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首页> 外文期刊>Frontiers in Microbiology >Abundance and Diversity of Denitrifying and Anammox Bacteria in Seasonally Hypoxic and Sulfidic Sediments of the Saline Lake Grevelingen
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Abundance and Diversity of Denitrifying and Anammox Bacteria in Seasonally Hypoxic and Sulfidic Sediments of the Saline Lake Grevelingen

机译:盐湖格里维林根季节性低氧和硫沉积物中反硝化和厌氧细菌的丰度和多样性

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Denitrifying and anammox bacteria are involved in the nitrogen cycling in marine sediments but the environmental factors that regulate the relative importance of these processes are not well constrained. Here, we evaluated the abundance, diversity, and potential activity of denitrifying, anammox, and sulfide-dependent denitrifying bacteria in the sediments of the seasonally hypoxic saline Lake Grevelingen, known to harbor an active microbial community involved in sulfur oxidation pathways. Depth distributions of 16S rRNA gene, nirS gene of denitrifying and anammox bacteria, aprA gene of sulfur-oxidizing and sulfate-reducing bacteria, and ladderane lipids of anammox bacteria were studied in sediments impacted by seasonally hypoxic bottom waters. Samples were collected down to 5 cm depth (1 cm resolution) at three different locations before (March) and during summer hypoxia (August). The abundance of denitrifying bacteria did not vary despite of differences in oxygen and sulfide availability in the sediments, whereas anammox bacteria were more abundant in the summer hypoxia but in those sediments with lower sulfide concentrations. The potential activity of denitrifying and anammox bacteria as well as of sulfur-oxidizing, including sulfide-dependent denitrifiers and sulfate-reducing bacteria, was potentially inhibited by the competition for nitrate and nitrite with cable and/or Beggiatoa -like bacteria in March and by the accumulation of sulfide in the summer hypoxia. The simultaneous presence and activity of organoheterotrophic denitrifying bacteria, sulfide-dependent denitrifiers, and anammox bacteria suggests a tight network of bacteria coupling carbon-, nitrogen-, and sulfur cycling in Lake Grevelingen sediments.
机译:反硝化细菌和厌氧氨氧化细菌参与了海洋沉积物中的氮循环,但是调节这些过程相对重要性的环境因素并未受到很好的限制。在这里,我们评估了季节性缺氧盐湖格里维林根(Lake Grevelingen)沉积物中的反硝化,厌氧氨氧化和依赖硫化物的反硝化细菌的丰度,多样性和潜在活性,该湖已知有活跃的微生物群落参与硫氧化途径。在季节性缺氧的底水影响下,研究了16S rRNA基因,反硝化和厌氧细菌的nirS基因,脱硫和还原硫酸盐的细菌的aprA基因以及厌氧细菌的梯丹脂质的深度分布。在3月之前和3月夏季缺氧期间(8月),在三个不同的位置采集到5厘米深(分辨率为1厘米)的样品。尽管沉积物中氧气和硫化物的利用率不同,反硝化细菌的丰度也没有变化,而夏季缺氧条件下但在硫化物浓度较低的沉积物中,厌氧氨氧化菌则更为丰富。硝化和厌氧细菌以及硫氧化的潜在活性,包括依赖于硫化物的反硝化剂和硫酸盐还原细菌,都可能受到三月份电缆和/或Beggiatoa细菌与硝酸盐和亚硝酸盐竞争的抑制,以及夏季缺氧时硫化物的积累。有机异养反硝化细菌,依赖于硫化物的反硝化细菌和厌氧氨氧化菌的同时存在和活性表明,在格里维林根湖沉积物中,细菌紧密结合着碳,氮和硫循环。

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