Gaofengshan, Dazu (Jurassic to of China)

Also known as Tatsu, Longang, Kao-feng-shan

Where: Chongqing (=Sichuan), China (29.7° N, 105.7° E: paleocoordinates 29.9° N, 110.3° E)

• coordinate based on nearby landmark

• outcrop-level geographic resolution

When: Upper Member (Shaximiao Formation), Bathonian to Bathonian (168.3 - 163.5 Ma)

• "Probably Shaximiao Formation"

•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; lithology not reported

Size class: macrofossils

Reposited in the IVPP

Primary reference: H. K. Yeh. 1963. Fossil turtles of China. Palaeontologia Sinica, New Series C 150:1-113 [E. Vlachos/E. Vlachos/E. Vlachos]more details

Purpose of describing collection: taxonomic analysis

PaleoDB collection 127732: authorized by Roger Benson, entered by Roger Benson on 22.05.2012

Creative Commons license: CC BY (attribution)

Taxonomic list

Reptilia
 Testudines -
Yehguia tatsuensis n. gen. n. sp.
Yehguia tatsuensis n. gen. n. sp. Yeh 1963 turtle
IVPP-V996, holotype: an incomplete shell with partially exposed girdles, hindlimbs and tail