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一种异养细菌对硫氰酸盐作为氮源的利用:降解途径涉及氨和连四硫酸盐的形成。

The utilization of thiocyanate as a nitrogen source by a heterotrophic bacterium: the degradative pathway involves formation of ammonia and tetrathionate.

作者信息

Stratford J, Dias A E, Knowles C J

机构信息

Biological Laboratory, University, Canterbury, Kent, UK.

出版信息

Microbiology (Reading). 1994 Oct;140 ( Pt 10):2657-62. doi: 10.1099/00221287-140-10-2657.

Abstract

A Gram-negative soil bacterium (isolate 26B) has been shown to utilize up to 100 mM thiocyanate as a source of nitrogen when supplied with glucose as the source of carbon and energy. During growth of isolate 26B with thiocyanate as the source of nitrogen, no ammonia, nitrate, nitrite, cyanide, cyanate, sulfate, sulfite, sulfide or carbonyl sulfide was detected in the growth medium. Growth of the bacterium on 14C-labelled thiocyanate (1.6 microCi) and glucose, yielded 14C-labelled carbon dioxide (0.9 microCi). The addition of 2.9 mM thiocyanate to a bacterial suspension in phosphate buffer (50 mM, pH 7.4) resulted in the utilization of 2.1 mM thiocyanate and the production of 2.0 mM ammonia. This activity was inducible and only occurred after growth of the bacterium with thiocyanate as the source of nitrogen. Tetrathionate (0.7 mM) was detected in the medium after the utilization of thiocyanate (2.4 mM) by a suspension of the bacterium in phosphate buffer, and thiosulfate (1.0 mM) was detected as an intermediate. The addition of sulfide or thiosulfate to the bacterial suspension also resulted in the formation of tetrathionate. The utilization of both of these compounds appeared to be constitutive. A pathway for thiocyanate utilization by isolate 26B is proposed which involves the hydrolysis of thiocyanate to produce cyanate and sulfide. The cyanate then undergoes further hydrolysis to form ammonia and carbon dioxide. The sulfide is ultimately oxidized to tetrathionate via a pathway which includes thiosulfate.

摘要

一种革兰氏阴性土壤细菌(菌株26B)已被证明,当提供葡萄糖作为碳源和能源时,它能够利用高达100 mM的硫氰酸盐作为氮源。在以硫氰酸盐作为氮源培养菌株26B的过程中,在生长培养基中未检测到氨、硝酸盐、亚硝酸盐、氰化物、氰酸盐、硫酸盐、亚硫酸盐、硫化物或羰基硫。该细菌在14C标记的硫氰酸盐(1.6微居里)和葡萄糖上生长,产生了14C标记的二氧化碳(0.9微居里)。向磷酸盐缓冲液(50 mM,pH 7.4)中的细菌悬液中添加2.9 mM硫氰酸盐,导致利用了2.1 mM硫氰酸盐并产生了2.0 mM氨。这种活性是可诱导的,并且仅在细菌以硫氰酸盐作为氮源生长后才出现。在细菌悬液在磷酸盐缓冲液中利用硫氰酸盐(2.4 mM)后,在培养基中检测到了连四硫酸盐(0.7 mM),并检测到硫代硫酸盐(1.0 mM)作为中间产物。向细菌悬液中添加硫化物或硫代硫酸盐也导致了连四硫酸盐的形成。对这两种化合物的利用似乎是组成型的。提出了菌株26B利用硫氰酸盐的途径,该途径涉及硫氰酸盐水解产生氰酸盐和硫化物。然后氰酸盐进一步水解形成氨和二氧化碳。硫化物最终通过包括硫代硫酸盐的途径被氧化为连四硫酸盐。

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