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Carbon accumulation in peatlands along a boreal to subarctic transect in eastern Canada

Bibliographic Data

ID12266609
AuthorsGuillaume Primeau (0000-0002-1371-3603, Université du Québec à Montréal, corresponding author), Michelle Garneau (0000-0002-1956-9243, Université du Québec à Montréal)
Year2021
Volume31
Issue5
Pages858-869
Publication date2021-01-17
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683620988031
OpenAlexW3122520681
LanguageEN
Citations received3
References cited61

In this study, we investigated the links between peat carbon accumulation and past ecological and hydrological conditions in three peatlands (Bouleau, Mista, Auassat) which developed along a South-North transect within a watershed encompassing the boreal and subarctic domain in Eastern Canada. Peatland development and long-term apparent rates of carbon accumulation (LORCA) were asynchronous in the watershed, suggesting an influence of both latitude and topography (altitude) on the length of the growing season (GGD 0 ). Results show that peat initiation within the three peatlands (respectively ca. 9070, 8400, and 6270 cal BP) was delayed after the deglaciation and that LORCA (respectively 35.5, 15.4, and 9.0 g C m −2 yr −1 ) decreased from South to North. Peatland development and fen to bog transitions were found to be almost synchronous for the two southernmost sites. The fen to bog transition in the northernmost subarctic site was delayed until the 20th century, owing to the less favorable climatic conditions. This suggests that recent warming has extended the length of the growing season and increased Sphagnum growth enough to potentially influence an ecosystem state-shift as observed in other Subarctic regions of eastern Canada

Biology · Bog · Boreal · Climate change · Geography · Peat · Physical geography · Subarctic climate · Transect · Watershed · Coastal wetland ecosystem dynamics · Environmental Science · Geology and Paleoclimatology Research · Peatlands and Wetlands Ecology · Ecology · Geology · Oceanography

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    Open Access•Mylène Robitaille, Michelle Garneau et al.•The Holocene•2021

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    Open Access•Léonie Perrier, Michelle Garneau et al.•The Holocene•2022

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    Open Access•Dale H Vitt, Melissa House•The Holocene•2023

  • Holocene development of maritime ombrotrophic peatlands of the St. Lawrence North Shore in eastern Canada

    Open Access•Gabriel Magnan, Michelle Garneau et al.•Quaternary Research•2014

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  • Flexible paleoclimate age-depth models using an autoregressive gamma process

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  • A testate amoeba-based transfer function for paleohydrological reconstruction from boreal and subarctic peatlands in northeastern Canada

    A Lamarre, G Magnan et al.•Quaternary International•2013

  • Holocene palaeoecological reconstruction of three boreal peatlands in the La Grande Rivière region, Québec, Canada

    Open Access•Véronique Beaulieu-Audy, Michelle Garneau et al.•The Holocene•2009

  • Estimating carbon accumulation rates of undrained mires in Finland–application to boreal and subarctic regions

    Open Access•Jukka Turunen, Erkki Tomppo et al.•The Holocene•2002

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  • Long-term and recent ecohydrological dynamics of patterned peatlands in north-central Quebec (Canada)

    Open Access•Mylène Robitaille, Michelle Garneau et al.•The Holocene•2021

  • Holocene carbon dynamics of boreal and subarctic peatlands from Québec, Canada

    Open Access•Michelle Garneau, Simon Van Bellen et al.•The Holocene•2014

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  • IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal BP

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Unique citing works3
Citations per year0.6
Citation span2021 - 2023 (3)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 3

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