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Titre du jeu de données : Saint_Acheul MIS 11 Interglacial tufa deposit
Mots-clés thématiques (thesaurus du GCMD) :
Paleoclimate>
Land Records>
Microfossils
Autres mots-clés (fr) :
Quaternaire
Mollusques
Autres mots-clés (gb) :
Paleoenvironment
Responsable(s) du jeu de données :
LIMONDIN-LOZOUET Nicole
Personne à contacter pour obtenir les informations sur le jeu de données :
LIMONDIN-LOZOUET
Nicole
Laboratoire de géographie physique Pierre BIROT (LGP)
UMR 8591
Résumé :
Recently a new cleaned profile at Saint-Acheul in the Somme valley (type section for the Lower Palaeolithic Acheulean industry), has provided an opportunity to undertake malacological analysis and ESR dating on a tufa deposit at the top of the fluvial sequence. The context of the basal alluvial sheet within the terrace system of the Middle Somme valley allows attribution of the fluvial deposits of Saint-Acheul to the Garenne Formation (Formation V of the system), which has been previously allocated to MIS 12 and 11. The upper part of the Saint-Acheul sequence (slope deposits) is mainly composed of Upper Saalian loess, overlain by Upper Pleistocene deposits and soils, separated from the fluvial beds by erosion and a long hiatus. The Upper Pleistocene succession includes an arctic brown soil horizon (the so-called "Sol de Saint Acheul"), representing the results of pedogenesis throughout the Weichselian Middle Pleniglacial (MIS 3). Chronostratigraphic interpretation of the underlying fluvial deposits is now consolidated by an ESR age determination on quartz (403 + ou - 73 kyrs BP), consistent with a MIS 11 allocation. Malacofaunas recovered from the tufa deposit are rich and diversified (60 taxa) and the presence of no less than 21 forest species point unequivocally to climatic optimum conditions. Fluvial taxa are represented by 17 aquatic species of slow-flowing water. Terrestrial habitats consist of open-grassland, as demonstrated by the strong development of Pupilla, Vallonia and Trichia species, and of wooded areas. Among the forest molluscs several species are out of their modern ranges (Platyla polita, Ena montana, Ruthenica filograna, Clausilia pumila, Macrogastra ventricosa, Perforatella bidentata, P. incarnata). Most noteworthy of all is the occurrence of the extinct Zonitid Retinella (Lyrodiscus) skertchlyi. These species belong to the particular "Lyrodiscus biome" recognised in several tufa deposits from north-west Europe, all allocated to MIS 11. Finally, these results reinforce the interpretation of the Somme terraces system as a model of river response to Milankovitch cycles during the Pleistocene.
Format des données : PDF (.pdf) -
Date de création :
2005-01-11
Date de mise à jour :
2006-11-24
Les publications :
Antoine P., Limondin-Lozouet N.
(2004).
Identification of MIS 11 Interglacial tufa deposit in the Somme valley (France): new results from the Saint-Acheul fluvial sequence.
Quaternaire
15,1-2,
41-52.
Date de début :
Date de fin :
Méthode de datation : Electron Spin Resonance (ESR)
Unité(s) stratigraphique(s) (International Stratigraphic Chart, UNESCO/IUGS/ICS, 2004) :
Phanerozoic
>Cenozoic
>Neogene
>Pleistocene
Coordonnées (en fraction décimale de degré) :
Coordonnée limite sud :
Coordonnée limite nord :
Coordonnée limite ouest :
Coordonnée limite est :
Altitude minimale :
Altitude maximale :
Pays :
France
Region / Continent :
Europe
Localité : Saint-Acheul
Etat d'acquisition : Complete
Fréquence de mise à jour : Unknown
Restriction sur l'accessibilité de l'ensemble des données :
none
Fichier de données :
Saint_Acheul.pdf
Restriction / condition d'utilisation : Contact LIMONDIN-LOZOUET Nicole
Rapport sur la qualité :
Contact LIMONDIN-LOZOUET Nicole