Liangtoutang Formation | |
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Stratigraphic range: Albian-Cenomanian ~ | |
Type | Geological formation |
Unit of | Tiantai Group |
Underlies | Chichengshan Formation |
Overlies | Tangshang Formation |
Thickness | About 300 m (980 ft) |
Lithology | |
Primary | Sandstone |
Location | |
Coordinates | 28°42′N120°12′E / 28.7°N 120.2°E |
Approximate paleocoordinates | 36°18′N120°00′E / 36.3°N 120.0°E |
Region | Zhejiang |
Country | China |
Extent | Huzhen Basin |
The Liangtoutang Formation, also referred to as the Laijia Formation is a geological formation located in Zhejiang, China. Its strata date back to the Albian to Cenomanian stages of the Cretaceous period, between 105.9 and 96 million years ago. [1] The lithology primarily consists of red sandstone.
Color key
| Notes Uncertain or tentative taxa are in small text; |
Ankylosaurs of the Liangtoutang Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Jinyunpelta [2] | J. sinensis | "An almost complete skull" and two partial postcranial skeletons | A ankylosaurine ankylosaurind | |||
Ornithopods of the Liangtoutang Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Yueosaurus [3] | Y. tiantaiensis | "Partial postcranial skeleton" | A thescelosaurine thescelosaurid | |||
Eggs of the Liangtoutang Formation | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Macroelongatoolithus | M. xixiaensis | |||||
Pachycorioolithus | P. jinyunensis | |||||
Testudoolithus | T. jiangi | |||||