Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian
Carboniferous
Devonian
Silurian
Ordovician
Cambrian
Neoproterozoic
Mesoproterozoic

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
BilikeBed Formation

BilikeBed Fm


Period: 
Neogene

Age Interval: 
Early Pliocene (Zanclean), N2 , (12a)


Province: 
Inner Mongolia

Type Locality and Naming

The type section is located at the Longgushan (dragon bones hill) (E114°29′, N42°08′), about 1.5 km northwest of the Bilike village, Dagaitan town, Huade County, central Nei Mongol. It was named by Qiu et al. (2013, in Wang et al., 2013). The construction of a railway track in 1990s transected and destroyed the type section.


Lithology and Thickness

The Bilike Bed is characterized by a series of lacustrine brownish-red siltstone and sandy mudstones. It contains abundant fossil mammas, fishes, amphibians, reptiles, freshwater mollusks, and charophytes. Its thickness is in range of 8~10.5 m.


Lithology Pattern: 
Siltstone


Relationships and Distribution

Lower contact

No underlying rock units could be seen in the type section.

Upper contact

In the type section, the Bilike Bed disconformably contacts with the overlain Quaternary deposits.

Regional extent

The formation is restrictedly distributed to the surrounding area of the Longgushan of the county of Huade, central Nei Mongol.


GeoJSON

null

Fossils

Mammals: Quyania cf. Q. chowi, Yanshuella primaeva, Desmana sp., Sorex minutoides, S. ertemteensis, S. pseudoalpinus, S. sp., Petenyia katrinae, Lunanosorex cf. L. lii, Parasoriculus tongi, Sulimskia ziegleri, Paenelimnoecus obtusus, Erinaceus mongolicus, Myotis cf. annectans, M. cf. M. horsfieldii, M. sp., Vespertilio cf. V. sinensis, Murina sp., Alilepus annectens, Ochotona lagreli, O. minor, Tamias ertemtensis, Sinotamias gravis, Prospermophilus orientalis, Hylopetes yani, Myomimus sinensis, Castor anderssoni, Sinozapus volkeri, Sicista wangi, S. bilikeensis, Lophocricetus grabaui, Paralophocricetus pusillus, Paralactaga suni, Brachyscirtetes cf. B. wimani, Dipus pliocenicus, Sinocricetus progressus, Nannocricetus mongolicus, Kowalskia zhengi, K. cf. K. similis, Microtodon cf. M. atavus, Anatolomys cf. A. teilhardi, Pseudomeriones abbreviates, Mimomys (Aratomys) bilikeensis, Prosiphneus cf. P. eriksoni, Apodemus lii, A. sp.Orientalomys sinensis, Chardinomys bilikeensis, Huaxiamys sp., Allorattus engesseri, Micromys kozaniensis. (Qiu and Storch, 2000; Qiu and Li, 2016)


Age 

Based on the faunal mammals, the age of the Bilike Bed is normally accepted that is in early Pliocene. The Bilike Fauna is one of the faunal representatives in the Gaozhuanian Stage of the continental Pliocene series in China (Deng et al., 2010). T. Deng et al. (2019; Neogene chapter of China Integrated Stratigraphy and Timescale) show the age span as lower Zanclean (but with wavy unconformity boundaries).

Age Span: 

    Beginning stage: 
Zanclean

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
5.34

    Ending stage: 
Zanclean

    Fraction up in the ending stage: 
0.4

    Ending date (Ma):  
4.64

Depositional setting

It is interpreted as a 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