江西乐平沿沟二叠纪末有孔虫的演变及对鲕状灰岩的古环境指示意义

田力; 童金南; 宋海军; 梁蕾; 杨利蓉; 宋虎跃; 王成刚; 赵小明; 孙冬英

doi:10.3799/dqkx.2014.140

Volume 39 Issue 11

Nov. 2014

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Article Navigation > Earth Science > 2014 > 39(11): 1473-1486

Tian Li, Tong Jinnan, Song Haijun, Liang Lei, Yang Lirong, Song Huyue, Wang Chenggang, Zhao Xiaoming, Sun Dongying, 2014. Foraminiferal Evolution and Formation of Oolitic Limestone near Permian-Triassic Boundary at Yangou Section, Jiangxi Province. Earth Science, 39(11): 1473-1486. doi: 10.3799/dqkx.2014.140

Citation:

Tian Li, Tong Jinnan, Song Haijun, Liang Lei, Yang Lirong, Song Huyue, Wang Chenggang, Zhao Xiaoming, Sun Dongying, 2014. Foraminiferal Evolution and Formation of Oolitic Limestone near Permian-Triassic Boundary at Yangou Section, Jiangxi Province. Earth Science, 39(11): 1473-1486. doi: 10.3799/dqkx.2014.140

Citation:

Tian Li, Tong Jinnan, Song Haijun, Liang Lei, Yang Lirong, Song Huyue, Wang Chenggang, Zhao Xiaoming, Sun Dongying, 2014. Foraminiferal Evolution and Formation of Oolitic Limestone near Permian-Triassic Boundary at Yangou Section, Jiangxi Province. Earth Science, 39(11): 1473-1486. doi: 10.3799/dqkx.2014.140

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Foraminiferal Evolution and Formation of Oolitic Limestone near Permian-Triassic Boundary at Yangou Section, Jiangxi Province

doi: 10.3799/dqkx.2014.140

1.
State Key Laboratorgy of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
2.
Wuhan Center of Geological Survey, China Geological Survey, Wuhan 430223, China
3.
Colloge of Tourism and Territorial Resources, Jiujiang University, Jiujiang 332005, China

Received Date: 2014-02-09
Publish Date: 2014-11-01

Abstract

Abstract

The homogeneous carbonate Permian-Triassic boundary section at Yangou records the integrated extinction process of the shallow marine area, which killed over 90% marine invertebrates. This study of foraminifers explores the extinction pattern and deposition progress during the Paleozoic-Mesozoic transition. In total, 39 species in 27 genera of foraminifers have been identified, including 7 species in 4 genera of fusulinids. The richness and diversity remarkably decrease at the top of Bed 21-2, marking the disappearance horizon. 4 distinct assemblages evolved within the Permian-Triassic boundary beds: the assemblages with low richness and low disparity replaced those with high richness and high disparity. The diversity and assemblage analysis exhibit a rapid decline process at the top of Bed 21-2. Whereas, the mixing of pre-extinction fauna, fusulinids, with post-extinction fauna, Hindeodus changxingensis, within the oolitic beds, implies that the fossil could be reworked to the shoal by the sea level changes. Meanwhile, the coating of foraminifers and aragonite-calcite cement around the grains indicate a catastrophic ocean with high water velocity, elevated microbes and carbonate super-saturation.
- Permian-Triassic,
- foraminifer,
- extinction,
- Yangou Section,
- paleontology

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References(69)

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Foraminiferal Evolution and Formation of Oolitic Limestone near Permian-Triassic Boundary at Yangou Section, Jiangxi Province

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