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 two contrasting states are likely the manifestations of extreme rainfall events established on the basis of the imprints of anomalously high/low drip flow rates discerned in the fabrics of the discontinuities...Negative and positive δ18O excursions above and below the mean value of 3.3‰ (thin lines in Figures 3a and 3b) are interpreted as hydroclimate events representing elevated and re- duced annual rainfall amounts, respectively...the stalagmite δ18O time series integrate interannual water budget changes... We argue that the two con- trasting states of δ18O (Figure 3b) are primarily driven by rainfall variability a"
Laboratory precision on the d18O measurement
NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized
Laboratory precision on the d13C measurement
Original published calibrated age of the sample in years BP
NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
Indication of whether the date is used in the original age model (opposite of rejected)
DSSG-4 (entity_id = 112): U-series data only appear in graphic form in the original publication (Aharon et al.2012) not tabular so they are not included here. Cover thickness are from Aharon et al 2010 GCA paper. d18O and d13C precision are from Aharon et al 2017 QSR paper for the Alabama lab.
d18O (S2LRaRacqzp90y): interpretation1_variable: '((( null ))) P /// precipitation' has been replaced by 'precipitation'
d13C (S2LRNQC3XinWsZ): paleoData_primaryTimeseries: '' has been replaced by 'TRUE'
d18O (S2LRaRacqzp90y): paleoData_meetsHoloceneHydroclimateCriteria: '' has been replaced by 'TRUE'
d18O (S2LRaRacqzp90y): paleoData_primaryTimeseries: '' has been replaced by 'TRUE'
d18O (S2LRaRacqzp90y): interpretation1_variable: 'precipitation' has been replaced by '((( null ))) P /// precipitation'
uncertainty (S2LR1HXWABLCip): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (S2LR1HXWABLCip): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (S2LR1HXWABLCip): interpretation4_scope: '' has been replaced by 'isotope'
uncertainty (S2LR1HXWABLCip): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (S2LR1HXWABLCip): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (S2LR7qHEoHjtRz): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (S2LR7qHEoHjtRz): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (S2LR7qHEoHjtRz): interpretation4_scope: '' has been replaced by 'isotope'
uncertainty (S2LR7qHEoHjtRz): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (S2LR7qHEoHjtRz): interpretation6_scope: '' has been replaced by 'isotope'
d13C (S2LRNQC3XinWsZ): interpretation2_scope: '' has been replaced by 'climate'
d13C (S2LRNQC3XinWsZ): interpretation3_scope: '' has been replaced by 'climate'
d13C (S2LRNQC3XinWsZ): interpretation4_scope: '' has been replaced by 'isotope'
d13C (S2LRNQC3XinWsZ): interpretation5_scope: '' has been replaced by 'isotope'
d13C (S2LRNQC3XinWsZ): interpretation6_scope: '' has been replaced by 'isotope'
hasHiatus (S2LRQwUwRySE9a): interpretation2_scope: '' has been replaced by 'climate'
hasHiatus (S2LRQwUwRySE9a): interpretation3_scope: '' has been replaced by 'climate'
hasHiatus (S2LRQwUwRySE9a): interpretation4_scope: '' has been replaced by 'isotope'
hasHiatus (S2LRQwUwRySE9a): interpretation5_scope: '' has been replaced by 'isotope'
hasHiatus (S2LRQwUwRySE9a): interpretation6_scope: '' has been replaced by 'isotope'
d18O (S2LRaRacqzp90y): interpretation2_scope: '' has been replaced by 'climate'
d18O (S2LRaRacqzp90y): interpretation3_scope: '' has been replaced by 'climate'
d18O (S2LRaRacqzp90y): interpretation4_scope: '' has been replaced by 'isotope'
d18O (S2LRaRacqzp90y): interpretation5_scope: '' has been replaced by 'isotope'
d18O (S2LRaRacqzp90y): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (S2LRe161oaIALG): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (S2LRe161oaIALG): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (S2LRe161oaIALG): interpretation4_scope: '' has been replaced by 'isotope'
uncertainty (S2LRe161oaIALG): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (S2LRe161oaIALG): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (S2LRgi9Gs4DcQS): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (S2LRgi9Gs4DcQS): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (S2LRgi9Gs4DcQS): interpretation4_scope: '' has been replaced by 'isotope'
uncertainty (S2LRgi9Gs4DcQS): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (S2LRgi9Gs4DcQS): interpretation6_scope: '' has been replaced by 'isotope'
mineralogy (S2LRgyEbZlbtHy): interpretation2_scope: '' has been replaced by 'climate'
mineralogy (S2LRgyEbZlbtHy): interpretation3_scope: '' has been replaced by 'climate'
mineralogy (S2LRgyEbZlbtHy): interpretation4_scope: '' has been replaced by 'isotope'
mineralogy (S2LRgyEbZlbtHy): interpretation5_scope: '' has been replaced by 'isotope'
mineralogy (S2LRgyEbZlbtHy): interpretation6_scope: '' has been replaced by 'isotope'
thickness (S2LRpvsDMtsOIW): interpretation2_scope: '' has been replaced by 'climate'
thickness (S2LRpvsDMtsOIW): interpretation3_scope: '' has been replaced by 'climate'
thickness (S2LRpvsDMtsOIW): interpretation4_scope: '' has been replaced by 'isotope'
thickness (S2LRpvsDMtsOIW): interpretation5_scope: '' has been replaced by 'isotope'
thickness (S2LRpvsDMtsOIW): interpretation6_scope: '' has been replaced by 'isotope'
correction (S2LRrTHs1xFtEi): interpretation2_scope: '' has been replaced by 'climate'
correction (S2LRrTHs1xFtEi): interpretation3_scope: '' has been replaced by 'climate'
correction (S2LRrTHs1xFtEi): interpretation4_scope: '' has been replaced by 'isotope'
correction (S2LRrTHs1xFtEi): interpretation5_scope: '' has been replaced by 'isotope'
correction (S2LRrTHs1xFtEi): interpretation6_scope: '' has been replaced by 'isotope'
sampleID (S2LRsMwbEtPbKp): interpretation2_scope: '' has been replaced by 'climate'
sampleID (S2LRsMwbEtPbKp): interpretation3_scope: '' has been replaced by 'climate'
sampleID (S2LRsMwbEtPbKp): interpretation4_scope: '' has been replaced by 'isotope'
sampleID (S2LRsMwbEtPbKp): interpretation5_scope: '' has been replaced by 'isotope'
sampleID (S2LRsMwbEtPbKp): interpretation6_scope: '' has been replaced by 'isotope'
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 'Paul Aharon and David Aldridge and John Hellstrom'
pub1_pages: '' has been replaced by '35--42'
pub1_title: '' has been replaced by 'Rainfall Variability and the Rise and Collapse of the Mississippian Chiefdoms: Evidence From a Desoto Caverns Stalagmite'
d18O (S2LRaRacqzp90y): paleoData_notes: '((( "The two contrasting states are likely the manifestations of extreme rainfall events established on the basis of the imprints of anomalously high/low drip flow rates discerned in the fabrics of the discontinuities...Negative and positive ��18O excursions above and below the mean value of 3.3��� (thin lines in Figures 3a and 3b) are interpreted as hydroclimate events representing elevated and re- duced annual rainfall amounts, respectively...the stalagmite ��18O time series integrate interannual water budget changes... We argue that the two con- trasting states of ��18O (Figure 3b) are primarily driven by rainfall variability a" ))) "The two contrasting states are likely the manifestations of extreme rainfall events established on the basis of the imprints of anomalously high/low drip flow rates discerned in the fabrics of the discontinuities...Negative and positive δ18O excursions above and below the mean value of 3.3‰ (thin lines in Figures 3a and 3b) are interpreted as hydroclimate events representing elevated and re- duced annual rainfall amounts, respectively...the stalagmite δ18O time series integrate interannual water budget changes... We argue that the two con- trasting states of δ18O (Figure 3b) are primarily driven by rainfall variability a" /// "The two contrasting states are likely the manifestations of extreme rainfall events established on the basis of the imprints of anomalously high/low drip flow rates discerned in the fabrics of the discontinuities...Negative and positive δ18O excursions above and below the mean value of 3.3‰ (thin lines in Figures 3a and 3b) are interpreted as hydroclimate events representing elevated and re- duced annual rainfall amounts, respectively...the stalagmite δ18O time series integrate interannual water budget changes... We argue that the two con- trasting states of δ18O (Figure 3b) are primarily driven by rainfall variability a"' has been replaced by '"The two contrasting states are likely the manifestations of extreme rainfall events established on the basis of the imprints of anomalously high/low drip flow rates discerned in the fabrics of the discontinuities...Negative and positive δ18O excursions above and below the mean value of 3.3‰ (thin lines in Figures 3a and 3b) are interpreted as hydroclimate events representing elevated and re- duced annual rainfall amounts, respectively...the stalagmite δ18O time series integrate interannual water budget changes... We argue that the two con- trasting states of δ18O (Figure 3b) are primarily driven by rainfall variability a"'
d18O (S2LRaRacqzp90y): paleoData_notes: '"The two contrasting states are likely the manifestations of extreme rainfall events established on the basis of the imprints of anomalously high/low drip flow rates discerned in the fabrics of the discontinuities...Negative and positive δ18O excursions above and below the mean value of 3.3‰ (thin lines in Figures 3a and 3b) are interpreted as hydroclimate events representing elevated and re- duced annual rainfall amounts, respectively...the stalagmite δ18O time series integrate interannual water budget changes... We argue that the two con- trasting states of δ18O (Figure 3b) are primarily driven by rainfall variability a"' has been replaced by '((( "The two contrasting states are likely the manifestations of extreme rainfall events established on the basis of the imprints of anomalously high/low drip flow rates discerned in the fabrics of the discontinuities...Negative and positive ��18O excursions above and below the mean value of 3.3��� (thin lines in Figures 3a and 3b) are interpreted as hydroclimate events representing elevated and re- duced annual rainfall amounts, respectively...the stalagmite ��18O time series integrate interannual water budget changes... We argue that the two con- trasting states of ��18O (Figure 3b) are primarily driven by rainfall variability a" ))) "The two contrasting states are likely the manifestations of extreme rainfall events established on the basis of the imprints of anomalously high/low drip flow rates discerned in the fabrics of the discontinuities...Negative and positive δ18O excursions above and below the mean value of 3.3‰ (thin lines in Figures 3a and 3b) are interpreted as hydroclimate events representing elevated and re- duced annual rainfall amounts, respectively...the stalagmite δ18O time series integrate interannual water budget changes... We argue that the two con- trasting states of δ18O (Figure 3b) are primarily driven by rainfall variability a" /// "The two contrasting states are likely the manifestations of extreme rainfall events established on the basis of the imprints of anomalously high/low drip flow rates discerned in the fabrics of the discontinuities...Negative and positive δ18O excursions above and below the mean value of 3.3‰ (thin lines in Figures 3a and 3b) are interpreted as hydroclimate events representing elevated and re- duced annual rainfall amounts, respectively...the stalagmite δ18O time series integrate interannual water budget changes... We argue that the two con- trasting states of δ18O (Figure 3b) are primarily driven by rainfall variability a"'
Updated lipdverse database entry with a changed file.
geo_elevation: '' has been replaced by '150'
uncertainty (S2LR1HXWABLCip): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LR1HXWABLCip): paleoData_variableName: 'd18OPrecision' has been replaced by 'uncertainty'
uncertainty (S2LR1HXWABLCip): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'
uncertainty (S2LR1HXWABLCip): paleoData_method: '' has been replaced by 'precision'
uncertainty (S2LR7qHEoHjtRz): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LR7qHEoHjtRz): paleoData_variableName: 'd18OStandard' has been replaced by 'uncertainty'
uncertainty (S2LR7qHEoHjtRz): paleoData_measurementMaterial: '' has been replaced by 'd18O carbonate'
uncertainty (S2LR7qHEoHjtRz): paleoData_method: '' has been replaced by 'standard'
uncertainty (S2LRe161oaIALG): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LRe161oaIALG): paleoData_variableName: 'd13CStandard' has been replaced by 'uncertainty'
uncertainty (S2LRe161oaIALG): paleoData_measurementMaterial: '' has been replaced by 'd13C'
uncertainty (S2LRe161oaIALG): paleoData_method: '' has been replaced by 'standard'
uncertainty (S2LRgi9Gs4DcQS): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_method has been standardized'
uncertainty (S2LRgi9Gs4DcQS): paleoData_variableName: 'd13CPrecision' has been replaced by 'uncertainty'
uncertainty (S2LRgi9Gs4DcQS): paleoData_measurementMaterial: '' has been replaced by 'd13C'
uncertainty (S2LRgi9Gs4DcQS): paleoData_method: '' has been replaced by 'precision'
depth (S2LRPTUbojwuvg): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
depth (S2LRPTUbojwuvg): paleoData_units: 'depth_sample' has been replaced by 'mm'
depth (S2LRPTUbojwuvg): paleoData_isPrimary: '' has been replaced by 'TRUE'
age (S2LRpuSwnXUXLg): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (S2LRpuSwnXUXLg): paleoData_units: 'BP' has been replaced by 'yr BP'
age (S2LRpuSwnXUXLg): paleoData_datum: '' has been replaced by '1950'
age (S2LRpuSwnXUXLg): paleoData_isPrimary: '' has been replaced by 'TRUE'
correction (S2LRrTHs1xFtEi): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized'
correction (S2LRrTHs1xFtEi): paleoData_variableName: 'hasAragoniteCorrection' has been replaced by 'correction'
correction (S2LRrTHs1xFtEi): paleoData_method: '' has been replaced by 'aragonite correction'
sampleID (S2LRsMwbEtPbKp): paleoData_variableName: 'sisalSampleID' has been replaced by 'sampleID'
d18O (S2LRaRacqzp90y): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
d18O (S2LRaRacqzp90y): interpretation1_variable: 'P' has been replaced by 'precipitation'
geo_elevation: '150' has been replaced by ''
d18OPrecision (S2LR1HXWABLCip): interpretation1_scope: '' has been replaced by 'climate'
d18OStandard (S2LR7qHEoHjtRz): interpretation1_scope: '' has been replaced by 'climate'
d13CStandard (S2LRe161oaIALG): interpretation1_scope: '' has been replaced by 'climate'
d13CPrecision (S2LRgi9Gs4DcQS): interpretation1_scope: '' has been replaced by 'climate'
mineralogy (S2LRgyEbZlbtHy): interpretation1_scope: '' has been replaced by 'climate'
d13C (S2LRNQC3XinWsZ): interpretation1_scope: '' has been replaced by 'climate'
thickness (S2LRpvsDMtsOIW): interpretation1_scope: '' has been replaced by 'climate'
hasHiatus (S2LRQwUwRySE9a): interpretation1_scope: '' has been replaced by 'climate'
hasAragoniteCorrection (S2LRrTHs1xFtEi): interpretation1_scope: '' has been replaced by 'climate'
sisalSampleID (S2LRsMwbEtPbKp): interpretation1_scope: '' has been replaced by 'climate'
d18OPrecision (S2LR1HXWABLCip): interpretation1_scope: 'climate' has been replaced by ''
d18OStandard (S2LR7qHEoHjtRz): interpretation1_scope: 'climate' has been replaced by ''
d18O (S2LRaRacqzp90y): interpretation1_variableGroup: '' has been replaced by 'P'
d13CStandard (S2LRe161oaIALG): interpretation1_scope: 'climate' has been replaced by ''
d13CPrecision (S2LRgi9Gs4DcQS): interpretation1_scope: 'climate' has been replaced by ''
mineralogy (S2LRgyEbZlbtHy): interpretation1_scope: 'climate' has been replaced by ''
d13C (S2LRNQC3XinWsZ): interpretation1_scope: 'climate' has been replaced by ''
thickness (S2LRpvsDMtsOIW): interpretation1_scope: 'climate' has been replaced by ''
hasHiatus (S2LRQwUwRySE9a): interpretation1_scope: 'climate' has been replaced by ''
hasAragoniteCorrection (S2LRrTHs1xFtEi): interpretation1_scope: 'climate' has been replaced by ''
sisalSampleID (S2LRsMwbEtPbKp): interpretation1_scope: 'climate' has been replaced by ''
d18O (S2LRaRacqzp90y): paleoData_proxyLumps: '' has been replaced by 'isotope'
d18O (S2LRaRacqzp90y): paleoData_proxyLumpsOriginal: '' has been replaced by 'd18O'
d13C (S2LRNQC3XinWsZ): paleoData_proxyLumps: '' has been replaced by 'isotope'
d13C (S2LRNQC3XinWsZ): paleoData_proxyLumpsOriginal: '' has been replaced by 'd13C'
age (S2LRpuSwnXUXLg): paleoData_units: 'yr BP' has been replaced by 'BP'
age (S2LRpuSwnXUXLg): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
age_type (S2LcR8b7NaUhCxE): chronData_variableName: 'ageType' has been replaced by 'age_type'
age_type (S2LcR8b7NaUhCxE): chronData_variableNameOriginal: '' has been replaced by 'ageType'
geo_gcmdLocation: '' has been replaced by 'North America>United States Of America>Alabama'
archiveType: 'speleothem' has been replaced by 'Speleothem'
d18O (S2LRaRacqzp90y): interpretation1_seasonality: '' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,458'
d18O (S2LRaRacqzp90y): interpretation1_direction: '' has been replaced by 'negative'
d18O (S2LRaRacqzp90y): interpretation1_scope: '' has been replaced by 'climate'
d18O (S2LRaRacqzp90y): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
d18O (S2LRaRacqzp90y): interpretation1_variable: '' has been replaced by 'P'
d18O (S2LRaRacqzp90y): interpretation1_variableDetail: '' has been replaced by '@surface'
d18O (S2LRaRacqzp90y): paleoData_notes: '' has been replaced by '"The two contrasting states are likely the manifestations of extreme rainfall events established on the basis of the imprints of anomalously high/low drip flow rates discerned in the fabrics of the discontinuities...Negative and positive δ18O excursions above and below the mean value of 3.3‰ (thin lines in Figures 3a and 3b) are interpreted as hydroclimate events representing elevated and re- duced annual rainfall amounts, respectively...the stalagmite δ18O time series integrate interannual water budget changes... We argue that the two con- trasting states of δ18O (Figure 3b) are primarily driven by rainfall variability a"'
d18O (S2LRaRacqzp90y): paleoData_proxy: '' has been replaced by 'd18O'
d18O (S2LRaRacqzp90y): paleoData_proxyDetail: '' has been replaced by 'aragonite'
d18O (S2LRaRacqzp90y): paleoData_proxyGeneral: '' has been replaced by 'isotope'
d18O (S2LRaRacqzp90y): paleoData_QCCertification: '' has been replaced by 'CH'
d13C (S2LRNQC3XinWsZ): paleoData_proxy: '' has been replaced by 'd13C'
d13C (S2LRNQC3XinWsZ): paleoData_proxyDetail: '' has been replaced by 'aragonite'
d13C (S2LRNQC3XinWsZ): paleoData_proxyGeneral: '' has been replaced by 'isotope'
Paul Aharon and David Aldridge and John Hellstrom
Aharon, P., Aldridge, D. and Hellstrom, J.: Rainfall Variability and the Rise and Collapse of the Mississippian Chiefdoms: Evidence From a Desoto Caverns Stalagmite, in Climates, Landscapes, and Civilizations, pp. 35<96>42, American Geophysical Union., 2013.
Rainfall Variability and the Rise and Collapse of the Mississippian Chiefdoms: Evidence From a Desoto Caverns Stalagmite
North America>United States Of America>Alabama