Pleistocene Collapse of the West Antarctic Ice Sheet
Some glacial sediment samples recovered from beneath the West Antarctic ice sheet at ice stream B contain Quaternary diatoms and up to 108 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 occur...
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American Association for the Advancement of Science
1998
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ftcaltechauth:oai:authors.library.caltech.edu:45887 2023-05-15T14:04:55+02:00 Pleistocene Collapse of the West Antarctic Ice Sheet Scherer, Reed P. Aldahan, Ala Tulaczyk, Slawek Possnert, Göran Engelhardt, Hermann Kamb, Barclay 1998-07-03 https://authors.library.caltech.edu/45887/ https://resolver.caltech.edu/CaltechAUTHORS:20140522-095331661 unknown American Association for the Advancement of Science Scherer, Reed P. and Aldahan, Ala and Tulaczyk, Slawek and Possnert, Göran and Engelhardt, Hermann and Kamb, Barclay (1998) Pleistocene Collapse of the West Antarctic Ice Sheet. Science, 281 (5373). pp. 82-85. ISSN 0036-8075. doi:10.1126/science.281.5373.82. https://resolver.caltech.edu/CaltechAUTHORS:20140522-095331661 <https://resolver.caltech.edu/CaltechAUTHORS:20140522-095331661> Article PeerReviewed 1998 ftcaltechauth https://doi.org/10.1126/science.281.5373.82 2021-11-11T18:57:51Z Some glacial sediment samples recovered from beneath the West Antarctic ice sheet at ice stream B contain Quaternary diatoms and up to 108 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. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Ice Stream B Caltech Authors (California Institute of Technology) Antarctic West Antarctic Ice Sheet Science 281 5373 82 85 |
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Open Polar |
collection |
Caltech Authors (California Institute of Technology) |
op_collection_id |
ftcaltechauth |
language |
unknown |
description |
Some glacial sediment samples recovered from beneath the West Antarctic ice sheet at ice stream B contain Quaternary diatoms and up to 108 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. |
format |
Article in Journal/Newspaper |
author |
Scherer, Reed P. Aldahan, Ala Tulaczyk, Slawek Possnert, Göran Engelhardt, Hermann Kamb, Barclay |
spellingShingle |
Scherer, Reed P. Aldahan, Ala Tulaczyk, Slawek Possnert, Göran Engelhardt, Hermann Kamb, Barclay Pleistocene Collapse of the West Antarctic Ice Sheet |
author_facet |
Scherer, Reed P. Aldahan, Ala Tulaczyk, Slawek Possnert, Göran Engelhardt, Hermann Kamb, Barclay |
author_sort |
Scherer, Reed P. |
title |
Pleistocene Collapse of the West Antarctic Ice Sheet |
title_short |
Pleistocene Collapse of the West Antarctic Ice Sheet |
title_full |
Pleistocene Collapse of the West Antarctic Ice Sheet |
title_fullStr |
Pleistocene Collapse of the West Antarctic Ice Sheet |
title_full_unstemmed |
Pleistocene Collapse of the West Antarctic Ice Sheet |
title_sort |
pleistocene collapse of the west antarctic ice sheet |
publisher |
American Association for the Advancement of Science |
publishDate |
1998 |
url |
https://authors.library.caltech.edu/45887/ https://resolver.caltech.edu/CaltechAUTHORS:20140522-095331661 |
geographic |
Antarctic West Antarctic Ice Sheet |
geographic_facet |
Antarctic West Antarctic Ice Sheet |
genre |
Antarc* Antarctic Ice Sheet Ice Stream B |
genre_facet |
Antarc* Antarctic Ice Sheet Ice Stream B |
op_relation |
Scherer, Reed P. and Aldahan, Ala and Tulaczyk, Slawek and Possnert, Göran and Engelhardt, Hermann and Kamb, Barclay (1998) Pleistocene Collapse of the West Antarctic Ice Sheet. Science, 281 (5373). pp. 82-85. ISSN 0036-8075. doi:10.1126/science.281.5373.82. https://resolver.caltech.edu/CaltechAUTHORS:20140522-095331661 <https://resolver.caltech.edu/CaltechAUTHORS:20140522-095331661> |
op_doi |
https://doi.org/10.1126/science.281.5373.82 |
container_title |
Science |
container_volume |
281 |
container_issue |
5373 |
container_start_page |
82 |
op_container_end_page |
85 |
_version_ |
1766276373871067136 |