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paleoData_longName: '' has been replaced by 'sisalSampleID'"], ["uncertaintyLow (S2LRxNqZaWA0fk): paleoData_method: '' has been replaced by 'linInterp'"], ["correction (S2LRyE9cb9aWud): paleoData_variableName: 'hasAragoniteCorrection' has been replaced by 'correction'"], ["correction (S2LRyE9cb9aWud): paleoData_longName: '' has been replaced by 'sisalSampleID'"], ["correction (S2LRyE9cb9aWud): paleoData_method: '' has been replaced by 'aragonite correction'"], ["depth (S2LRyKCLdH7ACb): paleoData_units: 'depth_sample' has been replaced by 'mm'"], ["depth (S2LRyKCLdH7ACb): paleoData_longName: '' has been replaced by 'sisalSampleID'"], ["uncertainty (S2LRzvIQkRpSd6): paleoData_variableName: 'd13CPrecision' has been replaced by 'uncertainty'"], ["uncertainty (S2LRzvIQkRpSd6): paleoData_isPrimary: '' has been replaced by 'FALSE'"], ["uncertainty (S2LRzvIQkRpSd6): paleoData_longName: '' has been replaced by 'sisalSampleID'"], ["uncertainty (S2LRzvIQkRpSd6): paleoData_measurementMaterial: '' has been replaced by 'd13C'"], ["uncertainty (S2LRzvIQkRpSd6): paleoData_method: '' has been replaced by 'precision'"] ], "Paleo Interpretation metadata": [ ["d18O (S2LR28keOuR7aP): interpretation1_variable: 'Mixed' has been replaced by 'deleteMe'"], ["d13C (S2LRSyMkE2lxgX): interpretation1_variable: 'Mixed' has been replaced by 'deleteMe'"] ] } }, { "version": "1.0.1", "lastVersion": "1.0.0", "curator": "nick", "timestamp": "2021-01-12 02:28:36 UTC", "changes": { "Paleo Interpretation metadata": [ ["d13CStandardComposite (S2LR0TWASqRjDr): interpretation1_scope: '' has been replaced by 'climate'"], ["d18OStandard (S2LR1djdIw9dCc): interpretation1_scope: '' has been replaced by 'climate'"], ["d18OPrecision (S2LR1Y2cFkoYEr): interpretation1_scope: '' has been replaced by 'climate'"], ["thickness (S2LR27fefTg1v3): interpretation1_scope: '' has been replaced by 'climate'"], ["d18OComposite (S2LR28keOuR7aP): interpretation1_scope: '' has been replaced by 'climate'"], ["d18OComposite 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been replaced by 'climate'"], ["d13C (S2LRooepVaPEdA): interpretation1_scope: '' has been replaced by 'climate'"], ["entityName (S2LRPPucpvGH7T): interpretation1_scope: '' has been replaced by 'climate'"], ["mineralogy (S2LRpyBfY3hCz1): interpretation1_scope: '' has been replaced by 'climate'"], ["sisalSampleID (S2LRRghRc44rWQ): interpretation1_scope: '' has been replaced by 'climate'"], ["mineralogy (S2LRSEoExacyyc): interpretation1_scope: '' has been replaced by 'climate'"], ["d13CComposite (S2LRSyMkE2lxgX): interpretation1_scope: '' has been replaced by 'climate'"], ["d13CComposite (S2LRSyMkE2lxgX): interpretation1_variable: '' has been replaced by 'Mixed'"], ["mineralogyComposite (S2LRtw5M8q0Dft): interpretation1_scope: '' has been replaced by 'climate'"], ["d13CStandard (S2LRUbdlH5O9ir): interpretation1_scope: '' has been replaced by 'climate'"], ["hasAragoniteCorrectionComposite (S2LRUbXObcyOBC): interpretation1_scope: '' has been replaced by 'climate'"], ["d18OPrecision (S2LRvbOUjwR3i1): interpretation1_scope: '' has been replaced by 'climate'"], ["d13CStandard (S2LRvGkjw7D9E0): interpretation1_scope: '' has been replaced by 'climate'"], ["sisalSampleIDComposite (S2LRVHQYRsN5vf): interpretation1_scope: '' has been replaced by 'climate'"], ["d18O (S2LRw0pHnMlZGo): interpretation1_scope: '' has been replaced by 'climate'"], ["thicknessComposite (S2LRWbpT0s2vy1): interpretation1_scope: '' has been replaced by 'climate'"], ["depthComposite (S2LRxBvuUq6IAs): interpretation1_scope: '' has been replaced by 'climate'"], ["hasAragoniteCorrection (S2LRyE9cb9aWud): interpretation1_scope: '' has been replaced by 'climate'"], ["d13CPrecision (S2LRzvIQkRpSd6): interpretation1_scope: '' has been replaced by 'climate'"] ], "Paleo Column metadata": [ ["thickness (S2LR27fefTg1v3): paleoData_QCCertification: '' has been replaced by 'CH'"], ["thickness (S2LR27fefTg1v3): paleoData_QCnotes: '' has been replaced by 'Denniston et al. (2013) plots both stals along a single timeseries. No overlap. \"The Cape Range stalagmite time series thus reveals for the first time the millennial-scale sensitivity of the moisture source variations in northwestern Australia, a result that has implications for precipitation dynamics across much of the continent.\"'"], ["d18OComposite (S2LR28keOuR7aP): paleoData_notes: '' has been replaced by '\"The origins of these stalagmite oxygen isotopic shifts do not appear to reflect increases in mean annual temperature but are tied here largely to changes in the d18O values of precipitation and may reflect a more southerly influence of the Indo-Australian summer monsoon at this time...A shift to lower stalagmite calcite d18O values coincident with HS1 likely reflects changing moisture or moisture source that could involve the positioning of the southern hemi- sphere westerlies, an increase in the strength/and or location of the IASM trough, tropical cyclone activity, and/or northwest cloud band activity\" (Denniston et al., 2013)'"], ["d18OComposite (S2LR28keOuR7aP): paleoData_proxy: '' has been replaced by 'd18O'"], ["d18OComposite (S2LR28keOuR7aP): paleoData_proxyDetail: '' has been replaced by 'calcite'"], ["d18OComposite (S2LR28keOuR7aP): paleoData_proxyGeneral: '' has been replaced by 'isotope'"], ["d18OComposite (S2LR28keOuR7aP): paleoData_QCCertification: '' has been replaced by 'CH'"], ["d18OComposite (S2LR28keOuR7aP): paleoData_QCnotes: '' has been replaced by 'Denniston et al. (2013) plots both stals along a single timeseries. No overlap. \"The Cape Range stalagmite time series thus reveals for the first time the millennial-scale sensitivity of the moisture source variations in northwestern Australia, a result that has implications for precipitation dynamics across much of the continent.\"'"], ["d18O (S2LRi9O9ddeKX5): paleoData_QCCertification: '' has been replaced by 'CH'"], ["d18O (S2LRi9O9ddeKX5): paleoData_QCnotes: '' has been replaced by 'Denniston et al. (2013) plots both stals along a single timeseries. No overlap. \"The Cape Range stalagmite time series thus reveals for the first time the millennial-scale sensitivity of the moisture source variations in northwestern Australia, a result that has implications for precipitation dynamics across much of the continent.\"'"], ["thickness (S2LRlpB8NoAYsX): paleoData_QCCertification: '' has been replaced by 'CH'"], ["thickness (S2LRlpB8NoAYsX): paleoData_QCnotes: '' has been replaced by 'Denniston et al. (2013) plots both stals along a single timeseries. No overlap. \"The Cape Range stalagmite time series thus reveals for the first time the millennial-scale sensitivity of the moisture source variations in northwestern Australia, a result that has implications for precipitation dynamics across much of the continent.\"'"], ["d13C (S2LRm9c9nwZ1WF): paleoData_QCCertification: '' has been replaced by 'CH'"], ["d13C (S2LRm9c9nwZ1WF): paleoData_QCnotes: '' has been replaced by 'Denniston et al. (2013) plots both stals along a single timeseries. No overlap. \"The Cape Range stalagmite time series thus reveals for the first time the millennial-scale sensitivity of the moisture source variations in northwestern Australia, a result that has implications for precipitation dynamics across much of the continent.\"'"], ["d13C (S2LRooepVaPEdA): paleoData_QCCertification: '' has been replaced by 'CH'"], ["d13C (S2LRooepVaPEdA): paleoData_QCnotes: '' has been replaced by 'Denniston et al. (2013) plots both stals along a single timeseries. No overlap. \"The Cape Range stalagmite time series thus reveals for the first time the millennial-scale sensitivity of the moisture source variations in northwestern Australia, a result that has implications for precipitation dynamics across much of the continent.\"'"], ["d13CComposite (S2LRSyMkE2lxgX): paleoData_notes: '' has been replaced by '\"Stalagmite d13C values at 6 ka are lower than expected for the modern C4-dominated vegetation and thin soils of Cape Range, suggesting that a more C3-rich envi- ronment was present during elevated rainfall conditions...Decreased d13C values in the early Holocene are a response to increased effective moisture, tempera- ture and possibly also atmospheric carbon dioxide levels. A middle Holocene minimum in stalagmite d13C and d18O values may reflect increased IASM rainfall, as recorded by regional pollen evidence.\" (Denniston et al., 2013)'"], ["d13CComposite (S2LRSyMkE2lxgX): paleoData_proxy: '' has been replaced by 'd13C'"], ["d13CComposite (S2LRSyMkE2lxgX): paleoData_proxyDetail: '' has been replaced by 'calcite'"], ["d13CComposite (S2LRSyMkE2lxgX): paleoData_proxyGeneral: '' has been replaced by 'isotope'"], ["d13CComposite (S2LRSyMkE2lxgX): paleoData_QCCertification: '' has been replaced by 'CH'"], ["d13CComposite (S2LRSyMkE2lxgX): paleoData_QCnotes: '' has been replaced by 'Denniston et al. (2013) plots both stals along a single timeseries. No overlap. \"The Cape Range stalagmite time series thus reveals for the first time the millennial-scale sensitivity of the moisture source variations in northwestern Australia, a result that has implications for precipitation dynamics across much of the continent.\"'"], ["d18O (S2LRw0pHnMlZGo): paleoData_QCCertification: '' has been replaced by 'CH'"], ["d18O (S2LRw0pHnMlZGo): paleoData_QCnotes: '' has been replaced by 'Denniston et al. (2013) plots both stals along a single timeseries. No overlap. \"The Cape Range stalagmite time series thus reveals for the first time the millennial-scale sensitivity of the moisture source variations in northwestern Australia, a result that has implications for precipitation dynamics across much of the continent.\"'"], ["thicknessComposite (S2LRWbpT0s2vy1): paleoData_QCCertification: '' has been replaced by 'CH'"], ["thicknessComposite (S2LRWbpT0s2vy1): paleoData_QCnotes: '' has been replaced by 'Denniston et al. (2013) plots both stals along a single timeseries. No overlap. \"The Cape Range stalagmite time series thus reveals for the first time the millennial-scale sensitivity of the moisture source variations in northwestern Australia, a result that has implications for precipitation dynamics across much of the continent.\"'"] ] } }, { "version": "1.0.0", "curator": "nick", "timestamp": "2020-09-29 14:28:37 UTC", "notes": "Created from SISALv2" } ], "neotomaDatasetId": null, "pub": [ { "citation": "Denniston, R. F., Asmerom, Y., Lachniet, M., Polyak, V. J., Hope, P., An, N., Rodzinyak, K. and Humphreys, W. F.: A Last Glacial Maximum through middle Holocene stalagmite record of coastal Western Australia climate, Quat. Sci. Rev., 77, 101<96>112, 2013.", "doi": "10.1016/j.quascirev.2013.07.002", "year": 2013, "author": [ { "name": null } ], "citeKey": null, "issue": null, "journal": null, "pages": null, "title": null, "volume": null } ], "geo": { "longitude": 113.9, "latitude": -22.1, "elevation": 100, "geology": "limestone", "hasMonitoring": "no", "rockAge": "unknown", "sisalSiteId": 214, "siteName": "Cave C126", "gcmdLocation": null }, "@context": "context.jsonld" }