生态与环境

旧石器时代至商周时期贵州遗址空间分布及其自然环境背景

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  • 1. 南京大学地理与海洋科学学院, 南京210093;
    2. 河海大学水文水资源学院, 南京210098;
    3. 贵州省文物考古研究所, 贵阳550004
李开封(1986-),男,河南虞城人,博士研究生,研究方向为自然地理与全球变化。E-mail:henanlkf@163.com

收稿日期: 2012-09-19

  修回日期: 2012-10-18

  网络出版日期: 2013-01-20

基金资助

国家自然科学基金项目(41171163; 40971115); 南京大学研究生科研创新基金项目(2012CL02); 国家社科基金重大项目(11&ZD183); 教育部高等学校博士学科点专项科研基金项目(20090091110036)

The archaeological sites distribution and its relationship with physical environment from around 260 ka BP to 221 BC in Guizhou Province

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  • 1. School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210093, China;
    2. College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China;
    3. Guizhou Provincial Institute of Cultural Relics and Archaeology, Guiyang 550004, China

Received date: 2012-09-19

  Revised date: 2012-10-18

  Online published: 2013-01-20

Supported by

National Natural Science Foundation of China, No.41171163, No.40971115; Scientific Research Foundation of Graduate School of Nanjing University, No.2012CL02; Major Program of National Social Science Foundation of China, No. 11&ZD183; University Doctoral Foundation of China, No.20090091110036

摘要

根据对贵州230 处遗址的时空变化分析发现, 贵州旧石器时代遗址集中分布在中部、西北部和黔西南等喀斯特发育的高海拔区域。至新石器时代, 遗址仍集中分布在中部、西北部和黔西南地区, 但南部、东部等沿河地带和中西部的山间坝子开始有遗址分布。到商周时期, 遗址主要分布在沿河地带和山间坝子里。其中, 东部和南部海拔低于1000 m的地区遗址多分布在沿河地带, 而西部和北部海拔高于1000 m的地区遗址则分布在山间坝子。贵州位于亚热带湿润气候区, 气候环境的冷暖干湿波动对从事渔猎、采集及原始农业生产的古人类影响不大, 人类居住空间变化更多的与贵州特殊的自然地理背景有关, 特别是喀斯特地貌发育及适宜农业生产地方的空间差异, 对贵州旧石器至商周时期的遗址分布影响显著。旧石器时代人类以采集和渔猎为生, 临近水源的天然溶洞是人类居住的首选。随农业的出现和发展, 便于农耕的沿河地带和山间坝子成为人类的生活居住地。故新石器时代, 贵州先民居住呈现洞穴和河流阶地或山间坝子并存;至商周时期, 农业成为人类的主要经济生产方式, 人类主要居住在沿河地带和山间坝子里。

本文引用格式

李开封, 朱诚, 王鑫浩, 曹波, 赵小帆 . 旧石器时代至商周时期贵州遗址空间分布及其自然环境背景[J]. 地理学报, 2013 , 68(1) : 58 -68 . DOI: 10.11821/xb201301008

Abstract

According to temporal-spatial distribution of 230 archaeological sites in Guizhou Province, we find that Paleolithic archaeological sites were concentrated in the central, northwestern and southwestern parts of this region, which were karst area with high-altitude and many caves suitable for human settlements. In the Neolithic period, archaeological sites distribution was similar to that in the Paleolithic period, and humans began to select basins and river terraces to reside simultaneously. During the Shang and Zhou dynasties, the archaeological sites were mainly distributed in the basins and river terraces, where farming dominated the economy. Lastly, the analysis of climate change in Late Pleistocene and Holocene suggests that climate fluctuations had little impact on human settlements, when people were engaged in fishing, hunting, gathering and farming. However the distinct physical environment in Guizhou played an important role in the changes of archaeological sites distribution, especially the spatial variability of karst landforms and suitable areas for agricultural development.

参考文献

[1] Department of Geography in Guizhou Normal University. Geography of Guizhou Province. Guiyang: Guizhou People'sPublishing House, 1990. [贵州师范大学地理系. 贵州省地理. 贵阳: 贵州人民出版社, 1990.]

[2] Zhang Senshui. Outline of the Paleolithic Cultures in Guizhou Province. Journal of Guiyang Normal College: SocialSciences, 1980, (2): 1-11.[张森水. 贵州旧石器文化概论. 贵阳师院学报: 社会科学版, 1980, (2): 1-11.]

[3] Guizhou Provincial Institute of Cultural Relics and Archaeology. Fifty years of archaeological work in GuizhouProvince//Fifty Years of Archaeological Work in China. Beijing: Cultural Relics Press, 1999: 390-400. [贵州省文物考古研究所. 贵州考古五十年//新中国考古五十年. 北京: 文物出版社, 1999: 390-400.]

[4] Wu Xiaohua. The discovery and compartment of archaeological sites of Guizhou Province from the Neolithic Period tothe Shang and Zhou dynasties in recent years. Sichuan Cultural Relics, 2011, (1): 43-67. [吴小华. 近年贵州高原新石器至商周时期文化遗存的发现与分区. 四川文物, 2011, (1): 43-67.]

[5] Liu Jiaqi, Lü Houyuan, Yuan Baoyin et al. Existence of human and environmental changes. Quaternary Sciences, 1998,(1): 80-85. [刘嘉麒, 吕厚远, 袁宝印等. 人类生存与环境演变. 第四纪研究, 1998, (1): 80-85.]

[6] Zhang Zhiheng, Huang Jianqiu, Wu Jianmin. Palaeolithic Archaeology of China. Nanjing: Nanjing University Press,2003: 9-14. [张之恒, 黄建秋, 吴建民. 中国旧石器时代考古. 南京: 南京大学出版社, 2003: 9-14.]

[7] González-Sampériz P, Utrilla P, Mazo C et al. Patterns of human occupation during the early Holocene in the CentralEbro Basin (NE Spain) in response to the 8.2 ka climatic event. Quaternary Research, 2009, 71: 121-132.

[8] Zong Y, Innes J B, Wang Z et al. Environmental change and Neolithic settlement movement in the lower Yangtzewetlands of China. The Holocene, 2011, 22(6): 659-673.

[9] Xu Qizhong. Geographical changes from the archaeological sites distribution during 7000-3000 a BP in northern part ofShandong Province. Archaeology, 1992, (11): 1023-1032. [徐其忠. 从古文化遗址分布看距今七千年— 三千年鲁北地区地理地形的变迁. 考古, 1992, (11): 1023-1032.]

[10] Han Jiagu. Changes of relationship between Neolithic cultures on both sides of Hebei Plain and the legendary floods.Archaeology, 2000, (5): 57-67. [韩嘉谷. 河北平原两侧新石器文化关系变化与传说中的洪水. 考古, 2000, (5): 57-67.]

[11] Du Yun. Neolithic ashs and historical environment in the Dongting Lake area. Journal of Central China NormalUniversity: Natural Science, 2002, 36(4): 516-520. [杜耘. 洞庭湖新石器文化遗址与古环境. 华中师范大学学报: 自然科学版, 2002, 36(4): 516-520.]

[12] Zhu C, Zheng C G, Ma C M 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.

[13] Huang Run, Zhu Cheng, Zheng Chaogui. Distribution of Neolithic sites and environmental change in Huaihe RiverBasin, Anhui Province. Acta Geographica Sinica, 2005, 60(5): 742-750. [黄润, 朱诚, 郑朝贵. 安徽淮河流域全新世环境演变对新石器遗址分布的影响. 地理学报, 2005, 60(5): 742-750.]

[14] An Chengbang, Wang Lin, Ji Duxue et al. The temporal and spatial changes of Neolithic cultures in Gansu-Qinghairegion and possible environmental forcing. Quaternary Sciences, 2006, 26(6): 923-927. [安成邦, 王琳, 吉笃学等. 甘青文化区新石器文化的时空变化和可能的环境动力. 第四纪研究, 2006, 26(6): 923-927.]

[15] Zhu Cheng, Zhong Yishun, Zheng Chaogui et al. Relationship of archaeological sites distribution and environmentfrom the Paleolithic Age to the Warring States Time in Hubei Province. Acta Geographica Sinica, 2007, 62(3):227-242. [朱诚, 钟宜顺, 郑朝贵等. 湖北旧石器至战国时期人类遗址分布与环境的关系. 地理学报, 2007, 62(3):227-242.]

[16] Deng Hui, Chen Yiyong, Jia Jingyu et al. Distribution patterns of the ancient cultural sites in the middle reaches of theYangtze River since 8500 a BP. Acta Geographica Sinica, 2009, 64(9): 1113-1125. [邓辉, 陈义勇, 贾敬禹等. 8500 aBP以来长江中游平原地区古文化遗址分布的演变. 地理学报, 2009, 64(9): 1113-1125.]

[17] Wu Li, Zhu Cheng, Zheng Chaogui et al. Response of prehistoric culture to climatic environmental changes sinceHolocene in Zhejiang, East China. Acta Geographica Sinica, 2012, 67(7): 904-916. [吴立, 朱诚, 郑朝贵等. 全新世以来浙江地区史前文化对环境变化的响应. 地理学报, 2012, 67(7): 904-916.]

[18] Yuan Sixun, Chen Tiemei, Gao Shijun. Uranium series chronological sequence of some Palaeolithic sites in SouthChina. Acta Anthropologica Sinica, 1986, 5(2): 179-190. [原思训, 陈铁梅, 高世君. 华南若干旧石器时代地点的铀系年代. 人类学学报, 1986, 5(2): 179-190.]

[19] Xi Keding. Guizhou in the Stone Age. Archaeology, 1994, (8): 701-709. [席克定. 贵州的石器时代考古. 考古, 1994,(8): 701-709.]

[20] Wang Hongguang. The new discovery and new perception in archaeology of Guizhou. Archaeology, 2006, (8):3-10. [王红光. 贵州考古的新发现和新认识. 考古, 2006, (8): 3-10.]

[21] Song Xianshi. The neolith and the Neolithic Period in Guizhou Province. Journal of Guizhou Literature and History,1992, (1): 27-31, 69. [宋先世. 贵州新石器与新石器时代. 贵州文史丛刊, 1992, (1): 27-31, 69.]

[22] Zhang Herong, Luo Erhu. On the Jigongshan Culture. Archaeology, 2006, (8): 57-66. [张合荣, 罗二虎. 试论鸡公山文化. 考古, 2006, (8): 57-66.]

[23] Zhang Herong. Achievement from excavation on Shang and Zhou dynasties site at Wayao, Qingchang town in BijieCity, Guizhou Province. Journal of Guizhou Literature and History, 2010, (1): 43-47. [张合荣. 毕节青场瓦窑商周遗址发掘主要收获. 贵州文史论丛, 2010, (1): 43-47.]

[24] Li Yanyuan. Thirty years of archaeological work in Guizhou Province. Guizhou Ethnic Studies, 1979, (1): 15-25. [李衍垣. 贵州文物考古三十年. 贵州民族研究, 1979, (1): 15-25.]

[25] Zhang Herong. Economy of Guizhou from the Stone Age to the Bronze Age. Journal of Guizhou Literature andHistory, 1996, (2): 25-30. [张合荣. 贵州石器时代至青铜时代的经济. 贵州文史丛刊, 1996, (2): 25-30.]

[26] Liu Enyuan. Discussion on the origin and development of primitive agriculture in Guizhou Province. Sichuan CulturalRelics, 2005, (1): 34-39. [刘恩元. 浅谈贵州原始农业起源与发展. 四川文物, 2005, (1): 34-39.]

[27] Peng Zicheng, Zhang Zhaofeng, Cai Yanjun et al. The paleoclimatic records from the late Pleistocene stalagmite inGuizhou Qixing Cave. Quaternary Sciences, 2002, 22(3): 273-282. [彭子成, 张兆峰, 蔡演军等. 贵州七星洞晚更新世晚期石笋的古气候环境记录. 第四纪研究, 2002, 22(3): 273-282.]

[28] Yuan Daoxian, Cheng Hai, Lawrence Edwards R et al. Timing, duration, and transitions of the last interglacial Asianmonsoon. Science, 2004, 304: 575-578.

[29] Zhang Meiliang, Cheng Hai, Yuan Daoxian et al. High-resolution climate records from two stalagmites in Qixin Cave,southern Guizhou, and Heinrich events during the last glacial period. Episodes, 2004, 27(2): 112-118.

[30] Liu Qiming. The paleoclimatic records and paleoecological-paleoenvironmental meanings of stalagmite fromLiangfeng Cave in Guizhou, China [D]. Beijing: Graduate University of Chinese Academy of Sciences, 2003. [刘启明. 贵州凉风洞石笋的古气候记录与古生态环境意义. 北京: 中国科学院研究生院, 2003.]

[31] Xu Xin. A discussion on the palaeoclimate in late Pleistocene in Shuicheng area of Guizhou. Geology of Guizhou,1988, 5(1): 72-77. [徐馨. 贵州水城地区晚更新世的古气候探讨. 贵州地质, 1988, 5(1): 72-77.]

[32] Chen Peiying, Zhou Qiyong, Lin Shuji. Palaeoenvironment from 15000 a B.P. to the present in Weining County,Guizhou: A study of Nantun peat-bed section. Geology of Guizhou, 1991, 8(2): 141-152. [陈佩英, 周启永, 林树基. 贵州威宁15000 年来来的古环境: 南屯泥炭层剖面研究. 贵州地质, 1991, 8(2): 141-152.]

[33] Chen Peiying, Zhou Qiyong, Lin Shuji et al. The Pleistocene palaeovegetation and palaeoclimate of Xiaoheitu,Anshun, Guizhou. Guizhou Science, 1994, 12(2): 24-31. [陈佩英, 周启永, 林树基等. 贵州安顺小黑土晚更新世古植被和古气候. 贵州科学, 1994, 12(2): 24-31.]

[34] Qiao Yulou, Chen Peiying, Shen Caiming et al. Quantitative reconstruction of vegetation and climate of Fanjingshansection in Guizhou during last 10000 years. Geochimica, 1996, 25(5): 445-447. [乔玉楼, 陈佩英, 沈才明等. 定量重建贵州梵净山一万年以来的植被与气候. 地球化学, 1996, 25(5): 445-457.]

[35] Song Xianshi. A journey of semicentury: A review on the achievements of Guizhou archaeology during 50 years.Social Sciences in Guizhou, 2005, (6): 152-153, 161. [宋先世. 半个世纪的征程: 贵州考古学50 年成就评述. 贵州社会科学, 2005, (6): 152-153, 161.]

[36] Li Zongfa. Division of karst landform in Guizhou. Guizhou Geology, 2011, 28(3): 177-181, 234. [李宗发. 贵州喀斯特地貌分区. 贵州地质, 2011, 28(3): 177-181, 234.]

[37] Zhou Bisu. The distribution and transmission of Neolithic culture in Southwest China, and their relationships withgeographical environment. Journal of Guizhou Literature and History, 1998, (1): 79-83. [周必素. 西南地区新石器时代文化的分布、传播与地理环境的关系. 贵州文史丛刊, 1998, (1): 79-83.]

[38] Zhang Chi. The emerged time of agriculture in South China and Southwest China and related problems. Relics fromSouth, 2009, (3): 64-71. [张弛. 华南和西南地区农业出现的时间及相关问题. 南方文物, 2009, (3): 64-71.]

[39] Li Yingfu, Chen Fang. Archaeological cultures during Shang and Zhou dynasties in Wujiang River valley surveyedfrom Qingyuan Site. Archaeology, 2010, (5): 79-91. [李映福, 陈芳. 从清源遗址看乌江流域商周时期的考古学文化.考古, 2010, (5): 79-91.]

[40] Sun Hua. A discussion on the Bronze culture in eastern Yunnan and western Guizhou: Taking Zhaotong of Yunnan andBijie of Guizhou as the center. Sichuan Cultural Relics, 2007, (5): 12-25. [孙华. 滇东黔西青铜文化初论: 以云南昭通及贵州毕节地区的考古材料为中心. 四川文物, 2007, (5): 12-25.]
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