巴丹吉林沙漠东南部末次间冰期环境演变：来自粒度、光释光（OSL）及14C测年的证据

摘要/Abstract

摘要： 巴丹吉林沙漠是中国第三大沙漠，分布着数百个大大小小的湖泊。为了探明巴丹吉林沙漠东南缘的古气候环境变迁，选取代表性的巴润宝日陶勒盖沉积露头作为研究对象，结合现代湖泊岩芯，采用C-M图、粒度频率曲线、粒度频率累计曲线、粒度参数和粒度组成等粒度特征分析方法，并结合光释光和¹⁴C年代数据，对巴丹吉林沙漠东南缘的巴润宝日陶勒盖剖面进行了研究。结果表明：粒度特征能够很好的反映研究区古环境的变化。分析表明，巴润宝日陶勒盖剖面为湖泊沉积物，其露头可能是巴润宝日陶勒盖湖泊连续发育的大湖泊的一个滨湖高地或者湖心岛；末次间冰期巴丹吉林沙漠发育有规模大于今天的湖泊，并且经历了MIS 5a和5c的暖期和MIS 5b的冷期，与末次间冰期西北地区的研究成果对比，结果是一致的；粒度频率曲线和粒度频率累计曲线的特征表明，BRGH剖面沉积物很可能就是沙漠的基底，这对于理解沙漠的形成时代和机理具有重要的意义。

关键词: 末次间冰期, 古气候环境, 粒度特征, 巴润宝日陶勒盖, 巴丹吉林沙漠

Abstract: Badain Jaran Desert is the third largest desert of China and also is the only desert in which megadunes distribute densely. The desert also develops hundreds of large and small lakes. The paleoclimatic and paleoenvironmental researches on the lake sediments are of significance for the further study on the formation mechanism of Badain Jaran Desert，etc. As the research object in this paper，Barunbaoritaolegai profile is the relatively typical one amomg these sedimentary outcrops which are located in the southeast of the Badain Jaran Desert. In previous studies，researchers had presumed the age of the sediment to the early Pleistocene. However，the detailed research on sedimentary outcrop has not been done. To ascertain paleoenvironmental evolution of southeast edge of the Badain Jaran Desert，this paper selects the representative Barunbaoritaolegai outcrop deposits as the research object. By combining modern lakes core and using the analysis methods of C-M figure，the frequency curve，the cumulative frequency curve，grain-size parameter，grain composition，and combing the results of OSL and ¹⁴C dating data，the authors carry out research on the Barunbaoritaolegai profile. Results show that combined with chronological data，the grain-size characteristics can reflect the change of the ancient environment in the study area well. According to the graph of the ages and grain-size parameters of Barunbaoritaolegai，the paleoenvironmental evolution which is reco- rded by the profile can be divided into three stages: the stage of the warm and wet climate during 106～93.65 ka BP，the stage of the dry and cold climate during 93.65～87.93 ka BP and the stage of the warm and wet climate during 87.93～81.98 ka BP. The comparative analysis of the C-M graph between Barunbaoritaolegai profile and modern lakes core indicates that the Barunbaoritaolegai profile belongs to the lacustrine deposit. The Barunbaoritaolegai outcrop is most probably a lakeside highland or an island in a lake which came from the continuous development of Barunbaoritaolegai lake. In addition，the analysis result indicates that the Badain Jaran Desert had developed lakes which are larger than today's during the last interglacial period，that the lake had experienced the warm periods of MIS 5a and 5c and cold period of MIS 5b，and that the results are consistent with those of the northwestern region in the last interglacial northwest. Furthermore，by the analysis on the characteristics of frequency curve and cumulative frequency curve，the authors find a breakthrough clue，that is the Barunbaoritaolegai profile deposits are likely to be the basement of the desert，which is of great importance for investigating the age and the formation mechanism of Badain Jaran Desert．

Key words: the last interglacial period, paleoclimate environment, characteristics of grain-size, Barunbaoritaolegai, Badain Jaran Desert

中图分类号:

P532

范小露，田明中，刘斯文. 巴丹吉林沙漠东南部末次间冰期环境演变：来自粒度、光释光（OSL）及¹⁴C测年的证据[J]. 干旱区地理, 2014, 37(5): 892-900.

FAN Xiao-lu，TIAN Ming-zhong，LIU Si-wen. Environmental change of southeastern Badain Jaran Desert during the last interglacial: evidences from the grain-size analysis，optically stimulated luminescence and radiocarbon dating[J]. , 2014, 37(5): 892-900.

参考文献

［1］ Narentuya，LIU Siwen，FAN Xiaolu，et al. Geomorphical features of the Badain Jaran desert lakes and its surrounding based on RS and GIS methods［J］. International Journal of Advancements in Computing Technology，2012，4（15）：74-80.

［2］钟德才. 中国沙海动态演化［M］. 兰州：甘肃文化出版社，1998.

［3］孙跃武，段吉业，程立人. 巴丹吉林地区中生代地层区划［J］. 长春科技大学学报，1999，29（4）：324-329.

［4］艾华国，王秀乾，冯昌寿. 巴丹吉林—腾格里盆地侏罗纪—早白垩世沉积特征［J］. 新疆石油地质，1994，15（3）：229-235.

［5］ LIAN O B，ROBERTS R G. Dating the Quaternary：Progress in luminescence dating of sediments［J］. Quaternary Science Reviews，2006，25（19-20）：2449-2468.

［6］ LI B，LI S H，WINTLE A G，et al. Isochron measurements of naturally irradiated K-feldspar grains［J］. Radiation Measurement，2007，42（8）：1315-1327.

［7］张静然. 末次间冰期以来季风边缘区黄旗海高湖面释光年代学及其环境意义［D］. 南昌：江西师范大学，2010.

［8］ CELINA C. Late Holocene lake sedimentology and climate change in southern Alberta，Canada［J］. Quaternary Research，1998，49：96-101.

［9］毕志伟，杨振京，徐建明，等. 塔里木盆地腹地第四纪沉积物粒度特征及其沉积环境［J］. 干旱区地理，2009，32（3）：335-339.

［10］常轶深，钱亦兵，王忠臣，等. 艾比湖地区南北典型断面的土壤粒度特征［J］. 干旱区地理，2012，35（6）：968-977.

［11］ PENG Y J，XIAO J L，NAKAMURA T，et al. Holocene East Asian monsoonal precipitation pattern revealed by grain-size distribution of core sediments of Daihai Lake in Inner Mongolia of north- central China［J］. Earth and Planetary Science Letters，2005，233：467-479．

［12］张登山，田丽慧，鲁瑞洁，等. 青海湖湖东沙地风沙沉积物的粒度特征［J］. 干旱区地理，2013，36（2）：203-211.

［13］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.

［14］马冀. 毛乌素沙漠南缘全新世光释光年代学及古气候环境记录［D］. 西安：西北大学，2011.

［15］朱宣清，何乃华. 运用粒度分析方法恢复河流地貌——以滹沱河为例［J］. 河北省科学院学报，1990，7（1）：17-29.

［16］ LU Huayu，STEVENS T，YI Shuangwen，et al. An erosional hiatus in Chinese loess sequences revealed by closely spaced optical dating［J］. Chinese Science Balletin，2006，51：2253-2259.

［17］ STEVENS T，ARMITAGE S J，LU Huayu，et al. Sedimentation and diagenesis of Chinese loess：Implications for the preservation of continuous high-resolution climate records［J］. Geology，2006，34：849-852.

［18］ LAI Zhongping，WINTLE A C. Locating the boundary between the Pleistocene and the Holocene in Chinese loess using luminescence［J］. The Holocene，2006，16：893-899.

［19］彭淑贞，朱丽君，肖国桥，等. 山东青州黄土的地层年代及其物质来源研究［J］. 干旱区地理，2010，33（6）：947-953.

［20］ LI S，CHEN Y，LI B，et al. OSL dating of sediments from deserts in northern China［J］. Quaternary Geochronology，2007，2（1-4）：23-28.

［21］ BUBENZER O，HILGERS A，RIEMER H. Luminescence dating and archaeology of Holocene fluvio-lacustrine sediments of Abu Tartur，Eastern Sahara［J］. Quaternary Geochronology，2007，2：314-321.

［22］ CUPPER M L. Luminescence and radiocarbon chronologies of playa sedimentation in the Murray Basin，southeastern Australia［J］. Quaternary Science Reviews，2006，25：2594-2607.

［23］ MADSEN D B，MA H Z，RHODE D，et al．Age constraints on the late Quaternary evolution of Qinghai Lake，Tibetan Plateau［J］．Quaternary Research，2008，69：316-325．

［24］ THOMAS D S G，BAILEY R，SHAW P A，et al. Late Quaternary high stands at Lake Chilwa，Malawi：Frequency，timing and possible forcing mechanisms in the last 44 ka［J］. Quaternary Science Reviews，2009，28：526-539.

［25］ BERGER G W，DORAN P T. Luminescence dating zeroing tests in Lake Hoare，Taylor Valley，Antarctica［J］. Journal of Paleolimnology，2003，25（4）：519-529.

［26］ LANG A，ZOLITSCHKA B. Optical dating of annually laminated lake sediments：A test case from Holzmaar，Germany［J］. Quaternary Science Reviews，2001，20（5-9）：737-742.

［27］ ARGILYAN E P，FORMAN S L，JOHNSTON J W，et al. Optically stimulated luminescence dating of Late Holocene raised strand plain sequences adjacent to Lakes Michigan and Superior，Upper Peninsula，Michigan，USA［J］. Quaternary Research，2005，63（2）：122-135.

［28］王乃昂，李卓伦，程弘毅，等. 阿拉善高原晚第四纪高湖面与大湖期的再探讨［J］. 科学通报，2011，56（17）：1367-1377.

［29］陈发虎，范育新，春喜，等. 晚第四纪“吉兰泰—河套”古大湖的初步研究［J］. 科学通报，2008，53（11）：1207-1219.

［30］ ZHANG H C，PENG J L，Ma Y Z，et al. Late Quaternary palaeolake levels in Tengger Desert，NW China［J］. Palaeogeography，Palaeoclimatology，Palaeoecology，2004，211：45-58.

［31］赵华，卢演俦，尹金辉. 科尔沁沙地全新世风沙沉积物的石英单测片蓝光释光测年和风沙活动年代学［J］. 核技术，2005，28（5）：367-374.

［32］ LU Huayu，MIAO Xiaodong，ZHOU Yali，et al. Late Quaternary aeolian activity in the Mu Us and Otindag dune fields（North China）and lagged response to insolation forcing［J］. Geophysical Research Letters，2005，32（21）：L21716，doi：10.1029/2005GL024 560．

［33］ SUN Jimin，LI Shenghua，HAN Peng，et al. Holocene environmental changes in the central Inner Mongolia，based on single-aliquot-quartz optical dating and multi-proxy study of dune sands［J］. Palaeogeography，Palaeoclimatology，Palaeoecology，2006，233（1-2）：51-62.

［34］ LU Huayu，JOSEPH A Mason，THOMAS Stevens，et al. Response of surface processes to climatic in the dunefields and Loess Plateau of North China during the Late Quaternary［J］. Earth Surface Processes and Landforms，2011，36（12）：1590-1603.

［35］ MCLAREN P，BOWLES D. The effects of sediment transport on grain-size distributions［J］. Journal of Sedimentary Petrology，1985，55：457-470．

［36］ CAO S，COLLINS M. Net sediment transport patterns inferred from grain-size trends，based upon definition of “transport vectors”［J］. Sedimentary Geology，1992，81：47-60.

［37］ MCMANUS J. Grain size determination and interpretation［M］//Tucker M，ed. Techniques in Sedimentology. Backwell：Oxford，1988：63-85.

［38］贾建军，高抒，薛允传. 图解法与矩法沉积物粒度参数的对比［J］. 海洋与湖沼，2002，23（6）：577-582.

［39］ PASSEGA R. Grain size representation by CM patterns as a geological tool［J］. Journal of Sedimentary Petrology，1964，34：830- 847.

［40］ ZHU D G，MENG X G，ZHAO X T，et al. Evolution of an ancient large lake in the southeast of the northern Tibetan Plateau［J］. Acta Geologica Sinica，2004，78（4）：982-992.

［41］李世杰，张宏亮，施雅风，等. 青藏高原甜水海盆地MIS 3阶段湖泊沉积与环境变化［J］. 第四纪研究，2008，28（1）：122-131.

［42］王富葆，马春梅，夏训城，等. 罗布泊地区自然环境演变及其对全球变化的响应［J］. 第四纪研究，2008，28（1）：150-153.

［43］史兴民，李有利，杨景春. 新疆玛纳斯湖变迁的气候和构造分析［J］. 地理科学，2008，28（2）：266-271.

［44］赵希涛，郑绵平，李道明. 青海格尔木三岔河组年龄测定与昆仑古湖发育［J］. 第四纪研究，2009，29（1）：89-97.

［45］ FAN Q S，LAI Z P，LONG H，et al. OSL chronology for lacustrine sediments recording high stands of Gahai Lake in Qaidam Basin，northeastern Qinghai-Tibetan Plateau［J］. Quaternary Geochronology，2010，5：223-227.

［46］ LIU X J，LAI Z P，LONG H，et al. Timing of high lake levels of Qinghai Lake in the Qinghai-Tibetan Plateau since last interglaciation based on quartz OSL dating［J］. Quaternary Geochronology，2010，5：218-222.

［47］赵希涛，朱大岗，吴中海，等. 西藏纳木错晚更新世以来的湖泊发育［J］. 地球学报，2002，23（4）：329-334.

［48］马志邦，赵希涛，朱大岗，等. 西藏纳木错湖相沉积物的铀系年代学研究［J］. 地球学报，2002，23（4）：311-316.

［49］朱大岗，孟宪刚，赵希涛，等. 西藏纳木错和藏北高原古大湖晚更新世以来的湖泊演化与气候变迁［J］. 中国地质，2004，31（3）：269-277.

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巴丹吉林沙漠东南部末次间冰期环境演变：来自粒度、光释光（OSL）及¹⁴C测年的证据

Environmental change of southeastern Badain Jaran Desert during the last interglacial: evidences from the grain-size analysis，optically stimulated luminescence and radiocarbon dating

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