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十年的土地利用导致塞拉多土壤的化学、生物化学和细菌群落结构发生变化。

A decade of land use contributes to changes in the chemistry, biochemistry and bacterial community structures of soils in the Cerrado.

机构信息

LEMM-Laboratório de Ecologia Microbiana Molecular, Instituto de Microbiologia Professor Paulo de Góes, Universidade Federal do Rio de Janeiro, Rio de Janeiro, Brazil.

出版信息

Antonie Van Leeuwenhoek. 2010 Oct;98(3):403-13. doi: 10.1007/s10482-010-9454-0. Epub 2010 May 21.

Abstract

The bacterial community structures (BCSs) of Cerrado soils cultivated under conventional tillage (CT), no-tillage (NT) and under native Cerrado (NC) vegetation were evaluated using PCR/DGGE of bacterial 16S rRNA (rrs) and rpoB genes and of Pseudomonas group genes. Soil chemical analysis, microbial biomass and the enzyme activities were also evaluated and correlated with the BCS measurements. The multivariate ordinations of DGGE profiles showed differences between the BCS of the NC area and those from cultivated areas. The BCSs of the CT and NT areas also differed in all DGGE fingerprints, including changes in the profile of Pseudomonas populations, indicating that agricultural systems can also be responsible for changes within specific microbial niches, although the clearest differences were found in the rpoB profiles. The MRPP analysis demonstrated significant differences between the BCSs from different soil layers of NT areas based on all gene fingerprints and those of NC areas based on bacterial 16S rRNA and rpoB genes fingerprints. No differences were observed in the microbial fingerprints of CT samples from different depths, indicating that ploughing affected the original BCS stratification. The BCS from NC areas, based on all gene fingerprints, could be related to higher levels of soil acidity and higher amounts of MBC and of phosphatase activity. In contrast, the BCSs from cultivated areas were related to higher levels of Ca + Mg, P and K, likely as a result of a history of chemical fertilisation in these areas. The relationships between rpoB and Pseudomonas BCSs and all chemical and biochemical properties of soils were significant, according to a Mantel test (P < 0.05), indicating that the different changes in soil properties induced by soil use or management may drive the formation of the soil BCS.

摘要

采用 PCR/DGGE 技术对常规耕作(CT)、免耕(NT)和原生塞拉多(NC)植被下种植的塞拉多土壤的细菌群落结构(BCS)进行了评估,分析了细菌 16S rRNA(rrs)和 rpoB 基因以及假单胞菌属基因。还评估了土壤化学分析、微生物生物量和酶活性,并将其与 BCS 测量结果相关联。DGGE 图谱的多元排序显示,NC 区与耕作区的 BCS 存在差异。CT 和 NT 区的 BCS 在所有 DGGE 指纹图谱中也存在差异,包括假单胞菌种群的图谱变化,表明农业系统也可能导致特定微生物小生境发生变化,尽管在 rpoB 图谱中发现的差异最明显。MRPP 分析表明,基于所有基因指纹图谱,NT 区不同土层的 BCS 与 NC 区的 BCS 存在显著差异,而基于细菌 16S rRNA 和 rpoB 基因指纹图谱,NT 区的 BCS 与 NC 区的 BCS 存在显著差异。CT 样本不同深度的微生物指纹图谱没有差异,表明耕作影响了原始 BCS 的分层。基于所有基因指纹图谱,NC 区的 BCS 可能与较高的土壤酸度、较高的 MBC 和较高的磷酸酶活性有关。相比之下,耕作区的 BCS 与较高的 Ca+Mg、P 和 K 水平有关,这可能是由于这些地区的历史化学施肥。Mantel 检验(P<0.05)表明,rpoB 和假单胞菌 BCS 与土壤所有化学和生物化学性质之间存在显著关系,这表明土壤利用或管理引起的土壤性质的不同变化可能会驱动土壤 BCS 的形成。

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