Many lateritic tropical soils on stable cratonic areas have developed over millions to 10's of millions of years. Some elements (e.g., alkalies, alkaline earths, Si) are extremely depleted by leaching, and others (A1, Fe, Ti) are greatly enriched. Commonly this enrichment is regarded as merely the accumulation of insoluble constituents, but inspection of the soil shows development of pisolites, nodules and other features indicating extensive dissolution/precipitation of Feand Al-oxides and -hydroxides. This paper suggests that cycling of elements through vegetation is an important part of soil development in these ancient soils. This project was initiated to investigate the processes forming "lateritic" gold deposits, in which a relatively small primary vein or similar Au deposit in bedrock mushrooms in the soil to become a significant Au enrichment in the laterite zone (Davy and E1-Ansary, 1986; Lecomte and Colin, 1989). The site of our investigation is the gold deposit of Igarape Bahia in the Serra Carajas mining region, Para Province, Brazil. In this region, a very ancient plateau surface furnishes the environment for major Fe, Mn and A1 deposits of the Carajas district (Beisiegel, 1982; Machamer et al., 1991 ) as well as a lateritic gold deposit at Igarape Bahia. The plateau surface is interpreted to have been developed in Cretaceous or early Tertiary (Beisiegel, 1982; Kotschoubey and Lemos, 1985 ). The entire region is covered by dense tropical rain forest. At the Igarape Bahia Au deposit, a narrow primary zone of Au-Cu mineralization at depth gives rise to a relatively rich Au deposit in lateritic soil. The deposit appears analogous to other lateritic Au accumulations in which the initial primary Agbearing gold grains are etched and become smaller, and new grains of Ag-poor gold grow in the laterite (Lecomte and Colin, 1989). A preliminary study indicated that considerable Au was present in vegetation over the deposit, so in a later sampling expedition an extensive group of vegetation samples was collected, along with soils and waters (Andrade et al., 1991; Bliss, 1991; Machesky et al., 1993). Vegetation sampling was concentrated along a traverse across the unmined F30 deposit, a satellite Au deposit --~ 1 km from the main Igarape Bahia deposit. Additional samples were collected at three background sites ~ 1, ~ 10 and ~ 30 km from the deposit. At the F30 deposit and at the 1 km background site, all species of tree and shrub were collected, with leaves, twigs and bark being collected from most species. Five specific species (a large tree, two bamboo species, and two bushes) were sampled along the traverse and at the background sites. Samples were washed, dried, chopped, homogenized and analyzed for ~ 40 elements by neutron activation (Activation laboratories Ltd., Ancaster, Ontario) and Xray fluorescence (Materials Characterization Lab, Penn State University).