Relationship of Archaeological Sites Distr ibution and Environment from the Paleolithic Age to the Warring States Time in Hubei Province

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  • 1. School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210093, China;
    2. Department of Geography, Chuzhou College, Chuzhou 239012, China

Received date: 2006-12-25

  Revised date: 2007-01-16

  Online published: 2007-03-25

Supported by

The Key Project of the National Natural Science Foundation of China, No.90411015; University Doctoral Foundation of China, No.20050284011; Open Foundation of the State Key Laboratory of Loess and Quaternary Geology from the Institute of Earth Environment, CAS, No.SKLLQG0503; Physical Geography of "985" Item and Foundation of Modern Analyses Center of Nanjing University

Abstract

1362 archaeological sites from the Paleolithic age to the Warring States time in Hubei Province increase gradually from west to east and from high to low. The number of Paleolithic sites with altitudes of 50-500 m account for 78% of the total, while 71%-95% of the sites from the Neolithic age to the Warring States time are distributed at the areas of 0-200 m. The temporal-spatial distribution of archeological sites in this area is mainly affected by two factors. For one thing, the human beings of every age need to choose the first on the second terrace as living sites which are near to the water source and are easy to withstand flood. Additionally, since downcutting of rivers can form new river valley and lateral erosion and accumulation of river in stable time of tectonic movement can result in gathering of many new terraces. So, the human beings migrated to adapt to the change of terrace location, which led to the number of sites increasing gradually in the lower areas of the central and eastern parts of this province. For other things, the temporal-spatial distribution of archeological sites in this area is affected by the climate condition. The Paleolithic sites are distributed mostly in the Hanjiang River Basin in northeastern Shiyan, southeast of Jingzhou and east of Jinmen, which is because rivers were distributed in higher areas in this period. During Chengbeixi cultural period, the sites are rare in the quondam Paleolithic sites distribution area, but manifold obviously along the Yangtze River near the southwest Yichang contrarily. The pollen record of Dajiuhu Lake indicates that only 23 Chengbeixi cultural sites may be related to more precipitation and flood during the Holocene wet and hot period. Daxi Culture, Qujialing Culture and Shijiahe Culture are corresponding to middle and top of the Dajiuhu pollen Zone IV, during which the climate is in order as a whole and is propitious to agricultural development. In the Qujialing Culture period, 32 of the former 34 Daxi Cultural sites disappeared, while 90 sites increase abruptly in the higher highlands in the north of Xiangfan-Jinmen-Xiaogan, which may respect with enlarging of water areas. Chu Culture period is corresponding to Dajiuhu pollen Zone V, which is warm and dry Holocene phase, but it seems that the climate condition is propitious to agricultural cultivation and the number of archeological sites increases heavily to 593. In addition, there are the least archaeological sites in the lake areas of the southeast Hubei Province because of low-lying topography with altitudes of 1-50 m and severest flood.

Cite this article

ZHU Cheng, ZHONG Yishun, ZHENG Chaogui, MA Chunmei, LI Lan . Relationship of Archaeological Sites Distr ibution and Environment from the Paleolithic Age to the Warring States Time in Hubei Province[J]. Acta Geographica Sinica, 2007 , 62(3) : 227 -242 . DOI: 10.11821/xb200703001

References


[1] ICSU. Dark nature: Rapid natural change and human responses. http://www.brunel.ac.uk/depts/geo/people/suzanneleroy. html, 2003.

[2] UNESCO. The role of Holocene environmental catastrophes in human history, IGCP 490. For details of the Mauritania meeting, January 2004. http://www.brunel.ac.uk/depts/geo/igcp490/igcp490home.html.

[3] 朱诚, 于世永, 卢春成. 长江三峡及江汉平原地区全新世环境考古与异常洪涝灾害研究. 地理学报, 1997, 52(3): 268-277.
[Zhu Cheng, Yu Shiyong, Lu Chuncheng. The study of Holocene environmental archaeology and extreme flood disaster in the Three Gorges of the Changjiang River and the Jianghan Plain. Acta Geographica Sinica, 1997, 52 (3): 268-277.]

[4] 国家文物局主编. 中国文物地图集·湖北分册(上). 西安: 西安地图出版社, 2002. 1-17.
[State Administration of Cultural Heritage. Cultural Relics Maps of China·Hubei Province (superior). Xi'an: Map Press of Xi'an, 2002. 1-17.]

[5] 张绪球. 屈家岭文化. 北京: 文物出版社, 2004. 2-147.
[Zhang Xuqiu. Qujialing Culture. Beijing: Cultural Relic Press, 2004. 2-147.]

[6] 王红星. 长江中游地区新石器时代遗址分布规律、文化中心的转移与环境变迁的关系. 江汉考古, 1998, (1): 53-61.
[Wang Hongxing. Relationship of the Nieolithic sites distribution, transfer of cultural centers and environment evolution in the middle reaches of the Yangtze River. Jianghan Archaeology, 1998, (1): 53-61.]

[7] 夏正楷, 邓辉, 武弘麟. 内蒙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.
[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.]

[8] 周卫健, 卢雪峰, 武振坤等. 若尔盖高原全新世气候变化的泥炭记录与加速器放射性碳测年. 科学通报, 2001, 46 (12): 1040-1044.
[Zhou Weijian, Lu Xuefeng, Wu Zhengkun et al. Peat record reflecting Holocene climatic change in the ZoigêPlateau and AMS radiocarbon dating. Chinese Science Bulletin, 2002, 47(1): 66-70.]

[9] Stuiver M, Reimer P J, Bard E et al. INTCAL98 radiocarbon age calibration 24,000~0 cal BP. Radiocarbon, 1998, 40: 1041-1083.

[10] Stuiver M, Reimer P J, Reimer R W. CALIB 5.0, 2005.
[WWW program and documentation, 2005.]

[11] Bronk Ramsey C. Radiocarbon calibration and analysis of stratigraphy: The OxCal Program. Radiocarbon, 1995, 37(2) 425-430.

[12] Bronk Ramsey C. Development of the Radiocarbon Program OxCal. Radiocarbon, 2001, 43(2A): 355-363.

[13] 刘兴起, 沈吉, 王苏民等. 青海湖16ka 以来的花粉记录及其古气候古环境演化. 科学通报, 2002, 47 (17): 1351-1355.
[Liu Xingqi, Shen Ji, Wang Sumin et al. A 16000-year pollen record of Qinghai Lake and its paleo-climate and paleoenvironment. Chinese Science Bulletin, 2002, 47(22): 1931-1936.]

[14] 沈吉, 刘兴起, Matsumoto R 等. 旧石器时代以来青海湖沉积物多指标高分辨率的古气候演化. 中国科学(D 辑), 2004, 34(6): 582-589.
[Shen Ji, Liu Xingqi, Matsumoto Ryo et al. A high-resolution climatic change since the Late Glacial Age inferred from multi-proxy of sediments in Qinghai Lake. Science in China (Series D), 2005, 4 (6): 742-751.]

[15] 覃嘉铭, 袁道先, 程海等. 新仙女木及全新世早中期气候突变事件: 贵州茂兰石笋氧同位素记录. 中国科学(D 辑), 2004, 34(1): 69-74.
[Qin Jiaming, Yuan Daoxian, Cheng Hai et al. The Y. D. and climate abrupt events in the early and middle Holocene: Stalagmite oxygen isotope record from Maolan, Guizhou, China. Science in China (Series D): 2005, 48(4): 530-537.]

[16] 邵晓华, 汪永进, 程海等. 全新世季风气候演化与干旱事件的湖北神农架石笋记录. 科学通报, 2006, 51(1): 80-86.
[Shao Xiaohua, Wang Yongjin, Cheng Hai et al. Long-term trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite δ18O record from Shennongjia in Central China. Chinese Science Bulletin, 2006, 51 (2): 221-228.]

[17] 朱诚, 马春梅, 张文卿等. 神农架大九湖15.753kaB.P. 以来的孢粉记录和环境演变. 第四纪研究, 2006, 26(5): 814-826.
[Zhu Cheng, Ma Chunmei, Zhang Wenqing et al. Pollen record and environmental changes since 15.753 kaB. P. from Dajiuhu Basin of Shennongjia, China. Quaternary Sciences, 2006, 26(5): 814-826.]

[18] Zhu Cheng, Zheng Chaogui, Ma Chunmei et al. On the Holocene sea-level highstand along the Yangtze Delta and Ningshao Plain, East China. Chinese Science Bulletin, 2003, 48(24): 2672-2683.

[19] 徐海, 洪业汤, 林庆华. 红原泥炭纤维素氧同位素指示的距今6ka 温度变化. 科学通报, 2002, 47(15): 1181-1186.
[Xu Hai, Hong Yetang, Lin Qinghua et al. Temperature variations in the past 6000 years inferred from δ18O of peat cellulose from Hongyuan, China. Chinese Science Bulletin, 2002, 4(18): 1578-1584.]

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