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《Journal of Glaciolgy and Geocryology》 2000-04
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Study on Climatic Significance of Fir Tree-Ring δ~(13) C from Zhaosu County of Xinjiang Region, China

CHEN Tuo 1 ,QIN Da he 1 ,LI Jiang feng 2 , REN Jia wen 1 ,LIU Xiao hong 1, SUN Wei zhen 1 (1.Laboratory of Ice Core and Cold Regions Environment, CAREERI, CAS,Lanzhou Gansu 730000, China; 2.Xinjiang Institute of Meteorolog  
Increasing concern on future climate changes and their potential impacts on mankind prompts scientists to explore a variety of historical and natural archives that can infer the past climatic changes. High-resolution time series data of tree-ring is one of them. In principle, when abundant CO 2 is available,plants tend to discriminate against 13 CO 2 relative to 12 CO 2 during photosynthesis. When stomata closure cuts off CO 2 supply in order to sustain operation under reduced CO 2 availability, continued carbon fixation is then necessarily less discriminating, while stomata closure is subjected to climatic change, especially change of temperature and (or) precipitation. This link between stomataclosureand 13 C / 12 Cratios (δ 13 C or Δ 13 C) in tree-rings forms the basis for a new potential method of climatic research. The research so far, however, has been confined mainly to North American and European continents, but in other regions a better understand of the past climatic changes in a global scale is needed. Therefore, the change of a tree-ring δ 13 C from a fir growing in the Zhaosu County of Xinjiang Region of China, 295 year old (1688~1982), was analyzed. There existed an obvious relationship between the carbon stable isotope discrimination(Δ 13 C) and precipitation, relative humidity, temperature and solar irradiation time, which were partly attributed to the shallow root systems of fir, and to shallow soil layer and steep slope of the sampled site. The further research shows that the above apparent relationship between Δ 13 C and temperature is a result of them correlating with precipitation or relative humidity, because precipitation or relative humidity is the primary limited factors of fir growth. Meanwhile, based on the function relationship between Δ 13 C and precipitation from June to May, the historic change of precipitation is reconstructed. Many dry and wet characteristics recorded in historical documents and tree-ring width inthe same region are also reflected in the tree-ringΔ 13 C series.
【Fund】: 中国科学院“九五”重大项目!(KZ95 1 A1 2 0 5 ;KZ95 1 A1 40 2 0 3;KZ95 2 S1 2 16 );; 中国科学院新疆地理与生态研究所阜康荒漠生
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