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生态学杂志 ›› 2021, Vol. 40 ›› Issue (7): 1947-1957.doi: 10.13292/j.1000-4890.202107.015

• 研究报告 • 上一篇    下一篇

川西高原4种典型针叶树径向生长对气候因子的响应  

张萌1,2,石松林1,2*,石春明3,白海1,2,李宗善4,彭培好1,2   

  1. 1成都理工大学旅游与城乡规划学院, 成都 610059; 2四川省社会科学重点研究基地(扩展)国家公园研究中心, 成都 610059; 3北京师范大学全球变化与地球系统科学研究院, 北京 100875; 4中国科学院生态环境研究中心城市与区域生态国家重点实验室, 北京 100085)
  • 出版日期:2021-07-10 发布日期:2021-07-09

Radial growth responses of four typical coniferous species to climatic factors in the Western Sichuan Plateau, China.

ZHANG Meng1,2, SHI Song-lin1,2*, SHI Chun-ming3, BAI Hai1,2, LI Zong-shan4, PENG Pei-hao1,2   

  1. (1College of Tourism and UrbanRural Planning, Chengdu University of Technology, Chengdu 610059, China; 2Research Center of National Park, Sichuan Key Research Base for Social Sciences, Chengdu 610059, China; 3College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China; 4State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Science, Chinese Academy of Sciences, Beijing100085, China).
  • Online:2021-07-10 Published:2021-07-09

摘要: 为揭示青藏高原东南缘不同针叶树种树木生长对气候因子的响应特征,用树木年轮学方法对川西道孚县高山针叶林优势树种鳞皮冷杉(Abies squamata)、川西云杉(Picea likiangensisvar. rubescens)、方枝柏(Juniperus saltuaria)和红杉(Larix potaninii)进行树芯采样,建立4个树种树轮宽度年表,探讨不同树种生长与气候因子间的关系。结果表明:4种针叶树径向生长对气候因子的响应存在明显差异,上一年及当年多数月份的平均最低温度对鳞皮冷杉和红杉径向生长具有显著促进作用,对川西云杉和方枝柏径向生长影响较小;上一年10月至当年3月的相对湿度对川西云杉径向生长具有显著抑制作用,对其他3种树木生长的限制较弱;自1958年以来,鳞皮冷杉与生长季(6—8月)平均最低温度保持着较为稳定的显著正相关关系,红杉和川西云杉与生长季平均最低温度的关系表现为先下降后上升的趋势,而方枝柏对平均最低温度响应敏感性呈现出逐渐下降的趋势,暗示着在未来气候变化背景下温度升高可能会促进鳞皮冷杉、红杉和川西云杉树木生长,而对方枝柏生长的影响不大,这可能会进一步改变该地区森林结构和组成。

关键词: 树木年轮, 径向生长, 气候变化, 青藏高原东南缘

Abstract: To reveal the growth responses of different coniferous species to climatic factors in the southeastern Tibetan Plateau, we used dendrochronological techniques to sample tree-ring cores of the dominant species of alpine coniferous forest in Daofu County, western Sichuan Province, including Abies squamata, Picea likiangensis var. rubescens, Juniperus saltuaria, and Larix potaninii. We developed treering width chronologies of the four species and conducted growth-climate relationship analyses to understand the influence of climatic factors on tree radial growth. The results showed that tree growth responses to climatic factors differed among the four species. The radial growth of A. squamata and L. potaniniiwas significantly positively associated with mean minimum temperature (Tmin) during most of the months in previous and current years, while the growth of P. likiangensis var. rubescens and J. saltuaria was not significantly correlated withTmin. Furthermore, relative humidity had strong limiting effect on the radial growth of P. likiangensis var. rubescens from previous October to current March, but had little influence on the growth of other three conifers. Since 1958, the relationship between the growth of A.squamataand the Tmin in growing season (June to August) has remained stable, the relationship of radial growth of L. potaniniiandP. likiangensis var.rubescens with theTmin in growing season decreased first and then increased, while the association between J.saltuaria radial growth and growing season Tmin has gradually decreased. Those results suggest that climate warming could benefit the development of A. squamata, L. potaninii and P. likiangensis var.rubescens and enhance tree radial growth, but weakly influence the radial growth of J. saltuaria, which may potentially affect stand structure and composition of alpine coniferous forest in this area.

Key words: tree-ring, radial tree growth, climate change, southeastern Tibetan Plateau.