Correspondence: James D.Lewis The Louis Calder Center and Biological Station, Department of Biological Sciences, Fordham University, 53 Whippoorwill Road, PO Box K, Armonk, NY 10504, USA. Fax: + 1 914 273 6346; E-mail: email@example.com
The interactive effects of elevated atmospheric CO2 and temperature on seasonal patterns of photosynthesis in Douglas fir (Psuedotsuga menziesii (Mirb.) Franco) seedlings were examined. Seedlings were grown in sunlit chambers controlled to track either ambient (~400 p.p.m.) CO2 or ambient +200 p.p.m. CO2, and either ambient temperature or ambient +4 °C. Light-saturated net photosynthetic rates were measured approximately monthly over a 21 month period. Elevated CO2 increased net photosynthetic rates by an average of 21% across temperature treatments during both the 1996 hydrologic year, the third year of exposure, and the 1997 hydrologic year. Elevated mean annual temperature increased net photosynthetic rates by an average of 33% across CO2 treatments during both years. Seasonal temperature changes also affected net photosynthetic rates. Across treatments, net photosynthetic rates were highest in the spring and autumn, and lowest in July, August and December–January. Seasonal increases in temperature were not correlated with increases in the relative photosynthetic response to elevated CO2. Seasonal shifts in the photosynthetic temperature optimum reduced temperature effects on the relative response to elevated CO2. These results suggest that the effects of elevated CO2 on net photosynthetic rates in Douglas fir are largely independent of temperature.
Douglas fir (Psuedotsuga menziesii (Mirb.) Franco) is a dominant tree species in the Pacific Northwest (Franklin & Dyrness 1988; Hermann & Lavender 1990), and half of its annual carbon uptake may occur between October and April (Waring & Franklin 1979; Emmingham 1982). Despite the ecological and economic importance of Douglas fir, few studies have examined temperature effects on Douglas fir responses to elevated CO2 either experimentally (Olszyk et al. 1998a) or through modelling (Franklin et al. 1991). Temperature effects may result from seasonal temperature changes and from temperature increases associated with climate change. Mean weekly temperatures in the Pacific Northwest often vary seasonally by 20 °C or more (Franklin & Dyrness 1988; Fig. 1), and low winter temperatures and high summer temperatures suppress photosynthesis in Douglas fir (Brix 1971; Hawkins et al. 1995). Mean annual temperatures in this region are predicted to increase by 2–3 °C in coastal areas and 3–4 °C in inland areas by 2080 compared to the 1961–90 means, based on the second Hadley Centre coupled ocean-atmosphere GCM (Johns et al. 1997) as provided on the IPCC Data Distribution Centre web-site (http://ipcc-ddc.cru.uea.ac.uk). Increasing temperatures during the winter should reduce temperature limitations on carbon uptake, and increasing temperatures during the summer should exacerbate temperature limitations on carbon uptake.
Effects of elevated temperature on net photosynthetic rates may be moderated by increasing atmospheric CO2 (Long 1991). Net photosynthetic rates decline rapidly as temperatures increase above the optimal temperature (Larcher 1995; Kozlowski & Pallardy 1996). Elevated CO2 increases temperature optima for photosynthesis in some C3 species (Idso & Idso 1994; Eamus, Duff & Berryman 1995). An increase of 200 p.p.m. above current atmospheric CO2 concentrations may shift temperature optima upward 3–4 °C (Long 1991), paralleling the increase in mean annual temperatures predicted to occur during the next century. By shifting temperature optima upward, elevated CO2 may ‘acclimate’ photosynthetic processes to future temperature regimes. However, increases in temperature optima may negatively affect net photosynthetic rates when temperatures are suboptimal, as often occurs during the winter months in the Pacific Northwest. Although shifts in temperature optima for photosynthesis alter seasonal patterns of carbon uptake (Berry & Björkman 1980), few studies have examined the effects of elevated CO2 on seasonal shifts in temperature optima of photosynthesis.
Changes in seasonal patterns of carbon uptake in response to elevated CO2 and temperature may also reflect changes in phenology (Morison & Lawlor 1999). Although elevated CO2 does not affect the phenology of Douglas fir seedlings (Olszyk et al. 1998a,b), temperature has been widely shown to affect the timing of processes such as bud break, shoot elongation, root elongation, and hardening-off (e.g. Campbell & Sugano 1975; Guak et al. 1998; Olszyk et al. 1998a,b). These processes may significantly increase carbon utilization (sink activity), changing the relative balance between carbon uptake (source activity) and carbon utilization. Because source–sink balance may regulate photosynthetic response to increasing CO2 (Arp 1991; Stitt 1991; Thomas & Strain 1991), changes in the seasonal pattern of source–sink balance may alter seasonal patterns in photosynthetic response to elevated CO2 (Tissue, Thomas & Strain 1996).
In this study, we examined the effects of seasonal variation in temperature and increased mean annual temperature on the relative photosynthetic response of Douglas fir to elevated CO2 over a 21-month period, beginning 27 months after treatments were initiated. Specifically, the following questions were addressed: (1) do seasonal changes in temperature affect the relative photosynthetic response to elevated CO2? (2) Does increasing the mean annual temperature increase the relative photosynthetic response to elevated CO2 at a particular measurement period? (3) Does elevated CO2 increase the temperature optima for photosynthesis?
MATERIALS AND METHODS
Douglas fir (Psuedotsuga menziesii (Mirb.) Franco) seed lots were collected at five low-elevation seed zones (<500 m) in the Coast Range, Willamette Valley and the west slopes of the Cascade Mountains around Corvallis, Oregon, USA. Seedlings were grown for 1 year in seed beds and 1 year in nursery beds. In June 1993, 14 seedlings were transplanted as bare-root, 2-year-old stock into each 1 m × 2 m surface area chamber at the US Environmental Protection Agency Environmental Research Laboratory in Corvallis, Oregon. Each chamber consisted of a sun-lit upper compartment (1·2–1·5 m high) where air temperature, CO2 concentration and vapour pressure deficit were monitored and controlled, and a lower soil lysimeter (1·0 m deep) filled with a native coarse-textured sandy loam in which soil parameters such as temperature and soil moisture were monitored (Tingey et al. 1996). Initial soil nitrogen concentrations in the A, B and C horizons were 0·12, 0·07 and 0·06%, respectively. Initial phosphorus concentrations in the A, B and C horizons were 7, 3 and 3 p.p.m., respectively. Ambient CO2 and air temperature were monitored at an adjacent meteorological station, and the chambers were controlled to continuously track either ambient CO2 or ambient +200 p.p.m. CO2 and ambient air temperature or ambient +4 °C (Tingey et al. 1996). The experimental design was a full factorial with two levels each of CO2 and temperature resulting in four treatments: ambient CO2 and ambient temperature (ACAT); ambient CO2 and elevated temperature (ACET); elevated CO2 and ambient temperature (ECAT); and elevated CO2 and elevated temperature (ECET). There were three chambers per treatment combination, and treatments were applied 24 h per day beginning in August 1993 and continuing until the end of the study (July 1997). Mid-day (1000–1400 Pacific standard time) CO2 concentrations during the growing season in 1996 typically ranged between 360 and 400 p.p.m. in the ambient CO2 treatment. Seedlings were grown under ambient light, and without supplemental nutrients. Soil moisture content was controlled to reflect seasonal changes in soil moisture typical for the wet winter–dry summer climate in the Pacific Northwest (Griffiths & Caldwell 1990; Griffiths et al. 1991). Weekly water additions to the ambient CO2: ambient temperature treatment were calculated on the basis of this pattern of soil moisture content. Water additions to the other treatments were the same as in the ambient CO2–ambient temperature treatment. Target dew point depression in the chambers was based on ambient conditions and controlled to have equivalent vapour pressure deficits (VPD) across treatments. Actual chamber conditions during the entire course of the experiment differed slightly from targets: elevated CO2 averaged 179 p.p.m. above ambient, elevated temperature averaged 3·5 °C above ambient, and the VPD in the elevated temperature treatments averaged 0·10 kPa above the VPD in the ambient temperature treatments.
Net photosynthetic rates were measured using infrared gas analysers built into a leaf cuvette in an open-flow gas exchange system (LI-6400; Li-Cor Inc., Lincoln, NE, USA). All measurements were made on intact fully expanded, unshaded needles from the most recent needle cohort (e.g. measurements made between November 1995 and July 1996 were performed on needles from the 1995 cohort). Needles were arranged in the cuvette such that self-shading was minimized and all needles were parallel to the plane of the leaf chamber. All measurements were made using ambient light. Photosynthetic photon flux densities (PPFD) at the upper leaf surface were typically 1400–2000 μmol photons m−2 s−1; no measurements were made below 800 μmol photons m−2 s−1. These PPFD are saturating for photosynthesis in Douglas fir needles (Bond et al. 1999; Lewis, Olszyk & Tingey 1999; Lewis et al. 2000). The airstream entering the cuvette was maintained at the growth CO2 concentration (either 360 or 560 p.p.m. CO2) using a computer-controlled CO2 mixing system supplied with the LI-6400. Needle, cuvette and air temperatures were measured with thermocouples linked to the LI-6400 computer. Needle temperature was maintained at the desired temperature using a computer-controlled Peltier module mounted on the cuvette. Mean needle temperature at each measurement period in the ambient temperature treatment is shown in Fig. 2. Measurements in the ambient +4 °C treatment were made at temperatures 4 °C higher than the needle temperatures used for the ambient temperature treatment. These temperatures reflect average chamber temperatures between 1000 and 1400 h during a given measurement period. All gas exchange para-meters were calculated according to Field, Ball & Berry (1989). Projected surface area of the measured needles was estimated using measurements of needle length and width.
Photosynthetic measurements began 27 months after treatments were initiated, and were measured approximately monthly between November 1995 and July 1997, when the experiment was terminated. Prior to each measurement, needles were equilibrated in the cuvette at saturating PPFD, the growth CO2 concentration, and the measurement temperature. Needles were considered equilibrated if gas exchange parameters were stable for 1 min. Measurements were initiated at approximately 0900 h Pacific standard time, and typically were completed by 1200 h Pacific standard time.
At each measurement period, the relative response of net photosynthetic rates to elevated CO2 was calculated for each temperature treatment. The relative response was calculated as the ratio of the mean net photosynthetic rate in the elevated CO2 treatment to the mean net photosynthetic rate in the ambient CO2 treatment measured at the growth CO2:
where AEC is the net photosynthetic rate in the elevated CO2 treatment and AAC is the net photosynthetic rate in the ambient CO2 treatment at the same measurement period. Using this approach, if the relative response = 2 then the net photosynthetic rate in the elevated CO2 treatment is twice the rate measured in the ambient CO2 treatment. If the net photosynthetic rate is the same in both CO2 treatments, the relative response = 1.
The effect of seasonal changes in temperature on net photosynthetic rates in each treatment was examined by comparing the mean net photosynthetic rate versus needle temperature for all measurement periods. An empirically based temperature response curve was calculated for each treatment using the following parabolic model:
where A is the net photosynthetic rate and T is the needle temperature in degrees C. To calculate the temperature optima for the photosynthetic response to seasonal changes in temperature, the equation for each curve was solved for the needle temperature for which the slope was zero.
Seasonal responses (weeks to months) of photosyn-thesis to temperature reflect acclimation of physiological processes to changing environmental conditions over time, including shifts in the short-term (minutes to hours) temperature optima for photosynthesis (Berry & Björkman 1980). To examine seasonal shifts in short-term temperature optima of photosynthesis, short-term temperature response curves were measured during winter, spring and summer of the 1996 hydrologic year. In February 1996, net photosynthetic rates were measured at five needle temperatures between 12 and 23 °C in all temperature treatments. Similar measurements were made between 17 and 28 °C in May 1996, and between 22 and 35 °C in August 1996. For each curve, leaf temperature was manipulated using the Peltier module mounted on the cuvette. For all measurements at a given measurement period, the water vapour content of the cuvette air was controlled to maintain a constant dew point depression. Prior to each measurement, needles were equilibrated in the cuvette at saturating PPFD, the growth CO2 concentration, the target water vapour content in the cuvette air, and the measurement temperature. Needles were considered equilibrated if gas exchange parameters were stable for 1 min. Individual measurements typically took 5 min to equilibrate, and temperature response curves generally were completed within 30 min. Measurements were initiated at approximately 0900 h Pacific standard time, and typically were completed by 1200 h Pacific standard time.
Treatment effects on seasonal patterns in photosynthesis were analysed using repeated measures analysis of variance with growth CO2 and temperature as the between-subjects factors and measurement period as the within-subjects factor. The effects of short-term temperature changes on net photosynthetic rates were analysed using repeated measures analysis of variance with growth CO2 and temperature as the between-subjects factors, and needle temperature as the within-subjects factor. Analyses were performed using the multivariate general linear model function (MGLH) in SYSTAT (Systat 1992). In general, photosynthesis was measured on one tree in each chamber per measurement period. Across the study period, individual branches were not repeatedly measured and measurements were made on several trees in each chamber. Because the chamber was the experimental unit, measurements made on multiple trees in a chamber at a given measurement period were combined and the mean value used in the analyses. Data from the 1996 and 1997 hydrologic years were analysed separately. The hydrologic year begins on 1 October in western Oregon, and represents the transition from the dry season to the wet season. One chamber each in the ambient CO2: ambient temperature treatment and the elevated CO2: ambient temperature treatment were excluded from the 1997 analyses because of extensive insect damage to trees in these chambers.
The annual patterns in measurement temperatures and net photosynthetic rates during the 1996 and 1997 hydrologic years are shown in Fig. 2. Needle temperatures were lowest in late December and early January, and peaked in late July and early August. Net photosynthetic rates generally were lowest in December–January and July–August, and peaked in March–May and October–November. Elevated CO2 significantly increased net photosynthetic rates across temperature treatments during both the 1996 (Fig. 2b) and 1997 hydrologic years (Fig. 2c). There was a significant interaction between temperature treatment and measurement period on net photosynthetic rates during the 1996 hydrologic year (Table 1). Elevated temperature increased net photosynthetic rates at all measurement periods except July (Fig. 2b). Throughout the 1997 hydrologic year, elevated temperature increased net photosynthetic rates (Fig. 2c). Although the effects of CO2 supply and growth temperature on net photosynthetic rates appeared to vary across measurement periods during the 1997 hydrologic year, these interactions were not significant (Table 1).
Table 1. Summary of F-values and their levels of statistical significance (P) from univariate comparisons (repeated measures analysis of variance) on mean light-saturated net photosynthetic rates during the 1996 and 1997 hydrologic years with CO2 supply and temperature as the between-subjects factors and measurement period as the within-subject factor. Results from multivariate and single degree of freedom polynomial contrasts were similar
1996 hydrologic year
1997 hydrologic year
CO2 supply (C)
Temperature × CO2
The relationship between measurement temperature and the relative response of net photosynthetic rates to elevated CO2 at each measurement period is shown in Fig. 3. The mean relative response was 1·21, and the relative response was >1 (i.e. elevated CO2 increased net photosynthetic rates) for approximately 90% of the measurement periods. When the correlation between needle temperature and the relative photosynthetic response to elevated CO2 was analysed separately for each temperature treatment and for each hydrologic year, there were no significant correlations in either temperature treatment (P = 0·42, 0·26 for ambient and elevated temperature, respectively; Fig. 3a) or hydrologic year (P = 0·67, 0·10 for 1996 and 1997, respectively; Fig. 3b). Similarly, when data were grouped across hydrologic years and temperature treatment, there was no significant correlation between needle temperature and the relative photosynthetic response to elevated CO2 (P = 0·14; Fig. 3c).
The effect of seasonal variation in temperature on net photosynthetic rate is shown in Fig. 4. Net photosynthetic rate increased as temperature increased from 5 °C, peaked between 15 and 20 °C, and generally decreased with increasing temperature above 25 °C across treatments. Between 10 and 25 °C net photosynthetic rates were at least 80% of the projected maximum rates (the maximum photosynthetic rate calculated from the model used to fit the temperature-response curve) for a given treatment. Net photosynthetic rates in the elevated temperature treatment generally were higher than in the ambient temperature treatment. In addition to assessing photosynthetic responses to temperature across the study period by combining the entire data set within each treatment, the optimal temperature for photosynthesis was calculated for each chamber in order to examine treatment effects on the temperature optimum. There were no significant effects of CO2 treatment (P = 0·899) or temperature treatment (P = 0·663) on the temperature optimum, nor was there a significant interaction between CO2 treatment and temperature treatment (P = 0·291). In the ambient temperature treatment, the mean (± SE) temperature optima were 18·6 ± 1·0 (ambient CO2 treatment) and 19·7 ± 1·3 (elevated CO2 treatment). In the elevated temperature treatment, the mean (± SE) temperature optima were 19·3 ± 0·7 (ambient CO2 treatment) and 17·9 ± 1·4 (elevated CO2 treatment). These temperature optima vary from the temperature optima calculated by combining all three chambers within a treatment because one chamber in each of two treatments was measured for only half of the study period but was given equal weighting in the chamber-based comparison.
In addition to examining the response of net photosynthetic rates to seasonal changes in temperature, we examined the effect of short-term (minutes to hours) changes in temperature on net photosynthetic rates. For a given measurement period, repeated measures analysis of variance indicated that net photosynthetic rates significantly varied across measurement temperatures (P < 0·05 in all cases). Growth in elevated CO2 significantly increased the short-term temperature optima for photosynthesis in February and May (P≤ 0·05 in both cases) but not August (P = 0·63). The short-term temperature optima in the ambient CO2 treatment were approximately 13 °C in February and approximately 20 °C in May 1996 (Fig. 5); temperature optima in the elevated CO2 treatment were approximately 17 °C in February and approximately 23 °C in May. In August 1996, the apparent optimum was approximately 23 °C in the ambient CO2 treatment and approximately 25 °C in the elevated CO2 treatment. However, because the apparent peak for the ambient CO2 treatment occurred at the lowest measurement temperature, the actual temperature optimum may have been lower at this date. The apparent increase in the temperature optimum between February and August was similar to the increase in the weekly mean maximum temperature over this interval (Fig. 1). Temperature treatment did not significantly affect the short-term temperature optima for photosynthesis (data not shown).
Growth in ambient +200 p.p.m. CO2 increased net photosynthetic rates of Douglas fir by an average of 21% across the third and fourth years of exposure compared to trees grown in ambient CO2. Over the same time interval, growth in ambient +4 °C increased net photosynthetic rates an average of 33% in comparison with trees grown in am-bient temperature. Although increasing temperature was expected to increase the relative photosynthetic response to elevated CO2, temperature treatment and seasonal changes in temperature did not significantly affect the relative response to elevated CO2. The effects of seasonal changes in temperature on the relative photosynthetic response to elevated CO2 have been shown to be limited by photosynthetic acclimation during long-term exposure to elevated CO2 (Samuelson & Seiler 1992; Samuelson & Seiler 1994; Curtis et al. 1995; Epron, Liozon & Mousseau 1996; Le Thiec & Dixon 1996; Lewis et al. 1996). However, because elevated CO2 significantly increased net photosynthetic rates across the study period, it is likely that other factors also mitigated temperature effects on the relative photosynthetic response to elevated CO2. The present results suggest that shifts in the short-term temperature optimum for photosynthesis may have reduced the effect of seasonal changes in temperature on the relative response to elevated CO2.
Between February and August 1996, the short-term temperature optima for photosynthesis shifted by approximately 10 °C higher in both CO2 treatments (Fig. 5). As a result of this shift, net photosynthetic rates were generally unaffected by seasonal shifts in temperature between 10 and 25 °C in both CO2 treatments, and the relative response to elevated CO2 showed little variation across this temperature range. These results parallel previous studies, which showed that the temperature optimum across seasons for photosynthesis in Douglas fir is approximately 10–20 °C (Helms 1964; Helms 1965; Brix 1967). As ambient temperatures fell within this range for most of the year, seasonal variation in net photosynthetic rates was only observed during early winter and midsummer, and the relative photosynthetic response to elevated CO2 was generally uniform for most of the year. Broad peaks in the temperature response of photosynthesis across an annual cycle have been observed in several tree species, probably due to seasonal shifts in short-term temperature optima for photosynthesis (Berry & Björkman 1980). Seasonal shifts in short-term temperature optima of as much as 15 °C have been observed in other temperate evergreen (Neilson, Ludlow & Jarvis 1972; Strain, Higginbotham & Mulroy 1976; Drew & Ledig 1981) and deciduous tree species (Aubuchon, Thompson & Hinckley 1978; Dougherty et al. 1979). These results suggest that seasonal shifts in short-term temperature optima for photosynthesis may regulate temperature effects on photosynthetic responses to elevated CO2 in some tree species.
Despite seasonal shifts in the short-term temperature optima for photosynthesis, winter temperatures in this study fell outside the temperature range considered optimal for Douglas fir (Brix 1971; Hawkins et al. 1995). As a result, reductions in net photosynthetic rates during the winter in this study probably reflect temperature effects on photosynthesis, particularly in the ambient temperature treatment. In the elevated temperature treatment, reductions in net photosynthetic rates during the winter months were minimized because the 4 °C increase in temperature brought air temperatures closer to the temperature that is optimum for photosynthesis (Fig. 1). During the summer months, measurement temperatures in both temperature treatments exceeded the optimal range for photosynthesis, and may partially account for reductions in net photosynthetic rates. In addition, summer-time carbon uptake may have been suppressed by limited water availability during the warm, dry summers that are characteristic of this region (Waring & Franklin 1979; Emmingham 1982) and that occurred during this study (M. Johnson et al. unpublished results).
The effects of seasonal changes in temperature on net photosynthetic rates were expected to be altered by elevated CO2 because increasing atmospheric CO2 is predicted to increase the temperature optimum for photosynthesis by altering the relative balance between photosynthesis and photorespiration (Long 1991). Increasing temperature reduces the CO2 specificity of Rubisco, increasing the proportion of potential photosynthesis lost to photorespiration (Brooks & Farquhar 1985). In contrast, increasing CO2 inhibits oxygenase activity (Lorimer 1981), reducing the inhibitory effects of increasing temperature on photosynthesis. Consistent with this prediction, short-term temperature-response curves indicate that elevated CO2 treatment increased the short-term (minutes to hours) temperature optima for photosynthesis (Fig. 5), as has been observed in other tree species (Idso & Idso 1994; Eamus et al. 1995). However, CO2 treatment did not have a significant effect on the temperature optimum for photosynthesis across seasons. The differential responses of photosynthesis to short-term versus seasonal changes in temperature may reflect the fact that seasonal changes in net photosynthetic rate also occur in response to a variety of abiotic and biotic factors other than temperature. For example, total incident solar radiation (Tolley & Strain 1984a; Lewis et al. 1999), nutrient availability (Curtis et al. 1995), water availability (Tolley & Strain 1984b; Le Thiec & Dixon 1996), mycorrhizal activity (Lewis & Strain 1996), sink activity (Epron et al. 1996; Tissue et al. 1997) and leaf age (Aoki & Yabuki 1977; Hicklenton & Jolliffe 1980) may influence seasonal patterns in photosynthetic responses to elevated CO2. The effects of these and other factors may reduce the direct effects of seasonal changes in temperature on photosynthesis relative to short-term changes in temperature. As a result, although increasing CO2 may increase the short-term temperature optima for photosynthesis, the overall effect on seasonal responses of photosynthesis to temperature appears to be minimal.
Increased net photosynthetic rates during the third and fourth years of growth in elevated CO2 are consistent with the photosynthetic response to elevated CO2 of Douglas fir seedlings during the first year of growth (Hollinger 1987). Additionally, the sustained response of net photosynthetic rates to elevated CO2 after four years of exposure parallels results from several studies on the effects of long-term (one or more years) exposure of field-grown trees to elevated CO2 (e.g. Idso, Kimball & Allen 1991; Gunderson, Norby & Wullschleger 1993; Eamus et al. 1995; Jones et al. 1995; Tissue, Griffin & Ball 1999). The relative increase in net photosynthetic rates due to growth in elevated CO2 was smaller (21%) than the mean response for tree species (44–66%) reported in recent reviews (Cuelemans & Mousseau 1994; Gunderson & Wullschleger 1994; Curtis 1996; Curtis & Wang 1998; Norby et al. 1999). The relatively low photosynthetic response to elevated CO2 may have resulted from a variety of factors. The reduced response may reflect the relatively low elevated CO2 treatment in this study (approximately 600 p.p.m.) in comparison with most studies (approximately 700 p.p.m.; Curtis & Wang 1998). However, in a free-air CO2 enrichment study where the elevated CO2 treatment was approximately 575 p.p.m., long-term exposure to elevated CO2 increased net photosynthetic rates in Pinus taeda by approximately 55% in mid-summer (Ellsworth 1999; Myers et al. 1999), and increased net photosynthetic rates of sun leaves by approximately 98% in Liquidambar styraciflua (Herrick & Thomas 1999). The relative response observed in this study also reflects 17 measurement periods across 2 years, whereas most studies measure net photosynthetic rates under optimal growth conditions at one or two periods. Additionally, Douglas fir may be relatively unresponsive to elevated CO2. Biomass accumulation in Douglas fir is not significantly increased by growth in elevated CO2 (Hollinger 1987; Mortensen 1994; Gorissen, Kuikman & Van de Beek 1995).
In summary, elevated CO2 and elevated growth temperature significantly increased net photosynthetic rates during the third and fourth year of exposure. Seasonal changes in temperature did not affect the relative response to elevated CO2 due to shifts in the short-term temperature optima for photosynthesis. In addition, the relative photosynthetic response to elevated CO2 in these trees was not affected by temperature treatment, or by light availability (Lewis et al. 1999). These results suggest elevated CO2 may increase carbon accumulation in Douglas fir. However, other studies have shown that long-term exposure to elevated CO2 does not increase biomass accumulation in Douglas fir. Several factors may limit the biomass response of trees to elevated CO2 (Norby et al. 1999). For example, older needles may be less responsive to elevated CO2 than the current-year needles measured in this study (Turnbull et al. 1998). Reductions in the leaf area ratio (leaf area per unit plant biomass) may also reduce biomass responses to elevated CO2 (Callaway et al. 1994; Lewis & Strain 1996). Similarly, although increasing temperatures associated with climate change may increase net photosynthetic rates and the potential for carbon uptake, increasing temperatures also increase foliar respiration rates in Douglas fir (e.g. Lewis et al. 1999), increasing the potential for carbon loss. As a result, increasing CO2 and increasing temperature associated with climate change are likely to increase needle-level net photosynthetic rates in Douglas fir seedlings, but the effect on biomass accumulation may be smaller than the effect on net photosynthetic rates.
We thank Joe Greene, Glenn Jarrell, Mark Johnson, Craig McFarlane, Paul Rygiewicz, Ron Waschmann, Jim Weber and Claudia Wise for their technical support in the design and execution of this study. Jacqui Johnson and Dave Myers improved earlier drafts of this manuscript. Seedlings were provided by the Weyerhauser Company.
The research described in this article has been funded by the U.S. Environmental Protection Agency. This document has been prepared at the EPA's Western Ecology Division in Corvallis, Oregon, through co-operative agreement CR-824072 with the National Research Council and through contract 68-C6–0005 with Dynamac, Inc. It has been subject to the agency's peer and administrative review and approved for publication. Mention of trade names or commercial products does not constitute endorsement or recommendation for use.