Version history for STfvZZbTivYEfORIuIGG - CO02KUBE
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:03:55.377602 UTC
- changes:
- Paleo Column metadata:
- year (MAT40723aa780): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT40723aa780): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- year (MATd5acec6c03): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MATd5acec6c03): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- d18O (Ocean2kHR_102): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (Ocean2kHR_102): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- Sr/Ca (Ocean2kHR_103): paleoData_isPrimary: NULL has been replaced
by ‘FALSE’
- Sr/Ca (Ocean2kHR_103): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:10:24.727527 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT40723aa780): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MATd5acec6c03): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (Ocean2kHR_102): interpretation2_basis: ‘This coral was not
directly calibrated since the top is not modern. They used other
calibrations (Porites), and not from Diploria labyrinthiformis. Using
more recent Goodkin calibration would be applicable to this coral. “we
used calibrations from the Atlantic and Pacific Oceans. For estimating
temperatures from coral skeletal d18O we used the gradient of the
temperature to N18O equation of Leder et al. (1996) obtained from
Florida corals (4.52i¿½C per mil in d18O).’ has been replaced by
NULL
- d18O (Ocean2kHR_102): interpretation2_direction: ‘negative’ has been
replaced by NULL
- d18O (Ocean2kHR_102): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_102): interpretation2_integrationTime: ‘~15
samples/year’ has been replaced by NULL
- d18O (Ocean2kHR_102): interpretation2_integrationTimeBasis: ‘The top
and base of the core section were U/Th-dated (measured at the Institut
fur Umweltphysik, Heidelberg, Germany), with a precision of �15 yr. The
midpoint of the top dated sample is 14 density band couplets above the
profile for geochemical measurements, and the midpoint of the bottom
dated sample is seven band couplets below the profile (Fig. 2). In other
words, the age model within the chronology is based on the annual
banding. According to band couplet counts and the number of annual
cycles in the d18O, the U/Th-dated sections differ in age by 104 yr,
while the difference is 130 yr according to their radiometric dates
(base: 1499, top: 1629 AD). To remove the surplus of 26 yr we adjusted
the radiometric ages by adding 13 yr to the bottom and subtracting 13 yr
from the top sample age. Therefore, individual years in our record are
correct with respect to their positions within the time series, but they
do not necessarily match calendar years. Years in the isotopic record
are defined by cyclic variations in d18O, which are assumed to be
annual, with each cycle spanning ca. 2.5-4 mm core length. Subannual
dating is based on the annual d18O cycles, where the most positive d18O
value in each cycle is assigned to the coldest average month, which, for
Bermuda, is March. This introduces a non-cumulative error of
approximately �1 month. The ages of other sampling points were linearly
interpolated according to their spatial distances along the sampling
profile.’ has been replaced by NULL
- d18O (Ocean2kHR_102): interpretation2_integrationTimeUncertainty:
‘15 years interannual and 1 month subannual’ has been replaced by
NULL
- d18O (Ocean2kHR_102):
interpretation2_integrationTimeUncertaintyType: ‘U-Th dating
uncertainty’ has been replaced by NULL
- d18O (Ocean2kHR_102): interpretation2_integrationTimeUnits: ‘Varies
needs to be interpolated’ has been replaced by NULL
- d18O (Ocean2kHR_102): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_102): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (Ocean2kHR_102): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_102): interpretation2_seasonality: ‘subannual’ has
been replaced by NULL
- d18O (Ocean2kHR_102): interpretation2_variable: ‘temperature’ has
been replaced by NULL
- d18O (Ocean2kHR_102): interpretation2_variableGroup: ‘Temperature’
has been replaced by NULL
- d18O (Ocean2kHR_102): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_102): interpretation2_variableGroupOriginal:
‘T_water’ has been replaced by NULL
- d18O (Ocean2kHR_102): interpretation3_scope: NULL has been replaced
by ‘climate’
- d18O (Ocean2kHR_102): interpretation4_basis: NULL has been replaced
by ‘This coral was not directly calibrated since the top is not modern.
They used other calibrations (Porites), and not from Diploria
labyrinthiformis. Using more recent Goodkin calibration would be
applicable to this coral. “we used calibrations from the Atlantic and
Pacific Oceans. For estimating temperatures from coral skeletal d18O we
used the gradient of the temperature to N18O equation of Leder et
al. (1996) obtained from Florida corals (4.52i¿½C per mil in
d18O).’
- d18O (Ocean2kHR_102): interpretation4_direction: NULL has been
replaced by ‘negative’
- d18O (Ocean2kHR_102): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_102): interpretation4_integrationTime: NULL has been
replaced by ‘~15 samples/year’
- d18O (Ocean2kHR_102): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘The top and base of the core section were U/Th-dated
(measured at the Institut fur Umweltphysik, Heidelberg, Germany), with a
precision of �15 yr. The midpoint of the top dated sample is 14 density
band couplets above the profile for geochemical measurements, and the
midpoint of the bottom dated sample is seven band couplets below the
profile (Fig. 2). In other words, the age model within the chronology is
based on the annual banding. According to band couplet counts and the
number of annual cycles in the d18O, the U/Th-dated sections differ in
age by 104 yr, while the difference is 130 yr according to their
radiometric dates (base: 1499, top: 1629 AD). To remove the surplus of
26 yr we adjusted the radiometric ages by adding 13 yr to the bottom and
subtracting 13 yr from the top sample age. Therefore, individual years
in our record are correct with respect to their positions within the
time series, but they do not necessarily match calendar years. Years in
the isotopic record are defined by cyclic variations in d18O, which are
assumed to be annual, with each cycle spanning ca. 2.5-4 mm core length.
Subannual dating is based on the annual d18O cycles, where the most
positive d18O value in each cycle is assigned to the coldest average
month, which, for Bermuda, is March. This introduces a non-cumulative
error of approximately �1 month. The ages of other sampling points were
linearly interpolated according to their spatial distances along the
sampling profile.’
- d18O (Ocean2kHR_102): interpretation4_integrationTimeUncertainty:
NULL has been replaced by ‘15 years interannual and 1 month
subannual’
- d18O (Ocean2kHR_102):
interpretation4_integrationTimeUncertaintyType: NULL has been replaced
by ‘U-Th dating uncertainty’
- d18O (Ocean2kHR_102): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘Varies needs to be interpolated’
- d18O (Ocean2kHR_102): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (Ocean2kHR_102): interpretation4_rank: NULL has been replaced
by ‘1’
- d18O (Ocean2kHR_102): interpretation4_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_102): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- d18O (Ocean2kHR_102): interpretation4_variable: NULL has been
replaced by ‘temperature’
- d18O (Ocean2kHR_102): interpretation4_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (Ocean2kHR_102): interpretation4_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_102): interpretation4_variableGroupOriginal: NULL
has been replaced by ‘T_water’
- d18O (Ocean2kHR_102): interpretation5_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_102): interpretation6_scope: NULL has been replaced
by ‘isotope’
- Sr/Ca (Ocean2kHR_103): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- Sr/Ca (Ocean2kHR_103): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- Sr/Ca (Ocean2kHR_103): interpretation3_scope: NULL has been replaced
by ‘climate’
- Sr/Ca (Ocean2kHR_103): interpretation4_inferredMaterial: NULL has
been replaced by ‘seawater’
- Sr/Ca (Ocean2kHR_103): interpretation4_scope: NULL has been replaced
by ‘isotope’
- Sr/Ca (Ocean2kHR_103): interpretation5_scope: NULL has been replaced
by ‘isotope’
- Sr/Ca (Ocean2kHR_103): interpretation6_scope: NULL has been replaced
by ‘isotope’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-08 22:57:50.642826 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_102): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- d18O (Ocean2kHR_102): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_102): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- Sr/Ca (Ocean2kHR_103): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- Sr/Ca (Ocean2kHR_103): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-08 22:57:50.131564 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_102): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- d18O (Ocean2kHR_102): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_102): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- Sr/Ca (Ocean2kHR_103): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- Sr/Ca (Ocean2kHR_103): interpretation1_variable: ‘T’ has been
replaced by ‘temperature’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:30:20.76833 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- year (MAT40723aa780): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT40723aa780): paleoData_longName: NULL has been replaced by
‘AD’
- year (MATd5acec6c03): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MATd5acec6c03): paleoData_longName: NULL has been replaced by
‘AD’
- d18O (Ocean2kHR_102): paleoData_longName: NULL has been replaced by
‘AD’
- Sr/Ca (Ocean2kHR_103): paleoData_longName: NULL has been replaced by
‘AD’