江汉平原钟桥遗址地层揭示的史前洪水事件

doi:10.11821/dlxb201507011

地理学报 ›› 2015, Vol. 70 ›› Issue (7): 1149-1164.doi: 10.11821/dlxb201507011

江汉平原钟桥遗址地层揭示的史前洪水事件

吴立^1,^2,³, 朱诚³(), 李枫⁴, 马春梅³, 李兰⁵, 孟华平⁶, 刘辉⁶, 王晓翠⁴, 谭艳³, 宋友桂²

1. 安徽师范大学国土资源与旅游学院,芜湖 241002
2. 中国科学院地球环境研究所黄土与第四纪地质国家重点实验室,西安 710054
3. 南京大学地理与海洋科学学院,南京 210023
4. 中国科学院南京地理与湖泊研究所湖泊与环境国家重点实验室,南京 210008
5. 四川大学历史文化学院,成都 610064
6. 湖北省文物考古研究所,武汉 430077

收稿日期:2015-03-17 修回日期:2015-04-21 出版日期:2015-07-20 发布日期:2015-08-11
作者简介:
作者简介：吴立(1985-), 男, 博士, 中国地理学会会员(S110008501M), 主要研究方向为地貌学与第四纪环境考古。
基金资助:
黄土与第四纪地质国家重点实验室开放基金项目(SKLLQG1422);国家自然科学基金项目(41401216, 41371204);安徽师范大学科研培育基金项目(2014glkypy05, 2014rcpy13)

Prehistoric flood events recorded at the Zhongqiao Neolithic Site in the Jianghan Plain, Central China

Li WU^1,^2,³, Cheng ZHU³(), Feng LI⁴, Chunmei MA³, Lan LI⁵, Huaping MENG⁶, Hui LIU⁶, Xiaocui WANG⁴, Yan TAN³, Yougui SONG²

1. College of Territorial Resources and Tourism, Anhui Normal University, Wuhu 241002, Anhui, China
2. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xi'an 710054, China
3. School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210023, China
4. State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography & Limnology, CAS, Nanjing 210008, China
5. School of History & Culture, Sichuan University, Chengdu 610064, China
6. Hubei Provincial Institute of Cultural Relics and Archaeology, Wuhan 430077, China

Received:2015-03-17 Revised:2015-04-21 Online:2015-07-20 Published:2015-08-11
Supported by:
Open Foundation of State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, No.SKLLQG1422;National Natural Science Foundation of China, No.41401216, No.41371204;Scientific Research Cultivating Foundation of Anhui Normal University, No.2014glkypy05, No.2014rcpy13

摘要/Abstract

摘要：

通过野外考古调查研究,利用对钟桥遗址疑似古洪水层和研究区现代洪水沉积物的锆石微形态、粒度、磁化率、Rb/Sr等地球化学指标的比较、AMS¹⁴C技术和考古器物断代,发现钟桥遗址在4800~4597 cal. a BP、4479~4367 cal. a BP和4168~3850 cal. a BP分别经历了三次古洪水事件并相应堆积了古洪水沉积层;结合江汉平原及其周边地区众多遗址的古洪水沉积层时代对比证据,揭示了屈家岭文化中晚期（4900~4600 cal. a BP）和石家河文化末期至夏代（4100~3800 cal. a BP）两次大洪水事件在江汉平原地区非常普遍。对史前洪水发生环境背景的进一步分析,反映江汉平原在5000~4500 a BP及4000 a BP前后的时段气候表现得不稳定,古洪水事件与气候环境变化驱动的江汉平原湖群扩张存在一定的联系,并影响区域新石器文化兴衰过程。同时,其它证据也表明该区社会发展过程和环境变化过程特别是古水文过程的矛盾在石家河文化末期已特别突出,发现具有全球意义的4000 a BP前后气候异常引起的大洪水事件是江汉平原地区石家河文化消亡的重要环境因素;而石家河文化末期该区内部或同中原以及其它地区间的冲突,都加速了石家河文化的崩溃。这些研究成果,提供了可靠的大禹时代史前洪水证据来说明其对新石器文化兴衰的社会影响,对于揭示4000 a BP气候事件中区域气候水文变化的响应规律,亦具有重要的科学意义。

关键词: 史前洪水, 钟桥遗址, 考古地层, 江汉平原, 全新世

Abstract:

Field archaeological investigations were carried out in the Jianghan Plain in the middle reaches of the Changjiang River. Based on the integrated study with a comparative analysis for characteristics of the modern flood sediments, multidisciplinary approaches such as the AMS¹⁴C and archaeological dating, micromorphology of zircon, grain size, magnetic susceptibility and geochemistry are conducted to identify paleoflood sediments archived at the Zhongqiao Site. The results indicate that three paleoflood events (i.e. 4800-4597 cal. a BP, 4479-4367 cal. a BP & 4168-3850 cal. a BP) occurred at the Zhongqiao Site. Comparisons of paleoflood deposit layers at numerous Neolithic sites show that two Holocene extraordinary paleoflood events occurred over the Jianghan Plain area at approximately 4900-4600 cal. a BP (i.e. mid-late Qujialing cultural period) and 4100-3800 cal. a BP (i.e. from late Shijiahe cultural period to the Xia Dynasty). Further analysis of the environmental background for the paleoflood occurrences suggested that there was great climate variability between approximately 5000-4500 a BP and ca 4000 a BP. These two paleoflood events were closely related with the expansion of Jianghan lakes driven by the climatic change, and influenced the rise and fall of regional Neolithic Culture. Other evidences also suggested that intensified discrepancy between social development and environmental change processes (especially the hydrological process) in the end of Shijiahe cultural period might be the key factor leading to the collapse of Shijiahe Culture. The severe extraordinary floods related to the climatic anomaly at ca 4000 a BP and political conflicts from internal or other cultural areas all accelerated the collapse of the Shijiahe Culture. These results gave us a better understanding of the climate change at ca 4000 a BP, and also provide evidence for the prehistoric flood events in the Great Yu age, which is considered to be the turning point from the Neolithic Age to the Bronze Age in China.

Key words: prehistoric floods, Zhongqiao Neolithic Site, archaeological stratum, Jianghan Plain, Holocene

吴立, 朱诚, 李枫, 马春梅, 李兰, 孟华平, 刘辉, 王晓翠, 谭艳, 宋友桂. 江汉平原钟桥遗址地层揭示的史前洪水事件[J]. 地理学报, 2015, 70(7): 1149-1164.

Li WU, Cheng ZHU, Feng LI, Chunmei MA, Lan LI, Huaping MENG, Hui LIU, Xiaocui WANG, Yan TAN, Yougui SONG. Prehistoric flood events recorded at the Zhongqiao Neolithic Site in the Jianghan Plain, Central China[J]. Acta Geographica Sinica, 2015, 70(7): 1149-1164.

图/表 8

图1

表1

钟桥遗址T0405探方剖面疑似古洪水层与一般文化层特征比较"

层位编号	层位属性	距地表深度(m)	根据出土器物确定的考古学地层年代	地层特征
1	耕土层	0.30	近现代时期	灰棕色粘土夹浊棕色砂质土,性质混杂,多植物根系,含许多草木灰、炭屑等
2a	明清文化层	0.40	明清时期	灰黄棕夹浊黄棕色粘土,夹极少量棕灰色斑粘土,极多植物根系,含青花瓷片、碎灰黑色陶片、锈斑及少量有机质
2b	明清文化层	0.51	明清时期	浊黄棕夹灰黄棕色团块粉砂质粘土,含植物根系、较多锈斑、青花瓷片及碎红色陶片等
3	唐宋文化层	0.80	唐宋时期	灰黄棕色粉砂质粘土,含植物根系及锈斑,较多有机质,出土宋代瓷片、碎灰黑色陶片等
4	石家河文化层	1.19	石家河文化晚期	棕灰色夹灰棕色粘土质粉砂,颜色质地混杂,含植物根系、碎红色陶片等,文化遗迹少,有团粒结构
5	疑似古洪水层	1.53	石家河文化晚期	灰黄棕色夹棕灰色粉砂质粘土,含植物种子结核状锈斑、虫孔等,扰动波纹大
6	石家河文化层	2.05	石家河文化中晚期	黑棕色粘土质粉砂,含植物及大量有机质,有虫孔、锈斑、大量红或红棕色碎陶片等文化遗迹
7	疑似古洪水层	2.49	石家河文化中期	灰黄棕色夹浊黄棕色粘土质粉砂,植物、有机质、虫孔较多,含大量锈斑及结核,有扰动波纹
8	石家河文化层	2.87	石家河文化早中期	棕色夹棕灰色粘土,植物、有机质多,有虫孔,锈斑多且有少量结核,多红或红棕色碎陶片
9	石家河文化层	3.30	石家河文化早期	黑棕色粘土质粉砂,含植物及大量有机质,虫孔多,有锈斑和结核,出土红或红棕色碎陶片
10	疑似古洪水层	3.55	屈家岭文化晚期	灰黄棕夹棕灰色粉砂质粘土,含植物,有虫孔,有机质多,有锈斑和结核,水份极多,未见底

表1

表2

图2

图3

表3

图4

图5

参考文献 72

[1]	Zhu Cheng, Xie Zhiren, Li Feng, et al.An Introduction to Global Change Science. Beijing: Science Press, 2012.
	[朱诚,谢志仁,李枫, 等. 全球变化科学导论. 北京: 科学出版社, 2012.]
[2]	Baker V R.The study of superfloods. Science, 2002, 295: 2379-2380.
[3]	Baker V R.Palaeoflood hydrology in a global context. Catena, 2006, 66: 161-168.
[4]	Baker V R.Paleoflood hydrology: Origin, progress, prospects. Geomorphology, 2008, 101: 1-13.
[5]	Greenbaum N, Schwartz U, Benito G, et al.Paleohydrology of extraordinary floods along the Swakop River at the margin of the Namib Desert and their paleoclimate implications. Quaternary Science Reviews, 2014, 103: 153-169.
[6]	Huang C C, Pang J, Zha X, et al.Holocene palaeoflood events recorded by slackwater deposits along the lower Jinghe River valley, middle Yellow River basin, China. Journal of Quaternary Science, 2012, 27(5): 485-493.
[7]	Zhou Fengqin, Tang Congsheng.Sediment Source and Accumulation Law of the Yangtze River. Wuhan: Changjiang Press, 2008.
	[周凤琴,唐从胜. 长江泥沙来源与堆积规律研究. 武汉: 长江出版社, 2008.]
[8]	Zhou Fengqin.A tentative inquiry into the changes in the flood level on Jingjiang River during the last 5000 years. // Tan Qixiang. Historical Geography. No.4. Shanghai: Shanghai People's Publishing House, 1986: 46-53.
	[周凤琴. 荆江近5000年来洪水位变迁的初步探讨. // 谭其骧. 历史地理. 第4辑. 上海: 上海人民出版社, 1986: 46-53.]
[9]	Zhou Fengqin.The periodic characteristics of Jingjiang River in its changes in the past//Tan Qixiang. Historical Geography. No.10. Shanghai: Shanghai People's Publishing House, 1992: 273-287.
	[周凤琴. 荆江历史变迁的阶段性特征. // 谭其骧. 历史地理. 第十辑. 上海: 上海人民出版社, 1992: 273-287.]
[10]	Zhu Cheng, Yu Shiyong, Lu Chuncheng.The study of Holocene environmental archaeology and extreme flood disaster in the Three Gorges of the Changjiang River and the Jianghan Plain. Acta Geographica Sinica, 1997, 52(3): 268-278.
	[朱诚, 于世永, 卢春成. 长江三峡及江汉平原地区全新世环境考古与异常洪涝灾害研究. 地理学报, 1997, 52(3): 268-278.]
[11]	Xie Yuanyun, Li Changan, Wang Qiuliang, et al.Sedimentary records of paleoflood events during the last 3000 years in Jianghan Plain. Scientia Geographica Sinica, 2007, 27(1): 81-84.
	[谢远云, 李长安, 王秋良, 等. 江汉平原近3000年来古洪水事件的沉积记录. 地理科学, 2007, 27(1): 81-84.]
[12]	Liu Peilin.The cyclic geography study on the historical floods in the Yangtze River. Advance in Earth Sciences, 2000, 15(5): 503-508.
	[刘沛林. 长江流域历史洪水的周期地理学研究. 地球科学进展, 2000, 15(5): 503-508.]
[13]	Li Lan, Wu Li, Zhu Cheng, et al.Relationship between archaeological sites distribution and environment from 1.15 Ma BP to 278 BC in Hubei Province. Journal of Geographical Sciences, 2011, 21(5): 909-925.
[14]	Wang Hongxing.Qujialing: Prehistoric Culture in the Middle Reaches of the Yangtze. Beijing: Cultural Relics Press, 2007.
[15]	Zhu C, Zheng C, Ma C, et al.Identifying paleoflood deposits archived in Zhongba Site, the Three Gorges reservoir region of the Yangtze River, China. Chinese Science Bulletin, 2005, 50(21): 2493-2504.
[16]	Zhu Cheng, Wu Li, Li Lan, et al.Research progress on Holocene environmental archaeology in the Yangtze River Valley, China. Acta Geographica Sinica, 2014, 69(9): 1268-1283.
	[朱诚, 吴立, 李兰, 等. 长江流域全新世环境考古研究进展. 地理学报, 2014, 69(9): 1268-1283.]
[17]	Yasuda Y, Fujiki T, Nasu H, et al. Environmental archaeology at the Chengtoushan site, Hunan Province, China,implications for environmental change and the rise and fall of the Yangtze River civilization. Quaternary International, 2004, 123-125: 149-158.
[18]	Hunan Provincial Institute of Archaeology and Cultural Relics, International Research Center of Japanese Culture. Chengtoushan in Lixian: Sino-Japan Cooperative Research on Environmental Archaeology in the Liyang Plain. Beijing: Cultural Relics Publishing House, 2007.
	[湖南省文物考古研究所, 国际日本文化研究中心. 澧县城头山: 中日合作澧阳平原环境考古与有关综合研究. 北京: 文物出版社, 2007.]
[19]	Guo Weimin.Culture and Society on Liyang Plain and Handong Area during the Neolithic Period. Beijing: Cultural Relics Press, 2010.
	[郭伟民. 新石器时代澧阳平原与汉东地区的文化和社会. 北京: 文物出版社, 2010.]
[20]	Wu L, Li F, Zhu C, et al.Holocene environmental change and archaeology, Yangtze River Valley, China: Review and prospects. Geoscience Frontiers, 2012, 3(6): 875-892.
[21]	Zhang Y, Huang C C, Pang J, et al.Holocene paleofloods related to climatic events in the upper reaches of the Hanjiang River valley, middle Yangtze River basin, China. Geomorphology, 2013, 195: 1-12.
[22]	Li B, Liu H, Wu L, et al.Linking the vicissitude of Neolithic cities with mid Holocene environment and climate changes in the middle Yangtze River, China. Quaternary International, 2014, 321: 22-28.
[23]	Jones D M.Environmental Archaeology: A Guide to the Theory and Practice of Methods, from Sampling and Recovery to Post-excavation. Swindon: English Heritage Publications, 2002: 17-23.
[24]	Zou Zhiqiang.Identification method of zircon. Marine Geology, 1997(2): 93-94.
	[邹志强. 锆石鉴定方法. 海洋地质, 1997(2): 93-94.]
[25]	Zhao Shaner.Crystallography and Mineralogy. Beijing: Higher Education Press, 2004.
	[赵珊茸. 结晶学及矿物学. 北京: 高等教育出版社, 2004.]
[26]	Zhang Hanzhi, Lu Huayu, Yi Shuangwen, et al.Zircon typological analyses of the major deserts/sand fields in northern China and its implication for identifying sediment source. Quaternary Sciences, 2013, 33(2): 334-344.
	[张瀚之, 鹿化煜, 弋双文, 等. 中国北方沙漠/沙地锆石形态特征及其对物源的指示. 第四纪研究, 2013, 33(2): 334-344.]
[27]	Reimer P J, Baillie M G L, Bard E, et al. IntCal09 and Marine09 radiocarbon age calibration curves, 0-50,000 years cal BP. Radiocarbon, 2009, 51(4): 1111-1150.
[28]	Huang Chunchang, Pang Jjiangli, Zha Xiaochun, et al.Prehistorical floods in the Guanzhong Basin in the Yellow River drainage area: A case study along the Qishuihe River Valley over the Zhouyuan Loess Tableland. Scientia Sinica: Terrae, 2011, 41(11): 1658-1669.
	[黄春长, 庞奖励, 查小春, 等. 黄河流域关中盆地史前大洪水研究: 以周原漆水河谷地为例. 中国科学: 地球科学, 2011, 41(11): 1658-1669.]
[29]	Zhu C, Ma C M, Xu W F, et al.Characteristics of paleoflood deposits archived in unit T0403 of Yuxi Site in the Three Gorges reservoir areas, China. Chinese Science Bulletin, 2008, 53(Suppl. I): 1-17.
[30]	Zhan Daojiang, Xie Yuebo. Paleoflood Research.Beijing: China Water & Power Press, 2001.
	[詹道江, 谢悦波. 古洪水研究. 北京: 中国水利水电出版社, 2001.]
[31]	Li F, Zhu C, Wu L, et al.Environmental humidity changes inferred from multi-indicators in the Jianghan Plain, Central China during the last 12700 years. Quaternary International, 2014, 349: 68-78.
[32]	Brown S L, Bierman P R, Lini A, et al.10000 yr record of extreme hydrologic events. Geology, 2000, 28(4): 335-338.
[33]	Kletetschka G, Banerjee S K.Magnetic stratigraphy of Chinese Loess as a record of natural fires. Geophysical Research Letters, 1995, 22(11): 1341-1343.
[34]	Shi Wei, Zhu Cheng, Xu Weifeng, et al.Relationship between abnormal phenomena of magnetic susceptibility curves of profiles and human activities at Zhongba Site in Chongqing. Acta Geographica Sinica, 2007, 62(3): 257-267.
	[史威, 朱诚, 徐伟峰, 等. 重庆中坝遗址剖面磁化率异常与人类活动的关系. 地理学报, 2007, 62(3): 257-267.]
[35]	Zhu Cheng, Ma Chunmei, Li Lan, et al.The progress in the study of environmental archaeology during the Holocene in Three Gorges Reservoir area of the Yangtze River. Earth Science Frontiers, 2010, 17(3): 222-232.
	[朱诚, 马春梅, 李兰, 等. 长江三峡库区全新世环境考古研究进展. 地学前缘, 2010, 17(3): 222-232.]
[36]	Wang Kunshan, Shi Xuefa, Liu Shengfa, et al.Spatial distribution of heavy minerals in the surface sediments from the western gulf of Thailand: Implications for sediment provenance and sedimentary environment. Quaternary Sciences, 2014, 34(3): 623-634.
	[王昆山, 石学法, 刘升发, 等. 泰国湾西部表层沉积物重矿物分布特征: 对物质来源和沉积环境的指示. 第四纪研究, 2014, 34(3): 623-634.]
[37]	Zhu Cheng, Li Lan, Liu Wanqing, et al.An Introduction to Environmental Archaeology. Beijing: Science Press, 2013.
	[朱诚, 李兰, 刘万青, 等. 环境考古概论. 北京: 科学出版社,2013.]
[38]	Shi Chenxi, Mo Duowen, Liu Hui, et al.Late Neolithic cultural evolution and environmental changes in Northern Jianghan Plain east of Hanjiang River. Quaternary Sciences, 2010, 30(2): 335-343.
	[史辰羲, 莫多闻, 刘辉, 等. 江汉平原北部汉水以东地区新石器晚期文化兴衰与环境的关系. 第四纪研究, 2010, 30(2): 335-343.]
[39]	Chen J, An Z, Head J.Variation of Rb/Sr ratios in the loess-paleosol sequences of Central China during the last 130,000 years and their implications for monsoon paleoclimatology. Quaternary Research, 1999, 51(3): 215-219.
[40]	Wang M J, Zheng H B, Xie X, et al.A 600-year flood history in the Yangtze River drainage: Comparison between a subaqueous delta and historical records. Chinese Science Bulletin, 2011, 56(2): 188-195.
[41]	Li Zhongxuan, Zhu Cheng, Zhang Guangsheng, et al.Relationship between human activity and environment of the Liaowadian Site in Hubei Province. Quaternary Sciences, 2008, 28(6): 1145-1159.
	[李中轩, 朱诚, 张广胜, 等. 湖北辽瓦店遗址地层记录的环境变迁与人类活动的关系研究. 第四纪研究, 2008, 28(6): 1145-1159.]
[42]	Shi Wei, Zhu Cheng, Li Shijie, et al.Climatic and environmental changes as well as ancient culture response in the Yangtze Gorges Region. Acta Geographica Sinica, 2009, 64(11): 1303-1318.
	[史威, 朱诚, 李世杰, 等. 长江三峡地区全新世环境演变及其古文化响应. 地理学报, 2009, 64(11): 1303-1318.]
[43]	Zhang Yufen, Li Changan, Chen Liang, et al.Magnetic fabric of Holocene palaeo-floods events in Jianghan Plain. Earth Science: Journal of China University of Geosciences, 2009, 34(6): 985-992.
	[张玉芬, 李长安, 陈亮, 等. 基于磁组构特征的江汉平原全新世古洪水事件. 地球科学: 中国地质大学学报, 2009, 34(6): 985-992.]
[44]	Wu Li.Environmental Archaeology of the Mid-Holocene Palaeofloods in the Jianghan Plain, Central China [D]. Nanjing: Nanjing University, 2013.
	[吴立. 江汉平原中全新世古洪水事件环境考古研究[D]. 南京: 南京大学, 2013.]
[45]	Yao G W.Investigation on the Yuezhouhu site in Mianyang. Jianghan Archaeology, 1986(3): 5-8.
	[姚高悟. 沔阳月洲湖遗址调查. 江汉考古, 1986(3): 5-8.]
[46]	Jingzhou Museum.The Guihuashu Neolithic site in Songzi County of Hubei Province. Archaeology, 1976(3): 187-196.
	[湖北省荆州地区博物馆. 湖北松滋县桂花树新石器时代遗址. 考古, 1976(3): 187-196.]
[47]	Peng Jinhua.Brief excavation report of the Lijiatai Site in Shashi of Hubei. Archaeology, 1995(3): 203-208.
	[彭锦华. 湖北沙市李家台遗址发掘简报. 考古, 1995(3): 203-208.]
[48]	Yang Ding'ai. The Hougang Neolithic Site in Xiejiadun of Macheng County//Chinese Society of Archaeology. Chinese Archaeology Almanac 1985. Beijing: Cultural Relics Press, 1985: 181-182.
	[杨定爱. 麻城县谢家墩后岗新石器时代遗址//中国考古学会. 中国考古学年鉴1985. 北京: 文物出版社, 1985: 181-182.]
[49]	Yi Guangshu.Four Lakes: One of the Jewels in the Jianghan Plain. Beijing: China Water & Power Press, 2008.
	[易光曙. 四湖:江汉平原的一颗明珠. 北京: 中国水利水电出版社, 2008.]
[50]	Compilation Committee of Hubei Chronicles of Water Conservancy. Hubei Chronicles of Water Conservancy. Beijing: China Water & Power Press, 2000.
	[湖北省水利志编纂委员会. 湖北水利志. 北京: 中国水利水电出版社, 2000.]
[51]	Xia Zhengkai.Environmental Archaeology: Principles and Practice. Beijing: Peking University Press, 2012.
	[夏正楷. 环境考古学: 理论与实践. 北京: 北京大学出版社, 2012.]
[52]	Wang Y, Cheng H, Edwards R L, et al.Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature, 2008, 451: 1090-1093.
[53]	Wang Y, Cheng H, Edwards R L, et al.The Holocene Asian monsoon: links to solar changes and North Atlantic climate. Science, 2005, 308: 854-857.
[54]	Zhu C, Ma C M, Yu S-Y, et al.A detailed pollen record of vegetation and climate changes in Central China during the past 16 000 years. Boreas, 2010, 39: 69-76.
[55]	Hong Y T, Hong B, Lin Q H, et al.Inverse phase oscillations between the East Asian and Indian Ocean summer monsoons during the last 12 000 years and paleo-El Niño. Earth and Planetary Science Letters, 2005, 231(3/4): 337-346.
[56]	Zhang Z, Wang S, Wu R.Environmental evolution and southwest monsoon changes in mid-Holocene recorded by lake sediments in Erhai Lake. Chinese Science Bulletin, 1999, 44(1): 94-96.
[57]	Qin J M, Lin Y S, Zhang M L, et al.High resolution records of δ13C and their paleoecological significance from stalagmites formed in Holocene Epoch in Guilin. Quaternary Sciences, 2000, 20(4): 351-358.
	[覃嘉铭, 林玉石, 张美良, 等. 桂林全新世石笋高分辨率δ13C记录及其古生态意义. 第四纪研究, 2000, 20(4): 351-358.]
[58]	Xie Yuanyun.Climatic environment change over 9 kaBP: Evidence from Jiangling area, Jianghan Plain, China [D]. Wuhan: China University of Geoscience, 2004.
	[谢远云. 江汉平原江陵地区9 kaBP以来的气候演化[D]. 武汉: 中国地质大学, 2004.]
[59]	Gu Yansheng, Ge Jiwen, Huang Junhua, et al.Climate Change and Human Activity and Its Relationship with the Evolution of the Jianghan Lakes over the Past 20000 Years. Beijing: Geological Publishing House, 2009.
	[顾延生, 葛继稳, 黄俊华, 等. 2万年来气候变化人类活动与江汉湖群演化. 北京: 地质出版社, 2009.]
[60]	Zhang Junna, Xia Zhengkai.Deposition evidences of the 4 ka BP flood events in Central China Plains. Acta Geographica Sinica, 2011, 66(5): 685-697.
	[张俊娜,夏正楷. 中原地区4 ka BP前后异常洪水事件的沉积证据. 地理学报, 2011, 66(5): 685-697.]
[61]	Wanner H, Beer J, Bütikofer J, et al.Mid- to Late Holocene climate change: an overview. Quaternary Science Reviews, 2008, 27: 1791-1828.
[62]	Deng Hui, Chen Yiyong, Jia Jingyu, et al.Distribution patterns of the ancient cultural sites in the middle reaches of the Yangtze River since 8500 a BP. Acta Geographica Sinica, 2009, 64(9): 1113-1125.
	[邓辉, 陈义勇, 贾敬禹, 等. 8500 a BP以来长江中游平原地区古文化遗址分布的演变. 地理学报, 2009, 64(9): 1113-1125.]
[63]	Da Haobo.Man-land Relationship in the Process of Civilization in the Middle Reaches of Yangtze River: A Case Study of Neolithic Age. Shanghai: Shanghai Ancient Books Publishing House, 2013.
	[笪浩波. 长江中游文明化进程中的人地关系: 以新石器时代为例. 上海: 上海古籍出版社, 2013.]
[64]	Wu W, Liu T.Possible role of the “Holocene Event 3” on the collapse of Neolithic Cultures around the Central Plain of China. Quaternary International, 2004, 117: 153-166.
[65]	Yin Hongbing.Subjugation of Sanmiao by Yu and origin of Chuman. Journal of Wuhan University of Science and Technology (Social Science Edition), 2011, 13(2): 136-142.
	[尹弘兵. 禹征三苗与楚蛮的起源. 武汉科技大学学报(社会科学版), 2011, 13(2): 136-142.]
[66]	Guo Lixin.Initial Social Complexity in the Middle Reaches of the Yangtze River (4300B.C.~2000B.C.). Shanghai: Shanghai Ancient Books Publishing House, 2005.
	[郭立新. 长江中游地区初期社会复杂化研究(4300B.C.~2000B.C.). 上海: 上海古籍出版社, 2005.]
[67]	Meng Huaping.Prehistoric Cultural Structure in the Middle Reaches of the Yangtze River. Wuhan: Yangtze Literature and Art Press, 1997.
	[孟华平. 长江中游史前文化结构研究. 武汉: 长江文艺出版社, 1997.]
[68]	Stanley J, Krom M D, Cliff R A, et al.Short contribution: Nile flow failure at the end of the Old Kingdom, Egypt: Strontium isotopic and petrologic evidence. Geoarchaeology, 2003, 18(3): 395-402.
[69]	Cullen H M, deMenocal P B, Hemming S, et al. Climate change and the collapse of the Akkadian empire: Evidence from the deep sea. Geology, 2000, 28(4): 379-382.
[70]	Staubwasser M, Sirocko F, Grootes P M, et al.Climate change at the 4.2 ka BP termination of Indus valley civilization and Holocene south Asian monsoon variability. Geophysical Research Letters, 2003, 30: 1425-1429.
[71]	Wu Wenxiang, Ge Quansheng.The possibility of occurring of the extraordinary floods on the eve of establishment of the Xia Dynasty and the historical truth of Dayu's successful regulating of flood waters. Quaternary Sciences, 2005, 25(6): 741-749.
	[吴文祥,葛全胜. 夏朝前夕洪水发生的可能性及大禹治水真相. 第四纪研究, 2005, 25(6): 741-749.]
[72]	Zhao Yan, Du Yun.Human activity and natural geographical environment of Wuhan City. Resources and Environment in the Yangtze Basin, 1998, 7(3): 278-283.
	[赵艳, 杜耘. 人类活动与武汉市自然地理环境. 长江流域资源与环境, 1998, 7(3): 278-283.]

采样位置	深度(cm)	测试编号	¹⁴C年代(a BP)	1s树轮校正年代(BC)	2s树轮校正年代(BC)	1s中值年代(cal. a BP)	2s中值年代(cal. a BP)
T0201-4	130	GZ3854	3189±23	1462(60.30%)1435	1500(100%)1420	3399±14	3410±40
T0405-6	154	GZ3855	3791±28	2283(42.95%)2248	2299(99.46%)2137	4216±18	4168±81
T0405-6	205	GZ3856	3937±24	2477(49.05%)2450	2491(96.01%)2342	4414±14	4367±75
T0405-8	250	GZ4102	4030±20	2534(75.67%)2493	2581(97.82%)2477	4464±21	4479±52
T0405-9	288	GZ3858	4119±25	2697(57.07%)2624	2714(56.47%)2579	4611±37	4597±68
T0204-12	-	GZ3859	5409±25	4327(76.72%)4282	4334(100%)4237	6255±23	6236±49

编号	深度(m)	浑圆柱状			浑圆状		四方双锥			复四方双锥			四方柱		总颗粒数	合计(%)
编号	深度(m)	颗粒数		百分比(%)		颗粒数	百分比(%)		颗粒数			百分比(%)	颗粒数	百分比(%)	颗粒数	百分比(%)
1-9	0.18	103	28.85		14	3.92	213	59.66		5	1.40		22	6.16	357	99.99
2a-19	0.37	359	32.05		18	1.61	655	58.48		30	2.68		58	5.18	1120	100
2b-25	0.49	172	30.07		13	2.27	369	64.51		6	1.05		12	2.10	572	100
3-31	0.60	129	29.25		20	4.54	264	59.86		12	2.72		16	3.63	441	100
4-51	0.99	169	29.96		22	3.90	322	57.09		9	1.60		42	7.45	564	100
5-77	1.35	170	49.28		18	5.22	139	40.29		8	2.32		10	2.90	345	100.01
5-84	1.42	247	51.14		22	4.55	198	40.99		3	0.62		13	2.69	483	99.99
6-112	1.77	441	22.98		139	7.24	1011	52.68		150	7.82		178	9.28	1919	100
7-142	2.19	162	46.96		17	4.93	152	44.06		3	0.87		11	3.19	345	100.01
7-158	2.35	217	48.44		25	5.58	181	40.40		8	1.79		17	3.79	448	100
8-175	2.56	101	30.51		23	6.95	171	51.66		15	4.53		21	6.34	331	99.99
10-218	3.41	1011	45.13		123	5.49	911	40.67		86	3.84		109,	4.87	2240	100
WCJ-1	-	535	47.26		38	3.36	506	44.70		15	1.33		38	3.36	1132	100.01
ESZ-1	-	779	48.96		30	1.89	713	44.81		12	0.75		57	3.58	1591	99.99
ESZ-2	-	602	48.67		44	3.56	531	42.93		17	1.37		43	3.48	1237	100.01
ZB-81	0.30	191	55.36		4	1.16	134	38.84		7	2.03		9	2.61	345	100
YX-04	-	53	60.92		3	3.45	28	32.18		1	1.15		2	2.30	87	100

江汉平原钟桥遗址地层揭示的史前洪水事件

Prehistoric flood events recorded at the Zhongqiao Neolithic Site in the Jianghan Plain, Central China

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