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Longdongshui Formation

Longdongshui Fm


Period: 
Devonian

Age Interval: 
D21 (53), Eifelian (early Middle Devonian)


Province: 
Guizhou

Type Locality and Naming

The type section is located in a gully about 300 m east of Longdongshui Village, 10 km east of Dushan County, Guizhou Province. It was named by Wang Yu et al. in 1964.


Lithology and Thickness

Dolomitic limestone It is mainly a set of carbonate rocks. The lower and middle parts are dominated by dolomitic limestone intercalated with limestone, and the upper part is limestone and clayey limestone with mudstone at top. It is 59.2 m in thickness.


Lithology Pattern: 
Dolomitic limestone


Relationships and Distribution

Lower contact

It is conformably onto the underlying Shujiaping Fm

Upper contact

No overlying rocks in the type section, but elsewhere the next unit is the Banzhai Fm.

Regional extent

It is restricted in Houershan mountains area in Dushan County.


GeoJSON

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Fossils

The formation contains abundant corals, brachiopods and a few trilobites, bryozoan, Stromatopora, gastropods and bivalves.

Brachiopods can be divided into a Xenospirifer fongi assemblage zone below and an Acrospirifer houershanensis assemblage zone above.

Corals are represented in the lower part by Lyrielasma qiannanense, Grypophyllum diluvianum, Tabularia devoniana, Dushanophrentis cystotabulata, etc., and in the upper part by Utaratuia sinensis, Sociophyllum minor, Breviseptopgyllum kochanense.


Age 


Age Span: 

    Beginning stage: 
Eifelian

    Fraction up in beginning stage: 
0.0

    Beginning date (Ma): 
394.30

    Ending stage: 
Eifelian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
385.30

Depositional setting

It is interpreted as a shallow open-marine facies. [Previous version had "lagoon"]


Depositional pattern:  


Additional Information


Compiler:  

(Xian Siyuan)