{"NOAAStudyId":"22274","contactInfo":{"address":"325 Broadway, E/NE31","city":"Boulder","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.","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":"2017-06-22","dataPublisher":"NOAA","dataType":"PALEOLIMNOLOGY","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/lake","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-lake-22274.xml","doi":null,"earliestYearBP":6000,"earliestYearCE":-4050,"entryId":"noaa-lake-22274","funding":[{"fundingAgency":"US National Science Foundation","fundingGrant":"AGS-1256970, AGS-1561121"}],"investigators":"Thompson, D.M.; Conroy, J.L.; Collins, A.; Hlohowskyj, S.; Overpeck, J.T.; Riedinger-Whitmore, M.; Cole, J.E.; Bush, M.B.; Corley, T.L.; Steinitz-Kannan, M.","mostRecentYearBP":-62,"mostRecentYearCE":2012,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/22274","originalSource":null,"publication":[{"abstract":"Finely laminated sediments within Bainbridge Crater Lake, Galápagos provide a record of El Niño-Southern Oscillation (ENSO) events over the Holocene. Despite the importance of this sediment record, hypotheses for how climate variability is preserved in the lake sediments have not been tested.  Here we present results of long-term monitoring of the local climate and limnology and a revised interpretation of the sediment record.  Brown-green, organic rich, siliciclastic laminae reflect warm, wet conditions typical of El Niño events, whereas carbonate and gypsum precipitate during cool, dry La Niña events and persistent dry periods, respectively.  Applying this new interpretation, we find ENSO events of both phases were generally less frequent during the mid-Holocene (~6100-4000 cal. years BP) relative to the last ~1500 cal. years.  Abundant carbonate laminations between 3500 and 3000 cal. years BP imply that conditions in the Galápagos region were cool and dry during this period when the tropical Pacific E-W SST gradient likely strengthened.  The frequency of El Niño and La Niña events then intensified dramatically around 1750-2000 cal. years BP, consistent with a weaker SST gradient and an increased frequency of ENSO events in other regional records. This strong interannual variability persisted until ~700 cal. years BP, when ENSO-related variability at the lake decreased as the SST gradient strengthened.  Persistent, dry conditions then dominated between 300 and 50 cal. years BP (AD 1650-1900, ± ~100 years), whereas wetter conditions and frequent El Niño events dominated in the most recent century.","author":{"name":"Thompson, D.M.; Conroy, J.L.; Collins, A.; Hlohowskyj, S.; Overpeck, J.T.; Riedinger-Whitmore, M.; Cole, J.E.; Bush, M.B.; Corley, T.L.; Steinitz Kannan, M."},"citation":"Thompson, D.M.; Conroy, J.L.; Collins, A.; Hlohowskyj, S.; Overpeck, J.T.; Riedinger-Whitmore, M.; Cole, J.E.; Bush, M.B.; Corley, T.L.; Steinitz Kannan, M. 2017. Tropical Pacific climate variability over the last 6000 years as recorded in Bainbridge Crater Lake, Galápagos. Paleoceanography. . ","edition":null,"identifier":null,"issue":null,"journal":"Paleoceanography","pages":null,"pubRank":"1","pubYear":2017,"reportNumber":null,"title":"Tropical Pacific climate variability over the last 6000 years as recorded in Bainbridge Crater Lake, Galápagos","type":"publication","volume":null},{"abstract":null,"author":{"name":"Melanie A. Riedinger, Miriam Steinitz-Kannan, William M. Last, Mark Brenner"},"citation":"Melanie A. Riedinger, Miriam Steinitz-Kannan, William M. Last, Mark Brenner. 2002. A ~6100 14C yr record of El Niño activity from the Galápagos Islands. Journal of Paleolimnology, 27(1), 1-7. doi: 10.1023/A:1013514408468","edition":null,"identifier":{"id":"10.1023/A:1013514408468","type":"doi","url":"http://dx.doi.org/10.1023/A:1013514408468"},"issue":"1","journal":"Journal of Paleolimnology","pages":"1-7","pubRank":"2","pubYear":2002,"reportNumber":null,"title":"A ~6100 14C yr record of El Niño activity from the Galápagos Islands","type":"publication","volume":"27"}],"reconstruction":"N","scienceKeywords":null,"site":[{"NOAASiteId":"57273","geo":{"geoType":"Feature","geometry":{"coordinates":["-.35","-90.57"],"type":"POINT"},"properties":{"easternmostLongitude":"-90.57","maxElevationMeters":"0","minElevationMeters":"0","northernmostLatitude":"-0.35","southernmostLatitude":"-0.35","westernmostLongitude":"-90.57"}},"locationName":"Ocean>Pacific Ocean>Eastern Pacific Ocean>Galapagos Islands","mappable":"Y","paleoData":[{"NOAADataTableId":"33383","coreLengthMeters":null,"dataFile":[{"NOAAKeywords":["earth 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