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Surface exposure to sunlight stimulates CO(2) release from permafrost soil carbon in the Arctic
Recent climate change has increased arctic soil temperatures and thawed large areas of permafrost, allowing for microbial respiration of previously frozen C. Furthermore, soil destabilization from melting ice has caused an increase in thermokarst failures that expose buried C and release dissolved o...
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| Autors principals: | , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2013
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3587192/ https://ncbi.nlm.nih.gov/pubmed/23401500 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1214104110 |
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