Zubov Ivan, Shpanov Dmitrij, Ponomareva Tamara, Aksenov Andrey
N. Laverov Federal Center for Integrated Arctic Research of the Ural Branch of the Russian Academy of Sciences, Arkhangelsk, Russia N. Laverov Federal Center for Integrated Arctic Research of the Ural Branch of the Russian Academy of Sciences Arkhangelsk Russia.
Northern (Arctic) Federal University named after M.V. Lomonosov, Arkhangelsk, Russia Northern (Arctic) Federal University named after M.V. Lomonosov Arkhangelsk Russia.
Biodivers Data J. 2024 Aug 21;12:e118448. doi: 10.3897/BDJ.12.e118448. eCollection 2024.
Wetlands occupy up to 35% of the boreal biome in Russia, according to various estimates. Boreal bogs are global carbon sinks, accounting for more than 65% of the soil carbon stored in the wetland ecosystems of the world. The decomposition of plant residues is one of the most important components of the carbon cycle in wetland systems, while the violation of their fragile balance due to climate change increases the rate of mineralisation of organic matter and releases large amounts of carbon to the atmosphere. The biochemical processes occurring in a peat deposit determine the intensity of the destruction of organic matter and gas exchange. However, the microbial communities of the boreal ombrotrophic bogs, regulating those processes, are poorly studied. Hence, a study of the prokaryote communities of the peat deposits of the southern White Sea coastal ombrotrophic bogs (mostly spread in north-western Russia) was carried out. The taxonomic composition of archaea and bacteria sampled from the deposit's depth of 0-310 cm was studied using high-throughput sequencing of V4 sites of 16S rRNA gene by Illumina technology. As a result, 105 species belonging to 19 phylums were identified. The dominant specific phyla were , and , the non-specific phylum being . Various groups of methanogenic, methylotrophic and nitrogen-fixing microorganisms were identified. Shannon's biodiversity ranged from 3.5 to 4.6 and ChaO1 - from 232 to 351, decreasing within the depth.
据各种估计,湿地占俄罗斯北方生物群落面积的35%。北方沼泽是全球碳汇,占世界湿地生态系统土壤碳储量的65%以上。植物残体的分解是湿地系统碳循环的最重要组成部分之一,而气候变化导致其脆弱平衡的破坏会增加有机物质的矿化速率,并向大气中释放大量碳。泥炭沉积物中发生的生化过程决定了有机物质的破坏强度和气体交换。然而,调节这些过程的北方雨养泥炭沼泽的微生物群落研究较少。因此,对白海沿岸南部雨养泥炭沼泽(主要分布在俄罗斯西北部)泥炭沉积物中的原核生物群落进行了研究。通过Illumina技术对16S rRNA基因V4位点进行高通量测序,研究了从沉积物0 - 310厘米深处采集的古菌和细菌的分类组成。结果,鉴定出了属于19个门的105个物种。主要的特定门是 、 和 ,非特定门是 。鉴定出了各种产甲烷、甲基营养和固氮微生物群。香农生物多样性范围为3.5至4.6,Chao1为232至351,随深度增加而降低。 (原文中部分特定门的名称未给出具体内容,用 表示)