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- W2354660923 abstract "A spore and pollen assemblage was discovered from the Chenjiawan Formation in the Zigui Basin, Hubei, which can be referred to the Cyathidites minor-Classopollis-Callialasporites assemblage of Middle Jurassic. In general, the character of the Chenjiawan assemblage is consistent with the assemblages in the Xietan Formation and the Shaximiao Formation of Middle Jurassic in the Zigui Basin. But there is a little difference between the early and the middle-later assemblages. The vertical distribution of spore and pollen flora in the Jurassic indicates that the weather has transformed from high to low humidity. The Early Jurassic features sub-tropic and tropic, hot and humid, with flourishing plants. Later, drought appears but the wet climate is still dominant. The early time of Middle Jurassic enters half dry weather becoming progressively drier. The Late Jurassic is an extremely drought world with few species of plants where Cheirolepidiaceae are predominent." @default.
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- W2354660923 date "2004-01-01" @default.
- W2354660923 modified "2023-09-27" @default.
- W2354660923 title "Discovery of the Middle Jurassic sporopollen assemblage in the Chenjiawan Formation of Zigui Basin, Hubei and its significance" @default.
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