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Funing Formation

Funing Fm


Period: 
Paleogene

Age Interval: 
Paleocene (23c)


Province: 
Jiangsu

Type Locality and Naming

The naming section is located in well Fuji No. 1, Funing County, northern Jiangsu basin. Named by the Petroleum Reconnaissance Party of Jiangsu Geoglogy Bureau and East China Bureau of Petroleum Exploration, in 1958.


Lithology and Thickness

From below to above four members may be distinguished: First member, ~700 m thick, is alternating beds of brownish red sandstone and dark brown mudstone, with black mudstone at the top, containing rich gypsum concretions; Second member, ~200–300 m thick, is dominated by grayish black mudstone with thin-bedded of muddy limestone, bioclastic limestone, muddy dolostone and oil shale, the base of which is marked by marlstone, oolitic limestone and bioclastic limestone; Third member, ~0–380 m thick, is alternating beds of grayish black and dark gray mudstone and muddy siltstone and sandstone; Fourth member, ~0–560 m thick, consists dominantly of dark gray and grayish black mudstone and silty mudstone, the upper part of which is intercalated with thin beds of organic limestone, oolitic limestone and worm tube limestone. The total thickness may reach more than 1500 m.


Lithology Pattern: 
Sandy claystone


Relationships and Distribution

Lower contact

It has a conformable or disconformable contact with the underlying Late Cretaceous Taizhou Fm.

Upper contact

Disconformable contact with the overlying Early Eocene Dainan Fm.

Regional extent

The formation is widespread in wells at Binhai, Funing, Sheyang, Jianhu, Hongze, Yancheng, Xinghua, Gaoyou, Xuyi, Dongtai, Taizhou and Jiangdu.


GeoJSON

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Fossils

This formation contains abundant fossils, mainly including ostracods, charophytes, sporopollen and vertebrates.


Age 

Its age was previously considered to be Paleocene to Eocene or Paleocene (Zheng et al., 1999). Recent study assigns this formation to Paleocene (Wang et al., 2019). which Wang, Y.Q., et al. (2019, Paleogene Integr. Strat. Timescale China; Sci. China: Earth Sci., 62) assign it as spanning entire Paleocene, with Member 1 as early through middle Danian, Members 2 and 3 as latest Danian through Selandian, and Member 4 as Thanetian.

Age Span: 

    Beginning stage: 
Danian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
66.04

    Ending stage: 
Thanetian

    Fraction up in the ending stage: 
0.0

    Ending date (Ma):  
59.24

Depositional setting

The formation is lakeshore, deltaic-brackish lake sedimentary sequence.


Depositional pattern:  

Additional Information


Compiler:  

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