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Dep. of Horticulture, Forestry, and Recreation Resources, Kansas State Univ., Manhattan, KS 66506-5506 USA
bhuang{at}oz.oznet.ksu.edu
| ABSTRACT |
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Abbreviations: LSD, least significance difference Pn, photosynthetic rate Rplant, Whole-plant respiration rate Rroot, root respiration rate TNC, total nonstructural carbohydrate
| INTRODUCTION |
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Photosynthesis is extremely sensitive to supraoptimal temperature and is often the first metabolic process that is damaged (Paulsen, 1994). Severe reduction in photosynthetic rate under supraoptimal temperature conditions has been observed in many plant species (Pearcy, 1977; Grover et al., 1986; Harding et al., 1990a, b; Wolf et al., 1990; Midmore and Prange, 1992; Stamps, 1994; Schwarz et al., 1997; Madsen and Brix, 1997; Huang et al., 1998a; Huang and Gao, 2000). Dark respiration rate often increases initially with increasing temperatures (Hansen and Jensen, 1977; Deal et al., 1990; Wolf et al., 1990; Ruter and Ingram, 1991; Huang et al., 1998a; Huang and Gao, 2000). However, the optimum temperature for photosynthesis is lower than that for respiration (Nilsen and Orcutt, 1996). Therefore, high temperatures may cause an imbalance between photosynthesis and respiration processes and carbohydrate depletion, particularly for creeping bentgrass that is mowed daily at low mowing height. Low mowing when temperature is high during summer imposes additional stress on the turf by removing large amounts of leaf area that are used for photosynthesis, while respiration continues (Huang et al., 1998a).
The present study was designed (i) to compare the differential effects of air vs. soil temperature on photosynthesis, respiration, and carbohydrate allocation and accumulation; and (ii) to determine whether heat stress injury to shoots from high air temperature or to roots from high soil temperature is related to alteration in carbohydrate metabolism in two cultivars of creeping bentgrass differing in heat tolerance. Previous studies (Huang et al., 1998a,b; Liu and Huang, 2000) demonstrated that L-93 is more heat tolerant than Penncross.
| Materials and methods |
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Shoots and roots were exposed to four air/soil temperature regimes: 20/20, 20/35, 35/20, and 35/35°C for 56 d. Constant day/night temperatures were tested mainly due to the difficulty of creating diurnal changes in soil temperatures using the water bath, although air and soil temperature always fluctuate in day/night rhythm. These test temperatures were chosen because 20°C is within the optimum range for the growth of cool-season grasses, and 35°C commonly occurs in warm climatic regions during mid-summer. Shoots were maintained at the ambient temperature (20 or 35°C) of the growth chambers, which was regulated by a temperature controller. Soil temperature was controlled by maintaining the entire root zone (40-cm-long soil column in a polyethylene bag) in water baths with predetermined temperatures (20 or 35°C). The low temperature was controlled by circulating cool water (1820°C), and the high temperature by using an immersion circulating heater (IC-2100, Fisher Scientific Inc. Pittsburgh, PA). The water was circulated continuously to maintain constant and uniform temperatures. Water levels were maintained at the top edge in each water bath during the experimental period.
Air temperatures at various distances from the canopy and soil temperatures at different depths from the soil surface were measured with thermocouples connected to a thermometer (Xu and Huang, 2000). In the 20/20°C treatment, both shoots and roots were maintained around 20°C; in the 20/35°C treatment, air temperature ranged from 23 to 25°C, and root-zone temperature was about 35°C; in the 35/20°C treatment, air temperature ranged from 32 to 35°C, while root-zone temperature ranged from 18 to 21°C; and in the 35/35°C treatment, air and root-zone temperatures were maintained at 33 to 36°C. Each temperature treatment was repeated in four water baths and growth chambers.
Temperature treatments were arranged in a completely randomized design with four replicates in repeated measurements randomly sampled each time (Kempthorne, 1952). Each of the two air temperatures (20 and 35°C) was replicated randomly in four growth chambers. High temperature and low temperature treatments were conducted sequentially in four chambers at each time. Each of two soil temperatures was replicated randomly in four water baths. Two water baths were placed in each growth chamber, with one being controlled at high soil temperature (35°C) and one at low soil temperature (20°C). All measurements were taken on four replicates sampled randomly from four chambers in each treatment at each measurement time. Effects of temperature and days of treatment (time) and their interactions were determined by analysis of variance according to the general linear model procedure of Statistical Analysis System (SAS Institute, Cary, NC). Differences between treatment means were determined by the least significance difference (LSD) test at the 0.05 probability level.
Canopy net photosynthetic rate (Pn) was measured from 1000 to 1400 h at various days of treatment using an LI-6400 portable gas exchange system (LI-COR Inc., Lincoln, NE). Dark respiration rates of the whole plant (shoots and roots) and soil (Rplant+soil), bare soil without grasses growing (Rsoil), and roots and soil (Rroot+soil) after detopping the shoots were measured during the night from 2000 to 2400 h with the LI-6400. The differences between Rplant+soil and Rroot+soil vs. Rsoil were used to estimate Rplant and Rroot as described in Biscoe et al. (1975) and Huang and Gao (2000). The Pn was expressed as CO2 uptake, and Rplant, and Rroot were expressed as CO2 evolution per unit canopy area, respectively. The amount of carbon consumed in respiration as a proportion of that produced in photosynthesis per day was calculated using the data of Pn and Rplant integrated over a 13-h photoperiod and an 11-h dark period, respectively. Daily carbon consumption to production ratio = (Rplant x 11)/(Pn x 13).
Total nonstructural carbohydrate (TNC) was determined using the method described by Ting (1959). Briefly, 20 to 50 mg oven-dried samples were transferred to 0.5 mL 0.1% clarase solutions and incubated at 38°C for 24 h. One milliters of hydrochloric acid (50%, v/v) then was added to the incubation solution. After the solution was incubated at room temperature for 18 h, 0.5 mL of 10 M NaOH solution was added. The pH value of the solution was adjusted to between 5 and 7 with 10 M NaOH solution. One milliliter of the solution was transferred to a 100-mL flask, and 5 mL of ferricyanide reagent was added. Then the flasks were placed in a boiling water bath for 10 min. After heating, the flasks were cooled quickly in running water. The solutions were neutralized partially with 10 mL of 1 M H2SO4 solution and mixed thoroughly until no more gas was evolved. Four milliliters of arsenomolybdate were added, and solutions were mixed again and then diluted to volume. The absorbance of the solution was measured at 515 nm with a spectrophotometer (Spectronic Instruments, Inc. Rochester, NY).
The carbon allocation pattern was determined using pulse 14CO2 labeling technique. Plants were enclosed in a clear plexiglass chamber (5 cm tall and 10 cm in diameter) and exposed to 7 µCi 14CO2 for 20 min. Excessive 14CO2 in the chamber was absorbed by bubbling the air in the chamber through a saturated NaOH solution for 10 min. Three days after labeling, shoots and roots were harvested, killed by exposure to 105°C for 15 min, and then dried in an oven at 75°C for 48 h. The samples were oxidized with a biological oxidizer (R.J. Harvey Instrument Corp., Hillsdale, NJ). 14C activities in shoots and roots were measured with a liquid scintillation analyzer (Packard, Deers Grove, IL) and the proportion of carbon allocated to roots was calculated.
| Results |
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Whole-Plant Respiration Rate (Rplant)
The Rplant at 20/35 and 35/35°C increased to above the control (20/20°C) level at 1 d of treatment and remained until 8 d for both cultivars (Fig. 2)
. The increase in Rplant within the first 8 d of treatment at 35/35°C was more dramatic for Penncross than for L-93. The Rplant decreased to below the control level after 35 d at both 20/35 and 35/35°C for Penncross but only at 35/35°C for L-93. The Rplant at 35/20°C was not significantly different from that at 20/20°C for either cultivar during the entire experimental period, but was lower than those at 20/35 and 35/35°C within 8 d of treatment for both cultivars. After 34 d of treatment, it was higher than those at 20/35 and 35/35°C for Penncross and higher than that at 35/35°C for L-93. At 35/35°C, L-93 maintained a lower respiration rate than Penncross during the first 8 d of treatment. At 20/35°C, L-93 had a higher respiration rate than Penncross after 34 d. Both cultivars had similar Rplant at 35/20 and 20/20°C. At 20/20 and 35/20°C, Pn was greater than Rplant; however, at 20/35 and 35/35, Rplant was higher than Pn for both cultivars (Fig. 1 and 2).
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Carbon-14 Allocation to Roots
The proportions of newly photosynthesized 14C allocated to roots of both cultivars were significantly lower than the control at 35/20 and 35/35°C after 23, 36, and 50 d of treatment and at 20/35°C after 23 and 36 d of treatment (Fig. 6)
. The proportion of carbon allocation to roots was higher at 35/20 than at 35/35°C for L-93 after 23, 36, and 50 d and for Penncross after 36 and 50 d, but was not different between 20/35 and 35/20°C. Specifically, an average of 25.0% of the total newly fixed 14C was allocated to roots for L-93 and 22.3% for Penncross at 20/20°C; 13% for L-93 and 12.0% for Penncross at 35/20°C; 13.5% for L-93 and 11.7% for Penncross at 20/35°C; and 3.7% for L-93 and 3.3% for Penncross at 35/35°C.
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| Discussion |
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The imbalance between carbon consumption and production and decreases in carbohydrate availability under high temperature conditions were caused mainly by the reduction in photosynthetic rate, because respiration rates were affected to a much lesser extent. Canopy Pn of both cultivars was reduced almost immediately after roots alone or both shoots and roots were exposed to high temperatures and declined rapidly to zero. Decreased Pn in response to supraoptimal soil temperatures also has been reported by others (Gur et al., 1972; Al-Khatib and Paulsen, 1984; Foster, 1986; Ruter and Ingram, 1992; Ziska, 1998). Such decreases in Pn could be due to the interruption of electron transport in photosystem II (Harding et al., 1990a); reduction in the activity of RuBP carboxylase (Grover et al., 1986; Ruter and Ingram, 1992); decreased chlorophyll content (Huang et al., 1998a); and leaf senescence caused by decreased cytokinin activity at elevated root-zone temperatures (Gur et al., 1972).
Respiration rate often increases with increasing temperatures (Ruter and Ingram, 1990, 1991; Huang and Gao, 2000). In our study, both Rplant and Rroot increased during the initial 8 d of exposure of roots alone or both roots and shoots to heat stress and then rapidly declined. However, Rplant was higher than Pn under either high soil or air/soil temperatures. Increased root respiration during the initial periods of heat stress may cause more consumption of carbohydrates. Increased soil temperature mainly elevates root maintenance respiration (Szaniawski and Kielkiewicz, 1982), which may result in insufficient carbohydrate levels needed for growth respiration and, thus, decreased growth (Gent and Enoch, 1983). The decreases in Rplant or Rroot after prolonged periods of heat stress may be due to limited carbohydrate availability and to the progressive degradation of enzymatic processes (Hurewitz and Janes, 1983).
Supraoptimal soil temperature alone or combined air/soil temperature inhibited 14C allocation to roots in both cultivars, as found in other species (Ruter and Ingram, 1990; Sattelmacher et al., 1990). The reduction in TNC content under high temperatures was also more severe for roots than for shoots. These results indicated that roots had lower priority than shoots when carbohydrates become limited during heat stress. Foster (1986) proposed that decreases in the amount of carbon allocated to roots when exposed to high soil temperatures was due to a physical blockage of the vascular system or to the loss of carbon as a result of increased root respiration rate. Less carbon allocated to roots and less carbohydrate in roots may result in the limited growth and death of roots that occur under high soil or air/soil temperature conditions in these two cultivars of creeping bentgrass (Xu and Huang, 2000). Schmidt and Snyder (1984) also reported TNC decreased as ambient temperatures were elevated in creeping bentgrass. However, Duff and Beard (1974) reported increased photosynthetic rate and increased level of ethanol and water-soluble sugars in creeping bentgrass with increasing temperatures. Both studies did not distinguish the effects of high soil temperature from high air temperatures.
Maintaining soil temperature at the optimum level while shoots were exposed to supraoptimal temperatures improved canopy Pn, reduced carbon consumption to production ratio, enhanced carbohydrate accumulation in roots, and increased carbon allocation to roots in both cultivars. Improved photosynthesis (Martin et al., 1989; Udomprasert et al., 1995b), more carbon allocation to roots (Ruter and Ingram, 1990), and delayed leaf senescence (Kuryanagi and Paulsen, 1988) in response to reduced soil temperature have been reported in several other species. In contrast, reducing air temperature while exposing roots to high temperatures had detrimental effects on carbohydrate metabolism. These results suggested that soil temperature was more important than air temperature in the regulation of photosynthesis, whole-plant or root respiration, and carbohydrate accumulation and partitioning.
In summary, this study clearly demonstrated that negative carbon balance and decreases in carbohydrate availability, especially decline in photosynthesis, contributed to the damage to shoots from high air temperatures or to roots from high soil temperatures. Moreover, roots played more important role than shoots in regulating carbohydrate metabolic responses to heat stress. Reducing soil temperature improved growth of creeping bentgrass under supraoptimal ambient temperatures (Xu and Huang, 2000), which could at least partially by maintaining a positive carbon balance.
| ACKNOWLEDGMENTS |
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Received for publication November 15, 1999.
| REFERENCES |
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