Lyu Zhao-Yang, Yun Rui-Xin, Wu Tao, Ma Yan-Jun, Chen Zhen-Ju, Jin Yu-Ting, Li Jun-Xia
Tree-ring Laboratory, College of Forestry, Shenyang Agricultural University, Shenyang 110866, China.
Kuduer Bureau of Forestry, Kuduer 022164, Inner Mongolia, China.
Ying Yong Sheng Tai Xue Bao. 2020 Jun;31(6):1889-1897. doi: 10.13287/j.1001-9332.202006.011.
Climate change has profound impacts on the structure and function of forest ecosystem. Under the background of climate warming, the growth patterns and climate responses of different species in different environments determine the development and stability of ecosystems. Using the method of tree chronology with ring width data of Betula platyphylla in Oakley Mountain of Daxing'an Mountains, we examined the relationship between the growth climate response of the pioneer B. platyphylla in larch forest and temperature rise and altitudinal changes. The results showed that climate warming resulted in the differentiation on B. platyphylla in different altitude. The radial growth of B. platyphylla increased significantly at the low altitude area (1050 m), while there were little changes at the relatively high altitude area (1250 m). Before the time of rapid warming (1980), the radial growth of B. platyphylla on two altitude areas were significantly stressed by low temperature in winter (October to February). During the period of rapid warming (1981-2010), low temperature stress in winter did not affect tree growth, with the growing season (May to July) temperature becoming the main limiting factors to the radial growth of B. platyphylla at the relatively high altitude areas. The growth of B. platyphylla increased in the low altitude stands with favorable water and heat conditions. The distribution of B. platyphylla may generally spread to high altitude sites in the study area under climate warming.
气候变化对森林生态系统的结构和功能有着深远影响。在气候变暖的背景下,不同环境中不同物种的生长模式和气候响应决定了生态系统的发展与稳定。利用树木年代学方法,结合大兴安岭奥克里堆山白桦的年轮宽度数据,我们研究了落叶松林先锋树种白桦的生长气候响应与气温升高和海拔变化之间的关系。结果表明,气候变暖导致不同海拔的白桦出现分化。低海拔地区(1050米)白桦的径向生长显著增加,而相对高海拔地区(1250米)变化不大。在快速变暖时期(1980年)之前,两个海拔地区白桦的径向生长均受到冬季(10月至2月)低温的显著抑制。在快速变暖时期(1981 - 2010年),冬季低温胁迫并未影响树木生长,生长季(5月至7月)的温度成为相对高海拔地区白桦径向生长的主要限制因素。在水热条件良好的低海拔林分中,白桦的生长有所增加。在气候变暖的情况下,研究区域内白桦的分布可能总体上会向高海拔地点扩展。