Peramelemorphia Ameghino, 1889
publication ID |
https://doi.org/10.1206/0003-0090.457.1.1 |
persistent identifier |
https://treatment.plazi.org/id/03EFDD5D-F6E9-68FB-DABE-FF4C19C5FD0E |
treatment provided by |
Felipe (2022-08-07 14:35:17, last updated 2022-08-08 12:28:52) |
scientific name |
Peramelemorphia Ameghino, 1889 |
status |
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Peramelemorphia Ameghino, 1889
CONTENTS: † Bulungu , † Galadi, Perameloidea , and † Yarala .
STEM AGE: 43.7 Mya (95% HPD: 39.6–47.4 Mya).
CROWN AGE: 31.4 Mya (95% HPD: 25.3–37.9 Mya).
UNAMBIGUOUS CRANIODENTAL SYNAPOMOR-
PHIES: Facial exposure of jugal deeply bifid, with distinct anterodorsal and anteroventral processes (char. 20: 0→1; ci = 1.000); lambdoid sesamoids present (char. 89: 0→1; ci = 1.000); M1 preparacrista absent or indistinct (char. 138: 0→1; ci = 0.333); M1 pseudopreparacrista present (char. 139: 0→1; ci = 0.333); and hypoconulid notch in anterior cingulid of m2–4 absent (char. 158: 0→1; ci = 0.500).
COMMENTS: Our estimate for the divergence between Peramelemorphia and Dasyuromorphia dates to the middle Eocene. As mentioned above (see Agreodontia), isolated dental remains from the early Eocene Tingamarra Local Fauna have been identified as putatively peramelemorphian, which would predate our estimate, but the Tingamarran specimens cannot be unequivocally referred to the Peramelemorphia . Instead, the oldest definitive peramelemorphians are late Oligocene ( Travouillon et al., 2013a, 2021; Warburton and Travouillon, 2016). The three fossils included here († Bulungu , † Galadi , † Yarala ) are late Oligocene to Miocene taxa (Muirhead and Filan, 1995; Muirhead, 2000; Travouillon et al., 2010, 2013b; Gurovich et al., 2014; Warburton and Travouillon, 2016) and they are recovered outside the peramelemorphian crown clade (Perameloidea; see below) in our analyses, as in previous phylogenetic studies ( Travouillon et al., 2010, 2013a, 2013b, 2014 a, 2015 b, 2019, 2021; Gurovich et al., 2014; Chamberlain et al., 2015; Travouillon and Phillips, 2018). Putative early perameloids are known from the middle Miocene ( Travouillon et al., 2014a; see Perameloidea below), but these were not included here because they are only known from isolated teeth.
A recent study by Abello and Candela (2019) included morphological and total evidence phylogenetic analyses that placed members of the South American family † Argyrolagidae in a clade that was sister to Peramelemorphia (represented by Echymipera and Perameles ), but the authors acknowledged that this geographically implausible relationship might reflect convergent evolution of similar derived tarsal features; based on available evidence, argyrolagids are most likely to be paucituberculatans (Sánchez-Villagra, 2001; Beck, 2017a; Zimicz and Goin, 2020) or polydolopimorphians (Goin et al., 2009a; Chornogubsky and Goin, 2015; Carneiro and Oliveira, 2017a, 2017b; Carneiro, 2018, 2019; Carneiro et al., 2018).
Rosa, B. B., G. A. R. Melo, and M. S. Barbeitos. 2019. Homoplasy-based partitioning outperforms alternatives in Bayesian analysis of discrete morphological data. Systematic Biology 68 (4): 657 - 671.
Travouillon, K. J., Y. Gurovich, R. M. D. Beck, and J. Muirhead. 2010. An exceptionally well-preserved short-snouted bandicoot (Marsupialia; Peramelemorphia) from Riversleigh's Oligo-Miocene deposits, northwestern Queensland, Australia. Journal of Vertebrate Paleontology 30 (5): 1528 - 1546.
Travouillon, K. J., R. M. D. Beck, S. J. Hand, and M. Archer. 2013 a. The oldest fossil record of bandicoots (Marsupialia; Peramelemorphia) from the late Oligocene of Australia. Palaeontologia Electronica 16 (2): 13 A.
Travouillon, K. J., Y. Gurovich, M. Archer, S. J. Hand, and J. Muirhead. 2013 b. The genus Galadi: three new bandicoots (Marsupialia, Peramelemorphia) from Riversleigh's Miocene deposits, Northwestern Queensland, Australia. Journal of Vertebrate Paleontology 33 (1): 153 - 168.
Travouillon, K. J., S. J. Hand, M. Archer, and K. H. Black. 2014 a. Earliest modern bandicoot and bilby (Marsupialia, Peramelidae and Thylacomyidae) from the Miocene of the Riversleigh World Heritage Area, northwestern Queensland, Australia. Journal of Vertebrate Paleontology 34 (2): 375 - 382.
Travouillon, K. J., and M. J. Phillips. 2018. Total evidence analysis of the phylogenetic relationships of bandicoots and bilbies (Marsupialia: Peramelemorphia): reassessment of two species and description of a new species. Zootaxa 4378 (2): 224 - 256.
Travouillon, K. J., R. M. D. Beck, and J. A. Case. 2021. Upper Oligocene - lower-Middle Miocene peramelemorphians from the Etadunna, Namba and Wipajiri formations of South Australia. Alcheringa: an Australasian Journal of Palaeontology 45 (1): 109 - 125.
Warburton, N. M., and K. J. Travouillon. 2016. The biology and palaeontology of the Peramelemorphia: a review of current knowledge and future research directions. Australian Journal of Zoology 64 (3): 151 - 181.
Yates, A. M. 2015 b. New craniodental remains of Wakaleo alcootaensis (Diprotodontia: Thylacoleonidae) a carnivorous marsupial from the late Miocene Alcoota Local Fauna of the Northern Territory, Australia. PeerJ 3: e 1408.
Zimicz, A. N., and F. J. Goin. 2020. A reassessment of the genus Groeberia Patterson, 1952 (Mammalia, Metatheria): functional and phylogenetic implications. Journal of Systematic Palaeontology 18 (12): 975 - 992.
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