| Liangtoutang Formation | |
|---|---|
|  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 | ||||||
|---|---|---|---|---|---|---|
| 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 | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images | 
| Yueosaurus [3] | Y. tiantaiensis | "Partial postcranial skeleton" | A thescelosaurine thescelosaurid | |||
| Eggs of the Liangtoutang Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images | 
| Macroelongatoolithus | M. xixiaensis | |||||
| Pachycorioolithus | P. jinyunensis | |||||
| Testudoolithus | T. jiangi | |||||