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Long term impact of mineral amendment on the distribution of the mineral weathering associated bacterial communities from the beech Scleroderma citrinum ectomycorrhizosphere

机译:矿物改良剂对山毛榉柠檬皮硬皮外生根际土壤矿物风化相关细菌群落分布的长期影响

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Liming is a known forest management procedure used to amend nutrient-poor soils such as soils of acidic forests to rectify cation deficiencies and to restore soil pH. However, although this procedure is well known for its beneficial effect on the forest trees, its relative impact on the functional and taxonomic diversity of the soil bacterial communities has been poorly investigated. In this study, we characterized the ability of the soil bacteria to weather soil minerals and to hydrolyze chitin. A collection of 80 bacterial strains was isolated from the Scleroderma citrinum ectomycorrhizosphere and the adjacent bulk soil in two stands of mature beeches (Fagus sylvatica) developed on very acidic soil and presenting two levels of calcium (Ca) availability: a control plot as well as a plot amended with Ca in 1973. All the bacterial isolates were identified by partial 16S rRNA gene sequence analysis as members of the genera Burkholderia, Bacillus, Dyella, Kitasatospora, Micrococcus, Paenibacillus, Pseudomonas, and Rhodanobacter. Using a microplate assay for quantifying the production of protons and the quantity of iron released from biotite, we demonstrated that the bacterial strains from the amended plot harbored a significant higher mineral weathering potential that the ones isolated from the control plot. Notably, the weathering efficacy of the ectomycorrhizosphere bacterial isolates was significantly greater than that of the bulk soil isolates in the control treatment but not in the amended plot. These data reveal that forest management, here mineral amendment, can strongly affect the structure of bacterial communities even over the long term
机译:石灰化是已知的森林管理程序,用于修正营养不足的土壤(例如酸性森林的土壤),以纠正阳离子缺陷并恢复土壤的pH值。但是,尽管此方法因其对林木的有益作用而广为人知,但对其对土壤细菌群落功能和分类多样性的相对影响尚未进行充分研究。在这项研究中,我们表征了土壤细菌抵御土壤矿物质和水解几丁质的能力。从柠檬皮硬皮病菌根外圈和相邻大块土壤中分离出80个细菌菌株,该两个土壤在酸性很强的土壤中发育并表现出两个水平的钙(Ca)利用率的成熟山毛榉(Fagus sylvatica)林分中。 1973年由Ca修改的一个地块。通过部分16S rRNA基因序列分析,所有细菌分离株都被鉴定为Burkholderia,芽孢杆菌,Dyella,Kitasatospora,Micrococcus,Paenibacillus,Pseudomonas和Rhodanobacter属。使用微孔板分析定量质子的产生和从黑云母中释放的铁的量,我们证明了从修正地块获得的细菌菌株比从对照地块分离出的细菌具有更高的矿物风化潜力。值得注意的是,在对照处理中,外生菌根细菌分离株的风化功效明显大于散装土壤分离菌的风化功效,但在修改后的田地中则没有。这些数据表明,森林管理(这里是矿物改良剂)即使在长期内也可以强烈影响细菌群落的结构。

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