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首页> 外文期刊>Geobiology >Direct in situ detection of cells in deep-sea sediment cores from the Peru Margin (ODP Leg 201, Site 1229)
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Direct in situ detection of cells in deep-sea sediment cores from the Peru Margin (ODP Leg 201, Site 1229)

机译:直接就地检测秘鲁边界的深海沉积物芯中的细胞(ODP Leg 201,Site 1229)

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摘要

Microbiological investigations of deep-sea sediments recovered from the Peru Margin during the ODP Leg 201 (Hole 1229A, 1-110 mbsf) demonstrated that microoganisms were a consistent component throughout the profile. Optimization of the dilution factorand DAPI-staining procedures for direct cell counts allowed the determination of the abundance of the entire microbial community, which was about 10~8 cells per g dry sediment, Microbial diversity in discrete samples taken from the 110-m profile was analysed using horseradish-peroxydase-rRNA-probes. In general, the majority of the detected cells belonged to the Eubacteria kingdom with a domin -ance of sulphate-reducing bacteria. The composition of the suflate-reducing community varied with depth. Desulfobacteriaceae were dominant in the uppermost sulphate-reducing zone and Desulfovibrionaceae at deeper depths in the upward diffusing sulphate-rich brines. Both sulphate-reducing groups were also detected in the methanogenic zone. Similarly, Archaea were detected throughout the profile, not only in the methano-genic zone but also in the upper and lower sulphate-reducing zones.
机译:在ODP腿201(Hole 1229A,1-110 mbsf)期间从秘鲁边界回收的深海沉积物的微生物学研究表明,微生物是整个剖面中一致的成分。通过对稀释因子和DAPI染色程序进行直接细胞计数的优化,可以确定整个微生物群落的丰度,即每克干沉积物中约有10〜8个细胞。从110米剖面获得的离散样品中的微生物多样性为使用辣根过氧化物酶-rRNA探针进行分析。通常,大多数检测到的细胞都属于真细菌界,主要具有减少硫酸盐的细菌。减少亚硫酸盐的群落的组成随深度而变化。在最上方的硫酸盐还原带中,脱硫细菌科占主导地位,而在向上扩散的富含硫酸盐的盐水中,更深的深度是脱硫弧菌科。在产甲烷区也检测到了两个硫酸盐还原基团。同样,古细菌在整个剖面中都被检测到,不仅在甲烷生成区,而且在硫酸盐还原区的上,下层都被检测到。

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