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Theoretically, progressive drought can force trees into negative carbon (C) balance by reducing stomatal conductance to prevent water loss, which also decreases C assimilation. At higher temperatures, negative C balance should be initiated at higher soil moisture because of increased respiratory demand and earlier stomatal closure. Few data are available on how these theoretical relationships integrate over the whole plant.
We exposed Thuja occidentalis to progressive drought under three temperature conditions (15, 25, and 35°C), and measured C and water fluxes using a whole-tree chamber design.
High transpiration rates at higher temperatures led to a rapid decline in soil moisture. During the progressive drought, soil moisture-driven changes in photosynthesis had a greater impact on the whole-plant C balance than respiration. The soil moisture content at which whole-plant C balance became negative increased with temperature, mainly as a result of higher respiration rates and an earlier onset of stomatal closure under a warmer condition.
Our results suggest that the effect of drought on whole-plant C balance is highly temperature-dependent. High temperature causes a negative C balance even under mild drought and may increase the risk of C starvation.
Forests represent large global stores of carbon (C) and account for the largest proportion of annual C exchange with the atmosphere (Phillips et al., 1998; Malhi et al., 1999; Le Quere et al., 2008; Pan et al., 2011; Ballantyne et al., 2012). The C balance of forest ecosystems is sensitive to climate change, which is influenced, for example, by increased growing season duration (Walther et al., 2002), changes in tree growth rates (Clark et al., 2003; Cole et al., 2009) and increased plant respiration and photosynthesis (Piao et al., 2008). There are different means of evaluating the C budget of an ecosystem, such as the widely used eddy covariance technique (Baldocchi, 2003). However, forest ecosystems are made up of individual trees that can respond differently to environmental conditions (e.g. isohydric and anisohydric species; see Tardieu & Simonneau, 1998). Hence, explaining changes in net forest C gain or loss depends on improved understanding of C fluxes at the level of individual trees.
The C balance of an individual plant is the difference between photosynthesis (C input) and respiration (C output). The sum of daytime CO2 uptake from photosynthesis minus the sum of 24 h CO2 release through respiration, referred to as the whole-plant daily C balance, is a meaningful indicator of C accumulation within plants (McCree, 1986). Under favorable conditions, a plant takes up more C than it consumes on a daily basis (C surplus) and the excess C is used for growth and synthesis of defense compounds or is stored in the form of nonstructural carbohydrates for future use, resulting in biomass increase (McCree, 1986; Estiarte & Peñuelas, 1999).
Environmental stresses can alter both photosynthetic and respiratory rates and therefore affect the plant C budget in the short term. The point of zero net C assimilation for the whole plant (i.e. when photosynthetic C uptake equals respiratory C loss on a 24 h basis) is a useful concept to investigate the whole-plant C balance under environmental stresses, and is defined here as the whole-plant C compensation point (CCP).
Under progressive drought, plant growth can be reduced at first (McDowell, 2011) and, as water stress progresses, photosynthesis will be curtailed when stomatal conductance is reduced to prevent water loss through transpiration (Bates & Hall, 1982; Schulze, 1986; McDowell et al., 2008a). However, maintenance respiration may not decline as fast as photosynthesis and the resulting C deficit forces plants to consume stored carbohydrates for respiration (McDowell, 2011). If this C deficit persists, plants will suffer from C starvation as carbohydrates are depleted (Sayer & Haywood, 2006; McDowell, 2011).
At elevated temperatures, enhanced transpiration can hasten the closure of stomata under water stress to prevent water loss (Schulze et al., 1973), simultaneously advancing the decline of photosynthesis. In addition, plants usually present higher maintenance respiration at higher temperatures (Atkin et al., 2000; Atkin & Tjoelker, 2003), which, combined with reductions in photosynthesis, could lead to a rapid depletion of C storage pools (McDowell, 2011). Some authors suggest that, under elevated temperature and drought, plants could be threatened by, or even die from, C starvation rather than hydraulic failure (McDowell et al., 2008a; Sala et al., 2010; Hartmann, 2011; McDowell, 2011). In support of this hypothesis, Adams et al. (2009) provided evidence that under drought stress, leaf-level respiratory C consumption by pinyon pines was significantly higher at elevated temperature (+ 4°C) than under ambient temperature. However, difficulties of scaling leaf-level observations of gas exchange to the whole plant did not allow quantification of the net C balance of these trees, owing to the mismatch between leaf-level CO2 exchange measurements and actual biomass responses (Evans & Dunstone, 1970; Wardlaw, 1990). Responses of plants to drought and high temperature have been mostly studied at the tissue level, while changes in whole-plant C balance have rarely been studied (but for studies in some crops, see McCree, 1986; Miller et al., 2001). To our knowledge, the combined effects of elevated temperature and drought on the whole-plant CCP have not been assessed.
In this study, we carried out a water stress experiment on Thuja occidentalis L. at three different temperatures (15, 25 and 35°C), and focused on tracking variations of the components (i.e. photosynthesis and respiration) of whole-plant daily C balance as soil moisture declined. T. occidentalis is a drought-tolerant evergreen coniferous species in the Cupressaceae family (Collier & Boyer, 1989). It grows in a wide range of moisture conditions, from swamps to cliff edges, making it an interesting choice for drought studies (Beals, 1965; Collier & Boyer, 1989; Kelly & Larson, 2003; Harlow et al., 2005). The average temperature of its natural habitat usually ranges from −12 to −4°C in winter and from 16 to 25°C in summer (Fowells, 1965). Our hypothesis was that trees would be forced into a negative C balance at higher soil moisture content when grown under high temperature (> 30°C) because of higher respiratory demand combined with reduced photosynthesis driven by earlier stomatal closure. At lower temperatures, trees should survive longer and reach the CCP at lower soil moisture contents. The results improve our understanding of the effects of environmental drivers on the whole-plant C balance, with implications for the mechanisms underlying drought-induced tree mortality.
Materials and Methods
Four-year-old trees of T. occidentalis L. (half-siblings) purchased from a regional nursery were transferred to plastic pots (14.5 cm diameter × 16 cm high) and kept well watered outdoors for c. 10 months. The trees were planted in a C-free mixture of vermiculate and sand (volumetric ratio 2 : 1) without any added organic matter. This ensured that CO2 released from the soil was solely derived from roots in our short-term experiment. Nutrients were supplied with a single application of instant fertilizer (Manna Wuxal Super 8-8-6 with microelements; Wilhelm Haug GmbH & Co. KG, Düsseldorf, Germany), combined with a slow-release conifer fertilizer (Substral Osmocote 11-8-17; Scotts Celaflor GmbH, Mainz, Germany). In July, 2012, nine healthy individuals (height from stem base = 58 ± 3 cm, diameter at stem base = 1.0 ± 0.2 cm) were randomly chosen and transferred into airtight cylindrical transparent chambers (17 cm diameter × 80 cm high, made of methyl methacrylate resin) connected to a measurement system to determine CO2 and H2O exchange. The chambers were placed in a climate chamber to control temperature and light. A plastic lid (acrylonitrile butadiene styrene resin) covered each pot and was used to separate the chamber into above- and below-ground compartments. The tree stem passed through center of the cover and was fitted with an airtight seal.
Three trees were randomly assigned to each of the three different temperatures (15, 25 and 35°C). A cycle of 12 h daylight, which was supplied by halogen lamps with a constant photosynthetically active radiation of 390 ± 10 μmol m−2 s−1 (the approximate light saturation point of T. occidentalis, Matthessears & Larson, 1991) measured inside the chambers at the top, was followed by 12 h of darkness. Air and soil temperatures within the chambers were kept constant during the experiment in each temperature treatment. As lighting had a heating effect on the temperature inside the chambers, the temperature outside the chambers was down-regulated 3–4°C during the daytime to maintain constant temperature inside the chambers. The growth substrate was watered to achieve field capacity (volumetric water content c. 50%) at the beginning (data from the first day at 25°C were missing as a result of technical failure), and pots were then left to dry with no further moisture addition until the end of the experiment. Trees were kept well watered and under their corresponding temperature treatment for 2 d before the experiment started to let them acclimate to the experimental conditions. Because of limited room in the growth chamber, the three temperature treatments were conducted in three separate trials and lasted for 34, 30 and 11 d, respectively. Trees from the different trials were not significantly different in size (height and basal stem diameter) or phenology at the start, to ensure comparability among trials. The experiment ended when transpiration approached zero (i.e. below 0.03 mol H2O d−1). At the end, the foliage of all the trees was brown and dry.
Ambient air with constant moisture ([CO2], 400 ± 20 ppm; δ13C-CO2, −9.2 ± 0.5‰; and vapor pressure deficit (VPD), 1.02, 1.90 and 3.94 kPa for 15, 25 and 35°C, respectively) was continuously pumped through above- and below-ground compartments of the chambers at constant rates (above ground, 5.5, 6.5 and 9.5 l min−1; below ground, 1.0, 1.0 and 1.5 l min−1 for 15, 25 and 35°C, respectively), which were controlled by needle valves outside the growth chamber. The difference in flow rates between temperatures was to ensure that the difference in the CO2 and H2O concentrations between incoming and outgoing air was within 60 ppm and 20‰, respectively. CO2 and H2O concentrations of the air entering and leaving each compartment were measured separately with a LI-6262 (Li-Cor Inc., Lincoln, NE, USA) once every hour for 6 min and 40 s, switching from one compartment to the next automatically with electromagnetic valves. Data were collected with a CR1000 data logger (Campbell Scientific Inc., Logan, UT, USA). Hourly CO2 and H2O fluxes (μmol h−1) in each compartment were calculated by
where [S]o and [S]e are the CO2 (or H2O) concentrations (ppm) of the air leaving and entering each compartment, respectively; FR is the air flow rate (l min−1) through each compartment; and 22.4 is the molar volume at standard temperature and pressure (l mol−1). The hourly fluxes were then summed to obtain a daily value. The daytime (12 h) CO2 flux from the above-ground compartment was defined as net photosynthesis (Pn) and the night-time (12 h) above-ground CO2 flux was defined as above-ground respiration. Root respiration was the summed 24 h below-ground CO2 flux. The sum of root and above-ground respiration on a daily basis is referred to as total respiration. The above-ground H2O flux was defined as transpiration and was divided into night-time (En) and daytime (Ed) components. Water-use efficiency (WUE) was calculated as Pn divided by the daytime transpiration (Ed) on a daily basis. Stomatal conductance (Gs, mol d−1) was estimated by (Jarvis & McNaughton, 1986; Whitehead, 1998; McDowell et al., 2008b)
During CO2 assimilation, a reduction in discrimination against 13C is considered to be a physiological indicator of drought stress (Farquhar et al., 1989). To reveal the variation of 13C discrimination as soil water content declines and drought stress increases, discrete air samples were taken from the air flow entering and leaving above-ground compartments every 1–3 d at a fixed time (i.e. 2 h after the light was switched on), and were analyzed for 13C composition in reference to Pee Dee Belemnite (δ13C) with a Delta+ XL Isotope Ratio Mass Spectrometry (IRMS, ThermoFinnigan, Bremen, Germany). δ13Cp indicates here the 13C composition of the CO2 assimilated by trees, computed from the mass balance of CO2 and 13CO2 of the air entering and leaving the chamber:
where δo and δe represent 13C composition of the CO2 in the air leaving and entering the chamber, respectively. We assumed the shift in δ13Cp mainly reflects photosynthetic fractionation.
A dendrometer (self-assembled with an 8 mm potentiometric linear transducer supplied by Megatron Elektronik AG & Co., Putzbrunn, Germany) was installed on the stem of one tree in each trial to measure stem diameter variation in response to drought as a proxy for water capacitance (Zweifel et al., 2005). We report here the difference in stem diameter (μm) at a given soil moisture from initial diameter. Soil moisture and air/soil temperature were monitored using a ThetaProbe ML2x (Delta-T Devices Ltd, Burwell, Cambridge, UK) and a 100 kΩ NTC Thermistor EC95 (Thermometrics Corporation, USA), respectively.
The stress point (SP) was defined as the first day that transpiration showed a significant decline from the average value of the previous days (t-test, P <0.05), and the mean soil moisture value (± SD) at the SP of the three individuals was compared among the three temperature treatments. For the period before the SP, it is assumed that no water stress was imposed and differences in respiration and photosynthesis rates reflected the influence of temperature only. The average values of each variable (i.e. Pn, respiration, transpiration, WUE, net C gain, ratio of respiration to Pn and δ13Cp) before the SP were computed and compared among the three temperature treatments. One-way ANOVA followed by a Holm–Šidák test (P <0.05) was applied to identify instances with statistically significant differences. For the period after the SP, we applied mixed-effects modeling to investigate how soil moisture and temperature influenced the C balance of the plants using net C gain, Pn, or total respiration as dependent variables. Interactions of soil volumetric water content (or Gs) and temperature were included as fixed effects and temperature as random effects to obtain separate intercepts and slopes for each temperature (see Supporting Information, Table S1, for a summary of the models). By modeling the temperature effect on the components of C gain, we aimed to separate the temperature effects on the whole-plant C balance from those of Pn (via stomatal conductance) and respiration.
To determine the CCP under each temperature treatment, a sigmoidal model was fitted to the daily net CO2 gain as a function of soil moisture, from the starting point to the lowest point:
where y is the daily net CO2 gain, x is the soil moisture and a–d are regression parameters. The point (measured as soil moisture) where net CO2 gain equals zero was defined as the CCP. All statistics were carried out with R, version 2.15.0 (R Development Core Team, 2012) and the package ‘lme4’ (Bates et al., 2012) was used in the mixed-effects modeling.
Pn and respiration showed similar patterns of response for all three temperature treatments as the soil dried out (Fig. 1a–c). Pn declined sharply after the SP and continued to decrease to values below the respiration rates. Respiration also decreased after the SP but not as fast as Pn. After the CCP, respiration rates showed a rapid decline, eventually reaching values close to zero. Daily net C gain began to decline at the SP and became negative after CCP (Fig. 1d). As total respiration declined to near zero at the end of the experiment, daily C gain increased again and reached approximately zero. As predicted, CCP was shifted by temperature and occurred at higher soil moisture contents (10.3, 13.4 and 20.4%, F =31.49, P <0.001) as the temperature increased (15, 25, and 35°C, respectively). In particular, 20% soil moisture was still wet enough for trees at 15°C to maintain normal photosynthesis and transpiration, while trees at 35°C with the same soil moisture content were already in net C deficit. Pn and total respiration at the CCP had already dropped to low rates at 15 and 25°C, while rates at 35°C remained high, suggesting that only mild stress was imposed at this point. Based on total respiration rates at the end of the experiment, trees at 25 and 35°C were dead (zero respiration) after 29 and 11 d, respectively, while trees at 15°C were still alive after 34 d (total respiration = 1.65 ± 0.18 mmol CO2 d−1) when we ended the experiment.
Cumulative net C gain (Fig. 2) showed different patterns among the three temperature treatments. Trees grown at 15°C accumulated much more C than trees grown at 25 or 35°C. At the end of the experiment, trees grown at 15 and 25°C still had not used up the equivalent amount of C accumulated during the experiment. However, trees grown at 35°C had already consumed, within 6 d, as much C as was accumulated during the experiment and seemingly relied on stored C for respiration after that.
After the onset of the SP (Fig. 3a), Pn declined as a result of decreasing daytime Gs (Fig. 3b). The higher temperature led to increased transpiration rates and hastened soil drying. Night-time transpiration rates remained low (not exceeding 1 mol H2O d−1) at 15 and 25°C (Fig. 3c). However, at 35°C night-time transpiration was much greater (even higher than daytime transpiration at 15 and 25°C). Night-time Gs showed a similar pattern for the three temperatures but was slightly lower at 25°C (Fig. 3d).
Water-use efficiency did not drop at the SP, and only dropped after the CCP (Fig. 4a) because Pn and daytime transpiration decreased proportionally after SP. After CCP, Pn declined faster than transpiration, leading to the decrease in WUE. Stems of the trees started to shrink after the SP (Fig. 4b), indicating reductions in stem water potential. The increased δ13Cp after the SP (Fig. 4c) indicated that stomatal conductance was limiting intercellular CO2 concentration during C assimilation and induced a decline in isotopic discrimination. Similar to former studies (Farquhar & Richards, 1984; Henderson et al., 1998), δ13Cp is well correlated with WUE at the three temperatures (Fig. S1).
Effect of temperature without drought stress
The SP, which indicates the onset of stomatal closure, occurred at lower soil moisture at 15°C than at 25 and 35°C (Fig. 5a). Before the SP, that is, before the onset of drought stress, temperature had a significant effect on the C balance. Respiration rates above and below ground increased with temperature and were significantly higher at 35°C (Fig. 5c,d), whereas Pn was not affected by temperature before the onset of drought stress (F =0.224, P =0.805, Fig. 5b). As a result, daily net C gain was significantly lower at 35°C than at 15°C (Fig. 5e). The ratio of total respiration to photosynthesis was c. 0.24 at 15°C but reached 0.33 and 0.60 at 25°C and 35°C, respectively (Fig. 5f). Night-time transpiration was much higher at 35°C (Fig. 5g). Daytime transpiration rates increased exponentially with temperature and were significantly different among temperature treatments (Fig. 5h). WUE dropped significantly as temperature increased and was five to seven times higher at 15°C than at 35°C (Fig. 5i). Similar to transpiration, night-time Gs was significantly lower at 15 and 25°C than at 35°C, while daytime Gs increased with temperature (Fig. 5j,k). δ13Cp was significantly higher at 15 than at 35°C (Fig. 5l), indicating that CO2 availability at the leaf level was not as limited at 35°C as it was at 15°C before the SP.
Interaction of drought stress and temperature
Temperature showed a significant effect on how the trees' C balance responded to declining soil moisture (Fig. 6). The Pn of trees grown at 15°C was more sensitive to soil moisture decline after drought stress developed than at higher temperatures (Fig. 6a), whereas response of total respiration to soil moisture was not significantly affected by temperature increase (Fig. 6b). Pn was more sensitive to soil moisture decline than respiration, making it more of a determinant of the tree C balance during progressive drought. Pn at lower temperatures was more sensitive to Gs than at higher temperatures (Fig. 6c), indicating that photosynthesis was more constrained by stomatal conductance at lower temperatures, which in turn made Gs more important for net C gain at 15°C (Fig. 6d).
Advance of the CCP at elevated temperature
This study revealed that changes in whole-plant C balance during drought stress are highly temperature-dependent. As hypothesized, C deficit occurred in trees at a high temperature (35°C) at a soil moisture content that may not be considered as drought for trees growing at a lower temperature (15°C). Former studies of whole-plant C balance in crops (McCree, 1986; Miller et al., 2001) also suggest that whole-plant C gain is inhibited under water stress and high temperature, but these studies did not separate the temperature and drought effects nor did they determine whole-plant CCP. Temperature did not affect how plant respiration responded to the progressive drought after the SP (Fig. 6b), while sensitivity of Pn to soil moisture decline was lower at higher temperatures (25 and 35°C) (Fig. 6a), which itself ran counter to the advance of the CCP at higher temperatures. Therefore, considering initial values before the SP, the earlier occurrence of CCP caused by high temperature was mainly attributed to the higher initial respiration rates (Fig. 5c,d) and an earlier onset of stomatal closure (i.e. SP, Fig. 5a), but not initial Pn (Fig. 5b).
Previous studies in vascular plants have demonstrated that elevated temperatures increase plant maintenance respiration (Atkin et al., 2000; Atkin & Tjoelker, 2003) and hasten stomatal closure as water stress develops (Schulze et al., 1973). These results are consistent with the patterns of the processes that caused the CCP to occur at higher moisture content under elevated temperature. In addition, as temperature rises beyond the optimum point, plant photosynthesis can be reduced (Bernacchi et al., 2001, 2002) and may further advance the CCP during drought/heat events. While the conditions imposed in our treatments may not realistically mirror anticipated patterns of climatic change, our results indicate that the combined effects of drought and elevated temperature have important implications for the C budget of vascular plants under a warmer and drier scenario.
Temperature effects on plant C balance without drought
Owing to technical constraints, we did not have well-watered trees as a control at each temperature in our experiment, which would have allowed us to separate the effects of temperature from those of declining soil moisture. Instead, we took the period before the SP at each trial as a baseline, assuming no major changes in plant physiology would occur during the experiment under strictly controlled conditions (i.e. without day-to-day variations in temperature and light conditions) if no water stress was imposed.
As temperatures increased from 15 to 35°C, net photosynthetic rates remained constant (Fig. 5b), while respiration increased with a Q10 (the rate of respiration change as temperature increases by 10°C) of c. 1.4. Stronger photosynthetic discrimination against 13C occurred at 35 than at 15°C (Fig. 5l), similar to what has been observed in studies on shrubs under experimental warming (Welker et al., 1993, 2004; Michelsen et al., 1996). This can be explained by the high stomatal conductance at 35°C (Fig. 5k), which kept intercellular CO2 concentration high and thereby enhanced C isotope discrimination (Farquhar et al., 1982, 1989). In addition, during the imposed progressive drought, the slopes of Pn to Gs (Fig. 6c), reflecting the gradient between ambient and intercellular CO2 concentration (ca–ci) (Farquhar & Sharkey, 1982), were lower at elevated temperatures. This suggests that intercellular CO2 concentration was highest at 35°C for a given Gs value, potentially another reason for the large 13C discrimination at 35°C.
High VPD is usually considered to have a negative effect on stomatal conductance (Gucci et al., 1996; Wullschleger et al., 2002), which in turn influences photosynthesis and C balance. Yet, elevated temperature can also widen the aperture of stomata at constant VPD (Schulze et al., 1973). Our results show that daytime Gs was higher under warmer conditions (Fig. 5k), indicating that direct temperature effects were much stronger than temperature effects via VPD. However, their individual contributions to changes in stomatal conductance as well as to the C balance need to be quantified in a specifically designed experiment.
Effects of temperature and drought on the plant C balance
During the progressive drought, Pn played a more important role than respiration in the C balance, because Pn was more sensitive than respiration to soil moisture decline at all temperatures (Fig. 6a,b). Temperature, including its effect on VPD, affected Pn through Gs (Fig. 6c), and, hence, the C balance (Fig. 6d). Respiration was primarily directly affected by temperature (Fig. 5c,d), rather than by temperature/drought interactions as indicated by parallel slopes of respiration over soil moisture (Fig. 6b).
We observed two distinct phases of drought stress response. In the first phase, Pn, respiration, transpiration, stem diameter and δ13Cp all started to decline after the SP (Figs 1, 3, 4). However, WUE started to decrease only around the CCP, characterizing the second phase of the response (Fig. 4). Before reaching the CCP, stomatal closure reduced both water loss and CO2 diffusion into leaves, thereby causing simultaneous reductions in Pn and transpiration. After the onset of the CCP, Pn decreased at a greater rate than transpiration, inducing a decline in WUE. One possible explanation is the nonlinear decrease of mesophyll conductance under drought conditions (Flexas et al., 2002), which may impede CO2 diffusion and induce a sudden decline in C fixation at the CCP. Another possibility is that, regardless of stomatal closure, there could be some metabolic impairment inhibiting CO2 fixation when plants reach a negative C balance. The rapid decline of respiration after the CCP may also have been induced by this (Fig. 1). Flexas & Medrano (2002) demonstrated that stomatal closure is the dominant limitation of photosynthesis under mild and moderate drought conditions, whereas, under severe drought, metabolic impairment (i.e. decreased ribulose-1,5-bisphosphate content) becomes the dominant limitation. Whether the CCP can actually indicate metabolic impairment needs to be further investigated. Given the usefulness of the CCP as an indicator of critical plant C and water relations, further exploration of the physiological processes and potential indicators of the CCP and how these vary with tree species may provide important insights.
Implications for mechanisms of drought-induced tree mortality
Our results suggest that high temperatures can increase the risk of C starvation by forcing trees to be C-deficient under relatively high soil moisture contents. McDowell et al. (2008a) suggested C starvation as a possible cause of drought-induced mortality, especially in warmer environments. In support of this point, Adams et al. (2009) demonstrated that higher temperatures increased cumulative respiration of plants at a leaf level under water stress. In our study, at the end of the 15 and 25°C trials, the amount of C that had been accumulated during the experimental period was still far from being depleted (Fig. 2). It seems that these trees were not C-limited at the end of the experiment, even though respiration rates had dropped to nearly zero. Given the rapid decline in their stem diameter at the end of the experiment (Fig. 4b), indicating a decrease of stem water content, hydraulic failure was the most likely main threat to tree survival at these temperatures. At 35°C, the amount of C respired by the trees exceeded what they had accumulated during the experimental period. At the time of their death, they had consumed up to 27 mmol (324 mg) more C than was accumulated during the experiment. However, given the stem diameter decline (Fig. 4b), hydraulic failure or an interaction between water stress and C deficiency (McDowell, 2011) was probably the cause of the death in these trees. Without sufficient data, we cannot determine the exact mortality mechanism. Still, it is obvious that plants experiencing higher temperatures accumulate less C and are more likely to become C-limited under the same soil moisture conditions.
With our whole-plant chamber design, we demonstrated that high temperature shifts the CCP of plants to higher soil moisture values. It can be inferred that a warming climate may cause physiological drought (i.e. C deficit) even when no meteorological or severe drought occurs, and may consequently threaten the survival of plants in more regions. Similarly, summer drought may impose a greater threat to plants than droughts during colder periods.
We sincerely thank Olaf Kolle and Petra Linke for their work in programming and air sample analysis, respectively. We are also very grateful to Frank Voigt and Bernd Schloeffel from the mechanical workshop at the Max Planck Institute for Biogeochemistry, who built the chambers and many installations, and to Saadat Malghani, who provided the pump for the experiment. This study was supported by Max Planck Institute for Biogeochemistry and partially by the National Natural Science Foundation of China (NSFC: no. 41071071).