ArticleNature communications2022
Wilkes subglacial basin ice sheet response to Southern Ocean warming during late Pleistocene interglacials.
Article in Nature communications, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. An erratum has been issued. Cited by 5 papers.
What it found
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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.
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.
Who cites it
5 citing papers in PubMed.
- Sequence of abrupt transitions in Antarctic drainage basins before and during the Mid-Pleistocene Transition.Nature communications · 2025Article
- Footprint of sustained poleward warm water flow within East Antarctic submarine canyons.Nature communications · 2024Article
- An ancient river landscape preserved beneath the East Antarctic Ice Sheet.Nature communications · 2023Article
- Multiple episodes of ice loss from the Wilkes Subglacial Basin during the Last Interglacial.Nature communications · 2023Article
- Increased warm water intrusions could cause mass loss in East Antarctica during the next 200 years.Nature communications · 2023Article
Corrections and comments
- Erratum issued
Authors and funding
10 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The response of the East Antarctic Ice Sheet to past intervals of oceanic and atmospheric warming is still not well constrained but is critical for understanding both past and future sea-level change. Furthermore, the ice sheet in the Wilkes Subglacial Basin appears to have undergone thinning and ice discharge events during recent decades. Here we combine glaciological evidence on ice sheet elevation from the TALDICE ice core with offshore sedimentological records and ice sheet modelling experiments to reconstruct the ice dynamics in the Wilkes Subglacial Basin over the past 350,000 years. Our results indicate that the Wilkes Subglacial Basin experienced an extensive retreat 330,000 years ago and a more limited retreat 125,000 years ago. These changes coincide with warmer Southern Ocean temperatures and elevated global mean sea level during those interglacial periods, confirming the sensitivity of the Wilkes Subglacial Basin ice sheet to ocean warming and its potential role in sea-level change.
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