Cranial morphology of a juvenile Triceratops skull from the Hell Creek Formation, McCone County, Montana, with comments on the fossil record of ontogenetically younger skulls
Cranial morphology of a juvenile Triceratops skull from the Hell Creek Formation, McCone County, Montana, with comments on the fossil record of ontogenetically younger skulls (in Through the end Cretaceous in the the type locality of the Hell Creek Formation in Montana and adjacent areas, Gregory P. Wilson (editor), William A. Clemens (editor), John R. Horner (editor) and Joseph H. Hartman (editor))
Special Paper - Geological Society of America (January 2014) 503: 333-347
- Archosauria
- Ceratopsia
- Ceratopsidae
- Chordata
- Cretaceous
- Diapsida
- dinosaurs
- fossil record
- Garfield County Montana
- Hell Creek Formation
- juvenile taxa
- McCone County Montana
- Mesozoic
- Montana
- morphology
- ontogeny
- Ornithischia
- preservation
- Reptilia
- size
- skull
- taphonomy
- Tetrapoda
- Triceratops
- United States
- Upper Cretaceous
- variations
- Vertebrata
- Fort Peck Lake
Here, we describe a juvenile Triceratops sp. skull, UCMP 136306, from the Hell Creek Formation, McCone County, Montana. The relative completeness and superb preservation of this skull contribute to an improved understanding of the cranial ontogeny, morphology, and individual variation in TRICERATOPS: Total skull length is 120 cm long (est.). UCMP 136306 is one of the most complete Triceratops skulls of this ontogenetic stage yet known. The cranial sutures are patent, and most are overlapping with minimal sinuosity, modest interdigitation, and overlapping flat sutural surfaces. The following cranial elements are preserved and described in this study: epinasal, rostral, quadrate, quadratojugal, jugal, pterygoid, dentary, surangular, postorbital horn, parietal, squamosal, epiparietal, episquamosal, occipital condyle, supraoccipital, and exoccipital. For decades following the initial description of Triceratops by O.C. Marsh in 1889, the typical collector attitude was "bigger is better." Emerging scientific institutions and museums with newly constructed exhibit halls demanded the biggest and newest dinosaurs. We hypothesize that this historical practice, influenced by facies and taphonomic factors in the Upper Cretaceous Hell Creek Formation, Montana (and contemporaneous formations in neighboring states), resulted in the underrepresentation of nonadult Triceratops in museum collections. This practice contributed to the false notion that nonadult Triceratops specimens are rarely preserved in the fossil record, until now.