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Bell, Phil R., Campione, Nicolás E. (2014) Taphonomy of the Danek Bonebed: a monodominant Edmontosaurus (Hadrosauridae) bonebed from the Horseshoe Canyon Formation, Alberta. Canadian Journal of Earth Sciences, 51 (11) 992-1006 doi:10.1139/cjes-2014-0062

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Reference TypeJournal (article/letter/editorial)
TitleTaphonomy of the Danek Bonebed: a monodominant Edmontosaurus (Hadrosauridae) bonebed from the Horseshoe Canyon Formation, Alberta
JournalCanadian Journal of Earth Sciences
AuthorsBell, Phil R.Author
Campione, Nicolás E.Author
Year2014 (November)Volume51
Issue11
PublisherCanadian Science Publishing
DOIdoi:10.1139/cjes-2014-0062Search in ResearchGate
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Mindat Ref. ID484989Long-form Identifiermindat:1:5:484989:0
GUID0
Full ReferenceBell, Phil R., Campione, Nicolás E. (2014) Taphonomy of the Danek Bonebed: a monodominant Edmontosaurus (Hadrosauridae) bonebed from the Horseshoe Canyon Formation, Alberta. Canadian Journal of Earth Sciences, 51 (11) 992-1006 doi:10.1139/cjes-2014-0062
Plain TextBell, Phil R., Campione, Nicolás E. (2014) Taphonomy of the Danek Bonebed: a monodominant Edmontosaurus (Hadrosauridae) bonebed from the Horseshoe Canyon Formation, Alberta. Canadian Journal of Earth Sciences, 51 (11) 992-1006 doi:10.1139/cjes-2014-0062
In(2014, November) Canadian Journal of Earth Sciences Vol. 51 (11) Canadian Science Publishing
Abstract/Notes The Danek Bonebed (Horsethief Member, Horseshoe Canyon Formation, Late Campanian) is dominated by the remains of at least 12 Edmontosaurus regalis. Skeletal remains of a tyrannosaurid and ceratopsid are also known. The predominantly disarticulated remains were interred on a periodically inundated floodplain and, although the cause of death is unknown, a sudden, catastrophic death explains the demographic spread, faunal diversity, rare greenstick fractures, and homogeneous weathering/abrasion categories of the assemblage. The Danek Bonebed shares a similar taphonomic signature to the Liscomb Bonebed (Prince Creek Formation, Alaska), but it is unique among all other described hadrosaurid bonebeds in the unusually high proportion of bite-marked bones (∼30%), suggesting scavenging played a major role in the reworking of the assemblage. The highest frequency of bite marks is found on small, often unidentifiable (and commonly ignored) bone fragments, underscoring the role that such fragments can play in taphonomic interpretation. Finally, the recognition of E. regalis from central Alberta is an important datum linking contemporaneous occurrences in southern Alberta with slightly older records of this species from the Wapiti Formation in northwestern Alberta.


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