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Consequently, the true cosmic dose rate received by the sample decreases according to the thickness of these deposits.
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Pour la datation par Résonance de Spin Électronique (ESR) d’émail dentaire, les données relatives à l’échantillon et à son contexte sédimentaire sont indispensables à la reconstruction des débits de dose associés.
It is therefore crucial to reconstruct the environment of the tooth to ensure a reliable age calculation, especially when variables such as the dose rate from the sediment represent more than 50 % of the total dose rate (e.g., Richard Hereinafter, we provide some recommendations on the tooth sampling strategy to follow for ESR dating, in order to collect suitable samples and to record important data needed for subsequent analyses and dose rates reconstruction.
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Consequently, we propose here some basic guidelines to help non-dating specialists intending to collect fossil teeth from archaeological or geological context for subsequent ESR dating purposes.
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In the case of “young” samples (e.g., from Upper Pleistocene deposits), and/or in a very low radioactive context, the contribution of the cosmic dose rate has proven to be significant: for instance, in the case of a cave, the roof thickness and the proximity of the sample from the cave entrance should be recorded and taken into account for cosmic dose rate estimation.