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Dipsalidictis krausei
Taxonomy
Dipsalidictis krausei was named by Gunnell and Gingerich (1991). Its type specimen is UM 69331, a partial skeleton (skull, left and right dentaries, and associated postcranial elements), and it is a 3D body fossil. Its type locality is Krause Quarry, which is in a Clarkforkian terrestrial horizon in Wyoming.
Synonymy list
Year | Name and author |
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1991 | Dipsalidictis krausei Gunnell and Gingerich p. 150 figs. Fig. 2, 3, 6F, 7B, E, H |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Dipsalidictis krausei Gunnell and Gingerich 1991
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Diagnosis
Reference | Diagnosis | |
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G. F. Gunnell and P. D. Gingerich 1991 | ipsalidictis krausei differs from D. platypus in being significantly larger, differs from D. aequidens in being smaller and in having less robust premolars, differs from D. transiens in having narrower lower molar talonids, a more anteroposteriorly compressed MI trigonid, and less robust premolars with P, lacking or having a very small anterior basal cusp. |
Measurements
No measurements are available
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Source: f = family, subc = subclass, c = class, subp = subphylum | |||||
References: Ji et al. 2002, Hendy et al. 2009, Lillegraven 1979, Gunnell 1998, Carroll 1988 |
Age range: base of the Tiffanian to the top of the Clarkforkian or 61.70000 to 54.90000 Ma
Collections (10 total)
Time interval | Ma | Country or state | Original ID and collection number |
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Tiffanian | USA (Wyoming) | Dipsalidictis krausei (190428 190456 190483) | |
Clarkforkian | USA (Wyoming) | Dipsalidictis krausei (15134 15159 164518 190455) Oxyaena transiens (type locality: 15087 15109 15176) |