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
Tantou Formation

Tantou Fm


Period: 
Paleogene

Age Interval: 
Late Paleocene (17a,b,c)


Province: 
Shandong

Type Locality and Naming

The naming section is located near Tantou Township ~25 km northeast of Luanchuan County, Henan. Named by Zhang Renjie in 1974.


Lithology and Thickness

Mainly grayish green, grayish white and grayish black mudstone, shale, oil shale and marlstone with sandstone. The lithology shows certain lateral change. In the vicinity of Tanyugou, Luanchuan County, the Lower part is grayish brown conglomerate with grayish green pebbly sandstone and sandy mudstone or alternating beds of them; the Middle part, mainly yellowish green mudstone with grayish brown, grayish white and grayish black sandstone, marlstone and oil shale; the Upper part, grayish yellow, yellowish green and grayish black mudstone, marlstone and oil shale. In the vicinity of Gaoyugou the lithology becomes fine; in the vicinity of Baizhuang about 5 km northeast of Tantou mainly light yellow sandy conglomerate is found. The thickness is about 130–450 m.


Lithology Pattern: 
Claystone


Relationships and Distribution

Lower contact

It has a conformable contact with the underlying Middle Paleocene Dazhang Fm.

Upper contact

Its upper part was eroded; so the top is not observed. Regionally, the next younger unit is the Lushi Fm.

Regional extent

This formation is distributed at Gaoyugou, Tanyugou, Tantou, Baizhuang and Ganlusi in Luanchuan County, and a similar horizon is possibly exposed in the vicinity of Dazhang, Songxian County.


GeoJSON

null

Fossils

This formation contains bivalves, ostracods, the turtles Sinoharianus sichuanensis and mammals. Ostracods occur in the middle and upper parts of the formation, mainly including such species as Cypris henanensis and Sinocypris funingensis. Fossil mammals occur in the middle part of the formation, mainly represented by Prodinoceratinae and Pantolambdodontidae (including Archaeolambdidae).


Age 

Wang, Y.Q. et al. (2019; Paleogene integrated stratigraphy and timescale of China) show it as spanning only the Thanetian

Age Span: 

    Beginning stage: 
Thanetian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
59.24

    Ending stage: 
Thanetian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
56.00

Depositional setting

It is interpreted to lacustine-swampy deposits.


Depositional pattern:  


Additional Information


Compiler:  

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