{"xmlId":"2219","NOAAStudyId":"2426","studyName":"Vostok - Deuterium Data and Temperature Reconstruction","doi":"https://doi.org/10.25921/pr2k-6520","uuid":"dd3e3c34-a65c-49d5-bff4-d2b7bfe2a553","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":"ICE CORES","investigators":"Lorius, C.; Jouzel, J.; Ritz, C.; Merlivat, L.; Barkov, N.I.; Korotkevich, Y.S.; Kotlyakov, V.M.","investigatorDetails":[{"firstName":"Claude","lastName":"Lorius","initials":"C.","orcId":null},{"firstName":"Jean","lastName":"Jouzel","initials":"J.","orcId":null},{"firstName":"Catherine","lastName":"Ritz","initials":"C.","orcId":"0000-0003-0785-8571"},{"firstName":"Liliane","lastName":"Merlivat","initials":"L.","orcId":"0000-0002-5489-4658"},{"firstName":"Nartsiss","lastName":"Barkov","initials":"N.I.","orcId":null},{"firstName":"Yevgeny","lastName":"Korotkevich","initials":"Y.S.","orcId":null},{"firstName":"Vladimir","lastName":"Kotlyakov","initials":"V.M.","orcId":"0000-0002-1458-0435"}],"version":"1.0","funding":[],"studyNotes":null,"onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/2426","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-icecore-2426.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-icecore-2426.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/ice-core","studyCode":null,"scienceKeywords":["Air Temperature Reconstruction"],"reconstruction":"Y","contributionDate":"1995-01-01","entryId":"noaa-icecore-2426","earliestYearBP":261000,"mostRecentYearBP":0,"earliestYearCE":-259050,"mostRecentYearCE":1950,"publication":[{"author":{"name":"Lorius C., J. Jouzel, C. Ritz, L. Merlivat, N.I. Barkov, Y.S. Korotkevitch, V.M. Kotlyakov"},"pubYear":1985,"title":"A 150,000-year climatic record from Antarctic ice","journal":"Nature","volume":"316","edition":null,"issue":null,"pages":"591-596","reportNumber":null,"citation":"Lorius C., J. Jouzel, C. Ritz, L. Merlivat, N.I. Barkov, Y.S. Korotkevitch, V.M. Kotlyakov. 1985. A 150,000-year climatic record from Antarctic ice. Nature, 316, 591-596. doi: 10.1038/316591a0","type":"publication","identifier":{"type":"doi","id":"10.1038/316591a0","url":"http://dx.doi.org/10.1038/316591a0"},"abstract":"During much of the Quaternary, the Earth's climate has undergone drastic changes most notably successive glacial and interglacial episodes. The past 150 kyr includes such a climatic cycle: the last interglacial, the last glacial and the present holocene interglacial. A new climatictime series for this period has been obtained using ´18 O data from an Antarctic ice core.","pubRank":"1"}],"site":[{"NOAASiteId":"19976","siteName":"Vostok","siteCode":null,"mappable":"Y","locationName":"Continent>Antarctica","geo":{"geoType":"Feature","geometry":{"type":"POINT","coordinates":["-78.47","106.8"]},"properties":{"southernmostLatitude":"-78.47","northernmostLatitude":"-78.47","westernmostLongitude":"106.8","easternmostLongitude":"106.8","minElevationMeters":"3488","maxElevationMeters":"3488"}},"paleoData":[{"dataTableName":"Vostok deuterium Lorius1985","NOAADataTableId":"38430","earliestYear":261000,"mostRecentYear":0,"timeUnit":"cal yr BP","earliestYearBP":261000,"mostRecentYearBP":0,"earliestYearCE":-259050,"mostRecentYearCE":1950,"coreLengthMeters":null,"dataTableNotes":null,"species":[],"dataFile":[{"fileUrl":"https://www.ncei.noaa.gov/pub/data/paleo/icecore/antarctica/vostok/vostok_deld.txt","urlDescription":"Data","linkText":"vostok_deld.txt","variables":[{"cvDataType":"CLIMATE RECONSTRUCTIONS|ICE CORES","cvWhat":"earth system variable>temperature variable>temperature>surface temperature","cvMaterial":"reconstruction material>isotope ratio>delta 2H","cvError":null,"cvUnit":"temperature unit>degree Celsius","cvSeasonality":null,"cvDetail":"anomalized|corrected","cvMethod":null,"cvAdditionalInfo":null,"cvFormat":"Numeric","cvShortName":null},{"cvDataType":"CLIMATE RECONSTRUCTIONS|ICE CORES","cvWhat":"depth variable>depth","cvMaterial":null,"cvError":null,"cvUnit":"length unit>meter","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":null,"cvFormat":"Numeric","cvShortName":null},{"cvDataType":"CLIMATE RECONSTRUCTIONS|ICE CORES","cvWhat":"age variable>age>ice age","cvMaterial":null,"cvError":null,"cvUnit":"time unit>age unit>calendar kiloyear before present","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":null,"cvFormat":"Numeric","cvShortName":null},{"cvDataType":"ICE CORES","cvWhat":"chemical composition>isotope>isotope ratio>delta 2H","cvMaterial":"hydrologic material>bulk ice","cvError":null,"cvUnit":"concentration unit>parts per notation unit>parts per thousand>per mil>per mil SMOW","cvSeasonality":null,"cvDetail":"interpolated","cvMethod":"laboratory method>spectroscopy>mass spectrometry>isotope ratio mass spectrometry","cvAdditionalInfo":null,"cvFormat":"Numeric","cvShortName":null}],"NOAAKeywords":["earth science>paleoclimate>ice core>hydrogen isotopes"]}]},{"dataTableName":"Vostok timescales Lorius1985","NOAADataTableId":"38431","earliestYear":261000,"mostRecentYear":0,"timeUnit":"cal yr BP","earliestYearBP":261000,"mostRecentYearBP":0,"earliestYearCE":-259050,"mostRecentYearCE":1950,"coreLengthMeters":null,"dataTableNotes":"Different timescales have been used for the interpretation of Vostok\r\nice core records. They are reported in ky BP.\r\n\r\n- The Lorius et al. timescale (column 2) has been derived by combining\r\na glaciological model, fully described in Ritz (1992) and an accumulation model\r\nin which past accumulation is derived from the temperature record reconstructed\r\nfrom the deuterium isotopic profile (see Lorius et al., 1985).\r\n\r\n- Sowers et al. correlated the d18O of paleoatmospheric O2 derived from\r\nthe Vostok 3G and 4G cores, into a record of changes in the d18O of sea water\r\nderived from records of the d18O of foraminifera (see Sowers et al., 1993).\r\nThis timescale is given in column 3.\r\n\r\n- The glaciological timescale of Lorius et al. (1985) has been extended\r\naccounting for a linear increase of modern accumulation upstream of Vostok.\r\nThis Extended Glaciological Timescale (EGT; column 4) is described in Jouzel et\r\nal. (1993).\r\n\r\n- Jouzel et al. (1996) have used a modified version of EGT (column 4)\r\nassuming that this timescale overestimates the increase of age with depth by\r\n12% for gas ages older than 112 ky BP.\r\n\r\n- Waelbroeck et al. (1995) have applied the orbital tuning approach to\r\nthe deuterium record to derive a timescale which is consistent with the SPECMAP\r\nmarine timescale. This orbitally derived timescale is given in column 6.\r\nIMPORTANT NOTE: because of filtering errors due to the finite length of the\r\nrecord, the upper and bottom 20 to 35 ky of the orbitally tuned chronology can\r\nnot be trusted. In the present file, the upper 35 ky of the orbitally tuned\r\nchronology have been replaced by the EGT timescale.","species":[],"dataFile":[{"fileUrl":"https://www.ncei.noaa.gov/pub/data/paleo/icecore/antarctica/vostok/vostok_time.txt","urlDescription":"Data","linkText":"vostok_time.txt","variables":[],"NOAAKeywords":["earth science>paleoclimate>ice core>atmospheric gas"]}]}]}],"reference":{"pastThesaurusSkos":"https://www.ncei.noaa.gov/access/paleo-search/skos/past-thesaurus.rdf","pastThesaurusExplorer":"https://www.ncei.noaa.gov/access/paleo-search/cvterms","gcmdKeywordThesaurus":"https://earthdata.nasa.gov/earth-observation-data/find-data/idn/gcmd-keywords"},"dataLicenseDescription":null,"dataLicenseUrl":null}