Swiss Federal Research Institute WSL, Birmensdorf, Switzerland.
Key Laboratory of Geographical Processes and Ecological Security of Changbai Mountains, Ministry of Education, Northeast Normal University, Changchun, China.
Glob Chang Biol. 2021 Jun;27(11):2491-2506. doi: 10.1111/gcb.15557. Epub 2021 Mar 19.
Above and belowground compartments in ecosystems are closely coupled on daily to annual timescales. In mature forests, this interlinkage and how it is impacted by drought is still poorly understood. Here, we pulse-labelled 100-year-old trees with CO within a 15-year-long irrigation experiment in a naturally dry pine forest to quantify how drought regime affects the transfer and use of assimilates from trees to the rhizosphere and associated microbial communities. It took 4 days until new C-labelled assimilates were allocated to the rhizosphere. One year later, the C signal of the 3-h long pulse labelling was still detectable in stem and soil respiration, which provides evidence that parts of the assimilates are stored in trees before they are used for metabolic processes in the rhizosphere. Irrigation removing the natural water stress reduced the mean C residence time from canopy uptake until soil respiration from 89 to 40 days. Moreover, irrigation increased the amount of assimilates transferred to and respired in the soil within the first 10 days by 370%. A small precipitation event rewetting surface soils altered this pattern rapidly and reduced the effect size to +35%. Microbial biomass incorporated 46 ± 5% and 31 ± 7% of the C used in the rhizosphere in the dry control and irrigation treatment respectively. Mapping the spatial distribution of soil-respired CO around the 10 pulse-labelled trees showed that tree rhizospheres extended laterally 2.8 times beyond tree canopies, implying that there is a strong overlap of the rhizosphere among adjacent trees. Irrigation increased the rhizosphere area by 60%, which gives evidence of a long-term acclimation of trees and their rhizosphere to the drought regime. The moisture-sensitive transfer and use of C in the rhizosphere has consequences for C allocation within trees, soil microbial communities and soil carbon storage.
生态系统的地上和地下部分在每日到年度的时间尺度上紧密相连。在成熟的森林中,这种相互联系以及干旱对其的影响仍知之甚少。在这里,我们在一个自然干燥的松林里进行了长达 15 年的灌溉实验,对 100 岁的树木进行了 CO 脉冲标记,以量化干旱制度如何影响同化产物从树木转移到根际和相关微生物群落的过程以及如何影响其转移和利用。直到第 4 天,新的 C 标记同化产物才被分配到根际。一年后,3 小时长的脉冲标记的 C 信号仍能在茎和土壤呼吸中检测到,这表明部分同化产物在被用于根际的代谢过程之前被储存在树木中。灌溉去除了自然水分胁迫,将从树冠吸收到土壤呼吸的平均 C 停留时间从 89 天减少到 40 天。此外,灌溉增加了前 10 天转移到土壤中并在土壤中呼吸的同化产物的量,增加了 370%。一场小的降水事件重新润湿了表层土壤,迅速改变了这一模式,并将效应大小降低到+35%。微生物生物量分别将根际中使用的 C 的 46±5%和 31±7%固定下来。在干旱对照和灌溉处理中。在围绕着 10 棵脉冲标记树的土壤呼吸 CO 的空间分布图显示,树木的根际在树冠之外向侧面延伸了 2.8 倍,这意味着相邻树木的根际有很强的重叠。灌溉增加了 60%的根际面积,这表明树木及其根际对干旱制度有长期的适应。根际中水分敏感的 C 转移和利用对树木内部的 C 分配、土壤微生物群落和土壤碳储存有影响。