Climate and Environmental Change

Transmutation of ancient settlements and environmental changes between 6000?2000 aBP in the Chaohu Lake Basin, East China

  • 1. School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210093, China;
    2. College of Territorial Resources and Tourism, Anhui Normal University, Wuhu 241000, Anhui, China;
    3. Center for Earth Observation and Digital Earth, CAS, Beijing 100190, China;
    4. Institute of Geology and Geophysics, CAS, Beijing 100029, China;
    5. College of Urban and Environmental Sciences, Peking University, Beijing 100871, China;
    6. Department of Urban Construction and Environment Science, West Anhui University, Lu&rsquo|an 237012, Anhui, China

Received date: 2009-06-06

  Revised date: 2009-11-20

  Online published: 2010-10-15

Supported by

Major Program of Natural Science Research at University of Anhui Province, No.ZD200908; National Science and Technology Support Program, No.2010BAK67B02; National Natural Science Foundation of China, No.41010104005; No.40971115


Based on the temporal-spatial distribution features of ancient settlement sites from the middle and late Neolithic Age to the Han dynasty in the Chaohu Lake Basin of Anhui Province, East China, using the methods of GIS combined with the reconstructed paleoenvironment by the records of lake sediment since Holocene, the transmutation of ancient settlements with response to environmental changes in this area has been discussed. Studies show that the main feature of transmutation of ancient settlements from the middle and late Neolithic Age to the Han Dynasty was that the distribution of settlements in this area changed from high altitudes to low ones and kept approaching the Chaohu Lake with the passage of time. These could be the response to the climate change from warm-moist to a relatively warm-dry condition during the middle Holocene, leading to the lake level fluctuations. The large area of exposed land provided enough space for human activities. These indicate that the above changes in geomorphologic evolution and hydrology influenced by climate conditions affected the transmutation of ancient settlements greatly. The distribution pattern of settlement sites was that the number of sites in the west was more than in the east. This pattern may be related to the geomorphologic conditions such as frequent channel shifting of the Yangtze River as well as flood disasters during the Holocene optimum. Therefore, climate change was the inducement of the transmutation of ancient settlements in the Chaohu Lake Basin, which exerted great influence on the distribution, expansion and development of the ancient settlements.

Cite this article

WU Li, WANG Xinyuan, ZHOU Kunshu, MO Duowen, ZHU Cheng, GAO Chao, ZHANG Guangsheng, LI Lan, LIU Li, HAN Weiguang . Transmutation of ancient settlements and environmental changes between 6000?2000 aBP in the Chaohu Lake Basin, East China[J]. Journal of Geographical Sciences, 2010 , 20(5) : 687 -700 . DOI: 10.1007/s11442-010-0804-7


[1] Alam A M, Xie S C, Wallis L A, 2009. Reconstructing late Holocene palaeoenvironments in Bangladesh: Phytolith analysis of archaeological soils from Somapura Mahavihara site in the Paharpur area, Badalgacchi Upazila, Naogaon District, Bangladesh. Journal of Archaeological Science, 36: 504–512.

[2] Anhui Provincial Institute of Cultural Relics and Archaeology, 2006. Lingjiatan. Beijing: Cultural Relics Publishing House. (in Chinese)

[3] Chen E H, 2002. Study on cultural characteristics of Chaohu Lake Basin on Pre-Qin Period. Journal of Chaohu College, 4(4): 25–30. (in Chinese)

[4] WU Li et al.: Transmutation of ancient settlements and environmental changes between 6000-2000 aBP 699 Chorography Compiling Commission of Anhui Province, 1998. Anhui Chorography: Relic. Beijing: Chronicles Press. (in Chinese)

[5] Chorography Compiling Commission of Anhui Province, 1999. Anhui Chorography: Natural Environment. Beijing: Chronicles Press. (in Chinese)

[6] Chorography Compiling Commission of Chaohu City, 1992. Chaohu Chorography. Hefei: Huangshan Publishing House. (in Chinese)

[7] Chu K C, 1973. A preliminary study on the climatic fluctuations during the last 5,000 years in China. Scientia Sinica, 16(2): 226–256.

[8] Cui Z J, Yang X Y, Xia Z K, 2002. Evolution of ancient culture types and regional differentiation of their propagation and succession models: a preliminary study. Quaternary Sciences, 22(5): 434–441. (in Chinese)

[9] Dou H S, Jiang J H, 2003. The Five Major Freshwater Lakes in China. Hefei: University of Science and Technology of China Press, 38–39. (in Chinese)

[10] Fan B, Xu S Y, Yu L Z et al., 2006. Phytolith in the sediment of the Lake Chaohu since Middle Holocene and its paleoenvironmental implications. Journal of Lake Sciences, 18(3): 273–279. (in Chinese)

[11] Fletcher R, 2008. Some spatial analyses of Chalcolithic settlement in Southern Israel. Journal of Archaeological Science, 35: 2048–2058.

[12] Gao H Z, Zhu C, Xu W F, 2007. Environmental change and cultural response around 4200 cal. yr BP in the Yishu River Basin, Shandong. Journal of Geographical Sciences, 17(3): 285–292.

[13] Gu W W, Zhu C, 2005. Distribution feature of Neolithic sites in North Jiangsu Province and environmental archaeological research on its relation with environmental variation. Scientia Geographica Sinica, 25(2): 239–243. (in Chinese)

[14] Hajar L, Boustani M H, Khater C et al., 2009. Environmental changes in Lebanon during the Holocene: Man vs. climate impacts. Journal of Arid Environments, xxx: 1–10.

[15] Han M L, Liu X Q, Fang C et al., 2007. The explanation of the selection of settlement and environment in the Western Liaohe River Valley during the middle Holocene epoch. Acta Geographica Sinica, 62(12): 1287–1298. (in Chinese)

[16] Haug G H, Güther D, Peterson L C et al., 2003. Climate and the collapse of Maya civilization. Science, 299: 1731–1735.

[17] Hoelzmann P, Keding B, Berke H et al., 2001. Environmental change and archaeology: Lake evolution and human occupation in the Eastern Sahara during the Holocene. Palaeogeography, Palaeoclimatology, Palaeoecology, 169: 193–217.

[18] Hou G L, Liu F G, Xiao L B et al., 2008. The transmutation of settlements of prehistoric cultures in eastern Qinghai caused by climate change. Acta Geographica Sinica, 63(1): 34–40. (in Chinese)

[19] Huang R, Zhu C, Guan Y et al., 2006. Impact of Holocene environmental change on temporal-spatial distribution of Neolithic sites in Huaihe River Basin, Anhui Province. Journal of Geographical Sciences, 16(2): 199–208.

[20] Jia T F, Dai X R, Zhang W G et al., 2006. Sediment records in Chaohu Lake and its significance on environmental change in Holocene. Scientia Geographica Sinica, 26(2): 706–711. (in Chinese)

[21] Jing Z C, 1991. Outline of environmental archaeology in western countries. In: Zhou K S. Research of Environmental Archaeology Vol.1. Beijing: Science Press, 35–40. (in Chinese)

[22] Li L, Zhu C, Lin L G et al., 2008. Transgression records between 7500–5400BC on the Stratum of the Luotuodun Site in Yixing, Jiangsu Province. Acta Geographica Sinica, 63(11): 1189–1197. (in Chinese)

[23] Mao L J, Mo D W, Jiang L P et al., 2008. Environmental change since mid-Pleistocene recorded in Shangshan archaeological site of Zhejiang. Journal of Geographical Sciences, 18(2): 247–256.

[24] Polyak V J, Asmerom Y, 2001. Late Holocene climate and cultural changes in the southwestern United States. Science, 294: 148–151.

[25] Qian Y C, 2007. Study on Beishantou burials at Chaohu City. Journal of Chaohu College, 9(1): 69–73. (in Chinese)

[26] Rua H, 2009. Geographic information systems in archaeological analysis: A predictive model in the detection of rural Roman villae. Journal of Archaeological Science, 36: 224–235.

[27] Sampériz P G, Utrilla P, Mazo C et al., 2008. Patterns of human occupation during the Early Holocene in the Central Ebro Basin (NE Spain) in response to the 8.2 ka climatic event. Quaternary Research, xxx: 1–12.

[28] Shao X H, Wang Y J, Cheng H et al., 2006. Long-term trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite δ 18O record from Shennongjia in Central China. Chinese Science Bulletin, 51(2): 221–228.

[29] Shi W, Ma C M, Zhu C et al., 2008. Analysis of stratigraphy on multi-profiles in the Taihu Lake region and paleoenvironmental events in the Liangzhu culture epoch. Geographical Research, 27(5): 1129–1138. (in Chinese)

[30] Tang L Y, Shen C M, Zhao X T et al., 1993. Vegetation and climate since Holocene based on Qingfeng Section, Jianhu, Jiangsu Province. Science in China (Series B), 23(6): 637–643. (in Chinese)

[31] Wang J, 2007. Lingjiatan: One of the areas where Chinese ancient civilization was born. Jianghuai Culture and History, 6: 14–33. (in Chinese)

[32] Wang X Y, He H, Qian Y C et al., 2005. An inference of ancient Juchao City based on environmental archaeology. Journal of Anhui Normal University (Natural Science), 28(1): 56–59. (in Chinese)

[33] Wang X Y, Mo D W, Wu L et al., 2008a. Pollen record from Chaohu Lake in the lower reaches of the Changjiang River and environmental changes since 9870 cal. aB.P. Quaternary Sciences, 28(4): 649–658. (in Chinese)

[34] Wang X Y, Wu L, Zhang G S et al., 2008b. Characteristics and environmental significance of magnetic susceptibility and grain size of lake sediments since Holocene in Chaohu Lake, Anhui Province. Scientia Geographica Sinica, 28(4): 548–553. (in Chinese)

[35] Wang X Y, Zhang G S, Wu L et al., 2008c. Environmental changes during early-middle Holocene from the sediment record of the Chaohu Lake, Anhui Province. Chinese Science Bulletin, 53(suppl. 1): 153–160.

[36] Wei S S, 1999. Study on the Ancient Chao State. Hefei: Anhui Science & Technology Publishing House, 18–21. (in Chinese)

[37] Wu L, Wang X Y, Zhang G S et al., 2008. Vegetation evolution and climate change since the Holocene recorded by pollen-charcoal assemblages from lacustrine sediments of Chaohu Lake in Anhui Province. Journal of Palaeogeography, 10(2): 183–192. (in Chinese)

[38] Yan W M, 1997. The settlement archaeology and research of prehistory. Cultural Relics, 6: 27–35. (in Chinese)

[39] Yang L X, 2000. Discovery and study on the Prehistory Jade in Anhui Province. Cultural Relic Research, 12: 14–24. (in Chinese)

[40] Zhang H Y, 2003. An introduction to the Prehistoric Archaeology in China. Beijing: Higher Education Press. (in Chinese)

[41] Zheng C G, Zhu C, Zhong Y S et al., 2008. Relationship between the temporal-spatial distribution of archaeological sites and natural environment from the Paleolithic Age to the Tang and Song dynasties in the Three Gorges Reservoir of Chongqing area. Chinese Science Bulletin, 53(suppl. 1): 107–128.

[42] Zhu C, Ma C M, Zhang W Q et al., 2006. Pollen record from Dajiuhu Basin of Shennongjia and environmental changes since 15.753kaB.P. Quaternary Sciences, 26(5): 814–826. (in Chinese)

[43] Zhu C, Zheng C G, Ma C M et al., 2003. On the Holocene sea-level highstand along the Yangtze Delta and Ningshao Plain, East China. Chinese Science Bulletin, 48(24): 2672–2683.

[44] Zhu C, Zhong Y S, Zheng C G et al., 2007. Relationship of archaeological sites distribution and environment from the Paleolithic Age to the Warring States Time in Hubei Province. Acta Geographica Sinica, 62(3): 227–242. (in Chinese)

[45] Zhu G Y, Zhu C, Ling S J et al., 2005. Spatial-temporal distribution of Neolithic and Xia-Shang–Zhou dynasties sites and relationship between human and environment in Anhui Province. Scientia Geographica Sinica, 25(3): 346–352. (in Chinese)