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Coahuilaceratops





Coahuilaceratops: Profile of a Prehistoric Giant


Coahuilaceratops

Coahuilaceratops (koh-ah-WEE-lah-SEH-rah-tops; “Coahuila horned face”) is a genus of chasmosaurine ceratopsid dinosaur that lived during the Late Cretaceous period, about 72.5 million years ago, in what is now Coahuila, Mexico. The name refers to the Mexican state where its fossils were discovered and its horned appearance (ceratops means “horned face”). Coahuilaceratops was first described in 2010 based on partial skeletal remains, including parts of the skull and bones from the body.

Description and Classification

Coahuilaceratops belonged to the Ceratopsidae family, a group of large, four-legged, plant-eating dinosaurs famous for their prominent horns and bony neck frills. Within this family, it is classified as a member of the Chasmosaurinae subfamily. Chasmosaurines, such as the well-known Triceratops and Chasmosaurus, typically had long frills and well-developed brow horns. Coahuilaceratops is estimated to have been about 6.7 meters (22 feet) long and may have weighed between 4 to 5 metric tons (approximately 9,000 to 11,000 pounds). It was a solidly built herbivore, designed for processing tough vegetation.

The first fossils of Coahuilaceratops were found in the late 1980s, with more material discovered in the early 2000s. These fossils were recovered from the Cerro del Pueblo Formation in Coahuila. The only known species, Coahuilaceratops magnacuerna, was scientifically named and described in 2010. The species name “magnacuerna” translates from Latin and Spanish to “great horn,” highlighting its most impressive feature.

Distinguishing Features

Coahuilaceratops possessed several notable features that help distinguish it from other ceratopsian dinosaurs:

  • Enormous Brow Horns: Its most striking characteristic was its exceptionally large brow horns located above its eyes. These are estimated to be among the largest brow horns of any known dinosaur, possibly exceeding 1.2 meters (4 feet) in length. The horns were robust and curved forward and slightly downward.
  • Relatively Short, Broad Frill: Compared to some other chasmosaurines, Coahuilaceratops had a neck frill that was relatively short from front to back but quite wide. This frill likely served purposes such as display for attracting mates or intimidating rivals, species recognition, or as an attachment point for strong jaw muscles.
  • Small Nasal Horn: It had a small, low, bump-like horn on its nose, which was much less prominent than its large brow horns.
  • Unique Frill Structure: The shape and arrangement of the bones and openings (fenestrae) in its frill were unique, contributing to its distinct appearance among chasmosaurine dinosaurs.

Paleoenvironment and Diet

Coahuilaceratops lived in what is now northern Mexico during the late Campanian stage of the Late Cretaceous period. Its fossils were discovered in the Cerro del Pueblo Formation, which preserves evidence of an ancient coastal plain or delta environment. This area was located near the southern end of the Western Interior Seaway, a large inland sea that divided North America at the time. The climate was warm and humid, supporting lush vegetation. This ecosystem was home to a variety of other dinosaurs, including duck-billed hadrosaurs and predatory tyrannosaurids.

As a ceratopsian dinosaur, Coahuilaceratops was an herbivore. It used its sharp, powerful beak to snip off tough plant matter, such as ferns, cycads, and early flowering plants. Further back in its jaws, Coahuilaceratops had dental batteries – many tightly packed teeth that were constantly replaced – which formed a grinding surface to shred the vegetation before swallowing.

Significance and Ongoing Research

The discovery of Coahuilaceratops is very important because it was the first chasmosaurine ceratopsid dinosaur to be formally named from Mexico. This finding extended the known geographic range of this group of dinosaurs much further south than previously recorded. It provides valuable information about the diversity of dinosaurs on Laramidia, the western landmass of North America during the Late Cretaceous, especially in its southern regions. The incredibly large brow horns of Coahuilaceratops also contribute to our understanding of the different forms and possible functions of these structures in horned dinosaurs; they might have been used for defense against predators, for display, or in contests between individuals.

Current research on Coahuilaceratops involves searching for more complete fossil specimens. More fossils would help paleontologists create a more detailed picture of its anatomy, how it grew, and its behavior. Scientists are also studying its evolutionary relationships with other ceratopsids, like Pentaceratops and Anchiceratops, to better understand how this diverse group of dinosaurs evolved. Further studies of the Cerro del Pueblo Formation continue to help reconstruct the ancient ecosystem where Coahuilaceratops thrived and how it interacted with other species.


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