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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Main Authors: Schmiedl, Gerhard, Mackensen, Andreas
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1997
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.728744
https://doi.pangaea.de/10.1594/PANGAEA.728744
id ftdatacite:10.1594/pangaea.728744
record_format openpolar
spelling 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
institution Open Polar
collection DataCite
op_collection_id 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
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