“…The Middle to Late Pleistocene boundary is characterized by the extinction of numerous small mammal taxa, including all the fossil shrew species (Stoetzel, 2013). During the Late Pleistocene, most of the present Moroccan species were recorded from several Late Pleistocene and Holocene sites, such as Irhoud Neanderthal (Jaeger, 1970(Jaeger, , 1975Amani and Geraads, 1998), Oulad Hamida 2 (Felids cave; Raynal et al, 2008;Geraads et al, 2010), Chrafate (Ouabhi et al, 2003), Ez Zarka (Ouabhi et al, 2003), Guenfouda (Aouraghe et al, 2010;Lopez-García et al, 2013), and El Harhoura 2 (Stoetzel, 2009;Stoetzel et al, 2010Stoetzel et al, , 2011. In Morocco, the presence of crocidurines concerns mostly C. russula, C. whitakeri and to a lesser extent also C. tarfayensis.…”