"Scenic view from atop Twin Rock" by U.S. National Park Service , public domain
Florissant Fossil BedsFossil Vertebrates |
featured in
National Parks Pocket Maps | ||
Colorado Pocket Maps |
Florissant Fossil Beds
Fossil Vertebrates
Giant redwood trees and buzzing insects called Florissant home, but they were not the only inhabitants.
Florissant was also home to tiny horses and vibrant birds, as well as other vertebrates. Vertebrates include
mammals, reptiles, birds, fish and amphibians. Vertebrate fossils are rare at Florissant due to the
environment they lived in and the difficulty in preserving their bodies, as they needed to be transported to
the water for preservation.
How do vertebrates fossilize?
There are a few ways that vertebrates can fossilize. Bones and teeth are usually the only parts that preserve since they are hard
and durable. Although rarer, sometimes feather and scale impressions can be preserved. Generally the harder the body part, the
greater likelihood of it being fossilized. There are a few modes of fossilization at Florissant like impressions or carbonization. It is
also possible to have several forms of fossilization in one fossil.
Carbonization forms the
thin, black films of carbon of
a fossil. This occurs when an
organism’s body is
compressed and decays all
the organic compounds
except for carbon. This
bird’s feathers were
carbonized after it drowned
and then was rapidly buried.
The thin layer of carbon still
show the fine details of the
feathers when they were
compressed.
1 cm
1 cm
Impressions form when the hard
parts of an animal are imprinted in
soft sediment, like mud, after
burial. The hard part, which later
decays away, then creates a mold.
Impressions include scales, bones
and feathers. This unidentified fish
had its ribs pressed into the mud
before becoming a rock, after
which the bones were destroyed.
Permineralization occurs
when a buried bone is
penetrated by groundwater
with dissolved minerals
through the bone’s pores.
Dissolved minerals can be
calcite, iron or silica. Over
time, the dissolved water
will deposit small crystals of
the dissolved minerals into
the tiny pores. The
permineralized bone shards
below still have visible
pores inside the bone.
1 cm
UCM-73039
What vertebrates existed in Eocene Florissant?
USNM-11955
Mouse Opossum (genus Nanodelphys)
These marsupials were once plentiful in North America but later became extirpated
here after having migrated to the southern hemisphere, where they diversified. They
typically measured 4 to 5 inches (10-13 cm) from head to tail and their diet consisted
of insects and small fruits. It is likely they spent most of their time in the trees to
avoid predators using their prehensile tail to aid in climbing.
1 cm
Suckers (genus Amyzon)
Suckers were 3 to 5 in (7-13cm) freshwater fish that lived at the bottom of the lake.
Amyzon suckers were a common fish, with three specimens collected from Florissant’s
deposits. They would have been omnivorous, feeding on the both plants and aquatic
organisms. While the genus Amyzon died out at the end of the Paleogene (23mya), the
family Catostomidae continues to this day in North America.
UCM-38711
1 cm
Brontotheres (genus Megacerops)
The largest of the animals to walk through Lake Florissant’s forests were brontotheres.
These giants were 8 feet (2.4m) tall and weighing as much as two tons(1.8 tonnes).
They sported a huge bifurcated horn above their nose for protection against predators
and by males to settle rivalries. They are most closely related to rhinos, but filled an
ecological role similar to modern day elephants. Unable to cope with the changing
climate, brontotheres went extinct at the end of the Eocene.
Primitive Horses (genus Mesohippus)
Considered to be transitional from the small ancestral horses to today’s large
modern horses, Mesohippus evolved greater speed with longer legs and three toes.
These primitive horses were only 3 feet (90cm) tall, which aided their ability to hide
from predators. Based on the structure of their teeth, Mesohippus were browsers (fed
on shrubs and trees), not grazers (grass eaters) like modern horses.
1 dm
UCM-65951
1 cm
Rail (family Rallidae)
Rails were slender birds with compact bodies that measured about a foot from head to
toe. Their long legs allowed them to wade through shallow water in search of food.
They fed on aquatic insects and crustaceans by using their long beaks to dig prey out.
Rails are still around today, inhabiting all continents except Antarctica, though they are
elusive and hard to find.
Are there more vertebrates?
Today, the monument has identified over 30 vertebrates. The collections contain other birds including a cuckoo and a roller. A
few years ago, a snake vertebra was found, which is the first reptile found at Florissant. The fish are the most abundant fossils in
the Florissant fossil record. This is because fish lived and died in the water whereas other animals’ carcasses would have to be
transported to the lake to be preserved. As excavations continue to take place, more bones, teeth and other hard parts may be
uncovered to reveal more animals that lived in the Florissant ecosystem.
Specimen photos labeled UCM for University of Colorado, or USNM for National Museum of Natural History are
the locations were they are housed in. Unlabeled ones are stored in the monument’s collections.