吐哈盆地中二叠世古气候重建：来自木化石年轮的证据

魏信祥; 张雄华; 黄兴; 栾腾飞

doi:10.3799/dqkx.2016.525

Volume 41 Issue 10

Oct. 2016

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Article Navigation > Earth Science > 2016 > 41(10): 1771-1780

Wei Xinxiang, Zhang Xionghua, Huang Xing, Luan Tengfei, 2016. Palaeoclimate Reconstruction of Middle Permian in Tuha Basin: Evidence from the Fossil Wood Growth Rings. Earth Science, 41(10): 1771-1780. doi: 10.3799/dqkx.2016.525

Citation:

Wei Xinxiang, Zhang Xionghua, Huang Xing, Luan Tengfei, 2016. Palaeoclimate Reconstruction of Middle Permian in Tuha Basin: Evidence from the Fossil Wood Growth Rings. Earth Science, 41(10): 1771-1780. doi: 10.3799/dqkx.2016.525

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Palaeoclimate Reconstruction of Middle Permian in Tuha Basin: Evidence from the Fossil Wood Growth Rings

doi: 10.3799/dqkx.2016.525

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Jiangxi Nuclear Industry Geological Bureau Testing Center, Nanchang 330002, China

Received Date: 2016-03-22
Publish Date: 2016-10-03

Abstract

Abstract

The collection of fossil wood growth rings data is helpful for rebuilding paleoclimate. Based on the statistical analysis of fossil wood growth rings from Middle Permian Taerlang Formation in the northeast edge of Tuha basin, the paleoclimate evolution of Middle Permian is reconstructed for the first time. The analysis of fossil wood growth rings shows that this area was subject to north subtropical climate with obvious seasonal variations during the Middle Permian. The paleoclimate was relatively warm, but intermittent hot climate had occurred. The low percentage of latewood and the abrupt transition between earlywood and latewood of some growth rings reflect that the seasonal variations were very obvious during the period of trees' growth. The paleoclimate was prevailed by a subtropical monsoon climate with hot and humid summer and dry and cold winter. The relatively high mean sensitivity (MS average of 0.4) of fossil woods indicates that trees were influenced by monsoon climate during the growth period, and the environment was very unstable with uneven annual precipitation. The change of consecutive growth ring width and the existence of false rings implies that the climate changed frequently and generally was humid with arid and semi-arid fluctuations.
- Tuha basin,
- Middle Permian,
- fossil wood,
- growth rings,
- climatology

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References(68)

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Palaeoclimate Reconstruction of Middle Permian in Tuha Basin: Evidence from the Fossil Wood Growth Rings

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