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Isotopic seasonality of fluvial-derived greenhouse gases implies active layer deepening

Datos Bibliográficos

ID15545693
AutoresMelissa Schwab (0000-0001-5600-4439, Jet Propulsion Laboratory, autor de correspondencia), Clayton D Elder (0000-0001-9831-2106, Ames Research Center), Xiaomei Xu (0000-0001-5677-2497, University of California, Irvine), C I Czimczik (0000-0002-8251-6603, University of California, Irvine), Charles E Miller (0000-0002-9380-4838, Jet Propulsion Laboratory)
Año2024
Volumen19
Número11
Páginas114096-114096
Fecha de publicación2024-10-01
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaEnvironmental Research Letters (JOURNAL)
Identificadores de la revistaISSN: 1748-9326 • E-ISSN: 1748-9326
EditorialIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ad820f
OpenAlexW4403055375
IdiomaEN
Referencias citadas105

Climate change in the northern circumpolar regions is rapidly thawing organic-rich permafrost soils, leading to the substantial release of dissolved CO 2 and CH 4 into river systems. This mobilization impacts local ecosystems and regional climate feedback loops, playing a crucial role in the Arctic carbon cycle. Here, we analyze the stable carbon ( δ 13 C) and radiocarbon (F 14 C) isotopic compositions of dissolved CO 2 and CH 4 in the Sagavanirktok and Kuparuk River watersheds on the North Slope, Alaska. By examining spatial and seasonal variations in these isotopic signatures, we identify patterns of carbon release and transport across the river continuum. We find consistent CO 2 isotopic values along the geomorphological gradient, reflecting a mixture of geogenic and biogenic sources integrated throughout the watershed. Bayesian mixing models further demonstrate a systematic depletion in 13 C and 14 C signatures of dissolved CO 2 sources from spring to fall, indicating increasing contributions of aged carbon as the active layer deepens. This seasonal deepening allows percolating groundwater to access deeper, older soil horizons, transporting CO 2 produced by aerobic and anaerobic soil respiration to streams and rivers. In contrast, we observe no clear relationships between the 13 C and 14 C compositions of dissolved CH 4 and landscape properties. Given the reduced solubility of CH 4 , which facilitates outgassing and limits its transport in aquatic systems, the isotopic signatures are likely indicative of localized contributions from streambeds, adjacent water saturated soils, and lake outflows. Our study illustrates that dissolved greenhouse gases are sensitive indicators of old carbon release from thawing permafrost and serve as early warning signals for permafrost carbon feedbacks. It establishes a crucial baseline for understanding the role of CO 2 and CH 4 in regional carbon cycling and Arctic environmental change

Active layer · Atmospheric sciences · Climatology · Earth science · Fluvial · Geomorphology · Geotechnical engineering · Greenhouse gas · Hydrology (agriculture · Layer (electronics · Seasonality · Statistics · Atmospheric and Environmental Gas Dynamics · Chemistry · Environmental Science · Mathematics · Geology · Oceanography

  • Permafrost is warming at a global scale

    Open Access•Boris K Biskaborn, Sharon L Smith et al.•Nature Communications•2019

  • The Arctic has warmed nearly four times faster than the globe since 1979

    Open Access•Mika Rantanen, Alexey Yu Karpechko et al.•Communications Earth & Environment•2022

  • Carbon isotope compositions of terrestrial C3 plants as indicators of (paleo)ecology and (paleo)climate

    Open Access•Matthew J Kohn•Proceedings of the National…•2010

  • Modifying a sealed tube zinc reduction method for preparation of AMS graphite targets

    Open Access•Xiaomei Xu, Susan E Trumbore et al.•Nuclear Instruments and Methods…•2007

  • Plumbing the Global Carbon Cycle

    Open Access•J J Cole, Yves T Prairie et al.•Ecosystems•2007

  • Inference from Iterative Simulation Using Multiple Sequences

    Andrew Gelman, Donald B Rubin•Statistical Science•1992

  • Longer thaw seasons increase nitrogen availability for leaching during fall in tundra soils

    Open Access•Claire C Treat, W M Wollheim et al.•Environmental Research Letters•2016

  • Biomass offsets little or none of permafrost carbon release from soils, streams, and wildfire

    Open Access•Benjamin W Abbott, Jeremy B Jones et al.•Environmental Research Letters•2016

  • Abundant pre-industrial carbon detected in Canadian Arctic headwaters

    Open Access•Joshua Dean, Ype Van Der Velde et al.•Environmental Research Letters•2017

  • Arctic-boreal lakes of interior Alaska dominated by contemporary carbon

    Open Access•Fenix Garcia‐Tigreros, Clayton D Elder et al.•Environmental Research Letters•2023

  • Development of perennial thaw zones in boreal hillslopes enhances potential mobilization of permafrost carbon

    Open Access•Michelle A Walvoord, Clifford I Voss et al.•Environmental Research Letters•2018

  • Atmospheric Radiocarbon for the Period 1950–2019

    Open Access•Quan Hua, Jocelyn C Turnbull et al.•Radiocarbon•2022

  • The Keck Carbon Cycle AMS Laboratory, University of California, Irvine

    Open Access•Robert K Beverly, Will Beaumont et al.•Radiocarbon•2010

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