{"NOAAStudyId":"2605","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":"2003-07-01","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-2605.xml","doi":null,"earliestYearBP":340830,"earliestYearCE":-338880,"entryId":"noaa-ocean-2605","funding":[],"investigators":"Pahnke, K.; Zahn, R.; Elderfield, H.; Schulz, M.","mostRecentYearBP":1951,"mostRecentYearCE":-1,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/2605","originalSource":null,"publication":[{"abstract":"In order to investigate rapid climatic changes at mid-southern latitudes, we have developed centennial-scale paleoceanographic records from the southwest Pacific that enable detailed comparison with Antarctic ice core records. These records suggest close coupling of mid-southern latitudes with Antarctic climate during deglacial and interglacial periods. Glacial sections display higher variability than is seen in Antarctic ice cores, which implies climatic decoupling between mid- and high southern latitudes due to enhanced circum-Antarctic circulation. Structural and temporal similarity with the Greenland ice core record is evident in glacial sections and suggests a degree of interhemispheric synchroneity not predicted from bipolar ice core correlations.","author":null,"citation":"Pahnke, K., R. Zahn, H. Elderfield, and M. Schulz. 2003. 340,000-Year centennial-scale marine record of southern hemisphere climatic oscillation. Science, 301(5635):948-952.","edition":null,"identifier":null,"issue":null,"journal":"Science","pages":null,"pubRank":"1","pubYear":2003,"reportNumber":null,"title":"340,000-Year centennial-scale marine record of southern hemisphere climatic oscillation","type":"publication","volume":null},{"abstract":null,"author":null,"citation":"Carter, L., H.L. Neil, and I.N. McCave. 2000. Glacial to interglacial changes in non-carbonate and carbonate accumulation in the SW Pacific Ocean, New Zealand. Palaeogeography, Palaeoclimatology, Palaeoecology 162:333-356.","edition":null,"identifier":null,"issue":null,"journal":"Palaeogeography, Palaeoclimatology, Palaeoecology","pages":null,"pubRank":"2","pubYear":2000,"reportNumber":null,"title":"Glacial to interglacial changes in non-carbonate and carbonate accumulation in the SW Pacific Ocean, New Zealand","type":"publication","volume":null},{"abstract":null,"author":null,"citation":"Voelker, A.H.L., P.M. Grootes, M.J. Nadeau, and M. Sarnthein. 2000. Radiocarbon levels in the Iceland Sea from 25-53 kyr and their link to the Earth's magnetic field intensity. Radiocarbon 42:437-452.","edition":null,"identifier":null,"issue":null,"journal":"Radiocarbon","pages":null,"pubRank":"3","pubYear":2000,"reportNumber":null,"title":"Radiocarbon levels in the Iceland Sea from 25-53 kyr and their link to the Earth's magnetic field intensity","type":"publication","volume":null},{"abstract":null,"author":null,"citation":"Shackleton, N.J. 2000. The 100,000-year ice-age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity. Science 289:1897-1902.","edition":null,"identifier":null,"issue":null,"journal":"Science","pages":null,"pubRank":"4","pubYear":2000,"reportNumber":null,"title":"The 100,000-year ice-age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity","type":"publication","volume":null},{"abstract":null,"author":null,"citation":"Wilson, C.J.N., V.R. Switsur, and A.P. Ward. 1998. A new 14C age for the Oruanui (Wairakei) eruption, New Zealand. Geological Magazine, 125:297-300.","edition":null,"identifier":null,"issue":null,"journal":"Geological Magazine","pages":null,"pubRank":"5","pubYear":1998,"reportNumber":null,"title":"A new 14C age for the Oruanui (Wairakei) eruption, New Zealand","type":"publication","volume":null},{"abstract":null,"author":null,"citation":"Stuiver, M., and P.J. Reimer. 1993. Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35:215-230.","edition":null,"identifier":null,"issue":null,"journal":"Radiocarbon","pages":null,"pubRank":"6","pubYear":1993,"reportNumber":null,"title":"Extended 14C database and revised CALIB radiocarbon calibration program","type":"publication","volume":null},{"abstract":null,"author":null,"citation":"Shackleton, N.J., M.A. Hall, and E. Vincent. 2000. Phase relationships between millennial scale events 64000 to 24000 years ago. Paleoceanography 15(6):565.","edition":null,"identifier":null,"issue":null,"journal":"Paleoceanography","pages":null,"pubRank":"7","pubYear":2000,"reportNumber":null,"title":"Phase relationships between millennial scale events 64000 to 24000 years ago","type":"publication","volume":null}],"reconstruction":"Y","scienceKeywords":["Sea Surface Temperature Reconstruction"],"site":[{"NOAASiteId":"19236","geo":{"geoType":"Feature","geometry":{"coordinates":["-45.53","174.93"],"type":"POINT"},"properties":{"easternmostLongitude":"174.93","maxElevationMeters":"-1210","minElevationMeters":"-1210","northernmostLatitude":"-45.53","southernmostLatitude":"-45.53","westernmostLongitude":"174.93"}},"locationName":"Ocean>Pacific Ocean>South Pacific Ocean","mappable":"Y","paleoData":[{"NOAADataTableId":"4289","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>paleocean>age control","earth science>paleoclimate>paleocean>reconstruction","earth science>paleoclimate>paleocean>trace metals in carbonates","earth science>paleoclimate>paleocean>oxygen isotopes"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/contributions_by_author/pahnke2003","linkText":"pahnke2003","urlDescription":"Original Data and Full Metadata","variables":[]},{"NOAAKeywords":["earth science>paleoclimate>paleocean>age control","earth science>paleoclimate>paleocean>oxygen isotopes","earth science>paleoclimate>paleocean>trace metals in carbonates","earth science>paleoclimate>paleocean>reconstruction"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/paleocean/sediment_files/complete/md972120-tab.txt","linkText":"md972120-tab.txt","urlDescription":"Alternate Format Data","variables":[{"cvAdditionalInfo":null,"cvDataType":"CLIMATE RECONSTRUCTIONS|PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":"reconstruction material>element or compound ratio>magnesium/calcium","cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"degree Celsius","cvWhat":"earth system variable>temperature variable>temperature>sea water temperature>sea surface temperature"},{"cvAdditionalInfo":null,"cvDataType":"PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"centimeter","cvWhat":"depth variable>depth"},{"cvAdditionalInfo":null,"cvDataType":"PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"calendar year before present","cvWhat":"age variable>age"},{"cvAdditionalInfo":"250 - 350 microns","cvDataType":"PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":"biological material>organism>foraminifer>planktic foraminifer>Globigerina sp.>Globigerina bulloides","cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"per mil PDB","cvWhat":"chemical composition>isotope>isotope ratio>delta 18O"},{"cvAdditionalInfo":null,"cvDataType":"PALEOCEANOGRAPHY","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":"biological material>organism>foraminifer>planktic foraminifer>Globigerina sp.>Globigerina bulloides","cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"dimensionless","cvWhat":"chemical composition>element or compound ratio>magnesium/calcium"}]}],"dataTableName":"MD97-2120 Mg/CaSST Pahnke2003","dataTableNotes":null,"earliestYear":340830,"earliestYearBP":340830,"earliestYearCE":-338880,"mostRecentYear":1951,"mostRecentYearBP":1951,"mostRecentYearCE":-1,"species":[],"timeUnit":"cal yr BP"}],"siteName":"MD97-2120"}],"studyCode":null,"studyName":"340 KYr SW Pacific d18O Data and Mg/Ca-based SST Reconstruction","studyNotes":"","version":"1.0","xmlId":"1676"}