{"NOAAStudyId":"12356","contactInfo":{"address":"325 Broadway, E/NE31","city":"Boulder","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.","country":"USA","dataCenterUrl":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data","email":"paleo@noaa.gov","fax":"303-497-6513","longName":"National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce ","phone":"303-497-6280","postalCode":"80305-3328","shortName":"DOC/NOAA/NESDIS/NCEI","state":"CO","type":"CONTACT INFORMATION"},"contributionDate":"2011-12-21","dataPublisher":"NOAA","dataType":"PALEOCEANOGRAPHY","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/paleoceanography","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-ocean-12356.xml","doi":null,"earliestYearBP":12368,"earliestYearCE":-10418,"entryId":"noaa-ocean-12356","funding":[{"fundingAgency":"US National Science Foundation","fundingGrant":"OCE-9709686, 9402198"}],"investigators":"Keigwin, L.D.; Boyle, E.A.","mostRecentYearBP":780,"mostRecentYearCE":1170,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/12356","originalSource":null,"publication":[{"abstract":"Throughout the last glacial cycle, reorganizations of deep ocean \r\nwater masses were coincident with rapid millennial-scale changes \r\nin climate. 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Boyle. 2000. \r\nDetecting Holocene Changes in Thermohaline Circulation. \r\nProceedings of the National Academy of Sciences \r\nof the United States of America, Vol. 97, No. 4, \r\npp. 1343-1346, Feb. 15, 2000. \r\nhttp://www.jstor.org/stable/121472","edition":null,"identifier":null,"issue":null,"journal":"Proceedings of the National Academy of Sciences","pages":null,"pubRank":"1","pubYear":2000,"reportNumber":null,"title":"Detecting Holocene Changes in Thermohaline Circulation","type":"publication","volume":null}],"reconstruction":"N","scienceKeywords":["Meridional Overturning Circulation (MOC)"],"site":[{"NOAASiteId":"52562","geo":{"geoType":"Feature","geometry":{"coordinates":["33.6867","-57.615"],"type":"POINT"},"properties":{"easternmostLongitude":"-57.615","maxElevationMeters":"-4583","minElevationMeters":"-4583","northernmostLatitude":"33.6867","southernmostLatitude":"33.6867","westernmostLongitude":"-57.615"}},"locationName":"Ocean>Atlantic Ocean>North Atlantic 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reconstruct Holocene changes in thermohaline circulation. \n\nCd/Ca and stable isotopes measured on Nutallides umbonifera and Cibicidoides \nspp., primarily C. wuellerstorfi, and Uvigerina. \n\n","version":"1.0","xmlId":"10418"}