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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-aIlo/L-isoleucine (All) ratios of about 0.5 and apparent AMS C-14 ages ranging from 41,000 to 34,000 yr B.P,, indicating that most paleosols formed during a relatively short mid-Wurm humid episode, The upper unit (paleosol 7) yielded more variable A/I ratios (ranging from 0.6 to 0.2) and a younger C-14 age of similar to 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 similar to 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-Wurm humid episode have likely ensured since then a fair closure of the radioactive system, (C) 1995 University of Washington.