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Caijiachong Formation

Caijiachong Fm


Period: 
Paleogene

Age Interval: 
Middle to Late Eocene , (20a)


Province: 
Yunnan

Type Locality and Naming

The naming section is located to the north of Caijiachong ~20 km southeast of the seat of Qujing County, Yunnan Province. Named by Pei Wenzhong in 1963.


Lithology and Thickness

According to the section across the Yuchuan basin from SE to NW north of Caijiachong measured by Wang Banyue et al. (1983), this formation may be divided into five beds; ascending they are: (1) grayish green mudstone; (2) light gray marlstone with variegated (grayish green, grayish yellow and yellowish red) mudstone and calcareous mudstone with clayey sandstone ad siltstone; (3) alternating light grayish green, thick-bedded siltstone and grayish green and grayish yellow mudstone and calcareous mudstone; (4) grayish green, thick-bedded marlstone and calcareous mudstone with gray green mudstone and light gray siltstone and fine sandstone, showing a nodular shape after weathered; and (5) light gray, siliceous siltstone and mudstone, which are light and show a grayish brown color when weathered, called locally “sheep-wool stone”. The total thickness is more than 200 m.


Lithology Pattern: 
Continental marl


Relationships and Distribution

Lower contact

The Middle Eocene Gelanghe Fm unconformably underlies it

Upper contact

The top of the formation is covered by the Quaternary.

Regional extent


GeoJSON

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Fossils

Fossils mainly occur in beds 2 and 4 of the above-mentioned section. Charophytes include Amblyochara subeiensis, Maedlerisphaera chinensis, Harrisichara vesifomis and Sphaerochara inconpicua; gastropods mainly include Bithynia largicirca and Assiminea pressoopercura; vertebrates include mammals in addition to fishes such as Cyprinidae and reptiles such crocodiles and turtles, of which mammals include Cadurcodon ardynensis, Gigantamynodon giganteus, Indricotherium qujingensis, Bothriodon chowi, Eucricetodon meridionalis, Sinosminthus inapetus and Lophiomeryx sp..


Age 

The age of this formation was suggested to be Early Oligocene in the past, but Wang, Y.Q. et al. (2019; Paleogene integrated stratigraphy and timescale of China) restricted it to Middle to Late Eocene.

Age Span: 

    Beginning stage: 
Bartonian

    Fraction up in beginning stage: 
0.4

    Beginning date (Ma): 
39.70

    Ending stage: 
Priabonian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
33.90

Depositional setting

It is interpreted to lacustrine deposits


Depositional pattern:  

Additional Information


Compiler:  

Tao Deng, Yuanqing Wang, Qian Li, et al.