Version history for il085HyHYUGXeanna5Vp - Hoqcave.VanRampelbergh.2013

Version: 1.0.14

lastVersion: 1.0.13
curator: nicholas
timestamp: 2023-08-10 22:55:14 UTC
changes:
- Base metadata:
  - originalDataUrl: ‘http://dx.doi.org/10.17864/1947.256’ has been replaced by ‘https://doi.org/10.17864/1947.256’
- Publication metadata:
  - pub1_author: NULL has been replaced by ‘Ma√OEt{’{e}} Van Rampelbergh and Dominik Fleitmann and Sophie Verheyden and Hai Cheng and Lawrence Edwards and Peter De Geest and David De Vleeschouwer and Stephen J. Burns and Albert Matter and Philippe Claeys and Eddy Keppens’
  - pub1_journal: NULL has been replaced by ‘Quaternary Science Reviews’
  - pub1_pages: NULL has been replaced by ‘129–142’
  - pub1_title: NULL has been replaced by ‘Mid- to late Holocene Indian Ocean Monsoon variability recorded in four speleothems from Socotra Island, Yemen’

Version: 1.0.13

lastVersion: 1.0.12
curator: nicholas
timestamp: 2023-05-31 20:38:44 UTC
changes:
- Paleo Column metadata:
  - d18O (S2LRAwkFTDejje): paleoData_notes: ‘((( ((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d18O (S2LRDg1jlgbIn8): paleoData_notes: ‘((( ((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRYaQyDMwILZ): paleoData_notes: ‘((( ((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRpSzKt5ew3h): paleoData_notes: ‘((( ((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’

Version: 1.0.12

lastVersion: 1.0.11
curator: nicholas
timestamp: 2023-05-30 15:48:55 UTC
changes:
- Paleo Column metadata:
  - d18O (S2LRAwkFTDejje): paleoData_notes: ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘((( ((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d18O (S2LRAwkFTDejje): paleoData_QCCertification: ‘CH’ has been replaced by ‘CH, CR’
  - d18O (S2LRDg1jlgbIn8): paleoData_notes: ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘((( ((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d18O (S2LRDg1jlgbIn8): paleoData_QCCertification: ‘CH’ has been replaced by ‘CH, CR’
  - d13C (S2LRYaQyDMwILZ): paleoData_notes: ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘((( ((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRYaQyDMwILZ): paleoData_QCCertification: ‘CH’ has been replaced by ‘CH, CR’
  - d13C (S2LRpSzKt5ew3h): paleoData_notes: ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘((( ((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRpSzKt5ew3h): paleoData_QCCertification: ‘CH’ has been replaced by ‘CH, CR’
- Paleo Interpretation metadata:
  - d18O (S2LRAwkFTDejje): interpretation1_seasonalityGeneral: ‘winterOnly’ has been replaced by ‘Winter’
  - d18O (S2LRDg1jlgbIn8): interpretation1_seasonalityGeneral: ‘winterOnly’ has been replaced by ‘Winter’
  - d13C (S2LRYaQyDMwILZ): interpretation1_seasonalityGeneral: ‘winterOnly’ has been replaced by ‘Winter’
  - d13C (S2LRpSzKt5ew3h): interpretation1_seasonalityGeneral: ‘winterOnly’ has been replaced by ‘Winter’

Version: 1.0.11

lastVersion: 1.0.10
curator: nicholas
timestamp: 2023-03-29 19:49:26 UTC
changes:
- Paleo Column metadata:
  - d18O (S2LRAwkFTDejje): paleoData_notes: ‘((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d18O (S2LRDg1jlgbIn8): paleoData_notes: ‘((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRYaQyDMwILZ): paleoData_notes: ‘((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRpSzKt5ew3h): paleoData_notes: ‘((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’

Version: 1.0.10

lastVersion: 1.0.9
curator: nicholas
timestamp: 2023-03-24 22:24:37 UTC
changes:
- Paleo Column metadata:
  - d18O (S2LRAwkFTDejje): paleoData_proxyGeneral: ‘isotope’ has been replaced by ‘isotopic’
  - d18O (S2LRDg1jlgbIn8): paleoData_proxyGeneral: ‘isotope’ has been replaced by ‘isotopic’
  - d13C (S2LRYaQyDMwILZ): paleoData_proxyGeneral: ‘isotope’ has been replaced by ‘isotopic’
  - d13C (S2LRpSzKt5ew3h): paleoData_proxyGeneral: ‘isotope’ has been replaced by ‘isotopic’

Version: 1.0.9

lastVersion: 1.0.8
curator: nicholas
timestamp: 2023-02-13 23:44:35 UTC
changes:
- Paleo Column metadata:
  - d18O (S2LRAwkFTDejje): paleoData_notes: ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d18O (S2LRDg1jlgbIn8): paleoData_notes: ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRpSzKt5ew3h): paleoData_notes: ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRYaQyDMwILZ): paleoData_notes: ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’ has been replaced by ‘((( “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the ��amount effect��, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) ))) “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013) /// “d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’

Version: 1.0.8

lastVersion: 1.0.7
curator: nicholas
timestamp: 2023-02-10 14:33:32 UTC
changes:
- Paleo Interpretation metadata:
  - uncertaintyHigh (S2LR3jI3H6oido): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyLow (S2LR3uwikQ00Yb): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyHigh (S2LR86CKAXVgU1): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyLow (S2LRA6RXGFeJ5x): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyLow (S2LRaUNP4RQWS0): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyHigh (S2LRbM5jdDkjNo): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyHigh (S2LRCGT5qaJt9u): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyHigh (S2LRgnrjxckw0g): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyLow (S2LRi4eygntgd9): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyHigh (S2LRjYcsIWmhgR): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyHigh (S2LRjZRw85WXLb): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyHigh (S2LRl47f0OQOcn): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyHigh (S2LRLfV6UxULbX): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyLow (S2LRNDkNbuNbrQ): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyLow (S2LRogf0R1H6Yr): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyLow (S2LRp3L24IDt3g): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyLow (S2LRQ2p2oBugz6): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyLow (S2LRqCccjrvp6H): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyLow (S2LRRGmvO6iGwS): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyHigh (S2LRStc9RNOceR): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyHigh (S2LRStTNzlcVwS): interpretation1_scope: NULL has been replaced by ‘climate’
  - uncertaintyLow (S2LRwgpzDptQCR): interpretation1_scope: NULL has been replaced by ‘climate’

Version: 1.0.7

lastVersion: 1.0.6
curator: nicholas
timestamp: 2023-02-09 15:46:00 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
- Geographic metadata:
  - geo_elevation: NULL has been replaced by ‘335’
- Paleo Column metadata:
  - correction (S2LR09uNEAWatI): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized; paleoData_method has been standardized’
  - correction (S2LR09uNEAWatI): paleoData_variableName: ‘hasAragoniteCorrectionComposite’ has been replaced by ‘correction’
  - correction (S2LR09uNEAWatI): paleoData_method: NULL has been replaced by ‘aragonite correction’
  - correction (S2LR09uNEAWatI): paleoData_summaryStatistic: NULL has been replaced by ‘composite’
  - uncertaintyHigh (S2LR3jI3H6oido): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyHigh (S2LR3jI3H6oido): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyHigh (S2LR3jI3H6oido): paleoData_variableName: ‘ageStalAgeUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
  - uncertaintyHigh (S2LR3jI3H6oido): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyHigh (S2LR3jI3H6oido): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyHigh (S2LR3jI3H6oido): paleoData_method: NULL has been replaced by ‘StalAge’
  - uncertaintyLow (S2LR3uwikQ00Yb): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyLow (S2LR3uwikQ00Yb): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyLow (S2LR3uwikQ00Yb): paleoData_variableName: ‘agecopRaUncertaintyLow’ has been replaced by ‘uncertaintyLow’
  - uncertaintyLow (S2LR3uwikQ00Yb): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyLow (S2LR3uwikQ00Yb): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyLow (S2LR3uwikQ00Yb): paleoData_method: NULL has been replaced by ‘copRa’
  - uncertainty (S2LR4LeIt5GTnl): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LR4LeIt5GTnl): paleoData_variableName: ‘d18OPrecision’ has been replaced by ‘uncertainty’
  - uncertainty (S2LR4LeIt5GTnl): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
  - uncertainty (S2LR4LeIt5GTnl): paleoData_method: NULL has been replaced by ‘precision’
  - sampleID (S2LR5rGrphEzs3): paleoData_variableName: ‘sisalSampleID’ has been replaced by ‘sampleID’
  - mineralogy (S2LR5suPDSzezQ): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized’
  - mineralogy (S2LR5suPDSzezQ): paleoData_variableName: ‘mineralogyComposite’ has been replaced by ‘mineralogy’
  - mineralogy (S2LR5suPDSzezQ): paleoData_summaryStatistic: NULL has been replaced by ‘composite’
  - age (S2LR5wj1UpfRj6): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LR5wj1UpfRj6): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LR5wj1UpfRj6): paleoData_variableName: ‘ageBacon’ has been replaced by ‘age’
  - age (S2LR5wj1UpfRj6): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LR5wj1UpfRj6): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - age (S2LR5wj1UpfRj6): paleoData_method: NULL has been replaced by ‘Bacon’
  - uncertainty (S2LR5xd8rvXaVG): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LR5xd8rvXaVG): paleoData_variableName: ‘d13CPrecision’ has been replaced by ‘uncertainty’
  - uncertainty (S2LR5xd8rvXaVG): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
  - uncertainty (S2LR5xd8rvXaVG): paleoData_method: NULL has been replaced by ‘precision’
  - uncertainty (S2LR6lmnNebcSx): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LR6lmnNebcSx): paleoData_variableName: ‘d18OStandardComposite’ has been replaced by ‘uncertainty’
  - uncertainty (S2LR6lmnNebcSx): paleoData_measurementMaterial: NULL has been replaced by ‘d18O’
  - uncertainty (S2LR6lmnNebcSx): paleoData_method: NULL has been replaced by ‘standard’
  - uncertainty (S2LR6lmnNebcSx): paleoData_summaryStatistic: NULL has been replaced by ‘composite’
  - age (S2LR70vqhhyP7k): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LR70vqhhyP7k): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LR70vqhhyP7k): paleoData_variableName: ‘agelinInterp’ has been replaced by ‘age’
  - age (S2LR70vqhhyP7k): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LR70vqhhyP7k): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - age (S2LR70vqhhyP7k): paleoData_method: NULL has been replaced by ‘linInterp’
  - age (S2LR7rEYZolO0L): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LR7rEYZolO0L): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LR7rEYZolO0L): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LR7rEYZolO0L): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - d13C (S2LR7tQhtTG333): paleoData_variableName: ‘d13CStandardComposite’ has been replaced by ‘d13C’
  - uncertaintyHigh (S2LR86CKAXVgU1): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyHigh (S2LR86CKAXVgU1): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyHigh (S2LR86CKAXVgU1): paleoData_variableName: ‘ageBaconUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
  - uncertaintyHigh (S2LR86CKAXVgU1): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyHigh (S2LR86CKAXVgU1): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyHigh (S2LR86CKAXVgU1): paleoData_method: NULL has been replaced by ‘Bacon’
  - age (S2LR8sWQxVslcM): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LR8sWQxVslcM): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LR8sWQxVslcM): paleoData_variableName: ‘agecopRa’ has been replaced by ‘age’
  - age (S2LR8sWQxVslcM): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LR8sWQxVslcM): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - age (S2LR8sWQxVslcM): paleoData_method: NULL has been replaced by ‘copRa’
  - d13C (S2LR9rSXs12WrM): paleoData_variableName: ‘d13CComposite’ has been replaced by ‘d13C’
  - correction (S2LRa0CueSKYhN): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized’
  - correction (S2LRa0CueSKYhN): paleoData_variableName: ‘hasAragoniteCorrection’ has been replaced by ‘correction’
  - correction (S2LRa0CueSKYhN): paleoData_method: NULL has been replaced by ‘aragonite correction’
  - uncertaintyLow (S2LRA6RXGFeJ5x): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyLow (S2LRA6RXGFeJ5x): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyLow (S2LRA6RXGFeJ5x): paleoData_variableName: ‘ageBaconUncertaintyLow’ has been replaced by ‘uncertaintyLow’
  - uncertaintyLow (S2LRA6RXGFeJ5x): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyLow (S2LRA6RXGFeJ5x): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyLow (S2LRA6RXGFeJ5x): paleoData_method: NULL has been replaced by ‘Bacon’
  - d18O (S2LRAc4LTUQ8qQ): paleoData_variableName: ‘d18OComposite’ has been replaced by ‘d18O’
  - uncertaintyLow (S2LRaUNP4RQWS0): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyLow (S2LRaUNP4RQWS0): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyLow (S2LRaUNP4RQWS0): paleoData_variableName: ‘ageBaconUncertaintyLow’ has been replaced by ‘uncertaintyLow’
  - uncertaintyLow (S2LRaUNP4RQWS0): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyLow (S2LRaUNP4RQWS0): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyLow (S2LRaUNP4RQWS0): paleoData_method: NULL has been replaced by ‘Bacon’
  - correction (S2LRBeUQ8raNbG): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized’
  - correction (S2LRBeUQ8raNbG): paleoData_variableName: ‘hasAragoniteCorrection’ has been replaced by ‘correction’
  - correction (S2LRBeUQ8raNbG): paleoData_method: NULL has been replaced by ‘aragonite correction’
  - uncertaintyHigh (S2LRbM5jdDkjNo): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyHigh (S2LRbM5jdDkjNo): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyHigh (S2LRbM5jdDkjNo): paleoData_variableName: ‘agecopRaUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
  - uncertaintyHigh (S2LRbM5jdDkjNo): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyHigh (S2LRbM5jdDkjNo): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyHigh (S2LRbM5jdDkjNo): paleoData_method: NULL has been replaced by ‘copRa’
  - uncertaintyHigh (S2LRCGT5qaJt9u): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyHigh (S2LRCGT5qaJt9u): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyHigh (S2LRCGT5qaJt9u): paleoData_variableName: ‘ageBaconUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
  - uncertaintyHigh (S2LRCGT5qaJt9u): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyHigh (S2LRCGT5qaJt9u): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyHigh (S2LRCGT5qaJt9u): paleoData_method: NULL has been replaced by ‘Bacon’
  - uncertainty (S2LRCQuHPhIa4D): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRCQuHPhIa4D): paleoData_variableName: ‘d18OPrecisionComposite’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRCQuHPhIa4D): paleoData_measurementMaterial: NULL has been replaced by ‘d18O’
  - uncertainty (S2LRCQuHPhIa4D): paleoData_method: NULL has been replaced by ‘precision’
  - uncertainty (S2LRCQuHPhIa4D): paleoData_summaryStatistic: NULL has been replaced by ‘composite’
  - correction (S2LRctczHzosGX): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized’
  - correction (S2LRctczHzosGX): paleoData_variableName: ‘hasAragoniteCorrection’ has been replaced by ‘correction’
  - correction (S2LRctczHzosGX): paleoData_method: NULL has been replaced by ‘aragonite correction’
  - uncertainty (S2LRCUNFyFxrCf): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRCUNFyFxrCf): paleoData_variableName: ‘d18OPrecision’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRCUNFyFxrCf): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
  - uncertainty (S2LRCUNFyFxrCf): paleoData_method: NULL has been replaced by ‘precision’
  - d13C (S2LRd4gHFIae9i): paleoData_variableName: ‘d13CPrecisionComposite’ has been replaced by ‘d13C’
  - uncertainty (S2LRD9gP2O7qg4): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRD9gP2O7qg4): paleoData_variableName: ‘d18OStandard’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRD9gP2O7qg4): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
  - uncertainty (S2LRD9gP2O7qg4): paleoData_method: NULL has been replaced by ‘standard’
  - depth (S2LRDPD9RgZJpl): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized’
  - depth (S2LRDPD9RgZJpl): paleoData_units: ‘depth_sample’ has been replaced by ‘mm’
  - depth (S2LRDPD9RgZJpl): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - depth (S2LREp53J1tQPb): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized’
  - depth (S2LREp53J1tQPb): paleoData_units: ‘depth_sample’ has been replaced by ‘mm’
  - depth (S2LREp53J1tQPb): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - age (S2LRfJniTua2bs): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRfJniTua2bs): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRfJniTua2bs): paleoData_variableName: ‘ageBchron’ has been replaced by ‘age’
  - age (S2LRfJniTua2bs): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRfJniTua2bs): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - age (S2LRfJniTua2bs): paleoData_method: NULL has been replaced by ‘Bchron’
  - uncertaintyHigh (S2LRgnrjxckw0g): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyHigh (S2LRgnrjxckw0g): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyHigh (S2LRgnrjxckw0g): paleoData_variableName: ‘ageBchronUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
  - uncertaintyHigh (S2LRgnrjxckw0g): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyHigh (S2LRgnrjxckw0g): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyHigh (S2LRgnrjxckw0g): paleoData_method: NULL has been replaced by ‘Bchron’
  - age (S2LRgZJ7h7MtVP): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRgZJ7h7MtVP): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRgZJ7h7MtVP): paleoData_variableName: ‘ageStalAge’ has been replaced by ‘age’
  - age (S2LRgZJ7h7MtVP): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRgZJ7h7MtVP): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - age (S2LRgZJ7h7MtVP): paleoData_method: NULL has been replaced by ‘StalAge’
  - age (S2LRh0UstDxV7t): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRh0UstDxV7t): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRh0UstDxV7t): paleoData_variableName: ‘ageBacon’ has been replaced by ‘age’
  - age (S2LRh0UstDxV7t): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRh0UstDxV7t): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - age (S2LRh0UstDxV7t): paleoData_method: NULL has been replaced by ‘Bacon’
  - uncertainty (S2LRHENNVj90YY): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRHENNVj90YY): paleoData_variableName: ‘d13CStandard’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRHENNVj90YY): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
  - uncertainty (S2LRHENNVj90YY): paleoData_method: NULL has been replaced by ‘standard’
  - uncertaintyLow (S2LRi4eygntgd9): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyLow (S2LRi4eygntgd9): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyLow (S2LRi4eygntgd9): paleoData_variableName: ‘ageStalAgeUncertaintyLow’ has been replaced by ‘uncertaintyLow’
  - uncertaintyLow (S2LRi4eygntgd9): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyLow (S2LRi4eygntgd9): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyLow (S2LRi4eygntgd9): paleoData_method: NULL has been replaced by ‘StalAge’
  - age (S2LRia1aI3Z93v): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRia1aI3Z93v): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRia1aI3Z93v): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRia1aI3Z93v): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - sampleID (S2LRIGt8RgQu0l): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized’
  - sampleID (S2LRIGt8RgQu0l): paleoData_variableName: ‘sisalSampleIDComposite’ has been replaced by ‘sampleID’
  - sampleID (S2LRIGt8RgQu0l): paleoData_summaryStatistic: NULL has been replaced by ‘composite’
  - uncertaintyHigh (S2LRjYcsIWmhgR): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyHigh (S2LRjYcsIWmhgR): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyHigh (S2LRjYcsIWmhgR): paleoData_variableName: ‘ageBchronUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
  - uncertaintyHigh (S2LRjYcsIWmhgR): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyHigh (S2LRjYcsIWmhgR): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyHigh (S2LRjYcsIWmhgR): paleoData_method: NULL has been replaced by ‘Bchron’
  - uncertaintyHigh (S2LRjZRw85WXLb): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyHigh (S2LRjZRw85WXLb): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyHigh (S2LRjZRw85WXLb): paleoData_variableName: ‘ageBchronUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
  - uncertaintyHigh (S2LRjZRw85WXLb): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyHigh (S2LRjZRw85WXLb): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyHigh (S2LRjZRw85WXLb): paleoData_method: NULL has been replaced by ‘Bchron’
  - depth (S2LRkymurivwJC): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized’
  - depth (S2LRkymurivwJC): paleoData_units: ‘depth_sample’ has been replaced by ‘mm’
  - depth (S2LRkymurivwJC): paleoData_variableName: ‘depthComposite’ has been replaced by ‘depth’
  - depth (S2LRkymurivwJC): paleoData_summaryStatistic: NULL has been replaced by ‘composite’
  - uncertaintyHigh (S2LRl47f0OQOcn): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyHigh (S2LRl47f0OQOcn): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyHigh (S2LRl47f0OQOcn): paleoData_variableName: ‘ageBaconUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
  - uncertaintyHigh (S2LRl47f0OQOcn): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyHigh (S2LRl47f0OQOcn): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyHigh (S2LRl47f0OQOcn): paleoData_method: NULL has been replaced by ‘Bacon’
  - depth (S2LRl7dT46irYN): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized’
  - depth (S2LRl7dT46irYN): paleoData_units: ‘depth_sample’ has been replaced by ‘mm’
  - depth (S2LRl7dT46irYN): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - uncertaintyHigh (S2LRLfV6UxULbX): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyHigh (S2LRLfV6UxULbX): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyHigh (S2LRLfV6UxULbX): paleoData_variableName: ‘ageBchronUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
  - uncertaintyHigh (S2LRLfV6UxULbX): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyHigh (S2LRLfV6UxULbX): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyHigh (S2LRLfV6UxULbX): paleoData_method: NULL has been replaced by ‘Bchron’
  - uncertaintyLow (S2LRNDkNbuNbrQ): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyLow (S2LRNDkNbuNbrQ): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyLow (S2LRNDkNbuNbrQ): paleoData_variableName: ‘ageBchronUncertaintyLow’ has been replaced by ‘uncertaintyLow’
  - uncertaintyLow (S2LRNDkNbuNbrQ): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyLow (S2LRNDkNbuNbrQ): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyLow (S2LRNDkNbuNbrQ): paleoData_method: NULL has been replaced by ‘Bchron’
  - uncertaintyLow (S2LRogf0R1H6Yr): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyLow (S2LRogf0R1H6Yr): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyLow (S2LRogf0R1H6Yr): paleoData_variableName: ‘ageBaconUncertaintyLow’ has been replaced by ‘uncertaintyLow’
  - uncertaintyLow (S2LRogf0R1H6Yr): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyLow (S2LRogf0R1H6Yr): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyLow (S2LRogf0R1H6Yr): paleoData_method: NULL has been replaced by ‘Bacon’
  - uncertaintyLow (S2LRp3L24IDt3g): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyLow (S2LRp3L24IDt3g): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyLow (S2LRp3L24IDt3g): paleoData_variableName: ‘agelinInterpUncertaintyLow’ has been replaced by ‘uncertaintyLow’
  - uncertaintyLow (S2LRp3L24IDt3g): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyLow (S2LRp3L24IDt3g): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyLow (S2LRp3L24IDt3g): paleoData_method: NULL has been replaced by ‘linInterp’
  - age (S2LRpM8VJdbYxF): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRpM8VJdbYxF): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRpM8VJdbYxF): paleoData_variableName: ‘ageBchron’ has been replaced by ‘age’
  - age (S2LRpM8VJdbYxF): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRpM8VJdbYxF): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - age (S2LRpM8VJdbYxF): paleoData_method: NULL has been replaced by ‘Bchron’
  - age (S2LRPNV2Tsopq8): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRPNV2Tsopq8): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRPNV2Tsopq8): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRPNV2Tsopq8): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - uncertaintyLow (S2LRQ2p2oBugz6): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyLow (S2LRQ2p2oBugz6): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyLow (S2LRQ2p2oBugz6): paleoData_variableName: ‘ageBchronUncertaintyLow’ has been replaced by ‘uncertaintyLow’
  - uncertaintyLow (S2LRQ2p2oBugz6): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyLow (S2LRQ2p2oBugz6): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyLow (S2LRQ2p2oBugz6): paleoData_method: NULL has been replaced by ‘Bchron’
  - uncertaintyLow (S2LRqCccjrvp6H): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyLow (S2LRqCccjrvp6H): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyLow (S2LRqCccjrvp6H): paleoData_variableName: ‘ageBaconUncertaintyLow’ has been replaced by ‘uncertaintyLow’
  - uncertaintyLow (S2LRqCccjrvp6H): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyLow (S2LRqCccjrvp6H): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyLow (S2LRqCccjrvp6H): paleoData_method: NULL has been replaced by ‘Bacon’
  - uncertaintyLow (S2LRRGmvO6iGwS): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyLow (S2LRRGmvO6iGwS): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyLow (S2LRRGmvO6iGwS): paleoData_variableName: ‘ageBchronUncertaintyLow’ has been replaced by ‘uncertaintyLow’
  - uncertaintyLow (S2LRRGmvO6iGwS): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyLow (S2LRRGmvO6iGwS): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyLow (S2LRRGmvO6iGwS): paleoData_method: NULL has been replaced by ‘Bchron’
  - uncertaintyHigh (S2LRStc9RNOceR): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyHigh (S2LRStc9RNOceR): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyHigh (S2LRStc9RNOceR): paleoData_variableName: ‘agelinInterpUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
  - uncertaintyHigh (S2LRStc9RNOceR): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyHigh (S2LRStc9RNOceR): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyHigh (S2LRStc9RNOceR): paleoData_method: NULL has been replaced by ‘linInterp’
  - uncertaintyHigh (S2LRStTNzlcVwS): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyHigh (S2LRStTNzlcVwS): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyHigh (S2LRStTNzlcVwS): paleoData_variableName: ‘ageBaconUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
  - uncertaintyHigh (S2LRStTNzlcVwS): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyHigh (S2LRStTNzlcVwS): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyHigh (S2LRStTNzlcVwS): paleoData_method: NULL has been replaced by ‘Bacon’
  - sampleID (S2LRt9ciGpVJ1N): paleoData_variableName: ‘sisalSampleID’ has been replaced by ‘sampleID’
  - sampleID (S2LRuNhRgJSXUk): paleoData_variableName: ‘sisalSampleID’ has been replaced by ‘sampleID’
  - uncertainty (S2LRuxFEbcJ2hJ): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRuxFEbcJ2hJ): paleoData_variableName: ‘d18OStandard’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRuxFEbcJ2hJ): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
  - uncertainty (S2LRuxFEbcJ2hJ): paleoData_method: NULL has been replaced by ‘standard’
  - age (S2LRv7vqWuHxHG): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRv7vqWuHxHG): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRv7vqWuHxHG): paleoData_variableName: ‘ageBchron’ has been replaced by ‘age’
  - age (S2LRv7vqWuHxHG): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRv7vqWuHxHG): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - age (S2LRv7vqWuHxHG): paleoData_method: NULL has been replaced by ‘Bchron’
  - uncertainty (S2LRVrO0zv3sdN): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRVrO0zv3sdN): paleoData_variableName: ‘d13CPrecision’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRVrO0zv3sdN): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
  - uncertainty (S2LRVrO0zv3sdN): paleoData_method: NULL has been replaced by ‘precision’
  - uncertainty (S2LRw7H5w8dnwS): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRw7H5w8dnwS): paleoData_variableName: ‘d13CStandard’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRw7H5w8dnwS): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
  - uncertainty (S2LRw7H5w8dnwS): paleoData_method: NULL has been replaced by ‘standard’
  - uncertaintyLow (S2LRwgpzDptQCR): paleoData_notes: NULL has been replaced by ‘NA; paleoData_inferredMaterial has been standardized; paleoData_method has been standardized; paleoData_datum has been standardized’
  - uncertaintyLow (S2LRwgpzDptQCR): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - uncertaintyLow (S2LRwgpzDptQCR): paleoData_variableName: ‘ageBchronUncertaintyLow’ has been replaced by ‘uncertaintyLow’
  - uncertaintyLow (S2LRwgpzDptQCR): paleoData_datum: NULL has been replaced by ‘1950’
  - uncertaintyLow (S2LRwgpzDptQCR): paleoData_inferredMaterial: NULL has been replaced by ‘age’
  - uncertaintyLow (S2LRwgpzDptQCR): paleoData_method: NULL has been replaced by ‘Bchron’
  - uncertainty (S2LRWmV8bgLclv): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRWmV8bgLclv): paleoData_variableName: ‘d18OStandard’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRWmV8bgLclv): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
  - uncertainty (S2LRWmV8bgLclv): paleoData_method: NULL has been replaced by ‘standard’
  - age (S2LRx4BDMGC9pY): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRx4BDMGC9pY): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRx4BDMGC9pY): paleoData_variableName: ‘ageBchron’ has been replaced by ‘age’
  - age (S2LRx4BDMGC9pY): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRx4BDMGC9pY): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - age (S2LRx4BDMGC9pY): paleoData_method: NULL has been replaced by ‘Bchron’
  - uncertainty (S2LRXMmEHlAvyl): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRXMmEHlAvyl): paleoData_variableName: ‘d18OPrecision’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRXMmEHlAvyl): paleoData_measurementMaterial: NULL has been replaced by ‘d18O carbonate’
  - uncertainty (S2LRXMmEHlAvyl): paleoData_method: NULL has been replaced by ‘precision’
  - age (S2LRxs9wSDh7SM): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRxs9wSDh7SM): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRxs9wSDh7SM): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRxs9wSDh7SM): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - age (S2LRXsxEgPjRqr): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRXsxEgPjRqr): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRXsxEgPjRqr): paleoData_variableName: ‘ageBacon’ has been replaced by ‘age’
  - age (S2LRXsxEgPjRqr): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRXsxEgPjRqr): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - age (S2LRXsxEgPjRqr): paleoData_method: NULL has been replaced by ‘Bacon’
  - age (S2LRypHRqNY6zW): paleoData_notes: NULL has been replaced by ‘NA; paleoData_method has been standardized; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (S2LRypHRqNY6zW): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (S2LRypHRqNY6zW): paleoData_variableName: ‘ageBacon’ has been replaced by ‘age’
  - age (S2LRypHRqNY6zW): paleoData_datum: NULL has been replaced by ‘1950’
  - age (S2LRypHRqNY6zW): paleoData_isPrimary: NULL has been replaced by ‘FALSE’
  - age (S2LRypHRqNY6zW): paleoData_method: NULL has been replaced by ‘Bacon’
  - notes (S2LRZ59Lzfy3fq): paleoData_variableName: ‘entityName’ has been replaced by ‘notes’
  - uncertainty (S2LRZM4iyB8WUW): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRZM4iyB8WUW): paleoData_variableName: ‘d13CPrecision’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRZM4iyB8WUW): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
  - uncertainty (S2LRZM4iyB8WUW): paleoData_method: NULL has been replaced by ‘precision’
  - uncertainty (S2LRzTyOrm509D): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized’
  - uncertainty (S2LRzTyOrm509D): paleoData_variableName: ‘d13CStandard’ has been replaced by ‘uncertainty’
  - uncertainty (S2LRzTyOrm509D): paleoData_measurementMaterial: NULL has been replaced by ‘d13C’
  - uncertainty (S2LRzTyOrm509D): paleoData_method: NULL has been replaced by ‘standard’
- Paleo Interpretation metadata:
  - d18O (S2LRAwkFTDejje): interpretation1_seasonality: ‘11,12,1,2,3’ has been replaced by ‘Nov-Mar’
  - d18O (S2LRAwkFTDejje): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’
  - d18O (S2LRDg1jlgbIn8): interpretation1_seasonality: ‘11,12,1,2,3’ has been replaced by ‘Nov-Mar’
  - d18O (S2LRDg1jlgbIn8): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’
  - d13C (S2LRpSzKt5ew3h): interpretation1_seasonality: ‘11,12,1,2,3’ has been replaced by ‘Nov-Mar’
  - d13C (S2LRpSzKt5ew3h): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’
  - d13C (S2LRYaQyDMwILZ): interpretation1_seasonality: ‘11,12,1,2,3’ has been replaced by ‘Nov-Mar’
  - d13C (S2LRYaQyDMwILZ): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’

Version: 1.0.6

lastVersion: 1.0.5
curator: nicholas
timestamp: 2022-07-28 17:32:45 UTC
changes:
- Geographic metadata:
  - geo_elevation: ‘335’ has been replaced by NULL

Version: 1.0.5

lastVersion: 1.0.4
curator: nicholas
timestamp: 2022-07-15 23:02:33 UTC
changes:
- Paleo Interpretation metadata:
  - hasAragoniteCorrectionComposite (S2LR09uNEAWatI): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OPrecision (S2LR4LeIt5GTnl): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleID (S2LR5rGrphEzs3): interpretation1_scope: NULL has been replaced by ‘climate’
  - mineralogyComposite (S2LR5suPDSzezQ): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CPrecision (S2LR5xd8rvXaVG): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandardComposite (S2LR6lmnNebcSx): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandardComposite (S2LR7tQhtTG333): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CComposite (S2LR9rSXs12WrM): interpretation1_scope: NULL has been replaced by ‘climate’
  - hasAragoniteCorrection (S2LRa0CueSKYhN): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OComposite (S2LRAc4LTUQ8qQ): interpretation1_scope: NULL has been replaced by ‘climate’
  - hasAragoniteCorrection (S2LRBeUQ8raNbG): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OPrecisionComposite (S2LRCQuHPhIa4D): interpretation1_scope: NULL has been replaced by ‘climate’
  - hasAragoniteCorrection (S2LRctczHzosGX): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OPrecision (S2LRCUNFyFxrCf): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CPrecisionComposite (S2LRd4gHFIae9i): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandard (S2LRD9gP2O7qg4): interpretation1_scope: NULL has been replaced by ‘climate’
  - mineralogy (S2LRDQLw2BnWWi): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandard (S2LRHENNVj90YY): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleIDComposite (S2LRIGt8RgQu0l): interpretation1_scope: NULL has been replaced by ‘climate’
  - depthComposite (S2LRkymurivwJC): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRT5MkdZPy5S): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleID (S2LRt9ciGpVJ1N): interpretation1_scope: NULL has been replaced by ‘climate’
  - mineralogy (S2LRUduIkFLNRB): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleID (S2LRuNhRgJSXUk): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandard (S2LRuxFEbcJ2hJ): interpretation1_scope: NULL has been replaced by ‘climate’
  - mineralogy (S2LRVOhRswecbD): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CPrecision (S2LRVrO0zv3sdN): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandard (S2LRw7H5w8dnwS): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandard (S2LRWmV8bgLclv): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OPrecision (S2LRXMmEHlAvyl): interpretation1_scope: NULL has been replaced by ‘climate’
  - entityName (S2LRZ59Lzfy3fq): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CPrecision (S2LRZM4iyB8WUW): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRzmttC6etFZ): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandard (S2LRzTyOrm509D): interpretation1_scope: NULL has been replaced by ‘climate’

Version: 1.0.4

lastVersion: 1.0.3
curator: nicholas
timestamp: 2022-05-18 00:26:31 UTC
changes:
- Paleo Interpretation metadata:
  - hasAragoniteCorrectionComposite (S2LR09uNEAWatI): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OPrecision (S2LR4LeIt5GTnl): interpretation1_scope: ‘climate’ has been replaced by NULL
  - sisalSampleID (S2LR5rGrphEzs3): interpretation1_scope: ‘climate’ has been replaced by NULL
  - mineralogyComposite (S2LR5suPDSzezQ): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CPrecision (S2LR5xd8rvXaVG): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OStandardComposite (S2LR6lmnNebcSx): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CStandardComposite (S2LR7tQhtTG333): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CComposite (S2LR9rSXs12WrM): interpretation1_scope: ‘climate’ has been replaced by NULL
  - hasAragoniteCorrection (S2LRa0CueSKYhN): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OComposite (S2LRAc4LTUQ8qQ): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18O (S2LRAwkFTDejje): interpretation1_variableGroup: NULL has been replaced by ‘P’
  - hasAragoniteCorrection (S2LRBeUQ8raNbG): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OPrecisionComposite (S2LRCQuHPhIa4D): interpretation1_scope: ‘climate’ has been replaced by NULL
  - hasAragoniteCorrection (S2LRctczHzosGX): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OPrecision (S2LRCUNFyFxrCf): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CPrecisionComposite (S2LRd4gHFIae9i): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OStandard (S2LRD9gP2O7qg4): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18O (S2LRDg1jlgbIn8): interpretation1_variableGroup: NULL has been replaced by ‘P’
  - mineralogy (S2LRDQLw2BnWWi): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CStandard (S2LRHENNVj90YY): interpretation1_scope: ‘climate’ has been replaced by NULL
  - sisalSampleIDComposite (S2LRIGt8RgQu0l): interpretation1_scope: ‘climate’ has been replaced by NULL
  - depthComposite (S2LRkymurivwJC): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13C (S2LRpSzKt5ew3h): interpretation1_variableGroup: NULL has been replaced by ‘P’
  - d13C (S2LRT5MkdZPy5S): interpretation1_scope: ‘climate’ has been replaced by NULL
  - sisalSampleID (S2LRt9ciGpVJ1N): interpretation1_scope: ‘climate’ has been replaced by NULL
  - mineralogy (S2LRUduIkFLNRB): interpretation1_scope: ‘climate’ has been replaced by NULL
  - sisalSampleID (S2LRuNhRgJSXUk): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OStandard (S2LRuxFEbcJ2hJ): interpretation1_scope: ‘climate’ has been replaced by NULL
  - mineralogy (S2LRVOhRswecbD): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CPrecision (S2LRVrO0zv3sdN): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CStandard (S2LRw7H5w8dnwS): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OStandard (S2LRWmV8bgLclv): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18OPrecision (S2LRXMmEHlAvyl): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13C (S2LRYaQyDMwILZ): interpretation1_variableGroup: NULL has been replaced by ‘P’
  - entityName (S2LRZ59Lzfy3fq): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CPrecision (S2LRZM4iyB8WUW): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d18O (S2LRzmttC6etFZ): interpretation1_scope: ‘climate’ has been replaced by NULL
  - d13CStandard (S2LRzTyOrm509D): interpretation1_scope: ‘climate’ has been replaced by NULL
- Paleo Column metadata:
  - ageStalAgeUncertaintyHigh (S2LR3jI3H6oido): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageStalAgeUncertaintyHigh (S2LR3jI3H6oido): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - agecopRaUncertaintyLow (S2LR3uwikQ00Yb): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - agecopRaUncertaintyLow (S2LR3uwikQ00Yb): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBacon (S2LR5wj1UpfRj6): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBacon (S2LR5wj1UpfRj6): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - agelinInterp (S2LR70vqhhyP7k): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - agelinInterp (S2LR70vqhhyP7k): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - age (S2LR7rEYZolO0L): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - age (S2LR7rEYZolO0L): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBaconUncertaintyHigh (S2LR86CKAXVgU1): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBaconUncertaintyHigh (S2LR86CKAXVgU1): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - agecopRa (S2LR8sWQxVslcM): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - agecopRa (S2LR8sWQxVslcM): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBaconUncertaintyLow (S2LRA6RXGFeJ5x): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBaconUncertaintyLow (S2LRA6RXGFeJ5x): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBaconUncertaintyLow (S2LRaUNP4RQWS0): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBaconUncertaintyLow (S2LRaUNP4RQWS0): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - d18O (S2LRAwkFTDejje): paleoData_proxyLumps: NULL has been replaced by ‘isotope’
  - d18O (S2LRAwkFTDejje): paleoData_proxyLumpsOriginal: NULL has been replaced by ‘d18O’
  - agecopRaUncertaintyHigh (S2LRbM5jdDkjNo): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - agecopRaUncertaintyHigh (S2LRbM5jdDkjNo): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBaconUncertaintyHigh (S2LRCGT5qaJt9u): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBaconUncertaintyHigh (S2LRCGT5qaJt9u): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - d18O (S2LRDg1jlgbIn8): paleoData_proxyLumps: NULL has been replaced by ‘isotope’
  - d18O (S2LRDg1jlgbIn8): paleoData_proxyLumpsOriginal: NULL has been replaced by ‘d18O’
  - ageBchron (S2LRfJniTua2bs): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchron (S2LRfJniTua2bs): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBchronUncertaintyHigh (S2LRgnrjxckw0g): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchronUncertaintyHigh (S2LRgnrjxckw0g): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageStalAge (S2LRgZJ7h7MtVP): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageStalAge (S2LRgZJ7h7MtVP): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBacon (S2LRh0UstDxV7t): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBacon (S2LRh0UstDxV7t): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageStalAgeUncertaintyLow (S2LRi4eygntgd9): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageStalAgeUncertaintyLow (S2LRi4eygntgd9): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - age (S2LRia1aI3Z93v): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - age (S2LRia1aI3Z93v): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBchronUncertaintyHigh (S2LRjYcsIWmhgR): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchronUncertaintyHigh (S2LRjYcsIWmhgR): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBchronUncertaintyHigh (S2LRjZRw85WXLb): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchronUncertaintyHigh (S2LRjZRw85WXLb): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBaconUncertaintyHigh (S2LRl47f0OQOcn): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBaconUncertaintyHigh (S2LRl47f0OQOcn): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBchronUncertaintyHigh (S2LRLfV6UxULbX): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchronUncertaintyHigh (S2LRLfV6UxULbX): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBchronUncertaintyLow (S2LRNDkNbuNbrQ): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchronUncertaintyLow (S2LRNDkNbuNbrQ): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBaconUncertaintyLow (S2LRogf0R1H6Yr): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBaconUncertaintyLow (S2LRogf0R1H6Yr): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - agelinInterpUncertaintyLow (S2LRp3L24IDt3g): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - agelinInterpUncertaintyLow (S2LRp3L24IDt3g): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBchron (S2LRpM8VJdbYxF): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchron (S2LRpM8VJdbYxF): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - age (S2LRPNV2Tsopq8): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - age (S2LRPNV2Tsopq8): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - d13C (S2LRpSzKt5ew3h): paleoData_proxyLumps: NULL has been replaced by ‘isotope’
  - d13C (S2LRpSzKt5ew3h): paleoData_proxyLumpsOriginal: NULL has been replaced by ‘d13C’
  - ageBchronUncertaintyLow (S2LRQ2p2oBugz6): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchronUncertaintyLow (S2LRQ2p2oBugz6): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBaconUncertaintyLow (S2LRqCccjrvp6H): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBaconUncertaintyLow (S2LRqCccjrvp6H): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBchronUncertaintyLow (S2LRRGmvO6iGwS): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchronUncertaintyLow (S2LRRGmvO6iGwS): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - agelinInterpUncertaintyHigh (S2LRStc9RNOceR): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - agelinInterpUncertaintyHigh (S2LRStc9RNOceR): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBaconUncertaintyHigh (S2LRStTNzlcVwS): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBaconUncertaintyHigh (S2LRStTNzlcVwS): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBchron (S2LRv7vqWuHxHG): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchron (S2LRv7vqWuHxHG): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBchronUncertaintyLow (S2LRwgpzDptQCR): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchronUncertaintyLow (S2LRwgpzDptQCR): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBchron (S2LRx4BDMGC9pY): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBchron (S2LRx4BDMGC9pY): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - age (S2LRxs9wSDh7SM): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - age (S2LRxs9wSDh7SM): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - ageBacon (S2LRXsxEgPjRqr): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBacon (S2LRXsxEgPjRqr): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
  - d13C (S2LRYaQyDMwILZ): paleoData_proxyLumps: NULL has been replaced by ‘isotope’
  - d13C (S2LRYaQyDMwILZ): paleoData_proxyLumpsOriginal: NULL has been replaced by ‘d13C’
  - ageBacon (S2LRypHRqNY6zW): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
  - ageBacon (S2LRypHRqNY6zW): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
- Chron Column metadata:
  - age_type (S2LcR3C2ZgakVDS): chronData_variableName: ‘ageType’ has been replaced by ‘age_type’
  - age_type (S2LcR3C2ZgakVDS): chronData_variableNameOriginal: NULL has been replaced by ‘ageType’
  - age_type (S2LcRtQf9kkImdJ): chronData_variableName: ‘ageType’ has been replaced by ‘age_type’
  - age_type (S2LcRtQf9kkImdJ): chronData_variableNameOriginal: NULL has been replaced by ‘ageType’
  - age_type (S2LcRY4603aeXeU): chronData_variableName: ‘ageType’ has been replaced by ‘age_type’
  - age_type (S2LcRY4603aeXeU): chronData_variableNameOriginal: NULL has been replaced by ‘ageType’

Version: 1.0.3

lastVersion: 1.0.2
curator: nicholas
timestamp: 2021-10-05 21:39:59 UTC
changes:
- Geographic metadata:
  - geo_gcmdLocation: ‘Yemen’ has been replaced by ‘Asia>Western Asia>Middle East>Yemen’

Version: 1.0.2

lastVersion: 1.0.1
curator: nick
timestamp: 2021-03-17 01:53:59 UTC
changes:
- Base metadata:
  - archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Interpretation metadata:
  - d18O (S2LRAwkFTDejje): interpretation1_seasonalityGeneral: ‘Winter’ has been replaced by ‘winterOnly’
  - d18O (S2LRDg1jlgbIn8): interpretation1_seasonalityGeneral: ‘Winter’ has been replaced by ‘winterOnly’
  - d13C (S2LRpSzKt5ew3h): interpretation1_seasonalityGeneral: ‘Winter’ has been replaced by ‘winterOnly’
  - d13C (S2LRYaQyDMwILZ): interpretation1_seasonalityGeneral: ‘Winter’ has been replaced by ‘winterOnly’

Version: 1.0.1

lastVersion: 1.0.0
curator: nick
timestamp: 2021-01-12 02:29:00 UTC
changes:
- Geographic metadata:
  - geo_gcmdLocation: NULL has been replaced by ‘Yemen’
- Paleo Interpretation metadata:
  - hasAragoniteCorrectionComposite (S2LR09uNEAWatI): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OPrecision (S2LR4LeIt5GTnl): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleID (S2LR5rGrphEzs3): interpretation1_scope: NULL has been replaced by ‘climate’
  - mineralogyComposite (S2LR5suPDSzezQ): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CPrecision (S2LR5xd8rvXaVG): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandardComposite (S2LR6lmnNebcSx): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandardComposite (S2LR7tQhtTG333): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CComposite (S2LR9rSXs12WrM): interpretation1_scope: NULL has been replaced by ‘climate’
  - hasAragoniteCorrection (S2LRa0CueSKYhN): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OComposite (S2LRAc4LTUQ8qQ): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRAwkFTDejje): interpretation1_direction: NULL has been replaced by ‘negative’
  - d18O (S2LRAwkFTDejje): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRAwkFTDejje): interpretation1_seasonality: NULL has been replaced by ‘11,12,1,2,3’
  - d18O (S2LRAwkFTDejje): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Winter’
  - d18O (S2LRAwkFTDejje): interpretation1_variable: NULL has been replaced by ‘P’
  - d18O (S2LRAwkFTDejje): interpretation1_variableDetail: NULL has been replaced by ‘amount@surface’
  - hasAragoniteCorrection (S2LRBeUQ8raNbG): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OPrecisionComposite (S2LRCQuHPhIa4D): interpretation1_scope: NULL has been replaced by ‘climate’
  - hasAragoniteCorrection (S2LRctczHzosGX): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OPrecision (S2LRCUNFyFxrCf): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CPrecisionComposite (S2LRd4gHFIae9i): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandard (S2LRD9gP2O7qg4): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRDg1jlgbIn8): interpretation1_direction: NULL has been replaced by ‘negative’
  - d18O (S2LRDg1jlgbIn8): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRDg1jlgbIn8): interpretation1_seasonality: NULL has been replaced by ‘11,12,1,2,3’
  - d18O (S2LRDg1jlgbIn8): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Winter’
  - d18O (S2LRDg1jlgbIn8): interpretation1_variable: NULL has been replaced by ‘P’
  - d18O (S2LRDg1jlgbIn8): interpretation1_variableDetail: NULL has been replaced by ‘amount@surface’
  - mineralogy (S2LRDQLw2BnWWi): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandard (S2LRHENNVj90YY): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleIDComposite (S2LRIGt8RgQu0l): interpretation1_scope: NULL has been replaced by ‘climate’
  - depthComposite (S2LRkymurivwJC): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRpSzKt5ew3h): interpretation1_direction: NULL has been replaced by ‘negative’
  - d13C (S2LRpSzKt5ew3h): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRpSzKt5ew3h): interpretation1_seasonality: NULL has been replaced by ‘11,12,1,2,3’
  - d13C (S2LRpSzKt5ew3h): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Winter’
  - d13C (S2LRpSzKt5ew3h): interpretation1_variable: NULL has been replaced by ‘P’
  - d13C (S2LRpSzKt5ew3h): interpretation1_variableDetail: NULL has been replaced by ‘amount@surface’
  - d13C (S2LRT5MkdZPy5S): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleID (S2LRt9ciGpVJ1N): interpretation1_scope: NULL has been replaced by ‘climate’
  - mineralogy (S2LRUduIkFLNRB): interpretation1_scope: NULL has been replaced by ‘climate’
  - sisalSampleID (S2LRuNhRgJSXUk): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandard (S2LRuxFEbcJ2hJ): interpretation1_scope: NULL has been replaced by ‘climate’
  - mineralogy (S2LRVOhRswecbD): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CPrecision (S2LRVrO0zv3sdN): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandard (S2LRw7H5w8dnwS): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OStandard (S2LRWmV8bgLclv): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18OPrecision (S2LRXMmEHlAvyl): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRYaQyDMwILZ): interpretation1_direction: NULL has been replaced by ‘negative’
  - d13C (S2LRYaQyDMwILZ): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13C (S2LRYaQyDMwILZ): interpretation1_seasonality: NULL has been replaced by ‘11,12,1,2,3’
  - d13C (S2LRYaQyDMwILZ): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Winter’
  - d13C (S2LRYaQyDMwILZ): interpretation1_variable: NULL has been replaced by ‘P’
  - d13C (S2LRYaQyDMwILZ): interpretation1_variableDetail: NULL has been replaced by ‘amount@surface’
  - entityName (S2LRZ59Lzfy3fq): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CPrecision (S2LRZM4iyB8WUW): interpretation1_scope: NULL has been replaced by ‘climate’
  - d18O (S2LRzmttC6etFZ): interpretation1_scope: NULL has been replaced by ‘climate’
  - d13CStandard (S2LRzTyOrm509D): interpretation1_scope: NULL has been replaced by ‘climate’
- Paleo Column metadata:
  - d18O (S2LRAwkFTDejje): paleoData_notes: NULL has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d18O (S2LRAwkFTDejje): paleoData_proxy: NULL has been replaced by ‘d18O’
  - d18O (S2LRAwkFTDejje): paleoData_proxyDetail: NULL has been replaced by ‘calcite’
  - d18O (S2LRAwkFTDejje): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
  - d18O (S2LRAwkFTDejje): paleoData_QCCertification: NULL has been replaced by ‘CH’
  - d18O (S2LRAwkFTDejje): paleoData_QCnotes: NULL has been replaced by ‘STM6; “Combined interpretation of the stalagmites STM1 and STM6 provides the best precipitation reconstruction for eastern Socotra”; No composite: “STM6 site will be more strongly affected by kinetic effects, as its growth rate is considerably lower compared to the one at the STM1 site” (Van Rampelbergh et al., 2013)’
  - d18O (S2LRDg1jlgbIn8): paleoData_notes: NULL has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d18O (S2LRDg1jlgbIn8): paleoData_proxy: NULL has been replaced by ‘d18O’
  - d18O (S2LRDg1jlgbIn8): paleoData_proxyDetail: NULL has been replaced by ‘calcite’
  - d18O (S2LRDg1jlgbIn8): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
  - d18O (S2LRDg1jlgbIn8): paleoData_QCCertification: NULL has been replaced by ‘CH’
  - d18O (S2LRDg1jlgbIn8): paleoData_QCnotes: NULL has been replaced by ‘STM1; “Combined interpretation of the stalagmites STM1 and STM6 provides the best precipitation reconstruction for eastern Socotra”; No composite: “STM6 site will be more strongly affected by kinetic effects, as its growth rate is considerably lower compared to the one at the STM1 site” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRpSzKt5ew3h): paleoData_notes: NULL has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRpSzKt5ew3h): paleoData_proxy: NULL has been replaced by ‘d13C’
  - d13C (S2LRpSzKt5ew3h): paleoData_proxyDetail: NULL has been replaced by ‘calcite’
  - d13C (S2LRpSzKt5ew3h): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
  - d13C (S2LRpSzKt5ew3h): paleoData_QCCertification: NULL has been replaced by ‘CH’
  - d13C (S2LRpSzKt5ew3h): paleoData_QCnotes: NULL has been replaced by ‘STM1; “Combined interpretation of the stalagmites STM1 and STM6 provides the best precipitation reconstruction for eastern Socotra”; No composite: “STM6 site will be more strongly affected by kinetic effects, as its growth rate is considerably lower compared to the one at the STM1 site” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRT5MkdZPy5S): paleoData_QCCertification: NULL has been replaced by ‘CH’
  - d13C (S2LRT5MkdZPy5S): paleoData_QCnotes: NULL has been replaced by ‘HQ1; “For stalagmite Hq1, sampled near the entrance, kinetic effects are related to enhanced ventilation” (Van Rampelbergh et al., 2013). Hq1 sampled at entrance to cave. STM1 and STM6 sampled at end of the cave.’
  - d13C (S2LRYaQyDMwILZ): paleoData_notes: NULL has been replaced by ‘“d18O and d13C and Mg/Ca and Sr/Ca signals in the stalagmites reflect precipitation amounts brought by the northeast winds….the “amount effect”, describing the inverse relationship between the amount of precipitation and its oxygen isotopic composition, is mainly responsible for changes in rainwater d18O…higher d18O and d13C values will always occur during drier conditions…northeast monsoon starts in the first half of November…The spring transition occurs at the end of March” (Van Rampelbergh et al., 2013)’
  - d13C (S2LRYaQyDMwILZ): paleoData_proxy: NULL has been replaced by ‘d13C’
  - d13C (S2LRYaQyDMwILZ): paleoData_proxyDetail: NULL has been replaced by ‘calcite’
  - d13C (S2LRYaQyDMwILZ): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
  - d13C (S2LRYaQyDMwILZ): paleoData_QCCertification: NULL has been replaced by ‘CH’
  - d13C (S2LRYaQyDMwILZ): paleoData_QCnotes: NULL has been replaced by ‘STM6; “Combined interpretation of the stalagmites STM1 and STM6 provides the best precipitation reconstruction for eastern Socotra”; No composite: “STM6 site will be more strongly affected by kinetic effects, as its growth rate is considerably lower compared to the one at the STM1 site” (Van Rampelbergh et al., 2013)’
  - d18O (S2LRzmttC6etFZ): paleoData_QCCertification: NULL has been replaced by ‘CH’
  - d18O (S2LRzmttC6etFZ): paleoData_QCnotes: NULL has been replaced by ‘HQ1; “For stalagmite Hq1, sampled near the entrance, kinetic effects are related to enhanced ventilation” (Van Rampelbergh et al., 2013). Hq1 sampled at entrance to cave. STM1 and STM6 sampled at end of the cave.’

Version: 1.0.0

curator: nick
timestamp: 2020-09-29 14:29:18 UTC
notes: Created from SISALv2