Late Pleistocene glaciation and retreat of ice sheet on the shelf of the South Orkney Plateau, West Antarctica
The research aims to provide insight into reconstruction of the Late Pleistocene glaciations and ice retreat that followed the Last Glacial Maximum. The study is based on multi-channel seismic profiling and multibeam survey conducted on the shelf during the 63-rd Russian Antarctic Expedition (2018)...
Published in: | Ice and Snow |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | Russian |
Published: |
Nauka
2021
|
Subjects: | |
Online Access: | https://doi.org/10.31857/S2076673421040109 https://doaj.org/article/3f5919a072f1450093bedc312699cbd5 |
id |
ftdoajarticles:oai:doaj.org/article:3f5919a072f1450093bedc312699cbd5 |
---|---|
record_format |
openpolar |
spelling |
ftdoajarticles:oai:doaj.org/article:3f5919a072f1450093bedc312699cbd5 2023-05-15T13:57:42+02:00 Late Pleistocene glaciation and retreat of ice sheet on the shelf of the South Orkney Plateau, West Antarctica G. L. Leitchenkov E. A. Bazhenova 2021-12-01T00:00:00Z https://doi.org/10.31857/S2076673421040109 https://doaj.org/article/3f5919a072f1450093bedc312699cbd5 RU rus Nauka https://ice-snow.igras.ru/jour/article/view/935 https://doaj.org/toc/2076-6734 https://doaj.org/toc/2412-3765 2076-6734 2412-3765 doi:10.31857/S2076673421040109 https://doaj.org/article/3f5919a072f1450093bedc312699cbd5 Лëд и снег, Vol 61, Iss 4, Pp 571-586 (2021) антарктика южно-оркнейское плато шельф многолучевое эхолотирование сейсморазведка батиметрия морена плейстоцен оледенение дегляциация Science Q article 2021 ftdoajarticles https://doi.org/10.31857/S2076673421040109 2023-03-19T01:40:11Z The research aims to provide insight into reconstruction of the Late Pleistocene glaciations and ice retreat that followed the Last Glacial Maximum. The study is based on multi-channel seismic profiling and multibeam survey conducted on the shelf during the 63-rd Russian Antarctic Expedition (2018) on RV «Akademik Alexander Karpinsky». The 560-channel, 7000-m-long streamer and the Atlas Hydrosweep MD-3/30 multibeam echo-sounder were used for seismic and multibeam survey, respectively. In addition, previously collected seismic data available from the Antarctic Seismic Data Library System and bathymetry data from the «International Bathymetry Chart of the Southern Ocean» (IBCSO) Project were involved for interpretation. The multibeam survey was carried out within the Signy Trough and its flanks with depths ranging from 180 to 400 m, and covered the area of about 1500 km2. The data were collected along 43 profiles spaced at 750 m to ensure enough overlap between swaths. Variety of submarine glacial landforms formed by grounded ice was identified on shelf of the South Orkney Plateau with use of seismic and multibeam data. The most prominent of these features is the large terminal moraine at the middle shelf (previously described as the mid-shelf break) marking the greatest ice extent at the LGM. Oceanward of the large terminal moraine, the plateau-like feature (delineated by 350 and 425 m isobaths) with relatively steep outer slope is recognized from seismic data and interpreted as the distal terminal moraine formed during the pre-LGM Pleistocene glaciation. Within the Signy Trough, submarine glacial landforms mapped by multibeam survey, reflect ice retreat after the LGM; these landforms include: subglacial lineation at the western flank of the northern Signy Trough indicating fast flowing grounded ice, transverse recessional moraine ridges, lateral shear moraine on the western flank and lateral marginal moraine on the eastern flank of the Trough, two grounding zone wedges, streamlined features (drumlins) and an ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Southern Ocean West Antarctica Антарктика Directory of Open Access Journals: DOAJ Articles Antarctic Southern Ocean The Antarctic West Antarctica South Orkney Plateau ENVELOPE(-44.157,-44.157,-60.690,-60.690) Ice and Snow 61 4 571 586 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
Russian |
topic |
антарктика южно-оркнейское плато шельф многолучевое эхолотирование сейсморазведка батиметрия морена плейстоцен оледенение дегляциация Science Q |
spellingShingle |
антарктика южно-оркнейское плато шельф многолучевое эхолотирование сейсморазведка батиметрия морена плейстоцен оледенение дегляциация Science Q G. L. Leitchenkov E. A. Bazhenova Late Pleistocene glaciation and retreat of ice sheet on the shelf of the South Orkney Plateau, West Antarctica |
topic_facet |
антарктика южно-оркнейское плато шельф многолучевое эхолотирование сейсморазведка батиметрия морена плейстоцен оледенение дегляциация Science Q |
description |
The research aims to provide insight into reconstruction of the Late Pleistocene glaciations and ice retreat that followed the Last Glacial Maximum. The study is based on multi-channel seismic profiling and multibeam survey conducted on the shelf during the 63-rd Russian Antarctic Expedition (2018) on RV «Akademik Alexander Karpinsky». The 560-channel, 7000-m-long streamer and the Atlas Hydrosweep MD-3/30 multibeam echo-sounder were used for seismic and multibeam survey, respectively. In addition, previously collected seismic data available from the Antarctic Seismic Data Library System and bathymetry data from the «International Bathymetry Chart of the Southern Ocean» (IBCSO) Project were involved for interpretation. The multibeam survey was carried out within the Signy Trough and its flanks with depths ranging from 180 to 400 m, and covered the area of about 1500 km2. The data were collected along 43 profiles spaced at 750 m to ensure enough overlap between swaths. Variety of submarine glacial landforms formed by grounded ice was identified on shelf of the South Orkney Plateau with use of seismic and multibeam data. The most prominent of these features is the large terminal moraine at the middle shelf (previously described as the mid-shelf break) marking the greatest ice extent at the LGM. Oceanward of the large terminal moraine, the plateau-like feature (delineated by 350 and 425 m isobaths) with relatively steep outer slope is recognized from seismic data and interpreted as the distal terminal moraine formed during the pre-LGM Pleistocene glaciation. Within the Signy Trough, submarine glacial landforms mapped by multibeam survey, reflect ice retreat after the LGM; these landforms include: subglacial lineation at the western flank of the northern Signy Trough indicating fast flowing grounded ice, transverse recessional moraine ridges, lateral shear moraine on the western flank and lateral marginal moraine on the eastern flank of the Trough, two grounding zone wedges, streamlined features (drumlins) and an ... |
format |
Article in Journal/Newspaper |
author |
G. L. Leitchenkov E. A. Bazhenova |
author_facet |
G. L. Leitchenkov E. A. Bazhenova |
author_sort |
G. L. Leitchenkov |
title |
Late Pleistocene glaciation and retreat of ice sheet on the shelf of the South Orkney Plateau, West Antarctica |
title_short |
Late Pleistocene glaciation and retreat of ice sheet on the shelf of the South Orkney Plateau, West Antarctica |
title_full |
Late Pleistocene glaciation and retreat of ice sheet on the shelf of the South Orkney Plateau, West Antarctica |
title_fullStr |
Late Pleistocene glaciation and retreat of ice sheet on the shelf of the South Orkney Plateau, West Antarctica |
title_full_unstemmed |
Late Pleistocene glaciation and retreat of ice sheet on the shelf of the South Orkney Plateau, West Antarctica |
title_sort |
late pleistocene glaciation and retreat of ice sheet on the shelf of the south orkney plateau, west antarctica |
publisher |
Nauka |
publishDate |
2021 |
url |
https://doi.org/10.31857/S2076673421040109 https://doaj.org/article/3f5919a072f1450093bedc312699cbd5 |
long_lat |
ENVELOPE(-44.157,-44.157,-60.690,-60.690) |
geographic |
Antarctic Southern Ocean The Antarctic West Antarctica South Orkney Plateau |
geographic_facet |
Antarctic Southern Ocean The Antarctic West Antarctica South Orkney Plateau |
genre |
Antarc* Antarctic Antarctica Ice Sheet Southern Ocean West Antarctica Антарктика |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Southern Ocean West Antarctica Антарктика |
op_source |
Лëд и снег, Vol 61, Iss 4, Pp 571-586 (2021) |
op_relation |
https://ice-snow.igras.ru/jour/article/view/935 https://doaj.org/toc/2076-6734 https://doaj.org/toc/2412-3765 2076-6734 2412-3765 doi:10.31857/S2076673421040109 https://doaj.org/article/3f5919a072f1450093bedc312699cbd5 |
op_doi |
https://doi.org/10.31857/S2076673421040109 |
container_title |
Ice and Snow |
container_volume |
61 |
container_issue |
4 |
container_start_page |
571 |
op_container_end_page |
586 |
_version_ |
1766265520672210944 |