Version history for nCYj44f2zrFfpch4GvkX - CO00DRBE
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2025-05-20 16:18:31.159995 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT489b5e257f): interpretation4_scope: NULL has been replaced
by ‘climate’
- year (MAT489b5e257f): interpretation5_scope: NULL has been replaced
by ‘climate’
- year (MATa3aa118919): interpretation4_scope: NULL has been replaced
by ‘climate’
- year (MATa3aa118919): interpretation5_scope: NULL has been replaced
by ‘climate’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:03:54.865811 UTC
- changes:
- Paleo Column metadata:
- year (MAT489b5e257f): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT489b5e257f): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- year (MATa3aa118919): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MATa3aa118919): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- d18O (Ocean2kHR_124): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (Ocean2kHR_124): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d18O (Ocean2kHR_125): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (Ocean2kHR_125): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:09:50.988085 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT489b5e257f): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT489b5e257f): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MAT489b5e257f): interpretation3_scope: NULL has been replaced
by ‘climate’
- year (MATa3aa118919): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MATa3aa118919): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MATa3aa118919): interpretation3_scope: NULL has been replaced
by ‘climate’
- d18O (Ocean2kHR_124): interpretation2_basis: ‘The availability of
instrumental climate data allow the comparison with the coral signal and
supports the interpretation of reconstructed past temperature anomalies.
The use of air temperatures is justified by the strong long-term
correspondence between Bermuda SST (COADS) of a 2 latitude by 2
longitude area and Bermuda air temperature during a 40-year period.’ has
been replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_coefficient: ‘0.58’ has been
replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_direction: ‘negative’ has been
replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_fraction: ‘0.81’ has been
replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_integrationTime: ‘3’ has been
replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_integrationTimeBasis:
‘X-radiographs were assessed from the skeleton slices to expose density
banding. Chronologies were achieved by counting the well-developed
density couplets. BDA 210 revealed continuous growth between 1825 and
1993, whereas BDA 215 and BDA 221 contain hiatuses. The bases of the
colonies, which were separated from the upper living parts by algal
growth, were 14C dated by AMS in the Leibnitz Laboratory in Kiel.
Precision of Dating came to 30 years. The stratigraphy obtained from
14C dating was confirmed by the strong correspondence of the present
proxy time series with a continuous 800-year coral skeletal chronology
from Bermuda, presented by P�tzold et al. (1998; see Fig. 3c).’ has been
replaced by NULL
- d18O (Ocean2kHR_124):
interpretation2_integrationTimeUncertaintyType: ‘chronological and
radiocarbon dating �30 years’ has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_integrationTimeUnits: ‘years’
has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (Ocean2kHR_124): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_124): interpretation2_seasonality: ‘Annual’ has been
replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_seasonalityOriginal: ‘Annual’
has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_variable: ‘temperature’ has
been replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_variableGroup: ‘Temperature’
has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation2_variableGroupOriginal:
‘T_water’ has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation3_basis: ‘the salinity effect on
the isotopic pool of the ambient seawater is considered a negligible
background signal and variations in coral d18O can be attributed to be
primarily driven by changes in SST.’ has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation3_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation3_integrationTime: ‘3’ has been
replaced by NULL
- d18O (Ocean2kHR_124): interpretation3_integrationTimeBasis:
‘X-radiographs were assessed from the skeleton slices to expose density
banding. Chronologies were achieved by counting the well-developed
density couplets. BDA 210 revealed continuous growth between 1825 and
1993, whereas BDA 215 and BDA 221 contain hiatuses. The bases of the
colonies, which were separated from the upper living parts by algal
growth, were 14C dated by AMS in the Leibnitz Laboratory in Kiel.
Precision of Dating came to 30 years. The stratigraphy obtained from
14C dating was confirmed by the strong correspondence of the present
proxy time series with a continuous 800-year coral skeletal chronology
from Bermuda, presented by P�tzold et al. (1998; see Fig. 3c).’ has been
replaced by NULL
- d18O (Ocean2kHR_124):
interpretation3_integrationTimeUncertaintyType: ‘chronological and
radiocarbon dating �30 years’ has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation3_integrationTimeUnits: ‘years’
has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation3_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation3_rank: ‘2’ has been replaced by
NULL
- d18O (Ocean2kHR_124): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_124): interpretation3_variable: ‘seawaterIsotope’
has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation3_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation3_variableGroupOriginal:
‘d18O_seawater’ has been replaced by NULL
- d18O (Ocean2kHR_124): interpretation4_basis: NULL has been replaced
by ‘The availability of instrumental climate data allow the comparison
with the coral signal and supports the interpretation of reconstructed
past temperature anomalies. The use of air temperatures is justified by
the strong long-term correspondence between Bermuda SST (COADS) of a 2
latitude by 2 longitude area and Bermuda air temperature during a
40-year period.’
- d18O (Ocean2kHR_124): interpretation4_coefficient: NULL has been
replaced by ‘0.58’
- d18O (Ocean2kHR_124): interpretation4_direction: NULL has been
replaced by ‘negative’
- d18O (Ocean2kHR_124): interpretation4_fraction: NULL has been
replaced by ‘0.81’
- d18O (Ocean2kHR_124): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_124): interpretation4_integrationTime: NULL has been
replaced by ‘3’
- d18O (Ocean2kHR_124): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘X-radiographs were assessed from the skeleton slices
to expose density banding. Chronologies were achieved by counting the
well-developed density couplets. BDA 210 revealed continuous growth
between 1825 and 1993, whereas BDA 215 and BDA 221 contain hiatuses. The
bases of the colonies, which were separated from the upper living parts
by algal growth, were 14C dated by AMS in the Leibnitz Laboratory in
Kiel. Precision of Dating came to 30 years. The stratigraphy obtained
from 14C dating was confirmed by the strong correspondence of the
present proxy time series with a continuous 800-year coral skeletal
chronology from Bermuda, presented by P�tzold et al. (1998; see Fig.
3c).’
- d18O (Ocean2kHR_124):
interpretation4_integrationTimeUncertaintyType: NULL has been replaced
by ‘chronological and radiocarbon dating �30 years’
- d18O (Ocean2kHR_124): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘years’
- d18O (Ocean2kHR_124): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_124): interpretation4_rank: NULL has been replaced
by ‘1’
- d18O (Ocean2kHR_124): interpretation4_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_124): interpretation4_seasonality: NULL has been
replaced by ‘Annual’
- d18O (Ocean2kHR_124): interpretation4_seasonalityOriginal: NULL has
been replaced by ‘Annual’
- d18O (Ocean2kHR_124): interpretation4_variable: NULL has been
replaced by ‘temperature’
- d18O (Ocean2kHR_124): interpretation4_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (Ocean2kHR_124): interpretation4_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_124): interpretation4_variableGroupOriginal: NULL
has been replaced by ‘T_water’
- d18O (Ocean2kHR_124): interpretation5_basis: NULL has been replaced
by ‘the salinity effect on the isotopic pool of the ambient seawater is
considered a negligible background signal and variations in coral d18O
can be attributed to be primarily driven by changes in SST.’
- d18O (Ocean2kHR_124): interpretation5_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_124): interpretation5_integrationTime: NULL has been
replaced by ‘3’
- d18O (Ocean2kHR_124): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘X-radiographs were assessed from the skeleton slices
to expose density banding. Chronologies were achieved by counting the
well-developed density couplets. BDA 210 revealed continuous growth
between 1825 and 1993, whereas BDA 215 and BDA 221 contain hiatuses. The
bases of the colonies, which were separated from the upper living parts
by algal growth, were 14C dated by AMS in the Leibnitz Laboratory in
Kiel. Precision of Dating came to 30 years. The stratigraphy obtained
from 14C dating was confirmed by the strong correspondence of the
present proxy time series with a continuous 800-year coral skeletal
chronology from Bermuda, presented by P�tzold et al. (1998; see Fig.
3c).’
- d18O (Ocean2kHR_124):
interpretation5_integrationTimeUncertaintyType: NULL has been replaced
by ‘chronological and radiocarbon dating �30 years’
- d18O (Ocean2kHR_124): interpretation5_integrationTimeUnits: NULL has
been replaced by ‘years’
- d18O (Ocean2kHR_124): interpretation5_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_124): interpretation5_rank: NULL has been replaced
by ‘2’
- d18O (Ocean2kHR_124): interpretation5_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_124): interpretation5_variable: NULL has been
replaced by ‘seawaterIsotope’
- d18O (Ocean2kHR_124): interpretation5_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (Ocean2kHR_124): interpretation5_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_124): interpretation5_variableGroupOriginal: NULL
has been replaced by ‘d18O_seawater’
- d18O (Ocean2kHR_124): interpretation6_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_125): interpretation2_basis: ‘The availability of
instrumental climate data allow the comparison with the coral signal and
supports the interpretation of reconstructed past temperature anomalies.
The use of air temperatures is justified by the strong long-term
correspondence between Bermuda SST (COADS) of a 2 latitude by 2
longitude area and Bermuda air temperature during a 40-year period.’ has
been replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_coefficient: ‘0.58’ has been
replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_direction: ‘negative’ has been
replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_fraction: ‘0.81’ has been
replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_integrationTime: ‘3’ has been
replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_integrationTimeBasis:
‘X-radiographs were assessed from the skeleton slices to expose density
banding. Chronologies were achieved by counting the well-developed
density couplets. BDA 210 revealed continuous growth between 1825 and
1993, whereas BDA 215 and BDA 221 contain hiatuses. The bases of the
colonies, which were separated from the upper living parts by algal
growth, were 14C dated by AMS in the Leibnitz Laboratory in Kiel.
Precision of Dating came to 30 years. The stratigraphy obtained from
14C dating was confirmed by the strong correspondence of the present
proxy time series with a continuous 800-year coral skeletal chronology
from Bermuda, presented by P�tzold et al. (1998; see Fig. 3c).’ has been
replaced by NULL
- d18O (Ocean2kHR_125):
interpretation2_integrationTimeUncertaintyType: ‘chronological and
radiocarbon dating �30 years’ has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_integrationTimeUnits: ‘years’
has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (Ocean2kHR_125): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_125): interpretation2_variable: ‘temperature’ has
been replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_variableGroup: ‘Temperature’
has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation2_variableGroupOriginal:
‘T_water’ has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation3_basis: ‘the salinity effect on
the isotopic pool of the ambient seawater is considered a negligible
background signal and variations in coral d18O can be attributed to be
primarily driven by changes in SST.’ has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation3_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation3_integrationTime: ‘3’ has been
replaced by NULL
- d18O (Ocean2kHR_125): interpretation3_integrationTimeBasis:
‘X-radiographs were assessed from the skeleton slices to expose density
banding. Chronologies were achieved by counting the well-developed
density couplets. BDA 210 revealed continuous growth between 1825 and
1993, whereas BDA 215 and BDA 221 contain hiatuses. The bases of the
colonies, which were separated from the upper living parts by algal
growth, were 14C dated by AMS in the Leibnitz Laboratory in Kiel.
Precision of Dating came to 30 years. The stratigraphy obtained from
14C dating was confirmed by the strong correspondence of the present
proxy time series with a continuous 800-year coral skeletal chronology
from Bermuda, presented by P�tzold et al. (1998; see Fig. 3c).’ has been
replaced by NULL
- d18O (Ocean2kHR_125):
interpretation3_integrationTimeUncertaintyType: ‘chronological and
radiocarbon dating �30 years’ has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation3_integrationTimeUnits: ‘years’
has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation3_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation3_rank: ‘2’ has been replaced by
NULL
- d18O (Ocean2kHR_125): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_125): interpretation3_variable: ‘seawaterIsotope’
has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation3_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation3_variableGroupOriginal:
‘d18O_seawater’ has been replaced by NULL
- d18O (Ocean2kHR_125): interpretation4_basis: NULL has been replaced
by ‘The availability of instrumental climate data allow the comparison
with the coral signal and supports the interpretation of reconstructed
past temperature anomalies. The use of air temperatures is justified by
the strong long-term correspondence between Bermuda SST (COADS) of a 2
latitude by 2 longitude area and Bermuda air temperature during a
40-year period.’
- d18O (Ocean2kHR_125): interpretation4_coefficient: NULL has been
replaced by ‘0.58’
- d18O (Ocean2kHR_125): interpretation4_direction: NULL has been
replaced by ‘negative’
- d18O (Ocean2kHR_125): interpretation4_fraction: NULL has been
replaced by ‘0.81’
- d18O (Ocean2kHR_125): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_125): interpretation4_integrationTime: NULL has been
replaced by ‘3’
- d18O (Ocean2kHR_125): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘X-radiographs were assessed from the skeleton slices
to expose density banding. Chronologies were achieved by counting the
well-developed density couplets. BDA 210 revealed continuous growth
between 1825 and 1993, whereas BDA 215 and BDA 221 contain hiatuses. The
bases of the colonies, which were separated from the upper living parts
by algal growth, were 14C dated by AMS in the Leibnitz Laboratory in
Kiel. Precision of Dating came to 30 years. The stratigraphy obtained
from 14C dating was confirmed by the strong correspondence of the
present proxy time series with a continuous 800-year coral skeletal
chronology from Bermuda, presented by P�tzold et al. (1998; see Fig.
3c).’
- d18O (Ocean2kHR_125):
interpretation4_integrationTimeUncertaintyType: NULL has been replaced
by ‘chronological and radiocarbon dating �30 years’
- d18O (Ocean2kHR_125): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘years’
- d18O (Ocean2kHR_125): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_125): interpretation4_rank: NULL has been replaced
by ‘1’
- d18O (Ocean2kHR_125): interpretation4_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_125): interpretation4_variable: NULL has been
replaced by ‘temperature’
- d18O (Ocean2kHR_125): interpretation4_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (Ocean2kHR_125): interpretation4_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_125): interpretation4_variableGroupOriginal: NULL
has been replaced by ‘T_water’
- d18O (Ocean2kHR_125): interpretation5_basis: NULL has been replaced
by ‘the salinity effect on the isotopic pool of the ambient seawater is
considered a negligible background signal and variations in coral d18O
can be attributed to be primarily driven by changes in SST.’
- d18O (Ocean2kHR_125): interpretation5_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_125): interpretation5_integrationTime: NULL has been
replaced by ‘3’
- d18O (Ocean2kHR_125): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘X-radiographs were assessed from the skeleton slices
to expose density banding. Chronologies were achieved by counting the
well-developed density couplets. BDA 210 revealed continuous growth
between 1825 and 1993, whereas BDA 215 and BDA 221 contain hiatuses. The
bases of the colonies, which were separated from the upper living parts
by algal growth, were 14C dated by AMS in the Leibnitz Laboratory in
Kiel. Precision of Dating came to 30 years. The stratigraphy obtained
from 14C dating was confirmed by the strong correspondence of the
present proxy time series with a continuous 800-year coral skeletal
chronology from Bermuda, presented by P�tzold et al. (1998; see Fig.
3c).’
- d18O (Ocean2kHR_125):
interpretation5_integrationTimeUncertaintyType: NULL has been replaced
by ‘chronological and radiocarbon dating �30 years’
- d18O (Ocean2kHR_125): interpretation5_integrationTimeUnits: NULL has
been replaced by ‘years’
- d18O (Ocean2kHR_125): interpretation5_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_125): interpretation5_rank: NULL has been replaced
by ‘2’
- d18O (Ocean2kHR_125): interpretation5_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_125): interpretation5_variable: NULL has been
replaced by ‘seawaterIsotope’
- d18O (Ocean2kHR_125): interpretation5_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (Ocean2kHR_125): interpretation5_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_125): interpretation5_variableGroupOriginal: NULL
has been replaced by ‘d18O_seawater’
- d18O (Ocean2kHR_125): interpretation6_scope: NULL has been replaced
by ‘isotope’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-08 22:53:26.715248 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_124): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_124): interpretation2_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d18O (Ocean2kHR_124): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_124): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- d18O (Ocean2kHR_125): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_125): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_125): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-08 22:53:26.461014 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_124): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_124): interpretation2_seasonality: ‘annual’ has been
replaced by ‘Annual’
- d18O (Ocean2kHR_124): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_124): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
- d18O (Ocean2kHR_125): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_125): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_125): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:30:20.161479 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- year (MAT489b5e257f): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT489b5e257f): paleoData_longName: NULL has been replaced by
‘AD’
- year (MATa3aa118919): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MATa3aa118919): paleoData_longName: NULL has been replaced by
‘AD’
- d18O (Ocean2kHR_124): paleoData_longName: NULL has been replaced by
‘AD’
- d18O (Ocean2kHR_125): paleoData_longName: NULL has been replaced by
‘AD’