Deep weathering and landscape evolution in a tropical plateau

• Published in: Catena (Giessen) 2011-06, Vol.85 (3), p.221-230
• Main Authors: Modenesi-Gauttieri, May Christine, de Toledo, Maria Cristina Motta, Hiruma, Silvio Takashi, Taioli, Fabio, Shimada, Helio
• Format: Article
• Language: English
• Subjects: altitude; Aluminum base alloys; Bayer process; Bgi / Prodig; Brazil; Climate; drilling; Evolution; Geomorphology; gibbsite; information sources; Intertropical non-arid areas; Landscape evolution; Landscapes; Lateritic saprolite; Mantle; Micromorphology; Passive margins; Phases; Physical geography; plateaus; saprolite; silicates; soil; tropics; Weathering
• ISSN: 0341-8162; 1872-6887
• DOI: 10.1016/j.catena.2011.01.006

The thick weathering profiles of humid tropical areas are an important, yet generally neglected, source of information on landscape evolution. Six complete profiles of the weathering mantle were sampled by drilling on the three stepped levels of the Campos do Jordão Plateau, on the NW flank of the Continental Rift of Southeastern Brazil. Mineralogical and micromorphological analyses of drill core samples, complemented by geochemical interpretations and by previous data on the upper saprolite, indicate continuity of a general lateritic trend during the entire process of mantle formation. Lateritization phases of different intensity were defined and considered to reflect adjustment to changes in environmental conditions created by the gradual uplift of the plateau to its present position. Older and more superficial materials related to intense lateritic weathering are characterized by allitization with direct formation of gibbsite from silicates, probably related to tropical climates existing immediately before the formation of the continental rift, during the Paleogene, and also before any significant increase in altitude. Monosialitization phase with general kaolinitization and restricted indirect formation of gibbsite from silicates could be associated to less aggressive climates that followed the Neogene (Miocene?) accentuation of uplift rates along the continental rift. The changes produced by uplift in the tropical climate eventually favored the development of a podzolization trend in soils above 1800 m. ►Polyphasic weathering mantle. ►Weathering regimes identified by mineralogical and micromorphological analyses. ►Two lateritic phases characterized by distinct paths of feldspar weathering. ►Weathering phases controlled by the rhythm of uplift of the plateau. ►Evidences highlight mantle profiles as palaeoecological records.