory adaptation to growth at high elevations is due to the lower temperatures experienced at elevation. Temperature is likely a major factor in shaping plant photosynthetic responses to growth at high elevations. The reduction in temperature associated with an increase in elevation from 2500 to 3500 m a.s.l. will result in lower photosynthetic activity (Brooks and Farquhar 1985). The two species with short leaf lifespans will be able to shed their foliage during winter, whereas the foliage of the evergreen Quercus species will have to withstand the months with the lowest temperatures. This will necessitate a degree of morphological (Cordell et al. 1998) and physiological (Körner and Diemer 1987) tolerance to low temperatures in the evergreen species (Ö quist and Huner 2003) and may account for the generally higher values of R n observed in the leaves of Q. spinosa at 3500 m a.s.l. Furthermore, the effect of the decline in temperature associated with increased elevation is more apparent in trees that are directly affected by atmospheric circulation than shrub or herb layer plants that are smaller and generally sheltered, and as a result under radiation can maintain a significantly higher temperature than the surrounding trees (Körner 2007). This differential effect of temperature changes at high elevation may contribute to the increase in G tot and photosynthetic capacity observed in S. atopantha and R. dentatus.

Conclusions
The three plant species analysed in this study exhibited significant physiological and morphological plasticity to enable growth at 2500 and 3500 m a.s.l., an elevational gradient equivalent to a 5.5 8C decline in temperature and 11.2 % reduction in pCO 2 . The results of this study suggest that the physiological and morphological adaptations required for growth at high elevations may be associated with plant growth habit and leaf economics.
AoB PLANTS www.aobplants.oxfordjournals.org Consistent with previous studies, all three species showed increased d 13 C, R n and leaf nitrogen at the higher elevation. However, critical differences in the photosynthetic and leaf gas exchange response to elevation were observed between the plants. The evergreen, Q. spinosa, showed reduced conductance to CO 2 and diminished levels of V cmax and J max at the higher elevation. In contrast, S. atopantha and R. dentatus with a leaf lifespan of ,9 months exhibited increased G tot and enhanced photosynthetic capacity to fix CO 2 at 3500 m. The selective pressures exerted by an increase in elevation may act differently dependent on the leaf lifespan of a species. Those species with short leaf lifespans can more fully exploit favourable growth conditions through increased conductance to CO 2 and A before shedding foliage as conditions become less conducive to photosynthesis. Whereas evergreen species need to invest in physically robust leaves and physiological protective mechanisms to endure unfavourable conditions, this may necessitate a decrease in G s to reduce water loss associated with the higher transpirative demands at higher elevations due to increased wind and radiation. Climate change may affect the plant species that compose high-elevation ecosystems differently depending on leaf economic traits as increased pCO 2 is likely to benefit evergreen species with thick sclerophyllous leaves to a greater extent than deciduous species.