Last Interglacial–Glacial sequence of palaeosols and calcareous slope deposits at Verteuil (Charente, southwest France)
BERTRAN, Pascal
Institut national de recherches archéologiques préventives - Centre de recherches archéologiques de Dijon [Inrap, Dijon]
De la Préhistoire à l'Actuel : Culture, Environnement et Anthropologie [PACEA]
Voir plus >
Institut national de recherches archéologiques préventives - Centre de recherches archéologiques de Dijon [Inrap, Dijon]
De la Préhistoire à l'Actuel : Culture, Environnement et Anthropologie [PACEA]
BERTRAN, Pascal
Institut national de recherches archéologiques préventives - Centre de recherches archéologiques de Dijon [Inrap, Dijon]
De la Préhistoire à l'Actuel : Culture, Environnement et Anthropologie [PACEA]
Institut national de recherches archéologiques préventives - Centre de recherches archéologiques de Dijon [Inrap, Dijon]
De la Préhistoire à l'Actuel : Culture, Environnement et Anthropologie [PACEA]
LIMONDIN-LOZOUET, Nicole
Laboratoire de géographie physique : Environnements Quaternaires et Actuels [LGP]
< Réduire
Laboratoire de géographie physique : Environnements Quaternaires et Actuels [LGP]
Langue
en
Article de revue
Ce document a été publié dans
Journal of Quaternary Science. 2023, vol. 38, n° 8, p. 1321-1336
Wiley
Résumé en anglais
The 12 m thick sequence of calcareous slope deposits and palaeosols exposed in a quarry at Verteuil (southwest France) has been studied and dated by optically stimulated luminescence. Emphasis was given to the identification ...Lire la suite >
The 12 m thick sequence of calcareous slope deposits and palaeosols exposed in a quarry at Verteuil (southwest France) has been studied and dated by optically stimulated luminescence. Emphasis was given to the identification and characterisation of palaeosols through geochemistry and micromorphology. The main clastic units, separated by major unconformities, were dated to MIS 6, MIS 5-4 and MIS 3-2. Stratified deposits ('grèzes litées'), consisting of alternating diamictic and matrix-free clastic beds and attributed to stacked stone-banked solifluction lobes, developed mainly after ca. 40 ka, i.e. during late MIS 3 and MIS 2. MIS 3 is recorded as a palaeosol complex including two humic A horizons overlying a chromic cambisol associated with burrows of ground squirrels, while MIS 5 corresponds to a reworked rubified chromic cambisol. Overall, this sequence shows similarities with the clastic deposits found in regional cave porches and rock shelters, strongly suggesting that anthropogenic activities did not significantly modify the climate-driven sedimentary and soil-forming processes at the Palaeolithic sites.< Réduire
Mots clés en anglais
OSL dating
palaeosols
southwest France
stratified slope deposits
Weichselian
Origine
Importé de halUnités de recherche