Carbon dioxide flux across a forest-field ecotone

CO₂ flux of a deciduous forest and an old-field surface, and the ecotone between these two typical southern U.S. ecological communities, was studied in July, 1989. Rates of CO₂ flux were greatest in the old field and least in the forest plots. The ecotone showed the greatest variation in CO₂ flux. These differences appear to be due to differences in soil surface temperature, the old field being more exposed to direct solar radiation. The ecotonal community represents a landscape property which should be considered in studies of the transfer of carbon across the soil-atmosphere boundary.