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Acta Prataculturae Sinica ›› 2019, Vol. 28 ›› Issue (2): 33-40.DOI: 10.11686/cyxb2018561

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Distribution of newly fixed carbon of Nitraria tangutorum in the plant-soil system

LI Xin-le1,2, BAO Fang1,*, WU Bo1, CAO Yan-li1, LIU Ming-hu2, DUAN Rui-bing2   

  1. 1.Institute of Desertification Studies, Chinese Academy of Forestry, Beijing 100091, China;
    2.Experimental Center of Desert Forestry, Chinese Academy of Forestry, Dengkou Desert Ecosystem Research Station of Inner Mongolia, Dengkou 015200, China
  • Received:2018-08-30 Online:2019-02-20 Published:2019-02-20
  • Contact: *E-mail: 34778953@qq.com

Abstract: Characterizing the carbon turnover in terrestrial ecosystems is critical for understanding and predicting carbon dynamics in ecosystems. We used in situ 13C pulse labeling to track photosynthetic carbon fluxes of Nitraria tangutorum from shoot to root and soil in the Ulanbuh Desert. The objectives of this study were: 1) To determine the transfer dynamics of newly photosynthesized carbon to different carbon pools including leaves, stems, roots, soil, and respiration. 2) To quantify the allocation rate of newly fixed carbon among different carbon pools. 3) to estimate the carbon budget of a N. tangutorum desert ecosystem. It was found that the distribution of 13C-newly fixed carbon in leaves, stems, and roots of N. tangutorum and in soil was significantly different in different labeling periods. The 13C abundance value in leaves and stems rose rapidly to the highest value after labeling for 1 h, at which point the 13C abundance value was 520.1‰ and 592.5‰, 14 and 20 times higher than the control, respectively. Thereafter, the 13C abundance value gradually decreased with time until it stabilized. The labeled 13C was found in the roots and soil after labeling 18 h, and the 13C abundance values reached 9.5‰ and -23.8‰, respectively. The amount of newly fixed carbon lost through shoot respiration and soil respiration reached a maximum after labeling for 1 h and 18 h, respectively. At the end of the labeling period, about 35.59% of labeled carbon was transferred to the shoots, 16.67% was retained in root, 31.92% was lost as respiration (shoot respiration+soil respiration) and 15.82% remained in the soil. In the three carbon pools, i.e., shoot, root, and soil pools, shoots consistently had the highest proportion of 13C in the plant-soil system during the 32 days. Based on the 13C partitioning pattern and biomass production, we estimate a total of 2895.6 kg C·ha-1·yr-1 was fixed by these desert plants during the vegetation growth season. This study suggests that N. tangutorum plays an important role in carbon sequestration in the carbon cycle of desert ecosystems.

Key words: desert plant, newly fixed carbon, distribution dynamics, distribution pattern, stable isotope