Trees tolerate an extreme heatwave via sustained transpirational cooling and increased leaf thermal tolerance

Heatwaves are likely to increase in frequency and intensity with climate change, which may impair tree function and forest C uptake. However, we have little information regarding the impact of extreme heatwaves on the physiological performance of large trees in the field. Here, we grew Eucalyptus pa...

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Bibliographic Details
Published in:Global change biology 2018-06, Vol.24 (6), p.2390-2402
Main Authors: Drake, John E., Tjoelker, Mark G., Vårhammar, Angelica, Medlyn, Belinda E., Reich, Peter B., Leigh, Andrea, Pfautsch, Sebastian, Blackman, Chris J., López, Rosana, Aspinwall, Michael J., Crous, Kristine Y., Duursma, Remko A., Kumarathunge, Dushan, De Kauwe, Martin G., Jiang, Mingkai, Nicotra, Adrienne B., Tissue, David T., Choat, Brendan, Atkin, Owen K., Barton, Craig V. M.
Format: Article
Language:English
Subjects:
Air temperature
Canopies
Canopy
Carbon dioxide
Climate Change
Climate models
Cooling
Decoupling
Environmental Sciences
Eucalyptus
Eucalyptus - physiology
Eucalyptus parramattensis
Forests
Global warming
Heat exchange
heatwave
High temperature
Hot Temperature
Landscape
latent cooling
Leaves
Life Sciences
Photosynthesis
Physiology
Plant Leaves - physiology
Plant Transpiration - physiology
Soil
Soil surfaces
temperature
Temperature tolerance
Thermal stress
thermal tolerance
Transpiration
Trees
Trees - physiology
Uptake
warming
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Summary:Heatwaves are likely to increase in frequency and intensity with climate change, which may impair tree function and forest C uptake. However, we have little information regarding the impact of extreme heatwaves on the physiological performance of large trees in the field. Here, we grew Eucalyptus parramattensis trees for 1 year with experimental warming (+3°C) in a field setting, until they were greater than 6 m tall. We withheld irrigation for 1 month to dry the surface soils and then implemented an extreme heatwave treatment of 4 consecutive days with air temperatures exceeding 43°C, while monitoring whole‐canopy exchange of CO2 and H2O, leaf temperatures, leaf thermal tolerance, and leaf and branch hydraulic status. The heatwave reduced midday canopy photosynthesis to near zero but transpiration persisted, maintaining canopy cooling. A standard photosynthetic model was unable to capture the observed decoupling between photosynthesis and transpiration at high temperatures, suggesting that climate models may underestimate a moderating feedback of vegetation on heatwave intensity. The heatwave also triggered a rapid increase in leaf thermal tolerance, such that leaf temperatures observed during the heatwave were maintained within the thermal limits of leaf function. All responses were equivalent for trees with a prior history of ambient and warmed (+3°C) temperatures, indicating that climate warming conferred no added tolerance of heatwaves expected in the future. This coordinated physiological response utilizing latent cooling and adjustment of thermal thresholds has implications for tree tolerance of future climate extremes as well as model predictions of future heatwave intensity at landscape and global scales. Heatwaves are likely to increase in frequency and intensity, but we know relatively little about how trees will respond. Here, we documented that large trees growing in the field responded to an extreme heatwave with a coordinated physiological response involving continued leaf cooling from transpiration and a rapid increase in leaf thermal tolerance. The Eucalyptus trees that we studied were remarkably capable of tolerating an extreme heatwave via mechanisms that have implications for future heatwave intensity and forest resilience in a warmer world.
ISSN:1354-1013
1365-2486
DOI:10.1111/gcb.14037