Management College, Ocean University of China, Qingdao, China.
Business College, Qingdao University, Qingdao, China.
Braz J Microbiol. 2024 Jun;55(2):1587-1599. doi: 10.1007/s42770-024-01298-x. Epub 2024 Apr 22.
Due to the inflow of meltwater from the Midre Lovénbreen glacier upstream of Kongsfjorden, the nutrient concentration of Kongsfjorden change from the estuary to the interior of the fjord. Our objective was to explore the changes in bacterial community structure and metabolism-related genes from the estuary to fjord by metagenomic analysis. Our data indicate that glacial meltwater input has altered the physicochemical properties of the fjords, with a significant effect, in particular, on fjords salinity, thus altering the relative abundance of some specific bacterial groups. In addition, we suggest that the salinity of a fjord is an important factor affecting the abundance of genes associated with the nitrogen and sulfur cycles in the fjord. Changes in salinity may affect the relative abundance of microbial populations that carry metabolic genes, thus affecting the relative abundance of genes associated with the nitrogen and sulfur cycles.
由于来自 Kongsfjorden 上游的 Midre Lovénbreen 冰川的融水流入,Kongsfjorden 的营养浓度从河口向峡湾内部发生变化。我们的目的是通过宏基因组分析来探讨从河口到峡湾的细菌群落结构和代谢相关基因的变化。我们的数据表明,冰川融水的输入改变了峡湾的理化性质,特别是对峡湾盐度有显著影响,从而改变了一些特定细菌群的相对丰度。此外,我们认为峡湾的盐度是影响与峡湾氮、硫循环相关基因丰度的重要因素。盐度的变化可能会影响携带代谢基因的微生物种群的相对丰度,从而影响与氮、硫循环相关的基因的相对丰度。