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豆科作物轮作抑制了甘蔗种植土壤中的硝化微生物群落。

Legume crop rotation suppressed nitrifying microbial community in a sugarcane cropping soil.

机构信息

School of Agriculture and Food Sciences, The University of Queensland, St Lucia, QLD 4072, Australia.

Sustainable Organic Solutions Pty Ltd, Indooroopilly, QLD 4068, Australia.

出版信息

Sci Rep. 2017 Dec 1;7(1):16707. doi: 10.1038/s41598-017-17080-z.

DOI:10.1038/s41598-017-17080-z
PMID:29196695
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5711877/
Abstract

Nitrifying microorganisms play an important role in nitrogen (N) cycling in agricultural soils as nitrification leads to accumulation of nitrate (NO) that is readily lost through leaching and denitrification, particularly in high rainfall regions. Legume crop rotation in sugarcane farming systems can suppress soil pathogens and improve soil health, but its effects on soil nitrifying microorganisms are not well understood. Using shotgun metagenomic sequencing, we investigated the impact of two legume break crops, peanut (Arachis hypogaea) and soybean (Glycine max), on the nitrifying communities in a sugarcane cropping soil. Cropping with either legume substantially increased abundances of soil bacteria and archaea and altered the microbial community composition, but did not significantly alter species richness and evenness relative to a bare fallow treatment. The ammonia oxidisers were mostly archaeal rather than bacterial, and were 24-44% less abundant in the legume cropping soils compared to the bare fallow. Furthermore, abundances of the archaeal amoA gene encoding ammonia monooxygenase in the soybean and peanut cropping soils were only 30-35% of that in the bare fallow. These results warrant further investigation into the mechanisms driving responses of ammonia oxidising communities and their nitrification capacity in soil during legume cropping.

摘要

硝化微生物在农业土壤的氮循环中起着重要作用,因为硝化作用导致硝酸盐(NO)的积累,而硝酸盐很容易通过淋溶和反硝化作用流失,特别是在高降雨地区。在甘蔗种植系统中,豆科作物轮作可以抑制土壤病原体并改善土壤健康,但人们对其对土壤硝化微生物的影响了解甚少。本研究采用高通量宏基因组测序技术,调查了两种豆科休耕作物(花生和大豆)对甘蔗种植土壤硝化微生物群落的影响。与休耕相比,种植任何一种豆科作物都显著增加了土壤细菌和古菌的丰度,并改变了微生物群落组成,但与休耕相比,物种丰富度和均匀度并没有显著改变。氨氧化菌主要是古菌而不是细菌,与休耕相比,豆科作物种植土壤中的氨氧化菌丰度降低了 24-44%。此外,大豆和花生种植土壤中编码氨单加氧酶的古菌 amoA 基因的丰度仅为休耕土壤的 30-35%。这些结果表明,需要进一步研究豆科作物种植期间氨氧化微生物及其硝化能力对土壤的响应机制。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/586f/5711877/e87304261858/41598_2017_17080_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/586f/5711877/77dc8fe93757/41598_2017_17080_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/586f/5711877/e87304261858/41598_2017_17080_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/586f/5711877/77dc8fe93757/41598_2017_17080_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/586f/5711877/e87304261858/41598_2017_17080_Fig2_HTML.jpg

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