Abstract
Photoassimilate distribution inside leaves is less studied than photosynthesis, and yet the topic is important as it gives insights into the vital roles played by leaves in plant survival. We combined greenhouse measurements of light response curves with 11C-labelling using leaves of 3-year-old potted Maesopsis eminii Engl. trees to improve our understanding of its leaf carbon physiology. This fast-growing pioneer tree species showed low photosynthetic rates for a common tropical pioneer during well-watered reference conditions (5.0 ± 0.7 µmol m−2 s−1), which further decreased in response to drought. 11C-autoradiography indicated active phloem loading and/or rapid phloem transport rates. Active loading is uncommon in tree species, but might be related to deciduousness traits and continuous investment in growth, like in herbaceous active loaders. Active loading involves higher carbon allocation to growth, which might explain why low photosynthetic rates were observed in this fast-growing species. These findings suggest that examining photoassimilate distribution and transport may be critical for understanding the role tree physiology plays in terrestrial carbon cycling.
Highlights
Changes in temperature, precipitation, CO2, and evapotranspiration are already eminent in African tropical rainforests, affecting their ecological processes [1]
Drought Pn,max significantly differed from Pn,max after re-watering, and Pn,max obtained under reference conditions (Tdrought < Trecovering ≈ Twell-watered ; Tdrought − Trecovering (p < 0.05), Tdrought
M. eminii is a pioneer with fast growth, expected to show a high photosynthetic rate, but this was not confirmed by our measurements
Summary
Precipitation, CO2 , and evapotranspiration are already eminent in African tropical rainforests, affecting their ecological processes [1]. These effects have gained increasing attention [2,3,4,5,6,7,8,9,10] as the biome represents 15% of worldwide forests, and dominates inter-annual carbon cycling with 50% [11,12]. Evidence is increasing that considerable uncertainties exist in assessing tropical carbon stocks [25,26,27], feeding the debate on how to implement tropical biomass models [28]. This points to the relevance of increasing our knowledge on the ecophysiological mechanisms underlying carbon sequestration
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