Department of Geography, University of British Columbia, Vancouver, BC, V6T 1Z2, Canada.
Department of Forest and Conservation Sciences, University of British Columbia, Vancouver, BC, V6T 1Z4, Canada.
Glob Chang Biol. 2017 May;23(5):1926-1941. doi: 10.1111/gcb.13554. Epub 2016 Nov 30.
Novel forest decline is increasing due to global environmental change, yet the causal factors and their interactions remain poorly understood. Using tree ring analyses, we show how climate and multiple biotic factors caused the decline of whitebark pine (Pinus albicaulis) in 16 stands in the southern Canadian Rockies. In our study area, 72% of whitebark pines were dead and 18% had partially dead crowns. Tree mortality peaked in the 1970s; however, the annual basal area increment of disturbed trees began to decline significantly in the late 1940s. Growth decline persisted up to 30 years before trees died from mountain pine beetle (Dendroctonus ponderosae), Ips spp. bark beetles or non-native blister rust pathogen (Cronartium ribicola). Climate-growth relations varied over time and differed among the healthy and disturbed subpopulations of whitebark pine. Prior to the 1940s, cool temperatures limited the growth of all subpopulations. Growth of live, healthy trees became limited by drought during the cool phase (1947 -1976) of the Pacific Decadal Oscillation (PDO) and then reverted to positive correlations with temperature during the subsequent warm PDO phase. In the 1940s, the climate-growth relations of the disturbed subpopulations diverged from the live, healthy trees with trees ultimately killed by mountain pine beetle diverging the most. We propose that multiple factors interacted over several decades to cause unprecedented rates of whitebark pine mortality. Climatic variation during the cool PDO phase caused drought stress that may have predisposed trees to blister rust. Subsequent decline in snowpack and warming temperatures likely incited further climatic stress and with blister rust reduced tree resistance to bark beetles. Ultimately, bark beetles and blister rust contributed to tree death. Our findings suggest the complexity of whitebark pine decline and the importance of considering multiway drought-disease-insect interactions over various timescales when interpreting forest decline.
由于全球环境变化,新的森林衰退现象正在增加,但因果因素及其相互作用仍知之甚少。我们使用树木年轮分析方法,展示了气候和多种生物因素如何导致南落矶山脉 16 个白松(Pinus albicaulis)种群的衰退。在我们的研究区域,72%的白松已经死亡,18%的白松树冠部分死亡。树木死亡率在 20 世纪 70 年代达到峰值;然而,受干扰树木的年基面积增量在 20 世纪 40 年代末开始显著下降。在白松遭受山松甲虫(Dendroctonus ponderosae)、Ips 属树皮甲虫或非本地疱锈病菌(Cronartium ribicola)侵袭而死亡之前,生长衰退持续了长达 30 年。气候与生长的关系随时间而变化,并且在白松的健康和受干扰的亚种群之间也有所不同。在 20 世纪 40 年代之前,凉爽的温度限制了所有亚种群的生长。在太平洋十年涛动(PDO)的凉爽阶段(1947 年至 1976 年),活的健康树木的生长受到干旱的限制,随后在随后的温暖 PDO 阶段与温度呈正相关。在 20 世纪 40 年代,受干扰亚种群的气候与生长关系与健康的活树分道扬镳,而最终被山松甲虫杀死的树木则分道扬镳最多。我们提出,几十年以来,多种因素相互作用导致了白松前所未有的死亡率。凉爽的 PDO 阶段的气候变异性导致干旱胁迫,这可能使树木易患疱锈病。随后雪量减少和气温升高可能会引发进一步的气候压力,而疱锈病会降低树木对树皮甲虫的抵抗力。最终,树皮甲虫和疱锈病导致树木死亡。我们的研究结果表明,白松衰退的复杂性以及在解释森林衰退时考虑多方面干旱-疾病-昆虫相互作用在不同时间尺度上的重要性。