• Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology
Volume 29 Issue 3
Sep.  2010
Turn off MathJax
Article Contents
YIN Jian-jun, QIN Jia-ming, LIN Yu-shi, YANG Yan, TANG Wei. Research progress on the recent 2 000 years’ climate change revealed by stalagmite record in China[J]. CARSOLOGICA SINICA, 2010, 29(3): 258-266. doi: 10.3969/j.issn.1001-4810.2010.03.007
Citation: YIN Jian-jun, QIN Jia-ming, LIN Yu-shi, YANG Yan, TANG Wei. Research progress on the recent 2 000 years’ climate change revealed by stalagmite record in China[J]. CARSOLOGICA SINICA, 2010, 29(3): 258-266. doi: 10.3969/j.issn.1001-4810.2010.03.007

Research progress on the recent 2 000 years’ climate change revealed by stalagmite record in China

doi: 10.3969/j.issn.1001-4810.2010.03.007
  • Received Date: 2009-03-16
  • Publish Date: 2010-09-25
  • The UN climate conference held in Copenhagen has directed more attention to the study on the recent 2 000 years’ climate change. The main achievements on study of climate change revealed by stalagmite record, eapecialy the climate change in the recent 2 000 years in China, is summarized in the paper as follows, a series of climate events in the recent 2 000 years are recorded by the stalagmite in China monsoon area; high resolution reconstruction is made; the temperature in hot month is reconstructed with annual resolution; and “circulation effect” is discovered by integrate research, etc. But there are also many problems need to be resolved, such as oxygen isotope mechanism, chronology, regional and typical stalagmite research as well. So it is proposed that the oxygen isotope mechanism research with resolution in annual scale, especially the whole migration and changes process of oxygen isotope from precipitation to stalagmite, should be enhanced; and the integrated study of stalagmite record’s respond mechanism to climate change by comparing with other proxy record should be done, and research on the recent 2 000 years’ chronology and on the regional and typical stalagmite should be enhanced.

     

  • loading
  • [1]
    Frank McDermott, David P. Mattey, Chris Hawkesworth. Centennial-Scale Holocene Climate Variability Revealed by a High-Resolution Speleothem δ18O Record from SW Ireland. SCIENCE, 2001, 294: 1328~1331.
    [2]
    Yancheva G, Nowaczyk N R, Mingram J, et al. Influence of the intertropical convergence zone on the East-Asian monsoon. Nature, 2007,445: 74—77.
    [3]
    Dansgaard W, J honson S , Moeller J , et al . One t housand centuries of climate record f rom Camp Century on t he Greenland ice sheet [J ].Science , 1969 ,166 :377 – 381.
    [4]
    姚檀栋,秦大河,田立德等.青藏高原2ka来温度与降水变化——古里雅冰芯记录[J].中国科学(D辑),1996,26(4):348-353.
    [5]
    施雅风,姚檀栋,杨保.近2000a古里雅冰芯10a尺度的气候变化及其与中国东部文献记录的比较[J].中国科学(D辑),1999,29(增刊1):79-86.
    [6]
    唐自华,穆桂金,陈冬梅等.昆仑山北坡近5000年以来黄土堆积的环境信息[J].第四纪研究,2007,27(4):598-606.
    [7]
    王鑫,王东晓,高荣珍等.南海珊瑚灰度记录中反映人类引起的气候变化信息[J].科学通报,2010,55(1):45-51.
    [8]
    沈吉,杨丽原,羊向东等.全新世以来云南洱海流域气候变化与人类活动的湖泊沉积记录[J].中国科学(D辑),2004,34(2):130-138.
    [9]
    张恩楼,沈吉,王苏民等.青海湖近900年来气候环境演变的湖泊沉积记录[J].湖泊科学,2002,14(1):32-38.
    [10]
    陈发虎,黄小忠,张家武等.新疆博斯腾湖记录的亚洲内陆干旱区小冰期湿润气候研究[J].中国科学(D辑),2007,37(1):77-85.
    [11]
    康兴成,张其花.青海都兰过去2000年来的气候重建及其变迁[J].地球科学进展,2000,15(2):215-221.
    [12]
    刘晓宏,秦大河,邵雪梅等.祁连山中部过去近千年温度变化的树轮记录[J].中国科学(D辑),2004,34(l):89-95.
    [13]
    洪冰,刘丛强,林庆华等.哈尼泥炭δ18O记录的过去14000年温度演变[J].中国科学(D辑),2009,39(5):626-637.
    [14]
    何报寅,张穗,蔡述明.近2600年神农架大九湖泥炭的气候变化记录[J].海洋地质与第四纪地质,2003,23(2):109-115.
    [15]
    崔美玲,罗运利,孙湘君.吉林哈尼湖钻孔5000年以来的古植被气候变化指示[J].海洋地质与第四纪地质,2006,26(5):117-122.
    [16]
    竺可祯.中国近五千年来气候变迁的初步研究[M].北京:科学出版社,1979: 475-498.
    [17]
    葛全胜,郑景云,方修琦等.过去2000a中国东部冬半年温度变化[J].第四纪研究,2002,22(2):166-173.
    [18]
    Zhang Pingzhong,Cheng Hai,Edwards R L et al.A test of climate,sun,and culture relationships from an 1810-year Chinese cave record[J].science,2008,322: 940-942.
    [19]
    Dorte Eide Paulsen, Hong-Chun Li, Teh-Lung Ku. Climate variability in central China over the last 1270 years revealed by high-resolution stalagmite records[J]. Quaternary Science Reviews,2003,22:691–701.
    [20]
    Tan Liangcheng, Cai Yanjun, Cheng Hai et al. Summer monsoon precipitation variations in central China over the past 750 years derived from a high-resolution absolute-dated stalagmite[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2009,280:432-439.
    [21]
    张德二.我国“中世纪暖期气候的初步推断[J].第四纪研究,1993,(1):7-15.
    [22]
    王绍武.小冰期气候的研究[J].第四纪研究,1995,(3):202-212.
    [23]
    刘禹,Won-Kyu-Park,蔡秋芳等.公元1840年以来东亚夏季风降水变化——以中国和韩国的树轮记录为例[J].中国科学(D辑),2003,33(6):543-549.
    [24]
    杨勋林,张平中,陈发虎.近50a来青藏高原东部高海拔洞穴现代石笋氧同位素组成及其含义[J].科学通报,2007,52(6):698-706.
    [25]
    Wang Y.J., Cheng H., R.L.Edwards, et al.A high-resolution absolute-dated late Pleistocene monsoon record from Hulu cave, China [J].science,2001,(294):2345-2348.
    [26]
    Wang Yongjin,Cheng Hai, R.L.Edwards, et al. The Holocene Asian Monsoon: Links to Solar Changes and North Atlantic Climate[J].science,2005,(308):854-857.
    [27]
    Wang Y.J., Cheng H., R.L.Edwards, et al. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years[J].nature,2008,(451):1090-1093.
    [28]
    Yuan Daoxian, Cheng H., R.L.Edwards, et al. Timing, Duration, and Transitions of the Last Interglacial Asian Monsoon[J].science,2004,(304):575-578.
    [29]
    Moore G.W. Speleothem—A new cave term[J].National Speleological:Society News,1952,10(6):2.
    [30]
    O’Neil J R, Clayton R N, Mayeda T K. Oxygen isotope fractionation in divalent metal carbonates[J]. Journal of Chemical Physics,1969,51:5547-5558.
    [31]
    Hendy C H. The isotopic geochemistry of speleothems- Pt. I. The calculation of the effects of different model of formation on the isotopic composition of speleothems and their applicability as paleoclimate indictors[J].Geochim et Cosmochim Acta,1971,35:801-824.
    [32]
    Edwards R L, Chen J H, Wasserburg G J. 238U-234U-230Th-232Th systematics and the precise measurement of time over the past 500,000 years. Earth and Planetary Science Letters, 1986, 81: 175-192.
    [33]
    W.X. Li, J. Lundberg, A. P. Dickin et al. High-precision mass-spectrometric uranium-series dating of cave deposits and implications for palaeoclimate studies[J]. Nature,1989, 339:534-536.
    [34]
    Isaac J.Winograd, Tyler B.Coplen, Barney J.Szabo, et al. A 250, 000-year climatic record from Great Basin vein calcite: Implications for Milankovitch theory. Science, 1988, 242(4883):1275-1280.
    [35]
    Dominik Fleitmann, Stephen J. Burns, Manfred Mudelsee, et al. Holocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman[J].science,2003,300(5626):1737-1739.
    [36]
    Hai Cheng, R. Lawrence Edwards, Wallace S. Broecker, et al. Ice age terminations [J]. science,2009,326(5950):248-252.
    [37]
    汪训一.桂林茅茅头大岩洞穴沉积物的放射性年龄及氧、碳同位素特征[J].科学通报,1985,(7):528-531.
    [38]
    覃嘉铭等.大气降水氢氧同位素与主要气候因素的相关性研究——以桂林雁山气象站多年监测数据为例.壳幔演化与成岩成矿同位素地球化学,地震出版社,1993:216-217.
    [39]
    覃嘉铭,袁道先,林玉石等.桂林44ka B.P.石笋同位素记录及其环境解译[J].地球学报,2000,21(4):407-416.
    [40]
    李红春,顾德隆,Lowel D. Stot等.高分辨率洞穴石笋稳定同位素应用之一——京津地区500 a来的气候变化——δ18O记录[J].中国科学(D辑),1998,28(2):181-186.
    [41]
    谭明.环流效应:中国季风区石笋氧同位素短尺度变化的气候意义——古气候记录与现代气候研究的一次对话[J].第四纪研究,2009,29(5):851-862.
    [42]
    蔡演军,彭子成,安芷生等.贵州七星洞全新世石笋的氧同位素记录及其指示的季风气侯变化[J].科学通报,46(16):1398-1402.
    [43]
    林玉石,张美良,覃嘉铭.云南宁蒗泸沽湖地区的古环境重建[J].中国岩溶,2001,20(3):174-182.
    [44]
    马志邦,李红春,夏明等.距今3ka来京东地区的古气温变化:石笋Mg/Sr记录[J].科学通报,2002,47(23):1829-1834.
    [45]
    张美良,袁道先,林玉石等.桂林响水洞6.00 ka B P以来石笋高分辨率的气候记录[J].地球学报,2003,24(5):439-444.
    [46]
    Hu Chaoyong,Gideon M. Henderson, Huang Junhua, et al. Quantification of Holocene Asian monsoon rainfall from spatially separated cave records[J]. Earth and Planetary Science Letters,2008,(266):221-232.
    [47]
    Jason Cosford, Qing Hairuo, Bruce Eglington, et al. East Asian monsoon variability since the Mid-Holocene recorded in a high-resolution,absolute-dated aragonite speleothem from eastern China[J]. Earth and Planetary Science Letters,2008, 275:296–307.
    [48]
    李红春,顾德隆,Dorte Paulsen等.陕南石笋稳定同位素记录中的古气候和古季风信息[J].地震地质,2000,22(增刊):63-78.
    [49]
    覃嘉铭,袁道先,林玉石等.公元8世纪以来贵州荔波石笋高分辨率的气候变化记录[J].中国岩溶,2008,27(3):266-272.
    [50]
    张美良,程海,林玉石等.贵州荔波1.5万年以来石笋高分辨率古气候环境记录[J].地球化学,2004,33(1):65-74.
    [51]
    张美良,程海,林玉石等.贵州荔波地区2000年来石笋高分辨率的气候记录[J].沉积学报,2006,24(3):339-348.
    [52]
    张美良,朱晓燕,程海等.贵州荔波1200年来石笋高分辨率的古气候环境记录[J].地球学报,2009,30(6):831-840.
    [53]
    何尧启,汪永进,孔兴功等.贵州董哥洞近1000a来高分辨率洞穴石笋δ18O记录[J].科学通报,2005,50(11):1114-1118.
    [54]
    F.Steinhilber, J. Beer, C. Fr?hlich. Total solar irradiance during the Holocene[J]. Geophsical research letters. 2009,36,L19704:1-5.
    [55]
    刘东生,谭明,秦小光等. 洞穴碳酸钙微层理在中国的首次发现及其对全球变化研究的意义[J].第四纪研究,1997,(1):41-51.
    [56]
    李彬,袁道先,林玉石等.桂林盘龙洞石笋发光性特征及其古环境记录的初步研究[J].地球学报,1997,18(4):400-406.
    [57]
    谭明,刘东生,秦小光等.北京石花洞全新世石笋微生长层与稳定同位素气候意义初步研究[J].中国岩溶,1997,16(1):1-10.
    [58]
    秦小光,刘东生,谭明等. 北京石花洞石笋微层灰度变化特征及其气候意义——Ⅱ.灰度的年际变化[J].中国科学(D辑),2000,30(3):239-248.
    [59]
    侯居峙,谭明,程海等.本溪水洞石笋微层年代学初步研究[J].中国科学(D辑),2001,31(5):387-392.
    [60]
    Tan Ming, Liu Tungsheng. Cyclic rapid warming on centennial-scale revealed by a 2650-year stalagmite record of warm season temperature[J].Geophysical research litters,2003,30(12):191-194.
    [61]
    谭明,邵雪梅,刘晓宏等.中国近千年石笋-树轮集成温度记录[J].气候变化研究进展,2006,2(3):113-116.
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article views (2076) PDF downloads(1530) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return