Pachyrhinosaurus lakustai
A New Species!
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Philip Currie, Wann Langston, Darren Tanke: A New Horned Dinosaur from an Upper Cretaceous Bone Bed in Alberta (published by National Research Council Canada and available at their website). Read
the press releases
here. |
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The
first Pachyrhinosaurus was unearthed and named by Charley Sternberg in
1946, from the
St. Mary Formation of Southwestern Alberta. Sternberg later
described the specimen as
P. canadensis in 1950.
The Pachyrhinosaurus was an Ornithischian dinosaur, belonging to the larger group of Ceratopsians, (horned, herbivorous dinosaurs). It lived in the late Cretaceous of North America, about 72-68 million years ago. The Pachyrhinosaurus was a fairly large animal (like the present day rhinoceros), reaching up to 23 feet in length. As its name suggests, it had a thick (pachy) bony knob on its nose (rhino) rather than a horn. Its relatively broad skull had a short crest or frill on the back. The beak was narrow. Pachyrhinosaurus remains are known from the North
slopes of Alaska, from Southern Alberta, and most importantly from the
Pipestone Creek Bonebed site close to the city of Grande Prairie Al Lakusta found the bonebed along Pipestone Creek
in 1972. The Pipestone Creek site was excavated by the Royal Tyrrell
Museum during the summers of 1986-89. It has extreme significance, because of
the density of
disarticulated skeletons. The bonebed contains up to 100 bones per square
meter. 3500 bones, including 14 skulls have been removed from the site.
Apparently, the site resulted from a mass mortality event. It is thought
that Pachyrhinosaurus herds migrated seasonally, following the
availability of plant food resources. During the migration our herd
crossed a river in flood. The animals may have panicked and
similarly to the mass mortality of the Quebec caribou herd in the early
1980’s, the dinosaurs perished in the flood. Five composite skeletons were created for
the ExTerra project, and one for the Royal Tyrrell Museum. One of these
skeletons is now on display at the Grande Prairie Regional College The Pipestone Creek site indicates that the herd
contained animals from juveniles to fully grown ones,
indicating they cared for their young. Because of the abundance of the
skulls, it could be established that some specimens had a convex nasal
boss, while others a
concave nasal boss. Also, these specimens had a unicorn horn in the
middle of the parietal bar over the eyes. |
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