{"xmlId":"2733","NOAAStudyId":"8667","studyName":"Barrows et al. 2000 Southwest Pacific Faunal-Based LGM SST Estimates","doi":"https://doi.org/10.25921/0wkw-4647","uuid":"4e08fbbc-b14b-47be-802e-a8cace641712","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":"Juggins, S.; Barrows, T.T.; De Deckker, P.; Martinez, J.I.; Thiede, J.","investigatorDetails":[{"firstName":"Steve","lastName":"Juggins","initials":"S.","orcId":"0000-0003-4466-424X"},{"firstName":"Timothy","lastName":"Barrows","initials":"T.T.","orcId":"0000-0003-2614-7177"},{"firstName":"Patrick","lastName":"De Deckker","initials":"P.","orcId":"0000-0003-3003-5143"},{"firstName":"José Ignacio","lastName":"Martinez","initials":"J.I.","orcId":null},{"firstName":"Jörn","lastName":"Thiede","initials":"J.","orcId":"0000-0002-3452-2208"}],"version":"1.0","funding":[],"studyNotes":null,"onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/8667","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-ocean-8667.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-ocean-8667.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/paleoceanography","studyCode":null,"scienceKeywords":["Sea Surface Temperature Reconstruction"],"reconstruction":"Y","contributionDate":"2001-07-01","entryId":"noaa-ocean-8667","earliestYearBP":null,"mostRecentYearBP":null,"earliestYearCE":null,"mostRecentYearCE":null,"publication":[{"author":{"name":"Barrows, T. T., S. Juggins, P. De Deckker, J. Thiede, J. I. Martinez"},"pubYear":2000,"title":"Sea-surface temperatures of the southwest Pacific Ocean during the Last Glacial Maximum","journal":"Paleoceanography","volume":"15","edition":null,"issue":"1","pages":"95-109","reportNumber":null,"citation":"Barrows, T. T., S. Juggins, P. De Deckker, J. Thiede, J. I. Martinez. 2000. Sea-surface temperatures of the southwest Pacific Ocean during the Last Glacial Maximum. Paleoceanography, 15(1), 95-109. doi: 10.1029/1999PA900047","type":"publication","identifier":{"type":"doi","id":"10.1029/1999PA900047","url":"http://dx.doi.org/10.1029/1999PA900047"},"abstract":"The southwest Pacific Ocean covers a broad range of surface-water conditions ranging from warm, salty water in the subtropical East Australian Current to fresher, cold water in the Circumpolar Current. Using a new database of planktonic foraminifera assemblages (AUSMAT-F2), we demonstrate that the modern analog technique can be used to accurately reconstruct the magnitude of sea-surfacetemperature (SST) in this region. We apply this technique to data from 29 deep-sea cores along a meridional transect of the southwest Pacific Ocean to estimate the magnitude of SST cooling during the Last Glacial Maximum. We find minimal cooling in the tropics (0°2°C), moderate cooling in the subtropical midlatitudes (2°6°C), and maximum cooling to the southeast of New Zealand (6°10°C). 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