AbstractThe resistance of xylem to cavitation has been proposed to be an important component of drought tolerance. Drought tolerance may play a role in the success of Juniperus (Cupressaceae) species, many of which are increasing in density and distribution in the western and central United States. We studied interspecific variation in vulnerability to water-stress-induced cavitation across Juniperus species. Our objectives were to compare root and stem vulnerability to cavitation in Juniperus species with distributions occurring along an aridity gradient and to determine if a tradeoff exists between resistance to cavitation and hydraulic conductivity. Stem (n=6-8) and shallow root (n=4-6) samples were collected in mid-summer, 2001, and vulnerability curves were constructed using the centrifugal force method to generate cavitation at known tensions. Stems of J. ashei (Ashe juniper), which is native to semi-arid central Texas, were most resistant, with a 50% loss of conductivity (Y50%) at –12.8 (±0.6) MPa. In contrast, stems of J. virginiana (eastern redcedar), which is native to the more mesic eastern United States, had Y50% at –5.9 (±0.2) MPa. Roots were more vulnerable than stems in three of five species. There was no evidence of a tradeoff between cavitation resistance and hydraulic conductance in roots or stems among species. Differences in vulnerability to cavitation in closely-related species suggest that cavitation resistance is an adaptation to arid environments and may play a role in determining species distributions. |
Background
Objectives
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MethodsStudy sites: Collection sites were as follows: J. ashei stems in Austin, TX, J. deppeana, J. monosperma, J. osteosperma, and J. scopulorum stems and roots near Flagstaff, AZ, J. virginiana stems and roots in central NC. Stems (n=6-8) and shallow (30-40 cm) roots (n=4-6) were collected in mid-morning in June and July, 2001, except for J. virginiana roots, which were collected in October, 2000.
Vulnerability curves and conductivity: A vulnerability curve describes the relationship of percent loss in hydraulic conductivity (% embolism) as a function of xylem tension (Y, MPa). We used the centrifuge technique (Pockman et al. 1995, Alder et al. 1997) to measure vulnerability of xylem to water-stress-induced cavitation. Stem and root segments were spun to sequential xylem tensions (Y, MPa), resulting in a measurable loss of hydraulic conductivity (kh).
To fit vulnerability curves and estimate Y50% (the water potential resulting in a 50% loss of conductivity), percent loss of conductivity (PLC) was modeled as an exponential sigmoidal function of water potential (Y) (Pammenter and Vander Willigen 1998): where b is Y50%. Conductivity (kh) was also normalized by cross-sectional stem area (ks) and leaf area (kl) to explore relationships with Y50%. Statistical analyses: We estimated Y50% by using the above equation and the nonlinear regression procedure of the S-PLUS statistical software package. Means were compared using t-tests and significance was determined by the Bonferroni correction for multiple comparisons. |
Results | |
| Figure 1: Stem vulnerability curves | Figure 2: Root vulnerability curves |
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| Figure 3: Y50% in stems and roots | |
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| Figure 4: Y50% versus hydraulic conductivity | |
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OBJECTIVE 1:
OBJECTIVE 2:
OBJECTIVE 3:
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Conclusions
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Alder, NN, WT Pockman, JS Sperry, and S Nuismer. 1997. Use of centrifugal force in the study of xylem cavitation. Journal of Experimental Botany 48:665-674.
Jackson, RB, JS Sperry, TE Dawson. 2000. Root water uptake and transport: using physiological processes in global predictions. Trends in Plant Science 5:482:488.
Pammenter, NW, and C Vander Willigen. 1998. A mathematical and statistical analysis of the curves illustrating vulnerability of xylem to cavitation. Tree Physiology 18:589-593.
Pockman, WT, JS Sperry, and JW O’Leary. 1995. Sustained and significant negative pressure in xylem. Nature 378:715-716.
West, NE 1988. Intermountain deserts, shrub steppes, and woodlands. North American Terrrestrial Vegetation (eds M. G. Barbour and W. D. Billings), pp 209-230. Cambridge University Press, Cambridge.
We thank Walnut Canyon National Monument and National Park Service staff, M. Sanders of Austin Parks and Recreation Department, N. Douglas, C. Moura, and K. Ogle. This study was funded by an NSF Graduate Research Fellowship to CJ W, a Duke University Giles/Keever grant to CJW, and a USDA grant to RBJ and WTP.
Contact information:Cynthia J. Willson | Hafiz Maherali | William T. Pockman | Robert B. Jackson
| cjw@duke.edu | maherali@duke.edu | pockman@unm.edu | jackson@duke.edu
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This poster was presented at the 2001 Ecological Society of America meeting.
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