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首页> 外文期刊>FEMS Microbiology Ecology >Vertical distributions of sulfate-reducing bacteria and methane-producing archaea quantified by oligonucleotide probe hybridization in the profundal sediment of a mesotrophic lake
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Vertical distributions of sulfate-reducing bacteria and methane-producing archaea quantified by oligonucleotide probe hybridization in the profundal sediment of a mesotrophic lake

机译:通过寡核苷酸探针杂交定量测定的中营养湖泊底泥中的硫酸盐还原细菌和产甲烷古菌的垂直分布

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Vertical distributions of sulfate-reducing bacteria and metbane-producing archaea were investigated in the profundal sediment of a freshwater lake using membrane-immobilized small subunit rRNA hybridization with group- and genus-specific oligonucleotide probes. The annual average of the relative abundance of small subunit rRNA hybridized with all probes for sulfate-reducing bacteria to total small subunit rRNA was 2.3% at 0-2 cm and increased with depth up to 22.9% at 8-14 cm where sulfate concentration was less than 10 nmol ml(-1) in interstitial water, suggesting that these bacteria may survive on alternative metabolisms. The signal of probe Dsv687 (the family Desulfovibrionaceae and some Geohacteraceae) was the main factor in this increase. The relative abundance of methane-producing archaea to total small subunit rRNA was highest (7.8%) at 8-14 cm, dominated by the order Methanosarcinales. The metabolic rates measured in the sediments demonstrated that the peaks of sulfate reduction and methane production were separated vertically, and were not linked to their small subunit rRNA distributions. Our data indicate that sulfate-reducing bacteria can coexist with methane-producing archaea from 0 to 20 cm in the freshwater lake sediment. (C) 2003 Federation of European Microbiological Societies. Published by Elsevier Science B.V. All rights reserved. [References: 47]
机译:使用膜固定的小亚基rRNA杂交组特异性和属特异性寡核苷酸探针,研究了淡水湖泊深层沉积物中硫酸盐还原细菌和产甲烷的古细菌的垂直分布。与所有硫酸盐还原细菌探针杂交的小亚基rRNA相对于总小亚基rRNA的年平均相对丰度在0-2 cm时为2.3%,并在8-14 cm时深度增加至22.9%,其中硫酸盐浓度为间隙水中的水少于10 nmol ml(-1),表明这些细菌可能在新陈代谢中存活。探针Dsv687(脱硫弧菌科和一些土生动物科)的信号是这种增加的主要因素。产甲烷的古细菌相对于总的小亚基rRNA的相对丰度最高(7.8%),位于8-14 cm,主要由甲烷八叠球菌组成。在沉积物中测得的代谢率表明,硫酸盐还原和甲烷生成的峰在垂直方向上是分开的,并且与它们小的亚基rRNA分布无关。我们的数据表明,在淡水湖沉积物中,硫酸盐还原细菌可以与甲烷生成古细菌共存,范围为0至20 cm。 (C)2003年欧洲微生物学会联合会。由Elsevier Science B.V.保留所有权利。 [参考:47]

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