环境考古

江苏宜兴骆驼墩遗址地层7500~5400BC 的 海侵事件记录

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  • 1. 南京大学地理与海洋科学学院, 南京210093;
    2. 南京博物院考古研究所, 南京210018;
    3. 上海同济大学海洋地质国家重点实验室, 上海200092;
    4. 南京地质古生物研究所, 南京210093;
    5. 重庆市文物考古研究所, 重庆400013
李兰(1983-), 女, 硕士。现从事环境考古研究。E-mail: lilanmengyu@126.com

收稿日期: 2008-07-23

  修回日期: 2008-09-01

  网络出版日期: 2008-11-25

基金资助

国家科技支撑计划项目课题(2006BAK21B02); 国家自然科学基金重大项目(90411015); 高校博士点基金 (20050284011); 南京大学现代分析中心测试基金(0209001309)

Transgression Records between 7500-5400BC on the Stratum of the Luotuodun Site in Yixing, Jiangsu Province

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  • 1. School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210093, China;
    2. Archaeological Institute of Nanjing Museum, Nanjing 210018, China;
    3. State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China;
    4. Nanjing Institute of Geology and Paleontology, Nanjing 210093, China;
    5. Cultural Relics and Archaeological Institute of Chongqing City, Chongqing 400013, China

Received date: 2008-07-23

  Revised date: 2008-09-01

  Online published: 2008-11-25

Supported by

National Science and Technology Project, No.2006BAK21B02; Major project of National Natural Science Foundation of China, No. 90411015; Foundation of Doctoral Program, No.20050284011; Test Foundation of Modern Analyses Center of Nanjing University, No.0209001309

摘要

在考古发掘基础上, 野外共采集样品217 个, 对遗址地层剖面中63 个样品进行了有孔虫、植物碎屑及种子化石等的鉴定分析, 对4 个地层相关样品进行了14C 测年及相关分析。 在第10 层的泥炭层中发现底栖有孔虫2 种1 属, 即压扁卷转虫(Ammonia compressiuscula) 和近亲卷转虫相似种(Ammonia cff.sobrina), 表明全新世以来骆驼墩遗址及其附近区域在马家浜 文化出现之前的7500~5400BC 之间曾经历过海侵事件; 共发现植物化石9 种450 颗, 鉴定结果共统计出4 (科)属, 即Polygonum sp. (蓼属未定种)、Scirpus sp. (藨草属未定种)、Najas sp. (茨藻属未定种)、Physalis sp. (酸浆属未定种), 多属湖泊、沼泽等水生环境。

本文引用格式

李兰,朱诚,林留根,赵泉鸿,史恭乐,朱寒冰 . 江苏宜兴骆驼墩遗址地层7500~5400BC 的 海侵事件记录[J]. 地理学报, 2008 , 63(11) : 1189 -1197 . DOI: 10.11821/xb200811008

Abstract

Based on archaeological excavations, 217 samples were collected, of which 63 were used for identification analysis of foraminifera, plant debris and seed fossils. The authors used four samples for 14C dating and correlation analysis. Through experiments, some conclusions can be drawn as follows. First, Bentic foraminifera was found in the 10th layer, such as Ammonia compressiuscula and Ammonia cff. sobrina, which shows that between 7500-5400 BC, before the appearance of the Majiabang culture, Luotuodun Site and its neighbouring regions had experienced transgression events. Second, we found 450 plant fossils at this site, such as Polygonum sp., Scirpus sp., Najas sp., Physalis sp., which lived in lakes, swamps and other aquatic environments.

参考文献


[1] Chen Zhongyuan, Hong Xueqing, Li Shan et al. Study of archaeology related environment evolution of Taihu Lake in southern Changjiang Delta plain. Acta Geographica Sinica, 1997, 52(2): 131-137.
[陈中原, 洪雪晴, 李山等. 太湖地区 环境考古. 地理学报, 1997, 52(2): 131-137.]

[2] An Zhimin. Neolithic age of China. Archaeology, 1981, (3): 252-260.
[安志敏. 中国的新石器时代. 考古, 1981, (3): 252-260.]

[3] Zhou Hong, Zheng Xiangmin. The impact of environmental changes on the development of prehistoric civilization: The decline of the ancient Liangzhu culture in the southern plain of Yangtze River Delta. Journal of East China Normal University (Natural Science), 2000, 28(4): 71-77.
[周鸿, 郑祥民. 试析环境演变对史前人类文明发展的影响: 以长江 三角洲南部平原良渚古文化衰变为例. 华东师范大学学报(自然科学版), 2000, 28(4): 71-77.]

[4] Archaeological Institute of Nanjing Museum. Excavation on the Luotuodun Neolithic Site in Yixing City, Jiangsu Province. Archaeology, 2003, (4): 3-11.
[南京博物院考古研究所. 江苏宜兴市骆驼墩新石器时代遗址的发掘. 考古, 2003, (7): 3-11.]

[5] Lin Liugen, Tian Mingli, Tan Guohua et al. New breakthroughs of the prehistoric archaeological surround the Pacific Ocean valley. China Cultural Heritage News, 2002, 1.
[林留根, 田名利, 谈国华等. 环太平洋流域史前考古新突破. 中 国文物报, 2002, 1.]

[6] Wang Pinxian, Zhang Jijun, Zhao Quanhong et al. Foraminifera and Ostracod: Distribution in the Coastal Area of the East China Sea. Beijing: China Ocean Press, 1988.
[汪品先, 章纪军, 赵泉鸿等. 东海底质中的有孔虫和介形虫. 北 京: 海洋出版社, 1988.]

[7] Huang Baoyu, Zhu Xianggen, Cai Huawei et al. Holocene molluscs in Luotuodun and Xixi of Yixing City, Jiangsu Province. Marine Sciences, 2005, 29(8): 84-94.
[黄宝玉, 朱祥根, 蔡华伟等. 江苏宜兴骆驼墩、西溪遗址全新世软体 动物. 海洋科学, 2005, 29(8): 84-94.]

[8] Xu Xuemin, William Y B Chang, Liu Jinling. Changes in vegetation and climate in the Taihu lake basin during the last 11000 years. Acta Palaeontologica Sinica, 1996, 35(2): 175-186.
[许雪珉, William Y B Chang, 刘金陵. 11000 年以来 太湖地区的植被与气候变化. 古生物学报, 1996, 35(2): 175-186.]

[9] Zhu Kezheng. Preliminary study on the climate changes since 5000 years in China. Science in China, 1973, (2): 168-189.
[竺可桢. 中国近五千年来气候变迁的初步研究. 中国科学, 1973, (2): 168-189.]

[10] Xu Xin. The environment Holocene evolution since the Holocene in the eastern China. In: Xu Xin, Zhu Minglun (eds.). Selection Works on Treatises of Quaternary Environment. Hongkong: Jinling Book Store Publishing Co. of Hong Kong, 1992. 56-64.
[徐馨. 中国东部全新世自然环境演变. 见: 徐馨, 朱明伦. 第四纪环境论文选集. 香港: 香港金陵 书社出版公司, 1992. 56-64.]

[11] Yang Huairen, Xie Zhiren. The relation of Holocene sea-level changes with formation and evolvement of Taihu Lake. In: Yang Huairen (ed.) Selection of Quaternary Ice and Quaternary Geology. Beijing: Geology Press, 1985.
[杨怀仁, 谢志仁. 全新世海面变化与太湖形成和演变. 见: 杨怀仁. 第四纪冰川与第四纪地质论文集. 北京: 地质出版社, 1985.]

[12] Shao Xusheng. On the transgression sediment in Holocene in Jintan, Jiangsu province. In: Yan Qinshang, Xu Shiyuan (eds.). On the Modern Sediment in Yangtze Delta. Shanghai: East China Normal University Press, 1987. 114-116.
[邵 虚生. 江苏金坛全新世海侵沉积层的研究. 见: 严钦尚, 许世远编. 长江三角洲现代沉积研究. 上海: 华东师范大学 出版社, 1987. 114-116.]

[13] Yan Qinshang, Xu Shiyuan. Holocene Deposits and Geomorphological Processes on the Northern Plain of the Jiangsu Province, China. Shanghai: Shanghai Science and Technological Literature Publishing House, 1993. 83.
[严钦尚, 许世 远. 苏北平原全新世沉积与地貌研究. 上海: 上海科学技术文献出版社, 1993. 83.]

[14] Yan Qinshang, Hong Xueqing. Holocene transgression on the southern deltaic plain of the Yangtze River Delta. In: Yan Qinshang, Xu Shiyuan (eds.). Recent Yangtze Delta Deposits. Shanghai: East China Normal University Press, 1987. 92-101.
[严钦尚, 洪雪晴. 长江三角洲南部平原全新世海侵问题. 见: 严钦尚, 许世远. 长江三角洲现代沉积 研究. 上海: 华东师范大学出版社, 1987. 92-101.]

[15] Jiang Menglin, Liu Zhiping. The Quaternary marine transgression in the northwest of Taihu Lake Plain. Jiangsu Geology, 2001, 25(2): 78-81.
[蒋梦林, 刘志平. 太湖平原西北部第四纪海侵. 江苏地质, 2001, 25(2): 78-81.]

[16] Yu Shiyong, Zhu Cheng, Qu Weizheng. Mid Holocene climatic transition and rapid interruption in Neolithic cultures in the eastern plain of Taihu Lake. Scientia Geographica Sinica, 1999, 19(6): 549-554.
[于世永, 朱诚, 曲维正. 太湖东岸 平原中全新世气候转型事件与新石器文化中断. 地理科学, 1999, 19(6): 549-554.]

[17] Jing Cunyi. The formation and evolution of Taihu Lake. Scientia Geographica Sinica, 1989, 9(4): 378-385.

[18] Zheng Xiangmin, Zhang Weiguo, Yu Lizhong et al. Paleoenvironmental changes in southern Yangtze Delta over the last 20,000 years. The Quaternary Research, 1994, 33(5): 379-384.

[19] Stanley D J, Chen Z. Neolithic settlement distributions as a function of sea level controlled topography in the Yangtze Delta, China. Geology, 1996, (12): 1083-1086.

[20] Zhang Jingwen, Li Guiying, Zhao Xitao. Chronological study of the Holocene sea-land shift in northern Jiangsu. Marine Science, 1983, (6): 8-11.
[张景文, 李桂英, 赵希涛. 苏北地区全新世海陆变迁的年代学研究.海洋科学, 1983, (6): 8-11.]

[21] Wang Zhanghua, Cheng Jie. Distribution of the Neolithic sites in the Changjiang coastal plains: Holocene transgression impact. Quaternary Sciences, 2004, 24(5): 537-545.
[王张华, 陈杰. 全新世海侵对长江口沿海平原新石器遗址分布 的影响. 第四纪研究, 2004, 24(5): 537-545.]

[22] Zhu Cheng, Zheng Chaogui, Ma Chunmei et al. New idea on the high sea level since 10 kaB.P. in the Changjiang Delta and Ningshao plains. Chinese Science Bulletin, 2003, 48(23): 2428-2438.
[朱诚, 郑朝贵, 马春梅等. 对长江三 角洲和宁绍平原一万年来高海面问题的新认识. 科学通报, 2003, 48(23): 2428-2438.]

[23] Xin Zhongbao, Xie Zhiren. Construction of the simulating model for geomorphic evolution of the Yangtze Delta, China. Acta Geographica Sinica, 2006, 61(5): 549-560.
[信忠保, 谢志仁. 长江三角洲地貌演变模拟模型的构建. 地 理学报, 2006, 61(5): 549-560.]

[24] Chen Jiyu, Yu Zhiying, Yun Caixing. The development of physiognomy of Yangtze Delta. Acta Geographica Sinica, 1959, 25(3): 201-220.
[陈吉余, 虞志英, 恽才兴. 长江三角洲的地貌发育. 地理学报, 1959, 25(3): 201-220.]

[25] Sun Shuncai. The relation of modern time sediment with the evolvement of Taihu Lake. Science in China (Series B), 1987, (12): 131-137.
[孙顺才. 太湖形成演变与现代沉积作用. 中国科学(B 辑) ,1987, (12) : 131-137.]

[26] Sun Shuncai. Is there transgression in the Taihu plain in Holocene? Acta Oceanologica Sinica, 1992, 14(4): 69-77.
[孙 顺才. 太湖平原有全新世海侵吗? 海洋学报, 1992, 14(4): 69-77.]

[27] Shen Hongyuan, Zhu Cheng, Zhang Qiang. Advance of the research on the environmental evolvement and environmental archaeology in the Yangtze Delta region. Advance in Earth Sciences, 2003, 18(4): 569-575.
[申洪源, 朱 诚, 张强. 长江三角洲地区环境演变与环境考古学研究进展. 地球科学进展, 2003, 18(4): 569-575.]

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