Paleontologist William Parks described skeleton
ROM 804 in 1926 as
Thescelosaurus warreni, which had in 1922 been discovered in what was then called the
Edmonton Formation near Rumsey Ferry on the
Red Deer River. When found, it consisted of a partial skull missing the
beak region, most of the left
pectoral girdle (including a
suprascapula, a bone more commonly found in
lizards, but which is believed to have been present in
cartilaginous form in some ornithopods due to the roughened ends of their
scapulae), the left arm except the hand, ribs and
sternal elements, a damaged left
pelvis, right
ischium, the left leg except for some toe bones, articulated
vertebrae from the back, hip, and tail, and a number of
ossified tendons that sheathed the end of the tail. The body of the animal had fallen on its left side, and most of the right side had been destroyed before burial; in addition, the head had been separated from the body, and the neck had been lost. Parks differentiated the new
species from
T. neglectus by leg proportions;
T. warreni had a longer
tibia than
femur, and longer toes. In 1940, he presented a more thorough comparison. He found several differences between the two genera throughout the body. He assigned
Parksosaurus to the
Hypsilophodontinae with
Hypsilophodon and
Dysalotosaurus, and
Thescelosaurus to the
Thescelosaurinae. The genus attracted little attention until
Peter Galton began his revision of hypsilophodonts in the 1970s.
Parksosaurus received a redescription in 1973, wherein it was considered to be related to a
Hypsilophodon\
Laosaurus\
L. minimus lineage. After this, it once again returned to obscurity. George Olshevsky emended the species name to
P. warrenae in 1992, because the species name honors a woman (Mrs. H. D. Warren who financially supported the research), but outside of Internet sites, the original spelling has been preferred. ==Classification==