Discovery of sporopollen assemblages of Yan'an Formation in Yanchi, Ordos basin, and its paleoclimate significances

被引:0
|
作者
He F. [1 ]
Zhang S. [2 ]
Jiang Z. [1 ]
Yang B. [2 ]
Yuan Q. [1 ]
Gong X. [2 ]
Guo C. [3 ]
Cao J. [1 ]
机构
[1] Sinopec North China Oil and - Gas Branchy Zhengzhou, Henan
[2] Cores and Samples Centre of Natural Resources, Hebei, Langfang
[3] Institute of Geology, Chinese Academy of Geological Sciences,, Beijing
来源
Dizhi Xuebao/Acta Geologica Sinica | 2024年 / 98卷 / 01期
关键词
clay minerals; Ordos basin; paleoclimate; sporopollen assemblage; Yan'an Formation;
D O I
10.19762/j.cnki.dizhixuebao.2023303
中图分类号
学科分类号
摘要
For rebuilding the paleoclimate and paleoenvironment during the early-middle Jurassic in the Yanchi area of the Ordos basin, -we analysis the palynological characteristics and clay minerals of the core Ningdong-2 , sporopollen assemblages and sporopollen spectra -were established. The lower part of the Yan'an Formation is the Inaperturopollenites-Psophosphaera-Protopinus assemblage, -whose age is the late Toarcian of Early Jurassic. The upper part of this formation is the Cyathidites-Deltoidospora-Cycadopitees assemblage, -whose age is early Middle Jurassic. The boundary of lower and middle Jurassic is located between 2144. 5 - 2153. 0 m of the core. The paleoclimate and paleovegetation established by pollen spectrum shows that the late Toarcian of early Jurassic period -was a -warm temperate semi-humid climate -whose vegetation type -was coniferous forest. The early Middle Jurassic -was generally subtropical humid climate, -whose vegetation appearance transformed from coniferous broadleaf mixed forest-grass type to the coniferous forest-dilute grass type. From the late Toarcian of Early Jurassic period to the early Middle Jurassic period, the humidity changed from semi-humid to wet while the temperature changed from low to high. This climate change trend was also found in clay minerals analysis. The climate shift has had a clear role in promoting coal gathering in the region. © 2024 Geological Society of China. All rights reserved.
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页码:200 / 213
页数:13
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