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Molecular and lipid biomarker analysis of a gypsum-hosted endoevaporitic microbial community

机译:石膏宿主的内蒸发微生物群落的分子和脂质生物标志物分析

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摘要

Modern evaporitic microbial ecosystems are important analogs for understanding the record of earliest life on Earth. Although mineral-depositing shallow-marine environments were prevalent during the Precambrian, few such environments are now available today for study. We investigated the molecular and lipid biomarker composition of an endoevaporitic gypsarenite microbial mat community in Guerrero Negro, Mexico. The 16S ribosomal RNA gene-based phylogenetic analyses of this mat corroborate prior observations indicating that characteristic layered microbial communities colonize gypsum deposits world-wide despite considerable textural and morphological variability. Membrane fatty acid analysis of the surface tan/orange and lower green mat crust layers indicated cell densities of 1.6x10(9) and 4.2x10(9)cellscm(-3), respectively. Several biomarker fatty acids, 7,10-hexadecadienoic, iso-heptadecenoic, 10-methylhexadecanoic, and a 12-methyloctadecenoic, correlated well with distributions of Euhalothece, Stenotrophomonas, Desulfohalobium, and Rhodobacterales, respectively, revealed by the phylogenetic analyses. Chlorophyll (Chl) a and cyanobacterial phylotypes were present at all depths in the mat. Bacteriochlorophyl (Bchl) a and Bchl c were first detected in the oxic-anoxic transition zone and increased with depth. A series of monomethylalkanes (MMA), 8-methylhexadecane, 8-methylheptadecane, and 9-methyloctadecane were present in the surface crust but increased in abundance in the lower anoxic layers. The MMA structures are similar to those identified previously in cultures of the marine Chloroflexus-like organism Candidatus Chlorothrix halophila' gen. nov., sp. nov., and may represent the Bchl c community. Novel 3-methylhopanoids were identified in cultures of marine purple non-sulfur bacteria and serve as a probable biomarker for this group in the lower anoxic purple and olive-black layers. Together microbial culture and environmental analyses support novel sources for lipid biomarkers in gypsum crust mats.
机译:现代的蒸发微生物生态系统是理解地球最早生命记录的重要类似物。尽管在前寒武纪期间沉积矿床的浅海环境普遍存在,但如今几乎没有这样的环境可供研究。我们调查了墨西哥格雷罗内格罗(Guerrero Negro)的内蒸发型石膏质微生物垫群落的分子和脂质生物标志物组成。该垫的基于16S核糖体RNA基因的系统发育分析证实了先前的观察结果,尽管结构和形态存在相当大的变异性,但特征性分层微生物群落仍在世界范围内遍及石膏沉积物。对表面棕褐色/橙色和下部绿色毡壳层的膜脂肪酸分析表明,细胞密度分别为1.6x10(9)和4.2x10(9)cellscm(-3)。系统发育分析揭示了几种生物标记脂肪酸,分别是7,10-十六碳二烯酸,异十七碳烯酸,10-甲基十六碳烯酸和12-甲基十八碳烯酸,与Euhalothece,Stenotrophomonas,Desulfohalobium和Rhodobacterales的分布密切相关。叶绿素(Chl)a和蓝细菌系统型存在于垫子的所有深度。细菌叶绿素(Bchl)a和Bchl c首先在有氧-缺氧过渡区中检测到,并随深度增加而增加。一系列的单甲基烷烃(MMA),8-甲基十六烷,8-甲基十七烷和9-甲基十八烷存在于地壳中,但在下部缺氧层中的丰度增加。 MMA的结构与以前在类似海洋弯曲杆菌的生物念珠菌嗜盐梭状芽胞杆菌基因中的鉴定相似。十一月,sp。 11月,可能代表Bchl c社区。在海洋紫色非硫细菌的培养物中鉴定出了新型的3-甲基类胡萝卜素,它们在较低的缺氧紫色和橄榄黑层中可作为该组的生物标记。微生物培养和环境分析共同支持了石膏硬皮垫中脂质生物标志物的新来源。

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