3 results

Anthrosols at archaeological sites in a karst environment in northern Minas Gerais

Bruno Nery Fernandes Vasconcelos, João Carlos Ker, Carlos Ernesto Gonçalves Reynaud Schaefer, André Pierre Prous Poirier, Felipe Vaz Andrade

01/Aug/2013

The occupation and territorial dispersion of the first settlers in South America, especially in Brazil, are still little known and require continuous interdisciplinary studies involving anthropology, archeology, and soil science. Under natural limestone shelters, pre-Columbian populations lived for thousands of years, introducing and removing materials of different nature and from different origins, resulting in the development of very peculiar anthropogenic soils, which have been little investigated so far. To deepen the knowledge on this type of soil, we evaluated the […]

Manganese oxides an iron ore province soils, Minas Gerais, Brazil

Amaury de Carvalho Filho, Nilton Curi, João José Granate de Sá e Melo Marques, Edgard Shinzato, Diego Antonio França de Freitas, Elen Alvarenga de Jesus, [...]

01/Jun/2011

The mineralogy of Mn oxides is highly variable and complex, since the number of minerals is large and the knowledge of their structures imprecise. In view of the scarcity of specific papers on Mn oxides in Brazilian soils and their unusually high contents in some soils of one of the Iron Ore Province (IOP) of Minas Gerais State, this study aimed to characterize the chemistry and mineralogy of these oxides in the soils of this region, stratifying them according to […]

Soil-landscape-parent material relationship and pedogenesis of some “Mar de Morros” soils

W. A. G. A. Nunes, J. C. Ker, C. E. G. R. Schaefer, E. I. Fernandes Filho, F. H. Gomes

01/Jun/2001

Little is known about the effect of mafic parent materials on soil genesis in the humid “Zona da Mata”, Minas Gerais, although there are many detailed studies on soils developed from felsic to mesocratic gneiss, notably Latosols and terrace Podzolic soils. To fill this gap, soils in two topolitosequences, comprising A and B or A and C horizons, were sampled and studied. In the first topolitosequence, at Serra de Guiricema, a Red-Yellow Latosol on the top, a Argilluvic Chernosol, a […]