{"data":{"id":"10.1594/pangaea.472219","type":"dois","attributes":{"doi":"10.1594/pangaea.472219","prefix":"10.1594","suffix":"pangaea.472219","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Welte, Dietrich Hugo","givenName":"Dietrich Hugo","familyName":"Welte","affiliation":[],"nameIdentifiers":[]},{"name":"Ebhardt, Götz","givenName":"Götz","familyName":"Ebhardt","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"Age determination of sediment core M1_251, Persian Gulf (Table 1)"}],"publisher":"PANGAEA","container":{},"publicationYear":1968,"subjects":[{"subject":"DEPTH, sediment/rock","subjectScheme":"Parameter"},{"subject":"Depth, top/min","subjectScheme":"Parameter"},{"subject":"Depth, bottom/max","subjectScheme":"Parameter"},{"subject":"Age, dated","subjectScheme":"Parameter"},{"subject":"Age, dated, standard deviation","subjectScheme":"Parameter"},{"subject":"Age, dated material","subjectScheme":"Parameter"},{"subject":"Kasten corer","subjectScheme":"Method"},{"subject":"Age, 14C conventional","subjectScheme":"Method"},{"subject":"M1","subjectScheme":"Campaign"},{"subject":"Meteor (1964)","subjectScheme":"Basis"}],"contributors":[],"dates":[{"date":"1965-03-25T00:00:00","dateType":"Collected"},{"date":"1968","dateType":"Issued"}],"language":"en","types":{"ris":"DATA","bibtex":"misc","citeproc":"dataset","schemaOrg":"Dataset","resourceType":"Supplementary Dataset","resourceTypeGeneral":"Dataset"},"relatedIdentifiers":[],"relatedItems":[],"sizes":["25 data points"],"formats":["text/tab-separated-values"],"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":"Sediments from a 3.40 m core out of the Persian Gulf were investigated for their content of straight chain paraffins and fatty acids. The samples range in age between 2000 and 9000 years (C-14-age of organic C). They contain 100-300 ppm of extractable fatcompounds and 20-70 ppm of hydrocarbons. There is no connection between the original distribution of the homologous series of n-fatty acids and n-paraffins. However, there is evidence that part of the n-fatty acids was reduced to n-paraffins, although the sediment itself does not look as if it were deposited under reducing conditions.","descriptionType":"Abstract"},{"description":"Supplement to: Welte, Dietrich Hugo; Ebhardt, Götz (1968): Die Verteilung höherer, geradkettiger Paraffine und Fettsäuren in einem Sedimentprofil aus dem Persischen Golf. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C1, 43-52","descriptionType":"Other"}],"geoLocations":[{"geoLocationPoint":{"pointLatitude":"26.316","pointLongitude":"56.916"}},{"geoLocationPlace":"Persian 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