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在产硫化物和产甲烷条件下,从丹麦奥胡斯湾不同生物地球化学区域富集的丙酸转化厌氧微生物群落。

Propionate Converting Anaerobic Microbial Communities Enriched from Distinct Biogeochemical Zones of Aarhus Bay, Denmark under Sulfidogenic and Methanogenic Conditions.

作者信息

Ozuolmez Derya, Stams Alfons J M, Plugge Caroline M

机构信息

Laboratory of Microbiology, Wageningen University & Research, Stippeneng 4, 6708 WE Wageningen, The Netherlands.

出版信息

Microorganisms. 2020 Mar 11;8(3):394. doi: 10.3390/microorganisms8030394.

Abstract

The relationship between predominant physiological types of prokaryotes in marine sediments and propionate degradation through sulfate reduction, fermentation, and methanogenesis was studied in marine sediments. Propionate conversion was assessed in slurries containing sediment from three different biogeochemical zones of Aarhus Bay, Denmark. Sediment slurries were amended with 0, 3, or 20 mM sulfate and incubated at 25 °C and 10 °C for 514-571 days. Methanogenesis in the sulfate zone and sulfate reduction in the methane zone slurries was observed. Both processes occurred simultaneously in enrichments originating from samples along the whole sediment. Bacterial community analysis revealed the dominance of and members in sulfate-amended slurries incubated at 25°C and 10°C. belonging to the family dominated sulfate-free methanogenic slurries at 25°C, whereas bacteria related to were dominant at 10°C. Archaeal community analysis revealed the prevalence of different genera belonging to in slurries incubated at different temperatures and amended with different sulfate concentrations. were only detected in the absence of sulfate. In summary, Aarhus Bay sediment zones contain sulfate reducers, syntrophs, and methanogens interacting with each other in the conversion of propionate. Our results indicate that in Aarhus Bay sediments, degraded propionate in syntrophic association with methanogens

摘要

在海洋沉积物中研究了原核生物的主要生理类型与通过硫酸盐还原、发酵和甲烷生成进行丙酸盐降解之间的关系。在含有来自丹麦奥胡斯湾三个不同生物地球化学区沉积物的泥浆中评估丙酸盐转化。向泥浆中添加0、3或20 mM硫酸盐,并在25℃和10℃下孵育514 - 571天。观察到硫酸盐区的甲烷生成和甲烷区泥浆中的硫酸盐还原。这两个过程在来自整个沉积物样品的富集物中同时发生。细菌群落分析显示,在25℃和10℃下孵育的添加硫酸盐的泥浆中, 和 成员占主导地位。在25℃下,属于 科的 在无硫酸盐的产甲烷泥浆中占主导,而在10℃下,与 相关的细菌占主导。古菌群落分析表明,在不同温度下孵育并添加不同硫酸盐浓度的泥浆中,属于 的不同属普遍存在。仅在无硫酸盐的情况下检测到 。总之,奥胡斯湾沉积物区域含有在丙酸盐转化过程中相互作用的硫酸盐还原菌、互营菌和产甲烷菌。我们的数据表明,在奥胡斯湾沉积物中, 与产甲烷菌以互营关系降解丙酸盐

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