Liu Min, Mao Zi Jun, Li Yue, Xia Zhi Yu
Heilongjiang Province Key Laboratory of Resistance Gene Engineering and Protection of Biodiversity in Cold Areas, Qiqihar University, Qiqihar 161006, Heilongjiang, China.
Ministry of Education Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin 150040, China.
Ying Yong Sheng Tai Xue Bao. 2018 Nov;29(11):3530-3540. doi: 10.13287/j.1001-9332.201811.010.
Dendrochronological techniques were used to study the response of radial growth of Pinus koraiensis with different diameter classes to climate change throughout the natural range of broad-leaved Korean pine forests, including Baishilazi Nature Reserve (40.9° N), Changbai Mountain Nature Reserve (42.4° N), Liangshui Nature Reserve (47.2° N), and Shengshan Nature Reserve (49.4° N). We investigated the similarities and differences of growth responses of different diameter classes to climate factors and clarified the key climate factors affecting the growth of P. koraiensis at different latitude sites. We explored the dynamic changes of the radial growth of P. koraiensis from the latitudinal gradient over the past 40 years. The results showed many similarities in the response of two diameter classes to local climate factors. Small diameter (diameter at breast height of 10-20 cm) trees were more sensitive to the changes of average minimum temperature of the current growing season and the meteorological factors of the previous year, whereas large diameter (diameter at breast height >40 cm) trees were more sensitive to the changes of average maximum temperature and average relative humidity of the current growing season. The key meteorological factors that affecting radial growth of P. koraiensis differed along the latitude gradient. In Baishilazi Nature Reserve, the southernmost plot, the key climate factors were the average maximum temperature and the average maximum temperature in the current growing season. In Shengshan Nature Reserve, the northernmost sample plot, the key climate factors were low temperature factors, such as the minimum temperature in all seasons, the average maximum temperature in winter, the average temperature of all seasons except for the end of previous growing season and the current growing season. The Palmer drought severity index (PDSI) in the current growth season and the end of the current growth season and the precipitation in the current growth season were the key climate factors in Changbai Mountain Nature Reserve. The average temperature of the current growing season was the key climate factor of Liangshui Nature Reserve. In recent four decades, with the rising of temperature, the radial growth of P. koraiensis of two diameter classes significantly decreased in the southernmost point, significantly increased in the northernmost point, and had no significant variation in middle latitudes.
利用树木年代学技术,研究了不同径级红松径向生长对气候变化的响应,研究范围涵盖了阔叶红松林的整个自然分布区,包括白石砬子自然保护区(北纬40.9°)、长白山自然保护区(北纬42.4°)、凉水自然保护区(北纬47.2°)和圣山自然保护区(北纬49.4°)。我们调查了不同径级对气候因子生长响应的异同,阐明了影响不同纬度地区红松生长的关键气候因子。我们探讨了过去40年红松径向生长随纬度梯度的动态变化。结果表明,两个径级对当地气候因子的响应有许多相似之处。小径级(胸径10 - 20厘米)树木对当前生长季平均最低温度和前一年气象因子的变化更为敏感,而大径级(胸径>40厘米)树木对当前生长季平均最高温度和平均相对湿度的变化更为敏感。影响红松径向生长的关键气象因子沿纬度梯度有所不同。在最南端的白石砬子自然保护区,关键气候因子是平均最高温度和当前生长季的平均最高温度。在最北端的圣山自然保护区样地,关键气候因子是低温因子,如各季节最低温度、冬季平均最高温度、除前一生长季末和当前生长季外各季节的平均温度。当前生长季和当前生长季末的帕尔默干旱严重指数(PDSI)以及当前生长季的降水量是长白山自然保护区的关键气候因子。当前生长季的平均温度是凉水自然保护区的关键气候因子。在最近的四十年里,随着温度升高,两个径级的红松径向生长在最南端显著下降,在最北端显著增加,在中纬度地区没有显著变化。