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Study on Environmental Change from 200 to 80K a B.P. in Hanyuan Sichuan Province from Lacustrine Deposits Record
Author: MengLi
Tutor: ZhangJianPing
School: Chinese Geology University (Beijing)
Course: Paleontology and stratigraphy
Keywords: Hanyuan areas Particle size analysis Environmental evolution Cause Analysis
CLC: P512.2
Type: Master's thesis
Year: 2009
Downloads: 64
Quote: 2
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Abstract
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Lake fishing village to the big trees the town of Sichuan Hanyuan placed sedimentary section as the research object , through rock stratigraphy , geomorphology , sedimentology method , combined with field recording , will be the profile roughly divided into 8 stages of deposition , three cycles of period large trees placed fish profile sedimentary stratigraphic sequence . The average grain size characteristics derived median diameter for 18.12μm, mostly clay , silt , fine sand interbedded . Layering and sorting , the frequency curve showed the bimodal characteristics , the little thick tail ; the Daihai , Xifeng loess , of Xuancheng river sediment particle size distribution and particle size parameters Comparison found Daihai the lake sediments , loess and river sediments significantly different , distinguish the genetic types of sediments and sedimentary environment , namely the large trees placed the fish profile main semi- deep lake - deep lake lake sediments , some lacustrine lake sediments . Large trees placed fish profiles basic achieve 1cm/100a resolution of stratigraphic and sedimentological studies analyzed by high-precision age . Deposition time of approximately 206.74 ~ 80.55 KaBP, formed during the late Middle Pleistocene to Late Pleistocene interim . The push to establish a large tree swing the fish profile high-resolution chronostratigraphic sequence by interpolation and outside . Large trees placed the fish section in the value of the particle size and magnetic susceptibility were positively correlated with Color L was negatively correlated . High school median particle size and magnetic susceptibility values ??, low L value indicates a the precipitation more warm and humid climate and environment ; low median particle size and magnetic susceptibility values ??, high L value indicates less precipitation warm and dry or cool and dry climate and environment . 200 ~ 80 KaBP Hanyuan paleoclimate eight stage of the process is divided into three periods : ( 1) Countdown to the second interglacial final (206.74 ~ 190.32 ka BP) mainly in warm, arid climate and environment ; ( 2 ) reciprocal second Ice Age (190.32 ~ 133.00 KaBP), mainly to cool and wet climate , sandwiched between a cool dry period ; (3) the last interglacial (133.00 ~ 80.55 ka BP) is warm and humid and warm dry fluctuate significantly climate and environment is mainly dominated by warm and humid climate . The Hanyuan precipitation is mainly controlled by changes in the intensity of solar radiation under the influence of the Indian monsoon . As for the temperature change is consistent with global climate change . But the Hanyuan the environment indicators record with them is not fully synchronized or consistent , reflect regional climate characteristics .
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CLC: > Astronomy,Earth Sciences > Geology > Dynamic geology > External force > Denudation,handling the role of the deposition
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