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Yarang Formation

Yarang Fm


Period: 
Devonian

Age Interval: 
D21 (66), Eifelian (early Middle Devonian)


Province: 
Guangxi

Type Locality and Naming

The type section is located at Chengbei roadside (110°21’E-22°45’N), 3.5 km of Beiliu City of Guangxi Zhuang Autonomous Region. It was named by Wang Yu and others in 1965.


Lithology and Thickness

Limestone. The Formation, about 400 m thick, can be subdivided into two parts. Lower part, about 160 m thick, is characterized by gray, dark gray bioclastic limestone intercalated with bird-eye limestone, fine laminated peloidal limestone, algal limestone and clayey limestone. Upper part, about 220 m thick, mainly consists of bioclastic limestone and dolomitic limestone.


Lithology Pattern: 
Limestone


Relationships and Distribution

Lower contact

It rests conformably on the Guitang Fm with a bed of fine-grained quartz sandstone at its base.

Upper contact

Conformable contact with the overlying Tungkangling Fm (Donggonling Fm), but the definite boundary is disputable.

Regional extent

The Formation is distributed in Beiliu area, representing a facies lateral shifting change of Gupa and Gucha Fm at west side of Dayaoshan Mts.


GeoJSON

null

Fossils

The lower part contains brachiopoda Eospriferina lachrymose-Athyrisina Assemblage Zone and coral Utarauia sinensis, and the upper part has a few coral Dendrostella sp.


Age 

Eifelian (early Middle Devonian)

Age Span: 

    Beginning stage: 
Eifelian

    Fraction up in beginning stage: 
0.4

    Beginning date (Ma): 
390.70

    Ending stage: 
Eifelian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
385.30

Depositional setting

It is interpreted as an open to semi-restricted platform setting.


Depositional pattern:  


Additional Information


Compiler:  

Hongfei Hou