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Bacterial community structure across environmental gradients in permafrost thaw ponds: methanotroph-rich ecosystems
Permafrost thawing leads to the formation of thermokarst ponds that potentially emit CO(2) and CH(4) to the atmosphere. In the Nunavik subarctic region (northern Québec, Canada), these numerous, shallow ponds become well-stratified during summer. This creates a physico-chemical gradient of temperatu...
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| Publié dans: | Front Microbiol |
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| Auteurs principaux: | , , , |
| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
Frontiers Media S.A.
2015
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| Sujets: | |
| Accès en ligne: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4396522/ https://ncbi.nlm.nih.gov/pubmed/25926816 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.3389/fmicb.2015.00192 |
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