植物生态学报 ›› 2010, Vol. 34 ›› Issue (2): 125-133.DOI: 10.3773/j.issn.1005-264x.2010.02.003

所属专题: 稳定同位素生态学

• 稳定同位素生态学专题论文 • 上一篇    下一篇

祁连山两种优势乔木叶片δ13C的海拔响应及其机理

张鹏1, 王刚2, 张涛1, 陈年来1,*()   

  1. 1甘肃农业大学资源与环境学院, 兰州 730070
    2兰州大学生命科学学院, 兰州 730000
  • 收稿日期:2008-10-08 接受日期:2009-01-21 出版日期:2010-10-08 发布日期:2010-02-01
  • 通讯作者: 陈年来
  • 作者简介:* E-mail: chennl@gsau.edu.cn

Responses of foliar δ13C in Sabina przewalskii and Picea crassifolia to altitude and its mechanism in the Qilian Mountains, China

ZHANG Peng1, WANG Gang2, ZHANG Tao1, CHEN Nian-Lai1,*()   

  1. 1College of Resources and Environmental Science, Gansu Agriculture University, Lanzhou 730070, China
    2College of Life Sciences, Lanzhou University, Lanzhou 730000, China
  • Received:2008-10-08 Accepted:2009-01-21 Online:2010-10-08 Published:2010-02-01
  • Contact: CHEN Nian-Lai

摘要:

以分布于祁连山北麓中段的两种优势乔木祁连圆柏(Sabina przewalskii)和青海云杉(Picea crassifolia)为研究对象, 分析了高山乔木叶片δ13C值对海拔(2 600-3 600 m)、土壤含水量和叶片含水量、叶片碳氮含量的响应及其机理。结果表明, 这两种乔木叶片δ13C值均随海拔升高呈增重趋势, 与海拔呈显著正相关关系(p < 0.000 1)。海拔2 600-3 600 m阳坡树种祁连圆柏叶片的δ13C值显著高于同海拔梯度阴坡树种青海云杉。祁连圆柏和青海云杉叶片的δ13C值均与年平均气温呈显著负相关关系(p < 0.000 1), 与年平均降水量呈显著正相关关系(p < 0.000 1)。祁连圆柏叶片δ13C值与土壤含水量(p < 0.000 1)、叶片含水量(p = 0.01)和叶片碳氮比(C/N) (p < 0.000 1)呈显著正相关关系, 与叶片全氮呈显著负相关关系(p < 0.000 1)。而青海云杉叶片δ13C值与土壤含水量、叶片全氮、叶片碳氮比和叶片含水量不相关。说明海拔变化引起的水热条件的改变, 尤其是温度变化对高山乔木叶片碳同位素分馏起主要作用, 但各个因子综合对高山植物叶片碳同位素分馏的作用机制可能比较复杂, 需进一步深入研究。

关键词: 海拔响应, 机理, 叶片δ13C值, 青海云杉, 祁连山, 祁连圆柏

Abstract:

Aims Sabina przewalskii and Picea crassifolia, widely distributed in the Qilian Mountains, were employed to analyze the response of leaf δ13C of subalpine trees to altitude and its mechanism.

Methods Leaf samples were taken at 2 600-3 600 m elevation in October 2007. The δ13C was determined using an isotope mass spectrometer, carbon content was estimated with the potassium dichromate method and nitrogen content was measured with the micro-Kjeldahl method. Data were evaluated with one-way analysis of variance and correlation analysis using SPSS version 11.5.

Important findings Foliar δ13C in both species was positively related to elevation (p < 0.000 1) and annual mean precipitation, but negatively related to annual temperature (p < 0.000 1). The δ13C value of S. przewalskii increased as leaf and soil water content increased, while that of P. crassifolia was not significantly related to soil water content, leaf water content, leaf N content or C/N ratio. Altitude, which can lead to changes of hydrothermal conditions, is the main factor influencing carbon isotope fractionation in these subalpine trees; however, the combined effects of various factors on the mechanism of action maybe more complicated and need further study.

Key words: altitudinal response, fractionation mechanism, leaf δ13C, Picea crassifolia, Qilian Mountains, Sabina przewalskii