Flathead Lake Biological Station, University of Montana, Polson, Montana, USA.
Department of Biological Sciences, Idaho State University, Pocatello, Idaho, USA.
Environ Microbiol. 2024 Mar;26(3):e16616. doi: 10.1111/1462-2920.16616.
Nitrification is an important control on the form and distribution of nitrogen in freshwater ecosystems. However, the seasonality of nitrogen pools and the diversity of organisms catalyzing this process have not been well documented in oligotrophic lakes. Here, we show that nitrogen pools and nitrifying organisms in Flathead Lake are temporally and vertically dynamic, with nitrifiers displaying specific preferences depending on the season. While the ammonia-oxidizing bacteria (AOB) Nitrosomonadaceae and nitrite-oxidizing bacteria (NOB) Nitrotoga dominate at depth in the summer, the ammonia-oxidizing archaea (AOA) Nitrososphaerota and NOB Nitrospirota become abundant in the winter. Given clear seasonality in ammonium, with higher concentrations during the summer, we hypothesize that the succession between these two nitrifying groups may be due to nitrogen affinity, with AOB more competitive when ammonia concentrations are higher and AOA when they are lower. Nitrifiers in Flathead Lake share more than 99% average nucleotide identity with those reported in other North American lakes but are distinct from those in Europe and Asia, indicating a role for geographic isolation as a factor controlling speciation among nitrifiers. Our study shows there are seasonal shifts in nitrogen pools and nitrifying populations, highlighting the dynamic spatial and temporal nature of nitrogen cycling in freshwater ecosystems.
硝化作用是淡水生态系统中氮素形态和分布的重要控制因素。然而,贫营养湖泊中氮素库的季节性和催化这一过程的生物多样性尚未得到很好的记录。在这里,我们表明,平头湖的氮素库和硝化生物具有时间和垂直动态性,硝化生物根据季节表现出特定的偏好。虽然夏季氨氧化细菌(AOB)硝化单胞菌科和亚硝酸盐氧化细菌(NOB)硝化螺菌在深部占主导地位,但氨氧化古菌(AOA)硝化螺旋菌和 NOB 硝化螺旋菌在冬季变得丰富。鉴于铵盐具有明显的季节性,夏季浓度较高,我们假设这两组硝化生物之间的演替可能是由于氮亲和力所致,当氨浓度较高时 AOB 更具竞争力,而当氨浓度较低时 AOA 更具竞争力。平头湖的硝化生物与其他北美的湖泊中报道的硝化生物具有超过 99%的平均核苷酸同一性,但与欧洲和亚洲的硝化生物不同,这表明地理隔离是控制硝化生物物种形成的因素之一。我们的研究表明,氮素库和硝化种群存在季节性变化,突出了淡水生态系统氮循环的动态时空性质。