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A row of small osteoderms (skin bones) was present down the middle of the neck
hollandite
Although found in the Green River Formation it eventually became extinct in North America
The pollen of Pterocarya is also relatively abundant in samples from the lower Parachute Creek Member and thus seems to be a somewhat common element of the lower ground forests of the Green River Eocene deposits
5 cm x 1 cm at the base of the tooth on the lingual side
Eocene Green River Unidentified Leaf P-PCM-16-007 Beetle A row of small osteodermsUnidentified Leaf Green River Formation Parachute Creek Member Middle Eocene Uintah County, Utah This is a very fine unidentified leaf from the Parachute Creek beds. It has pinnate veins and a smooth margin. The upper part of the Green River Formation in the eastern Uinta Basin is present in two stratigraphic intervals separated by approximately 250 m of sandstone, siltstone, marlstone and lacustrine limestone (micrite, boundstone, grainstone). The
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