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Pulai Formation

Pulai Fm


Period: 
Devonian

Age Interval: 
D22-D31 (40), Givetian to Frasnian (late Middle to early Late Devonian)


Province: 
Gansu

Type Locality and Naming

The type section is located at Dangduogou, 24 km northwest of Diebu County, Gansu. It was named by Cao Xuanduo et al. in 1987.


Lithology and Thickness

It is dominated by fine-grained clastic rock.

Lower member, 53.3 m thick, is mainly black silty shale intercalated with thin- to medium-bedded micrite, with a top bed of more than 10 m of massive sparry algae-bearing sandy bioclastic limestone.

Upper member, 214.2 m thick, is mainly black to gray carbonate-bearing shale intercalated with a few thin-bedded lenses of sandy micrite.


Lithology Pattern: 
Shallow-marine marl


Relationships and Distribution

Lower contact

It conformably overlies on the Xiawuna Fm.

Upper contact

It conformably underlies the Cakuohe Fm.

Regional extent


GeoJSON

null

Fossils

Lower member contains abundant small size brachiopod and solitary coral and is characterized by tentaculites Nowakia otomari acme zone.

Upper member - lower part mainly yields Nowakia postotomari-Wedekindella clarkei assemblage zone, and the upper part has the coral Grypophyllum mackenziense-Temnophyllum longiseptatum assemblage zone.

Conodont Icriodus symmetricus and tentaculites Striatostyliolina raristriata appear on the top.


Age 

Givetian to Frasnian (late Middle to early Late Devonian)

Age Span: 

    Beginning stage: 
Givetian

    Fraction up in beginning stage: 
0.6

    Beginning date (Ma): 
381.46

    Ending stage: 
Frasnian

    Fraction up in the ending stage: 
0.2

    Ending date (Ma):  
377.34

Depositional setting

It is interpreted as a neritic shelf to basin facies.


Depositional pattern:  


Additional Information


Compiler:  

(Cao Xuanduo)