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Didion-Gency, M.

Publications and source records attributed to Didion-Gency, M..

3 recordsLinked to original sources

Living on the edge: warmer climate reduces leaf thermal safety margins and causes gas exchange decoupling in Mediterranean shrubs

Global warming pushes plants close to their leaf thermal limits, altering carbon uptake, growth and survival. Therefore, investigating leaf thermal tolerance adjustment is essential to understand future vegetation dynamics, especially in high-risk Mediterranean shrubs facing hot and dry summers. We measured dark-adapted leaf fluorescence (Fv/Fm), thermal thresholds (Tcrit, T50, Tmax), optimal assimilation temperature (Topt), thermal safety margin (TSM), leaf and air- temperatures (Tair, Tleaf) and gas exchange (A, gs, E) in six shrub species in six sites along a climatic gradient in Catalonia, Spain. We found that Topt increased as conditions warmed, while Fv/Fm and Tmax showed quadratic responses decreasing in the warmest sites. Hence, TSM declined and approached 0 at the hottest sites, indicating that shrubs were operating close to their thermal limits. Warmer Tair under high levels of solar radiation raised Tleaf, though some species maintained Tleaf < Tair during daytime, suggesting a passive or active leaf cooling at high temperatures exceeding solar energy. Moreover, E remained high despite low A at higher Tleaf, revealing a decoupling of gas exchange at high temperatures. Incorporating leaf thermal tolerance adjustments and gas exchange decoupling at extreme temperatures into vegetation models could improve predictions of shrub function and dynamics under warmer climates. HighlightOur study highlights that Mediterranean shrubs have limited capacity to adjust leaf thermal tolerance at warmer sites, resulting in narrower thermal safety margins. The decrease in leaf temperatures through evaporative cooling may not compensate for the more frequent and intense heatwaves, leading to irreversible damage. These findings highlight the importance of incorporating leaf thermal tolerance adjustment and gas exchange decoupling into future vegetation models.

ecology↗

Decoupling of stomatal conductance from net assimilation at high temperature as a mechanism to increase transpiration

O_LIPhotosynthetic assimilation (Anet) and stomatal conductance (gs) are usually strongly coupled, but this relationship is decreased or even lost at high temperatures (Tair). The contributions of environmental drivers (Tair, vapour pressure deficit (VPD), and soil moisture) in interaction with the physiological mechanisms behind this process are still unclear. C_LIO_LIWe exposed saplings of three temperate and tropical species to rising Tair (20 to 40{degrees}C) at low (1.2 to 1.9 kPa) and increasing VPD (1.1 to 5.6 kPa), and at stable Tair (35{degrees}C) to increasing VPD (1.4 to 4.3 kPa) under well-watered or chronic soil drought conditions ([&le;]10 %). Anet, gs, and transpiration (E) in the light and the dark and leaf thermoregulation were tracked throughout the experiment. C_LIO_LIWhen VPD remained low, gs continued to increase while Anet decreased at Tair > 35{degrees}C, leading to stomatal decoupling. In contrast, under rising VPD, trees maintained the coupling between Anet and gs at high Tair. C_LIO_LIWhile a decoupling of Anet and gs only occurred when VPD was low, Anet and E decoupled under both VPD regimes at high Tair. C_LIO_LIOur results indicate that, since gs and VPD collectively drive E, stomatal decoupling is needed to increase E when VPD is not sufficiently high. C_LI

plant biology↗

Chronic warming and dry soils limit carbon uptake and growth despite a longer growing season in beech and oak

Progressively warmer and drier conditions impact tree phenology and carbon cycling with large consequences for forest carbon balance. However, it remains unclear how individual impacts of warming and drier soils differ from their combined one and how species interactions modulate tree responses. Using mesocosms, we assessed the multi-year impact of continuous air warming and lower soil moisture acting alone or combined on phenology, leaf-level photosynthesis, non-structural carbohydrate concentrations, and aboveground growth of young European beech and Downy oak trees. We further tested how species interactions (monocultures vs. mixtures) modulated these effects. Warming prolonged the growing season of both species but reduced growth for oak. In contrast, lower moisture did not impact phenology but reduced trees assimilation and growth for both species. Combined impacts of warming and drier soils did not differ from single ones. Performances of both species in the mixtures were enhanced compared to the monocultures under extreme conditions. Our work revealed that higher temperature and lower soil moisture have contrasting impacts on phenology vs. leaf-level assimilation and growth, with the former being driven by temperature and the latter by moisture. Furthermore, we show a compensation of the negative impacts of extreme events by tree species interactions.

physiology↗