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Enumeration of Chemoorganotrophic Carbonyl Sulfide (COS)-degrading Microorganisms by the Most Probable Number Method

机译:用最可能数法枚举降解化学有机营养的羰基硫(COS)的微生物。

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摘要

Carbonyl sulfide (COS) is the most abundant sulfur compound in the atmosphere, and, thus, is important in the global sulfur cycle. Soil is a major sink of atmospheric COS and the numerical distribution of soil microorganisms that degrade COS is indispensable for estimating the COS-degrading potential of soil. However, difficulties are associated with counting COS-degrading microorganisms using culture-dependent approaches, such as the most probable number (MPN) method, because of the chemical hydrolysis of COS by water. We herein developed a two-step MPN method for COS-degrading microorganisms: the first step for chemoorganotrophic growth that supported a sufficient number of cells for COS degradation in the second step. Our new MPN analysis of various environmental samples revealed that the cell density of COS-degrading microorganisms in forest soils ranged between 10 and 10 MPN (g dry soil) , which was markedly higher than those in volcanic deposit and water samples, and strongly correlated with the rate of COS degradation in environmental samples. Numerically dominant COS degraders that were isolated from the MPN-positive culture were related to bacteria in the orders and . The present results provide numerical evidence for the ubiquity of COS-degrading microbes in natural environments.
机译:羰基硫(COS)是大气中最丰富的硫化合物,因此在全球硫循环中很重要。土壤是大气COS的主要汇聚地,降解COS的土壤微生物的数值分布对于估算土壤的COS降解潜力是必不可少的。但是,由于水对COS的化学水解作用,使用依赖于培养的方法(例如最可能的数(MPN)方法)对降解COS的微生物进行计数存在困难。我们在本文中开发了一种用于COS降解微生物的两步MPN方法:第一步是化学有机营养生长,第二步支持足够数量的细胞用于COS降解。我们对各种环境样品进行的新MPN分析表明,森林土壤中降解COS的微生物的细胞密度介于10到10 MPN(克干土壤)之间,明显高于火山沉积物和水样中的微生物,并且与环境样品中COS降解的速率。从MPN阳性培养物中分离出的数量占优势的COS降解物与细菌的顺序有关。目前的结果为自然环境中普遍存在的COS降解微生物提供了数值证据。

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