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The depositional Environment at Shuidonggou Locality 2 in Northwest China at similar to 72-18 kaBP
Liu Decheng; Gao Xing; Liu Enfa; Pei Shuwen; Chen Fuyou; Zhang Shuqin; gaoxing@ivpp.ac.cn
2012
发表期刊ACTA GEOL SIN-ENGL
ISSN1000-9515
卷号86期号:6页码:1539—1546
摘要Shuidonggou site has abundant Paleolithic remains of Late Pleistocene deposition. Studying the evolution of depositional environments is essential to the comprehensive understanding of the living conditions of ancient populations. To reconstruct the depositional environment at Shuidonggou, we carried out archaeological excavations and collected systematic deposition samples at the key position of Shuidonggou Locality 2 for grain size analysis and sporopollen statistics. The environmental evolution around the Shuidonggou site generally underwent four stages at similar to 7218 kaBP. During the first stage (similar to 7241 kaBP), the river developed with gravel and sand stratums. During the second stage (41 similar to 34 kaBP), a swamp with numerous aquatic plants formed. In the third stage (34-29 kaBP), site formation was characterized by shallow lake depositional conditions; the climate was relatively warm and humid. The marginal bank depositional conditions deteriorated during the fourth stage (29-18 kaBP), and the site underwent several dry events; the climate also became drier and colder.
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收录类别SCI收录
WOS记录号WOS:000313494000022
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文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/4233
专题中科院古脊椎所(2000年以后)
古人类及旧石器研究室
通讯作者gaoxing@ivpp.ac.cn
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GB/T 7714
Liu Decheng,Gao Xing,Liu Enfa,et al. The depositional Environment at Shuidonggou Locality 2 in Northwest China at similar to 72-18 kaBP[J]. ACTA GEOL SIN-ENGL,2012,86(6):1539—1546.
APA Liu Decheng.,Gao Xing.,Liu Enfa.,Pei Shuwen.,Chen Fuyou.,...&gaoxing@ivpp.ac.cn.(2012).The depositional Environment at Shuidonggou Locality 2 in Northwest China at similar to 72-18 kaBP.ACTA GEOL SIN-ENGL,86(6),1539—1546.
MLA Liu Decheng,et al."The depositional Environment at Shuidonggou Locality 2 in Northwest China at similar to 72-18 kaBP".ACTA GEOL SIN-ENGL 86.6(2012):1539—1546.
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