Benthic foraminifera analysis of two sediments cores from the northern Cape Basin in the eastern South Atlantic Ocean ...
Two late Quaternary sediment cores from the northern Cape Basin in the eastern South Atlantic Ocean were analyzed for their benthic foraminiferal content and benthic stable carbon isotope composition. The locations of the cores were selected such that both of them presently are bathed by North Atlan...
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ftdatacite:10.1594/pangaea.728744 2024-09-15T18:19:01+00:00 Benthic foraminifera analysis of two sediments cores from the northern Cape Basin in the eastern South Atlantic Ocean ... Schmiedl, Gerhard Mackensen, Andreas 1997 application/zip https://dx.doi.org/10.1594/pangaea.728744 https://doi.pangaea.de/10.1594/PANGAEA.728744 en eng PANGAEA https://dx.doi.org/10.1016/s0031-0182(96)00137-x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Gravity corer Kiel type M12/1 M20/2 Meteor 1986 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 1997 ftdatacite https://doi.org/10.1594/pangaea.72874410.1016/s0031-0182(96)00137-x 2024-07-03T13:10:33Z Two late Quaternary sediment cores from the northern Cape Basin in the eastern South Atlantic Ocean were analyzed for their benthic foraminiferal content and benthic stable carbon isotope composition. The locations of the cores were selected such that both of them presently are bathed by North Atlantic Deep Water (NADW) and past changes in deep water circulation should be recorded simultaneously at both locations. However, the areas are different in terms of primary production. One core was recovered from the nutrient-depleted Walvis Ridge area, whereas the other one is from the continental slope just below the coastal upwelling mixing area where present day organic matter fluxes are shown to be moderately high. Recent data served as the basis for the interpretation of the late Quaternary faunal fluctuations and the paleoceanographic reconstruction.During the last 450,000 years, NADW flux into the eastern South Atlantic Ocean has been restricted to interglacial periods, with the strongest dominance of a ... : Supplement to: Schmiedl, Gerhard; Mackensen, Andreas (1997): Late Quaternary paleoproductivity and deep water circulation in the eastern South Altantic Ocean: Evidence from benthic foraminifera. Palaeogeography, Palaeoclimatology, Palaeoecology, 130(1-4), 43-80 ... Article in Journal/Newspaper NADW North Atlantic Deep Water North Atlantic South Atlantic Ocean DataCite |
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Open Polar |
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ftdatacite |
language |
English |
topic |
Gravity corer Kiel type M12/1 M20/2 Meteor 1986 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
spellingShingle |
Gravity corer Kiel type M12/1 M20/2 Meteor 1986 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Schmiedl, Gerhard Mackensen, Andreas Benthic foraminifera analysis of two sediments cores from the northern Cape Basin in the eastern South Atlantic Ocean ... |
topic_facet |
Gravity corer Kiel type M12/1 M20/2 Meteor 1986 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
description |
Two late Quaternary sediment cores from the northern Cape Basin in the eastern South Atlantic Ocean were analyzed for their benthic foraminiferal content and benthic stable carbon isotope composition. The locations of the cores were selected such that both of them presently are bathed by North Atlantic Deep Water (NADW) and past changes in deep water circulation should be recorded simultaneously at both locations. However, the areas are different in terms of primary production. One core was recovered from the nutrient-depleted Walvis Ridge area, whereas the other one is from the continental slope just below the coastal upwelling mixing area where present day organic matter fluxes are shown to be moderately high. Recent data served as the basis for the interpretation of the late Quaternary faunal fluctuations and the paleoceanographic reconstruction.During the last 450,000 years, NADW flux into the eastern South Atlantic Ocean has been restricted to interglacial periods, with the strongest dominance of a ... : Supplement to: Schmiedl, Gerhard; Mackensen, Andreas (1997): Late Quaternary paleoproductivity and deep water circulation in the eastern South Altantic Ocean: Evidence from benthic foraminifera. Palaeogeography, Palaeoclimatology, Palaeoecology, 130(1-4), 43-80 ... |
format |
Article in Journal/Newspaper |
author |
Schmiedl, Gerhard Mackensen, Andreas |
author_facet |
Schmiedl, Gerhard Mackensen, Andreas |
author_sort |
Schmiedl, Gerhard |
title |
Benthic foraminifera analysis of two sediments cores from the northern Cape Basin in the eastern South Atlantic Ocean ... |
title_short |
Benthic foraminifera analysis of two sediments cores from the northern Cape Basin in the eastern South Atlantic Ocean ... |
title_full |
Benthic foraminifera analysis of two sediments cores from the northern Cape Basin in the eastern South Atlantic Ocean ... |
title_fullStr |
Benthic foraminifera analysis of two sediments cores from the northern Cape Basin in the eastern South Atlantic Ocean ... |
title_full_unstemmed |
Benthic foraminifera analysis of two sediments cores from the northern Cape Basin in the eastern South Atlantic Ocean ... |
title_sort |
benthic foraminifera analysis of two sediments cores from the northern cape basin in the eastern south atlantic ocean ... |
publisher |
PANGAEA |
publishDate |
1997 |
url |
https://dx.doi.org/10.1594/pangaea.728744 https://doi.pangaea.de/10.1594/PANGAEA.728744 |
genre |
NADW North Atlantic Deep Water North Atlantic South Atlantic Ocean |
genre_facet |
NADW North Atlantic Deep Water North Atlantic South Atlantic Ocean |
op_relation |
https://dx.doi.org/10.1016/s0031-0182(96)00137-x |
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.72874410.1016/s0031-0182(96)00137-x |
_version_ |
1810457109741961216 |