Also known as Yangchuanosaurus type site
Where: Sichuan, China (29.3° N, 105.7° E: paleocoordinates 29.6° N, 110.4° E)
• coordinate stated in text
• small collection-level geographic resolution
When: Upper Member (Shaximiao Formation), Bathonian to Bathonian (168.3 - 163.5 Ma)
• Several radiometric ages have been reported for the Shaximiao Formation, including 167 Ma or 172 Ma (Zong and Shi, 1997), 167–172 Ma or 178–169 Ma (Gou et al., 2000), 163±3 Ma (Li et al., 2010), 160±4 Ma (Luo et al., 2014), 158±7 Ma (Qian et al., 2016), and 159±2 Ma (Wang et al., 2018). However, more recent studies suggest an older age; Dai et al. 2022 reported a maximum depositional age for the bone-bearing layers of the lower member of the Shaximiao formation to be Bjaocan. Zhou et al. 2022 also supported a late Middle Jurassic age for the Shaximiao Formation (Bathonian-Callovian).
• bed-level stratigraphic resolution
Environment/lithology: terrestrial; red, sandy mudstone
Size class: macrofossils
Collected by Yang & Cheng in 1976-1977
Collection methods: salvage, quarrying, mechanical,
Primary reference: Z. Dong, Y. Zhang, X. Li and S. Zhou. 1978. [A new carnosaur from Yongchuan County, Sichuan Province]. Ke Xue Tong Bao [Science Newsletter] 23(5):302-304 [M. Carrano/M. Carrano]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 49790: authorized by Matthew Carrano, entered by Matthew Carrano on 26.04.2005
Creative Commons license: CC BY (attribution)
Taxonomic list
Reptilia | |
Yangchuanosaurus shangyouensis n. gen. n. sp.
Yangchuanosaurus shangyouensis n. gen. n. sp. Dong et al. 1978 allosauroid |