Nasutoceratops is a genus of ceratopsid dinosaur that lived in North America during the Late Cretaceous period, about 76.0–75.5 million years ago. The first known specimens were discovered in Utah in the Kaiparowits Formation of the Grand Staircase–Escalante National Monument (GSENM) from 2006 onwards, including a subadult skull with both a partial postcranial skeleton and rare skin impressions, and two other partial skulls. In 2013, the subadult was made the holotype of the new genus and species Nasutoceratops titusi; the generic name means "large-nosed horned face", and the specific name honors the paleontologist Alan L. Titus for his work at the GSENM. The dinosaur was noted for its large nose in news reports, and later featured in Jurassic World films. The holotype skull of Nasutoceratops is approximately 1.5 m (4.9 ft) long; its body length has been estimated at 4.5 m (14.8 ft), and its weight at 1.5 t (1.7 short tons). Nasutoceratops is distinct in features such as the snout region being unusually deep but short from front to back, with the external nostril forming 75% of the skull length in front of the eye sockets. The nasal bones were possibly pneumatized (air-filled), which is unknown in other ceratopsids. Its nasal horn is low and blade-like while the brow horns point forward and are approximately 40% of the total skull length; they are up to 457 mm (18.0 in), the longest known of any centrosaurine, and have been likened to those of a Texas Longhorn bull. The neck frill is almost circular with its widest point at the middle. The epiossifications on the margins of the frill are shaped like low crescents, and there is one at the midline at the top of the frill, unlike in other centrosaurines. Nasutoceratops was a basal (early diverging) member of Centrosaurinae, and may have formed a distinct clade within this group, Nasutoceratopsini, with its closest relatives. The function of the deep front of the skull of Nasutoceratops is unknown, but may have been related to mastication. The functions of ceratopsian frills and horns have been debated, and include signalling, combat, and species recognition. The forward oriented brow horns of Nasutoceratops may have enabled interlocking with opponents, as in modern bovids. The Kaiparowits Formation dates to the late Campanian age and was deposited on Laramidia, an island continent, when North America was divided at the center by the Western Interior Seaway. This environment was dominated by wetlands and supported a diverse fauna, including other ceratopsians. Based in part on the relationship between Nasutoceratops and other centrosaurines from around the same time, it has been proposed that Laramidia was divided into dinosaur "provinces" with separate endemic species, but this has been contested.
Discovery and naming
Since 2000, the Natural History Museum of Utah (UMNH) and the Bureau of Land Management have been conducting paleontological surveys of the Kaiparowits Formation at the Grand Staircase–Escalante National Monument (GSENM) in southern Utah. This national monument was established in 1996 in part for the preservation and study of its fossils, and the surveys there have yielded a wide array of unique dinosaur fossils. Field crews from other institutions have also participated, and the collaborative effort is known as the Kaiparowits Basin Project. Among the discoveries that have been made are three new ceratopsian (horned dinosaur) taxa, one of which was identified from UMNH Locality VP 940 discovered by the then graduate student and technician Eric K. Lund during the 2006 field season. Prior to this project, the only ceratopsian remains found in the formation were uninformative, isolated teeth, and centrosaurines were known almost exclusively from the northern part of western North America. Excavated fossils of the new ceratopsian were transported to the UMNH, where the blocks were prepared by volunteers with pneumatic air scribes and needles and subsequently reassembled; it took a few years for the team to assemble the skull of this dinosaur. It was preliminarily referred to as "Kaiparowits new taxon C" and identified as a centrosaurine (the first member of this ceratopsid group known from the formation) in 2010, and as "Kaiparowits centrosaurine A" in 2013. Three specimens of this dinosaur were collected; UMNH VP 16800 in 2006, and UMNH VP 19469 and UMNH VP 19466 in subsequent years. The paleontologists Scott D. Sampson, Lund, Mark A. Loewen, Andrew A. Farke, and Katherine E. Clayton briefly described and scientifically named the new genus and species Nasutoceratops titusi in 2013, with specimen UMNH VP 16800 as the holotype (on which the scientific name is based). The generic name is derived from the Latin word nasutus meaning "large-nosed", and ceratops, which means "horned face" in Latinized Greek. The specific name titusi is an eponym that honors the paleontologist Alan L. Titus for his important efforts in recovering fossils from the GSENM. Lund had informally used the spelling Nasutuceratops for this dinosaur in his 2010 thesis wherein he also described it. In 2016, Lund, Sampson, and Loewen published a more detailed description of the preserved fossil material.
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