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十年的灌溉改变了半干旱松树林的土壤微生物群落。

A decade of irrigation transforms the soil microbiome of a semi-arid pine forest.

作者信息

Hartmann Martin, Brunner Ivano, Hagedorn Frank, Bardgett Richard D, Stierli Beat, Herzog Claude, Chen Xiamei, Zingg Andreas, Graf-Pannatier Elisabeth, Rigling Andreas, Frey Beat

机构信息

Swiss Federal Research Institute WSL, 8903, Birmensdorf, Switzerland.

School of Earth and Environmental Sciences, Michael Smith Building, The University of Manchester, M13 9PT, Manchester, UK.

出版信息

Mol Ecol. 2017 Feb;26(4):1190-1206. doi: 10.1111/mec.13995. Epub 2017 Jan 21.

DOI:10.1111/mec.13995
PMID:28028891
Abstract

The impact of climate change on the soil microbiome potentially alters the biogeochemical cycle of terrestrial ecosystems. In semi-arid environments, water availability is a major constraint on biogeochemical cycles due to the combination of high summer temperatures and low rainfall. Here, we explored how 10 years of irrigation of a water-limited pine forest in the central European Alps altered the soil microbiome and associated ecosystem functioning. A decade of irrigation stimulated tree growth, resulting in higher crown cover, larger yearly increments of tree biomass, increased litter fall and greater root biomass. Greater amounts of plant-derived inputs associated with increased primary production in the irrigated forest stands stimulated soil microbial activity coupled with pronounced shifts in the microbiome from largely oligotrophic to more copiotrophic lifestyles. Microbial groups benefitting from increased resource availabilities (litter, rhizodeposits) thrived under irrigation, leading to enhanced soil organic matter mineralization and carbon respired from irrigated soils. This unique long-term study provides new insights into the impact of precipitation changes on the soil microbiome and associated ecosystem functioning in a water-limited pine forest ecosystem and improves our understanding of the persistency of long-term soil carbon stocks in a changing climate.

摘要

气候变化对土壤微生物群落的影响可能会改变陆地生态系统的生物地球化学循环。在半干旱环境中,由于夏季高温和低降雨的共同作用,水资源的可利用性是生物地球化学循环的主要限制因素。在此,我们探究了中欧阿尔卑斯山地区对一个水资源有限的松林进行十年灌溉是如何改变土壤微生物群落以及相关的生态系统功能的。十年的灌溉促进了树木生长,导致树冠覆盖率更高、树木生物量的年增量更大、凋落物增加以及根系生物量更大。与灌溉林分中初级生产增加相关的更多植物源输入刺激了土壤微生物活动,同时微生物群落从主要的贫营养型向更富营养型的生活方式发生了显著转变。受益于资源可用性增加(凋落物、根际沉积物)的微生物类群在灌溉条件下茁壮成长,导致土壤有机质矿化增强以及灌溉土壤中碳的呼吸作用增强。这项独特的长期研究为降水变化对水资源有限的松林生态系统中土壤微生物群落及相关生态系统功能的影响提供了新的见解,并增进了我们对气候变化下长期土壤碳储量持续性的理解。

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