| A | B | C | D | E | F | G | H | I | J | K | L | M | N | O | P | Q | R | S | T | |
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1 | Base Metadata | Publication Metadata | Geographic metadata | |||||||||||||||||
2 | LiPDVersion | 1.2 | pub1_DOI | 10.1016/j.palaeo.2014.07.039 | geo_latitude | 10.3 | ||||||||||||||
3 | archiveType | Coral (CO) | pub1_author | Wu, H. | geo_longitude | -109.22 | ||||||||||||||
4 | dataSetName | CO14WUCL | pub1_dataUrl | https://www.ncdc.noaa.gov/cdo/f?p=519:1:::::P1_STUDY_ID:17380 | geo_siteName | Clipperton Atoll | ||||||||||||||
5 | collectionName | F1B | pub1_pubYear | 2014 | ||||||||||||||||
6 | googleMetadataWorksheet | on4461z | ||||||||||||||||||
7 | googleSpreadSheetKey | 1MjIjGINZkkCuTq4taZWDJS0Ddmx_knTJApUoI8PiNao | ||||||||||||||||||
8 | maxYear | 1956.79 | ||||||||||||||||||
9 | minYear | 1874.08 | ||||||||||||||||||
10 | ||||||||||||||||||||
11 | paleoData column metadata | |||||||||||||||||||
12 | paleoData_TSid | paleoData_variableName | paleoData_description | paleoData_units | paleoData_QCnotes | paleoData_instrument | paleoData_iso2kUI | paleoData_measurementMaterial | paleoData_measurementStandard | paleoData_paleoDataTableName | paleoData_paleoMeasurementTableNumber | paleoData_paleoNumber | paleoData_uncertaintyAnalytical | paleoData_variableType | isotopeInterpretation_inferredMaterial | isotopeInterpretation_integrationTime | isotopeInterpretation_integrationTimeBasis | isotopeInterpretation_integrationTimeUncertainty | isotopeInterpretation_integrationTimeUncertaintyType | isotopeInterpretation_integrationTimeUnits |
13 | LPD5769e44e | year | Year AD | AD | s1 | 1 | 1 | |||||||||||||
14 | CO14WUCL01A | ?18O | ?18O of the coral skeleton | ? | Fossil coral - this record was used to determine the variability of d18Osw by deconvoluing the d18O signal using Sr/Ca data | Micromass Optima isotope ratio mass spectrometer coupled to a Multiprep carbonate inlet system at UMR 5805 EPOC | CO14WUCL01A | coral carbonate | VPDB | s1 | 1 | 1 | 0.05 per mill for standrad (NBS19) | interpolated | seawater | 1 | "The age of colony CF1B was determined by 230Th/U-dating following established methodology (Edwards et al., 1987; Shen et al., 2002).Three dates were performed at the top, middle, and bottom of the CF1B core. All ages were corrected for the effect of detrital Th contamination assuming a bulk earth 232Th/238U weight ratio of 3.8 for the detritus and 230Th, 234U, and 238U in secular equilibri- um. The reliability of the determined 230Th/U-ages was verified using established criteria such as initial 234U/238U in agreement with 234U/ 238U of modern seawater (i.e., 146 � 3?) (Shen et al., 2008). | 5 years | U/Th error | month |