首页> 美国卫生研究院文献>Microorganisms >Propionate Converting Anaerobic Microbial Communities Enriched from Distinct Biogeochemical Zones of Aarhus Bay Denmark under Sulfidogenic and Methanogenic Conditions
【2h】

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

机译:在成矿作用和产甲烷作用下从丹麦奥胡斯湾不同生物地球化学区富集的丙酸转化厌氧微生物群落

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

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.
机译:研究了海洋沉积物中原核生物的主要生理类型与丙酸盐通过硫酸盐还原,发酵和甲烷生成的降解之间的关系。在含有来自丹麦奥尔胡斯湾三个不同生物地球化学区的沉积物的浆液中评估了丙酸转化率。用0、3或20 mM硫酸盐修正沉淀浆,并在25°C和10°C下温育514–571天。观察到硫酸盐区的甲烷生成和甲烷区浆液中的硫酸盐还原。这两个过程同时发生,富集来自沿整个沉积物的样品。细菌群落分析显示,在25°C和10°C下温育的硫酸盐改良浆液中,其成员具有优势。属于该家族的细菌在25°C时占主导地位,而无硫酸盐的产甲烷浆液则在10°C时占主导地位。古细菌群落分析揭示了在不同温度下孵育并用不同硫酸盐浓度修正的浆液中属于不同属的流行。仅在不存在硫酸盐的情况下才能检测到。总而言之,奥尔胡斯湾沉积物区域包含硫酸盐还原剂,同养菌和产甲烷菌,它们在丙酸酯的转化中相互作用。我们的结果表明,在奥尔胡斯湾沉积物中,降解的丙酸根与产甲烷菌呈同养关系。

著录项

相似文献

  • 外文文献
  • 专利
代理获取

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号