Sols fossiles du Terrefort toulousain. Leur signification paléoclimatique.
- 1 January 1981
- journal article
- research article
- Published by PERSEE Program in Bulletin de l'Association française pour l'étude du quaternaire
- Vol. 18 (3) , 149-158
- https://doi.org/10.3406/quate.1981.2095
Abstract
The study of paleosols formed on slope deposits in the region of Toulouse has enabled the authors to complete the chronostratigraphy of the adjacent loess. The importance of the Late Quaternary deposits, linked to hydric erosion, is recognised and the absence of periglacial forms and cryostructures is noted. A correlation of the periods of pedogenesis and the known interstades of Wurm III and IV is proposed.Keywords
This publication has 1 reference indexed in Scilit:
- Pédogenèses quaternaires dans la région toulousaine. Les loess et leurs colluvions comme marqueur chronologiqueBulletin de l'Association française pour l'étude du quaternaire, 1978