Published online 23 September 2005
Published in Crop Sci 45:2374-2382 (2005)
© 2005 Crop Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
CROP PHYSIOLOGY & METABOLISM
Physiological Limitations to Photosynthetic Carbon Assimilation in Cotton under Water Stress
Said Ennahlia and
Hugh J. Earlb,*
a Dep. of Crop and Soil Sciences, Univ. of Georgia, Athens, GA 30602-7272
b Dep. of Plant Agriculture, Univ. of Guelph, Guelph, ON, Canada N1G 2W1
* Corresponding author (hjearl{at}uoguelph.ca)
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ABSTRACT
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Water stress may reduce leaf net photosynthetic carbon assimilation (AN) through both stomatal effects, which reduce the leaf internal CO2 concentration (Ci), and nonstomatal effects, which result in reduced AN at a given level of Ci. However, the leaf gas exchange techniques used to calculate Ci are susceptible to important artifacts when applied to water-stressed leaves, making such Ci estimates unreliable. As an alternative to Ci, the CO2 concentration in the chloroplast (CC) can be calculated from simultaneous measurements of AN from gas exchange measurements, and the thylakoid electron flux from chlorophyll fluorometry. This permits diffusional effects (stomatal plus mesophyll limitations to CO2 diffusion) to be differentiated from chloroplast-level effects. We used this method to investigate physiological restrictions to photosynthesis in leaves of water stressed cotton (Gossypium hirsutum L.) plants in a series of greenhouse experiments. A null-balance lysimeter was used to slowly induce four distinct levels of water stress. Combined leaf gas exchange/chlorophyll fluorescence measurements differentiated the treatments more effectively than gas exchange measurements alone. All treatments reduced CC, but only the two most severe stress treatments significantly increased nondiffusional restrictions, detectable as a reduction in the slope of AN on CC. In a second experiment, recovery of leaf photosynthesis was determined 24 and 48 h after relief of a severe stress by rewatering. Recovery of the AN/CC relationship was substantial but incomplete after 24 h and did not recover further by 48 h after rewatering, indicating lasting chloroplast-level injury as a result of the stress. Similar experiments should be conducted under field conditions to determine if water stress results in irreversible chloroplast-level injury in field-grown cotton.
Abbreviations:
, leaf fractional absorption of incident PPFD AN, leaf net CO2 assimilation rate AG, leaf gross CO2 assimilation rate AN-C, leaf net CO2 assimilation rate corrected for sample chamber leakage AN-M, measured leaf net CO2 assimilation rate (uncorrected for sample chamber leakage) CA, ambient CO2 concentration CC, CO2 concentration at the carboxylation site in the chloroplast Ci, leaf internal CO2 concentration CS, CO2 concentration in the sample chamber DAP, days after planting
II, quantum efficiency of Photosystem II
II, fraction of absorbed PPFD absorbed by the antennae of Photosystem II FS, steady state chlorophyll fluorescence signal F'M, maximum (light saturated) chlorophyll fluorescence signal GL, sample chamber conductance to CO2 flux (leakage) GM, mesophyll conductance to CO2 in the liquid phase GS, stomatal conductance to water vapor IRGA, infrared gas analyzer Je, electron flux through Photosystem II KS, CO2/O2 specificity ratio of RubisCO L, leaf area in the sample chamber LRWC, leaf relative water content OC, oxygen concentration at the carboxylation site in the chloroplast PPFD, photosynthetic photon flux density RD, rate of leaf respiration in the dark RSWC, relative soil water content vC, velocity of the carboxylation reaction of RubisCO vO, velocity of the oxygenation reaction of RubisCO WD, pot plus soil dry weight WP, plant fresh weight WS, pot plus soil water saturated weight WT, pot target weight
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INTRODUCTION
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SOIL WATER DEFICITS constitute a primary limitation to crop productivity in many regions of the world. An enhanced mechanistic understanding of how water stress affects crop growth could benefit current efforts to create more drought tolerant crop cultivars (Turner, 1997) by identifying those specific traits that determine crop performance under water deficit conditions and which are amenable to alteration either through genetic transformation or conventional breeding approaches. Reduced photosynthetic carbon assimilation (and therefore reduced crop dry matter accumulation) is a principal effect of soil water deficit in cotton and other crops. At the level of the whole canopy, the effects of water deficits on cotton leaf area expansion and absorption of photosynthetically active radiation are easily measured and have been well documented (Turner et al., 1986; Puech-Suanzes et al., 1989; Ball et al., 1994). Water stress also affects the efficiency with which absorbed radiation is used to carry out carbon fixation at the leaf level, and the mechanisms by which this occurs have been the subject of many studies in a variety of species over the past three decades. There is now a broad consensus that stomatal closure and the consequent reduction in leaf internal CO2 concentration (Ci) are the major reason for reduced leaf photosynthetic rates under mild or moderate water stress (reviewed by Chaves, 1991; Cornic, 2000; Flexas et al., 2004). However, under severe water stress photosynthesis may also be restricted by nonstomatal effects, that is, inhibition or downregulation of photosynthesis at the level of the chloroplast, such that the net C assimilation rate (AN) is reduced at a given Ci. Since the early 1980s, many researchers have measured leaf gas exchange parameters and used some variation of the method developed by von Caemmerer and Farquhar (1981) to calculate Ci. In field studies with cotton, water stress has often been found to alter the relationship of AN to Ci, thus implicating nonstomatal effects in the suppression of photosynthesis (e.g., Ephrath et al., 1993; Faver et al., 1996). However, this method has been called into question because of important artifacts that can invalidate the gas exchange-based estimates of Ci in drought stressed leaves. First, the gas exchange equations used to calculate Ci rely on the assumptions that the diffusive pathways for water vapor and CO2 are the same, and that essentially all such diffusion occurs through the stomata. In water stressed leaves with very low stomatal conductance (Gs), these assumptions are not met, since under these conditions a significant fraction of total water vapor exchange may occur directly through the cuticle, and resistance to diffusion through the epidermalcuticular pathway is typically more than an order of magnitude greater for CO2 than for water vapor (Boyer et al., 1997). Since the gas exchange equations are seldom corrected for cuticular transpiration, Ci can be greatly overestimated when Gs is low (Kirschbaum and Pearcy, 1988; Meyer and Genty, 1998). Second, overestimation of Ci also occurs if water stress results in heterogeneous ("patchy") stomatal closure (Downton et al., 1988; Meyer and Genty, 1998). In either case, overestimation of Ci may lead to the erroneous conclusion that water stress has resulted in increased nonstomatal limitations to photosynthesis.
More recently, combined measurements of leaf gas exchange and chlorophyll fluorescence have been used to investigate the involvement of nonstomatal effects in limiting photosynthesis under water stress. Dai et al. (1992) and Sánchez-Rodríguez et al. (1999) found that the ratio of Photosystem II efficiency (
II, from chlorophyll fluorometry) to AN increased as Ci decreased. They established the relationship between Ci and
II:AN under water-replete conditions (where gas exchange-based estimates of Ci are reliable), and then used it to estimate Ci in water stressed leaves from measurements of AN and
II alone. In both of these studies, putative increases in nonstomatal limitations were indicated by the traditional analysis of the AN/Ci relationship but not when Ci was determined from the
II/AN ratio. A related approach is to calculate the CO2 concentration at the carboxylation site in the chloroplast (CC) from (i) estimates of the thylakoid electron flux (Je) from chlorophyll fluorescence and (ii) gas exchange-based measurements of AN and dark respiration (RD) (Epron et al., 1995; Lal et al., 1996; Flexas et al., 2002; see Materials and Methods for relevant theory). Again, such studies have generally found a stable relationship between AN and CC, indicating little or no involvement of increased limitations at the chloroplast level in restricting photosynthesis under water stress, even when the AN/Ci relationship suggests that such effects are present (Lal et al., 1996; Flexas et al., 2002; Cornic and Fresneau, 2002). Only under very severe stress (AN reduced by more than 80%) are chloroplast-level effects typically observed (Flexas et al., 2004).
It is possible for CC to be reduced by water stress even when Ci is not affected, since recent evidence suggests that the resistance to diffusion of CO2 in the mesophyll (i.e., in the liquid phase from the substomatal cavity to the carboxylation site in the chloroplast) may also be increased by severe water stress (Flexas et al., 2004). Examination of the AN/Ci relationship (when Ci estimates are reliable) permits differentiation between stomatal and nonstomatal limitations, while examination of the AN/CC relationship permits differentiation between total diffusional (stomatal plus mesophyll) and nondiffusional (chloroplast-level) limitations.
The first objective of the present work was to use combined leaf gas exchange and chlorophyll fluorescence measurements to quantify chloroplast-level limitations to photosynthesis in cotton leaves under four different levels of water stress. Small differences in photosynthetic activity under very severe water stress are not likely to result in important differences in crop productivity, since only a minor fraction of total seasonal C assimilation typically occurs under severe stress conditions. However, the extent of recovery of photosynthetic capacity following relief of a severe soil water deficit may be an important determinant of subsequent growth and productivity. Accordingly, in a second experiment, a severe water stress treatment was imposed, and then the extent of recovery of the resulting limitations to photosynthesis was determined 24 and 48 h following relief of the stress by rewatering.
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MATERIALS AND METHODS
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Plant Material
Experiments were conducted in a greenhouse in Athens, GA, USA (34°N, 84°W). Cotton (cv. Delta Pearl) plants were grown in 2.5-L plastic food containers (Berry Plastics Corp., Evansville, IN) with drainage holes added. The soil was a Pacolet sandy loam (a member of the clayey, Kaolinitic, thermic family of Typic Hapludults) amended with sand to a texture of 800 g kg1 sand, 120 g kg1 silt, and 80 g kg1 clay. The pots were filled with 3300 g of soil. Seeds were sown five to a pot in February 2003 (Exp. 1) or April 2003 (Exp. 2) and fertilized with 50 mL of a 0.8% (w/v) solution of 20-20-20 (%N, P and K as N, P2O5 and K2O equivalents) fertilizer plus micronutrients (Miller Greenhouse Special, Miller Chemical and Fertilizer Co. Corp., Hanover, PA). Cotyledons were expanded and horizontal at 10 to 12 d after planting (DAP); at this time, plants were thinned to one per pot, and an additional 50 mL of fertilizer solution was added twice weekly thereafter. Air temperatures were maintained at 27 ± 4°C during the day and 20 ± 2°C during the night. Photoperiod was extended to 16 h with overhead 400-W metal halide lamps that produced a supplemental photosynthetic photon flux density (PPFD) of approximately 230 µmol m2 s1 at the tops of the plants. To prevent water stress during the initial growth stages, water was maintained at between 55 and 85% of soil water holding capacity by daily weighing and watering of the pots until water stress treatments were begun at between 35 and 45 DAP.
Relative Soil Water Content and Soil Water Holding Capacity
Before planting, soil water holding capacity was determined by watering two extra pots to excess, capping them with plastic lids, then allowing them to drain until reaching a constant weight (the saturated weight, WS). The soil was then dried in an 80°C forced air dryer until it had reached constant weight, and the pot dry weight (WD) was taken as the sum of the soil dry weight, the pot weight and the lid weight. Relative soil water content (RSWC) was calculated as:
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where WP is an estimate of plant fresh weight from destructive harvest of roots and shoots of two extra plants per experiment just before beginning the water stress treatments.
Water Stress Treatments
Water stress treatments were imposed with a 16-balance gravimetric lysimeter and computer controlled watering system, which is described in detail by Earl (2003). Each pot sat on an electronic balance, and its weight was monitored continuously by a computer. Whenever plant transpiration caused the weight of a pot to decline by 15 g below the target weight for that pot at that point in the experiment, the computer activated a solenoid valve, allowing water to flow to that pot via vinyl tubing until the pot weight was 15 g above its target weight. The target weight (WT) for each balance was calculated by the computer software as:
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where RSWC is the target relative soil water content expressed as a fraction between 0 and 1. New target RSWC values for each balance were entered manually on a daily basis as required by the experimental protocol.
In Exp. 1, four pots were randomly assigned to each of four treatments: well watered (75% RSWC), mild water stress (25% RSWC), moderate water stress (15% RSWC), and severe water stress (5% RSWC). The automated watering system was programmed to permit soil water to decline by a maximum of 10% RSWC per day because of transpiration; once a pot weight had declined by this amount in a single day, its weight was maintained within 15 g (approximately 2.5% RSWC) of the target weight for the rest of the day. Similarly, when a pot had reached its target final weight range, the watering system maintained it within 15 g of that weight (Fig. 1)
. Once the "severe water stress" pot reached its final weight (usually actually about 10% RSWC, near the lower limit of transpirable soil water) and had been maintained there for one day, physiological parameters were measured for all four treatments in that replication.

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Fig. 1. Relative soil water content vs. time for the control treatment (75% RSWC) and three water stress treatments in Exp. 1 (top) and for the control, stress, and two recovery treatments in Exp. 2 (bottom). Each trace represents typical data for a single pot.
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Experiment 2 was conducted to investigate the time course of recovery of leaf physiological parameters on relief of the water stress by rewatering. Two of the treatments were the same as for Exp. 1control (75% RSWC) and severe stress (5% RSWC). The two recovery treatments were severe stress followed by 1 or 2 d of recovery (rewatered to 75% RSWC 24 or 48 h before physiological measurements were made). Within a replication, the drought stress simulation protocol for the different stress and recovery treatments were begun on different days so that the physiological measurements could be made on all four plants on the same day (Fig. 1). This experiment was conducted twice, with four replications the first time and three replications the second time.
For both Exp. 1 and Exp. 2, the drought stress protocols were initiated sequentially for the different replications so that physiological measurements were made on only one replication per day. The measurement day was between 44 and 47 DAP in Exp. 1 and between 49 and 58 DAP in Exp. 2, depending on the replication. The four pots within a replication were also grouped together on four adjacent lysimeter balances, in a randomized complete block design.
Gas Exchange and Fluorescence Measurements
Fluorescence measurements were made on the second youngest fully expanded leaves with two Portable Photosynthesis Systems (Model LI-6400, LI-COR Inc., Lincoln NE) each fitted with a Leaf Chamber Fluorometer (Model LI-6400-40). At the beginning of each measuring day, the infrared gas analyzers (IRGAs) of the LI-6400 were calibrated as per the manufacturer's instructions, and the fluorometer signal offset was zeroed. The flow rate of air through the sample chamber was set at 250 µmol s1, and leaf temperature was maintained at 27 ± 0.8°C by the chamber thermoelectric coolers. The sample chamber CO2 concentration was adjusted to 360 µL L1 with the system's CO2 injector (Model 6400-01, LI-COR).
The modulation frequency of the fluorometer measuring light was 10 kHz under actinic illumination and increased to 20 kHz during saturating pulses. The measuring light intensity was set to Level 10, and the gain setting was 20. For determination of the steady state fluorescence signal under actinic illumination (FS), the sampling rate was 0.5 Hz, but this was increased to 20 Hz for determination of the maximum fluorescence signal
during saturating pulses. Pulse duration was 0.8 s, which was determined in preliminary experiments to be adequate to achieve the apparent F'M.
Each leaf was dark adapted for approximately 45 min before introducing it into the measurement chamber. Once inside the chamber additional time was allowed so that leaf temperature, stomatal conductance, and leaf CO2 exchange reached steady state. At this point, net CO2 efflux from the leaf was recorded as an estimate of dark respiration (RD), and then incident PPFD was set to 1500 µmol m2 s1, with approximately 90% of the actinic light provided by the fluorometer's red LEDs and 10% by the blue LEDs. The leaf was allowed to achieve steady state GS and AN at a chamber CO2 concentration of 360 µL L1 (standard conditions) before making the first fluorescence measurements. Then, measurements were made at different chamber CO2 concentration [produced by using reference side (incoming) CO2 concentrations of 50, 100, 200, 400, 500, 700, 1000, 1500, 2000, and 2400 µL L1]. At each level of CO2 concentration, sufficient time was allowed for the leaf to reach a steady state AN, then leaf gas exchange data were recorded and FS and F'M were determined three times, using three saturating pulse intensity settings (4, 6, and 10) applied in random order. Three pulse intensities were used because previous work had shown that apparent F'M determined with a single pulse of intensity 10 underestimated the true F'M with this instrumentation under similar experimental conditions (Earl and Ennahli, 2004). A linear regression of apparent F'M on 1/PPFD during the saturating pulse provided an estimate of the true F'M for each measurement (Fig. 2)
(Markgraf and Berry, 1990; Earl and Ennahli, 2004). Simultaneously with leaf gas exchange measurements, the CO2 concentration of the air in the vicinity of the measurement chamber was determined with another IRGA (Model 6200, LI-COR). The entire work area was well ventilated with an electric fan to prevent large fluctuations in CO2 concentration external to the chamber.

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Fig. 2. Determining the true light saturated F'M by the three-pulse method. Apparent F'M was determined for three 0.8-s pulses of different PPFD, then the light-saturated F'M (at infinite PPFD) was estimated as the intercept of the linear regression of apparent F'M on the inverse of PPFD during the pulse. Example data are shown for leaves from each of the three water stress treatments in Exp. 1. Actinic PPFD during the measurement was 1500 µmol m2 s1 in every case.
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Leaf Water Status and PAR Absorption
In Exp. 1, leaf relative water content (LRWC) and leaf water potential were determined for the same leaves used for gas exchangefluorescence measurements as soon as the measurements were completed. Three 2-cm diameter leaf disks were extracted and their fresh weight was determined. They were then submerged for 24 h at room temperature in distilled water to determine their turgid weight, then dried over 24 h at 80°C to determine their dry weight. LRWC was calculated as
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An additional five 1-cm diameter leaf disks per leaf were extracted and used to determine leaf water potential according to Brown and Bartos (1982) with thermocouple psychrometers (Wescor Inc., Logan, UT).
Leaf absorption of incident PPFD (
) was determined for each leaf with an LI-1800-12S external integrating sphere (LICOR) connected to a reflectance spectrometer (Unispec, PP Systems, Haverhill, MA). Leaf transmittance and reflectance measurements were made at 3.6-nm intervals between 400 and 700 nm, and
of the actinic light in the LI-6400 chamber was calculated as described by Earl and Tollenaar (1997).
Calculations and Data Analysis
Measurements of AN were corrected for leakage of CO2 across the leaf chamber gasket as
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where AN C and AN M are the leakage corrected and apparent (measured) leaf net CO2 assimilation rates, respectively, with units of µmol CO2 m2 s1, GL is a CO2 leakage coefficient for the chamber determined in preliminary experiments (2.5 x 107 mol s1, data not shown), L is the leaf area in the chamber (2.0 x 104 m2), and CS and CA are the sample chamber and external (ambient) CO2 concentrations, respectively, with units of µmol CO2 mol1 air. This correction was minor when AN was high or when CS CA was small. However, it constituted a substantial fraction of apparent AN for water stressed leaves when CS was very high or very low compared with CA. Values of Ci were also recalculated from the leakage corrected values of AN. Hereafter all mention of AN, RD, and Ci refers to leakage corrected estimates.
Mitochondrial respiration of illuminated leaves was assumed to be equal to RD, and so gross CO2 assimilation (AG) was estimated as AN + RD. Quantum efficiency of Photosystem II (
II) was estimated according to Genty et al. (1989) as
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and thylakoid linear electron flux (Je) was then calculated as
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where
II is the fraction of absorbed PPFD absorbed by the antennae of Photosystem II (Loreto et al., 1994). A value of 0.45 was used for
II (Earl and Ennahli, 2004). Assuming that four electrons are consumed per carboxylation or oxygenation of RuBP by RubisCO and that electron flux to alternate sinks is negligible,
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where vC and vO are the rates of carboxylation and oxygenation, respectively. A release of 0.5 CO2 is expected per oxygenation event, so
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Combining these last two equations shows that vC/vO may be estimated from measurements of AG and Je as
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The value of CC was then calculated following Lal et al. (1996) as
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where OC is the partial pressure of oxygen at the carboxylation site, assuming a negligible O2 concentration gradient between the atmosphere and the carboxylation site (Gerbaud and André, 1987), and KS is the CO2/O2 specificity of RubisCO, adjusted for leaf temperature (Woodrow and Berry, 1988). This method considers both OC and CC in gas-phase equivalents, rather than the actual dissolved concentrations at the carboxylation site, thus making the CC values more conveniently comparable to Ci values. That is, the temperature correction of KS adjusts for temperature effects on both RubisCO CO2/O2 specificity and CO2 and O2 solubility.
Preliminary analysis revealed that the relationship between AN and CC remained linear up to a CC value of 150 µL L1 for all treatments. The initial slope of this relationship was determined for each leaf via regression analysis, making use only of data for which CC was below 150 µL L1. Analysis of variance was used to determine significant (P < 0.05) treatment effects on LRWC, leaf water potential, the initial slope of the AN/CC curve, RD, leaf absorption of PAR, and (at standard conditions and steady state), GS, AN, Ci,
II, Je, vC/vO, and CC. Treatment means were separated by a protected LSD test at the P = 0.05 probability level.
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RESULTS
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In Exp. 1, both leaf water potential and LRWC declined as RSWC decreased, and in the case of leaf water potential, all four RSWC treatments differed significantly from one another (Table 1). There was a strong linear relationship between LRWC and leaf water potential across the four treatment means (R2 = 0.97; regression not shown). Relative to the control treatment (75% RSWC), mild water stress (25% RSWC) did not produce statistically significant decreases in AN and GS, but the more severe stresses (15 and 5% RSWC) reduced both AN and GS to near zero (Table 1). The mild stress also did not produce statistically significant changes in
II and Je, but when Je and AN were used to calculate vC/vO, this ratio was significantly lower in the mild stress treatment than in the control. The two most severe stress treatments greatly suppressed
II, Je, and vC/vO relative to the control and mild stress treatments, and
II and Je were significantly lower in the 5% RSWC treatment than the 15% RSWC treatment (Table 1). RD and
averaged 1.4 µmol m2 s1 and 0.89, respectively, and were not significantly affected by the treatments (data not shown).
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Table 1. Effect of relative soil water content (RSWC) on leaf water potential ( l), leaf relative water content (LRWC), net CO2 assimilation rate (AN), stomatal conductance (GS), calculated leaf internal CO2 concentration (Ci), quantum efficiency of Photosystem II ( II), electron flux through Photosystem II (Je), the ratio of carboxylation to oxygenation of ribulose bisphosphate by RubisCO (vC/vO), the calculated CO2 concentration at the carboxylation site (CC), and the slope of AN on CC in Exp. 1. Measurements were made between 44 and 47 d after planting, depending on the replication.
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Estimates of Ci appeared to be inaccurate under the two most severe stress treatments in Exp. 1 with, for example, extremely large values often being calculated. This large variation prevented significant treatment effects on Ci from being detected (Table 1). By contrast, calculated CC was significantly lower for the mild water stress treatment than the control treatment and was also significantly lower in the two most severe stress treatments than in the mild stress treatment (Table 1). When the sample chamber CO2 concentration was varied to produce a range of Ci, the control and mild stress treatments generally showed the expected smooth, curvilinear relationship between AN and Ci. However, the 5% RSWC treatment rarely showed such a smooth AN/Ci curve, since the Ci estimates were highly variable and appeared to be inaccurate (Fig. 3)
. By contrast, all treatments generally produced smooth curves when AN was graphed against CC (Fig. 3).

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Fig. 3. Examples of the relationship between AN and Ci (top) and AN and CC (bottom) for each of the four water stress treatments in Exp. 1.
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The initial slope of AN/CC did not differ between the 75 and 25% RSWC treatments but was significantly reduced by the 15% RSWC treatment. Also, the most severe stress treatment reduced the AN/CC slope significantly relative to the 15% RSWC treatment (Table 1).
In general, leaf photosynthetic activity of control plants, as measured by AN, Je, and the slope of AN/CC was higher in Exp. 2 than in Exp. 1 (compare Tables 1 and 2). Also, the 5% RSWC treatment seemed to be somewhat less severe in Exp. 2, as evidenced by the slightly larger values of AN and GS. As in Exp. 1, the 5% RSWC treatment in Exp. 2 produced highly variable estimates of Ci, and significantly reduced
II, Je, vC/vO, CC, and the initial slope of AN/CC. Rewatering produced substantial recovery of most parameters after 24 h, but AN,
II, Je, and AN/CC remained significantly depressed relative to control plants. By contrast, CC and vC/vO did not differ from controls 24 h after rewatering. There was no significant change in any measured parameter between 24 and 48 h after rewatering (Table 2). As in Exp. 1, RD and
were unaffected by the treatments in Exp. 2 (average values of 1.6 µmol m2 s1 and 0.89, respectively; data not shown).
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Table 2. Net CO2 assimilation rate (AN), stomatal conductance (GS), calculated leaf internal CO2 concentration (Ci), quantum efficiency of Photosystem II ( II), electron flux through Photosystem II (Je), the ratio of carboxylation to oxygenation of ribulose bisphosphate by RubisCO (vC/vO), the calculated CO2 concentration at the carboxylation site (CC), and the slope of AN on CC under control conditions (75% RSWC), severe water stress (5% RSWC) and 24 and 48 h after rewatering severely water stressed plants in Exp. 2. Measurements were made between 49 and 58 d after planting, depending on the replication.
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DISCUSSION
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On the basis of gas exchange measurements alone (AN and GS), the four water stress treatments in Exp. 1 appeared to produce only two statistically distinct classes of stress level, with the 75 and 25% RSWC treatments comprising one class and the 15 and 5% RSWC treatments the other. However, measurements of leaf water potential indicated four distinct stress levels. In addition, combined gas exchange and chlorophyll fluorescence measurements indicated that the 25% RSWC treatment produced a lower CC (and therefore a lower vC/vO) than the control treatment. This difference in CC could be detected even though differences in GS and Ci were not statistically significant (even when the data from the 15 and 5% RSWC treatments were removed from the ANOVA, there was still no significant treatment effect on Ci; data not shown). The two most severe stress treatments were also indistinguishable from one another on the basis of gas exchange data only but were shown to be physiologically distinct on the basis of (i) a lower Je and (ii) a reduced AN/CC slope in the 5% RSWC treatment than the 15% RSWC treatment (Table 1). Both of these treatments reduced AN by more than 95%. Such severe stress is often associated with chloroplast level effects that cannot be attributed to reduced CC (Medrano et al., 2002; Souza et al., 2004), as also indicated here by the significantly reduced AN/CC slope relative to the control.
In total, the results of Exp. 1 are consistent with the model suggested by Medrano et al. (2002), where mild stress reduces AN through its effects on CC, resulting in increased photorespiration (decreased vC/vO) but no reduction in Je or carboxylation efficiency (AN/CC). As stress becomes more severe and CC declines further, Je and carboxylation efficiency are also suppressed (Medrano et al., 2002).
Thus, there were both diffusional and nondiffusional components to the suppression of photosynthesis under severe stress in Exp. 1, and this was observed again in the 5% RSWC treatment in Exp. 2 (Table 2); the 5% RSWC treatment significantly reduced both CC and AN/CC. Upon rewatering, only the nondiffusional component remained, since CC recovered completely, but AN/CC was still significantly suppressed (Table 2). The reduction in AN/CC under water stress should not necessarily be considered indicative of injury to the photosynthetic apparatus, since it might simply represent downregulation of photosynthetic capacity that is appropriate given the reduced availability of CO2 in the chloroplast (Escalona et al., 1999). However, the lasting effect of water stress on AN/CC observed even 48 h after rewatering (Table 2) can only be seen as loss of photosynthetic function at the chloroplast level, although the exact nature of this apparent injury is not clear. Souza et al. (2004) found that water stress promoted accumulation of soluble sugars in Vigna unguiculata (L.) Walp. leaves, suggesting the possibility of an end product inhibition of photosynthesis. However, that inhibition was completely relieved within a few days of rewatering, unlike what was observed in the present work. It would be of interest to make similar measurements of AN/CC on field-grown cotton to see if levels of water stress in the field comparable to those in the present work (near zero GS, severe leaf wilting, LWRC below 70%) would also result in a lasting inhibition of AN and AN/CC or if recovery would be complete on rewatering.
As discussed above, estimates of Ci based on leaf gas exchange measurements are generally considered to be unreliable under conditions of severe water stress when GS is very low. However, it should be noted that a relatively high Ci concurrently with a low CC is not always indicative of a poor Ci estimate. A large Ci:CC ratio can also arise when the conductance to diffusion of CO2 in the mesophyll from the substomatal cavity to the carboxylation site in the chloroplast (GM) is very low. Recent results suggest that GM is determined by an enzymatic process (Bernacchi et al., 2002) and can be reduced by water stress (Flexas et al., 2004). Such a decrease in conductance to CO2 diffusion in the mesophyll would constitute a nonstomatal limitation to photosynthesis but would not directly affect the AN/CC slope. The reduced AN/CC slope observed in the present work indicates a chloroplast level limitation to photosynthesis, not an increased resistance to diffusion in the mesophyll.
We observed that AN/Ci curves tended to be erratic under water stress, while AN/CC curves were more consistent (e.g., Fig. 3). Besides the two different artifacts already discussed that can cause Ci to be overestimated under water stress, calculated Ci is also very sensitive to small errors in the estimate of AN; when AN is understimated (for instance, because of random IRGA noise), the gas exchange calculations produce an overestimate of Ci and vice versa. This amplification of the original error further reduces the quality of the data and increases error variance in the AN/Ci curve. By contrast, calculated values of CC are increased by overestimates of AN and decreased by underestimates of AN. The effect is that AN/CC data tend to be "self correcting," producing artificially smooth curves.
In conclusion, combined measurements of leaf gas exchange and chlorophyll fluorescence revealed that levels of water stress that appeared to be similar on the basis of leaf gas exchange measurements only were actually physiologically distinct. Mild stress produced measurable reductions in vC/vO and CC, even though AN was not significantly affected. This was consistent with a reduced availability of CO2 at the carboxylation site because of reduced GS (and possibly GM); there was no evidence of inhibition of photosynthesis at the level of the chloroplast. By contrast, under severe stress both diffusive limitations and chloroplast-level limitations were increased, as evidenced by a reduced CC and a reduced AN/CC slope, respectively. Rewatering of severely stressed plants completely reversed the diffusive limitation (CC returned to control levels), but AN/CC did not recover completely and AN continued to be significantly reduced relative to control plants because of a lasting chloroplast-level inhibition.
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NOTES
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This research was funded by the USDA NRI Plant Responses to the Environment Program, and by state and Hatch funds allocated to the Georgia Agric. Exp. Stn.
Received for publication February 15, 2005.
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REFERENCES
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