Refers to the unique identifier for the sample (as given in sample table)
NA; paleoData_isPrimary has been standardized
Description of the mineralogy of the sample
Indication of whether the isotope measurements have been corrected in aragonite samples
NA; paleoData_method has been standardized
((( null ))) "The Holocene variability in the East Asian summer monsoon (EASM) based on speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017) /// "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem d18O...the d18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the d18O value" (Kyoung-nam et al., 2017)
SISAL Note: Entity BN-1 (entity_id = 468): Depths for U/Th dates are not available.
Laboratory precision on the d18O measurement
NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized
Original published calibrated age of the sample in years BP
NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
The laboratory number of the dated sample
Uncorrected age of the dated sample in years
Positive uncertainty of the uncorrected age of the dated sample in years
Negative uncertainty of the uncorrected age of the dated sample in years
Indication of whether the date is used in the original age model (opposite of rejected)
238U 2-sigma uncertainty of dated sample in ppb
232Th content of the dated sample in ppt
232Th 2-sigma uncertainty of the dated sample in ppt
230Th/232Th activity ratio of the dated sample
230Th/232Th activity ratio 2-sigma uncertainty of the dated sample
230Th/238U activity ratio of the dated sample
230Th/238U activity ratio 2-sigma uncertainty of the dated sample
234U/238U activity ratio of the dated sample
234U/238U activity ratio 2-sigma uncertainty of the dated sample
Description of the half-life used for 230Th and 234U for U/Th samples
Corrected age of the dated sample in years
Positive uncertainty of corrected age of the dated sample in years
Negative uncertainty of corrected age of the dated sample in years
Entity BN-1 (entity_id = 468): Depths for U/Th dates are not available.
d18O (S2LRShfLt8O8RR): paleoData_proxyGeneral: '((( null ))) isotope /// isotopic' has been replaced by 'isotopic'
d18O (S2LRShfLt8O8RR): paleoData_QCCertification: '((( null ))) CH /// CH, CR' has been replaced by 'CH, CR'
d18O (S2LRShfLt8O8RR): interpretation1_seasonality: '((( null ))) Summer /// Jun-Aug' has been replaced by 'Jun-Aug'
d18O (S2LRShfLt8O8RR): interpretation1_variable: '((( null ))) P /// precipitation' has been replaced by 'precipitation'
d18O (S2LRShfLt8O8RR): paleoData_notes: '"The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem d18O...the d18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the d18O value" (Kyoung-nam et al., 2017)' has been replaced by '((( null ))) "The Holocene variability in the East Asian summer monsoon (EASM) based on speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017) /// "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem d18O...the d18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the d18O value" (Kyoung-nam et al., 2017)'
d18O (S2LRShfLt8O8RR): paleoData_proxyGeneral: 'isotopic' has been replaced by '((( null ))) isotope /// isotopic'
d18O (S2LRShfLt8O8RR): paleoData_QCCertification: 'CH, CR' has been replaced by '((( null ))) CH /// CH, CR'
d18O (S2LRShfLt8O8RR): paleoData_meetsHoloceneHydroclimateCriteria: '' has been replaced by 'TRUE'
d18O (S2LRShfLt8O8RR): paleoData_primaryTimeseries: '' has been replaced by 'TRUE'
d18O (S2LRShfLt8O8RR): interpretation1_seasonality: 'Jun-Aug' has been replaced by '((( null ))) Summer /// Jun-Aug'
d18O (S2LRShfLt8O8RR): interpretation1_variable: 'precipitation' has been replaced by '((( null ))) P /// precipitation'
sampleID (S2LRATXEOFZC8m): interpretation2_scope: '' has been replaced by 'climate'
sampleID (S2LRATXEOFZC8m): interpretation3_scope: '' has been replaced by 'climate'
sampleID (S2LRATXEOFZC8m): interpretation4_scope: '' has been replaced by 'isotope'
sampleID (S2LRATXEOFZC8m): interpretation5_scope: '' has been replaced by 'isotope'
sampleID (S2LRATXEOFZC8m): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (S2LRPCxfRth88a): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (S2LRPCxfRth88a): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (S2LRPCxfRth88a): interpretation4_scope: '' has been replaced by 'isotope'
uncertainty (S2LRPCxfRth88a): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (S2LRPCxfRth88a): interpretation6_scope: '' has been replaced by 'isotope'
d18O (S2LRShfLt8O8RR): interpretation2_scope: '' has been replaced by 'climate'
d18O (S2LRShfLt8O8RR): interpretation3_scope: '' has been replaced by 'climate'
d18O (S2LRShfLt8O8RR): interpretation4_scope: '' has been replaced by 'isotope'
d18O (S2LRShfLt8O8RR): interpretation5_scope: '' has been replaced by 'isotope'
d18O (S2LRShfLt8O8RR): interpretation6_scope: '' has been replaced by 'isotope'
correction (S2LReJwIPZAMzF): interpretation2_scope: '' has been replaced by 'climate'
correction (S2LReJwIPZAMzF): interpretation3_scope: '' has been replaced by 'climate'
correction (S2LReJwIPZAMzF): interpretation4_scope: '' has been replaced by 'isotope'
correction (S2LReJwIPZAMzF): interpretation5_scope: '' has been replaced by 'isotope'
correction (S2LReJwIPZAMzF): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (S2LRsNaJzs9trQ): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (S2LRsNaJzs9trQ): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (S2LRsNaJzs9trQ): interpretation4_scope: '' has been replaced by 'isotope'
uncertainty (S2LRsNaJzs9trQ): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (S2LRsNaJzs9trQ): interpretation6_scope: '' has been replaced by 'isotope'
mineralogy (S2LRzuJIo4qN8X): interpretation2_scope: '' has been replaced by 'climate'
mineralogy (S2LRzuJIo4qN8X): interpretation3_scope: '' has been replaced by 'climate'
mineralogy (S2LRzuJIo4qN8X): interpretation4_scope: '' has been replaced by 'isotope'
mineralogy (S2LRzuJIo4qN8X): interpretation5_scope: '' has been replaced by 'isotope'
mineralogy (S2LRzuJIo4qN8X): interpretation6_scope: '' has been replaced by 'isotope'
originalDataUrl: 'http://dx.doi.org/10.17864/1947.256' has been replaced by 'https://doi.org/10.17864/1947.256'
pub1_author: '' has been replaced by 'Kyoung-nam Jo and Sangheon Yi and Jin-Yong Lee and Kyung Sik Woo and Hai Cheng and Lawrence R. Edwards and Sang-Tae Kim'
pub1_journal: '' has been replaced by 'Scientific Reports'
pub1_title: '' has been replaced by '1000-Year Quasi-Periodicity of Weak Monsoon Events in Temperate Northeast Asia since the Mid-Holocene'
d18O (S2LRShfLt8O8RR): paleoData_notes: '((( ((( "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem ��18O...the ��18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the ��18O value" (Kyoung-nam et al., 2017) ))) "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017) /// "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017) ))) "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem d18O...the d18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the d18O value" (Kyoung-nam et al., 2017) /// "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017)' has been replaced by '"The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem d18O...the d18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the d18O value" (Kyoung-nam et al., 2017)'
d18O (S2LRShfLt8O8RR): paleoData_notes: '"The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017)' has been replaced by '((( ((( "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem ��18O...the ��18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the ��18O value" (Kyoung-nam et al., 2017) ))) "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017) /// "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017) ))) "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem d18O...the d18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the d18O value" (Kyoung-nam et al., 2017) /// "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017)'
d18O (S2LRShfLt8O8RR): paleoData_QCCertification: 'CH' has been replaced by 'CH, CR'
d18O (S2LRShfLt8O8RR): interpretation1_seasonalityGeneral: 'summerOnly' has been replaced by 'Summer'
d18O (S2LRShfLt8O8RR): paleoData_notes: '((( "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem ��18O...the ��18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the ��18O value" (Kyoung-nam et al., 2017) ))) "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017) /// "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017)' has been replaced by '"The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017)'
d18O (S2LRShfLt8O8RR): paleoData_proxyGeneral: 'isotope' has been replaced by 'isotopic'
d18O (S2LRShfLt8O8RR): paleoData_notes: '"The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017)' has been replaced by '((( "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem ��18O...the ��18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the ��18O value" (Kyoung-nam et al., 2017) ))) "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017) /// "The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017)'
Updated lipdverse database entry with a changed file.
geo_elevation: '' has been replaced by '250'
sampleID (S2LRATXEOFZC8m): paleoData_variableName: 'sisalSampleID' has been replaced by 'sampleID'
correction (S2LReJwIPZAMzF): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized'
correction (S2LReJwIPZAMzF): paleoData_variableName: 'hasAragoniteCorrection' has been replaced by 'correction'
correction (S2LReJwIPZAMzF): paleoData_method: '' has been replaced by 'aragonite correction'
depth (S2LRh0BisGZl81): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
depth (S2LRh0BisGZl81): paleoData_units: 'depth_sample' has been replaced by 'mm'
depth (S2LRh0BisGZl81): paleoData_isPrimary: '' has been replaced by 'TRUE'
age (S2LRkAG6NZmcdb): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LRkAG6NZmcdb): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LRkAG6NZmcdb): paleoData_datum: '' has been replaced by '1950'
age (S2LRkAG6NZmcdb): paleoData_isPrimary: '' has been replaced by 'TRUE'
uncertainty (S2LRPCxfRth88a): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LRPCxfRth88a): paleoData_variableName: 'd18OStandard' has been replaced by 'uncertainty'
uncertainty (S2LRPCxfRth88a): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRPCxfRth88a): paleoData_method: '' has been replaced by 'standard'
uncertainty (S2LRsNaJzs9trQ): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LRsNaJzs9trQ): paleoData_variableName: 'd18OPrecision' has been replaced by 'uncertainty'
uncertainty (S2LRsNaJzs9trQ): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRsNaJzs9trQ): paleoData_method: '' has been replaced by 'precision'
d18O (S2LRShfLt8O8RR): interpretation1_seasonality: '6,7,8' has been replaced by 'Jun-Aug'
d18O (S2LRShfLt8O8RR): interpretation1_variable: 'P' has been replaced by 'precipitation'
geo_elevation: '250' has been replaced by ''
sisalSampleID (S2LRATXEOFZC8m): interpretation1_scope: '' has been replaced by 'climate'
hasAragoniteCorrection (S2LReJwIPZAMzF): interpretation1_scope: '' has been replaced by 'climate'
d18OStandard (S2LRPCxfRth88a): interpretation1_scope: '' has been replaced by 'climate'
d18OPrecision (S2LRsNaJzs9trQ): interpretation1_scope: '' has been replaced by 'climate'
mineralogy (S2LRzuJIo4qN8X): interpretation1_scope: '' has been replaced by 'climate'
sisalSampleID (S2LRATXEOFZC8m): interpretation1_scope: 'climate' has been replaced by ''
hasAragoniteCorrection (S2LReJwIPZAMzF): interpretation1_scope: 'climate' has been replaced by ''
d18OStandard (S2LRPCxfRth88a): interpretation1_scope: 'climate' has been replaced by ''
d18O (S2LRShfLt8O8RR): interpretation1_variableGroup: '' has been replaced by 'P'
d18OPrecision (S2LRsNaJzs9trQ): interpretation1_scope: 'climate' has been replaced by ''
mineralogy (S2LRzuJIo4qN8X): interpretation1_scope: 'climate' has been replaced by ''
age (S2LRkAG6NZmcdb): paleoData_units: 'yr BP' has been replaced by 'BP'
age (S2LRkAG6NZmcdb): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
d18O (S2LRShfLt8O8RR): paleoData_proxyLumps: '' has been replaced by 'isotope'
d18O (S2LRShfLt8O8RR): paleoData_proxyLumpsOriginal: '' has been replaced by 'd18O'
age_type (S2LcRg71IpRfLZr): chronData_variableName: 'ageType' has been replaced by 'age_type'
age_type (S2LcRg71IpRfLZr): chronData_variableNameOriginal: '' has been replaced by 'ageType'
d18O (S2LRShfLt8O8RR): interpretation1_seasonality: 'summer' has been replaced by '6,7,8'
geo_gcmdLocation: '' has been replaced by 'Asia>Eastern Asia>South Korea'
archiveType: 'speleothem' has been replaced by 'Speleothem'
d18O (S2LRShfLt8O8RR): paleoData_notes: '"The Holocene variability in the East Asian summer monsoon (EASM) based on speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017)' has been replaced by '"The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017)'
d18O (S2LRShfLt8O8RR): interpretation1_seasonality: 'Summer' has been replaced by 'summer'
d18O (S2LRShfLt8O8RR): interpretation1_seasonalityGeneral: 'Summer' has been replaced by 'summerOnly'
d18O (S2LRShfLt8O8RR): interpretation1_direction: '' has been replaced by 'negative'
d18O (S2LRShfLt8O8RR): interpretation1_scope: '' has been replaced by 'climate'
d18O (S2LRShfLt8O8RR): interpretation1_seasonality: '' has been replaced by 'Summer'
d18O (S2LRShfLt8O8RR): interpretation1_seasonalityGeneral: '' has been replaced by 'Summer'
d18O (S2LRShfLt8O8RR): interpretation1_variable: '' has been replaced by 'P'
d18O (S2LRShfLt8O8RR): interpretation1_variableDetail: '' has been replaced by 'amount@surface'
d18O (S2LRShfLt8O8RR): paleoData_notes: '' has been replaced by '"The Holocene variability in the East Asian summer monsoon (EASM) based on speleothem δ18O...the δ18O value of precipitation on the KP is affected by the amount of rainfall in summer and the temperature in winter...the amount of rain during the summer is the major factor controlling the δ18O value" (Kyoung-nam et al., 2017)'
d18O (S2LRShfLt8O8RR): paleoData_proxy: '' has been replaced by 'd18O'
d18O (S2LRShfLt8O8RR): paleoData_proxyDetail: '' has been replaced by 'calcite'
d18O (S2LRShfLt8O8RR): paleoData_proxyGeneral: '' has been replaced by 'isotope'
d18O (S2LRShfLt8O8RR): paleoData_QCCertification: '' has been replaced by 'CH'
d18O (S2LRShfLt8O8RR): paleoData_QCnotes: '' has been replaced by 'SISAL Note: Entity BN-1 (entity_id = 468): Depths for U/Th dates are not available.'
Kyoung-nam Jo and Sangheon Yi and Jin-Yong Lee and Kyung Sik Woo and Hai Cheng and Lawrence R. Edwards and Sang-Tae Kim
Jo, K., Yi, S., Lee, J.-Y., Woo, K. S., Cheng, H., Edwards, L. R. and Kim, S.-T.: 1000-Year Quasi-Periodicity of Weak Monsoon Events in Temperate Northeast Asia since the Mid-Holocene, Sci. Rep., 7(1), 15196, 2017.
1000-Year Quasi-Periodicity of Weak Monsoon Events in Temperate Northeast Asia since the Mid-Holocene