{"xmlId":"2772","NOAAStudyId":"8681","studyName":"Cronin et al. 2007 Chesapeake Bay 8.2k Sea Level Rise Data","doi":"https://doi.org/10.25921/e2dm-sx68","uuid":"c2df9194-3a16-4d2f-9839-52f5173c145c","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":"Cronin, T.M.; Vogt, P.R.; Willard, D.A.; Thunell, R.C.; Halka, J.; Berke, M.A.; Pohlman, J.","investigatorDetails":[{"firstName":"Thomas","lastName":"Cronin","initials":"T.M.","orcId":"0000-0002-2643-0979"},{"firstName":"Peter","lastName":"Vogt","initials":"P.R.","orcId":null},{"firstName":"Debra","lastName":"Willard","initials":"D.A.","orcId":"0000-0003-4878-0942"},{"firstName":"Robert","lastName":"Thunell","initials":"R.C.","orcId":"0000-0001-7052-1707"},{"firstName":"Jeffrey","lastName":"Halka","initials":"J.","orcId":null},{"firstName":"Melissa","lastName":"Berke","initials":"M.A.","orcId":"0000-0003-4810-3773"},{"firstName":"John","lastName":"Pohlman","initials":"J.","orcId":"0000-0002-3563-4586"}],"version":"1.0","funding":[],"studyNotes":null,"onlineResourceLink":"https://www.ncei.noaa.gov/access/paleo-search/study/8681","difMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-ocean-8681.xml","isoMetadataLink":"https://www.ncei.noaa.gov/pub/data/metadata/published/paleo/iso/xml/noaa-ocean-8681.xml","originalSource":null,"dataTypeInformation":"https://www.ncei.noaa.gov/products/paleoclimatology/paleoceanography","studyCode":null,"scienceKeywords":null,"reconstruction":"N","contributionDate":"2008-04-18","entryId":"noaa-ocean-8681","earliestYearBP":9210,"mostRecentYearBP":6600,"earliestYearCE":-7260,"mostRecentYearCE":-4650,"publication":[{"author":{"name":"Cronin, T.M., P.R. Vogt, D.A. Willard, R. Thunell, J. Halka, M. Berke, and J. Pohlman"},"pubYear":2007,"title":"Rapid sea level rise and ice sheet response to 8,200-year climate event","journal":"Geophysical Research Letters","volume":"34","edition":null,"issue":"20","pages":null,"reportNumber":"L20603","citation":"Cronin, T.M., P.R. Vogt, D.A. Willard, R. Thunell, J. Halka, M. Berke, and J. Pohlman. 2007. Rapid sea level rise and ice sheet response to 8,200-year climate event. Geophysical Research Letters, 34(20), L20603. doi: 10.1029/2007GL031318","type":"publication","identifier":{"type":"doi","id":"10.1029/2007GL031318","url":"http://dx.doi.org/10.1029/2007GL031318"},"abstract":"The largest abrupt climatic reversal of the Holocene interglacial, the cooling event 8.68.2 thousand years ago (ka), was probably caused by catastrophic release of glacial Lake Agassiz-Ojibway, which slowed Atlantic meridional overturning circulation (AMOC) and cooled global climate. Geophysical surveys and sediment cores from Chesapeake Bay reveal the pattern of sea level rise during this event. Sea level rose <14 m between 9.5 to 7.5 ka, a pattern consistent with coral records and the ICE-5G glacio-isostatic adjustment model. There were two distinct periods at <8.98.8 and <8.27.6 ka when Chesapeake marshes were drown as sea level rose rapidly at least <12 mm yr1. The latter event occurred after the 8.68.2 ka cooling event, coincided with extreme warming and vigorous AMOC centered on 7.9 ka, and may have been due to Antarctic Ice Sheet decay.","pubRank":"1"}],"site":[{"NOAASiteId":"56388","siteName":"Chesapeake Bay","siteCode":null,"mappable":"N","locationName":"Continent>North America>United States Of America","geo":{"geoType":"Feature","geometry":{"type":"POLYGON","coordinates":["37","40","-77","-76"]},"properties":{"southernmostLatitude":"37","northernmostLatitude":"40","westernmostLongitude":"-77","easternmostLongitude":"-76","minElevationMeters":null,"maxElevationMeters":null}},"paleoData":[{"dataTableName":"Chesapeake SeaLevel Cronin2007","NOAADataTableId":"34937","earliestYear":9210,"mostRecentYear":6600,"timeUnit":"cal yr BP","earliestYearBP":9210,"mostRecentYearBP":6600,"earliestYearCE":-7260,"mostRecentYearCE":-4650,"coreLengthMeters":null,"dataTableNotes":null,"species":[],"dataFile":[{"fileUrl":"https://www.ncei.noaa.gov/pub/data/paleo/contributions_by_author/cronin2007/cronin2007.txt","urlDescription":"Original Data and Full Metadata","linkText":"cronin2007.txt","variables":[{"cvDataType":"PALEOCEANOGRAPHY","cvWhat":"sampling metadata>longitude","cvMaterial":null,"cvError":null,"cvUnit":"angle unit>degree>degree west","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":null,"cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCEANOGRAPHY","cvWhat":"biological material>organism>foraminifer>foraminiferal index","cvMaterial":null,"cvError":null,"cvUnit":"concentration unit>percent","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":"total foraminifera","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCEANOGRAPHY","cvWhat":"biological material>organism>foraminifer>foraminiferal index>total agglutinated foraminifers","cvMaterial":null,"cvError":null,"cvUnit":"concentration unit>percent","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":"marsh species","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCEANOGRAPHY","cvWhat":"chemical composition>isotope>isotope ratio>delta 18O","cvMaterial":null,"cvError":null,"cvUnit":"concentration unit>parts per notation unit>parts per thousand>per mil>per mil VPDB","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":null,"cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCEANOGRAPHY","cvWhat":"chemical composition>isotope>isotope ratio>delta 13C","cvMaterial":null,"cvError":null,"cvUnit":"concentration unit>parts per notation unit>parts per thousand>per mil>per mil VPDB","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":null,"cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCEANOGRAPHY","cvWhat":"biological material>organism>ostracod>ostracod index>total ostracods","cvMaterial":null,"cvError":null,"cvUnit":"concentration unit>percent","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":"total ostracods","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCEANOGRAPHY","cvWhat":"biological material>organism>ostracod>identified ostracod","cvMaterial":null,"cvError":null,"cvUnit":"concentration unit>percent","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":"Loxoconcha polyhaline taxon","cvFormat":"Numeric","cvShortName":null},{"cvDataType":"PALEOCEANOGRAPHY","cvWhat":"biological material>organism>ostracod>identified ostracod","cvMaterial":null,"cvError":null,"cvUnit":"concentration unit>percent","cvSeasonality":null,"cvDetail":null,"cvMethod":null,"cvAdditionalInfo":"Cytheromorpha curta; 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