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《Journal of Stratigraphy》 1986-01
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Ordovician palaeoenvironmental reconstruction of Yichang area, W. Hubei

Chen Xu and Qiu Jing-yu  
The Ordovician faunal and depositional characters indicate that the Nantsinkuan and Fen-hsiang Formations (Tremadocian) are mainly high subtidal with partially intertidal deposits; the Hunghuayuan and Dawan Formations (Arenigian) are from high subtidal to low subtidal deposits; the Kuniutan, Miaopo, Pagoda, Linh siang, and Wufeng Formations are all subtidal deposits. The Dawan Formation and the Miaopo Formation indicate the Arenigian and Ca-radocian sea transgressions and the top of the Kuniutan Formation as well as the top of the Wufeng Formation (the Dalmanitina-Hirnantia bed) indicate the sea regressions. These two transgressions and two regressions are coincided with the eustatic sea level changes. The Tremadocian and Arenigian trensgressions increased and brought the Kiaerograptus and the Glyptog-raptus austrodentatus graptolite faunas to the Yangtze Platform.The secondary dolomitization during the early Tremadocian (the Nantsinkuan Formation) is discussed. The so-called cracked Pagoda limestone is considered to be and under-seawater shrinkage limestone. The nodular limestone of the Linhsiang Formation was formed when the under-seawater shrinkage highly developed.
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