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Phylogenetic Diversity and Ecological Pattern of Ammonia-oxidizing Archaea in the Surface Sediments of the Western Pacific

机译:西太平洋表层沉积物中氨氧化古菌的系统发育多样性和生态模式

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摘要

The phylogenetic diversity of ammonia-oxidizing archaea (AOA) was surveyed in the surface sediments from the northern part of the South China Sea (SCS). The distribution pattern of AOA in the western Pacific was discussed through comparing the SCS with other areas in the western Pacific including Changjiang Estuary and the adjacent East China Sea where high input of anthropogenic nitrogen was evident, the tropical West Pacific Continental Margins close to the Philippines, the deep-sea methane seep sediments in the Okhotsk Sea, the cold deep sea of Northeastern Japan Sea, and the hydrothermal field in the Southern Okinawa Trough. These various environments provide a wide spectrum of physical and chemical conditions for a better understanding of the distribution pattern and diversities of AOA in the western Pacific. Under these different conditions, the distinct community composition between shallow and deep-sea sediments was clearly delineated based on the UniFrac PCoA and Jackknife Environmental Cluster analyses. Phylogenetic analyses showed that a few ammonia-oxidizing archaeal subclades in the marine water column/sediment clade and endemic lineages were indicative phylotypes for some environments. Higher phylogenetic diversity was observed in the Philippines while lower diversity in the hydrothermal vent habitat. Water depth and possibly with other environmental factors could be the main driving forces to shape the phylogenetic diversity of AOA observed, not only in the SCS but also in the whole western Pacific. The multivariate regression tree analysis also supported this observation consistently. Moreover, the functions of current and other climate factors were also discussed in comparison of phylogenetic diversity. The information collectively provides important insights into the ecophysiological requirements of uncultured ammonia-oxidizing archaeal lineages in the western Pacific Ocean. © 2011 The Author(s).
机译:在南海北部(SCS)的表层沉积物中调查了氨氧化古细菌(AOA)的系统发育多样性。通过将南海与西南太平洋的其他区域(包括长江口和邻近的东海,其中人为氮的输入量很明显),西太平洋大陆边缘靠近菲律宾的南太平洋海域进行了比较,讨论了西太平洋AOA的分布模式。 ,鄂霍次克海,日本东北海的冷深海以及冲绳海槽南部的热液田中的深海甲烷渗透沉积物。这些不同的环境提供了广泛的物理和化学条件,以便更好地了解西太平洋地区AOA的分布模式和多样性。在这些不同条件下,根据UniFrac PCoA和Jackknife环境聚类分析,清楚地描述了浅海和深海沉积物之间独特的群落组成。系统发育分析表明,海水柱/沉积物进化枝和地方血统中的一些氨氧化古细菌次生细菌在某些环境下是指示性系统型。菲律宾观察到较高的系统发育多样性,而热液喷口栖息地的多样性较低。不仅在南海,而且在整个西太平洋,水深和可能还有其他环境因素也可能是形成AOA系统发育多样性的主要驱动力。多元回归树分析也一致地支持了这一观察。此外,在系统发育多样性比较中还讨论了当前和其他气候因素的功能。这些信息共同提供了对西太平洋未培养的氨氧化古生菌谱系的生态生理要求的重要见解。 ©2011作者。

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  • 作者

    Cao H; Gu JD; Li M; Hong Y;

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  • 年度 2011
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  • 原文格式 PDF
  • 正文语种 eng
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