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Relative Role of Eukaryotic and Prokaryotic Microorganisms in Phenanthrene Transformation in Coastal Sediments

机译:真核和原核微生物在沿海沉积物中菲转化中的相对作用

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The relative role of eukaryotic versus prokaryotic microorganisms in phenanthrene transformation was measured in slurries of coastal sediment by two different approaches: detection of marker metabolites and use of selective inhibitors on phenanthrene biotransformation. Phenanthrene biotransformation was measured by polar metabolite formation and CO2 evolution from [9-14C]phenanthrene. Radiolabeled metabolites were tentatively identified by high-performance liquid chromatography (HPLC) separation combined with UV/visible spectral analysis of HPLC peaks and comparison to authentic standards. Both yeasts and bacteria transformed phenanthrene in slurries of coastal sediment. Two products of phenanthrene oxidation by fungi, phenanthrene trans-3,4-dihydrodiol and 3-phenanthrol, were produced in yeast-inoculated sterile sediment. However, only products of phenanthrene oxidation typical of bacterial transformation, 1-hydroxy-2-naphthoic acid and phenanthrene cis-3,4-dihydrodiol, were isolated from slurries of coastal sediment with natural microbial populations. Phenanthrene trans-dihydrodiols or other products of fungal oxidation of phenanthrene were not detected in the slurry containing a natural microbial population. A predominant role for bacterial transformation of phenanthrene was also suggested from selective inhibitor experiments. Addition of streptomycin to slurries, at a concentration which suppressed bacterial viable counts and rates of [methyl-3H]thymidine uptake, completely inhibited phenanthrene transformation. Treatment with colchicine, at a concentration which suppressed yeast viable counts, depressed phenanthrene transformation by 40%, and this was likely due to nontarget inhibition of bacterial activity. The relative contribution of eukaryotic microorganisms to phenanthrene transformation in inoculated sterile sediment was estimated to be less than 3% of the total activity. We conclude that the predominant degraders of phenanthrene in muddy coastal sediments are bacteria and not eukaryotic microorganisms.
机译:通过两种不同的方法在沿海沉积物的浆液中测量了真核微生物与原核微生物在菲转化中的相对作用:检测标记代谢物和在菲生物转化中使用选择性抑制剂。通过[9-14C]菲的极性代谢物形成和CO2的释放来测量菲的生物转化。通过高效液相色谱(HPLC)分离结合HPLC峰的UV /可见光谱分析并与真实标准品进行比较,初步确定了放射性标记的代谢物。酵母菌和细菌都会在沿海沉积物的浆液中转化菲。在酵母菌接种的无菌沉淀物中产生了两种被真菌氧化的菲,菲反式3,4-二氢二醇和3-菲酚。然而,仅从具有天然微生物种群的沿海沉积物浆液中分离出细菌转化典型的菲氧化产物1-羟基-2-萘甲酸和菲顺-3,4-二氢二醇。在包含天然微生物种群的浆液中未检测到菲反式二氢二醇或菲的其他真菌氧化产物。选择性抑制剂实验还表明,菲在细菌转化中起主要作用。将链霉素添加到浆液中的浓度可以抑制细菌的存活数量和[甲基-3H]胸苷的摄取速率,从而完全抑制了菲的转化。用秋水仙碱处理,其浓度可抑制酵母的存活计数,使菲转化降低40%,这可能是由于非靶标抑制细菌活性所致。估计真核微生物对接种的无菌沉积物中菲转化的相对贡献小于总活性的3%。我们得出的结论是,在沿海泥泞沉积物中菲的主要降解物是细菌,而不是真核微生物。

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