{"xmlId":"2922","NOAAStudyId":"5935","studyName":"Keigwin 1998 Northwest Pacific Stable Isotope Data","doi":"https://doi.org/10.25921/5x5j-kx93","uuid":"37588e13-2107-48a9-869d-3513abca08cd","dataPublisher":"NOAA","contactInfo":{"type":"CONTACT INFORMATION","shortName":"DOC/NOAA/NESDIS/NCEI","longName":"National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce ","address":"325 Broadway, E/NE31","city":"Boulder","state":"CO","postalCode":"80305-3328","country":"USA","dataCenterUrl":"https://www.ncei.noaa.gov/products/paleoclimatology","email":"paleo@noaa.gov","phone":"828-271-4800","fax":null,"constraints":"Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site."},"dataType":"PALEOCEANOGRAPHY","investigators":"Keigwin, L.D.","investigatorDetails":[{"firstName":"Lloyd","lastName":"Keigwin","initials":"L.D.","orcId":null}],"version":"1.0","funding":[],"studyNotes":null,"onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/5935","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-ocean-5935.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-ocean-5935.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/paleoceanography","studyCode":null,"scienceKeywords":null,"reconstruction":"N","contributionDate":"2003-11-14","entryId":"noaa-ocean-5935","earliestYearBP":23000,"mostRecentYearBP":0,"earliestYearCE":-21050,"mostRecentYearCE":1950,"publication":[{"author":{"name":"Keigwin, L.D."},"pubYear":1998,"title":"Glacial-age hydrography of the far northwest Pacific Ocean","journal":"Paleoceanography","volume":"13","edition":null,"issue":"4","pages":"323-339","reportNumber":null,"citation":"Keigwin, L.D. 1998. Glacial-age hydrography of the far northwest Pacific Ocean. Paleoceanography, 13(4), 323-339. doi: 10.1029/98PA00874","type":"publication","identifier":{"type":"doi","id":"10.1029/98PA00874","url":"http://dx.doi.org/10.1029/98PA00874"},"abstract":"Stable isotope data on benthic foraminifera from more than 30 cores on the northern Emperor Seamounts and in the Okhotsk Sea are synthesized in paleohydrographic profiles spanning the depth range 10004000 m. Holocene (core-top) benthic foraminiferal ´18O and ´13C data are calibrated to modern hydrographic properties through measurements of ´13C of £CO2 and ´18O of seawater. Cibicidoides stable isotope ratios are close to the ´13C and equilibrium ´18O of seawater, whereas Uvigerina ´18O and ´13C are variably offset from Cibicidoides. Glacial maximum ´13C of Cibicidoides displays a different vertical profile than that of the Holocene. When results are adjusted by +0.320 to account for the secular change in ´13C during the last glacial maximum, the data coincide with the modern seawater and foraminiferal curves deeper than <2 km. However, at shallower depths ´13C gradually increases by as much as 10 above the modern value. Furthermore, above 2 km the benthic ´18O decreases by <0.50. These results are consistent with a benthic front at <2 km in the North Pacific [see Herguera et al., 1992], but they differ from interpretations based on trace metal data which indicate a source of nutrient-depleted deep water during glaciation. The isotopic data suggest that during glaciation there was a better ventilated watermass at intermediate depths in the far northwestern Pacific, it was relatively fresher than deep waters there, and deep waters were as nutrient-rich as today.","pubRank":"1"}],"site":[{"NOAASiteId":"56325","siteName":"RNDB-11PC","siteCode":null,"mappable":"Y","locationName":"Ocean>Pacific Ocean>North Pacific Ocean","geo":{"geoType":"Feature","geometry":{"type":"POINT","coordinates":["51.0733","167.975"]},"properties":{"southernmostLatitude":"51.0733","northernmostLatitude":"51.0733","westernmostLongitude":"167.975","easternmostLongitude":"167.975","minElevationMeters":"-3225","maxElevationMeters":"-3225"}},"paleoData":[{"dataTableName":"Keigwin1998","NOAADataTableId":"33091","earliestYear":23000,"mostRecentYear":0,"timeUnit":"cal yr 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