Version history for yZ874JD7h0OCRUETqUrr - CO08HEVE
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2025-05-20 16:18:34.623013 UTC
- changes:
- Paleo Interpretation metadata:
- year (MATf8d8b6ebd4): interpretation4_scope: NULL has been replaced
by ‘climate’
- year (MATf8d8b6ebd4): interpretation5_scope: NULL has been replaced
by ‘climate’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:03:58.619838 UTC
- changes:
- Paleo Column metadata:
- year (MATf8d8b6ebd4): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MATf8d8b6ebd4): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- d18O (Ocean2kHR_096): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (Ocean2kHR_096): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:13:37.576256 UTC
- changes:
- Paleo Interpretation metadata:
- year (MATf8d8b6ebd4): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MATf8d8b6ebd4): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MATf8d8b6ebd4): interpretation3_scope: NULL has been replaced
by ‘climate’
- d18O (Ocean2kHR_096): interpretation2_basis: ‘Hetzinger 2006
calibration and general d18O to SST slope for corals used (-0.2)’ has
been replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_coefficient: ‘-0.2’ has been
replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_direction: ‘negative’ has been
replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_fraction: ‘0.3364’ has been
replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_integrationTime: ‘1’ has been
replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_integrationTimeBasis:
‘Chronology was developed on the basis of the seasonal cycle in coral
?18O, and by counting the well-developed annual density bands. The coral
?18O-record extends from 1918 to 2004. The measured skeletal d18O
minimum (maximum) was assigned to the month September (February) which
represents the average seasonal SST maximum (minimum) at the study site.
Linear interpolation was used in order to obtain monthly resolution for
statistical analysis.’ has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_integrationTimeUncertainty:
‘~1?2 months in any given year, no errors given for annual chronology’
has been replaced by NULL
- d18O (Ocean2kHR_096):
interpretation2_integrationTimeUncertaintyType: ‘chronological’ has been
replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_integrationTimeUnits: ‘month’
has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (Ocean2kHR_096): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_096): interpretation2_seasonality: ‘subannual’ has
been replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_variable: ‘temperature’ has
been replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_variableGroup: ‘Temperature’
has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation2_variableGroupOriginal:
‘T_water’ has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_basis: ‘However, the magnitude
of the multidecadal variations in coral d18O is larger than expected
based on SST alone. The standard deviation of the smoothed SST index
shown in Figure 1B is 0.12i¿½C (based on SST from the HadISSTv.1.1
database; Rayner et al., 2003), while the standard deviation of coral
!18O is 0.06?, which would correspond to 0.3 i¿½C, assuming
well-established relationships. Hence, ~50% of the amplitude is due to
variations in d18Oseawater. The d18Oseawater contribution is estimated
by calculating the d18Oresidual (i.e., by subtracting the SST component
from measured coral d18O; for details see GSA Data Repository). Figure
1C compares the d18Oresidual with a regional precipitation index
computed from weather stations in the southeastern Caribbean, which
includes the study site. The d18Oresidual and precipitation are highly
correlated at low frequencies, implying that multidecadal d18Oseawater
variations are primarily atmosphere-driven (r = ?0.46; 1923?1998; and r
= ?0.67 for detrended values).’ has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_direction: ‘negative’ has been
replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_integrationTime: ‘1’ has been
replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_integrationTimeBasis:
‘Chronology was developed on the basis of the seasonal cycle in coral
?18O, and by counting the well-developed annual density bands. The coral
?18O-record extends from 1918 to 2004. The measured skeletal d18O
minimum (maximum) was assigned to the month September (February) which
represents the average seasonal SST maximum (minimum) at the study site.
Linear interpolation was used in order to obtain monthly resolution for
statistical analysis.’ has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_integrationTimeUncertainty:
‘~1?2 months in any given year, no errors given for annual chronology’
has been replaced by NULL
- d18O (Ocean2kHR_096):
interpretation3_integrationTimeUncertaintyType: ‘chronological’ has been
replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_integrationTimeUnits: ‘month’
has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_rank: ‘2’ has been replaced by
NULL
- d18O (Ocean2kHR_096): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_096): interpretation3_variable: ‘seawaterIsotope’
has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation3_variableGroupOriginal:
‘d18O_seawater’ has been replaced by NULL
- d18O (Ocean2kHR_096): interpretation4_basis: NULL has been replaced
by ‘Hetzinger 2006 calibration and general d18O to SST slope for corals
used (-0.2)’
- d18O (Ocean2kHR_096): interpretation4_coefficient: NULL has been
replaced by ‘-0.2’
- d18O (Ocean2kHR_096): interpretation4_direction: NULL has been
replaced by ‘negative’
- d18O (Ocean2kHR_096): interpretation4_fraction: NULL has been
replaced by ‘0.3364’
- d18O (Ocean2kHR_096): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_096): interpretation4_integrationTime: NULL has been
replaced by ‘1’
- d18O (Ocean2kHR_096): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘Chronology was developed on the basis of the seasonal
cycle in coral ?18O, and by counting the well-developed annual density
bands. The coral ?18O-record extends from 1918 to 2004. The measured
skeletal d18O minimum (maximum) was assigned to the month September
(February) which represents the average seasonal SST maximum (minimum)
at the study site. Linear interpolation was used in order to obtain
monthly resolution for statistical analysis.’
- d18O (Ocean2kHR_096): interpretation4_integrationTimeUncertainty:
NULL has been replaced by ‘~1?2 months in any given year, no errors
given for annual chronology’
- d18O (Ocean2kHR_096):
interpretation4_integrationTimeUncertaintyType: NULL has been replaced
by ‘chronological’
- d18O (Ocean2kHR_096): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘month’
- d18O (Ocean2kHR_096): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_096): interpretation4_rank: NULL has been replaced
by ‘1’
- d18O (Ocean2kHR_096): interpretation4_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_096): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- d18O (Ocean2kHR_096): interpretation4_variable: NULL has been
replaced by ‘temperature’
- d18O (Ocean2kHR_096): interpretation4_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (Ocean2kHR_096): interpretation4_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_096): interpretation4_variableGroupOriginal: NULL
has been replaced by ‘T_water’
- d18O (Ocean2kHR_096): interpretation5_basis: NULL has been replaced
by ‘However, the magnitude of the multidecadal variations in coral d18O
is larger than expected based on SST alone. The standard deviation of
the smoothed SST index shown in Figure 1B is 0.12i¿½C (based on SST from
the HadISSTv.1.1 database; Rayner et al., 2003), while the standard
deviation of coral !18O is 0.06?, which would correspond to 0.3 i¿½C,
assuming well-established relationships. Hence, ~50% of the amplitude is
due to variations in d18Oseawater. The d18Oseawater contribution is
estimated by calculating the d18Oresidual (i.e., by subtracting the SST
component from measured coral d18O; for details see GSA Data
Repository). Figure 1C compares the d18Oresidual with a regional
precipitation index computed from weather stations in the southeastern
Caribbean, which includes the study site. The d18Oresidual and
precipitation are highly correlated at low frequencies, implying that
multidecadal d18Oseawater variations are primarily atmosphere-driven (r
= ?0.46; 1923?1998; and r = ?0.67 for detrended values).’
- d18O (Ocean2kHR_096): interpretation5_direction: NULL has been
replaced by ‘negative’
- d18O (Ocean2kHR_096): interpretation5_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_096): interpretation5_integrationTime: NULL has been
replaced by ‘1’
- d18O (Ocean2kHR_096): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘Chronology was developed on the basis of the seasonal
cycle in coral ?18O, and by counting the well-developed annual density
bands. The coral ?18O-record extends from 1918 to 2004. The measured
skeletal d18O minimum (maximum) was assigned to the month September
(February) which represents the average seasonal SST maximum (minimum)
at the study site. Linear interpolation was used in order to obtain
monthly resolution for statistical analysis.’
- d18O (Ocean2kHR_096): interpretation5_integrationTimeUncertainty:
NULL has been replaced by ‘~1?2 months in any given year, no errors
given for annual chronology’
- d18O (Ocean2kHR_096):
interpretation5_integrationTimeUncertaintyType: NULL has been replaced
by ‘chronological’
- d18O (Ocean2kHR_096): interpretation5_integrationTimeUnits: NULL has
been replaced by ‘month’
- d18O (Ocean2kHR_096): interpretation5_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_096): interpretation5_rank: NULL has been replaced
by ‘2’
- d18O (Ocean2kHR_096): interpretation5_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_096): interpretation5_variable: NULL has been
replaced by ‘seawaterIsotope’
- d18O (Ocean2kHR_096): interpretation5_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d18O (Ocean2kHR_096): interpretation5_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_096): interpretation5_variableGroupOriginal: NULL
has been replaced by ‘d18O_seawater’
- d18O (Ocean2kHR_096): interpretation6_scope: NULL has been replaced
by ‘isotope’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 20:52:14.459008 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_096): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- d18O (Ocean2kHR_096): interpretation1_variable: ‘temperature and
precipitation’ has been replaced by ‘temperature’
- d18O (Ocean2kHR_096): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_096): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-09 17:37:30.976567 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_096): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- d18O (Ocean2kHR_096): interpretation1_variable: ‘temperature and
precipitation’ has been replaced by ‘temperature’
- d18O (Ocean2kHR_096): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_096): interpretation3_variable: ‘d18O_seawater’ has
been replaced by ‘seawaterIsotope’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:30:23.972004 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- year (MATf8d8b6ebd4): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MATf8d8b6ebd4): paleoData_longName: NULL has been replaced by
‘AD’
- d18O (Ocean2kHR_096): paleoData_longName: NULL has been replaced by
‘AD’