ArticleScience advances2023
Constraining the contribution of the Antarctic Ice Sheet to Last Interglacial sea level.
Article in Science advances, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 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.
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Who cites it
6 citing papers in PubMed, 34 citations in OpenAlex.
- North American ice sheet persistence into past interglacials should inform future projections.Nature communications · 2026Review
- Episodic reef growth in the Last Interglacial driven by competing influence of polar ice sheets to sea level rise.Science advances · 2025Article
- Genomic Introgression and Adaptation of Southern Seabird Species Facilitate Recent Polar Colonization.Molecular biology and evolution · 2025Article
- The Ronne Ice Shelf survived the last interglacial.Nature · 2025Article
- Warming of +1.5 °C is too high for polar ice sheets.Communications earth & environment · 2025Review
- East Antarctic warming forced by ice loss during the Last Interglacial.Nature communications · 2024Article
Corrections and comments
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Authors and funding
8 authors at 6 institutions in 3 countries.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Polar temperatures during the Last Interglacial [LIG; ~129 to 116 thousand years (ka)] were warmer than today, making this time period an important testing ground to better understand how ice sheets respond to warming. However, it remains debated how much and when the Antarctic and Greenland ice sheets changed during this period. Here, we present a combination of new and existing absolutely dated LIG sea-level observations from Britain, France, and Denmark. Because of glacial isostatic adjustment (GIA), the LIG Greenland ice melt contribution to sea-level change in this region is small, which allows us to constrain Antarctic ice change. We find that the Antarctic contribution to LIG global mean sea level peaked early in the interglacial (before 126 ka), with a maximum contribution of 5.7 m (50th percentile, 3.6 to 8.7 m central 68% probability) before declining. Our results support an asynchronous melt history over the LIG, with an early Antarctic contribution followed by later Greenland Ice Sheet mass loss.
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Registered trials
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