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Climate change drives a shift in peatland ecosystem plant community: Implications for ecosystem function and stability

机译:气候变化推动泥炭地生态系统植物群落的转变:对生态系统功能和稳定性的影响

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The composition of a peatland plant community has considerable effect on a range of ecosystem functions. Peatland plant community structure is predicted to change under future climate change, making the quantification of the direction and magnitude of this change a research priority. We subjected intact, replicated vegetated poor fen peat monoliths to elevated temperatures, increased atmospheric carbon dioxide (CO2), and two water table levels in a factorial design to determine the individual and synergistic effects of climate change factors on the poor fen plant community composition. We identify three indicators of a regime shift occurring in our experimental poor fen system under climate change: nonlinear decline of Sphagnum at temperatures 8 degrees C above ambient conditions, concomitant increases in Carex spp. at temperatures 4 degrees C above ambient conditions suggesting a weakening of Sphagnum feedbacks on peat accumulation, and increased variance of the plant community composition and pore water pH through time. A temperature increase of +4 degrees C appeared to be a threshold for increased vascular plant abundance; however the magnitude of change was species dependent. Elevated temperature combined with elevated CO2 had a synergistic effect on large graminoid species abundance, with a 15 times increase as compared to control conditions. Community analyses suggested that the balance between dominant plant species was tipped from Sphagnum to a graminoid-dominated system by the combination of climate change factors. Our findings indicate that changes in peatland plant community composition are likely under future climate change conditions, with a demonstrated shift toward a dominance of graminoid species in poor fens.
机译:泥炭地植物群落的组成对一系列生态系统功能具有相当大的影响。泥炭地植物群落结构预计将在未来的气候变化下发生变化,因此将这种变化的方向和幅度的量化作为研究重点。我们对完整的,复制的植被贫芬泥炭整料进行了高温处理,增加了大气中的二氧化碳(CO2)以及两个水位,通过析因设计确定了气候变化因素对贫芬植物群落组成的个体和协同作用。我们确定了在气候变化下我们的实验性芬系统中发生的政权转移的三个指标:在高于环境温度8摄氏度的温度下,水藓的非线性下降,随之而来的Carex spp的增加。在高于环境温度4摄氏度的温度下,表明泥炭对泥炭积累的反馈减弱,并且随着时间的推移植物群落组成和孔隙水pH的变化增加。温度升高+4摄氏度似乎是增加维管束植物丰度的一个阈值。但是变化的幅度取决于物种。升高的温度与升高的CO2结合在一起对大型类禾动物物种的丰度具有协同作用,与对照条件相比增加了15倍。社区分析表明,通过气候变化因素的结合,优势植物物种之间的平衡从泥炭藓转变为以类粉体为主的系统。我们的发现表明,在未来的气候变化条件下,泥炭地植物群落的组成可能会发生变化,在贫瘠的环境中,已证明其向着类粒动物的优势地位转移。

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