Snow Microorganisms Colonise Arctic Soils Following Snow Melt

Arctic soils are constantly subjected to microbial invasion from either airborne, marine, or animal sources, which may impact local microbial communities and ecosystem functioning. However, in winter, Arctic soils are isolated from outside sources other than snow, which is the sole source of microor...

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Bibliographic Details
Published in:Microbial Ecology
Main Authors: Malard, Lucie A., Bergk-Pinto, Benoit, Layton, Rose, Vogel, Timothy M., Larose, Catherine, Pearce, David A.
Format: Text
Language:English
Published: Springer US 2023
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10497451/
http://www.ncbi.nlm.nih.gov/pubmed/36939866
https://doi.org/10.1007/s00248-023-02204-y
Description
Summary:Arctic soils are constantly subjected to microbial invasion from either airborne, marine, or animal sources, which may impact local microbial communities and ecosystem functioning. However, in winter, Arctic soils are isolated from outside sources other than snow, which is the sole source of microorganisms. Successful colonisation of soil by snow microorganisms depends on the ability to survive and compete of both, the invading and resident community. Using shallow shotgun metagenome sequencing and amplicon sequencing, this study monitored snow and soil microbial communities throughout snow melt to investigate the colonisation process of Arctic soils. Microbial colonisation likely occurred as all the characteristics of successful colonisation were observed. The colonising microorganisms originating from the snow were already adapted to the local environmental conditions and were subsequently subjected to many similar conditions in the Arctic soil. Furthermore, competition-related genes (e.g. motility and virulence) increased in snow samples as the snow melted. Overall, one hundred potentially successful colonisers were identified in the soil and, thus, demonstrated the deposition and growth of snow microorganisms in soils during melt. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s00248-023-02204-y.