Coupling of geochemical and geophysical measurements to characterize iron and organic carbon co-mobility upon permafrost thaw in an Arctic peatland in Abisko, Sweden.

Permafrost region covers 24% of the Earth’s total area and holds 1460-1600 Pg of carbon. A significant portion of this carbon (1035 ± 150 Pg) can be found in top three meters of the soil. With the degradation of permafrost due to the increase in air temperature in high latitudes (0.6 °C over the...

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Bibliographic Details
Main Authors: du Bois d'Aische, Eléonore, Thomas, Maxime, Jonard, François, Villani, Maëlle, Hirst, Catherine, Giesler, Reiner, Mörth, Carl-Magnus, Lundin, Erik, Opfergelt, Sophie, 7ème colloque climat et impacts
Other Authors: UCL - SST/ELI/ELIE - Environmental Sciences
Format: Conference Object
Language:English
Published: 2022
Subjects:
Online Access:http://hdl.handle.net/2078.1/268740