Canopy CO concentrations in a tropical rainforest in French Guiana were measured continuously for 5 days during the 1994 dry season and the 1995 wet season. Carbon dioxide concentrations ([CO]) throughout the canopy (0.02-38 m) showed a distinct daily pattern, were well-stratified and decreased with increasing height into the canopy. During both seasons, daytime [CO] in the upper and middle canopy decreased on average 7-10 μmol mol below tropospheric baseline values measured at Barbados. Within the main part of the canopy (≥ 0.7 m), [CO] did not differ between the wet and dry seasons. In contrast, [CO] below 0.7 m were generally higher during the dry season, resulting in larger [CO] gradients. Supporting this observation, soil CO efflux was on average higher during the dry season than during the wet season, either due to diffusive limitations and/or to oxygen deficiency of root and microbial respiration. Soil respiration rates decreased by 40% after strong rain events, resulting in a rapid decrease in canopy [CO] immediately above the forest floor of about 50␣μmol mol. Temporal and spatial variations in [CO] were reflected in changes of δC and δO values. Tight relationships were observed between δC and δO of canopy CO during both seasons (r > 0.86). The most depleted δC and δO values were measured immediately above the forest floor (δC = -16.4‰; δO = 39.1‰ SMOW). Gradients in the isotope ratios of CO between the top of the canopy and the forest floor ranged between 2.0‰ and 6.3‰ for δC, and between 1.0‰ and 3.5‰ for δO. The δC and calculated c /c of foliage at three different positions were similar for the dry and wet seasons indicating that the canopy maintained a constant ratio of photosynthesis to stomatal conductance. About 20% of the differences in δC within the canopy was accounted for by source air effects, the remaining 80% must be due to changes in c /c. Plotting 1/[CO] vs. the corresponding δC ratios resulted in very tight, linear relationships (r = 0.99), with no significant differences between the two seasons, suggesting negligible seasonal variability in turbulent mixing relative to ecosystem gas exchange. The intercepts of these relationships that should be indicative of the δC of respired sources were close to the measured δC of soil respired CO and to the δC of litter and soil organic matter. Estimates of carbon isotope discrimination of the entire ecosystem, Δ, were calculated as 20.3‰ during the dry season and as 20.5‰ during the wet season.