WU Jian, SHEN Ji. PALEOENVIRONMENTAL AND PALEOCLIMATIC CHANGES REFLECTED BY DIFFUSE REFLECTANCE SPECTROSCOPY AND MAGNETIC SUSCEPTIBILITY FROM XINGKAI LAKE SEDIMENTS[J]. Marine Geology & Quaternary Geology, 2009, 29(3): 123-131. DOI: 10.3724/SP.J.1140.2009.03123
Citation: WU Jian, SHEN Ji. PALEOENVIRONMENTAL AND PALEOCLIMATIC CHANGES REFLECTED BY DIFFUSE REFLECTANCE SPECTROSCOPY AND MAGNETIC SUSCEPTIBILITY FROM XINGKAI LAKE SEDIMENTS[J]. Marine Geology & Quaternary Geology, 2009, 29(3): 123-131. DOI: 10.3724/SP.J.1140.2009.03123

PALEOENVIRONMENTAL AND PALEOCLIMATIC CHANGES REFLECTED BY DIFFUSE REFLECTANCE SPECTROSCOPY AND MAGNETIC SUSCEPTIBILITY FROM XINGKAI LAKE SEDIMENTS

More Information
  • Received Date: January 12, 2009
  • Revised Date: April 06, 2009
  • The Xingkai Lake, a transboundary lake by China and Russia, is the largest freshwater lake in Northeast Asia. We used diffuse reflectance spectroscopy and magnetic susceptibility to characterize the sediments in a 269 cm long core from deepwater in the northern part of the lake. Redness in sediment is primarily related to wet-warm climate,which seems to monitor paleoclimatic changes in the area; brightness has a good correlation with magnetic susceptibility,clay,TOC and redness, and likewise, magnetic susceptibility with clay. As lacustrine sediment becomes coarser, magnetic susceptibility generally decreases in the core.So both brightness and magnetic susceptibility can be used as a proxy indicator of palaeoclimate evolution in the area.Climate changes recorded by the lake sediments from Xingkai Lake were mainly characterized by the warm-wet and cold-dry alternation,based on accelerator mass spectrometry (AMS) radiocarbon chronology. An extreme cold-dry period occurred during 28 480~26 160 cal.aBP, especially during 27 050~26 160 cal.aBP.It was colder drier,with redness decreasing evidently.During 26 160~22 880 cal.aBP,redness reached the lowest value while climate transited to warm and wet conditions. 22 880~18 185 cal.aBP was a very cold period with very poor pollen grain in the sediments corresponding to the Last Glacial Maximum(LGM). 18 185~12 650 cal.aBP was a frequent oscillation period of redness and magnetic susceptibility correlating with Bølling/Older Dryas/Allerød warm period. A sharp fluctuation of redness, brightness and magnetic susceptibility occurred around the Younger Dryas cold event, at about 90~78 cm depth in the core. During 11 500~4 570 cal.aBP, redness increased to higher values, indicating a wet and warm climate in Holocene, and 8 000~5 000 cal.aBP represented Holocene Megathemal period(Holocene thermal optimum) with the highest redness value of the horizon in the area.During 4 570~1 470 cal.aBP,redness and magnetic susceptibility decreased markedly, reflecting the prevalence of cold-dry climate. Since 1 470 cal.aBP, frequency dependent susceptibility and redness increased drastically, climate became warm-wet again, and human activities resulted in remarkable increase of erosion and more terrestria1 material carried into the 1ake.
  • [1]
    王志国.吉林金川泥炭纤维素稳定碳同位素组成序列与东北季风区五千多年来的环境变迁[J].矿物岩石地球化学通报,1998,17(1):52-54.

    [WANG Zhiguo. Reconstruction of past 5000-year humidity changes of northeast China using δ13C values of peat cellulose in Jinchuan region, Jilin Province[J].Bulletin of Mineralogy, Petrology and Geochemistry,1998,17(1):52-54.]
    [2]
    李文漪.中国第四纪植被与环境[M].北京:科学出版社,1998:230.[LI Wenyi.Vegetation and Environment during the Quaternary in China[M].Beijing:Science Press, 1998:230.]
    [3]
    刘嘉麒,倪云燕,储国强.第四纪的主要气候事件[J]. 第四纪研究,2001,21(3):239-248.

    [LIU Jiaqi,NI Yunyan, CHU Guoqiang. Main paleoclimatic events in the Quaternary[J].Quternary Sciences, 2001,21(3):239-248.]
    [4]
    胡守云,邓成龙,Appel E,等.湖泊沉积物磁学性质的环境意义[J].科学通报,2001,46(17):1491-1494.

    [HU Shouyun,DENG Chenglong, Appe E.Environmental magnetic studies of lacustrine sediments[J]. Chinese Science Bulletin, 2002, 47(7):613-616.]
    [5]
    姜月华,殷鸿福,王润华.环境磁学理论、方法和研究进展[J].地球学报,2004, 25:357-362.[JIANG Yuehua, YIN Hongfu,WANG Runhua. The theory, method and research progress of environmental magnetism[J].Acta Geoscientica Sinica, 2004

    , 25:357-362.]
    [6]
    俞立中,许羽,张卫国. 湖泊沉积物的矿物磁性测量及其环境应用[J]. 地球物理学进展,1995, 10(1):11-22.

    [YU Lizhong,XU Yu,ZHANG Weiguo.Magnetic measurement on lake sediment and its environmental application[J].Progress in Geophysics, 1995, 10(1):11-22.]
    [7]
    Grygar T, Kadlec J, Pruner P, et al.Paleoenvironmental record in Lake Baikal sediments:Environmental changes in the last 160 ky[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2006,237:240-254.
    [8]
    JI Junfeng, SHEN Ji,William Balsam, et al.Asian monsoon oscillations in the northeastern Qinghai-Tibet Plateau since the late glacial as interpreted from visible reflectance of Qinghai Lake sediments[J]. Earth and Planetary Science Letters, 2005,233:61-70.
    [9]
    裘善文,万恩璞,李凤华,等. 兴凯湖北部平原的发展与湿地的形成[J]. 湿地科学, 2007, 5(2):153-158.

    [QIU Shanwen, WAN Enpu, LI Fenghua, et al. Development of the plain in the north of the Xingkai Lake and formation of its wetlands[J].Wetland Science, 2007, 5(2):153-158.]
    [10]
    张淑芹,邓伟,阎敏华,等. 中国兴凯湖北岸平原晚全新世花粉记录及泥炭沼泽形成[J]. 湿地科学,2004,2(2):110-115.

    [ZHANG Shuqin, DENG Wei,YAN Minhua. Pollen record and forming process of the peatland in Late Holocene in the north bank of the Xingkai Lake, China[J].Wetland Science, 2004, 2(2):110-115.]
    [11]
    孟凡志,赵艳波,崔玉玲.兴凯湖生态水位分析[J]. 水资源保护,2008,24(6):46-48.

    [MENG Fanzhi, ZHAO Yanbo, CUI Yuling. Analysis of ecological water level of Xingkai Lake[J]. Water Resources Protection, 2008, 24(6):46-48.]
    [12]
    万波,钟以章.东北地区的新构造运动特征分析及新构造运动分区[J]. 东北地震研究,1997,13(4):64-75.

    [WAN Bo, ZHONG Yizhang. Features analysis and divisions of new tectonic movement in northeast China[J]. Seismological Research Northeast China,1997,13(4):64-75.]
    [13]
    Balsam W L, Deaton B C. Sediment dispersal in the Atlantic Ocean:evaluation by visible light spectra[J]. Reviews in Aquatic Sciences, 1991, 4:411-447.
    [14]
    Hughen K, Lehman S,Southon J,et al. 14C Activity and global carbon cycle changes over the past 50000 years[J]. Science, 2004, 303(9):202-207.
    [15]
    Korotkii A M, Grebennikova T A, et al. Lacustrine transgressions in the late Cenozoic Ussuri-Khanka depression (Primor'e)[J].Russian Journal of Pacific Geology, 2007, 1(4):53-68.
    [16]
    Svante B, Michael J C W, Les C C, et al. An event stratigraphy for the Last Termination in the North Atlantic region based on the Greenland ice-core record:a proposal by the intimate group[J].Journal of Quaternary Science, 1998, 13(4):283-292.
    [17]
    吴艳宏,王苏民,侯新花. 青藏高原中部错鄂全新世湖泊沉积物年代学研究[J]. 中国科学D辑,2006, 36(8):713-722.

    [WU Yanhong, WANG Sumin, HOU Xinhua. Chronology of Holocene lacustrine sediments in Co Ngoin, central Tibetan Plateau[J]. Science in China (Series D), 2006,49(9):991-1001.]
    [18]
    Zhou L P, Oldfield F, Wintle A G, et al. Partly pedogenic origin of magnetic variations in Chinese loess[J].Nature, 1990, 346:737-739.
    [19]
    Thompson R, Oldfield F. Environmental Magnetism[M]. London:Allen and Unwzn,1986:11-18.
    [20]
    王建,刘泽纯,姜文英,等.磁化率与粒度、矿物的关系及其古环境意义[J].地理学报,1996,51(2):155-163.

    [WANG Jian,LIU Zechun, JIANG Wenying, et al. A relationship between susceptibility and grain-size and minerals,and their paleoenvironmental implication[J].Acta Geographica Sinica,1996,51(2):155-163.]
    [21]
    Dearing J A, Jones R T, Shen Ji, et al. Using multiple archives to understand past and present climate-human-environment interactions:the lake Erhai catchment, Yunnan Province, China[J]. Journal of Paleoliminology, 2008, 40:3-31.
    [22]
    张振克,沈吉,羊向东,等.近8 ka来云南洱海湖泊沉积记录的气候变化与夏季印度季风强弱变化的关系[J].亚热带资源与环境学报, 2008,3(3):1-6.

    [ZHANG Zhenke, SHEN Ji, YANG Xiangdong, et al. Climate changes and Indian Monsoon variations recorded by the lacustrine sediments from Erhai Lake, Yunnan Province during the past 8 ka[J]. Journal of Subtropical Resources and Environment, 2008, 3(3):1-6.]
    [23]
    Yu Lizhong,Oldfield F,Wu Yushu,et al.Paleoenvironmental implications of magnetic measurements on sediment core from Kuniming Basin, Southwest China[J]. Journary of Paleoliminology, 1990, 3:95-111.
    [24]
    Qu Wenchuan, Xue Bin, Dickman M D, et al. A 14000-year record of paleoenvironmental change in the western basin of China's third largest lake, Lake Taihu[J]. Hydrobiologia, 2000, 432:113-120.
    [25]
    王心源,吴立,张广胜,等.安徽巢湖全新世湖泊沉积物磁化率与粒度组合的变化特征及其环境意义[J].地理科学,2008,28(4):549-553.

    [WANG Xinyuan,WU Li,ZHANG Guangsheng, et al. Characteristics and environmental significance of magnetic susceptibility and grain size of lake sediments since Holocene in Chaohu Lake, Anhui Province[J]. Acta Geographica Sinica, 2008,28(4):549-553.]
    [26]
    Balsam W L, Deaton B C, Damusth J E. Evaluating the optical lightness as a proxy for carbonate content in marine sediment cores:implication for marine sedimentation[J]. Marine Geology, 1999, 161:141-53.
    [27]
    Balsam W L, Ji J F, Chen J. Climatic interpretation of the Luochuan and Lingtai loess sections, China, based on changing iron oxide mineralogy and magnetic susceptibility[J]. Earth and Planetary Science Letters, 2004, 223:335-348.
    [28]
    Vodyanitskii Y N, Vasil'ev A A, Kozheva A V, et al. Influence of iron-containing pigments on the color of soils on alluvium of the middle Kama Plain[J]. Eurasian Soil Science, 2007, 40(3):289-301.
    [29]
    杨胜利,方小敏,李吉均,等. 表土颜色和气候定性至半定量关系研究[J]. 中国科学D辑,2001,31(增刊):175-181.[YANG Shengli, FANG Xiaomin, LI Jijun, et al.Transformation functions of soil color and climate[J]. Science in China (Series D),2001

    ,44(S1):218-226.]
    [30]
    陈一萌,陈兴盛,宫辉力,等.土壤颜色——一个可靠的气候变化代用指标[J].干旱区地理,2006,29(3):309-313.

    [CHEN Yimeng, CHEN Xingsheng, GONG Huili, et al. Soil color-a new sensitive indicator for climatic change[J]. Arid Land Geography, 2006,29(3):309-313.]
    [31]
    YIN Yong,FANG Nianqiao, HU Chaoyong, et al. Relative brightness index and its climatic significance from lacustrine sediment of Napahai lake, Northwestern Yunnan Plateau, China[J]. Chinese Geographical Science, 2002, 12(3):249-253.
    [32]
    Yang S L, Chen S Y, Yan M D, et al. Soil color:a new sensitive indicator for climatic change[J].Chinese Science Bulletin, 1999, 44(S1):282-285.
    [33]
    夏玉梅,汪佩芳.密山杨木3000多年来气候变化的泥炭记录[J]. 地理研究,2000,19(1):53-59.

    [XIA Yumei, WANG Peifang. Peat record of climate change since 3000 years in Yangmu, Mishan Region[J]. Geographical Research, 2000, 19(1):53-59.]
    [34]
    王曼华.我国东北平原晚更新世晚期植物群与古气候指标初探[J]. 冰川冻土, 1987,9(3):229-238.

    [WANG Manhua. Preliminary study of palaeovegetation and palaeoclimatic index in the later period of late Pleistocene in Northeast Plain of China[J].Journal of Glaciology and Geocryology, 1987,9(3):229-238.]
    [35]
    孙建中,王淑英,王雨灼,等.东北末次冰期的古环境[J].中国第四纪研究,1985,6(1):82-89.

    [SUN Jianzhong,WANG Shuying,WANG Yuzhuo, et al. Paleoenvironment of the Last Glacial stage in Northeast China[J]. China Quaternary Research, 1985, 6(1):82-89.]
    [36]
    徐文铎,何兴元,陈玮,等.长白山植被类型特征与演替规律的研究[J].生态学杂志,2004,23(5):162-174

    [XU Wenduo, HE Xingyuan, CHEN Wei, et al. Characteristics and succession rules of vegetation types in Changbai Mountain[J]. Chinese Journal of Ecology, 2004, 23(5):162-174.]
    [37]
    Michael Z, Roland Z, Bruno G. A 240000-year stable carbon and nitrogen isotope record from a loess-like palaeosol sequence in the Tumara Valley, Northeast Siberia[J]. Chemical Geology, 2007, 242:307-318.
    [38]
    Wang J S, Grimley D A., Xu C G, et al. Soil magnetic susceptibility reflects soil moisture regimes and the adaptability of tree species to these regimes[J]. Forest Ecology and Management, 2008, 255:1664-1673.
    [39]
    ZHOU Weijian, Douglas J.Variability of monsoon climate in East Asia at the end of the Last Glaciation[J]. Quaternary Research,1996,46(3):219-229.
    [40]
    AN Zhisheng, Stephen C.Episode of strengthened summer monsoon climate of Younger Dryas age on the Loess Plateau of central China[J]. Quaternary Research, 1993, 39(1):45-54.
    [41]
    闾国年.距今三万年来西北太平洋洋流系统变化的初步研究[J]. 海洋科学,1989(3):13-20.[LÜ

    ; Guonian. Changes of ocean current system in the western North Pacific since 30000 aBP[J]. Marine Science, 1989(3):13-20.]
    [42]
    Kyung E L. Surface water changes recorded in Late Quaternary marine sediments of the Ulleung Basin, East Sea (Japan Sea)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2007,247(1-2):18-31.
    [43]
    Bazarova V B, Klimin M A. New pollen records of Late Pleistocene and Holocene changes of environment and climate in the Lower Amur River basin, NE Eurasia[J]. Quaternary International, 2008, 179(1):9-19.
    [44]
    叶永英,严富华,麦学舜. 东北三江平原几个钻孔剖面的孢粉组合分析及其意义[J]. 地质科学, 1983, 3:259-267.[YE Yongying,YAN Fuhua,MAI Xueshun.The sporo-pollen assemblages in three well logs from Three-River Plain, Northeast China and their geological singnificance[J].Scientia Geologica Sinica, 1983

    , 3:259-267.]
    [45]
    张玉兰.同江地区中全新世以来的植被与环境研究[J]. 同济大学学报,2003, 31(6):668-671.

    [ZHANG Yulan. Studies on vegetation and environment since mid-Holocene in Tongjiang region, Heilongjiang Province[J]. Journal of Tongji University, 2003,31(6):668-671.]
    [46]
    刘金陵. 长白山区孤山屯沼泽地13000年以来的植被和气候变化[J].古生物学报,1989,28(4):495-511.

    [LIU Jinling. Vegetational and climatic changes at Gushantun bog in Jilin, NE China since 13000 aBP[J]. Acta Palaeontologica Sinica, 1989,28(4):495-511.]
    [47]
    Kuzmin Y V, Jull A J T, Jones G A. Early agriculture in Primorye, Russian Far East:new radiocarbon and pollen data from Late Neolithic sites[J].Journal of Archaeological Science, 1998, 25:813-816.
    [48]
    Kuzmin Y V. People and environment in the Russian Far East from Paleolithic to Middle Ages:chronology, palaeogeography, interaction[J]. GeoJournal, 1995,35(1):79-83.
    [49]
    张振克,吴瑞金,朱育新,等. 云南洱海流域人类活动的湖泊沉积记录分析[J]. 地理学报,2000,50(1):66-74.

    [ZHANG Zhenke, WU Ruijin, ZHU Yuxin, et al. Lacustrine records of human activities in the catchment of Erhai Lake,Yunnan Province[J]. Acta Geographica Sinica, 2000, 50(1):66-74.]
    [50]
    张振克,吴瑞金,王苏民. 岱海湖泊沉积物频率磁化率对历史时期环境变化的反映[J]. 地理研究,1998, 17(3):297-302.

    [ZHANG Zhenke,WU Ruijin,WANG Sumin. Implications of magnetic of frequency dependent susceptibility on environmental changes from lacustrine sediments in Daihai Lake[J]. Geographical Research, 1998, 17(3):297-302.]
  • Related Articles

    [1]LIU Dezheng, XIA Fei. Characteristics of grain size and magnetic susceptibility of the Late Quaternary sediments from core 07SR01 in the middle Jiangsu coast and their paleoenvironmental significances[J]. Marine Geology & Quaternary Geology, 2021, 41(5): 210-220. DOI: 10.16562/j.cnki.0256-1492.2021051901
    [2]DU Jing, LU Ruijie, LIU Xiaokang, LV Zhiqiang, CHEN Lu. Magnetic susceptibility of aeolian sediments deposited since Holocene in the East of Qinghai Lake and its environmental implications[J]. Marine Geology & Quaternary Geology, 2018, 38(2): 175-184. DOI: 10.16562/j.cnki.0256-1492.2018.02.018
    [3]WANG Jingzhong, WU Jinglu, ZENG Haiao. GRAIN-SIZE CHARACTERISTICS AND ITS ENVIRONMENTAL SIGNIFICANCE OF LAKE CHENPUHAI SEDIMENTS IN HETAO PLAIN, INNER MONGOLIA[J]. Marine Geology & Quaternary Geology, 2014, 34(5): 137-144. DOI: 10.3724/SP.J.1140.2014.05137
    [4]TENG Xiaohua, ZHANG Zhigao, PENG Wenbin, ZAN Jinbo, FANG Xiaomin. ROCK-MAGNETIC CHARACTERISTICS OF THE TIANSHAN LOESS AND THE MECHANISM FOR ENHANCING MAGNETIC SUSCEPTIBILITY[J]. Marine Geology & Quaternary Geology, 2013, 33(5): 147-154. DOI: 10.3724/SP.J.1140.2013.05147
    [5]XU Longsheng, WU Jinglu. LAKE ENVIRONMENTAL CHARACTERISTICS RECOREDED BY ISOTOPES IN SEDIMENTS OF DAPU AREA IN LAKE TAIHU[J]. Marine Geology & Quaternary Geology, 2013, 33(2): 137-142. DOI: 10.3724/SP.J.1140.2013.02137
    [6]ZHANG Hongliang, FANG Xianglin, FENG Qinglai, ZOU Shengli. ENVIRONMENT EVOLUTION INFERRED WITH PHYTOLITHS FROM LACUSTRINE DEPOSITS OF XINGYUN LAKE[J]. Marine Geology & Quaternary Geology, 2012, 32(5): 123-129. DOI: 10.3724/SP.J.1140.2012.05123
    [7]ZHAO Jiaju, LV Yanbin, AN Chengbang, TAO Shichen, ZHENG Tongming, DONG Weimia. CARBONATES IN LACUSTRINE SEDIMENTS OF LAKE BALIKUN, XINJIANG, CHINA[J]. Marine Geology & Quaternary Geology, 2010, 30(6): 125-131. DOI: 10.3724/SP.J.1140.2010.06125
    [8]ZHANG Jiangyong, GAO Hongfang, PENG Xuechao, ZHANGYulan, WANG Yingmin. COMPARISON OF MAGNETIC SUSCEPTIBILITY OF LATE QUATERNARY SEDIMENT DERIVED FROM SLOPES IN THE SOUTH CHINA SEA AND IMPLICATION FOR PALEOCEANOGRAPHY[J]. Marine Geology & Quaternary Geology, 2010, 30(4): 151-164. DOI: 10.3724/SP.J.1140.2010.04151
    [9]WANG Yong, PAN Bao-tian, GUAN Qing-yu, WANG Jian-li. MAGNETIC SUSCEPTIBILITY VARIATION IN SEMI-ARID REGION OF NORTHWESTERN CHINA[J]. Marine Geology & Quaternary Geology, 2008, 28(1): 111-114.
    [10]YAO Yuan, ZHANG En-lou, SHEN Ji, JIANG Qing-feng. HUMAN ACTIVITIES INDICATED BY LACUSTRINE DEPOSITION IN THE REGION OF SHUDU LAKE[J]. Marine Geology & Quaternary Geology, 2007, 27(5): 115-120.

Catalog

    Article views (1894) PDF downloads (25) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return