Research output: Contribution to journal › Article › peer-review
Linking the composition of cryoconite prokaryotic communities in the Arctic, Antarctic, and Central Caucasus with their chemical characteristics. / Гладков, Григорий Валерьевич; Кимеклис, Анастасия Кирилловна; Темботов, Рустам Хасанбиевич; Иванов, Михаил; Андронов, Евгений Евгеньевич; Абакумов, Евгений Васильевич.
In: Scientific Reports, Vol. 14, No. 1, 15838, 01.12.2024.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Linking the composition of cryoconite prokaryotic communities in the Arctic, Antarctic, and Central Caucasus with their chemical characteristics
AU - Гладков, Григорий Валерьевич
AU - Кимеклис, Анастасия Кирилловна
AU - Темботов, Рустам Хасанбиевич
AU - Иванов, Михаил
AU - Андронов, Евгений Евгеньевич
AU - Абакумов, Евгений Васильевич
PY - 2024/6/11
Y1 - 2024/6/11
N2 - Cryoconites are the deposits on the surface of glaciers that create specific ecological niches for the development of microorganism communities. The sediment material can vary in origin, structure, and nutrient content, creating local variations in the growth conditions. An additional factor of variability is the location of the glaciers, as they are found in different climatic zones in the high mountain regions and closer to the poles. Here, using the analysis of amplicon sequencing of the 16S rRNA gene, we studied the taxonomic composition of the prokaryotic communities from glaciers from remote regions, including the Arctic (Mushketova on the Severnaya Zemlya, IGAN in Polar Ural), Antarctic (Pimpirev on the Livingstone Island) and Central Caucasus (Skhelda and Garabashi) and connected it with the variation of the physicochemical characteristics of the substrate: pH, carbon, nitrogen, macro- and microelements. The cryoconite microbiomes were comprised of specific for this environment phyla (mostly Pseudomonadota, Cyanobacteria, Bacteroidota, Acidobacteriota, and Actinobacteriota), but each glacier had a unique taxonomic imprint. The core microbiome between regions was composed of only a few ASVs, among which the most likely globally distributed ones attributed to Polaromonas sp., Rhodoferax sp., Cryobacterium sp., and Hymenobacter frigidus. The WGSNA defined clusters of co-occurring ASVs between microbiomes, that significantly change their abundance corresponding with the variation of chemical parameters of cryoconites, but do not fully coincide with their regional separation. Thus, our work demonstrates that the chemical characteristics of the sediment material can explain the variation in the cryoconite prokaryotic community which is not always linked to geographic isolation.
AB - Cryoconites are the deposits on the surface of glaciers that create specific ecological niches for the development of microorganism communities. The sediment material can vary in origin, structure, and nutrient content, creating local variations in the growth conditions. An additional factor of variability is the location of the glaciers, as they are found in different climatic zones in the high mountain regions and closer to the poles. Here, using the analysis of amplicon sequencing of the 16S rRNA gene, we studied the taxonomic composition of the prokaryotic communities from glaciers from remote regions, including the Arctic (Mushketova on the Severnaya Zemlya, IGAN in Polar Ural), Antarctic (Pimpirev on the Livingstone Island) and Central Caucasus (Skhelda and Garabashi) and connected it with the variation of the physicochemical characteristics of the substrate: pH, carbon, nitrogen, macro- and microelements. The cryoconite microbiomes were comprised of specific for this environment phyla (mostly Pseudomonadota, Cyanobacteria, Bacteroidota, Acidobacteriota, and Actinobacteriota), but each glacier had a unique taxonomic imprint. The core microbiome between regions was composed of only a few ASVs, among which the most likely globally distributed ones attributed to Polaromonas sp., Rhodoferax sp., Cryobacterium sp., and Hymenobacter frigidus. The WGSNA defined clusters of co-occurring ASVs between microbiomes, that significantly change their abundance corresponding with the variation of chemical parameters of cryoconites, but do not fully coincide with their regional separation. Thus, our work demonstrates that the chemical characteristics of the sediment material can explain the variation in the cryoconite prokaryotic community which is not always linked to geographic isolation.
KW - Antarctic Regions
KW - Arctic Regions
KW - Bacteria/genetics
KW - Geologic Sediments/microbiology
KW - Ice Cover/microbiology
KW - Microbiota/genetics
KW - Phylogeny
KW - RNA, Ribosomal, 16S/genetics
KW - 16S rRNA
KW - Geographic location
KW - Cryoconite
KW - Amplicon sequencing
KW - Prokaryotic community
KW - Chemical parameters
UR - https://www.mendeley.com/catalogue/e6531c32-479a-3508-90cb-d8ad695eb87b/
U2 - 10.1038/s41598-024-64452-3
DO - 10.1038/s41598-024-64452-3
M3 - Article
C2 - 38982048
VL - 14
JO - Scientific Reports
JF - Scientific Reports
SN - 2045-2322
IS - 1
M1 - 15838
ER -
ID: 121259632