Evidence map›Paper›PMID 34911949›Full record

ArticleNature communications2021

Sea-ice derived meltwater stratification slows the biological carbon pump: results from continuous observations.

Wilken-Jon von Appen, Anya M Waite, Melanie Bergmann, Christina Bienhold, Olaf Boebel, Astrid Bracher, Boris Cisewski, Jonas Hagemann, Mario Hoppema, Morten H Iversen and 16 more

Open access · goldAbstract read
In one paragraph

Article in Nature communications, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 17 papers.

0numbers the graph read from it
0cells of the map it votes in
17citing papers in PubMed
7.7field-weighted citation impact, top 2% of its field
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

17 citing papers in PubMed, 99 citations in OpenAlex.

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  9. Nitrogen fixation under declining Arctic sea ice.Communications earth & environment · 2025
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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

26 authors at 2 institutions in 3 countries.

Wilken-Jon von AppenAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany. Wilken-Jon.von.Appen@awi.de.ORCID http://orcid.org/0000-0002-7200-0099
Anya M WaiteAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.
Melanie BergmannAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0001-5212-9808
Christina BienholdAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.
Olaf BoebelAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.
Astrid BracherAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0003-3025-5517
Boris CisewskiThünen Institute of Sea Fisheries, Bremerhaven, Germany.ORCID http://orcid.org/0000-0002-1130-6107
Jonas HagemannAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0002-5407-7746
Mario HoppemaAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0002-2326-619X
Morten H IversenAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0002-5287-1110
Christian KonradAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.
Thomas KrumpenAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.
Normen LochthofenAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0002-2652-5302
Katja MetfiesAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0003-3073-8033
Barbara NiehoffAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.
Eva-Maria NöthigAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0002-7527-7827
Autun PurserAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0001-5427-0151
Ian SalterAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0002-4513-0314
Matthias SchaberThünen Institute of Sea Fisheries, Bremerhaven, Germany.
Daniel ScholzAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0001-7500-5365
Thomas SoltwedelAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.
Sinhue Torres-ValdesAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0003-2749-4170
Claudia WekerleAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.
Frank WenzhöferAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0002-4621-0586
Matthias WietzAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0002-9786-3026
Antje BoetiusAlfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0003-2117-4176
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung · DEHochschule Bremerhaven · DE

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The ocean moderates the world's climate through absorption of heat and carbon, but how much carbon the ocean will continue to absorb remains unknown. The North Atlantic Ocean west (Baffin Bay/Labrador Sea) and east (Fram Strait/Greenland Sea) of Greenland features the most intense absorption of anthropogenic carbon globally; the biological carbon pump (BCP) contributes substantially. As Arctic sea-ice melts, the BCP changes, impacting global climate and other critical ocean attributes (e.g. biodiversity). Full understanding requires year-round observations across a range of ice conditions. Here we present such observations: autonomously collected Eulerian continuous 24-month time-series in Fram Strait. We show that, compared to ice-unaffected conditions, sea-ice derived meltwater stratification slows the BCP by 4 months, a shift from an export to a retention system, with measurable impacts on benthic communities. This has implications for ecosystem dynamics in the future warmer Arctic where the seasonal ice zone is expected to expand.

Indexed as

CarbonIce CoverSeawaterAtlantic OceanCarbon CycleClimate ChangeEcosystemGreenlandNewfoundland and LabradorCarbon

Identifiers

PMID34911949
PMCPMC8674288
OpenAlexW4200583974

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

Registered trials

None linked

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.