Institut for Biologi

Aarhus University Seal / Aarhus Universitets segl

André Pellerin

Legacy of Holocene Landscape Changes on Soil Biogeochemistry: A Perspective From Paleo-Active Layers in Northwestern Canada

Publikation: Bidrag til tidsskrift/Konferencebidrag i tidsskrift /Bidrag til avisTidsskriftartikelForskningpeer review


  • Denis Lacelle, t of Biology, University of Ottawa, 30-268 Marie Curie, Ottawa, Ontario K1N 6N5, Canada
  • ,
  • Marielle Fontaine, t of Biology, University of Ottawa, 30-268 Marie Curie, Ottawa, Ontario K1N 6N5, Canada
  • ,
  • André Pellerin
  • Steve V. Kokelj, Government of the Northwest Territories
  • ,
  • Ian D. Clark, t of Biology, University of Ottawa, 30-268 Marie Curie, Ottawa, Ontario K1N 6N5, Canada

Recent climate warming is contributing to permafrost degradation and vegetation change; however, little is known about the legacy of Holocene landscape change on contemporary soil biogeochemical conditions. In permafrost soils of northwestern Canada, widespread permafrost degradation occurred during the early Holocene warm interval and its impacts on soil biogeochemistry are archived in the paleo-active layer. Here we show contrasting profiles of soil soluble chemistry and organic carbon composition at sites affected by different types of permafrost degradation. At sites that experienced increased depth of thaw, the relict active layer contained a lower abundance of soluble ions than the underlying undisturbed permafrost; however, both the relict active layer and undisturbed permafrost contained mainly old recalcitrant organics suggesting that minor microbial degradation of organics had occurred. At sites that experienced past thaw slumping, the relict active layer had a higher solute content and contained both young-degradable and old-recalcitrant organics due to the integration of slumped surface organic mats into the colluvial soils or vegetation re-colonizing the surface of the former slump. Our results show that permafrost degradation that occurred during the early to mid-Holocene have preconditioned the biogeochemical conditions in near-surface permafrost soils such that significant local variability exist following past landscape changes. Thus, determining the state of soil soluble chemistry and SOC in permafrost should be done within a paleo-landscape change framework to better forecast CO2–CH4 emissions and solutes release from thawing permafrost.

TidsskriftJournal of Geophysical Research: Biogeosciences
Sider (fra-til)2662-2679
Antal sider18
StatusUdgivet - 2019

Se relationer på Aarhus Universitet Citationsformater

ID: 170902102