Tree Physiology 32, 219–231 doi:10.1093/treephys/tpr141 Research paper Temperature responses of leaf net photosynthesis: the role of component processes 1Hawkesbury Institute for the Environment, University of Western Sydney-Hawkesbury Campus, Locked Bag 1797, Penrith, NSW 2751, Australia; 2Department of Biological Sciences, Macquarie University, North Ryde, NSW 2109, Australia; *Corresponding author: ([email protected]) Received October 3, 2011; accepted December 12, 2011; published online January 25, 2012; handling Editor Jörg-Peter Schnitzler The response of photosynthesis to temperature is a central facet of plant response to climate. Such responses have been found to be highly variable among species and among studies. Understanding this variability is key when trying to predict the effects of rising global temperatures on plant productivity. There are three major factors affecting the response of leaf net photosynthesis to temperature (An –T): (i) photosynthetic biochemistry, (ii) respiration and (iii) vapour pressure deficit (D) and stomatal sensitivity to vapour pressure deficit during measurements. The overall goal of our study was to quantify the relative contribution of each of these factors in determining the response of An to temperature. We first conducted a sensitivity analysis with a coupled photosynthesis–stomatal (An –gs) model, using ranges for parameters of each factor taken from the literature, and quantified how these parameters affected the An –T response. Second, we applied the An –gs model to two example sets of field data, which had different optimum temperatures (Topt) of An, to analyse which factors were most important in causing the difference. We found that each of the three factors could have an equally large effect on Topt of An. In our comparison between two field datasets, the major cause for the difference in Topt was not the biochemical component, but rather the differences in respiratory components and in D conditions during measurements. We concluded that shifts in An –T responses are not always driven by acclimation of photosynthetic biochemistry, but can result from other factors. The D conditions during measurements and stomatal responses to D also need to be quantified if we are to better understand and predict shifts in An –T with climate. Keywords: climate warming, leaf net photosynthesis, leaf respiration, stomatal conductance, temperature response, vapour pressure deficit Introduction In order to understand how climate affects the productivity of plants, and to predict how climate warming may influence CO2 uptake, a more detailed understanding of the controls on leaf photosynthesis is needed (Woodward 1987, Cao and Woodward 1998, Kirschbaum 2004). The typical response of leaf net photosynthesis (An) to temperature (T) can be described by a peaked surface (Fitter and Hay 2002), with low photosynthesis at cool temperatures, increasing to a maximum rate at optimal temperatures and then decreasing again at very high temperatures. This peaked temperature response has been described many times in the literature for a wide range of species (Berry and Björkman 1980, Kirschbaum and Farquhar 1984, Battaglia et al. 1996, Fitter and Hay 2002). In the last decade there has been a great increase in plant and ecosystem warming experiments, many of which evaluate the response of photosynthesis to temperature (Battaglia et al. 1996, Gunderson et al. 2000, Shaw et al. 2000, Cunningham and Read 2002, Robakowski et al. 2002, Turnbull et al. 2002, Niu et al. 2006, 2008, Way and Sage 2008, © The Author 2012. This is an Open Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (http://creativecommons.org/licenses/by-nc/3.0/uk/) which permits unrestricted non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited. Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 Yan-Shih Lin1*, Belinda E. Medlyn2 and David S. Ellsworth1 220 Lin et al. Figure 1. Dependence of light-saturated net photosynthesis (An) on temperature among different species from previous studies. Solid black lines indicate a study on six bedding plants in Niu et al. (2008); dotted black lines indicate a study on Agastache urticifolia, Cineraria maritima, Petunia × hybrida and Plumbago auriculata in Niu et al. (2006); dash-dot-dashed black line indicates a study on Picea mariana in Way and Sage (2008); thin dotted black line indicates a study on Quercus rubra in Gunderson et al. (2010); dash-dot-dot-dashed black line indicates a study on Pinus cembra from Wieser et al. (2010); grey solid lines indicate a study on Eucalyptus globulus and grey dotted lines indicate a study on Eucalyptus nitens in Battaglia et al. (1996). Tree Physiology Volume 32, 2012 processes is temperature dependent (Harley et al. 1992, Leuning 2002, Medlyn et al. 2002a). The temperature dependences of these biochemical limitations have frequently been described in the form of mathematical models based on the Arrhenius equation for enzyme activity as a function of temperature (for Vc max), and a peaked function incorporating effects of enzyme deactivation and conformational changes with warming (for Jmax) (Harley et al. 1992, Medlyn et al. 2002a). The difference in temperature responses for Vc max and Jmax occurs because the thylakoid membrane complex involved in generating phosphorylated compounds for RuBP regeneration is more sensitive than the rate of carboxylation to high temperatures, due to changes in whole-chain electron transport (Sage and Kubien 2007). Differences in the An–T response among species or growth conditions are commonly attributed to differences in the temperature dependence of these biochemical processes (Walcroft et al. 1997, Hikosaka et al. 2006). Higher plants vary considerably in temperature sensitivities of Vc max and Jmax (Medlyn et al. 2002a, Kattge and Knorr 2007), which may potentially indicate adaptation in these responses. Changes in different aspects of the temperature responses of Vc max and Jmax have also been invoked to explain observed photosynthetic acclimation (June et al. 2004, Onoda et al. 2005, Hikosaka et al. 2006, Kattge and Knorr 2007). In particular, previous studies have highlighted changes in the activation energy of Vc max, the thermal optimum of Jmax and the ratio of Jmax to Vc max as parameters that can underlie acclimation to temperature (Hikosaka et al. 1999, Wilson and Baldocchi 2000, June et al. 2004, Onoda et al. 2005, Kattge and Knorr 2007). In addition to the effects of temperature on photosynthetic biochemistry, effects on respiratory and stomatal processes may also be important. Net leaf photosynthesis is given by gross photosynthesis less leaf respiration. Leaf respiration is also a temperature-dependent process, and contributes to the overall An–T response. It has been suggested that the ratio of gross photosynthesis to dark respiration is lower in warmer versus cooler conditions (Atkin and Tjoelker 2003). It has therefore been hypothesized that increases in respiration with temperature may become increasingly responsible for decreased net photosynthesis under progressively higher temperatures (Kirschbaum 1999). Hence examination of mitochondrial respiration as a component of net photosynthesis is important to consider in the overall temperature response of C3 plants. Stomatal regulation of the internal CO2 concentration (Ci) is the third key process determining the overall temperature response. The role of stomatal conductance in regulating net photosynthesis is well known (Wong et al. 1979). Stomata may respond to temperature itself (Hendrickson et al. 2004, Mott and Peak 2010), as well as the increase in vapour pressure deficit, D, that tends to accompany increasing t emperature Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 Bronson and Gower 2010, Gunderson et al. 2010, Silim et al. 2010, Wieser et al. 2010). The A n –T responses are highly variable among studies (Figure 1). This variability may be the result of both acclimation to temperature, which involves shortto long-term changes at organismal level, and adaptation to temperature, which involves evolutionary changes in different environments. However, the mechanisms underlying variability in An–T responses are not well understood, and acclimation and adaptation are therefore not easily predictable. There are three primary sets of processes that control the An–T response, namely biochemical, respiratory and stomatal processes. Much of the effort to date to understand variability in An–T responses has focused on biochemical processes. The two major biochemical processes thought to limit photosynthesis are the carboxylation of ribulose-1,5-bisphosphate (RuBP) and electron transport photochemistry for the regeneration of RuBP in the Calvin cycle (Farquhar et al. 1980). A third biochemical process, triose-phosphate utilization (TPU), can also limit photosynthesis at high internal CO2 concentrations or with chilling (Sharkey 1985, Sage and Kubien 2007). The biochemical model of C3 photosynthesis proposed by Farquhar et al. (1980) has been widely applied to describe the temperature dependence of component biochemical processes underlying leaf photosynthesis (Long 1991, Dreyer et al. 2001, Medlyn et al. 2002b, Kattge and Knorr 2007). In this photosynthesis model, leaf photosynthesis is assumed to be limited by either the maximum Rubisco carboxylation rate (Vc max) or the maximum RuBP regeneration rate (Jmax). Each of the biochemical Temperature responses of photosynthesis 221 Materials and methods Model We used a coupled photosynthesis–stomatal conductance (An–gs) model for our study. The standard biochemical model of photosynthesis (Farquhar et al. 1980) was coupled to the stomatal model proposed by Medlyn et al. (2011). In the standard biochemical model of photosynthesis, the net CO2 assimilation rate can be determined by either the Rubisco-limited photosynthesis (Ac) or the RuBP regenerationlimited photosynthesis (Aj). We modelled these limitations to photosynthesis following Medlyn et al. (2002a) and Kattge and Knorr (2007). The TPU limitation was not considered in this analysis, due to lack of parameters for the temperature response of this limitation across species. This omission is consistent with other studies of temperature acclimation of photosynthesis (e.g., Medlyn et al. 2002a, 2000b, Kattge and Knorr 2007). Also following those studies, mesophyll conductance (gm) was not explicitly included in our An–gs model. Although a role for gm in temperature acclimation has been proposed (Warren and Dreyer 2006), this component is difficult to quantify accurately from A–Ci curves alone and is best estimated with multiple independent measures of photosynthetic performance, which were not available for this study. In this study, therefore, Vc max and Jmax are ‘apparent’ values, rather than actual, and their temperature responses incorporate the temperature responses of gm. For the temperature dependence of the Michaelis–Menten coefficient of Rubisco and the CO2 compensation point in the absence of mitochondrial respiration in the Farquhar model, we used parameters proposed by Bernacchi et al. (2001) as described in Medlyn et al. (2002a). The temperature dependence of apparent Vc max and Jmax has been described previously in Medlyn et al. (2002a) and Leuning (2002). These temperature dependencies were modelled by two functions (see Medlyn et al. 2002a). The first function is the standard Arrhenius function E (T − 298) (1) f(Tk ) = k25 exp a k 298RTk where Ea is the activation energy and k25 is the apparent Vc max or Jmax value at 25 °C. R is the universal gas constant (8.314 J mol−1 K−1) and Tk is the leaf temperature in K. The activation energy term Ea describes the exponential rate of rise of enzyme activity with the increase of temperature. The second function is a modified form of the Arrhenius function, which yields a peaked function (Harley et al. 1992), and is given by E (T − 298) 1 + exp (298∆S − Hd / 298R ) f(Tk ) = k25 exp a k 1 + exp (Tk ∆S − Hd / Tk R ) 298RTk (2) where Hd is the deactivation energy and ΔS is the entropy term. Hd describes the rate of decrease of the function above the optimum. In this study, the Arrhenius and peaked functions were used to model the temperature dependence of apparent Vc max and Jmax, respectively. In order to reduce the number of parameters Tree Physiology Online at http://www.treephys.oxfordjournals.org Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 (Sage and Sharkey 1987, Leuning 1995, Day 2000). Stomatal regulation can affect the An –T response in two major ways. First, stomatal aperture depends on the value of D during measurements. In some experiments, for example those using controlled systems (such as growth chambers), D may be held constant. In other experiments, particularly field experiments, such control over D may not be possible, resulting in increasing D with T. Additionally, D is determined by water vapour content of the air, which can vary significantly among seasons and environments. In warm environments or in summer, the water vapour content of the air tends to be higher than in cool environments or in winter, giving a higher dewpoint and, for a given T, a lower D. The difference in D at a given T will change An –T response through its effect on stomatal conductance. There is considerable variation among woody plant species in sensitivity to D, and some studies suggest that this sensitivity may be dependent on growth temperature (Lloyd and Farquhar 1994, Medlyn et al. 2011). As such, there may also be acclimation of stomatal sensitivity to D that affects the An –T response measured in different seasons. Both aspects—stomatal sensitivity to D and stomatal acclimation to D—can contribute to the role of stomatal regulation in the overall A n –T response. Thus, there are a set of processes that can contribute to the overall temperature response of photosynthesis. In this study, we aimed to quantify the relative roles of photosynthetic biochemistry, stomatal control and respiration in determining the response of leaf net photosynthesis to temperature, using a coupled photosynthesis–stomatal (An–gs) model. Firstly, we carried out a comprehensive sensitivity analysis. We identified the range of each relevant parameter value from the literature and used this parameter range to quantify the relative sensitivity of the optimum temperature (Topt) of An to each process. Second, we applied the coupled An–gs model to photosynthetic data from two species measured in field experiments to identify the mechanistic causes underpinning differences in the temperature response of An. The two datasets came from a eucalypt species growing in NSW, Australia, and a pine species growing in North Carolina, USA. The An–T response differed between the two species. The model was applied in a stepwise fashion to identify which processes contributed most to the differences in observed temperature response between the species. 222 Lin et al. in the model to avoid over-parameterization, the deactivation energy (Hd) of Jmax was assumed as a constant of 200 kJ mol−1 for the model fitting (Medlyn et al. 2002a). The day respiration rate (Rd) in the model is calculated using a standardized rate of respiration at 25 °C (Rd25) and a temperature response equation based on the Q10 coefficient (Ryan 1991, Aber and Federer 1992, Melillo et al. 1993, Schimel et al. 1997, Cramer et al. 1999) given by Rd = R25Q10(T −25)/10 (3) g A gs = g0 + 1 + 1 n (4) D Ca where g0 and g1 are model coefficients. This model is similar in form to the widely used empirical models of Ball et al. (1987) and Leuning (1995), but is based on the theory of optimal stomatal behaviour (Cowan and Farquhar 1977, Hari et al. 1987), so that parameter values are interpretable. Medlyn et al. (2011) found that the intercept parameter, g0, was not significantly different from zero or was very close to zero across various tree species; thus we assumed that g0 = 0 in our model. The slope parameter, g1, is related to the marginal water cost of carbon to the plant. It is also predicted to increase with growth temperature (Medlyn et al. 2011). The simultaneous solution for photosynthesis and stomatal models proposed by Leuning (1990) was adapted for use in this study. Sensitivity analysis to component processes We conducted a sensitivity analysis in order to evaluate how each temperature-dependent parameter contributes to the overall temperature dependence of net photosynthesis rate, based on the coupled An–gs model described above. We simulated the An–T response curve for leaf temperature from 10 to 45 °C. For our baseline, we used biochemical and stomatal parameters of Eucalyptus crebra (see below), and held D constant at 1 kPa. We then varied parameters from biochemical, respiratory and stomatal components one at a time, and examined the resulting change in the An–T response curve. For each parameter, the range of values was taken from previous Tree Physiology Volume 32, 2012 Field data We further investigated the contribution of different processes in determining An–T responses by applying the coupled model to two different sets of temperature response data obtained from field-grown evergreen trees. We used published data from Pinus taeda L. in the Blackwood Division of Duke Forest (Orange County, NC, USA; 35 °58′N, 79 °5′W) (Crous and Ellsworth 2004) and unpublished data from Eucalyptus crebra F. Muell. in the Hawkesbury Forest Experiment (HFE) Eucalyptus common garden site (Richmond, NSW, Australia; 33 °36′S, 150 °44′E). The Blackwood Division of Duke Forest is located in a warm and humid climatic area with a mean daily maximum temperature of 31.5 °C in the hottest month and a mean daily minimum temperature of −3.5 °C in the coldest month. The common garden site is located in a sub-humid temperate climate with a mean daily maximum temperature of 29 °C in the hottest month and a mean daily minimum temperature of 3 °C in the coldest month. The long-term mean annual rainfall is 1118 and 801 mm for Blackwood Division of Duke Forest and HFE common garden, respectively. In each of these studies, the response of photosynthetic biochemistry to temperature was quantified by measuring An–Ci responses at a range of temperatures. Field measurements of the response of An to step changes in Ca were made using the LI-6400 portable photosynthesis system (LI-COR, Inc., Lincoln, NE, USA). The light source was set to 1800 µmol m−2 s−1 with the LI-COR LED light source for both E. crebra and P. taeda, thus allowing us to measure the potential maximum rate of An as a function of different Ca levels at light saturation. In both cases, measurements were begun at ambient Ca and then progressed through a series of stepwise changes in Ca to superambient, saturating Ca. The An–Ci responses were measured on P. taeda needles in the upper canopy in December 2000 (i.e. midwinter) at four different temperature levels (10, 20, 28 Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 Here Q10 denotes the factor by which Rd increases for every 10 °C rise in the temperature T (°C), noting that the temperature response of Rd may not necessarily be equivalent to that of Rdark (Atkin et al. 2000). The photosynthesis model was coupled to the stomatal model proposed by Medlyn et al. (2011). In this model, stomatal conductance is a function of net photosynthesis rate (An), external air CO2 concentration (Ca) and leaf-air vapour pressure deficit (D), derived as (Medlyn et al. 2011) literature reviews (Table 1). Only values for woody plant species were used. The relative contribution of biochemical component processes was evaluated by altering Ea, Ha, ΔS and the ratio of Jmax:Vcmax (J/V) at 25 °C over the ranges found in the review by Kattge and Knorr (2007). For the respiratory component, the relative contribution was evaluated by altering the day respiration rate at 25 °C (Rd25) over the range reported by Reich et al. (1998), and the Q10 values over the range reported by Tjoelker et al. (2001) (Table 1). For the stomatal component, g1 was evaluated over the range of stomatal coefficients obtained for woody species by Medlyn et al. (2011). Several alternative scenarios were developed for measurement D. In two scenarios, D was held constant, as might occur if D was controlled during measurements. The values of D selected were 1 and 2.5 kPa. In two further scenarios, the dewpoint was held constant (dewpoint at 8 and 24 °C), as might occur if T was increased without attempting to control D. Temperature responses of photosynthesis 223 Table 1. Parameter values used in sensitivity analysis. References for the parameter values are as follows: 1: Kattge and Knorr (2007); 2: Reich et al. (1998); 3: Tjoelker et al. (2001); 4: Medlyn et al. (2011). The modelled range in values of Topt corresponding to the range in parameter values is shown in the final column. The abbreviations are denoted as follows: Vc max: maximum Rubisco carboxylation rate; Ea: activation energy for Vc max; Jmax: maximum RuBP regeneration rate; Ha: activation energy for Jmax; ΔS: entropy term; J/V: ratio of Jmax to Vc max; Rd25: leaf day respiration rate at 25 °C; Q10: factor by which the leaf day respiration rate increases for every 10° rise in the temperature; g1: stomatal model coefficient (Medlyn et al. 2011); D: leaf to air vapour pressure deficit. Range of values Ea 51.3 109.3 31.2 kJ mol−1 78 0.626 kJ mol−1 K−1 0.656 1.46 Unitless 2.72 0.4 μmol m−2 s−1 3.7 1.3 Unitless 2.98 3 Unitless 13.1 Constant D = 1 kPa Constant D = 2.5 kPa Constant dewpoint at 8 °C Constant dewpoint at 24 °C5 kJ mol−1 Ha ΔS J/V2 Rd25 Q103 g1 D 1Out Unit Reference 1 Topt (°C) Ac–Rd Aj –Rd An 21.1 27.6 27.6 27.6 34.6 27.6 21.2 36.8 32.8 30.3 26.1 29.8 25.7 25.9 29.8 27.64 25.3 22.3 24.1 21.1 28.4 26.3 26.3 26.3 26.3 26.3 26.3 29.3 24.9 28.6 24.8 24.4 29.2 26.34 23.8 19.9 24.1 1 1 1 1 2 3 4 Change in Topt of An (°C) 26.3 26.3 26.3 26.3 26.3 26.3 29.3 24.9 28.6 24.8 24.4 29.2 26.34 23.8 19.9 24.1 7.3 0 0 0 4.4 3.8 4.8 2.5 5.4 2.2 of the simulated temperature range. 2V c max held constant. 3Based on the temperature range from 20–30 °C. Topt for the sensitivity analysis. 5Simulated temperature range: 24.1–45 °C. 4Baseline and 35 °C). Measurements on E. crebra leaves were made at three temperature levels (15, 25 and 32 °C) in late August 2008 (i.e., late winter). In all cases, leaves were enclosed in the leaf cuvette at the target temperature and ambient Ca level for at least 30 min before An–Ci curve measurements were conducted, and then allowed to equilibrate for another 30 min at the new temperature prior to the next set of An–Ci curve measurements. The order of temperatures used was either progressive (for E. crebra) or random (P. taeda). In addition to the An–Ci curve measurements, two independent sets of temperature responses of light-saturated net photosynthetic rate data were used to test the modelling results. These measurements were made at saturated light and ambient atmospheric CO2 concentration. The light-saturated net photosynthetic rate responses to changes in temperature were measured on P. taeda from the Blackwood Division of Duke Forest (Orange County, NC, USA) at a range of seasonal temperatures in December 1996 and 1997 as described in Ellsworth (2000). A similar set of measurements was made on E. crebra at the HFE Eucalyptus common garden site (Richmond, NSW, Australia) at seven temperature levels (15, 20, 25, 30, 35, 40 and 45 °C) in August 2009. Model application to data The model was parameterized as follows. For E. crebra, the photosynthetic parameters, apparent Vc max and Jmax, at different temperatures were fitted to each An–Ci curve using leastsquares linear regression as described in Wullschleger (1993) and Ellsworth (2000), respectively. The parameters for temperature responses of apparent Vc max and Jmax were then fitted in SigmaPlot (v. 11.0, Systat Software Inc., Chicago, IL, USA) based on Eqs. (1) and (2), respectively. For P. taeda, published parameters for the temperature responses of apparent Vc max and Jmax, obtained from the An–Ci data described above, were used (Medlyn et al. 2002a). To characterize the day respiration rate of two species, the rate of respiration at 25 °C (Rd25) was fitted from 2008 An–Ci curves dataset for E. crebra, and taken from Hamilton et al. (2001) for P. taeda. Since there is no study directly quantifying the respiration Q10 value for E. crebra, we assumed the value as 2, which is widely used in modelling the respiration responses of temperature from leaf to ecosystem scales (Ryan 1991, Aber and Federer 1992, Melillo et al. 1993, Cox et al. 2000, Radtke and Robinson 2006, Atkin et al. 2008). For the stomatal model, parameters for E. crebra were obtained by fitting Eq. (4) to the 2009 An–T dataset described above. Tree Physiology Online at http://www.treephys.oxfordjournals.org Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 Parameter 224 Lin et al. Biochemical components: Ea, Ha, ΔS and J/V We first considered the effect of parameters describing temperature effects on the biochemical limitations to photosynthesis, Respiratory components: Rd25 and Q10 An increase in Rd25 from 0.4 to 3.7 µmol m−2 s−1, and an increase in Q10 from 1.3 to 2.98 µmol m−2 s−1, both reduce Topt Results Sensitivity analysis to component processes Table 2. Parameter values used in field data analysis. Species are denoted as follows: EC, Eucalyptus crebra; PT, Pinus taeda. Standard deviations are given for completeness but are not used in the analysis. Topt of An was fitted for field data using a quadratic equation. Biochemical components Vc max EC PT Ea (SD) kJ mol−1 62.99 (2.97) 60.88 (1.92) Jmax Vc max25 (SD) μmol m−2 s−1 87.68 (3.28) 57.05 (9.33) References Ha (SD) kJ mol−1 31.19 (3.02) 37.87 (19.86) Respiration components Rd25 μmol m−2 s−1 Q10 μmol m−2 s−1 References EC PT −2.47 −0.54 2 2.71 This study Hamilton et al. (2001) EC PT Vapour pressure deficit D kPa D = 0.378 × exp(0.0702 × T) D = 0.245 × exp(0.0706 × T) Tree Physiology Volume 32, 2012 Fitted from field data Fitted from field data Jmax25 (SD) μmol m−2 s−1 170.83 (3.23) 98.5 (3.75) ΔS kJ mol−1 K−1 0.626 0.630 Stomatal components g0 mol m−2 s−1 g1 Unitless References 0 0 4.3 4.8 This study Medlyn et al. (2011) Fitted Topt of An From field data °C 16.2 24.5 This study Medlyn et al. (2002a, 2002b) Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 To assess the relative contribution of biochemical components, respiratory components and stomatal components to both optimal temperature (Topt) and optimum rate of An, one main parameter at a time was changed, using the published data range across woody plant species. The results are shown in Figure 2. The effect on Topt is shown in Table 1. namely Ea, Ha and ΔS, and the ratio between the two major biochemical limitations, which is characterized by the ratio of Jmax to Vc max at 25 °C. Figure 2a–d shows the effects of changes in each of these parameters on the temperature response of An. An increase in the activation energy of Rubisco, Ea, from 51.3 to 109.3 kJ mol−1 had a large effect on the temperature response, increasing both Topt, from 21.1 to 28.4 °C (Table 1), and the maximum rate of An, by 19%. On the other hand, changes in the parameters describing the temperature dependence of RuBP regeneration, Ha and ΔS from 31.2 to 78.0 kJ mol−1 and from 0.626 to 0.656 kJ mol−1 K−1, respectively, did not alter either Topt or the maximum rate of An. A higher Ha, however, resulted in a lower initial rate of An at lower temperature (<20 °C), and a higher ΔS caused a reduction in An at higher temperature (>30 °C). It is worth noting that whether altering Ea or Ha would change Topt depends on which process is limiting at optimal temperature. The limiting process depends on the ratio of apparent Jmax to Vc max (J/V). Since the baseline An–T curve in our sensitivity analysis is Ac-limited, it is not surprising that modifying Ea causes a change in Topt whereas modifying Ha or ΔS does not. An increase in the J/V ratio from 1.42 to 2.72 reduces the temperature at which the change in biochemical limitation occurs (i.e., from Ac to Aj), from 26.4 to <10 °C. However, such a change in the J/V ratio does not affect either Topt or the maximum rate of An when other parameters are held constant (Table 1). Parameters for P. taeda were taken from Medlyn et al. (2011), who fitted Eq. (4) to a large dataset of stomatal conductance measurements made at the Duke Forest site. In this analysis, we first simulated the An–T curve for each species based on these parameterizations, for temperatures ranging from 10 to 45 °C. The model was driven by measured values of D at each temperature. Then, individual sets of parameters (biochemical, respiratory and stomatal parameters, and measurement D values) were changed from one species value to the other species value, one set of parameters at a time, to evaluate the relative contribution of each component to the overall temperature dependence of An (Table 2). Our goal in this analysis was to identify the key process(es) causing the differences in temperature response between the two species. Temperature responses of photosynthesis 225 significantly. The change in Rd25 has the largest effect on Topt, causing a decrease from 29.3 to 24.9 °C, while the change in Q10 causes a reduction in Topt from 28.6 to 24.8 °C (Table 2). However, the major effect of higher Rd25 or Q10 on the temperature response is a large reduction in An at higher temperature (>35 °C) (Figure 2e and f). Stomatal components: g1 and D The stomatal parameter g1 also has a large effect on the temperature response curve. An increase in g1 from 3.0 to 13.1 caused an increase in Topt from 24.4 to 29.2 °C, and the maximum rate of An increased from 14.8 to 22.7 µmol m−2 s−1. In contrast, increasing D tends to lower both Topt and the maximum rate of An. Consequently, assuming a temperaturedependent D in the model analysis markedly lowers Topt of An compared with the Topt when D is held constant. The Topt of An when D is held constant at 1 or 2.5 kPa is 26.3 and 23.8 °C, respectively. In contrast, if D is assumed to vary with T, with a dewpoint at 8 or 24 °C, Topt is reduced to 19.9 or 24.1 °C, respectively. Tree Physiology Online at http://www.treephys.oxfordjournals.org Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 Figure 2. Simulated temperature dependency of light-saturated leaf photosynthesis (An) under different ranges of (i) biochemical components: Ea, Ha, J/V, ΔS (a, b, c, d); (ii) respiration components: Rd25, Q10 (e, f); (iii) stomatal components: g1 (g); and (iv) vapour pressure deficit: D (h). Parameter ranges for sensitivity analysis are given in the figure and were chosen based on previous studies on woody plant species (Reich et al. 1998, Kattge and Knorr 2007, Medlyn et al. 2011). Photosynthetic and stomatal parameters for the model simulation baseline are given in Table 2 (for E. crebra) with constant D = 1 kPa. Black lines denote the limited processes for An, and grey lines denote the non-limited processes for An. 226 Lin et al. Overall, each of the component processes was equally important to the shift of Topt of An. While varying respiratory components (Rd25 and Q10) changed Topt of An to around 3.8– 4.4 °C in the sensitivity analysis, varying D and Ea altered Topt of An up to 6.4 and 7.3 °C, respectively (Table 1). Field data example Tree Physiology Volume 32, 2012 Figure 3. Dependence of light-saturated net photosynthesis (An) on temperature, according to model simulations and field data. Relationships are shown for Eucalyptus crebra (a) and Pinus taeda (b). Solid lines indicate the model results derived from photosynthetic, stomatal and vapour pressure deficit parameters for each species given in Table 2. Open circles and triangles indicate field data. Other lines indicate simulation results when one set of component parameters is changed to that for the other species (red: vapour pressure deficit; green: biochemical parameters; yellow: respiratory parameters; blue: stomatal conductance parameter). 1.3 °C increase for E. crebra and a 2.2 °C reduction for P. taeda. However, the parameters for the biochemical component for the two datasets were very similar, so there was virtually no difference in An–T responses when swapping the biochemical component. Discussion Photosynthetic responses to temperature are central to plant carbon balance, particularly in different climates or under different thermal regimes. However, An –T responses are very variable among studies (Leuning 2002, Medlyn et al. 2002a, Katul et al. 2003, Kattge and Knorr 2007) and among species (Figure 1). Understanding and quantifying this variability is crucial when trying to predict the effects of rising global temperatures on plant productivity. However, as yet, we have a poor quantitative understanding of the mechanisms causing this variability (Dreyer et al. 2001, Medlyn et al. 2002a, Hikosaka et al. 2007). There has been some progress made in understanding how the biochemical component of photosynthesis acclimates to growth temperature (Medlyn et al. 2002a; Hikosaka et al. 2006; Kattge and Knorr 2007). Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 We now examine an example comparison between two sets of field data for E. crebra and P. taeda. Responses of An to temperature were measured in field conditions and are shown in Figure 3. The Topt of An was estimated from these data by quadratic fitting and differed considerably between the species: values obtained were 16.2 and 24.5 °C for E. crebra and P. taeda, respectively. As shown in Table 2, there were several differences between the species that could have contributed to the difference in Topt. There were small differences in the parameters for the biochemical (Ea, Ha and ΔS) and stomatal components (g1). There was a large difference in the respiratory component: E. crebra had nearly five times higher Rd25 than P. taeda. In addition, the measurement D differed between the experiments. Both were field datasets in which D was not well controlled: the dewpoint was approximately constant and D increased with warming temperature. The dewpoints of the two datasets were approximately 8 and 16 °C for E. crebra and P. taeda, respectively (Table 2). This difference in dewpoint resulted in a higher D of approximately 0.75 kPa across the temperature range for E. crebra. We applied the An–gs model to these two datasets to analyse why Topt differed, and to quantify the role of each of the different components. First, the Topt of An was 20.9 and 23.2 °C according to simulated An–T curves for E. crebra and P. taeda, respectively (Table 3; Figure 3). Simulated Topt values were thus lower for E. crebra, as were measured Topt values. For both E. crebra and P. taeda, we changed each parameter, one set at a time, to the value for the other species and observed the effect on simulated Topt (Table 3, Figure 3). This sensitivity analysis shows that the difference in the respiration rate between the two species was the most important factor contributing to the difference in An–T response between the two species. Changing the respiration rate changed Topt of An by 1.9 °C lower and 1.1 °C higher for P. taeda and E. crebra, respectively. This result is not surprising, since Rd25 for E. crebra is nearly five times higher than that for P. taeda. The relative contributions of g1 and D were also important in An–T responses, despite the fact that there are only relatively small differences in the two parameters. The small change in g1 from 4.3 to 4.8 changed Topt of An by 0.7 °C, from 20.9 to 21.6 °C in E. crebra and from 23.2 to 22.5 °C in P. taeda. Swapping the different D conditions between the two datasets also resulted in a large shift in Topt of An, for both species—a Temperature responses of photosynthesis 227 Table 3. Sensitivity analysis of the response of An and its components for two sets of field data. For both E. crebra and P. taeda, each parameter was changed, one set at a time, to the value for the other species (Table 2), and the effect on simulated Topt was observed. Species Simulated from the An –gs model Sensitivity analysis Topt Changed parameters Ac (°C) Aj (°C) An (°C) EC 22.6 25.0 20.9 PT 24.1 29.8 23.2 However, as demonstrated in our study, there are three major components affecting the A n –T response, each of which may significantly affect the An –T response (Tables 1 and 2; Figures 2 and 3). Thus we need to understand and quantify the role of each of these components to be able to predict A n –T responses. Vapour pressure deficit (D) A key point demonstrated in our sensitivity analysis is that differences in measurement D alone can change the Topt (Table 1; Figure 2h), without any acclimation of plant function. As measurement D increases, stomata close, causing a reduction in Ci, which results in a decrease in temperature optimum (Sage and Kubien 2007). This effect of measurement D has important implications for the interpretation of shifts in A n –T responses. For example, in warmer climates or warmer seasons, dewpoint is generally higher, meaning that at a given temperature, D is lower. Many examples of changes in Topt with season or climate may be at least partially due to this shift in dewpoint and associated D, rather than any acclimation to growth temperature. For example, Baldocchi et al. (2001) found that the temperature optimum for canopy CO2 uptake increases with mean summer temperature (their Figure 9), and interpreted this change as an adaptive response to climate. However, increasing dewpoint with increasing summer temperature could also explain this response. Similarly, shifts in Topt observed in warming experiments do not necessarily indicate plant acclimation to temperature. The effect of changes in D on temperature optima needs to be first quantified and factored out, before it can be concluded that acclimation has occurred. Different experiments take different approaches to the control of D. In some studies D is fully controlled and may be held constant (e.g., using a climate chamber to achieve the desired ambient air condition) (Dreyer et al. 2001, Cunningham and Read 2006), but such studies typically Ac (°C) Aj (°C) An (°C) 21.9 22.6 23.4 24.1 24.9 24.1 23.4 21.8 26.8 25.0 25.9 26.6 28.3 29.8 29.1 28.1 20.2 22.0 21.6 22.2 23.9 21.3 22.5 21.0 Change in Topt of An (°C) −0.7 +1.1 +0.7 +1.3 +0.7 −1.9 −0.7 −2.2 only allow small plants to be studied, and often do not track realistic diel or seasonal temperature variations. In other studies, temperature is manipulated while holding air water vapour content constant, which is effectively the same as holding dewpoint constant. As shown in Figure 2h, these two approaches would result in markedly different values for Topt of An. Thus, values of Topt from these two types of study cannot easily be directly compared. Current climate change scenarios suggest that relative humidity is likely to remain constant in future (CSIRO 2007, Amthor et al. 2010), which would result in a different D–T relationship from either of these two types of study. To predict Topt under such conditions, we either need experiments that attempt to maintain relative humidity constant, or else we need to quantify responses to T and D separately so that these can be combined to make predictions for a range of possible future conditions. The latter approach is clearly more flexible. It is very difficult to control D with experimental warming especially in the field, particularly under a wide range of desired temperatures. Nevertheless, it is crucial to know the D–T relationship in a given set of measurements if we are to be able to correctly interpret measured photosynthetic responses to temperature. Unfortunately, many warming experiments fail to adequately monitor or report D (Saxe et al. 2001, Aronson and McNulty 2009). If warming experiments are to inform models of plant temperature responses, D must be routinely monitored and reported. Sensitivity of stomatal conductance to D Stomatal conductance, through its control of intercellular CO2 concentration (Ci), is clearly a key element mediating the overall temperature response of An (Katul et al. 2000). It appears that gs is more sensitive to the change of D with rising temperature than to temperature itself, because the Ci:Ca ratio tends to remain constant if D is held constant independent of temperature (von Caemmerer and Farquhar 1981, Ehleringer Tree Physiology Online at http://www.treephys.oxfordjournals.org Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 Ea, Ha, ΔS Rd25, Q10 g1 D Ea, Ha, ΔS Rd25, Q10 g1 D Topt 228 Lin et al. Respiratory processes Day respiration rate (Rd) is generally a small fraction of An, and therefore at most physiological temperatures it would not be an important control over net photosynthesis. However, in the case of species with low photosynthetic rate, such as spruce species, much of the differences in An–T responses can be attributed to changes in Rd (Way and Sage 2008). In addition, certain conditions could be expected to increase the ratio of Rd to An and therefore increase the importance of the temperature response of Rd. The temperature response of day respiration rate (Rd) is commonly described by a temperature coefficient model (Q10; Eq. (3)) with a constant Q10 value of 2.0 to estimate the t emperature-dependent Rd (Ryan 1991, Aber and Federer 1992, Melillo et al. 1993, Schimel et al. 1997, Cramer et al. 1999). However, long-term (weeks to months) temperature acclimation of Rd reported by previous studies (Atkin et al. 2000, Tjoelker et al. 2001, Ow et al. 2008, Tjoelker et al. 2009) suggests that a temperature-dependent Q10 value might better estimate the Rd at higher temperature. Despite potentially overestimating Rd at higher temperature by using a constant Q10 value in our study, our results demonstrated that the offset contribution of Rd to An, Tree Physiology Volume 32, 2012 as well as to Topt of An are equally important compared with other process components considered in the study (Table 1; Figure 2e and f). Thus the role of respiratory component should also be stressed when analysing An–T responses. Biochemical processes The key biochemical component processes of photosynthesis are (i) carboxylation of RuBP, characterized by the maximum Rubisco activity Vc max, and (ii) electron transport and RuBP regeneration, characterized by the maximum electron transport rate Jmax. Some progress has been made in quantifying temperature acclimation and adaptation of these processes. In most species, the dependence of apparent Vc max on temperature can be described by an Arrhenius function, because it increases near-exponentially over a wide range of temperatures and does not deactivate until very high, near-lethal temperatures (>50 °C; Eq. (2)) (Leuning 2002, Medlyn et al., 2002a, Salvucci and Crafts-Brandner 2004). Previous studies suggest that the activation energy (Ea) of apparent Vc max increases with growth temperature (Medlyn et al. 2002a, Hikosaka et al. 2006, Hikosaka et al. 2007, Kattge and Knorr 2007). This change in Ea with growth temperature has been ascribed to changes in the mesophyll CO2 conductance gm (Makino et al. 1994, Law and Crafts-Brandner 1999, Bernacchi et al. 2002, Salvucci and Crafts-Brandner 2004, Warren and Dreyer 2006). The increase of Ea for apparent Vc max is likely to result in the increase of Topt of An in some species, as shown in the sensitivity analysis (Figure 2a). Hikosaka et al. (2006) suggests an increase in Topt by 0.54 °C per 1 kJ mol−1 increase in Ea for Plantago asiatica; however, we found a much smaller fraction increase in Topt in tree species (0.13 °C per 1 kJ mol−1 increase in Ea) based on our An –gs model (Figure 2a). Different Ha or J/V might change the temperature at which the limiting step shifting occurred. Aj may be the limiting step for leaf photosynthesis under certain conditions, such as under elevated CO2 or measuring at temperature lower than growth temperature (Sage 1990, Onoda et al. 2005, Hikosaka et al. 2006). However, this does not change the Topt of An nor the optimum rate of An (Figure 2b–d). Given that Aj is limiting at much higher Ci in plants (Kirschbaum and Farquhar 1984) and that Aj-limited photosynthesis may occur at temperatures lower than Topt of An (Onoda et al. 2005), Ac may often be the limiting step for light-saturated An at Topt at ambient CO2 (Figure 2a–d). Conclusions Using a coupled photosynthesis–stomatal conductance model, we investigated the role of the three key components involved in determining the temperature responses of photosynthesis: photosynthetic biochemistry, respiration and stomatal sensitivity to D. We found that each of the three processes was quantitatively important, suggesting that each needs to be quantified Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 and Cerling 1995, Leuning 1995). However, stomatal conductance may also acclimate to changes in growth temperature. While previous studies have discussed the mechanisms involved in temperature acclimation of the photosynthetic biochemistry (Medlyn et al. 2002a, Hikosaka et al. 2006, Kattge and Knorr 2007), very little attention has been paid to the question of whether stomatal conductance also acclimates to environmental conditions. As shown in Figure 2g, changes in the stomatal conductance–photosynthesis relationship (g1 parameter) can have a major impact on the An–T relationship. We found that a small difference in this parameter between Pinus taeda and Eucalyptus crebra could have caused a 0.7 °C difference in Topt (Table 3). There are theoretical reasons for expecting acclimation in g1 in response to temperature (Medlyn et al. 2011). The very limited amount of data available thus far suggests that acclimation of the stomatal sensitivity to D may occur. For example, Lloyd and Farquhar (1994) found that, at a given D, the Ci:Ca ratio was lower in cool environments than in warm temperate environments. Consistent with this observation, Medlyn et al. (2011) observed that the g1 parameter appeared to increase with growth temperature. Leuning (1990) also reported an increase in the slope of the Ball–Berry stomatal conductance– photosynthesis relationship between spring and summer in field-grown Eucalyptus grandis. These observed changes all act in the direction of causing higher optimal temperatures for photosynthesis. Further experimental studies are needed to investigate whether acclimation of stomatal conductance and the Ci:Ca ratio occurs, and to what extent such acclimation can explain changes in the Topt of An. Temperature responses of photosynthesis 229 Funding We acknowledge funding by the Australian Government’s Department of Climate Change and the Department of Agriculture, Fisheries and Forestry for the Hawkesbury Forest Experiment. The senior author was partially supported by a UWS International Postgraduate Research Scholarship with UWS International Award (UWSIPRS/UWSIA) and a National Climate Change Adaptation Research Facility (NCCARF-PIARN) scholarship from The Primary Industries Adaptation Research Network. References Aber, J.D. and C.A. Federer. 1992. A generalized, lumped-parameter model of photosynthesis, evapotranspiration and net primary production in temperate and boreal forest ecosystems. Oecologia 92:463–474. Amthor, J.S., P.J. Hanson, R.J. Norby and S.D. Wullschleger. 2010. A comment on ‘Appropriate experimental ecosystem warming methods by ecosystem, objective, and practicality’ by Aronson and McNulty. Agric. For. Meteorol. 150:497–498. Aronson, E.L. and S.G. McNulty. 2009. Appropriate experimental ecosystem warming methods by ecosystem, objective, and practicality. Agric. For. Meteorol. 149:1791–1799. Atkin, O.K. and M.G. Tjoelker. 2003. Thermal acclimation and the dynamic response of plant respiration to temperature. Trends Plant Sci. 8:343–351. Atkin, O.K., C. Holly and M.C. Ball. 2000. Acclimation of snow gum (Eucalyptus pauciflora) leaf respiration to seasonal and diurnal variations in temperature: the importance of changes in the capacity and temperature sensitivity of respiration. Plant, Cell Environ. 23:15–26. Atkin, O.K., L.J. Atkinson, R.A. Fisher, C.D. Campbell, J. ZaragozaCastells, J.W. Pitchford, F.I. Woodward and V. Hurry. 2008. Using temperature-dependent changes in leaf scaling relationships to quantitatively account for thermal acclimation of respiration in a coupled global climate–vegetation model. Glob. Change Biol. 14:2709–2726. Baldocchi, D., E. Falge, L. Gu, R. et al. 2001. FLUXNET: a new tool to study the temporal and spatial variability of ecosystem-scale carbon dioxide, water vapor, and energy flux densities. Bull. Am. Meteorol. Soc. 82:2415–2434. Ball, J., I.E. Woodrow and J. Berry. 1987. A model predicting stomatal conductance and its contribution to the control of photosynthesis under different environmental conditions. Prog. Photosyn. 4:221–224. Battaglia, M., C. Beadle and S. Loughhead. 1996. Photosynthetic temperature responses of Eucalyptus globulus and Eucalyptus nitens. Tree Physiol. 16:81–89. Bernacchi, C.J., E.L. Singsaas, C. Pimentel, A.R. Portis Jr and S.P. Long. 2001. Improved temperature response functions for models of Rubisco-limited photosynthesis. Plant, Cell Environ. 24:253–259. Bernacchi, C.J., A.R. Portis, H. Nakano, S. Von Caemmerer and S.P. Long. 2002. Temperature response of mesophyll conductance. Implications for the determination of Rubisco enzyme kinetics and for limitations to photosynthesis in vivo. Plant Physiol. 130:1992–1998. Berry, J. and O. Björkman. 1980. Photosynthetic response and adaption to temperature in higher plant. Annu. Rev. Plant Physiol. 31:491–543. Bronson, D.R. and S.T. Gower. 2010. Ecosystem warming does not affect photosynthesis or aboveground autotrophic respiration for boreal black spruce. Tree Physiol. 30:441–449. Cao, M. and F.I. Woodward. 1998. Net primary and ecosystem production and carbon stocks of terrestrial ecosystems and their responses to climate change. Glob. Change Biol. 4:185–198. Cowan, I.R. and G.D. Farquhar. 1977. Stomatal function in relation to leaf metabolism and environment. Symp. Soc. Exp. Biol. 31:471–505. Cox, P.M., R.A. Betts, C.D. Jones, S.A. Spall and I.J. Totterdell. 2000. Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model. Nature 408:184–187. Cramer, W., D.W. Kicklighter, A. Bondeau, B. Moore II, G. Churkina, B. Nemry, A. Ruimy and A.L. Schloss. 1999. Comparing global models of terrestrial net primary productivity (NPP): overview and key results. Glob. Change Biol. 5:1–15. Crous, K.Y. and D.S. Ellsworth. 2004. Canopy position affects photosynthetic adjustments to long-term elevated CO2 concentration (FACE) in aging needles in a mature Pinus taeda forest. Tree Physiol. 24:961–970. CSIRO. 2007. Climate change in Australia: technical report 2007. Canberra, Australia, 148 p. Cunningham, S.C. and J. Read. 2002. Comparison of temperate and tropical rainforest tree species: photosynthetic responses to growth temperature. Oecologia 133:112–119. Cunningham, S.C. and J. Read. 2006. Foliar temperature tolerance of temperate and tropical evergreen rain forest trees of Australia. Tree Physiol. 26:1435–1443. Day, M.E. 2000. Influence of temperature and leaf-to-air vapor pressure deficit on net photosynthesis and stomatal conductance in red spruce (Picea rubens). Tree Physiol. 20:57–63. Dreyer, E., X. Le Roux, P. Montpied, F.A. Daudet and F. Masson. 2001. Temperature response of leaf photosynthetic capacity in seedlings from seven temperate tree species. Tree Physiol. 21:223–232. Tree Physiology Online at http://www.treephys.oxfordjournals.org Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 to be able to predict the temperature responses of photosynthesis. In particular, we show that changes in measurement D can significantly change the Topt of An, implying that differences in Topt in different seasons or climates do not necessarily indicate plant acclimation to temperature. Thus, measurements of Topt of An alone are not informative for understanding plant responses to temperature. To fully quantify the An–T response, it would be desirable to conduct measurements targeted at each process component, including An–Ci curves at different temperatures to quantify biochemical responses, diurnal An–gs responses to quantify stomatal acclimation, and An–PAR responses to quantify the role of respiration, in addition to careful monitoring of D conditions throughout. In large-scale, well-resourced warming experiments, such detailed measurements may be possible. Where it is not possible to take such measurements, however, photosynthesis– temperature responses can be quantitatively analysed with the aid of a model such as that presented here, in order to gain insight into which components are driving observed temperature responses. In summary, we stand to learn much more from photosynthetic temperature responses in relation to climate when the component processes regulating An are analysed, and measurement D conditions are clearly reported. 230 Lin et al. Tree Physiology Volume 32, 2012 ribulose-1,5-bisphosphate carboxylase/oxygenase. Plant Physiol. 120:173–181. Leuning, R. 1990. Modelling stomatal behaviour and photosynthesis of Eucalyptus grandis. Aust. J. Plant Physiol. 17:159–175. Leuning, R. 1995. A critical appraisal of a combined stomatal-photosynthesis model for C3 plants. Plant, Cell Environ. 18:339–355. Leuning, R. 2002. Temperature dependence of two parameters in a photosynthesis model. Plant, Cell Environ. 25:1205–1210. Lloyd, J. and G.D. Farquhar. 1994. 13C discrimination during CO2 assimilation by the terrestrial biosphere. Oecologia 99:201–215. Long, S.P. 1991. Modification of the response of photosynthetic productivity to rising temperature by atmospheric CO2 concentration: has its importance been underestimated? Plant, Cell Environ. 14:729–739. Makino, A., H. Nakano and T. Mae. 1994. Effects of growth temperature on the responses of ribulose-1,5-bisphosphate carboxylase, electron transport components, and sucrose synthesis enzymes to leaf nitrogen in rice, and their relationships to photosynthesis. Plant Physiol. 105:1231–1238. Medlyn, B.E., E. Dreyer, D. Ellsworth, M. et al. 2002a. Temperature response of parameters of a biochemically based model of photosynthesis. II. A review of experimental data. Plant, Cell Environ. 25:1167–1179. Medlyn, B.E., D. Loustau and S. Delzon. 2002b. Temperature response of parameters of a biochemically based model of photosynthesis. I. Seasonal changes in mature maritime pine (Pinus pinaster Ait.). Plant, Cell Environ. 25:1155–1165. Medlyn, B.E., R.A. Duursma, D. Eamus, D.S. Ellsworth, C. Prentice, C.V.M. Barton, K.Y. Crous, P. Angelis, M. Freeman and L. Wingate. 2011. Reconciling the optimal and empirical approaches to modelling stomatal conductance. Glob. Change Biol. 17:2134–2144. Melillo, J.M., A.D. McGuire, D.W. Kicklighter, B. Moore Iii, C.J. Vorosmarty and A.L. Schloss. 1993. Global climate change and terrestrial net primary production. Nature 363:234–240. Mott, K.A. and D. Peak. 2010. Stomatal responses to humidity and temperature in darkness. Plant, Cell Environ. 33:1084–1090. Niu, G., D.S. Rodriguez and Y.T. Wang. 2006. Impact of drought and temperature on growth and leaf gas exchange of six bedding plant species under greenhouse conditions. HortScience 41:1408–1411. Niu, S., Z. Li, J. Xia, Y. Han, M. Wu and S. Wan. 2008. Climatic warming changes plant photosynthesis and its temperature dependence in a temperate steppe of northern China. Environ. Exp. Bot. 63:91–101. Onoda, Y., K. Hikosaka and T. Hirose. 2005. The balance between RuBP carboxylation and RuBP regeneration: a mechanism underlying the interspecific variation in acclimation of photosynthesis to seasonal change in temperature. Funct. Plant Biol. 32:903–910. Ow, L.F., D. Whitehead, A.S. Walcroft and M.H. Turnbull. 2008. Thermal acclimation of respiration but not photosynthesis in Pinus radiata. Funct. Plant Biol. 35:448–461. Radtke, P.J. and A.P. Robinson. 2006. A Bayesian strategy for combining predictions from empirical and process-based models. Ecol. Model. 190:287–298. Reich, P.B., M.B. Walters, D.S. Ellsworth, J.M. Vose, J.C. Volin, C. Gresham and W.D. Bowman. 1998. Relationships of leaf dark respiration to leaf nitrogen, specific leaf area and leaf life-span: a test across biomes and functional groups. Oecologia 114:471–482. Robakowski, P., P. Montpied and E. Dreyer. 2002. Temperature response of photosynthesis of silver fir (Abies alba Mill.) seedlings. Ann. For. Sci. 59:163–170. Ryan, M.G. 1991. Effects of climate change on plant respiration. Ecol. Appl. 1:157–167. Sage, R.F. 1990. A model describing the regulation of ribulose1,5-bisphosphate carboxylase, electron transport, and triose Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 Ehleringer, J.R. and T.E. Cerling. 1995. Atmospheric CO2 and the ratio of intercellular to ambient CO2 concentrations in plants. Tree Physiol. 15:105–111. Ellsworth, D.S. 2000. Seasonal CO2 assimilation and stomatal limitations in a Pinus taeda canopy. Tree Physiol. 20:435–445. Farquhar, G.D., S. von Caemmerer and J.A. Berry. 1980. A biochemical model of photosynthetic CO2 assimilation in leaves of C3 species. Planta 149:78–90. Fitter, A. and R.K.M. Hay. 2002. Environmental physiology of plants. Academic Press, San Diego, CA. Gunderson, C.A., R.J. Norby and S.D. Wullschleger. 2000. Acclimation of photosynthesis and respiration to simulated climatic warming in northern and southern populations of Acer saccharum: laboratory and field evidence. Tree Physiol. 20:87–96. Gunderson, C.A., K.H. O’Hara, C.M. Campion, A.V. Walker and N.T. Edwards. 2010. Thermal plasticity of photosynthesis: the role of acclimation in forest responses to a warming climate. Glob. Change Biol. 16:2272–2286. Hamilton, J.G., R.B. Thomas and E.H. Delucia. 2001. Direct and indirect effects of elevated CO2 on leaf respiration in a forest ecosystem. Plant, Cell Environ. 24:975–982. Hari, P., A. Mäkelä, E. Korpilahti and M. Holmberg. 1987. Optimal control of gas exchange. Tree Physiol. 2:169–175. Harley, P.C., R.B. Thomas, J.F. Reynolds and B.R. Strain. 1992. Modelling photosynthesis of cotton grown in elevated CO2. Plant, Cell Environ. 15:271–282. Hendrickson, L., M.C. Ball, J.T. Wood, W.S. Chow and R.T. Furbank. 2004. Low temperature effects on photosynthesis and growth of grapevine. Plant, Cell Environ. 27:795–809. Hikosaka, K., A. Murakami and T. Hirose. 1999. Balancing carboxylation and regeneration of ribulose-1,5-bisphosphate in leaf photosynthesis: temperature acclimation of an evergreen tree, Quercus myrsinaefolia. Plant, Cell Environ. 22:841–849. Hikosaka, K., K. Ishikawa, A. Borjigidai, O. Muller and Y. Onoda. 2006. Temperature acclimation of photosynthesis: mechanisms involved in the changes in temperature dependence of photosynthetic rate. J. Exp. Bot. 57:291–302. Hikosaka, K., E. Nabeshima and T. Hiura. 2007. Seasonal changes in the temperature response of photosynthesis in canopy leaves of Quercus crispula in a cool-temperate forest. Tree Physiol. 27:1035–1041. June, T., J.R. Evans and G.D. Farquhar. 2004. A simple new equation for the reversible temperature dependence of photosynthetic electron transport: a study on soybean leaf. Funct. Plant Biol. 31:275–283. Kattge, J. and W. Knorr. 2007. Temperature acclimation in a biochemical model of photosynthesis: a reanalysis of data from 36 species. Plant, Cell Environ. 30:1176–1190. Katul, G., R. Leuning and R. Oren. 2003. Relationship between plant hydraulic and biochemical properties derived from a steady-state coupled water and carbon transport model. Plant, Cell Environ. 26:339–350. Katul, G.G., D.S. Ellsworth and C.T. Lai. 2000. Modelling assimilation and intercellular CO2 from measured conductance: a synthesis of approaches. Plant, Cell Environ. 23:1313–1328. Kirschbaum, M.U.F. 1999. Modelling forest growth and carbon storage in response to increasing CO2 and temperature. Tellus 51B:871–888. Kirschbaum, M.U.F. 2004. Direct and indirect climate change effects on photosynthesis and transpiration. Plant Biol. 6:242–253. Kirschbaum, M.U.F. and G.D. Farquhar. 1984. Temperature dependence of whole-leaf photosynthesis in Eucalyptus pauciflora Sieb. ex Spreng. Aust. J. Plant Physiol. 11:519–538. Law, R.D. and S.J. Crafts-Brandner. 1999. Inhibition and acclimation of photosynthesis to heat stress is closely correlated with activation of Temperature responses of photosynthesis 231 Turnbull, M.H., R. Murthy and K.L. Griffin. 2002. The relative impacts of daytime and night-time warming on photosynthetic capacity in Populus deltoides. Plant, Cell Environ. 25:1729–1737. von Caemmerer, S. and G.D. Farquhar. 1981. Some relationships between the biochemistry of photosynthesis and the gas exchange of leaves. Planta 153:376–387. Walcroft, A.S., D. Whitehead, W.B. Silvester and F.M. Kelliher. 1997. The response of photosynthetic model parameters to temperature and nitrogen concentration in Pinus radiata D. Don. Plant, Cell Environ. 20:1338–1348. Warren, C.R. and E. Dreyer. 2006. Temperature response of photosynthesis and internal conductance to CO2: results from two independent approaches. J. Exp. Bot. 57:3057–3067. Way, D.A. and R.F. Sage. 2008. Thermal acclimation of photosynthesis in black spruce [Picea mariana (Mill.) B.S.P.]. Plant, Cell Environ. 31:1250–1262. Wieser, G., W. Oberhuber, L. Walder, D. Spieler and A. Gruber. 2010. Photosynthetic temperature adaptation of Pinus cembra within the timberline ecotone of the Central Austrian Alps. Ann. For. Sci. 67:201p1–201p8. Wilson, K.B. and D.D. Baldocchi. 2000. Seasonal and interannual variability of energy fluxes over a broadleaved temperate deciduous forest in North America. Agric. For. Meteorol. 100:1–18. Wong, S.C., I.R. Cowan and G.D. Farquhar. 1979. Stomatal conductance correlates with photosynthetic capacity. Nature 282:424–426. Woodward, F.I. 1987. Climate and plant distribution. Cambridge University Press, Cambridge. Wullschleger, S.D. 1993. Biochemical limitations to carbon assimilation in C3 plants—a retrospective analysis of the A/Ci curves from 109 species. J. Exp. Bot. 44:907–920. Tree Physiology Online at http://www.treephys.oxfordjournals.org Downloaded from http://treephys.oxfordjournals.org/ at University of Western Sydney on September 17, 2014 hosphate use in response to light intensity and CO2 in C3 plants. p Plant Physiol. 94:1728–1734. Sage, R.F. and D.S. Kubien. 2007. The temperature response of C3 and C4 photosynthesis. Plant, Cell Environ. 30:1086–1106. Sage, R.F. and T.D. Sharkey. 1987. The effect of temperature on the occurrence of O2 and CO2 insensitive photosynthesis in field-grown plants. Plant Physiol. 84:658–664. Salvucci, M.E. and S.J. Crafts-Brandner. 2004. Relationship between the heat tolerance of photosynthesis and the thermal stability of rubisco activase in plants from contrasting thermal environments. Plant Physiol. 134:1460–1470. Saxe, H., M.G.R. Cannell, Ø. Johnsen, M.G. Ryan and G. Vourlitis. 2001. Tree and forest functioning in response to global warming. New Phytol. 149:369–400. Schimel, D.S., B.H. Braswell, W. Emanuel, B. et al. 1997. Continental scale variability in ecosystem processes: models, data, and the role of disturbance. Ecol. Monogr. 67:251–271. Sharkey, T.D. 1985. Photosynthesis in intact leaves of C3 plants: physics, physiology and rate limitations. Bot. Rev. 51:53–105. Shaw, M.R., M.E. Loik and J. Harte. 2000. Gas exchange and water relations of two Rocky Mountain shrub species exposed to a climate change manipulation. Plant Ecol. 146:197–206. Silim, S.N., N. Ryan and D.S. Kubien. 2010. Temperature responses of photosynthesis and respiration in Populus balsamifera L.: acclimation versus adaptation. Photosynth. Res. 104:19–30. Tjoelker, M.G., J. Oleksyn and P.B. Reich. 2001. Modelling respiration of vegetation: evidence for a general temperature-dependent Q10. Glob. Change Biol. 7:223–230. Tjoelker, M.G., J. Oleksyn, G. Lorenc-Plucinska and P.B. Reich. 2009. Acclimation of respiratory temperature responses in northern and southern populations of Pinus banksiana. New Phytol. 181:218–229.
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