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Published on July 3, 2008; 10.1104/pp.108.123521

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Received May 26, 2008
Accepted June 23, 2008

Conifers, angiosperm trees and lianas: growth, whole-plant water and nitrogen use efficiency, and stable isotope composition ({delta}13C and {delta}18O) of seedlings grown in a tropical environment

Lucas A. Cernusak *, Klaus Winter , Jorge Aranda , and Benjamin L. Turner

Smithsonian Tropical Research Institute, Apartado 0843-03092, Balboa, Ancon, Republic of Panama

* Corresponding author; email: lucas.cernusak{at}cdu.edu.au.

Seedlings of several species of gymnosperm trees, angiosperm trees, and angiosperm lianas were grown under tropical field conditions in the Republic of Panama; physiological processes controlling plant C and water fluxes were assessed across this functionally diverse range of species. Relative growth rate, r, was primarily controlled by the ratio of leaf area to plant mass, of which specific leaf area was a key component. Instantaneous photosynthesis, when expressed on a leaf-mass basis, explained 69% of variation in r (P<0.0001, n=94). Mean r of angiosperms was significantly higher than that of the gymnosperms; within angiosperms, mean r of lianas was higher than that of trees. Whole-plant N use efficiency was also significantly higher in angiosperm than in gymnosperm species, and was primarily controlled by the rate of photosynthesis for a given amount of leaf N. Whole-plant water use efficiency, TEc, varied significantly among species, and was primarily controlled by ci/ca, the ratio of intercellular to ambient CO2 partial pressures during photosynthesis. Instantaneous measurements of ci/ca explained 51% of variation in TEc (P<0.0001, n=94). Whole-plant 13C discrimination also varied significantly as a function of ci/ca (R2=0.57, P<0.0001, n=94), and was, accordingly, a good predictor of TEc. The 18O enrichment of stem dry matter was primarily controlled by the predicted 18O enrichment of evaporative sites within leaves (R2=0.61, P<0.0001, n=94), with some residual variation explained by mean transpiration rate. Measurements of C and O stable isotope ratios could provide a useful means of parameterizing physiological models of tropical forest trees.




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