{"data":{"id":"10.1594/pangaea.669644","type":"dois","attributes":{"doi":"10.1594/pangaea.669644","prefix":"10.1594","suffix":"pangaea.669644","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Berger, Glenn W","givenName":"Glenn W","familyName":"Berger","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"Fine-silt luminescence dating and mineral composition of sediments from the Arctic Ocean"}],"publisher":"PANGAEA","container":{},"publicationYear":2007,"subjects":[{"subject":"Box corer","subjectScheme":"Method"},{"subject":"Giant gravity corer","subjectScheme":"Method"},{"subject":"Kasten corer","subjectScheme":"Method"},{"subject":"Gravity corer (Kiel type)","subjectScheme":"Method"},{"subject":"Giant box corer","subjectScheme":"Method"},{"subject":"Giant piston corer","subjectScheme":"Method"},{"subject":"ARK-IV/3","subjectScheme":"Campaign"},{"subject":"ARK-VIII/3","subjectScheme":"Campaign"},{"subject":"Polarstern","subjectScheme":"Basis"}],"contributors":[],"dates":[{"date":"2007","dateType":"Issued"}],"language":"en","types":{"ris":"GEN","bibtex":"misc","citeproc":"article","schemaOrg":"Collection","resourceType":"Supplementary Publication Series of Datasets","resourceTypeGeneral":"Collection"},"relatedIdentifiers":[{"relationType":"IsSupplementTo","relatedIdentifier":"10.1016/j.quascirev.2005.07.024","relatedIdentifierType":"DOI"}],"relatedItems":[],"sizes":["18 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":"New geochronometers are needed for sediments of the Arctic Ocean spanning at least the last half million years, largely because oxygen-isotope stratigraphy is relatively ineffective in this ocean, and because other dating techniques require significant assumptions about sedimentation rates. Multi-aliquot luminescence sediment-dating procedures were applied to polymineral, fine-silt samples from 9 core-top and 37 deeper samples from 20 cores representing 19 sites across the Arctic Ocean. Most samples have independent age assignments and other known properties (e.g., % coarse fraction, % carbonate, U-Th isotopes). Thick-source alpha-particle counting indicates that for most regions the contribution of measured unsupported 230Th and 231Pa to calculated dose rates is","descriptionType":"Abstract"},{"description":"Supplement to: Berger, Glenn W (2006): Trans-arctic-ocean tests of fine-silt luminescence sediment dating provide a basis for an additional geochronometer for this region. Quaternary Science Reviews, 25(19-20), 2529-2551","descriptionType":"Other"}],"geoLocations":[{"geoLocationBox":{"eastBoundLongitude":"-2.5568000000000097","northBoundLatitude":"88.87","southBoundLatitude":"71.07","westBoundLongitude":"9.6168"}},{"geoLocationPlace":"Arctic Ocean"},{"geoLocationPlace":"Svalbard"},{"geoLocationPlace":"Antarctic Ocean"},{"geoLocationPlace":"Gakkel Ridge, Arctic Ocean"},{"geoLocationPlace":"Amundsen Basin"},{"geoLocationPlace":"Lomonosov Ridge, Arctic Ocean"},{"geoLocationPlace":"Morris Jesup 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