Sphenopsalis
| Sphenopsalis Temporal range:Thanetian
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|---|---|
Scientific classification
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Mammalia |
| Order: | †Multituberculata |
| Family: | †Lambdopsalidae [1] |
| Genus: | †Sphenopsalis |
| Species: | †S. nobilis
|
| Binomial name | |
| †Sphenopsalis nobilis Matthew, Granger & Simpson, 1928
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Sphenopsalisis agenusof extinctmammalfrom thePaleoceneof what is now CentralAsia.It was a member of the extinctorderMultituberculata,and lies within the suborderCimolodontaand the superfamilyTaeniolabidoidea.The genus was named byWilliam Diller Matthew,W. Granger andGeorge Gaylord Simpsonin 1928.
Many workers believe that members of the Taeniolabidoidea, such asSphenopsalis,are all quite similar. For example, they all share a short wide snout and a blocky head[2]so it is probably instructive to look at a close and more commonly occurring relative,Lambdopsalis bulla,a likely burrower.[3][4][5]
This organism is found in the fossil record from 59-55 million years ago, during theThanetianage.[6]One distinguishing feature of this genus is a single rooted 4th premolar (P4).[7]Based on the structure of their teeth,Sphenopsalisappears to have been a leaf eater (foliovore).[8]They and/or their close relatives may have been partially adapted to a digging (fossorial) lifestyle.[9]
The one known species,Sphenopsalis nobilis,was also named by Matthew, Granger and Simpson in 1928. It has been found in the Late PaleoceneNomogenandKhashat FormationofMongoliaandChina.For many years, this species was only known from a handful of fragmentary teeth and bones, but Mao et al discovered additional specimens in 2016 that allowed for more detailed analysis.[10]TheAmerican Museum of Natural HistoryinNew York Cityhas several fragmentary specimens in its collection. [11]
Notes
[edit]- ^Williamson et al, 2015
- ^Kielan-Jarowoska and Hurum, 2001, pg 418-419
- ^Kielan-Jarowoska and Sloan, 1979, pg 195
- ^Kielan-Jarowoska and Qi, 1990, pp 91-92
- ^Mao et al, 2016 pp 443-445
- ^Wilson et al 2012, Supplemental Table 3
- ^Williamson et al, 2016 p 192
- ^Williamson et al, 2016 p 204
- ^Kielan-Jaworowska and Qi 1990, p 91
- ^Mao et al, 2016
- ^Williamson et al, 2016, pg 196
References
[edit]- Dykes, Trevor."Mesozoic Mammals;Eucosmodontidae, Microcosmodontidae and Taeniolabidoidea, an internet directory".Archived fromthe originalon 16 July 2012.
- Kielan-Jaworowska Z., Hurum J.H. (2001)."Phylogeny and Systematics of multituberculate mammals"(PDF).Palaeontology.44(3): 389–429.doi:10.1111/1475-4983.00185.S2CID83592270.
- Kielan-Jaworowska, Zofia; Qi, Tao (1990). "Fossorial adaptations of a Taeniolabidoid Multituberculate mammal from the Eocene of China".Vertebrata PalAsiatica.28(2): 83–94.
- Kielan-Jaworowska, Kielan; Sloan, Robert E. (1979). "Catopsalis (Multituberculata) from Asia and North America and the problem of taeniolabidid dispersal in the Late Cretaceous".Acta Palaeontologica Polonica.24(2): 187–197.
- Mao, Fang-Yuan; Wang, Yang-Qing; Meng, Jin (2016)."New specimens of the multituberculate mammal Sphenopsalis from China: Implications for phylogeny and biology of taeniolabidoids".Acta Palaeontologica Polonica.61(2): 429–454.doi:10.4202/app.00117.2014.
- Williamson, Thomas E.; Brusatte, Stephen L.; Secord, Ross; Shelley, Sarah (2016). "A new taeniolabidoid multituberculate (Mammalia) from the middle Puercan of the Nacimiento Formation, New Mexico, and a revision of taeniolabidoid systematics and phylogeny".Zoological Journal of the Linnean Society.177:183–208.doi:10.1111/zoj.12336.
- Wilson, Gregory P.; Evans, Alistair R.; Corfe, Ian J.; Smits, Peter D.; Fortelius, Mikael; Jernvall, Jukka (2012). "Adaptive radiation of multituberculate mammals before the extinction of dinosaurs".Nature.483(7390): 457–460.doi:10.1038/nature10880.PMID22419156.S2CID4419772.
Further reading
[edit]- Matthew, et al. (1928), "Paleocene Multituberculates from Mongolia".Am. Museum Novitates331,p. 1-4.
- Simmons, N.B. and Miao, D. 1986. Paraphyly of Catopsalis (Mammalia: Multituberculata) and its biogeographic implications. University of Wyoming, Contributions to Geology, Special Paper, 3, 87±94.
