Guanling Formation
Guanling Formation Stratigraphic range: early-mid Anisian () ~ | |
---|---|
Type | Geological formation |
Underlies | Yangliujing Formation |
Overlies | Jialingjiang Formation |
Lithology | |
Primary | Mudstone, limestone |
Other | Dolostone |
Location | |
Coordinates | 25°30′N 104°54′E / 25.5°N 104.9°ECoordinates: 25°30′N 104°54′E / 25.5°N 104.9°E |
Approximate paleocoordinates | 11°42′N 94°12′E / 11.7°N 94.2°E |
Region | Guizhou & Yunnan Provinces |
Country | China |
Extent | Yunnan–Guizhou Plateau |
Guanling Formation (China) |
The Guanling Formation is a Middle Triassic (Anisian or in the regional chronostratigraphy) geologic formation in southwestern China.
Description[]
The formation encompasses two members. The first member is primarily calcareous mudstone and dolomite, indicative of a coastal environment. The second member is a thicker marine sequence of dark micritic limestone with some dolomite. Two distinct fossil assemblages are found in the second member. The older Luoping biota preserves abundant arthropods along with fossils from other invertebrates and vertebrates, which are rare but well-preserved. The slightly younger Panxian fauna has a more diverse and common assortment of marine reptiles such as sauropterygians.[1]
Fossil content[]
Among others, the following fossils were reported from the formation:
References[]
- ^ Benton, Michael J.; Zhang, Qiyue; Hu, Shixue; Chen, Zhong-Qiang; Wen, Wen; Liu, Jun; Huang, Jinyuan; Zhou, Changyong; Xie, Tao; Tong, Jinnan; Choo, Brian (2013-10-01). "Exceptional vertebrate biotas from the Triassic of China, and the expansion of marine ecosystems after the Permo-Triassic mass extinction". Earth-Science Reviews. 125: 199–243. doi:10.1016/j.earscirev.2013.05.014. ISSN 0012-8252.
- Guanling Formation
- Geologic formations of China
- Triassic System of Asia
- Triassic China
- Limestone formations
- Dolomite formations
- Mudstone formations
- Lagoonal deposits
- Deep marine deposits
- Open marine deposits
- Shallow marine deposits