Version history for kU3VWOpBh8HXKOjuwN18 - CO14WUCL
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:04:01.209302 UTC
- changes:
- Paleo Column metadata:
- d18O (CO14WUCL01A): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d18O (CO14WUCL01A): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- year (MATf94ce6eaeb): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MATf94ce6eaeb): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:13:39.482783 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (CO14WUCL01A): interpretation1_direction: ‘negative’ has been
replaced by NULL
- d18O (CO14WUCL01A): interpretation1_inferredMaterial: ‘seawater’ has
been replaced by NULL
- d18O (CO14WUCL01A): interpretation1_integrationTime: ‘1’ has been
replaced by NULL
- d18O (CO14WUCL01A): interpretation1_integrationTimeBasis: ‘The age
of colony CF1B was determined by 230Th/U-dating following established
methodology (Edwards et al., 1987; Shen et al., 2002).Three dates were
performed at the top, middle, and bottom of the CF1B core. All ages were
corrected for the effect of detrital Th contamination assuming a bulk
earth 232Th/238U weight ratio of 3.8 for the detritus and 230Th, 234U,
and 238U in secular equilibri- um. The reliability of the determined
230Th/U-ages was verified using established criteria such as initial
234U/238U in agreement with 234U/ 238U of modern seawater (i.e., 146 �
3?) (Shen et al., 2008).,5 years,U/Th
error,month,,,,,,,,,,,,,,,,,,,,,,,,,Fossil coral - this record was used
to determine the variability of d18Osw by deconvoluing the d18O signal
using Sr/Ca data,,https://docs.google.com/spreadsheets/d/1MjIjGINZkkCuTq4taZWDJS0Ddmx_knTJApUoI8PiNao
Ocean2kHR_026,CO14ZIHO,Ocn_154,CO14ZIHO01A,coral,zinke2014corals,Zinke,
J. , Rountrey, A. , Feng, M. , Xie, S.-P. , Dissard, D. , Rankenburg, K.
, Lough, J.M. , McCulloch, M.T.,2014,10.1038/ncomms4607,Zinke, J., A.
Rountrey, M. Feng, S.P. Xie, D. Dissard, K. Rankenburg, J. Lough, and
M.T. McCulloch. 2014. Corals record long-term Leeuwin Current
variability including Ningaloo Ni�o/Ni�a since 1795. Nature
Communications, 5, 3607. doi: 10.1038/ncomms4607,,,,,,Zinke,
J.,zinke2014ocean2khrDataCitation,World Data Center for
Paleoclimatology,
,Ocean2kHR-IndianAbrolhosZinke2014HAB10A,dataCitation,https://www.ncdc.noaa.gov/paleo/study/16316,-28.4589,113.749,-8,Houtman
Abrolhos,1848,2010,x_18O,?,?18O of the coral skeleton,;
climateInterpretation_seasonality changed - was originally 1 2 3 4 5 6 7
8 9 10 11 12,coral carbonate,T,sea_surface,1 2 3 4 5 6 7 8 9 10 11
12,negative,,,seawater,1,We used the published bimonthly coral d18O
record of Kuhnert et al.12 as our reference coral because the presence
of seasonal cycles provided the best age control for all cores.The age
model of the new corals was determined by assigning 1 year of growth to
a couplet of high- and low-density banding in X-ray-positive prints
cross-checked with luminescence banding. The high-density bands were
equivalent to summer and low density to winter. The coral d18O record of
Kuhnert et al. was averaged annually (January?December), and then each
individual annually resolved coral proxy record was normalized to its
variance relative to the 1900?1993 reference period. We used the COFECHA
tool to aid in cross-dating the annual time series. We aligned the new
annually resolved Sr/Ca and d18O records (normalized relative to the
1900?1993 reference period) with the Kuhnert et al. annual time series,
and averaged all records to form a composite chronology that extends
from 1795 to 2010.”’ has been replaced by NULL
- d18O (CO14WUCL01A): interpretation1_integrationTimeUnits: ‘year’ has
been replaced by NULL
- d18O (CO14WUCL01A): interpretation1_mathematicalRelation: ‘linear’
has been replaced by NULL
- d18O (CO14WUCL01A): interpretation1_rank: ‘1’ has been replaced by
NULL
- d18O (CO14WUCL01A): interpretation1_scope: ‘isotope’ has been
replaced by ‘climate’
- d18O (CO14WUCL01A): interpretation1_seasonality: ‘subannual’ has
been replaced by NULL
- d18O (CO14WUCL01A): interpretation1_variable: ‘temperature’ has been
replaced by NULL
- d18O (CO14WUCL01A): interpretation1_variableGroup: ‘Temperature’ has
been replaced by NULL
- d18O (CO14WUCL01A): interpretation1_variableGroupDirection:
‘negative’ has been replaced by NULL
- d18O (CO14WUCL01A): interpretation1_variableGroupOriginal: ‘T_water’
has been replaced by NULL
- d18O (CO14WUCL01A): interpretation2_scope: NULL has been replaced by
‘climate’
- d18O (CO14WUCL01A): interpretation3_scope: NULL has been replaced by
‘climate’
- d18O (CO14WUCL01A): interpretation4_direction: NULL has been
replaced by ‘negative’
- d18O (CO14WUCL01A): interpretation4_inferredMaterial: NULL has been
replaced by ‘seawater’
- d18O (CO14WUCL01A): interpretation4_integrationTime: NULL has been
replaced by ‘1’
- d18O (CO14WUCL01A): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘The age of colony CF1B was determined by
230Th/U-dating following established methodology (Edwards et al., 1987;
Shen et al., 2002).Three dates were performed at the top, middle, and
bottom of the CF1B core. All ages were corrected for the effect of
detrital Th contamination assuming a bulk earth 232Th/238U weight ratio
of 3.8 for the detritus and 230Th, 234U, and 238U in secular equilibri-
um. The reliability of the determined 230Th/U-ages was verified using
established criteria such as initial 234U/238U in agreement with 234U/
238U of modern seawater (i.e., 146 � 3?) (Shen et al., 2008).,5
years,U/Th error,month,,,,,,,,,,,,,,,,,,,,,,,,,Fossil coral - this
record was used to determine the variability of d18Osw by deconvoluing
the d18O signal using Sr/Ca data,,https://docs.google.com/spreadsheets/d/1MjIjGINZkkCuTq4taZWDJS0Ddmx_knTJApUoI8PiNao
Ocean2kHR_026,CO14ZIHO,Ocn_154,CO14ZIHO01A,coral,zinke2014corals,Zinke,
J. , Rountrey, A. , Feng, M. , Xie, S.-P. , Dissard, D. , Rankenburg, K.
, Lough, J.M. , McCulloch, M.T.,2014,10.1038/ncomms4607,Zinke, J., A.
Rountrey, M. Feng, S.P. Xie, D. Dissard, K. Rankenburg, J. Lough, and
M.T. McCulloch. 2014. Corals record long-term Leeuwin Current
variability including Ningaloo Ni�o/Ni�a since 1795. Nature
Communications, 5, 3607. doi: 10.1038/ncomms4607,,,,,,Zinke,
J.,zinke2014ocean2khrDataCitation,World Data Center for
Paleoclimatology,
,Ocean2kHR-IndianAbrolhosZinke2014HAB10A,dataCitation,https://www.ncdc.noaa.gov/paleo/study/16316,-28.4589,113.749,-8,Houtman
Abrolhos,1848,2010,x_18O,?,?18O of the coral skeleton,;
climateInterpretation_seasonality changed - was originally 1 2 3 4 5 6 7
8 9 10 11 12,coral carbonate,T,sea_surface,1 2 3 4 5 6 7 8 9 10 11
12,negative,,,seawater,1,We used the published bimonthly coral d18O
record of Kuhnert et al.12 as our reference coral because the presence
of seasonal cycles provided the best age control for all cores.The age
model of the new corals was determined by assigning 1 year of growth to
a couplet of high- and low-density banding in X-ray-positive prints
cross-checked with luminescence banding. The high-density bands were
equivalent to summer and low density to winter. The coral d18O record of
Kuhnert et al. was averaged annually (January?December), and then each
individual annually resolved coral proxy record was normalized to its
variance relative to the 1900?1993 reference period. We used the COFECHA
tool to aid in cross-dating the annual time series. We aligned the new
annually resolved Sr/Ca and d18O records (normalized relative to the
1900?1993 reference period) with the Kuhnert et al. annual time series,
and averaged all records to form a composite chronology that extends
from 1795 to 2010.”’
- d18O (CO14WUCL01A): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘year’
- d18O (CO14WUCL01A): interpretation4_mathematicalRelation: NULL has
been replaced by ‘linear’
- d18O (CO14WUCL01A): interpretation4_rank: NULL has been replaced by
‘1’
- d18O (CO14WUCL01A): interpretation4_scope: NULL has been replaced by
‘isotope’
- d18O (CO14WUCL01A): interpretation4_seasonality: NULL has been
replaced by ‘subannual’
- d18O (CO14WUCL01A): interpretation4_variable: NULL has been replaced
by ‘temperature’
- d18O (CO14WUCL01A): interpretation4_variableGroup: NULL has been
replaced by ‘Temperature’
- d18O (CO14WUCL01A): interpretation4_variableGroupDirection: NULL has
been replaced by ‘negative’
- d18O (CO14WUCL01A): interpretation4_variableGroupOriginal: NULL has
been replaced by ‘T_water’
- d18O (CO14WUCL01A): interpretation5_scope: NULL has been replaced by
‘isotope’
- d18O (CO14WUCL01A): interpretation6_scope: NULL has been replaced by
‘isotope’
- year (MATf94ce6eaeb): interpretation1_scope: NULL has been replaced
by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 21:10:08.707703 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (CO14WUCL01A): interpretation1_variable: ‘T_water’ has been
replaced by ‘temperature’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-09 17:37:34.502613 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (CO14WUCL01A): interpretation1_variable: ‘T_water’ has been
replaced by ‘temperature’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:30:25.804222 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- d18O (CO14WUCL01A): paleoData_longName: NULL has been replaced by
‘AD’
- year (MATf94ce6eaeb): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MATf94ce6eaeb): paleoData_longName: NULL has been replaced by
‘AD’