“…However, other species, including at least three from the SMG – Chama iudicai (Pastorino, 1991), Tegula atra (Lesson, 1830) and Glycymeris sanmatiensis (Bayer & Gordillo, 2013) – became extinct, apparently during the glaciations, and were only found in the oldest Quaternary deposits surrounding this gulf (Pastorino, 1991; Bayer & Gordillo, 2013; Gordillo et al ., 2014; Charó et al ., 2014). A warmer period called the Hypsithermal occurred during the middle Holocene (between 6000 and 4500 years bp ), in which temperatures were slightly higher (Schellmann & Radtke, 2010) than during the rest of the Holocene and the sea level transgression produced geomorphological changes along the Patagonian coastline (Kokot et al, 2004; Favier-Dubois & Kokot, 2011). This global event is reflected in changing marine mollusc assemblages (Gordillo et al , 2011; Charó et al , 2013).…”