Journal of Plant Ecology Volume 6, Number 5, Pages 418–427 october 2013 doi:10.1093/jpe/rtt010 available online at www.jpe.oxfordjournals.org Grazing alters warming effects on leaf photosynthesis and respiration in Gentiana straminea, an alpine forb species Haihua Shen1,2,*, Shiping Wang3 and Yanhong Tang1 1 Center for Environmental Biology and Ecosystem Studies, National Institute for Environmental Studies, Onogawa 16-2, Tsukuba, Ibaraki 305-8506, Japan 2 State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China 3 Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China *Correspondence address: State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China. Tel: +86-10-62836896; E-mail: [email protected] Abstract Aims Vast grasslands on the Tibetan Plateau are almost all under livestock grazing. It is unclear, however, what is the role that the grazing will play in carbon cycle of the grassland under future climate warming. We found in our previous study that experimental warming can shift the optimum temperature of saturated photosynthetic rate into higher temperature in alpine plants. In this study, we proposed and tested the hypothesis that livestock grazing would alter the warming effect on photosynthetic and respiration through changing physical environments of grassland plants. Methods Experimental warming was carried by using an infrared heating system to increase the air temperature by 1.2 and 1.7°C during the day and night, respectively. The warming and ambient temperature treatments were crossed over to the two grazing treatments, grazing and un-grazed treatments, respectively. To assess the effects of grazing and warming, we examined photosynthesis, dark respiration, maximum rates of the photosynthetic electron transport (Jmax), RuBP carboxylation (Vcmax) and temperature sensitivity of respiration Q10 in Gentiana straminea, an alpine species widely distributed on the Tibetan grassland. Leaf morphological and chemical properties were also examined to understand the physiological responses. Important findings 1) Light-saturated photosynthetic rate (Amax) of G. straminea showed similar temperature optimum at around 16°C in plants from all experimental conditions. Experimental warming increased Amax at all measuring temperatures from 10 to 25°C, but the positive effect of the warming occurred only in plants grown under the un-grazed conditions. Under the same measuring temperature, Amax was significantly higher in plants from the grazed than the un-grazed condition. 2) There was significant crossing effect of warming and grazing on the temperature sensitivity (Q10) of leaf dark respiration. Under the un-grazed condition, plants from the warming treatment showed lower respiration rate but similar Q10 in comparison with plants from the ambient temperature treatment. However, under the grazed condition Q10 was significantly lower in plants from the warming than the ambient treatment. 3) The results indicate that livestock grazing can alter the warming effects on leaf photosynthesis and temperature sensitivity of leaf dark respiration through changing physical environment of the grassland plants. The study suggests for the first time that grazing effects should be taken into account in predicting global warming effects on photosynthesis and respiration of plants in those grasslands with livestock grazing. Keywords: alpine plant, grazing, photosynthesis, respiration, temperature acclimation Received: 24 June 2012 Revised: 21 January 2013 Accepted: 26 January 2013 © The Author 2013. Published by Oxford University Press on behalf of the Institute of Botany, Chinese Academy of Sciences and the Botanical Society of China. All rights reserved. For permissions, please email: [email protected] Shen et al. | Grazing alters warming effects on understory forb419 Introduction Plant photosynthesis and respiration are the dominant biological processes regulating biosphere–atmosphere carbon exchange (Ryan 1991; Valentini et al. 2000; Silim et al. 2010). Increasing temperatures as a result of global warming can have profound impacts on these two processes, which in turn affect CO2 concentrations in the atmosphere and hence global warming (Dewar et al. 1999; Gunderson et al. 2000; Atkin and Tjoelker 2003). Understanding the two processes in relation to temperature is needed in order to predict the carbon budget of ecosystems in response to future global warming. Plant photosynthesis and respiration rates are strongly temperature dependent. As instantaneous response, the photosynthetic rate generally rises with temperature increases up to an optimum temperature and then decreases with further increases in temperature. As acclimation, this relationship between instantaneous photosynthetic rate and measuring temperature varies with growth temperature of plants; for example, the thermal optimum of photosynthesis is typically adjusted to approximate growth temperature (e.g. Pearcy 1977; Berry and Björkman 1980; Hikosaka et al. 2006). Similarly, as instantaneous response, the respiration rate (R) increases exponentially with temperature, and the relationship also varies with growth temperature; R usually decreases with the increase of growth temperature under the same measuring temperature (Atkin and Tjoelker 2003; Atkin et al. 2005; Tjoelker et al. 2009). Since the magnitude of plant responses to temperature differs between photosynthesis and respiration, the carbon balance and plant growth can change under warming conditions (Morison and Morecroft 2006; Bruhn et al. 2007; Way and Sage 2008; Shen et al. 2009). Consequently, the temperature dependencies of these two processes become a primary determinant of how plants will respond to global warming (Silim et al. 2010). The temperature dependence of photosynthesis and respiration also varies with growth environments other than temperature, such as radiation and water availability (Tranquillini et al. 1986; Robakowski et al. 2003; Bauerle et al. 2007; Alonso et al. 2009; Yamori et al. 2010). For example, growth light can affect temperature dependency of photosynthetic rate because light regime changes nitrogen allocation between photosynthetic components (Yamori et al. 2010). In grasslands, the growth environments including radiation regimes can be often modified by livestock grazing (Jones 2000; Shen et al. 2009; Jeddi and Chaieb 2010); for example, reduced vegetation coverage by grazing increased irradiance for some forb plants within grasslands (Dahlgren and Driscoll 1994; Wan et al. 2002; Klein et al. 2005). It is, therefore, reasonable to expect that temperature response and/or acclimation of photosynthesis and respiration can differ under grazing compared with un-grazed condition. However, to our knowledge, little information is available for addressing how livestock grazing affects temperature response and acclimation of the two physiological processes in alpine grasslands, though many observations have been reported focusing on temperature response and acclimation of photosynthesis and respiration under various other environments (e.g. Larigauderie and Körner 1995; Atkin et al. 2000; Atkin et al. 2006; Shen et al. 2009). Tibetan Plateau, extending over 2.5 million km2, holds the largest alpine grassland in the world. The grassland here, like other Eurasian grasslands, is almost all under livestock grazing (Cao et al. 2004). Because of the vast area and high sensitivity of the alpine grassland in response to climate change, clarifying the effect of livestock grazing on plant carbon budget will be needed for further assessment on the uncertainty of terrestrial carbon cycle under global warming conditions. We have previously examined the warming effect on photosynthesis and respiration of Gentiana straminea, a typical understory forb in most meadows on the Tibetan Plateau, through an open top chamber experiment and found that the experimental warming shifted the optimum temperature of photosynthesis (Shen et al. 2009). In the current study, we hypothesized that livestock grazing may change temperature response and/ or acclimation of photosynthesis and respiration of grassland plants through changing physical environments. We tested the hypothesis by examining the combined effects of experimental warming and grazing on photosynthesis and respiration of G. straminea. We also examined leaf morphology and biochemical components to explain the effects of experimental treatments on the two physiological responses. MATERIALS AND METHODS Study site and plant materials The field site was an alpine meadow (37°37’N, 101°12’E, 3250 m elevation) located at the northeastern edge of Tibetan Plateau in a large valley surrounded by the Qilian Mountains. The mean annual temperature for the 25 years from 1976 to 2001 was −1.7°C, and mean annual precipitation was 560 mm, over 80% of which falls during the summer monsoon season (Wang et al. 1999). The soil of the study site is classified as a Mat Cry-gelic Cambisol (Chinese Soil Taxonomy Research Group 1995). The controlled warming–grazing experiment by infrared heating system (FATE) was started from May 2006. The set point of canopy temperature difference between heated and corresponding reference plots was 1.2°C during the day and 1.7°C at night (Luo et al. 2010). To investigate the independent and/or combined effect of warming and grazing, a two-factorial design (warming and grazing) was used, with four replicates for each of four treatments: ambient with un-grazed (A/U), ambient with grazing (A/G), warming with un-grazed (W/U) and warming with grazing (W/G). In total, 16 plots with 3-m diameter were used in a complete randomized block distribution in the field. Livestock grazing regimes were achieved by fencing one adult Tibetan sheep in the plot for ~2 h in 15 August 2006, and by fencing two adult Tibetan sheep for ~1 h in every month from July to 420 Journal of Plant Ecology September since 2007. More details about the experimental design are described by Luo et al. (2010). Gentiana straminea is one of the most common forb species of meadows of the Tibetan Plateau and the Himalayan region. This species is a non-palatable plant that the livestock—sheep, yak and horses—tend to avoid. The linear-shaped leaves of this species grow diagonally from the soil surface to the top of the canopy and are 20–30 cm long when mature, which cannot reach the top of canopy in un-grazed treatment (Shen et al. 2009). Assessment of the micro-environment To examine the effect of warming and grazing on micro-environments, in each treatment regime, we installed and fixed one quantum sensor (GaAsP Photodiode G1118; Hamamatsu City, Japan) on a horizontal plane at the average height of the G. straminea leaves. All quantum sensors were calibrated in sunlight and in artificial shade against a standard quantum sensor (Li-Cor Model 190S; Li-Cor, Lincoln, NE) before the test measurements (Shen et al. 2009). We recorded photosynthetic photon flux density (PPFD) and leaf temperature at 1-min intervals from 3 August to 8 August 2009 using a datalogger (Thermic 2300A; EtoDenki Ltd., Tokyo, Japan). We measured leaf temperature by attaching two copper-constantan thermocouples firmly on the adaxial side of the leaf with ventilated bandage that is highly permeable to CO2 and H2O. Leaf morphology and biochemistry Leaf morphology and biochemical components provide basic information for explaining any change in photosynthesis and respiration (Björkman 1981; Boardman 1997). Many leaf traits are often important indicators for assessing grazing effect (e.g. Diaz et al. 2001; Diaz et al. 2007). In July 2008, to examine the change in leaf size under different treatments without destruction of leaves, we first scanned 165 leaves from plants growing outside the experimental site to a computer and estimated the individual leaf size (i.e. the area of an individual leaf) by using ImageJ software (ImageJ 1.42q, National Institutes of Health, Washington, DC). The length and width of these sample leaves were measured with a digital caliper. From the measurements, we obtained the following statistical model: Leaf size = 0.69 × leaf length × leaf width (R 2 = 0.97; P < 0.001, n = 165) To obtain individual leaf size and leaf mass per unit area (LMA, gm−2) controlling for changes due to leaf age, we sampled 12 individual uppermost fully expanded leaves for each of the four treatment regimes. These leaves are randomly determined from different ramets in different plots of each treatment. We then estimated the leaf size from the above regression model and measured the dry weight (oven dried at 80°C for 24 h) for each individual leaves. LMA was then obtained for each leaf. To measure the content of chlorophyll a and b and carotenoid concentrations, the leaves were cut into small pieces after we had taken the photosynthetic measurements and were then placed in separate bottles containing 10 ml of ethanol, acetone and water (4.5:4.5:1 [v/v/v]). The resulting solution was stabilized in tightly closed bottles that were kept in a refrigerator (about 5°C) in the dark for nearly 3 weeks. Absorbance of the chlorophyll and carotenoid solution was analyzed at wavelengths of 663, 645 and 440 nm by using a UV-Vis spectrophotometer (UV-1601; Shimadzu, Tokyo, Japan). The chlorophyll a and b and carotenoid concentrations were calculated according to methods provided by Zhu (1990). Photosynthetic response to PPFD, temperature and intercellular CO2 concentration Leaf gas exchange was measured on fully expanded intact leaves in the field with an LI-6400 portable photosynthesis measurement system (Li-Cor, Inc.) in July 2008. Four plants were randomly decided in each treatment regime for measurements under PPFD conditions of 0, 25, 50, 100, 250, 500, 1000 and 1500 µmol m−2 s−1, each combined with four temperatures (10, 15, 20, and 25°C) in the sample chamber. During these measurements, we maintained the CO2 concentration at 370 µmol mol−1. The relative humidity was controlled to between 60 and 70% by using a water-bubbling system or desiccant to adjust the inflowing air (Shen et al. 2009). We fitted the maximum photosynthetic rate (Amax) to the measured temperature by two-dimensional polynomial curves and estimated the optimum temperature of Amax and relevant Amax from these two-dimensional polynomial functions. To obtain the maximum rates of photosynthetic electron transport (Jmax) and RuBP carboxylation (Vcmax), following the method by Yamori et al. (2005), we measured the CO2 dependence of photosynthesis under CO2 concentrations of 0, 50, 100, 150, 370 and 1000 µL L−1 in the ambient air (Ca). Light intensity was set to 1000 µmol m−2 s−1 at three temperatures (15, 20 and 25°C). At each CO2 concentration, net photosynthetic rate (A) and intercellular CO2 concentration were calculated. We calculated Jmax and Vcmax from the following equations (Farquhar et al. 1980): O Vc max = (IS )×Γ * +K c 1 + K o J max = ( A1000 + Rd )×(4C i + 8Γ *) Ci − Γ * where, A1000 is the net photosynthetic rate at the highest Ca of 1000 µL L−1 CO2. IS is the initial slope of the A versus Ci curve obtained with the data measured at Ca of 0, 50, 100 and 150 µL L−1. The Other details are referred elsewhere (Yamori et al. 2005; Shen et al. 2009). Shen et al. | Grazing alters warming effects on understory forb421 Response of respiration rate to temperature The short-term temperature sensitivity of the respiration rate is described by Q10: 10 R (T −T0 ) Q10 = T , RT 0 where, RT0 and RT are values of leaf dark respiration (R) measured on a reference leaf temperature (T, T0), respectively, and a second leaf T, where R is induced by rapid warming. Data analysis We used analysis of variance (ANOVA) of repeated-measures and least significant different (LSD) multiple comparison to identify treatment effect in environmental parameters, leaf morphology, biochemical and physiological parameters between plants from different treatments using SPSS Version 11.5 (SPSS Inc., Chicago, IL, USA). Because the photosynthetic rate within grazed and un-grazed conditions varied, we compared the relative responses by converting the results into the percentage of change between warming and ambient regimes—for example, percent of warming-induced change in Amax (the relative warming effect on Amax, RWEAmax = (Amax.w− Amax.a)/Amax.a) —and then compared these percentages to assess the effect of grazing on the changes with the photosynthetic rate in response to temperature. P-value above 0.05 was judged to be statistically significant in this study. RESULTS Growth irradiance and leaf temperature PPFD measured on a horizontal plane at the average height of the G. straminea leaves was significantly higher under the grazed condition than in the un-grazed condition (Fig. 1a), which was about eight times higher on a clear day and about three times higher on a cloudy day (data not shown). Approximately 90% of the PPFD data from the un-grazed condition were <250 µmol m−2 s−1, and no readings above 750 µmol m−2 s−1 were obtained (Fig. 1b). Leaf temperatures measured by either daily mean (24-h mean), or daytime mean (from 8:00AM to 20:00PM, local time), or nighttime mean were all significantly higher under the warming treatments than in the ambient temperature treatments within grazed and/or un-grazed treatments (Fig. 1c). However, the difference of the daytime and nighttime mean leaf temperatures between the two temperature treatments was significantly smaller under the grazed conditions than the un-grazed conditions (Fig. 1d). Leaf morphology and biochemistry The experimental grazing significantly reduced individual leaf size and total leaf area per ramet (Tables 1 and 2). However, the grazing effect on leaf size and total leaf area did not depend on the temperature treatment (Table 2). The experimental warming significantly decreased the total chlorophyll content (Chl a+b), the ratio of chlorophyll a and b (Chl a/b) and carotenoid content, while grazing tended to slightly increase all the above biochemical components (Tables 1 and 2). However, the interaction effect of warming and grazing was not statistically significant (Table 2). Response of light-saturated photosynthesis and respiration Plants from all the four experimental treatments showed an increase in light-saturated photosynthesis (Amax) with an increase in measuring temperature from 10 to 15°C and then a decrease in Amax under higher measuring temperatures (Fig. 2a). This decrease in Amax with higher temperatures was more notable in plants from the grazed conditions (Fig. 2a). Amax at the optimum temperature was significantly higher in plants from the grazed than from the un-grazed conditions. In ambient temperature treatments, for example, the Amax was about 22% higher in plants from the grazed than the ungrazed treatment (Fig. 2a; Tables 1 and 2). The relative warming effect (RWEAmax) on Amax was significantly higher in the un-grazed conditions than in the grazed conditions (Fig. 2b). In the un-grazed conditions, Amax was consistently about 9% higher in plants from the warming plots than in those from the ambient temperature plots when measuring temperatures were 10, 15 and 20°C (Fig. 2b). However, under the grazed conditions, Amax was almost similar between plants from the two different temperature treatments. The dark respiration rates (R) increased exponentially with increasing temperature in all treatments (Fig. 3). In plants from the un-grazed conditions, R tended to be about 0.15 µmol m−2 s−1 constantly smaller at all measuring temperatures in plants from the warming than the ambient temperature treatment, which resulted in similar Q10 of R for leaves from the two treatments in the un-grazed conditions. However, in plants from the grazed conditions, the Q10 was significantly higher in plants in ambient temperature plots than under the experimental warming plots (Tables 1 and 2). Temperature response of RuBP regeneration and RuBP carboxylation To understand the underlying biochemical mechanisms involved in the response of photosynthesis to temperature, we compared the maximum rate of electron transport (Jmax) and the maximum rate of carboxylation (Vcmax) between the four experimental treatments (Fig. 4). Jmax, which was derived from CO2 response curves at different measuring temperatures, was consistently higher at all the measurement temperatures under the ambient than the warming regimes in un-grazed treatment, but this difference was not observed plants from grazed treatment (Figs 4a and b). The maximum rate of carboxylation (Vcmax) showed higher values in plants 422 Journal of Plant Ecology Figure 1: physical environmental variation under different experimental conditions. (a) Daily total photosynthetic photon flux density (PPFD) under grazed and un-grazed conditions. (b) Frequency distribution of PPFD under grazed and un-grazed conditions. (c): Leaf temperatures measured on two leaves of Gentiana straminea for each of four experimental treatments. (d) Increases in leaf temperature under un-grazed (W/U–A/U) and grazed (W/G–A/G) conditions. Different lower-case letters (a, b and c) indicate statistically significant difference at P < 0.05 from least significant difference multiple comparison. from the ambient compared with warming treatment under both grazing conditions. The difference was statistically significant under measurement temperatures of 15 and 20°C in plants from the un-grazed treatment but those of 20–25°C from the grazed treatment (Figs 4c and d). Discussion Photosynthetic response and acclimation to temperature changes The instantaneous response of Amax to measuring temperature in G. straminea followed a similar pattern with our previous report: Amax increased with the increase of temperature below around 16°C and then decreased with temperature increase (Shen et al. 2009). The optimum temperature of Amax is very close to the average daily temperature of the alpine meadow observed during the growing season by Kato et al. (2004). However, the experimental warming effects on photosynthesis, that is, the acclimation of photosynthesis to growth temperature, differed with the observation in our previous study (Shen et al. 2009). The optimum temperature of Amax was similar in plants grown under the two temperature conditions in this study but shifted into higher temperature in plants grown from the high temperature in the previous observation. This discrepancy may be due to the small temperature difference in the current study. Temperature elevation was greater in the OTC experiment than in the current warming experiment. In general, an increase of 1ºC in growth temperature can lead to a shift of 0.10–0.59ºC in the optimum temperature in different plants (see review by Hikosaka et al. 2006). This means that a shift of 1°C in the thermal optimal of Amax needs a change in the temperature environment of 5–10°C. In our previous study, OTCs increased the mean daytime leaf temperature by 3.3°C, whereas the FATE system used in the current study only increased the mean daytime leaf temperature by about 1.6°C (Fig. 1). Many other studies suggest that there is a high variability in the degree of photosynthetic acclimation to experimental warming among species, with some species exhibiting full acclimation and others incapable of even partial acclimation (e.g. Pearcy 1977; Berry and Björkman 1980; Larigauderie and Körner 1995; Xiong et al. 2000; Hikosaka et al. 2006; Dillaway and Kruger 2010). Our observation from this and the previous studies suggests that within the same species, the temperature optimum of Amax varies with the changed magnitudes of growth temperature. A significant change of the optimum may require a constant change around 3°C in this alpine species, G. straminea. The lower thermal acclimation is consistent with some alpine plants and Shen et al. | Grazing alters warming effects on understory forb423 Table 1: the leaf morphology, chlorophyll content, photosynthetic and respiration parameters of Gentiana straminea growing under different environmental conditions A/U W/U A/G W/G Leaf morphology Individual leaf size (cm2) 14.2 ± 0.7b 2 13.7 ± 1.1b b 12.9 ± 1.1ab ab 10.9 ± 0.5a 61.3 ± 4.9 a 55.0 ± 5.9 53.6 ± 3.7a 83.3 ± 3.2a Total leaf area per ramet (cm ) 69.5 ± 3.6 LMA (g/m2) 76.6 ± 2.9ab 77.4 ± 3.1ab 71.3 ± 5.1b 1.40 ± 0.10ab 1.19 ± 0.05a 1.52 ± 0.14b 1.26 ± 0.08ab a b 3.67 ± 0.06ab b Leaf biochemistry Chlorophyll (a+b) content (mg/FWg) b The ratio of chlorophyll a and b 3.71 ± 0.02 3.55 ± 0.05 b Carotenoid content (mg/FWg) 3.74 ± 0.04 a 0.34 ± 0.02 0.28 ± 0.01 0.37 ± 0.03 0.31 ± 0.01ab 15.8 ± 0.2a 15.9 ± 0.2a 16.1 ± 0.2a 16.1 ± 0.3a b Leaf physiology Optimal temperature for Amax (°C) −2 −1 15.1 ± 0.6 16.8 ± 1.0 16.9 ± 0.5b 11.4 ± 0.7a 14.3 ± 0.4ab 16.1 ± 0.8bc 17.0 ± 1.1c 1.76 ± 0.07a 1.91 ± 0.07a 2.41 ± 0.10b 1.98 ± 0.10a Amax at the optimal temperature (µmol m s ) 13.6 ± 0.2 Amax/R at the optimal temperature Q10 of dark respiration a ab LMA = Leaf mass per unit area; A/U = ambient temperature with un-grazed regime; W/U = warming treatment with un-grazed regime; A/G = ambient temperature with grazed regime, W/G = warming treatment with grazed regime. Data represent means ± standard error. Different lower case letters (a, b and c) indicate statistically significant differences between experimental treatments (Least significant difference multiple comparison, P < 0.05). Table 2: two-way analysis of variance (ANOVA) for estimated effects of warming and grazing on the morphological, biochemical and physiological parameters of Gentiana straminea F and (P) value of two-way ANOVA Warming Grazing Warming × Grazing Leaf morphology Individual leaf size (cm2) 2.34 (ns) 2 5.92 (0.016) 0.79 (ns) Total leaf area per ramet (cm ) 1.10 (ns) 5.74 (0.023) 0.54 (ns) Leaf mass per unit area (LMA, g/m2) 3.16 (ns) 0.01 (ns) 2.40 (ns) Chlorophyll (a+b) content (mg/FWg) 5.88 (0.032) 1.00 (ns) 0.06 (ns) The ratio of chlorophyll a and b 6.74 (0.023) 2.90 (ns) 1.06 (ns) Carotenoid content (mg/FWg) 12.16 (0.005) 3.25 (ns) 0.03 (ns) Leaf biochemistry Leaf physiology Optimal temperature for Amax (°C) 0.55 (ns) Amax at the optimal temperature (µmol m−2 s−1) 0.93 (ns) 12.06 (0.005) Amax/R at the optimal temperature 3.74 (0.077) 16.34 (0.002) Q10 of dark respiration 2.55 (ns) 17.02 (0.001) cold-insensitive species. Alpine plants have lower thermal acclimation compared with lowland plants (Atkin et al. 2006), and cold-acclimated crop species showed higher temperature homeostasis of photosynthesis than cold-sensitive species (Campbell et al. 2007; Yamori et al. 2009). Our study suggests that modelers may be able to predict temperature optimum of photosynthesis of alpine plants on the plateau without considering the effects of growth temperature if the average temperature changes within 1–2°C. 0.00 (ns) 0.15 (ns) 0.59 (ns) 0.55 (ns) 10.87 (0.006) Livestock grazing effects on the photosynthesis and its temperature response Our result indicates however that grazing significantly affected Amax at the optimal temperature and tended to reduce the relative effect of warming on the Amax (Tables 1, 2). Since G. straminea is a non-palatable forb and we measured fullsized healthy leaves, the differences in the photosynthetic capacity in plants between the grazed and un-grazed plots are not likely to be the direct effect of grazing. There are several 424 Journal of Plant Ecology indirect environmental factors that might have affected Amax. The most decisive effect of grazing was perhaps the change in growth irradiance. Leaves of G. straminea in the grazed plot received about three to eight times the PPFD received in the un-grazed plot (Figs 1a, b), which can also lead to a high photosynthetic rate, and a high Vcmax, but not necessarily Jmax. This is also supported by the results that plants from the grazed treatment tended to have ‘sun leaves’ with smaller leaf size and higher chlorophyll content compared with leaves from the un-grazed condition (Tables 1 and 2). Nitrogen availability could be another factor because sheep excrement and urine may increase soil N in the grazed plots. The increase of soil N can affect the photosynthetic performance, which may be responsible for the higher chlorophyll content in the grazed plots in the study. Livestock grazing alter the temperature response of respiration Figure 2: (a) Light-saturated photosynthetic rate (Amax) as a function of measuring temperature in Gentiana straminea having grown under ambient temperature with un-grazed treatment (A/U,○); under warming with un-grazed treatments (W/U, ● ); under ambient temperature with grazed treatment (A/G, △); and under warming with grazed treatment (W/G, ▲). Values represent mean ± standard error of four samples. The curves were fitted by two-dimensional polynomial function between Amax and measuring temperature. (b) Relative warming effect of Amax (RWEAmax) in plants with un-grazed (● ) grazed (▲) treatments. RWEAmax is the ratio of (Amax.w−Amax.a) /Amax.a, where Amax.w is the averaged Amax of 4 plants in the warming treatment and Amax.a is the averaged Amax of 4 plants in the ambient temperature treatment. The least significant difference comparison indicated a significant difference between the grazed and the un-grazed treatment (P < 0.05). Grazing altered temperature acclimation of dark respiration in leaves of G. straminea (Fig. 3; Table 1). Atkin and Tjoekler (2003) tried to distinguish two types of respiratory acclimation to temperature, with type I acclimation changing predominately in Q10 values, but nothing under low test temperatures and type II acclimation having respiration rate changes under all test temperatures (Atkin and Tjoelker 2003; Shen et al. 2009). In the current study, the temperature acclimation of respiration in the un-grazed regime appeared to be type II; that is, R was lower under warming conditions than under ambient conditions at all test temperatures though there was a large difference between individual plants, whereas Q10 was not significantly different between the ambient and warming treatments (Fig. 3a; Table 1). However, in grazed plots, Q10 was significantly lower under warming conditions than under ambient conditions, and thus temperature acclimation appears to have been type I. Although the mechanisms for the two types have not yet been clarified, a number of studies have shown that Q10 values Figure 3: dark respiration rate (R) as a function of measurement temperature in Gentiana straminea under warming or ambient conditions with un-grazed treatments (a) and warming or ambient conditions with grazed treatments (b). Mean ± standard error for four leaves of different ramets. Abbreviations and symbols are the same as in Fig. 2a. Shen et al. | Grazing alters warming effects on understory forb425 Figure 4: effect of temperature on the maximum rate of electron transport (Jmax, a, b) and the maximum rate of carboxylation (Vcmax, c, d) from un-grazed regimes (a, c) and grazed regimes (b, d). Data represent means ± standard error, n = 4. Asterisks indicate statistically significant differences of contrasting regimes for each measured temperature (Least significant difference comparison, *P < 0.05). are highest at high concentrations of respiratory substrates (e.g. Covey-Crump et al. 2002), whereas a similar response was observed in mitochondria isolated from soybean cotyledons (Atkin et al. 2002). The high Q10 values found in the grazed plots in our study can be explained by the fact that leaves receiving high levels of light have increased concentrations of mitochondrial protein per unit leaf area and mass (Noguchi et al. 2005), as well as increased substrate availability (AzcónBieto and Osmond 1983), and/or increased ATP turnover (Lambers 1985; Noguchi et al. 1996). However, some other studies have also shown that the Q10 values of leaf respiration are not dependent on growth irradiance and concurrent rates of photosynthesis (Bolstad et al. 1999; Hartley et al. 2006; Zaragoza-Castells et al. 2007). Conclusion and implication of the study In conclusion, this study indicates that livestock grazing can alter the effect of temperature elevation on leaf morphology and physiology of understory plants through changing light and other physical environments of these plants, implying the important consequences of change in plant community structure under climate change. Despite of extensive livestock grazing all over the Eurasian grasslands, we have little information to assess the effects of livestock grazing on the response of plant physiology to global warming in these grasslands. Our results first demonstrated the importance of livestock grazing on photosynthesis and respiration. The study suggests that we need to take the effects of livestock grazing into account in future assessments of the impacts of climate change on carbon cycle in grassland ecosystems. Further studies are needed to examine how different grazing intensities affect temperature response and acclimation of grassland species. Funding National Natural Science Foundation of China (31000177) and Sumitomo Foundation of Japan, a strategic JapaneseChinese Cooperative Program on ‘Climate Change’: Integrated assessment and prediction of carbon dynamics in relation to climate changes in grasslands on the Qinghai-Tibetan and Mongolian Plateaus, and the National Basic Research Program (2010CB833502). Acknowledgements We are grateful to Izumi Washitani and Nishihiro Jun for providing us with LI-6400 in the field measurement. We also thank Dr Song Gu, Dr Shengbo Shi, Dr Yingnian Li and Dr Xinquan Zhao for their valuable comments and assistance in this study. 426 References Alonso A, Pérez P, Martínez-Carrasco R (2009) Growth in elevated CO2 enhances temperature response of photosynthesis in wheat. Physiol Plant 135:109–20. Atkin OK, Bruhn D, Hurry VM, et al. (2005) The hot and the cold: unraveling the variable response of plant respiration to temperature. Funct Plant Biol 32:87−105. 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