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An improved fluorescence in situ hybridization protocol for the identification of bacteria and archaea in marine sediments

机译:一种改进的荧光原位杂交方案,用于鉴定海洋沉积物中的细菌和古细菌

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In situ identification of prokaryotic cells in subsurface sediments is hampered by the low cellular rRNA contents of the target organisms. Fluorescence in situ hybridization with catalyzed reporter deposition (CARD-FISH) has the potential to overcome this limitation, and was therefore optimized for a 40 cm deep sediment core sampled from a tidal sandy flat of the German Wadden Sea. Treatment with methanol and H2O2 inactivated endogenous peroxidases and effectively reduced the background signal. Percentage of DAPI stained cells detected with the probe combination EUB(I-III), targeting nearly all the Bacteria, were comparable for CARD-FISH with a horseradish peroxidase (HRP)-labeled probe and FISH with a fluorescently monolabeled probe in the 2-3 cm depth interval (92% and 82%, respectively), but significantly higher with the HRP-labeled probe at 35-40 cm, the deepest layer sampled (63% with HRP vs. 26% with monolabeled probe). With CARD-FISH Alphaproteobacteria and the Desuflobulbaceae group of sulfate-reducing bacteria were detected only in the upper layers. In contrast, Desulfiosarcinales, the Bacteroidetes group, Planctomycetes, Betaproteobacteria, and Gammaproteobacteria were found at all depths. Archaea were detectable with ARCH915-HRP after achromopeptidase treatment. Surprisingly, aggregates of Bacteria and Archaea were found, below 12 cm depth, that strongly resemble consortia involved in anoxic oxidation of methane that have previously been found in sediments near methane hydrate deposits. With the optimized CARD-FISH protocol, microbial populations could also be detected in deeper sediment horizons. Furthermore, the intensity of the CARD-FISH signals improved detection of rare organisms such as Archaea. (C) 2004 Federation of European Microbiological Societies. Published by Elsevier B.V. All rights reserved.
机译:靶标生物的低细胞rRNA含量阻碍了地下沉积物中原核细胞的原位鉴定。荧光原位杂交与催化报道分子沉积(CARD-FISH)具有克服这一局限性的潜力,因此针对从德国沃登海潮汐沙质平地取样的40厘米深的沉积岩心进行了优化。用甲醇和H2O2处理可灭活内源性过氧化物酶并有效降低背景信号。用探针组合EUB(I-III)靶向几乎所有细菌的DAPI染色细胞的百分比与使用辣根过氧化物酶(HRP)标记的探针的CARD-FISH和使用荧光单标记探针的FISH(2- 3厘米深度间隔(分别为92%和82%),但在35-40厘米处使用HRP标记的探针显着更高,这是采样的最深层(HRP分别为63%和单标记探针的26%)。使用CARD-FISH时,仅在上层中检测到了Alteproteobacteria细菌和Desuflobulbaceae组的硫酸盐还原菌。相反,在所有深度都发现了脱硫龙,拟杆菌属,扁平菌,β变形杆菌和γ变形杆菌。染色体肽酶处理后,用ARCH915-HRP可检测到古细菌。出乎意料的是,发现细菌和古细菌的聚集体在12 cm深度以下,非常类似于先前在甲烷水合物矿床附近的沉积物中发现的参与甲烷缺氧氧化的财团。通过优化的CARD-FISH方案,还可以在更深的沉积层中检测到微生物种群。此外,CARD-FISH信号的强度改善了对稀有生物(如古细菌)的检测。 (C)2004年欧洲微生物学会联合会。由Elsevier B.V.发布。保留所有权利。

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