A new Late Miocene stem Octodontoid (Rodentia: Caviomorpha: Octochinchilloi) from the Solimões Formation (Brazil): paleobiogeographic implications

• Published in: Journal of vertebrate paleontology Vol. 44; no. 1
• Main Authors: Fontoura, Emmanuelle, Boivin, Myriam, Marivaux, Laurent, Antoine, Pierre-Olivier, Stutz, Narla S., Negri, Francisco Ricardo, Ribeiro, Ana Maria, Kerber, Leonardo
• Format: Journal Article
• Language: English
• Published: Taylor & Francis 02-01-2024; Society of Vertebrate Paleontology
• Subjects: Animal biology; Earth Sciences; Life Sciences; Paleontology; Sciences of the Universe; Vertebrate Zoology
• ISSN: 0272-4634; 1937-2809
• DOI: 10.1080/02724634.2024.2382822

Caviomorphs are the neotropical hystricognathous rodents (Ctenohystrica: Hystricognathi: Caviomorpha). Octodontoidea are today the richest and most speciose clade of caviomorphs. Their fossil record also reveals a wide array of extinct species, including Acarechimys, a taxon with a widespread South American distribution and extensive temporal range. This genus comprises at least five species documented in deposits ranging from the late Oligocene to the Middle Miocene. Here, we report the discovery of a new species of Acarechimys from Upper Miocene deposits of the Envira River (PRE06 outcrop), situated in the Acre State, western Brazilian Amazonia. The new species differs from the other species of the genus in having lower molars with a strong posterior arm of the metaconid, the presence of a mesostylid (usually prominent) and a neomesolophid forwardly directed and connected to the metalophulid I on m1 but not on m2-3, and the absence of posterior arm of the protoconid. This taxon represents the youngest known species of the Acarechimys lineage to date. Its occurrence in Western Amazonia strengthens support for the hypothesis that South American rodent lineages survived longer during the Neogene at low latitudes than in the southern regions of the continent.