“…Thus, this indicates that Notiomastodon platensis was present, at least, by the Early Pleistocene (Ensenadan) in South America (Soibelzon, 2008). Although N. platensis is recorded continuously from the Early Pleistocene to earliest Holocene (11 ± 6 ka; Dantas et al, 2013), most remains are from the Late Pleistocene, such as those from the Aguas de Arax a assemblage (60 ± 5 ka; Simpson and Paula Couto, 1957;Avilla et al, 2013), Chuí Creek, in Southern Brazil (44 ± 3 ka, 52 ± 7 and 80 ± 10 ka, Lopes et al, 2013), Tanque Loma (23.4e18 ka; Lindsey and Lopez, 2015), Quebrada Colorada, Chimborazo, in Ecuador (41.0e40.0 ka; Rom an-Carri on, unpublished results), Monte Verde (11.8 ± 200 ka and 13.5 ± 250 ka; Dillehay, 1989;Labarca Encina and Alberdi, 2011;Recabarren et al, 2014), Nochaco, Regi on de Los Lagos (16.1 ± 750 ka, Recabarren et al, 2014) and Mupulmo, Osorno, in Chile (18,700 ± 900 ka; Recabarren et al, 2014).…”