河南省史前人类遗址的时空分布及其驱动因子

doi:10.11821/dlxb201311008

Abstract

Abstract: Based on the ArcGis10.0 platform, this article analyzed the geographic indexes of prehistoric human sites in the Yangshao Cultural Period (approx. 6.9-6.0 ka BP) and in the Longshan Cultural Period (approx. 4.6-4.0 ka BP) in Henan, i.e. spatial distribution, river-orientation, spatial agglomeration etc. Results showed that 18.8% of the sites in Yangshao period are distributed within 1 km river-buffer area, while there were 16.5% in Longshan period, indicating that human activity in Longshan period became weaker at river-orientation. In contrast to the Yangshao period, spatial agglomeration indexes of the western part of Henan, Nanyang Basin and Yinghe-and-Huaihe river basin respectively increased by 0.006, 0.016 and 0.021, which suggested that human activity in Longshan-period was restricted by natural environment. At 4.0 ka BP, Henan was subjected to the cooling events, accompanied by natural disasters such as drought, flood and low temperature, which accelerated the spread of human activities. At that time, the exotic cultures such as Shijiahe and Dawenkou expanded into Henan and complicated the spatial-temporal patterns of human activities.

Key words: Yangshao cultural sites, Longshan cultural sites, Henan province, paleo-environment evolution, time-spatial distribution

LI Zhongxuan, ZHU Cheng, WU Guoxi, ZHENG Chaogui, SHAO Shixun, FENG Feifan, WANG Ning. Spatial and temporal distribution of prehistoric human sites and its driving factors in Henan province[J].Acta Geographica Sinica, 2013, 68(11): 1527-1537.

References

[1] Hou Guangliang, Liu Fenggui. Impact of climate changes on prehistoric cultures in East Qinghai. Acta Geographica Sinica, 2004, 59(6): 841-846.[侯光良, 刘峰贵. 青海东部史前文化对气候变化的响应. 地理学报, 2004, 59(6): 841-846.]
[2] Liu Fenggui, Hou Guangliang, Zhang Yili et al. Impact of abrupt climate change on prehistoric culture in Northeast Qinghai. Acta Geographica Sinica 2005, 60(5): 733-741.[刘峰贵, 侯光良, 张镱锂等. 中全新世气候突变对青海东北部史前文化的影响. 地理学报, 2005, 60(5): 733-741.]
[3] Li Yiyiin, Cui Haiting, Hu Jinming. Analysis for ecological background of ancient civilization in Xiliaohe River Basin. Quaternary Sciences, 2003, 23(3): 291-298.[李宜垠, 崔海亭, 胡金明. 西辽河流域古代文明的生态背景分析. 第四纪研究, 2003, 23(3): 291-298.]
[4] 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.
[5] Gao Huazhong, Zhu Cheng, Xu Weifeng. Environmental change and cultural response around 4200 cal. yr BP in the Yishu River Basin, Shandong. Journal of Geographical Sciences, 2007, 17(3): 285-289.
[6] Zheng C G, Zhu C, Zhong Y S et al. Relationship between natural environment and time-spatial distribution of the archaeological sites in the reservoir area of Chongqing from Paleolithic Age to the Tang-Song Dynasty. Chinese Science Bulletin, 2008, 53(Suppl.1): 102-114.
[7] Deng Hui, Chen Yiyong, Jia Jingyu. Evolution of paleo-culture distribution in mid-stream plain of Yangtze River since 8500 aBP. Acta Geographica Sinica, 2009, 64(9): 1113-1125.[邓辉, 陈义勇, 贾敬禹. 8500aBP 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.]
[8] Wu Li, Zhu Cheng, Zheng Chaogui et al. Response of prehistoric culture to climate environmental changes since Holocene in Zhejiang, East China. Acta Geographica Sinica, 2012, 67(7): 903-916.[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): 903-916.]
[9] Zhang Juzhong. Dynamic reflecting on lineage of Neolithic cultures in middle and lower reaches of Yellow River. Zhongyuan Cultural Relics, 2006, (6): 18-25.[张居中. 黄河中下游地区新石器时代文化谱系的动态思考. 中原文物, 2006, (6): 18-25.]
[10] State Administration of Cultural Heritage. An Atlas of Chinese Cultural Relics in Henan Province. Beijing: Cultural Relics Press, 2009.[国家文物局. 中国文物地图集·河南分册. 北京: 文物出版社, 2009.]
[11] Li Shuicheng. Regional comparison: Environment and evolution of settlements. Archaeology and Cultural Relics, 2002, (6): 33-38.[李水城. 区域对比: 环境与聚落的演进. 考古与文物, 2002, (6): 33-38.]
[12] Zhu Kezhen. A preliminary study on climate change in China since last 5000a. Science in China, 1973, 16(2):226-256.[竺可桢. 中国近五千年来气侯变迁的初步研究. 中国科学, 1973, 16(2): 226-256.]
[13] Shi Yafeng, Kong Zhaochen, Wang Sumin et al. The Holocene Megathermal climate in China and its characteristics// Shi Yafeng, Kong Zhaochen et al. Climate and Environment in Megathermal Period of Holocene in China. Beijing: China Ocean Press, 1992: 1-18.[施雅风, 孔昭宸, 王苏民等. 中国全新世大暖期气候与环境的基本特征//施雅风, 孔昭宸. 中国全新世大暖期气候与环境. 北京: 海洋出版社, 1992: 1-18.]
[14] Wang Shaowu, Huang Jianbin. Drought-flood change and process of Chinese culture in the mid-Holocene. Advance of Natural Sciences, 2006, 16(10): 1238-1244.[王绍武, 黄建斌. 全新世中期的旱涝变化与中华文明的进程. 自然科学进展, 2006, 16(10): 1238-1244.]
[15] Dong Guanghui, Xia Zhengkai, Liu Decheng et al. Influence of human activity during the period of cultural origin on soil chemical properties in Mengjin, Henan. Journal of Lanzhou University: Natural Science Edition, 2007, 43(1): 6-10.[董广辉, 夏正楷, 刘德成等. 文明起源时期河南孟津地区人类活动对土壤化学性质的影响. 兰州大学学报: 自然科学版, 2007, 43(1): 6-10.]
[16] Guo Zhiyong, Zhai Qiumin, Shen Juan. Paleo-climate change recorded by lake deposits in the Mianchi Basin of the middle reach of Yellow River. Quaternary Sciences, 2011, 31(1): 150-163.[郭志永, 翟秋敏, 沈娟. 黄河中游渑池盆地湖泊沉积记录的古气候变化及其意义. 第四纪研究, 2011, 31(1): 150-163.]
[17] Cao Wen, Xia Zhengkai. Measurement of the dissolvable salts in the mid-Holocene lake sediments of Mengjin, Henan. Acta Scientiarum Naturalium Universitatis Pekinensis, 2008, 44(6): 933-937.[曹雯, 夏正楷. 河南孟津寺河南中全新世湖泊沉积物的易溶盐测定及其古水文意义. 北京大学学报: 自然科学版, 2008, 44(6): 933-937.]
[18] He Zhong, Huang Chunchang, Zhou Jie et al. Holocene Loess and its deposition dynamics in the upper reaches of the Huaihe River. Journal of Desert Research, 2010, 30(4): 816-823.[何忠, 黄春长, 周杰等. 淮河上游全新世黄土及其沉积动力系统研究. 中国沙漠, 2010, 30(4): 816-823.]
[19] Li Shengli, Huang Chunchang, Pang Jiangli. Records of Holocene sandstorm activity in the Yellow River floodplain. Acta Sedimentologica Sinica, 2008, 26(1): 144-150.[李胜利, 黄春长, 庞奖励. 黄河泛滥平原全新世沙尘暴活动的历史记录. 沉积学报, 2008, 26(1): 144-150.]
[20] Bond G, Kromer B, Beer J et al. Persistent solar influence on North Atlantic climate during the Holocene. Science, 2001, 294: 2130-2136.
[21] Cullen H M, de Menocal P B, Hemming S et al. Climate change and the collapse of the Akkadian Empire: Evidence from the deep sea. Geology, 2000, 28(4): 379-382.
[22] Bond G, Showers W, Cheseby M et al. A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science, 1997, 278: 1257-1266.
[23] Yao Tandong, Shi Yafeng. Holocene climate changes recorded by the Dunde ice core in the Qilian Mountain//Shi Yafeng, Kong Zhaochen et al. Climate and Environment in Megathermal Period of Holocene in China. Beijing: China Ocean Press, 1992: 206-211.[姚檀栋, 施雅风. 祁连山敦德冰芯记录的全新世气候变化//施雅风, 孔昭宸. 中国全新世大暖期气候与环境. 北京: 海洋出版社, 1992: 206-211.]
[24] Xu Hai, Hong Yetang, Lin Qinghua et al. Temperature change since last 6 ka revealed by oxygen isotope of mud sediments. Chinese Science Bulletin, 2002, 47(15): 1181-1186.[徐海, 洪业汤, 林庆华等. 红原泥炭氧同位素指示的距今6ka温度变化. 科学通报, 2002, 47(15): 1181-1186.]
[25] Shao Xiaohua, Wang Yongjin, Cheng Hai et al. Holocene monsoon change and the dry events recorded by stalagmite. Chinese Science Bulletin, 2006, 51(1): 80-86.[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.]
[26] Liang Liang, Xia Zhengkai, Liu Decheng. Reconstruction of the paleo-environment in central North China during 5000aBP to 4000aBP: Evidence from mollusks fossil. Acta Scientiarum Naturalium Universitatis Pekinensis, 2003, 39 (4): 532-537.[梁亮, 夏正楷, 刘德成. 中原地区距今5000-4000 年间古环境建的软体动物化石证据. 北京大学学报: 自然科学版, 2003, 39(4): 532-537.]
[27] North Greenland Ice Core Project Members. High-resolution record of Northern Hemisphere climate extending into the last interglacial period. Nature, 2004, 431: 147-151.
[28] WangY J, Cheng H, Lawrence Edwards R et al. The Holocene Asian Monsoon: Links to solar changes and North Atlantic climate. Science, 2005, 308: 854-857.
[29] Kong Zhaochen, Liu Changjiang, Zhang Juzhong. Discovery of plant remains in the Neolithic site at the Bancun site, Mianchi County, Henan Province and their significance in human environment. Acta Anthropologica Sinica, 1999, 18 (4): 291-295.[孔昭宸, 刘长江, 张居中. 渑池班村新石器遗址植物遗存及其在人类环境学上的意义. 人类学报, 1999, 18(4): 291-295.]
[30] Kong Zhaochen, Liu Changjiang, Zhang Juzhong. Discovery of 8 kaBP rice remains unearthed in Jiahu of Wuyang County and its anthropological significance. Archaeology, 1996, (12): 78-83.[孔昭宸, 刘长江, 张居中. 河南舞阳县贾湖遗址八千年前水稻遗存的发现及其在环境考古学上的意义. 考古, 1996, (12): 78-83.]
[31] Zhang Juzhong, Yin Ruochun, Yang Yuzhang et al. Rice-farming archaeological investigation in mid-reaches of the Huaihe River. Agricultural Archaeology, 2003, (3): 84-91.[张居中, 尹若春, 杨玉璋等. 淮河中游地区稻作农业考古调查报告. 农业考古, 2003, (3): 84-91.]
[32] Kong Zhaochen, Liu Changjiang, Zhang Juzhong et al. Plant remains of archaeological sites in China and primitive agriculture. Zhongyuan Cultural Relics, 2003, (2): 4-13.[孔昭宸, 刘长江, 张居中等. 中国考古遗址植物遗存与原始农业. 中原文物, 2003, (2): 4-13.]
[33] Zhao Zhijun. A study of agricultural economy during 2500 B.C.-1500B.C.//Institute of Archaeology, CASS. Sci-Tech Archaeology: Volume Ⅱ. Beijing: Science Press, 2007: 1-11.[赵志军. 公元前2500 年-公元前1500 年中原地区农业经济研究//中国社科院考古所. 科技考古: 第二辑. 北京: 科学出版社, 2007: 1-11.]
[34] Henan Meteorological Network. http://www.henanqx.gov.cn/public/climate/16154.html.[河南气象网. http://www. henanqx.gov.cn/public/climate/16154.html.]
[35] Zhang Xuelian, Qiu Shihua, Bo Guancheng et al. Analysis of human bone ¹³C, ¹⁵N in the Erlitou Site and Taosi Site// Institute of Archaeology, CASS. Sci-Tech Archaeology: Volume Ⅱ. Beijing: Science Press, 2007: 41-48.[张雪莲, 仇士华, 薄官成等. 二里头遗址、陶寺遗址部分人骨碳十三、氮十五分析//中国社科院考古所. 科技考古: 第二辑. 北京: 科学出版社, 2007: 41-48.]
[36] Wu Wenxiang, Hu Ying, Zhou Yang. Climate abrupt change and ancient cultural fall. Journal of Paleogeography, 2009, 11(4): 455-463.[吴文祥, 胡莹, 周扬. 气候突变与古文明衰落. 古地理学报, 2009, 11(4): 455-463.]
[37] Wu Xihao, An Zhisheng, Wang Sumin et al. Time-spatial evolution of East Asia monsoon in the Holocene optimum period, China. Quaternary Sciences, 1994, (1): 24-37.[吴锡浩, 安芷生, 王苏民等. 中国全新世气候适宜期东亚季风时空变迁. 第四纪研究, 1994, (1): 24-37.]

Spatial and temporal distribution of prehistoric human sites and its driving factors in Henan province

PDF (PC)

Like

Knowledge

Cited

Abstract

Cite this article

share this article

References

Related Articles 8

Metrics

Comments

[1]	ZHAO Jianji, WANG Yanhua, WANG Jue, MIAO Changhong. The spatial spillover effects of prefectural cities on county's industrial structure during the "province governing county" reform [J]. Acta Geographica Sinica, 2020, 75(2): 286-301.
[2]	LI Xiaojian, ZHOU Xiongfei, WEI Chunjiang, KONG Yunfeng. Locational Changes of Banking Services in the Less Developed Region of China since 1980: The Case of Henan Province [J]. Acta Geographica Sinica, 2006, 61(4): 414-424.
[3]	QIAN Huaisui, REN Yuyu, Li Mingxia. Changes of Cotton Climate Risk Degree in Henan Province [J]. Acta Geographica Sinica, 2006, 61(3): 319-326.
[4]	LIANG Guofu, DING Shengyan. Changes of Landscape Patterns along the Yellow River in Henan Province from 1987 to 2002 [J]. Acta Geographica Sinica, 2005, 60(4): 665-672.
[5]	DING Shengyan, LIANG Guofu. Landscape Pattern Change of Regional Wetland along the Yellow River in Henan Province in the Last Two Decades [J]. Acta Geographica Sinica, 2004, 59(5): 653-661.
[6]	LI Xiaojian. The Role of Rural Household Behavior in Economic Development of Less Developed Rural Area: a Case Study of Western Henan Mountainous and Hilly Region, China [J]. Acta Geographica Sinica, 2002, 57(4): 459-468.
[7]	Zhou Shouming, Liu Baosui. GEOCHEMICAL CHARACTERISTICS OF RARE EARTHELEMENTS IN THE SOILS OF HENAN PROVINCE [J]. Acta Geographica Sinica, 1989, 44(4): 478-486.
[8]	Sun Dexiang. CONTENT AND DISTRIBUTION OF TRACE ELEMENTS IN SOILS OF HENAN PROVINCE [J]. Acta Geographica Sinica, 1988, 43(1): 79-87.