Limited release of previously-frozen C and increased new peat formation after thaw in permafrost peatlands

Permafrost stores globally significant amounts of carbon (C) which may start to decompose and be released to

Bibliographic Details
Published in:Soil Biology and Biochemistry
Main Authors: Estop-Aragonés, C. (Cristian), Cooper, M.D.A. (Mark D.A.), Fisher, J.P. (James P.), Thierry, A. (Aaron), Garnett, M.H. (Mark H.), Charman, D.J. (Dan J.), Murton, J.B. (Julian B.), Phoenix, G.K. (Gareth K.), Treharne, R. (Rachael), Sanderson, N.K. (Nicole K.), Burn, C. (Christopher R.), Kokelj, S.V. (Steve V.), Wolfe, S.A. (Stephen A), Lewkowicz, A.G. (Antoni G.), Williams, M. (Mathew), Hartley, I.P. (Iain P.)
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Greenhouse gases
Peatlands
Permafrost thaw
Radiocarbon
Thermokarst
Wildfire
permafrost
Online Access:https://ir.library.carleton.ca/pub/17262
https://doi.org/10.1016/j.soilbio.2017.12.010
Description
Summary:Permafrost stores globally significant amounts of carbon (C) which may start to decompose and be released to

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