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(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controlling the δ18O value\" (Kyoung-nam et al., 2017)'"], ["d18O (S2LRShfLt8O8RR): paleoData_QCCertification: 'CH' has been replaced by 'CH, CR'"] ], "Paleo Interpretation metadata": [ ["d18O (S2LRShfLt8O8RR): interpretation1_seasonalityGeneral: 'summerOnly' has been replaced by 'Summer'"] ] } }, { "version": "1.0.11", "lastVersion": "1.0.10", "curator": "nicholas", "timestamp": "2023-05-12 21:48:58 UTC", "changes": { "Paleo Column metadata": [ ["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amount of rain during the summer is the major factor controlling the δ18O value\" (Kyoung-nam et al., 2017)' has been replaced by '\"The Holocene variability in the East Asian summer monsoon (EASM) based on Speleothem δ18O...the δ18O value of precipitation on the KP is affected by the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)'"] ] } }, { "version": "1.0.10", "lastVersion": "1.0.9", "curator": "nicholas", "timestamp": "2023-03-24 22:23:40 UTC", "changes": { "Paleo Column metadata": [ ["d18O (S2LRShfLt8O8RR): paleoData_proxyGeneral: 'isotope' has been replaced by 'isotopic'"] ] } }, { "version": "1.0.9", "lastVersion": "1.0.8", "curator": "nicholas", "timestamp": "2023-02-13 23:37:18 UTC", "changes": { "Paleo Column metadata": [ ["d18O (S2LRShfLt8O8RR): paleoData_notes: '\"The Holocene variability in the East Asian summer monsoon 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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)'"] ] } }, { "version": "1.0.8", "lastVersion": "1.0.7", "curator": "nicholas", "timestamp": "2023-02-09 15:28:55 UTC", "notes": "Updated lipdverse database entry with a changed file.", "changes": { "Geographic metadata": [ ["geo_elevation: '' has been replaced by '250'"] ], "Paleo Column metadata": [ ["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 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["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'"] ], "Paleo Interpretation metadata": [ ["d18O (S2LRShfLt8O8RR): interpretation1_seasonality: '6,7,8' has been replaced by 'Jun-Aug'"], ["d18O (S2LRShfLt8O8RR): interpretation1_variable: 'P' has been replaced by 'precipitation'"] ] } }, { "version": "1.0.7", "lastVersion": "1.0.6", "curator": "nicholas", "timestamp": 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chronData_variableNameOriginal: '' has been replaced by 'ageType'"] ] } }, { "version": "1.0.4", "lastVersion": "1.0.3", "curator": "nicholas", "timestamp": "2021-11-17 02:05:24 UTC", "changes": { "Paleo Interpretation metadata": [ ["d18O (S2LRShfLt8O8RR): interpretation1_seasonality: 'summer' has been replaced by '6,7,8'"] ] } }, { "version": "1.0.3", "lastVersion": "1.0.2", "curator": "nicholas", "timestamp": "2021-10-05 21:38:16 UTC", "changes": { "Geographic metadata": [ ["geo_gcmdLocation: '' has been replaced by 'Asia>Eastern Asia>South Korea'"] ] } }, { "version": "1.0.2", "lastVersion": "1.0.1", "curator": "nick", "timestamp": "2021-03-17 01:51:47 UTC", "changes": { "Base metadata": [ ["archiveType: 'speleothem' has been replaced by 'Speleothem'"] ], "Paleo Column metadata": [ ["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)'"] ], "Paleo Interpretation metadata": [ ["d18O (S2LRShfLt8O8RR): interpretation1_seasonality: 'Summer' has been replaced by 'summer'"], ["d18O (S2LRShfLt8O8RR): interpretation1_seasonalityGeneral: 'Summer' has been replaced by 'summerOnly'"] ] } }, { "version": "1.0.1", "lastVersion": "1.0.0", "curator": "nick", "timestamp": "2021-01-12 02:28:25 UTC", "changes": { "Paleo Interpretation metadata": [ ["sisalSampleID (S2LRATXEOFZC8m): interpretation1_scope: '' has been replaced by 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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.'"] ] } }, { "version": "1.0.0", "curator": "nick", "timestamp": "2020-09-29 14:28:43 UTC", "notes": "Created from SISALv2" } ], "neotomaDatasetId": null, "pub": [ { "author": [ { "name": "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" } ], "citation": "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.", "year": 2017, "doi": "10.1038/s41598-017-15566-4", "journal": "Scientific Reports", "title": "1000-Year Quasi-Periodicity of Weak Monsoon Events in Temperate Northeast Asia since the Mid-Holocene", "citeKey": null, "issue": null, "pages": null, "volume": null } ], "geo": { "longitude": 128.58, "latitude": 37.27, "elevation": 250, "siteName": "Baeg-nyong cave", "sisalSiteId": 220, "geology": "limestone", "rockAge": "Ordovician", "hasMonitoring": "yes", "gcmdLocation": "Asia>Eastern Asia>South Korea" }, "@context": "context.jsonld" }