Journal
MICROBIOME
Volume 10, Issue 1, Pages -Publisher
BMC
DOI: 10.1186/s40168-022-01238-7
Keywords
Glacier ecosystem; Cryoconite; Metagenomics; Denitrification; Cyanobacteria; Phycobilisome; Chromatic acclimation
Categories
Funding
- JSPS KAKENHI [19K23766, 19H01143, 20K21840, 21H03588]
- Arctic Challenge for Sustainability II (ArCS II) [JPMXD1420318865]
- Institute for Fermentation, Osaka [G-2020-2-133]
- Great Britain Sasakawa Foundation [3998]
- NERC [NE/V012991/1]
- Grants-in-Aid for Scientific Research [21H03588, 20K21840, 19K23766] Funding Source: KAKEN
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This study provided the first characterization of the taxonomic and metabolic diversities of cryoconite from different geographical areas. It was found that cryoconite bacterial communities in Asia and Polar regions show distinct compositions and metabolic characteristics, indicating the influence of environmental factors on the assemblage of cryoconite communities.
Background: Cryoconite granules are mineral-microbial aggregates found on glacier surfaces worldwide and are hotspots of biogeochemical reactions in glacier ecosystems. However, despite their importance within glacier ecosystems, the geographical diversity of taxonomic assemblages and metabolic potential of cryoconite communities around the globe remain unclear. In particular, the genomic content of cryoconite communities on Asia's high mountain glaciers, which represent a substantial portion of Earth's ice masses, has rarely been reported. Therefore, in this study, to elucidate the taxonomic and ecological diversities of cryoconite bacterial consortia on a global scale, we conducted shotgun metagenomic sequencing of cryoconite acquired from a range of geographical areas comprising Polar (Arctic and Antarctic) and Asian alpine regions. Results: Our metagenomic data indicate that compositions of both bacterial taxa and functional genes are particularly distinctive for Asian cryoconite. Read abundance of the genes responsible for denitrification was significantly more abundant in Asian cryoconite than the Polar cryoconite, implying that denitrification is more enhanced in Asian glaciers. The taxonomic composition of Cyanobacteria, the key primary producers in cryoconite communities, also differs between the Polar and Asian samples. Analyses on the metagenome-assembled genomes and fluorescence emission spectra reveal that Asian cryoconite is dominated by multiple cyanobacterial lineages possessing phycoerythrin, a green light-harvesting component for photosynthesis. In contrast, Polar cryoconite is dominated by a single cyanobacterial species Phormidesmis priestleyi that does not possess phycoerythrin. These findings suggest that the assemblage of cryoconite bacterial communities respond to regional- or glacier-specific physicochemical conditions, such as the availability of nutrients (e.g., nitrate and dissolved organic carbon) and light (i.e., incident shortwave radiation). Conclusions: Our genome-resolved metagenomics provides the first characterization of the taxonomic and metabolic diversities of cryoconite from contrasting geographical areas, highlighted by the distinct light-harvesting approaches of Cyanobacteria and nitrogen utilization between Polar and Asian cryoconite, and implies the existence of environmental controls on the assemblage of cryoconite communities. These findings deepen our understanding of the biodiversity and biogeochemical cycles of glacier ecosystems, which are susceptible to ongoing climate change and glacier decline, on a global scale.
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