Bog bacterial community: data from north-western Russia

• Published in: Biodiversity Data Journal
• Main Authors: Zubov,Ivan, Shpanov,Dmitrij, Ponomareva,Tamara, Aksenov,Andrey
• Format: Article in Journal/Newspaper
• Language: English
• Published: Pensoft Publishers 2024
• Subjects: barcode amplicon sequencing; 16S rRNA gene; prokaryote; high-moor peat; bog; biodiversity; north-western Russia; North-Western Russia; White Sea
• Online Access: https://doi.org/10.3897/BDJ.12.e118448; https://bdj.pensoft.net/article/118448/; https://bdj.pensoft.net/article/118448/download/pdf/

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 Pseudomonadota, Acidobacteriota and Verrucomicrobiota, the non-specific phylum being Desulfobacterota. 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.