1Earth and Biosphere Institute, School of Geography, University of Leeds, Leeds, LS2 9JT, UK
2Max-Planck-Institut fuer Biogeochemie, Jena, Germany
3Instituto de Investigación de Recursos Biológicos, Alexander von Humboldt, Bogotá, Colombia
4UMR-ECOFOG, INRA, 97310, Korou, French Guiana, France
5Centro de Energia Nuclear na Agricultura, Piracicaba, Brazil
6Institito Nacional de Pesquisas da Amazônia, Manaus, Brazil
7Centre for Ecology and Hydrology, Wallingford, UK
8Instituto Venezuelano de Investigaciones Científicas, Caracas, Venezuela
*now at: Fieldwork Assistance, Postfach 101022, 07710 Jena, Germany
**now at: Department of Earth System Science, University of California, 2103 Croul Hall, Irvine, CA, 92697-3100, USA
***now at: Geography and Ecosystem Analysis, Lund University, Lund, Sweden
†deceased on 29 June 2006
Received: 18 Dec 2008 – Discussion started: 08 Apr 2009
Abstract. Soil samples were collected in six South American countries in a total of 71 different 1 ha forest plots across the Amazon Basin as part of the RAINFOR project. They were analysed for total and exchangeable cations, C, N, pH with various P fractions also determined. Physical properties were also examined and an index of soil physical quality proposed. A diverse range of soils was found. For the western areas near the Andean cordillera and the southern and northern fringes, soils tend to be distributed among the lower pedogenetic levels, while the central and eastern areas of Amazonia have more intensely weathered soils. This gives rise to a large variation of soil chemical and physical properties across the Basin, with soil properties varying predictably along a gradient of pedogenic development. Nutrient pools generally increased slightly in concentration from the youngest to the intermediate aged soils after which a gradual decline was observed with the lowest values found in the most weathered soils. Soil physical properties were strongly correlated with soil fertility, with favourable physical properties occurring in highly weathered and nutrient depleted soils and with the least weathered, more fertile soils having higher incidence of limiting physical properties. Soil phosphorus concentrations varied markedly in accordance with weathering extent and appear to exert an important influence on the nitrogen cycle of Amazon forest soils.
Revised: 19 Mar 2010 – Accepted: 24 Apr 2010 – Published: 17 May 2010
Quesada, C. A., Lloyd, J., Schwarz, M., Patiño, S., Baker, T. R., Czimczik, C., Fyllas, N. M., Martinelli, L., Nardoto, G. B., Schmerler, J., Santos, A. J. B., Hodnett, M. G., Herrera, R., Luizão, F. J., Arneth, A., Lloyd, G., Dezzeo, N., Hilke, I., Kuhlmann, I., Raessler, M., Brand, W. A., Geilmann, H., Moraes Filho, J. O., Carvalho, F. P., Araujo Filho, R. N., Chaves, J. E., Cruz Junior, O. F., Pimentel, T. P., and Paiva, R.: Variations in chemical and physical properties of Amazon forest soils in relation to their genesis, Biogeosciences, 7, 1515-1541, doi:10.5194/bg-7-1515-2010, 2010.