Aquatic biomass is a major source to particulate organic matter export in large Arctic rivers ...

Arctic rivers provide an integrated signature of the changing landscape and transmit signals of change to the ocean. Here, we use a decade of particulate organic matter (POM) compositional data to deconvolute multiple allochthonous and autochthonous pan-Arctic and watershed-specific sources. Constra...

Full description

Bibliographic Details
Main Authors: Behnke, Megan I., Tank, Suzanne E., McClelland, James W., Holmes, Robert M., Haghipour, Negar, Eglinton, Timothy I., Raymond, Peter A., Suslova, Anya, Zhulidov, Alexander V., Gurtovaya, Tatiana, Zimov, Nikita, Zimov, Sergey, Mutter, Edda A., Amos, Edwin, Spencer, Robert G. M.
Format: Text
Language:English
Published: ETH Zurich 2023
Subjects:
Online Access:https://dx.doi.org/10.3929/ethz-b-000604581
http://hdl.handle.net/20.500.11850/604581
id ftdatacite:10.3929/ethz-b-000604581
record_format openpolar
spelling ftdatacite:10.3929/ethz-b-000604581 2024-09-30T14:28:47+00:00 Aquatic biomass is a major source to particulate organic matter export in large Arctic rivers ... Behnke, Megan I. Tank, Suzanne E. McClelland, James W. Holmes, Robert M. Haghipour, Negar Eglinton, Timothy I. Raymond, Peter A. Suslova, Anya Zhulidov, Alexander V. Gurtovaya, Tatiana Zimov, Nikita Zimov, Sergey Mutter, Edda A. Amos, Edwin Spencer, Robert G. M. 2023 application/pdf https://dx.doi.org/10.3929/ethz-b-000604581 http://hdl.handle.net/20.500.11850/604581 en eng ETH Zurich Arctic rivers particulate organic matter endmember carbon flux Text Journal Article ScholarlyArticle article-journal 2023 ftdatacite https://doi.org/10.3929/ethz-b-000604581 2024-09-02T07:54:09Z Arctic rivers provide an integrated signature of the changing landscape and transmit signals of change to the ocean. Here, we use a decade of particulate organic matter (POM) compositional data to deconvolute multiple allochthonous and autochthonous pan-Arctic and watershed-specific sources. Constraints from carbon-to-nitrogen ratios (C:N), δ13C, and Δ14C signatures reveal a large, hitherto overlooked contribution from aquatic biomass. Separation in Δ14C age is enhanced by splitting soil sources into shallow and deep pools (mean ± SD: -228 ± 211 vs. -492 ± 173‰) rather than traditional active layer and permafrost pools (-300 ± 236 vs. -441 ± 215‰) that do not represent permafrost-free Arctic regions. We estimate that 39 to 60% (5 to 95% credible interval) of the annual pan-Arctic POM flux (averaging 4,391 Gg/y particulate organic carbon from 2012 to 2019) comes from aquatic biomass. The remainder is sourced from yedoma, deep soils, shallow soils, petrogenic inputs, and fresh terrestrial production. Climate ... : Proceedings of the National Academy of Sciences of the United States of America, 120 (12) ... Text Arctic permafrost DataCite Arctic
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Arctic
rivers
particulate organic matter
endmember
carbon flux
spellingShingle Arctic
rivers
particulate organic matter
endmember
carbon flux
Behnke, Megan I.
Tank, Suzanne E.
McClelland, James W.
Holmes, Robert M.
Haghipour, Negar
Eglinton, Timothy I.
Raymond, Peter A.
Suslova, Anya
Zhulidov, Alexander V.
Gurtovaya, Tatiana
Zimov, Nikita
Zimov, Sergey
Mutter, Edda A.
Amos, Edwin
Spencer, Robert G. M.
Aquatic biomass is a major source to particulate organic matter export in large Arctic rivers ...
topic_facet Arctic
rivers
particulate organic matter
endmember
carbon flux
description Arctic rivers provide an integrated signature of the changing landscape and transmit signals of change to the ocean. Here, we use a decade of particulate organic matter (POM) compositional data to deconvolute multiple allochthonous and autochthonous pan-Arctic and watershed-specific sources. Constraints from carbon-to-nitrogen ratios (C:N), δ13C, and Δ14C signatures reveal a large, hitherto overlooked contribution from aquatic biomass. Separation in Δ14C age is enhanced by splitting soil sources into shallow and deep pools (mean ± SD: -228 ± 211 vs. -492 ± 173‰) rather than traditional active layer and permafrost pools (-300 ± 236 vs. -441 ± 215‰) that do not represent permafrost-free Arctic regions. We estimate that 39 to 60% (5 to 95% credible interval) of the annual pan-Arctic POM flux (averaging 4,391 Gg/y particulate organic carbon from 2012 to 2019) comes from aquatic biomass. The remainder is sourced from yedoma, deep soils, shallow soils, petrogenic inputs, and fresh terrestrial production. Climate ... : Proceedings of the National Academy of Sciences of the United States of America, 120 (12) ...
format Text
author Behnke, Megan I.
Tank, Suzanne E.
McClelland, James W.
Holmes, Robert M.
Haghipour, Negar
Eglinton, Timothy I.
Raymond, Peter A.
Suslova, Anya
Zhulidov, Alexander V.
Gurtovaya, Tatiana
Zimov, Nikita
Zimov, Sergey
Mutter, Edda A.
Amos, Edwin
Spencer, Robert G. M.
author_facet Behnke, Megan I.
Tank, Suzanne E.
McClelland, James W.
Holmes, Robert M.
Haghipour, Negar
Eglinton, Timothy I.
Raymond, Peter A.
Suslova, Anya
Zhulidov, Alexander V.
Gurtovaya, Tatiana
Zimov, Nikita
Zimov, Sergey
Mutter, Edda A.
Amos, Edwin
Spencer, Robert G. M.
author_sort Behnke, Megan I.
title Aquatic biomass is a major source to particulate organic matter export in large Arctic rivers ...
title_short Aquatic biomass is a major source to particulate organic matter export in large Arctic rivers ...
title_full Aquatic biomass is a major source to particulate organic matter export in large Arctic rivers ...
title_fullStr Aquatic biomass is a major source to particulate organic matter export in large Arctic rivers ...
title_full_unstemmed Aquatic biomass is a major source to particulate organic matter export in large Arctic rivers ...
title_sort aquatic biomass is a major source to particulate organic matter export in large arctic rivers ...
publisher ETH Zurich
publishDate 2023
url https://dx.doi.org/10.3929/ethz-b-000604581
http://hdl.handle.net/20.500.11850/604581
geographic Arctic
geographic_facet Arctic
genre Arctic
permafrost
genre_facet Arctic
permafrost
op_doi https://doi.org/10.3929/ethz-b-000604581
_version_ 1811634294527885312