{"data":{"id":"10.1594/pangaea.548418","type":"dois","attributes":{"doi":"10.1594/pangaea.548418","prefix":"10.1594","suffix":"pangaea.548418","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Diester-Haass, Lieselotte","givenName":"Lieselotte","familyName":"Diester-Haass","affiliation":[],"nameIdentifiers":[]},{"name":"Schrader, Hans-Jürgen","givenName":"Hans-Jürgen","familyName":"Schrader","affiliation":[],"nameIdentifiers":[]},{"name":"Thiede, Jörn","givenName":"Jörn","familyName":"Thiede","nameIdentifiers":[{"schemeUri":"https://orcid.org","nameIdentifier":"https://orcid.org/0000-0002-3452-2208","nameIdentifierScheme":"ORCID"}],"affiliation":[]}],"titles":[{"title":"Sedimentological and paleoclimatological investigation of two sediment cores off Cape Barbas, North-West Africa"}],"publisher":"PANGAEA","container":{},"publicationYear":1973,"subjects":[{"subject":"Kasten corer","subjectScheme":"Method"},{"subject":"M25","subjectScheme":"Campaign"},{"subject":"Meteor (1964)","subjectScheme":"Basis"},{"subject":"Institute for Geosciences, Christian Albrechts University, Kiel (GIK/IfG)","subjectScheme":"Project"}],"contributors":[],"dates":[{"date":"1973","dateType":"Issued"}],"language":"en","types":{"ris":"GEN","bibtex":"misc","citeproc":"article","schemaOrg":"Collection","resourceType":"Supplementary Publication Series of Datasets","resourceTypeGeneral":"Collection"},"relatedIdentifiers":[],"relatedItems":[],"sizes":["8 datasets"],"formats":["application/zip"],"version":null,"rightsList":[{"rights":"Creative Commons Attribution 3.0 Unported","rightsUri":"https://creativecommons.org/licenses/by/3.0/legalcode","schemeUri":"https://spdx.org/licenses/","rightsIdentifier":"cc-by-3.0","rightsIdentifierScheme":"SPDX"}],"descriptions":[{"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 \u0026gt; 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 temperatures, was found in core GIK12310-4 at 250 to 350 cm in the lower part of the Y zone.The plankton/benthos ratio of foraminifera, the benthos/radiolaria ratio and water temperatures derived from planktonic foraminifera, differ in both cores in the Holocene, and are nearly identical during the Wuerm.","descriptionType":"Abstract"},{"description":"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","descriptionType":"Other"}],"geoLocations":[{"geoLocationBox":{"eastBoundLongitude":"-17.745","northBoundLatitude":"23.4983333333","southBoundLatitude":"23.135","westBoundLongitude":"-18.7166666666"}},{"geoLocationPlace":"East 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