{ "paleoData": [ { "measurementTable": [ { "tableName": "paleo1measurement1", "year": { "coralExtensionRate": "13", "coralExtensionRateNotes": "13 ± 3 mm/year; 30 μm/day ± 19% RSD", "coralTissueThickness": "5", "core": "Davies 2; Davies 2 side", "datum": null, "description": null, "gbr14CDate": "NA", "gbr14CDateUncertainty": "NA", "gbrChronologyNotes": "SrCa time series was derived by scaling of the distance axis for 1989 to 1993.", "gbrDataCoverageGroup": "3", "gbrDatingNotes": null, "gbrIsAnomaly": "FALSE", "gbrIsDatabaseDuplicate": "TRUE", "gbrUThDate": "NA", "gbrUThDateUncertainty": "NA", "hasTimeTsid": "GBRCD.AL03DAV01_2.year", "isPrimary": true, "jcpMeasured": "NA", "jcpUsed": "FALSE", "longName": "calendar year AD", "measurementInstrument": null, "measurementMaterialScreening": "No", "measurementMethod": null, "notes": "500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. 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See Table 1 in Alibert et al. (2003) for standards measurements. In-house pressed-powder coral standard and NIST 614 glass standard.' has been replaced by '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. In-house pressed-powder coral standard and NIST 614 glass standard.'"], ["BaCa (GBRCD.AL03DAV01_2.BaCa): paleoData_notes: '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. 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In-house pressed-powder coral standard and NIST 614 glass standard.' has been replaced by '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. In-house pressed-powder coral standard and NIST 614 glass standard.'"], ["Distance (GBRCD.AL03DAV01_2.Distance): paleoData_notes: '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. In-house pressed-powder coral standard and NIST 614 glass standard.' has been replaced by '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. In-house pressed-powder coral standard and NIST 614 glass standard.'"], ["Mn (GBRCD.AL03DAV01_2.Mn): paleoData_notes: '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. In-house pressed-powder coral standard and NIST 614 glass standard.' has been replaced by '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. In-house pressed-powder coral standard and NIST 614 glass standard.'"], ["MnCa (GBRCD.AL03DAV01_2.MnCa): paleoData_notes: '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. In-house pressed-powder coral standard and NIST 614 glass standard.' has been replaced by '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. In-house pressed-powder coral standard and NIST 614 glass standard.'"], ["P (GBRCD.AL03DAV01_2.P): paleoData_notes: '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. In-house pressed-powder coral standard and NIST 614 glass standard.' has been replaced by '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. In-house pressed-powder coral standard and NIST 614 glass standard.'"], ["Y (GBRCD.AL03DAV01_2.Y): paleoData_notes: '500 x 50 μm rectangular laser beam is scanned along the coral growth axis at 2 mm per min with first scan at at 5 Hz and then the second scan at 20 Hz pulse rate for different trace elements and isotopes. See Table 1 in Alibert et al. (2003) for standards measurements. 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(2003)", "gbrHasAlternateCalibration": "FALSE", "gbrIsCompositeCalibration": "FALSE", "gbrIsCoreIDOtherStudy": "TRUE", "gbrIsSstCalibration": "FALSE", "gbrUseSstCalibration": "FALSE", "hasIGSN": null, "lipdverseLink": "https://lipdverse.org/data/AL03DAV01_2/1_0_6", "lipdVersion": 1.3, "maxYear": 1993.7932, "minYear": 1989.4452, "notes": null, "originalDataUrl": "https://doi.org/10.25921/ddhn-hf49", "pub": [ { "altDataURL": null, "author": "Alibert, C., Kinsley, L., Fallon, S.J., McCulloch, M.T., Berkelmans, R. & McAllister, F.", "citation": "Alibert, C., Kinsley, L., Fallon, S.J., McCulloch, M.T., Berkelmans, R. & McAllister, F. (2003), 'Source of trace element variability in Great Barrier Reef corals affected by the Burdekin flood plumes', Geochimica et Cosmochimica Acta, 67 (2), 231-246, 10.1016/S0016-7037(02)01055-4.", "doi": "10.1016/S0016-7037(02)01055-4", "doiData": "10.25921/ddhn-hf49", "firstAuthor": "Alibert, C.", "journal": "Geochimica et Cosmochimica Acta", "title": "Source of trace element variability in Great Barrier Reef corals affected by the Burdekin flood plumes", "year": 2003 } ], "geo": { "elevation": -3.1, "latitude": -18.8, "location": null, "longitude": 147.7, "notes": "GPS coordinates offset from Davies Reef. Reef located -18.82, 147.64 for reef from 'Reefs and shoals – Queensland' geodatabase. Upper surface 3.1 m below low tide mark.", "siteName": "Davies Reef" }, "@context": "context.jsonld" }