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Evidence of biogeography in surface ocean bacterioplankton assemblages

机译:表层海洋浮游生物组合中生物地理学的证据

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Regardless of the importance of bacterial assemblages as essential components of ecosystems, little is knownabout how their populations are structured. We analyzed the composition and turnover rates, based on 16SrDNA sequences, of surface water oceanic bacterial assemblages of the fraction between 0.1 and 0.8 pm along alatitudinal gradient (45°6'42"N in the North Atlantic to 15°8'37"S in the South Pacific) including geographicdistance, temperature, chlorophyll a and salinity. Here we show that oceanic bacterial assemblages between0.1 and 0.8 pm, can be structured by a variety of environmental interactions that include separation by distanceand chlorophyll a concentration in temperate North Atlantic coastal samples and temperature in tropicalAtlantic and Pacific coastal and open ocean samples. Bacterial phyla composition diverged between temperateand tropical regions. This study suggests that some bacterial assemblages could be structured both byenvironmental and spatial factors, while others by environmental factors alone.
机译:不管细菌集合作为生态系统的基本组成部分的重要性如何,对其种群的结构如何都知之甚少。我们基于16SrDNA序列分析了沿垂直梯度(北大西洋45°6'42“ N至15°8'37” S沿0.1至0.8 pm的表面水海洋细菌组合的组成和周转率在南太平洋),包括地理距离,温度,叶绿素a和盐度。在这里,我们表明,0.1至0.8 pm之间的海洋细菌集合可以通过多种环境相互作用来构造,包括通过距离和叶绿素的分离来分离北温带沿海样本中的浓度以及热带大西洋和太平洋沿海和远洋样本中的温度。细菌门的组成在温带和热带地区之间有所不同。这项研究表明,某些细菌集合体可以由环境和空间因素构成,而另一些细菌仅由环境因素构成。

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