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Near-Bottom Hypoxia Impacts Dynamics of Bacterioplankton Assemblage throughout Water Column of the Gulf of Finland (Baltic Sea)

机译:近底部低氧影响整个芬兰湾(波罗的海)水柱中的浮游细菌组装动力学

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摘要

Over the past century the spread of hypoxia in the Baltic Sea has been drastic, reaching its ‘arm’ into the easternmost sub-basin, the Gulf of Finland. The hydrographic and climatological properties of the gulf offer a broad suite of discrete niches for microbial communities. The current study explores spatiotemporal dynamics of bacterioplankton community in the Gulf of Finland using massively parallel sequencing of 16S rRNA fragments obtained by amplifying community DNA from spring to autumn period. The presence of redoxcline and drastic seasonal changes make spatiotemporal dynamics of bacterioplankton community composition (BCC) and abundances in such estuary remarkably complex. To the best of our knowledge, this is the first study that analyses spatiotemporal dynamics of BCC in relation to phytoplankton bloom throughout the water column (and redoxcline), not only at the surface layer. We conclude that capability to survive (or benefit from) shifts between oxic and hypoxic conditions is vital adaptation for bacteria to thrive in such environments. Our results contribute to the understanding of emerging patterns in BCCs that occupy hydrographically similar estuaries dispersed all over the world, and we suggest the presence of a global redox- and salinity-driven metacommunity. These results have important implications for understanding long-term ecological and biogeochemical impacts of hypoxia expansion in the Baltic Sea (and similar ecosystems), as well as global biogeography of bacteria specialized inhabiting similar ecosystems.
机译:在过去的一个世纪中,低氧在波罗的海的蔓延十分剧烈,到达了其“支臂”,进入了最东部的次流域芬兰湾。海湾的水文和气候特性为微生物群落提供了广泛的离散生态位。本研究使用从春季到秋季扩增群落DNA的16S rRNA片段的大规模平行测序方法,探索了芬兰湾浮游细菌群落的时空动态。氧化还原菌的存在和剧烈的季节变化使浮游细菌群落组成(BCC)的时空动态和河口中的丰度非常复杂。据我们所知,这是第一个分析BCC与整个水柱(和氧化还原层)中不仅在表层的浮游植物开花有关的时空动态的研究。我们得出的结论是,在有氧和低氧条件之间转换的生存能力(或从中受益)是细菌在此类环境中壮成长的重要适应条件。我们的结果有助于理解BCC中新兴的模式,这些BCC占据了分布在世界各地的与水文相似的河口,并且我们建议存在一个由氧化还原和盐度驱动的全球性元社区。这些结果对于了解低氧在波罗的海(和类似生态系统)中的长期生态和生物地球化学影响,以及对居住在类似生态系统中的细菌的全球生物地理学具有重要意义。

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