Sediment record of the last 1.8 Ma in the Amundsen Sea, supplement to: Hillenbrand, Claus-Dieter; Fütterer, Dieter K; Grobe, Hannes; Frederichs, Thomas (2002): No evidence for a Pleistocene collapse of the West Antarctic Ice Sheet from continental margin sediments recovered in the Amundsen Sea. Geo-Marine Letters, 22(2), 51-59
Records of glaciomarine deposition recovered from the West Antarctic continental margin in the Amundsen Sea allow the reconstruction of the behaviour of the West Antarctic Ice Sheet (WAIS) in response to the natural climatic changes of the last 1.8 million years. Contents of gravel-sized and lithoge...
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Online Access: | https://dx.doi.org/10.1594/pangaea.711660 https://doi.pangaea.de/10.1594/PANGAEA.711660 |
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ftdatacite:10.1594/pangaea.711660 2023-05-15T13:23:36+02:00 Sediment record of the last 1.8 Ma in the Amundsen Sea, supplement to: Hillenbrand, Claus-Dieter; Fütterer, Dieter K; Grobe, Hannes; Frederichs, Thomas (2002): No evidence for a Pleistocene collapse of the West Antarctic Ice Sheet from continental margin sediments recovered in the Amundsen Sea. Geo-Marine Letters, 22(2), 51-59 Hillenbrand, Claus-Dieter Fütterer, Dieter K Grobe, Hannes Frederichs, Thomas 2002 application/zip https://dx.doi.org/10.1594/pangaea.711660 https://doi.pangaea.de/10.1594/PANGAEA.711660 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.1007/s00367-002-0097-7 https://dx.doi.org/10.2312/bzp_0346_2000 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Giant box corer MultiCorer Gravity corer Kiel type ANT-VI/2 ANT-XI/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Silicon Cycling in the World Ocean SINOPS Supplementary Collection of Datasets Collection article 2002 ftdatacite https://doi.org/10.1594/pangaea.711660 https://doi.org/10.1007/s00367-002-0097-7 https://doi.org/10.2312/bzp_0346_2000 2022-02-08T16:24:46Z Records of glaciomarine deposition recovered from the West Antarctic continental margin in the Amundsen Sea allow the reconstruction of the behaviour of the West Antarctic Ice Sheet (WAIS) in response to the natural climatic changes of the last 1.8 million years. Contents of gravel-sized and lithogenic components represent the input and redeposition of glaciogenic debris, whereas variations in the proportions of the calcareous sediment fraction reflect palaeoproductivity changes. All proxies, which are regarded as sensitive to a WAIS collapse, changed markedly during the global climatic cycles, but do not confirm a complete disintegration of the WAIS during the Pleistocene. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Amundsen Sea Antarctic Hannes ENVELOPE(18.064,18.064,69.390,69.390) West Antarctic Ice Sheet |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Giant box corer MultiCorer Gravity corer Kiel type ANT-VI/2 ANT-XI/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Silicon Cycling in the World Ocean SINOPS |
spellingShingle |
Giant box corer MultiCorer Gravity corer Kiel type ANT-VI/2 ANT-XI/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Silicon Cycling in the World Ocean SINOPS Hillenbrand, Claus-Dieter Fütterer, Dieter K Grobe, Hannes Frederichs, Thomas Sediment record of the last 1.8 Ma in the Amundsen Sea, supplement to: Hillenbrand, Claus-Dieter; Fütterer, Dieter K; Grobe, Hannes; Frederichs, Thomas (2002): No evidence for a Pleistocene collapse of the West Antarctic Ice Sheet from continental margin sediments recovered in the Amundsen Sea. Geo-Marine Letters, 22(2), 51-59 |
topic_facet |
Giant box corer MultiCorer Gravity corer Kiel type ANT-VI/2 ANT-XI/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Silicon Cycling in the World Ocean SINOPS |
description |
Records of glaciomarine deposition recovered from the West Antarctic continental margin in the Amundsen Sea allow the reconstruction of the behaviour of the West Antarctic Ice Sheet (WAIS) in response to the natural climatic changes of the last 1.8 million years. Contents of gravel-sized and lithogenic components represent the input and redeposition of glaciogenic debris, whereas variations in the proportions of the calcareous sediment fraction reflect palaeoproductivity changes. All proxies, which are regarded as sensitive to a WAIS collapse, changed markedly during the global climatic cycles, but do not confirm a complete disintegration of the WAIS during the Pleistocene. |
format |
Article in Journal/Newspaper |
author |
Hillenbrand, Claus-Dieter Fütterer, Dieter K Grobe, Hannes Frederichs, Thomas |
author_facet |
Hillenbrand, Claus-Dieter Fütterer, Dieter K Grobe, Hannes Frederichs, Thomas |
author_sort |
Hillenbrand, Claus-Dieter |
title |
Sediment record of the last 1.8 Ma in the Amundsen Sea, supplement to: Hillenbrand, Claus-Dieter; Fütterer, Dieter K; Grobe, Hannes; Frederichs, Thomas (2002): No evidence for a Pleistocene collapse of the West Antarctic Ice Sheet from continental margin sediments recovered in the Amundsen Sea. Geo-Marine Letters, 22(2), 51-59 |
title_short |
Sediment record of the last 1.8 Ma in the Amundsen Sea, supplement to: Hillenbrand, Claus-Dieter; Fütterer, Dieter K; Grobe, Hannes; Frederichs, Thomas (2002): No evidence for a Pleistocene collapse of the West Antarctic Ice Sheet from continental margin sediments recovered in the Amundsen Sea. Geo-Marine Letters, 22(2), 51-59 |
title_full |
Sediment record of the last 1.8 Ma in the Amundsen Sea, supplement to: Hillenbrand, Claus-Dieter; Fütterer, Dieter K; Grobe, Hannes; Frederichs, Thomas (2002): No evidence for a Pleistocene collapse of the West Antarctic Ice Sheet from continental margin sediments recovered in the Amundsen Sea. Geo-Marine Letters, 22(2), 51-59 |
title_fullStr |
Sediment record of the last 1.8 Ma in the Amundsen Sea, supplement to: Hillenbrand, Claus-Dieter; Fütterer, Dieter K; Grobe, Hannes; Frederichs, Thomas (2002): No evidence for a Pleistocene collapse of the West Antarctic Ice Sheet from continental margin sediments recovered in the Amundsen Sea. Geo-Marine Letters, 22(2), 51-59 |
title_full_unstemmed |
Sediment record of the last 1.8 Ma in the Amundsen Sea, supplement to: Hillenbrand, Claus-Dieter; Fütterer, Dieter K; Grobe, Hannes; Frederichs, Thomas (2002): No evidence for a Pleistocene collapse of the West Antarctic Ice Sheet from continental margin sediments recovered in the Amundsen Sea. Geo-Marine Letters, 22(2), 51-59 |
title_sort |
sediment record of the last 1.8 ma in the amundsen sea, supplement to: hillenbrand, claus-dieter; fütterer, dieter k; grobe, hannes; frederichs, thomas (2002): no evidence for a pleistocene collapse of the west antarctic ice sheet from continental margin sediments recovered in the amundsen sea. geo-marine letters, 22(2), 51-59 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2002 |
url |
https://dx.doi.org/10.1594/pangaea.711660 https://doi.pangaea.de/10.1594/PANGAEA.711660 |
long_lat |
ENVELOPE(18.064,18.064,69.390,69.390) |
geographic |
Amundsen Sea Antarctic Hannes West Antarctic Ice Sheet |
geographic_facet |
Amundsen Sea Antarctic Hannes West Antarctic Ice Sheet |
genre |
Amundsen Sea Antarc* Antarctic Ice Sheet |
genre_facet |
Amundsen Sea Antarc* Antarctic Ice Sheet |
op_relation |
https://dx.doi.org/10.1007/s00367-002-0097-7 https://dx.doi.org/10.2312/bzp_0346_2000 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.711660 https://doi.org/10.1007/s00367-002-0097-7 https://doi.org/10.2312/bzp_0346_2000 |
_version_ |
1766373430457794560 |