1. Introduction
As worldwide climates have changed, the distribution and composition of plant communities have shifted, and are expected to continue adjusting in the future [1]-[3]. The atmospheric CO2 level was approximately 1500 ppm at the end of the Cretaceous (55 × 106 years ago) which did not decline for 1000 years [4] [5]. Approximately 125,000 years ago the atmospheric CO2 level was about 230 ppm with a corresponding temperature 6˚C below the current level [6]. Current atmospheric CO2 levels are increasing at approximately 3 parts per million per year (2024 mean level = 427 ppm) with temperatures increasing at 0.20˚C/10 years (2024 mean level = 16.24˚C) [7].
Plant communities and animal populations changed in the past and existing communities and populations will change in density and distributions in the future as atmospheric carbon levels and temperatures increase, but how populations will change is uncertain [1] [4] [8].
The land surface of central North America was grasslands and covered 20% of the surface in the past several thousand years [9]. These grasslands changed due to cultivation and the introduction of large herds of domestic ungulate [10]-[12]. Many of these overgrazed grasslands have been encroached by various Juniperus species from the Atlantic to the Pacific coasts through the Great Plains to the low and mid-elevations of the mountains of North America [13]-[15] and have been treated as stable communities [16] [17]. Nevertheless, studies suggested the Juniperus are pioneer species and will develop into various woodlands [18]-[20].
Central Texas currently has many communities with various densities of J. ashei Buchh. and Quercus virginiana Mill. (Ashe juniper and hill country live oak, [15] [21] [22]. The Texas Juniperus communities are generally similar in overall structure and environmental characteristics to Juniperus woodlands from all over the world [23]. Although, associated species are very different and sometimes have very limited distributions [21] [24]. Canopy density is highly variable in Texas with Juniperus communities having cover between 40% and 90% [25] [26] and open areas that have juvenile woody species, grasses and herbaceous plants [12] [27]. There are few studies that have investigated understory woody seedlings and herbaceous plants responses to predicted future climate changes of higher CO2 concentration and temperature [1] [4] [8]. Due to the shifting climate, some of the current low-density woody species may be lost or recruited into the canopy. Therefore, the future density of species and structure for these areas in central Texas is unknown.
The shift in an ecosystem from a grassland to a woodland would entail major shifts in biomass from mostly belowground for grasslands to mostly aboveground for woodlands [28]. These ecosystem shifts could alter regional terrestrial and atmospheric biogeochemistry especially if the woodlands act as a carbon and nitrogen sink [29]-[31]. Processes could include nutrient cycling and availability which would influence primary production, competition for resources, species richness, community composition as well as species interactions [32]. But how these factors would change in an atmosphere high in CO2 and temperature are not known. In addition, it is not known how seedlings of the adult Juniperus and other species would respond.
CO2 concentration has been shown to be limiting in some communities and increasing levels promoted higher photosynthetic uptake and growth for some species [33]-[35]. However, work showing effects of elevated CO2, temperature, and light levels on J. ashei or on any Juniperus woodland communities has not been carried out. There have been a few studies that examined the gas exchange responses of associated species but none dealing with J. ashei [2] [34] [36].
Currently, J. ashei dominates the woodlands across central Texas similarly to other worldwide Juniperus communities dominated by their specific local Juniperus species, but the associated species are quite different with some in Texas being endemic to the central Texas region [24] [36] [37]. We hypothesize that due to the changing environmental conditions, specifically increased CO2 concentration and temperature, the future community composition and structure will also change. In this study, we investigated the photosynthetic response of mature J. ashei to short-term increases in temperature and CO2 concentrations through various light levels and compared them to their current ambient responses. These results were then used to evaluate their potential effects on J. ashei’s role in the future community dynamics of central Texas.
2. Materials and Methods
2.1. Community Structure
All gas exchange measurements were made on mature Juniperus ashei leaves on the south side of trees on the western part of the University of Texas at San Antonio campus in central Texas (29.58030 N and −98.62403 W). Area topography is rolling with low slopes between 4.5˚ and 13.5˚ and soils that are clayey-skeletal, smectitic, thermic lithic calciustolls [38] in the Tarrant association with surface horizons between 0 and 25 cm thick [39]. The area geology is composed of heavily fractured limestone over limestone bedrock. Climate is subtropical sub-humid [40] having a mean annual temperature of 20˚C with means of 9.6˚C in January and 29.4˚C in July [41]. Precipitation is also highly variable usually 78.7 cm/yr and bimodal, very little in June and July and peaks in May 10 with 7 cm and September with 8.7 cm [41]. There was no domestic grazing or domestic livestock present in the study area for the past 75 years. There are large areas of Juniperus ashei/Quercus virginiana woodlands or savannas on former grassland sites in central Texas which are considered representative of similar communities found in this area [42].
Mature J. ashei plants in relatively undisturbed J. ashei/Q. virginiana woodland communities were selected randomly for measurements. Mean density and basal area of the communities examined was determined but limited information about community structure is presented here [2] [33]. Trees found were all identified, counted and measured. Concise but succinct information about community structure is presented below for the major species found.
2.2. Gas Exchange
Gas exchange responses at both ambient and elevated levels of CO2 and temperature were made. Three plants were randomly selected in the summer of 2007. On each replicate plant one main stem tip at breast height, approximately 137 cm above the soil surface was selected and only mature, non-damaged stems were used. Steady state photosynthetic light response curves (Anet vs. PPFD) were measured on full grown stem tips with completely expanded leaves at mid-day (1000 - 1400 hrs) when relative humidity had stabilized [43]. Leaves one cm from the growing stem tip were 1.07 ± 0.27 mm (mean ± 1.0 SD) in length and those five cm from the growing tip were 2.17 ± 0.34 mm in length and leaves surrounded the entire stem tip.
To measure leaf gas exchange, a branch tip or cluster with several secondary branches all with many small leaves was placed into the cuvette chamber. The stems were all parallel in the chamber in a single plane configuration and all at 90˚ to the light source. At least 66% of the cuvette chamber was covered. After the gas exchange measurements were made Leaf area within the chamber was measured with a LI-COR LI 3000A portable area meter. Each sample was measured in the scanner three times and the mean was determined and used as a correction and manually entered into the Li-6400® to adjust each curve. Measurements made and recorded were: Anet (net photosynthesis = µmolCO2·m−2·s−1), Ci (intercellular [CO2] = µmolCO2·molair−1), Tleaf (chamber leaf temperature = ˚C), Tair (air temperature outside the chamber = ˚C), PPFD (photosynthetic active radiation = mol·m−2·s−1), g (stomatal conductance = molH2O·m−2·s−1) and E (transpiration = mmolH2O·m−2·s−1).
2.3. Chamber Set-Up
The gas exchange chamber was used to mimic varying degrees of environmental modifications with the stem cluster in the chamber attached to the plant. Conditions adjusted or manipulated were the light level, CO2 concentration, and temperature. Relative humidity was kept at 30% - 40% and the gas flow rate was set at 400 µmol·s−1. Coefficient of variation stabilized (<1%) before recording and moving to the next measurement. Light levels started at 1800 µmol·m−2·s−1 and decreased to 1600, 1400, 1200, 1000, 800, 600, 400, 200, 100, 75, 50, 25, 10, 5 and finally 0 µmol·m−2·s−1. Light curves and CO2 response curves were measured for different combinations of the leaf chamber CO2 and temperature environments.
The leaf chamber was first set at the mean atmospheric CO2 level (390 µL/L) for 2007 and a temperature of 35˚C. This temperature was chosen based on the mean high temperatures for San Antonio during the summer months of June, July and August. Light curves were repeated holding the ambient CO2 constant while raising the chamber temperature to 40˚C and then to 45˚C. Next, the leaf chamber CO2 was raised to 1.5 times the 2007 CO2 levels to 585 µL/L. Light curves were completed at a temperature of 35˚C, 40˚C and 45˚C. This process was then repeated with the leaf chamber CO2 level set at twice the 2007 ambient level at 780 µL/L. Lastly, CO2 response curves were measured at a canopy shade light level (700 µmol·m−2·s−1). Measurements were made at 35˚C, 40˚C and 45˚C.
2.4. Analysis
The data analysis was completed using Microsoft Excel© and JMP© IN 5.1. Significant differences were measured using the JMP© IN 5.1 software with a repeated measures MANOVA on the photosynthetic rate curves including intercellular CO2 concentrations, stomatal conductance and transpiration. The light level, PPFD, was the repeat variable [44]. Water use efficiency (WUE) was calculated by dividing the photosynthetic rate by the transpiration rate and also analyzed using a repeated measures MANOVA. Significance levels used for all tests were P ≤ 0.05. Normality was checked with the Shapiro-Wilk W test and homogeneity of variance with Bartlett’s test and log transformed as necessary. A standard least squared ANOVA was used to detect significant differences in each curve at each CO2 concentration and temperature combination. However, this is a curve-to-curve comparison and individual CO2 uptake was not compared at individual light levels on each plant and each replication.
For other measurements, they were derived from Excel® plots of the LICOR® Li-6400 measurements. Included were maximum photosynthetic rate (Amax) which was the highest Anet measured for each replicate or a mean of the highest Anet values that were not significantly different. The dark respiration rate (Rd) was the gas exchange rate at PPFD = 0 µmol·m−2·s−1. The quantum yield (Ø) was the linear initial slope relationship calculated using the dark values and Anet at increasing PPFD until the regression coefficient of the slope decreased. The light compensation point (Lcp) was calculated as the PPFD when Anet = 0 µmolCO2·m−2/s−1 using the linear regression of the initial response. The light saturation point (Lsp) was the light level when the initial slope reached Amax. A standard least squared ANOVA was used to determine significant differences for the CO2 concentration and temperature effects. Tukey-Kramer HSD multiple comparison tests were used to determine differences between pair wise comparisons [44].
3. Results
3.1. Community Structure
The community overstory had a mean canopy density of 1840 plants/ha and was found to be dominated by Juniperus ashei with a relative density in the canopy of 61% ± 12% (mean ± one standard deviation). The other major canopy species was Quercus virginiana with a relative canopy density of 36% ± 6%. Additional community species with relative densities of 0.06% - 1.80% were Celtis laevigata (sugarberry or hackberry), Diospyros texana (Texas persimmon), Prosopis glandulosa (mesquite), Calia secundiflora (Texas mountain laurel), Ulmus crassifolia (cedar elm), and Ungnadia speciosa (Mexican buckeye).
3.2. Photosynthetic Curves
The mean curves of the photosynthetic rates for Juniperus ashei are shown by temperature and CO2 concentration with light level being fixed (Figure 1(A) and Figure 1(B)). The photosynthetic rates by temperature show a statistical difference (MANOVA, P = 0.0452). When the temperature was increased there was a non-significant decrease in photosynthetic rate by approximately 9% between the 35˚C and 40˚C curves and an additional non-significant decrease of 13% between the 40˚C to 45˚C (P = 0.4104 and P = 0.2876 respectively). However, there was a significant decrease in photosynthesis between the 35˚C and the 45˚C curves (P = 0.0446, Figure 1(A)).
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Figure 1. Mean repeated measures MANOVA curves of the photosynthetic rates for Juniperus ashei displayed by temperature (A) and CO2 (B) treatment is for main effects only. P-values are shown from the repeated measures MANOVA for the main effects (Temperature and CO2). Like letters at the end of the curves indicate no significant difference between the curves. Data is from three replicates at three concentrations of CO2 (390, 585 and 780 µL/L) and three temperatures (35˚C, 40˚C and 45˚C). Representative error bars are shown indicating ± one standard deviation.
The comparison of the mean photosynthesis rates by CO2 levels shows a significant difference between the three curves at different CO2 levels (MANOVA, P = 0.0003, Figure 1(B)). The total increase was 51% for the curves as the CO2 concentration increased. The CO2 curves showed a similar significant difference between the ambient (390 µL/L) or low CO2 concentration and the middle (585 µL/L) concentration (≈25% increase, P = 0.0306) and the middle and high (780 µL/L) CO2 concentration (≈26% increase, P = 0.0318).
Repeated measures MANOVAs were used to investigate the main effects of light levels, CO2 concentration and temperature on Juniperus ashei. Because the interactions were not significant except for water use efficiency they were removed from the MANOVA (Table 1). For J. ashei as light levels were increased all factors measured changed as the temperature and the CO2 concentrations were increased. However, there were no significant temperature effects on; conduction, intercellular [CO2] concentrations, or transpiration (Table 1). Temperature only had a significant effect on the photosynthetic rates and water use efficiency (WUE). For CO2 concentration there were significant effects on photosynthetic rates, stomatal conduction, intercellular [CO2] concentration, and WUE. Transpiration rate was not significantly affected by increased temperature or CO2 (Table 1).
Table 1. Table of P-values for repeated measures MANOVAs of gas exchange curves for Juniperus ashei comparing main effects of temperature and CO2 at 16 light levels that were held constant (interactions were not significantly different and removed from the models). Data is from three replicates at three CO2 concentrations (390, 585 and 780 µL/L) and three temperatures (35˚C, 40˚C and 45˚C). Significant entries are bold.
Repeated measures MANOVA P-values for Juniperus ashei-without interaction |
Main Effects |
Photosynthetic
Rate |
Stomatal
conductance |
Intercellular CO2 concentration |
Transpiration |
Water Use
Efficiency |
Temperature |
0.0452 |
0.1732 |
0.5070 |
0.2026 |
<0.0001 |
CO2 |
0.0003 |
0.0044 |
<0.0001 |
0.1047 |
<0.0001 |
The maximum photosynthetic rate (Amax) did not change with temperature (ANOVA, P = 0.1468, Table 2). Temperature had little effect on the mean Amax although it did drop by 18% with a standard error of 0.92 µmolCO2·m−2·s−1. The Amax did change significantly with CO2 concentration (ANOVA, P < 0.0001, Table 2). In addition, Tukey comparisons of the CO2 effect showed significant differences between each concentration. Elevating CO2 increased Amax from 9.42 µmolCO2·m−2·s−1. for the ambient CO2 concentration to 12.97 µmolCO2·m−2·s−1. for the middle CO2 concentration and to 17.20 µmolCO2·m−2·s−1. for the high CO2 concentration. This was a total Amax increase of approximately 45% from the low to high CO2 concentration. The interaction term was not significant (P = 0.5961, not shown).
The light saturation point (Lsp) was not significantly different by temperature (ANOVA, P = 0.8776, Table 2). The mean Lsp for the three temperatures were different by 5% with a standard deviation of 23.8 µmolCO2·m−2·s−1. Elevating CO2 had a significant effect on Lsp (ANOVA, P = 0.0001, Table 2). A Tukey comparison showed a significant difference between values for the ambient CO2 Lsp and both the medium CO2 and high CO2 Lsp. There was no significant difference for Lsp between the middle and the high CO2 concentrations. The interaction term was not significant (P = 0.8929, not shown).
Table 2. Factors measured and P-values for Standard Least Squared ANOVAs for Juniperus ashei. Data is from three replicates at three CO2 concentrations (390, 585 and 780 µL/L) and three temperatures (35˚C, 40˚C and 45˚C). Interactions were not significantly different and not shown. Bold entries are significant at 0.05 or less. Capital letters next to a value in a column are significantly different.
Factors And Significance Levels |
Treatment |
Amax |
Lsp |
Lcp |
Rd |
Ø |
CO2 390 |
9.42A |
258A |
21.8A |
1.82A |
0.047A |
CO2 585 |
12.97B |
402B |
35.6A |
1.72A |
0.037A |
CO2 780 |
17.20C |
423B |
33.1A |
1.98A |
0.047A |
Significance |
P = 0.0001 |
P = 0.0001 |
P = 0.3729 |
P = 0.4446 |
P = 0.2075 |
35˚C |
14.46a |
353a |
23.5a |
1.33a |
0.046a |
40˚C |
13.32a |
359a |
26.0a |
0.88ab |
0.044a |
45˚C |
11.82a |
370a |
41.0b |
2.32b |
0.041a |
Significance |
P = 0.1468 |
P = 0.8776 |
P = 0.0003 |
P = 0.0007 |
P = 0.6881 |
The light compensation point (Lcp) showed a significant difference by temperature (ANOVA, P = 0.0003, Table 2) but not by CO2 concentration (ANOVA, P = 0.3729, Table 2). A Tukey comparison showed the 35˚C Lcp was not significantly different than the 40˚C Lcp. The 45˚C Lcp was significantly different from both the 35˚C Lcp and the 40˚C Lcp. There were no significant differences in the Lcp for CO2 concentration (ANOVA, P = 0.3729). The interaction term was not significant (P = 0.5166, not shown).
The ANOVA for the dark respiration rates (Rd) showed a significant difference by temperature but not by CO2 concentration (P = 0.0007 and P = 0.4446, Table 2). Tukey comparison showed the 35˚C Rd was significantly different from the 45˚C Rd while the 40˚C Rd was not significantly different from either the 35˚C or the 45˚C Rd. The CO2 concentration showed no trend with Rd values with increasing CO2 concentration (ANOVA, P = 0.4446). The interaction term was not significant (P = 0.4226, not shown).
The quantum yield (Ø) showed no statistical trend based on temperature (ANOVA, P = 0.6881, Table 2). As with temperature, the CO2 ANOVA showed no significant effect on the Ø values (P = 0.2075, Table 2). The interaction term was not significant (P = 0.9163, not shown).
The mean curves of the water use efficiency (WUE) for J. ashei are shown by temperature, CO2 and light effects (Figure 2(A) and Figure 2(B)). Water use efficiency was significantly different when compared by temperature (MANOVA, P < 0.0001, Figure 2(A)). Water use efficiency values decreased from a plateau of approximately 3.5 mmol·mol−1 to approximately 2.5 mmol·mol−1 as temperature increased to 45˚C or by a total of 21%. The comparisons by CO2 concentration were also statistically significant between the curves (repeated measures MANOVA, P < 0.0001, Figure 2(B)). The curves generally increased as the light levels increased and as the CO2 concentration increased. At the ambient (390 µL/L) or low CO2 concentration the WUE value was lowest at approximately 2.1 mmol·mol−1 (Figure 2(B)). At the highest CO2 concentration, the WUE value increased approximately 50% to a value of approximately 4.2 mmol·mol−1.
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Figure 2. Presented are repeated measures MANOVA curves of main effects on water use efficiency for Juniperus ashei displayed by temperature (A) and CO2 concentration (B) with light levels held constant. P-values are shown from the repeated measures MANOVAs. No like letters at the end of the curves indicate significant difference between curves. There were three concentrations of CO2 (390, 585 and 780 µL/L) and three temperatures (35˚C, 40˚C and 45˚C).
Because there was a significant interaction between light level, temperature, and CO2 concentration for the WUE response an additional figure is presented to demonstrate the effect (Figure 3). The WUE increased with light level (PFD, right axis front to back) and with CO2 concentration (light, dotted to gray shade within each temperature level), but decreased overall with each temperature (X-axis-left to right).
Figure 3. Mean repeated measures MANOVA curves of the water use efficiency for J. ashei interaction of temperature and CO2 concentration. The CO2 concentrations are shown below the plot and represent the three plots within each temperature array. Data is from three replicates at three concentrations of CO2 (390, 585 and 780 µL/L) and three temperatures (35˚C, 40˚C and 45˚C) and 16 light levels.
Figure 4. Photosynthetic response curves for increasing CO2 levels (A) and three temperature (35˚C, 40˚C and 45˚C) and (B) water use efficiency curves for J. ashei at increasing CO2 levels, a light level of 700 µmol∙m−2∙s−1 and three temperatures. Each curve was plotted from a mean of three replicates. P-values are shown from the repeated measures MANOVAs. Error bars are shown indicating ± one standard deviation.
Figures that represent the photosynthetic rate and water use efficiency CO2 response to temperature are shown below (Figure 4(A) and Figure 4(B)). Both the CO2 photosynthetic response and water use efficiency increase with increasing CO2 concentration. Neither curve seems to reach a plateau. The curves follow the same basic trend, with no significant difference to increasing temperature. None of the repeated measures MANOVAs performed on the photosynthetic response, intercellular [CO2], stomatal conductance, and transpiration were significantly different by temperature (Data not shown; P = 0.3405, P = 0.4603, P = 0.1345, P = 0.9629, respectively).
4. Discussion
There are approximately 60 Juniperus species that are present in various places across the Northern Hemisphere occurring from near the equator in Africa and Central America north to the arctic Circle [23]. There are 13 species of Juniperus in North America stretching from Canada in the north through the United States and south into Mexico and Central America [45] [46] Juniperus ashei is a major species in many central Texas woodland communities [37] [47]. In this study, we examined effects of ambient and elevated light levels, atmospheric CO2 and associated higher temperatures on J. ashei gas exchange responses. Comparisons of our results with other species [2] [33] [36] [48] strengthen the position that J. ashei is not a shade-adapted species but more of a sun species [49]-[51].
Sun species tend to have a high maximum photosynthetic rate (Amax), light saturation point (Lsp), light compensation point (Lcp) and dark respiration rates (Rd). Juniperus ashei was shown in this study to have a relatively high Amax value under ambient and at elevated CO2 levels (9.42 - 17.20 µmolCO2·m−2·s−1), as well as also high Lsp, Lcp, and Rd, which indicates it is a low sun or shade intolerant species and will remain so in an elevated CO2 atmosphere. Juniperus ashei Amax values did not change significantly with temperature (11.82 - 14.46 µmolCO2·m−2·s−1) but did increase significantly when CO2 levels were increased (9.42 - 17.20 µmolCO2·m−2·s−1). The light saturation point (Lsp) did not change significantly with temperature but did increase significantly with elevated levels of CO2 which tracks the values of the Amax. The light compensation was not significantly affected by elevated levels of CO2 but almost doubled at the highest temperature J. ashei leaves were exposed to. This was due to increased metabolism at the higher exposure temperature [1] [49].
While the MANOVA analysis showed an overall slight significant decrease in photosynthetic response as the temperature increased for J. ashei, the Amax Least Standard Squares ANOVA comparison did not. A strong reaction would most likely be considered a hindrance to their competitive ability in a higher temperature environment, so this mixed result suggests a minimal impact. Juniperus ashei may further have an ameliorating effect to any temperature influenced competitive disadvantage since it showed a significant increase in photosynthetic rate to elevated CO2. In the semi-arid environment found in central Texas, water use efficiency may play a significant role in species survival and competitive advantage, and changes in plant response due to elevated temperature and CO2 directly affect the species water use efficiency.
The modification to the overall WUE is of note and it closely mimicked the light curves. This is due to the photosynthetic responses decreasing in the low light environment while the transpiration rate only decreased slightly over the lower light levels. As light and CO2 levels increase the water use efficiency increases but there was a significant decrease with increasing temperature. This significant interaction shows that at lower light levels, this species can not properly regulate water loss which is further exacerbated by a rise in temperature. Juniperus ashei juveniles have high mortalities at low light levels and a decrease in water use efficiency might play a role in future survival and recruitment below a canopy [52]. Species that are shade-tolerant usually regulate water use efficiency at reduced light levels allowing them to persist below the canopy. Some of the other species in these woodland understory communities are shrubs with sun species growth characteristics found at canopy edges or canopy breaks [37]. In these communities, there was an absence of many shade species found in the understory which is not fully explained by physiological characteristics of J. ashei the target species in this study.
Over the past century, there has been a large increase in the overall number and density of the large native herbivores in central Texas [53] [54]. Increases in density and number of large herbivores have been found to cause alterations to the local plant community compositions and dynamics in habitats all over the world [19] [55]-[59]. Almost all woody species in the study area are susceptible to juvenile herbivory and populations have a minimal cohort for recruiting except J. ashei [37]. The herbivory of J. ashei was not examined directly in the current study, however it is not eaten by Odocoileus virginianus, white-tailed deer [20]. This herbivore has been shown to cause establishment difficulties for many plant species in central Texas woodlands [54] [55] [57] [60].
Juniperus woodlands appear to be successional communities [1] [17] [37]. In the eastern North American deciduous forests, Juniperus plants are often found in gaps, blow downs or on shallow soil in glades [61]. In western North America, Juniperus tends to occur above the desert communities and above the arid or semiarid grasslands, but usually below the higher-elevation pine, spruce, or fir forests [12] [16] [17]. In central Texas, J. ashei establishes on hillsides and in former grasslands on shallow soil [22] [27].
Juniperus woodlands in many parts of the world are probably caused by a number of factors, with constant high levels of grass herbivory and a reduction of grassland fire frequency being dominant [10] [22] [37]. Juniperus and other early successional woody species, are favored with the reduction of grassland fire frequency producing various savannas and woodlands [59]. Overgrazing by domestic animals reduces the biomass and growth of the grasses while allowing the woody species to take advantage of the reduced competition for resources [1] [59] [61]. This difficulty in maintenance of the C4 southern grasses is certainly domestic animal herbivory but for various woody species it seems possibly to be competition for water by more shade tolerant species [19] [58] [62]-[65]. The study species is found in arid and semi-arid zones where droughts are common. In related species like J. excelsa, a decrease in photosynthesis during drought has been observed [66]. Also, in drought studies, Juniperus Amax was greatest near zero water potential and lowest when stressed at low water potential [65] [66]. Furthermore, J. ashei seedlings are strongly influenced by light levels, with higher light levels leading to interactions between water and nutrients that support continued growth [28]. In future studies the importance of drought on J. ashei seedlings should be examined along with interactions with other important environmental factors.
5. Conclusion
Over the past century, plant communities have been changed through the increased browsing pressure from large herbivores as well as the suppression of grassland fires. In the more recent decades and going into the future this has been and will be further complicated by the increasing air temperatures and CO2 concentrations. Some species will be able to take advantage of the new conditions and expand their numbers, while other species lose competitive advantage and decline in number potentially resulting in different and new dominant species and community structure. We expect these central Texas Juniperus/Quercus woodlands will be part of these shifts and dynamic changes. Based off our study results, we believe J. ashei will gain some competitive advantages in the higher light levels of the open woodland canopy gaps with higher future CO2 concentrations which should allow it to encroach and establish better in those areas. But below the canopy in the lower light levels, it does not seem to maintain the same advantages which means it may be replaced or at least lose some of its dominance within the existing woodland areas. Studying community dynamics and predicting future community composition has always been a challenging mission but with the added complications of forecasted environmental changes this has become an even more enigmatic puzzle to tease apart.
Acknowledgements
We would like to thank Samantha Daywood and Jason Gagliardi for their help in the field, especially in data collection. Thanks to Dr. Janis Bush who helped with various aspects of the work reported here. Many helpful suggestions were made by Jason Gagliardi, who read an earlier iteration of this manuscript.