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首页> 外文期刊>Applied Microbiology >Intact Polar and Core Glycerol Dibiphytanyl Glycerol Tetraether Lipids of Group I.1a and I.1b Thaumarchaeota in Soil
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Intact Polar and Core Glycerol Dibiphytanyl Glycerol Tetraether Lipids of Group I.1a and I.1b Thaumarchaeota in Soil

机译:I.1a和I.1b伞菌科土壤中完整的极性和核心甘油双双植物基甘油四醚脂

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Ecological studies of thaumarchaeota often apply glycerol dibiphytanyl glycerol tetraether (GDGT)-based intact membrane lipids. However, these components have only been characterized for thaumarchaeota from aquatic environments. Thaumarchaeota have been shown to play an important role in the nitrogen cycle in soil as ammonium oxidizers, and GDGTs are common lipids encountered in soil. We report the core and intact polar lipid (IPL) GDGTs produced by three newly available thaumarchaeota isolated from grassland soil in Austria (“ Nitrososphaera viennensis ,” group I.1b) and enriched from agricultural soils in South Korea (“ Candidatus Nitrosoarchaeum koreensis” MY1, group I.1a; and “ Candidatus Nitrososphaera” strain JG1, group I.1b). The soil thaumarchaeota all synthesize crenarchaeol as their major core GDGT, in agreement with the fact that crenarchaeol has also been detected in thaumarchaeota from aquatic environments. The crenarchaeol regioisomer apparently is produced in significant quantities only by soil thaumarchaeota of the I.1b subgroup. In addition, GDGTs with 0 to 4 cyclopentane moieties and GDGTs containing an additional hydroxyl group were detected. The IPL head groups of their membrane lipids comprised mainly monohexose, dihexose, trihexose, phosphohexose, and hexose-phosphohexose moieties. The hexose-phosphohexose head group bound to crenarchaeol occurred in all soil thaumarchaeota, and this IPL is at present the only lipid that is detected in all thaumarchaeota analyzed so far. This specificity and its lability indicate that it is the most suitable biomarker lipid to trace living thaumarchaeota. This study, in combination with previous studies, also suggests that hydroxylated GDGTs occur in the I.1a, but not in the I.1b, subgroup of the thaumarchaeota.
机译:thaumarchaeota的生态学研究通常会使用基于甘油双双植物基甘油四醚(GDGT)的完整膜脂质。但是,这些成分仅针对水生环境中的金藻。已经证明,伞菌在土壤中的氮循环中起铵氧化剂的作用,而GDGTs是土壤中常见的脂质。我们报告了从奥地利草地土壤(“ Nitrososphaera viennensis”,I.1b组)中分离出的三个新近获得的thaumarchaeota和韩国(“ Candidatus Nitrosoarchaeum koreensis” MY1)从农业土壤中富集的三种新获得的thaumarchaeota产生的核心和完整的极性脂质(IPL)GDGT。 ,I.1a组;以及“白色念珠菌”菌株JG1,I.1b组)。土壤thaumarchaeota都合成了crenarchaeol作为其主要核心GDGT,这与在水生环境中thaumarchaeota中也检测到crenarchaeol的事实是一致的。环戊烯醇区域异构体显然仅由I.1b亚组的土壤thaumarchaeota产生。另外,检测到具有0至4个环戊烷部分的GDGT和含有额外羟基的GDGT。它们的膜脂质的IPL头基主要包括单己糖,二己糖,三己糖,磷酸己糖和己糖-磷酸己糖部分。绑定到Crenarchaeol的己糖-磷酸己糖头基存在于所有土壤thaumarchaeota中,该IPL是目前为止在所有thaumarchaeota中检测到的唯一脂质。这种特异性及其不稳定性表明它是最适合追踪活的伞菌的生物标志物脂质。这项研究与以前的研究相结合,还表明羟基化的GDGTs在thaumarchaeota的亚群I.1a中发生,而不在I.1b中发生。

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