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Baiyaya Formation

Baiyaya Fm


Period: 
Silurian

Age Interval: 
Upper Telychian to Lower Wenlock of Silurian (S2), (42)


Province: 
Shaanxi

Type Locality and Naming

It was named by Xiang Liwen, Lin Baoyu and Nan Runshan in 1960 and published in Paleontology Atlas of Qingling in 1963. The type section is Baiyaya section in Mingzhu District, Langao County, Shaanxi Province. Coordinate: 108°49′E, 32°22′N.

Synonym: (白崖垭组)


Lithology and Thickness

The formation is characterized by the grey limestone and grey black bioclastic limestone, with several interbeds of pyroclastic porphyritic sandstone and conglomerate. It is 145 m in thickness at the type section.


Lithology Pattern: 
Reef limestone


Relationships and Distribution

Lower contact

It is conformable contacted with the underlying Wujiahe Fm

Upper contact

It is conformable contacted with the overlying Doushangou Fm

Regional extent

The thickness increases from west to east, 40 m thick at the Wujiahe section, 145 m at the type section, and 432 m thick near the Langao County in east.


GeoJSON

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Fossils

It is fossiliferous with abundant corals Mesofavosites oculiporoides, M. obliquus, Subalveolites panderi, Halysites sussmilchi, Antherolites septosus; brachiopod Eocoelia sp., Nalivkinia sp., Glassia sp.; a few graptolite Monoclimacis cf. linnarssoni and stromatoporoid, etc.


Age 

The age is ranging from Pterospathodus eopennatus conodont superzone of Lower-Middle Llandovery to Kockelella ranuliformis conodont superzone of Lower Wenlock according to Chen Zhongyang et al. (2019). Transgressive base (begins ca. 70% to end of Telychian). Overlying Anpinglaing Fm also has transgressive base.

Age Span: 

    Beginning stage: 
Telychian

    Fraction up in beginning stage: 
0.85

    Beginning date (Ma): 
433.78

    Ending stage: 
Sheinwoodian

    Fraction up in the ending stage: 
0.5.

    Ending date (Ma):  
431.78

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Wang Chuanshang and Wang Xiaofeng