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Impact of Seasonal Hypoxia on Activity and Community Structure of Chemolithoautotrophic Bacteria in a Coastal Sediment

机译:季节性缺氧对滨海沉积物中化学自养细菌活性和群落结构的影响

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摘要

Seasonal hypoxia in coastal systems drastically changes the availability of electron acceptors in bottom water, which alters the sedimentary reoxidation of reduced compounds. However, the effect of seasonal hypoxia on the chemolithoautotrophic community that catalyzes these reoxidation reactions is rarely studied. Here, we examine the changes in activity and structure of the sedimentary chemolithoautotrophic bacterial community of a seasonally hypoxic saline basin under oxic (spring) and hypoxic (summer) conditions. Combined 16S rRNA gene amplicon sequencing and analysis of phospholipid-derived fatty acids indicated a major temporal shift in community structure. Aerobic sulfur-oxidizing Gammaproteobacteria (Thiotrichales) and Epsilonproteobacteria (Campylobacterales) were prevalent during spring, whereas Deltaproteobacteria (Desulfobacterales) related to sulfate-reducing bacteria prevailed during summer hypoxia. Chemolithoautotrophy rates in the surface sediment were three times higher in spring than in summer. The depth distribution of chemolithoautotrophy was linked to the distinct sulfur oxidation mechanisms identified through microsensor profiling, i.e., canonical sulfur oxidation, electrogenic sulfur oxidation by cable bacteria, and sulfide oxidation coupled to nitrate reduction by Beggiatoaceae. The metabolic diversity of the sulfur-oxidizing bacterial community suggests a complex niche partitioning within the sediment, probably driven by the availability of reduced sulfur compounds (H2S, S-o, and S2O32 ) and electron acceptors (O-2 and NO3 ) regulated by seasonal hypoxia.
机译:沿海系统中的季节性缺氧极大地改变了底层水中电子受体的可用性,从而改变了还原化合物的沉积再氧化作用。然而,很少研究季节性缺氧对催化这些再氧化反应的化学自养群落的影响。在这里,我们研究了季节性缺氧盐水盆地的沉积化学石自养细菌群落在含氧(春季)和缺氧(夏季)条件下的活动和结构的变化。结合 16S rRNA 基因扩增子测序和磷脂衍生脂肪酸的分析表明群落结构存在重大时间变化。需氧硫氧化γ变形菌(Thiotrichales)和枸杞变形菌(Campylobacterales)在春季盛行,而与硫酸盐还原菌相关的Deltaproteobacteria(Desulfobacterales)在夏季缺氧时盛行。春季表层沉积物中的化学自养速率是夏季的三倍。化学自养的深度分布与通过微传感器分析确定的不同硫氧化机制有关,即典型的硫氧化、电缆细菌的电硫氧化以及贝吉亚科的硫化物氧化与硝酸盐还原耦合。硫氧化细菌群落的代谢多样性表明沉积物内存在复杂的生态位划分,这可能是由季节性缺氧调节的还原硫化合物(H2S、S-o 和 S2O32)和电子受体(O-2 和 NO3)的可用性驱动的。

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