Leaf warming in the canopy of mature tropical trees reduced photosynthesis due to downregulation of photosynthetic capacity and reduced stomatal conductance
Corresponding Author
Kristine Y. Crous
Hawkesbury Institute for the Environment, Western Sydney University, Penrith, NSW, 2751 Australia
School of Science, Western Sydney University, Penrith, NSW, 2751 Australia
Author for correspondence:
Kristine Y. Crous
Email: [email protected]
Search for more papers by this authorKali B. Middleby
Centre for Tropical Environmental and Sustainability Science (TESS) and College of Science and Engineering, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorAlexander W. Cheesman
Centre for Tropical Environmental and Sustainability Science (TESS) and College of Science and Engineering, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorAngelina Y. M. Bouet
Centre for Tropical Environmental and Sustainability Science (TESS) and College of Science and Engineering, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorMichele Schiffer
Division of Research – Research Infrastructure, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorMichael J. Liddell
Centre for Tropical Environmental and Sustainability Science (TESS) and College of Science and Engineering, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorCraig V. M. Barton
Hawkesbury Institute for the Environment, Western Sydney University, Penrith, NSW, 2751 Australia
Search for more papers by this authorLucas A. Cernusak
Centre for Tropical Environmental and Sustainability Science (TESS) and College of Science and Engineering, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorCorresponding Author
Kristine Y. Crous
Hawkesbury Institute for the Environment, Western Sydney University, Penrith, NSW, 2751 Australia
School of Science, Western Sydney University, Penrith, NSW, 2751 Australia
Author for correspondence:
Kristine Y. Crous
Email: [email protected]
Search for more papers by this authorKali B. Middleby
Centre for Tropical Environmental and Sustainability Science (TESS) and College of Science and Engineering, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorAlexander W. Cheesman
Centre for Tropical Environmental and Sustainability Science (TESS) and College of Science and Engineering, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorAngelina Y. M. Bouet
Centre for Tropical Environmental and Sustainability Science (TESS) and College of Science and Engineering, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorMichele Schiffer
Division of Research – Research Infrastructure, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorMichael J. Liddell
Centre for Tropical Environmental and Sustainability Science (TESS) and College of Science and Engineering, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorCraig V. M. Barton
Hawkesbury Institute for the Environment, Western Sydney University, Penrith, NSW, 2751 Australia
Search for more papers by this authorLucas A. Cernusak
Centre for Tropical Environmental and Sustainability Science (TESS) and College of Science and Engineering, James Cook University, Cairns, Qld, 4878 Australia
Search for more papers by this authorSummary
- Tropical forests play a large role in the global carbon cycle by annually absorbing 30% of our annual carbon emissions. However, these forests have evolved under relatively stable temperature conditions and may be sensitive to current climate warming. Few experiments have investigated the effects of warming on large, mature trees to better understand how higher temperatures affect these forests in situ.
- We targeted four tree species (Endiandra microneura, Castanospermum australe, Cleistanthus myrianthus and Myristica globosa) of the Australian tropical rainforest and warmed leaves in the canopy by 4°C for 8 months. We measured temperature response curves of photosynthesis and respiration, and determined the critical temperatures for chloroplast function based on Chl fluorescence.
- Both stomatal conductance and photosynthesis were strongly reduced by 48 and 35%, respectively, with warming. While reduced stomatal conductance was likely in response to higher vapour pressure deficit, the biochemistry of photosynthesis responded to higher temperatures via reduced Vcmax25 (−28%) and Jmax25 (−29%). There was no shift of the Topt of photosynthesis. Concurrently, respiration rates at a common temperature did not change in response to warming, suggesting limited respiratory thermal acclimation.
- This combination of physiological responses to leaf warming in mature tropical trees may suggest a reduced carbon sink with future warming in tropical forests.
Open Research
Data availability
Data are published openly in WSU Institutional repository ResearchDirect.
Kristine Crous (2024): Dataset for leaf warming in the canopy of mature tropical trees in Australia. Western Sydney University. https://doi.org/10.26183/w8yx-dh13.
Supporting Information
Filename | Description |
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nph20320-sup-0001-FigsS1-S5.pdfPDF document, 451.9 KB |
Fig. S1 Daily means and one SD of leaf heater temperature differentials (Tdiff) with a target of 4°C warming on average over the study period (May–December 2021). Fig. S2 Example of the temperature response curve of base Chl fluorescence (Fo) from c. 15 to 60°C to derive Tcrit, with measured datapoints of Endiandra microneura indicated in black dots. Fig. S3 Means and SE of the mean of photosynthetic parameters in control and warmed leaves during the cooler period of the year (August, grey bars) and the warmer period of the year (December (Dec), open bars). Fig. S4 Means and SE of stomatal conductance (gs) as a function of leaf temperature (Tleaf) during the photosynthesis-temperature measurements for control, nonwarmed leaves in blue and warmed leaves in red in four tropical species. Fig. S5 Boxplots measured across warming treatments in two seasons of the year for dark respiration at a common temperature of 25°C (R25), the temperature sensitivity (or slope) of the respiration-temperature response curve (Q10), mass-based leaf nitrogen (Nmass) and leaf mass per area ratio (LMA) in the cooler August period (grey) and the warmer December period (red) in four species. Please note: Wiley is not responsible for the content or functionality of any Supporting Information supplied by the authors. Any queries (other than missing material) should be directed to the New Phytologist Central Office. |
Please note: The publisher is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.
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