苏北梁王城遗址黄泛层初步研究A PRELIMINARY STUDY ON THE STRATA OF YELLOW RIVER OVERFLOW IN THE LIANGWANGCHENG SITE IN NORTHERN JIANGSU
黄铿,朱诚,马春梅,林留根
摘要(Abstract)：
基于黄河下游流域考古遗址中第一次发现的黄泛地层,对苏北梁王城遗址T3902探方南壁剖面上部自然淤积层采样,结合考古断代,并参照历史资料,通过分析重砂矿物和粒度两方面的实验结果,揭示出考古遗址中黄泛地层的沉积物特征。旨在为今后环境考古中对黄泛地层的判别和对比提供可靠的科学依据,特别是为在黄河下游洪泛区考古遗址中疑似黄泛层的确认提供依据。
关键词(KeyWords)： 重砂矿物;粒度特征;黄泛地层;第四系;梁王城遗址;江苏
基金项目(Foundation): 教育部高等学校博士点基金项目(No.20050284011);; 高等学校博士学科点专项科研基金(新教师基金课题);; 苏北典型新石器遗址的环境考古研究(No.20070284067)共同资助
作者(Author): 黄铿,朱诚,马春梅,林留根
参考文献(References)：
- 蔡明理,王颖编.1999.黄河三角洲发育演变及对渤、黄海的影响.南京:河海大学出版社.71—72
- 杜恕环,李保生,温小浩,李后信,牛东风,欧先交,邱世藩.2007.岭南东江流域MIS2阶段红色沙质沉积物粒度分布特征分析.中国沙漠,5(27):771—774
- 何凡能,邹宝山.1993.历史时期黄河下游北流及其对地理环境的影响.见:钮仲勋主编.黄河流域环境演变与水沙运行规律研究文集(第四集).北京:地质出版社.106—113
- 姜加虎,窦鸿身.2003.中国五大淡水湖.合肥:中国科学技术大学出版社.34—35
- 钮仲勋,张义丰.1993.历史时期黄河下游南泛及其对地理环境的影响.见:钮仲勋主编.黄河流域环境演变与水沙运行规律研究文集(第四集).北京:地质出版社.114—119
- 谭其骧主编.1982.中国历史地图集(第六、七、八集).北京:中国地图出版社.
- 王守春.1992.黄河流域气候环境变化的考古文化与文字记录.见:施雅风主编.中国全新世大暖期气候与环境.北京:海洋出版社.175—184
- 卫艳,舒强,陈晔.2005.苏北盆地兴化1#钻孔的沉积物粒度特征及其古环境意义.南京师范大学学报,2(28):101—107
- 吴祥定,钮仲勋,王守春.1994.历史时期黄河流域环境变迁与水沙变化.北京:气象出版社.144—150
- 夏正楷,杨晓燕.2003.我国北方4kaB.P.前后异常洪水事件的初步研究.第四纪研究,23(6):667—674
- 谢瑞琚编.2002.甘青地区史前考古.北京:文物出版社.111—130
- 徐馨,何才华,沈志达,曹琼英,王雪瑜,张之恒,刘雪娴,尤坤元,王开发,陈佩英编.1992.第四纪环境研究方法.贵阳:贵州科技出版社.74—75
- 杨晓燕,夏正楷,崔之久.2005.黄河上游全新世特大洪水及其沉积特征.第四纪研究,25(1):80—85
- 要吉花,谭利华,魏全伟,萧凌波.2005.黄河下游环境变迁在巨野钻孔沉积特征上的响应.北京师范大学学报,2(41):199—203
- 姚鲁烽.1993.黄河下游历史洪水研究.见:钮仲勋主编.黄河流域环境演变与水沙运行规律研究文集(第四集).北京:地质出版社.52—61
- 张强,朱诚,姜彤,张之恒.2002.江苏海安青墩地区新石器时代环境考古.地理研究,4(23):513—520
- 张芸,朱诚,张强,郑若葵.2001.长江三峡大宁河流域3000年来的沉积环境和风尘堆积.海洋地质与第四纪地质,21(4):83—88
- 张芸,朱诚,张强,张之恒.2004.长江三峡大宁河流域的沉积环境与古洪水研究.中国历史文物,(2):83—88
- 赵景波,周晓红,孙贵贞.2007.咸阳渭河高漫滩沉积洪水变化研究.沉积学报,25(4):597—602
- 朱诚,于世永,史威,戴东升,赵宁曦.1997.南京江北地区全新世沉积与古洪水研究.地理研究,(4):23—30
- 朱诚,郑朝贵,马春梅,孙智彬,朱光耀,王慧麟,高华中,王朋岭,黄润.2005.长江三峡库区中坝遗址地层古洪水沉积判别研究.科学通报,20(50):2240—2250
- 竺可桢.1973.中国近五千年来气候变迁的初步研究.中国科学,(2):168—189
- 左大康主编.1989.黄河流域环境演变与水沙运行规律研究文集(第一集).北京:地质出版社.1—9
- Cai Ming-li&Wang Ying eds.1999.Effects of the Yellow RiverDelta’s development and evolution to Bo Sea and the YellowSea.Nanjing:University of River-Sea Publishing House.71—72
- Du Shu-huan,Li Bao-sheng,Wen Xiao-hao,Li Hou-xin,Niu Dong-feng,Ou Xian-jiao&Qiu Shi-fan.2007.Grain-size distributioncharacteristics of red sandy sedi ments in Dongjiang River Val-ley,southern Nanling Mountains during MIS2phase.Journalof Desert Research,27(5):771—774
- Folk R L.1966.Areview of grain size parameters.Sedi mentology,6:73—93
- He Fan-neng&Zou Bao-shan.1993.The Lower Yellow Rivernorthern flows andits i mpacts to the geographical environmentin historical period.In:Niu Zhong-xun ed.Study on environmental evolution of the Yellow River Basin and its water-sandoperation rules(the Fourth Part).Beijing:Geological PublishingHouse.106—113
- Jiang Jia-hu&Dou Hong-shen.2003.The five biggest lakesin Chi-na.Hefei:University of Science and Technology of China Press.34—35
- Mcmanus J.1988.Grain size determination and interpretation.In:Tucker Med.Techniquesin sedi mentology.Oxford:Backwell.63—85
- Niu Zhong-xun&Zhang Yi-feng.1993.The Lower Yellow Riversouthern flows andits i mpacts to the geographical environmentin historical period(A).In:Niu Zhong-xun ed.Study on envi-ronmental evolution of the Yellow River Basin and its water-sand operation rules(the Fourth Part).Beijing:GeologicalPublishing House.114—119
- Tan Qi-xiang ed.1982.The historical atlas of China(sixth,seventhand eighth).Beijing:Sino Maps Press.
- Visher G S.1969.Grain size distribution and depositional proces-ses.Journal of Sedi mentary Petrology,39:1074—1106
- Wang Shou-chun.1992.The archaeological cultures and written re-cords on cli mate and environment changes of the Yellow RiverVally.In:Shi Ya-feng ed.The cli mate and environment of theHolocene great warm period.Beijing:China Ocean Press.175—184
- Wei Yan,Shu Qiang&Chen Ye.2005.Grain size characteristicsand their paleo-environmental significance of Xinghua1#coresedi mentsin northern Jiangsu Basin,China.Journal of NanjingNomal University(Natural Science),28(2):101—107
- Wu Xiang-ding,Niu Zhong-xun&Wang Shou-chun.1994.Changesof the Yellow River vally environment,water and sedi ment.Beijing:China Meteorological Press.144—150
- Xia Zheng-kai&Yang Xiao-yan.2003.Preli minary study on theflood events4kaB.P.in North China.Quaternary Sciences,23(6):667—674
- Xie Rui-ju ed.2002.The prehistoric archaeology of Gansu-Qinghaiareas.Beijing:Cultural Relics Press.111—130
- Xu Xin,He Cai-hua,Shen Da-ying,Cao Qiong-ying,Wang Xue-yu,Zhang Zhi-heng,Liu Xue-xian,You Kun-yuan,Wang Kai-fa&Chen Pei-ying eds.1992.Research methods of the paleo-environment during Quaternary.Guiyang:Guizhou Science andTechnology Publishing House.74—75
- Yang Xiao-yan,Xia Zheng-kai&Cui Zhi-jiu.2005.Holocene ex-treme floods andits sedi mentary characteristic in the upper rea-ches of the Yellow River.Quaternary Sciences,25(1):80—85
- Yao Ji-hua,Tan Li-hua,Wei Quan-wei&Xiao Ling-bo.2005.En-vironment changes of the backword positionin the Yellow Riverrespounds to Juye deposit characteristics.Journal of BeijingNormal University(Natural Science),41(2):199—203
- Yao Lu-feng.1993.The historical flood research on the lower rea-ches of the Yellow River.In:Niu Zhong-xun ed.Study on en-vironmental evolution of the Yellow River basin and its water-sand operation rules(The Fourth Part).Beijing:GeologicalPublishing House.52—61
- Yu Shi-yong,Zhu Cheng,Song Jianet al.2000.Role of cli mate inthe rise and fall of Neolithic cultures on the Yangtze Delta.Bo-reas,29:157—165
- Zhang Qiang,Zhu Cheng,Jiang Tong&Zhang Zhi-heng.2002.Environmental archaeological study on the Qingdun site,Hai'an,Jiangsu province,duringthe Neolithic cultural period.Geo-graphical Research,23(4):513—520
- Zhang Yun,Zhu Cheng,Zhang Qiang&Zheng Ruo-kui.2001.Sedi mentary environment and eolian deposits in past3000a inDaning valley of the Three Gorges of the Yangtze River.MarineGeology&Quaternary Geology,21(4):83—88
- Zhang Yun,Zhu Cheng,Zhang Qiang&Zhang Zhi-heng.2004.Researche on sedi ment environment and paleo-flood in Daningriver basin of Yangtze River Three Gorges.Chinese HistoricalCultural Relics,(2):83—88
- Zhao Jing-bo,Zhou Xiao-hong&Sun Gui-zhen.2007.Research onflood change indicated by deposit in high valley flat profile ofWeihe River in Xianyang.Acta Sedi mentlogica Sinica,25(4):597—602
- Zhu Cheng,Yu Shi-yong,Shi Wei,Dai Dong-sheng&Zhao Ning-xi.1997.Holocene deposits and paleo-floods on the north bankof the Yangtze River,Nanjing area.Geographical Research,(4):23—30
- Zhu Cheng,Zheng Chao-gui,Ma Chun-mei,Yang Xiao-xuan,GaoXi-zhen,Wang Hai-ming&Shao Jiu-hua.2003.On the Hol-ocene sea-level highstand along the Yangtze Delta and NingshaoPlain,East China.Chinese Science Bulletin,48(24):2672—2683
- Zhu Cheng,Zheng Chao-gui,Ma Chun-mei,Sun Zhi-bin,ZhuGuang-yao,Wang Hui-lin,Gao Hua-zhong,Wang Peng-ling&Huang Run.2005.Identifying paleoflood deposits archived inZhongba Site,the Three Gorges Reservoir region of the Yan-gtze River,China.Chinese Science Bulletin,50(21):2493—2504
- Zhu Ke-zhen.1973.Pri mary research on China cli mate changes over5000years.China Sciences,(2):168—189
- Zuo Da-kang ed.1989.Study on environmental evolution of theYellow River basin and its water-sand operation rules(FirstPart).Beijing:Geological publishing House.1—9