{"data":{"id":"10.1594/pangaea.690363","type":"dois","attributes":{"doi":"10.1594/pangaea.690363","prefix":"10.1594","suffix":"pangaea.690363","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Martínez, José Ignacio","givenName":"José Ignacio","familyName":"Martínez","affiliation":[],"nameIdentifiers":[]},{"name":"De Deckker, Patrick","givenName":"Patrick","familyName":"De Deckker","nameIdentifiers":[{"schemeUri":"https://orcid.org","nameIdentifier":"https://orcid.org/0000-0003-3003-5143","nameIdentifierScheme":"ORCID"}],"affiliation":[]},{"name":"Chivas, Allan R","givenName":"Allan R","familyName":"Chivas","nameIdentifiers":[{"schemeUri":"https://orcid.org","nameIdentifier":"https://orcid.org/0000-0002-1459-6330","nameIdentifierScheme":"ORCID"}],"affiliation":[]}],"titles":[{"title":"Stable oxygen and carbon isotope ratios of Globigerinoides sacculifer of ODP Hole 134-828A from the Southwest Pacific (Table 2)"}],"publisher":"PANGAEA","container":{},"publicationYear":1997,"subjects":[{"subject":"DEPTH, sediment/rock","subjectScheme":"Parameter"},{"subject":"Sample code/label","subjectScheme":"Parameter"},{"subject":"Globigerinoides sacculifer, δ18O","subjectScheme":"Parameter"},{"subject":"Globigerinoides sacculifer, δ13C","subjectScheme":"Parameter"},{"subject":"Drilling/drill rig","subjectScheme":"Method"},{"subject":"DSDP/ODP/IODP sample designation","subjectScheme":"Method"},{"subject":"Mass spectrometer Finnigan MAT 251","subjectScheme":"Method"},{"subject":"Leg134","subjectScheme":"Campaign"},{"subject":"Joides Resolution","subjectScheme":"Basis"},{"subject":"Ocean Drilling Program (ODP)","subjectScheme":"Project"}],"contributors":[],"dates":[{"date":"1997","dateType":"Issued"}],"language":"en","types":{"ris":"DATA","bibtex":"misc","citeproc":"dataset","schemaOrg":"Dataset","resourceType":"Supplementary Dataset","resourceTypeGeneral":"Dataset"},"relatedIdentifiers":[{"relationType":"IsSupplementTo","relatedIdentifier":"10.1016/s0377-8398(97)00029-7","relatedIdentifierType":"DOI"}],"relatedItems":[],"sizes":["657 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":"Oxygen-isotope analyses of planktonic foraminifera from 57 western Pacific deep-sea cores are compared for the Holocene and the Last Glacial Maximum (LGM). Carbonate dissolution, sedimentation rates/bioturbation, sample density, and vital effects are assessed before the sea-surface salinity signal of these records is reconstructed. Average glacial-interglacial Delta delta18O values in the western Pacific are found to be close to those in the Atlantic Ocean (1.76 ‰ in the Pacific compared to 1.80 ‰ in the Atlantic), questioning previous suggestions of a larger salinity difference between the Atlantic and the Pacific oceans during the LGM. During the LGM, sea-surface salinity was higher in the western Pacific than today (by \u0026gt;~1 ‰), implying that evaporation minus precipitation was higher all over the region. The minimum change in sea-surface salinity occurred around the equator at the core of the Western Pacific Warm Pool. Holocene high-amplitude, high-frequency fluctuations in planktonic delta18O records north and south of the present limits of the Western Pacific Warm Pool are indicative of sea-surface temperature and/or sea-surface salinity variations related to its expansion and contraction at the scale of thousands of years. Such high-amplitude, high-frequency fluctuations at the edge of the WPWP are best documented in the delta18O signal of ODP Hole 828A offshore Vanuatu, so far the best high-resolution record for the western Pacific.","descriptionType":"Abstract"},{"description":"Supplement to: Martínez, José Ignacio; De Deckker, Patrick; Chivas, Allan R (1997): New estimates for salinity changes in the Western Pacific Warm Pool during the Last Glacial Maximum: oxygen-isotope evidence. Marine Micropaleontology, 32(3-4), 311-340","descriptionType":"Other"}],"geoLocations":[{"geoLocationPoint":{"pointLatitude":"-15.288","pointLongitude":"166.284"}},{"geoLocationPlace":"Coral 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