Multidecadal records of intrinsic water-use efficiency in the desert shrub Encelia farinosa reveal strong responses to climate change
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Contributed by James R. Ehleringer, June 10, 2020 (sent for review April 29, 2020; reviewed by Travis E. Huxman and Susan Schwinning)

Significance
As the proportion of land area covered by arid land vegetation continues to expand and water limitations for plants increase, understanding if and how desert shrubs are responding to environmental change has become more urgent. Among two populations of Mojave Desert shrubs, we found that intrinsic water-use efficiency has increased substantially over the last three decades in response to increasing aridity and CO2 concentration. While increases in intrinsic water-use efficiency have been widely assumed to mitigate negative effects of decreasing water availability, precise effects on plant productivity, reproduction, and survival remain unknown.
Abstract
While tree rings have enabled interannual examination of the influence of climate on trees, this is not possible for most shrubs. Here, we leverage a multidecadal record of annual foliar carbon isotope ratio collections coupled with 39 y of survey data from two populations of the drought-deciduous desert shrub Encelia farinosa to provide insight into water-use dynamics and climate. This carbon isotope record provides a unique opportunity to examine the response of desert shrubs to increasing temperature and water stress in a region where climate is changing rapidly. Population mean carbon isotope ratios fluctuated predictably in response to interannual variations in temperature, vapor pressure deficit, and precipitation, and responses were similar among individuals. We leveraged the well-established relationships between leaf carbon isotope ratios and the ratio of intracellular to ambient CO2 concentrations to calculate intrinsic water-use efficiency (iWUE) of the plants and to quantify plant responses to long-term environmental change. The population mean iWUE value increased by 53 to 58% over the study period, much more than the 20 to 30% increase that has been measured in forests [J. Peñuelas, J. G. Canadell, R. Ogaya, Glob. Ecol. Biogeogr. 20, 597–608 (2011)]. Changes were associated with both increased CO2 concentration and increased water stress. Individuals whose lifetimes spanned the entire study period exhibited increases in iWUE that were very similar to the population mean, suggesting that there was significant plasticity within individuals rather than selection at the population scale.
Footnotes
- ↵1To whom correspondence may be addressed. Email: jim.ehleringer{at}utah.edu.
This contribution is part of the special series of Inaugural Articles by members of the National Academy of Sciences elected in 2016.
Author contributions: J.R.E. designed research; A.W.D., N.Q.B., D.R.S., and J.R.E. performed research; A.W.D., N.Q.B., and J.R.E. analyzed data; and A.W.D., N.Q.B., D.R.S., and J.R.E. wrote the paper.
Reviewers: T.E.H., University of California, Irvine; and S.S., Texas State University.
The authors declare no competing interest.
This article contains supporting information online at https://www.pnas.org/lookup/suppl/doi:10.1073/pnas.2008345117/-/DCSupplemental.
Data Availability.
All data that are reported in this manuscript are provided in SI Appendix, Table S4, including data on climate, CO2 concentration and δ13C, population and sample sizes, and population mean δ13C values, ci/ca ratios, and iWUE values.
- Copyright © 2020 the Author(s). Published by PNAS.
This open access article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND).
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