Sedimentary record of the last glaciation of the Bellingshausen Sea, West Antarctica ...

Upper Quaternary marine sediments recovered from the West Antarctic continental margin are characterized by a distinct lithological succession allowing the reconstruction of past environmental changes. Massive, homogenous diamictons were deposited elsewhere on the margin during the last glacial peri...

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Main Authors: Hillenbrand, Claus-Dieter, Baesler, Anja, Grobe, Hannes
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2005
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.711337
https://doi.pangaea.de/10.1594/PANGAEA.711337
id ftdatacite:10.1594/pangaea.711337
record_format openpolar
spelling ftdatacite:10.1594/pangaea.711337 2024-09-15T17:47:51+00:00 Sedimentary record of the last glaciation of the Bellingshausen Sea, West Antarctica ... Hillenbrand, Claus-Dieter Baesler, Anja Grobe, Hannes 2005 application/zip https://dx.doi.org/10.1594/pangaea.711337 https://doi.pangaea.de/10.1594/PANGAEA.711337 en eng PANGAEA https://dx.doi.org/10.1016/j.margeo.2005.01.007 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type ANT-XI/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2005 ftdatacite https://doi.org/10.1594/pangaea.71133710.1016/j.margeo.2005.01.007 2024-07-03T13:10:33Z Upper Quaternary marine sediments recovered from the West Antarctic continental margin are characterized by a distinct lithological succession allowing the reconstruction of past environmental changes. Massive, homogenous diamictons were deposited elsewhere on the margin during the last glacial period, when grounded ice masses advanced across the shelf. Sedimentological investigations using a multi-proxy approach and examination of the margin topography suggest that during this time a deformation till and subsequently a glaciomarine till were deposited on the shelf, while glaciogenic debris flows were deposited on the slope and rise. The comparison of the clay mineral assemblages in the matrix of the diamictons with clay mineral assemblages of potential source areas reveals distinct pathways of grounded ice flow on the shelf. Lithogenic sandy muds overlying the diamictons were deposited by meltwater flows and/or marine currents on the shelf, and by turbidity currents and marine currents on the slope and ... : Supplement to: Hillenbrand, Claus-Dieter; Baesler, Anja; Grobe, Hannes (2005): The sedimentary record of the last glaciation in the western Bellingshausen Sea (West Antarctica): Implications for the interpretation of diamictons in a polar-marine setting. Marine Geology, 216(4), 191-204 ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Bellingshausen Sea West Antarctica DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
ANT-XI/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Gravity corer Kiel type
ANT-XI/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Hillenbrand, Claus-Dieter
Baesler, Anja
Grobe, Hannes
Sedimentary record of the last glaciation of the Bellingshausen Sea, West Antarctica ...
topic_facet Gravity corer Kiel type
ANT-XI/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description Upper Quaternary marine sediments recovered from the West Antarctic continental margin are characterized by a distinct lithological succession allowing the reconstruction of past environmental changes. Massive, homogenous diamictons were deposited elsewhere on the margin during the last glacial period, when grounded ice masses advanced across the shelf. Sedimentological investigations using a multi-proxy approach and examination of the margin topography suggest that during this time a deformation till and subsequently a glaciomarine till were deposited on the shelf, while glaciogenic debris flows were deposited on the slope and rise. The comparison of the clay mineral assemblages in the matrix of the diamictons with clay mineral assemblages of potential source areas reveals distinct pathways of grounded ice flow on the shelf. Lithogenic sandy muds overlying the diamictons were deposited by meltwater flows and/or marine currents on the shelf, and by turbidity currents and marine currents on the slope and ... : Supplement to: Hillenbrand, Claus-Dieter; Baesler, Anja; Grobe, Hannes (2005): The sedimentary record of the last glaciation in the western Bellingshausen Sea (West Antarctica): Implications for the interpretation of diamictons in a polar-marine setting. Marine Geology, 216(4), 191-204 ...
format Article in Journal/Newspaper
author Hillenbrand, Claus-Dieter
Baesler, Anja
Grobe, Hannes
author_facet Hillenbrand, Claus-Dieter
Baesler, Anja
Grobe, Hannes
author_sort Hillenbrand, Claus-Dieter
title Sedimentary record of the last glaciation of the Bellingshausen Sea, West Antarctica ...
title_short Sedimentary record of the last glaciation of the Bellingshausen Sea, West Antarctica ...
title_full Sedimentary record of the last glaciation of the Bellingshausen Sea, West Antarctica ...
title_fullStr Sedimentary record of the last glaciation of the Bellingshausen Sea, West Antarctica ...
title_full_unstemmed Sedimentary record of the last glaciation of the Bellingshausen Sea, West Antarctica ...
title_sort sedimentary record of the last glaciation of the bellingshausen sea, west antarctica ...
publisher PANGAEA
publishDate 2005
url https://dx.doi.org/10.1594/pangaea.711337
https://doi.pangaea.de/10.1594/PANGAEA.711337
genre Antarc*
Antarctic
Antarctica
Bellingshausen Sea
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
Bellingshausen Sea
West Antarctica
op_relation https://dx.doi.org/10.1016/j.margeo.2005.01.007
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.71133710.1016/j.margeo.2005.01.007
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