LATE
CRETACEOUS
HELL CREEK FORMATION.
The Hell Creek formation of Montana and the Dakotas
represents the only well studied terminal Late Cretaceous fauna. It
contains a varied group of theropods, ornithipods, pachycephalosaurs,
ankylosaurs and ceratopsids. The flowering plants dominate the flora;
conifers are locally common with ferns and their allies primarily in a
herbaceous role. The last of the dinosaurs are found here. Also the
most famous dinosaurs Tyrannosaurus and Triceratops are from here. It has been the popular vision of
dinosaurs and how they lived. The number of species compared to early
periods appears to decline. This could be a sign of environmental stress
conversely it could also be a sign that the regression of the inland seas
allowed for a larger more uniform territory favoring less speciation. No
fossil site of the same age have been found so we have no idea if the is
representative of dinosaur populations elsewhere. At the end of the period
a massive meteor or comet stuck the Yucatan. No undisbuted dinosaurs have been found
after that event. It marks the end of the age of the dinosaurs.
mouse over diorama pics for figure information.
Recent discoveries have given us more information about Tyrannosaurus (
Tyrant Lizard), Albertosaurus and Daspletosaurus have become rare but Tyrannosaurus seems to have been relatively common.. They even may have formed family
groups with a mated pair and offspring of various ages.
Flowering plants were the most diverse plants of the day, although ferns and conifers may still have been more common in terms of numbers.
The terminal Late Cretaceous fauna seems to have a lower diversity
of dinosaur species than the preceding period. The total number of species
is lower and the ecosystems seem to be dominated by just one or two of the
remaining species. Edmontosaurus and Triceratops are the most common
dinosaurs; others are uncommon or rare. Edmontosaurus is
very similar looking and closely related to Anatotitan, Anatosaurus in North America as well as Shantungosaurus in China.
Ankylosaurs are common in
the Scollard formation of Alberta that overlaps in time with the Hell Creek
formation. Its close relative Ankylosaurus in the fossil record succeeds Euoplocephalus. While earlier pachycephalosaurs were small to medium size
animals, Pachycephalosaurus was the giant of the family at 15 feet long. Known
mostly from skulls, it has been speculated these washed down from the dry
interior of the continent.
Previous Late Cretaceous next tyrannosaurs