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Geological formation in Yunnan, China From Wikipedia, the free encyclopedia
The Fengjiahe Formation is a geological formation in China. It dates back to the Early Jurassic, most likely to the Pliensbachian.[1] The formation is up to 1500 metres thick and consists of "purple-red mudstone and argillaceous siltstone interbedded with gray-green and yellow-green quartz sandstone and feldspathic quartz sandstone"[2]
Fengjiahe Formation | |
---|---|
Stratigraphic range: | |
Type | Geological formation |
Underlies | Zhanghe Formation |
Overlies | Shezi Formation |
Thickness | Up to 1,500 m (4,900 ft) |
Lithology | |
Primary | Mudstone, siltstone |
Other | Sandstone |
Location | |
Coordinates | 24.7°N 101.6°E |
Approximate paleocoordinates | 32.7°N 99.8°E |
Region | Yunnan |
Country | China |
Extent | Yimen Basin |
Theropod tracks geographically present in Yunnan, China.[3]
Vertebrates | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Shuangbaisaurus | S. anlongbaoensis | Shuangbai County | Lower part of formation | Partial skull with lower jaw | A crested basal theropod, probably a junior synonym of Sinosaurus | |
Chinshakiangosaurus[3] | C. chunghoensis[3] | Geographically present in Yunnan, China.[3] | A basal sauropod | |||
Irisosaurus[4][5] | I. yimenensis | A sauropodiform sauropomorph | ||||
Lufengosaurus[2] | L. huenei | A massospondylid sauropodomorph | ||||
Y. youngi[3] |
"[Ten] partial skeletons, skull, adult."[6] |
A plateosaurid sauropodomorph | ||||
Yunnanosaurus[1] | Y. youngi | A sauropodiform sauropodomorph | ||||
Yuxisaurus[7] | Y. kopchicki | Yuxi Prefecture, Yunnan, China | Upper | Partial skeleton including a partial skull, cervical and dorsal vertebrae, scapulae, right humerus, left femur, and osteoderms | A basal thyreophoran | |
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