Marsupials (Mammalia, Metatheria) from the Brule Formation (Whitneyan, Oligocene) North Dakota

被引:1
|
作者
Korth, William W. [1 ,2 ]
Boyd, Clint A. [3 ]
Emry, Robert J. [4 ]
Person, Jeff J. [3 ]
机构
[1] Rochester Inst Vertebrate Paleontol, 265 Carling Rd, Rochester, NY 14610 USA
[2] Rochester Museum & Sci Ctr, 657 East Ave, Rochester, NY 14607 USA
[3] North Dakota Geol Survey, 600 East Blvd Ave, Bismarck, ND 58505 USA
[4] Natl Museum Nat Hist, Dept Paleobiol, Smithsonian Inst, POB 37012,MRC 121, Washington, DC 20013 USA
关键词
TERTIARY; HERPETOTHERIUM; RODENTS; RANCH;
D O I
10.1017/jpa.2020.41
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Five marsupial species are recognized from the Brule Formation at two localities in southwestern North Dakota: Fitterer Ranch and Obritsch Ranch (middle Oligocene; Whitneyan North American Land Mammal Age [NALMA]). The herpetotheriids Herpetotherium fugax Cope, 1873a, Copedelphys superstes new species, and the peradectid Nanodelphys hunti (Cope, 1873b) are represented at both localities. A fourth species is H. sp., cf. H. merriami (Stock and Furlong, 1922), represented by a single specimen from Fitterer Ranch, being limited elsewhere to the later Arikareean NALMA. A fifth species is represented by two isolated lower cheek teeth, interpreted as m1s, from Fitterer Ranch that are unique in lacking a trigonid (only two cusps present) while having a well-developed talonid. These specimens are referred to an indeterminate herpetotheriine species. The new species of Copedelphys is distinct from other species of the genus in that the anterior two lower molars are enlarged relative to the posterior molars. Overall, this new species is more similar in proportions to the latest Eocene (Chadronian) C. titanelix (Matthew, 1903) than the Oligocene (Orellan and Whitneyan) C. stevensoni (Cope, 1873b). This study adds a third and fourth Whitneyan marsupial fauna from the Great Plains region of North America, increases the known diversity of Whitneyan marsupials, and provides further evidence that marsupial diversity during the late Paleogene in North America was relatively stable until the late early Arikareean NALMA. UUID: http://zoobank.org/b8534802-b9ed-4120-baca-fc72917f7d6a
引用
收藏
页码:193 / 204
页数:12
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