Edmontosaurus

MEANING: Edmonton lizard

PERIOD: Late Cretaceous

CONTINENT: North America

Edmontosaurus was among the largest hadrosaurs, reaching up to 12 m in length, with an estimated mass of around 6 t. It was a bulky animal with a long, laterally flattened tail and a head with an expanded, duck-like beak. The fore legs were not as heavily built as the hind legs, but were long enough to be used in standing or movement.

Edmontosaurus is from the Late Cretaceous. The Cretaceous is the third and final geological period of the Mesozoic Era, with the Late Cretaceous making up roughly the second half of it, lasting from about 100 to 66 million years ago. It was a time of significant evolutionary change, with dinosaurs reaching their greatest diversity before the mass extinction at the end of the Cretaceous.

The Cretaceous was a period with a relatively warm climate, though the Late Cretaceous experienced a global cooling trend, caused by falling levels of carbon dioxide in the atmosphere. The continents were nearing their present positions, but high sea levels flooded low-lying regions, turning Europe into an archipelago, and forming the Western Interior Seaway in North America. These seas were home to a variety of marine reptiles, including mosasaurs and plesiosaurs, while pterosaurs and birds shared the skies.

On land, dinosaurs continued to thrive and diversify during the Late Cretaceous, producing many of the most well-known goups, including tyrannosaurs, hadrosaurs, and pachycephalosaurs. Established Cretaceous dinosaur clades like the ceratopsians, ankylosaurs, and dromaeosaurs continued to flourish. Sauropod species consisted almost exclusively of titanosaurs, which seemed to be confined to the Southern Hemisphere for much of the Late Cretaceous. Flowering plants and grasses diversified and spread, becoming the dominant flora similar to what we see today.

The Cretaceous (along with the Mesozoic) ended with the Cretaceous–Paleogene (K–Pg) extinction event, a large mass extinction in which many groups, including non-avian dinosaurs, pterosaurs, and large marine reptiles, died out. This event, likely triggered by an asteroid impact, is marked by the abrupt K–Pg boundary, a distinct geologic layer separating the Mesozoic and Cenozoic Eras. In its aftermath, mammals and avian dinosaurs rapidly diversified, becoming the dominant land animals of the Cenozoic Era.

Edmontosaurus is a hadrosaur. Hadrosaurs, casually known as duck-billed dinosaurs, are ornithischian dinosaurs that were common in the Late Cretaceous period. Hadrosaurs were among the most dominant herbivores in Asia and North America, and toward the end of the Cretaceous several lineages dispersed into Europe, Africa, and South America.

Hadrosaurs are known for the flat duck-bill appearance of their snouts. They also had teeth in the back of their mouths that were stacked into complex structures known as dental batteries. Some derived species had large impressive crests on their heads, likely used for sexual display and communication. They were facultative bipeds, meaning they could choose to locomote using only their hind legs, or on all fours, depending on the activity and speed with which they needed to move. The young of some species walked mostly on two legs, and the adults on four.