These
footprints were found in late Triassic / Early Jurassic Period sediments
from about 200 million years ago. At that time, the supercontinent of Pangea
was rifting apart and the Atlantic Ocean was beginning to form. Mudflats
along the western shore of this new seaway provided the perfect environment
for the preservation of the footprints of dinosaurs that passed along the
beaches.
Trace fossils such as tracks, or footprints are given different
scientific names from the animals that made them, because it is difficult or
impossible to be sure which animal made which track. However, structure of
the foot and shape of the footprint can allow some educated guesses. Some
scientists have suggested that Eubrontes is the footprint of
Dilophosaurus, and Grallator is the track of a small theropod
dinosaur like Coelophysis . These tracks exhibit three toes, like
those of birds, and were originally thought to have been bird tracks.
The study of trace fossils is the field of ichnology, Fossil footprints
tell us much about the shape, size, stance, and speed of otherwise
unknown prehistoric animals. In addition to offering clues about the
behavior of individual animals, trace fossils can provide insights into
group behavior.