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This update is based on COPRA (Breitenbach et al., 2012) using a PCH spline.", "lipdverseLink": "https://lipdverse.org/data/kIqa3TTGgcnZyKo7W6D3/1_0_12", "maxYear": 9284.1656, "minYear": 1690.0776, "agesPerKyr": 0, "hasDepth": 1, "nUniqueAges": 6, "nUniqueGoodAges": 0, "nUniqueOtherAges": 0, "otherAgesPerKyr": "0", "lipdVersion": 1.3, "datasetVersion": "1.0.12", "changelog": [ { "version": "1.0.12", "lastVersion": "1.0.11", "curator": "nicholas", "timestamp": "2023-08-10 22:44:49 UTC", "changes": { "Base metadata": [ ["originalDataUrl: 'http://dx.doi.org/10.17864/1947.256' has been replaced by 'https://doi.org/10.17864/1947.256'"] ], "Publication metadata": [ ["pub1_author: '' has been replaced by 'Andrew Lorrey and Paul Williams and Jim Salinger and Tim Martin and Jonathan Palmer and Anthony Fowler and Jian-xin Zhao and Helen Neil'"], ["pub1_journal: '' has been replaced by 'Quaternary International'"], ["pub1_pages: '' has been replaced by '52--75'"], ["pub1_title: '' has been replaced by 'Speleothem stable isotope records interpreted within a multi-proxy framework and implications for New Zealand palaeoclimate reconstruction'"] ] } }, { "version": "1.0.11", "lastVersion": "1.0.10", "curator": "nicholas", "timestamp": "2023-03-29 19:43:17 UTC", "changes": { "Paleo Interpretation metadata": [ ["d13C (S2LRGkmEev8vMC): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'"] ] } }, { "version": "1.0.10", "lastVersion": "1.0.9", "curator": "nicholas", "timestamp": "2023-02-13 23:39:04 UTC", "changes": { "Paleo Interpretation metadata": [ ["uncertaintyHigh (S2LRcaL3UOBX1e): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyHigh (S2LRD0xJcGerum): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyHigh (S2LRGc2Lm1XO0Y): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyLow (S2LRgQ1PCgHDV9): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyLow 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chronData_variableName: 'ageType' has been replaced by 'age_type'"], ["age_type (S2LcRKzsDpwnXGo): chronData_variableNameOriginal: '' has been replaced by 'ageType'"] ] } }, { "version": "1.0.5", "lastVersion": "1.0.4", "curator": "nicholas", "timestamp": "2021-11-17 02:05:44 UTC", "changes": { "Paleo Interpretation metadata": [ ["d13C (S2LRGkmEev8vMC): interpretation1_variable: 'M' has been replaced by 'P-E'"] ] } }, { "version": "1.0.4", "lastVersion": "1.0.3", "curator": "nicholas", "timestamp": "2021-10-05 21:38:36 UTC", "changes": { "Geographic metadata": [ ["geo_gcmdLocation: '' has been replaced by 'Australia/New Zealand>New Zealand'"] ] } }, { "version": "1.0.3", "lastVersion": "1.0.2", "curator": "nick", "timestamp": "2021-04-13 02:31:14 UTC", "changes": { "Paleo Interpretation metadata": [ ["d13C (S2LRGkmEev8vMC): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,46' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,12'"] ] } }, { "version": "1.0.2", "lastVersion": "1.0.1", "curator": "nick", "timestamp": "2021-03-17 01:52:07 UTC", "changes": { "Base metadata": [ ["archiveType: 'speleothem' has been replaced by 'Speleothem'"] ], "Paleo Column metadata": [ ["d13C (S2LRGkmEev8vMC): paleoData_notes: '\"master speleothem d13C records, variations tracked changes in relative regional precipitation...This comparison suggests the WSI master speleothem d13C record contains a strong regional palaeo- precipitation signal... less-negative d13C values in the WSI master speleothem record coincide with dry periods\" (Lorrey et al., 2008)' has been replaced by '\"master Speleothem d13C records, variations tracked changes in relative regional precipitation...This comparison suggests the WSI master Speleothem d13C record contains a strong regional palaeo- precipitation signal... less-negative d13C values in the WSI master Speleothem record coincide with dry periods\" (Lorrey et al., 2008)'"], ["d13C (S2LRGkmEev8vMC): paleoData_QCnotes: '\"The WSI master speleothem record is a composite chronology composed of data from four speleothems sourced from Aurora, Calcite, Doubtful Xanadu, and Waiau \" (Lorrey et al., 2008). However, no data identified for this composite. Locations far enough away from each other to keep seperate' has been replaced by '\"The WSI master Speleothem record is a composite chronology composed of data from four Speleothems sourced from Aurora, Calcite, Doubtful Xanadu, and Waiau \" (Lorrey et al., 2008). However, no data identified for this composite. Locations far enough away from each other to keep seperate'"], ["d18O (S2LRGljwzGXa5q): paleoData_notes: '\"The d18O master speleothem record for both regions varied with temperature change... more negative d18O values coinciding with cool periods and positive d18O excursions with warm periods...The identification of d18O fluctuations in the WSI master speleothem record that are in agreement with other palaeo-temperature proxies from WSI confirms that the d18O signal in this record can be employed as a palaeo-temperature proxy\" (Lorrey et al., 2008)' has been replaced by '\"The d18O master Speleothem record for both regions varied with temperature change... more negative d18O values coinciding with cool periods and positive d18O excursions with warm periods...The identification of d18O fluctuations in the WSI master Speleothem record that are in agreement with other palaeo-temperature proxies from WSI confirms that the d18O signal in this record can be employed as a palaeo-temperature proxy\" (Lorrey et al., 2008)'"], ["d18O (S2LRGljwzGXa5q): paleoData_QCnotes: '\"The WSI master speleothem record is a composite chronology composed of data from four speleothems sourced from Aurora, Calcite, Doubtful Xanadu, and Waiau \" (Lorrey et al., 2008). However, no data identified for this composite. Locations far enough away from each other to keep seperate.' has been replaced by '\"The WSI master Speleothem record is a composite chronology composed of data from four Speleothems sourced from Aurora, Calcite, Doubtful Xanadu, and Waiau \" (Lorrey et al., 2008). However, no data identified for this composite. Locations far enough away from each other to keep seperate.'"] ], "Paleo Interpretation metadata": [ ["d13C (S2LRGkmEev8vMC): interpretation1_seasonality: '' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,46'"] ] } }, { "version": "1.0.1", "lastVersion": "1.0.0", "curator": "nick", "timestamp": "2021-01-12 02:28:35 UTC", "changes": { "Paleo Interpretation metadata": [ ["sisalSampleID (S2LR08iKTu7Gnk): interpretation1_scope: '' has been replaced by 'climate'"], ["hasAragoniteCorrection (S2LRaGUxNOzgVR): interpretation1_scope: '' has been replaced by 'climate'"], ["d18OStandard (S2LRArwQZOkcRQ): interpretation1_scope: '' has been replaced by 'climate'"], ["d13C (S2LRGkmEev8vMC): interpretation1_direction: '' has been replaced by 'negative'"], ["d13C (S2LRGkmEev8vMC): interpretation1_scope: '' has been replaced by 'climate'"], ["d13C (S2LRGkmEev8vMC): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'"], ["d13C (S2LRGkmEev8vMC): interpretation1_variable: '' has been replaced by 'M'"], ["d13C (S2LRGkmEev8vMC): interpretation1_variableDetail: '' has been replaced by '@surface'"], ["d18O (S2LRGljwzGXa5q): interpretation1_direction: '' has been replaced by 'positive'"], ["d18O (S2LRGljwzGXa5q): interpretation1_scope: '' has been replaced by 'climate'"], ["d18O (S2LRGljwzGXa5q): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'"], ["d18O (S2LRGljwzGXa5q): interpretation1_variable: '' has been replaced by 'T'"], ["d18O (S2LRGljwzGXa5q): interpretation1_variableDetail: '' has been replaced by '@surface'"], ["d13CStandard (S2LRMn5r5uZt3u): interpretation1_scope: '' has been replaced by 'climate'"], ["d13CPrecision (S2LRsFDdyJe2hm): interpretation1_scope: '' has been replaced by 'climate'"], ["mineralogy (S2LRw4CVS4b94V): interpretation1_scope: '' has been replaced by 'climate'"], ["d18OPrecision (S2LRxixdA3bt1O): interpretation1_scope: '' has been replaced by 'climate'"] ], "Paleo Column metadata": [ ["d13C (S2LRGkmEev8vMC): paleoData_notes: '' has been replaced by '\"master speleothem d13C records, variations tracked changes in relative regional precipitation...This comparison suggests the WSI master speleothem d13C record contains a strong regional palaeo- precipitation signal... less-negative d13C values in the WSI master speleothem record coincide with dry periods\" (Lorrey et al., 2008)'"], ["d13C (S2LRGkmEev8vMC): paleoData_proxy: '' has been replaced by 'd13C'"], ["d13C (S2LRGkmEev8vMC): paleoData_proxyDetail: '' has been replaced by 'calcite'"], ["d13C (S2LRGkmEev8vMC): paleoData_proxyGeneral: '' has been replaced by 'isotope'"], ["d13C (S2LRGkmEev8vMC): paleoData_QCCertification: '' has been replaced by 'CH'"], ["d13C (S2LRGkmEev8vMC): paleoData_QCnotes: '' has been replaced by '\"The WSI master speleothem record is a composite chronology composed of data from four speleothems sourced from Aurora, Calcite, Doubtful Xanadu, and Waiau \" (Lorrey et al., 2008). However, no data identified for this composite. Locations far enough away from each other to keep seperate'"], ["d18O (S2LRGljwzGXa5q): paleoData_notes: '' has been replaced by '\"The d18O master speleothem record for both regions varied with temperature change... more negative d18O values coinciding with cool periods and positive d18O excursions with warm periods...The identification of d18O fluctuations in the WSI master speleothem record that are in agreement with other palaeo-temperature proxies from WSI confirms that the d18O signal in this record can be employed as a palaeo-temperature proxy\" (Lorrey et al., 2008)'"], ["d18O (S2LRGljwzGXa5q): paleoData_proxy: '' has been replaced by 'd18O'"], ["d18O (S2LRGljwzGXa5q): paleoData_proxyDetail: '' has been replaced by 'calcite'"], ["d18O (S2LRGljwzGXa5q): paleoData_proxyGeneral: '' has been replaced by 'isotope'"], ["d18O (S2LRGljwzGXa5q): paleoData_QCCertification: '' has been replaced by 'CH'"], ["d18O (S2LRGljwzGXa5q): paleoData_QCnotes: '' has been replaced by '\"The WSI master speleothem record is a composite chronology composed of data from four speleothems sourced from Aurora, Calcite, Doubtful Xanadu, and Waiau \" (Lorrey et al., 2008). However, no data identified for this composite. Locations far enough away from each other to keep seperate.'"] ] } }, { "version": "1.0.0", "curator": "nick", "timestamp": "2020-09-29 14:27:41 UTC", "notes": "Created from SISALv2" } ], "neotomaDatasetId": null, "pub": [ { "author": [ { "name": "Andrew Lorrey and Paul Williams and Jim Salinger and Tim Martin and Jonathan Palmer and Anthony Fowler and Jian-xin Zhao and Helen Neil" } ], "citation": "Lorrey, A., Williams, P., Salinger, J., Martin, T., Palmer, J., Fowler, A., Zhao, J. and Neil, H.: Speleothem stable isotope records interpreted within a multi-proxy framework and implications for New Zealand palaeoclimate reconstruction, Quat. Int., 187(1), 52<96>75, 2008.", "year": 2008, "doi": "10.1016/j.quaint.2007.09.039", "journal": "Quaternary International", "pages": "52--75", "title": "Speleothem stable isotope records interpreted within a multi-proxy framework and implications for New Zealand palaeoclimate reconstruction", "issue": null, "volume": null } ], "geo": { "longitude": 167.74, "latitude": -46.02, "elevation": 1025, "siteName": "Calcite cave (Mt Luxmore, Fiordland)", "sisalSiteId": 162, "geology": "limestone", "rockAge": "Oligocene", "hasMonitoring": "unknown", "gcmdLocation": "Australia/New Zealand>New Zealand" }, "@context": "context.jsonld" }