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Pleistocene Collapse of the West Antarctic Ice Sheet
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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Cited by
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Sea-level rise due to polar ice-sheet mass loss during past warm periods
Dutton, A., Carlson, A. E., Long, A. J., Milne, G. A., Clark, P. U., DeConto, R., Horton, B. P., Rahmstorf, S., & Raymo, M. E. (2015) · Science · doi:10.1126/science.aaa4019 · Cited by 846
Interglacials of the last 800,000 years
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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
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- 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.