“…Based on a number of recent numeric dates obtained through a variety of techniques (Guérin et al 2012; Jankowski 2018), we are able to demonstrate the overlap in the sequences of Roc de Marsal and Pech IV and tentatively assign them to various OIS stages. However, we used other data, such as macrofauna (Hodgkins 2018;Hodgkins et al 2016;Niven 2013Niven , 2018Castel et al 2016), microfauna (Marquay as reported in Sandgathe et al 2008), phytoliths (Cabanes as reported in Sandgathe et al 2008), and sedimentology (Sandgathe et al 2008;Goldberg et al 2018) to reach conclusions about the climate at the time a layer was being deposited Reille and De Beaulieu, 1990) and the occupations took place. Not only at Roc de Marsal and Pech IV, but also at other sites, for example, La Ferrassie, La Quina, Chez Pinaud Jonzac, and Abri Peyrony, there is particularly good faunal preservation resulting in significant assemblages for paleontological analysis and paleoclimatic reconstruction, corroborated by chronometric dates and geological evidence.…”