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西太平洋暖池深海沉积物中古菌的系统发育分析。

Phylogenetic analysis of Archaea in the deep-sea sediments of west Pacific Warm Pool.

作者信息

Wang Peng, Xiao Xiang, Wang Fengping

机构信息

College of Marine Life Science, Ocean University of China, Qingdao, PR China.

出版信息

Extremophiles. 2005 Jun;9(3):209-17. doi: 10.1007/s00792-005-0436-5. Epub 2005 Mar 11.

Abstract

Archaea are known to play important roles in carbon cycling in marine sediments. The main compositions of archaeal community in five deep-sea sediment samples collected from west Pacific Warm Pool area (WP-0, WP-1, WP-2, WP-3, WP-4), and in five sediment layers (1 cm-, 3 cm-, 6 cm-, 10 cm-, 12 cm- layer) of the 12 cm sediment core of WP-0 were checked and compared by denaturing gradient gel electrophoresis and 16 S rRNA gene sequencing. It was revealed that all the deep-sea sediment samples checked contained members of non-thermophilic marine group I crenarchaeota as the predominant archaeal group. To further detect groups of archaea possibly relating with C1 metabolism, PCR amplification was carried out using primers targeting methane-oxidizing archaea. Although no methane-oxidizing archaea was detected, a group of novel archaea (named as WPA) was instead identified from all these five WP samples by clone analysis. They could be placed in the euryarchaeota kingdom, separated into two distinct groups, the main group was peripherally related with methanogens, the other group related with Thermoplasma. The vertical distributions of WPA, archaea and bacteria along the WP-0 sediment column were determined by quantitative-PCR. It was found that bacteria dominated at all depths, the numbers of bacteria were 10-10(4) times more than those of archaea. The proportion of archaea versus bacteria had a depth related increasing tendency, it was lowest at the first layer (0.01%), reached highest at the 12 cm- layer (10%). WPA only constituted a small proportion of the archaeal community (0.05% to 5%) of west Pacific Warm Pool sediment.

摘要

已知古菌在海洋沉积物的碳循环中发挥着重要作用。通过变性梯度凝胶电泳和16S rRNA基因测序,对从西太平洋暖池区域采集的5个深海沉积物样本(WP - 0、WP - 1、WP - 2、WP - 3、WP - 4)以及WP - 0的12厘米沉积物岩芯的5个沉积层(1厘米层、3厘米层、6厘米层、10厘米层、12厘米层)中古菌群落的主要组成进行了检测和比较。结果表明,所有检测的深海沉积物样本中均含有非嗜热海洋I类泉古菌成员作为主要古菌类群。为了进一步检测可能与C1代谢相关的古菌类群,使用靶向甲烷氧化古菌的引物进行了PCR扩增。虽然未检测到甲烷氧化古菌,但通过克隆分析从所有这5个WP样本中鉴定出了一组新型古菌(命名为WPA)。它们可归入广古菌界,分为两个不同的组,主要组与产甲烷菌有外围关系,另一组与嗜热栖热菌有关。通过定量PCR测定了WPA、古菌和细菌沿WP - 0沉积柱的垂直分布。结果发现,细菌在所有深度均占主导地位,细菌数量比古菌多10 - 10⁴倍。古菌与细菌的比例有随深度增加的趋势,在第一层最低(0.01%),在12厘米层最高(10%)。WPA仅占西太平洋暖池沉积物古菌群落的一小部分(0.05%至5%)。

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