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Confirmation of Occurrence of Hydroxamate Siderophores in Soil by a Novel Escherichia coli Bioassay

机译:通过新型大肠杆菌生物测定法确认土壤中异羟肟酸铁载体的存在

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摘要

The occurrence of ferrichrome-type hydroxamate siderophores in soil was confirmed. In the presence of the iron-scavenging chelator ethylenediamine[di(o-hydroxyphenylacetic)acid], soil extract stimulated the growth of an Escherichia coli strain possessing the ferrichrome transport protein (TonA) but did not stimulate growth of a strain lacking this protein (TonA?). The siderophore concentration in a 1:1 (soil-water) extract was estimated to be approximately 78 nM. Specificity of the assay was supported by the absence of significant differential strain responses to ferric citrate, ferric 2,3-dihydroxybenzoate, enterochelin, ferrioxamine B, coprogen, and triacetylfusigen.
机译:确认在土壤中存在铁铬型异羟肟酸酯铁载体。在有铁清除螯合剂乙二胺[二(邻羟基苯乙酸)酸]存在下,土壤提取物刺激了具有铁铬转运蛋白(TonA)的大肠杆菌菌株的生长,但没有刺激缺乏该蛋白的菌株的生长( TonA?)。 1:1(土壤-水)提取物中的铁载体浓度估计约为78 nM。该测定的特异性得到了对柠檬酸铁,2,3-二羟基苯甲酸铁,肠螯合素,铁氧嘧啶B,辅生素和三乙酰基fusigen的显着差异应变反应的支持。

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