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by 'P.W. Williams and D.N.T. King and J.-X. Zhao and K.D. Collerson'"], ["pub1_journal: '' has been replaced by 'Earth and Planetary Science Letters'"], ["pub1_pages: '' has been replaced by '301--317'"], ["pub1_title: '' has been replaced by 'Late Pleistocene to Holocene composite speleothem 18O and 13C chronologies from South Island, New Zealand{\\textemdash}did a global Younger Dryas really exist?'"] ] } }, { "version": "1.0.11", "lastVersion": "1.0.10", "curator": "nicholas", "timestamp": "2023-03-29 20:06:40 UTC", "changes": { "Paleo Interpretation metadata": [ ["d13C (S2LRQTAjCiqPX4): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'"] ] } }, { "version": "1.0.10", "lastVersion": "1.0.9", "curator": "nicholas", "timestamp": "2023-02-13 23:59:29 UTC", "changes": { "Paleo Interpretation metadata": [ ["uncertaintyLow (S2LR3PcO1XVTD8): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyLow (S2LRIdyOEwv414): interpretation1_scope: '' has been replaced by 'climate'"], ["uncertaintyHigh 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It is clear that a large but unknown part of the variability of d18Oc in our records must be due to influences other than temperature...temperature appears to be the first-order driver of d18Oc change in our record,\" (Williams et al., 2015)'"], ["d18O (S2LRKAZbVB72KV): paleoData_proxy: '' has been replaced by 'd18O'"], ["d18O (S2LRKAZbVB72KV): paleoData_proxyDetail: '' has been replaced by 'calcite'"], ["d18O (S2LRKAZbVB72KV): paleoData_proxyGeneral: '' has been replaced by 'isotope'"], ["d18O (S2LRKAZbVB72KV): paleoData_QCCertification: '' has been replaced by 'CH'"], ["d18O (S2LRKAZbVB72KV): paleoData_QCnotes: '' has been replaced by 'Included in multi-site composite from WNA: \"SouthIsland.Williams.2005\"'"], ["d13C (S2LRQTAjCiqPX4): paleoData_notes: '' has been replaced by '\"Increased plant growth associated with climatic amelioration during the late- glacial early Holocene transition saw a marked decrease in d13Cc values [50], and wet conditions are also associated with reduced values...13C is interpreted as responding negatively to increases in atmospheric CO2 concentration, biological activity and precipitation amount.\" (Williams et al., 2005)'"], ["d13C (S2LRQTAjCiqPX4): paleoData_proxy: '' has been replaced by 'd13C'"], ["d13C (S2LRQTAjCiqPX4): paleoData_proxyDetail: '' has been replaced by 'calcite'"], ["d13C (S2LRQTAjCiqPX4): paleoData_proxyGeneral: '' has been replaced by 'isotope'"], ["d13C (S2LRQTAjCiqPX4): paleoData_QCCertification: '' has been replaced by 'CH'"], ["d13C (S2LRQTAjCiqPX4): paleoData_QCnotes: '' has been replaced by 'Included in multi-site composite from WNA: \"SouthIsland.Williams.2005\"'"] ] } }, { "version": "1.0.0", "curator": "nick", "timestamp": "2020-09-29 14:27:48 UTC", "notes": "Created from SISALv2" } ], "neotomaDatasetId": null, "pub": [ { "author": [ { "name": "P.W. Williams and D.N.T. King and J.-X. Zhao and K.D. Collerson" } ], "citation": "Williams, P. W., King, D. N. T., Zhao, J.-X. and Collerson, K. D.: Late Pleistocene to Holocene composite speleothem 18O and 13C chronologies from South Island, New Zealand<97>did a global Younger Dryas really exist?, Earth Planet. Sci. Lett., 230(3<96>4), 301<96>317, 2005.", "year": 2005, "doi": "10.1016/j.epsl.2004.10.024", "journal": "Earth and Planetary Science Letters", "pages": "301--317", "title": "Late Pleistocene to Holocene composite speleothem 18O and 13C chronologies from South Island, New Zealand{\\textemdash}did a global Younger Dryas really exist?", "citeKey": null, "issue": null, "volume": null } ], "geo": { "longitude": 171.4, "latitude": -42.1, "elevation": 95, "siteName": "Wazpretti cave", "sisalSiteId": 168, "geology": "limestone", "rockAge": "unknown", "hasMonitoring": "unknown", "gcmdLocation": "Australia/New Zealand>New Zealand" }, "@context": "context.jsonld" }