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
"the regional climate is characteristically wet in winter and nearly 60% of the annual precipitation occurs from November to March when the East Asian winter monsoon (EAWM) brings moisture from the Japan Sea warmed by the Tsushima Warm Current. Rainwater d18O values near the cave generally decrease with the precipitation amount, indicating an amount effect. The stalagmite d18O profile has had a concurrent trend with winter precipitation observed near the cave since 1924...These agreements suggest that the Fukugaguchi stalagmite d18O record reflects the EAWM intensity"
CR: winter "monsoon" record, so westerlies...
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
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
Initial 230Th/232Th activity ratio for the detrital correction
Initial 230Th/232Th activity ratio uncertainty for the detrital correction
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 FG01 (entity_id = 117): Information on whether it is actively forming could not be retrieved.
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 'Tomomi Sone and Akihiro Kano and Tomoyo Okumura and Kenji Kashiwagi and Masako Hori and Xiuyang Jiang and Chuan-Chou Shen'
pub1_journal: '' has been replaced by 'Quaternary Science Reviews'
pub1_pages: '' has been replaced by '150--160'
pub1_title: '' has been replaced by 'Holocene stalagmite oxygen isotopic record from the Japan Sea side of the Japanese Islands, as a new proxy of the East Asian winter monsoon'
d18O (S2LRjzNSFesB0T): paleoData_notes: '"the regional climate is characteristically wet in winter and nearly 60% of the annual precipitation occurs from November to March when the East Asian winter monsoon (EAWM) brings moisture from the Japan Sea warmed by the Tsushima Warm Current. Rainwater d18O values near the cave generally decrease with the precipitation amount, indicating an amount effect. The stalagmite d18O profile has had a concurrent trend with winter precipitation observed near the cave since 1924...These agreements suggest that the Fuku- gaguchi stalagmite d18O record reflects the EAWM intensity"' has been replaced by '"the regional climate is characteristically wet in winter and nearly 60% of the annual precipitation occurs from November to March when the East Asian winter monsoon (EAWM) brings moisture from the Japan Sea warmed by the Tsushima Warm Current. Rainwater d18O values near the cave generally decrease with the precipitation amount, indicating an amount effect. The stalagmite d18O profile has had a concurrent trend with winter precipitation observed near the cave since 1924...These agreements suggest that the Fukugaguchi stalagmite d18O record reflects the EAWM intensity"'
d18O (S2LRjzNSFesB0T): paleoData_QCCertification: 'CH' has been replaced by 'CH, CR'
d18O (S2LRjzNSFesB0T): paleoData_QCnotes: '' has been replaced by 'CR: winter "monsoon" record, so westerlies...'
d18O (S2LRjzNSFesB0T): interpretation1_seasonalityGeneral: 'winterOnly' has been replaced by 'Winter'
d18O (S2LRjzNSFesB0T): paleoData_proxyGeneral: 'isotope' has been replaced by 'isotopic'
Updated lipdverse database entry with a changed file.
geo_elevation: '' has been replaced by '170'
age (S2LR8X30vPDVou): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LR8X30vPDVou): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LR8X30vPDVou): paleoData_datum: '' has been replaced by '1950'
age (S2LR8X30vPDVou): paleoData_isPrimary: '' has been replaced by 'TRUE'
uncertainty (S2LRcFnDcpaSAJ): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LRcFnDcpaSAJ): paleoData_variableName: 'd18OPrecision' has been replaced by 'uncertainty'
uncertainty (S2LRcFnDcpaSAJ): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRcFnDcpaSAJ): paleoData_method: '' has been replaced by 'precision'
depth (S2LRGtjt7JFmbg): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
depth (S2LRGtjt7JFmbg): paleoData_units: 'depth_sample' has been replaced by 'mm'
depth (S2LRGtjt7JFmbg): paleoData_isPrimary: '' has been replaced by 'TRUE'
sampleID (S2LRKcasCyZIn8): paleoData_variableName: 'sisalSampleID' has been replaced by 'sampleID'
correction (S2LRsUeTypzylJ): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized'
correction (S2LRsUeTypzylJ): paleoData_variableName: 'hasAragoniteCorrection' has been replaced by 'correction'
correction (S2LRsUeTypzylJ): paleoData_method: '' has been replaced by 'aragonite correction'
uncertainty (S2LRTLgDOsy6Vu): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LRTLgDOsy6Vu): paleoData_variableName: 'd18OStandard' has been replaced by 'uncertainty'
uncertainty (S2LRTLgDOsy6Vu): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'
uncertainty (S2LRTLgDOsy6Vu): paleoData_method: '' has been replaced by 'standard'
d18O (S2LRjzNSFesB0T): interpretation1_seasonality: '11,12,1,2,3' has been replaced by 'Nov-Mar'
d18O (S2LRjzNSFesB0T): interpretation1_variable: 'P' has been replaced by 'precipitation'
geo_elevation: '170' has been replaced by ''
d18OPrecision (S2LRcFnDcpaSAJ): interpretation1_scope: '' has been replaced by 'climate'
mineralogy (S2LRHJvDuytaEN): interpretation1_scope: '' has been replaced by 'climate'
sisalSampleID (S2LRKcasCyZIn8): interpretation1_scope: '' has been replaced by 'climate'
hasAragoniteCorrection (S2LRsUeTypzylJ): interpretation1_scope: '' has been replaced by 'climate'
hasHiatus (S2LRtfOug1rtaG): interpretation1_scope: '' has been replaced by 'climate'
d18OStandard (S2LRTLgDOsy6Vu): interpretation1_scope: '' has been replaced by 'climate'
age (S2LR8X30vPDVou): paleoData_units: 'yr BP' has been replaced by 'BP'
age (S2LR8X30vPDVou): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
d18O (S2LRjzNSFesB0T): paleoData_proxyLumps: '' has been replaced by 'isotope'
d18O (S2LRjzNSFesB0T): paleoData_proxyLumpsOriginal: '' has been replaced by 'd18O'
d18OPrecision (S2LRcFnDcpaSAJ): interpretation1_scope: 'climate' has been replaced by ''
mineralogy (S2LRHJvDuytaEN): interpretation1_scope: 'climate' has been replaced by ''
d18O (S2LRjzNSFesB0T): interpretation1_variableGroup: '' has been replaced by 'P'
sisalSampleID (S2LRKcasCyZIn8): interpretation1_scope: 'climate' has been replaced by ''
hasAragoniteCorrection (S2LRsUeTypzylJ): interpretation1_scope: 'climate' has been replaced by ''
hasHiatus (S2LRtfOug1rtaG): interpretation1_scope: 'climate' has been replaced by ''
d18OStandard (S2LRTLgDOsy6Vu): interpretation1_scope: 'climate' has been replaced by ''
age_type (S2LcRbPkKo9iqlf): chronData_variableName: 'ageType' has been replaced by 'age_type'
age_type (S2LcRbPkKo9iqlf): chronData_variableNameOriginal: '' has been replaced by 'ageType'
geo_gcmdLocation: '' has been replaced by 'Asia>Eastern Asia>Japan'
archiveType: 'speleothem' has been replaced by 'Speleothem'
d18O (S2LRjzNSFesB0T): interpretation1_seasonalityGeneral: 'Winter' has been replaced by 'winterOnly'
d18O (S2LRjzNSFesB0T): interpretation1_direction: '' has been replaced by 'negative'
d18O (S2LRjzNSFesB0T): interpretation1_scope: '' has been replaced by 'climate'
d18O (S2LRjzNSFesB0T): interpretation1_seasonality: '' has been replaced by '11,12,1,2,3'
d18O (S2LRjzNSFesB0T): interpretation1_seasonalityGeneral: '' has been replaced by 'Winter'
d18O (S2LRjzNSFesB0T): interpretation1_variable: '' has been replaced by 'P'
d18O (S2LRjzNSFesB0T): interpretation1_variableDetail: '' has been replaced by 'amount@surface'
d18O (S2LRjzNSFesB0T): paleoData_notes: '' has been replaced by '"the regional climate is characteristically wet in winter and nearly 60% of the annual precipitation occurs from November to March when the East Asian winter monsoon (EAWM) brings moisture from the Japan Sea warmed by the Tsushima Warm Current. Rainwater d18O values near the cave generally decrease with the precipitation amount, indicating an amount effect. The stalagmite d18O profile has had a concurrent trend with winter precipitation observed near the cave since 1924...These agreements suggest that the Fuku- gaguchi stalagmite d18O record reflects the EAWM intensity"'
d18O (S2LRjzNSFesB0T): paleoData_proxy: '' has been replaced by 'd18O'
d18O (S2LRjzNSFesB0T): paleoData_proxyDetail: '' has been replaced by 'calcite'
d18O (S2LRjzNSFesB0T): paleoData_proxyGeneral: '' has been replaced by 'isotope'
d18O (S2LRjzNSFesB0T): paleoData_QCCertification: '' has been replaced by 'CH'
Tomomi Sone and Akihiro Kano and Tomoyo Okumura and Kenji Kashiwagi and Masako Hori and Xiuyang Jiang and Chuan-Chou Shen
Sone, T., Kano, A., Okumura, T., Kashiwagi, K., Hori, M., Jiang, X. and Shen, C.-C.: Holocene stalagmite oxygen isotopic record from the Japan Sea side of the Japanese Islands, as a new proxy of the East Asian winter monsoon, Quat. Sci. Rev., 75, 150<96>160, 2013.
Holocene stalagmite oxygen isotopic record from the Japan Sea side of the Japanese Islands, as a new proxy of the East Asian winter monsoon