Soil geochemistry confines microbial abundances across an Arctic landscape; Implications for net carbon exchange with the atmosphere
A large portion of the World’s terrestrial organic carbon is stored in Arctic permafrost soils.However, due to permafrost warming and increased in situ microbial mineralisation of released carbon,greenhouse gas releases from Arctic soils are increasing, including methane (CH4 (g) ). To identify envi...
Main Authors: | , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Springer
2014
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Subjects: | |
Online Access: | https://eprint.ncl.ac.uk/fulltext.aspx?url=199035/38A47329-0B10-4335-B11C-0A383E9F5E16.pdf&pub_id=199035 |