Journal
FUNCTIONAL PLANT BIOLOGY
Volume 43, Issue 5, Pages 468-478Publisher
CSIRO PUBLISHING
DOI: 10.1071/FP15320
Keywords
carbon balance; gas exchange; global warming; photosynthetic temperature response; stomatal conductance; tropical forest
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Funding
- Smithsonian Tropical Research Institute FOREST-GEO postdoctoral research fellowship
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Tropical forests play a critical role in the global carbon cycle, but our limited understanding of the physiological sensitivity of tropical forest trees to environmental factors complicates predictions of tropical carbon fluxes in a changing climate. We determined the short-term temperature response of leaf photosynthesis and respiration of seedlings of three tropical tree species from Panama. For one of the species net CO2 exchange was also measured in situ. Dark respiration of all species increased linearly - not exponentially - over a similar to 30 degrees C temperature range. The early-successional species Ficus insipida Willd. and Ochroma pyramidale (Cav. ex Lam.) Urb. had higher temperature optima for photosynthesis (T-opt) and higher photosynthesis rates at T-opt than the late-successional species Calophyllum longifolium Willd. The decrease in photosynthesis above T-opt could be assigned, in part, to observed temperature-stimulated photorespiration and decreasing stomatal conductance (g(S)), with unmeasured processes such as respiration in the light, Rubisco deactivation, and changing membrane properties probably playing important additional roles, particularly at very high temperatures. As temperature increased above T-opt, g(S) of laboratory-measured leaves first decreased, followed by an increase at temperatures >40-45 degrees C. In contrast, g(S) of canopy leaves of F. insipida in the field continued to decrease with increasing temperature, causing complete suppression of photosynthesis at similar to 45 degrees C, whereas photosynthesis in the laboratory did not reach zero until leaf temperature was similar to 50 degrees C. Models parameterised with laboratory-derived data should be validated against field observations when they are used to predict tropical forest carbon fluxes.
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