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Confirmation of an interglacial age for the Condat tufa (Dordogne, France) from biostratigraphic and isotopic data
Author(s) -
Preece R. C.,
Thorpe P. M.,
Robinson J. E.
Publication year - 1986
Publication title -
journal of quaternary science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.142
H-Index - 94
eISSN - 1099-1417
pISSN - 0267-8179
DOI - 10.1002/jqs.3390010107
Subject(s) - tufa , geology , radiocarbon dating , paleontology , facies , interglacial , quaternary , pleistocene , holocene , biostratigraphy , carbonate , structural basin , materials science , metallurgy
The Condat tufa is a localised deposit, reaching 8.2m in thickness, composed of freshwater carbonates deposited in a complex series of environments which include marsh, spring and stream facies. Five radiocarbon determinations had previously been obtained from different stratigraphic levels within the tufa and had given a consistent series, ranging from 12320 ± 175 BP to 31050 ± 1500BP. Although the youngest two dates, from near the surface of the tufa, had been rejected as being anomalously young, the older dates were regarded as indicating tufa formation during the last cold stage. Biostratigraphic analyses of the molluscan and ostracod faunas, presented here, demonstrate that the tufa formed under fully temperate conditions throughout. The occurrence of certain snails that are either locally extinct (e.g. Belgrandia marginata ) or unknown living in western France (e.g. Daudebardia brevipes ), together with the geomorphological setting, suggest that the tufa is of interglacial age. New radiocarbon determinations of the Condat tufa all proved to be >33 Ka BP and support this conclusion.