Abstract
Plant metabolic activity in arid and semi-arid environments is largely tied to episodic precipitation events or “pulses”. The ability of plants to take up and utilize rain pulses during the growing season in these water-limited ecosystems is determined in part by pulse timing, intensity and amount, and by hydrological properties of the soil that translate precipitation into plant-available soil moisture. We assessed the sensitivity of an invasive woody plant, velvet mesquite (Prosopis velutina Woot.), to large (35 mm) and small (10 mm) isotopically labeled irrigation pulses on two contrasting soil textures (sandy-loam vs. loamy-clay) in semi-desert grassland in southeastern Arizona, USA. Predawn leaf water potential (Ψpd), the isotopic abundance of deuterium in stem water (δD), the abundance of 13C in soluble leaf sugar (δ13C), and percent volumetric soil water content (θv) were measured prior to irrigation and repeatedly for 2 weeks following irrigation. Plant water potential and the percent of pulse water present in the stem xylem indicated that although mesquite trees on both coarse- and fine-textured soils quickly responded to the large irrigation pulse, the magnitude and duration of this response substantially differed between soil textures. After reaching a maximum 4 days after the irrigation, the fraction of pulse water in stem xylem decreased more rapidly on the loamy-clay soil than the sandy-loam soil. Similarly, on both soil textures mesquite significantly responded to the 10-mm pulse. However, the magnitude of this response was substantially greater for mesquite on the sandy-loam soil compared to loamy-clay soil. The relationship between Ψpd and δ13C of leaf-soluble carbohydrates over the pulse period did not differ between plants at the two sites, indicating that differences in photosynthetic response of mesquite trees to the moisture pulses was a function of soil water availability within the rooting zone rather than differences in plant biochemical or physiological constraints. Patterns of resource acquisition by mesquite during the dynamic wetting–drying cycle following rainfall pulses is controlled by a complex interaction between pulse size and soil hydraulic properties. A better understanding of how this interaction affects plant water availability and photosynthetic response is needed to predict how grassland structure and function will respond to climate change.
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Acknowledgements
We thank Andrea Scartazza (CNR, Porano, Italy) for his indispensable assistance during the carbohydrate extraction and Bill Cable for his assistance in the field. We also thank Mark Larson (University of Wyoming, Laramie, USA) for helping with the carbon isotope analysis. The valuable help of Michael Whitchurch during the manuscript preparation is also acknowledged. Precipitation and temperature data were provided by the SRER database. This study was sponsored by the Student Final Project Fund from the University of Arizona and a USDA-NRI Grant (# 00-35101-9308).
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Fravolini, A., Hultine, K.R., Brugnoli, E. et al. Precipitation pulse use by an invasive woody legume: the role of soil texture and pulse size. Oecologia 144, 618–627 (2005). https://doi.org/10.1007/s00442-005-0078-4
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DOI: https://doi.org/10.1007/s00442-005-0078-4