Active microbial ecosystem in glacier basal ice fuelled by iron and silicate comminution‐derived hydrogen

The basal zone of glaciers is characterized by physicochemical properties that are distinct from firnified ice due to strong interactions with underlying substrate and bedrock. Basal ice (BI) ecology and the roles that the microbiota play in biogeochemical cycling, weathering, and proglacial soil fo...

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Detalles Bibliográficos
Autores principales: Toubes‐Rodrigo, Mario, Potgieter‐Vermaak, Sanja, Sen, Robin, Oddsdóttir, Edda S., Elliott, David, Cook, Simon
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2021
Materias:
Original Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8289488/
https://www.ncbi.nlm.nih.gov/pubmed/34459543
http://dx.doi.org/10.1002/mbo3.1200

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8289488/
https://www.ncbi.nlm.nih.gov/pubmed/34459543
http://dx.doi.org/10.1002/mbo3.1200

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