ArticleProceedings of the National Academy of Sciences of the United States of America2020
A new sea-level record for the Neogene/Quaternary boundary reveals transition to a more stable East Antarctic Ice Sheet.
Article in Proceedings of the National Academy of Sciences of the United States of America, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.
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Who cites it
6 citing papers in PubMed, 72 citations in OpenAlex.
- A continental-scale Eurasian ice sheet 2.4 million years ago.Nature communications · 2026Article
- South Pacific sea surface temperature and global ocean circulation changes since the late Miocene.Nature communications · 2025Article
- Article
- Orbital and suborbital temperature variability in the central Mediterranean across the Pliocene/Pleistocene transition.PloS one · 2024Article
- Climate-controlled submarine landslides on the Antarctic continental margin.Nature communications · 2023Article
- Episodes of Early Pleistocene West Antarctic Ice Sheet Retreat Recorded by Iceberg Alley Sediments.Paleoceanography and paleoclimatology · 2022Article
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Authors and funding
7 authors at 4 institutions in 2 countries.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Sea-level rise resulting from the instability of polar continental ice sheets represents a major socioeconomic hazard arising from anthropogenic warming, but the response of the largest component of Earth's cryosphere, the East Antarctic Ice Sheet (EAIS), to global warming is poorly understood. Here we present a detailed record of North Atlantic deep-ocean temperature, global sea-level, and ice-volume change for ∼2.75 to 2.4 Ma ago, when atmospheric partial pressure of carbon dioxide (
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