Redistribution of soil organic matter by permafrost disturbance in the Canadian High Arctic

• Published in: Biogeochemistry
• Main Authors: Grewer, David M., Lafrenière, Melissa J., Lamoureux, Scott F., Simpson, Myrna J.
• Format: Other/Unknown Material
• Language: English
• Published: Springer International Publishing 2016
• Subjects: Cape Bounty; Soil organic matter characterization; Active layer detachments; Solvent extractable biomarkers; Solid-state 13C nuclear magnetic resonance; Arctic; Nunavut; Canada; permafrost
• Online Access: http://hdl.handle.net/1807/81096; https://doi.org/10.1007/s10533-016-0215-7

This is an accepted manuscript of a published article. With increased warming in the Arctic, permafrost thaw may induce localized physical disturbance of slopes. These disturbances, referred to as active layer detachments (ALDs), redistribute soil across the landscape, potentially releasing previously unavailable carbon (C). In 2007–2008, widespread ALD activity was reported at the Cape Bounty Arctic Watershed Observatory in Nunavut, Canada. Our study investigated organic matter (OM) composition in soil profiles from ALD-impacted and undisturbed areas. Solid-state 13C nuclear magnetic resonance (NMR) and solvent-extractable biomarkers were used to characterize soil OM. Throughout the disturbed upslope profile, where surface soils and vegetation had been removed, NMR revealed low O-alkyl C content and biomarker analysis revealed low concentrations of solvent-extractable compounds suggesting enhanced erosion of labile-rich OM by the ALD. In the disturbed downslope region, vegetation remained intact but displaced material from upslope produced lateral compression ridges at the surface. High O-alkyl content in the surface horizon was consistent with enrichment of carbohydrates and peptides, but low concentrations of labile biomarkers (i.e., sugars) suggested the presence of relatively unaltered labile-rich OM. Decreased O-alkyl content and biomarker concentrations below the surface contrasted with the undisturbed profile and may indicate the loss of well-established pre-ALD surface drainage with compression ridge formation. However, pre-ALD profile composition remains unknown and the observed decreases may result from nominal pre-ALD OM inputs. These results are the first to establish OM composition in ALD-impacted soil profiles, suggesting reallocation of permafrost-derived soil C to areas where degradation or erosion may contribute to increased C losses from disturbed Arctic soils.