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Large soil carbon storage in terrestrial ecosystems of Canada
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  • Camile Sothe,
  • Alemu Gonsamo,
  • Joyce Arabian,
  • Werner A Kurz,
  • Sarah A Finkelstein,
  • James Snider
Camile Sothe
McMaster University, McMaster University

Corresponding Author:[email protected]

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Alemu Gonsamo
McMaster University, McMaster University
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Joyce Arabian
WWF-Canada, WWF-Canada
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Werner A Kurz
Natural Resources Canada, Natural Resources Canada
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Sarah A Finkelstein
University of Toronto, University of Toronto
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James Snider
WWF-Canada, WWF-Canada
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Abstract

Terrestrial ecosystems of Canada store a large amount of organic carbon (C) in soils, peats and plant materials, yet little is known about the C stock size and distributions, both spatially and in various C pools. As temperature rises, C is becoming available for disturbance, decomposition and eventual release into the atmosphere, which makes the quantification of C stocks in terrestrial ecosystems of Canada of high interest for the assessment of climate change impacts and conservation efforts. We used a large number of field measurements, multisource satellite, climate and topographic data and a machine learning algorithm to produce the first wall-to-wall estimates of C stocks and uncertainties in plants and soils of Canada at 250 m spatial resolution. Our findings show that above and belowground live biomass and detritus store a total of 21.1 Pg C. Whereas the Canadian soils store 384 (±214, 90% confidence interval) Pg organic C in the top 1 m, 92 Pg C of which are stored in peatlands, confirming that the soil organic C dominates terrestrial carbon stocks in Canada. We also find previously under-reported large soil organic C stocks in forested peatlands on the boreal shields of Canada. Given that Canada is warming twice the global average rate and Canadian soils store approximately 25% of world soil C stocks in top 1 m, initiatives to understand their vulnerabilities to climate change and disturbance are indispensable not only for Canada but also for the global C budget and cycle.
Feb 2022Published in Global Biogeochemical Cycles volume 36 issue 2. 10.1029/2021GB007213