Skip to main content
Log in

Paleo-environmental changes in the Yangtze Delta during past 8000 years

  • Landforms And Earth Surface Processes
  • Published:
Journal of Geographical Sciences Aims and scope Submit manuscript

Abstract

The Yangtze Delta is one of the economically most developed areas in China. It is located in the eastern China monsoon region. Archaeological excavations and environment-archaeology studies over many years in this region provide exceptional information about climate changes, development of human civilization and also human-environment interactions. Archaeological excavations made in the study region reveal that the development of Neolithic cultures is not continuous, which may be a result of extreme climatic events. The analysis of14C-dated buried paleotrees, peat and shell ridges show the rise and fall of human civilization in the study area. The research results presented in this paper confirm that human civilization collapsed six times in the Yangtze Delta, matching six high sea level epoches, peat accumulation and buried paleotrees formation periods respectively. This indicates that human activities in the Yangtze Delta are controlled by local climate changes and changing hydrological conditions. The collapse of the Liangzhu culture (5000 aBP-3800 aBP) in about 4000 aBP, after a tremendous flooding event, followed by a relatively backward Maqiao culture (3800 aBP-3200 aBP) confused researchers and aroused their great interest. The research results in this paper show that the collapse of the Liangzhu culture is a result of several factors, for example war and food shortage, but the flooding event occurred in the late Liangzhu culture epoch is the main factor therein.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Beck J W, Recy J, Taylor Fet al., 1997. Abrupt changes in early Holocene tropical sea surface temperature derived from coral records.Nature, 385: 705–707.

    Article  Google Scholar 

  • Bender M, Sowers T, Dicksonn Met al., 1994. Climate correlations between Greenland and Antarctica during the past 100,000 years.Nature, 372: 663–666.

    Article  Google Scholar 

  • Curtis J H, Hodell D A, Brenner M, 1996. Climate variability on the Yucatan Peninsula (Mexico) during the past 3500 years, and implication for Maya cultural evolution.Quaternary Research, 46: 37–47.

    Article  Google Scholar 

  • Daniel J S, Chen Z Y, 1996. Neolithic settlement distribution as a function of sea level controlled topography in the Yangtze Delta, China.Geology, 12: 1083–1086.

    Google Scholar 

  • Federico V, Alfredo A, Marcelo Fet al., 1999. Subantarctic macrotidal flats, cheniers and beaches in San Sebastian Bay, Tierra Del Fuego, Argentina.Marine Geology, 160: 301–326.

    Article  Google Scholar 

  • Hodell D A, Curtis J H, Brenner M, 1995. Possible role of climate in the collapse of Classic Maya civilization.Nature, 375: 391–394.

    Article  Google Scholar 

  • Huang X P, 1984. Further analysis on the Neolithic culture in the Taihu lake region.Study on Prehistorical, 3: 14–21. (in Chinese)

    Google Scholar 

  • Jing C Y, 1989. Development of Neolithic and middle Neolithic human culture and environment in the Taihu Plain.Journal of Nanjing Normal University (Natural Science Version), 3: 81–87. (in Chinese)

    Google Scholar 

  • Jordan J W, Mason O K, 1999. A 5000 year record of intertidal peat stratigraphy and sea level change from northwest Alaska.Quaternary International, 60: 37–47.

    Article  Google Scholar 

  • Liu C, Wu L, Cao M, 1985. Sedimentary characteristics, formation and chronology of shell ridges on the Yangtze Delta.Acta Oceanologica Sinica, 7: 55–66. (in Chinese)

    Google Scholar 

  • Lynn O, 1990. Peat accumulation in northern wetlands.Quaternary Research, 33: 377–386.

    Article  Google Scholar 

  • Mason O K, 1990. Beach Ridge Geomorphology of Kotzebue Sound: Implications or Paleoclimatology and Archeology. PhD Dissertation, University of Alaska, 262.

  • Meese D A, Gow A J, Grootes Pet al., 1994. The accumulation record from the GISP2 core as an indicator of climate change throughout the Holocene.Science, 266: 1680–1682.

    Article  Google Scholar 

  • Ni H, Ji L, 1997. Environment changes and the formation of the lake systems in the Yangchenghu lake region from the Neolithic sites.Lake Science, 1: 35–40. (in Chinese)

    Google Scholar 

  • Obrien S R, Mayewski P A, Meeker L Det al., 1995. Complexity of Holocene climate as reconstructed from a Greenland ice core.Science, 270: 1962–1964.

    Article  Google Scholar 

  • Oertel G F, Kraft J C, Kearney M Set al., 1992. A rational theory for barrier-lagoon development. In: Quaternary Coasts of the United States: Marine and Lacustrine Systems. Society of Economic Paleontologists and Mineralogists (SEPM Special Publication No. 48), 77–87.

  • Ovenden L, 1990. Peat accumulation in northern wetlands.Quaternary Research, 33: 377–386.

    Article  Google Scholar 

  • Psuty N P, 1966. The geomorphology of beach ridges in Tabasco. Louisiana State Univ. Coastal Studies Inst. Techn. Report, No.30, 51.

  • Stuiver M, Reimer P J, 1993. Extended14C data base and revised Calib 3.014C age calibration program.Radiocarbon, 215–230.

  • Wu G T, 1994. Relics study in the Changshu region. Suzhou: Guwuxuan Publishing House, 23–30. (in Chinese)

    Google Scholar 

  • Wu J, 1988. Distribution of the prehistoric sites and environment changes on the Yangtze Delta.Southeastern Cultures, 6: 16–35. (in Chinese)

    Google Scholar 

  • Yang H R, Xie Z R, Yang D Y, 1987. Formation and evolution of the Taihu Lake and the Holocene sea level. In: Collection of the Quaternary Glaciation and Quaternary Geology. Beijing: Publishing House of Geology, 49–64. (in Chinese)

    Google Scholar 

  • Yu S, Zhu C, Song Jet al., 2000. Role of climate in the rise and fall of Neolithic cultures on the Yangtze Delta.Boreas, 29: 157–165.

    Article  Google Scholar 

  • Zhang Q, Zhu C, 2001. Environmental evolution since the late Pleistocene on the North Bank of the Yangtze River.Scientia Geographica Sinica, 21(6): 87–91. (in Chinese)

    Google Scholar 

  • Zhang S, Yan Q, Guo X, 1982. Shell ridges on the coastal plain of Shanghai.Journal of East China Normal University (Natural Science Edition), 3: 81–93. (in Chinese)

    Google Scholar 

  • Zhang X Y, Cai S M, Sun S C, 1994. Evolution of the Dongting Lake since the Holocene.Lake Science, 1: 13–21. (in Chinese)

    Google Scholar 

  • Zheng X, 1999. Aeolian sediment and environment in the Yangtze Delta and the ocean region. Shanghai: Publishing House of East China Normal University, 1–50. (in Chinese)

    Google Scholar 

  • Zhou H, Zheng X M, 2000. Role of environment changes on prehistorical human civilization: taking the collapse of Liangzhu culture in the north part of the Changjiang delta plain as an example.Journal of East China Normal University (Natural Science Version), 4: 71–77. (in Chinese)

    Google Scholar 

  • Zoltai S C, Vitt D H, 1990. Holocene climatic change and the distribution of peatlands in western interior Canada.Quaternary Research, 33: 231–240.

    Article  Google Scholar 

  • Zou H B, 2000. 50-year Archaeology of the Jiangsu Province. Nanjing: Jiangsu Publishing House, 71–90. (in Chinese)

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Zhang Qiang.

Additional information

Foundation item: Knowledge Innovation Project of CAS, No.KZCX3-SW-331; National Natural Science Foundation of China, No. 40271112

Author: Zhang Qiang (1974–), Ph.D., specialized in the Yangtze floods and climatic changes.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Zhang, Q., Jiang, T., Shi, Y. et al. Paleo-environmental changes in the Yangtze Delta during past 8000 years. J. Geogr. Sci. 14 (Suppl 1), 105–112 (2004). https://doi.org/10.1007/BF02873097

Download citation

  • Received:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02873097

Key words

Navigation