The Explanation of the Selection of Settlement and Environment in the Western Liaohe River Valley during the Middle Holocene Epoch

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  • 1. College of Urban and Environmental Sciences of Peking University, Beijing 100871, China;
    2. School of Geoscience and Space Science of Peking University, Beijing 100871, China

Received date: 2007-03-12

  Revised date: 2007-07-02

  Online published: 2007-12-25

Supported by

National Natural Science Foundation of China, No.40471031

Abstract

The paper focuses on the environmental explanation of the selection of settlement sites belonging to different types of archaeological culture in the middle Holocene Epoch, Western Liaohe River Valley. Through Chi-square Test, the authors point out that the settlements in the target region were mainly distributed in the sloping field of 400-500 m above sea level and the distribution presents spatial and temporal changes. The settlements in 8000-6000 a BP concentrated on the sloping field of 400-500 m above sea level. The settlements in 6000-3000 a BP were extending from the core area of 400-500 m above sea level to the higher and lower directions. While showing the preference of the height of 400-500 m above sea level, the settlements in the Western Liaohe River Valley in the middle Holocene Epoch demonstrated a horizontal amassment in the sloping field 10-40 m away from the riverbed. From the environmental explanation of the selection of settlement sites belonging to different types of archaeological culture, the paper gets three main findings: 1) the Western Liaohe River Valley could be divided into two parts, the woodland and the grassland, according to the style of living of the people. The periphery of the woodland is the living space of the people 8000-6000 a BP, when gathering, fishing and hunting were the main life style. The grassland is the main distribution area of primitive agriculture. 6000-3000 a BP is the vital period for the development of primitive agriculture, during which the settlements had a trend expanding from the periphery of woodland to the grassland. The sequence of the settlement sites defines the spatial and regional features of environment. 2) Though the Holocene Epoch experienced a prominent warming period, the animal and vegetation resources were far from abundant, restricted by the zonality constraints of the Western Liaohe River Valley. The living resources reserves could only afford the living of the people in 8000-6000 a BP when the population density was very low. In 6000-3000 a BP, the growth of population had exceeded the environmental capacity of this area. To fulfill the survival requirement, primitive agriculture was developing gradually and new man-land relationship was established. 3) Using thickness of the cultural sediments to analyze the continuance of the settlements in the middle Holocene Epoch, the paper points out that the population density then was much sparser than modern times. Considering the environmental capacity and population density, agriculture cultivation in the middle Holocene Epoch did not cause significant environmental disturbance.

Cite this article

HAN Maoli, LIU Xiaoquan, FANG Chen, ZHANG Yi, LI Qingmiao, ZHAO Yuhui . The Explanation of the Selection of Settlement and Environment in the Western Liaohe River Valley during the Middle Holocene Epoch[J]. Acta Geographica Sinica, 2007 , 62(12) : 1287 -1298 . DOI: 10.11821/xb200712005

References


[1] Chang Kwang-chih. Rethinking Archaeology. New York: Random House, 1967. 32-48.

[2] Xia Zhengkai, Deng Hui, Wu Honglin. Geomorphologic background of the prehistoric cultural evolution in the Xar Moron River Basin, Inner Mongolia. Acta Geographica Sinica, 2000, 55(3): 329-336.
[夏正楷, 邓辉, 武弘麟. 内蒙古西 拉木伦河流域考古文化演变的地貌背景分析. 地理学报, 2000, 55(3): 329-336.]

[3] Guo Dashun. Hongshan Wenhua. Beijing: Cultural Relics Publishing House, 2005. 20-25.
[郭大顺. 红山文化. 北京: 文 物出版社, 2005. 20-25.]

[4] The Chifeng International Collaborative Archeological Research Project. Regional Archeology in Eastern Inner Mongolia: A Methodological Exploration. Beijing: Science Press, 2003. 26-36.
[赤峰中美联合考古项目. 内蒙古东部(赤峰) 区域 考古调查阶段性报告. 北京: 科学出版社, 2003. 26-36.]

[5] Liu Guoxiang. A preliminary probing into the settlement pattern of Xing Long Wa Culture. Archaeology and Cultural Relics, 2001, (6): 58-67.
[刘国祥. 兴隆洼文化聚落初探. 考古与文物, 2001, (6): 58-67.]

[6] Kong Zhaochen, Du Naiqiu. Reports on plants of Xinglongwa cultural remains in Aohan Banner of Inner Mongolia. Archaeology, 1985, (10): 873-874.
[孔昭辰, 杜乃秋. 内蒙古敖汉旗兴隆洼遗址植物的初步报告. 考古, 1985, (10): 873-874.]

[7] Jane Mcintosh. How We Know What We Know about the Past. New York: The Paul Press Ltd., 1986. 156-157.

[8] Chen Chun. Theory and Research on Archeology. Shanghai: Academia Press, 2003. 227-237.
[陈淳. 考古学的理论与研 究. 上海: 学林出版社, 2003. 227-237.]

[9] Shi Yafeng, Kong Zhaochen, Wang Sumin. Basic Features of Climatis and Environments during Holocene Megathermal in China. Shi Yafeng (ed.). The Climates and Environments of Holocene Megathermal in China. Beijing: China Ocean Press, 1992. 1-18.
[施雅风, 孔昭辰, 王苏民. 中国全新世大暖期气候与环境的基本特征. 见: 施雅风主编. 中国全新 世大暖期气候与环境. 北京: 海洋出版社, 1992. 1-18.]

[10] Qiu Shanwen, Li Qusheng, Xia Yumei. Paleosoil and Holocene environment in the sandy land of Northeast China. In: Shi Yafeng (ed.). The Climates and Environments of Holocene Megathermal in China. Beijing: China Ocean Press, 1992. 153-160.
[裘善文, 李取生, 夏玉梅. 东北西部沙地古土壤与全新世环境. 见: 施雅风主编. 中国全新世大暖期 气候与环境. 北京: 海洋出版社, 1992. 153-160.]

[11] The Chifeng International Collaborative Archeological Research Project Regional Archeology in Eastern Inner Mongolia: A Methodological Exploration. Beijing: Science Press, 2003. 62-72, 178.
[赤峰中美联合考古项目. 内蒙古 东部(赤峰) 区域考古调查阶段性报告. 北京: 科学出版社, 2003. 62-72, 178.]

[12] The Chifeng International Collaborative Archeological Research Project Regional Archeology in Eastern Inner Mongolia: A Methodological Exploration. Beijing: Science Press, 2003. 100.
[赤峰中美联合考古项目. 内蒙古东部 (赤峰) 区域考古调查阶段性报告. 北京: 科学出版社, 2003. 100.]

[13] Cohan M N. The Food Crisis in Prehistory: Over Population and the Origin of Agriculture. New Haven: Yale University Press, 1977. 18-70.

[14] MacNeish R S. Reflections on my search for the beginning of agriculture in Mexico. In: Willey G R (ed.). Archaeological Research in Retrospect. Cambridge, Masssachusetts: Winthrop Publishing Inc., 1974. 207-234.

[15] Kong Zhaochen, Du Naiqiu, Xu Qinghai. Paleoclimatic Fluctuation Reflected in Flora of Holocene Megathermal in the Northern Part of China. In: Shi Yafeng (ed.). The Climates and Environments of Holocene Megathermal in China. Beijing: China Ocean Press, 1992. 48-65.
[孔昭辰, 杜乃秋, 许清海. 中国北方全新世大暖期植物群的古气候波动. 见: 施雅风主编. 中国全新世大暖期气候与环境. 北京: 海洋出版社, 1992. 48-65.

[16] Wu Jihua, Zheng Xinsheng. A Preliminary Probe on the Transition of Soil and Vegetation in the Recent 8000 Years in the Overlapping Belt of Agriculture and Stockbreeding, North China. Zhang Lansheng (ed.). Environmental Changing and Predicting in North China's Overlapping Belt of Agriculture and Stockbreeding in Holocene Epoch. Beijing: Geological Publishing House, 1992. 55-70.
[武吉华, 郑新生. 中国北方农牧交错带(赤峰市沙区) 8000 年来土壤和 植被演变初探. 见: 张兰生主编. 中国北方农牧交错带全新世环境演变及预测. 北京: 地质出版社, 1992. 55-70.

[17] State Administration of Culture Heritage (ed.). The Atlas of the Cultural Relics in the Inner Mongolia. Xi'an: Xi'an Maps Press, 2003. 112-131.
[国家文物局主编. 中国文物地图集·内蒙古自治区分册. 西安: 西安地图出版社, 2003. 112-131.]

[18] Han Maoli. Distribution of settlements and environmental choices in the Xila Mulun River Valley and its neighborhood during the Liao Dynasty. Acta Geographica Sinica, 2004, 59(4): 543-549.
[韩茂莉. 辽代西拉木伦河流域及毗邻地区 聚落分布与环境选择. 地理学报, 2004, 59(4): 543-549.]

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