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The Earthworm Gut: an Ideal Habitat for Ingested N2O-Producing Microorganisms

机译:Gu肠:摄取N2O的微生物的理想栖息地

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摘要

The in vivo production of nitrous oxide (N2O) by earthworms is due to their gut microbiota, and it is hypothesized that the microenvironment of the gut activates ingested N2O-producing soil bacteria. In situ measurement of N2O and O2 with microsensors demonstrated that the earthworm gut is anoxic and the site of N2O production. The gut had a pH of 6.9 and an average water content of approximately 50%. The water content within the gut decreased from the anterior end to the posterior end. In contrast, the concentration of N2O increased from the anterior end to the mid-gut region and then decreased along the posterior part of the gut. Compared to the soil in which worms lived and fed, the gut of the earthworm was highly enriched in total carbon, organic carbon, and total nitrogen and had a C/N ratio of 7 (compared to a C/N ratio of 12 in soil). The aqueous phase of gut contents contained up to 80 mM glucose and numerous compounds that were indicative of anaerobic metabolism, including up to 9 mM formate, 8 mM acetate, 3 mM lactate, and 2 mM succinate. Compared to the soil contents, nitrite and ammonium were enriched in the gut up to 10- and 100-fold, respectively. The production of N2O by soil was induced when the gut environment was simulated in anoxic microcosms for 24 h (the approximate time for passage of soil through the earthworm). Anoxia, high osmolarity, nitrite, and nitrate were the dominant factors that stimulated the production of N2O. Supplemental organic carbon had a very minimal stimulatory effect on the production of N2O, and addition of buffer or ammonium had essentially no effect on the initial N2O production rates. However, a combination of supplements yielded rates greater than that obtained mathematically for single supplements, suggesting that the maximum rates observed were due to synergistic effects of supplements. Collectively, these results indicate that the special microenvironment of the earthworm gut is ideally suited for N2O-producing bacteria and support the hypothesis that the in situ conditions of the earthworm gut activate ingested N2O-producing soil bacteria during gut passage.
机译:The体内的一氧化二氮(N2O)产生是由于它们的肠道菌群,据推测,肠道的微环境会激活摄入的产生N2O的土壤细菌。用微传感器对N2O和O2的原位测量表明demonstrated肠是缺氧的并且是N2O产生的场所。肠道的pH值为6.9,平均水含量约为50%。肠道内的水分从前端到后端降低。相反,N2O的浓度从前端到肠中部区域增加,然后沿肠道的后部减少。与蠕虫生活和觅食的土壤相比,earth的肠道富含高碳,高碳和高氮,碳氮比为7(土壤碳氮比为12) )。肠内容物的水相包含高达80 mM的葡萄糖和许多指示无氧代谢的化合物,包括高达9 mM的甲酸,8 mM的乙酸盐,3 mM的乳酸和2 mM的琥珀酸盐。与土壤含量相比,肠道中的亚硝酸盐和铵盐含量分别高达10倍和100倍。当在缺氧的微观环境中模拟肠道环境24小时(土壤通过the的大约时间)时,便诱导了土壤中N2O的产生。缺氧,高渗透压,亚硝酸盐和硝酸盐是刺激N2O产生的主要因素。补充有机碳对N2O的产生具有非常小的刺激作用,而添加缓冲液或铵对初始N2O的产生速率基本上没有影响。然而,补充剂的组合产生的速率大于数学上单个补充剂获得的速率,这表明观察到的最大速率是由于补充剂的协同作用。总体而言,这些结果表明worm肠道的特殊微环境非常适合于产生N2O的细菌,并支持the肠道的原位条件激活肠道通过过程中摄入的产生N2O的土壤细菌这一假设。

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