{"xmlId":"2745","NOAAStudyId":"8671","studyName":"Bond et al. 2001 North Atlantic Holocene Drift Ice Proxy Data","doi":"https://doi.org/10.25921/bgvh-nb23","uuid":"27a84a59-8b08-424e-95db-f92dc7ded82e","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":"Evans, M.N.; Muscheler, R.; Bond, G.C.; Kromer, B.; Beer, J.; Showers, W.; Hoffmann, S.S.; Lotti-Bond, R.; Hajdas, I.; Bonani, G.","investigatorDetails":[{"firstName":"Michael","lastName":"Evans","initials":"M.N.","orcId":"0000-0003-3727-6898"},{"firstName":"Raimund","lastName":"Muscheler","initials":"R.","orcId":"0000-0003-2772-3631"},{"firstName":"Gerard","lastName":"Bond","initials":"G.C.","orcId":null},{"firstName":"Bernd","lastName":"Kromer","initials":"B.","orcId":"0000-0003-1058-4436"},{"firstName":"Jürg","lastName":"Beer","initials":"J.","orcId":null},{"firstName":"William","lastName":"Showers","initials":"W.","orcId":null},{"firstName":"Sharon","lastName":"Hoffmann","initials":"S.S.","orcId":null},{"firstName":"Rusty","lastName":"Lotti-Bond","initials":"R.","orcId":null},{"firstName":"Irka","lastName":"Hajdas","initials":"I.","orcId":"0000-0003-2373-2725"},{"firstName":"Georges","lastName":"Bonani","initials":"G.","orcId":null}],"version":"1.0","funding":[],"studyNotes":null,"onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/8671","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-ocean-8671.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-ocean-8671.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/paleoceanography","studyCode":null,"scienceKeywords":null,"reconstruction":"N","contributionDate":"2008-03-04","entryId":"noaa-ocean-8671","earliestYearBP":11500,"mostRecentYearBP":0,"earliestYearCE":-9550,"mostRecentYearCE":1950,"publication":[{"author":{"name":"Bond, G.C., B. Kromer, J. Beer, R. Muscheler, M.N. Evans, W. Showers, S. Hoffmann, R. Lotti-Bond, I. Hajdas, and G. Bonani"},"pubYear":2001,"title":"Persistent Solar Influence on North Atlantic Climate During the Holocene","journal":"Science","volume":"294","edition":null,"issue":"5549","pages":"2130-2136","reportNumber":null,"citation":"Bond, G.C., B. Kromer, J. Beer, R. Muscheler, M.N. Evans, W. Showers, S. Hoffmann, R. Lotti-Bond, I. Hajdas, and G. Bonani. 2001. Persistent Solar Influence on North Atlantic Climate During the Holocene. Science, 294(5549), 2130-2136. doi: 10.1126/science.1065680","type":"publication","identifier":{"type":"doi","id":"10.1126/science.1065680","url":"http://dx.doi.org/10.1126/science.1065680"},"abstract":"Surface winds and surface ocean hydrography in the subpolar North Atlantic appear to have been influenced by variations in solar output through the entire Holocene. The evidence comes from a close correlation between inferred changes in production rates of the cosmogenic nuclides carbon-14 and beryllium-10 and centennial to millennial time scale changes in proxies of drift ice measured in deep-sea sediment cores. A solar forcing mechanism therefore may underlie at least the Holocene segment of the North Atlantic's 1500-year cycle. The surface hydrographic changes may have affected production of North Atlantic Deep Water, potentially providing an additional mechanism for amplifying the solar signals and transmitting them globally.","pubRank":"1"}],"site":[{"NOAASiteId":"57115","siteName":"VM28-14","siteCode":null,"mappable":"Y","locationName":"Ocean>Atlantic Ocean>North Atlantic Ocean","geo":{"geoType":"Feature","geometry":{"type":"POINT","coordinates":["64.7833","-29.5667"]},"properties":{"southernmostLatitude":"64.7833","northernmostLatitude":"64.7833","westernmostLongitude":"-29.5667","easternmostLongitude":"-29.5667","minElevationMeters":"-1855","maxElevationMeters":"-1855"}},"paleoData":[{"dataTableName":"Bond2001","NOAADataTableId":"32805","earliestYear":11500,"mostRecentYear":0,"timeUnit":"cal yr 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