2017
DOI: 10.1017/jpa.2017.53
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Patagonian Eocene Archaeopithecidae Ameghino, 1897 (Notoungulata): systematic revision, phylogeny and biostratigraphy

Abstract: Abstract.-The Archaeopithecidae is a very poorly known group of native ungulates from the Eocene of Patagonia (Argentina), whose alpha taxonomy has remained obscure since Ameghino's times. It is traditionally considered as a family representative of the Casamayoran (middle Eocene) South American Land Mammal Age, and is thought to be morphologically close to the notopithecids. After studying >200 specimens from several institutions, including all the type specimens, a taxonomic overestimation is established. Ou… Show more

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Cited by 15 publications
(17 citation statements)
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“…The peculiar eruption sequence (d)P/p4→(d)P/p3→(d)P/p2) described here for the Interatheriinae was observed in the Eocene henricosborniid Henricosbornia (Vera, 2016) and other Typotheria, such as the Eocene Archaeopithecidae Archaeopithecus (Vera, 2017), the Notopithecinae (Vera, 2013; Vera and Cerdeño, 2014), except for Guilielmoscottia plicifera Ameghino, 1901 (sequence P/p3→P/p4→P/p2), and the hegetotheriids Paedotherium (Cerdeño et al, 2017), Hegetotherium mirabile , and Pachyrukhos moyani (M.F., personal observation). The simultaneous presence of dP2 and P3–4 described for the leontinid Coquenia bondi (Deraco and García López, 2011) and of the barely worn P/p2 along with more-worn P/p3–4 observed in the notohippid Notohippus toxodontoides (personal observation) allows us to infer the same delay in the eruption of P2 as the interatheriines studied here, but P/p4 and P/p3 erupt almost simoultanesly.…”
Section: Discussionmentioning
confidence: 50%
“…The peculiar eruption sequence (d)P/p4→(d)P/p3→(d)P/p2) described here for the Interatheriinae was observed in the Eocene henricosborniid Henricosbornia (Vera, 2016) and other Typotheria, such as the Eocene Archaeopithecidae Archaeopithecus (Vera, 2017), the Notopithecinae (Vera, 2013; Vera and Cerdeño, 2014), except for Guilielmoscottia plicifera Ameghino, 1901 (sequence P/p3→P/p4→P/p2), and the hegetotheriids Paedotherium (Cerdeño et al, 2017), Hegetotherium mirabile , and Pachyrukhos moyani (M.F., personal observation). The simultaneous presence of dP2 and P3–4 described for the leontinid Coquenia bondi (Deraco and García López, 2011) and of the barely worn P/p2 along with more-worn P/p3–4 observed in the notohippid Notohippus toxodontoides (personal observation) allows us to infer the same delay in the eruption of P2 as the interatheriines studied here, but P/p4 and P/p3 erupt almost simoultanesly.…”
Section: Discussionmentioning
confidence: 50%
“…For extinct mammals, we used predictive equations (Supporting Information: appendix ) according to osteological variables, such as astragalus (Tsubamoto, 2014; n = 80), calcaneus (Tsubamoto, 2019; n = 69), and dental measurements (Janis, 1990; n = 136; Scarano et al, 2011; n = 35). Data sets of dental measurements (length of first lower molar, second upper molar, lower molar raw, third lower molar) were taken from different authors (Simpson, 1948; Vera, 2017; Vera & Krause, 2020). Body mass estimation from the circumference of the humerus and femur follows Campione and Evans (2012).…”
Section: Methodsmentioning
confidence: 99%
“…Using data taken from long bones (humerus and femur), tarsus (astragalus and calcaneus), and teeth (Simpson, 1948;Vera, 2012Vera, , 2017Vera & Krause, 2020; this work; Table 2), we estimated the range of body masses for N. murinus and N. adapinus applying different models (Campione & Evans, 2012;Janis, 1990;Scarano et al, 2011;Tsubamoto, 2014Tsubamoto, , 2019. The body mass range for N. murinus (MPEF-PV 1115) was estimated between 8.5 and 20 kg (Figure 11c), which indicates a medium-sized mammal.…”
Section: Body Massmentioning
confidence: 99%
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“…Traditionally, shape and age variation in the dentition of extinct native South America ungulates (Notoungulata) has been described in terms of both qualitative (morphological) and quantitative (linear dimensions or other measurements) changes, taking a controversial role in the systematics of several groups (e.g., Billet, De Muizon, & Quispe, ; Billet et al, ; Cerdeño, Montalvo, & Sostillo, ; Cerdeño, Reguero, & Vera, ; Cerdeño et al, ; Croft, Reguero, Bond, Wyss, & Flynn, ; Francis, ; Madden, ; Vera, ). For instance, using geometric morphometrics to analyze high‐crowned upper and lower teeth, Ercoli, Candela, Rasia, and Ramírez () revalidated a species of Paedotherium (Hegetotheriidae) from the Late Miocene; however, no previous GM analysis has been done on the low‐crowned dentition of Eocene notoungulates.…”
Section: Introductionmentioning
confidence: 99%