Didelphodon coyi Fox and Naylor, 1986

Fox, Richard C. & Naylor, Bruce G., 2006, Stagodontid marsupials from the Late Cretaceous of Canada and their systematic and functional implications, Acta Palaeontologica Polonica 51 (1), pp. 13-36 : 20

publication ID

https://doi.org/ 10.5281/zenodo.13272084

persistent identifier

https://treatment.plazi.org/id/364A4435-FFAD-FFFD-FFB8-FEAE3498FBAE

treatment provided by

Felipe

scientific name

Didelphodon coyi Fox and Naylor, 1986
status

 

Didelphodon coyi Fox and Naylor, 1986

Figs. 1C View Fig , 2 View Fig , 3A, B View Fig .

Holotype: TMP 84.64 View Materials .1, incomplete right dentary containing p3, m3–4 ( Fox and Naylor 1986: figs. 3, 4). Edmontonian Land Mammal Age (early Maastrichtian), Michichi Creek , Alberta.

New material.—TMP 91.166.1, an incomplete right dentary containing p1–3, m1–2, m4 (broken), and roots of the canine, two incisors, and m3 contained in their alveoli, from Paintearth Creek, Alberta; TMP 90.12.29, an incomplete left dentary with heavily worn and broken p3, alveoli for m1–4, the canine, p1? and p2, from the type locality, Michichi Creek, Alberta ( Fox and Naylor 1986) (both of these localities are in the Horseshoe Canyon Formation, with exact coordinates on file at the Royal Tyrrell Museum of Palaeontology); TMP 94.125.125, incomplete right maxilla with P3, M1 and damaged M2, from the latest Cretaceous (latest Maastrichtian; Lancian) Scollard Formation at KUA−1 [see Lillegraven (1969) for description of the locality and Archibald (1982) for account of the Trochu local fauna; see Fox (1974) and Fox and Naylor (2003) for important additions to this local fauna].

Although the dentary TMP 90.12 View Materials .29 was found at the type locality and is from the opposite side of the jaw than the holotype , the two specimens are clearly from different individuals as evidenced, for example, by the deep wear exhibited on p3 of TMP 90.12 View Materials .29 and the virtually unworn p3 of the holotype .

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