{"data":{"id":"10.1594/pangaea.715010","type":"dois","attributes":{"doi":"10.1594/pangaea.715010","prefix":"10.1594","suffix":"pangaea.715010","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Channell, James E T","givenName":"James E T","familyName":"Channell","nameIdentifiers":[{"schemeUri":"https://orcid.org","nameIdentifier":"https://orcid.org/0000-0003-2382-3985","nameIdentifierScheme":"ORCID"}],"affiliation":[]},{"name":"Hodell, David A","givenName":"David A","familyName":"Hodell","nameIdentifiers":[{"schemeUri":"https://orcid.org","nameIdentifier":"https://orcid.org/0000-0001-8537-1588","nameIdentifierScheme":"ORCID"}],"affiliation":[]},{"name":"Lehman, Benoît","givenName":"Benoît","familyName":"Lehman","affiliation":[],"nameIdentifiers":[]}],"titles":[{"title":"Age model of ODP Site 162-983"}],"publisher":"PANGAEA","container":{},"publicationYear":1997,"subjects":[{"subject":"Composite Core","subjectScheme":"Method"},{"subject":"Leg162","subjectScheme":"Campaign"},{"subject":"Joides Resolution","subjectScheme":"Basis"},{"subject":"Ocean Drilling Program (ODP)","subjectScheme":"Project"}],"contributors":[],"dates":[{"date":"1997","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/s0012-821x(97)00164-7","relatedIdentifierType":"DOI"}],"relatedItems":[],"sizes":["2 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":"At ODP Site 983, relative geomagnetic paleointensity and planktic and benthic delta18O records have been acquired for the last 350 kyr. The mean sedimentation rate in this interval is 11.3 cm/kyr. Magnetic properties and hysteresis ratios indicate that pseudo-single domain magnetite is the remanence carrier. Volume susceptibility (kappa), anhysteretic (ARM) and isothermal (IRM) remanence values vary by a factor of 3-4, well within the criteria usually cited for paleointensity studies. Natural remanent magnetization (NRM) is normalized by ARM and IRM to acquire the paleointensity proxy. Arithmetic means of NRM/ARM and NRM/IRM, calculated for five demagnetization steps in the 25-45 mT range, constitute the relative paleointensity estimates. Some paleointensity lows (particularly those at ~40, ~120 and ~188 ka) are associated with directional excursions of the field, especially the event at ~188 ka (referred to here as the Iceland Basin Event) that constitutes a short-lived polarity reversal. For the last 200 kyr, the records can be correlated with other high-resolution paleointensity records such as those from the Labrador Sea, Mediterranean/Somali Basin and Sulu Sea, implying that the millennial scale features are globally synchronous. A labeling system for paleointensity features is proposed that ties prominent highs and lows to oxygen isotope stages.","descriptionType":"Abstract"},{"description":"Supplement to: Channell, James E T; Hodell, David A; Lehman, Benoît (1997): Relative geomagnetic paleointensity and d18O at ODP Site 983 (Gardar Drift, North Atlantic) since 350 ka. Earth and Planetary Science Letters, 153(1-2), 103-118","descriptionType":"Other"}],"geoLocations":[{"geoLocationPoint":{"pointLatitude":"60.403499999999994","pointLongitude":"-23.640666666666597"}},{"geoLocationPlace":"North Atlantic 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