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U-Series Dating by the TIMS Technique of Land Snails from Paleosols in the Canary Islands

Published online by Cambridge University Press:  20 January 2017

Claude Hillaire-Marcel ,
Bassam Ghaleb ,
Clément Gariépy ,
Cari Zazo ,
Manolo Hoyos  and
Jose-Luis Goy
Claude Hillaire-Marcel
Affiliation:
Centre de recherche en géochimie isotopique et en géochronologie (GEOTOP), Université du Québec à Montréal, Boíte postale 8888, succursale "Centre-Ville," Montréal, Québec, H3C 3P8, Canada
Bassam Ghaleb
Affiliation:
Centre de recherche en géochimie isotopique et en géochronologie (GEOTOP), Université du Québec à Montréal, Boíte postale 8888, succursale "Centre-Ville," Montréal, Québec, H3C 3P8, Canada
Clément Gariépy
Affiliation:
Centre de recherche en géochimie isotopique et en géochronologie (GEOTOP), Université du Québec à Montréal, Boíte postale 8888, succursale "Centre-Ville," Montréal, Québec, H3C 3P8, Canada
Cari Zazo
Affiliation:
Museo nacional de Ciencias naturales, José Gutierrez Abascal, 2, 28006 Madrid, Spain
Manolo Hoyos
Affiliation:
Museo nacional de Ciencias naturales, José Gutierrez Abascal, 2, 28006 Madrid, Spain
Jose-Luis Goy
Affiliation:
Departamento de Geologia, Facultad de Ciencias, Universidad de Salamanca, 37008 Salamanca, Spain
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Abstract

A sequence of seven superimposed paleosols developed on eolian calcarenites and alluvium was sampled on the island of Lanzarote in order to examine the possibility of dating land snail shells by the U-series method, using a TIMS technique allowing measurement of U and Th isotopes in very small samples. In the lower six units, the fossil shells yielded D-allo/L-isoleucine (A/I) ratios of about 0.5 and apparent AMS 14C ages ranging from 41,000 to 34,000 yr B.P., indicating that most paleosols formed during a relatively short mid-Würm humid episode. The upper unit (paleosol 7) yielded more variable A/I ratios (ranging from 0.6 to 0.2) and a younger 14C age ∼27,000 yr B.P. Most samples contained enough U to allow the calculation of U-series ages, after correction for the presence of a detrital component. In samples containing a few tens of ppb of U (paleosols 1, 2, 3, 6, and 7), the ages are strongly dependent upon the model used for the correction. In samples containing more than 300 ppb of U (paleosols 4 and 5), concordant ages of ∼31,000 ± 1000 yr were obtained regardless of the correction model used. U uptake in these shells occurred during one single early diagenetic phase, soon after burial, since shells of modern snails do not contain any significant amount of U. The arid conditions subsequent to the mid-Würm humid episode have likely ensured since then a fair closure of the radioactive system.

Type
Research Article
Information
Quaternary Research , Volume 44 , Issue 2 , September 1995 , pp. 276 - 282
Copyright
University of Washington

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