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生态学杂志 ›› 2025, Vol. 44 ›› Issue (11): 3531-3539.doi: 10.13292/j.1000-4890.202511.025

• 研究报告 • 上一篇    下一篇

西藏东部两个主要建群树种径向生长水热响应分异的海拔阈值

钟元1,2,郑嘉诚1,2,贾恒锋1,2,邱红岩1,吕利新1*   

  1. 1中国科学院植物研究所植被与环境变化重点实验室, 北京 100093; 2中国科学院大学, 北京 100049)
  • 出版日期:2025-11-10 发布日期:2025-11-06

Altitudinal thresholds in hydrothermal responses of radial growth for two dominant tree species in eastern Tibet.

ZHONG Yuan1,2, ZHENG Jiacheng1,2, JIA Hengfeng1,2, QIU Hongyan1, LYU Lixin1*   

  1. (1 Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing 100093, China; 2University of Chinese Academy of Sciences, Beijing 100049, China).

  • Online:2025-11-10 Published:2025-11-06

摘要: 同一树种生长对水热因子的响应可能沿海拔梯度发生分异,但这一分异出现的海拔阈值缺乏研究,影响了气候变化背景下森林生长动态预测的准确性。本研究选取西藏东部川西云杉(Picea likiangensis var. rubescens)(阴坡)和大果圆柏(Juniperus tibetica)(阳坡)作为研究对象,基于树木年轮学方法,分别建立了5条标准化树轮宽度指数年表,并通过Pearson相关等分析方法探讨了树木径向生长对水热因子的响应特征。结果表明:川西云杉和大果圆柏径向生长主要受当年4—6月温度和降水影响,随海拔升高,阴坡的川西云杉径向生长与温度由负相关转为正相关,树轮宽度指数与降水的相关性逐渐下降,并由正相关转变为负相关;树木生长与水热因子相关关系发生转变的海拔阈值为4360~4410 m;而阳坡大果圆柏的树轮宽度指数与温度呈显著负相关,与降水呈显著正相关,相关系数没有沿海拔梯度发生符号转变。综上,川西云杉径向生长在高海拔受低温限制,在低海拔受水分亏缺限制;大果圆柏径向生长则在所有海拔都受水分亏缺限制。树木径向生长对水热因子的响应表现出显著的海拔阈值效应,这一现象揭示了森林生长动态具有明显的海拔依赖性和生态复杂性。因此,系统检验并精确界定水热转换的海拔阈值对于提升森林动态预测模型的准确性和可靠性具有重要的科学意义。


关键词: 川西云杉, 大果圆柏, 树木生长, 气候响应, 海拔阈值

Abstract: The growth responses of trees to hydrothermal conditions may vary across different tree species and change along altitudinal gradients. However, the patterns of these changes remain unclear, limiting the accuracy of forest growth predictions under future climate change. Using dendrochronological methods, we established five standardized tree-ring width chronologies for Picea likiangensis var. rubescens (north-facing slope) and Juniperus tibetica (south-facing slope) in eastern Tibet, and investigated the response characteristics of radial growth to hydrothermal factors through Pearson correlation analysis and other analytical approaches. The results showed that the growth of both species was primarily influenced by temperature and precipitation in the growing season (April to June). The correlation between tree-ring width and temperature for P. likiangensis changed from negative to positive with increasing altitude, with a significant positive relationship between the correlation coefficients and altitude (R2=0.86). Conversely, the correlation between treering width and precipitation changed from positive to negative with increasing altitude, and such change had a significant negative correlation with altitude (R2=0.93). The altitudinal threshold in which these correlations reversed was identified between 4360 m and 4410 m. In contrast, no such reversal was observed for J. tibetica on sunny slopes, and its radial growth remained negatively correlated with temperature and positively correlated with precipitation across the entire altitudinal gradient. These results suggest that the growth of P. likiangensis at higher altitudes is limited by low temperatures and by water deficit at lower altitudes. The growth of J. tibetica is consistently limited by water availability across all altitudes. The altitudinal threshold effect of tree growth in response to hydrothermal factors reveals the pronounced altitude dependence and ecological complexity of forest growth dynamics. Therefore, systematically examining and precisely defining the altitudinal thresholds of hydrothermal transitions is of significant scientific importance for improving the accuracy and reliability of forest dynamic prediction models.


Key words: Picea likiangensis var. rubescens, Juniperus tibetica, tree growth, climate response, altitude threshold