...
首页> 外文期刊>Microbial Ecology: An International Journal >Anaerobic Methane-Oxidizing Microbial Community in a Coastal Marine Sediment: Anaerobic Methanotrophy Dominated by ANME-3
【24h】

Anaerobic Methane-Oxidizing Microbial Community in a Coastal Marine Sediment: Anaerobic Methanotrophy Dominated by ANME-3

机译:沿海海洋沉积物的厌氧甲烷氧化微生物群落:Anaerobic甲基萎缩由ANME-3主导

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

The microbial community inhabiting the shallow sulfate-methane transition zone in coastal sediments from marine Lake Grevelingen (The Netherlands) was characterized, and the ability of the microorganisms to carry out anaerobic oxidation of methane coupled to sulfate reduction was assessed in activity tests. In vitro activity tests of the sediment with methane and sulfate demonstrated sulfide production coupled to the simultaneous consumption of sulfate and methane at approximately equimolar ratios over a period of 150 days. The maximum sulfate reduction rate was 5 mu mol sulfate per gram dry weight per day during the incubation period. Diverse archaeal and bacterial clades were retrieved from the sediment with the majority of them clustered with Euryarchaeota, Thaumarcheota, Bacteroidetes, and Proteobacteria. The 16S rRNA gene sequence analysis showed that the sediment from marine Lake Grevelingen contained anaerobic methanotrophic Archaea (ANME) and methanogens as archaeal clades with a role in the methane cycling. ANME at the studied site mainly belong to the ANME-3 clade. This study provides one of the few reports for the presence of ANME-3 in a shallow coastal sediment. Sulfate-reducing bacteria from Desulfobulbus clades were found among the sulfate reducers, however, with very low relative abundance. Desulfobulbus has previously been commonly found associated with ANME, whereas in our study, ANME-3 and Desulfobulbus were not observed simultaneously in clusters, suggesting the possibility of independent AOM by ANME-3.
机译:居住在沿海沉积物中沿海沉积物(荷兰)的浅硫酸盐 - 甲烷过渡区的微生物群落的特征在于,在活性试验中评估了微生物进行甲烷的厌氧氧化氧化甲烷。用甲烷和硫酸盐的沉淀物的体外活性试验表明硫化物产生与硫酸盐和甲烷同时消耗约150天的等摩尔比率。在孵育期间,每克干重量为每克干重量为5μmol硫酸盐。从沉淀物中取出不同的古物和细菌植物,其中大多数与euryarcheoota,thaumarcheota,bacteroides和proteobacteria聚集。 16S rRNA基因序列分析表明,来自海洋湖Grevelingen的沉积物含有厌氧培养型古代(ANME)和甲烷酮作为甲烷循环中作用的古代片状。研究现场的ANME主要属于ANME-3思工。本研究提供了少数报告中的一些报告,用于在浅沿海沉积物中存在Anme-3。然而,在硫酸盐还原剂中发现了从脱硫液的硫酸盐的细菌发现,然而,具有非常低的相对丰度。脱硫常见的是与ANME相关的常见发现,而在我们的研究中,在群集中没有同时观察到ANME-3和脱硫,表明ANME-3的独立AOM的可能性。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

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