Evidence map›Paper›PMID 41093831›Full record

ArticleNature communications2025

Southern Ocean evidence for recurring West Antarctic Ice Sheet destabilization during Marine Isotope Stage 11.

L Jebasinski, D A Frick, A K I U Kapuge, C Basak, M Saavedra-Pellitero, G Winckler, F Lamy, J Gottschalk

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in Nature communications, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing 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

1 citing paper in PubMed.

  1. Article
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

8 authors.

L JebasinskiInstitute of Geosciences, Kiel University, Kiel, Germany. lena.jebasinski@ifg.uni-kiel.de.ORCID http://orcid.org/0009-0006-7931-5356
D A FrickInstitute of Geosciences, Kiel University, Kiel, Germany.ORCID http://orcid.org/0000-0002-8530-3064
A K I U KapugeDepartment of Earth Sciences, University of Delaware, Newark, DE, USA.
C BasakDepartment of Earth Sciences, University of Delaware, Newark, DE, USA.
M Saavedra-PelliteroSchool of the Environment and Life Sciences, University of Portsmouth, Portsmouth, UK.ORCID http://orcid.org/0000-0003-0621-7932
G WincklerColumbia Climate School, Columbia University, New York, NY, USA.ORCID http://orcid.org/0000-0001-8718-2684
F LamyAlfred Wegener Institute (AWI) Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany.ORCID http://orcid.org/0000-0001-5952-1765
J GottschalkInstitute of Geosciences, Kiel University, Kiel, Germany.ORCID http://orcid.org/0000-0002-0403-3059

Funding

National Science Foundation (NSF) OCE 2406582
6 · The paper itself

Abstract

Millennial-scale deoxygenation of Antarctic Bottom Water (AABW) in the Atlantic Southern Ocean during past interglacials was linked to West Antarctic Ice Sheet (WAIS) melt-driven suppression of dense water formation along the Antarctic margin. However, the circum-Antarctic extent of these 'AABW stagnation events' and drivers of WAIS retreat remain unclear. Here, we identify recurring bottom water O

Identifiers

PMID41093831
PMCPMC12528459

What OpenQuestion holds

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LicenceCC BY
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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.