C-14 dating of charcoal in the soil for the study of biological remount ofsoil matter and of the colluvium in the formation of ferralsols of Sao Paulo State, southern Brazil
Sem. Gouveia et Lcr. Pessenda, C-14 dating of charcoal in the soil for the study of biological remount ofsoil matter and of the colluvium in the formation of ferralsols of Sao Paulo State, southern Brazil, CR AC S IIA, 330(2), 2000, pp. 133-138
Citations number
12
Categorie Soggetti
Earth Sciences
Journal title
COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DELA TERRE ET DES PLANETES
This paper complements a scientific investigation, published in a precedent
Compte Rendu, that showed that the burial of charcoal in a oxisol of the M
inas Gerais Slate, southern Brazil, is a result of the biological remount o
f soil matter removed from deeper parts by the fauna. Such transported mate
rial would then constitute the soil layer containing charcoal (generally up
to 2 m). The new results obtained at two sites in Sao Paulo State confirm,
on the one hand, the role of the fauna in the development of these oxisols
and, on the other hand, that colluvium can intervene in the burial of char
coal. (C) 2000 Academie des sciences / Editions scientifiques et medicales
Elsevier SAS.