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From Wikipedia, the free encyclopedia
The Ejinhoro Formation (simplified Chinese: 伊金霍洛组; traditional Chinese: 伊金霍洛組; pinyin: Yījīnhuòluò Zǔ) is a geological formation in Inner Mongolia, north China, whose strata date back to the Early Cretaceous period (Aptian/Albian age.[1]
Ejinhoro Formation | |
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Stratigraphic range: Aptian-Albian | |
Type | Geological formation |
Lithology | |
Primary | Sandstone |
Other | Mudstone, siltstone |
Location | |
Coordinates | 39.4°N 108.4°E |
Approximate paleocoordinates | 40.5°N 105.5°E |
Region | Inner Mongolia |
Country | China |
Extent | Ordos Basin |
Dinosaur remains are among the fossils that have been recovered from the formation.[2]
Dinosaurs | ||||
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Taxa | Presence | Notes | Images | |
Genus:
|
Isolated teeth. |
A sauropod. |
||
|
A ceratopsian. | |||
|
A large saurischian. | |||
|
"Near-complete articulated skeleton."[5] |
A troodontid. | ||
|
Isolated teeth. |
A stegosaurid. | ||
|
A large stegosaurid. "Partial skeleton, plate, vertebra, adult."[6] | |||
Indeterminate pterosaur remains have also been recovered from the formation.[7]