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a Harvard University, Department of Organismic and Evolutionary Biology, The Biological Laboratories, 16 Divinity Avenue, Cambridge, Massachusetts 02138
| ABSTRACT |
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Key Words: incongruency of resources; diurnal cycles gaps Polygonaceae Rumex crispus photosynthesis water use efficiency
| INTRODUCTION |
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Light environments near the soil surface vary considerably in intensity, duration and temporal availability at different positions within a forest gap (Canham and Marks, 1985; Denslow, 1987; Canham et al., 1990). In tall herbaceous vegetation, such as in old fields, a similar pattern of light variation occurs within gaps (McConnaughay and Bazzaz, 1987). Diurnal movements of direct beam radiation are most significant on the east-west axis of a gap (Bazzaz and Wayne, 1994). In northeastern North America, northwest portions of large gaps receive direct beam radiation 2.02.5 h earlier than northeast portions, although both receive similar daily total photosynthetic photon flux density (PPFD) (Canham et al., 1990; Bazzaz and Wayne, 1994; Sipe and Bazzaz, 1995).
Likewise, CO2 concentrations at various distances above the soil surface have been shown to have distinct diurnal patterns in herbaceous environments (Schwartz and Bazzaz, 1973) and in forest environments (Bazzaz and Williams, 1991; Thomas and Bazzaz, 1993). We have found that empirical measurements of CO2 profiles in various understory and gap environments at the Harvard experimental forest indicate that peak values of CO2 in midsummer at or near the soil surface are reached in the early morning, while significantly lower concentrations occur in the early afternoon (P. B. Voss, unpublished data). At opposite sides of a gap, variations in the timing of high light may result in different degrees of temporal incongruency with the diurnal fluctuations of CO2 (Wayne and Bazzaz, 1993).
This study addressed the question of how the incongruent availability of resources affects plants early in their development. We were specifically interested in the effects of diurnal incongruency of peak values of light and carbon dioxide. We created four treatments simulating the west and east sides of a gap and two controls. In all treatments, plants were exposed to high light for 3 h either in the morning or afternoon and low light the rest of the day, with a total photoperiod of 14 h (see Fig. 1). In two of the treatments, CO2 concentration followed a sinusoidal curve over a 24-h period reaching a maximum of 800 ppm in the morning and a minimum of 400 ppm in the afternoon. In the control treatments CO2 concentration was held constant at 600 ppm so that all treatments would have the same mean CO2 concentration. The first treatment simulated the west side of a gap with peak light in the morning and peak CO2 in the morning (hereafter called AM diurnal). The second treatment simulated the east side of a gap with peak light in the afternoon and peak CO2 in the morning (hereafter called PM diurnal). The two control treatments had peak light in the morning and afternoon, respectively, but steady-state values of CO2 across the day (called AM steady-state and PM steady-state). Using a model species, Rumex crispus, an early successional plant which can be found in herbaceous gaps and occasionally in large forest gaps, we tested several predictions: (1) diurnal timing of optimal levels of light and CO2 will affect carbon assimilation, growth patterns, and water use efficiency of plants; (2) plants that receive high levels of light and CO2 incongruently will assimilate carbon at lower rates, show reduced growth, and have lower water use efficiency relative to plants which receive resources congruently; and (3) the rank order of performance among the different treatments will be AM diurnal > AM steady-state > PM steady-state > PM diurnal.
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| MATERIALS AND METHODS |
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We developed a bench-top environmental control system with four treatments in a fully crossed design of two CO2 regimes and two light regimes. Treatments were replicated in three blocks with a total of 40 seedlings. Seedlings were exposed either to diurnal fluctuations in CO2 concentration or to a constant CO2 concentration. The constant CO2 treatment was 600 ppm (± about 15 ppm). The diurnal fluctuations followed a sine curve with a mean of 600 ppm, reaching a maximum of 800 ppm at 0600 and a minimum of 400 ppm at 1800 (see Fig. 1). The shape and phase of this diurnal pattern were designed to simulate the forest floor environment at ~15 cm above the soil surface at the Harvard Forest in Petersham, Massachusetts, in several sites representative of where R. crispus is often found (P. B. Voss and F. A. Bazzaz, unpublished data). The amplitude of our treatment cycle, however, is somewhat larger than the amplitude of a typical diurnal cycle in the field (maximum 600700 ppm, minimum 370450 ppm). Given the subtlety of our treatments, we opted to increase this amplitude in order to amplify the potential treatment effect.
Within each of the CO2 regimes were two light treatments. One group of plants received 3 h of direct light (850 µmol·m·s high-intensity discharge lamps) in the morning (08001100), while the other group received 3 h of direct light in the afternoon (13001600). All plants received diffuse light (~55 µmol·m·s) during the remaining daytime hours. These lower light levels were designed to approximate the understory light conditions at the Harvard Forest (Bazzaz and Wayne, 1994). All four treatments received the same total photosynthetic photon flux density (PPFD) and the same mean CO2 concentration during daylight hours. Relative humidity (RH) and temperature conditions (25°C, 6070% RH) were identical for all treatments.
Our system was based on an "open" design in which fresh air was drawn continuously from a roof-top tower (with an intake at 15 m above roof level), humidified, and washed with distilled water, injected with CO2, and supplied to all chambers. The chambers themselves consisted of acrylic plastic aquariums (25 x 15 x 15 deep). Each pair of these chambers (one diurnal CO2 and one steady-state CO2) was placed inside a plastic bin containing circulating water at a controlled temperature. The water circulation and temperature control system was common to all chambers, minimizing the among-treatment variance. Air flowing into each chamber first passed through a 1-m copper pipe immersed in the water bath. This temperature equilibration, in combination with the controlled chamber wall temperature, allowed for excellent environmental control. Air temperature, humidity, and light levels were measured once per minute. While air temperatures drifted above their set points during high-light periods, the effect was common to all treatments, and in many ways is an accurate representation of field conditions.
Because of the complexity of CO2 control, we created only two CO2 treatments (diurnal and steady-state), and divided the flow equally among the chambers. CO2 concentrations were measured every 60 s inside representative growth chambers and were used in feedback loops to control the rate of CO2 addition to the two airstreams. The time constant (chamber volume/air flow rate) was <4 s, and air was distributed evenly using a bottom plenum. We rotated our CO2 treatments every 3 d so that the steady-state mixing volume for one period was changed to the diurnal mixing volume during the next. Since each mixing volume remained attached to the same set of six chambers, plants were moved to follow their treatment each time the CO2 control was changed. This rotation eliminated any potential mixing volume effects. Independent CO2 and relative humidity measurements using a LI-COR 6200 gas analyzer (LI-COR, Lincoln, Nebraska) confirmed that the CO2 concentrations in all of the chambers matched the programmed values and that RH was uniform within and across chambers.
Seeds from one population, collected in Cambridge, Massachusetts, were broadcast on the soil surface in 6.0 cm diameter peat pots containing Redi-Earth Peat Lite Mix(TM) potting soil. All seeds were germinated in the same light and CO2 conditions (~500 µmols·m·s and 350 ppm). To improve chances of uniform starting biomass, germinants were thinned to two plants per pot 5 d after planting, and all additional germinants were removed on a daily basis. In two of the blocks, three individuals were placed in each chamber; in one block, four individuals were placed in each chamber. All plants were given a total of 2.77 mg of Peter's Solution (20:20:20 NPK) diluted in 50-mL H2O aliquots per plant per week.
Physiology and growth
Two weeks after exposing plants to treatment conditions we measured photosynthetic and conductance rates to trace diurnal patterns of carbon assimilation and stomatal control. Using a LI-COR 6200 photosynthesis system, we measured specific leaves for three individuals from each treatment, one from each block, at seven time intervals throughout the day. CO2 and light levels were carefully monitored during gas exchange measurements to ensure that they matched set treatment values. CO2 concentrations were within 10 ppm of the set value. The first of three observations from the LI-COR 6200 was used in all cases unless the first observation was faulty. This minimized the problem of declining CO2 partial pressures within the cuvette during measurements. Care was taken to maintain the leaves in the horizontal plane (the plane in which they were growing) during measurements. This ensured a light environment inside the cuvette within 5 µmol·m·s of the target value. The measurement at 0700 is missing for one plant each in the AM diurnal and AM steady-state treatments. These two data points were estimated, in order to calculate the integrated measures, by averaging the values for the other two plants in each treatment at that time.
Two days after measuring gas exchange, we harvested individuals from each treatment. All 40 plants were harvested, ten from each treatment. For each plant we measured leaf area in square centimetres using a LI-COR leaf area machine and leaf mass (without petioles), shoot mass, root mass, and total dry biomass in grams.
Statistical analysis
Two-way analysis of variance was conducted to test the effects of CO2 treatment, light treatment, block, and the interaction of CO2 and light using Data Desk (Velleman, 1992). Blocks were treated as random factors, and block by factor interactions were not included in the model if there was no significant block effect, according to Bancroft's rules (Bancroft, 1964). Dependent variables included total biomass in grams, specific leaf mass in milligrams per square centimetre, maximum photosynthetic rates (average value during high light in micromoles of carbon per square metre per second), maximum conductance rates (millimoles of water per square metre per second), daily integrated carbon gain (moles of carbon per plant per day), integrated water loss (moles of water per square metre per day), and water use efficiency (WUE) calculated as the ratio of integrated carbon gain to integrated water loss.
| RESULTS |
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Integrated water use efficiency (WUE) showed a significant light effect (P < 0.0005) and CO2 by light interaction (P < 0.02, Table 1). WUE was highest in plants receiving high morning light and diurnally varying CO2 and lowest in plants receiving high afternoon light and diurnally varying CO2 (P < 0.0005). Within the morning high-light treatments, plants receiving diurnally varying CO2 were not significantly different from the control, but their WUE was significantly lower than the control within the afternoon high-light treatments (P < 0.04). Trends in photosynthetic rates, carbon gain, and water use efficiency were consistent with the predicted rank order response of AM diurnal < AM steady-state < PM steady-state < PM diurnal (water loss followed the opposite trend: AM diurnal > AM steady-state > PM steady-state > PM diurnal), although there was no significant difference between the AM diurnal and AM steady-state treatments.
Growth and leaf morphology
Consistent with trends in photosynthetic rates and daily carbon gain, total biomass was highest in plants receiving intense morning light and diurnally varying CO2 and lowest in plants receiving intense afternoon light and diurnally varying CO2 (difference of means: P < 0.0006, Fig. 4). Analysis of variance for all treatments showed a significant light effect (P < 0.0008), but there was no significant light by CO2 interaction (P < 1.0). Specific leaf mass showed a highly significant CO2 by light interaction (P < 0.002). Specific leaf mass of plants in the AM diurnal treatment were significantly higher than that of plants in the steady-state CO2 control (P < 0.0001); plants in the PM diurnal treatment showed lower specific leaf mass than the PM steady-state treatment, but this difference was not significant. Trends in both biomass rate and specific leaf mass followed the predicted rank order of response: AM diurnal > AM steady-state > PM steady-state > PM diurnal, although differences between individual treatments were not always significantly different.
| DISCUSSION |
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Although total light and CO2 availability across the day were the same in all treatments, plants that received afternoon high light and diurnally varying CO2 assimilated less daily carbon than plants in other treatments, particularly those in morning high light with diurnally varying CO2. This is due to the likelihood that plants receiving afternoon high light could not respond to the higher CO2 levels in the morning, but only to the lower CO2 levels present during peak light availability. Many studies show higher photosynthetic rates and greater daily integrated carbon gain at higher CO2 concentrations (Bazzaz, 1990; Poorter, 1993; Ceulemans and Mousseau, 1994). In the afternoon light treatments, the lower carbon gain for the diurnally varying CO2 treatment relative to the steady-state treatment is consistent with these findings if, in fact, these plants cannot take advantage of peak CO2 concentrations.
A CO2-saturation effect is suggested by the fact that higher CO2 levels within the AM diurnal treatment did not lead to an increase in photosynthetic rate compared with the AM steady-state control. It is possible that plants did not respond to a difference between 600 ppm (steady-state treatment) and 800 ppm (diurnal treatment) in terms of carbon assimilation because they reached their maximum carboxylation capacity at 600 ppm. Despite this phenomenon, conductance and transpiration rates were significantly affected by diurnally varying CO2 relative to the CO2 control. This led to an increase in water use efficiency for plants receiving peak levels of light and CO2 congruently. This is consistent with previous evidence showing that elevated CO2 reduces stomatal conductance, which leads to reduced water loss (transpiration) and increased water use efficiency (Bazzaz, 1990; Woodward, Thompson, and McKee, 1991; Allen et al., 1994; Diemer, 1994).
Growth and morphological responses
In previous studies, specific leaf mass of herbaceous plants was found to be significantly higher when plants were grown at elevated CO2 (Bazzaz, Coleman, and Morse, 1990; Garbutt, Williams, and Bazzaz, 1990). In experiments with annuals grown in different light intensities, specific leaf mass also increased (specific leaf area decreased) with increasing light levels (Sultan and Bazzaz, 1993; Ashton and Berlyn, 1994). Our data show a distinct and highly significant difference in specific leaf mass for plants receiving high morning light and diurnally varying CO2 relative to the other treatments, demonstrating the responsiveness of specific leaf mass to congruency of light and CO2. Hence, plants may respond to congruent availability of resources in the same way as they would respond to higher total resource levels.
Significant light effects were found for all character responses considered, providing strong evidence that differences in the diurnal timing of lighteven with the same total photosynthetic photon flux density and the same variance in intensity, frequency, and duration of lighthave important consequences for seedlings and may significantly affect survivorship, particularly in competitive conditions. Conductance, transpiration, daily integrated water loss, and water use efficiency, total leaf mass, and specific leaf mass all showed significant light by CO2 interactions, suggesting performance was enhanced when peak values of resources were congruent and diminished when they were incongruent. Although conductance and water loss were decreased by the congruency of peak values of CO2 and light in the morning and increased by the incongruency of peak values of CO2 during the afternoon high-light window, photosynthesis and biomass were only affected by the incongruency of peak values of CO2 and light.
Trends for all of the water-related and morphological character responses were consistent with predicted rank order of performance, even though the treatments were not all significantly different from each other, suggesting that differences in congruencies of high light with optimal CO2 concentrations, independent of total resource availability, can significantly affect seedling performance. In general, plants were negatively affected by the incongruency of CO2 and light more than they were affected by the congruency of CO2 and light.
An important implication of this study is that east and west sides of large gaps, which differ in their diurnal time courses of light availability and CO2 concentrations, may provide differential advantages for competitively interacting species early in their development. Further investigation is needed to determine whether temporal and spatial heterogeneity in resource availability significantly influences plant performance under field conditions. If so, diurnal variations and congruencies in critical resources may turn out to be important factors in gap partitioning and in the organization of regenerating communities.
| FOOTNOTES |
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2 Author for correspondence (Phone: 617-495-8791, Fax: 617-496-5223, E-mail:jcavender{at}oeb.harvard.edu) ![]()
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