Abstract. Over the past three decades, tropical forest clearing and burning have greatly altered the Amazonian landscape by increasing the cover of pastures and secondary forests. The alteration of biogeochemical processes on these lands is of particular interest on highly weathered Oxisols that cover large areas in the region because of concerns regarding possible nutrient limitation in agricultural land uses and during forest regrowth. The objectives of this study were to quantify (1) the reaccumulation of nutrients in biomass of secondary land uses, (2) changes in soil nutrient contents, (3) internal nutrient cycles, and (4) input-output budgets for the landscape mosaic.Nutrient stocks and fluxes were quantified from 1996 to 1998 in mature forest, 19-yrold secondary forest, degraded pastureland, and managed pastureland in the Brazilian state of Pará. Mature forests contain 130 Mg C/ha in aboveground biomass while secondary forest, degraded pasture, and managed pasture contain 34, 4, and 3 Mg C/ha, respectively. Reaccumulation of N, P, K, Ca, and Mg in aboveground biomass of secondary forest was 20%, 21%, 42%, 50%, and 27% of that present in mature forest, while degraded pasture contained 2%, 4%, 15%, 11%, and 6%. Managed pasture had similar accumulations as degraded pasture except for Ca (3%).Changes in soil stocks of C, N, and P were not detected among land uses, except in fertilized managed pastures, where total soil P (0-10 cm) was elevated. Conversely, Mehlich-III-extractable P of all secondary lands were very low (Ͻ1 g/g) and were 1 kg/ha less than contents (0-10 cm) in mature forest. NaOH-extractable P was present in 100-fold higher concentrations and may gradually contribute to meeting plant demands over decadal time scales. Soil cation contents (0-20 cm) were elevated in secondary lands with increases of ϳ85, 500, and 75 kg/ha for K, Ca, and Mg, respectively. These increases could account for a substantial portion of cation contents originally in the aboveground biomass of mature forest.The recycling of nutrients through ϳ9.0 Mg·ha Ϫ1 ·yr Ϫ1 of litterfall in secondary forest of 132, 2.8, 32, 106, and 23 kg·ha Ϫ1 ·yr Ϫ1 for N, P, K, Ca, and Mg, respectively, is similar to mature forest. Nutrient returns in both pasturelands were smaller for all elements except K, which was similar to the forested sites. In these pasture ecosystems, grass turnover has replaced litterfall return as the predominate mechanism of nutrient recycling.Soil solution fluxes of total N were higher in mature forest (12 kg·ha Ϫ1 ·yr Ϫ1 at 25 cm depth) compared to secondary lands (Ͻ4 kg·ha Ϫ1 ·yr
Ϫ1), indicating that cycling of available forms of N has diminished. Conversely, fluxes of cationic elements appear elevated in secondary lands and are charge balanced in solution by HCO 3 Ϫ derived from biological activity in the soil surface. Despite detectable increases in soil cation fluxes, rainwater inputs and stream water outputs of these elements across the watershed were not significantly different.The aggregate picture for this la...