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Slow Recovery of Mire Vegetation from Environmental Perturbations Caused by a Heat Wave and Experimental Fertilization

机译:从热浪和实验施肥引起的环境扰动中缓慢恢复泥潭植被

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摘要

We monitored vegetation changes in an alpine mire after stopping an experiment of nutrient addition, during which the mire experienced a heat wave. We aimed at assessing the capacity of mire vegetation to recover towards the original state. Nitrogen and phosphorus were added during the growing seasons of 2002-2009. We recorded periodically the cover of all vascular plant species and moss species from 2002 to 2012, i.e., 9 years after the heat wave and 3 years after discontinuing fertilization. The principal effect of the 2003 heat wave consisted in a rapid increase in cover of vascular plants and a parallel decrease in cover of mosses. These trends slowed down after 6 years and almost totally halted 9 years after the heat wave. The heat wave was the main driver of vegetation changes but the vegetation also responded to fertilization. Species within plant functional types (PFTs) showed differing responses to the heat wave and/or fertilization. The mire vegetation showed poor capacity to recover towards the initial conditions. Changes in vegetation composition were determined by individualistic responses of species to varying ecological factors. Grouping plant species into PFTs may conceal important differences in the responses of mire vegetation to environmental changes.
机译:在停止营养添加实验之后,我们监测了高山沼泽中的植被变化,在此期间沼泽经历了热浪。我们旨在评估泥潭植被恢复到原始状态的能力。在2002-2009年的生长季节中添加了氮和磷。我们定期记录2002年至2012年期间所有维管植物物种和苔藓物种的覆盖率,即热浪后9年和停止施肥后3年。 2003年热浪的主要影响是维管植物的覆盖率迅速增加,而苔藓的覆盖率平行下降。这些趋势在6年后放慢,在热浪9年后几乎完全停止。热浪是植被变化的主要驱动力,但植被对施肥也有响应。植物功能类型(PFT)中的物种对热波和/或施肥的反应不同。泥泞的植被显示出恢复初始状态的能力差。植被组成的变化取决于物种对各种生态因素的个体反应。将植物物种分组为PFTs可能掩盖了泥泞植被对环境变化的响应方面的重要差异。

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