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Variations in Archaeal and Bacterial Diversity Associated with the Sulfate-Methane Transition Zone in Continental Margin Sediments (Santa Barbara Basin California)

机译:与大陆边缘沉积物中硫酸盐-甲烷过渡区相关的古细菌和细菌多样性的变化(加利福尼亚州圣巴巴拉盆地)

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摘要

The sulfate-methane transition zone (SMTZ) is a widespread feature of continental margins, representing a diffusion-controlled interface where there is enhanced microbial activity. SMTZ microbial activity is commonly associated with the anaerobic oxidation of methane (AOM), which is carried out by syntrophic associations between sulfate-reducing bacteria and methane-oxidizing archaea. While our understanding of the microorganisms catalyzing AOM has advanced, the diversity and ecological role of the greater microbial assemblage associated with the SMTZ have not been well characterized. In this study, the microbial diversity above, within, and beneath the Santa Barbara Basin SMTZ was described. ANME-1-related archaeal phylotypes appear to be the primary methane oxidizers in the Santa Barbara Basin SMTZ, which was independently supported by exclusive recovery of related methyl coenzyme M reductase genes (mcrA). Sulfate-reducing Deltaproteobacteria phylotypes affiliated with the Desulfobacterales and Desulfosarcina-Desulfococcus clades were also enriched in the SMTZ, as confirmed by analysis of dissimilatory sulfite reductase (dsr) gene diversity. Statistical methods demonstrated that there was a close relationship between the microbial assemblages recovered from the two horizons associated with the geochemically defined SMTZ, which could be distinguished from microbial diversity recovered from the sulfate-replete overlying horizons and methane-rich sediment beneath the transition zone. Comparison of the Santa Barbara Basin SMTZ microbial assemblage to microbial assemblages of methane seeps and other organic matter-rich sedimentary environments suggests that bacterial groups not typically associated with AOM, such as Planctomycetes and candidate division JS1, are additionally enriched within the SMTZ and may represent a common bacterial signature of many SMTZ environments worldwide.
机译:硫酸盐甲烷转换区(SMTZ)是大陆边缘的一个普遍特征,代表了扩散控制的界面,微生物活动增强。 SMTZ微生物活性通常与甲烷的厌氧氧化(AOM)有关,这是通过减少硫酸盐的细菌与甲烷氧化的古细菌之间的同养关联来进行的。虽然我们对催化AOM的微生物的理解已经提高,但与SMTZ相关的更大的微生物组合的多样性和生态作用尚未得到很好的表征。在这项研究中,描述了圣巴巴拉盆地SMTZ之上,之内和之下的微生物多样性。 ANME-1相关的古细菌系统型似乎是圣塔芭芭拉盆地SMTZ的主要甲烷氧化剂,其得到相关甲基辅酶M还原酶基因(mcrA)的独家回收得到独立支持。通过对异亚硫酸盐还原酶(dsr)基因多样性的分析证实,与脱硫细菌和脱硫球菌-脱硫球菌进化枝相关的减少硫酸盐的Deltaproteobacteria系统型也很丰富。统计方法表明,从与地球化学定义的SMTZ相关的两个地层中回收的微生物组合之间存在密切的关系,这可以与从富含硫酸盐的上地层中回收的微生物多样性和过渡带下方的富含甲烷的沉积物区别开来。圣塔芭芭拉盆地SMTZ微生物组合与甲烷渗漏和其他富含有机物的沉积环境的微生物组合的比较表明,通常与AOM不相关的细菌类,例如浮萍菌和候选类JS1,在SMTZ内另外富集,可能代表全球许多SMTZ环境的常见细菌特征。

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