Zhang Jingli, Zhou Yong, Zhou Guangsheng, Xiao Chunwang
State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, the Chinese Academy of Sciences, Beijing, China ; University of Chinese Academy of Sciences, Beijing, China.
PLoS One. 2013 Jun 18;8(6):e66668. doi: 10.1371/journal.pone.0066668. Print 2013.
Many theoretical researches predicted that the larch species would decrease drastically in China under future climatic changes. However, responses of the structural and compositional changes of Gmelin larch (Larix gmelinii var. gmelinii) forests to climatic changes have rarely been reported.
METHODOLOGY/PRINCIPAL FINDINGS: Field survey was conducted to examine the structures and compositions of natural Gmelin larch forests along a climatic gradient. Stepwise linear regression analyses incorporating linear and quadratic components of climatic and non-climatic factors were performed on the structural and compositional attributes of those natural Gmelin larch forests. Isothermality, Max Temperature of Warmest Month (TempWarmestMonth), Precipitation of Wettest Month (PrecipWettestMonth), Precipitation Seasonality (PrecipSeasonality) and Precipitation of Driest Quarter (PrecipDriestQuarter) were observed to be effective climatic factors in controlling structure and composition of Gmelin larch forests. Isothermality significantly affected total basal area of larch, while TempWarmestMonth, PrecipWettestMonth and PrecipSeasonality significantly affected total basal area of Mongolian pine, and PrecipDriestQuarter significantly affected mean DBH of larch, stand density of larch and total basal area of spruce and fir.
CONCLUSIONS/SIGNIFICANCE: The summer and winter temperatures and precipitations are all predicted to increase in future in Northeast China. Our results showed the increase of total basal area of spruce and fir, the suppression of regeneration and the decrease of stand density of larch under increased winter precipitation, and the decrease of total basal area of larch under increased summer temperature in the region of current Gmelin larch forest. Therefore, we suggest that larch would decrease and spruce and fir would increase in the region of future Gmelin larch forest.
许多理论研究预测,在未来气候变化的情况下,中国的落叶松物种数量将急剧减少。然而,很少有报道提及兴安落叶松林(Larix gmelinii var. gmelinii)的结构和组成变化对气候变化的响应。
方法/主要发现:通过实地调查研究了沿气候梯度的天然兴安落叶松林的结构和组成。对这些天然兴安落叶松林的结构和组成属性进行了逐步线性回归分析,分析纳入了气候和非气候因素的线性和二次成分。等温性、最暖月最高温度(TempWarmestMonth)、最湿月降水量(PrecipWettestMonth)、降水季节性(PrecipSeasonality)和最干季度降水量(PrecipDriestQuarter)被认为是控制兴安落叶松林结构和组成的有效气候因素。等温性显著影响落叶松的总断面积,而最暖月最高温度、最湿月降水量和降水季节性显著影响樟子松的总断面积,最干季度降水量显著影响落叶松的平均胸径、落叶松的林分密度以及云杉和冷杉的总断面积。
结论/意义:预计中国东北地区未来夏季和冬季的气温和降水量都会增加。我们的研究结果表明,在当前兴安落叶松林地区,冬季降水量增加会导致云杉和冷杉的总断面积增加、更新受到抑制以及落叶松林分密度降低,夏季温度升高会导致落叶松的总断面积减少。因此,我们认为在未来兴安落叶松林地区,落叶松数量将减少,而云杉和冷杉数量将增加。