Palsa Uplift Identified by Stable Isotope Depth Profiles and Relation of δ15N to C/N Ratio

Palsas develop as permafrost aggradation uplifts peat out of the zone influenced by groundwater. Here we relate δ15N values to C/N ratios along depth profiles through palsas in two peatlands near Abisko, northern Sweden, to identify perturbation of the peat. The perturbation by uplift as well as the...

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Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Jan Paul Krüger, Franz Conen, Jens Leifeld, Christine Alewell
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Ice
Online Access:https://doi.org/10.1002/ppp.1936