“…-There is no reliable archaeological sequence documenting the transition between the Upper Solutrean and the Salpetrian: Upper Solutrean is lacking at La Salpêtrière (Bazile, 1990;Boccaccio, 1999) and other Salpetrian assemblages are from undatable single-layered open-air sites (Boccaccio, 2006a;2006b;Bazile and Boccaccio, 2008); -Upper Solutrean is poorly documented in the Rhône valley, both typo-technologically and chronologically: Baume d'Oullins (Bazile and Bazile-Robert, 1979) is the only known evidence, yielding Salpetrian-type shouldered points together with "pointes à face plane" (Bazile and Boccaccio, 2007) suggesting a possible mix between Early Solutrean and Salpetrian components; -Evidence of Salpetrian-type shouldered points within Upper Solutrean assemblages is documented and vice versa: as pointed out by G. Boccaccio (2005, p. 458), scarce but clear evidence from Le Fourneau-du-Diable, Dordogne, shows high typotechnological similarities with Salpetrian standards; similarly, the Salpetrian assemblage of the La Rouvière open-air site, Ardèche, gave a typical Atlantic-type Upper Solutrean shouldered point manufactured with flat and invasive retouch applied on a non-Salpetrian blank (Boccaccio, 2005, p. 231); note that the raw material used to produce the latter artifact was potentially acquired from the Turonian outcrops of the Cher valley (Delvigne et al, 2017); -The archaeological succession between Salpetrian and raclette-yielding Badegoulian is known at the Petite Grotte de Bize, Aude: despite the limitation of these old excavations (see table 1), Bize provides a unique relative chronology confirming this succession; the challenge is now to give an age to this transition in order to know if it occurred prior to the emergence of Lassac-type assemblages ca. 21,5 cal ka BP (figure 2 and 6b; ongoing research in the framework of the LA_BA project, Ducasse and Sacchi dir.…”