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Youhe Formation

Youhe Fm


Period: 
Neogene

Age Interval: 
Late Pliocene (Piacenzian), N2 , (18)


Province: 
Shaanxi

Type Locality and Naming

Xue (1981) didn’t assign the type section. Zheng et al. (1999) proposed a reference section located at Zhangjiapo-Lujiahao section near the You River, Weinan City, Shaanxi Province. We recommend a lectostratotype for this formation, which is located at the Songjia Gully section (E109°30′, N34°25′), west of the Youhe Reservoir, about 7 km south of Weinan City. This formation was named by Xue (1981). However, it has not been widely accepted. BGMRS(Shaanxi)P (1989, 1998) didn’t employ this formation.

Synonym: This formation is equal to the original “Green Sanmen” (Chinese Association for Quaternary Research, 1959). Zheng et al. (1999) considered that the unpublished “Zhangjiapo Fm” is a synonym of the Youhe Fm. Wang et al. (2013) suggested that both the “Zhangjiapo Fm” and the Youhe Fm are essentially parts of the Sanmen Fm and should be incorporated into the Sanmen Fm.


Lithology and Thickness

It is mainly characterized by greyish-green or cyanic grey sandy mudstones and muddy sandstones with interlayers of marlstones. It contains fossil mammals, reptiles, fishes, bivalves, gastropods, ostracods, and sporopollens. Its thickness is about 36 m.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

In the reference section, the Youhe Fm unconformably contacts with the underlying late Miocene Jiulaopo Fm.

Upper contact

In the reference section, the Youhe Fm disconformably contacts with the overlying Quaternary Sanmen Fm. See YangjiawanNeogene Fm, which seems to be the next younger regional unit.

Regional extent

This formation is distributed to downstream of the You River, Heyang, and Baoji area, Shaanxi Province.


GeoJSON

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Fossils

Mammals: Mimomys youhenicus (including M. orientalis), Criectulus sp., Epimys sp., Chardinomys sp. (pro. Mus sp.), Spermophilus sp., Ochotonoides cf. O. complicidens, Nyctereutes sinensis, Elephas youheensis, Proboscidipparion pater (pro. Hipparion houfenense), Rhinocerotidae, Sus sp., Sus subtriquetra, Cervaitus sp., Cervus sp. Fishes: Cyprinus sp., Ctenopharyngodon sp., Mylopharyngodon sp. (Xue, 1981)


Age 

Based on the fossil mammals, the Youhe Fm can be correlated to the Daodi Fm in the Nihewan Basin, Hebei Province, and is in age of late Pliocene. The Youhe Fm in Songjia Gully has a magnetic dating in range of 2.5~3.4 Ma by Yue and Xue (1996).

Age Span: 

    Beginning stage: 
Piacenzian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
3.60

    Ending stage: 
Piacenzian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
2.58

Depositional setting

It is interpreted as river-lake environment.


Depositional pattern:  

Additional Information


Compiler:  

Tao Deng, Sukuan Hou, J.Z. Qigao, Q. Li, Q.Q. Shi, B.Y. Sun, S.Q. Wang, F.X. Wu