汉江上游全新世特大古洪水事件光释光测年研究

王恒松; 黄春长; 周亚利; 熊康宁

汉江上游全新世特大古洪水事件光释光测年研究

1.
贵州师范大学中国南方喀斯特研究院贵阳 550001;
2.
贵州省喀斯特山地生态环境国家重点实验室培育基地贵阳 550001;
3.
陕西师范大学旅游与环境学院西安 710062

基金项目: 国家自然科学基金重点项目(批准号:41030637)、教育部博士点基金项目(批准号: 20110202130002)、国家重大科技支撑项目(编号:2011BAC09B01)与中央高校基本科研业务费专项基金项目(编号: GK200902020,GK200901007)联合资助

详细信息

作者简介:
王恒松男 1967年出生教授资源开发与全球变化、喀斯特地貌与洞穴、石漠化综合治理 E-mail: wanghengsong796@163.com

通讯作者:
黄春长男教授 E-mail: cchuang@snnu.edu.cn

中图分类号: P532

计量

文章访问数: 684
HTML全文浏览量: 4
PDF下载量: 847
被引次数: 0

OSL Dating and Climatic Change Record of the Holocene Paleoflood Events in the Upper Reaches of Hanjiang River, China

1.
Institute of South China Karst, Guizhou Normal University, Guiyang 550001;
2.
State Key Laboratory Incubation Base for Karst Mountain Ecology Environment of Guizhou Province, Guiyang 550001;
3.
College of Tourism and Environment, Shaanxi Normal University, Xi'an 710062

摘要

摘要: 古洪水事件对中国古代文明的演变进程产生过重大影响,古洪水水文学研究是全球变化研究的前沿课题.通过野外深入考察,在汉江上游河谷阶地上,发现典型的全新世剖面中赋存古洪水滞流沉积层,记录了古洪水事件的气候水文信息.选择三个剖面系统采样,应用SAR法的Post-IR OSL技术对样品进行测年研究,获得了14个OSL年龄数据.结合样品的粒度成分和磁化率等气候替代指标测定分析,获得了全新世洪水事件与气候变化关系的记录.证明在距今9.5~8.5 ka和3.2~2.8 ka前,汉江上游经历了2个特大洪水期.该流域黄土—古土壤剖面记录了全新世早期气温回升增湿的气候,由于大气波动失稳,出现了9~8 ka前的全球降温事件;中期土壤成壤强烈,记录了温暖湿润的气候;晚期形成的现代黄土和表土层,记录了相对干旱的气候.由此揭示了在全新世早期气候波动失稳和中期向晚期过渡的气候转折时期,气候变化剧烈,降水变率增大,是导致特大古洪水事件频发的主要原因,这也是该区域气候水文事件对全球气候变化响应规律的具体表现.
- 光释光测年 /
- 全新世 /
- 古洪水事件 /
- 气候变化 /
- 汉江上游河谷
Abstract: Field investigation was carried out from Xunyang to Yunxian along the upper Hanjiang River valley, typical palaeoflood slackwater deposit interbedded in loess-like sediments were found in the profile of XTZ, NGK and JJTZ, which indicate these bedded slackwater deposits recorded the information of palaeoflood events. Systematic sampling for optical dating was carried out on these profiles. The Post-IR OSL single aliquot regeneration (SAR) protocol was used to determine equivalent and 14 OSL ages were obtained. The results show that there were two stage extreme palaeofloods occurred 9.5~8.5 ka B.P. and 3.2~2.8 ka B.P, respectively. According to the analysis of grain-size distribution and magnetic susceptibility, the relationship between Holocene palaeoflood events and climate change was established. The transitional loess (L_t) was dated to 11 500~8 500 a B.P. It has recorded the climatic shift from cold and moist to amelioration during the Early Holocene and dust storm activity gradually decreased. The Luvisol (S₀) was dated 8 500~ 3 100 a B.P. It has recorded the warm-humid climate during the mid-Holocene Climatic Optimum. This is a period with more intensified pedogenesis. The loess (L₀) was dated to 3 100 a B.P. that has recorded the climate decline during the Late Holocene and dust storms were obviously intensified to form modern loess. Environment records from all over the world revealed the temperature rising, relative precipitation increasing and climatic fluctuation during the period of 9.5~8.5 ka, which lead to abrupt climate events occured frequently such as cooling, flood and drought; during the period of 3.2~2.8 ka, that is a turning period from the Middle Holocene to the Late Holocene, climate changing to aridity, climate change intensively, atmosphere instability and precipitation variability. Therefore, climate changing and transformation were the main reason of frequent flood occurence. The climatic Hydrography event recorded during 9.5~8.5 ka and 3.2~2.8 ka represents the concrete manifestation of the hydrological system to global climate change. The regional responses of the hydrological system. It is significant to understand the regional responses of the hydrological system to global climate change.
- OSL dating /
- Holocene /
- palaeoflood event /
- weather changes /
- Upper Hanjiang River Valley

HTML全文

参考文献(72)

[1]	Page K, Nanson G, Price D J. Chronology of Murrumbidgee River paleochannels on the riverine plain, southeastern Australia [J]. Quaternary Science, 1996, 11(2): 311-326
[2]	Forman S L, Ennis G. The effect of light intensity and spectra on the reduction of thermoluminescence of nearshore sediments from Spitsbergen, Svalbard[J]. Geophysical Resiews Letters, 1991, 18(4): 1727-1730
[3]	Wintle A G, Murray A S. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols [J]. Radiation Measurements, 2006, 41(4): 369-391
[4]	Murray A S, Olley J M. Precision and accuracy in the optically stimulated luminescence dating of sedimentary quartz: A status review [J]. Geochronometria, 2002, 21(6): 1-16
[5]	Lang A, Wagner G A. Infra-red stimulated luminescence dating of Holocene colluvial sediments using the 410 nm emission[J]. Quaternary Science Reviews, 1997, 16(3): 393-396
[6]	Fuchs M, Fischer M, Reverman R. Colluvial and alluvial sediment archives temporally resolved by OSL dating: Implications for reconstructing soil erosion [J]. Quaternary Geochronology, 2010, 12(5): 269-273
[7]	赖忠平,张景昭,卢演俦. 沙漠黄土边界带湖相沉积糜地湾剖面红外释光测年[J]. 海洋地质与第四纪地质,2001,21(1):75-79 [Lai Zhongping, Zhang Jingzhao, Lu Yanchou. IRSL dating of lacustrine sediments in Midwan section from loess and desert transitional zone in China [J]. Marine Geology & Quaternary Geology, 2001, 21(1): 75-79]
[8]	Zhang J F, Zhou L P, Yue S Y. Dating fluvial sediments by optically stimulated luminescence:selection of equivalent doses for age calculation[J]. Quaternary Science Reviews, 2003, 22(3): 1123-1129
[9]	张家富,周力平,姚书春,等. 湖泊沉积物的¹⁴C和光释光测年[J]. 第四纪研究,2007,27(4):522-528 [Zhang Jiafu, Zhou Liping, Yao Shuchun, et al. Radiocarbon and optical dating of lacustrine sediments[J]. Quaternary Sciences, 2007, 27(4): 522-528]
[10]	樊启顺,赖忠平,刘向军,等. 晚第四纪柴达木盆地东部古湖泊高湖面光释光年代学[J]. 地质学报,2010,84(11):1652-1660 [Fan Qishun, Lai Zhongping, Liu Xiangjun, et al. Luminescence chronology of high lake levels of paleolakes in the Late Quaternary eastern Qaidam Basin[J]. Acta Geologica Sinica, 2010, 84(11): 1652-1660]
[11]	Zheng Y E, Zhou L P, Zhang J F. Optical dating of the upper 22 m of cored sediments from Daihai Lake, northern China[J]. Quaternary Geochronology, 2010, 21(5): 228-232
[12]	Zhao H, Lu Y C, Wang C M,et al. Re-OSL dating of aeolian and fluvial sediments from Nihewan Basin, northern China and its environmental application[J]. Quaternary Geochronology, 2010, 23(5): 159-163
[13]	王恒松,黄春长,周亚利,等. 关中西部千河流域全新世古洪水事件光释光测年研究[J]. 中国科学(D辑):地球科学,2012,42(3):390-401 [Wang Hengsong, Huang Chunchang, Zhou Yali, et al. OSL dating of the Holocene paleoflood events on the Qianhe River in the Guanzhou Basin, China[J]. Science China (Seri. D): Earth Science, 2012, 42(3): 390-401]
[14]	查小春,黄春长,庞奖励,等. 汉江上游郧西段全新世古洪水事件研究[J]. 地理学报,2012,67(5):671-680 [Zha Xiaochun, Huang Chunchang, Pang Jiangli,et al. The Holocene palaeoflood events in the Yunxi Reach in the upper reaches of Hanjiang River [J]. Acta Geographica Sinica, 2012, 67(5): 671-680]
[15]	李晓刚,黄春长,庞奖励,等. 汉江上游白河段万年尺度洪水水文学研究[J]. 地理科学,2012,32(8):971-978 [Li Xiaogang, Huang Chunchang, Pang Jiangli, et al. Palaeoflood hydrological study in the Baihe Reach in the upper reaches of the Hanjiang River[J]. Scientia Geographica Sinica, 2012, 32(8): 971-978]
[16]	王龙升,黄春长,庞奖励,等. 旬阳东段汉江全新世古洪水研究[J]. 地理科学进展,2012,31(9):1141-1148 [Wang Longsheng, Huang Chunchang, Pang Jiangli, et al. Holocene palaeofloods recorded in the East Xunyang Reach in the Upper Hanjiang River[J]. Progress in Geography, 2012, 31(9): 1141-1148]
[17]	乔晶,庞奖励,黄春长,等. 汉江上游郧县段全新世古洪水滞流沉积物特征[J]. 地理科学进展,2012,31(11):1467-1474 [Qiao Jing, Pang Jiangli, Huang Chunchang, et al. Characteristics of palaeoflood slackwater deposits of Yunxian county in the upper reaches of the Hanjiang River[J]. Progress in Geography, 2012, 31(11): 1467-1474]
[18]	周亮,黄春长,周亚利,等. 汉江上游郧县段全新世特大洪水事件光释光测年研究[J]. 长江流域资源与环境,2013,22(4):502-511 [Zhou Liang, Huang Chunchang, Zhou Yali, et al. OSL dating of the palaeoflood events in the Yunxian Reach of the Upper Hanjiang River[J]. Resources and Environment in the Yangtze Basin, 2013, 22(4): 502-511]
[19]	顾洪亮,黄春长,周亚利,等. 汉江上游湖北段低阶地风成黄土—古土壤释光测年研究[J]. 第四纪研究,2012,32(3):516-526 [Gu Hongliang, Huang Chunchang, Zhou Yali, et al. OSL dating of the Holocene eolian loess and palaeosol on the low terrace land in the upper Hanjiang River valley[J]. Quaternary Sciences, 2012, 32(3): 516-526]
[20]	乔晶,庞奖励,黄春长,等. 汉江上游郧县前坊段全新世古洪水水文学研究[J]. 长江流域资源与环境,2012,21(5):533-539 [Qiao Jing, Pang Jiangli, Huang Chunchang, et al. Palaeoflood hydrological study in the Qianfang section of Yunxian county in the upper reaches of the Hanjiang River[J]. Resources and Environment in the Yangtze Basin, 2012, 21(5): 533-539]
[21]	刘建芳,查小春,黄春长. 汉江上游郧县尚家河段全新世古洪水水文学研究[J]. 水土保持学报,2013,27(2):90-94 [Liu Jianfang, Zha Xiaochun, Huang Chunchang. Palaeoflood hydrological study in the Yun County Reach in the upper reaches of the Hanjiang River [J]. Journal of Soil and Water conservation, 2013, 27(2): 90-94]
[22]	吴帅虎,庞奖励,黄春长,等. 汉江上游郧县辽瓦店全新世古洪水研究[J]. 水土保持通报,2012,32(6):182-186 [Wu Shuaihu, Pang Jiangli, Huang Chunchang, et al. Palaeoflood study in Liaowadian site of Yunxian county in upper reaches of Hanjiang River[J]. Bulletin of Soil and Water Conservation, 2012, 32(6): 182-186]
[23]	虎亚伟,庞奖励,黄春长,等. 汉江上游郧西段全新世古洪水水文学研究[J]. 自然灾害学报,2012,21(5):55-59 [Hu Yawei, Pang Jiangli, Huang Chunchang, et al. Hydrological study on Holocene palaeoflood at Yunxi section of upper reaches of Hanjiang River[J]. Journal of Natural Disasters, 2012, 21(5): 55-59]
[24]	许洁,黄春长,庞奖励,等. 汉江上游安康东段全新世古洪水沉积学与水文学研究[J]. 湖泊科学,2013,25(3):445-454 [Xu Jie, Huang Chunchang, Pang Jiangli, et al. Sedimentological and hydrological studies of the palaeoflood events in the Ankang east section in the upper reaches of the Hanjiang River[J]. Journal of Lake Science, 2013, 25(3): 445-454]
[25]	吴帅虎,庞奖励,黄春长,等. 汉江上游河谷古洪水滞流沉积物特征[J]. 土壤通报,2012,44(2):271-276 [Wu Shuaihu, Pang Jiangli, Huang Chunchang, et al. The palaeoflood slackwater sediments feature in the valley of the upper reaches of the Hanjiang River [J]. Journal of Soil Science, 2012, 44(2): 271-276]
[26]	杨建超,庞奖励,黄春长,等. 汉江上游郧县辽瓦店剖面粒度组成特征及其意义[J]. 中国沙漠,2013,33(3):682-687 [Yang Jianchao,Pang Jiangli, Huang Chunchang, et al. Grain-size distribution and significance in Liaowadian Profile in the Upper Hanjiang River Valley, China[J]. Journal of Desert Research, 2013, 33(3): 682-687]
[27]	王朝建,庞奖励,黄春长,等. 汉江上游谷地黄褐土粒度组成特征及其意义[J]. 陕西师范大学学报:自然科学版,2012,40(3):76-80 [Wang Chaojian, Pang Jiangli, Huang Chunchang, et al. The grain construction of the yellow cinamon soil and its significance in the upper reaches of Hanjiang valley [J]. Journal of Shaanxi Normal University: Natural Science Edition, 2012, 40(3): 76-80]
[28]	杨永德,邹宁,郭希望,等. 汉江上游水文特性的初步分析[J]. 水文,1997,9(2):54-56 [Yang Yongde, Zou Ning, Guo Xiwang, et al. Preliminary analysis of hydrological characteristics in the upper reaches of the Hanjiang River[J]. Journal of China Hydrology, 1997, 9(2): 54-56]
[29]	Benito G, Thorndycraft V R. Palaeoflood hydrology and its role in applied hydrological sciences [J]. Journal of Hydrology, 2005, 313(8): 3-15
[30]	Sridhar A. A mid-late Holocene flood record from the alluvial reach of the Mahi River, Western India [J]. Catena, 2007, 70(5): 330-339
[31]	Thorndycraft V R, Benito G. The Holocene fluvial chronology ofSpain: evidence from a newly compiled radiocarbon database [J]. Quaternary Science Reviews 2006, 25(1): 223-234
[32]	Sheffer N A, Rico M, Enzel Y, et al. The palaeoflood record of the Gardon River, France: A comparison with the extreme 2002 flood event [J]. Geomorphology, 2008, 98(12): 71-83
[33]	Huang Chunchang, Pang Jiangli, Zha Xiaochun, et al. Extraordinary floods of 4 100-4 000 a B.P. recorded at the late neolithic ruins in the Jinghe River gorges, middle reach of the Yellow River, China [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 289(6): 1-9
[34]	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[J]. 中国科学(D辑):地球科学,2011,41(11):1658-1669 [Huang Chunchang, Pang Jiangli, Zha Xiaochun, et al. Prehistorical floods in the Guanzhong Basin in the Yellow River drainage area[J]. Science China (Seri. D): Earth Science, 2011, 41(11): 1658-1669]
[35]	Huang Chunchang, Pang Jiangli, Zha Xiaochun, et al. Extraordinary floods related to the climatic event at 4200 a BP on the Qishuihe River, middle reaches of the Yellow River, China [J]. Quaternary Science Reviews, 2011, 30(8): 460-468
[36]	Huang Chunchang, Pang Jiangli, Zha Xiaochun, et al. Impact of monsoonal climatic change on Holocene overbank flooding along theSushui River within the Middle Reaches of the Yellow River, China [J]. Quaternary Science Reviews, 2007, 26(12): 2247-2264
[37]	李瑜琴,黄春长,查小春,等. 泾河中游龙山文化晚期特大洪水水文学研究[J]. 地理学报,2009,64(5):541-552 [Li Yuqin, Huang Chunchang, Zha Xiaochun, et al. Palaeoflood occurrence in the late period of the Longshan Culture in the middle reaches of the Jinghe River[J]. Acta Geographica Sinca, 2009, 64(5): 541-552]
[38]	Prescott J R, Hutton J T. Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long-term time variations [J]. Radiation Measurements, 1994, 23(7): 497-500
[39]	Lai Z P, Zller L, Fuchsb M,et al. Alpha efficiency determination for OSL of quartz extracted from Chinese loess [J]. Radiation Measurements, 2008, 43(8): 767-770
[40]	Adamiec G, Aitken M J. Dose-rate conversion factors: update [J]. Ancient TL, 1998, 16(4/5/6): 37-50
[41]	Aitken M J. An Introduction to Optical Dating [M]. London: Oxford University Press, 1998: 1-359
[42]	Murray A S, Wintle A G. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol [J]. Radiation Measurements, 2000, 32(5): 57-73
[43]	Wintle A G, Murray A S. Luminescence sensitivity changes in quartz [J]. Radiation Measurements, 1999, 30(8): 107-118
[44]	Steffen D, Preusser F, Schlunegger F. OSL quartz age underestimation due to unstable signal components [J]. Quaternary Geochronology, 2009, 4(5): 353-362
[45]	Ou X J, Xu L B, Lai Z P,et al. Potential of quartz OSL dating on moraine deposists from eastern Tibetan Plateau using SAR protocol [J]. Quaternary Geochronology, 2010, 5(6): 257-262
[46]	Bailey R M, Singarayer J S, Ward S,et al. Identification of partial resetting using De as a function of illumination time [J]. Radiation Measurements, 2003, 37(4): 511-518
[47]	Li S H. Optical dating: insufficiently bleached sediments [J]. Radiation Measurements, 1994, 23(23): 563-567
[48]	黄春长,庞奖励,黄萍,等. 关中盆地西部黄土台塬全新世气候事件研究[J]. 干旱区地理,2002,25(1):10-15 [Huang Chunchang, Pang Jiangli, Huang Ping, et al. Holocene climatic events on the loess tableland in the western Guanzhong Basin,China[J]. Arid Land Geography, 2002, 25(1): 10-15]
[49]	殷春敏,邱维理,李容全. 全新世华北平原古洪水 [J]. 北京师范大学学报:自然科学版,2001,37(2):280-284 [Yin Chunmin, Qiu Weili, Li Rongquan. Holocene paleofloods in the North China Plain [J]. Journal of Beijing Normal University: Natural Science, 2001, 37(2): 280-284]
[50]	Huang C C, Pang J L, Chen S E,et al. Charcoal records of the fire history in the Holocene loss-soil sequences over the Southern Loess Plateau of China [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 239(2): 28-44
[51]	庞奖励,黄春长,周亚利,等. 汉江上游谷地全新世风成黄土及其成壤改造特征[J]. 地理学报,2011,66(11):1562-1573 [Pang Jiangli, Huang Chunchang, Zhou Yali, et al. Holocene aeolian loess and its pedogenic modification in the Upper Hanjiang River Valley, China[J]. Acta Geographica Sinica, 2011, 66(11): 1562-1573]
[52]	Dong J G, Wang Y J, Cheng H,et al. A high-resolution stalagmite record of the Holocene East Asian monsoon from Mt Shennongjia, central China [J]. Holocene, 2010, 20(2): 257-264
[53]	姜修洋,何尧启,沈川洲,等. 全新世黔北降水特征的石笋记录及适宜期结束时间在亚洲季风区的不等时性[J]. 科学通报,2012,57(1):73-79 [Jiang Xiouyang, He Yaoqi, Shen Chuanzhou, et al. Stalagmite-inferred Holocene precipitation in northern Guizhou Province, China, and asynchronous termination of the climatic optimum in the Asian monsoon territory[J]. Chinese Science Bulletin, 2012, 57(1): 73-79]
[54]	邵晓华,汪永进,程海,等. 全新世季风气候演化与干旱事件的湖北神农架石笋记录[J]. 科学通报,2006,51(1):80-86 [Shao Xiaohua,Wang Yongjin,Cheng Hai, et al. Holocene climate evolution Stalagmite-inferred Holocene Monsoon climate evolution and drought events in Shennongjia Hubei province, China[J]. Chinese Science Bulletin, 2006, 51(1): 80-86]
[55]	朱诚,马春梅,黄林燕,等. 南京江北地区9490~4840 aB.P.环境演变的地层记录研究[J]. 地质论评,2005,51(3):347-352 [Zhu Cheng, Ma Chunmei, Huang Linyan, et al. Stratigraphic record of environmental evolution during 9490~4840 a B.P. on the north bank of the Yangtze River, Nanjing area[J]. Geological Review, 2005, 51(3): 347-352]
[56]	薛滨,瞿文川,吴艳宏,等. 太湖晚冰期—全新世气候、环境变化的沉积记录[J]. 湖泊科学,1998,10(2):30-36 [Xue Bin,Qu Wenchuan, Wu Yanhong, et al. Sedimentological record of paleoenvironment of Taihu Lake in Late-Glacial to Holocene[J]. Journal of Lake Science, 1998, 10(2): 30-36]
[57]	宋长青,孙湘君,Saito Y. 冲绳海槽B-3GC钻孔柱状样花粉记录的古环境信息[J]. 科学通报,2001,46(2):153-158 [Song Changqing, Sun Xiangjun, Saito Y. Pollen records of B-3GC drilling cores of paleoenvironmental information of Okinawa Trough[J]. Chinese Science Bulletin, 2001, 46(2): 153-158]
[58]	吴敬禄,沈吉,王苏民,等. 新疆艾比湖地区湖泊沉积记录的早全新世气候环境特征[J]. 中国科学(D辑):地球科学,2003,33(6):569-574 [Wu Jinglu, Shen Ji, Wang Sumin, et al. Lake sedimentological record of paleoenvironment of Ebinur Lake in Early Holocene[J]. Science China (Seri. D): Earth Science, 2003, 33(6): 569-574]
[59]	Sarah L B, Paul R B, Andrea L, et al. 10000 yr record of extreme hydrologic events[J]. Geology, 2000, 28(4): 335-338
[60]	Harrison S P, Yu G, Tarasov P E. Late Quaternary lake-level record from northern Eurasia [J]. Quaternary Research, 1996, 45(2): 138-159
[61]	Benito G, Alfonso Sopeña, Yolanda Sáchez-Moya,et al. Palaeoflood record of the Tagus River(Central Spain) during the Late Pleistocene and Holocene[J]. Quaternary Seience Reviews, 2003, 22(4/5/6): 1737-1756
[62]	Benito G, Thomdycraft V R, Rico M,et al. Palaeoflood and floodplain records from Spain:Evidence for long- term climate variability and environrnental changes[J]. Geomorphology, 2008, 101(5/6/7): 68-77
[63]	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[J]. 地理科学,2007,27(1):81-84 [Xie Yuanyun, Li Chang'an, Wang Qiuliang, et al. Sedimentary records of paleoflood events during the last 3000 years in Jianghan Plain[J]. Scientia Geographica Sinica, 2007, 27(1): 81-84]
[64]	朱诚,郑朝贵,马春梅,等. 长江三峡库区中坝遗址地层古洪水沉积判别研究[J]. 科学通报,2005,50(20):2240-2250 [Zhu Cheng, Zheng Chaogui, Ma Chunmei, et al. Study on identification paleoflood deposits in Zhongba Site in Yangtze River Three Gorges[J]. Chinese Science Bulletin, 2005, 50(20): 2240-2250]
[65]	王恒松,黄春长,周亚利,等. 渭河咸阳段全新世古洪水事件光释光测年研究[J]. 沉积学报,2012,30(2):102-111 [Wang Hengsong, Huang Chunchang, Zhou Yali, et al. OSL dating research of palaeoflood events in the middle reaches of the Weihe River[J]. Acta Sedimentologica Sinica, 2012, 30(2): 102-111]
[66]	O’Brien S R, Mayewski P A, Meeker L D,et al. Complexity of Holocene climate as reconstructed from a Greenland ice core[J]. Science, 1995, 270(5244): 1962-1964
[67]	Peng Y, Xiao J, Nakamura T, et al. Holocene East Asian monsoonal precipitation pattern revealed by grain-size distribution of core sediments of the Daihai Lake in Inner Mongolia of north central China[J].Earth and Planetary Science Letters, 2005, 233(3/4): 467-479
[68]	Wang Y, Chan H, Edwards R L,et al. The Holocene Asian monsoon: Links to solar changes and North Atlantic climate [J]. Science, 2005, 308: 854-857
[69]	Yang D Y, Yu G, Xie Y B,et al. Sedimentary records of large Holocene floods from the middle reaches of the Yellow River, China [J]. Geomorphology, 2000, 33(1/2): 73-88
[70]	Booth R K, Jackson S T, Forman S L,et al. A severe centennial-scale drought in mid-continental North America 4200 years ago and apparent global linkages [J]. Holocene, 2005, 15: 321-328
[71]	Arz H W, Lamy F, Ptzold J. A pronounced dry event recorded around 4.2 ka in brine sediments from the northern Red Sea [J]. Quaternary Research, 2006, 66(3): 432-441
[72]	吴文祥,刘东生. 4000aB.P.前后降温事件与中华文明的诞生[J]. 第四纪研究,2001,21(5):443-451 [Wu Wenxiang, Liu Tungsheng. 4 000a B.P. Event and its implications for the origin of ancient Chinese civilization [J]. Quaternary Sciences, 2001, 21(5): 443-451]

[1]	张振球, 张伟宏, 刘树双, 翟秀敏, 邵庆丰. 贵州石笋记录的中晚全新世东亚夏季风变化 . 沉积学报, 2023, 41(1): 196-205. doi: 10.14027/j.issn.1000-0550.2021.077
[2]	吴小力, 李荣西, 李小刚, 赵帮胜, 刘福田, 覃小丽, 赵迪, 刘齐, 张艳妮. 青藏高原东北缘宁南盆地晚古近纪气候变化及其驱动机制 . 沉积学报, 2023, 41(1): 206-218. doi: 10.14027/j.issn.1000-0550.2021.082
[3]	张威, 马瑞丰, 刘亮, 杨蝉玉, 刘畅, 柴乐. 辽东半岛全新世沉积物记录的古气候变化研究进展 . 沉积学报, 2022, 40(5): 1355-1366. doi: 10.14027/j.issn.1000-0550.2021.009
[4]	薛红盼, 曾方明. 青海湖东岸全新世风成沉积地球化学特征及其古气候意义 . 沉积学报, 2021, 39(5): 1198-1207. doi: 10.14027/j.issn.1000-0550.2020.066
[5]	张文静, 李志忠, 靳建辉, 郑斐, 李志星, 徐晓琳, 程延. 海南岛东北海岸风沙沉积的光释光年代学意义 . 沉积学报, 2021, 39(4): 995-1003. doi: 10.14027/j.issn.1000-0550.2020.033
[6]	温瑞艳, 庞奖励, 黄春长, 查小春, 周亚利, 雷晨, 炊郁达, 毛沛妮. 天水樊家城黄土剖面记录的全新世环境及人地关系变化研究 . 沉积学报, 2020, 38(2): 349-357. doi: 10.14027/j.issn.1000-0550.2019.016
[7]	刘璐, 庞奖励, 黄春长, 周亚利, 周强, 胡迎, 张玉柱, 郭永强, 陈莹璐, 戎晓庆, 尚瑞清. 黄河上游官亭盆地古洪积扇前沿全新世地层序列研究 . 沉积学报, 2020, 38(6): 1239-1248. doi: 10.14027/j.issn.1000-0550.2020.009
[8]	王兆夺, 黄春长, 庞奖励, 刘安娜, 周亚利, 查小春. 甘肃庄浪全新世黄土土壤物源分析及古气候恢复重建 . 沉积学报, 2020, 38(4): 781-789. doi: 10.14027/j.issn.1000-0550.2019.077
[9]	李卓仑, 高有红, 李若兰, 王乃昂, 朱瑞霞. 阿拉善沙漠全新世钙质根管形成机制及其古环境指示意义:来自微观形态学证据 . 沉积学报, 2018, 36(6): 1131-1138. doi: 10.14027/j.issn.1000-0550.2018.111
[10]	白雪莘, 张卫国, 董艳, 潘大东, 王张华, 孙千里, 陈静, 陈中原, 刘晋嫣. 长江三角洲全新世地层中潮滩沉积磁性特征及其古环境意义 . 沉积学报, 2016, 34(6): 1165-1175. doi: 10.14027/j.cnki.cjxb.2016.06.014
[11]	. 全新世以来巴里坤湖面积变化及气候环境记录 . 沉积学报, 2014, 32(1): 93-100.
[12]	. 青藏高原纳木错湖近150年来气候变化的湖泊沉积记录 . 沉积学报, 2014, 32(4): 669-676.
[13]	. 汉江上游尚家河段全新世古洪水事件光释光测年研究 . 沉积学报, 2014, 32(2): 306-313.
[14]	. 渭河咸阳段全新世古洪水事件光释光测年研究 . 沉积学报, 2012, 30(2): 346-355.
[15]	. 中晚全新世科尔沁沙地沉积物化学特征及其气候变化 . 沉积学报, 2012, 30(3): 536-546.
[16]	. 中亚昭苏黄土剖面粒度记录的末次冰期以来气候变化历史 . 沉积学报, 2011, 29(6): 1170-1179.
[17]	赵景波李胜利. 西安高陵马坊滩渭河洪水变化研究 . 沉积学报, 2006, 24(06): 857-863.
[18]	曹红霞, 张云翔, 岳乐平, 王煜. 毛乌素沙地全新世地层粒度组成特征及古气候意义 . 沉积学报, 2003, 21(3): 482-486.
[19]	薛春汀. 关于江苏建湖庆丰剖面全新世沉积环境与海面变化关系的讨论 . 沉积学报, 2002, 20(1): 174-177.
[20]	秦作栋, 冯起. 塔克拉玛干沙漠北部平原区全新世沉积与气候变化的关系——以肖塘剖面为例 . 沉积学报, 1997, 15(1): 168-171.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 684
HTML全文浏览量: 4
PDF下载量: 847
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

汉江上游全新世特大古洪水事件光释光测年研究

作者简介:
王恒松男 1967年出生教授资源开发与全球变化、喀斯特地貌与洞穴、石漠化综合治理 E-mail: wanghengsong796@163.com

通讯作者:
黄春长男教授 E-mail: cchuang@snnu.edu.cn

计量

OSL Dating and Climatic Change Record of the Holocene Paleoflood Events in the Upper Reaches of Hanjiang River, China

计量

目录

汉江上游全新世特大古洪水事件光释光测年研究

1. 贵州师范大学中国南方喀斯特研究院贵阳 550001;

2. 贵州省喀斯特山地生态环境国家重点实验室培育基地贵阳 550001;

3. 陕西师范大学旅游与环境学院西安 710062

作者简介:
王恒松男 1967年出生教授资源开发与全球变化、喀斯特地貌与洞穴、石漠化综合治理 E-mail: wanghengsong796@163.com

通讯作者: 黄春长男教授 E-mail: cchuang@snnu.edu.cn

English Abstract

OSL Dating and Climatic Change Record of the Holocene Paleoflood Events in the Upper Reaches of Hanjiang River, China

1. Institute of South China Karst, Guizhou Normal University, Guiyang 550001;

2. State Key Laboratory Incubation Base for Karst Mountain Ecology Environment of Guizhou Province, Guiyang 550001;

3. College of Tourism and Environment, Shaanxi Normal University, Xi'an 710062

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

汉江上游全新世特大古洪水事件光释光测年研究

作者简介: 王恒松 男 1967年出生 教授 资源开发与全球变化、喀斯特地貌与洞穴、石漠化综合治理 E-mail: wanghengsong796@163.com

通讯作者: 黄春长 男 教授 E-mail: cchuang@snnu.edu.cn

计量

出版历程

OSL Dating and Climatic Change Record of the Holocene Paleoflood Events in the Upper Reaches of Hanjiang River, China

计量

出版历程

目录

汉江上游全新世特大古洪水事件光释光测年研究

1. 贵州师范大学中国南方喀斯特研究院 贵阳 550001; 2. 贵州省喀斯特山地生态环境国家重点实验室培育基地 贵阳 550001; 3. 陕西师范大学旅游与环境学院 西安 710062

作者简介: 王恒松 男 1967年出生 教授 资源开发与全球变化、喀斯特地貌与洞穴、石漠化综合治理 E-mail: wanghengsong796@163.com

通讯作者: 黄春长 男 教授 E-mail: cchuang@snnu.edu.cn

English Abstract

OSL Dating and Climatic Change Record of the Holocene Paleoflood Events in the Upper Reaches of Hanjiang River, China

1. Institute of South China Karst, Guizhou Normal University, Guiyang 550001; 2. State Key Laboratory Incubation Base for Karst Mountain Ecology Environment of Guizhou Province, Guiyang 550001; 3. College of Tourism and Environment, Shaanxi Normal University, Xi'an 710062

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
王恒松男 1967年出生教授资源开发与全球变化、喀斯特地貌与洞穴、石漠化综合治理 E-mail: wanghengsong796@163.com

通讯作者:
黄春长男教授 E-mail: cchuang@snnu.edu.cn

1. 贵州师范大学中国南方喀斯特研究院贵阳 550001;

2. 贵州省喀斯特山地生态环境国家重点实验室培育基地贵阳 550001;

3. 陕西师范大学旅游与环境学院西安 710062

作者简介:
王恒松男 1967年出生教授资源开发与全球变化、喀斯特地貌与洞穴、石漠化综合治理 E-mail: wanghengsong796@163.com

通讯作者: 黄春长男教授 E-mail: cchuang@snnu.edu.cn

1. Institute of South China Karst, Guizhou Normal University, Guiyang 550001;

2. State Key Laboratory Incubation Base for Karst Mountain Ecology Environment of Guizhou Province, Guiyang 550001;

3. College of Tourism and Environment, Shaanxi Normal University, Xi'an 710062