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Circum-Arctic release of terrestrial carbon varies between regions and sources

Author

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  • Jannik Martens

    (Stockholm University
    Bolin Centre for Climate Research, Stockholm University
    Lamont-Doherty Earth Observatory of Columbia University)

  • Birgit Wild

    (Stockholm University
    Bolin Centre for Climate Research, Stockholm University)

  • Igor Semiletov

    (Il’ichov Pacific Oceanological Institute FEB RAS
    Higher School of Economics (HSE)
    Tomsk State University (TSU))

  • Oleg V. Dudarev

    (Il’ichov Pacific Oceanological Institute FEB RAS
    Tomsk State University (TSU))

  • Örjan Gustafsson

    (Stockholm University
    Bolin Centre for Climate Research, Stockholm University)

Abstract

Arctic change is expected to destabilize terrestrial carbon (terrOC) in soils and permafrost, leading to fluvial release, greenhouse gas emission and climate feedback. However, landscape heterogeneity and location-specific observations complicate large-scale assessments of terrOC mobilization. Here we reveal differences in terrOC release, deduced from the Circum-Arctic Sediment Carbon Database (CASCADE) using source-diagnostic (δ13C-Δ14C) and carbon accumulation data. The results show five-times larger terrOC release from the Eurasian than from the American Arctic. Most of the circum-Arctic terrOC originates from near-surface soils (61%); 30% stems from Pleistocene-age permafrost. TerrOC translocation, relative to land-based terrOC stocks, varies by a factor of five between circum-Arctic regions. Shelf seas with higher relative terrOC translocation follow the spatial pattern of recent Arctic warming, while such with lower translocation reflect long-distance lateral transport with efficient remineralization of terrOC. This study provides a receptor-based perspective for how terrOC release varies across the circum-Arctic.

Suggested Citation

  • Jannik Martens & Birgit Wild & Igor Semiletov & Oleg V. Dudarev & Örjan Gustafsson, 2022. "Circum-Arctic release of terrestrial carbon varies between regions and sources," Nature Communications, Nature, vol. 13(1), pages 1-10, December.
    • Handle: RePEc:nat:natcom:v:13:y:2022:i:1:d:10.1038_s41467-022-33541-0
    DOI: 10.1038/s41467-022-33541-0
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