In 1966, Uruguayan geologists Héctor Goso and Jorge Bossi defined the Raigón Formation, which they subdivided into the San José Member (the same as Francis and Mones' San José Formation) below and the San Bautista Member above.[2] In 1988, Álvaro Mones identified Lower Pleistocene levels in the San José Member.[3] In 2002, American geologist H. McDonald and Uruguayan paleontologist Daniel Perea suggested the formation may represent a wide timespan from the Montehermosan all the way to the Ensenadan.[4]
^ abcBossi, J.; Ortiz, A.; Perea, D. (2009). "Pliocene to middle Pleistocene in Uruguay: A model of climate evolution". Quaternary International. 210 (1–2): 37–43. doi:10.1016/j.quaint.2009.08.011.
^Goso, H.; Bossi, J. (1966). "Cenozoico". In Bossi, J. (ed.). Geología del Uruguay [Geology of Uruguay] (in Spanish). Universidad de la República, Montevideo. pp. 259–301.
^Mones, A. (1988). "Notas paleontológicas uruguayas. IV. Nuevos registros de mamíferos fósiles de la Formación San José (Plioceno–Plesitoceno inferior?) (Mammalia: Xenarthra; Artiodactyla; Rodentia)". Comunicaciones Paleontologicas Museo Nacional de Historia Natural de Montevideo. 20: 255–277.
^Mcdonald, H. G.; Perea, D. (2002). "The large scelidothere Catonyx tarijensis (Xenarthra, Mylodontidae) from the Pleistocene of Uruguay". Journal of Vertebrate Paleontology. 22 (3): 677–683. doi:10.1671/0272-4634(2002)022[0677:tlsctx]2.0.co;2. S2CID86021240.
^ abcdefgFerrero, B.S.; Schmidt, G.I.; Pérez-Garcia, M.I.; Perea, D.; Ribeiro, A.M. (23 February 2022). "A new Toxodontidae (Mammalia, Notoungulata) from the Upper Pliocene-Lower Pleistocene of Uruguay". Journal of Vertebrate Paleontology: 1–12. doi:10.1080/02724634.2021.2023167.
^Ubilla, M.; Gaudioso, P. J.; Perea, D. (2019). "First fossil record of a bat (Chiroptera, Phyllostomidae) from Uruguay (Plio-Pleistocene, South America): a giant desmodontine". Historical Biology. 33 (2): 138. doi:10.1080/08912963.2019.1590352. S2CID132321589.
^Corona, A.; Perea, D.; Ubilla, M. (2019). "A new genus of Proterotheriinae (Mammalia, Litopterna) from the Pleistocene of Uruguay". Journal of Vertebrate Paleontology: e1567523. doi:10.1080/02724634.2019.1567523.
^Gasparini, G.M.; Ubilla, M. (2011). "Platygonus sp. (Mammalia: Tayassuidae) in Uruguay (Raigón? Formation; Pliocene–early Pleistocene), comments about its distribution and palaeoenvironmental significance in South America". Journal of Natural History. 45 (45–46): 2855–2870. doi:10.1080/00222933.2011.620716. hdl:11336/95660.
^Prevosti, Francisco J.; Forasiepi, Analía M. (2015). "4. South American Fossil Carnivorans (Order Carnivora)". Evolution of South American Mammalian Predators During the Cenozoic: Paleobiogeographic and Paleoenvironmental Contingencies. Springer International Publishing. p. 98. ISBN9783319037011.
^McDonald, H.G.; Werdelin, L. (2018). Shaw, C.A.; McDonald, H.G.; Werdelin, L. (eds.). Smilodon: The Iconic Sabertooth. Johns Hopkins University Press. p. 70. ISBN9781421425573.