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Chinese Journal of Applied Ecology ›› 2020, Vol. 31 ›› Issue (6): 1800-1806.doi: 10.13287/j.1001-9332.202006.024

• Special Features of Stable Isotope Ecology • Previous Articles     Next Articles

Effects of soil water stress and atmospheric CO2 concentration on photosynthetic and post-photosynthetic fractionation

DING Bing-bing1, ZHANG Yong-e2, YU Xin-xiao1*, JIA Guo-dong1, WANG Yu-song1, ZHENG Peng-fei1, JIANG Tao1, XIA Juan-juan1   

  1. 1Ministry of Education Key Laboratory of Soil and Water Conservation and Desertification Combating, Beijing Forestry University, Beijing 100083, China;
    2Institute of Sediment Research, China Institute of Water Resources and Hydropower Research, Beijing 100038, China
  • Received:2019-12-25 Online:2020-06-15 Published:2020-06-15
  • Contact: * E-mail: yuxinxiao111@126.com
  • Supported by:
    This work was supported by the Key Project of National Natural Science Foundation of China (41877152).

Abstract: Analysis of plant photosynthesis and post-photosynthetic fractionation can improve our understanding of plant physiology and water management. By measuring δ13C in the atmosphere, and δ13C of soluble compounds in leaves and branch phloem of Platycladus orientalis, we examined discrimination pattern, including atmosphere-leaf discrimination during photosynthesis (ΔCa-leaf) and leaf-twig discrimination during post-photosynthesis (ΔCleaf-phlo), in response to changes of soil water content (SWC) and atmospheric CO2 concentration (Ca). The results showed that ΔCa-leaf reached a maximum of 13.06‰ at 95%-100% field water-holding capacity (FC) and Ca 400 μmol·mol-1, and a minimum of 8.63‰ at 35%-45% FC and Ca 800 μmol·mol-1. Both stomatal conductance and mesophyll cell conductance showed a significant linear positive correlation with ΔCa-leaf, with a correlation coefficient of 0.43 and 0.44, respectively. ΔCleaf-phlo was not affected by SWC and Ca. Our results provide mechanism of carbon isotopes fractionation and a theoretical basis for plant survival strategies in response to future climate change.