内蒙古林西地区晚二叠世-早三叠世孢粉组合及三叠系的发现

杨兵; 张雄华; 葛梦春; 赵省民; 韦一; 黄兴; 栾腾飞; 魏信祥; 杨志勇

doi:10.3799/dqkx.2014.074

Volume 39 Issue 7

Jul. 2014

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Article Navigation > Earth Science > 2014 > 39(7): 784-794

Yang Bing, Zhang Xionghua, Ge Mengchun, Zhao Shengmin, Wei Yi, Huang Xing, Luan Tengfei, Wei Xinxiang, Yang Zhiyong, 2014. Late Permian-Early Triassic Palynological Assemblages in Linxi, Inner Mongolia and Discovery of Triassic Strata. Earth Science, 39(7): 784-794. doi: 10.3799/dqkx.2014.074

Citation:

Yang Bing, Zhang Xionghua, Ge Mengchun, Zhao Shengmin, Wei Yi, Huang Xing, Luan Tengfei, Wei Xinxiang, Yang Zhiyong, 2014. Late Permian-Early Triassic Palynological Assemblages in Linxi, Inner Mongolia and Discovery of Triassic Strata. Earth Science, 39(7): 784-794. doi: 10.3799/dqkx.2014.074

Citation:

Yang Bing, Zhang Xionghua, Ge Mengchun, Zhao Shengmin, Wei Yi, Huang Xing, Luan Tengfei, Wei Xinxiang, Yang Zhiyong, 2014. Late Permian-Early Triassic Palynological Assemblages in Linxi, Inner Mongolia and Discovery of Triassic Strata. Earth Science, 39(7): 784-794. doi: 10.3799/dqkx.2014.074

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Late Permian-Early Triassic Palynological Assemblages in Linxi, Inner Mongolia and Discovery of Triassic Strata

doi: 10.3799/dqkx.2014.074

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Oil & Gas Survey, China Geological Survey, Beijing 100029, China
3.
The Third Institute and Mineral Exploration of Gansu Provincial Bureau of Geology and Mineral Resources, Lanzhou 730050, China

Received Date: 2013-09-04
Publish Date: 2014-07-15

Abstract

Abstract

Large amount of spores and pollen (mainly consist of pteridophyta spores and gymnospermous pollen), including 54 genera and 90 species, were discovered in the fifth member of Late Permian Linxi Formation, Guandi section, Linxi, Inner Mongolia. The fifth member of Linxi Formation was assumed to belong to the Late Permian, for the preservations of special Late Permian spores and pollen, and biostratigraphic correlations to adjacent areas. 9 genera and 9 species were also found from the sixth member of Linxi Formation. They should belong to the Early Triassic, for the existing characteristics of the Early Triassic palynological assemblages. In addition, the lithology of the sixth member of Linxi Formation varies from that of the underlain parts of Linxi Formation, but similar to that of adjacent Laolongtou Formation, for the yielding of purple-gray silty slate and volcanic breccias interbeds. The sixth member of Linxi Formation might belong to the Early Triassic Laolongtou Formation, evidenced by the integration of lithology, fossils, paleo-climate records and correlations to adjacent areas. The Permian-Triassic boundary is placed in the interval between the fifth member of Linxi Formation and Laolongtou Formation.
- palynological assemblage,
- Late Permian,
- Early Triassic,
- Linxi Formation,
- Laolongtou Formation,
- stratigraphy

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References(61)

References

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Late Permian-Early Triassic Palynological Assemblages in Linxi, Inner Mongolia and Discovery of Triassic Strata

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