“…However, several regional syntheses of changes in faunal communities proposed the upper part of the Combe-Grenal sequence to span the period from MIS 5 (130-82 ka) to the beginning of MIS 3 (57-29 ka) (Discamps et al, 2011;Faivre et al, 2014;Discamps and Royer, 2017). Faunal data from on-going excavations has, however, highlighted substantial recovery biases in Bordes' faunal collections (Discamps and Faivre, 2017), calling into question previously proposed chronological models (Guadelli and Laville, 1990;Discamps et al, 2011;Morin et al, 2014). In parallel, an analysis of the small mammal assemblages (Marquet, 1989) highlighted only minimal changes in environmental conditions between the Quina and Discoid/Levallois levels, the former containing several more cold-adapted species, such as snow vole (Chionomysnivalis).…”