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首页> 外文期刊>Global change biology >Soil warming and CO2 enrichment induce biomass shifts in alpine tree line vegetation
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Soil warming and CO2 enrichment induce biomass shifts in alpine tree line vegetation

机译:土壤变暖和CO2富集引起高寒乔木植被的生物量转移

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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 9years of free air CO2 enrichment (+200ppm; 2001-2009) and 6years of soil warming (+4 degrees C; 2007-2012). The study contained two key tree line species, Larix decidua and Pinus uncinata, both approximately 40years 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% (5.7kgm(-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 2mm in diameter at 0-20cm 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.
机译:人们对高山林木生态系统对大气中二氧化碳浓度增加和全球变暖的反应知之甚少。我们在瑞士的一棵树上进行了一项实验,调查了9年的自由空气CO2富集(+ 200ppm; 2001-2009年)和6年的土壤变暖(+4摄氏度; 2007-2012年)后植被生物量的变化。该研究包含了两个重要的树系物种,落叶松和落叶松,都大约有40年的历史,生长在矮灌木为主的健康植被中。 2012年,我们收获并测量了所有树木(包括根系),地上地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二氧化碳富集更为明显,并且处理之间没有相互作用。在含有松属植物的温暖地块中,植物总生物量增加,而在落叶松中则没有。该响应是由树木质量的变化(+ 50%)驱动的,该变化平均贡献了植物总质量的84%(5.7kgm(-2))。通过加热(+ 100%),松树的粗根质量尤其增加,从而增加了根质量分数。 CO2升高导致落叶松茎基部面积的相对生长速率增加,但两种树种的最终生物量均没有变化。土壤变暖或CO2升高不会改变地下总的地下质量。但是,两种处理都增加了牛痘苗的质量,随着升温,粒状体的质量下降了,两种处理的前菜和非维管植物(苔藓和地衣)的质量都降低了。细根在土壤变暖下表现出明显的减少(在土壤深度为0-20cm时,直径小于2mm的所有根为-40%),但随着CO2浓度的增加而没有变化。我们的研究结果表明,特别是在全球变暖的情况下,将提高总体生产力并改变生物量分配的格局。但是,单个物种和功能组对这些环境变化的反应不同,对生态系统的结构和功能产生影响。

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