LI Pian, ZHANG Maoheng, KONG Xinggong, ZHANG Chunxia, WANG Yongjin, ZHAO Kan. A STALAGMITE-RECORD OF EAST ASIAN SUMMER MONSOON IN THE LAST 2000 YEARS AND ITS CORRELATION WITH HISTORICAL RECORDS[J]. Marine Geology & Quaternary Geology, 2010, 30(4): 201-208. DOI: 10.3724/SP.J.1140.2010.04201
Citation: LI Pian, ZHANG Maoheng, KONG Xinggong, ZHANG Chunxia, WANG Yongjin, ZHAO Kan. A STALAGMITE-RECORD OF EAST ASIAN SUMMER MONSOON IN THE LAST 2000 YEARS AND ITS CORRELATION WITH HISTORICAL RECORDS[J]. Marine Geology & Quaternary Geology, 2010, 30(4): 201-208. DOI: 10.3724/SP.J.1140.2010.04201

A STALAGMITE-RECORD OF EAST ASIAN SUMMER MONSOON IN THE LAST 2000 YEARS AND ITS CORRELATION WITH HISTORICAL RECORDS

More Information
  • Received Date: January 10, 2010
  • Revised Date: March 17, 2010
  • A 4-5 year resolution oxygen isotope record based on 21230Th dates and 486 oxygen isotope data from a 236-mm-long stalagmite, which was collected from Xi-niu Cave in Shengnongjia, Hubei Province, provides a detailed history of the East Asian Summer Monsoon (EASM) during the past 2000 years. Our δ18O sequence reveals that EASM intensity gradually weakened in the last 2000 years, superimposed by numerous decades or century-scale aridity/moisture oscillations, showing a characteristics of the typical Medieval Warming Period and Little Ice Age. The δ18O record generally correlates well with the summer insolation at 33°N, indicating that the long-term trend of the EASM is likely modulated by summer insolation. A comparison with history literatures shows that periods of constant negative δ18O values (stable moisture periods) occur during the Han and Tang Dynasties, while intervals of positive yet large oscillation in δ18O values (aridity and abrupt monsoon variability) correspond to the War Era, Song and Ming Dynasties, indicating frequent plagues of aridity/flood. This relationship suggests a clear link between climate change and the demise of these dynasties, and climate variability probably played an important role in Culture evolution.
  • [1]
    Thompson L G, Yao T, Thompson E M, et al. A high-resolution millennial record of the south Asian monsoon from Himalayan ice cores[J]. Science, 2000, 289:1916-1919.
    [2]
    刘禹,安芷生,Hans W Linerholm, 等. 青藏高原中东部过去2485年以来温度变化的树轮记录[J]. 中国科学D辑, 2009, 39(2):166-176.

    [LIU Yu, AN Zhisheng, Linderholm H W,et al. Annual temperatures during the last 2485 years in the mid-eastern Tibetan Plateau inferred from tree rings[J]. Science in China Series D:Earth Sciences. 2009, 52(3):348-359.]
    [3]
    Yancheva G, Nowaczyk N R, Mingram J, et al. Influence of the intertropical convergence zone on the East Asian monsoon[J]. Nature, 2007, 445(4):74-77.
    [4]
    Tan M, Liu T S, Hou J Z, et al. Cyclic rapid warming on centennial-scale revealed by a 2650-year stalagmite record of warm season temperature[J]. Geophysical Research Letters, 2003, 30(12):1617-1620.
    [5]
    Zhang P Z, Cheng H, 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.
    [6]
    Hu C Y, Henderson G M, Huang J H, et al. Quantification of Holocene Asian monsoon rainfall from spatially separated cave records[J]. Earth and Planetary Science Letters, 2008, 266:221-232.
    [7]
    Bond G, Kromer B, Beer J, et al. Persistent solar influence on North Atlantic climate during the Holocene[J]. Science, 2001, 294:2130-2136.
    [8]
    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.
    [9]
    Flieitmann D, Burns S J, Mudelsee M, et al. Holocene for-cing of the Indian monsoon recorded in a stalagmite from Southern Oman[J]. Science, 2003, 300:1737-1739.
    [10]
    Hu F S, Kaufman D, Yoneji S, et al. Cyclic variation and solar forcing of Holocene climate in the Alaskan Subarctic[J]. Science, 2003, 301:1890-1893.
    [11]
    Neff U, Burns S J, Mangini A, et al. Strong coherence between solar variability and the monsoon in Oman between 9 and 6 kyr ago[J]. Nature, 2001, 411:290-293.
    [12]
    Gupta A K, Anderson D M, Overpeck J T. Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean[J]. Nature, 2003, 421:354-357.
    [13]
    Rind D. The sun's role in climate variations[J]. Science, 296:673-677.
    [14]
    Carslaw K S, Harrison R G, Kirkby J. Cosmic rays, clouds, and climate[J]. Science, 2002, 298:1732-1737.
    [15]
    Haug G H, Cunther D, Peterson L C, et al. Climate and the collapse of Maya civilization[J]. Science, 2003, 299:1731-1735.
    [16]
    Polyak V J, Asmerom Y. Late Holocene climate and cultural changes in the southwestern United States[J]. Science, 2001, 294:148-151.
    [17]
    Peter B, deMenocal P B. Cultural responses to climate change during the late Holocene[J]. Science, 2001, 292:667-673.
    [18]
    Zhang De'er, Lu L H. Anti-correlation of summer/winter monsoons?[J]. Nature, 2007, 450:7-9.
    [19]
    朱兆泉, 宋朝枢. 神农架自然保护区科学考察集[M]. 北京:中国林业出版社, 1999:38-41.[ZHU Zhaoquan, SONG Chaoshu. Scienrtific Survey of Shengnongjia Nature Conservation[M]. Beijing:China Forestry Publishing House, 1999:38

    -41.]
    [20]
    Shen C C, Edwards R L, Cheng H, et al. Uranium and thorium isotopic and concentration measurements by magnetic sector inductively coupled plasma mass spectrometer[J]. Chemical Geology, 2002, 185:165-178.
    [21]
    Gonfiantini R, Roche M A, Olivry J C, et al. The altitude effect on the isotopic composition of tropical rains[J]. Chemical Geology, 2001, 181:147-167.
    [22]
    Hendy C H, Wilson A T. Paleoclimatic data from speleothems[J]. Nature, 1968, 219:48-51.
    [23]
    ONeil J R, Clayton R N, Mayeda T K. Oxygen isotope fractionation in divalent metal carbonate[J]. Journal Chemistry Physics, 1969, 51:5547-5558.
    [24]
    Hendy E J, Gagan M K, Alibert C A, et al. Abrupt decrease in tropical Pacific sea surface salinity at end of little ice age[J]. Science, 2002, 295:1511-1514.
    [25]
    Goosse H, Arzel O, Luterbacher J, et al. The origin of the European "Medieval Warm Period"[J]. Climate of the Past, 2003, 2:99-113.
    [26]
    Yong C J, Ford D C, Gray J, et al. Stable isotope studies of cave seepage water[J]. Chemical Geology, 1985, 58:97-105.
    [27]
    Rozanski K, Araguas A L, Gonfiantini R. Isotope patterns in the modern global precipitation.[C]//In:Swart P K, Lohmann K C, Savin S,et al. Climate Change in continental climate records, America Geophysical Union, Geophysical Monograph, 1993, 78:1-36.
    [28]
    Johnson K R, Ingram B L. Spatial and temporal variability in the stable isotope systematic of modern precipitation in China:implications for paleoclimate reconstructions[J]. Earth and Planetary Science Letters, 2004, 220:365-377.
    [29]
    谢燕,汪永进,姜修洋. 盛冰期数十年尺度东亚季风变化的洞穴石笋记录[J]. 海洋地质与第四纪地质, 2008, 28(4):43-49.

    [XIE Yan, WANG Yongjin, JIANG Xiuyang. Decadal-scale climate change of east Asian monsoon during the last glacial maximum from stalagmite record[J]. Marine Geology and Quaternary Geology, 2008, 28(4):43-49.]
    [30]
    Abrantes F, Lebreiro S, Rodrigues T, et al. Shallow-marine sediment cores record climate variability and earthquake activity off Lisbon (Portugal) for the last 2000 years[J]. Quaternary Science Review,2005, 24:2477-2494.
    [31]
    竺可桢. 中国近五千年来气候变迁的初步研究[J]. 中国科学, 1973, 2:168-189.[ZHU Kezhen. The primary study of the last 5000

    years climate changes in China[J]. Science in China, 2:168-189.]
    [32]
    施雅风, 姚檀栋, 杨保. 近2000a古里雅冰心10 a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, 1999, 29(增1):79-86.[SHI Yafeng, YAO Tandong, YANG Bao. Decadal climatic variations recorded in Guliya ice core and comparison with the historical documentary data from East China during the last 2000 years[J]. Science in China Series D:Earth Sciences, 1999

    , 42(Supp1):91-100.]
    [33]
    Yang B, Braeuning A, Johnson K R, et al. General characteristics of temperature variation in China during the last two millennia[J]. Geophysical Research Letters, 2002, 29:381-384.
    [34]
    Paulsen D E,Li H C,Lu T L. Climate variability in central China over the last 1270 years revealed by high-resolution stalagmite records[J]. Quaternary Science Reviews, 2003, 22:691-701.
    [35]
    Haug G H, Hughen K A, Sigman D M, et al. Southward migration of the Interposal Convergence Zone through the Holocene[J]. Science, 2001, 293:1304-1308.
    [36]
    Watanabe T, Winter A, Oba T. Seasonal changes in sea surface temperature and salinity during the Little Ice Age in the Caribbean Sea deduced from Mg/Ca and18O/16O ratios in co-rals[J]. Marine Geology, 2001, 173:21-35.
    [37]
    Hodell D A,Brenner M,Curtis J H, et al. Climate change on the Yucatan Peninsula during the little ice age[J]. Quaternary Research, 2005, 63:109-121.
    [38]
    Gupta A K, Anderson D M, Overpeck J T. Southwest monsoon during the Holocene and their links to the North Atlantic Ocean[J]. Nature, 2003, 421:354-357.
    [39]
    Wang X F, Auler A S, Edwards R L, et al. Millennial-scale precipitation changes in southern Brazil over the past 90000 years[J]. Geophys Res. Lett. 2007, 34:699-706.
    [40]
    Xu H, Hong Y T, Lin Q H, et al. Temperature responses to quasi-100-yr solar variability during the past 6000 years based on δ18O of peat cellulose in Hongyuan, eastern Qinghai-Tibet plateau, China[J]. Palaeogeograpgy, Palaeoclimatology, Palaeoecology, 2006, 230:155-164.
    [41]
    Shindell D, Rind D, Balachandran N, et al. Solar cycle variability, ozone, and climate[J]. Science, 1999, 284:305-308.
    [42]
    Solanki S K, Usoskin I G, Kromer B, et al. Unusual activity of the sun during recent decades compared to the previous 11000 years[J]. Nature, 2004, 431:1084-1087.
    [43]
    Bard E, Raisbeck G, Yiou F, et al. Solar irradiance during the last 1200 years based on cosmogenic[J]. Tellus, 2000, 52B:985-992.
    [44]
    杨希义. 唐代关中农业经济的主要产品及其地理分布[J]. 西北大学学报:哲学社会科会学版,1986, 1:72-79.[YANG Xiyi. Mostly farm produce and geographical distribution of agricultural economy in the Tang Dynasty in Guanzhong area[J]. Journal of Northwest University:Philosophy and Social Sciences Edition, 1986

    , 1:72-79.]
    [45]
    刘俊文. 唐代水害史论[J]. 北京大学学报:哲学社会科学版, 1988, 2:48-62.[LIU Junwen. History of flood in Tang Dynasty[J]. Journal of Peking University:Philosophy & Social Sciences Edition, 1988

    , 2:48-62.]
    [46]
    Zhang De'er. Severe draught events as revealed in the climate records of China and their temperature situations over the last 1000 years[J]. Acta Meteorological Sinica, 2005, 19(4):485-491.
    [47]
    王曾瑜. 宋代文明的历史地位[J]. 河北学刊, 2006, 26(5):94-104.

    [WANG Zengyu. More recognitions of the historical position of the Song dynasty history[J]. Hebei Academic Joumal, 2006, 26(5):94-104.]
  • Related Articles

    [1]YANG Huihui, ZHOU Youmin, ZHONG Yi, LIU Qingsong. Variations and mechanisms of the Asian summer monsoon revealed by stalagmite δ18O records[J]. Marine Geology & Quaternary Geology, 2024, 44(1): 143-155. DOI: 10.16562/j.cnki.0256-1492.2023020801
    [2]ZHANG Pu, LIU Wei-guo, QIANG xiao-ke. VEGETATION COVERAGE AND MONSOON VARIATION RECORDED BY STABLE CARBON ISOTOPE OF LOES SINCE 2.5MA[J]. Marine Geology & Quaternary Geology, 2013, 33(1): 137-143. DOI: 10.3724/SP.J.1140.2013.01137
    [3]DONG Jinguo, DIAO Wei, KONG Xinggong. VARIATION IN URANIUM ISOTOPES OF STALAGMITES FROM SANBAO CAVE, HUBEI PROVINCE: IMPLICATIONS FOR PALAEOCLIMATE[J]. Marine Geology & Quaternary Geology, 2013, 33(1): 129-135. DOI: 10.3724/SP.J.1140.2013.01129
    [4]DONG Jinguo, ZHANG Fu. THE MID-HOLOCENE CLIMATE VARIATION INFERRED FROM A DATED STALAGMITE RECORD FROM WANGJIAWEI CAVE, NORTHEAST CHINA[J]. Marine Geology & Quaternary Geology, 2012, 32(1): 119-125. DOI: 10.3724/SP.J.1140.2012.01119
    [5]JIANG Xiuyang, LI Zhizhong, SHEN Chuanzhou, LI Jinquan. 2100~590 ABP STALAGMITE STABLE ISOTOPE RECORDS FROM TIAN'E CAVE AND THEIR REGIONAL CLIMATE SIGNIFICANCE[J]. Marine Geology & Quaternary Geology, 2011, 31(3): 117-122. DOI: 10.3724/SP.J.1140.2011.03117
    [6]CUI Yingfang, WANG Yongjin, LIU Dianbing. HIGH-RESOLUTION STALAGMITE δ18O RECORDS OF ASIAN MONSOON CHANGES IN SOUTHWEST GUIZHOU DURING THE LATE EPISODE OF MIS3: A TEST OF THE BI-POLAR SEE-SAW MODEL AT CENTENNIAL SCALE[J]. Marine Geology & Quaternary Geology, 2011, 31(3): 101-107. DOI: 10.3724/SP.J.1140.2011.03101
    [7]TONG Kai, WANG Yong-jin, CHENG Hai, JIANG Xiu-yang. EAST ASIAN SUMMER MONSOON RECORD OVER 571~476 kaBP FROM A STALAGMITE IN SHENNONGJIA[J]. Marine Geology & Quaternary Geology, 2007, 27(4): 111-116.
    [8]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.
    [9]JIANG Xiu-yang, WANG Yong-jin, KONG Xing-gong, XIA Zhi-feng. CENTENNIAL-SCALE EAST ASIAN MONSOON PRECIPITATION RECORD OVER 140~124 kaBP FROM A STALAGMITE IN SHENNONGJIA[J]. Marine Geology & Quaternary Geology, 2006, 26(3): 39-44.
    [10]RAO Zhi-guo, CHEN Fa-hu, WANG Hai-bin, ZHANG Jia-wu, ZHU Zhao-yu. EASTERN ASIAN SUMMER MONSOON VARIATION DURING MIS5e AS RECORDED BY PALEOSOL S1 AT JIUZHOUTAI LOESS SECTION[J]. Marine Geology & Quaternary Geology, 2006, 26(2): 103-111.

Catalog

    Article views (1808) PDF downloads (20) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return