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Chinle Formation (Late Triassic)
It was one of the last in a line of mammoth species
This is a very fine unidentified leaf from the Parachute Creek beds
It was known for over half of the 20th century as Antrodemus
This formation is interpreted as a semi-arid environment with distinct wet and dry seasons
Oligocene Oreodont Merycoidodon VF-WR-17-002 Lobster Chinle Formation (Late Triassic)Merycoidodon sp. Brule Formation Middle Oligocene Niobrara County, Wyoming This is an excellent example of a Merycoidodon maxilla from the Middle Oligocene Brule Formation. This example is from the right side of the skull and contains 3 molars and one premolar. The specimen is from a young adult as indicated by the minimal ware seen on the typical selenodont teeth. The maxilla section is about 8 cm long. More fossils from the White River Group can be
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