LONG Hao, MA Hai-zhou, WANG Nai-ang, LI Yu, WANG Chen-hua. MID-HOLOCENE CLIMATE VARIATIONS FROM LAKE RECORDS OF NW TENGGER DESERT[J]. Marine Geology & Quaternary Geology, 2007, 27(3): 105-111.
Citation: LONG Hao, MA Hai-zhou, WANG Nai-ang, LI Yu, WANG Chen-hua. MID-HOLOCENE CLIMATE VARIATIONS FROM LAKE RECORDS OF NW TENGGER DESERT[J]. Marine Geology & Quaternary Geology, 2007, 27(3): 105-111.
shu

MID-HOLOCENE CLIMATE VARIATIONS FROM LAKE RECORDS OF NW TENGGER DESERT

  • 1 Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China;

  • 2 School of Resources and Environment, Lanzhou University, Lanzhou 730000, China

More Information
  • Received Date: November 19, 2006
  • Revised Date: January 21, 2007
    Abstract
  • QTL section of 6.92 m depth is taken from Qingtu palaeolake, the terminal lake of Shiyang drainage located in NW Tengger Desert. Based on the detailed dating results, multi-proxy analysis of QTL section, including grain size, carbonate, TOC, C/N and δ13C of organic matter, was used to document regional climatic changes during 9~3 cal.kaBP. The climate evolution in the study area during 9~3 cal.kaBP is divided into four stages:①from cold and dry to warm and humid during the period of 9~7.8 cal.kaBP, ②a significant drought interval of multicentennial scale between 7.8~7.5 cal.kaBP, ③Holocene optimum characterized by a warm and moist climate during the period of 7.5~5 cal.kaBP, ④from humid to dry during 5~3 cal.kaBP.
    • FullText(HTML)
    • References (31)
  • [1]
    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,1992,22(12):1300-1308.

    [SHI Ya-feng, KONG Zhao-chen, WANG Su-min, et al. The climatic fluctuations and important events of Holocene Megathermal in China[J]. Science in China (Series B), 1992, 22(12):1300-1308.]
    [2]
    Shi Y F, Kong Z C, Wang S M, et al. Mid-Holocene climates and environment in China[J]. Global and Planetary Change, 1993, 7(1-3):219-233.
    [3]
    施雅风,孔昭宸,王苏民,等. 中国全新世大暖期鼎盛阶段的气候与环境[J]. 中国科学B辑,1993,23(8):865-873.

    [SHI Ya-feng, KONG Zhao-chen, WANG Su-min, et al. The Holocene Megathermal climate and environment in China[J]. Science in China (Series B), 1993,23(8):865-873.]
    [4]
    Li X Q, Zhou W J, An Z S, et al. The vegetation and monsoon variation at the desert-loess transition belt at Midiwan in northern China for the last 13 ka[J].The Holocene, 2003, 13(5):770-784.
    [5]
    Chen C T, Lan H C, Lou J Y, et al. The dry Holocene Megathermal in Inner Mongolia[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2003, 193:181-200.
    [6]
    Chen F H, Wu W, Holmes J A, et al. A mid-Holocene drought interval as evidenced by lake desiccation in the Alashan Plateau, Inner Mongolia, China[J]. Chinese Science Bulletin, 2003, 48(14):1401-1410.
    [7]
    冯绳武. 民勤绿洲的水系演变[J]. 地理学报,1963,29(3):241-249.

    [FENG Sheng-wu. The evolution of the drainage system of the Minqin oasis[J]. Acta Geographica Sinica,1963, 29(3):241-249.]
    [8]
    王乃昂,李吉均,曹继秀,等. 青土湖近6000年来沉积气候记录研究——兼论四五世纪气候回暖[J]. 地理科学,1999,19(2):119-124.

    [WANG Nai-ang,LI JI-jun, CAO Ji-xiu, et al. A preliminary research on the climate records of lacustrine deposits of Qingtu lake in the last 6000 years[J]. Chinese Geographical Science, 1999, 9(4):335-341.]
    [9]
    Zhang H C, Ma Y Z, Wunnemann B, et al. A Holocene climatic record from arid northwestern China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2000, 162:389-401.
    [10]
    邬光剑,潘保田,管清玉,等. 祁连山东段北麓近10 ka来的气候变化初步研究[J]. 中国沙漠, 1998,18(3):193-200.

    [WU Guang-jian, PAN Bao-tian, GUAN Qing-yu, et al. Climate changes in the north piedmont of eastern Qilian Mountains since 10 kaBP[J]. Journal of Desert Research, 1998, 18(3):193-200.]
    [11]
    Chen F H, Zhu Y, Li J J, et al. Abrupt Holocene changes of the Asian monsoon at millennial and centennial-scales:Evidence from lake sediment document in Minqin Basin, NW China[J]. Chinese Science Bulletin, 2001, 46(23):1942-1947.
    [12]
    Chen F H, Shi Q, Wang J M. Environmental changes documented by sedimentation of Lake Yema in arid China since the late glaciation[J]. Journal of Palaeolimnology, 1999, 22:159-169.
    [13]
    朱艳,陈发虎,Madsen B D. 石羊河流域早全新世湖泊孢粉记录及其环境意义[J]. 科学通报,2001,46(19):1596-1602.

    [ZHU Yan, CHEN Fa-hu, Madsen B D. The environmental signal of an early Holocene pollen record from Shiyang River basin lake sediments, NW China[J]. Chinese Science Bulletin,2001,47(4):267-273.]
    [14]
    Pachur H J, Wunnman B, Zhang H C, et al. Lake evolution in the Tengger Desert, Northwest China, during the last 40000 years[J]. Quaternary Research, 1995, 44:171-180.
    [15]
    陈敬安,万国江,张峰,等. 不同时间尺度下的湖泊沉积物环境纪录——以沉积物粒度为例[J].中国科学D辑,2003,33(6):563-568.

    [CHEN Jing-an, WAN Guo-jiang, ZHANG Feng, et al. Environmental records of lacustrine sediments in different time scales:Sediment grain size as an example[J]. Science in China (Series D), 2004, 47(10):954-960.]
    [16]
    孙千里,周杰,肖举乐. 岱海沉积物粒度特征及其古气候意义[J]. 海洋地质与第四纪地质,2001,21(1):93-95.

    [SUN Qian-li, ZHOU Jie, XIAO Ju-le. Grain-size characteristics of lake Daihai sediments and its palaeoenvironment significance[J]. Marine Geology and Quaternary Geology, 2001, 21(1):93-95.]
    [17]
    Meyers P A. Applications of organic geochemistry to paleolimnological reconstructions:a summary of examples from the Laurentian Great Lakes[J].Organic Geochemistry,2003, 34:261-289.
    [18]
    Meyers P A. Organic geochemical proxies of paleoceangraphic, paleolimnologic and paleoclimatic processes[J].Organic Geochemistry,1997, 27:213-250.
    [19]
    Meyers P A. Preservation of elemental and isotopic source identification of sedimentary organic matter[J]. Chemical Geology, 1994, 144:289-302.
    [20]
    Xu H, Ai L, Tang L C, Stable isotopes in bulk carbonates and organic matter in recent sediments of Lake Qinghai and their climatic implications[J]. Chemical Geology, 2006, 235:262-275.
    [21]
    沈吉,刘兴起,Matsumoto R,等. 晚冰期以来青海湖沉积物多指标高分辨率的古气候演化[J]. 中国科学D辑,2004,34(6):582-589.

    [SHEN Ji, LIU Xing-qi, Matsumoto R, et al. A high-resolution climatic change since the Late Glacial Age inferred from multi-proxy of sediments in Qinghai Lake[J]. Science in China (Series D), 2005, 48(6):742-751.]
    [22]
    刘兴起, 沈吉, 王苏民, 等. 16 ka以来青海湖湖相自生碳酸盐沉积记录的古气候[J]. 高校地质学报, 2003, 9(1):38-46.

    [LIU Xing-qi, SHEN Ji, WANG Su-min, et al. A 16000-year palaeoclimatic record derived from authigenetic carbonate of lacustrine sediment in Qinghai lake[J]. Geological Journal of China Universities, 2003, 9(1):38-46.]
    [23]
    Stuiver M, Reimer P J, Braziunas T F. High precision radiocarbon age calibration for terrestrial and marine samples[J]. Radiocarbon, 1998, 40:1127-1151.
    [24]
    姚檀栋, 施雅风. 祁连山敦德冰芯记录的全新世气候变化[C]//中国全新世大暖期气候与环境. 北京:海洋出版社, 1992:206-211.[YAO Tan-dong, SHI Ya-feng. Holocene climate changes recorded in Dunde ice core from Qilian mountain[C]//The Holocene Megathermal climate and environment in China. Beijing:China Ocean Press, 1992:206

    -211.]
    [25]
    Sun J M, Li S H, Han P, 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, 233:51-62.
    [26]
    Xiao J L, Xu Q H, Nakamura T, et al. Holocene vegetation variation in the Daihai Lake region of north-central China:a direct indication of the Asian monsoon climatic history[J]. Quaternary Science Reviews, 2004,23:1669-1679.
    [27]
    Lister G S, Kelts K, Chen K Z, et al. Lake Qinghai, China:closed-basin lake levels and the oxygen isotope record for ostracoda since the last Pleistocene[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1991, 84:141-162.
    [28]
    Hong Y T, Hong B, Lin Q H, et al. Correlation between Indian Ocean summer monsoon and North Atlantic climate during the Holocene[J]. Earth and Planetary Science Letters, 2003, 211:371-380.
    [29]
    Shao X H, Wang Y J.Cheng H, et al. Long-term trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite δ18O record from Shennongjia in Central China[J].Chinese Science Bulletin, 2006,51(2):221-228.
    [30]
    Wang Y J, Cheng H, Edwards R L, et al. The Holocene Asian Monsoon:Links to Solar Changes and North Atlantic Climate[J]. Science, 2005, 308:854-857.
    [31]
    Herzschuh U, Winter K, Wunnemann B, et al. A general cooling trend on the central Tibetan Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra[J]. Quaternary International, 2006, 154-155:113-121.
    • Related Articles

  • Related Articles

    [1]YANG Shixiong, YE Siyuan, HE Lei, YUAN Hongming, ZHAO Guangming, DING Xigui, PEI Shaofeng, LU Jingfang. Geochemical and clay mineral characteristics of the Holocene sediments on the west coast of Bohai Bay and their implications for environmental and climatic changes[J]. Marine Geology & Quaternary Geology, 2021, 41(2): 75-87. DOI: 10.16562/j.cnki.0256-1492.2020092901
    [2]FU Mengxuan, YU Shiyong, WU Jinjia, CHEN Shiyue, HOU Zhanfang, ZHOU Ruiwen, LI Zheng, WEI Benjie. Mid-to-Late Holocene climate changes on the southern margin of the Badain Jaran Desert: Evidence from the Gaotai Lake sediments[J]. Marine Geology & Quaternary Geology, 2020, 40(4): 192-203. DOI: 10.16562/j.cnki.0256-1492.2019110602
    [3]MENG Jie, WEN Xiaohao, LI Baosheng, NIU Dongfeng, ZHAO Zhanlun, SUN Yefeng, YANG Qinjiang. GRAIN-SIZE DISTRIBUTION ALONG THETUMEN SECTION OF SOUTHERN TENGGER DESERT, NORTHWESTERN CHINA AND ITS PALEOCLIMATIC IMPLICATIONS DURING THE LAST DEGLACIAL[J]. Marine Geology & Quaternary Geology, 2016, 36(1): 165-176. DOI: 10.16562/j.cnki.0256-1492.2016.01.017
    [4]LI Yongfei, YU Ge, LI Chunhai, HU Shouyun, SHEN Huadong, YIN Gang. ENVIORNMENT RECONSTRUCTION OF MID-HOLOCENE PALEO-LAKES IN ZHENGZHOU AND SURROUNDING REGIONS AND THE SIGNIFICANCE FOR HUMAN CULTURAL DEVELOPMENT IN CENTRAL CHINA[J]. Marine Geology & Quaternary Geology, 2014, 34(3): 143-154. DOI: 10.3724/SP.J.1140.2014.03143
    [5]CHEN Xuemei, LI Guoqiang, HUANG Xiaozhong, ZHAO Hui. THE VEGETATION CHENGES IN ULAN BUH DESERT SINCE THE LAST GLACIAL: POLLEN EVIDENCE FROM CORE WL10ZK-1[J]. Marine Geology & Quaternary Geology, 2013, 33(4): 169-174. DOI: 10.3724/SP.J.1140.2013.04169
    [6]GUO Jing, LI Jun, ZHAO Qi, FANG Rong, YANG Qili, ZHANG Chengjun. THE GRAIN SIZE AND ELEMENT RECORD OF THE DRY MID-HOLOCENE LAKE IN THE TENGGER NUUR, INNER MONGOLIA PLATEAU, CHINA[J]. Marine Geology & Quaternary Geology, 2012, 32(5): 115-122. DOI: 10.3724/SP.J.1140.2012.05115
    [7]WU Xudong, SHEN Ji, WANG Yong. HOLOCENE PALEOENVIRONMENTAL EVOLUTION OF THE HUGUANGYAN MAAR LAKE[J]. Marine Geology & Quaternary Geology, 2011, 31(4): 155-162. DOI: 10.3724/SP.J.1140.2011.04155
    [8]LI Zhi-fei, LÜ Yan-bin, TAO Shi-chen, AN Cheng-bang. HOLOCENE CLIMATE CHANGES IN EASTERN XINJIANG: A CASE STUDY ON BARKOL LAKE[J]. Marine Geology & Quaternary Geology, 2008, 28(6): 107-112. DOI: 10.3724/SP.J.1140.2008.06107
    [9]WU Jiang-ying, WANG Yong-jin, KONG Xing-gong. EVOLUTION AND ABRUPT CHANGES OF THE HOLOCENE ASIAN MONSOON CLIMATE RECORDED BY STALAGMITE IN BAIGU CAVE IN GUIZHOU[J]. Marine Geology & Quaternary Geology, 2006, 26(5): 55-60.
    [10]YANG Dong, FANG Xiao-min, DONG Guang-rong, PENG Zi-cheng, LI Ji-jun. AEOLIAN DEPOSIT EVIDENCE FOR FORMATION AND EVOLUTION OF THE TENGGER DESERT IN THE NORTH OF CHINA SINCE EARLY PLEISTOCENE[J]. Marine Geology & Quaternary Geology, 2006, 26(1): 93-100.

Catalog

    WANG Chen-hua

    • 2 School of Resources and Environment, Lanzhou University, Lanzhou 730000, China

    1. On this Site
    2. On Google Scholar
    3. On PubMed
    Get Citation
    PDF
    XML
    Article views (1740) PDF downloads (8) 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: hydzbjb@163.com

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

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return