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Geochemistry Records of Palaeoenvironment from Sanfangwan Neolithic Site in Jianghan Plain, Central China

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Proceedings of the 2012 International Conference on Information Technology and Software Engineering

Part of the book series: Lecture Notes in Electrical Engineering ((LNEE,volume 211))

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Abstract

The culture of Qujialing (5100-4500 cal. a BP) is a representative of Chinese civilization in the Jianghan Plain, middle reaches of the Yangtze River. Nevertheless, limited geochemical data are available on this prehistoric culture in relation to environment in this region. In this study, geochemical records on TOC, TN, C/N ratio and δ 13C extracted from sludge sediments of unit T1610 profile at the Sanfangwan Neolithic site of late Qujialing period (4800-4500 cal. a BP) were integrated to clarify the palaeoenvironment, palaeoecology and human activities during the late Holocene in the Jianghan Plain. The results suggest that palaeo-environment changes in the Sanfangwan site went through three stages (i.e. warm and humid → mild and slightly wet → relatively warm and humid) during the late Qujialing period. C3 plants occupied most parts around the studied area. An overall warm and humid climate around the Sanfangwan site resulted in the establishment of a more stable and predominantly C3 plant forest ecosystems, which have provided effective protections against human impact and climate change and substantively push the development of agriculture that led to the Qujialing culture flourishing. During this period, the emergence of rammed earthen walls and moats of the Sanfangwan site might mark the inception of the Chinese civilization in the Jianghan Plain, middle reaches of the Yangtze River. The geochemical records of palaeoenvironment evolution from the Sanfangwan Neolithic site are in good accordance with those of adjacent area. It responded to regional environmental change of the middle Yangtze River.

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References

  1. Stuiver M (1975) Climate versus changes in 13C content of the organic component of lake sediments during the Late Quaternary. Quat Res 5(2):251–262

    Article  Google Scholar 

  2. Boutton TW, Archer SR, Midwood AJ, Zitzer SF (1998) δ 13C values of soil organic carbon and their use in documenting vegetation change in a subtropical savanna ecosystem. Geoderma 82(1–3):5–41

    Article  Google Scholar 

  3. Shen J, Wang Y, Liu XQ, Matsumoto R (2006) A 16 ka climate record deduced from δ13C and C/N ratio in Qinghai Lake sediments, northeastern Tibetan Plateau. Chin J Oceanol Limnol 24(2):103–110

    Article  Google Scholar 

  4. Lu HY, Zhou YL, Liu WG, Mason J (2012) Organic stable carbon isotopic composition reveals late Quaternary vegetation changes in the dune fields of northern China. Quat Res 77(3):433–444

    Article  Google Scholar 

  5. Cerling TE, Quade J, Wang Y, Bowman JR (1989) Carbon isotopes in soils and palaeosols as ecology and palaeoecology indicators. Nature 341:138–139

    Article  Google Scholar 

  6. Zhong W, Xue JB, Cao JX, Zheng YM, Ma QH, Ouyang J, Cai Y, Zeng ZG, Liu W (2010) Bulk organic carbon isotopic record of lacustrine sediments in Dahu Swamp, eastern Nanling Mountains in South China: implication for catchment environmental and climatic changes in the last 16,000 years. J Asian Earth Sci 38:162–169

    Article  Google Scholar 

  7. Zhou B, Zheng HB, Yang WG, Wei GJ, Li L, Wang H (2011) Organic carbon records since the last glacial period in the Northern South China Sea sediments: implications for vegetation and environmental changes. Quat Sci 31(3):498–505

    Google Scholar 

  8. Zhou B, Shen CD, Zheng HB, Zhao MX, Sun YM (2009) Vegetation evolution on the central Chinese Loess Plateau since late Quaternary evidenced by elemental carbon isotopic composition. Chin Sci Bull 54(12):2082–2089

    Article  Google Scholar 

  9. Hogan CM (2011) Respiration. In: McGinley M (ed) Encyclopedia of earth. National Council for Science and the Environment, Washington

    Google Scholar 

  10. Ma CM, Zhu C, Zheng CG, Wu CL, Guan Y, Zhao ZP, Huang LY, Huang R (2008) High-resolution geochemistry records of climate changes since late-glacial from Dajiuhu peat in Shennongjia Mountains, Central China. Chin Sci Bull 53(Supp. I):28–41

    Google Scholar 

  11. Shen J, Liu XQ, Matsumoto R, Wang SM, Yang XD (2005) A high-resolution climatic change since the Late Glacial Age inferred from multi-proxy of sediments in Qinghai Lake. Sci China, Ser D Earth Sci 48(6):742–751

    Article  Google Scholar 

  12. Jiang QF, Shen J, Liu XQ, Zhang EL, Xiao XY (2007) A high-resolution climatic change since Holocene inferred from multi-proxy of lake sediment in westerly area of China. Chin Sci Bull 52(14):1970–1979

    Article  Google Scholar 

  13. Shen J, Liu XQ, Wang SM, Matsumoto R (2005) Palaeoclimatic changes in the Qinghai Lake area during the last 18,000 years. Quatern Int 136(1):131–140

    Article  Google Scholar 

  14. Krishnamurthy RV, Bhattacharya SK, Kusumgar S (1986) Palaeoclimatic changes deduced from 13C/12C and C/N ratios of Karewa lake sediments, India. Nature 323:150–152

    Article  Google Scholar 

  15. Meyers PA, Ishiwatari R (1993) Lacustrine organic geochemistry-an overview of indicators of organic matter sources and diagenesis in lake sediments. Org Geochem 20(7):867–900

    Article  Google Scholar 

Download references

Acknowledgments

We thank Dr. Enlou Zhang and Yilan Liu for their help in laboratory work. This work was jointly funded by the National Natural Science Foundation of China (Grant Nos. 40971115, and 41171163), Scientific Research Foundation of Graduate School of Nanjing University, Project 985 (Grant No. 2011CL11), Major Program of National Social Science Foundation of China (Grant No. 11&ZD183), National Key Technology R&D Program of China (Grant No. 2010BAK67B02), Interdisciplinary Research Program of Nanjing University (Grant No. NJUDC2012002).

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Correspondence to Cheng Zhu .

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Wu, L. et al. (2013). Geochemistry Records of Palaeoenvironment from Sanfangwan Neolithic Site in Jianghan Plain, Central China. In: Lu, W., Cai, G., Liu, W., Xing, W. (eds) Proceedings of the 2012 International Conference on Information Technology and Software Engineering. Lecture Notes in Electrical Engineering, vol 211. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-34522-7_10

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  • DOI: https://doi.org/10.1007/978-3-642-34522-7_10

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