Abstract

The fossil record of centrosaurine ceratopsids is largely restricted to the northern region of western North America (Alberta, Montana and Alaska). Exceptions consist of single taxa from Utah (Diabloceratops) and China (Sinoceratops), plus otherwise fragmentary remains from the southern Western Interior of North America. Here, we describe a remarkable new taxon, Nasutoceratops titusi n. gen. et sp., from the late Campanian Kaiparowits Formation of Utah, represented by multiple specimens, including a nearly complete skull and partial postcranial skeleton. Autapomorphies include an enlarged narial region, pneumatic nasal ornamentation, abbreviated snout and elongate, rostrolaterally directed supraorbital horncores. The subrectangular parietosquamosal frill is relatively unadorned and broadest in the mid-region. A phylogenetic analysis indicates that Nasutoceratops is the sister taxon to Avaceratops, and that a previously unknown subclade of centrosaurines branched off early in the group's history and persisted for several million years during the late Campanian. As the first well-represented southern centrosaurine comparable in age to the bulk of northern forms, Nasutoceratops provides strong support for the provincialism hypothesis, which posits that Laramidia—the western landmass formed by inundation of the central region of North America by the Western Interior Seaway—hosted at least two coeval dinosaur communities for over a million years of late Campanian time.

Highlights

  • During the Late Cretaceous, elevated global sea levels subdivided North America into eastern and western landmasses—Appalachia and Laramidia, respectively— for about 27 million years

  • The lack of centrosaurine remains discovered in the American southwest prompted some investigators to postulate their existence only in the northern region of the p1 pf p0 p ff nh f nh ins np nh n p1

  • Nasutoceratops can be confidently placed within Centrosaurinae on the basis of a suite of synapomorphies, including: premaxilla with pronounced ventral angle; subcircular narial region; presence of narial spine composed of nasal and premaxilla and rostrocaudally abbreviated squamosal with stepped caudomedian margin

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Summary

Introduction

During the Late Cretaceous, elevated global sea levels subdivided North America into eastern and western landmasses—Appalachia and Laramidia, respectively— for about 27 million years (approx. 95–68 Myr ago). Within Ceratopsidae, centrosaurines are known overwhelmingly from the northern region of Laramidia, with 15 of 17 named species recovered from Alberta, Montana and Alaska. License http://creativecommons.org/licenses/by/3.0/, which permits unrestricted use, provided the original author and source are credited. Unknown dinosaur assemblage from the late Campanian Kaiparowits Formation [1]. We report the discovery of a remarkable new long-horned centrosaurine from the Kaiparowits Formation, to our knowledge the first late Campanian member of this clade described from southern Laramidia. This taxon sheds light on the evolution of Centrosaurinae and offers key insights into Laramidian dinosaur provincialism

Systematic palaeontology
Description
Discussion
Findings
11. Sampson SD et al 2010 Grand Staircase-Escalante
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