From Handwiki - Reading time: 2 min| Meng-Yin Formation Stratigraphic range: Berriasian-Valanginian ~145–133 Ma | |
|---|---|
| Type | Geological formation |
| Lithology | |
| Primary | Sandstone |
| Other | Siltstone |
| Location | |
| Coordinates | [ ⚑ ] : 35°54′N 118°00′E / 35.9°N 118.0°E |
| Paleocoordinates | [ ⚑ ] 36°54′N 120°12′E / 36.9°N 120.2°E |
| Region | Shandong |
| Country | |
The Meng-Yin or Mengyin Formation (simplified Chinese: 蒙阴组; traditional Chinese: 蒙陰組; pinyin: Méngyīn Zǔ) is a geological formation in Shandong, China, whose strata date back to the Berriasian and Valanginian stages of the Early Cretaceous.[1][2]
Dinosaur remains are among the fossils that have been recovered from the formation.[3] The type material for the titanosauriform dinosaur Euhelopus was excavated at this formation by Otto Zdansky in 1923, in green/yellow sandstone and green/yellow siltstone that were deposited during the Barremian or Aptian stages of the Cretaceous period, approximately 129 to 113 million years ago.[4]
Both the genus and species of Mengyinaia mengyinensis were named after the formation.
Indeterminate stegosaurid remains have been found in Shandong, China.[3]
| Vertebrates from the Meng-Yin Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Euhelopus[3] | E. zdanskyi[3] | Shandong[3] | "Skull and partial postcranial skeleton, additional fragmentary skeleton."[5] | |||
| Mengshanosaurus | M. minimus | A choristodere belonging to Neochoristodera | ||||