Leaf photosynthetic, economics and hydraulic traits are decoupled among genotypes of a widespread species of eucalypt grown under ambient and elevated CO2
Summary
- Leaf economics and hydraulic traits strongly influence photosynthesis. While the level of coordination among these traits can differ between sets of species, leaf functional trait coordination within species remains poorly understood. Furthermore, elevated concentrations of atmospheric CO2 commonly influence the expression of leaf photosynthetic, economics and hydraulic traits in contrasting ways, yet the effect of variable concentrations of atmospheric CO2 on patterns of trait coordination within species remains largely untested.
- We examined the relationships among key leaf photosynthetic (e.g. net photosynthesis and photosynthetic biochemistry), economics and water-use (e.g. leaf mass per unit area and stomatal conductance) and hydraulic traits (e.g. vein density) in 14 genotypes of Eucalyptus camaldulensis grown in ambient (aCO2) and elevated (eCO2) [CO2]. We examined the level of coordination among leaf traits in aCO2 and then assessed whether growth in eCO2 altered that coordination.
- We found that leaf traits related to photosynthetic capacity, economics and water-use, and hydraulics were decoupled among genotypes grown in aCO2, yet strong relationships were generally observed among suites of traits within each ‘functional group’.
- Significant responses to growth in eCO2 were observed for most leaf photosynthetic and economics and water-use traits, with the magnitude and direction of the response varying among traits. In contrast, leaf hydraulics traits were unaffected by variable growth CO2. Despite this, growth in eCO2 did not substantially alter patterns of leaf trait coordination observed in aCO2.
- These results suggest suites of leaf traits associated with photosynthetic capacity, economics and water-use and hydraulics, respectively, can form independent axes of variation among genotypes of a single species, regardless of growth CO2. Although growth in eCO2 did not substantially alter patterns of trait coordination, decoupling of leaf functional traits among genotypes may allow genetically distinct populations to produce novel combinations of traits that may be adaptive in response to changes in their local environment.
Introduction
Studies of functional trait coordination in leaves have greatly advanced our understanding of leaf structure and function (Givnish 1987; Sack et al. 2003; Brodribb, Feild & Sack 2010) and helped identify the biophysical constraints and trade-offs that underlie key ecological strategies (Westoby et al. 2002). From an economics perspective, consistency in the relationships among many leaf functional traits within and across biomes is suggestive of a unified plant traits spectrum, whereby all species are characterized along a single axis of variation in terms of fast, medium or slow plant function (Reich 2014). Across species, evidence for a single axis of trait variation is drawn from correlations among leaf economics traits that define plant ecological strategies with fast to slow photosynthetic payback relative to leaf investment (Wright et al. 2004), and from evidence that leaves with more efficient hydraulic systems tend to have higher photosynthetic rates (Sack et al. 2003; Brodribb, Feild & Jordan 2007). The common connection between leaf economics and leaf hydraulics in serving photosynthesis has also led to proposals that hydraulic traits such as vein density (VD) are predictive of the leaf economics spectrum (Blonder et al. 2011). However, leaf functional traits may not always vary in such a coordinated manner. Recent studies in diverse forest systems have observed trait decoupling among drought tolerance and economics traits (Marechaux et al. 2015), and among leaf hydraulic and leaf economics traits (Li et al. 2015), suggesting that different functional trait combinations are possible within leaves. Functional trait coordination in leaves might also be decoupled in response to environmental change such as elevated atmospheric [CO2] (eCO2), which commonly induces differential responses in leaf functional traits.
A common response of C3 plants to eCO2 is increased net photosynthesis and decreased stomatal conductance. Longer term growth under eCO2 may also lead to photosynthetic down-regulation (Ainsworth & Rogers 2007) and changes in a suite of functional and structural traits associated with leaf gas exchange and water transport (hydraulic) systems (Franks et al. 2013; Rico et al. 2013). Plant growth in eCO2 may reduce stomatal density (Woodward & Kelly 1995) via feedback loops that optimize water loss relative to long-term carbon gain (Franks et al. 2012). Plant growth in eCO2 may also reduce leaf traits associated with water supply, such as VD, so that investment in water transport capacity is also optimized relative to photosynthetic carbon gain (Brodribb & Jordan 2011). However, experimental studies suggest that leaf hydraulics can be decoupled from gas-exchange traits in eCO2 (Uhl & Mosbrugger 1999; Locke et al. 2013). Leaf-level responses to eCO2 may also include increased leaf mass per area (LMA), due to increases in leaf thickness and carbohydrate accumulation, and a reduction in leaf nitrogen content (Ainsworth & Long 2005; Leakey et al. 2009). Taken together, such potentially differential responses to growth in eCO2 may act to alter patterns of trait coordination within leaves.
Species often vary substantially in their physiological response to eCO2 (Ainsworth & Rogers 2007; Hovenden & Williams 2010). However, intraspecific (i.e. genotypic) variation in trait responsiveness may also be significant (Bernacchi et al. 2003; Davey et al. 2006) and important in determining population and species performance under climate change (Moran, Hartig & Bell 2016). Despite this, the linkages among leaf functional traits are rarely examined within a given species (but see Aspinwall et al. 2013; Niinemets 2015), and it is unclear the degree to which variable CO2 may alter coordination of leaf functional traits within species. Determining leaf functional trait coordination among genotypes could provide insight into patterns of physiological divergence within species. Moreover, determining how eCO2 influences leaf trait coordination among genotypes could provide an integrative view of genotypic variation in leaf functional trait responses to eCO2.
Widely distributed species of Eucalyptus represent potentially useful and important models for studying patterns of leaf functional trait coordination within species. Eucalypts dominate forest and woodland communities throughout Australia and are economically important as major forestry species worldwide. Numerous studies have examined growth and physiological traits among Eucalyptus provenances in response to changes in soil moisture, salinity, light and temperature (Bedon et al. 2012; Bush et al. 2013; Drake et al. 2015), while other studies have examined changes in leaf structure and function in response to variable growth [CO2] in individual eucalypt species (Smith et al. 2012). However, to the best of our knowledge, there are no studies that have examined the relationships between leaf functional traits among Eucalyptus genotypes and how these relationships are potentially altered under eCO2.
Here, we assessed the linkages among key leaf photosynthetic, economics and hydraulic traits (see Table 2) across 14 Eucalyptus camaldulensis (subsp. camaldulensis) genotypes, representing six provenances, grown under non-limiting water and nutrient conditions at ambient [CO2]. We tested the specific hypothesis that genetic variation in leaf photosynthetic, economic and hydraulic traits would occur along a single axis of variation (Reich 2014) on the basis that (i) leaf hydraulic traits (especially VD) underpin key aspects of the leaf economics spectrum (Blonder et al. 2011); and (ii) both leaf hydraulic and economics traits influence rates of leaf photosynthesis (Wright et al. 2004; Brodribb, Feild & Jordan 2007; Wyka et al. 2012). We also examined genetic variation in the response of each trait to growth in eCO2. Because the magnitude and direction of the eCO2 response can vary among leaf traits, we also hypothesized that growth in eCO2 will alter patterns of coordination of leaf functional traits among genotypes.
Materials and methods
Species and Experimental Conditions
Fourteen genotypes of Eucalyptus camaldulensis subsp. camaldulensis (River Red Gum) were included in this study. Eucalyptus camaldulensis is distributed widely across mainland Australia and is an important component of floodplain and riparian environments. The distribution of subspecies, camaldulensis, encompasses much of the Murray – Darling River basin of New South Wales and Victoria and extends into parts of Queensland and South Australia (Atlas of Living Australia). The subspecies’ distribution extends across significant gradients of temperature (mean annual temperature range 13·6–19·2 °C) and precipitation (mean annual precipitation range is 275–750 mm). Previous work has found limited genetic structure among populations within this subspecies, indicating high levels of gene flow and genetic diversity (Dillon et al. 2015).
In our study, clonal plants were propagated from each genotype that had been grown from seed collected from an open-pollinated mother tree (i.e. half-sib family). The mother trees originated from six provenances representing different geographic and climatic origins throughout the subspecies distribution (Table 1). The clones of each genotype were prepared via vegetative propagation of rooted cuttings. The cuttings were established in 38 mm diameter × 210 mm tall containers filled with potting mix, and grown in a common shade house for roughly 2 months. The cuttings were transplanted into 6·9 L cylindrical pots with several ~1 cm diameter drainage holes and grown in a naturally lit glasshouse facility at Western Sydney University in Richmond NSW, Australia (see Resco de Dios et al. 2015), once average stem height (H) and basal diameter (D) reached 25 cm and 2 mm respectively. Each pot contained 7·5 kg of coarse textured soil (Australian Native Landscape Pty, Ltd, Bagerys Creek, NSW, Australia), with a pH of 6·5. To ensure that no nutrient limitations occurred, the plants were fertilized every fortnight with a commercial liquid fertilizer (500 mL Aquasol, at 1·6 g L−1; 23% N, 4% P, 18% K, 0·05% Zn, 0·06% Cu, 0·013% Mo, 0·15% Mn, 0·06% Fe, 0·011% B; Yates Australia, Padstow, NSW, Australia).
Provenance | Lat (°S) | Long (°E) | MAT (°C) | MAP (mm) | ET (mm) | G |
---|---|---|---|---|---|---|
Coonawarra | 37·2 | 140·42 | 14·5 | 646 | 1029 | 2 |
Yass River | 34·53 | 149·02 | 13·9 | 395 | 1141 | 2 |
Ovens Valley | 36·36 | 146·47 | 15 | 331 | 1214 | 2 |
Barmah | 35·5 | 145·07 | 16·3 | 644 | 1331 | 2 |
Condobolin | 33·06 | 147·09 | 17·6 | 393 | 1440 | 2 |
Nyngan | 31·33 | 147·11 | 19·2 | 345 | 1565 | 4 |
- MAT, mean annual temperature; MAP, mean annual precipitation; ET, evaporation, G, number of genotypes in the study from each provenance.
Eight to 16 replicate clones of each genotype were grown in two CO2 concentrations; ambient (aCO2, 400 μmol mol−1) and elevated (eCO2, 640 μmol mol−1). The study design was a randomized split-plot design with two glasshouse rooms per CO2 treatment. For each CO2 treatment, replicate plants of each genotype were split into two groups and randomly assigned to one of the two rooms. Each group (glasshouse room) of plants was considered a block, and the unit of replication was the individual plant. Within each room, plants were rotated weekly to reduce potential location effects on plant performance. Mean daytime and night-time air temperature and relative humidity within the glasshouse were 26 and 17 °C, and 45 and 60% respectively, which is representative of average summer values in Richmond. All pots were hand-watered daily (using charcoal-filtered tap-water) to field capacity which ensured that soil moisture was not limiting.
Gas-Exchange Parameters
Leaf-level net photosynthesis CO2 response (A-Ci) curve measurements were made on all replicates of each genotype in each growth CO2 treatment using several cross-calibrated Li-Cor 6400-XT portable infrared gas analysers (Li-Cor Inc., Lincoln, NE, USA) with a 2 × 3 cm2 cuvette head and a red and blue LED light source. A-Ci curve measurements were made on mature, fully expanded, upper canopy leaves after roughly 60 days of growth under the CO2 treatments. Measurements were conducted on consecutive days (~9), and gas-exchange analysers were randomly assigned to glasshouse bays each day. The order in which replicates of each genotype within each CO2 treatment were measured was random. For all measurements, light conditions within the cuvette were controlled at a photosynthetic photon flux density of 1800 μmol m−2 s−1 and block temperature was fixed at the daytime growth temperature of 26 °C. The Li-Cor 6400 desiccant tubes were used to control water vapour inside the cuvette, so that vapour pressure deficit (VPD) was 1·4 ± 0·02 (standard error) kPa. Prior to beginning each A-Ci curve, steady-state rates of leaf net photosynthesis (Anet, μmol m−2 s−1) and stomatal conductance to water vapour (gs, mol m−2 s−1) were measured at the growth [CO2]. Following steady-state measurements, A-Ci curves were produced by measuring Anet at 10 reference CO2 (Ca) concentrations, ranging from 0 to 1000 μmol mol−1. A biochemical model of photosynthesis (Farquhar & von Caemmerer 1982) was used to parameterize the A-Ci curve data for each plant. The model estimates the maximum rate of carboxylation (Vcmax; μmol m−2 s−1) and the potential rate of electron transport for RuBP regeneration at 1000 μmol m−2 s−1 (J1000; μmol m−2 s−1). Because we did not measure leaf mesophyll conductance to CO2 (gm), which is known to show variable responses to growth under eCO2 across species (Flexas et al. 2012), Vcmax and J1000 are apparent values based on intercellular [CO2] (Ci) rather than [CO2] concentration at the chloroplast. The model was fit using the plantecophys package (Duursma 2015) in r v3.2 (R Core Team, 2015).
VD and Stomatal Traits
Vein density and stomatal traits were measured on fully expanded leaves sampled from the upper canopy of individual plants after roughly 70 days of growth under the CO2 treatments. To determine VD, we sampled one leaf from each of three replicate plants of each genotype within each CO2 treatment. Veins located centrally in the lamina of each leaf were exposed by removing an area of ~1 cm2 of epidermis and top layers of palisade mesophyll with a razor blade. These ‘windows’ into the leaf venation were cut out and chemically cleared using 20% household bleach. Cleared leaf sections were stained with saffranine-O and counter stained with fast-green and semi-permanently mounted on glass slides using glycerol jelly. VD was calculated as the total length of vein (mm) per unit area (mm2) of image taken at 10× magnification using a digital camera (Leica DCF 500, Cambridge, UK) mounted to a light microscope (Olympus BX60, Center Valley, PA, USA). Each image focused on an area of leaf venation away from 2nd order veins, which do not contribute substantially to total vein length compared to higher order veins (Sack & Scoffoni 2013). Image analysis was performed using imagej (http://imagej.nih.gov/ij/).

where d is the diffusivity of water vapour in air (m2 s−1); ʋ, the molar volume of air (m3 mol−1); D, stomatal density (m−2); amax, the maximum area of the open stomatal pore (m2); l, the depth of the stomatal chamber (equivalent to the width of a single guard cell). The amax was estimated as π (p/2)2, where p is the length of the stomatal pore.
Leaf Economics Traits
Plants were harvested within a week, after approximately 80 days of growth under the CO2 treatments. Total tree leaf area (LA, cm2) of each plant was determined by measuring the LA of all leaves using a LA meter (LI-3100C; Li-Cor Inc, Lincoln, Nebraska). Total leaf dry mass was determined after oven drying at 70 °C to a constant mass, and a specific leaf area (SLA, cm2 g−1) was calculated as the ratio of LA to total leaf dry mass. Leaf carbon (C) and nitrogen (N) content were determined on a subsample of dried leaf material from each tree collected at the harvest. Leaves were ground into a fine powder using a ball grinder, stored under desiccation, and leaf N concentration were determined using a combustion elemental analyser (CE Instruments, Wigan, UK). Nitrogen per unit LA (Narea; g [N] m−2) was obtained by the quotient of N per unit leaf mass (g kg−1) and adjusted to a m2 basis. Following determination of non-structural carbohydrates (see below), we calculated TNC-free LMA (LMAnoTNC).
Leaf starch (Lstarch; g kg−1) and leaf soluble sugars (Lsugars; g kg−1) were determined on recently mature, sunlit leaves, sampled from the upper canopy. Leaf collections were made mid-morning, after 11 weeks of plant growth under the treatment conditions. The leaf samples were flash frozen in liquid N, freeze-dried, ground to a fine powder in a ball mill, and then extracted three times with 2 mL of a methanol-chloroform-water (12 : 5 : 3 v/v) solution to separate the soluble sugars from the starch (pellet fraction). Starch was hydrolyzed from the pellet with 5 mL of perchloric acid (35% v/v) for 30 min. Lstarch and Lsugars concentrations were determined using a colorimetric phenol-sulphuric method (Tissue & Wright 1995).
Leaf 13C composition (δ13Cleaf) was measured using an Isochrom continuous-flow mass spectrometer (Micromass, Manchester, UK) following combustion in the elemental analyser. δ13Cleaf was converted to discrimination values using mean values for previously measured 13C composition in the aCO2 and eCO2 treatments in the glasshouse: δ13Cair; −9·83‰ and −17·02‰ for aCO2 and eCO2, respectively, relative to Vienna Pee Dee Belemnite (Lewis et al. 2015). Leaf carbon isotope discrimination (Δ13C) is inversely related to δ13Cleaf, and is calculated as: Δ13C = (δ13Cair – δ13Cleaf)/(1 + δ13Cleaf/1000) (Farquhar & Richards 1984).
Data Analysis
Linear mixed effects models were conducted using the ‘lme4’ package (Bates et al. 2015) in r v3.2 (R Core Team, 2015) to test the main effects of growth treatment CO2 concentration (CO2), genotype (G) and their interactions (CO2 × G) on all response variables, with the exception of SD and gwmax which had not been assigned to individual replicates at the time of sampling (a Student's t-test was used to compare SD and gwmax across CO2 treatments). In the mixed effects models, glasshouse bay nested within CO2 treatment was treated as a random effect. We assessed homogeneity of variance by examining plots of the residuals (Y-axis) vs. the predicted values (X-axis) from each model and ensured that the residuals were normally distributed around ‘0’ and variance in the residuals did not vary with changes in the predicted values. If the CO2 × G term was significant in the model, we interpreted this as an indication that genotypes differed in their response to eCO2 (indicating intraspecific variation in phenotypic plasticity). Genotype mean CO2 response ratios were also calculated for each trait [i.e. mean (eCO2)/mean (aCO2)].
We did not test the effect of ‘provenance’ for several reasons. First, our primary objective was to examine patterns of leaf trait coordination across as many genotypes as possible. Secondly, a related objective was to determine the degree of genetic differentiation in leaf traits, and examine relationships between genotype leaf trait means and responsiveness to eCO2 (i.e. plasticity). With six provenances, neither analysis is feasible at the provenance level. In addition, the number of genotypes and replicate plants from within each provenance was unbalanced, making tests of provenance differences and provenance variation in responses to eCO2 (i.e. CO2 × provenance) problematic to interpret.
Pearson correlation analysis was performed for all pairwise trait comparisons of genotype means within each CO2 treatment. We also examined covariation among genotype means within each CO2 treatment for leaf photosynthetic, economics and hydraulic traits (with the exception of Lstarch and Lsugars) using principal components analysis (PCA) with orthogonal (varimax) factor rotation in sas v9.3 (PROC FACTOR, SAS Institute Inc. 2010 Cary, NC). We excluded Lstarch and Lsugars from the PCA because these traits had not been measured across all 14 genotypes. Parallel analysis was used to determine the number of principal components (PC's) to retain (Franklin et al. 1995; Peres-Neto, Jackson & Somers 2005).
Results
Genotypes showed substantial differentiation in many leaf physiological, economics and hydraulic traits (Table 2). For example, averaged across both CO2 treatments, Narea and LMA varied by 42% and 41%, respectively, among genotypes. In comparison, genotypes showed comparatively less variation in Anet (18%) and VD (16%). Stomatal traits such as SD (37%) and gwmax (43%) also varied substantially among genotypes, as did the ratio of SD displayed on each side of the leaf (i.e. the degree of amphistomy; 31%). With the exception of Lsugars, genotypes showed no significant (P > 0·05) variation in leaf trait responses to variable growth [CO2], i.e. there was no evidence of G × CO2 interactions (Table 2).
Trait | Symbol | Unit | n | aCO2 | eCO2 | anova results | |||||
---|---|---|---|---|---|---|---|---|---|---|---|
CO2 | Genotype (G) | G × CO2 | |||||||||
d.f. | χ2 | d.f. | χ2 | d.f. | χ2 | ||||||
Photosynthetic | |||||||||||
Net photosynthesis at growth CO2 | A net | μmol m−2 s−1 | 14 (154) | 26·0 ± 0·4 | 33·4 ± 0·5 | 1 | 199*** | 13 | 42·9*** | 13 | 21·5 |
Max. rate of Rubisco carboxylation | V cmax | μmol m−2 s−1 | 14 (153) | 109 ± 2 | 102 ± 2 | 1 | 9·10** | 13 | 36·6*** | 13 | 17·2 |
Potential rate of electron transport | J 1000 | μmol m−2 s−1 | 14 (153) | 198 ± 3 | 198 ± 4 | 1 | 0·0008 | 13 | 22·4* | 13 | 6·55 |
Leaf economics and water-use | |||||||||||
Stomatal conductance | g s | mol m−2 s−1 | 14 (144) | 0·72 ± 0·03 | 0·58 ± 0·03 | 1 | 19·7*** | 13 | 22·2 | 13 | 15·6 |
Leaf mass per unit area | LMA | g m−2 | 14 (156) | 69·4 ± 1·6 | 83·2 ± 1·8 | 1 | 67·1*** | 13 | 165*** | 13 | 8·02 |
Nitrogen per unit leaf area | N area | g [N] m−2 | 14 (156) | 1·80 ± 0·05 | 1·71 ± 0·04 | 1 | 6·09* | 13 | 183*** | 13 | 6·67 |
Leaf starch concentration | L starch | g kg−1 | 9 (98) | 81·7 ± 4·4 | 110 ± 5 | 1 | 21·0*** | 8 | 37·2*** | 8 | 1·63 |
Leaf soluble sugar concentration | L sugars | g kg−1 | 9 (98) | 49·9 ± 1·7 | 49·5 ± 1·4 | 1 | 0·05 | 8 | 32·4*** | 8 | 38·8*** |
TNC-free LMA | LMA noTNC | g m−2 | 9 (98) | 60·2 ± 1·8 | 68·7 ± 1·9 | 1 | 30·5*** | 8 | 196*** | 8 | 3·9 |
Leaf carbon isotope iscrimination | Δ13C | ‰ | 14 (156) | 24·0 ± 0·1 | 20·7 ± 0·1 | 1 | 912*** | 13 | 75·4*** | 13 | 5·19 |
Leaf hydraulics | |||||||||||
Vein density | VD | mm mm−2 | 14 (111) | 10·5 ± 0·1 | 10·6 ± 0·1 | 1 | 0·9 | 13 | 73·8*** | 13 | 18·9 |
Stomatal density | SD | no. mm−2 | 14 (136) | 311 ± 7 | 306 ± 7 | ||||||
Maximum stomatal conductance to water vapour | g wmax | mol m−2 s−1 | 14 (136) | 3·03 ± 0·12 | 2·91 ± 0·08 |
- LMA, leaf mass per area.
- Chi-squared values denoted with ***, **, and *are significant at P < 0·0001, P < 0·01 and P ≤ 0·05 respectively.
Averaged across genotypes, growth in eCO2 significantly increased Anet, LMA and Lstarch and decreased gs, Vcmax and Narea, while there was no significant [CO2] treatment effect on J1000, Lsugars and VD (Fig. 1; Table 2). In addition, LMAnoTNC significantly decreased in eCO2 indicating that eCO2-induced increases in LMA were due to leaf structural (leaf thickness) and carbohydrate level changes. Student's t-test comparison of stomatal traits, which were not included in the anova indicated that eCO2 did not affect SD (t = 0·51, P = 0·6) or gwmax (t = 0·89, P = 0·38).

Trait Coordination in aCO2
Under aCO2, PCA of genotype means identified three independent axes which cumulatively explained 78% of the total variation in genotype mean leaf trait values (Table 3; Fig. 2). The first PC accounted for 35% of the total variation and was correlated with leaf economics and water-use traits (positively with LMA, Narea and gwmax, and negatively with gs and Δ13C). The second PC (32% of total variation) was positively correlated with photosynthetic traits Anet, Vcmax and J1000. Finally, the third PC (12% of total variation) was positively correlated with hydraulic traits VD, SD and gwmax.
Growth CO2 | aCO2 | eCO2 | ||||
---|---|---|---|---|---|---|
PC 1 | PC 2 | PC 3 | PC 1 | PC 2 | PC 3 | |
Eigenvalue | 3·51 | 3·15 | 1·15 | 3·86 | 2·2 | 1·68 |
Variance explained | 35% | 32% | 12% | 38% | 22% | 17% |
Photosynthetic | ||||||
A net | −0·25 | 0·90 | −0·28 | −0·25 | 0·85 | 0·37 |
V cmax | 0·01 | 0·91 | −0·17 | 0·17 | 0·90 | 0·06 |
J 1000 | 0·14 | 0·91 | −0·10 | −0·07 | 0·95 | −0·01 |
Leaf economics | ||||||
g s | −0·83 | −0·09 | −0·06 | 0·12 | 0·30 | 0·68 |
Leaf mass per area | 0·87 | −0·14 | −0·22 | 0·94 | −0·17 | −0·01 |
N area | 0·93 | 0·04 | −0·13 | 0·84 | −0·12 | 0·01 |
Δ13C | −0·81 | 0·0 | 0·07 | −0·74 | 0·13 | 0·22 |
Leaf hydraulics | ||||||
Vein density | −0·09 | −0·14 | 0·83 | −0·01 | 0·15 | 0·91 |
SD | −0·13 | −0·34 | 0·74 | 0·67 | −0·24 | 0·43 |
g wmax | −0·65 | −0·07 | 0·51 | −0·19 | −0·07 | 0·83 |
- Bolded values are those with Eigen scores >0·5, indicating significant association with corresponding PC axes. Trait abbreviations are provided in Table 2.

The separation of co-related traits into three functional groups was broadly supported by univariate correlations between genotype means (Table 4). Among leaf traits measured under aCO2, Anet was positively correlated with Vcmax (r = 0·87, P < 0·0001) and J1000 (r = 0·79, P < 0·0001), but was unrelated to gs and all leaf economics (e.g. LMA and Narea) and hydraulic traits (e.g. VD) respectively (Table 4). Under aCO2, VD was not significantly correlated with SD or gwmax, and was unrelated to gs and all leaf economics traits respectively (Table 4). In contrast, significant relationships were observed among leaf economics and water-use traits; gs was negatively correlated with LMA and Narea, and positively correlated with Δ13C; while Δ13C was negatively correlated with LMA and Narea (Table 4).
A net | V cmax | J 1000 | g s | LMA | N area | L starch | L sugars | Δ13C | Vein density | SD | g wmax | |
---|---|---|---|---|---|---|---|---|---|---|---|---|
A net | 0·85 | 0·75 | 0·41 | −0·35 | −0·26 | −0·21 | 0·62 | 0·32 | 0·46 | 0·23 | 0·26 | |
V cmax | 0·87 | 0·78 | 0·15 | −0·21 | −0·03 | −0·21 | 0·49 | 0·41 | 0·12 | 0·06 | 0·01 | |
J 1000 | 0·79 | 0·74 | 0·23 | −0·11 | −0·03 | 0·05 | 0·03 | −0·03 | 0·09 | −0·28 | −0·08 | |
g s | 0·24 | −0·06 | −0·22 | −0·16 | −0·36 | 0·37 | 0·49 | 0·20 | 0·67 | 0·17 | 0·34 | |
LMA | −0·25 | −0·07 | −0·02 | −0·59 | 0·91 | 0·27 | 0·28 | −0·57 | −0·18 | −0·23 | 0·33 | |
N area | −0·14 | 0·07 | 0·18 | −0·73 | 0·91 | −0·20 | −0·13 | −0·41 | −0·13 | −0·37 | −0·01 | |
L starch | −0·21 | −0·19 | −0·51 | 0·29 | 0·27 | 0·08 | −0·27 | −0·34 | 0·01 | −0·68 | −0·52 | |
L sugars | −0·05 | −0·04 | 0·03 | −0·30 | 0·28 | 0·38 | −0·46 | 0·63 | 0·74 | 0·72 | 0·67 | |
Δ13C | 0·16 | 0·04 | −0·12 | 0·65 | −0·57 | −0·66 | −0·43 | 0·08 | 0·15 | 0·51 | 0·38 | |
Vein density | −0·33 | −0·31 | −0·25 | 0·15 | −0·18 | −0·21 | 0·05 | −0·06 | 0·05 | 0·30 | 0·64 | |
SD | −0·46 | −0·35 | −0·37 | −0·06 | −0·23 | −0·12 | −0·48 | 0·34 | 0·21 | 0·45 | 0·57 | |
g wmax | −0·37 | −0·13 | −0·08 | −0·45 | 0·33 | 0·36 | −0·13 | −0·01 | −0·41 | 0·32 | 0·25 |
- LMA, leaf mass per area.
- All traits were log-transformed to improve normality. Bolded values indicate significant correlations (P < 0·05) between pairs of independent traits. Trait abbreviations are provided in Table 2.
Trait Coordination in eCO2
Growth in eCO2 did not substantially alter (with two exceptions) the patterns of functional coordination among leaf traits observed under aCO2 (Table 3; Fig. 2). The PCA identified three independent axes of trait variation, with each PC broadly associated with leaf economics and water-use traits (PC1, 38% of total variation), leaf photosynthetic traits (PC2, 22% of total variation) and leaf hydraulics traits (PC3, 17% of total variation) respectively. Two traits were observed to shift their PC grouping under eCO2: gs shifted from the leaf economics PC to the leaf hydraulics PC, while SD shifted from the leaf hydraulics PC to the leaf economics PC.
In eCO2, strong pairwise trait correlations were observed among photosynthetic traits, but fewer correlations were observed among leaf economics and water-use traits compared to aCO2 (Table 4). In agreement with the PCA, variation in gs was significantly correlated with VD under eCO2, which in turn was correlated with gwmax. In addition, a significant positive correlation was observed between VD and Lsugars (r = 0·74, P = 0·02).
Discussion
Genotypes of E. camaldulensis subsp. camaldulensis showed substantial differentiation across CO2 treatments in nearly all leaf traits, despite evidence of limited genetic structure among populations of this subspecies (Dillon et al. 2015). This level of genotypic variation allowed us to examine patterns of coordination among leaf functional traits. Across genotypes grown in aCO2, we found that leaf traits were clustered into three separate syndromes associated with leaf photosynthetic capacity, leaf economics and water-use, and leaf hydraulics respectively. This suggests that key sets of leaf functional traits do not align themselves along a single axis of variation across genotypes of E. camaldulensis, as recently proposed for functional trait variation across species (Reich 2014). Instead, it suggests independent functional trait dimensions may exist within leaves (Li et al. 2015; Marechaux et al. 2015), even within a single species. Furthermore, we found that growth in eCO2 did not substantially alter these functional groupings, despite differences in the magnitude and direction of eCO2 effects among the trait variables.
Decoupling of Leaf Functional Traits
Across genotypes, we expected leaf photosynthetic, economics and hydraulic traits to covary along a single axis of trait variation (Reich 2014). This expectation was based on theory that hydraulic traits such as VD underlie key aspects of the leaf economics spectrum (Blonder et al. 2011), and evidence that leaf hydraulics and economics traits both influence rates of photosynthesis (Wright et al. 2004; Brodribb, Feild & Jordan 2007). Our within-species findings add to evidence that sets of leaf functional traits can vary independently from each other, and are consistent with studies that have observed independence between leaf economics and hydraulic traits across diverse sets of species (Sack et al. 2013; Li et al. 2015).
We found that leaf hydraulic traits such as VD were unrelated to net photosynthesis and stomatal conductance among E. camaldulensis genotypes. These results support emerging reports of weak coordination between VD and leaf gas exchange across some sets of angiosperms (Walls 2011; Gleason et al. 2016) and suggest that the evolutionary drivers linking hydraulics and gas exchange are not completely understood. We also found that photosynthetic traits were unrelated to both leaf investment (LMA) and leaf N, indicating that photosynthetic capacity can vary among E. camaldulensis genotypes without covariation in key aspects of leaf structure and nitrogen concentration. These results contrast with previous studies that have observed positive relationships among photosynthesis and leaf economics traits on an area basis (Wright et al. 2004), especially among species with structurally similar leaves (Wyka et al. 2012). Finally, stomatal conductance and ΔC13 were most closely related to leaf economics traits, indicating a potentially strong influence of leaf tissue structure on CO2-water exchange dynamics (Zwieniecki & Boyce 2014).
Our study was conducted under non-limiting nutrient and soil moisture conditions in an environmentally controlled glasshouse. This approach is somewhat similar to a common garden experiment and allowed us to assess the genetic basis of trait variation in E. camaldulensis subsp. camaldulensis. In comparison, most studies of leaf functional traits examine patterns of cross-species variation along gradients of resource availability (light, water, nutrients and temperature) in the field (Westoby et al. 2002; Poorter et al. 2009). In these studies, the range of trait values is often very large, making it easier to detect adaptive patterns of coordination within and across habitats (e.g. Reich et al. 2003). However, it is not always possible to distinguish between genetic and environmental (plastic) sources of trait variation in these cross-species comparisons, the latter of which may alter leaf trait relationships within species (Niinemets 2015). In our study, leaf traits were strongly differentiated among genotypes; however, the range of values across genotypes for each trait was relatively small, thereby making it difficult to detect significant trait–trait correlations.
In cross-species comparisons, trait decoupling may be due to evolutionary divergence among plant lineages in different aspects of leaf structure and function (Li et al. 2015; Marechaux et al. 2015). Such evolutionary divergences are relatively constrained among genotypes of a single species. However, our within-species results provide insight into the eco-evolutionary potential for divergence in plant functional traits that lead to multiple trait dimensionalities and which are important for explaining community assembly theory across biomes (Laughlin 2014). Across species, independent trait dimensions may arise as a result of the physical separation of leaf structures associated with different sets of traits. Li et al. (2015) utilized this argument to explain why leaf economics and hydraulic traits were unrelated across a diverse group of tropical-subtropical angiosperms. Central to their argument was that leaves typically contain two functional sublayers; the upper palisade- (associated with traits such as leaf N that influence photosynthetic capacity; Vcmax) and the lower spongy-mesophyll (associated with traits such vein and stomatal density that influence hydraulic capacity). Processes within each sublayer can vary independently in different growth situations, while traits such as LMA integrate tissue structures of the entire leaf. Although this framework is appealing for understanding how multiple trait combinations could arise, it breaks down to some extent in the current study. Eucalyptus camaldulensis leaves are iso-bilateral (i.e. they do not have a clearly defined ‘upper’ and ‘lower’ surface), suggesting both sides of the leaf are functionally equivalent. Nevertheless, genotypes did vary significantly in the degree of leaf amphistomy they displayed (the ratio of stomata on each side of the leaf), which may have altered the relationships between leaf structural, hydraulic and gas-exchange traits (Brodribb, Jordan & Carpenter 2013). It might also help explain the lack of significant correlation between VD and stomatal traits across genotypes.
Although the magnitude and direction of eCO2 effects differed among the trait variables, eCO2 did not substantially alter patterns of leaf functional coordination among genotypes. PCA again revealed three independent axes of trait variation in eCO2, with individual traits generally adhering to the same ‘functional groupings’ defined in aCO2. There were, however, two notable exceptions. Among genotypes grown in eCO2, stomatal density shifted towards the leaf economics syndrome, consistent with previous reports of coordination between stomatal density, LMA and cell size (Loranger & Shipley 2010; Brodribb, Jordan & Carpenter 2013), while stomatal conductance shifted towards the hydraulic traits syndrome, and was in fact strongly correlated with VD across genotypes. This correlation between VD and stomatal conductance suggests some degree of coordination among genotypes between hydraulic supply and leaf water-use in response to growth in eCO2, even though VD was overall unresponsive to eCO2 while stomatal conductance declined significantly. VD was also significantly correlated with leaf soluble sugars (P < 0·05) and weakly correlated with net photosynthesis (P < 0·1) across genotypes, but only when grown in eCO2. Taken together, these results are intriguing and may highlight a possible role of leaf venation in determining the level of the eCO2 response in leaf water-use and carbon traits, in terms of its influence on water transport capacity via the xylem and sugar export capacity via the phloem. It may also help explain the overall lack of adjustment in VD in response to eCO2 on the basis of contrasting functional demand between reductions in leaf water-use and increases in photosynthetic activity (Muller et al. 2014).
Trait-Mean Responses to eCO2
Growth in eCO2 significantly increased net photosynthesis, presumably as a result of increased [CO2] at the sites of carbon fixation, which increases rates of Rubisco carboxylation and decreases photorespiration (Long et al. 2004). Importantly, this stimulation in photosynthesis occurred despite an overall reduction in photosynthetic capacity (Vcmax), leaf N content and stomatal conductance, and an increase in LMA. In E. camaldulensis, we found that eCO2-induced increases in LMA were due to increased leaf thickness and increased foliar concentrations of non-structural carbohydrates, consistent with eCO2 responses in other tree seedlings (Tjoelker, Oleksyn & Reich 1998; Smith et al. 2012; Duan et al. 2013). However, there was no evidence to suggest these changes in leaf structure and carbohydrate levels inhibited the stimulation of photosynthesis in E. camaldulensis in eCO2. Similar findings have been reported in other fast-growing species (Davey et al. 2006), including eucalypts (Crous et al. 2013), and may indicate that E. camaldulensis maintains, at least initially, high carbon sink demand in response to growth in eCO2.
Averaged across genotypes, we found little difference in VD between CO2 treatments, suggesting leaf hydraulics do not acclimate to growth in eCO2 in E. camaldulensis. These findings do not support expectations that VD would be reduced in eCO2 in accordance with reductions in stomatal conductance and hydraulic demand. It is possible that the relatively short duration of the experiment (3 months) did not allow sufficient time for leaf structural traits related to the venation. They are consistent, however, with previous studies reporting a lack of response in VD (Uhl & Mosbrugger 1999) and leaf hydraulic capacity (Locke et al. 2013) in response to eCO2. Importantly, our results indicate that hydraulic capacity did not inhibit increased photosynthesis in this species in eCO2. Stomatal size and density were also unaffected by eCO2. While this lack of response in stomatal traits in E. camaldulensis is in contrast to the response in many woody species in variable CO2 (Woodward & Kelly 1995), it is consistent with a recent study in a closely related species of Melaleuca that showed a lack of response in stomatal traits to historical changes in atmospheric CO2 (Hill, Hill & Watling 2015). It could be hypothesized that the overall lack of eCO2 responsiveness in leaf venation and stomatal traits may have been due to the relatively short duration of the experiment (3 months). However, other studies have clearly shown that hydraulic traits can respond to changes in CO2 (Phillips et al. 2011) and light conditions (Carins Murphy, Jordan & Brodribb 2012) within a similar time frame. Furthermore, because hydraulic traits were measured on recently developed canopy leaves, there was opportunity for older leaves to detect and transmit potential signals to induce an appropriate developmental response by stomata (Lake et al. 2001) and leaf veins (Sack et al. 2012) of new leaves.
Conclusion
We provide evidence that key leaf functional traits can vary independently among genotypes of a single species grown under common conditions. Such trait decoupling may allow different ecotypes or populations to produce novel combinations of adaptive traits in response to changing environmental conditions, without potential constraints of covariation with other leaf traits. Over evolutionary time, this process may underpin patterns of multiple trait dimensionalities, similar to observations across diverse sets of species (Laughlin 2014; Li et al. 2015). Nevertheless, our results suggest that elevated concentrations of atmospheric [CO2] may not act strongly in altering patterns of trait coordination already apparent under ambient conditions. We recommend that future work in this area should consider the roles of environmental (plastic) and genetic sources of variation in explaining patterns of leaf trait coordination.
Acknowledgements
We thank Danielle Creek, John Drake, Michael Loik, Sebastian Psfautch, Paul Rymer, Anita Wesolowski and many others from HIE who helped with data collection. We appreciate technical assistance in light microscopy by Liz Kabanov. We also thank Graham Farquhar, Michael Battaglia, Libby Pinkard, Tony O'Grady and Florian Bush for their useful comments on the manuscript. This study was funded by a Science Industry Endowment Fund (SIEF; project code RP04-122), and supported by the Hawkesbury Institute for the Environment (HIE), Western Sydney University. VRD acknowledges a Ramón y Cajal Fellowship (RYC-2012-10970).
Data accessibility
The data are deposited in the Dryad Digital Repository: http://dx.doi.org/10.5061/dryad.5tm76 (Blackman et al. 2016) and will be available 3 years from publication.