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《Marine Geology & Quaternary Geology》 2002-04
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CLIMATIC RECONSTRUCTION FROM THE TREERINGδ~(13)C VALUES OF PINUS BUNGEANA DURING THE PAST 70 YEARS IN BEIJING

SUN Yanrong1, MU Zhiguo1,CUI Haiting2(1Department of Earth and Space Science, Peking University, Beijing 100871,China;2Department of City and Urban, Peking University, Beijing 100871,China)  
For δ13C of αcellulose of Pinus bungeana,tree rings are analyzed in Peking University. Combined with the records of Beijing Meteorological Station, the regressional equations of δ13C and climate factors are constructed, then the parameters are reconstructed. The calculated values are identical with the true values. The results indicate that δ13C values of tree ring αcellulose in Beijing area from 1928 to 1999 show significant correlation with average temperature from March to September and average precipitation rate from June to September during the past 70 years. The heavy δ13C is corresponding to low temperature from March to September and little precipitation from June to September, the light δ13C is corresponding to high temperature from March to September and much precipitation from June to September. In this article, we show that δ13C value of tree ring αcellulose in Beijing is closely related to temperature and precipitation during the growth, and it can be used as a substitute index of climate. To a certain extent, the study shows that there is an important relationship between δ13C values of tree ring αcellulose and climatic factor in monsoonal area. 
【Fund】: 国家自然科学基金资助项目(40071082)
【CateGory Index】: P597.2
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