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Une étude de lames minces a été effectuée dans des coprolithes du Tell néolithique d'Hârşova. Deux variétés de coprolithes, compacte et friable, peuvent être distinguées. Les deux types de coprolithes contiennent des débris d'os, témoins de leur origine carnivore ou omnivore. Des observations complémentaires des lames minces sous cathodoluminescence ont révélé, à divers degrés, la présence de calcite...
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