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土壤增温和 CO2 富集导致高山树线植被生物量的变化。

Soil warming and CO2 enrichment induce biomass shifts in alpine tree line vegetation.

机构信息

WSL Institute for Snow and Avalanche Research - SLF, Flüelastrasse 11, CH-7260, Davos Dorf, Switzerland; Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, CH-8903, Birmensdorf, Switzerland.

出版信息

Glob Chang Biol. 2015 May;21(5):2005-21. doi: 10.1111/gcb.12819. Epub 2015 Jan 30.

Abstract

Responses of alpine tree line ecosystems to increasing atmospheric CO2 concentrations and global warming are poorly understood. We used an experiment at the Swiss tree line to investigate changes in vegetation biomass after 9 years of free air CO2 enrichment (+200 ppm; 2001-2009) and 6 years of soil warming (+4 °C; 2007-2012). The study contained two key tree line species, Larix decidua and Pinus uncinata, both approximately 40 years old, growing in heath vegetation dominated by dwarf shrubs. In 2012, we harvested and measured biomass of all trees (including root systems), above-ground understorey vegetation and fine roots. Overall, soil warming had clearer effects on plant biomass than CO2 enrichment, and there were no interactive effects between treatments. Total plant biomass increased in warmed plots containing Pinus but not in those with Larix. This response was driven by changes in tree mass (+50%), which contributed an average of 84% (5.7 kg m(-2) ) of total plant mass. Pinus coarse root mass was especially enhanced by warming (+100%), yielding an increased root mass fraction. Elevated CO2 led to an increased relative growth rate of Larix stem basal area but no change in the final biomass of either tree species. Total understorey above-ground mass was not altered by soil warming or elevated CO2 . However, Vaccinium myrtillus mass increased with both treatments, graminoid mass declined with warming, and forb and nonvascular plant (moss and lichen) mass decreased with both treatments. Fine roots showed a substantial reduction under soil warming (-40% for all roots <2 mm in diameter at 0-20 cm soil depth) but no change with CO2 enrichment. Our findings suggest that enhanced overall productivity and shifts in biomass allocation will occur at the tree line, particularly with global warming. However, individual species and functional groups will respond differently to these environmental changes, with consequences for ecosystem structure and functioning.

摘要

高山树线生态系统对大气 CO2 浓度增加和全球变暖的响应还知之甚少。我们利用瑞士树线的一项实验,研究了在自由空气 CO2 富集(+200ppm;2001-2009 年)和土壤增温(+4°C;2007-2012 年)9 年后植被生物量的变化。该研究包含两种关键的树线物种,即落叶松和欧洲赤松,它们都大约有 40 年的树龄,生长在以矮灌木为主的石南植被中。2012 年,我们收获并测量了所有树木(包括根系)、地上林下植被和细根的生物量。总体而言,土壤增温对植物生物量的影响比 CO2 富集更为明显,而且处理之间没有相互作用。在含有欧洲赤松的增温样地中,总植物生物量增加,但在含有落叶松的样地中没有增加。这种响应是由树木质量的变化驱动的(增加了 50%),平均贡献了总植物质量的 84%(5.7kgm-2)。欧洲赤松粗根质量尤其受到增温的影响(增加了 100%),导致根质量分数增加。高 CO2 导致落叶松树干基部面积的相对生长率增加,但两种树种的最终生物量都没有变化。土壤增温和高 CO2 都没有改变林下地上总生物量。然而,Vaccinium myrtillus 的生物量随着两种处理的增加而增加,禾本科植物的生物量随着增温而减少,而草本植物和非维管束植物(苔藓和地衣)的生物量随着两种处理而减少。细根在土壤增温下显著减少(所有直径<2mm的细根在 0-20cm 土壤深度下减少了 40%),而 CO2 富集则没有变化。我们的研究结果表明,在树线地区,特别是随着全球变暖,整体生产力的提高和生物量分配的变化将会发生。然而,个别物种和功能群将对这些环境变化做出不同的响应,从而对生态系统结构和功能产生影响。

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