Landscape and climatic controls on spatial and temporal variation in soil CO 2 efflux in an Eastern Amazonian Rainforest, Caxiuanã, Brazil

Abstract

Quantification of temporal and spatial variation of soil CO 2 emissions is essential for an accurate interpretation of tower-based measurements of net ecosystem exchange. Here, we measured in the old-growth forest of Caxiuana, Eastern Amazonia soil CO 2 efflux and its environmental controls from two Oxisol sites with contrasting soil texture and at different landscape positions. Average CO 2 efflux was 21% higher for sand (3.93 ± 0.06 μmol CO 2 m −2 s −1) than for the clay (3.08 ± 0.07 μmol CO 2 m −2 s −1). No difference was detected for soil temperature between sites, while soil water content in sandy soil (23.2 ± 0.33%) was much lower than the clay soil (34.5 ± 0.98%), for the 2-year period. Soil CO 2 efflux did not differ between dry and wet season, but we detected a significant interaction between season and topographic position. The variation caused by topography was in the same order of magnitude as temporal variation. Mean contribution of the litter layer to the CO 2 efflux rates was 20% and varied from 25% during the wet season to close to 0% during the dry season. The relation between soil water content and soil CO 2 efflux showed an optimum for both soil textures but the shape and optimum of the curves were different. The results of our study illustrate that soil moisture is an important driver of temporal variations in soil CO 2 efflux in this old-growth forest. When extrapolating soil CO 2 efflux to larger areas, the significant influences of soil texture, litter, and the interaction of topographical position and time illustrate that it is necessary to include some of the complexity of landscapes.