Department of Biology, University of Washington, PO Box 351800, Seattle, Washington, 98195, USA.
Ecol Lett. 2020 Jan;23(1):140-148. doi: 10.1111/ele.13416. Epub 2019 Oct 30.
Ecologists expect species and biomes to shift poleward and upward with climate change, but non-climatic factors complicate these predictions. In mountains, forests are expected to expand upward along climate gradients into subalpine/alpine meadows, while meadows expand upward onto bare ground. However, soils also vary across elevation, with bare soil above the meadows potentially poorer for plant establishment. Poor soil might constrain expansion at meadows' upper edges, while rich meadow soil might facilitate contraction at lower edges by promoting tree establishment. We assessed climate and soil effects on establishment by transplanting soil and seedlings of meadow and tree species across climate gradients on Mount Rainier. There were considerable interspecific differences, but some generalisations emerged. Survival often declined with earlier snow disappearance, with somewhat smaller declines in meadow soil. Size often increased with earlier snow disappearance, with larger increases in meadow soil. Thus, soil patterns may complicate range shifts.
生态学家预计,随着气候变化,物种和生物群落将向两极和高海拔地区转移,但非气候因素使这些预测变得复杂。在山区,森林预计将沿着气候梯度向上扩展到亚高山/高山草甸,而草甸则向上扩展到裸露的地面。然而,土壤也随海拔而变化,草甸上方的裸露土壤可能不利于植物的建立。贫瘠的土壤可能会限制草甸上部边缘的扩张,而肥沃的草甸土壤可能会通过促进树木的建立而促进下部边缘的收缩。我们通过在雷尼尔山的气候梯度上移栽草甸和树木物种的土壤和幼苗来评估气候和土壤对建立的影响。存在着相当大的种间差异,但也出现了一些概括。存活率通常随着雪的提前消失而下降,而在草甸土壤中下降幅度较小。大小通常随着雪的提前消失而增加,在草甸土壤中增加幅度较大。因此,土壤模式可能会使分布范围的变化变得复杂。