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Use of the 14CLeucine Incorporation Technique To Measure Bacterial Production in River Sediments and the Epiphyton

机译:14C亮氨酸掺入技术在河流沉积物和附生植物中细菌生产的测量

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摘要

Bacterial production is a key parameter for the understanding of carbon cycling in aquatic ecosystems, yet it remains difficult to measure in many aquatic habitats. We therefore tested the applicability of the [14C]leucine incorporation technique for the measurement of bulk bacterial production in various habitats of a lowland river ecosystem. To evaluate the method, we determined (i) extraction efficiencies of bacterial protein from the sediments, (ii) substrate saturation of leucine in sediments, the biofilms on aquatic plants (epiphyton), and the pelagic zone, (iii) bacterial activities at different leucine concentrations, (iv) specificity of leucine uptake by bacteria, and (v) the effect of the incubation technique (perfused-core incubation versus slurry incubation) on leucine incorporation into protein. Bacterial protein was best extracted from sediments and precipitated by hot trichloroacetic acid treatment following ultrasonication. For epiphyton, an alkaline-extraction procedure was most efficient. Leucine incorporation saturation occurred at 1 μM in epiphyton and 100 nM in the pelagic zone. Saturation curves in sediments were difficult to model but showed the first level of leucine saturation at 50 μM. Increased uptake at higher leucine concentrations could be partly attributed to eukaryotes. Addition of micromolar concentrations of leucine did not enhance bacterial electron transport activity or DNA replication activity. Similar rates of leucine incorporation into protein calculated for whole sediment cores were observed after slurry and perfused-core incubations, but the rates exhibited strong vertical gradients after the core incubation. We conclude that the leucine incorporation method can measure bacterial production in a wide range of aquatic habitats, including fluvial sediments, if substrate saturation and isotope dilution are determined.
机译:细菌生产是了解水生生态系统中碳循环的关键参数,但在许多水生生境中仍然很难测量。因此,我们测试了[ 14 C]亮氨酸掺入技术在测量低地河流生态系统各种生境中的大量细菌生产中的适用性。为了评估该方法,我们确定了(i)从沉积物中提取细菌蛋白的效率,(ii)沉积物中亮氨酸的底物饱和度,水生植物(表藻)上的生物膜和中上层带,(iii)不同条件下的细菌活性亮氨酸浓度,(iv)细菌对亮氨酸摄取的特异性,以及(v)孵育技术(灌注核心孵育与浆液孵育)对亮氨酸掺入蛋白质的影响。细菌蛋白最好从沉淀物中提取,并在超声处理后通过热三氯乙酸处理沉淀。对于附生植物,碱性提取过程最有效。亮氨酸的掺入饱和度在附生植物中为1μM,在中上层区域为100 nM。沉积物中的饱和度曲线很难建模,但显示出亮氨酸饱和度的第一水平为50μM。在较高的亮氨酸浓度下摄取增加可能部分归因于真核生物。加入微摩尔浓度的亮氨酸并不能增强细菌电子转运活性或DNA复制活性。在浆液和灌注芯孵育后,可以观察到亮氨酸掺入蛋白质的比率(对于整个沉积物核心而言)相似,但是在核心孵育后,速率显示出很强的垂直梯度。我们得出的结论是,如果确定了底物饱和度和同位素稀释度,则亮氨酸掺入法可以测量多种水生生境(包括河流沉积物)中的细菌产量。

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