B087-01
How does photosynthetic response to elevated CO2 compare at the leaf and canopy scales? A case study with Eucalyptus saligna saplings grown in whole-tree chambers

Monday, 14 December 2020: 16:00
Virtual
Mingkai Jiang1, Dushan Kumarathunge2, Jinyan Yang3, Martin Gerard De Kauwe4, Benjamin Smith5, Anthony Walker6, Sönke Zaehle7, Craig VM Barton8, Kristine Crous9, David Ellsworth9, David Tissue1 and Belinda Medlyn10, (1)University of Western Sydney, Penrith, NSW, Australia, (2)Coconut Research Institute of Sri Lanka, Plant Physiology Division, Lunuwila, Sri Lanka, (3)Western Sydney University, Hawkesbury Institute for the Environments, Penrith, NSW, Australia, (4)ARC Centre of Excellence for Climate Extremes, University of New South Wales, Sydney, NSW, Australia, (5)Hawkesbury Institute for the Environment, Western Sydney University, Penrith, Australia, (6)Oak Ridge National Laboratory, Oak Ridge, TN, United States, (7)Max Planck Institute for Biogeochemistry, Jena, Germany, (8)Western Sydney University, Hawkesbury Institute for the Environment, Richmond, Australia, (9)Hawkesbury Institute for the Environment, Western Sydney University, Richmond, NSW, Australia, (10)Western Sydney University, Hawkesbury Institute for the Environment, Sydney, Australia
Abstract:
Accurate representation of canopy photosynthesis (A) and its sensitivity to rising atmospheric CO2 (Ca) in terrestrial biosphere models is essential for the robust projection of the carbon-climate feedback under climate change. Theory indicates that the sensitivity of A to rising Ca depends on the most limiting process. At low Ca, A is mostly limited by Rubisco carboxylation and increases near-linearly with rising Ca. Above an inflection point, A becomes mainly limited by RuBP regeneration and is less sensitive to further increases in Ca. Hence, the relative contribution of Rubisco- and RuBP regeneration-limitation to A is a critical modeling feature that constrains the sensitivity of terrestrial carbon cycle responses to rising Ca. Whilst leaf-level A-Ca measurements are abundant and different leaf-to-canopy scaling schemes are available for canopy A estimates, the extent to which canopy A-Ca responses differ from those of the leaf is largely untested. Here we describe Ca drawdown experiments using Eucalyptus saligna saplings grown in whole-tree chambers. The whole-canopy A-Ca responses were quantified for different canopy layers (i.e. whole canopy, top + middle, and top layers). We incorporated leaf-level measurements into the multi-assumption architecture and testbed (MATT) to estimate canopy A-Ca sensitivity based on different leaf-to-canopy scaling schemes. Our assessment identifies crucial disagreement in canopy A-Ca estimates between the data and modeling results. This data-model intercomparison therefore has direct implications to reduce model-based variability in predicting the terrestrial A-Ca responses under future climate change.