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Youping Formation

Youping Fm


Period: 
Paleogene

Age Interval: 
early Early Eocene (22)


Province: 
Hubei

Type Locality and Naming

Hubei - NW. The naming section is located at Youping, Fangxian County, Hubei Province. Named by Lei Yizhen, Zhang Qingru and Sun Quanying in 1979 and formally published in the monograph “Biostratigraphy (5): the Three Gorges Region of the Yangtze River” in 1987.


Lithology and Thickness

Lower part is brown, very thick- to thick-bedded conglomerate with sandy conglomerate and sandstone lenses. Middle and Upper parts are alternating beds of brownish red, medium- to thick-bedded conglomerate and silty mudstone, with yellowing brown fine sandstone, coffee mudstone and grayish green sandy conglomerate; mudstone contains abundant calcareous concretions. The thickness is ~270 m.


Lithology Pattern: 
Conglomerate


Relationships and Distribution

Lower contact

It is in conformable contact with the underlying Eocene Guanbingchang Fm.

Upper contact

It is in conformable contact with the overlying Eocene Longmaigou Fm.

Regional extent


GeoJSON

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Fossils

According to Lei Yizhen et al., the fossil mammals contained in this formation include Rhombomylus sp, Asiocoryphodon lophodontus and Mesonychids. In these fossils, Asiocoryphodon and Rhombomylus were not found in the post-early Eocene strata in the past. In addition, Huang Xueshi has recently found a kind of Hyopsodus, which further demonstrates that the age of the Youping Formation should be early Eocene.


Age 

Its age was previously considered to be Early Eocene (Zheng et al., 1999). Recent study assigns this formation to early Early Eocene corresponding to the Lingchan Stage (Li et al., 2019).

Age Span: 

    Beginning stage: 
Ypresian

    Fraction up in beginning stage: 
0.3

    Beginning date (Ma): 
53.62

    Ending stage: 
Ypresian

    Fraction up in the ending stage: 
0.7

    Ending date (Ma):  
50.45

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

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