Early Neolithic vegetation history, fire regime and human activity at Kuahuqiao, Lower Yangtze River, East China: New and improved insight
Shu, Junwu (舒军武)1,2; Wang, Weiming (王伟铭)1; Jiang, Leping3; Takahara, Hikaru2
2010-11-01
发表期刊QUATERNARY INTERNATIONAL
ISSN1040-6182
卷号227期号:1页码:10-21
摘要

A new 2.6-m long archaeological sedimentary profile from Kuahuqiao, Zhejiang Province, was examined for pollen-phytolith-charcoal microfossil content. The results bring a new and improved insight into the previously established vegetation sequence, contributing to better understanding the interaction between vegetation, fire and human activity in the early Neolithic Lower Yangtze, discussed in the context of archaeological record and published available data. Three distinctive phases were well represented: the nature-dominated phase (c. 8250-7950 cal. BP), the human-affected phase (c. 7950-7400 cal. BP) and the marine-controlled phase (post-7400 cal. BP), considering vegetation changes, human impact, and environment dynamics. Around 8300 cal. BP, the mixed broadleaved evergreen and deciduous forest, mainly consisting of Quercus, Pinus, Cyclobalanopsis, Liquidambar, and Ulmus/Zelkova, developed at Kuahuqiao. It was initially opened by the early local Neolithic hunters and foragers by means of fire since c.7950 cal. BP, indicated by abundant microfossil charcoal in cultural layers. The disturbed forest in the lowlands progressively retreated and was predominately replaced by a Poaceae-dominated vegetation pattern, suggesting increasingly intensified human interference including rice cultivation since 7760 cal. BP. Quercus and Pinus were the main components among the woods targeted by humans in the local small basin, strongly supported by archaeological records as well. However, the short period of Alnus flourishing reported elsewhere is not documented in the pollen sequence. In addition, the combined pollen and archaeological evidence shows that the well recorded local spread of Typha around 7400 cal. BP could mainly be a natural response to the expansion of water regime in addition to the result of human management of the environment. The increasing water level was presumably induced by the local blocked hydrological ecosystem as a result of its retrogression prompted by rising sea level, before the Kuahuqiao Culture ended in the subsequent marine transgression. (C) 2010 Elsevier Ltd and INQUA. All rights reserved.

DOI10.1016/j.quaint.2010.04.010
语种英语
关键词[WOS]Environmental-change ; Rice Domestication ; Sediment Storage ; Delta ; Record ; Agriculture ; Pollen ; Settlement ; Bp
资助项目Knowledge Innovation, Chinese Academy of Sciences[KZCX2-YW-155] ; National Science Foundation of China[40901032] ; Chinese Academy of Sciences[0823020208]
WOS研究方向Physical Geography ; Geology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号WOS:000283900700003
项目资助者Knowledge Innovation, Chinese Academy of Sciences ; National Science Foundation of China ; Chinese Academy of Sciences
出版者PERGAMON-ELSEVIER SCIENCE LTD
文献类型期刊论文
条目标识符http://ir.nigpas.ac.cn/handle/332004/405
专题中国科学院南京地质古生物研究所
其他
通讯作者Shu, Junwu (舒军武)
作者单位1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China
2.Kyoto Prefectural Univ, Kyoto 6068522, Japan
3.Zhejiang Prov Inst Archaeol & Cultural Rel, Hangzhou 310014, Zhejiang, Peoples R China
第一作者单位中国科学院南京地质古生物研究所
通讯作者单位中国科学院南京地质古生物研究所
推荐引用方式
GB/T 7714
Shu, Junwu ,Wang, Weiming ,Jiang, Leping,et al. Early Neolithic vegetation history, fire regime and human activity at Kuahuqiao, Lower Yangtze River, East China: New and improved insight[J]. QUATERNARY INTERNATIONAL,2010,227(1):10-21.
APA Shu, Junwu ,Wang, Weiming ,Jiang, Leping,&Takahara, Hikaru.(2010).Early Neolithic vegetation history, fire regime and human activity at Kuahuqiao, Lower Yangtze River, East China: New and improved insight.QUATERNARY INTERNATIONAL,227(1),10-21.
MLA Shu, Junwu ,et al."Early Neolithic vegetation history, fire regime and human activity at Kuahuqiao, Lower Yangtze River, East China: New and improved insight".QUATERNARY INTERNATIONAL 227.1(2010):10-21.
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