Misplaced Pages

Yangliujing Formation

Article snapshot taken from Wikipedia with creative commons attribution-sharealike license. Give it a read and then ask your questions in the chat. We can research this topic together.
Geological formation in southern China
Yangliujing Formation
Stratigraphic range: late Anisian-Ladinian
246–242 Ma PreꞒ O S D C P T J K Pg N
TypeGeological formation
UnderliesZhuganpo Formation
OverliesGuanling Formation
Lithology
PrimaryDolomite
OtherLimestone
Location
Coordinates25°54′N 105°30′E / 25.9°N 105.5°E / 25.9; 105.5
Approximate paleocoordinates12°18′N 94°30′E / 12.3°N 94.5°E / 12.3; 94.5
RegionGuizhou & Yunnan Provinces
Country China
ExtentYunnan–Guizhou Plateau
Yangliujing Formation is located in ChinaYangliujing FormationYangliujing Formation (China)Show map of ChinaYangliujing Formation is located in GuizhouYangliujing FormationYangliujing Formation (Guizhou)Show map of Guizhou

The Yangliujing Formation is a Middle Triassic geologic unit found in the Guizhou and Yunnan Provinces of southern China.

Description

Most of the formation is represented by massive dolomites, indicative of a shallow-water depositional environment. Fossils are generally rare, but conodonts from the Anisian-Ladinian boundary (namely several species of Neogondolella) are known from the lower part of the formation. Some marine reptiles have been found in dolomitic limestone near Dingxiao, an area of Guizhou sometimes considered to preserve the upper part of the Yangliujing Formation. However, under a more restrictive definition of the Yangliujing Formation, the fossils of Dingxiao would instead belong to the overlying Zhuganpo Formation.

Fossil content

The following fossils have been reported from the formation:

Fish
Brachiopods
Bivalves
Crinoids
Conodonts

References

  1. Benton et al., 2013
  2. Sun et al., 2016

Bibliography

Categories: