Terai土壤的化学异养硫氧化微生物I.微生物对无机和有机硫的氧化,从蔗糖-硫代硫酸钠琼脂中分离

N. Chattopadhyaya , B.K. Dey
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引用次数: 1

摘要

在21个化学异养型硫氧化微生物中,从具有代表性的印度Terai土壤中分离出蔗糖-硫代硫酸钠琼脂板- Mollisol目喜马拉雅山麓土壤(典型Haplaquept)。13株为细菌,12株属于芽孢杆菌属,1株属于微球菌属,3株属于链霉菌属放线菌。五个分离株是真菌——两个属青霉菌,三个属曲霉。其中,高效硫氧化剂为芽孢杆菌- TSB5和TSB6、链霉菌- TSA1和曲霉- TSF3和TSF5。总的来说,无机硫源硫代硫酸钠的氧化作用基本上高于有机硫源l -胱氨酸的氧化作用。该属的总体效率依次为曲霉、青霉菌、链霉菌、芽孢杆菌和微球菌。Aus repräsentativen indischen Terai-Böden (am Fuß des Himalaja-Gebirges), die Inceptisol-Haplaquept-Bodentypen entsprechen, wurden auf sugar - natriumthiosulfate - agarplatten 21 chemoheterotrophe schwefelo -oxidierende microorganismen isoliert。微苯分离菌株waren Bakterien, 12株gehörten zur Gattung Bacillus, 2株zur Gattung Micrococcus, 3株zur Gattung Streptomyces. 5分离菌株waren Pilze, 2株青霉菌,3株anten曲霉。2芽孢杆菌:TSB5和TSB6,链霉菌和TSA1在曲霉分离物TSF3和TSF5之间死亡。Allgemein war die Schwefeloxidation aufden organchen S-Quellen (na -硫代硫酸盐)wesentlich höher也auder organchen S-Quelle 1-Cystin。细菌:曲霉、青霉、链霉菌、芽孢杆菌、粘球菌。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Chemoheterotrophic Sulfur Oxidising Microorganisms of a Terai Soil I. Oxidation of Inorganic and Organic Sulfur by Microorganisms, Isolated in Sucrose-Sodiumthiosulfate Agar

Among twenty one chemoheterotrophic sulfur-oxidising microorganisms, isolated in sucrose-sodium-thiosulfate agar plates from a representative Indian Terai Soil — a Himalayan foot hill soil of the Order Mollisol (Typic Haplaquept). Thirteen isolates were bacteria, twelve belong to the genus Bacillus, and one to Micrococcus, three actinomycetes to the genus Streptomyces. Five isolates were fungi — two of the genus Penicillium, and three of the genus Aspergillus. Of these, the efficient sulfur oxidisers were Bacillus spp — TSB5 and TSB6, Streptomyces sp. — TSA1, and Aspergillus spp. — TSF3 and TSF5. In general, the oxidation by the isolates was essentially higher from the inorganic sulfur source, sodiumthiosulfate than from the organic sulfur source, L-cystine. The overall efficiency of the genera decreases in following order Aspergillus, Penicillium, Streptomyces, Bacillus and Micrococcus.

Aus repräsentativen indischen Terai-Böden (am Fuß des Himalaja-Gebirges), die Inceptisol-Haplaquept-Bodentypen entsprechen, wurden auf Saccharose-Natriumthiosulfat-Agarplatten 21 chemoheterotrophe Schwefel-oxidierende Mikroorganismen isoliert. 16 Mikrobenisolate waren Bakterien, 12 davon gehörten zur Gattung Bacillus, einer zur Gattung Micrococcus, 3 zur Gattung Streptomyces. 5 Isolate waren Pilze, 2 Penicillium- und 3 Aspergillus-Anten. Von diesen waren die effizientesten Schwefeloxidanten 2 Bacillusspezies: TSB5 und TSB6, ein Streptomycesholat TSA1 sowie die beiden Aspergillusisolate TSF3 und TSF5. Allgemein war die Schwefeloxidation auf den anorganischen S-Quellen (Na-thiosulfat) wesentlich höher als auf der organischen S-Quelle 1-Cystin. Die Schwefeloxidation nahm ab in der Reihenfolge: Aspergillus, Penicillium, Streptomyces, Bacillus, Mucrococcus.

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