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Wangyou - Tangkou, Yizhou District, Hechi, Guangxi, China
| Formation | Wangyou |
|---|---|
| Member | Tangkou |
| Age: | 359 - 323 Ma Paleozoic |
| Interval | Mississippian |
| Lithology | mudstone/"limestone" |
| Number of Collections | 1 |
| Number of Occurrences | 3 |
Recorded Sample Locations
| Location | Region | Stratigraphic Name |
|---|---|---|
| Bed 135 of Duolingshan Fm Lali | Yizhou District, Hechi, Guangxi, China | Wangyou - Tangkou |
Associated Units
| Stratigraphic Name | Age | Lithology | Occurrence Records |
|---|---|---|---|
| Donggangling | 388 - 383 Ma Devonian | limestone, "limestone"/chert, "limestone"/"shale", "shale"/"limestone", framestone, lime mudstone/rudstone, floatstone/wackestone | 139 |
| Doulingshan | 359 - 299 Ma Paleozoic | limestone | 34 |
| Laoyefen | 382 - 372 Ma Late/Upper Devonian | lime mudstone, "limestone" | 236 |
| Tongchejiang | 359 - 331 Ma Paleozoic | shale/"limestone" | 18 |
| Wangyou - Lasha | 359 - 347 Ma Paleozoic | lime mudstone, "limestone" | 83 |
| Wuzhishan | 365 - 359 Ma Late/Upper Devonian | lime mudstone, "limestone" | 514 |
| Xiangtian | 380 - 376 Ma Late/Upper Devonian | lime mudstone | 101 |
Recorded Fossils
| Accepted Name | Hierarchy | Age |
|---|---|---|
 Spathognathodus sp.genus | Animalia : Chordata : Conodonta : Spathognathodus | 358.9 - 323.2 Ma Paleozoic |
| Protognathodus meischneri species | Animalia : Chordata : Conodonta : Ozarkodinida : Idiognathodontidae : Protognathodus : Protognathodus meischneri | 358.9 - 323.2 Ma Paleozoic |
| Polygnathus sp. genus | Animalia : Chordata : Polygnathidae : Polygnathus | 358.9 - 323.2 Ma Paleozoic |
References
| Ji Q., Ziegler W. (1993) The Lali Section: An Excellent Reference Section for Upper Devonian in South China, Courier Forschungsinstitut Senckenberg 157, 1-182 |
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
