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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":"2010-09-10","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-9775.xml","doi":null,"earliestYearBP":473780,"earliestYearCE":-471830,"entryId":"noaa-ocean-9775","funding":[{"fundingAgency":"Natural Environment Research Council PhD Studentship","fundingGrant":"NER/S/A/2005/13226"},{"fundingAgency":"Natural Environment Research Council radiocarbon allocation","fundingGrant":"1194.1006 and 1235.1007"},{"fundingAgency":"Natural Environment Research Council LSMSF Grant","fundingGrant":"lsmsfbris008"},{"fundingAgency":"Natural Environment Research Council Isotope Geoscience Facility","fundingGrant":"IP/894/0506"}],"investigators":"Dickson, A.J.; Beer, C.J.; Dempsey, C.; Maslin, M.A.; Bendle, J.A.; McClymont, E.L.; Pancost, R.D.","mostRecentYearBP":0,"mostRecentYearCE":1950,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/9775","originalSource":null,"publication":[{"abstract":null,"author":null,"citation":"Dickson, A.J., M.J. Leng, M.A. Maslin, H.J. Sloane, J. Green, J.A. Bendle, E.L. McClymont and R.D. Pancost. 2010. Atlantic overturning circulation and Agulhas leakage influences on southeast Atlantic upper ocean hydrography during marine isotope stage 11. Paleoceanography, 25, PA3208.\n","edition":null,"identifier":{"id":"10.1029/2009PA001830","type":"doi","url":"http://dx.doi.org/10.1029/2009PA001830"},"issue":null,"journal":"Paleoceanography","pages":null,"pubRank":"2","pubYear":2010,"reportNumber":null,"title":"Atlantic overturning circulation and Agulhas leakage influences on southeast Atlantic upper ocean hydrography during marine isotope stage 11","type":"publication","volume":null},{"abstract":null,"author":null,"citation":"Dickson, A.J., M.J. Leng and M.A. Maslin. 2008. Mid-depth South Atlantic Ocean circulation and chemical stratification during MIS-10 to 12: implications for atmospheric CO2. Climate of the Past 4, 333-344.\r\n","edition":null,"identifier":{"id":"10.5194/cp-4-333-2008","type":"doi","url":"http://dx.doi.org/10.5194/cp-4-333-2008"},"issue":null,"journal":"Climate of the Past","pages":null,"pubRank":"3","pubYear":2008,"reportNumber":null,"title":"Mid-depth South Atlantic Ocean circulation and chemical stratification during MIS-10 to 12: implications for atmospheric CO2","type":"publication","volume":null},{"abstract":"The interglacial known as Marine Isotope Stage 11 has been proposed to be analogous to the Holocene, owing to similarities in the amplitudes of orbital forcing. It has been difficult to compare the periods, however, because of the long duration of Stage 11 and a lack of detailed knowledge of any extreme climate events that may have occurred. Here we use the distinctive phasing between seasurface temperatures and the oxygen-isotope records of benthic foraminifera in the southeast Atlantic Ocean to stratigraphically align the Holocene interglacial with the first half of the Marine Isotope Stage 11 interglacial optimum. This alignment suggests that the second half of Marine Isotope Stage 11 should not be used as a reference for 'pre-anthropogenic' greenhouse-gas emissions. By compiling benthic carbon-isotope records from sites in the Atlantic Ocean on a single timescale, we also find that meridional overturning circulation strengthened about 415,000 years ago, at a time of high orbital obliquity. We propose that this mechanism transported heat to the high northern latitudes, inhibiting significant ice-sheet build-up and prolonging interglacial conditions. We suggest that this mechanism may have also prolonged other interglacial periods throughout the past 800,000 years.\n","author":null,"citation":"Dickson, A.J., C.J. Beer, C. Dempsey, M.A. Maslin, J.A. Bendle, E.L. McClymont, and R.D. Pancost. 2009. Oceanic forcing of the Marine Isotope Stage 11 interglacial. Nature Geoscience 2, 428-433.\n","edition":null,"identifier":{"id":"10.1038/ngeo527","type":"doi","url":"http://dx.doi.org/10.1038/ngeo527"},"issue":null,"journal":"Nature Geoscience","pages":null,"pubRank":"1","pubYear":2009,"reportNumber":null,"title":"Oceanic forcing of the Marine Isotope Stage 11 interglacial","type":"publication","volume":null}],"reconstruction":"Y","scienceKeywords":["Sea Surface Temperature Reconstruction","Meridional Overturning Circulation (MOC)"],"site":[{"NOAASiteId":"31223","geo":{"geoType":"Feature","geometry":{"coordinates":["-28.9833","13.833333"],"type":"POINT"},"properties":{"easternmostLongitude":"13.833333","maxElevationMeters":"-1997","minElevationMeters":"-1997","northernmostLatitude":"-28.9833","southernmostLatitude":"-28.9833","westernmostLongitude":"13.833333"}},"locationName":"Ocean>Atlantic Ocean>South Atlantic Ocean","mappable":"Y","paleoData":[{"NOAADataTableId":"18600","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth 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