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与传统的生态强化管理相比,生态强化管理促进了有益于土壤蛋白质水解的微生物群落,从而增强了农业生态系统在气候变化引起的降雨模式下的功能。

Compared to conventional, ecological intensive management promotes beneficial proteolytic soil microbial communities for agro-ecosystem functioning under climate change-induced rain regimes.

机构信息

Department of Soil Sciences, Research Institute of Organic Agriculture (FiBL), Ackerstrasse 113, 5070, Frick, Switzerland.

Organic Farming with focus on Sustainable Soil Use, Karl-Glöckner-Str. 21 C, Justus-Liebig University Giessen, 35394, Giessen, Germany.

出版信息

Sci Rep. 2020 Apr 29;10(1):7296. doi: 10.1038/s41598-020-64279-8.

DOI:10.1038/s41598-020-64279-8
PMID:32350402
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7190635/
Abstract

Projected climate change and rainfall variability will affect soil microbial communities, biogeochemical cycling and agriculture. Nitrogen (N) is the most limiting nutrient in agroecosystems and its cycling and availability is highly dependent on microbial driven processes. In agroecosystems, hydrolysis of organic nitrogen (N) is an important step in controlling soil N availability. We analyzed the effect of management (ecological intensive vs. conventional intensive) on N-cycling processes and involved microbial communities under climate change-induced rain regimes. Terrestrial model ecosystems originating from agroecosystems across Europe were subjected to four different rain regimes for 263 days. Using structural equation modelling we identified direct impacts of rain regimes on N-cycling processes, whereas N-related microbial communities were more resistant. In addition to rain regimes, management indirectly affected N-cycling processes via modifications of N-related microbial community composition. Ecological intensive management promoted a beneficial N-related microbial community composition involved in N-cycling processes under climate change-induced rain regimes. Exploratory analyses identified phosphorus-associated litter properties as possible drivers for the observed management effects on N-related microbial community composition. This work provides novel insights into mechanisms controlling agro-ecosystem functioning under climate change.

摘要

预计气候变化和降雨变化将影响土壤微生物群落、生物地球化学循环和农业。氮 (N) 是农业生态系统中最受限制的养分,其循环和可用性高度依赖于微生物驱动的过程。在农业生态系统中,有机氮 (N) 的水解是控制土壤 N 有效性的重要步骤。我们分析了管理(生态集约化与传统集约化)对气候变化诱导的降雨模式下 N 循环过程和相关微生物群落的影响。源自欧洲农业生态系统的陆地模型生态系统在 263 天内经历了四种不同的降雨模式。使用结构方程模型,我们确定了降雨模式对 N 循环过程的直接影响,而与 N 相关的微生物群落则更具抵抗力。除了降雨模式外,管理还通过改变与 N 相关的微生物群落组成间接影响 N 循环过程。生态集约化管理促进了与气候变化诱导的降雨模式下 N 循环过程相关的有益的 N 相关微生物群落组成。探索性分析确定了与磷相关的凋落物特性可能是管理对与 N 相关的微生物群落组成的影响的驱动因素。这项工作为控制气候变化下农业生态系统功能的机制提供了新的见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6a45/7190635/f36838786033/41598_2020_64279_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6a45/7190635/e8d6f22bda8c/41598_2020_64279_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6a45/7190635/ef4a7ebb9d88/41598_2020_64279_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6a45/7190635/f36838786033/41598_2020_64279_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6a45/7190635/e8d6f22bda8c/41598_2020_64279_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6a45/7190635/ef4a7ebb9d88/41598_2020_64279_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6a45/7190635/f36838786033/41598_2020_64279_Fig3_HTML.jpg

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