XIAN Feng, ZHOU Wei-jian, YU Xue-feng, LU Xue-feng, A J T Jull, Lars G Franzén. EVIDENCE FOR ABRUPT CHANGES OF THE ASIAN MONSOON DURING THE HOLOCENE: FROM THE PEAT RECORDS OF TIBETAN PLATEAU[J]. Marine Geology & Quaternary Geology, 2006, 26(1): 41-45.
Citation: XIAN Feng, ZHOU Wei-jian, YU Xue-feng, LU Xue-feng, A J T Jull, Lars G Franzén. EVIDENCE FOR ABRUPT CHANGES OF THE ASIAN MONSOON DURING THE HOLOCENE: FROM THE PEAT RECORDS OF TIBETAN PLATEAU[J]. Marine Geology & Quaternary Geology, 2006, 26(1): 41-45.
shu

EVIDENCE FOR ABRUPT CHANGES OF THE ASIAN MONSOON DURING THE HOLOCENE: FROM THE PEAT RECORDS OF TIBETAN PLATEAU

  • 1 Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China;

  • 2 Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;

  • 3 NSF-AMS Facility, University of Arizona, Arizona AZ 85721, USA;

  • 4 Department of Earth Sciences, Göteborg University, P. O. Box 460 SE-405 30 Göteborg, Sweden

More Information
  • Received Date: June 26, 2005
  • Revised Date: October 16, 2005
    Graphical Abstract
    • Abstract
  • Based on the proxies of peat such as TOC, grey scale and ash content, we reconstruct the evolution history of the Asian monsoon during the Holocene. Nine cold and dry events which can be correlated to both ice rafting events recorded in high latitude North Atlantic Ocean sediment cores and cooling events in the low latitude SST are recognized. Spectral analysis of the TOC data indicates that there exists series of periodicities of 1.428 ka,0.512 ka,0.255 ka and 0.217 ka.This further confirms the existence of centennial-millennial scale climatic rhythm in mid-latitude areas, reflecting the global significance of the rapid changes of climate during the Holocene.
    • FullText(HTML)
    • References (35)
  • [1]
    Dansgaard W, Johnsen S J, Clausen H B, et al. Evidence for general instability of past climate from a 250-kyr ice-core record[J]. Nature, 1993, 364:218-220.
    [2]
    McManus J F, Bond G C, Broecker W S, et al. High resolution climate records from the Atlantic during the last interglacial[J]. Nature, 1994, 371:326-329.
    [3]
    Bender M, Sowers T, Dickson M L, et al. Climate correlations between Greenland and Antarctica during the past 100000 years[J]. Nature, 1994, 372:663-666.
    [4]
    Chen F H, Bloemendal J, Wang J M, et al. High-resolution multi-proxy climate records from Chinese loess:Evidence for rapid climatic changes between 70 ka and 10 ka[J]. Paleo.Paleo.Palaeo., 1997, 130:323-335.
    [5]
    GUO Zheng-tang, Petit-Maire N, LIU Tung-sheng. Holocene abrupt environmental changes in the arid regions in Africa and Asia[J]. Paleogeography, 1999, 1(1):68.
    [6]
    Zhou S Z, Chen F H, Pan B T, et al. Environmental changes during the Holocene in the Western China on millennial timescale[J]. The Holocene, 1991, 1(2):151-156.
    [7]
    Oppo D W, McManus J F, Cullen J L. Abrupt climate events 500000 to 340000 years ago:evidence from subpolar North Atlantic sediments[J]. Science, 1998, 277:1867-1870.
    [8]
    McManus J F, Oppo D W, Cullen J L. A 0.5-million-year record of millennial-scale climate variability in the North Atlantic[J]. Science, 1999, 283(5404):971-975.
    [9]
    Orien S R, Mayewski P A, Meeker L D, et al. Complexity of Holocene climate as reconstructed from a Greenland ice core[J]. Science, 1995, 270:1962-1964.
    [10]
    Bond G, Showers W, Cheseby M, et al. A pervasive millennial-scale cycle in North Atlantic Holocene and Glacial climates[J]. Science, 1997, 278:1257-1266.
    [11]
    ZHOU Wei-jian, LU Xue-feng, WU Zhen-kun, et al. Peat record reflecting Holocene climatic change in the Zoige Plateau and AMS radiocarbon dating.[J]. Chinese Science Bulletin, 2002, 47(1):66-70.
    [12]
    Campbell I D, Campbell C, Apps M J, et al. Late Holocene~1500 year climatic periodficities and their implications[J]. Geology, 1998, 26:471-473.
    [13]
    施雅风, 孔昭宸, 王苏民, 等. 中国全新世大暖期的气候波动与重要事件[J].中国科学B辑,1992,12:1300-1308.[SHI Ya-feng, KONG Zhao-chen, WANG Su-min, et al. Climatic fluctuations and special events during the Holocene Optimum of China[J]. Science in China(Series B), 1992

    , 12:1300-1308.]
    [14]
    Gasse F, Van C E. Abrupt post-glacial climate events in West Asia and North Africa monsoon domains[J]. Earth and Planetary Science Letters, 1994,126:435-456.
    [15]
    Huang C C, Zhao J, Pang J L, et al.A regional aridity phase and its possible cultureal impact during the Holocene Magathermal in the Guanzhong Basin[J]. The Holocene, 2000, 10(1):135-142.
    [16]
    CHEN Fa-hu, ZHU Yan, LI Ji-jun, et al. Abrupt Holocene changes of the Asian monsoon at millenial and centennial scales[J]. Chinese Science Bulletin, 2001, 46(23):1942-1947.
    [17]
    孙广友, 罗新正, Turner R E. 青藏东北部若尔盖高原全新世泥炭沉积年代学研究[J].沉积学报, 2001, 19(2):177-181.

    [SUN Guang-you, LUO Xin-zheng,Turner R E.A study on peat deposition chronology of Holocene of Zoigê Plateau in the northeast Qinghai Tibetan Plateau[J]. Acta Sedimentologica Sinica, 2001, 19(2):177-181.]
    [18]
    徐海, 洪业汤, 林庆华, 等. 红原泥炭纤维素氧同位素指示的距今6000年温度变化[J]. 科学通报, 2002, 47(15):1181-1186.

    [XU Hai, HONG Ye-tang, LIN Qing-hua, et al. Temperature variations in past 6000 years inferred from δ18O of Peat Cellulose from Hongyuan, China[J]. Chinese Science Bulletin, 2002, 47(15):1181-1186.]
    [19]
    Gasse F, Arnold M, Fontes J C, et al. A 13000-year climate record from western Tibet[J]. Nature, 1991, 353:742.
    [20]
    ZHOU Wei-jian, Doinahue D J, Porter S C, et al. Variability of monsoon climate in east Asia at the end of the last glaciation[J]. Quaternary Research, 1996,46:219.
    [21]
    ZHOU Wei-jian, LU Xue-feng, WU Zhen-kun, et al. Peat record reflecting Holocene climatic change in the Zoigê Plateau and AMS radiocarbon dating[J]. Chinese Science Bulletin, 2002, 47(1):66-70.
    [22]
    Wanyner R K.Peat in Greens:knows, unknowns and speculations[M]. Soil Science,1987:5-8.
    [23]
    Stuiver M, Reimer B, Braziunas T. High-precision radiocarbon age calibration for terrestrial and marine samples[J]. Radiocarbon, 1998,49(3):1127-1151
    [24]
    XIAO Jia-yi, ZHOU Wei-jian, AN Zhi-sheng, et al. Evidence for the Younger Dryas event in the eastern part of Nanling region[J]. Acta Botanic Sinica(in Chinese), 1998, 40(11):1079.
    [25]
    Bond G, Kromer B, Beer J, et al. Persistent solar influence on North Atlantic climate during the Holocene[J]. Science, 2001, 294:2130-2136.
    [26]
    Sirocko F, Samthein M, Erlenkeuser H. Century-scale events in monsoonal climate over the past 24000 years[J]. Nature, 1993,364:322-324.
    [27]
    Thomson D. Spectrum estimation and harmonic analysis[C]. Proceedings of the IEEE, 1982, 70(9):1055.
    [28]
    Stuiver M, Braziunas T. Sun, ocean, climate and atmospheric 14CO2:an evaluation of causal and spectral relationships[J]. Holocene, 1993, 3(4):289.
    [29]
    Gleissberg W. A table of secular variations of the solar cycle[J]. Terrestrial Magnetism and Atmospheric Electricity, 1994, 49:243.
    [30]
    Sirocko F, Garbe-Schonberg D, McIntyre A, et al. Teleconnections between the subtropical monsoon and high-latitude climates during the last deglaciation[J]. Science, 1996, 272:526.
    [31]
    许靖华. 太阳、气候、饥饿与民族大迁移[J]. 中国科学D辑, 1998, 28(4):366-384.

    [XU Jing-hua. The sun, climate, starvation and nation's migration[J].Science in China(Series D), 1998, 28(4):366-384.]
    [32]
    Bianchi G G, McCave I N. Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland[J]. Nature, 1999, 397:515-517.
    [33]
    ZHOU Wei-jian, Head M J, LU Xue-feng, et al. Teleconnection of climatic events between east Asia and polar high latitude areas during the last deglaciation[J]. Palaeo. Palaeo.Palae., 1999, 152:163.
    [34]
    Hoyt D V, Schatten K H. The Role of The Sun in Climate Change[M]. Oxford:Oxford University Press, 1997.
    [35]
    Beer J, Mende W,Stellmacher R. The role of The sun in climate forcing[J]. Quaternary Science Review, 2000, 19:403-415.
    • Related Articles

  • Related Articles

    [1]WANG Yuhan, AN Fuyuan, LIU Xiangjun. Regional characteristics and mechanisms of lake water level decline in the Tibetan Plateau since 2 000 years ago[J]. Marine Geology & Quaternary Geology, 2024, 44(2): 55-68. DOI: 10.16562/j.cnki.0256-1492.2024021801
    [2]SHI Xuefa, LI Jingrui, QIAO Shuqing, LIU Shengfa, WAN Shiming, YANG Shouye. Research progress of the Tibetan Plateau - Bay of Bengal “source-sink” system since the Last Glacial Maximum[J]. Marine Geology & Quaternary Geology, 2023, 43(3): 14-25. DOI: 10.16562/j.cnki.0256-1492.2023061201
    [3]HU Yun, HE Mengying, XU Huan, Tin Aung Myint, ZHANG Bihui, BIAN Zixuan, ZHENG Hongbo. Application of two heavy mineral analysis methods in the provenance study of Irrawaddy River sediments on the southeastern margin of Tibetan Plateau[J]. Marine Geology & Quaternary Geology, 2022, 42(4): 181-193. DOI: 10.16562/j.cnki.0256-1492.2021112901
    [4]CHEN Zixuan, YANG Shengli, SU Yating, LIU Xiaojing, CHEN Hui, ZHOU Jiantao, LI Pushuang, YANG Junhuai, WANG Shuyuan, XIA Dunsheng. Spatial variation of surface soil color in the eastern Tibetan Plateau and its environmental significance[J]. Marine Geology & Quaternary Geology, 2022, 42(4): 171-180. DOI: 10.16562/j.cnki.0256-1492.2022032103
    [5]GONG Jianming, ZHANG Li, ZHANG Jian, LI Yonghong, CHEN Xiaohui, WANG Weichao, YANG Zhicheng. DISCUSSION ON GAS HYDRATE ACCUMULATION CONDITIONS IN WULI PERMAFROST ZONE, QINGHAI-TIBETAN PLATEAU[J]. Marine Geology & Quaternary Geology, 2015, 35(1): 145-151. DOI: 10.3724/SP.J.1140.2015.01145
    [6]HOU Zhanfang, ZHANG Jun, SONG Chunhui, LI Jijun, LIU Jia, LIU Shanpin, HUI Zhengchuang, PENG Tingjiang. THE OXYGEN AND CARBON ISOTOPIC RECORDS OF MIOCENE SEDIMENTS IN THE TIANSHUI BASIN OF THE NORTHESTERN TIBETAN PLATEAU AND THEIR PALEOCLIMATIC IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2011, 31(3): 69-78. DOI: 10.3724/SP.J.1140.2011.03069
    [7]WEI Haicheng, MA Haizhou, ZHENG Zhuo, PAN Anding, HUANG Kangyou, WANG Zhiying, ZHAI Jun. CHARACTERISTICS OF POLLEN ASSEMBLAGES OF SURFACE SAMPLES FROM THE NORTH-EASTERN TIBETAN PLATEAU AND THEIR IMPLICATIONS FOR VEGETATION AND CLIMATE[J]. Marine Geology & Quaternary Geology, 2010, 30(4): 187-192. DOI: 10.3724/SP.J.1140.2010.04187
    [8]LIU Dongyan, PENG Shasha, QIAO Yansong, XIE Ruihuang. EVOLUTION OF THE SOUTHWEST MONSOON ON ORBITAL TIME-SCALE REVEALED BY A LOESS-PALEOSOL SEQUENCE ON THE SOUTHEASTERN MARGIN OF THE QINGHAI-TIBETAN PLATEAU FOR THE LAST 1.16 Ma[J]. Marine Geology & Quaternary Geology, 2009, 29(5): 115-121. DOI: 10.3724/SP.J.1140.2009.05115
    [9]ZHANG Ran, LIU Xiao-dong, AN Zhi-sheng. RESEARCH PROGRESS IN METHODOLOGY FOR PALEOELEVATION RECONSTRUCTION OF THE TIBETAN PLATEAU[J]. Marine Geology & Quaternary Geology, 2008, 28(5): 129-136.
    [10]YANG Sheng-li, FANG Xiao-min, SHI Zheng-tao, SONG Chun-hui. DRYING EVENT AT 500 kaBP RECORDED BY THE CHENGDU CLAY GRAIN SIZE AT THE EASTERN MARGIN OF THE TIBETAN PLATEAU[J]. Marine Geology & Quaternary Geology, 2008, 28(2): 105-114.

Catalog

    Get Citation
    PDF
    XML
    Article views (1682) PDF downloads (6) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles
    WeChat WeChat
    Order Code Order Code

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return