Radiolarian fauna of sediment core MD96-2089 off Lüderitz, Namibia ...
The study of radiolarian assemblages from Core MD 962086 provides new information on the variability in the upwelling intensity and origin of upwelled water masses over the past 350 ky in one of the major filamentous regions of the Benguela Upwelling System (BUS), located off Lüderitz, Namibia. The...
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ftdatacite:10.1594/pangaea.714867 2024-09-15T17:43:21+00:00 Radiolarian fauna of sediment core MD96-2089 off Lüderitz, Namibia ... Jacot des Combes, Hélène Abelmann, Andrea 2007 application/zip https://dx.doi.org/10.1594/pangaea.714867 https://doi.pangaea.de/10.1594/PANGAEA.714867 en eng PANGAEA https://dx.doi.org/10.1016/j.marmicro.2006.08.004 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Calypso Corer MD105 Marion Dufresne 1995 International Marine Global Change Study IMAGES Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 article Collection Supplementary Publication Series of Datasets 2007 ftdatacite https://doi.org/10.1594/pangaea.71486710.1016/j.marmicro.2006.08.004 2024-08-01T10:58:30Z The study of radiolarian assemblages from Core MD 962086 provides new information on the variability in the upwelling intensity and origin of upwelled water masses over the past 350 ky in one of the major filamentous regions of the Benguela Upwelling System (BUS), located off Lüderitz, Namibia. The use of key radiolarian species to trace the source of upwelled waters, and the use of a radiolarian-based upwelling index (URI) to reconstruct the upwelling intensity represent the first use of radiolarians for paleoceanographic reconstructions in the BUS. These radiolarian-based proxies indicate strongest upwelling during Marine Isotope Stages (MIS) 3, 5, and 8, which compares well with other studies. While during MIS 3 and 8, the radiolarian-based proxies indicate the influx of waters of Southern Ocean origin, they also point to the increased influence of tropical waters during the lower portion of MIS 5. During MIS 2, 4 and 6 the radiolarian assemblages indicate generally lower upwelling intensities, although ... : Supplement to: Jacot des Combes, Hélène; Abelmann, Andrea (2007): A 350-ky radiolarian record off Lüderitz, Namibia - evidence for changes in the upwelling regime. Marine Micropaleontology, 62(3), 194-210 ... Article in Journal/Newspaper Antarc* Antarctic Sea ice Southern Ocean DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Calypso Corer MD105 Marion Dufresne 1995 International Marine Global Change Study IMAGES Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
spellingShingle |
Calypso Corer MD105 Marion Dufresne 1995 International Marine Global Change Study IMAGES Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 Jacot des Combes, Hélène Abelmann, Andrea Radiolarian fauna of sediment core MD96-2089 off Lüderitz, Namibia ... |
topic_facet |
Calypso Corer MD105 Marion Dufresne 1995 International Marine Global Change Study IMAGES Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas SPP1158 |
description |
The study of radiolarian assemblages from Core MD 962086 provides new information on the variability in the upwelling intensity and origin of upwelled water masses over the past 350 ky in one of the major filamentous regions of the Benguela Upwelling System (BUS), located off Lüderitz, Namibia. The use of key radiolarian species to trace the source of upwelled waters, and the use of a radiolarian-based upwelling index (URI) to reconstruct the upwelling intensity represent the first use of radiolarians for paleoceanographic reconstructions in the BUS. These radiolarian-based proxies indicate strongest upwelling during Marine Isotope Stages (MIS) 3, 5, and 8, which compares well with other studies. While during MIS 3 and 8, the radiolarian-based proxies indicate the influx of waters of Southern Ocean origin, they also point to the increased influence of tropical waters during the lower portion of MIS 5. During MIS 2, 4 and 6 the radiolarian assemblages indicate generally lower upwelling intensities, although ... : Supplement to: Jacot des Combes, Hélène; Abelmann, Andrea (2007): A 350-ky radiolarian record off Lüderitz, Namibia - evidence for changes in the upwelling regime. Marine Micropaleontology, 62(3), 194-210 ... |
format |
Article in Journal/Newspaper |
author |
Jacot des Combes, Hélène Abelmann, Andrea |
author_facet |
Jacot des Combes, Hélène Abelmann, Andrea |
author_sort |
Jacot des Combes, Hélène |
title |
Radiolarian fauna of sediment core MD96-2089 off Lüderitz, Namibia ... |
title_short |
Radiolarian fauna of sediment core MD96-2089 off Lüderitz, Namibia ... |
title_full |
Radiolarian fauna of sediment core MD96-2089 off Lüderitz, Namibia ... |
title_fullStr |
Radiolarian fauna of sediment core MD96-2089 off Lüderitz, Namibia ... |
title_full_unstemmed |
Radiolarian fauna of sediment core MD96-2089 off Lüderitz, Namibia ... |
title_sort |
radiolarian fauna of sediment core md96-2089 off lüderitz, namibia ... |
publisher |
PANGAEA |
publishDate |
2007 |
url |
https://dx.doi.org/10.1594/pangaea.714867 https://doi.pangaea.de/10.1594/PANGAEA.714867 |
genre |
Antarc* Antarctic Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Sea ice Southern Ocean |
op_relation |
https://dx.doi.org/10.1016/j.marmicro.2006.08.004 |
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.71486710.1016/j.marmicro.2006.08.004 |
_version_ |
1810490301742055424 |