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从亚历山大港的海水和沉积物中分离并计数海洋放线菌。

Isolation and enumeration of marine actinomycetes from seawater and sediments in Alexandria.

作者信息

Ghanem Nevine B., Sabry Soraya A., El-Sherif Zeinab M., Abu El-Ela Gehan A.

机构信息

Department of Botany, Faculty of Science, Alexandria University, Egypt.

出版信息

J Gen Appl Microbiol. 2000 Jun;46(3):105-111. doi: 10.2323/jgam.46.105.

Abstract

Actinomycetes were isolated from near-shore marine sediments and water at four different sites in Alexandria. Statistical analysis revealed that variation in temperature, pH, and dissolved phosphate were of insignificant values, but that variation in total nitrogen and organic matter were significant. The treatment of sediments and water samples by heat resulted in a selective reduction of the nonactinomycetal heterotrophic microflora. Four selective culture media were used for counting actinomycetes in marine water and sediments. The starch nitrate medium favored the growth of these microorganisms. The diversity and counts of actinomycetes varied with the seasonal variation, and the highest counts were detected in dry warm seasons. The numbers of this bacterial group in sediments exceeded by far their numbers in seawater. A positive correlation was found between population size and location. Actinomycetes were found in the highest numbers in the upper layers (0-20 cm depth). In a few cases, the counts of actinomycetes showed bimodal maxima 0-20 and 60-100 cm deep. Sediments were the best source of marine actinomycetes, and their distribution varied depending on the depth from which samples were collected. The ratio of actinomycetes to the total microflora ranged from 0.48 to 2.29, depending on location.

摘要

放线菌是从亚历山大港四个不同地点的近岸海洋沉积物和海水中分离出来的。统计分析表明,温度、pH值和溶解磷酸盐的变化值不显著,但总氮和有机物的变化显著。对沉积物和水样进行加热处理导致非放线菌异养微生物群落选择性减少。使用四种选择性培养基对海水中和沉积物中的放线菌进行计数。淀粉硝酸盐培养基有利于这些微生物的生长。放线菌的多样性和数量随季节变化而变化,在干燥温暖季节检测到的数量最高。该细菌群落在沉积物中的数量远远超过其在海水中的数量。发现种群大小与位置之间存在正相关。在上层(0-20厘米深度)发现的放线菌数量最多。在少数情况下,放线菌数量在0-20厘米和60-100厘米深处呈现双峰最大值。沉积物是海洋放线菌的最佳来源,其分布因采集样品的深度而异。放线菌与总微生物群落的比例因位置而异,范围在0.48至2.29之间。

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