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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Detalles Bibliográficos
Autores principales: Crevecoeur, Sophie, Vincent, Warwick F., Comte, Jérôme, Lovejoy, Connie
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2015
Materias:
Microbiology
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4396522/
https://www.ncbi.nlm.nih.gov/pubmed/25926816
http://dx.doi.org/10.3389/fmicb.2015.00192

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4396522/
https://www.ncbi.nlm.nih.gov/pubmed/25926816
http://dx.doi.org/10.3389/fmicb.2015.00192

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