Environmental change since mid-Pleistocene recorded in Shangshan achaeological site of Zhejiang
文献类型：期刊论文
| 作者 | Mao Longjiang1; Mo Duowen1; Jiang Leping2; Jia Yaofeng3,4; Liu Xiaoyan; Li Minglin1; Zhou Kunshu5; Shi Chenxi1 |
| 刊名 | JOURNAL OF GEOGRAPHICAL SCIENCES
 |
| 出版日期 | 2008-05-01 |
| 卷号 | 18期号:2页码:247-256 |
| 关键词 | environmental change reticulate red clay TL/OSL dating mid-Pleistocene Shangshan culture Zhejiang |
| ISSN号 | 1009-637X |
| DOI | 10.1007/s11442-008-0247-6 |
| 文献子类 | Article |
| 英文摘要 | At about 173 ka BP of the late period of mid-Pleistocene, the second terrace of the river had been formed as a result of uplift happening in Shangshan area because of the climate, sea level change and tectonic action. Between 173-75 ka BP, aeolian deposited on the terrace, a layer of reticulate red clayey soil about 80-100 cm thick deposited and developed under the warmer and higher temperature. In the last glacial period, the drop of the temperature and the decrease of the precipitation induced the dust-storms increased, A layer of Xiashu loess about 1.0-1.5 m thick accumulated on Shangshan terrace in the last glacial, which has the reticulate red clayey soil buried. At the beginning of the Holocene (11500 a BP-), temperature went higher gradually and precipitation got more, the pre-persons moved on the Shangshan terrace (11,400-8600 a BP), which is one of the most important archaeological sites, and can connect the paleolithic culture with Neolithic culture. It could be assumed from the results that the lower reaches of the Yangtze River are the home of rice cultivation, too. The lower place to the west of the Shangshan site experienced the two cycles process of the fluvial facies and the lacustrine facies, indicating that the water source of the pre-historical Shangshan is the river water or lake water. Two AIVIS (14)C age proved the water source disappeared more than 1000 years ago. |
| WOS关键词 | PLATEAU ; CHINA |
| WOS研究方向 | Physical Geography |
| 语种 | 英语 |
| WOS记录号 | WOS:000254970800011 |
| 出版者 | SCIENCE PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/69602]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Mao Longjiang |
| 作者单位 | 1.Peking Univ, Coll Urban & Environm Sci, Beijing 100871, Peoples R China 2.Zhejiang Prov Inst Cultural Rel & Archaeol, Hangzhou 310014, Peoples R China 3.Shaanxi Normal Univ, Dept Tourism & Environm, Xian 710062, Peoples R China 4.Hengyang Normal Univ, Dept Resources Environm & Tourism, Hengyang 421008, Peoples R China 5.CAS, Inst Geol & Geophys, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Mao Longjiang,Mo Duowen,Jiang Leping,et al. Environmental change since mid-Pleistocene recorded in Shangshan achaeological site of Zhejiang[J]. JOURNAL OF GEOGRAPHICAL SCIENCES,2008,18(2):247-256. |
| APA | Mao Longjiang.,Mo Duowen.,Jiang Leping.,Jia Yaofeng.,Liu Xiaoyan.,...&Shi Chenxi.(2008).Environmental change since mid-Pleistocene recorded in Shangshan achaeological site of Zhejiang.JOURNAL OF GEOGRAPHICAL SCIENCES,18(2),247-256. |
| MLA | Mao Longjiang,et al."Environmental change since mid-Pleistocene recorded in Shangshan achaeological site of Zhejiang".JOURNAL OF GEOGRAPHICAL SCIENCES 18.2(2008):247-256. |
入库方式： OAI收割
来源：地质与地球物理研究所
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