| Analysis of sedimentary-geomorphologic variation and the living environment of hominids at the Shuidonggou Paleolithic site | |
| Gao Xing1; Yuan BaoYin2; Pei ShuWen1; Wang HuiMin3; Chen FuYou1; Feng XingWu1; Xing, G (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China. | |
| 2008-07-01 | |
| 发表期刊 | CHINESE SCIENCE BULLETIN
 |
| ISSN | 1001-6538 |
| 卷号 | 53期号:13页码:2025-2032 |
| 文章类型 | Article |
| 摘要 | Shuidonggou is one of the most important Upper Paleolithic sites in North China. Due to the presence of rich human remains, animal fossils, abundant sporopollen and unique geological sequence, it is the type site for Late Pleistocene to Holocene human occupation and environmental change in the Ningxia-Inner Mongolia region. Many scholars suggest that the site should be named the "Shuidonggou Formation" of Late Pleistocene in North China. Dating results indicate that ancient human activities at the site took place 30-24 ka (Marine Isotope Stage [MIS] 3). The climate at that time was warmer and moister than present day, and adequate precipitation led to the formation of water pack depressions where broad-leaf trees and sparse forest vegetations, as well as herbivorous animals flourished, making the area suitable for early human hunting, gathering and survival. The Neolithic human occupation happened 9-5 ka at the site, while similar environmental conditions with MIS3 occurred. The absence of human activity record in the region during the Last Glacial Maximum (MIS2) suggests that the environment was too harsh for humans to live there.; Shuidonggou is one of the most important Upper Paleolithic sites in North China. Due to the presence of rich human remains, animal fossils, abundant sporopollen and unique geological sequence, it is the type site for Late Pleistocene to Holocene human occupation and environmental change in the Ningxia-Inner Mongolia region. Many scholars suggest that the site should be named the "Shuidonggou Formation" of Late Pleistocene in North China. Dating results indicate that ancient human activities at the site took place 30-24 ka (Marine Isotope Stage [MIS] 3). The climate at that time was warmer and moister than present day, and adequate precipitation led to the formation of water pack depressions where broad-leaf trees and sparse forest vegetations, as well as herbivorous animals flourished, making the area suitable for early human hunting, gathering and survival. The Neolithic human occupation happened 9-5 ka at the site, while similar environmental conditions with MIS3 occurred. The absence of human activity record in the region during the Last Glacial Maximum (MIS2) suggests that the environment was too harsh for humans to live there. |
| 关键词 | Shuidonggou Late Paleolithic Paleoenvironment Shuidonggou Formation |
| WOS标题词 | Science & Technology |
| URL | 查看原文 |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS研究方向 | Science & Technology - Other Topics |
| WOS类目 | Multidisciplinary Sciences |
| WOS记录号 | WOS:000257327400016 |
| 引用统计 | |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://119.78.100.205/handle/311034/3231 |
| 专题 | 古人类及旧石器研究室 |
| 通讯作者 | Xing, G (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China. |
| 作者单位 | 1.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 3.Inst Archeol Ningxia Hui Autonomous Reg, Yinchuan 750001, Peoples R China |
| 推荐引用方式 GB/T 7714 | Gao Xing,Yuan BaoYin,Pei ShuWen,et al. Analysis of sedimentary-geomorphologic variation and the living environment of hominids at the Shuidonggou Paleolithic site[J]. CHINESE SCIENCE BULLETIN,2008,53(13):2025-2032. |
| APA | Gao Xing.,Yuan BaoYin.,Pei ShuWen.,Wang HuiMin.,Chen FuYou.,...&Xing, G .(2008).Analysis of sedimentary-geomorphologic variation and the living environment of hominids at the Shuidonggou Paleolithic site.CHINESE SCIENCE BULLETIN,53(13),2025-2032. |
| MLA | Gao Xing,et al."Analysis of sedimentary-geomorphologic variation and the living environment of hominids at the Shuidonggou Paleolithic site".CHINESE SCIENCE BULLETIN 53.13(2008):2025-2032. |
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