Version history for 8yG74c3je9wOKwzZiwnQ -
Aljojuca.Bhattacharya.2015
Version: 1.0.18
- lastVersion: 1.0.17
- curator: nicholas
- timestamp: 2023-08-10 22:40:11 UTC
- changes:
- Base metadata:
- Paleo Column metadata:
- Al2O3 (WEBfa22dabc): paleoData_proxy: ‘((( mineralogy ))) deleteMe
/// Al2O3’ has been replaced by ‘Al2O3’
Version: 1.0.17
- lastVersion: 1.0.16
- curator: nicholas
- timestamp: 2023-07-05 00:32:08 UTC
- changes:
- Paleo Column metadata:
- Al2O3 (WEBfa22dabc): paleoData_proxy: ‘Al2O3’ has been replaced by
‘((( mineralogy ))) deleteMe /// Al2O3’
Version: 1.0.16
- lastVersion: 1.0.15
- curator: nicholas
- timestamp: 2023-05-31 20:37:48 UTC
- changes:
- Paleo Column metadata:
- d18O (WEB4ef1e8b8): paleoData_notes: ‘((( ((( “We interpret changes
in ��18O as indicative of changes in the ratio of evaporation and
precipitation (E/P). An increase in the evaporation relative to
precipitation increases the 18O content of lakewater: H218O tends to
evaporate more slowly than H216O, and the higher 16O content of
atmospheric water vapor means that 16O is preferentially returned to the
lake in precipitation (47). A higher (lower) ratio of evaporation to
precipitation would therefore result in higher (lower) ��18O”;
paleoData_units updated ))) “We interpret changes in δ18O as indicative
of changes in the ratio of evaporation and precipitation (E/P). An
increase in the evaporation relative to precipitation increases the 18O
content of lakewater: H218O tends to evaporate more slowly than H216O,
and the higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) δ18O” /// “We interpret changes in δ18O as indicative of
changes in the ratio of evaporation and precipitation (E/P). An increase
in the evaporation relative to precipitation increases the 18O content
of lakewater: H218O tends to evaporate more slowly than H216O, and the
higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) δ18O” ))) “We interpret changes in d18O as indicative of
changes in the ratio of evaporation and precipitation (E/P). An increase
in the evaporation relative to precipitation increases the 18O content
of lakewater: H218O tends to evaporate more slowly than H216O, and the
higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) d18O” /// “We interpret changes in δ18O as indicative of
changes in the ratio of evaporation and precipitation (E/P). An increase
in the evaporation relative to precipitation increases the 18O content
of lakewater: H218O tends to evaporate more slowly than H216O, and the
higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) δ18O”’ has been replaced by ‘“We interpret changes in
d18O as indicative of changes in the ratio of evaporation and
precipitation (E/P). An increase in the evaporation relative to
precipitation increases the 18O content of lakewater: H218O tends to
evaporate more slowly than H216O, and the higher 16O content of
atmospheric water vapor means that 16O is preferentially returned to the
lake in precipitation (47). A higher (lower) ratio of evaporation to
precipitation would therefore result in higher (lower) d18O”’
Version: 1.0.15
- lastVersion: 1.0.14
- curator: nicholas
- timestamp: 2023-05-30 15:48:00 UTC
- changes:
- Paleo Column metadata:
- d18O (WEB4ef1e8b8): paleoData_notes: ‘“We interpret changes in δ18O
as indicative of changes in the ratio of evaporation and precipitation
(E/P). An increase in the evaporation relative to precipitation
increases the 18O content of lakewater: H218O tends to evaporate more
slowly than H216O, and the higher 16O content of atmospheric water vapor
means that 16O is preferentially returned to the lake in precipitation
(47). A higher (lower) ratio of evaporation to precipitation would
therefore result in higher (lower) δ18O”’ has been replaced by ‘((( (((
“We interpret changes in ��18O as indicative of changes in the ratio of
evaporation and precipitation (E/P). An increase in the evaporation
relative to precipitation increases the 18O content of lakewater: H218O
tends to evaporate more slowly than H216O, and the higher 16O content of
atmospheric water vapor means that 16O is preferentially returned to the
lake in precipitation (47). A higher (lower) ratio of evaporation to
precipitation would therefore result in higher (lower) ��18O”;
paleoData_units updated ))) “We interpret changes in δ18O as indicative
of changes in the ratio of evaporation and precipitation (E/P). An
increase in the evaporation relative to precipitation increases the 18O
content of lakewater: H218O tends to evaporate more slowly than H216O,
and the higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) δ18O” /// “We interpret changes in δ18O as indicative of
changes in the ratio of evaporation and precipitation (E/P). An increase
in the evaporation relative to precipitation increases the 18O content
of lakewater: H218O tends to evaporate more slowly than H216O, and the
higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) δ18O” ))) “We interpret changes in d18O as indicative of
changes in the ratio of evaporation and precipitation (E/P). An increase
in the evaporation relative to precipitation increases the 18O content
of lakewater: H218O tends to evaporate more slowly than H216O, and the
higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) d18O” /// “We interpret changes in δ18O as indicative of
changes in the ratio of evaporation and precipitation (E/P). An increase
in the evaporation relative to precipitation increases the 18O content
of lakewater: H218O tends to evaporate more slowly than H216O, and the
higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) δ18O”’
- d18O (WEB4ef1e8b8): paleoData_QCCertification: ‘CH’ has been
replaced by ‘CH, CR’
- Al2O3 (WEBfa22dabc): paleoData_notes: ‘We interpret the mass % of
Al2O3 as an indicator of input of plagioclase and secondary clay
minerals from the maar slope walls into the lake system. The flux of Al
increases during wet conditions, when enhanced slopewash transports
terrigenous material into the lake system’ has been replaced by ‘“We
interpret the mass % of Al2O3 as an indicator of input of plagioclase
and secondary clay minerals from the maar slope walls into the lake
system. The flux of Al increases during wet conditions, when enhanced
slopewash transports terrigenous material into the lake system”’
- Al2O3 (WEBfa22dabc): paleoData_proxyGeneral: ‘biophysical’ has been
replaced by ‘mineral’
- Al2O3 (WEBfa22dabc): paleoData_QCCertification: NULL has been
replaced by ‘CR’
- Al2O3 (WEBfa22dabc): paleoData_QCnotes: ‘Length <4000yrs’ has
been replaced by ‘Length <4000yrs, but reasonable to include.’
- Paleo Interpretation metadata:
- d18O (WEB4ef1e8b8): interpretation1_variableDetail: ‘lake@surface’ has been
replaced by ‘@surface’
- Al2O3 (WEBfa22dabc): interpretation1_direction: ‘negative’ has been
replaced by ‘positive’
- Al2O3 (WEBfa22dabc): interpretation1_seasonality: NULL has been
replaced by ‘Annual’
- Al2O3 (WEBfa22dabc): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Annual’
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2023-05-12 21:48:15 UTC
- changes:
- Paleo Column metadata:
- d18O (WEB4ef1e8b8): paleoData_notes: ‘((( “We interpret changes in
��18O as indicative of changes in the ratio of evaporation and
precipitation (E/P). An increase in the evaporation relative to
precipitation increases the 18O content of lakewater: H218O tends to
evaporate more slowly than H216O, and the higher 16O content of
atmospheric water vapor means that 16O is preferentially returned to the
lake in precipitation (47). A higher (lower) ratio of evaporation to
precipitation would therefore result in higher (lower) ��18O”;
paleoData_units updated ))) “We interpret changes in δ18O as indicative
of changes in the ratio of evaporation and precipitation (E/P). An
increase in the evaporation relative to precipitation increases the 18O
content of lakewater: H218O tends to evaporate more slowly than H216O,
and the higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) δ18O” /// “We interpret changes in δ18O as indicative of
changes in the ratio of evaporation and precipitation (E/P). An increase
in the evaporation relative to precipitation increases the 18O content
of lakewater: H218O tends to evaporate more slowly than H216O, and the
higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) δ18O”’ has been replaced by ‘“We interpret changes in
δ18O as indicative of changes in the ratio of evaporation and
precipitation (E/P). An increase in the evaporation relative to
precipitation increases the 18O content of lakewater: H218O tends to
evaporate more slowly than H216O, and the higher 16O content of
atmospheric water vapor means that 16O is preferentially returned to the
lake in precipitation (47). A higher (lower) ratio of evaporation to
precipitation would therefore result in higher (lower) δ18O”’
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2023-03-24 22:23:39 UTC
- changes:
- Paleo Column metadata:
- d18O (WEB4ef1e8b8): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d13C (WEB5d337c69): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- Al2O3 (WEBfa22dabc): paleoData_proxy: NULL has been replaced by
‘Al2O3’
- Paleo Interpretation metadata:
- d18O (WEB4ef1e8b8): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
- Al2O3 (WEBfa22dabc): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
- Al2O3 (WEBfa22dabc): interpretation1_variableDetail: NULL has been
replaced by ‘runoff@catchment’
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-02-13 23:36:40 UTC
- changes:
- Paleo Column metadata:
- d18O (WEB4ef1e8b8): paleoData_notes: ‘“We interpret changes in δ18O
as indicative of changes in the ratio of evaporation and precipitation
(E/P). An increase in the evaporation relative to precipitation
increases the 18O content of lakewater: H218O tends to evaporate more
slowly than H216O, and the higher 16O content of atmospheric water vapor
means that 16O is preferentially returned to the lake in precipitation
(47). A higher (lower) ratio of evaporation to precipitation would
therefore result in higher (lower) δ18O”’ has been replaced by ‘((( “We
interpret changes in ��18O as indicative of changes in the ratio of
evaporation and precipitation (E/P). An increase in the evaporation
relative to precipitation increases the 18O content of lakewater: H218O
tends to evaporate more slowly than H216O, and the higher 16O content of
atmospheric water vapor means that 16O is preferentially returned to the
lake in precipitation (47). A higher (lower) ratio of evaporation to
precipitation would therefore result in higher (lower) ��18O”;
paleoData_units updated ))) “We interpret changes in δ18O as indicative
of changes in the ratio of evaporation and precipitation (E/P). An
increase in the evaporation relative to precipitation increases the 18O
content of lakewater: H218O tends to evaporate more slowly than H216O,
and the higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) δ18O” /// “We interpret changes in δ18O as indicative of
changes in the ratio of evaporation and precipitation (E/P). An increase
in the evaporation relative to precipitation increases the 18O content
of lakewater: H218O tends to evaporate more slowly than H216O, and the
higher 16O content of atmospheric water vapor means that 16O is
preferentially returned to the lake in precipitation (47). A higher
(lower) ratio of evaporation to precipitation would therefore result in
higher (lower) δ18O”’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-02-10 14:32:50 UTC
- changes:
- Paleo Interpretation metadata:
- uncertaintyLow95 (WEB0e036388): interpretation1_scope: NULL has been
replaced by ‘climate’
- uncertaintyLow95 (WEBa76a84ed): interpretation1_scope: NULL has been
replaced by ‘climate’
- uncertaintyHigh95 (WEBba2196c8): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh95 (WEBfa96b5b1): interpretation1_scope: NULL has
been replaced by ‘climate’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-02-09 15:26:46 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Geographic metadata:
- geo_elevation: NULL has been replaced by ‘2376’
- Paleo Column metadata:
- age (WEB00e0403b): paleoData_notes: NULL has been replaced by ‘NA;
paleoData_isPrimary has been standardized; paleoData_datum has been
standardized’
- age (WEB00e0403b): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (WEB00e0403b): paleoData_datum: NULL has been replaced by
‘1950’
- age (WEB00e0403b): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- PC1 (WEB08871912): paleoData_notes: NULL has been replaced by ‘NA;
paleoData_method has been standardized’
- PC1 (WEB08871912): paleoData_method: NULL has been replaced by
‘principal components’
- uncertaintyLow95 (WEB0e036388): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_summaryStatistic has been standardized;
paleoData_inferredMaterial has been standardized; paleoData_datum has
been standardized’
- uncertaintyLow95 (WEB0e036388): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow95 (WEB0e036388): paleoData_variableName:
‘age_calBP95-’ has been replaced by ‘uncertaintyLow95’
- uncertaintyLow95 (WEB0e036388): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow95 (WEB0e036388): paleoData_inferredMaterial: NULL has
been replaced by ‘age’
- uncertaintyLow95 (WEB0e036388): paleoData_summaryStatistic: NULL has
been replaced by ‘quantile 2.5’
- d18O (WEB4ef1e8b8): paleoData_units: ‘pemil’ has been replaced by
‘permil’
- depth (WEB5429e74b): paleoData_notes: NULL has been replaced by ‘NA;
paleoData_isPrimary has been standardized’
- depth (WEB5429e74b): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- age (WEB5f66e134): paleoData_notes: NULL has been replaced by ‘NA;
paleoData_isPrimary has been standardized; paleoData_datum has been
standardized’
- age (WEB5f66e134): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (WEB5f66e134): paleoData_datum: NULL has been replaced by
‘1950’
- age (WEB5f66e134): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- depth (WEB60c27894): paleoData_notes: NULL has been replaced by ‘NA;
paleoData_isPrimary has been standardized’
- depth (WEB60c27894): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- uncertaintyLow95 (WEBa76a84ed): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_summaryStatistic has been standardized;
paleoData_inferredMaterial has been standardized; paleoData_datum has
been standardized’
- uncertaintyLow95 (WEBa76a84ed): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow95 (WEBa76a84ed): paleoData_variableName:
‘age_calBP95-’ has been replaced by ‘uncertaintyLow95’
- uncertaintyLow95 (WEBa76a84ed): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow95 (WEBa76a84ed): paleoData_inferredMaterial: NULL has
been replaced by ‘age’
- uncertaintyLow95 (WEBa76a84ed): paleoData_summaryStatistic: NULL has
been replaced by ‘quantile 2.5’
- uncertaintyHigh95 (WEBba2196c8): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_summaryStatistic has been standardized;
paleoData_inferredMaterial has been standardized’
- uncertaintyHigh95 (WEBba2196c8): paleoData_variableName:
‘age_calBP95+’ has been replaced by ‘uncertaintyHigh95’
- uncertaintyHigh95 (WEBba2196c8): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyHigh95 (WEBba2196c8): paleoData_summaryStatistic: NULL
has been replaced by ‘quantile 97.5’
- Al2O3 (WEBfa22dabc): paleoData_proxy: ‘mineralogy’ has been replaced
by NULL
- Al2O3 (WEBfa22dabc): paleoData_variableName: ‘AL2O3’ has been
replaced by ‘Al2O3’
- uncertaintyHigh95 (WEBfa96b5b1): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_summaryStatistic has been standardized;
paleoData_inferredMaterial has been standardized; paleoData_datum has
been standardized’
- uncertaintyHigh95 (WEBfa96b5b1): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyHigh95 (WEBfa96b5b1): paleoData_variableName:
‘age_calBP95+’ has been replaced by ‘uncertaintyHigh95’
- uncertaintyHigh95 (WEBfa96b5b1): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh95 (WEBfa96b5b1): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyHigh95 (WEBfa96b5b1): paleoData_summaryStatistic: NULL
has been replaced by ‘quantile 97.5’
- Paleo Interpretation metadata:
- d18O (WEB4ef1e8b8): interpretation1_seasonality:
‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘Annual’
- Al2O3 (WEBfa22dabc): interpretation1_variable: ‘M’ has been replaced
by ‘P-E’
Version: 1.0.9
- lastVersion: 1.0.8
- curator: nicholas
- timestamp: 2022-07-28 17:26:56 UTC
- changes:
- Base metadata:
- Geographic metadata:
- geo_elevation: ‘2376’ has been replaced by NULL
Version: 1.0.8
- lastVersion: 1.0.7
- curator: nicholas
- timestamp: 2022-07-15 22:57:19 UTC
- changes:
- Paleo Interpretation metadata:
- PC1 (WEB08871912): interpretation1_scope: NULL has been replaced by
‘climate’
- d13C (WEB5d337c69): interpretation1_scope: NULL has been replaced by
‘climate’
- CaO (WEB77e5368a): interpretation1_scope: NULL has been replaced by
‘climate’
- Zr (WEB830b4789): interpretation1_scope: NULL has been replaced by
‘climate’
- Ti (WEBc4d3fb76): interpretation1_scope: NULL has been replaced by
‘climate’
Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2022-05-18 00:24:24 UTC
- changes:
- Paleo Interpretation metadata:
- PC1 (WEB08871912): interpretation1_scope: ‘climate’ has been
replaced by NULL
- d18O (WEB4ef1e8b8): interpretation1_variableGroup: ‘M’ has been
replaced by ‘P-E’
- d13C (WEB5d337c69): interpretation1_scope: ‘climate’ has been
replaced by NULL
- CaO (WEB77e5368a): interpretation1_scope: ‘climate’ has been
replaced by NULL
- Zr (WEB830b4789): interpretation1_scope: ‘climate’ has been replaced
by NULL
- Ti (WEBc4d3fb76): interpretation1_scope: ‘climate’ has been replaced
by NULL
- Paleo Column metadata:
- d18O (WEB4ef1e8b8): paleoData_mostRecentCompilations: NULL has been
replaced by ‘HoloceneAbruptChange-0_10_0’
- AL2O3 (WEBfa22dabc): paleoData_mostRecentCompilations: NULL has been
replaced by ‘HoloceneAbruptChange-0_10_0’
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2021-10-05 21:38:08 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: NULL has been replaced by ‘North
America>Mexico’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nick
- timestamp: 2021-04-13 02:30:37 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (WEB4ef1e8b8): interpretation1_seasonality:
‘1,2,3,4,5,6,7,8,9,10,11,337’ has been replaced by
‘1,2,3,4,5,6,7,8,9,10,11,12’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nick
- timestamp: 2021-03-17 01:51:39 UTC
- changes:
- Paleo Interpretation metadata:
- PC1 (WEB08871912): interpretation1_scope: NULL has been replaced by
‘climate’
- d18O (WEB4ef1e8b8): interpretation1_variable: ‘M’ has been replaced
by ‘P-E’
- d18O (WEB4ef1e8b8): interpretation1_seasonality: NULL has been
replaced by ‘1,2,3,4,5,6,7,8,9,10,11,337’
- d18O (WEB4ef1e8b8): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Annual’
- d18O (WEB4ef1e8b8): interpretation1_variableDetail: NULL has been
replaced by ‘lake@surface’
- d13C (WEB5d337c69): interpretation1_scope: NULL has been replaced by
‘climate’
- CaO (WEB77e5368a): interpretation1_scope: NULL has been replaced by
‘climate’
- Zr (WEB830b4789): interpretation1_scope: NULL has been replaced by
‘climate’
- Ti (WEBc4d3fb76): interpretation1_scope: NULL has been replaced by
‘climate’
- Paleo Column metadata:
- d18O (WEB4ef1e8b8): paleoData_notes: NULL has been replaced by ‘“We
interpret changes in δ18O as indicative of changes in the ratio of
evaporation and precipitation (E/P). An increase in the evaporation
relative to precipitation increases the 18O content of lakewater: H218O
tends to evaporate more slowly than H216O, and the higher 16O content of
atmospheric water vapor means that 16O is preferentially returned to the
lake in precipitation (47). A higher (lower) ratio of evaporation to
precipitation would therefore result in higher (lower) δ18O”’
- d18O (WEB4ef1e8b8): paleoData_units: ‘unitless’ has been replaced by
‘pemil’
- d18O (WEB4ef1e8b8): paleoData_proxyDetail: NULL has been replaced by
‘authigenic calcite’
- d18O (WEB4ef1e8b8): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- AL2O3 (WEBfa22dabc): paleoData_QCnotes: NULL has been replaced by
‘Length <4000yrs’
- Paleo Calibration metadata:
- d18O (WEB4ef1e8b8): calibration_method: NULL has been replaced by
‘VPDB’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nick
- timestamp: 2021-01-18 21:36:51 UTC
- changes:
- Paleo Interpretation metadata:
- PC1 (WEB08871912): interpretation1_scope: ‘climate’ has been
replaced by NULL
- d13C (WEB5d337c69): interpretation1_scope: ‘climate’ has been
replaced by NULL
- CaO (WEB77e5368a): interpretation1_scope: ‘climate’ has been
replaced by NULL
- Zr (WEB830b4789): interpretation1_scope: ‘climate’ has been replaced
by NULL
- Ti (WEBc4d3fb76): interpretation1_scope: ‘climate’ has been replaced
by NULL
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nick
- timestamp: 2021-01-15 18:46:31 UTC
- changes:
- Paleo Interpretation metadata:
- PC1 (WEB08871912): interpretation1_scope: NULL has been replaced by
‘climate’
- d13C (WEB5d337c69): interpretation1_scope: NULL has been replaced by
‘climate’
- CaO (WEB77e5368a): interpretation1_scope: NULL has been replaced by
‘climate’
- Zr (WEB830b4789): interpretation1_scope: NULL has been replaced by
‘climate’
- Ti (WEBc4d3fb76): interpretation1_scope: NULL has been replaced by
‘climate’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2020-10-08 12:40:23 UTC
- changes:
- Paleo Column metadata:
- d18O (WEB4ef1e8b8): paleoData_proxy: ‘permil’ has been replaced by
‘d18O’
- d18O (WEB4ef1e8b8): paleoData_proxyLumps: ‘permil’ has been replaced
by ‘isotope’
- d18O (WEB4ef1e8b8): paleoData_proxyLumpsOriginal: NULL has been
replaced by ‘d18O’
- d18O (WEB4ef1e8b8): paleoData_proxyGeneral: NULL has been replaced
by ‘isotope’
- d13C (WEB5d337c69): paleoData_proxy: ‘permil’ has been replaced by
‘d13C’
- d13C (WEB5d337c69): paleoData_proxyLumps: ‘permil’ has been replaced
by ‘isotope’
- d13C (WEB5d337c69): paleoData_proxyLumpsOriginal: NULL has been
replaced by ‘d13C’
- d13C (WEB5d337c69): paleoData_proxyGeneral: NULL has been replaced
by ‘isotope’
- AL2O3 (WEBfa22dabc): paleoData_proxy: ‘mineral’ has been replaced by
‘mineralogy’
- AL2O3 (WEBfa22dabc): paleoData_proxyLumps: ‘biophysical’ has been
replaced by ‘mineralogy’
- AL2O3 (WEBfa22dabc): paleoData_notes: NULL has been replaced by ‘We
interpret the mass % of Al2O3 as an indicator of input of plagioclase
and secondary clay minerals from the maar slope walls into the lake
system. The flux of Al increases during wet conditions, when enhanced
slopewash transports terrigenous material into the lake system’
- AL2O3 (WEBfa22dabc): paleoData_proxyGeneral: NULL has been replaced
by ‘biophysical’
Version: 1.0.0
- curator: nick
- timestamp: 2020-08-21 15:36:30 UTC
- notes: This marks the creation of the changelog, and marks
the status of this dataset as of mid 2020
- changes: