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Morrosaurus

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Morrosaurus

Morrosaurus (MOR-roh-SAWR-us; “Lizard from El Morro”) is a genus of ornithopod dinosaur that lived during the Late Cretaceous period, approximately 71 to 66 million years ago. Its fossils were discovered on James Ross Island in Antarctica. The name refers to “El Morro,” a distinctive rock formation near where the dinosaur’s remains were found. Morrosaurus was first described by paleontologists in 2016 based on a partial hindlimb.

Description and Classification

Morrosaurus was a relatively small to medium-sized herbivorous dinosaur. Based on its leg bones, scientists believe it was a slender and agile animal, likely capable of running quickly to escape predators. The known fossils include parts of its femur (thigh bone), tibia and fibula (lower leg bones), and foot bones. These bones show features that help classify Morrosaurus within the larger group of plant-eating dinosaurs called Ornithopoda.

Specifically, Morrosaurus is considered a basal (an early or more primitive type) member of a group called Iguanodontia. It belongs to a particular family of Southern Hemisphere ornithopods known as Elasmaria. This group includes other small to medium-sized, two-legged plant-eaters found in South America and Antarctica, such as Trinisaura and Talenkauen. These dinosaurs shared common ancestors and lived on the ancient supercontinent of Gondwana.

Distinguishing Features

Morrosaurus had some unique features, mostly found in its leg and foot bones, that help scientists tell it apart from other dinosaurs:

  • Its leg bones were long and slender, indicating it was built for speed.
  • The fourth trochanter, a prominent bump on its thigh bone where powerful leg muscles attached, had a distinct, somewhat rectangular shape and pointed forward.
  • The parts of its thigh bone that formed the knee joint (called condyles) had specific shapes.
  • One of the bones in its outer foot (the fifth metatarsal) was much smaller and more reduced than in most other related ornithopod dinosaurs.

Paleoenvironment and Diet

Morrosaurus lived in Antarctica during the very end of the dinosaur age, in what is known as the Late Maastrichtian epoch. At that time, Antarctica was located near the South Pole, but it was not covered in thick ice sheets like it is today. The climate was much warmer than modern Antarctica, though it would have experienced cool temperatures and long periods of winter darkness followed by summer daylight. The environment was likely a mix of coastal plains and forests, with plants like conifers, ferns, and an increasing number of early flowering plants.

As an ornithopod, Morrosaurus was a herbivore, meaning it ate plants. Although teeth from Morrosaurus itself have not been found, related dinosaurs had teeth suited for grinding up tough plant material. It likely fed on low-growing vegetation available in its polar habitat, such as ferns, cycads, and small shrubs.

Significance and Ongoing Research

The discovery of Morrosaurus is important because it adds to our knowledge of dinosaur life in Antarctica, a continent from which relatively few dinosaur fossils have been recovered. It shows that even in polar regions, diverse dinosaur communities existed. Morrosaurus and its relatives in the Elasmaria group, like Macrogryphosaurus and Anabisetia, demonstrate that these types of ornithopods were widespread in the southern parts of Gondwana.

Ongoing research continues to explore the fossils of Morrosaurus to better understand its anatomy, how it moved, and its exact relationship to other ornithopods. Scientists are also keen to find more fossils in Antarctica. Each new discovery helps paint a clearer picture of the unique ecosystems that existed at the Earth’s poles during the Mesozoic Era and how these animals adapted to high-latitude environments with their seasonal extremes of light and temperature.



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