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Abstract Carbon dioxide and water vapour fluxes were measured for 55 days by eddy covariance over an undisturbed tropical rain forest in Rondonia, Brazil. Profiles of CO 2 inside the canopy were also measured. During the night, CO 2 concentration frequently built up to 500 ppm throughout the canopy as a result of low rates of exchange with the atmosphere. In the early morning hours, ventilation of the canopy occurred. Ecosystem gas exchange was calculated from a knowledge of fluxes above the canopy and changes of CO 2 stored inside the canopy. Typically, uptake by the canopy was 15 μmol m −2 s −1 in bright sunlight and dark respiration was 6‐7 μmol m −2 s −1 The quantum requirement at low irradiance was: 40 mol photons per mol of CO 2 . Bulk stomatal conductance of the ecosystem was maximal in the early morning (0.4‐1.0 mol m −2 s −1 ) and declined over the course of the day as leaf‐to‐air vapour pressure difference increased.
Grace et al. (Wed,) studied this question.
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