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Erdengtu Formation

Erdengtu Fm


Period: 
Neogene

Age Interval: 
Latest Miocene (Messinian), N1 , (12a)


Province: 
Inner Mongolia

Type Locality and Naming

Central-Eastern Inner Mongolia. The type section is located at the “Ertemte section” (E114°05′, N41°52′), southeast of Erdengtu (=Ertemte) village, Huade County, central Nei Mongol. It is derived from the “Ertemte Bed” named by Andersson (1923), and formally erected by Zheng et al. (1999).

Synonym: Ertemte Fm; Gao et al. (2014a) treated the Haerebo Fm (=Harr Obo Fm) as a synonym of the Erdengtu Fm.


Lithology and Thickness

The Erdengtu Fm is characterized by a series of light grey, yellowish-brown, and reddish-yellow sandy mudstones. Its upper part is rich in calcium. It contains abundant fossil sporopollens, charophytes, gastropods, bivalves, fishes, amphibians, reptiles, and mammals. Its thickness is around 1 m.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

No underlying rock unit could be seen in the type section. Regionally, the next older unit is the widespread Tongguer Fm

Upper contact

In the type section, the Erdengtu Fm disconformably contacts with the overlain Quaternary deposits.

Regional extent

The formation is restrictedly distributed to the surrounding area of the Dabsun-Nor Lake in the county of Huade, central Nei Mongol.


GeoJSON

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Fossils

Mammals: “Erinaceusmongolicus, Sorex minutoides, S. ertemteensis, S. pseudoalpinus, Zelceina kormosi, Alloblarinella sinica, Paenepetenyia zhudingi, Cokia kowalskae, Paranourosorex inexspctatus, Paenelimnoecus obtusus, Quyania chowi, Yanshuella primaeva, Chiroptera gen. et sp. indet., Alilepus annectens, Ochotona lagreli, O. minor, Pseudaplodon asiaticus, Tamias ertemtensis, Sciurus sp., Sinotamias gravis, Prospermophilus orientalis, Plioptaurista rugosa, Hylopetes auctor, Myomimus sinensis, Leptodontomys gansus, Dipoides anatolicus, Castor anderssoni, Eozapus similis, Sinozapus sp., Sicista wangi, S. ertemteensis, Lophocricetus grabaui, Paralophocricetus pusillus, Paralactaga suni, Brachyscirtetes wimani, Dipus faudator, Sinocricetus zdanskyi, Nannocricetus mongolicus, Kowalskia similis, K. neimengensis, Microtoscoptes praetermissus, Microtodon atavus, Anatolomys teilhardi, Pseudomeriones abbreviates, Prosiphneus eriksoni, Hansdebuijnia pusilla, Karnimatoides hipparionus, Apodemus orientalis, Orientalomys primitivus, Micromys chalceus, Meles suillus, Promephitis alexejevi, Hipparion sp., “Paracervulusbrevis, Honanotherium sp.. (Falhbusch et al., 1983; Storch, 1987; Qiu and Li, 2016)


Age 

T. Deng et al. (2019; Neogene chapter of China Integrated Stratigraphy and Timescale) show the Ertemte Fm Bed (currently in Column 12) as both younger and overlying the Baogeda Ula Fm; rather than equivalent in age as given in the older China Lexicon = only late Messinian.

Age Span: 

    Beginning stage: 
Messinian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
6.29

    Ending stage: 
Messinian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
5.34

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