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Exchange of a Conjugative Plasmid At Different Soil Moisture Levels Between Streptomyces Species Colonizing Artificial Soil Aggregates

机译:在不同土壤水分水平下,定植在人工土壤聚集体中的链霉菌种之间交换质粒的交换

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Spores of a Streptomyces lividans strain (donor) bearing the recombinant conjugative plasmid pIJ303, which codes for thiostrepton resistance, and spores of a plasmid-free Streptomyces parvulus strain (recipient) were added together to finely-sieved, sterile silt loam soil. This bulk soil was adjusted to either 20%, 35% or 45% of the soil’s water holding capacity. To this inoculated bulk soil were added sterile, nutrient- amended, artificial soil aggregates. After incubation to allow streptomycete growth and aggregate colonization, both the sieved bulk soil and the aggregates were assayed for numbers of transconjugants by spread- planting on a thiostrepton – agar selective medium. This allowed estimation of parental ability to colonize nutrient – rich soil sites at different soil moisture levels, and comparison of plasmid exchange frequency in the nonamended bulk soil versus the nutrient – rich soil aggregates. Plasmid exchange was detected only on aggregates of about 20% water holding capacity or less (4.2% wt/wt H20). The soil moisture threshold for heterotrophic streptomycete activity appeared to lie between 2.87% and 4.2% wt/wt H20 for the nutrient- amended soil aggregates. Introduction The ability to colonize and occupy solid substrates in soil, such as plant or animal remains, is vital to the growth and existence of soil microorganisms (Hissett and Gray, 1976). Genetically-engineered microorganisms (GEMs) which are released into the soil environment have to compete with native soil microorganisms during colonization and occupation of soil microhabitats. The outcome of such competitive colonization helps determine whether a GEM persists in the environment or dies off, influencing whether the GEM is able to manifest effects in the soil environment, or is able to transfer its DNA to native soil microorganisms (Stotzky and Babich, 1986). Gene transfer events between soil prokaryotes have effects on phenomena including microbial evolution in general, and more specifically the spread of antibiotic resistance genes to microorganisms affecting human and animal health (reviewed by Thomas and Nielsen, 2005). Conjugation is one of the major types of gene transfer events, and is known to occur between many types of prokaryotes, including Streptomyces (reviewed by Marsh and Wellington, 1994; and Strap and Crawford, 2007).The filamentous growth habit of some microorganisms (such as Streptomyces spp.) allows them to bridge air-filled pores in dry soil and to penetrate solid substrates (Griffin, 1981). Studies have been conducted on colonization of plant materials (Keinath and Loria, 1989; Lewis, 1970; Mayfield et al., 1972; Watson and Williams, 1974) and of autoclaved soil or of nutrients in amended soil (Bleakley and Crawford, 1989; Lloyd, 1969; Mayfield et al., 1972) by streptomycetes. Conjugation-mediated plasmid exchange has been observed between streptomycetes as they colonize autoclaved soil ( Bleakley and Crawford, 1989; Rafii and Crawford, 1988; and reviewed by Strap and Crawford, 2007). Plasmid transfer frequency between certain streptomycete strains has been found to be highest when nutrients are added to relatively dry soil (Bleakley and Crawford, 1989). The nutrients in that previous study were mixed throughout the soil matrix, probably affording multiple nutritional “hot-spots” at which streptomycete hyphae met, fused and participated in conjugation-mediated plasmid exchange.The purpose of the present study was to see if larger, macroscopic “hot-spots” in the form of artificially molded, nutrient-amended soil aggregates would result in the same pattern of plasmid exchange as previously observed between a Streptomyces lividans donor and a Streptomyces parvulus recipient. The hypothesis was that plasmid exchange would be most frequent between hyphae on nutrient-amended, relatively dry soil aggregates. Heterotrophic microbial activity in bulk soil and aggregates was assayed using a fluorescein diacetate (FDA) hydrolysis assay,
机译:将带有重组结合质粒pIJ303(编码硫链丝菌抗性)的链霉菌链霉菌菌株(供体)的孢子和无质粒链霉菌菌株(受体)的孢子一起添加到细筛分的无菌淤泥壤土中。将这种散装土壤调整为土壤保水量的20%,35%或45%。向该接种的大块土壤中添加无菌,经过营养素改良的人造土壤集料。孵育使链霉菌生长并聚集后,通过在thiostrepton –琼脂选择性培养基上铺展,对筛分的大块土壤和团聚体中的转导结合物进行了分析。这样可以估算父母在不同土壤水分水平下富营养化土壤位点定殖的能力,并可以比较未经改良的散装土壤与富营养化土壤团聚体中质粒交换频率。仅在持水量约为20%或更低(4.2%wt / wt H2O)的聚集体上检测到质粒交换。对于营养改良土壤团聚体,异养链霉菌活性的土壤水分阈值似乎在2.87%至4.2%wt / wt H2O之间。简介能够在土壤中(例如植物或动物残骸)定居并占据其固体基质的能力,对于土壤微生物的生长和生存至关重要(Hissett和Gray,1976)。被释放到土壤环境中的基因工程微生物(GEM)必须在土壤微生境的定殖和占领过程中与天然土壤微生物竞争。这种竞争性殖民化的结果有助于确定GEM是否在环境中持续存在或死亡,从而影响GEM是否能够在土壤环境中发挥作用,或者是否能够将其DNA转移至天然土壤微生物(Stotzky和Babich,1986年) )。土壤原核生物之间的基因转移事件通常会影响包括微生物进化在内的各种现象,更具体而言,是抗生素抗性基因向影响人类和动物健康的微生物的传播(Thomas and Nielsen,2005年综述)。结合是基因转移事件的主要类型之一,并且已知发生在许多类型的原核生物之间,包括链霉菌(由Marsh和Wellington审查,1994年;以及Strap和Crawford,2007年)。某些微生物的丝状生长习性(例如链霉菌属(Streptomyces spp。))可以使它们弥合干燥土壤中的空气孔并渗透固体基质(Griffin,1981)。已经进行了关于植物材料定殖的研究(Keinath和Loria,1989; Lewis,1970; Mayfield等,1972; Watson和Williams,1974)和高压灭菌的土壤或改良土壤中的养分(Bleakley和Crawford,1989; 1989)。 Lloyd,1969; Mayfield等,1972)。当链霉菌在高压灭菌的土壤中定殖时,已观察到缀合介导的质粒交换(Bleakley和Crawford,1989; Rafii和Crawford,1988;以及Strap和Crawford,2007)。当在相对干燥的土壤中添加养分时,发现某些链霉菌菌株之间的质粒转移频率最高(Bleakley和Crawford,1989)。该先前研究中的营养成分在整个土壤基质中混合在一起,可能提供了链霉菌丝菌丝相遇,融合并参与缀合介导的质粒交换的多个营养“热点”。本研究的目的是观察是否更大,人工模制,经过营养改良的土壤团聚体形式的宏观“热点”,将导致质粒交换的模式与以前在淡紫色链霉菌供体和小链霉菌受体之间观察到的模式相同。假设是,在经过营养改良,相对干燥的土壤聚集体上的菌丝之间,质粒交换最频繁。使用荧光素二乙酸酯(FDA)水解测定法测定散装土壤和团聚体中的异养微生物活性,

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