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Faunal remains from radiocarbon-dated soils within landslip debris from The Undercliff,Isle of Wight,Southern England
Institution:1. Sciences de la Terre, Université du Québec à Chicoutimi, Chicoutimi G7H 2B1, Canada;2. Departamento de Geología, Centro de Excelencia en Geotermia de los Andes (CEGA), Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago, Chile;1. Departamento de Ciencias Geológicas, Universidad Católica del Norte, Av. Angamos 0610, Antofagasta, Chile;2. GET, Université de Toulouse, IRD, CNRS, UPS, 14 avenue E. Belin, 31400 Toulouse, France;3. Departamento de Ingeniería y Geotécnia, Pontificia Universidad Católica de Chile, Av. Vicuña Mackenna 4860, Santiago, Chile;4. Mineral Deposit Research Unit, Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, 2020–2207 Main Mall, Vancouver, BC V6T 1Z4, Canada;5. Departamento de Petrología y Geoquímica, Fac. CC. Geológicas, Universidad Complutense de Madrid, C/ José Antonio Novais, Madrid 28040, Spain
Abstract:An examination of coastal sections of landslip material forming The Undercliff of the Isle of Wight has revealed the presence of buried soils, in places, within the debris. Critical sections at Binnel Point and St. Catherine's Point have been logged and the contained vertebrate and molluscan faunas analysed. The Mollusca from both sites are very similar and indicate a shaded environment, contrasting sharply with the immediate local environments today. The vertebrates, present only at Binnel Point, again suggest woodland. The presence of red squirrel (Sciurus vulgaris) and dormouse (Muscardinus avellanarius) is especially noteworthy constituting their earliest and only secure British fossil records respectively. Some marine shells (Patella, Gibbula) and remains of larger vertebrates (including red deer) possibly represent midden debris. Charcoal from the lower soil at Binnel Point yielded a radiocarbon date of 4480 ± 100 bp (BM-1737) indicating that at least some of the middens at Binnel date from the Neolithic, much earlier than previously demonstrated. The sections at St. Catherine's Point provided no evidence of human occupation but yielded two further radiocarbon dates of 4490 ± 40 bp (SRR-1813) and 3960 ± 50 bp (SRR-1947) from wood incorporated within the landslips. The significance of these dates in relation to the history of landslipping is discussed.
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