新疆罗布泊地区33.9 ka BP以来沉积物粒度记录的环境演化过程

doi:10.12118/j.issn.1000-6060.2025.648

Abstract

Abstract:

The evolution of the mid-latitude westerly climate system is crucial for understanding interaction mechanisms between high- and low-latitude climate systems. The Tarim Basin, located in the typical arid to semiarid zone influenced by the Northern Hemisphere westerlies, serves as a key region for deciphering the coupling between the North Atlantic and Asian monsoon systems. However, debates remain regarding its moisture-heat configuration patterns and their co-evolution with global climate systems. This study analyzes grain-size fractions from 295 samples of the 0.00-16.10 m sediment core ZK0205 in the Luobei Depression of Lop Nur, Xinjiang, China. Three environmentally sensitive grain-size fractions are identified: Clay (<5 μm), silt (5-63 μm), and sand (>63 μm), which are interpreted as indicators of runoff input, aeolian activity intensity, and strong hydrodynamics, respectively, based on sedimentary characteristics of arid lake basins and modern observational data. Supported by an AMS ¹⁴C chronological framework, the environmental evolution of the study area since 33.9 ka BP was reconstructed. The main findings are as follows: (1) The Lop Nur region experienced humid conditions during MIS3, which shifted to arid conditions during MIS2. Overall, the Holocene was characterized by warm and dry conditions, revealing phased changes in moisture-heat configuration on a millennial scale. (2) Comparison between grain-size fraction variations and the Greenland NGRIP ice core δ¹⁸O record indicates that the region responded sensitively to Northern Hemisphere millennial-scale climate events. Notably, the response pattern shifted systematically with background climate states (warm periods MIS1/MIS3 against cold periods MIS2). (3) Located at the boundary between the core westerlies domain and its transitional margin, the climate evolution of Lop Nur was constrained by global climatic background conditions and jointly influenced by the westerlies and Asian monsoon systems. This interplay results in high complex regional climatic variability.

Key words: Lop Nur, lacustrine deposit, grain-size analysis, stratigraphic composition, arid Central Asia

YI Tingnan, CHANG Hong, LUO Jiaxin, LONG Xueying, MA Baocheng, ZHAO Liangliang. Grain-size record of environmental evolution in the Lop Nur in Xinjiang since 33.9 ka BP[J].Arid Land Geography, 2026, 49(8): 1687-1699.

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References 70

[1]	An C B, Tao S C, Zhao J J, et al. Late Quaternary (30.7—9.0 cal ka BP) vegetation history in Central Asia inferred from pollen records of Lake Balikun northwest China[J]. Journal of Paleolimnology, 2012, 49: 145-154. doi: 10.1007/s10933-012-9649-7
[2]	Luo C, Peng Z C, Yang D, et al. A lacustrine record from Lop Nur, Xinjiang, China: Implications for paleoclimate change during Late Pleistocene[J]. Journal of Asian Earth Sciences, 2009, 34(1): 38-45. doi: 10.1016/j.jseaes.2008.03.011
[3]	Rhodes T E, Gasse F, Lin R F, et al. A Late Pleistocene-Holocene lacustrine record from Lake Manas, Zunggar (northern Xinjiang, western China)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1996, 120(1-2): 105-121. doi: 10.1016/0031-0182(95)00037-2
[4]	Herzschuh U, Harald K, Mischke S. Temperature variability and vertical vegetation belt shifts during the last -50000 yr in the Qilian Mountains (NE margin of the Tibetan Plateau, China)[J]. Quaternary Research, 2006, 66(1): 133-146. doi: 10.1016/j.yqres.2006.03.001
[5]	Lehmkuhl F, Haselein F. Quaternary Paleoenvironmental change on the Tibetan Plateau and adjacent areas (western China and western Mongolia)[J]. Quaternary International, 2000, 65-66: 121-145. doi: 10.1016/S1040-6182(99)00040-3
[6]	An Z S. The history and variability of the East Asian Paleomonsoon climate[J]. Quaternary Science Reviews, 2000, 19(1-5): 171-187. doi: 10.1016/S0277-3791(99)00060-8
[7]	Zhou W J, Head J, Deng L. Climatic changes in northern China since the Late Pleistocene and its response to global change[J]. Quaternary International, 2001, 83-85: 285-292. doi: 10.1016/S1040-6182(01)00046-5
[8]	李吉均. 中国西北地区晚更新世以来环境变迁模式[J]. 第四纪研究, 1990, 10(3): 197-204.
	[Li Jijun. The patterns of environmental changes since Late Pleistocene in northwestern China[J]. Quaternary Sciences, 1990, 10(3): 197-204.]
[9]	王宁, 刘卫国, 常宏, 等. 中更新世以来新疆罗布泊地区气候演化过程[J]. 海洋地质与第四纪地质, 2009, 29(2): 131-137.
	[Wang Ning, Liu Weiguo, Chang Hong, et al. Evolutionary process of the climate of Lop Nur region of Xinjiang since Mid-Pleistocene[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 131-137.]
[10]	Yang D, Peng Z C, Luo C, et al. High-resolution pollen sequence from Lop Nur, Xinjiang, China: Implications on environmental changes during the Late Pleistocene to the Early Holocene[J]. Review of Palaeobotany and Palynology, 2013, 192: 32-41. doi: 10.1016/j.revpalbo.2012.12.002
[11]	李文, 穆桂金, 林永崇, 等. 罗布泊盐湖沉积物磁性特征及其环境意义[J]. 干旱区研究, 2021, 38(1): 257-266. doi: 10.13866/j.azr.2021.01.27
	[Li Wen, Mu Guijin, Lin Yongchong, et al. Magnetic properties of Lop Nur saline sediments and the environmental implications[J]. Arid Zone Research, 2021, 38(1): 257-266.] doi: 10.13866/j.azr.2021.01.27
[12]	Liu J, Wang R J, Zhao Y, et al. A 40000-year record of aridity and dust activity at Lop Nur, Tarim Basin, northwestern China[J]. Quaternary Science Reviews, 2019, 211: 208-221. doi: 10.1016/j.quascirev.2019.03.023
[13]	Li G Q, Yang H, Stevens T, et al. Differential ice volume and orbital modulation of Quaternary moisture patterns between Central and East Asia[J]. Earth and Planetary Science Letters, 2019, 530: 115901, doi: 10.1016/j.epsl.2019.115901.
[14]	于秋莲, 张展适, 杜后发. 粒度分析在古环境中的应用[J]. 能源研究与管理, 2010(2): 49-52.
	[Yu Qiulian, Zhang Zhanshi, Du Houfa. The application of granularity analysis in paleoenvironment[J]. Energy Research and Management, 2010(2): 49-52.]
[15]	Porter S C, An Z S. Correlation between climate events in the North Atlantic and China during the last glaciation[J]. Nature, 1995, 375: 305-308. doi: 10.1038/375305a0
[16]	Sun Y B, Clemens S C, Guo F, et al. High-sedimentation-rate loess records: A new window into understanding orbital-and millennial-scale monsoon variability[J]. Earth-Science Reviews, 2021, 220: 103731, doi: 10.1016/j.earscirev.2021.103731.
[17]	Zhang J G, Lü D Y, Chen H Y, et al. Evolution of sedimentary environment in the eastern Henan Basin since the Late Pliocene[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2024, 633: 111896, doi: 10.1016/j.palaeo.2023.111896.
[18]	李晨光. 中国北方湖泊沉积物粒度特征及环境指示意义[D]. 哈尔滨: 哈尔滨师范大学, 2020.
	[Li Chenguang. Grain size characteristics and environmental indicators of lake sediments in northern China[D]. Harbin: Harbin Normal University, 2020.]
[19]	杨艺, 王汝建, 刘健, 等. 新疆罗布泊45 ka BP以来沉积物粒度敏感组分记录的区域沙尘活动历史[J]. 地学前缘, 2015, 22(5): 247-258. doi: 10.13745/j.esf.2015.05.021
	[Yang Yi, Wang Rujian, Liu Jian, et al. Regional dust activity history during the past 45 ka reflected by sensitive grain-size components in Lop Nur, Xinjiang[J]. Earth Science Frontiers, 2015, 22(5): 247-258.]
[20]	易庭楠, 常宏, 杨茂洁, 等. 盐类矿物去除对盐湖沉积粒度分析的意义——以罗布泊为例[J]. 盐湖研究, 2026, 34(1): 51-59.
	[Yi Tingnan, Chang Hong, Yang Maojie, et al. The significance of evaporite mineral removal in salt lake sediment particle size analysis: A case study from Lop Nur[J]. Journal of Salt Lake Research, 2026, 34(1): 51-59.] doi: 10.3724/j.yhyj.2025033
[21]	夏训诚, 王富葆, 赵元杰. 中国罗布泊[M]. 北京: 科学出版社, 2007: 28-303.
	[Xia Xuncheng, Wang Fubao, Zhao Yuanjie. The Lop Nur of China[M]. Beijing: Science Press, 2007: 28-303.]
[22]	王弭力, 刘成林, 焦鹏程, 等. 罗布泊盐湖钾盐资源[M]. 北京: 地质出版社, 2001: 31-32.
	[Wang Mili, Liu Chenglin, Jiao Pengcheng, et al. Potassium salt resources of Lop Nur Lake[M]. Beijing: Geological Publishing House, 2001: 31-32.]
[23]	罗超, 彭子成, 刘卫国, 等. 新仙女木事件在罗布泊湖相沉积物中的记录[J]. 地球科学(中国地质大学学报), 2008, 33(2): 190-196.
	[Luo Chao, Peng Zicheng, Liu Weiguo, et al. Evidence from the lacustrine sediments of Lop-Nur Lake, northwest China for the Younger Dryas Event[J]. Earth Sciences (Journal of China University of Geosciences), 2008, 33(2): 190-196.]
[24]	Chang H, An Z S, Wu F, et al. Late Miocene-early Pleistocene climate change in the mid-latitude westerlies and their influence on Asian monsoon as constrained by the K/Al ratio record from drill core Ls2 in the Tarim Basin[J]. Catena, 2017, 153: 75-82. doi: 10.1016/j.catena.2017.02.002
[25]	李保国, 马黎春, 蒋平安, 等. 罗布泊“大耳朵”干盐湖区地形特征与干涸时间讨论[J]. 科学通报, 2008, 53(3): 327-334.
	[Li Baoguo, Ma Lichun, Jiang Ping’an, et al. Topographic characteristics and discussion on the desiccation time of the “Big Ear” dry salt lake area in Lop Nur[J]. Chinese Science Bulletin, 2008, 53(3): 327-334.]
[26]	袁革新, 陈剑杰, 赵振华, 等. 罗布泊地区第四纪环境演化若干新认识[J]. 现代应用物理, 2013, 4(3): 293-298.
	[Yuan Gexin, Chen Jianjie, Zhao Zhenhua, et al. Some latest cognitions in environmental evolution of Lop Nur in the Quaternary period[J]. Modern Applied Physics, 2013, 4(3): 293-298.]
[27]	刘成林. 罗布泊盐湖钾盐矿床形成条件与规律[M]. 北京: 科学出版社, 2020: 1-220.
	[Liu Chenglin. Formation conditions and regularities of potash deposits in the Lop Nur Salt Lake[M]. Beijing: Science Press, 2020: 1-220.]
[28]	Luo J X, He M Y, Chang H, et al. Does climate change lead to potash deposits? A perspective of Lop Nur Salt Lake, China[J]. Quaternary International, 2024, 692: 56-72. doi: 10.1016/j.quaint.2024.03.003
[29]	鹿化煜, 安芷生. 黄土高原黄土粒度组成的古气候意义[J]. 中国科学(D辑), 1998, 28: 278-283.
	[Lu Huayu, An Zhisheng. Paleoclimatic significance of grain size of loess-palaeosol deposit in Chinese Loess Plateau[J]. Science in China (Series D), 1998, 28: 278-283.]
[30]	蒲晓强, 钟少军. 不同的前处理方法对南黄海沉积物粒度测试的影响[J]. 海洋地质动态, 2009, 25(5): 15-18.
	[Pu Xiaoqiang, Zhong Shaojun. Influence of different pretreatment methods on grain size analysis of sediments from South Yellow Sea[J]. Marine Geology Frontiers, 2009, 25(5): 15-18.]
[31]	张成琦, 李育, 周雪花, 等. 晚第四纪湖泊沉积物盐类与碎屑矿物反相关关系的沉积学解释[J]. 冰川冻土, 2015, 37(1): 95-108. doi: 10.7522/j.issn.1000-0240.2015.0010
	[Zhang Chengqi, Li Yu, Zhou Xuehua, et al. A sedimentological interpretation of the inverse correlation between saline minerals and detrital minerals in the Late Quaternary lake sediments[J]. Journal of Glaciology and Geocryology, 2015, 37(1): 95-108.] doi: 10.7522/j.issn.1000-0240.2015.0010
[32]	程鹏, 卢雪峰, 杜花, 等. 青海湖老碳效应的时空变化初步研究[J]. 地球环境学报, 2016, 7(4): 357-365.
	[Cheng Peng, Lu Xuefeng, Du Hua, et al. The preliminary study of spatio-temporal change of old carbon effect in Lake Qinghai (NE Tibet-Qinghai Plateau), China[J]. Journal of Earth Environment, 2016, 7(4): 357-365.]
[33]	张瑜, 马黎春, 王凯. 罗布泊干盐湖第四纪环境演变研究进展[J]. 地球科学进展, 2022, 37(2): 149-164. doi: 10.11867/j.issn.1001-8166.2022.005
	[Zhang Yu, Ma Lichun, Wang Kai. Research progress of Quaternary environmental evolution in Lop Nor Playa[J]. Advances in Earth Science, 2022, 37(2): 149-164.] doi: 10.11867/j.issn.1001-8166.2022.005
[34]	Zhang J F, Liu C L, Wu X H, et al. Optically stimulated luminescence and radiocarbon dating of sediments from Lop Nur (Lop Nor), China[J]. Quaternary Geochronology, 2012, 10: 150-155. doi: 10.1016/j.quageo.2011.12.001
[35]	刘成林, 焦鹏程, 陈永志, 等. 罗布泊盐湖晚更新世末期芒硝岩沉积及其古气候意义[J]. 地球学报, 2008, 29(4): 397-404.
	[Liu Chenglin, Jiao Pengcheng, Chen Yongzhi, et al. Late Pleistocene mirabilite deposition in the Lop Nur Saline Lake, Xinjiang, and its paleoclimate implications[J]. Acta Geoscientica Sinica, 2008, 29(4): 397-404.]
[36]	于苗苗, 蒙红卫, 陈金龙, 等. 云南湖泊碳库效应[J]. 第四纪研究, 2023, 43(2): 390-402.
	[Yu Miaomiao, Meng Hongwei, Chen Jinlong, et al. The radiocarbon reservoir effects of lakes in Yunnan[J]. Quaternary Sciences, 2023, 43(2): 390-402.]
[37]	刘成林, 焦鹏程, 王弭力, 等. 罗布泊盐湖巨量钙芒硝沉积及其成钾效应分析[J]. 矿床地质, 2007(3): 322-329.
	[Liu Chenglin, Jiao Pengcheng, Wang Mili, et al. Sedimentation of glauberite and its effect on potash deposits formation in Lop Nur Salt Lake, Xinjiang, China[J]. Mineral Deposits, 2007(3): 322-329.]
[38]	罗超, 刘卫国, 彭子成, 等. 新疆罗北洼地湖相沉积物有机碳同位素的变化序列及其古环境意义[J]. 第四纪研究, 2008, 28(4): 621-628.
	[Luo Chao, Liu Weiguo, Peng Zicheng, et al. Stable carbon isotope record of organic matter from the Lop Nur lacustrine sediments in Xinjiang, northwestern China[J]. Quaternary Sciences, 2008, 28(4): 621-628.]
[39]	吕凤琳, 刘成林, 焦鹏程, 等. 罗布泊第四纪湖盆物源与盆地构造演化特征: 来自LDK01孔碎屑锆石U-Pb年龄证据[J]. 地质学报, 2018, 92(8): 1571-1588.
	[Lü Fenglin, Liu Chenglin, Jiao Pengcheng, et al. Provenance of the Quaternary Lake Basin and tectonic evolution of the basin in Lop Nur: Evidence from detrital zircon U-Pb age of core LDK01[J]. Acta Geologica Sinica, 2018, 92(8): 1571-1588.]
[40]	刘成林, 焦鹏程, 陈永志, 等. 罗布泊断陷带内形成富钾卤水机理研究[J]. 矿床地质, 2010, 29(4): 602-608.
	[Liu Chenglin, Jiao Pengcheng, Chen Yongzhi, et al. Formation mechanism of potash-bearing brine in fault belts of Lop Nur Lake, Xinjiang[J]. Mineral Deposits, 2010, 29(4): 602-608.]
[41]	焦鹏程, 刘成林, 颜辉, 等. 新疆罗布泊盐湖深部钾盐找矿新进展[J]. 地质学报, 2014, 88(6): 1011-1024.
	[Jiao Pengcheng, Liu Chenglin, Yan Hui, et al. New progress of potassium prospecting in deep salt lake of Lop Nur Region in Xinjiang[J]. Acta Geologica Sinica, 2014, 88(6): 1011-1024.] doi: 10.1111/acgs.2014.88.issue-s2
[42]	Luo J X, He M Y, Chang H, et al. Organic geochemistry analysis to decipher temporal carbon variations in Lop Nur Salt Lake, China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2025, 661: 112735, doi: 10.1016/j.palaeo.2025.112735.
[43]	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.
	[Sun Qianli, Zhou Jie, Xiao Jule. Grain-size characteristics of Lake Daihai sediments and its paleaoenvironment significance[J]. Marine Geology & Quaternary Geology, 2001, 21(1): 93-95.]
[44]	孙东怀, 安芷生, 苏瑞侠, 等. 古环境中沉积物粒度组分分离的数学方法及其应用[J]. 自然科学进展, 2001, 11(3): 47-54.
	[Sun Donghuai, An Zhisheng, Su Ruixia, et al. Mathematical method for separating grain-size components of sediment and its application in paleoenvironment[J]. Progress in Natural Science, 2001, 11(3): 47-54.]
[45]	肖雨琳. 北疆地区湖泊沉积记录的近2400年来湿度变化与水文动态[D]. 兰州: 兰州大学, 2022.
	[Xiao Yulin. Moisture changes and hydrological dynamics recorded by lake sediments in northern Xinjiang over the past 2400 years[D]. Lanzhou: Lanzhou University, 2022.]
[46]	薛积彬, 钟巍. 干旱区湖泊沉积物粒度组分记录的区域沙尘活动历史: 以新疆巴里坤湖为例[J]. 沉积学报, 2008, 26(4): 647-654, 669.
	[Xue Jibin, Zhong Wei. Variations in dust event reflected by grain-size component of lacustrine records in droughty area: A case study on Barkol Lake, Xinjiang, China[J]. Acta Sedimentologica Sinica, 2008, 26(4): 647-654, 669.]
[47]	沈吉, 汪勇, 羊向东, 等. 湖泊沉积记录的区域风沙特征及湖泊演化历史: 以陕西红碱淖湖泊为例[J]. 科学通报, 2006, 51(1): 87-92.
	[Shen Ji, Wang Yong, Yang Xiangdong, et al. Regional wind-sand characteristics and lake evolution history recorded in lake sediments: A case study of Hongjiannao Lake in Shaanxi Province[J]. Chinese Science Bulletin, 2006, 51(1): 87-92.]
[48]	马龙, 吴敬禄. 新疆湖泊沉积记录的气候水文变化及其环境效应[J]. 干旱区研究, 2009, 26(6): 786-792. doi: 10.13866/j.azr.2009.06.011
	[Ma Long, Wu Jinglu. Climatic and hydrological change and environmental response recorded in lacustrine sediment in Xinjiang[J]. Arid Zone Research, 2009, 26(6): 786-792.] doi: 10.3724/SP.J.1148.2009.00786
[49]	Chen F H, Qiang M R, Zhou A F, 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): 2149-2160. doi: 10.1002/jgrd.v118.5
[50]	Chen S Q, Liu J B, Chen J H, et al. Differences in the evolutionary pattern of dust storms over the past 2000 years between eastern and western China and the driving mechanisms[J]. Science China Earth Sciences, 2020, 63(9): 1422-1424. doi: 10.1007/s11430-020-9632-y
[51]	段含明, 艾里西尔·库尔班, 张燕, 等. 近百年来罗布泊最后干涸时间的评述[J]. 干旱区研究, 2013, 30(3): 541-549.
	[Duan Hanming, Kurban Erisier, Zhang Yan, et al. Review of the studies about the latest dried-up time of the Lop Nur Lake in recent 100 years[J]. Arid Zone Research, 2013, 30(3): 541-549.]
[52]	李开封, 穆桂金, 徐立帅, 等. 塔里木河干流古河道表层沉积物粒度特征及其意义[J]. 水土保持通报, 2012, 32(1): 161-164.
	[Li Kaifeng, Mu Guijin, Xu Lishuai, et al. Grain size characteristics and their significance for surface sediment of paleochannels along main stream of Tarim River[J]. Bulletin of Soil and Water Conservation, 2012, 32(1): 161-164.]
[53]	Chen F H, Chen J, Huang W, et al. Westerlies Asia and monsoonal Asia: Spatiotemporal differences in climate change and possible mechanisms on decadal to sub-orbital timescales[J]. Earth-Science Reviews, 2019, 192: 337-354. doi: 10.1016/j.earscirev.2019.03.005
[54]	刘蔚, 王涛. 我国沙尘暴变化及降尘特征研究[J]. 干旱区资源与环境, 2004, 18(1): 26-32.
	[Liu Wei, Wang Tao. Research on the variation and characteristics of dust storms in China[J]. Journal of Arid Land Resources and Environment, 2004, 18(1): 26-32.]
[55]	孙东怀, 鹿化煜, Rea David, 等. 中国黄土粒度的双峰分布及其古气候意义[J]. 沉积学报, 2000, 18(3): 327-335.
	[Sun Donghuai, Lu Huayu, Rea David, et al. Bimode grain-size distribution of Chinese loess and its paleoclimate implication[J]. Acta Sedimentologica Sinica, 2000, 18(3): 327-335.]
[56]	Vandenberghe J. Grain size of fine-grained windblown sediment: A powerful proxy for process identification[J]. Earth-Science Reviews, 2013, 121: 18-30. doi: 10.1016/j.earscirev.2013.03.001
[57]	朱青, 王富葆, 曹琼英, 等. 罗布泊全新世沉积特征及其环境意义[J]. 地层学杂志, 2009, 33(3): 283-290.
	[Zhu Qing, Wang Fubao, Cao Qiongying, et al. Grain size distribution characteristics and changes of Lop-Nur Lake sediments during the past 10000 years[J]. Journal of Stratigraphy, 2009, 33(3): 283-290.]
[58]	Sun J M, Liu T S. The age of the Taklimakan Desert[J]. Science, 2006, 312: 1621, doi: 10.1126/science.1124616. pmid: 16778048
[59]	Xiao J L, Fan J W, Zhou L, et al. A model for linking grain-size component to lake level status of a modern clastic lake[J]. Journal of Asian Earth Sciences, 2013, 69: 149-158. doi: 10.1016/j.jseaes.2012.07.003
[60]	Chen F H, Huang X Z, Zhang J W, et al. Humid little ice age in arid Central Asia documented by Bosten Lake, Xinjiang, China[J]. Science China Earth Sciences, 2006, 49(12): 1280-1290. doi: 10.1007/s11430-006-2027-4
[61]	吕爽, 韩文霞, 张涛, 等. 塔里木盆地南缘8.5 ka以来的黄土岩石磁学特征及其磁化率变化机制[J]. 地球物理学报, 2019, 62(8): 3053-3066. doi: 10.6038/cjg2019M0443
	[Lü Shuang, Han Wenxia, Zhang Tao, et al. Rock magnetic characteristics and magnetic susceptibility change mechanism of the loess since 8.5 ka in the southern margin of Tarim Basin[J]. Chinese Journal of Geophysics, 2019, 62(8): 3053-3066.]
[62]	Han W X, Lü S, Appel E, et al. Dust storm outbreak in Central Asia after -3.5 kyr BP[J]. Geophysical Research Letters, 2019, 46(13): 7063-7856. doi: 10.1002/grl.v46.13
[63]	常秋芳, 常宏. 罗布泊Ls2孔近7.1 Ma以来沉积物的环境磁学研究[J]. 第四纪研究, 2013, 33(5): 876-888.
	[Chang Qiufang, Chang Hong. The environmental magnetism study of core Ls2 in Lop Nur, Tarim since 7.1 Ma[J]. Quaternary Sciences, 2013, 33(5): 876-888.]
[64]	Vinther B M, Clausen H B, Johnsen S J, et al. A synchronized dating of three Greenland ice cores throughout the Holocene[J]. Journal of Geophysical Research: Atmospheres, 2006, 111: D13102, doi: 10.1029/2005JD006921.
[65]	Rasmussen S O, Andersen K K, Svensson A M, et al. A new Greenland ice core chronology for the last glacial termination[J]. Journal of Geophysical Research: Atmospheres, 2006, 111: D06102, doi: 10.1029/2005JD006079.
[66]	Andersen K K, Svensson A, Johnsen S J, et al. The Greenland ice core chronology 2005, 15-42 ka. Part 1: Constructing the time scale[J]. Quaternary Science Reviews, 2006, 25(23-24): 3246-3257. doi: 10.1016/j.quascirev.2006.08.002
[67]	Wang Y J, Cheng H, Edwards R L, et al. A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave, China[J]. Science, 2001, 294(5550): 2345-2348. pmid: 11743199
[68]	程良清, 宋友桂, 李越, 等. 粒度端元模型在新疆黄土粉尘来源与古气候研究中的初步应用[J]. 沉积学报, 2018, 36(6): 1148-1156.
	[Cheng Liangqing, Song Yougui, Li Yue, et al. Preliminary application of grain size end member model for dust source tracing of Xinjiang loess and paleoclimate reconstruction[J]. Acta Sedimentologica Sinica, 2018, 36(6): 1148-1156.]
[69]	Cheng H, Zhang P Z, Spotl C, et al. The climatic cyclicity in semiarid-arid Central Asia over the past 500000 years[J]. Geophysical Research Letters, 2012, 39(1): L01705, doi: 10.1029/2011GL050202.
[70]	李稚, 朱成刚, 汪家友, 等. 东昆仑库木库里盆地典型湖泊水量蒸发损失估算[J]. 干旱区地理, 2024, 47(8): 1263-1276. doi: 10.12118/j.issn.1000-6060.2024.166
	[Li Zhi, Zhu Chenggang, Wang Jiayou, et al. Estimation of evaporation loss from typical lakes in the Kumukuli Basin, East Kunlun Mountains[J]. Arid Land Geography, 2024, 47(8): 1263-1276.] doi: 10.12118/j.issn.1000-6060.2024.166

深度/m	岩性地层
0.00~1.54	浅灰黄色细粒石盐集合含少量细砂，松散堆积，石盐晶体呈无色透明
1.54~3.54	浅灰色细粒石膏集合含少量粉砂，石膏晶体呈灰白色细粒针状集合排列
3.54~4.54	灰黄色块状粉砂含少量石膏隐晶质，偶见石盐
4.54~5.42	灰白色块状粉砂含细粒石盐及少量黏土
5.42~6.72	灰黑色块状黏土含粉砂及少量细粒石膏
6.72~11.96	深灰色块状细粒钙芒硝含粉砂钙芒硝晶体呈灰色鳞板状、片状集合，与粉砂胶结，可见少量孔隙。在9.21~11.00 m阶段，粉砂与细砂含量增多
11.96~15.85	黑绿色块状黏土含少量粉砂，偶见钙芒硝隐晶体。15 m后钙芒硝含量逐渐增加颜色转为灰黄色
15.85~16.10	灰绿色块状细粒钙芒硝胶结粉砂，结构坚硬致密

实验室编号	样品编号	深度/m	材料	测试年龄/ka BP	校正年龄/ka BP	数据质量
XA55102	ZK0205-5H-2	3.68	有机沉积物	10.200±0.030	9.926±0.073	有效
XA55103	ZK0205-5H-7	3.98	有机沉积物	10.000±0.030	9.860±0.168	剔除
XA50296	ZK0205-14C-2	5.24	有机沉积物	10.705±0.030	10.763±0.029	剔除
XA55104	ZK0205-7H-5	5.67	有机沉积物	14.850±0.040	16.220±0.096	有效
XA50297	ZK0205-14C-3	10.70	有机沉积物	23.170±0.060	25.510±0.185	有效
XA50298	ZK0205-14C-4	11.20	有机沉积物	12.425±0.040	12.639±0.303	剔除
XA55105	ZK0205-11H-29	12.60	有机沉积物	25.000±0.040	27.352±0.320	有效
XA55106	ZK0205-12H-23	14.34	有机沉积物	28.095±0.125	30.052±0.324	有效
XA50300	ZK0205-14C-6	15.98	有机沉积物	36.450±0.150	34.580±0.310	有效

深度/m	平均粒径/μm	中值粒径/μm	标准偏差/μm
0.00~1.54	18.30~115.00	6.24~20.50	0.833~1.361
1.54~3.54	9.17~41.10	4.90~12.60	1.112~1.521
3.54~4.54	7.43~40.60	4.84~29.20	1.008~1.447
4.54~5.42	8.48~17.60	4.88~9.97	1.147~1.436
5.42~6.72	10.50~26.50	5.44~12.80	1.113~1.286
6.72~11.96	8.98~235.11	5.08~220.00	0.876~2.191
11.96~15.85	2.04~158.00	0.79~173.00	0.945~1.947
15.85~16.10	14.00~75.20	15.90~16.10	0.970~1.333

Grain-size record of environmental evolution in the Lop Nur in Xinjiang since 33.9 ka BP

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