1] Plant-Soil Interactions, Agroscope Reckenholz-Tänikon Research Station ART, Zürich, Switzerland [2] Institute of Evolutionary Biology and Environmental Studies, University of Zürich, Zürich, Switzerland.
Plant-Microbe Interactions, Institute of Environmental Biology, Faculty of Science, Utrecht University, Utrecht, The Netherlands.
ISME J. 2014 Jun;8(6):1336-45. doi: 10.1038/ismej.2013.224. Epub 2013 Dec 19.
N2O is a potent greenhouse gas involved in the destruction of the protective ozone layer in the stratosphere and contributing to global warming. The ecological processes regulating its emissions from soil are still poorly understood. Here, we show that the presence of arbuscular mycorrhizal fungi (AMF), a dominant group of soil fungi, which form symbiotic associations with the majority of land plants and which influence a range of important ecosystem functions, can induce a reduction in N2O emissions from soil. To test for a functional relationship between AMF and N2O emissions, we manipulated the abundance of AMF in two independent greenhouse experiments using two different approaches (sterilized and re-inoculated soil and non-mycorrhizal tomato mutants) and two different soils. N2O emissions were increased by 42 and 33% in microcosms with reduced AMF abundance compared to microcosms with a well-established AMF community, suggesting that AMF regulate N2O emissions. This could partly be explained by increased N immobilization into microbial or plant biomass, reduced concentrations of mineral soil N as a substrate for N2O emission and altered water relations. Moreover, the abundance of key genes responsible for N2O production (nirK) was negatively and for N2O consumption (nosZ) positively correlated to AMF abundance, indicating that the regulation of N2O emissions is transmitted by AMF-induced changes in the soil microbial community. Our results suggest that the disruption of the AMF symbiosis through intensification of agricultural practices may further contribute to increased N2O emissions.
一氧化二氮是一种强效温室气体,它会破坏平流层中的保护臭氧层,并导致全球变暖。目前,我们对调节其从土壤中排放的生态过程仍知之甚少。在这里,我们表明,丛枝菌根真菌(AMF)的存在会导致土壤中一氧化二氮排放量减少,AMF 是土壤真菌中的主要群体,与大多数陆生植物形成共生关系,并影响一系列重要的生态系统功能。为了检验 AMF 和一氧化二氮排放之间是否存在功能关系,我们采用两种不同的方法(灭菌和再接种土壤以及非菌根番茄突变体)和两种不同的土壤,在两个独立的温室实验中操纵 AMF 的丰度。与具有成熟 AMF 群落的微宇宙相比,减少 AMF 丰度的微宇宙中一氧化二氮排放量增加了 42%和 33%,这表明 AMF 调节了一氧化二氮排放。这部分可以通过增加微生物或植物生物量中的氮固定、减少矿物土壤氮作为一氧化二氮排放的底物浓度以及改变水分关系来解释。此外,负责一氧化二氮产生(nirK)的关键基因的丰度与 AMF 丰度呈负相关,而负责一氧化二氮消耗(nosZ)的关键基因的丰度与 AMF 丰度呈正相关,这表明 AMF 通过诱导土壤微生物群落的变化来调节一氧化二氮排放。我们的研究结果表明,通过农业实践的强化破坏丛枝菌根共生关系可能会进一步导致一氧化二氮排放量的增加。