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应用生态学报 ›› 2019, Vol. 30 ›› Issue (10): 3327-3335.doi: 10.13287/j.1001-9332.201910.023

• 研究论文 • 上一篇    下一篇

长白山红松年轮碳同位素与净初级生产力的关系

刁浩宇1,2, 王安志1, 袁凤辉1, 关德新1, 吴家兵1*   

  1. 1中国科学院沈阳应用生态研究所, 中国科学院森林生态与管理重点实验室, 沈阳 110016;
    2中国科学院大学, 北京 100049
  • 收稿日期:2019-04-18 出版日期:2019-10-20 发布日期:2019-10-20
  • 通讯作者: *E-mail: wujb@iae.ac.cn
  • 作者简介:刁浩宇, 男, 1994年生, 硕士研究生. 主要从事气候生态学研究. E-mail: dhy_1011@163.com
  • 基金资助:
    国家自然科学基金项目(31870625,31670707,41675112)资助

Relationship between tree ring δ13C and net primary productivity of Pinus koraiensis in Changbai Mountain, China

DIAO Hao-yu1,2, WANG An-zhi1, YUAN Feng-hui1, GUAN De-xin1, WU Jia-bing1*   

  1. 1Key Laboratory of Forestry Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China;
    2University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2019-04-18 Online:2019-10-20 Published:2019-10-20
  • Contact: *E-mail: wujb@iae.ac.cn
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (31870625, 31670707, 41675112).

摘要: 解析树木年轮碳同位素变化是揭示气候与环境变化的有效途径,然而少有研究分析年轮碳同位素对森林净初级生产力(NPP)的指示效应.基于生长季气象因子,分析了长白山红松年轮δ13C记录序列与阔叶红松林红松种群NPP变化趋势以及两者之间的相关关系.结果表明: 1970年以前,研究区红松年轮δ13C与红松种群NPP变化同步,且两者间呈极显著线性正相关关系,年轮δ13C记录了气候变化对红松种群NPP的影响;1970年以后,红松年轮δ13C与红松种群NPP变化出现分异,两者呈负相关关系但相关性不显著,表明干旱等其他环境因子的影响使年轮δ13C对气候变化的敏感性和对NPP指示性降低.这一相关关系在红松年轮δ13C与当年和下一年红松种群NPP之间都存在,表明当年环境状况对来年红松生长的重要意义.说明长白山红松年轮δ13C对红松种群NPP有良好的指示性,树木年轮δ13C有重建森林历史NPP长期变化的潜力.

Abstract: Carbon isotope in tree ring is an effective indicator of climate and environmental change. However, few studies have analyzed the indication effect of tree ring carbon isotope on net primary productivity (NPP) of forests. Based on meteorological factors of growing seasons, we analyzed the variation trend and the relationship between the tree ring δ13C chronosequence of Korean pine (Pinus koraiensis) and net primary productivity (NPP) of Korean pine in Changbai Mountain. We found that before 1970, the change of Korean pine tree ring δ13C and NPP was synchronous, with a highly significant linear positive correlation between them, indicating that tree ring δ13C recorded the impacts of climate change on NPP. After 1970, tree ring δ13C was negatively correlated with NPP but not statistically significant, meaning that other environmental factors such as severe droughts reduced the sensitivity of tree ring δ13C to climate change and the recording of NPP by tree ring δ13C. The δ13C of the current year was also correlated with the corresponding NPP in the following year, which indicated that the current year’s environmental conditions were of great significance to the growth of Korean pine in the following year. This study showed that tree ring δ13C was a good indicator of the NPP of Korean pine in Changbai Mountain and that tree ring δ13C had the potential to reconstruct long-term changes of forest NPP in the history.