Environmental changes in biodiversity hotspot ecosystems of
South Ecuador: RESPonse and feedback effECTs (FOR2730)

Resumen:

Understanding the response of net nitrogen (N) mineralization to climate and land-use change is important to predict the effect of environmental change on the biodiversity and nutrient supply of the tropical montane forest in Ecuador. Slow mineralization or microbial immobilization may limit the availability of N, although organic N stocks in soils are high. To determine the roles of land use and climate for N mineralization in the mineral topsoil, field incubations over 31 days were conducted with the help of soil-filled PVC cylinders in forest and pasture soils along a land-use and elevation gradient from 1000-3000 m above sea level (a.s.l.). The experiment made use of a threefold replicated, full-factorial design with two land-use types and three elevations. The incubation cylinders were closed both at the bottom and the top and therefore only permitted horizontal water and element fluxes through lateral slits. Start and end concentration of NH4-N and NO3-N were determined in 1 M KCl extracts to calculate net N mineralization as the sum of ammonification and nitrification rates. Ammonification was significantly higher under pasture than under forest, except at 3000 m a.s.l., where the highest ammonification rates were detected on the forest plots. Nitrification was, in contrast, significantly higher under forest than under pasture, with highest nitrification rates at 2000 m a.s.l. Although the climate was wetter and cooler at higher elevations, mean N mineralization in the mineral soil on the forest sites significantly increased with elevation. On pastures, N mineralization was not significantly related with elevation, which may be explained by soil management and farming intensity. The slope of the regression line of δ13C values on soil organic C concentrations in 10-cm soil layers revealed a close relationship with the N mineralization rates, indicating that the short-term field incubations reflected the long-term C mineralization regime. The shift to higher δ13C values with increasing depth of the soil profile was related to N turnover and could thus serve as predictor of N mineralization rates on the forest sites, but not on the pastures, where the vertical distribution of the δ13C values was altered by the input of organic matter from C4 grasses after land-use change. Furthermore, the relationship between the slope of the regression line of the enrichment of δ13C values on soil depth and N mineralization measured by in-situ incubation depended on the parent material. The topsoils developed from granodiorite showed lower N mineralization rates than those developed from phyllite and meta-sandstone. Different soil texture, rooting depth, nutrient availability, and different organic layers may provide possible explanations for the observed differences.