Evidence map›Paper›PMID 42215471›Full record

ArticleNature communications2026

Large stocks of permafrost soil organic carbon and nitrogen in Arctic river deltas.

Matthias Fuchs, Torsten Sachs, Loeka L Jongejans, Jens Strauss, Gustaf Hugelius, Gerald V Frost, Benjamin M Jones, Steven V Kokelj, Lars Kutzbach, Ingmar Nitze and 13 more

Abstract read
In one paragraph

Article in Nature communications, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

0numbers the graph read from it
0cells of the map it votes in
0citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

0 citing papers in PubMed.

No citing paper in PubMed yet.

4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

23 authors.

Matthias FuchsRenewable and Sustainable Energy Institute, University of Colorado Boulder, Boulder, CO, USA. matthias.fuchs@colorado.edu.ORCID http://orcid.org/0000-0003-3529-8284
Torsten SachsGFZ Helmholtz Centre for Geosciences, Potsdam, Germany.ORCID http://orcid.org/0000-0002-9959-4771
Loeka L JongejansAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany.ORCID http://orcid.org/0000-0002-0383-4567
Jens StraussAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany.ORCID http://orcid.org/0000-0003-4678-4982
Gustaf HugeliusStockholm University, Department of Physical Geography, Stockholm, Sweden.ORCID http://orcid.org/0000-0002-8096-1594
Gerald V FrostAlaska Biological Research, Inc., Fairbanks, AK, USA.ORCID http://orcid.org/0000-0002-5134-0334
Benjamin M JonesUniversity of Alaska Fairbanks, Institute of Northern Engineering, Fairbanks, AK, USA.ORCID http://orcid.org/0000-0002-1517-4711
Steven V KokeljNorthwest Territories Geological Survey, Government of Northwest Territories, Yellowknife, NT, Canada.ORCID http://orcid.org/0000-0002-2840-2605
Lars KutzbachDepartment of Earth System Sciences, University of Hamburg, Hamburg, Germany.ORCID http://orcid.org/0000-0003-2631-2742
Ingmar NitzeAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany.ORCID http://orcid.org/0000-0002-1165-6852
Pier Paul OverduinAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany.ORCID http://orcid.org/0000-0001-9849-4712
Juri PalmtagStockholm University, Department of Physical Geography, Stockholm, Sweden.
Chien-Lu PingUniversity of Alaska Fairbanks, Palmer Research Center, Agriculture and Forestry Experiment Station, Palmer, AK, USA.
Oleg S PokrovskyGeoscience and Environment Toulouse, CNRS, University of Toulouse, Toulouse, France.ORCID http://orcid.org/0000-0002-3155-7069
Elizaveta RivkinaKovda Institute of Physicochemical, and Biological Problems in Soil Science, Russian Academy of Sciences, Pushchino, Russia.ORCID http://orcid.org/0000-0001-7949-8056
Alexandra RungeGFZ Helmholtz Centre for Geosciences, Potsdam, Germany.
Lutz SchirrmeisterAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany.ORCID http://orcid.org/0000-0001-9455-0596
Georg SchwambornEberswalde University for Sustainable Development, Department LGW, Eberswalde, Germany.ORCID http://orcid.org/0000-0001-9635-0539
Matthias B SiewertUmeå University, Department of Ecology and Environmental Science, Umeå, Sweden.ORCID http://orcid.org/0000-0003-2890-8873
Claire TreatAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany.ORCID http://orcid.org/0000-0002-1225-8178
Alexandra VeremeevaAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany.ORCID http://orcid.org/0000-0002-6716-9260
Sebastian ZubrzyckiUniversität Hamburg, Earth and Society Research Hub, School of Integrated Climate and Earth System Sciences, Hamburg, Germany.ORCID http://orcid.org/0000-0002-6398-9173
Guido GrosseAlfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany.ORCID http://orcid.org/0000-0001-5895-2141

Funding

Bundesministerium für Bildung und Forschung (Federal Ministry of Education and Research) 03F0764BDeutsche Forschungsgemeinschaft (German Research Foundation) 164232461EC | EC Seventh Framework Programm | FP7 Ideas: European Research Council (FP7-IDEAS-ERC - Specific Programme: 'Ideas' Implementing the Seventh Framework Programme of the European Community for Research, Technological Development and Demonstration Activities (2007 to 2013)) 338335EC | Horizon 2020 Framework Programme (EU Framework Programme for Research and Innovation H2020) 773421National Science Foundation (NSF) OISE-1927553National Science Foundation (NSF) OPP-1903735National Science Foundation (NSF) OPP-2336164
6 · The paper itself

Abstract

Arctic deltas are highly dynamic environments at the land-ocean interface that have acted as long-term sinks of sediment, carbon (C), and nitrogen (N). Climate impacts Arctic deltas and their upstream catchments through sea-level rise, altered river discharge, increased sediment fluxes, intensified biogeochemical cycling, and permafrost thaw. As a result, soil C and N in Arctic delta deposits are becoming more bioavailable. Here, we present a C and N inventory for Arctic delta compiled from over 1600 soil samples spanning 17 river deltas. We estimate that Arctic delta deposits store 57.5 ( + 9.2/-8.2) Pg C and 3.8 ( + 0.8/-0.7) Pg N across a combined area of nearly 100,000 km², representing large and potentially vulnerable biogeochemical pools. Our findings underscore the potentially pivotal role of Arctic deltas in the pan-Arctic carbon cycle and highlight their importance as dynamic zones of both C and N storage and release in a rapidly changing Arctic.

Identifiers

PMID42215471
PMCPMC13402344

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LicenceCC BY-NC-ND
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Registered trials

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.