Harrison Benjamin K, Zhang Husen, Berelson Will, Orphan Victoria J
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA.
Appl Environ Microbiol. 2009 Mar;75(6):1487-99. doi: 10.1128/AEM.01812-08. Epub 2009 Jan 9.
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.
硫酸盐-甲烷过渡带(SMTZ)是大陆边缘广泛存在的一个特征,代表着一个受扩散控制的界面,这里微生物活动增强。SMTZ的微生物活动通常与甲烷的厌氧氧化(AOM)有关,这是由硫酸盐还原菌和甲烷氧化古菌之间的互营共生关系来进行的。虽然我们对催化AOM的微生物的理解已有进展,但与SMTZ相关的更广泛微生物群落的多样性和生态作用尚未得到很好的描述。在本研究中,描述了圣巴巴拉盆地SMTZ上方、内部和下方的微生物多样性。与ANME-1相关的古菌系统发育型似乎是圣巴巴拉盆地SMTZ中的主要甲烷氧化菌,相关甲基辅酶M还原酶基因(mcrA)的独家回收独立支持了这一点。通过异化亚硫酸盐还原酶(dsr)基因多样性分析证实,与脱硫杆菌目和脱硫八叠球菌-脱硫球菌进化枝相关的硫酸盐还原δ-变形菌系统发育型在SMTZ中也有富集。统计方法表明,从与地球化学定义的SMTZ相关的两个层位中回收的微生物群落之间存在密切关系,这可以与从富含硫酸盐的上覆层位和过渡带下方富含甲烷的沉积物中回收的微生物多样性区分开来。将圣巴巴拉盆地SMTZ的微生物群落与甲烷冷泉和其他富含有机物的沉积环境的微生物群落进行比较表明,通常与AOM无关的细菌类群,如浮霉菌门和候选分类群JS1,在SMTZ中也有额外的富集,可能代表了全球许多SMTZ环境中常见的细菌特征。