Understanding sources of variation in plant water-use efficiency.
Stomata regulate carbon dioxide (CO2) uptake by photosynthesis and water loss through transpiration. Accurate model representation of this process, called stomatal conductance, is therefore key for modeling CO2 and water fluxes. The approaches used to represent stomatal conductance in models vary. Current understanding of the drivers of the variation in a key parameter in those models—the slope parameter, which is a measure of plant water-use efficiency—is still limited, particularly in the tropics. Scientists from Brookhaven National Laboratory and the Next-Generation Ecosystem Experiments (NGEE)–Tropics team evaluated the ability of current model formulations to predict observed stomatal conductance, including the inclusion of leaf water potential, and investigated the sources of variation in the slope parameter. They found that inclusion of leaf water potential did not improve model predictions and that model formulations that included vapor pressure deficit performed better than those that relied on relative humidity.
Although the value of stomatal slope can have a large impact on simulated carbon and water fluxes, the understanding of what drives the variation in slope parameter is still limited. This study presents a novel integration of rare measurements of gas exchange from the upper canopy of a tropical forest in Panama and a suite of plant traits with analysis that advances the understanding of dominant drivers of stomatal slope variability and identifies a practical, trait-based approach to improve modeling of carbon and water exchange in tropical forests.
Stomatal slope is inferred from an example stomatal conductance model. For a given CO2 assimilation rate, atmospheric CO2 concentration, and leaf-to-air vapor pressure deficit (collectively, the x-axis), a higher slope means that plants maintain a higher stomatal conductance (y-axis) for a given photosynthetic rate. As such, the slope parameter is an indicator of plant water use efficiency, and a greater slope equates to a lower water use efficiency. The team performed diurnal gas exchange measurements (resulting in background scatterplots) for two example species (Ventilago ferruginea and Terminalia amazonia).
BER Program Manager
U.S. Department of Energy Office of Science, Office of Biological and Environmental Research
Earth and Environmental Systems Sciences Division (SC-33.1)
Environmental System Science
Brookhaven National Laboratory
This work was funded by the Next-Generation Ecosystem Experiments (NGEE)–Tropics project in the Terrestrial Ecosystem Science (TES) program of the Office of Biological and Environmental Research (BER), within the U.S. Department of Energy (DOE) Office of Science.
Wu, J., S. P. Serbin, K. S. Ely, B. T. Wolfe, L. T. Dickman, C. Grossiord, S. T. Michaletz, A. D. Collins, M. Detto, N. G. McDowell, S. J. Wright, and A. Rogers. “The response of stomatal conductance to seasonal drought in tropical forests.” Global Change Biology 26(2), 823–39. (2020). [DOI:10.1111/gcb.14820].
SC-33.1 Earth and Environmental Sciences Division, BER
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