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Miaopo Formation

Miaopo Fm


Period: 
Ordovician

Age Interval: 
Darriwilian, (44, 45)


Province: 
Hubei, Sichuan, Anhui

Type Locality and Naming

The type section is at Miaopo in Fenxiang 17 km northwest of Yichang City, Hubei. The reference section is at Huanghuachang 5 km northwest of Yichang City (Zeng et al., 1983). The Miaopo Fm is derived from the Miaopo Shale proposed by Zhang Wentang in 1957.

In 1962, Zhang Wentang renamed the Miaopo Shale first the Miaopo Shale Fm then the Miaopo Fm. Wang Xiaofeng et al. (1980) suggested that the upper boundary of the Miaopo Fm coincides roughly with that of the Climacograptus peltifer zone. In 1983, Zeng Qingluan et al. studied in detail the lithology and fauna of the Miaopo Fm.

Synonym: (庙坡组)


Lithology and Thickness

The formation is composed of yellow, dark gray or yellowish green hydromica claystone intercalated with thin-bedded limestone. In the type area, the Miaopo Fm is 2.5 m thick.


Lithology Pattern: 
Pelagic marl


Relationships and Distribution

Lower contact

On the incompletely developed upper Pygodus serra subzone and the manganese nodules occurring on the discontinuity, the Miaopo Fm rests disconformably on the nodular limestone of the Guniutan Fm

Upper contact

It is conformably overlain by the limestone with polygonal cracks at the base of the Baota Fm

Regional extent

With a persistent lithology, the Miaopo Fm is restricted to Chengkou (2.7 m thick), eastern Gorge area (2.2-2.6 m thick) of Sichuan, and Hexian (1.8 m thick) of Anhui. In Hexian, no graptolite of Nemagraptus gracilis assemblage and conodont of Pygodus anserinus assemblage and Prioniodus alobatus assemblage have been found from the Miaopo Fm, indicating an upper boundary lower than in the type area.


GeoJSON

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Fossils

At the three Gorges district, the Miaopo Fm includes graptolite Husterograptus teretiusculus zone, Nemagraptus gracilis zone; conodont Pygodus serra zone, Pygodus anserinus zone, Eoplacognathus yianyeensis zone Prioniodus alobatus zone; cephalopod Lituites-Tridacinoceras zone; trilobite Birmanites-Telephops zone, in ascending order. Ge Meiyu (1957) and Mu Enzhi (1959) studied the graptolite from the Miaopo Shale.


Age 

Darriwilian-Sandbian. The Miaopo Shale had previously been thought to be Middle Ordovician in age. [Upper limit of age span used here for graphics is adjusted for later carbon-isotope and cyclostratigraphy interpretations of the overlying Pagoda Fm (Baota Fm); and as used by Yuandong Zhang, Renbin Zhan et al., 2019, Ordovician integrative stratigraphy and timescale of China. Science China: Earth Sciences, 62: 61-88.]

Age Span: 

    Beginning stage: 
Darriwilian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
463.80

    Ending stage: 
Sandbian

    Fraction up in the ending stage: 
0.7

    Ending date (Ma):  
454.38

Depositional setting


Depositional pattern:  


Additional Information


Compiler:  

Jianpo Wang and Xiaofeng Wang