太湖地区多剖面地层学分析与良渚期环境事件
收稿日期: 2007-05-17
修回日期: 2007-12-23
网络出版日期: 2008-09-25
基金资助
国家自然科学青年基金资助项目(40701190)和中科院南京地理与湖泊研究所博士后基金资助项目。
Analysis of stratigraphy on multi-profiles in the Taihu Lake region and paleoenvironmental events in the Liangzhu culture epoch
Received date: 2007-05-17
Revised date: 2007-12-23
Online published: 2008-09-25
Supported by
国家自然科学青年基金资助项目(40701190)和中科院南京地理与湖泊研究所博士后基金资助项目。
太湖地区多剖面地层学分析和环境考古研究表明:本区良渚期为全新世大暖期中气候逐渐向干凉转变的时期,但大部分时间里仍略比今天暖湿。良渚期末气候走入低谷并剧烈波动,良渚期侵蚀面反映一次较长时间的海面下降过程,气候剧烈波动的转型期与海面下降至低海面过程相一致。此时本区洪积层、埋藏遗址及遗址地层中文化间歇层等发育皆反映古洪水泛滥事件的存在;而良渚期侵蚀面上的铁锰结核聚集现象及现没于水下的众多良渚期开挖的古井等遗迹还反映出这一时期也曾发生过气候干燥事件。分析认为良渚文化繁荣发展期陆地面积扩大,气候略好于今天;而良渚文化衰亡期则处于4300~3800aB. P.间的水、旱灾丛生的低海面气候异常期。
史 威, 马春梅, 朱 诚, 王富葆, 李世杰 . 太湖地区多剖面地层学分析与良渚期环境事件[J]. 地理研究, 2008 , 27(5) : 1129 -1138 . DOI: 10.11821/yj2008050016
The Shahe profile in Dongling, Liyang, the Caoxieshan site in Weiting, Suzhou and Maqiao site in Maqiao town, Shanghai are chosen as the major research objects on stratigraphy, from which we analyze and study the paleo-corroding surface, deposit characteristics, sporo pollens, chemical elements, 14C dating and climate transformation curve transformed by chemical composition from the stratum of the Maqiao site in Shanghai, combined with the analysis of the regional paleoenvironment and environmental archaeology as well as the research results of the temporal and spatial distribution of archaeological sites since the Neolithic Age in the Taihu Lake region. The research results indicate that the climate of Liangzhu epoch in the Taihu Lake region increasingly changed towards colder and drier than that of its former time in Holocene Megathermal period, however, much more time of it was still warmer and wetter than today. In the end of Liangzhu epoch, the climate was at the lowest position and showed rapid and violent fluctuation, which matched well a long time course of sea-level falling that was reflected by the paleo-corroding surface of Liangzhu epoch. The flood accumulation layers, the buried ancient trees, the buried archaeological sites and cultural interruption, etc. prove the existence of the ancient floods; the iron manganese concretion and the ancient wells under water such as the Taihu Lake, Chenghu Lake and the Taishidian in Zhouzhuang etc. today reflect on the dry periods or drought events. The background of Liangzhu cultural development was that the sea-level in the Taihu Lake region was slowly falling, the area of fresh-water lakes and marshes were increasingly decreasing, which made the land increasingly exposed; in the meantime, the climate was slightly better than that of today. In 4300-3800aB. P., the low sea-level, the abnormal climate as well as the frequently occurred floods and droughts were the environmental background of Liangzhu culture towards the decline and fall.We think that the direct reason for the decline and fall of Liangzhu culture is more complicated than we have imagined ever, however, the frequently occurring floods and droughts as well as the abnormal climate should be seriously fatal hit for Liangzhu people living on the paddy growing, fishing and hunting.
[1] 朱诚,史威,于世永,等.上海马桥地区6000年来环境演变的沉积学研究.应用基础与工程科学学报,1996,4(1):5~11.
[2] Zhu Cheng, Song jian, You Kunyuan. Formation of the cultural interruption of the Maqiao site, Shanghai. Chinese Science Bulletin,1996,41(2):148~152.
[3] 朱诚,史威,宋友桂.长江三角洲地区七千年以来古洪水灾害的环境考古研究.见:崔鹏.海峡两岸山地灾害与环境保育研究(第一卷).成都:四川科技出版社,1998.85~90.
[4] 于世永,朱诚,史威.上海马桥地区全新世中晚期环境演变.海洋学报,1998,20(1):58~64.
[5] 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.
[6] Yu S Y, Zhu C, Song J,et al. Role of climate in the rise and fall of Neolithic culture on the Yangtze Delta. Boreas,2000,29:157~165.
[7] 于世永,朱诚,王富葆,等.太湖流域全新世气候-海面短期振荡事件及其对新石器文化的影响.地理科学,2000,20(4):331~336.
[8] Zhu Cheng, Yu Shiyong, Zhang Qiang,et al. Neolithic cultural interruptions and Holocene buried palaeo-trees in the Yangtze Delta. Journal of Nanjing University (Natural Sciences),2000,36(6):693~701.
[9] 朱诚,郑朝贵,马春梅,等.对长江三角洲及宁绍平原一万年来高海面的新认识.科学通报,2003,48(23):2428~2438.
[10] 史威,朱诚.太湖流域水灾演变与环境变迁的相关分析.自然灾害学报,2004,(1):32~37.
[11] Zhang Qiang, Jiang Tong, Shi Yafeng,et al.Paleo-environmental changes in the Yangtze Delta during the past 8000 years. Journal of Geographical Science,2004,14(1):105~112.
[12] Zhang Qiang, Zhu Cheng, Liu Chunling,et al. Environmental change and its impacts on human settlement in the Yangtze Delta, P.R. China. Catena,2005,60:267~277.
[13] 蒋卫东.自然环境变迁与良渚文化兴衰关系的思考.华夏考古,2003,(2):38~45.
[14] 申洪源,朱诚,贾玉连.太湖流域地貌与环境变迁对新石器文化传承的影响.地理科学,2004,24(5):580~585.
[15] 曹峻.略论自然环境在太湖流域文明化进程中的地位.东南文化,2004,(3):10~13.
[16] 萧家仪,郭平,王丹,等.太湖平原全新世中晚期古植被、古环境与古文化.南京师大学报(自然科学版),2004,27(2):91~97.
[17] 高蒙河.长江下游文明化初期的人地关系.复旦学报(社会科学版),2005,(2):128~139.
[18] 陈杰.良渚文明兴衰的生态史观.东南文化,2005,(5):33~40.
[19] 曹琼英,王富葆,韩辉友.苏南和宁镇地区三万年以来地层的划分及自然环境变化中的若干问题.中国第四纪研究,1989,(1):122~131.
[20] 孔昭宸,杜乃秋,王富葆,等.句容宝华山山龙眼化石植物群的发现及其在气候学和植物学上的意义.第四纪研究,1991,(4):329~335.
[21] 陈纯.考古学理论.上海:复旦大学出版社,2004.205~206.
[22] Schick K D. Experimentally-derived criteria for assessing hydrologic disturbance of archaeological sites. In: Nash D T, Petraglia M D (eds. ). Natural Formation Processes and the Archaeological Record. BAR International Series,1987,352: 86~107.
[23] 朱诚,于世永,史威,等.南京江北地区全新世沉积与古洪水研究.地理研究,1997,(4):23~30.
[24] 萧家仪.江苏吴县龙南遗址孢粉组合及其环境考古意义.见:周昆叔 主编.环境考古研究(第一辑).北京:科学出版社,1991.157~163.
[25] 洪雪晴.全新世低温事件及海面波动.见:扬子庚,林和茂 主编.中国近海及沿海地区第四纪进程与事件.北京:海洋出版社,1989.114.
[26] 黄翡,王伟铭,李民昌.苏州草鞋山遗址新石器时代以来的植硅石研究.微体古生物学报,1998,15(1):79~84.
[27] 谷建祥,周厚本,李民昌,等.对草鞋山遗址马家浜文化时期稻作农业的初步认识.东南文化,1998,(3):15~24.
[28] 汤陵华,佐藤洋一郎,宇田津彻朗,等.中国草鞋山遗址古代稻种类型.江苏农业学报,1999,15(4)193~197.
[29] Goldschmidt V M. Geochemistry. Clarendon: Oxford at the Clarendon Press, 1954. 336~524.
[30] 汪永进,王建,刘金陵,等.东太湖全新世水下河道沉积特征及环境演变.古生物学报,1996,35(2):224~231.
[31] 林承坤.长江三角洲古地理与新石器时代文化的关系.文物集刊(第一辑),1980,(1):147~151.
[32] 潘凤英,石尚群,邱淑彰,等.全新世以来苏南地区古地理演变.地理研究,1984,3(3):64~74.
[33] 吴县文物管理委员会.吴县通安古井清理简报.东南文化,1987,(2):18~21.
[34] 上海文物保管委员会.上海青浦福泉山遗址崧泽文化遗存.考古学报,1990,(3):28~34.
[35] 何培元.从庐山第四纪地层中高价铁与低价铁的比值关系探讨古温度变化.中国地质科学院地质力学研究所所刊,1989,13:61~69.
[36] 刘会平,王开发.沪杭苏地区若干文化遗址的孢粉—气候对应分析.地理科学,1998,18(4):368~373.
[37] Maley J. The African rainforest vegetation and palaeoenvironments during late Quaternary. Climate Change,1991,19:79~98.
[38] Weiss H. Late third millennium abrupt climate change and social collapse in West Asia and Egypt. In: Dalfes H N, Kukla G, Weiss H(eds. ).Third Millennium BC Climate Change and Old World Collapse. Berlin, Heidelberg: Springer Verlag,1997.711~723.
[39] Weiss H. Bradley R S. What drives societal collapse? Science,2001,291:609~610.
[40] 许靖华.太阳、气候、饥荒与民族大迁移.中国科学,D辑,1998,28(4):366~384.
[41] Singh G, Joshi R D, Singh A B. Stratigraphic and radiocarbon evidence for the age and development of three salt lakes deposits in Rajasthan, India. Quaternary Researches,1972,2:496~505.
[42] Bryson R A, Swain A M. Holocene variations of monsoon rainfall in Rajasthan. Quaternary Researches,1981,16:135~145.
[43] Bentaleb I, Caratini C, Fontugne M,et al.Monsoon regime variations during the late Holocene in the south western India. In: Dalfes H N, Kukla G, Weiss H(eds. ). Third Millennium BC Climate Change and Old World Collapse. Heidelberg: Springer Verlag, 1977.475~488.
[44] 赵伯乐.永恒涅槃——古印度文明探秘.昆明:云南人民出版社,1999.17~23.
[45] 谢崇安.沉沙中的失乐园,追踪上古印度文明.重庆:重庆出版社,2002.122~132.
[46] 方修琦,张兰生.我国北方农牧交错带3500aB. P.的降水突变事件研究.北京师范大学学报(自然科学版),1998,34(增刊):18~23.
[47] 高广仁,邵望平.中华文明发祥地之一—岱海历史文化区.史前研究,1984,(1):7~14.
[48] 邓辉.全新世大暖期燕北地区人地关系的演变.地理学报,1997,52(1):64~71.
[49] 吴文祥,刘东生.4000aB. P.前后降温事件与中华文明的诞生.第四纪研究,2001,21(5):443~451.
[50] 施雅风,孔昭宸,王苏民,等.中国全新世大暖期气候与环境的基本特征.见:施雅风 主编,孔昭宸 副主编.中国全新世大暖期气候与环境.北京:海洋出版社,1992.1~8.
[51] Suzuki H. 3500 years age-climatic changes and ancient civilizations. Bulletin of the Department of Geography, University of Tokyo,1979,11:43~58.
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