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Diversity and abundance of anammox bacterial community in the deep-ocean surface sediment from equatorial Pacific

机译:赤道太平洋深海表层沉积物中厌氧氨氧化细菌群落的多样性和丰度

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The community structure and diversity of anaerobic ammonium oxidation (anammox) bacteria in the surface sediments of equatorial Pacific were investigated by phylogenic analysis of 16S rRNA and hydrazine oxidoreductase (hzo) genes and PCoA (principal coordinates analysis) statistical analysis. Results indicated that 16S rRNA and hzo sequences in the P2 (off the center of western Pacific warm pool) and P3 (in the eastern equatorial Pacific) sites all belong to the Candidatus "Scalindua", the dominate anammox bacteria in the low-temperature marine environment proved by previous studies. However, in the P1 site (in center of warm pool of western Pacific), large part of 16S rRNA gene sequences formed a separated cluster. Meanwhile, hzo gene sequences from P1 sediment also grouped into a single cluster. PCoA analysis demonstrated that the anammox community structure in the P1 has significant geographical distributional difference from that of P2, P3, and other marine environments based on 16S rRNA and hzo genes. The abundances of anammox bacteria in surface sediments of equatorial Pacific were quantified by q-PCR analysis of hzo genes, which ranged from 3.98 × 10~3 to 1.17 × 10~4 copies g-1 dry sediments. These results suggested that a special anammox bacteria phylotypes exist in the surface sediment of the western Pacific warm pool, which adapted to the specific habitat and maybe involved in the nitrogen loss process from the fixed inventory in the habitat.
机译:通过对16S rRNA和肼氧化还原酶(hzo)基因的系统发育分析以及PCoA(主要坐标分析)统计分析,研究了赤道​​太平洋表层沉积物中厌氧铵氧化细菌的群落结构和多样性。结果表明,P2(位于西太平洋暖池中心)和P3(位于赤道东太平洋)位点的16S rRNA和hzo序列均属于低温海洋中主要的厌氧细菌念珠菌“ Scalindua”。以前的研究证明环境。然而,在P1位点(在西太平洋暖池中心),大部分16S rRNA基因序列形成了一个分离的簇。同时,P1沉积物中的hzo基因序列也分组为一个簇。 PCoA分析表明,P1中的厌氧菌群落结构与P2,P3和其他基于16S rRNA和hzo基因的海洋环境具有明显的地理分布差异。通过hzo基因的q-PCR分析定量了赤道太平洋表层沉积物中的厌氧细菌的丰度,其范围从3.98×10〜3到1.17×10〜4个g-1干沉积物。这些结果表明,在西太平洋暖池的表层沉积物中存在特殊的厌氧细菌菌系,其适应于特定的生境,并可能从生境中的固定种群中参与了氮的损失过程。

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