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A new horned dinosaur reveals convergent evolution in cranial ornamentation in Ceratopsidae.
Curr Biol. 2015 Jun 15; 25(12):1641-8.CB

Abstract

Ceratopsid (horned) dinosaurs are an iconic group of large-bodied, quadrupedal, herbivorous dinosaurs that evolved in the Late Cretaceous and were largely restricted to western North America [1-5]. Ceratopsids are easily recognized by their cranial ornamentation in the form of nasal and postorbital horns and frill (capped by epiossifications); these structures show high morphological disparity and also represent the largest cranial display structures known to have evolved [2, 4]. Despite their restricted occurrence in time and space, this group has one of the best fossil records within Dinosauria, showing a rapid diversification in horn and frill morphology [1]. Here a new genus and species of chasmosaurine ceratopsid is described based on a nearly complete and three-dimensionally preserved cranium recovered from the uppermost St. Mary River Formation (Maastrichtian) of southwestern Alberta. Regaliceratops peterhewsi gen. et sp. nov. exhibits many unique characters of the frill and is characterized by a large nasal horncore, small postorbital horncores, and massive parietal epiossifications. Cranial morphology, particularly the epiossifications, suggests close affinity with the late Campanian/early Maastrichian taxon Anchiceratops, as well as with the late Maastrichtian taxon Triceratops. A median epiparietal necessitates a reassessment of epiossification homology and results in a more resolved phylogeny. Most surprisingly, Regaliceratops exhibits a suite of cranial ornamentations that are superficially similar to Campanian centrosaurines, indicating both exploration of novel display morphospace in Chasmosaurinae, especially Maastrichtian forms, and convergent evolution in horn morphology with the recently extinct Centrosaurinae. This marks the first time that evolutionary convergence in horn-like display structures has been demonstrated between dinosaur clades, similar to those seen in fossil and extant mammals [6].

Authors+Show Affiliations

Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, AB T0J 0Y0, Canada. Electronic address: caleb.brown@gov.ab.ca.Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, AB T0J 0Y0, Canada.

Pub Type(s)

Journal Article
Research Support, Non-U.S. Gov't

Language

eng

PubMed ID

26051892

Citation

Brown, Caleb M., and Donald M. Henderson. "A New Horned Dinosaur Reveals Convergent Evolution in Cranial Ornamentation in Ceratopsidae." Current Biology : CB, vol. 25, no. 12, 2015, pp. 1641-8.
Brown CM, Henderson DM. A new horned dinosaur reveals convergent evolution in cranial ornamentation in Ceratopsidae. Curr Biol. 2015;25(12):1641-8.
Brown, C. M., & Henderson, D. M. (2015). A new horned dinosaur reveals convergent evolution in cranial ornamentation in Ceratopsidae. Current Biology : CB, 25(12), 1641-8. https://doi.org/10.1016/j.cub.2015.04.041
Brown CM, Henderson DM. A New Horned Dinosaur Reveals Convergent Evolution in Cranial Ornamentation in Ceratopsidae. Curr Biol. 2015 Jun 15;25(12):1641-8. PubMed PMID: 26051892.
* Article titles in AMA citation format should be in sentence-case
TY - JOUR T1 - A new horned dinosaur reveals convergent evolution in cranial ornamentation in Ceratopsidae. AU - Brown,Caleb M, AU - Henderson,Donald M, Y1 - 2015/06/04/ PY - 2015/03/14/received PY - 2015/04/20/revised PY - 2015/04/20/accepted PY - 2015/6/9/entrez PY - 2015/6/9/pubmed PY - 2016/12/15/medline SP - 1641 EP - 8 JF - Current biology : CB JO - Curr Biol VL - 25 IS - 12 N2 - Ceratopsid (horned) dinosaurs are an iconic group of large-bodied, quadrupedal, herbivorous dinosaurs that evolved in the Late Cretaceous and were largely restricted to western North America [1-5]. Ceratopsids are easily recognized by their cranial ornamentation in the form of nasal and postorbital horns and frill (capped by epiossifications); these structures show high morphological disparity and also represent the largest cranial display structures known to have evolved [2, 4]. Despite their restricted occurrence in time and space, this group has one of the best fossil records within Dinosauria, showing a rapid diversification in horn and frill morphology [1]. Here a new genus and species of chasmosaurine ceratopsid is described based on a nearly complete and three-dimensionally preserved cranium recovered from the uppermost St. Mary River Formation (Maastrichtian) of southwestern Alberta. Regaliceratops peterhewsi gen. et sp. nov. exhibits many unique characters of the frill and is characterized by a large nasal horncore, small postorbital horncores, and massive parietal epiossifications. Cranial morphology, particularly the epiossifications, suggests close affinity with the late Campanian/early Maastrichian taxon Anchiceratops, as well as with the late Maastrichtian taxon Triceratops. A median epiparietal necessitates a reassessment of epiossification homology and results in a more resolved phylogeny. Most surprisingly, Regaliceratops exhibits a suite of cranial ornamentations that are superficially similar to Campanian centrosaurines, indicating both exploration of novel display morphospace in Chasmosaurinae, especially Maastrichtian forms, and convergent evolution in horn morphology with the recently extinct Centrosaurinae. This marks the first time that evolutionary convergence in horn-like display structures has been demonstrated between dinosaur clades, similar to those seen in fossil and extant mammals [6]. SN - 1879-0445 UR - https://www.unboundmedicine.com/medline/citation/26051892/A_new_horned_dinosaur_reveals_convergent_evolution_in_cranial_ornamentation_in_Ceratopsidae_ DB - PRIME DP - Unbound Medicine ER -