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利用基因探针辅助从土壤中回收和鉴定功能上占主导地位的2,4-二氯苯氧乙酸降解菌群。

Use of gene probes to aid in recovery and identification of functionally dominant 2,4-dichlorophenoxyacetic acid-degrading populations in soil.

作者信息

Ka J O, Holben W E, Tiedje J M

机构信息

Department of Microbiology, Michigan State University, East Lansing 48824.

出版信息

Appl Environ Microbiol. 1994 Apr;60(4):1116-20. doi: 10.1128/aem.60.4.1116-1120.1994.

Abstract

The herbicide 2,4-dichlorophenoxyacetic acid (2,4-D) was applied to soils in microcosms, and degradation was monitored after each of five repeated additions. Total DNAs were isolated from soil bacterial communities after each 2,4-D treatment. The DNA samples were analyzed on slot blots and Southern blots by using a tfdA gene probe subcloned from plasmid pJP4 and a Spa probe derived from a different 2,4-D-degrading isolate, a Sphingomonas paucimobilis strain. 2,4-D applied to soil was quickly degraded by indigenous microbial populations. As determined by slot blot analyses of DNA from a Michigan soil, the increase in hybridization signal in response to 2,4-D treatments was greater with the Spa probe than with the tfdA probe. In contrast, the DNA from a Saskatchewan soil exhibited an increase in hybridization signal with the tfdA probe. This indicated that a population with 2,4-D-degradative gene sequences different from the tfdA gene sequence was dominant in the Michigan site, but not in the Saskatchewan site. A Southern blot analysis of DNA from Michigan soil showed that the dominant 2,4-D-degrading population was S. paucimobilis 1443. A less dominant 2,4-D-degrading population was detected with the tfdA probe; further analysis revealed that this population was a Pseudomonas pickettii 712. These gene probe analyses revealed that an important population carrying out 2,4-D degradation was not detected when the canonical tfdA gene probe was used. After a series of new strains were isolated, we identified a probe to detect and identify the dominant members of this new group.

摘要

将除草剂2,4-二氯苯氧乙酸(2,4-D)施用于微观世界的土壤中,并在五次重复添加中的每次添加后监测其降解情况。每次2,4-D处理后,从土壤细菌群落中分离总DNA。使用从质粒pJP4亚克隆的tfdA基因探针和来自不同的2,4-D降解分离株——少动鞘氨醇单胞菌菌株的Spa探针,对DNA样品进行狭缝印迹和Southern印迹分析。施用于土壤的2,4-D被本地微生物群体迅速降解。通过对密歇根州土壤DNA的狭缝印迹分析确定,Spa探针响应2,4-D处理的杂交信号增加比tfdA探针更大。相比之下,萨斯喀彻温省土壤的DNA与tfdA探针杂交信号增加。这表明具有不同于tfdA基因序列的2,4-D降解基因序列的群体在密歇根州的位点占主导地位,但在萨斯喀彻温省的位点并非如此。对密歇根州土壤DNA的Southern印迹分析表明,占主导地位的2,4-D降解群体是少动鞘氨醇单胞菌1443。用tfdA探针检测到一个不太占主导地位的2,4-D降解群体;进一步分析表明该群体是皮氏假单胞菌712。这些基因探针分析表明,当使用标准tfdA基因探针时,未检测到进行2,4-D降解的重要群体。在分离出一系列新菌株后,我们鉴定出一种探针来检测和鉴定这个新群体的主要成员。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2b78/201447/9ef14763c3d1/aem00021-0078-a.jpg

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