抚顺盆地中-晚始新世古植被与古气候

韦一; 杨兵; 夏浩东; 邓会娟

doi:10.3799/dqkx.2020.142

Volume 46 Issue 5

May 2021

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Wei Yi, Yang Bing, Xia Haodong, Deng Huijuan, 2021. Paleovegetation and Paleoclimate during Mid-Late Eocene in Fushun Basin. Earth Science, 46(5): 1848-1861. doi: 10.3799/dqkx.2020.142

Citation:

Wei Yi, Yang Bing, Xia Haodong, Deng Huijuan, 2021. Paleovegetation and Paleoclimate during Mid-Late Eocene in Fushun Basin. Earth Science, 46(5): 1848-1861. doi: 10.3799/dqkx.2020.142

Wei Yi, Yang Bing, Xia Haodong, Deng Huijuan, 2021. Paleovegetation and Paleoclimate during Mid-Late Eocene in Fushun Basin. Earth Science, 46(5): 1848-1861. doi: 10.3799/dqkx.2020.142

Citation:

Wei Yi, Yang Bing, Xia Haodong, Deng Huijuan, 2021. Paleovegetation and Paleoclimate during Mid-Late Eocene in Fushun Basin. Earth Science, 46(5): 1848-1861. doi: 10.3799/dqkx.2020.142

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Paleovegetation and Paleoclimate during Mid-Late Eocene in Fushun Basin

doi: 10.3799/dqkx.2020.142

Wei Yi^{1
,
,},
Yang Bing^{2
,
,
,},
Xia Haodong²,
Deng Huijuan²

1.
School of Safety Engineering, North China Institute of Science and Technology, Langfang 065201, China
2.
Cores and Samples Centre of Natural Resources, Langfang 065201, China

Received Date: 2020-06-15
Publish Date: 2021-05-15

Abstract

Abstract

For rebuilding the paleoclimate during Mid-Late Eocene in Northeast China, it analyzes the palynological characteristics in Fusun basin. Combining coniss analysis with co-existence approach, it quantitatively reconstructs the paleoclimate parameters in research area. 67 genera are identified and divided into 5 assemblages as: (Ⅰ) Quercoidites-Tricolpopollenites-Betulaceoipollenites Assemblage; (Ⅱ) Piceapollis-Tiliaepollenites-Chenopodipollis Assemblage; (Ⅲ) Quercoidites-Betulaceoipollenites-Ulmipollenites Assemblage; (Ⅳ)Pinuspollenites-Abietineaepollenites-Ephedripites Assemblage; (Ⅴ) Betulaceoipollenites-Taxodiaceaepollenites-Quercoidites Assemblage. The age of assemblages Ⅰ, Ⅱ, Ⅲ belongs to Middle Eocene, and the age of assemblages Ⅳ, Ⅴ belongs to Late Eocene. The vegetation types of the basin experienced the transformation as deciduous broadleaf forest-steppe type vegetation→coniferous and broadleaf mixed forest-steppe type vegetation→deciduous broadleaf forest-steppe type vegetation→ coniferous forest→coniferous broadleaf mixed forest. The climatic zone changed from subtropical-temperate to temperate, the humidity changed from humid to semi-humid, and the average annual moderate and annual average rainfall decreased. This trend is coupled with the global temperature trend.
- Fushun basin,
- Eocene,
- sporopollen assemblage,
- paleoclimate,
- co-existence approach,
- environmental geology

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References(46)

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Paleovegetation and Paleoclimate during Mid-Late Eocene in Fushun Basin

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