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Seasonal and interannual variability of the marine bacterioplankton community throughout the water column over ten years

机译:十年来整个水域海洋浮游植物群落的季节性和年际变化

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摘要

Microbial activities that affect global oceanographic and atmospheric processes happen throughout the water column, yet the long-term ecological dynamics of microbes have been studied largely in the euphotic zone and adjacent seasonally mixed depths. We investigated temporal patterns in the community structure of free-living bacteria, by sampling approximately monthly from 5 m, the deep chlorophyll maximum (∼15–40 m), 150, 500 and 890 m, in San Pedro Channel (maximum depth 900 m, hypoxic below ∼500 m), off the coast of Southern California. Community structure and biodiversity (inverse Simpson index) showed seasonal patterns near the surface and bottom of the water column, but not at intermediate depths. Inverse Simpson's index was highest in the winter in surface waters and in the spring at 890 m, and varied interannually at all depths. Biodiversity appeared to be driven partially by exchange of microbes between depths and was highest when communities were changing slowly over time. Meanwhile, communities from the surface through 500 m varied interannually. After accounting for seasonality, several environmental parameters co-varied with community structure at the surface and 890 m, but not at the intermediate depths. Abundant and seasonally variable groups included, at 890 m, Nitrospina, Flavobacteria and Marine Group A. Seasonality at 890 m is likely driven by variability in sinking particles, which originate in surface waters, pass transiently through the middle water column and accumulate on the seafloor where they alter the chemical environment. Seasonal subeuphotic groups are likely those whose ecology is strongly influenced by these particles. This surface-to-bottom, decade-long, study identifies seasonality and interannual variability not only of overall community structure, but also of numerous taxonomic groups and near-species level operational taxonomic units.
机译:影响全球海洋和大气过程的微生物活动遍及整个水域,但是对微生物的长期生态动力学的研究主要集中在富营养区和邻近的季节性混合深度。我们通过从圣佩德罗海峡(最大深度为900 m)的5 m处,大约每月一次从5 m(深叶绿素最大值(约15–40 m),150、500和890 m),大约每月取样,研究了自由活动细菌的群落结构的时间模式。 ,在〜500 them以下为低氧),位于南加州沿海。群落结构和生物多样性(辛普森指数倒数)在水柱表面和底部附近表现出季节性格局,但在中间深度却没有。冬季,地表水和春季的辛普森指数都最高,为890 m,并且在所有深度每年都有变化。生物多样性似乎是由不同深度之间的微生物交换所部分驱动的,而当社区随着时间的推移缓慢变化时,生物多样性是最高的。同时,从地表到500μm的群落每年都在变化。考虑季节性因素后,表层和890 m处的几个环境参数与群落结构共同变化,但在中间深度则没有变化。 890 m,Nitrospina,Flavobacteria和Marine A组包括大量和季节性可变的组。890m的季节性可能受下沉颗粒的变化驱动,这些下沉颗粒起源于地表水,暂时穿过中间水柱并积聚在海底他们在那里改变化学环境。季节性的亚光群体可能是那些生态受到这些颗粒强烈影响的群体。这项从下到下的长达十年的研究不仅确定了整个社区结构的季节性和年际变化,而且还确定了许多生物分类群和近物种水平的操作生物分类单位的季节性和年际变化。

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