Sedimentology on cores off Filchner Shelf Ice, Weddell Sea, Antarctica ...

The sediments of 14 box cores and 7 gravity cores, mainly taken directly in front of the Filchner(-Ronne) ice shelf northwest of Berkner Island (Weddell Sea), allowed to distinguish six sediment types. On the one hand,the retreat of the at first grounded and then floated ice from the last glacial ma...

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Main Authors: Wessels, Martin, Fütterer, Dieter K, Grobe, Hannes
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1989
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.701301
https://doi.pangaea.de/10.1594/PANGAEA.701301
id ftdatacite:10.1594/pangaea.701301
record_format openpolar
spelling ftdatacite:10.1594/pangaea.701301 2024-09-15T17:47:50+00:00 Sedimentology on cores off Filchner Shelf Ice, Weddell Sea, Antarctica ... Wessels, Martin Fütterer, Dieter K Grobe, Hannes 1989 application/zip https://dx.doi.org/10.1594/pangaea.701301 https://doi.pangaea.de/10.1594/PANGAEA.701301 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Giant box corer Gravity corer Kiel type ANT-II/4 ANT-IV/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 1989 ftdatacite https://doi.org/10.1594/pangaea.701301 2024-07-03T13:10:33Z The sediments of 14 box cores and 7 gravity cores, mainly taken directly in front of the Filchner(-Ronne) ice shelf northwest of Berkner Island (Weddell Sea), allowed to distinguish six sediment types. On the one hand,the retreat of the at first grounded and then floated ice from the last glacial maximum is documented. On the other hand,the sediments give an insight into extensive Holocene sediment deposition and remobilization northwest of Berkner Island.The ortho till was deposited directly by the grounded ice sheet and is lacking any marine influence. After floating of the ice shelf, partly very weIl stratified, partly unstratified, non-bioturbated paratill is deposited beneath the ice shelf. Lack of IRD-content in the paratill immediately above the orthotill indicates freezing at the bottom of the ice, at least for a short period after the ice became afloat. The orthotill and paratill contain small amounts of fragmented Tertiary diatoms, which allow the conclusion, that glacial-marine sediments in the ... : Supplement to: Wessels, Martin (1989): Sedimentationsprozesse an der Filchner Schelfeiskante, Antarktis. Diploma Thesis, Institut und Museum für Geologie und Paläontologie der Georg-August-Universität zu Göttingen (in Zusammenarbeit mit dem Alfred-Wegener-Institut), 126 pp ... Article in Journal/Newspaper Antarc* Antarctica Antarktis* Berkner Island Filchner Ronne Ice Shelf Filchner-Ronne Ice Shelf Ice Sheet Ice Shelf Ronne Ice Shelf Schelfeis* Weddell Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Giant box corer
Gravity corer Kiel type
ANT-II/4
ANT-IV/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Giant box corer
Gravity corer Kiel type
ANT-II/4
ANT-IV/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Wessels, Martin
Fütterer, Dieter K
Grobe, Hannes
Sedimentology on cores off Filchner Shelf Ice, Weddell Sea, Antarctica ...
topic_facet Giant box corer
Gravity corer Kiel type
ANT-II/4
ANT-IV/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description The sediments of 14 box cores and 7 gravity cores, mainly taken directly in front of the Filchner(-Ronne) ice shelf northwest of Berkner Island (Weddell Sea), allowed to distinguish six sediment types. On the one hand,the retreat of the at first grounded and then floated ice from the last glacial maximum is documented. On the other hand,the sediments give an insight into extensive Holocene sediment deposition and remobilization northwest of Berkner Island.The ortho till was deposited directly by the grounded ice sheet and is lacking any marine influence. After floating of the ice shelf, partly very weIl stratified, partly unstratified, non-bioturbated paratill is deposited beneath the ice shelf. Lack of IRD-content in the paratill immediately above the orthotill indicates freezing at the bottom of the ice, at least for a short period after the ice became afloat. The orthotill and paratill contain small amounts of fragmented Tertiary diatoms, which allow the conclusion, that glacial-marine sediments in the ... : Supplement to: Wessels, Martin (1989): Sedimentationsprozesse an der Filchner Schelfeiskante, Antarktis. Diploma Thesis, Institut und Museum für Geologie und Paläontologie der Georg-August-Universität zu Göttingen (in Zusammenarbeit mit dem Alfred-Wegener-Institut), 126 pp ...
format Article in Journal/Newspaper
author Wessels, Martin
Fütterer, Dieter K
Grobe, Hannes
author_facet Wessels, Martin
Fütterer, Dieter K
Grobe, Hannes
author_sort Wessels, Martin
title Sedimentology on cores off Filchner Shelf Ice, Weddell Sea, Antarctica ...
title_short Sedimentology on cores off Filchner Shelf Ice, Weddell Sea, Antarctica ...
title_full Sedimentology on cores off Filchner Shelf Ice, Weddell Sea, Antarctica ...
title_fullStr Sedimentology on cores off Filchner Shelf Ice, Weddell Sea, Antarctica ...
title_full_unstemmed Sedimentology on cores off Filchner Shelf Ice, Weddell Sea, Antarctica ...
title_sort sedimentology on cores off filchner shelf ice, weddell sea, antarctica ...
publisher PANGAEA
publishDate 1989
url https://dx.doi.org/10.1594/pangaea.701301
https://doi.pangaea.de/10.1594/PANGAEA.701301
genre Antarc*
Antarctica
Antarktis*
Berkner Island
Filchner Ronne Ice Shelf
Filchner-Ronne Ice Shelf
Ice Sheet
Ice Shelf
Ronne Ice Shelf
Schelfeis*
Weddell Sea
genre_facet Antarc*
Antarctica
Antarktis*
Berkner Island
Filchner Ronne Ice Shelf
Filchner-Ronne Ice Shelf
Ice Sheet
Ice Shelf
Ronne Ice Shelf
Schelfeis*
Weddell Sea
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.701301
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