1948
DOI: 10.3406/bspf.1948.2432
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Un bâton orné du Magdalénien final de Loubressac, commune de Mazerolles (Vienne)

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Cited by 5 publications
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“…The (possibly Magdalenian) bone baton SOL AA.5 from La Roche de Solutré (Bourgogne, France; Joconde database) has a single perforation and is therefore more similar to Gough's Cave batons than the ones from Swabian Jura, though the curved incisions on the edge of the perforation of SOL AA.5 are generally thinner and more numerous. A slightly different screw thread like pattern (with circular grooves orientated along the perforation edges) has been noted on T-shaped antler batons from the Aurignacian of Dordogne (Blanchard I, La Souquette, Castanet, Le Poisson;Peyrony 1932Peyrony , 1935 and the Upper Magdalenian antler baton from Loubressac Cave in the same area (Leclerc and Pradel 1948). Additionally, we have identified parallel dashes engraved on the lower edge of the perforation of the Magdalenian antler baton MAN PL 55064 from Le Placard Cave (Charente, France; Fig.…”
Section: Discussionmentioning
confidence: 89%
“…The (possibly Magdalenian) bone baton SOL AA.5 from La Roche de Solutré (Bourgogne, France; Joconde database) has a single perforation and is therefore more similar to Gough's Cave batons than the ones from Swabian Jura, though the curved incisions on the edge of the perforation of SOL AA.5 are generally thinner and more numerous. A slightly different screw thread like pattern (with circular grooves orientated along the perforation edges) has been noted on T-shaped antler batons from the Aurignacian of Dordogne (Blanchard I, La Souquette, Castanet, Le Poisson;Peyrony 1932Peyrony , 1935 and the Upper Magdalenian antler baton from Loubressac Cave in the same area (Leclerc and Pradel 1948). Additionally, we have identified parallel dashes engraved on the lower edge of the perforation of the Magdalenian antler baton MAN PL 55064 from Le Placard Cave (Charente, France; Fig.…”
Section: Discussionmentioning
confidence: 89%
“…Perforated batons have been documented in the Aurignacian and Gravettian periods dating in Central Europe to before the Last Glacial Maximum (LGM), but they are particularly numerous during the Magdalenian, which postdates the LGM (18,19). In general, the insides of the holes are smooth, but some specimens include spiral grooves inside or adjacent to the holes similar to that seen on the ivory artifacts from the Swabian Aurignacian (20)(21)(22)(23)(24)(25)(26)(27)(28). Some researchers have suggested that the grooves may originate from reworking the holes rather than their serving a function in their own right (19).…”
Section: Resultsmentioning
confidence: 99%