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Comparison of 2,4-Dichlorophenoxyacetic Acid Degradation and Plasmid Transfer in Soil Resulting from Bioaugmentation with Two Different pJP4 Donors

机译:两种不同pJP4供体生物强化导致土壤中2,4-二氯苯氧基乙酸的降解和质粒转移的比较

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摘要

A pilot field study was conducted to assess the impact of bioaugmentation with two plasmid pJP4-bearing microorganisms: the natural host, Ralstonia eutropha JMP134, and a laboratory-generated strain amenable to donor counterselection, Escherichia coli D11. The R. eutropha strain contained chromosomal genes necessary for mineralization of 2,4-dichlorophenoxyacetic acid (2,4-D), while the E. coli strain did not. The soil system was contaminated with 2,4-D alone or was cocontaminated with 2,4-D and Cd. Plasmid transfer to indigenous populations, plasmid persistence in soil, and degradation of 2,4-D were monitored over a 63-day period in the bioreactors. To assess the impact of contaminant reexposure, aliquots of bioreactor soil were reamended with additional 2,4-D. Both introduced donors remained culturable and transferred plasmid pJP4 to indigenous recipients, although to different extents. Isolated transconjugants were members of the Burkholderia and Ralstonia genera, suggesting multiple, if not successive, plasmid transfers. Upon a second exposure to 2,4-D, enhanced degradation was observed for all treatments, suggesting microbial adaptation to 2,4-D. Upon reexposure, degradation was most rapid for the E. coli D11-inoculated treatments. Cd did not significantly impact 2,4-D degradation or transconjugant formation. This study demonstrated that the choice of donor microorganism might be a key factor to consider for bioaugmentation efforts. In addition, the establishment of an array of stable indigenous plasmid hosts at sites with potential for reexposure or long-term contamination may be particularly useful.
机译:进行了一项初步的现场研究,以评估带有两种质粒pJP4的微生物对生物增强的影响:天然宿主,富营养小球藻(Ralstonia eutropha)JMP134,和实验室产生的,适合供体反选择的菌株,大肠杆菌D11。富营养R.菌株含有2,4-dichlorophenoxyacetic acid(2,4-D)矿化所需的染色体基因,而E. coli菌株则没有。土壤系统仅被2,4-D污染,或被2,4-D和Cd共同污染。在生物反应器中,在63天的时间内监测了质粒向土著种群的转移,质粒在土壤中的持久性以及2,4-D的降解。为了评估污染物再暴露的影响,将生物反应器土壤的等分试样重新添加了额外的2,4-D。尽管程度不同,两个引入的供体仍可培养并将质粒pJP4转移至土著受体。分离的转导结合体是伯克霍尔德氏菌属和拉尔斯顿氏菌属的成员,表明存在多次(如果不是连续的)质粒转移。在第二次暴露于2,4-D后,所有处理均观察到降解增强,表明微生物对2,4-D的适应性强。再暴露后,大肠杆菌D11接种处理的降解最快。 Cd对2,4-D降解或共轭结合物的形成没有明显影响。这项研究表明,供体微生物的选择可能是考虑进行生物强化的关键因素。另外,在可能再暴露或长期污染的位点建立稳定的本地质粒宿主阵列可能特别有用。

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