Paleomagnetic on three sediment cores from the Antarctic continental slope in the Weddell Sea ...

Four cores from the Antarctic continental margin located between 50 and 200 km from the present-day ice shelf edge, were selected for sedimentological and mass spectrometer analysis. The first stable isotope records of the Southern Polar Ocean can be correlated in detail with global isotope stratigr...

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Published in:Applied Geography
Main Authors: Grobe, Hannes, Mackensen, Andreas, Hubberten, Hans-Wolfgang, Spieß, Volkhard, Fütterer, Dieter K
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1990
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.587842
https://doi.pangaea.de/10.1594/PANGAEA.587842
id ftdatacite:10.1594/pangaea.587842
record_format openpolar
spelling ftdatacite:10.1594/pangaea.587842 2024-09-15T17:41:04+00:00 Paleomagnetic on three sediment cores from the Antarctic continental slope in the Weddell Sea ... Grobe, Hannes Mackensen, Andreas Hubberten, Hans-Wolfgang Spieß, Volkhard Fütterer, Dieter K 1990 application/zip https://dx.doi.org/10.1594/pangaea.587842 https://doi.pangaea.de/10.1594/PANGAEA.587842 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.588236 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type ANT-IV/3 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 1990 ftdatacite https://doi.org/10.1594/pangaea.58784210.1594/pangaea.588236 2024-07-03T13:10:16Z Four cores from the Antarctic continental margin located between 50 and 200 km from the present-day ice shelf edge, were selected for sedimentological and mass spectrometer analysis. The first stable isotope records of the Southern Polar Ocean can be correlated in detail with global isotope stratigraphy. Together with magnetostratigraphic, sedimentological and micropaleontological data, the record provides stratigraphic and paleoceanographic information back to the Jaramillo subchron (910 kyr). Although the isotope values have been altered by diagenetic processes in the sediments, which are poor in carbonate, an interpretation is possible via correlation with the sedimentological parameters. Oxygen isotope data give indications for a meltwater spike at the beginning of interglacials, when large scale melting of parts of the ice shelves took place. The synchronous record of the benthic and planktonic d13C-signals reflect continuous bottom water formation also during glacials. Primary productivity was strictly ... : Paleomagnetic of PS1388-3 see doi:10.1594/PANGAEA.51317 ... Article in Journal/Newspaper Antarc* Antarctic Ice Shelf Ice Shelves Weddell Sea DataCite Applied Geography 119 102216
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
ANT-IV/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Gravity corer Kiel type
ANT-IV/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Grobe, Hannes
Mackensen, Andreas
Hubberten, Hans-Wolfgang
Spieß, Volkhard
Fütterer, Dieter K
Paleomagnetic on three sediment cores from the Antarctic continental slope in the Weddell Sea ...
topic_facet Gravity corer Kiel type
ANT-IV/3
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description Four cores from the Antarctic continental margin located between 50 and 200 km from the present-day ice shelf edge, were selected for sedimentological and mass spectrometer analysis. The first stable isotope records of the Southern Polar Ocean can be correlated in detail with global isotope stratigraphy. Together with magnetostratigraphic, sedimentological and micropaleontological data, the record provides stratigraphic and paleoceanographic information back to the Jaramillo subchron (910 kyr). Although the isotope values have been altered by diagenetic processes in the sediments, which are poor in carbonate, an interpretation is possible via correlation with the sedimentological parameters. Oxygen isotope data give indications for a meltwater spike at the beginning of interglacials, when large scale melting of parts of the ice shelves took place. The synchronous record of the benthic and planktonic d13C-signals reflect continuous bottom water formation also during glacials. Primary productivity was strictly ... : Paleomagnetic of PS1388-3 see doi:10.1594/PANGAEA.51317 ...
format Article in Journal/Newspaper
author Grobe, Hannes
Mackensen, Andreas
Hubberten, Hans-Wolfgang
Spieß, Volkhard
Fütterer, Dieter K
author_facet Grobe, Hannes
Mackensen, Andreas
Hubberten, Hans-Wolfgang
Spieß, Volkhard
Fütterer, Dieter K
author_sort Grobe, Hannes
title Paleomagnetic on three sediment cores from the Antarctic continental slope in the Weddell Sea ...
title_short Paleomagnetic on three sediment cores from the Antarctic continental slope in the Weddell Sea ...
title_full Paleomagnetic on three sediment cores from the Antarctic continental slope in the Weddell Sea ...
title_fullStr Paleomagnetic on three sediment cores from the Antarctic continental slope in the Weddell Sea ...
title_full_unstemmed Paleomagnetic on three sediment cores from the Antarctic continental slope in the Weddell Sea ...
title_sort paleomagnetic on three sediment cores from the antarctic continental slope in the weddell sea ...
publisher PANGAEA
publishDate 1990
url https://dx.doi.org/10.1594/pangaea.587842
https://doi.pangaea.de/10.1594/PANGAEA.587842
genre Antarc*
Antarctic
Ice Shelf
Ice Shelves
Weddell Sea
genre_facet Antarc*
Antarctic
Ice Shelf
Ice Shelves
Weddell Sea
op_relation https://dx.doi.org/10.1594/pangaea.588236
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.58784210.1594/pangaea.588236
container_title Applied Geography
container_volume 119
container_start_page 102216
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