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CAD. LAB. XEOL. LAXE 26 (2001) Holocene Brown Bears in natural traps 333 Table 4. Metrical data (in mm) for brown bear skulls and upper teeth of Mont Ventoux natural traps. Data from DONAT-AYACHE (1997). Table 5. Metrical data (in mm) for brown bear mandibles of Mont Ventoux natural traps. Data from DONAT-AYACHE (1997). and Taubach, and Upper Pleistocene cave sites of Grimaldi (grotte du Prince), Régourdou, Jaurens and Flavigny (table 7). Most Ursus arctos discoveries come from (partial) isolated skeletons for which chronological background cannot be refined without radiometric data. All of skeletal parts have been found (figure 6): unfused bones of young individuals and closed epiphyseal long bones of (sub)adult
334 CREGUT & FOSSE CAD. LAB. XEOL. LAXE 26 (2001) Table 6. Metrical data (in mm) for brown bear lower teeth of Mont Ventoux natural traps. Data from DONAT-AYACHE (1997). Figure 5. Osteometric data of adult brown bear lower carnassials (mm) from Mont Ventoux natural traps; comparisons with pleistocene and holocene specimens. skeletons are mixed and great concentrations of bones do not allow a reconstruction (refittings) of all individuals. Young individuals are especially abundant, most of them belong to new born / first winter individuals (MV4 NISP= 4634; MNI= 87, table 8; MV2 NISP= 2000; MN= 30) whose ages have been estimated from lower tooth eruption/wear stages on known-age samples (DIT-
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