Abstract
A TUFF for which a 40Ar/39Ar date of 12.18±1.03 Myr has been obtained is located in the lower level of the Bou Hanifia continental formation (= Oued el Hammam), several metres below the famous Hipparion primigenium locality1–3. The tuff forms a continuous layer in the lower part of the continental formation and can be observed on either side of the Oued el Hammam Dam. The Hipparion fossiliferous horizon (Bou Hanifia I) lies in a second deposit of greatly weathered tuffs and has yielded a few micromammal remains. About 15 m above Bou Hanifia I, a second micromammal locality has been discovered (Bou Hanifia II)4.
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AMEUR, R., JAEGER, JJ. & MICHAUX, J. Radiometric age of early Hipparion fauna in North-west Africa. Nature 261, 38–39 (1976). https://doi.org/10.1038/261038a0
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DOI: https://doi.org/10.1038/261038a0
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