欢迎访问《应用生态学报》官方网站,今天是 分享到:

应用生态学报 ›› 2020, Vol. 31 ›› Issue (10): 3568-3578.doi: 10.13287/j.1001-9332.202010.026

• 综合评述 • 上一篇    下一篇

碳氮稳定同位素技术在青藏高原高寒草甸生态系统研究中的应用: 进展与展望

周春丽1,2, 李以康1*, 曹广民1, 朋措吉1,2, 宋明华3, 徐兴良3, 周华坤1, 林丽1   

  1. 1中国科学院西北高原生物研究所, 青海省寒区恢复生态学重点实验室, 西宁 810008;
    2中国科学院大学, 北京 100049;
    3中国科学院地理科学与资源研究所, 生态系统网络观测与模拟重点实验室, 北京 100101
  • 收稿日期:2020-04-21 接受日期:2020-08-12 出版日期:2020-10-15 发布日期:2021-04-15
  • 通讯作者: * E-mail: liyikang501@163.com
  • 作者简介:周春丽, 女, 1996年生, 硕士研究生。主要从事高寒草地适应性管理研究。E-mail: zhoucl@nwipb.cas.cn
  • 基金资助:
    第二次青藏高原综合科学考察研究项目(2019QZKK0302)和青海省重点研发与转化计划项目(2019-SF-152)资助

Carbon and nitrogen stable isotopes technology in the researches on alpine meadow ecosystem in Qinghai-Tibet Plateau: Progress and prospect

ZHOU Chun-li1,2, LI Yi-kang1*, CAO Guang-min1, PENG Cuo-ji1,2, SONG Ming-hua3, XU Xing-liang3, ZHOU Hua-kun1, LIN Li1   

  1. 1Qinghai Province Key Laboratory of Restoration Ecology for Cold Regions, Northwest Institute of Plateau Biology, Chinese Academy of Sciences, Xining 810008, China;
    2University of Chinese Aca-demy of Sciences, Beijing 100049, China;
    3Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
  • Received:2020-04-21 Accepted:2020-08-12 Online:2020-10-15 Published:2021-04-15
  • Contact: * E-mail: liyikang501@163.com
  • Supported by:
    Second Tibetan Plateau Scientific Expedition and Research (STEP) Program (2019QZKK0302), and the Key R&D and Transformation Project of Qinghai Province (2019-SF-152).

摘要: 碳氮稳定同位素技术在草地生态系统研究中的应用日渐广泛,本文针对其在青藏高原高寒草甸生态系统中的研究与应用进行了总结。首先,探讨了环境因子(海拔、水肥、草地退化、温度)对青藏高原高寒草甸碳氮同位素组成(δ13C、δ15N)的影响:高寒草甸植物δ13C值与海拔呈正相关,与大气压强、草地退化和温度均呈负相关,与降水的关系尚有争议;土壤δ13C值与海拔和草地退化呈正相关;植被的δ15N值与水肥呈正相关,土壤的δ15N值与草地退化呈负相关。其次,综述了近年来该技术在高寒草甸植物光合型鉴定、植物水分利用、食物链营养关系、碳氮循环等方面的研究进展。最后,对碳氮稳定同位素技术在研究高寒草甸土壤有机碳与土壤呼吸、重现植被类型更替和气候演化历史、土壤N2O溯源、探究高寒草甸退化的原因、藏药与动物食品产地溯源等方面的应用前景进行了展望,以期进一步发挥其在青藏高原高寒草甸研究中的潜力。

关键词: 碳稳定同位素, 氮稳定同位素, 青藏高原, 高寒草甸生态系统, 碳氮循环

Abstract: Carbon and nitrogen stable isotopic technique has been widely used in research of glassland ecosystems. Here, we summarized studies using carbon and nitrogen stable isotopes in the alpine meadow ecosystem on the Qinghai-Tibet Plateau. Firstly, we reviewed the environmental factors which influenced carbon and nitrogen isotope composition (δ13C and δ15N) of plants and soils in alpine meadow, such as altitude, moisture, fertilization, grassland degradation, and temperature. The values of plant δ13C were positively correlated with altitude, and negatively correlated with atmospheric pressure, grassland degradation and temperature. The relationship between plant δ13C and precipitation was non-linear. The values of soil δ13C were positively correlated with altitude and grassland degradation. The values of plant δ15N were positively correlated with soil moisture and fertilization, and negatively correlated with grassland degradation. Secondly, we reviewed the current application and progresses of 13C and 15N in the identification of plant photosynthetic type, water use, nutrient transport along food chain and carbon and nitrogen cycle in the alpine meadow. Finally, we prospected the 13C and 15N isotopes application in researches on soil organic carbon and soil respiration in the alpine meadow, transitions of vegetation type, and climate change, soil N2O trace, exploration of vegetation degradation, identification of the origin of Tibetan medicine and animal food, etc. 13C and 15N isotopes could be widely used and play important roles in researches on the alpine ecosystems.

Key words: 13C isotope, 15N isotope, Qinghai-Tibet Plateau, alpine meadow ecosystem, nutrient cycle