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应用生态学报 ›› 2017, Vol. 28 ›› Issue (7): 2231-2238.doi: 10.13287/j.1001-9332.201707.004

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典型滨岸草地生态系统碳稳定同位素组成及分布特征

吴健1,2, 沙晨燕1, 王敏1, 吴建强1, 谭娟1, 齐晓宝1, 黄沈发1,2*   

  1. 1上海市环境科学研究院, 上海 200233
    2华东师范大学生态与环境科学学院, 上海 200062
  • 收稿日期:2016-09-18 修回日期:2017-03-29 发布日期:2017-07-18
  • 通讯作者: *mail:huangsf@saes.sh.cn
  • 作者简介:吴健,男,1977年生,博士.主要从事生态过程与修复研究.E-mail:wuj@saes.sh.cn
  • 基金资助:
    本文由上海市科学技术委员会科研计划项目(STCSM-13231203600)资助

Composition and distribution characteristics of stable carbon isotope in typical riparian grassland ecosystem

WU Jian1,2, SHA Chen-yan1, WANG Min1, WU Jian-qiang1, TAN Juan1, QI Xiao-bao1, HUANG Shen-fa1,2*   

  1. 1Shanghai Academy of Environmental Sciences, Shanghai 200233, China
    2College of Ecological and Environmental Science, East China Normal University, Shanghai 200062, China
  • Received:2016-09-18 Revised:2017-03-29 Published:2017-07-18
  • Contact: *mail:huangsf@saes.sh.cn
  • Supported by:
    This work was supported by the Research Project of Science and Technology Commission of Shanghai Municipality (STCSM-13231203600).

摘要: 通过测定上海市青浦区东风港百慕大、白花三叶草、高羊茅和白茅等4种典型滨岸草本植物各组织以及不同垂直深度土壤有机质δ13C值,对滨岸草地生态系统的植物-土壤碳稳定同位素特征进行了分析.结果表明: 白花三叶草、高羊茅属于C3植物,百慕大、白茅属于C4植物,其茎叶、凋落物和根系各组织间δ13C值无显著差异.C3和C4植物样带表层土壤有机质δ13C值随着土壤深度递增而呈现截然不同的变化特征,这与样带本底δ13C值以及碳稳定同位素分馏效应有关,同时还受植物根系分布深度的影响.植物输入是土壤有机碳(SOC)的最主要来源,植物有机体δ13C组成对土壤有机质δ13C值有直接影响,植物各组分δ13C值与土壤有机质δ13C值均存在极显著相关.4种草本植物样带SOC含量与δ13C值均呈极显著相关,其中,C3植物样带SOC含量与δ13C值呈线性负相关,C4植物样带SOC含量与δ13C值呈线性正相关.

Abstract: Plant-soil carbon stable isotope characteristics of riparian herbaceous ecosystem were ana-lyzed by measuring the δ13C value of plant tissues from four typical riparian herbaceous plants, which were Cynodon dactylon, Trifolium repens, Festuca arundinacea and Imperata cylindrical, and that of soil organic carbon (SOC) from different vertical depths along Dongfeng Port River in Qingpu District, Shanghai. The result showed that T. repens and F. arundinacea were C3 plants while C. dactylon and I. cylindrical were C4 plants. There was no significant difference between the δ13C va-lue of stem and leaf, litter and root of the four herbaceous plants. The surface SOC δ13C value of C3 and C4 plants strips showed different trends with soil depth, which could be related to the background SOC δ13C value, soil carbon stable isotope fractionation effect and plant root distribution depth as well. Plant input was the main source of SOC and the δ13C composition of plant organisms had direct effect on the SOC δ13C value. The δ13C value of plant components were significantly correlated with the δ13C value of SOC. The SOC content and δ13C value were significantly correlated in the four herbaceous plants strips. The SOC content and δ13C value showed linear negative correlation in C3 plant strips and linear positive correlation in C4 plant strips.