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
Shizikou Formation

Shizikou Fm


Period: 
Paleogene

Age Interval: 
Early Paleocene, (25b)


Province: 
Jiangxi

Type Locality and Naming

The naming section is located in the area from Shizikou Village to Tianxinli, Qinglong Township, more than 10 km northeast of Dayu County, southern Jiangxi. Named by Tong Yongsheng et al. in 1976.


Lithology and Thickness

Mainly brick-red and purplish red pebbly sandstone and sandy mudstone with mudstone and grayish green sandstone dominantly of fluvial facies. Generally the lithology of lower part of this formation becomes coarse, usually intercalated with sandy conglomerate, and laterally the lithology is not persistent. Generally speaking, the lithology is coarser on the western margin of the basin, and eastward the lithology becomes finer, being mudstone with sandstone. The thickness is up to 128 m.


Lithology Pattern: 
Sandstone


Relationships and Distribution

Lower contact

The formation has a disconformable contact with the underlying Late Cretaceous Nanxiong Fm (which is in adjacent Guangdong province). However, in southernmost Jiangxi, the next older regional unit is the early-Late Cretaceous Zhutian Fm of the Ganzhou Gr (Cret column 39b)

Upper contact

Conformable contact with the overlying Paleocene Chijiang Fm.

Regional extent

It is mainly distributed at Huyanshan and Shizikou of Qinglong Township and Chijiang and Xincunli of Chijiang Township, Dayu County, southern Jiangxi.


GeoJSON

null

Fossils

The fossil types found in the formation up to now are monotonous, but the individuals are rich; the fossils are buried sporadically. Mammals are restricted to Bemalambda shizikouensis and Pantolambdodon of Bemalambdids of Pantodonta.


Age 

Wang, Y.Q., et al. (2019, Paleogene Integr. Strat. Timescale China; Sci. China: Earth Sci., 62) assign as early through mid-late Danian.

Age Span: 

    Beginning stage: 
Danian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
66.04

    Ending stage: 
Danian

    Fraction up in the ending stage: 
0.9

    Ending date (Ma):  
62.10

Depositional setting

The formation belongs to fluvial facies.


Depositional pattern:  

Additional Information


Compiler:  

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