Pacific Northwest Research Station, USDA Forest Service, 11175 Auke Lake Way, Juneau, Alaska, 99801, USA.
Department of Natural Resources & Environmental Science, University of Nevada, Reno, 1664 N. Virginia Ave, Reno, Nevada, 89557, USA.
Ecology. 2021 Dec;102(12):e03525. doi: 10.1002/ecy.3525. Epub 2021 Sep 23.
Climate change is shifting forest tree species distributions across elevational and latitudinal gradients, and these changes are often pronounced at ecotones where species meet their climatic bounds and are replaced by other species. Using an extensive ecotone composed of lower-montane white fir (Abies concolor var. lowiana) and upper-montane red fir (Abies magnifica var. magnifica) in the central Sierra Nevada range of California, USA, we (1) examined how the demographics of the ecotone have responded to recent climate using a field observational study and a historical dataset, (2) quantified climate drivers across species life stages using contemporary demographic data, and (3) tested the potential impacts of future climate on species-specific seedling survival and growth in a fully factorial growth chamber experiment that varied temperature, growing season length, and water availability. A re-examination of the ecotone midpoint after 35 yr suggested a reduction in A. concolor sapling and tree densities and a rise in A. magnifica proportional dominance between surveys. Seedling abundances across the ecotone indicated that A. magnifica tends to dominate the regeneration layer and currently forms an important component of the seedling community at elevations below those where A. magnifica saplings or trees begin to co-dominate stands. Observational and experimental assessments suggest that temperature and precipitation serve as important drivers, differentiating A. concolor vs. A. magnifica distributions, and are primary stressors at the seedling stage. Seedlings of both species were adversely affected by experimental climate treatments, although A. concolor exhibited greater survival and a more conservative growth strategy under extreme climatic stress than A. magnifica. Projections indicate that historical climate conditions will rise by an amount greater than the ecotone's current elevational extent by the end of the 21st century. Differential drivers of species abundances suggest that the projected climate will expand conditions that promote A. concolor abundance and impede A. magnifica abundance across the ecotone; however, disturbance activity and microclimatic conditions will also influence regeneration and overstory tree dynamics. Our study demonstrates the importance of quantifying species-specific responses to climate and indicates that widespread regeneration failure may be one possible consequence in which species exhibit strong sensitivity to projected climate conditions.
气候变化正在改变森林树种在海拔和纬度梯度上的分布,而这些变化在物种达到气候极限并被其他物种取代的生态交错带通常更为明显。本研究使用美国加利福尼亚州内华达山脉中下部山区的低海拔白冷杉(Abies concolor var. lowiana)和上部山区的红冷杉(Abies magnifica var. magnifica)组成的广泛生态交错带,(1)通过野外观测研究和历史数据集来研究生态交错带的种群动态对近期气候变化的响应情况,(2)使用当代种群数据量化物种各个生命阶段的气候驱动因素,(3)在一个完全因子生长室实验中测试未来气候对特定物种幼苗存活和生长的潜在影响,该实验在温度、生长季节长度和水分可用性方面进行了变化。35 年后对生态交错带中点的重新检查表明,A. concolor 幼树和树木的密度降低,A. magnifica 的比例优势增加。整个生态交错带的幼苗丰度表明,A. magnifica 倾向于主导更新层,并且目前在 A. magnifica 幼树或树木开始共同主宰林分的海拔以下,形成了幼苗群落的重要组成部分。观测和实验评估表明,温度和降水是重要的驱动因素,区分了 A. concolor 和 A. magnifica 的分布,并且是幼苗阶段的主要胁迫因素。两种树种的幼苗都受到实验气候处理的不利影响,尽管 A. concolor 在极端气候胁迫下的存活和更保守的生长策略优于 A. magnifica。预测表明,到 21 世纪末,历史气候条件的上升幅度将超过生态交错带目前的海拔范围。物种丰度的不同驱动因素表明,预计的气候将扩大促进 A. concolor 丰度的条件,并阻碍生态交错带中 A. magnifica 丰度的条件;然而,干扰活动和小气候条件也将影响更新和林冠树木动态。我们的研究表明量化物种对气候的特定响应的重要性,并表明广泛的再生失败可能是物种对预计气候条件表现出强烈敏感性的一个可能后果。