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中国沙漠  2019, Vol. 39 Issue (2): 86-95    DOI: 10.7522/j.issn.1000-694X.2018.00058
    
基于粒度数据重建的近2 000 a新疆博斯腾湖区域风沙活动
周刚平, 黄小忠, 王宗礼, 张军, 谢海超
兰州大学 资源环境学院/西部环境教育部重点实验室, 甘肃 兰州 730000
Eolian Activity History Reconstructed by Bosten Lake Grain Size Data over the Past~2 000 Years
Zhou Gangping, Huang Xiaozhong, Wang Zongli, Zhang Jun, Xie Haichao
College of Earth and Environmental Sciences/MOE Key Laboratory of Western China's Environmental System, Lanzhou University, Lanzhou 730000, China
 全文: PDF(10639 KB)  
摘要: 干旱区风沙活动对全球环境和区域人类活动都可能造成巨大的影响。位于亚洲内陆的塔里木盆地是全球风沙活动最强烈的地区之一,然而该区域历史时期高分辨率的风沙活动记录比较缺少。博斯腾湖作为中国最大的内陆淡水湖,东南角湖区三面为沙丘包围,远离河流影响,可获得该区域的风沙活动记录。以博斯腾湖东南角钻取的长2.07 m沉积岩芯(BH08B)为研究对象,基于AMS 14C年代学框架,利用粒级-标准偏差模型和端元分析模型,提取钻孔沉积物中对环境变化敏感的粒度组分。结果表明:粒径变化的敏感组分2(>19.35 μm)和端元分析的风成沙端元EM2+EM3含量具有很好的一致性,均能指示研究区近2 000 a的风沙活动历史。重建结果表明:280-410 AD和1320-1800 AD两个时段风沙活动最强,410-1320 AD风沙活动最弱,而70-280 AD和1800 AD以来两个时段整体表现为较弱、低频率风沙活动。对比其他指示温度和湿度变化的古气候指标显示:风沙活动主要出现在冷期(如魏晋南北朝冷期和小冰期),气候变冷,西伯利亚高压强度增加,春季高压解体时风力增强,致使风沙活动频繁;干旱区风沙活动主要受温度控制,与干湿变化相关性不明显。值得注意的是,区域在280-410 AD的强风沙活动可能导致了楼兰古城的废弃。
关键词: 南疆博斯腾湖粒级-标准偏差端元分析风沙活动    
Abstract: Eolian activity in arid areas can result in global-scale climate change as well as severely disrupt regional human activities. The Tarim Basin, located in the interior of Asia, is one of the regions with the strongest eolian activity in the world. However, high resolution records of late Quaternary eolian activity in this area are relatively scarce. Here we present the results of grain-size based regional eolian activity reconstructions from the Bosten Lake in the Yanqi Basin, Xinjiang, NW China. The sediment core, BH08B, was drilled in the southeastern part of Bosten Lake, which is surrounded by sand dunes and is isolated from fluvial influence. As two usually used methods of environment dynamics in arid area, the grain size-standard deviation curves and end-menmber models extracted grain-size sensitive component 2 (>19.35 μm) and end-member 2 and 3 were used to reconstruct the history of eolian activity over the past nearly 2 000 years. The grain-size sensitive component 2 (>19.35 μm) and end-member 2 and 3 extracted by grain size-standard deviation curves and end-member models should relate to eolian activities in this region, and the two proxies were used to reconstruct the history of eolian activity over the past nearly 2000 years. The results indicate the periods 280-410 AD and 1320-1800 AD were characterized by the most intense eolian activity. Conversely the period 410-1320 AD was characterized by the weakest eolian activity. However, 70-280 AD and since 1800 AD, eolian activity was also very low with few distinct accretionary episodes. On the basis of comparisons with independent climate records, phases of intense eolian activity mainly occurred during cold, dry climatic conditions, whilst weak eolian activity corresponded to relatively warm and humid climatic condition. The variable of temperature was found to provide highest explanation for intensity of eolian processes. Lower temperatures likely resulted in a strengthening of the Siberian High (SH) and then strengthen the ground wind when SH breaking out in spring accordingly. It is worth noting that the stronger eolian activity during 280-410 AD recorded in the Bosten Lake may have led to the abandonment of the ancient city of Loulan on the northern side of the Tarim Basin.
Key words: Southern Xinjiang    Bosten Lake    grain size-standard deviation    end-member analysis    eolian activity
收稿日期: 2018-03-28 出版日期: 2019-04-11
:  P531  
基金资助: 国家自然科学基金项目(41571182);国家重点研发计划项目(2017YFA0603403)
通讯作者: 黄小忠(E-mail:xzhuang@lzu.edu.cn)     E-mail: xzhuang@lzu.edu.cn
作者简介: 周刚平(1991-),男,四川达州人,硕士研究生,研究方向为湖泊沉积学与环境变化。E-mail:zhougp16@lzu.edu.cn
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引用本文:

周刚平, 黄小忠, 王宗礼, 张军, 谢海超. 基于粒度数据重建的近2 000 a新疆博斯腾湖区域风沙活动[J]. 中国沙漠, 2019, 39(2): 86-95.

Zhou Gangping, Huang Xiaozhong, Wang Zongli, Zhang Jun, Xie Haichao. Eolian Activity History Reconstructed by Bosten Lake Grain Size Data over the Past~2 000 Years. Journal of Desert Research, 2019, 39(2): 86-95.

链接本文:

http://www.desert.ac.cn/CN/10.7522/j.issn.1000-694X.2018.00058        http://www.desert.ac.cn/CN/Y2019/V39/I2/86

[1] Jia R,Liu Y,Chen B,et al.Source and transportation of summer dust over the Tibetan Plateau[J].Atmospheric Environment,2015,123:210-219.
[2] 杨兴华,李红军,何清,等.塔克拉玛干沙漠荒漠过渡带春季风沙活动特征——以肖塘为例[J].中国沙漠,2012,32(4):915-920.
[3] Chen S,Huang J,Kang L,et al.Emission,transport,and radiative effects of mineral dust from the Taklimakan and Gobi deserts:comparison of measurements and model results[J].Atmospheric Chemistry & Physics,2017,17(1/2/3):1-43.
[4] Ridgwell A J.Dust in the Earth system:the biogeochemical linking of land,air and sea[J].Philosophical Transactions Mathematical Physical & Engineering Sciences,2002,360(1801):2905-2924.
[5] Shen J.Spatiotemporal variations of Chinese lakes and their driving mechanisms since the Last Glacial Maximum:a review and synthesis of lacustrine sediment archives[J].Chinese Science Bulletin,2013,58(1):17-31.
[6] Yang X,Preusserb F,Radtkec U.Late Quaternary environmental changes in the Taklamakan Desert,western China,inferred from OSL-dated lacustrine and aeolian deposits[J].Quaternary Science Reviews,2006,25(9):923-932.
[7] Long H,Shen J,Chen J,et al.Holocene moisture variations over the arid central Asia revealed by a comprehensive sand-dune record from the central Tian Shan,NW China[J].Quaternary Science Reviews,2017,174:13-32.
[8] 李晋昌,苏志珠,胡光印.风沙活动强度的常用判断指标及其应用评述[J].中国沙漠,2010,30(4):788-795.
[9] 陈发虎,黄小忠,张家武,等.新疆博斯腾湖记录的亚洲内陆干旱区小冰期湿润气候研究[J].中国科学,2007,37(1):77-85.
[10] 黄小忠,陈发虎,肖舜,等.新疆博斯腾湖沉积物粒度的古环境意义初探[J].湖泊科学,2008,20(3):291-297.
[11] Chen F,Qiang M,Zhou A,et al.A 2000-year dust storm record from Lake Sugan in the dust source area of arid China[J].Journal of Geophysical Research Atmospheres,2013,118(5):1-12.
[12] Qiang M,Liu Y,Jin Y,et al.Holocene record of aeolian activity from Genggahai Lake,northeastern Qinghai-Tibetan Plateau,China[J].Geophysical Research Letters,2014,41(2):589-595.
[13] 王永波,刘兴起,张恩楼,等.青藏高原北部可可西里地区近4000年来尘暴事件初探——来自库赛湖沉积物粒度的证据[J].沉积学报,2009,27(4):691-696.
[14] 程其畴.博斯腾湖研究[M].南京:河海大学出版社,1995:1-7.
[15] 刘强吉,武胜利.新疆博斯腾湖流域风沙环境特征[J].中国沙漠,2015,35(5):1128-1135.
[16] 王苏民.窦鸿身.中国湖泊志[M].北京:科学出版社,1998:490.
[17] 黄小忠.新疆博斯腾湖记录的亚洲中部干旱区全新世气候变化研究[D].兰州:兰州大学,2006.
[18] 周刚.新疆博斯腾湖记录的我国西北干旱区过去2000年气候变化研究[D].兰州:兰州大学,2011.
[19] Lu H,An Z.Paleoclimatic significance of grain size of loess-palaeosol deposit in Chinese Loess Plateau[J].Science China Earth Sciences,1998,41(6):626-631.
[20] Sun J,Zhu X.Temporal variations in Pb isotopes and trace element concentrations within Chinese eolian deposits during the past 8 Ma:implications for provenance change[J].Earth & Planetary Science Letters,2010,290(3/4):438-447.
[21] Ding Z L,Sun J M,Yang S L,et al.Geochemistry of the Pliocene red clay formation in the Chinese Loess Plateau and implications for its origin,source provenance and paleoclimate change[J].Geochimica Et Cosmochimica Acta,2001,65(6):901-913.
[22] 陈圣乾,王鑫,陈建徽,等.山西公海湖泊沉积物记录的大气粉尘现代过程[J].中国沙漠,2017,37(2):228-236.
[23] Wang W L,Blum P,Boulay S,et al.Mineralogy and sedimentology of pleistocene sediment in the South China Sea (ODP Site 1144)[C]//Proceedings of the Ocean Drilling Program Scientific Results,2003:184.
[24] Weltje G J.End-member modeling of compositional data:numerical-statistical algorithms for solving the explicit mixing problem[J].Mathematical Geosciences,1997,29(4):503-549.
[25] Guan Q,Pan B,Li N,et al.Loess record of the evolution history of severe sandstorms in the Tengger Desert during the Last Interglacial Period (MIS5)[J].Geosciences Journal,2010,14(2):155-162.
[26] 隆浩,王乃昂,马海州,等.腾格里沙漠西北缘湖泊沉积记录的区域风沙特征[J].沉积学报,2007,25(4):626-631.
[27] Prins M A,Vriend M,Nugteren G,et al.Late Quaternary aeolian dust input variability on the Chinese Loess Plateau:inferences from unmixing of loess grain-size records[J].Quaternary Science Reviews,2007,26(1/2):230-242.
[28] Liu X,Dong H,Yang X,et al.Late Holocene forcing of the Asian winter and summer monsoon as evidenced by proxy records from the northern Qinghai-Tibetan Plateau[J].Earth & Planetary Science Letters,2009,280(1):276-284.
[29] Paterson G A,Heslop D.New methods for unmixing sediment grain size data[J].Geochemistry Geophysics Geosystems,2015,16(12):4494-4506.
[30] Sun D,Bloemendal J,Rea D K,et al.Bimodal grain-size distribution of Chinese loess,and its palaeoclimatic implications[J].Catena,2004,55(3):325-340.
[31] 孙千里,周杰,肖举乐.岱海沉积物粒度特征及其古环境意义[J].海洋地质与第四纪地质,2001,21(1):93-95.
[32] 安福元,马海州,魏海成,等.柴达木盆地察尔汗湖相沉积物的粒度分布模式及其环境意义[J].干旱区地理,2013,36(2):212-220.
[33] 樊恒文,肖洪浪,段争虎,等.中国沙漠地区降尘特征与影响因素分析[J].中国沙漠,2002,22(6):559-565.
[34] Qiang M,Chen F,Wang Z,et al.Aeolian deposits at the southeastern margin of the Tengger Desert (China):implications for surface wind strength in the Asian dust source area over the past 20,000 years[J].Palaeogeography Palaeoclimatology Palaeoecology,2010,286(1/2):66-80.
[35] Jiang H,Ding Z.Eolian grain-size signature of the Sikouzi lacustrine sediments (Chinese Loess Plateau):implications for Neogene evolution of the East-Asian winter monsoon[J].Geological Society of America Bulletin,2010,122(5/6):843-854.
[36] Huang X Z,Chen F H,Fan Y X,et al.Dry late-glacial and early Holocene climate in arid central Asia indicated by lithological and palynological evidence from Bosten Lake,China[J].Quaternary International,2009,194(1):19-27.
[37] Ge Q,Zheng J,Fang X,et al.Winter half-year temperature reconstruction for the middle and lower reaches of the Yellow River and Yangtze River,China,during the past 2000 years[J].Holocene,2003,13(6):933-940.
[38] 姚檀栋,秦大河,田立德,等.青藏高原2 ka来温度与降水变化——古里雅冰芯记录[J].中国科学,1996,26(4):348-353.
[39] Meeker L D,Mayewski P A.A 1400-year high-resolution record of atmospheric circulation over the North Atlantic and Asia[J].Holocene,2002,12(3):257-266.
[40] Yang B,Bräuning A,Zhang Z,et al.Dust storm frequency and its relation to climate changes in Northern China during the past 1000 years[J].Atmospheric Environment,2007,41(40):9288-9299.
[41] 张自银,杨保.中国北方过去2000年沙尘事件与气候变化[J].第四纪研究,2006,26(6):905-914.
[42] An C,Zhao Y.Paleohydrological and paleoclimatic oscillations during MIS3 revealed by multi-proxies from Balikun Lake,NW China[C]//EGU General Assembly Conference Abstracts,2016.
[43] 葛全胜,郑景云,满志敏,等.过去2000年中国温度变化研究的几个问题[J].自然科学进展,2004,14(4):449-455.
[44] Huang X,Oberhänsli H,Suchodoletz H V,et al.Dust deposition in the Aral Sea:implications for changes in atmospheric circulation in central Asia during the past 2000 years[J].Quaternary Science Reviews,2011,30(25):3661-3674.
[45] He Y,Zhao C,Song M,et al.Onset of frequent dust storms in northern China at~AD 1100[J].Scientific Reports,2015,5(648):17111.
[46] Zhang D.Synoptic-climatic studies of dust fall in China since historictime[J].Scientia Sinica(Series B),1984,27(8):825-836.
[47] Feng Q,Endo K,Cheng G.Dust storms in China:a case study of dust storm variation and dust characteristics[J].Bulletin of Engineering Geology and the Environment,2002,61(3):53-261.
[48] 李世杰,王小天,夏威岚,等.青藏高原苟鲁错湖泊沉积记录的小冰期气候变化[J].第四纪研究,2004,24(5):578-584.
[49] 周爱锋.晚全新世苏干湖年纹层沉积及其环境记录[D].兰州:兰州大学,2007.
[50] Qin X,Liu J,Jia H,et al.New evidence of agricultural activity and environmental change associated with the ancient Loulan kingdom,China,around 1500 years ago[J].Holocene,2012,22(1):53-61.
[51] 谢丽.绿洲农业开发与楼兰古国生态环境的变迁[J].中国农史,2001,20(1):16-26.
[52] 玄奘.大唐西域记[M].北京:中华书局,1988.
[53] Mischke S,Liu C L,Zhang J F,et al.The world's earliest Aral-Sea type disaster:the decline of the Loulan Kingdom in the Tarim Basin[J].Scientific Reports,2017,7:43102.
[54] Wünnemann B,Mischke S,Chen F H.Holocene sedimentary record from Bosten Lake,China[J].Palaeogeography Palaeoclimatology Palaeoecology,2006,234(2):223-238.
[55] Liu C,Zhang J F,Jiao P,et al.The holocene history of lop Nur and its palaeoclimate implications[J].Quaternary Science Reviews,2016,148:163-175.
[56] Zhang J,Huang X Z,Wang Z L,et al.A late-Holocene pollen record from the western Qilian Mountains and its implications for climate change and human activity along the Silk Road,Northwestern China[J].The Holocene,2018,28:1141-1150.
[57] Herzschuh U,Tarasov P,Wünnemann B,et al.Holocene vegetation and climate of the Alashan Plateau,NW China,reconstructed from pollen data[J].Palaeogeography Palaeoclimatology Palaeoecology,2004,211(1):1-17.
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