We measured whole-tree transpiration of mature Fagus sylvatica and Picea abies trees exposed to ambient and twice-ambient O-3 regimes (1xO(3) and 2xO(3) free-air fumigation). After eight years, mean daily total transpiration did not vary with the O-3 regime over the 31 days of our study, even though individual daily values increased with increasing daily O-3 peaks in both species. Although the environmental parameters were similar at 1xO(3) and 2xO(3), the main factors affecting daily transpiration were vapour pressure deficit in 2xO(3) spruce and O-3 peaks in beech. For a mechanistic explanation, we measured O-3-induced sluggish stomatal responses to variable light (sunflecks) by means of leaf-level gas exchange measurements only in the species where O-3 was a significant factor for transpiration, i.e., beech. Stomata were always slower in closing than in opening. The 2xO(3) stomata were slower in opening and mostly in closing than 1xO(3) stomata, so that O-3 uptake and water loss were amplified before a steady state was reached. Such delay in the stomatal reaction suggests caution when assessing stomatal conductance under O-3 pollution, because recording gas exchange at the time photosynthesis reached an equilibrium resulted in a significant overestimation of stomatal conductance when stomata were closing (ab. 90% at 1xO(3) and 250% at 2xO(3)). Sun and shade leaves showed similar sluggish responses, thus suggesting that sluggishness may occur within the entire crown. The fact that total transpiration was similar at 1xO(3) and 2xO(3), however, suggests that the higher water loss due to stomatal sluggishness was offset by lower steady-state stomatal conductance at 2xO(3). In conclusion, O-3 exposure amplified short-term water loss from mature beech trees by slowing stomatal dynamics, while decreased long-term water loss because of lower steady-state stomatal conductance. Over the short term of this experiment, the two responses offset each other and no effect on total transpiration was observed.

Ozone Amplifies Water Loss from Mature Trees in the Short Term But Decreases It in the Long Term

Paoletti, Elena;
2020

Abstract

We measured whole-tree transpiration of mature Fagus sylvatica and Picea abies trees exposed to ambient and twice-ambient O-3 regimes (1xO(3) and 2xO(3) free-air fumigation). After eight years, mean daily total transpiration did not vary with the O-3 regime over the 31 days of our study, even though individual daily values increased with increasing daily O-3 peaks in both species. Although the environmental parameters were similar at 1xO(3) and 2xO(3), the main factors affecting daily transpiration were vapour pressure deficit in 2xO(3) spruce and O-3 peaks in beech. For a mechanistic explanation, we measured O-3-induced sluggish stomatal responses to variable light (sunflecks) by means of leaf-level gas exchange measurements only in the species where O-3 was a significant factor for transpiration, i.e., beech. Stomata were always slower in closing than in opening. The 2xO(3) stomata were slower in opening and mostly in closing than 1xO(3) stomata, so that O-3 uptake and water loss were amplified before a steady state was reached. Such delay in the stomatal reaction suggests caution when assessing stomatal conductance under O-3 pollution, because recording gas exchange at the time photosynthesis reached an equilibrium resulted in a significant overestimation of stomatal conductance when stomata were closing (ab. 90% at 1xO(3) and 250% at 2xO(3)). Sun and shade leaves showed similar sluggish responses, thus suggesting that sluggishness may occur within the entire crown. The fact that total transpiration was similar at 1xO(3) and 2xO(3), however, suggests that the higher water loss due to stomatal sluggishness was offset by lower steady-state stomatal conductance at 2xO(3). In conclusion, O-3 exposure amplified short-term water loss from mature beech trees by slowing stomatal dynamics, while decreased long-term water loss because of lower steady-state stomatal conductance. Over the short term of this experiment, the two responses offset each other and no effect on total transpiration was observed.
2020
Istituto di Ricerca sugli Ecosistemi Terrestri - IRET
sunflecks
Kranzberg
stomatal sluggishness
transpiration
tropospheric ozone
water cycle
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/407523
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