Version history for 09jkQGxNrQNHdhWMIpXM - GeoB7702-3.Castaneda.2016

Version: 1.0.19

lastVersion: 1.0.18
curator: nicholas
timestamp: 2023-08-10 22:51:55 UTC
changes:
- Paleo Interpretation metadata:
  - d2H (LPDf79af672): interpretation1_variable: ‘((( Mixed ))) deleteMe /// precipitation’ has been replaced by ‘precipitation’

Version: 1.0.18

lastVersion: 1.0.17
curator: nicholas
timestamp: 2023-07-05 00:40:16 UTC
changes:
- Publication metadata:
  - pub1_doi: NULL has been replaced by ‘10.1016/j.epsl.2015.12.014’
- Paleo Interpretation metadata:
  - d2H (LPDf79af672): interpretation1_variable: ‘precipitation’ has been replaced by ‘((( Mixed ))) deleteMe /// precipitation’

Version: 1.0.17

lastVersion: 1.0.16
curator: nicholas
timestamp: 2023-05-31 20:38:33 UTC
changes:
- Paleo Interpretation metadata:
  - d2H (LPDf79af672): interpretation1_seasonality: ‘((( null ))) Annual /// Summer’ has been replaced by ‘Annual’
- Paleo Column metadata:
  - Fe/Al (WEB5427a58b): paleoData_notes: ‘((( ((( “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_units updated; paleoData_proxyGeneral has been standardized ))) “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized /// “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized ))) “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP signaling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,” /// “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized’ has been replaced by ‘“Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized’

Version: 1.0.16

lastVersion: 1.0.15
curator: nicholas
timestamp: 2023-05-30 15:48:43 UTC
changes:
- Paleo Column metadata:
  - d13C (LPD17ad91b2): paleoData_QCCertification: NULL has been replaced by ‘CR’
  - pH (LPD277e0621): paleoData_notes: NULL has been replaced by ‘“Soil pH reconstructed from the CBT index. Lower (more acidic) values are indicative of wetter conditions.” “The CBT Index provides an independent hydroclimate proxy and can be used as a relative indicator of wet versus arid conditions because higher precipitation leads to lower (more acidic) pH values. Overall trends in the CBT-derived soil pH record (Fig. 4h) track the dDwax record (Fig. 4f).”’
  - pH (LPD277e0621): paleoData_proxy: ‘pH’ has been replaced by ‘CBT’
  - pH (LPD277e0621): paleoData_proxyGeneral: ‘biophysical’ has been replaced by ‘biomarker’
  - pH (LPD277e0621): paleoData_QCCertification: NULL has been replaced by ‘CR’
  - d2H (LPDf79af672): paleoData_notes: NULL has been replaced by ‘“dDwax has been interpreted to mainly reflect variability in precipitation amount in tropical Africa”’
  - d2H (LPDf79af672): paleoData_QCCertification: ‘CH’ has been replaced by ‘CH, CR’
  - d2H (LPDf79af672): paleoData_QCnotes: ‘“While δDwax is often interpreted to reflect precipitation amount in the African tropics, our data suggest that shifting moisture sources, related to migrations of the tropical rainbelt and CAB, also contributed to isotopic variability. As δDwax may behave non-linearly due to the additional influence of changing moisture sources, care should be taken when interpreting δDwax records from areas falling under the influence of isotopically distinct moisture sources.” (Castaneda et al., 2016)’ has been replaced by ‘“While dDwax is often interpreted to reflect precipitation amount in the African tropics, our data suggest that shifting moisture sources, related to migrations of the tropical rainbelt and CAB, also contributed to isotopic variability. As dDwax may behave non-linearly due to the additional influence of changing moisture sources, care should be taken when interpreting dDwax records from areas falling under the influence of isotopically distinct moisture sources.” (Castaneda et al., 2016)’
  - MS (WEB279cd5b2): paleoData_notes: ‘“A final hydroclimate proxy is provided by the MS record. Bulk soil MS provides a proxy for rainfall based on the premise that MS reflects the degree of pedogenesis, which increases with increasing rainfall (Balsam et al., 2011). Furthermore, it has been proposed that MS provides a quantitative rainfall proxy when appropriate statistical models are developed and calibrated for a specific re- gion, necessary because relationships between MS and rainfall may be either linear or non-linear (Maher and Possolo, 2013). We find that the GeoB7702-3 MS record is in close agreement with the δDwax record, supporting its use as a rainfall proxy”’ has been replaced by ‘“A final hydroclimate proxy is provided by the MS record. Bulk soil MS provides a proxy for rainfall based on the premise that MS reflects the degree of pedogenesis, which increases with increasing rainfall (Balsam et al., 2011). Furthermore, it has been proposed that MS provides a quantitative rainfall proxy when appropriate statistical models are developed and calibrated for a specific re- gion, necessary because relationships between MS and rainfall may be either linear or non-linear (Maher and Possolo, 2013). We find that the GeoB7702-3 MS record is in close agreement with the dDwax record, supporting its use as a rainfall proxy”’
  - MS (WEB279cd5b2): paleoData_proxyGeneral: ‘biophysical’ has been replaced by ‘sedimentology’
  - MS (WEB279cd5b2): paleoData_QCCertification: NULL has been replaced by ‘CR’
  - Fe/Al (WEB5427a58b): paleoData_notes: ‘“Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized’ has been replaced by ‘((( ((( “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_units updated; paleoData_proxyGeneral has been standardized ))) “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized /// “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized ))) “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP signaling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,” /// “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized’
  - Fe/Al (WEB5427a58b): paleoData_QCCertification: NULL has been replaced by ‘CR’
  - Ti/Ca (WEBc666b28d): paleoData_notes: ‘NA; paleoData_proxyGeneral has been standardized’ has been replaced by ‘“Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP signaling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”’
  - Ti/Ca (WEBc666b28d): paleoData_QCCertification: NULL has been replaced by ‘CR’
- Paleo Interpretation metadata:
  - d2H (LPDf79af672): interpretation1_seasonality: ‘Summer’ has been replaced by ‘((( null ))) Annual /// Summer’
  - d2H (LPDf79af672): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’
  - d2H (LPDf79af672): interpretation1_variableDetail: ‘monsoon’ has been replaced by ‘amount@surface’
  - Fe/Al (WEB5427a58b): interpretation1_variableDetail: ‘discharge’ has been replaced by ‘runnoff@catchment’
  - Ti/Ca (WEBc666b28d): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’
  - Ti/Ca (WEBc666b28d): interpretation1_variableDetail: ‘discharge’ has been replaced by ‘runnoff@catchment’

Version: 1.0.15

lastVersion: 1.0.14
curator: nicholas
timestamp: 2023-05-25 17:42:53 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
- Geographic metadata:
  - geo_elevation: NULL has been replaced by ‘-562’

Version: 1.0.14

lastVersion: 1.0.13
curator: nicholas
timestamp: 2023-05-12 21:55:07 UTC
changes:
- Paleo Column metadata:
  - Fe/Al (WEB5427a58b): paleoData_notes: ‘((( “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_units updated; paleoData_proxyGeneral has been standardized ))) “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized /// “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized’ has been replaced by ‘“Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized’

Version: 1.0.13

lastVersion: 1.0.12
curator: nicholas
timestamp: 2023-05-09 22:31:27 UTC
changes:
- Paleo Interpretation metadata:
  - d13C (LPD17ad91b2): interpretation1_seasonality: ‘((( ((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual ))) Annual /// Annual’ has been replaced by ‘Annual’
  - pH (LPD277e0621): interpretation1_seasonality: ‘((( ((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual ))) Annual /// Annual’ has been replaced by ‘Annual’
  - d2H (LPDf79af672): interpretation1_seasonality: NULL has been replaced by ‘Summer’
  - d2H (LPDf79af672): interpretation1_variable: NULL has been replaced by ‘precipitation’

Version: 1.0.12

lastVersion: 1.0.11
curator: nicholas
timestamp: 2023-03-29 19:47:35 UTC
changes:
- Paleo Interpretation metadata:
  - d13C (LPD17ad91b2): interpretation1_seasonality: ‘Annual’ has been replaced by ‘((( ((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual ))) Annual /// Annual’
  - pH (LPD277e0621): interpretation1_seasonality: ‘Annual’ has been replaced by ‘((( ((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual ))) Annual /// Annual’

Version: 1.0.11

lastVersion: 1.0.10
curator: nicholas
timestamp: 2023-03-24 22:24:25 UTC
changes:
- Paleo Column metadata:
  - d13C (LPD17ad91b2): paleoData_proxyGeneral: ‘isotope’ has been replaced by ‘isotopic’
  - temperature (LPD6a7b432f): paleoData_proxyGeneral: ‘other biomarker’ has been replaced by ‘biomarker’
  - d2H (LPDf79af672): paleoData_proxyGeneral: ‘isotope’ has been replaced by ‘isotopic’
- Paleo Interpretation metadata:
  - d13C (LPD17ad91b2): interpretation1_seasonality: ‘((( ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual ))) Annual /// ((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’ has been replaced by ‘Annual’
  - d13C (LPD17ad91b2): interpretation1_variable: ‘P-E’ has been replaced by ‘effectivePrecipitation’
  - pH (LPD277e0621): interpretation1_seasonality: ‘((( ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual ))) Annual /// ((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’ has been replaced by ‘Annual’
  - pH (LPD277e0621): interpretation1_variable: ‘P-E’ has been replaced by ‘effectivePrecipitation’

Version: 1.0.10

lastVersion: 1.0.9
curator: nicholas
timestamp: 2023-02-16 23:25:01 UTC
changes:
- Paleo Interpretation metadata:
  - d13C (LPD17ad91b2): interpretation1_seasonality: ‘((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’ has been replaced by ‘((( ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual ))) Annual /// ((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’
  - pH (LPD277e0621): interpretation1_seasonality: ‘((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’ has been replaced by ‘((( ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual ))) Annual /// ((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’

Version: 1.0.9

lastVersion: 1.0.8
curator: nicholas
timestamp: 2023-02-13 23:42:50 UTC
changes:
- Paleo Interpretation metadata:
  - d13C (LPD17ad91b2): interpretation1_seasonality: ‘((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’ has been replaced by ‘((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’
  - pH (LPD277e0621): interpretation1_seasonality: ‘((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’ has been replaced by ‘((( null ))) ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual /// ((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’
- Paleo Column metadata:
  - Fe/Al (WEB5427a58b): paleoData_notes: ‘“Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized’ has been replaced by ‘((( “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_units updated; paleoData_proxyGeneral has been standardized ))) “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized /// “Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized’

Version: 1.0.8

lastVersion: 1.0.7
curator: nicholas
timestamp: 2023-02-09 15:42:27 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
- Paleo Column metadata:
  - uncertainty1s (LPD10136429): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized’
  - uncertainty1s (LPD10136429): paleoData_variableName: ‘C31d13Csd’ has been replaced by ‘uncertainty1s’
  - uncertainty1s (LPD10136429): paleoData_measurementMaterial: NULL has been replaced by ‘d13C C31’
  - uncertainty1s (LPD10136429): paleoData_summaryStatistic: NULL has been replaced by ‘1 sigma’
  - d13C (LPD17ad91b2): paleoData_datum: NULL has been replaced by ‘VSMOW’
  - d13C (LPD17ad91b2): paleoData_notes: ‘““Aridity is recog- nized as the dominant control on the large-scale distribution of C3 versus C4 vegetation in tropical Africa”“’ has been replaced by ‘““Aridity is recog- nized as the dominant control on the large-scale distribution of C3 versus C4 vegetation in tropical Africa”“; paleoData_datum has been standardized’
  - d13C (LPD17ad91b2): paleoData_units: ‘permil VSMOW’ has been replaced by ‘permil’
  - uncertainty1s (LPD2326672b): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized’
  - uncertainty1s (LPD2326672b): paleoData_variableName: ‘MBTsd’ has been replaced by ‘uncertainty1s’
  - uncertainty1s (LPD2326672b): paleoData_measurementMaterial: NULL has been replaced by ‘MBT’
  - uncertainty1s (LPD2326672b): paleoData_summaryStatistic: NULL has been replaced by ‘1 sigma’
  - d2H (LPD36e20a5f): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized’
  - d2H (LPD36e20a5f): paleoData_variableName: ‘C31dD’ has been replaced by ‘d2H’
  - d2H (LPD36e20a5f): paleoData_measurementMaterial: NULL has been replaced by ‘C31’
  - d2H (LPD3798724b): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized’
  - d2H (LPD3798724b): paleoData_variableName: ‘C31dDsd’ has been replaced by ‘d2H’
  - d2H (LPD3798724b): paleoData_measurementMaterial: NULL has been replaced by ‘C31’
  - uncertainty1s (LPDf2234b39): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized’
  - uncertainty1s (LPDf2234b39): paleoData_variableName: ‘CBTsd’ has been replaced by ‘uncertainty1s’
  - uncertainty1s (LPDf2234b39): paleoData_measurementMaterial: NULL has been replaced by ‘CBT’
  - uncertainty1s (LPDf2234b39): paleoData_summaryStatistic: NULL has been replaced by ‘1 sigma’
  - depth (REpcleODBtH): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized’
  - depth (REpcleODBtH): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - age (RM6vnGWCDqU): paleoData_datum: NULL has been replaced by ‘1950’
  - age (RM6vnGWCDqU): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (RM6vnGWCDqU): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
  - age (RM6vnGWCDqU): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - year (RQtIL8JzjpP): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized’
  - year (RQtIL8JzjpP): paleoData_units: ‘AD’ has been replaced by ‘yr AD’
  - year (RQtIL8JzjpP): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - age (WEB0c263fc0): paleoData_datum: NULL has been replaced by ‘1950’
  - age (WEB0c263fc0): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (WEB0c263fc0): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - age (WEB191f16f3): paleoData_datum: NULL has been replaced by ‘1950’
  - age (WEB191f16f3): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
  - age (WEB191f16f3): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - MS (WEB279cd5b2): paleoData_proxy: ‘Magnetic Susceptibility’ has been replaced by ‘magnetic susceptibility’
  - MS (WEB279cd5b2): paleoData_units: ‘10^-6SI’ has been replaced by ‘SI’
  - Fe/Al (WEB5427a58b): paleoData_notes: ‘“Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”’ has been replaced by ‘“Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”; paleoData_proxyGeneral has been standardized’
  - Fe/Al (WEB5427a58b): paleoData_proxyGeneral: NULL has been replaced by ‘elemental’
  - Fe/Al (WEB5427a58b): paleoData_units: ‘ratio cps’ has been replaced by ‘ratio’
  - depth (WEBc4de9ba7): paleoData_variableName: ‘Depth’ has been replaced by ‘depth’
  - Ti/Ca (WEBc666b28d): paleoData_notes: NULL has been replaced by ‘NA; paleoData_proxyGeneral has been standardized’
  - Ti/Ca (WEBc666b28d): paleoData_proxyGeneral: NULL has been replaced by ‘elemental’
  - Ti/Ca (WEBc666b28d): paleoData_units: ‘ratio cps’ has been replaced by ‘ratio’
  - depth (WEBfa4c75f3): paleoData_variableName: ‘Depth’ has been replaced by ‘depth’
- Paleo Interpretation metadata:
  - temperature (LPD6a7b432f): interpretation1_variable: ‘T’ has been replaced by ‘temperature’
  - d2H (LPDf79af672): interpretation1_variable: ‘Mixed’ has been replaced by NULL
  - MS (WEB279cd5b2): interpretation1_seasonality: ‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘Annual’
  - MS (WEB279cd5b2): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’
  - Fe/Al (WEB5427a58b): interpretation1_seasonality: ‘annual’ has been replaced by ‘Annual’
  - Fe/Al (WEB5427a58b): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’
  - Ti/Ca (WEBc666b28d): interpretation1_seasonality: ‘annual’ has been replaced by ‘Annual’
  - Ti/Ca (WEBc666b28d): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’

Version: 1.0.7

lastVersion: 1.0.6
curator: nicholas
timestamp: 2023-01-27 00:05:05 UTC
changes:
- Publication metadata:
  - pub1_author: ‘list(list(name = “Castañeda, Isla S.”), list(name = “Schouten, Stefan”), list(name = “Pätzold, Jürgen”), list(name = “Lucassen, Friedrich”), list(name = “Kasemann, Simone”), list(name = “Kuhlmann, Holger”), list(name = “Schefuß, Enno”))’ has been replaced by ‘Castaneda, Isla S.’
  - pub1_doi: ‘10.1016/j.epsl.2015.12.014’ has been replaced by NULL
- Geographic metadata:
  - geo_elevation: ‘-562’ has been replaced by NULL
- Paleo Column metadata:
  - d13C (LPD17ad91b2): paleoData_proxy: NULL has been replaced by ‘d13C’
  - d13C (LPD17ad91b2): paleoData_proxyDetail: NULL has been replaced by ‘C31n-alkane’
  - d13C (LPD17ad91b2): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
  - d13C (LPD17ad91b2): paleoData_units: ‘permil’ has been replaced by ‘permil VSMOW’
  - d13C (LPD17ad91b2): paleoData_variableName: ‘C31d13C_PDB’ has been replaced by ‘d13C’
  - d13C (LPD17ad91b2): paleoData_notes: NULL has been replaced by ‘““Aridity is recog- nized as the dominant control on the large-scale distribution of C3 versus C4 vegetation in tropical Africa”“’
  - pH (LPD277e0621): paleoData_proxy: NULL has been replaced by ‘pH’
  - pH (LPD277e0621): paleoData_proxyGeneral: NULL has been replaced by ‘biophysical’
  - MS (WEB279cd5b2): paleoData_proxyGeneral: NULL has been replaced by ‘biophysical’
  - MS (WEB279cd5b2): paleoData_notes: NULL has been replaced by ‘“A final hydroclimate proxy is provided by the MS record. Bulk soil MS provides a proxy for rainfall based on the premise that MS reflects the degree of pedogenesis, which increases with increasing rainfall (Balsam et al., 2011). Furthermore, it has been proposed that MS provides a quantitative rainfall proxy when appropriate statistical models are developed and calibrated for a specific re- gion, necessary because relationships between MS and rainfall may be either linear or non-linear (Maher and Possolo, 2013). We find that the GeoB7702-3 MS record is in close agreement with the δDwax record, supporting its use as a rainfall proxy”’
  - Fe/Al (WEB5427a58b): paleoData_notes: NULL has been replaced by ‘“Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”’
- Paleo Interpretation metadata:
  - d13C (LPD17ad91b2): interpretation1_seasonality: ‘annual’ has been replaced by ‘((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’
  - d13C (LPD17ad91b2): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’
  - pH (LPD277e0621): interpretation1_seasonality: ‘annual’ has been replaced by ‘((( null ))) 1,2,3,4,5,6,7,8,9,10,11,12 /// annual’
  - pH (LPD277e0621): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’
  - MS (WEB279cd5b2): interpretation1_seasonality: ‘annual’ has been replaced by ‘1,2,3,4,5,6,7,8,9,10,11,12’
  - MS (WEB279cd5b2): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’
  - Fe/Al (WEB5427a58b): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’

Version: 1.0.6

lastVersion: 1.0.5
curator: nicholas
timestamp: 2023-01-26 22:59:52 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
- Publication metadata:
  - pub1_author: ‘Castaneda, Isla S.’ has been replaced by ‘list(list(name = “Castañeda, Isla S.”), list(name = “Schouten, Stefan”), list(name = “Pätzold, Jürgen”), list(name = “Lucassen, Friedrich”), list(name = “Kasemann, Simone”), list(name = “Kuhlmann, Holger”), list(name = “Schefuß, Enno”))’
  - pub1_doi: NULL has been replaced by ‘10.1016/j.epsl.2015.12.014’
- Geographic metadata:
  - geo_elevation: NULL has been replaced by ‘-562’
- Paleo Column metadata:
  - C31d13C_PDB (LPD17ad91b2): paleoData_notes: ‘““Aridity is recog- nized as the dominant control on the large-scale distribution of C3 versus C4 vegetation in tropical Africa”“’ has been replaced by NULL
  - C31d13C_PDB (LPD17ad91b2): paleoData_proxy: ‘d13C’ has been replaced by NULL
  - C31d13C_PDB (LPD17ad91b2): paleoData_proxyDetail: ‘C31n-alkane’ has been replaced by NULL
  - C31d13C_PDB (LPD17ad91b2): paleoData_proxyGeneral: ‘isotope’ has been replaced by NULL
  - C31d13C_PDB (LPD17ad91b2): paleoData_units: ‘permil VSMOW’ has been replaced by ‘permil’
  - C31d13C_PDB (LPD17ad91b2): paleoData_variableName: ‘d13C’ has been replaced by ‘C31d13C_PDB’
  - pH (LPD277e0621): paleoData_proxy: ‘pH’ has been replaced by NULL
  - pH (LPD277e0621): paleoData_proxyGeneral: ‘biophysical’ has been replaced by NULL
  - MS (WEB279cd5b2): paleoData_notes: ‘“A final hydroclimate proxy is provided by the MS record. Bulk soil MS provides a proxy for rainfall based on the premise that MS reflects the degree of pedogenesis, which increases with increasing rainfall (Balsam et al., 2011). Furthermore, it has been proposed that MS provides a quantitative rainfall proxy when appropriate statistical models are developed and calibrated for a specific re- gion, necessary because relationships between MS and rainfall may be either linear or non-linear (Maher and Possolo, 2013). We find that the GeoB7702-3 MS record is in close agreement with the δDwax record, supporting its use as a rainfall proxy”’ has been replaced by NULL
  - MS (WEB279cd5b2): paleoData_proxyGeneral: ‘biophysical’ has been replaced by NULL
  - Fe/Al (WEB5427a58b): paleoData_notes: ‘“Ti to calcium (Ca) ratios are often used to examine terrigenous versus marine input. In GeoB7702-3 the lowest Fe/Al and Ti/Ca ratios are from ca. 15.7 to 14 ka BP sig- naling low runoff (Figs. 4a, 4b). We note that the Ti/Al and Fe/Ca ratios (not plotted) yield exactly the same trends as the Fe/Al and Ti/Ca records,”’ has been replaced by NULL
- Paleo Interpretation metadata:
  - C31d13C_PDB (LPD17ad91b2): interpretation1_seasonality: ‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘annual’
  - C31d13C_PDB (LPD17ad91b2): interpretation1_seasonalityGeneral: ‘Annual’ has been replaced by NULL
  - pH (LPD277e0621): interpretation1_seasonality: ‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘annual’
  - pH (LPD277e0621): interpretation1_seasonalityGeneral: ‘Annual’ has been replaced by NULL
  - MS (WEB279cd5b2): interpretation1_seasonality: ‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘annual’
  - MS (WEB279cd5b2): interpretation1_seasonalityGeneral: ‘Annual’ has been replaced by NULL
  - Fe/Al (WEB5427a58b): interpretation1_seasonalityGeneral: ‘Annual’ has been replaced by NULL

Version: 1.0.5

lastVersion: 1.0.4
curator: nick
timestamp: 2021-04-13 02:32:25 UTC
changes:
- Paleo Interpretation metadata:
  - temperature (LPD6a7b432f): interpretation1_seasonality: ‘annual’ has been replaced by NULL

Version: 1.0.4

lastVersion: 1.0.3
curator: nick
timestamp: 2021-03-17 01:53:26 UTC
changes:
- Paleo Interpretation metadata:
  - C31d13Csd (LPD10136429): interpretation1_scope: NULL has been replaced by ‘climate’
  - C31d13C_PDB (LPD17ad91b2): interpretation1_scope: NULL has been replaced by ‘climate’
  - MBT (LPD1be767d8): interpretation1_scope: NULL has been replaced by ‘climate’
  - MBTsd (LPD2326672b): interpretation1_scope: NULL has been replaced by ‘climate’
  - pH (LPD277e0621): interpretation1_scope: NULL has been replaced by ‘climate’
  - C31dD (LPD36e20a5f): interpretation1_scope: NULL has been replaced by ‘climate’
  - C31dDsd (LPD3798724b): interpretation1_scope: NULL has been replaced by ‘climate’
  - CBTsd (LPDf2234b39): interpretation1_scope: NULL has been replaced by ‘climate’
  - d2H (LPDf79af672): interpretation1_variable: ‘M’ has been replaced by ‘Mixed’
  - CBT (LPDfe736bed): interpretation1_scope: NULL has been replaced by ‘climate’
- Paleo Column metadata:
  - d2H (LPDf79af672): paleoData_proxyDetail: NULL has been replaced by ‘leaf wax’
  - d2H (LPDf79af672): paleoData_QCCertification: NULL has been replaced by ‘CH’
  - d2H (LPDf79af672): paleoData_QCnotes: NULL has been replaced by ‘“While δDwax is often interpreted to reflect precipitation amount in the African tropics, our data suggest that shifting moisture sources, related to migrations of the tropical rainbelt and CAB, also contributed to isotopic variability. As δDwax may behave non-linearly due to the additional influence of changing moisture sources, care should be taken when interpreting δDwax records from areas falling under the influence of isotopically distinct moisture sources.” (Castaneda et al., 2016)’
  - d2H (LPDf79af672): paleoData_variableName: ‘C31dDSmow-ice’ has been replaced by ‘d2H’

Version: 1.0.3

lastVersion: 1.0.2
curator: nick
timestamp: 2021-01-18 21:38:10 UTC
changes:
- Paleo Interpretation metadata:
  - C31d13Csd (LPD10136429): interpretation1_scope: ‘climate’ has been replaced by NULL
  - C31d13C_PDB (LPD17ad91b2): interpretation1_scope: ‘climate’ has been replaced by NULL
  - MBT (LPD1be767d8): interpretation1_scope: ‘climate’ has been replaced by NULL
  - MBTsd (LPD2326672b): interpretation1_scope: ‘climate’ has been replaced by NULL
  - pH (LPD277e0621): interpretation1_scope: ‘climate’ has been replaced by NULL
  - C31dD (LPD36e20a5f): interpretation1_scope: ‘climate’ has been replaced by NULL
  - C31dDsd (LPD3798724b): interpretation1_scope: ‘climate’ has been replaced by NULL
  - CBTsd (LPDf2234b39): interpretation1_scope: ‘climate’ has been replaced by NULL
  - CBT (LPDfe736bed): interpretation1_scope: ‘climate’ has been replaced by NULL

Version: 1.0.2

lastVersion: 1.0.1
curator: nick
timestamp: 2021-01-15 18:47:50 UTC
changes:
- Paleo Interpretation metadata:
  - C31d13Csd (LPD10136429): interpretation1_scope: NULL has been replaced by ‘climate’
  - C31d13C_PDB (LPD17ad91b2): interpretation1_scope: NULL has been replaced by ‘climate’
  - MBT (LPD1be767d8): interpretation1_scope: NULL has been replaced by ‘climate’
  - MBTsd (LPD2326672b): interpretation1_scope: NULL has been replaced by ‘climate’
  - pH (LPD277e0621): interpretation1_scope: NULL has been replaced by ‘climate’
  - C31dD (LPD36e20a5f): interpretation1_scope: NULL has been replaced by ‘climate’
  - C31dDsd (LPD3798724b): interpretation1_scope: NULL has been replaced by ‘climate’
  - CBTsd (LPDf2234b39): interpretation1_scope: NULL has been replaced by ‘climate’
  - CBT (LPDfe736bed): interpretation1_scope: NULL has been replaced by ‘climate’

Version: 1.0.1

lastVersion: 1.0.0
curator: nick
timestamp: 2020-10-08 12:41:40 UTC
changes:
- Paleo Column metadata:
  - C31dDSmow-ice (LPDf79af672): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’

Version: 1.0.0

curator: nick
timestamp: 2020-08-21 15:36:32 UTC
notes: This marks the creation of the changelog, and marks the status of this dataset as of mid 2020
changes:
- Setup:
  - Changelog created