Did fires drive Holocene carbon sequestration in boreal ombrotrophic peatlands of eastern Canada?

Simon van Bellen, Michelle Garneau, Adam Ali, Yves Bergeron

Research output: Contribution to journalArticle

12 Citations (Scopus)

Abstract

Wildfire is an important factor on carbon sequestration in the North American boreal biomes. Being globally important stocks of organic carbon, peatlands may be less sensitive to burning in comparison with upland forests, especially wet unforested ombrotrophic ecosystems as found in northeastern Canada. We aimed to determine if peatland fires have driven carbon accumulation patterns during the Holocene. To cover spatial variability, six cores from three peatlands in the Eastmain region of Quebec were analyzed for stratigraphic charcoal accumulation. Results show that regional Holocene peatland fire frequency was ~ 2.4 fires 1000 yr - 1, showing a gradually declining trend since 4000 cal yr BP, although inter- and intra-peatland variability was very high. Charcoal peak magnitudes, however, were significantly higher between 1400 and 400 cal yr BP, possibly reflecting higher charcoal production driven by differential climatic forcing aspects. Carbon accumulation rates generally declined towards the late-Holocene with minimum values of ~ 10 g m - 2 yr - 1 around 1500 cal yr BP. The absence of a clear correlation between peatland fire regimes and carbon accumulation indicates that fire regimes have not been a driving factor on carbon sequestration at the millennial time scale.

Original languageEnglish
Pages (from-to)50-59
Number of pages10
JournalQuaternary Research
Volume78
Issue number1
Early online date25 Apr 2012
DOIs
Publication statusPublished - Jul 2012

    Fingerprint

Keywords

  • peat
  • Quebec
  • charcoal analysis
  • neoglacial
  • bog
  • accumulation
  • charAnalysis
  • threshold

Cite this