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The systematic examination of the VI and early V millennium BCE pottery from the Arene Candide Cave (Finale Ligure, Western Liguria) revealed several charred macroremains embedded in the paste, as well as imprints of a wide range of botanical remains.

The laser-probe ages are lower than the minimum ages measured on the populations of grains by the step-heating method.

As previously suggested by Lo Bello and co-workers for the pumice flow of Neschers belonging to the same volcanic massif, the saddle-shaped age spectra are ascribed to the different Ar-release patterns of two populations of K-feldspars: (1) young sanidine phenocrysts of the pumices; and (2) old K-feldspars plucked from the Hercynian basement during the explosive eruption.

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Measurements of both the granitic rocks from surrounding areas and the granitic xenoliths included in pumices give ages around 330 Ma and show that most of the xenocrysts included in the pumices did not lose significant amounts of argon during the eruption.

With the Ar step-heating method, we were able to detect contamination of Quaternary K-feldspars by Hercynian K-feldspars as low as 0.25ℵ.

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