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...

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Bibliographic Details
Main Authors: Gray ND, McCann CM, Christgen B, Ahammad SZ, Roberts JA, Graham DW
Format: Article in Journal/Newspaper
Language:unknown
Published: Springer 2014
Subjects:
Rho
Online Access:https://eprint.ncl.ac.uk/fulltext.aspx?url=199035/38A47329-0B10-4335-B11C-0A383E9F5E16.pdf&pub_id=199035