Coronosaurus Brinkmani

''Coronosaurus'' is a genus of centrosaurine ceratopsian dinosaurs which lived in the Late Cretaceous, in the middle Campanian stage. Its remains, two bone beds, were discovered by Phillip J. Currie in the Oldman Formation of Alberta, Canada, and its type and only species, ''Coronosaurus brinkmani'', was first described in 2005, as a new species within the genus '' Centrosaurus''. Later studies questioned the presence of a direct relationship, and in 2012 it was named as a separate genus. ''Coronosaurus'' means "crowned lizard", coming from "''corona''", Latin for crown, and "''sauros''", Greek for lizard; this name refers to the unique, crown-like shape of the horns on the top of its frill.

Like other ceratopsids, ''Coronosaurus'' had a large frill and horns on its head. These include a small pair of brow horns over its eyes, a large nasal horn on its snout, and, unique among ceratopsians, irregular, spiky bone masses on its frill. Growing up to around long and in weight, it was mid-sized for its kind. The genus is classified as a member of the Centrosaurini, a group of derived centrosaurines which has also been found include taxa such as ''Styracosaurus'', '' Spinops'', ''Rubeosaurus'', and '' Centrosaurus'', the genus it was originally placed within.

Discovery and naming

''Coronosaurus'' is known from two bone beds, BB 138 and MRR BB, located in the upper unit of the Oldman Formation, of the Belly River Group, excavated by Philip Currie between 1996 and 2000.M.J. Ryan and A.P. Russell, 2003, "New centrosaurine ceratopsids from the late Campanian of Alberta and Montana and a review of contemporaneous and regional patterns of centrosaurine evolution", ''Journal of Vertebrate Paleontology'' 23(3): 91A Most of the ceratopsid material, if not all, from BB 138 in Dinosaur Provincial Park, Alberta, and the MRR BB near Warner, Alberta, was referred to ''C. brinkmani''. Bone bed 138 is located approximately from Brooks, Alberta, in the Oldman Formation and below the contact with the Dinosaur Park Formation. The MRR BB located approximately southwest of BB 138, is also from the Oldman Formation. These bone beds date to the middle Campanian stage of the Late Cretaceous period. Both the specimens and the precise localities are archived at the Royal Tyrrell Museum of Palaeontology, in Drumheller, Alberta.

Michael J. Ryan and Anthony P. Russell described and named the type species, then as '' Centrosaurus brinkmani'', in 2005. Later studies, however, did not recover a monophyletic clade with the genus' type species ''Centrosaurus apertus'' in phylogenetic analyses. Due to this, Ryan, David C. Evans and Kieran M. Shepherd erected the genus ''Coronosaurus'' for the species in 2012. The generic name is derived from the Latin ''corona'', meaning "crown" in reference to the multiple occurrences of extra epiparietals that cover the posterior margin of its parietal, giving it a crown-like appearance, and ''saurus'' (Latinized from Greek ''sauros''), meaning "lizard". The specific name ''brinkmani'' honors Donald Brinkman, for his research in palaeoecology of the Late Cretaceous environments of Alberta. In 2020, in response to the COVID-19 pandemic, Ryan was asked about the naming of the dinosaur, and stated he came up with it because its frill ornamentation made him think of the corona of the sun. He also stated his fellow students at the time had jokingly called it ‘broccoli-ceratops’.

The holotype of ''Coronosaurus'' is TMP 2002.68.1. It is a large adult-sized parietal with an almost complete midline bar and a partial posterior bar with left P1–P3 processes and the partially eroded right P1-P2. The specimen lacks the extreme anterior margin of the midline bar that forms the posterior wall of the frontal fontanelle and the paper-thin lateral margins that define the medial margins of the supraorbital foramina. Other significant specimens according to Ryan & Russell (2005) include TMP 2002.68.3 (a parietal), TMP 2002.68.10 (a postorbital), and TMP 2002.68.5 ( supraorbitals).

Description

''Coronosaurus'' is a medium-sized centrosaurine ceratopsid. Gregory S. Paul in 2010 estimated its body length at and its weight at .Paul, G.S., 2010, ''The Princeton Field Guide to Dinosaurs'', Princeton University Press p. 260 It had as an adult inflated supraorbital horncores — the "brow horns" above the eye sockets — but not elongated as in ''Zuniceratops'', chasmosaurines, and more basal centrosaurines (like ''Albertaceratops'' and '' Diabloceratops''), that project laterally (to the sides) over the orbit. As a sub-adult its postorbital horncores are pyramidal in shape with a slight lateral inflection of the distal, upper, one half.

Uniquely among ceratopsians, ''Coronosaurus'' possesses a number of accessory epiparietal ossifications rear parietal frill of the skull that fuse to the posterior and dorsal frill surface. They develop through ontogeny, the growth of the individual, as short spines that may fuse along their adjacent margins into larger, irregular bone masses. They are located close to the midline of the frill in a closely packed bunch above the base of the first epiparietal (P1), the bone spur that at each side growths downwards over the large opening in each frill half. They contribute to the substance of P1 and, through fusion, form a composite epiparietal, that is equivalent to the second epiparietal (P2) normally formed in a more lateral position. The P1 bases can thus be considered the growth positions of the second epiparietals, the P2 loci. ''Coronosaurus'' has also a uniquely shaped P3 epiparietal. It is variably developed as a short tongue-like hook or tapered spike that is oriented dorsolaterally, following the curve of the frill.

Otherwise, as far as is known ''Coronosaurus'' resembles its relatives '' Centrosaurus'' and ''Styracosaurus'' in its morphology. For example, the nasal of ''Coronosaurus'' closely resembles that of ''Centrosaurus apertus'' in its unfused juvenile or subadult and fused adult forms and appears to have undergone a similar ontogenetic changes. Its erect, laterally compressed nasal horn core has a blunt tip that is formed from the fusion of the opposing nasals. It sits over the posterior portion of the external nares, as it does in all centrosaurines. All juvenile and most adult specimens have gently recurved anterior and posterior margins resulting in most horns having an apex that is oriented at least slightly caudally (backwards).

Classification

In its original description, Ryan & Russell (2005) considered ''Coronosaurus'' to represent a new species of ''Centrosaurus'' on the basis of a small phylogenetic analysis. It included seventeen characters and nine taxa. ''Coronosaurus'' (as ''Centrosaurus brinkmani'') and ''C. apertus'' grouped at the base of the Centrosaurinae, while ''Styracosaurus'' was found to be more closely related to ''Pachyrhinosaurus'', and other derived centrosaurines, than to ''Centrosaurus''. In 2011, Anthony R. Fiorillo and Ronald S. Tykoski modified the analysis of Currie ''et al.'' (2008), with 54 characters, to include more taxa, such as ''C. brinkmani''. They found ''C. brinkmani'' to be the sister taxon of the clade of ''Styracosaurus'' and ''C. apertus'', while ''Pachyrhinosaurus'' and other derived centrosaurines were in a separate lineage. Thus, this analysis found no support for the monophyly of ''Centrosaurus''.

Later, Farke ''et al.'' (2011) used 97 morphological characters to assess the phylogenetic position of a new taxon which they named '' Spinops''. ''Spinops'' was found to be in a polytomy with ''Centrosaurus apertus'', ''C. brinkmani'' and ''Styracosaurus'', and therefore ''C. brinkmani'' was excluded from the analysis to increase the resolution. Finally, Ryan, Evans & Shepherd (2012) used the data matrix of Farke ''et al.'' (2011) to assess the phylogenetic position of ''Xenoceratops''. Their revised analysis had significantly better resolution than that presented by Farke ''et al.'' (2011), due in part to the additional scoring of missing characters for some taxa based on direct observation of their specimens. For example, five additional characters were scored for ''C. brinkmani''. In the resultant tree, it was found to be in more advanced position than ''Spinops'' and ''C. apertus'', as the sister taxon of ''Styracosaurus''. Thus the new generic name, ''Coronosaurus'', was given to it. The cladogram presented below follows a phylogenetic analysis by Chiba ''et al.'' (2017):

Paleoecology

Studies suggest that the paleoenvironment of the Oldman Formation was an ancient coastal plain.Eberth, D.A., and Hamblin, A.P., 1993 , Tectonic, stratigraphic, and sedimentologic significance of a regional discontinuity in the upper Judith River Group (Belly River wedge) of southern Alberta, Saskatchewan, and northern Montana : Canadian Journal of Earth Sciences, 30, 174‒200. In addition to remains of ''Coronosaurus'', this formation has produced the remains of the theropods ''Saurornitholestes'', ''Daspletosaurus'', '' Troodon'', ''Dromaeosaurus'' and ''Hesperonychus'', the ceratopsids ''Albertaceratops'', ''Chasmosaurus'', and ''Anchiceratops'', the hadrosaurids '' Brachylophosaurus'', ''Gryposaurus'', ''Parasaurolophus'', and ''Corythosaurus'', the thescelosaurid '' Albertadromeus'' and the ankylosaurid '' Scolosaurus''.

See also

* Timeline of ceratopsian research

References

{{Taxonbar, from=Q135802
Fossils of Canada
Centrosaurines
Late Cretaceous dinosaurs of North America
Fossil taxa described in 2012
Monotypic dinosaur genera
Oldman fauna
Paleontology in Alberta
Campanian genus first appearances
Campanian genus extinctions
Ornithischian genera