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Home » Fossils » Green River Formation Fossilss » Green River Fossil Bat, Crayfish, Turtles

Green River Fossils: Bats, Crayfish, Horse, Turtles


Introduction



The Green River Formation has yielded some of the best-preserved and oldest fossil bats ever found. It has also produced a variety of other unusual fossils such as the turtles, crayfish and horses. The photos shown below are by the National Park Service - Fossil Butte National Monument.

More Fossils!     Plants,   Animals,   Insects,   Fish

Green River fossil turtle
This 1.7 meter (5 foot 6 inch) softshell turtle is one of the largest turtles from Fossil Lake. During the Eocene, trionychid turtles reached maximum size. Today, North America's largest softshell turtles reach 51 cm (20 inches) in length. National Park Service photo.


Green River fossil turtle
This ten-inch-long turtle belongs to the Baenidae family, an extinct North American group. Shell characteristics, a very long tail and recurved claws suggest they were strong bottom walking turtles. National Park Service photo.


Green River fossil horse
Most mammal fossils consist of teeth and bone fragments. This fully-articulated early horse is an extremely rare find and to date, the only horse found in the Green River Formation. National Park Service photo.


Green River fossil stingray
Heliobatus radians had small teeth for crushing snails and other mollusks and barbed spines on the tail for defense. National Park Service photo.



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Green River fossil bat
This 5.5 inch long bat is the most primitive bat known. Claws on each finger of its wings indicate it was probably an agile climber and crawled along and under tree branches searching for insects. National Park Service photo.




Turritella
"Turritella Agate" is the name given to a brownish gem material that contains spectacular fossil snail shells entoumbed in a semitransparent agate. It is possibly the best-known fossil from the Green River Formation. When the Green River was being deposited, the spiral-shaped shells accumulated in the sediments of the shallow inland sea. A few lenses of this snail-bearing sediment were then agatized by the deposition of fine-grained silica (chalcedony - also known as agate) into the cavities of the shells and the voids between then. If the sediment was completely agatized it has potential lapidary (gem cutting) potential.

Although millions of people have called this material "Turritella" for several decades the name is actually incorrect. Somehow it acquired the Turritella name after a genus of fossil snails that are very similar to the shells in the agate. The proper name of the snails is "Elimia tenera" a member of the Pleuroteridae family. Perhaps a better name would be "Elimia Agate" which is not quite as elegant.

To learn more about the Turritella - Elimia naming error visit the Museum of the Earth website, which is authored by the Paleontological Research Institution - people who know what they are talking about when it comes to fossils.


Green River fossil crayfish
Crayfish lived in the shallow, near-shore water of Fossil Lake. Procambarus is known only from the Eocene deposits of Fossil Lake. Its closest living relative, Austrocambarus, is found in Mexico. National Park Service photo.


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