Disentangling the relative impacts of precipitation reduction
and vapour pressure deficit (VPD) on plant water dynamics
and determining whether acclimation may influence these
patterns in the future is an important challenge. Here, we
report sap flux density (FD), stomatal conductance (Gs),
hydraulic conductivity (KL) and xylem anatomy in piñon pine
(Pinus edulis) and juniper (Juniperus monosperma) trees
subjected to five years of precipitation reduction, atmospheric
warming (elevated VPD) and their combined effects. No
acclimation occurred under precipitation reduction: lower Gs
and FD were found for both species compared to ambient
conditions. Warming reduced the sensibility of stomata to
VPD for both species but resulted in the maintenance of Gs
and FD to ambient levels only for piñon. For juniper, reduced
soil moisture under warming negated benefits of stomatal
adjustments and resulted in reduced FD, Gs and KL. Although
reduced stomatal sensitivity to VPD also occurred under
combined stresses, reductions in Gs, FD and KL took place to
similar levels as under single stresses for both species. Our
results show that stomatal conductance adjustments to high
VPD could minimize but not entirely prevent additive effects
of warming and drying on water use and carbon acquisition
of trees in semi-arid regions.
Revised: February 4, 2021 |
Published: August 14, 2017
Citation
Grossiord C., S. Sevanto, I. Borrego, A.M. Chan, A.D. Collins, L.T. Dickman, and P.J. Hudson, et al. 2017.Tree water dynamics in a drying and warming world.Plant, Cell & Environment 40, no. 9:1861-1873.PNNL-SA-129758.doi:10.1111/pce.12991