腐殖假单胞菌(pWW0)对土壤中对甲基- 14c -苯甲酸盐的矿化作用

E Duque, S Marqués, J L Ramos
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引用次数: 0

摘要

携带TOL原型质粒pWW0的恶臭假单胞菌通过后裂解途径代谢对苯甲酸酯。在有机质相对丰富的土壤等复杂环境中,我们观察到对甲基- 14c -苯甲酸酯的代谢,这可以作为14CO2从标记的烷基芳体演化来监测。土壤中二氧化碳的线性演化至少持续了一个月,尽管烷基烃的有效矿化需要适当的传质,以使细菌细胞和目标化学物质保持密切接触。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mineralization of p-methyl-14C-benzoate in soils by Pseudomonas putida (pWW0).

Pseudomonas putida bearing the archetypal TOL plasmid pWW0 metabolizes p-methylbenzoate through a meta-cleavage pathway. In complex environments such as soils that are relatively rich in organic matter, we observed metabolism of p-methyl-14C-benzoate, which could be monitored as 14CO2 evolution from the labelled alkylaromatic. Linear 14CO2 evolution in soils took place for at least a month, although efficient mineralization of the alkylaromatic required appropriate mass transfer to allow the bacterial cell and target chemical to remain in close contact.

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