Weathering characteristics and lithology of samples from the Rauer Group, Antarctica, obtained in February/March 2007, and conducted with field support of POLARSTERN cruise ANT-XXIII/9 ...
The presence of glacial sediments across the Rauer Group indicates that the East Antarctic ice sheet formerly covered the entire archipelago and has since retreated at least 15 km from its maximum extent. The degree of weathering of these glacial sediments suggests that ice retreat from this maximum...
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ftdatacite:10.1594/pangaea.858210 2024-09-15T17:46:45+00:00 Weathering characteristics and lithology of samples from the Rauer Group, Antarctica, obtained in February/March 2007, and conducted with field support of POLARSTERN cruise ANT-XXIII/9 ... White, Duanne A Bennike, Ole Berg, Sonja Harley, S Fink, David Kiernan, Kevin W McConnell, Anne Wagner, Bernd 2009 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.858210 https://doi.pangaea.de/10.1594/PANGAEA.858210 en eng PANGAEA https://dx.doi.org/10.1016/j.yqres.2009.04.001 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Optional event label Date/Time of event Date/Time of event 2 Latitude of event Longitude of event Elevation of event Area/locality Deposit type Distance Number Standard deviation Comment Weathering Index Gneiss Geological sample Rock sample Schmidt hammer bedrock rebound Moriwaki Degree of Weathering MDoW ANT-XXIII/9 Polarstern Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Dataset dataset Supplementary Dataset 2009 ftdatacite https://doi.org/10.1594/pangaea.85821010.1016/j.yqres.2009.04.001 2024-07-03T13:11:36Z The presence of glacial sediments across the Rauer Group indicates that the East Antarctic ice sheet formerly covered the entire archipelago and has since retreated at least 15 km from its maximum extent. The degree of weathering of these glacial sediments suggests that ice retreat from this maximum position occurred sometime during the latter half of the last glacial cycle. Following this phase of retreat, the ice sheet margin has not expanded more than ~1 km seaward of its present position. This pattern of ice sheet change matches that recorded in Vestfold Hills, providing further evidence that the diminutive Marine Isotope Stage 2 ice sheet advance in the nearby Larsemann Hills may have been influenced by local factors rather than a regional ice-sheet response to climate and sea-level change. ... : Supplement to: White, Duanne A; Bennike, Ole; Berg, Sonja; Harley, S; Fink, David; Kiernan, Kevin W; McConnell, Anne; Wagner, Bernd (2009): Geomorphology and glacial history of Rauer Group, East Antarctica. Quaternary Research, 72(1), 80-90 ... Dataset Antarc* Antarctic Antarctica East Antarctica Ice Sheet Sea ice DataCite |
institution |
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collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Optional event label Date/Time of event Date/Time of event 2 Latitude of event Longitude of event Elevation of event Area/locality Deposit type Distance Number Standard deviation Comment Weathering Index Gneiss Geological sample Rock sample Schmidt hammer bedrock rebound Moriwaki Degree of Weathering MDoW ANT-XXIII/9 Polarstern Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
spellingShingle |
Event label Optional event label Date/Time of event Date/Time of event 2 Latitude of event Longitude of event Elevation of event Area/locality Deposit type Distance Number Standard deviation Comment Weathering Index Gneiss Geological sample Rock sample Schmidt hammer bedrock rebound Moriwaki Degree of Weathering MDoW ANT-XXIII/9 Polarstern Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 White, Duanne A Bennike, Ole Berg, Sonja Harley, S Fink, David Kiernan, Kevin W McConnell, Anne Wagner, Bernd Weathering characteristics and lithology of samples from the Rauer Group, Antarctica, obtained in February/March 2007, and conducted with field support of POLARSTERN cruise ANT-XXIII/9 ... |
topic_facet |
Event label Optional event label Date/Time of event Date/Time of event 2 Latitude of event Longitude of event Elevation of event Area/locality Deposit type Distance Number Standard deviation Comment Weathering Index Gneiss Geological sample Rock sample Schmidt hammer bedrock rebound Moriwaki Degree of Weathering MDoW ANT-XXIII/9 Polarstern Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
description |
The presence of glacial sediments across the Rauer Group indicates that the East Antarctic ice sheet formerly covered the entire archipelago and has since retreated at least 15 km from its maximum extent. The degree of weathering of these glacial sediments suggests that ice retreat from this maximum position occurred sometime during the latter half of the last glacial cycle. Following this phase of retreat, the ice sheet margin has not expanded more than ~1 km seaward of its present position. This pattern of ice sheet change matches that recorded in Vestfold Hills, providing further evidence that the diminutive Marine Isotope Stage 2 ice sheet advance in the nearby Larsemann Hills may have been influenced by local factors rather than a regional ice-sheet response to climate and sea-level change. ... : Supplement to: White, Duanne A; Bennike, Ole; Berg, Sonja; Harley, S; Fink, David; Kiernan, Kevin W; McConnell, Anne; Wagner, Bernd (2009): Geomorphology and glacial history of Rauer Group, East Antarctica. Quaternary Research, 72(1), 80-90 ... |
format |
Dataset |
author |
White, Duanne A Bennike, Ole Berg, Sonja Harley, S Fink, David Kiernan, Kevin W McConnell, Anne Wagner, Bernd |
author_facet |
White, Duanne A Bennike, Ole Berg, Sonja Harley, S Fink, David Kiernan, Kevin W McConnell, Anne Wagner, Bernd |
author_sort |
White, Duanne A |
title |
Weathering characteristics and lithology of samples from the Rauer Group, Antarctica, obtained in February/March 2007, and conducted with field support of POLARSTERN cruise ANT-XXIII/9 ... |
title_short |
Weathering characteristics and lithology of samples from the Rauer Group, Antarctica, obtained in February/March 2007, and conducted with field support of POLARSTERN cruise ANT-XXIII/9 ... |
title_full |
Weathering characteristics and lithology of samples from the Rauer Group, Antarctica, obtained in February/March 2007, and conducted with field support of POLARSTERN cruise ANT-XXIII/9 ... |
title_fullStr |
Weathering characteristics and lithology of samples from the Rauer Group, Antarctica, obtained in February/March 2007, and conducted with field support of POLARSTERN cruise ANT-XXIII/9 ... |
title_full_unstemmed |
Weathering characteristics and lithology of samples from the Rauer Group, Antarctica, obtained in February/March 2007, and conducted with field support of POLARSTERN cruise ANT-XXIII/9 ... |
title_sort |
weathering characteristics and lithology of samples from the rauer group, antarctica, obtained in february/march 2007, and conducted with field support of polarstern cruise ant-xxiii/9 ... |
publisher |
PANGAEA |
publishDate |
2009 |
url |
https://dx.doi.org/10.1594/pangaea.858210 https://doi.pangaea.de/10.1594/PANGAEA.858210 |
genre |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet Sea ice |
genre_facet |
Antarc* Antarctic Antarctica East Antarctica Ice Sheet Sea ice |
op_relation |
https://dx.doi.org/10.1016/j.yqres.2009.04.001 |
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.85821010.1016/j.yqres.2009.04.001 |
_version_ |
1810495102746886144 |