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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Online Access: | https://dx.doi.org/10.1594/pangaea.587842 https://doi.pangaea.de/10.1594/PANGAEA.587842 |
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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 |
_version_ |
1810487144599257088 |