Sedimentological analysis of eight cores from the Amundsen Sea ...
Recent palaeoglaciological studies on the West Antarctic shelf have mainly focused on the wide embayments of the Ross and Amundsen seas in order to reconstruct the extent and subsequent retreat of the West Antarctic Ice Sheet (WAIS) since the Last Glacial Maximum (LGM). However, the narrower shelf s...
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ftdatacite:10.1594/pangaea.818175 2024-09-15T17:39:04+00:00 Sedimentological analysis of eight cores from the Amundsen Sea ... Klages, Johann Philipp Kuhn, Gerhard Hillenbrand, Claus-Dieter Graham, Alastair G C Smith, James A Larter, Robert D Gohl, Karsten 2014 application/zip https://dx.doi.org/10.1594/pangaea.818175 https://doi.pangaea.de/10.1594/PANGAEA.818175 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2014.02.017 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type Giant box corer ANT-XXVI/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2014 ftdatacite https://doi.org/10.1594/pangaea.81817510.1016/j.quascirev.2014.02.017 2024-07-03T13:16:23Z Recent palaeoglaciological studies on the West Antarctic shelf have mainly focused on the wide embayments of the Ross and Amundsen seas in order to reconstruct the extent and subsequent retreat of the West Antarctic Ice Sheet (WAIS) since the Last Glacial Maximum (LGM). However, the narrower shelf sectors between these two major embayments have remained largely unstudied in previous geological investigations despite them covering extensive areas of the West Antarctic shelf. Here, we present the first systematic marine geological and geophysical survey of a shelf sector offshore from the Hobbs Coast. It is dominated by a large grounding zone wedge (GZW), which fills the base of a palaeo-ice stream trough on the inner shelf and marks a phase of stabilization of the grounding line during general WAIS retreat following the last maximum ice-sheet extent in this particular area (referred to as the Local Last Glacial Maximum, 'LLGM'). Reliable age determination on calcareous microfossils from the infill of a ... : Supplement to: Klages, Johann Philipp; Kuhn, Gerhard; Hillenbrand, Claus-Dieter; Graham, Alastair G C; Smith, James A; Larter, Robert D; Gohl, Karsten; Wacker, Lukas (2014): Retreat of the West Antarctic Ice Sheet from the western Amundsen Sea shelf at a pre- or early LGM stage. Quaternary Science Reviews, 91, 1-15 ... Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Hobbs coast Ice Sheet DataCite |
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DataCite |
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language |
English |
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Gravity corer Kiel type Giant box corer ANT-XXVI/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
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Gravity corer Kiel type Giant box corer ANT-XXVI/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Klages, Johann Philipp Kuhn, Gerhard Hillenbrand, Claus-Dieter Graham, Alastair G C Smith, James A Larter, Robert D Gohl, Karsten Sedimentological analysis of eight cores from the Amundsen Sea ... |
topic_facet |
Gravity corer Kiel type Giant box corer ANT-XXVI/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
description |
Recent palaeoglaciological studies on the West Antarctic shelf have mainly focused on the wide embayments of the Ross and Amundsen seas in order to reconstruct the extent and subsequent retreat of the West Antarctic Ice Sheet (WAIS) since the Last Glacial Maximum (LGM). However, the narrower shelf sectors between these two major embayments have remained largely unstudied in previous geological investigations despite them covering extensive areas of the West Antarctic shelf. Here, we present the first systematic marine geological and geophysical survey of a shelf sector offshore from the Hobbs Coast. It is dominated by a large grounding zone wedge (GZW), which fills the base of a palaeo-ice stream trough on the inner shelf and marks a phase of stabilization of the grounding line during general WAIS retreat following the last maximum ice-sheet extent in this particular area (referred to as the Local Last Glacial Maximum, 'LLGM'). Reliable age determination on calcareous microfossils from the infill of a ... : Supplement to: Klages, Johann Philipp; Kuhn, Gerhard; Hillenbrand, Claus-Dieter; Graham, Alastair G C; Smith, James A; Larter, Robert D; Gohl, Karsten; Wacker, Lukas (2014): Retreat of the West Antarctic Ice Sheet from the western Amundsen Sea shelf at a pre- or early LGM stage. Quaternary Science Reviews, 91, 1-15 ... |
format |
Article in Journal/Newspaper |
author |
Klages, Johann Philipp Kuhn, Gerhard Hillenbrand, Claus-Dieter Graham, Alastair G C Smith, James A Larter, Robert D Gohl, Karsten |
author_facet |
Klages, Johann Philipp Kuhn, Gerhard Hillenbrand, Claus-Dieter Graham, Alastair G C Smith, James A Larter, Robert D Gohl, Karsten |
author_sort |
Klages, Johann Philipp |
title |
Sedimentological analysis of eight cores from the Amundsen Sea ... |
title_short |
Sedimentological analysis of eight cores from the Amundsen Sea ... |
title_full |
Sedimentological analysis of eight cores from the Amundsen Sea ... |
title_fullStr |
Sedimentological analysis of eight cores from the Amundsen Sea ... |
title_full_unstemmed |
Sedimentological analysis of eight cores from the Amundsen Sea ... |
title_sort |
sedimentological analysis of eight cores from the amundsen sea ... |
publisher |
PANGAEA |
publishDate |
2014 |
url |
https://dx.doi.org/10.1594/pangaea.818175 https://doi.pangaea.de/10.1594/PANGAEA.818175 |
genre |
Amundsen Sea Antarc* Antarctic Hobbs coast Ice Sheet |
genre_facet |
Amundsen Sea Antarc* Antarctic Hobbs coast Ice Sheet |
op_relation |
https://dx.doi.org/10.1016/j.quascirev.2014.02.017 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.81817510.1016/j.quascirev.2014.02.017 |
_version_ |
1810477304390877184 |