Please use this identifier to cite or link to this item: https://hdl.handle.net/1959.11/14856
Title: Faunal assemblages from the upper Horseshoe Canyon Formation, an early Maastrichtian cool-climate assemblage from Alberta, with special reference to the 'Albertosaurus sarcophagus' bonebed
Contributor(s): Larson, Derek W (author); Brinkman, Donald B (author); Bell, Phil (author)orcid 
Publication Date: 2010
DOI: 10.1139/E10-005
Handle Link: https://hdl.handle.net/1959.11/14856
Abstract: The faunal assemblage from the early Maastrichtian portion of the Horseshoe Canyon Formation is described on the basis of four new vertebrate microfossil localities and remains from the Albertosaurus bonebed. All of the localities sampled were deposited during a cool, dry climate at a palaeolatitude of ~58°N. Thus, these assemblages provide insight into a northern cool-climate assemblage in the early Maastrichtian of western North America. This fauna is characterized by the presence of taxa with more northern affinities, such as Holostean A, champsosaurs, Troodon, and toothed birds. Warm-climate taxa, such as crocodylians, large and diverse turtles, and albanerpetontids are notable in their absence. The 'Albertosaurus' bonebed locality at the top of unit 4 of the Horseshoe Canyon Formation was deposited during the initial stages of a trend to a warmer and wetter climate that is represented in unit 5. The bonebed shares many taxa with the underlying vertebrate microfossil localities. However, a notable difference is the presence of Atrociraptor marshalli from the 'Albertosaurus' bonebed but not the other localities in the upper Horseshoe Canyon Formation. The presence of Atrociraptor may be attributable to this change in climate rather than local ecological conditions. Also, the assemblages are different in the paucity of fish remains in the bonebed, and the relative rarity of shed hadrosaur teeth. The low abundance of aquatic taxa and rarity of shed teeth of hadrosaurs indicate that the locality is largely autochthonous, with little material being transported into the site.
Publication Type: Journal Article
Source of Publication: Canadian Journal of Earth Sciences, 47(9), p. 1159-1181
Publisher: NRC Research Press
Place of Publication: Canada
ISSN: 1480-3313
0008-4077
Field of Research (FOR): 060302 Biogeography and Phylogeography
040308 Palaeontology (incl Palynology)
060301 Animal Systematics and Taxonomy
Peer Reviewed: Yes
HERDC Category Description: C1 Refereed Article in a Scholarly Journal
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