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Effects of ecological engineered oxygenation on the bacterial community structure in an anoxic fjord in western Sweden

机译:生态工程氧合对瑞典西部缺氧峡湾细菌群落结构的影响

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摘要

Oxygen-depleted bodies of water are becoming increasingly common in marine ecosystems. Solutions to reverse this trend are needed and under development, for example, by the Baltic deep-water OXygenation (BOX) project. In the framework of this project, the Swedish Byfjord was chosen for a pilot study, investigating the effects of an engineered oxygenation on long-term anoxic bottom waters. The strong stratification of the water column of the Byfjord was broken up by pumping surface water into the deeper layers, triggering several inflows of oxygen-rich water and increasing oxygen levels in the lower water column and the benthic zone up to 110 μmol l−1.We used molecular ecologic methods to study changes in bacterial community structure in response to the oxygenation in the Byfjord. Water column samples from before, during and after the oxygenation as well as from two nearby control fjords were analyzed. Our results showed a strong shift in bacterial community composition when the bottom water in the Byfjord became oxic. Initially dominant indicator species for oxygen minimum zones such as members of the SUP05 clade declined in abundance during the oxygenation event and nearly vanished after the oxygenation was accomplished. In contrast, aerobic species like SAR11 that initially were restricted to surface waters could later be detected deep into the water column. Overall, the bacterial community in the formerly anoxic bottom waters changed to a community structure similar to those found in oxic waters, showing that an engineered oxygenation of a large body of anoxic marine water is possible and emulates that of a natural oxygenation event.
机译:缺氧水体在海洋生态系统中变得越来越普遍。需要逆转这种趋势的解决方案,并且正在开发中,例如,波罗的海深水制氧(BOX)项目。在该项目的框架中,选择了瑞典比弗峡湾进行试点研究,以研究工程化氧合对长期缺氧底水的影响。通过将地表水泵入更深的层,破坏了比尔峡湾水柱的强烈分层,触发了几次富氧水的流入,并增加了下部水柱和底栖地带的氧气含量,最高可达110μmol·l -1 。我们使用分子生态学方法研究了比弗峡湾中氧合作用对细菌群落结构的影响。分析了氧合之前,期间和之后以及附近两个控制峡湾的水柱样品。我们的结果显示,当Byfjord的底部水变成有氧时,细菌群落组成发生了很大变化。最初,氧最低区域的主要指示剂种类(例如SUP05进化枝的成员)在氧合过程中丰度下降,在氧合完成后几乎消失。相反,最初仅限于地表水的好氧物种如SAR11后来可以在水柱深处被检测到。总体而言,以前缺氧的底水中细菌群落变成了类似于在含氧水中发现的群落结构,这表明可以对大量的缺氧海水进行工程氧化,并且可以模拟自然的氧合事件。

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