Sedimentological and paleoclimatological investigation of two sediment cores off Cape Barbas, North-West Africa ...

Two box cores taken off Cape Barbas (North-West Africa) have been studied using three methods. The analyses of the coarse fraction, of biogenic opal and of planktonic foraminifera revealed :1. Core GIK12310-4 penetrates Z, Y, X and upper part of W zone, whereas core GIK12379-1 penetrates Z and upper...

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Main Authors: Diester-Haass, Lieselotte, Schrader, Hans-Jürgen, Thiede, Jörn
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1973
Subjects:
M25
Online Access:https://dx.doi.org/10.1594/pangaea.548418
https://doi.pangaea.de/10.1594/PANGAEA.548418
id ftdatacite:10.1594/pangaea.548418
record_format openpolar
spelling ftdatacite:10.1594/pangaea.548418 2024-09-15T18:31:04+00:00 Sedimentological and paleoclimatological investigation of two sediment cores off Cape Barbas, North-West Africa ... Diester-Haass, Lieselotte Schrader, Hans-Jürgen Thiede, Jörn 1973 application/zip https://dx.doi.org/10.1594/pangaea.548418 https://doi.pangaea.de/10.1594/PANGAEA.548418 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Kasten corer M25 Meteor 1964 Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG article Collection Supplementary Publication Series of Datasets 1973 ftdatacite https://doi.org/10.1594/pangaea.548418 2024-08-01T11:00:37Z Two box cores taken off Cape Barbas (North-West Africa) have been studied using three methods. The analyses of the coarse fraction, of biogenic opal and of planktonic foraminifera revealed :1. Core GIK12310-4 penetrates Z, Y, X and upper part of W zone, whereas core GIK12379-1 penetrates Z and upper part of Y zone.2. Holocene sedimentation rates are 2.5 cm/1000 y for core GIK12310-4 and 6.0 cm/1000 y for core GIK12379-1. During the Y zone 5 cm/l000 y were sedimented incore GIK12310-4 and > 10-20 cm/1000 y in core GIK12379-1.3. Paleoclimatohgical results are: arid climate and relatively warm water temperatures during the Holocene (Z zone) and during X zone; humid climate and relatively cool water temperatures within the Wuerm (Y zone) (with a non-dated more arid interval found in the middle part of the Y zone) and in the upper part of the W zone.4. Increased contents of benthos and radiolaria in the Y zone indicate upwelling. Upwelling, characterized by high content of biogenic opal and low water ... : Supplement to: Diester-Haass, Lieselotte; Schrader, Hans-Jürgen; Thiede, Jörn (1973): Sedimentological and paleoclimatological investigations of two pelagic ooze cores off Cape barbas, North-West Africa. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C16, 19-66 ... Article in Journal/Newspaper Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Kasten corer
M25
Meteor 1964
Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
spellingShingle Kasten corer
M25
Meteor 1964
Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
Diester-Haass, Lieselotte
Schrader, Hans-Jürgen
Thiede, Jörn
Sedimentological and paleoclimatological investigation of two sediment cores off Cape Barbas, North-West Africa ...
topic_facet Kasten corer
M25
Meteor 1964
Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
description Two box cores taken off Cape Barbas (North-West Africa) have been studied using three methods. The analyses of the coarse fraction, of biogenic opal and of planktonic foraminifera revealed :1. Core GIK12310-4 penetrates Z, Y, X and upper part of W zone, whereas core GIK12379-1 penetrates Z and upper part of Y zone.2. Holocene sedimentation rates are 2.5 cm/1000 y for core GIK12310-4 and 6.0 cm/1000 y for core GIK12379-1. During the Y zone 5 cm/l000 y were sedimented incore GIK12310-4 and > 10-20 cm/1000 y in core GIK12379-1.3. Paleoclimatohgical results are: arid climate and relatively warm water temperatures during the Holocene (Z zone) and during X zone; humid climate and relatively cool water temperatures within the Wuerm (Y zone) (with a non-dated more arid interval found in the middle part of the Y zone) and in the upper part of the W zone.4. Increased contents of benthos and radiolaria in the Y zone indicate upwelling. Upwelling, characterized by high content of biogenic opal and low water ... : Supplement to: Diester-Haass, Lieselotte; Schrader, Hans-Jürgen; Thiede, Jörn (1973): Sedimentological and paleoclimatological investigations of two pelagic ooze cores off Cape barbas, North-West Africa. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C16, 19-66 ...
format Article in Journal/Newspaper
author Diester-Haass, Lieselotte
Schrader, Hans-Jürgen
Thiede, Jörn
author_facet Diester-Haass, Lieselotte
Schrader, Hans-Jürgen
Thiede, Jörn
author_sort Diester-Haass, Lieselotte
title Sedimentological and paleoclimatological investigation of two sediment cores off Cape Barbas, North-West Africa ...
title_short Sedimentological and paleoclimatological investigation of two sediment cores off Cape Barbas, North-West Africa ...
title_full Sedimentological and paleoclimatological investigation of two sediment cores off Cape Barbas, North-West Africa ...
title_fullStr Sedimentological and paleoclimatological investigation of two sediment cores off Cape Barbas, North-West Africa ...
title_full_unstemmed Sedimentological and paleoclimatological investigation of two sediment cores off Cape Barbas, North-West Africa ...
title_sort sedimentological and paleoclimatological investigation of two sediment cores off cape barbas, north-west africa ...
publisher PANGAEA
publishDate 1973
url https://dx.doi.org/10.1594/pangaea.548418
https://doi.pangaea.de/10.1594/PANGAEA.548418
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
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.548418
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