Sphaerotholus is a genus of dinosaur from the Upper Cretaceous of the western United States and Canada. To date, five species have been described: the type species, S. goodwini, from the Den-na-zin Member of the Kirtland Formation and possibly the Fossil Forest Member of the Fruitland Formation (Late Campanian) of San Juan County, New Mexico, USA; S. buchholtzae, from the Hell Creek Formation (Late Maastrichtian) of western Carter County, Montana, USA and the Frenchman Formation of Saskatchewan, Canada; S. edmontonensis, from the Horseshoe Canyon Formation of Alberta, Canada; S. lyonsi, from the Dinosaur Park Formation (Campanian) of Alberta, Canada; and S. triregnum from the Hell Creek Formation of Garfield County, Montana, USA.
History of discovery
The
etymology of
Sphaerotholus is a combination of the
Greek language sphaira, meaning "ball", and
tholos, meaning "dome", and is a reference to the characteristically dome-shaped pachycephalosaurian skull. The survival of
Sphaerotholus from the Campanian of New Mexico to the end of the Maastrichtian of Montana demonstrates that this
taxon had both a relatively long duration (approximately 7-8 million years) and a widespread distribution. Williamson and Carr, who first described the
genus in 2002, diagnose it as follows: "Differs from all other pachycephalosaurids where known in the possession of a parietosquamosal bar that decreases in depth laterally as seen in caudal view and is bordered by a single row of nodes and one lateroventral corner node."
Sphaerotholus is considered a highly
Synapomorphy pachycephalosaur.
Species
Sphaerotholus goodwini
The
holotype of the type species (NMMNH P-27403, New Mexico Museum of Natural History) consists of an incomplete skull lacking the facial and palatal elements. The species is diagnosed as follows: "
Sphaerotholus which in caudal view possesses a parietosquamosal bar that reduces in depth laterally to a lesser extent than in
S. buchholtzae and the
parietal is reduced to a thin slip between the
." The species name honors
paleontologist Mark Goodwin for his work with pachycephalosaurian dinosaurs.
It has been suggested that
Stegoceras novomexicanum is a juvenile representative of this species, because the parietal shelf that morphologically distinguishes
S. novomexicanum from
Sphaerotholus goodwini disappears through growth in
Stegoceras validum.
Sphaerotholus edmontonensis
Troodon edmontonensis was described by Brown and Schlaikjer in 1943 on the basis of three domes from the Horseshoe Canyon Formation of Alberta.
Williamson and Carr considered the species to be invalid,
but in 2010 Nicholas Longrich et al. created the novel combination
Sphaerotholus edmontonensis that could be distinguished from
S. goodwini by the paired hornlets on the back of the dome, and from
S. buchholtzae by the elongate parietals.
It was once considered a species of
Stegoceras and was about the same size, reaching in length and in body mass.
Sphaerotholus buchholtzae
The holotype of
S. buchholtzae (TMP 87.113.3) consists of an incomplete skull, found in the Hell Creek Formation. The species was diagnosed as having a parietal that is widely exposed between the squamosals and wide enough to bear parietosquamosal nodes, a shallower caudal margin of the parietosquamosal shelf, the lateral corner node is reduced in size and located above the ventral margin of the parietosquamosal bar, and the nodes in the lateral margin of the parietosquamosal shelf reduced on the squamosal and coalescing into a ridge on the postorbital.
The specific name honors Emily A. Buchholtz for her extensive work with pachycephalosaurians.
Sullivan (2003) considered S. buchholtzae a junior synonym of Prenocephale edmontonensis (or Sphaerotholus edmontonensis).
Sphaerotholus lyonsi
Described by Woodruff, Schott, and Evans in 2023 based on an immature specimen. Lived in the Dinosaur Park Formation in Canada, c. 76 million years ago. It is characterized by a double row of small bony nodes along the back of its skull, as opposed to the single row of large nodes in
S. goodwini,
S. edmontonensis, and
S. buchholtzae.
Sphaerotholus triregnum
Described by Woodruff, Schott, and Evans in 2023 based on a subadult specimen. Lived in the middle section of the Hell Creek Formation in
Montana, USA.
It is characterized by a triple row of small bony nodes along the back of its skull, as opposed to the single row of large nodes in
S. buchholtzae and
S. edmontonensis.
It is named for the resemblance of its domed skull with a triple "crown"-like appearance of nodes to the
Papal tiara or "Triregnum".
Classification
In their 2023 description of
S. lyonsi and
S. triregnum, Woodruff, Schott & Evans analyzed the placement of the genus
Sphaerotholus within the Pachycephalosauria. They recovered all proposed species of
Sphaerotholus as a monophyletic group of derived pachycephalosaurines, as the
sister taxon to the Pachycephalosaurini. The results of their phylogenetic analyses are shown in the
cladogram below:
See also
-
Timeline of pachycephalosaur research
Sources
External links
-
dinosaur.net.cn (includes photograph of the type skull of Sphaerotholus goodwini and a life restoration of same)
