{"NOAAStudyId":"1886","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":"1996-07-01","dataPublisher":"NOAA","dataType":"CORALS AND SCLEROSPONGES","dataTypeInformation":"https://www.ncdc.noaa.gov/data-access/paleoclimatology-data/datasets/coral-sclerosponge","difMetadataLink":"http://www1.ncdc.noaa.gov/pub/data/metadata/published/paleo/dif/xml/noaa-coral-1886.xml","doi":null,"earliestYearBP":126,"earliestYearCE":1824,"entryId":"noaa-coral-1886","funding":[],"investigators":"Swart, P.K.; Healy, G.F.; Dodge, R.E.; Kramer, P.; Hudson, H.J.; Halley, R.B.; Robblee, M.B.","mostRecentYearBP":-36,"mostRecentYearCE":1986,"onlineResourceLink":"https://www.ncdc.noaa.gov/paleo/study/1886","originalSource":null,"publication":[{"abstract":"A 160 year record of skeletal d13C and d18O was examined in a specimen of the coral Solenastrea bournoni growing in Florida Bay. Variations in the d18O of the skeleton can be correlated to changes in salinity while changes in the d13C reflect cycling of organic material within the Bay. Based on the correlation between salinity and skeletal d18O, we have concluded that there has been no long term increase in salinity in this area of Florida Bay over the past 160 years. Using salinity correlations between the various basins obtained from instrumental data, we have been able to extend our interpretations to other parts of Florida Bay reaching similar conclusions. In contrast to current ideas which have focused on changes in Florida Bay water quality over the past 20-yr history of the Bay as causative in its decline, we have determined that changes in water quality in this basin were already set in motion between 1905 and 1912 by the construction of the Florida East Coast Railway from Miami to Key West. The construction of the railway resulted in the restriction of the exchange of water between the Florida reef tract and the Gulf of Mexico causing Florida Bay to become more eutrophic. Evidence of this process is observed in the sudden shift to relatively lower d13C values coincident with railway construction. Natural events also appear to have influenced the water in the Bay. Between 1912 and 1948 frequent hurricanes had the effect of increasing exchange of water between the Bay and reef tract and removing large quantities of organic rich sediments. However, since 1948 the number of hurricanes affecting the area has decreased and the products of the oxidation of organic material have been increasingly retained within the basin promoting the initiation of eutrophic conditions.","author":null,"citation":"Swart, P.K., G.F. Healy, R.E. Dodge, P. Kramer, H.J. Hudson, R.B. Halley, and M.B. Robblee. 1996. The stable oxygen and carbon isotopic record from a coral growing in Florida Bay: A 160 year record of climatic and anthropogenic influence. Palaeogeography, Palaeoclimatology, Palaeoecology 123(1-4):219-237.","edition":null,"identifier":null,"issue":null,"journal":"Palaeogeography, Palaeoclimatology, Palaeoecology","pages":null,"pubRank":"1","pubYear":1996,"reportNumber":null,"title":"The stable oxygen and carbon isotopic record from a coral growing in Florida Bay: A 160 year record of climatic and anthropogenic influence","type":"publication","volume":null}],"reconstruction":"N","scienceKeywords":null,"site":[{"NOAASiteId":"1931","geo":{"geoType":"Feature","geometry":{"coordinates":["24.93","-80.75"],"type":"POINT"},"properties":{"easternmostLongitude":"-80.75","maxElevationMeters":"-5","minElevationMeters":"-5","northernmostLatitude":"24.93","southernmostLatitude":"24.93","westernmostLongitude":"-80.75"}},"locationName":"Continent>North America>United States Of America>Florida","mappable":"Y","paleoData":[{"NOAADataTableId":"1993","coreLengthMeters":0,"dataFile":[{"NOAAKeywords":["earth science>paleoclimate>corals and sclerosponges>carbon isotopes","earth science>paleoclimate>corals and sclerosponges>oxygen isotopes"],"fileUrl":"https://www1.ncdc.noaa.gov/pub/data/paleo/coral/atlantic/swart1996-bour_noaa.txt","linkText":"swart1996-bour_noaa.txt","urlDescription":"Coral","variables":[{"cvAdditionalInfo":null,"cvDataType":"CORALS AND SCLEROSPONGES","cvDetail":null,"cvError":null,"cvFormat":"Numeric","cvMaterial":null,"cvMethod":null,"cvSeasonality":null,"cvShortName":null,"cvUnit":"year Common Era","cvWhat":"age variable>age"},{"cvAdditionalInfo":null,"cvDataType":"CORALS AND SCLEROSPONGES","cvDetail":"interpolated","cvError":null,"cvFormat":"Numeric","cvMaterial":"biological material>organism>coral>Siderastrea sp.","cvMethod":"isotope ratio mass spectrometry","cvSeasonality":"annual","cvShortName":null,"cvUnit":"per mil PDB","cvWhat":"chemical composition>isotope>isotope ratio>delta 18O"},{"cvAdditionalInfo":null,"cvDataType":"CORALS AND SCLEROSPONGES","cvDetail":"interpolated","cvError":null,"cvFormat":"Numeric","cvMaterial":"biological material>organism>coral>Siderastrea sp.","cvMethod":"isotope ratio mass spectrometry","cvSeasonality":"annual","cvShortName":null,"cvUnit":"per mil PDB","cvWhat":"chemical composition>isotope>isotope ratio>delta 13C"}]}],"dataTableName":"FB6","dataTableNotes":null,"earliestYear":1824,"earliestYearBP":126,"earliestYearCE":1824,"mostRecentYear":1986,"mostRecentYearBP":-36,"mostRecentYearCE":1986,"species":[],"timeUnit":"AD"}],"siteName":"Florida Bay"}],"studyCode":null,"studyName":"Florida Bay - Stable Isotope Data","studyNotes":null,"version":"1.0","xmlId":"1134"}