EGU24-7683, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-7683
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Disentangling direct effects of temperature and vapour pressure deficit on leaf gas exchange: mechanistic insights from online stable isotope techniques

Haoyu Diao1, Lucas A. Cernusak2, Matthias Saurer1, Arthur Gessler1,3, Rolf T.W. Siegwolf1, and Marco M. Lehmann1
Haoyu Diao et al.
  • 1Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf 8903, Switzerland
  • 2College of Science and Engineering, James Cook University, Cairns, Queensland 4879, Australia
  • 3Institute of Terrestrial Ecosystems, ETH Zurich, Zurich 8092, Switzerland

Strong covariation between temperature and vapour pressure deficit (VPD) in nature creates challenges for understanding the direct effects of the two on leaf gas exchange. Measurements of stable isotope discrimination in CO2 and H2O provide additional insights into physiological and biochemical processes during leaf gas exchange. We investigated mechanistic causes of variations in net photosynthesis rate (An) and stomatal conductance (gs) with increasing temperature at constant VPD and increasing VPD at constant temperatures.

We conducted combined leaf gas exchange and online isotope discrimination measurements on four common European tree species (Fagus sylvatica, Picea abies, Quercus petraea, and Tilia cordata) (1) across a temperature range of 5–40°C, while maintaining a constant VPD (~0.8 kPa) and (2) across a VPD range of 1–4 kPa, while maintaining a constant temperature (~30°C). The experiments were conducted without soil water limitation. The whole plant along with the whole instrumental setup were heated to prevent condensation when the dew point temperature within the leaf cuvette was higher than the room temperature.

Above the optimum temperature for photosynthesis (~30°C), we observed a decoupling of gs and An across all tested species, with gs increasing but An decreasing. Measurements of carbon and oxygen isotope discrimination indicated that during this decoupling, mesophyll conductance to the chloroplast decreased consistently and significantly among species; however, this reduction did not lead to reductions in CO2 concentration at the chloroplast surface or the chloroplast stroma. Both gs and An decreased, while the transpiration rate increased with increasing VPD. The relative humidity inside the leaf, derived from the oxygen isotope discrimination measurements, decreased from 100% to around 70% with increasing VPD, suggesting a progressive unsaturation of vapour pressure in the substomatal cavity. Accounting for the unsaturation, we found decreased CO2 concentration in the intercellular air spaces and at the chloroplast stroma with increasing VPD; however, mesophyll conductance and CO2 concentration at the chloroplast surface remained relatively stable.

We conclude that the effects of temperature and VPD on leaf gas exchange are distinctly different. The reduction in An at higher temperatures, unlike that at higher VPD, was not associated with stomatal closure and thus a restricted supply of CO2 to the chloroplasts. Instead, it was more likely caused by Rubisco deactivation and/or a reduction of the electron transport rate. The unsaturation of vapour pressure inside leaves must not be ignored at VPD higher than 1 kPa, as it is vital for accurate estimations of gs and the CO2 concentration in the internal air spaces of leaves. Under non limiting soil water supply, the increases in leaf water loss due to increased leaf transpiration at higher temperature and VPD are important for plants to strategically cope with severe heat and dry conditions.

How to cite: Diao, H., Cernusak, L. A., Saurer, M., Gessler, A., Siegwolf, R. T. W., and Lehmann, M. M.: Disentangling direct effects of temperature and vapour pressure deficit on leaf gas exchange: mechanistic insights from online stable isotope techniques, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-7683, https://doi.org/10.5194/egusphere-egu24-7683, 2024.