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Acidification alters the composition of ammonia-oxidizing microbial assemblages in marine mesocosms

机译:酸化改变了海洋生物膜中氨氧化微生物组合的组成

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Increasing atmospheric CO_2 concentrations are causing decreased pH over vast expanses of the ocean. This decreasing pH may alter bio-geochemical cycling of carbon and nitrogen via the microbial process of nitrification, a key process that couples these cycles in the ocean, but which is often sensitive to acidic conditions. Recent reports have indicated a decrease in oceanic nitrification rates under experimentally lowered pH. How the composition and abundance of ammonia-oxidizing bacteria (AOB) and archaea (AOA) assemblages respond to decreasing oceanic pH is unknown. We sampled microbes from 2 different acidification experiments and used a combination of qPCR and functional gene microarrays for the ammonia monooxygenase gene (amoA) to assess how acidification alters the structure of ammonia oxidizer assemblages. We show that despite widely different experimental conditions, acidification consistently altered the community composition of AOB by increasing the relative abundance of taxa related to the Nitrosomonas ureae clade. In one experiment, this increase was sufficient to cause an increase in the overall abundance of AOB. There were no systematic shifts in the community structure or abundance of AOA in either experiment. These different responses to acidification underscore the important role of microbial community structure in the resiliency of marine ecosystems.
机译:大气中CO_2浓度的增加导致大片海洋pH值降低。 pH值的降低可能会通过硝化作用的微生物过程改变碳和氮的生物地球化学循环,这是与海洋中这些循环耦合的关键过程,但通常对酸性条件敏感。最近的报告表明,在实验性降低pH值的情况下,海洋硝化速率会降低。未知的氨氧化细菌(AOB)和古细菌(AOA)组合的组成和丰度如何响应海洋pH降低。我们从2个不同的酸化实验中采样了微生物,并使用了qPCR和功能基因微阵列的氨单加氧酶基因(amoA)组合来评估酸化如何改变氨氧化装置的结构。我们显示,尽管实验条件差异很大,但酸化通过增加与硝化单胞菌属进化枝相关的分类单元的相对丰度,不断改变了AOB的群落组成。在一个实验中,这种增加足以引起AOB总体丰度的增加。在两个实验中,群落结构或AOA的含量均未发生系统性变化。这些对酸化的不同反应强调了微生物群落结构在海洋生态系统弹性中的重要作用。

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