Version history for ToPssJKe7rwUBIS3l5aK - CO04ZIMG
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2025-05-20 16:18:33.138835 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT4c306207d3): interpretation3_scope: NULL has been replaced
by ‘climate’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:03:57.226234 UTC
- changes:
- Paleo Column metadata:
- year (MAT4c306207d3): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT4c306207d3): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- d18O (Ocean2kHR_020): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (Ocean2kHR_020): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:13:30.617125 UTC
- changes:
- Paleo Interpretation metadata:
- year (MAT4c306207d3): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT4c306207d3): interpretation2_scope: NULL has been replaced
by ‘climate’
- d18O (Ocean2kHR_020): interpretation2_basis: ‘A correlation of
seasonal mean rainfall anomalies derived from the NCEP/NCAR reanalysis
data set (1948-1995; averaged over 3545E, 20-30S; http://www.
cdc.noaa.gov/cdc/data.ncep.reanalysis.derived.html) with coral d18O
shows a clear relationship during austral summer (NDJF) significant
above the 90% level (Fig. 6). This also holds for a correlation with
South African summer rainfall averaged over 25-30E and 15-25S
(significant N95%) (Fig. 6). Thus, summer coral d18O is also related to
changes in the regional hydrologic (P/E) balance’ has been replaced by
NULL
- d18O (Ocean2kHR_020): interpretation2_direction: ‘negative’ has been
replaced by NULL
- d18O (Ocean2kHR_020): interpretation2_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_020): interpretation2_integrationTime: ‘2-Jan’ has
been replaced by NULL
- d18O (Ocean2kHR_020): interpretation2_integrationTimeBasis: ‘We use
the pronounced seasonal cycle in d18O and Sr/Ca to develop the final
chronology of the coral core and assigned the highest d18O and Sr/Ca
values to august 15 of each year, which is on average the coldest month.
[…] The d18O and Sr/Ca time series were interpolated linearly into 6 and
12 equi- distant points for any given year between these anchor points
using the Analyseries software,.083 to 0.167 yrs,chronological,months,on
a seasonal scale coral d18O and Sr/Ca at this location primarily
reflects SST variability (Fig. 5; Table 1). “’ has been replaced by
NULL
- d18O (Ocean2kHR_020):
interpretation2_integrationTimeUncertaintyType: ‘decrease’ has been
replaced by NULL
- d18O (Ocean2kHR_020): interpretation2_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (Ocean2kHR_020): interpretation2_rank: ‘1’ has been replaced by
NULL
- d18O (Ocean2kHR_020): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_020): interpretation2_seasonality: ‘subannual’ has
been replaced by NULL
- d18O (Ocean2kHR_020): interpretation2_variable: ‘temperature’ has
been replaced by NULL
- d18O (Ocean2kHR_020): interpretation2_variableGroup: ‘Temperature’
has been replaced by NULL
- d18O (Ocean2kHR_020): interpretation2_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (Ocean2kHR_020): interpretation2_variableGroupOriginal:
‘T_water’ has been replaced by NULL
- d18O (Ocean2kHR_020): interpretation3_direction: ‘2’ has been
replaced by NULL
- d18O (Ocean2kHR_020): interpretation3_inferredMaterial: ‘seawater’
has been replaced by NULL
- d18O (Ocean2kHR_020): interpretation3_integrationTime: ‘2-Jan’ has
been replaced by NULL
- d18O (Ocean2kHR_020): interpretation3_integrationTimeBasis: ‘We use
the pronounced seasonal cycle in d18O and Sr/Ca to develop the final
chronology of the coral core and assigned the highest d18O and Sr/Ca
values to august 15 of each year, which is on average the coldest month.
[…] The d18O and Sr/Ca time series were interpolated linearly into 6 and
12 equi- distant points for any given year between these anchor points
using the Analyseries software|.083 to 0.167 yrs|chronological|months|on
a seasonal scale coral d18O and Sr/Ca at this location primarily
reflects SST variability (Fig. 5; Table 1). “’ has been replaced by
NULL
- d18O (Ocean2kHR_020):
interpretation3_integrationTimeUncertaintyType: ‘decrease’ has been
replaced by NULL
- d18O (Ocean2kHR_020): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (Ocean2kHR_020): interpretation4_integrationTimeBasis: ‘We use
the pronounced seasonal cycle in d18O and Sr/Ca to develop the final
chronology of the coral core and assigned the highest d18O and Sr/Ca
values to august 15 of each year, which is on average the coldest month.
[…] The d18O and Sr/Ca time series were interpolated linearly into 6 and
12 equi- distant points for any given year between these anchor points
using the Analyseries software|.083 to 0.167 yrs|chronological|months|on
a seasonal scale coral d18O and Sr/Ca at this location primarily
reflects SST variability (Fig. 5; Table 1). “’ has been replaced by ‘We
use the pronounced seasonal cycle in d18O and Sr/Ca to develop the final
chronology of the coral core and assigned the highest d18O and Sr/Ca
values to august 15 of each year, which is on average the coldest month.
[…] The d18O and Sr/Ca time series were interpolated linearly into 6 and
12 equi- distant points for any given year between these anchor points
using the Analyseries software,.083 to 0.167 yrs,chronological,months,on
a seasonal scale coral d18O and Sr/Ca at this location primarily
reflects SST variability (Fig. 5; Table 1). “’
- d18O (Ocean2kHR_020): interpretation4_mathematicalRelation: ‘Sr/Ca
avaiable for select intervals’ has been replaced by ‘linear’
- d18O (Ocean2kHR_020): interpretation4_variableGroup: ‘JZ, NJA’ has
been replaced by ‘Temperature’
- d18O (Ocean2kHR_020): interpretation4_basis: NULL has been replaced
by ‘A correlation of seasonal mean rainfall anomalies derived from the
NCEP/NCAR reanalysis data set (1948-1995; averaged over 3545E, 20-30S;
http://www.
cdc.noaa.gov/cdc/data.ncep.reanalysis.derived.html) with coral d18O
shows a clear relationship during austral summer (NDJF) significant
above the 90% level (Fig. 6). This also holds for a correlation with
South African summer rainfall averaged over 25-30E and 15-25S
(significant N95%) (Fig. 6). Thus, summer coral d18O is also related to
changes in the regional hydrologic (P/E) balance’
- d18O (Ocean2kHR_020): interpretation4_direction: NULL has been
replaced by ‘negative’
- d18O (Ocean2kHR_020): interpretation4_rank: NULL has been replaced
by ‘1’
- d18O (Ocean2kHR_020): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- d18O (Ocean2kHR_020): interpretation4_variableGroupDirection: NULL
has been replaced by ‘negative’
- d18O (Ocean2kHR_020): interpretation4_variableGroupOriginal: NULL
has been replaced by ‘T_water’
- d18O (Ocean2kHR_020): interpretation5_direction: NULL has been
replaced by ‘2’
- d18O (Ocean2kHR_020): interpretation5_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_020): interpretation5_integrationTime: NULL has been
replaced by ‘2-Jan’
- d18O (Ocean2kHR_020): interpretation5_integrationTimeBasis: NULL has
been replaced by ‘We use the pronounced seasonal cycle in d18O and Sr/Ca
to develop the final chronology of the coral core and assigned the
highest d18O and Sr/Ca values to august 15 of each year, which is on
average the coldest month. […] The d18O and Sr/Ca time series were
interpolated linearly into 6 and 12 equi- distant points for any given
year between these anchor points using the Analyseries software|.083 to
0.167 yrs|chronological|months|on a seasonal scale coral d18O and Sr/Ca
at this location primarily reflects SST variability (Fig. 5; Table 1).
“’
- d18O (Ocean2kHR_020):
interpretation5_integrationTimeUncertaintyType: NULL has been replaced
by ‘decrease’
- d18O (Ocean2kHR_020): interpretation5_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_020): interpretation6_inferredMaterial: NULL has
been replaced by ‘seawater’
- d18O (Ocean2kHR_020): interpretation6_integrationTime: NULL has been
replaced by ‘2-Jan’
- d18O (Ocean2kHR_020): interpretation6_integrationTimeBasis: NULL has
been replaced by ‘We use the pronounced seasonal cycle in d18O and Sr/Ca
to develop the final chronology of the coral core and assigned the
highest d18O and Sr/Ca values to august 15 of each year, which is on
average the coldest month. […] The d18O and Sr/Ca time series were
interpolated linearly into 6 and 12 equi- distant points for any given
year between these anchor points using the Analyseries software|.083 to
0.167 yrs|chronological|months|on a seasonal scale coral d18O and Sr/Ca
at this location primarily reflects SST variability (Fig. 5; Table 1).
“’
- d18O (Ocean2kHR_020):
interpretation6_integrationTimeUncertaintyType: NULL has been replaced
by ‘decrease’
- d18O (Ocean2kHR_020): interpretation6_mathematicalRelation: NULL has
been replaced by ‘Sr/Ca avaiable for select intervals’
- d18O (Ocean2kHR_020): interpretation6_scope: NULL has been replaced
by ‘isotope’
- d18O (Ocean2kHR_020): interpretation6_variable: NULL has been
replaced by ‘temperature’
- d18O (Ocean2kHR_020): interpretation6_variableGroup: NULL has been
replaced by ‘JZ, NJA’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-08 23:24:45.293586 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_020): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- d18O (Ocean2kHR_020): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (Ocean2kHR_020): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_020): interpretation4_variable: ‘JZ, NJA’ has been
replaced by ‘temperature’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-08 23:24:44.601386 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (Ocean2kHR_020): interpretation1_seasonality: ‘not applicable
(subannually resolved)’ has been replaced by ‘subannual’
- d18O (Ocean2kHR_020): interpretation1_variable: ‘temperature and
salinity’ has been replaced by ‘temperature’
- d18O (Ocean2kHR_020): interpretation2_variable: ‘T_water’ has been
replaced by ‘temperature’
- d18O (Ocean2kHR_020): interpretation4_variable: ‘JZ, NJA’ has been
replaced by ‘temperature’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:30:22.434892 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- year (MAT4c306207d3): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT4c306207d3): paleoData_longName: NULL has been replaced by
‘AD’
- d18O (Ocean2kHR_020): paleoData_longName: NULL has been replaced by
‘AD’