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Daodi Formation

Daodi Fm


Period: 
Neogene

Age Interval: 
Late Pliocene (Piacenzian), N2 , (16a)


Province: 
Hebei

Type Locality and Naming

Nihewan Basin. The type section is located at the Laowo Gully (E114°39′, N40°08′), about 750 m north of Daodi village, Nanxinzhuang town, Yangyuan County, Hebei Province (Cai et al., 2013 in Wang et al., 2013). It was formally named by Du et al. (1988).

Synonyms: Zhang et al. (2003) regarded this formation as a junior synonym of the Yuxian Fm proposed by Wang (1982). Pang (2003) suggested that this formation is a junior synonym of the Shixia Fm named by Huang and Guo (1981). Cai et al. (2013, in Wang et al., 2013) restricted the Daodi Fm to layer 3~9 of the Laowogou section (Cai, 1987; Du et al., 1988), and regarded that it is a synonym of the Yuxian Fm but didn’t decide the priority of these two formations.


Lithology and Thickness

The Daodi Fm is characterized by a series of fluvio-palustrine grey and greyish-green silty clays and light-yellow fine sands, silts, and gravels. It contains mammalian, sporopollen, ostracod, bivalve, gastropod, fish, and reptile fossils. Its thickness is about 30 m.


Lithology Pattern: 
Siltstone


Relationships and Distribution

Lower contact

In the type section, the Daodi Fm disconformably contacts with the underlying Upper Pliocene Shixia Fm (red clay) (=Huliuhe Fm).

Upper contact

In the type section, the Daodi Fm disconformably contacts with the overlying Lower to Middle Pleistocene Nihewan Fm.

Regional extent

The formation is restrictedly distributed to both downstream sides of the Huliu River in the Nihewan Basin, Hebei Province.


GeoJSON

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Fossils

Mammals: Sorex sp., Paenelimnoecus chinensis, Ochotona sp., Sinocricetus progressus, Nannocricetus mongolicus, Ungaromys spp., Mimomys sp., Mimomys sp. 2., Mesosiphneus praetingi, Pliosiphneus sp. 2, Pseudomeriones complicidens, Dipus fraudator, Paralactaga anderssoni, Micromys tedfordi, Apodemus zhangwagouensis, Chardinomys yusheensis, C. nihowanicus, ?Karnimata sp., Saidomys sp. . (Cai, 1987; Li et al., 2008) Ostracoda: Candona, Candoniella. Sporopollens: Pinuspollenites sp..


Age 


Age Span: 

    Beginning stage: 
Gelasian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
2.58

    Ending stage: 
Gelasian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
2.19

Depositional setting

It is interpreted as a river, lake, or swamp 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