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Chemolithotrophic Primary Production in a Subglacial Ecosystem
Glacial comminution of bedrock generates fresh mineral surfaces capable of sustaining chemotrophic microbial communities under the dark conditions that pervade subglacial habitats. Geochemical and isotopic evidence suggests that pyrite oxidation is a dominant weathering process generating protons th...
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| Autors principals: | , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
American Society for Microbiology
2014
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4178699/ https://ncbi.nlm.nih.gov/pubmed/25085483 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1128/AEM.01956-14 |
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