DVL-0001Specimen Record
Illustration of Acrocanthosaurus atokensis

Acrocanthosaurus

Acrocanthosaurus atokensis

AK-roh-KAN-thoh-SOR-us at-oh-KEN-sis

This sail-backed predator was North America's apex hunter before T. rex existed, sporting distinctive high spines along its back that may have supported a muscular ridge.

Did you know?

The famous Glen Rose trackways in Texas may show an Acrocanthosaurus stalking a sauropod—one of the only potential 'hunt scenes' preserved in the fossil record

About

Acrocanthosaurus was one of the largest and most fearsome predators to ever stalk North America. This massive roamed the continent during the Early Cretaceous, roughly 113 to 110 million years ago, making it the dominant land predator of its time—tens of millions of years before Tyrannosaurus rex would evolve. Its name, meaning "high-spined lizard," refers to the tall along its that likely supported a thick muscular ridge or low sail running from neck to tail.

As a member of the family—the "shark-toothed lizards"—Acrocanthosaurus possessed blade-like teeth designed for slicing through flesh rather than crushing bone. Its skull alone measured over four feet long, and its relatively large arms ending in three-fingered hands with massive claws made it a more versatile hunter than later tyrannosaurs. Evidence suggests it may have hunted the giant sauropods like Sauroposeidon that shared its environment.

The first Acrocanthosaurus remains were discovered in Atoka County, Oklahoma in the 1940s by J. Willis Stovall and Wann Langston Jr., who formally described and named the species in 1950. The most complete specimen, nicknamed "Fran," was discovered in Texas in 1990 and is now displayed at the North Carolina Museum of Natural Sciences. evidence from the famous Glen Rose Formation in Texas may preserve an Acrocanthosaurus pursuing a , offering a rare glimpse into predator-prey dynamics.

Remarkably, Acrocanthosaurus achieved a continent-wide distribution, with fossils found from Wyoming and Oklahoma in the west to Maryland in the east—suggesting this was highly adaptable and successful across diverse Early Cretaceous ecosystems.

First described1950
Discovered byJ. Willis Stovall and Wann Langston Jr.
Type specimenOMNH 10146