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Chinese Journal of Applied Ecology ›› 2003, Vol. ›› Issue (9): 1469-1472.

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Dynamics of atmospheric6 13C in the past 440 years in Aleitai, Xinjiang

CHEN Tuo1, QIN Dahe1, LIU Xiao-hong1, REN Jiawen1, LI Jiangfeng 2   

  1. 1. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
    2. Xinjiang Institute of Meteorology, Urumchi 830002, China
  • Received:2001-03-27 Revised:2001-11-07

Abstract: Since industrial revolution, a large amount of anthropogenic CO2 from fossil fuel combustion and deforestation has been emitted into atmosphere, and thus, the atmospheric CO2 concentration increased rapidly, while the δ13C in atmospheric CO2 became lower and lower due to Suess effect.Therefore, the prediction of δ13C is crucial for studying global changes.In order to make an accurate prediction, it is necessary to understand its historical variation.The dynamics of δ13C in plants can sensitively reflect it.In this paper, the dynamics of δ13C in atmospheric CO2 in the past 440 years in Aleitai, Xinjiang were reconstructed by using tree-ring δ13C series and plant stable carbon isotope fractionation model.The results showed that atmospheric δ13C value was relatively constant before 1850 (R2=0.052), which was about -6.60‰, while a sharp decrease in atmospheric δ13C with an average of - 7.02‰ was found since 1850 (R2=0.65).Compared with those from ice core bubbles, more fluctuations were found in atmospheric 8 Cderived from tree-ring series, possibly due to the higher resolution of the latter, and the difference of real atmospheric δ13C between the growth site of the tree and the globe.

Key words: Tree ring, Atmosphere, 13C, Model

CLC Number: