Department of Crop and Soil Sciences and of Microbiology and Public Health, Michigan State University, East Lansing, Michigan 48824.
Appl Environ Microbiol. 1993 Oct;59(10):3297-305. doi: 10.1128/aem.59.10.3297-3305.1993.
Experiments were undertaken to explain the occurrence of a high denitrification capacity in anaerobic, NO(3)-free habitats. Deep layers of freshwater sediments that were buried more than 40 years ago and digested sludge were the habitats studied. The denitrifier populations were 3.1 x 10 and 3.1 x 10 cells cm in deep sediments from a river and lake, respectively, and 5.3 x 10 cells cm in digested sludge. The denitrification capacities of the samples reflected the population densities. Strict anaerobic procedures were used to obtain the predominant isolates that would grow on anaerobic medium with NO(3). All strict anaerobes isolated failed to denitrify. All isolates that denitrified were aerobic, gram-negative bacteria, particularly species of Pseudomonas and Alcaligenes. No detectable growth was observed when these strains were incubated with electron acceptors other than NO(3) or O(2). When representative isolates were added to sterile, O(2)- and NO(3)-free porewater from their original locations at their natural densities (10 cells cm), no change in viable population was noted over 3 months of incubation. Metabolic activity was demonstrated in these cells by slow formation of formazan granules when exposed to tetrazolium and by observation of motile cells. When [C]glucose was added to cell suspensions of the pseudomonads that had been starved for 3 months without electron acceptors (O(2) or NO(3)), C-labeled products, including cell biomass, CO(2), and fermentation products, were produced. The high denitrification capacity of these anaerobic environments appears to be due to conventional respiratory denitrifiers. These organisms have the capacity for long-term survival without O(2) or NO(3) and appear to be capable of providing for their maintenance by carrying on a low level of fermentation.
实验旨在解释在无氧、无硝酸盐的环境中存在高反硝化能力的现象。研究的生境是深层淡水沉积物,这些沉积物是 40 多年前埋藏的,还有消化污泥。河流和湖泊深层沉积物中的反硝化菌种群密度分别为 3.1×10 和 3.1×10 细胞/cm,消化污泥中的种群密度为 5.3×10 细胞/cm。样品的反硝化能力反映了种群密度。采用严格的厌氧程序获得主要的分离物,这些分离物可以在含有硝酸盐的厌氧培养基上生长。所有分离出来的严格厌氧菌都不能进行反硝化。所有能够反硝化的分离物都是需氧革兰氏阴性菌,特别是假单胞菌和产碱杆菌属的物种。当这些菌株在含有除硝酸盐或氧以外的电子受体的条件下培养时,没有观察到可检测的生长。当将代表性分离物添加到无菌、无氧和无硝酸盐的来自其原始位置的孔水中时,在 3 个月的孵育过程中,没有观察到活细胞数量的变化。在这些细胞中,通过暴露于四唑和观察游动细胞,缓慢形成甲臜颗粒来证明代谢活性。当将饥饿 3 个月而没有电子受体(氧或硝酸盐)的假单胞菌细胞悬液中的 [C]葡萄糖添加时,会产生包括细胞生物量、CO2 和发酵产物在内的 C 标记产物。这些厌氧环境的高反硝化能力似乎归因于传统的呼吸反硝化菌。这些生物体在没有氧或硝酸盐的情况下具有长期生存的能力,并且似乎能够通过进行低水平的发酵来维持自身。