Climate Gradients Underlie Geographical Variations in iWUE and δ 15N Values of Encelia

• Published in: Plant-environment interactions (Hoboken, N.J. : 2018) Vol. 6; no. 4
• Main Authors: Lengyel, Tegan E., Karavan‐Jahromi, Iman, Driscoll, Avery W., Ehleringer, James R.
• Format: Journal Article
• Language: English
• Published: Hoboken John Wiley and Sons Inc 28.08.2025
• DOI: 10.1002/pei3.70080

This study assessed variations in leaf intrinsic water use efficiency (iWUE) and δ 15 N values among Encelia , a genus of drought‐deciduous shrubs distributed across arid regions of southwestern North America between 1972 and 1980 when climates were cooler than today. We hypothesized that geographical variations in climate would significantly influence iWUE, a response to water‐related climate constraints, and δ 15 N values, a proxy for the balance between N 2 fixation and denitrification. Leaf samples were collected from six species of Encelia across 78 sites representing the genus range. The δ 15 N and δ 13 C values of these samples were measured and analyzed to identify drivers of spatial variability. Significant variations among iWUE and δ 15 N values were observed as a function of climate, along a spring–summer precipitation gradient. Precipitation and vapor pressure deficit (VPD) were significant drivers of variations in iWUE values, with iWUE increasing with VPD and/or decreasing precipitation, as would be predicted based on water‐related constraints on leaf gas exchange. Climate values were significant drivers of variations in δ 15 N values, with lower δ 15 N values occurring in cooler temperature, spring‐growing plants (northern latitudes) than in warmer summer‐growing plants (southern latitudes). Encelia leaf iWUE and δ 15 N observations suggest few, if any, species‐specific differences; but more likely that there is high plasticity in these values driven by variations in climate. Variations in the intrinsic water use efficiency and nitrogen isotope ratios of the desert shrub Encelia are associated with climate. Higher intrinsic water use efficiencies are associated with drier climates, whereas higher nitrogen isotope ratios are associated with warmer year‐round temperatures.