AN OVERVIEW OF THE RESEARCH ON THE ENVIRONMENTAL EVOLVEMENT AND HUMAN-ENVIRONMENT RELATIONSHIP IN HOLOCENE EPOCH OF THE YANGTZE DELTA

C. Guang-jie, W. Jian
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引用次数: 3

Abstract

This paper aims to summarize the past research on environmental evolvement and human-environment relationship in the Yangtze delta, and to put forward some issues for further study. Much attention has been paid to the Yangtze delta formation and evolution from academic circle for its important role in regional economic growth and ecological environment.Many researches indicate that Yangtze delta has been the continental environment suitable for human settlement since the Holocene epoch.A large numbers of Neolithic sites, relics and wells excavated were discovered. After the termination of the Last Glaciation Age, the sea-level in the Yangtze delta was on the increase, and during about 7~6.5 kaBP,the sea-level reached the greatest range, closing to the sea-level of today. Sea-level changes and flooding events played an important role in the rise and fall of human civilization in the Yangtze delta region. The study of archaeological excavation and environmental archaeology indicate that the cultural interrupt in the sections of Neolithic sites are mostly the results of frequently occurred flooding events and extreme climatic events in this research filed. During the 3 kaBP,there is a great change of human-environment relationship. There are many methods to study environmental evolvement such as ~14C, spore and pollen, Geochemistrytechnique, etc. The main content of the following research in the field will focus on multi-proxy , high-resolution, quantificational and synthetical research. Meanwhile,it is quite necessary to emphasis on study of the temporal and spatial evolution of modern environmental evolution to find the path for sustainable development for human-environment relationship.
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长江三角洲全新世环境演变与人地关系研究综述
本文旨在对长江三角洲环境演变及人地关系的研究现状进行总结,并提出今后需要进一步研究的问题。由于长江三角洲在区域经济增长和生态环境中的重要作用,其形成与演化受到学术界的广泛关注。大量研究表明,自全新世以来,长江三角洲一直是适宜人类居住的大陆环境。发掘出大量新石器时代遗址、遗迹和水井。末次冰期结束后,长江三角洲海平面呈上升趋势,在约7~6.5 kaBP期间,海平面达到最大范围,接近今天的海平面。海平面变化和洪水事件对长江三角洲地区人类文明的兴衰起了重要作用。考古发掘和环境考古研究表明,新石器时代遗址剖面的文化中断主要是该研究领域频繁发生的洪水事件和极端气候事件的结果。在3kabp期间,人与环境的关系发生了很大的变化。研究环境演化的方法有~14C、孢子和花粉、地球化学技术等。该领域后续研究的主要内容将是多代理、高分辨率、定量和综合研究。同时,重视现代环境演化的时空演化研究,寻找人与环境关系可持续发展的路径是十分必要的。
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