Tropical rain forests are among the most important and least monitored of t
errestrial ecosystems. In recent years, their influence on atmospheric conc
entrations of carbon dioxide and water vapor has become the subject of much
speculation. Here we present results from a yearlong study of CO2 fluxes.
at a tropical forest in central Amazonia, using the micrometeorological tec
hnique of eddy covariance. The diurnal cycle of CO2 flux was consistent wit
h previous shortterm studies in tropical rain forests, implying that the Am
azonian rain forest shows a fair degree of spatial uniformity in bulk ecoph
ysiological characteristics. Typical peak daytime photosynthesis rates were
24-28 mu mol CO2 m(-2) s(-1), and respiration rates were 6-8 mu mol CO2 m(
-1) s(-1). There was significant seasonality in peak photosynthesis over th
e year, which appeared strongly correlated with soil moisture content. On t
he other hand, there was no evidence of strong seasonality in soil respirat
ion. Central Amazonia has only a short, 3 month dry season, not atypical of
tropical rain forest, and it is therefore likely that large areas of Amazo
nia exhibit significant seasonality in photosynthetic capacity. The gross p
rimary production was calculated to be 30 t C ha(-1) yr(-1). An analysis of
data quality is included in the appendix.