Albertonykus (meaning "Alberta claw") is an extinct genus of alvarezsaurid dinosaur from the Maastrichtian-age (Upper Cretaceous) rocks of the Horseshoe Canyon Formation of Alberta, Canada. It is known from forelimb and hindlimb remains from multiple individuals. All but two of the specimens come from a bonebed dominated by Albertosaurus, located at the top of Unit 4 of the Horseshoe Canyon Formation,Larson, D. W., Brinkman, D. B., & Bell, P. R. (2010). Faunal assemblages from the upper Horseshoe Canyon Formation, an early Maastrichtian cool-climate assemblage from Alberta, with special reference to the Albertosaurus sarcophagus bonebed This article is one of a series of papers published in this Special Issue on the theme Albertosaurus. Canadian Journal of Earth Sciences, 47(9), 1159-1181. dating to ~68.5 million years ago.
Albertonykus is interpreted as having fed on wood-nesting because the forelimbs appear specialized for digging but are too short for burrowing. Albertonykus is the earliest known alvarezsaurid. Isolated bones of alvarezsaurids are known from late Maastrichtian rocks in Montana and Wyoming (United States). The bones now belonged to a new genus, Trierarchuncus.
The type species is A. borealis, described by Nick Longrich and Phillip Currie in 2009. The specific name ( borealis) means "north".
Renewed quarrying in the Albertosaurus bonebed in Dry Island Provincial Park again produced the remains of over twenty specimens of Albertosaurus, and the quarry has yet to be fully excavated. It is not known why so many tyrannosaurs were found in one place: paleontologist Nick Longrich speculated that the site was part of a predator trap, where trapped prey animals drew predators to their deaths.
At the same site, over a dozen arm and leg bones belonging to an unknown species of small theropod were in 2002 excavated by a team of scientist led by Philip John Currie of the University of Alberta. The bones were then stored at the Royal Tyrrell Museum in Alberta. Ken Than, National Geographic News Jeanna Bryner, MSNBC.com In 2005 Nick Longrich, then a student at the University of Calgary, happened upon the small fossils while comparing Albertosaurus claws to other dinosaur species. Longrich recognized the fossils as alvarezsaurid, concluding that they represented a new species. Other fragments of Albertonykus were then recognized in the collections, which had not been identified as a separate species.
Possible prey items were evaluated and compared with the fossil record of social insects. were not an important part of the ecosystem during the Cretaceous, and mound-building termites do not appear until the Eocene. This leaves the possibility that Albertonykus preyed on wood-nesting termites. This hypothesis was tested by examining petrified wood from the Horseshoe Canyon Formation, where Albertonykus was found. The wood found there frequently contains borings, which resemble those of termites.
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