Litter decomposition, microbial biomass and activity of soil organisms in three agroforestry sites in central Amazonia

Soil organisms play a central role in the decomposition of organic matter. The activity of soil organisms was comparatively examined in three experimental sites in central Amazonia (Brazil): a peach palm monoculture (Bactris gasipaes) a, rubber tree plantation (Hevea sp.), and an agroforestry system (four tree species planted in rows, the space between covered by upcoming secondary vegetation). The overall decomposition rates in the systems and the role of different groups of soil organisms (macrofauna, mesofauna, microflora) were studied with leaf litter (Vismia guianensis) enclosed in litter bags. Microbial respiration and biomass (SIR method) in litter and soil were measured (IRGA). Microbial respiration in all sites decreased in the gradient litter > topsoil (0–5 cm) > soil at 5–15 cm. The highest decomposition rate was always observed in the litter bags of coarse mesh size, pointing to the crucial role of the macrofauna in maintaining a high decomposition rate of the organic material in all systems. The Hevea (k = 3.4) and the Bactris plantation (k=3.1) both showed the highest decomposition rates, followed by the polyculture system (k=1.9). The Bactris plantation also had the highest level of microbial respiration and biomass in litter and soil. We discuss these findings in the light of data on rainfall, pH and canopy closure. They suggest that microclimate is a more important factor than biomass in determining litter decomposition rates and activity of soil organisms at these sites.