Penglaizhen Formation
| Penglaizhen Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Geological formation |
| Underlies | Cangxi Formation, Jianguan Formation |
| Overlies | Suining Formation |
| Location | |
| Region | Asia |
| Country |  China |
The Penglaizhen Formation (simplified Chinese: 蓬莱镇组; traditional Chinese: 蓬萊鎮組; pinyin: Péngláizhèn Zǔ), is a geological formation in Sichuan, China. It was formerly thought to be Late Jurassic in age. However, the underlying Suining Formation has been dated to the Mid Cretaceous, so the formation must be this age or later[1] However a subsequent study suggested that the dates for the formation had been altered by geologic processes, and there dating the Suining Formation to the around the Jurassic Cretaceous boundary about 145 Ma, which means that Penglaizhen Formation is likely Early Cretaceous in age.[2] Dinosaur remains are among the fossils that have been recovered from the formation.[3]
Vertebrate paleofauna
Indeterminate ornithischian tracks have been recovered from Penglaizhen outcrops in Sichuan, China.[3]
| Genus | Species | Presence | Notes | Images |
|---|---|---|---|---|
|
M. anyuensis[3] |
|
See also
References
- ^ http://engine.scichina.com/publisher/scp/journal/SCES/62/1/10.1007/s11430-017-9268-7?slug=fulltext
- ^ Huang, Diying (19 October 2018). "Jurassic integrative stratigraphy and timescale of China". Science China Earth Sciences. 62 (1): 223–255. doi:10.1007/s11430-017-9268-7. ISSN 1674-7313.
- ^ a b c d e Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Jurassic, Asia)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 550–552. ISBN 0-520-24209-2.
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