| rdfs:comment
| - In 2010, Canadian fossil hunter Wendy Sloboda found a centrosaurine bonebed in the Pinhorn Provincial Grazing Reserve south of the Milk River, County of Forty Mile No. 8, Alberta. In 2011, a team of the Royal Tyrrell Museum explored the site and began excavating fossils. Next year, a deep overburden was removed. In 2013 and 2014, numerous fossils were discovered.[1]
- In 2010, Canadian fossil hunter Wendy Sloboba found a centrosaurine bonebed in the Pinhorn Provincial Grazing Reserve south of the Milk River, County of Forty Mile No. 8, Alberta. In 2011, a team of the Royal Tyrrell Museum explored the site and began excavating fossils. Next year, a deep overburden was removed. In 2013 and 2014, numerous fossils were discovered.
|
| abstract
| - In 2010, Canadian fossil hunter Wendy Sloboba found a centrosaurine bonebed in the Pinhorn Provincial Grazing Reserve south of the Milk River, County of Forty Mile No. 8, Alberta. In 2011, a team of the Royal Tyrrell Museum explored the site and began excavating fossils. Next year, a deep overburden was removed. In 2013 and 2014, numerous fossils were discovered. In 2015, paleontologists David Evans and Michael Ryan named and described the type species Wendiceratops pinhornensis. The generic name combines a reference to Wendy Sloboda with a Latinised Greek ~ceratops, "horn face". The specific name refers to the provenance from the Pinhorn Reserve. Wendiceratops was the second ceratopsian discovered and named in 2015. The discovery of this new horned dinosaur species - starting from the ground in Alberta, through scientific study and restoration, all the way to its eventual reconstruction and public display in The Royal Ontario Museum (ROM) - was captured in the HISTORY series and companion website Dino Hunt Canada. The holotype, TMP 2011.051.0009, was found in a layer of the Oldman Formation, dating from the Campanian. The layer of mudstone, forty centimetres thick and probably deposited in a single event, has an upper possible age of 79 million years and a lower age of 78.7 million years. The holotype consists of a right parietal bone. Under the assumption that the bonebed contained only a single centrosaurine species, all additional centrosaurine material was referred to Wendiceratops pinhornensis, for a total of 184 specimens representing several individuals, including juveniles. The bones compromise elements from the skull, lower jaws, vertebral column, shoulder girdle, pelvis and limbs. They are largely disarticulated. In addition to the Wendiceratops bones, remains were found of tyrannosaurid theropods, crocodiles, gars and plants.
- In 2010, Canadian fossil hunter Wendy Sloboda found a centrosaurine bonebed in the Pinhorn Provincial Grazing Reserve south of the Milk River, County of Forty Mile No. 8, Alberta. In 2011, a team of the Royal Tyrrell Museum explored the site and began excavating fossils. Next year, a deep overburden was removed. In 2013 and 2014, numerous fossils were discovered.[1] In 2015, paleontologists David Evans and Michael Ryan named and described the type species Wendiceratops pinhornensis. The generic name combines a reference to Wendy Sloboda with a Latinised Greek ~ceratops, "horn face". The specific name refers to the provenance from the Pinhorn Reserve.[1] Wendiceratops was the second ceratopsian discovered and named in 2015.[2] The discovery of this new horned dinosaur species - starting from the ground in Alberta, through scientific study and restoration, all the way to its eventual reconstruction and public display in The Royal Ontario Museum (ROM) - was captured in the HISTORY series and companion website Dino Hunt Canada.[3] The holotype, TMP 2011.051.0009, was found in a layer of the Oldman Formation, dating from the Campanian. The layer of mudstone, forty centimetres thick and probably deposited in a single event, has an upper possible age of 79 million years and a lower age of 78.7 million years. The holotype consists of a right parietal bone. Under the assumption that the bonebed contained only a single centrosaurine species, all additional centrosaurine material was referred to Wendiceratops pinhornensis, for a total of 184 specimens representing several individuals, including juveniles. The bones comprise elements from the skull, lower jaws, vertebral column, shoulder girdle, pelvis and limbs. They are largely disarticulated. In addition to the Wendiceratops bones, remains were found of tyrannosaurid theropods, crocodiles, gars and plants.
|
![[RDF Data]](/fct/images/sw-rdf-blue.png)