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Microbial Thiocyanate Utilization under Highly Alkaline Conditions

机译:碱性条件下微生物硫氰酸盐的利用

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摘要

Three kinds of alkaliphilic bacteria able to utilize thiocyanate (CNS) at pH 10 were found in highly alkaline soda lake sediments and soda soils. The first group included obligate heterotrophs that utilized thiocyanate as a nitrogen source while growing at pH 10 with acetate as carbon and energy sources. Most of the heterotrophic strains were able to oxidize sulfide and thiosulfate to tetrathionate. The second group included obligately autotrophic sulfur-oxidizing alkaliphiles which utilized thiocyanate nitrogen during growth with thiosulfate as the energy source. Genetic analysis demonstrated that both the heterotrophic and autotrophic alkaliphiles that utilized thiocyanate as a nitrogen source were related to the previously described sulfur-oxidizing alkaliphiles belonging to the gamma subdivision of the division Proteobacteria (the Halomonas group for the heterotrophs and the genus Thioalkalivibrio for autotrophs). The third group included obligately autotrophic sulfur-oxidizing alkaliphilic bacteria able to utilize thiocyanate as a sole source of energy. These bacteria could be enriched on mineral medium with thiocyanate at pH 10. Growth with thiocyanate was usually much slower than growth with thiosulfate, although the biomass yield on thiocyanate was higher. Of the four strains isolated, the three vibrio-shaped strains were genetically closely related to the previously described sulfur-oxidizing alkaliphiles belonging to the genus Thioalkalivibrio. The rod-shaped isolate differed from the other isolates by its ability to accumulate large amounts of elemental sulfur inside its cells and by its ability to oxidize carbon disulfide. Despite its low DNA homology with and substantial phenotypic differences from the vibrio-shaped strains, this isolate also belonged to the genus Thioalkalivibrio according to a phylogenetic analysis. The heterotrophic and autotrophic alkaliphiles that grew with thiocyanate as an N source possessed a relatively high level of cyanase activity which converted cyanate (CNO) to ammonia and CO2. On the other hand, cyanase activity either was absent or was present at very low levels in the autotrophic strains grown on thiocyanate as the sole energy and N source. As a result, large amounts of cyanate were found to accumulate in the media during utilization of thiocyanate at pH 10 in batch and thiocyanate-limited continuous cultures. This is a first direct proof of a “cyanate pathway” in pure cultures of thiocyanate-degrading bacteria. Since it is relatively stable under alkaline conditions, cyanate is likely to play a role as an N buffer that keeps the alkaliphilic bacteria safe from inhibition by free ammonia, which otherwise would reach toxic levels during dissimilatory degradation of thiocyanate.
机译:在高碱性苏打湖沉积物和苏打土壤中发现了三种能够在pH 10下利用硫氰酸盐(CNS -)的嗜碱细菌。第一组包括专性异养菌,其利用硫氰酸盐作为氮源,同时在pH为10的条件下生长,乙酸盐为碳和能源。大多数异养菌株能够将硫化物和硫代硫酸盐氧化为四硫代酸盐。第二组包括专心自养的硫氧化亲碱,其在生长过程中以硫代硫酸盐为能源利用了硫氰酸盐氮。遗传分析表明,利用硫氰酸盐作为氮源的异养和自养亲碱都与先前描述的属于氧化细菌丙种细分的硫氧化亲碱有关(异养生物为Halomonas组,自养生物为硫代盐溶弧菌属)。 。第三类包括专性自养硫氧化的嗜碱细菌,能够利用硫氰酸盐作为唯一的能源。这些细菌可以在pH为10的含硫氰酸盐的矿物培养基上富集,尽管硫氰酸盐的生物量产率较高,但硫氰酸盐的生长通常比硫氰酸盐的生长慢得多。在分离出的四个菌株中,三个弧形菌株在遗传上与前面所述的硫代碱溶弧菌属的硫氧化性亲碱密切相关。棒状隔离物与其他隔离物的不同之处在于其在其细胞内积累大量元素硫的能力以及其氧化二硫化碳的能力。尽管它的低DNA同源性和与弧菌形毒株之间存在明显的表型差异,但根据系统发育分析,该分离株也属于硫代碱弧菌属。以硫氰酸盐作为氮源生长的异养和自养亲碱具有较高水平的氰化酶活性,可将氰酸盐(CNO -)转化为氨和CO2。另一方面,在以硫氰酸盐作为唯一能源和氮源生长的自养菌株中,氰化酶活性不存在或以非常低的水平存在。结果,在分批和硫氰酸盐受限的连续培养物中,在pH 10的硫氰酸盐利用过程中,发现大量的氰酸盐积聚在培养基中。这是纯降解硫氰酸盐细菌的培养物中“氰酸盐途径”的第一个直接证据。由于氰酸盐在碱性条件下相对稳定,因此有可能作为N缓冲液发挥作用,使嗜碱细菌免受游离氨的抑制,否则游离氨会在硫氰酸盐的异化降解过程中达到毒性水平。

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