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Cited by 309

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Pleistocene Collapse of the West Antarctic Ice Sheet

Scherer, Reed P., Aldahan, Ala, Tulaczyk, Slawek, Possnert, Göran, Engelhardt, Hermann, Kamb, Barclay·1998·Science

Abstract

Some glacial sediment samples recovered from beneath the West Antarctic ice sheet at ice stream B contain Quaternary diatoms and up to 10 8 atoms of beryllium-10 per gram. Other samples contain no Quaternary diatoms and only background levels of beryllium-10 (less than 10 6 atoms per gram). The occurrence of young diatoms and high concentrations of beryllium-10 beneath grounded ice indicates that the Ross Embayment was an open marine environment after a late Pleistocene collapse of the marine ice sheet.

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Metadata

Authors
Scherer, R. P., Aldahan, A., Tulaczyk, S., Possnert, G., Engelhardt, H., & Kamb, B.
Venue
Science
Published
1998-07-03
Volume
281
Issue
5373
Pages
82-85
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W1974258673
Cited by
309
References
0
FWCI
5.28
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Pleistocene Collapse of the West Antarctic Ice Sheet. https://app.cochat.ai/papers/10.1126/science.281.5373.82
The paper
Scherer, R. P., Aldahan, A., Tulaczyk, S., Possnert, G., Engelhardt, H., & Kamb, B. (1998). Pleistocene Collapse of the West Antarctic Ice Sheet. Science. https://doi.org/10.1126/science.281.5373.82

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.