Version history for qwzBpj4YBi4g9zSX21Vj -
KNI-51.Denniston.2013
Version: 1.0.18
- lastVersion: 1.0.17
- curator: nicholas
- timestamp: 2025-06-25 22:46:20.401947 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRhTtQNZMrVu): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LRhTtQNZMrVu): paleoData_QCCertification: ‘((( null ))) CH
/// CH, CR’ has been replaced by ‘CH, CR’
- d18O (S2LRhTtQNZMrVu): paleoData_QCnotes: ‘((( null ))) “For eight
of these 11 stalagmites, age models and oxygen isotopic ratios were
previously published (Denniston et al., 2013b); three KNI-51 stalagmite
records are newly reported here” (Denniston et al., 2017) (https://www.ncdc.noaa.gov/paleo-search/study/22990)
SISAL Note: “KNI-51-0 (entity_id = 331), KNI-51-3 (entity_id = 332),
KNI-51-4 (entity_id = 333), KNI-51-7 (entity_id = 334), KNI-51-10
(entity_id = 335), KNI-51-11 (entity_id = 336), KNI-51-A2-side1
(entity_id = 337), KNI-51-A2-side2 (entity_id = 338), KNI-51-C
(entity_id = 339), KNI-51-F (entity_id = 340), KNI-51-G (entity_id =
341), KNI-51-H (entity_id = 342), KNI-51-I (entity_id = 343), KNI-51-J
(entity_id = 344), KNI-51-N (entity_id = 345), KNI-51-O (entity_id =
346), KNI-51-A1 (entity_id = 418) and KNI-51-P (entity_id = 419): all
samples have been corrected by -1 permil to be a calcite equivalent. In
the original paper, entity KN51-10 was arbitrarily offset by -1 permil
to match other records; this offset has been removed. 234U/238U values
for KNI-51-1 (entity_id = 637) and KNI-51-8 (entity_id = 638) are
derived from d234U” /// Composite created from all stals (as in Figure 4
of Denniston et al., 2013). KNI-51-10 values adjusted by -1 (only in
composite) to match analysis of original paper. The adjustment was
removed by SISAL to provide raw data. “For eight of these 11
stalagmites, age models and oxygen isotopic ratios were previously
published (Denniston et al., 2013b); three KNI-51 stalagmite records are
newly reported here” (Denniston et al., 2017) (https://www.ncdc.noaa.gov/paleo-search/study/22990)
SISAL Note: “KNI-51-0 (entity_id = 331), KNI-51-3 (entity_id = 332),
KNI-51-4 (entity_id = 333), KNI-51-7 (entity_id = 334), KNI-51-10
(entity_id = 335), KNI-51-11 (entity_id = 336), KNI-51-A2-side1
(entity_id = 337), KNI-51-A2-side2 (entity_id = 338), KNI-51-C
(entity_id = 339), KNI-51-F (entity_id = 340), KNI-51-G (entity_id =
341), KNI-51-H (entity_id = 342), KNI-51-I (entity_id = 343), KNI-51-J
(entity_id = 344), KNI-51-N (entity_id = 345), KNI-51-O (entity_id =
346), KNI-51-A1 (entity_id = 418) and KNI-51-P (entity_id = 419): all
samples have been corrected by -1 permil to be a calcite equivalent. In
the original paper, entity KN51-10 was arbitrarily offset by -1 permil
to match other records; this offset has been removed. 234U/238U values
for KNI-51-1 (entity_id = 637) and KNI-51-8 (entity_id = 638) are
derived from d234U”’ has been replaced by ‘Composite created from all
stals (as in Figure 4 of Denniston et al., 2013). KNI-51-10 values
adjusted by -1 (only in composite) to match analysis of original paper.
The adjustment was removed by SISAL to provide raw data. “For eight of
these 11 stalagmites, age models and oxygen isotopic ratios were
previously published (Denniston et al., 2013b); three KNI-51 stalagmite
records are newly reported here” (Denniston et al., 2017) (https://www.ncdc.noaa.gov/paleo-search/study/22990)
SISAL Note: “KNI-51-0 (entity_id = 331), KNI-51-3 (entity_id = 332),
KNI-51-4 (entity_id = 333), KNI-51-7 (entity_id = 334), KNI-51-10
(entity_id = 335), KNI-51-11 (entity_id = 336), KNI-51-A2-side1
(entity_id = 337), KNI-51-A2-side2 (entity_id = 338), KNI-51-C
(entity_id = 339), KNI-51-F (entity_id = 340), KNI-51-G (entity_id =
341), KNI-51-H (entity_id = 342), KNI-51-I (entity_id = 343), KNI-51-J
(entity_id = 344), KNI-51-N (entity_id = 345), KNI-51-O (entity_id =
346), KNI-51-A1 (entity_id = 418) and KNI-51-P (entity_id = 419): all
samples have been corrected by -1 permil to be a calcite equivalent. In
the original paper, entity KN51-10 was arbitrarily offset by -1 permil
to match other records; this offset has been removed. 234U/238U values
for KNI-51-1 (entity_id = 637) and KNI-51-8 (entity_id = 638) are
derived from d234U”’
- Paleo Interpretation metadata:
- d18O (S2LRhTtQNZMrVu): interpretation1_variable: ‘((( null ))) M ///
precipitation’ has been replaced by ‘precipitation’
Version: 1.0.17
- lastVersion: 1.0.16
- curator: nicholas
- timestamp: 2025-06-25 21:22:01.647835 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRhTtQNZMrVu): paleoData_notes: ‘“increased monsoon rainfall
(lower d18O values) at KNI-51 coincides with increased rainfall
northward across the Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen
isotopic values in stalagmites are a commonly used proxy for tropical
paleohydrology and are related to amount effects in monsoon rainwater,
the primary source of oxygen in Speleothem carbonate. Analysis of d18O
values of precipitation from Darwin, Australia, the closest Global
Network of Isotopes in Precipitation station to either cave, are closely
tied to monthly precipitation amount” (Denniston et al., 2017)
“Stalagmite oxygen isotopic values track monsoon intensity via amount
effects in precipitation and reveal a dynamic Holocene IASM…interpreting
our stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)’
has been replaced by ‘((( null ))) “increased monsoon rainfall (lower
δ18O values) at KNI-51 coincides with increased rainfall northward
across the Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen isotopic
values in stalagmites are a commonly used proxy for tropical
paleohydrology and are related to amount effects in monsoon rainwater,
the primary source of oxygen in speleothem carbonate. Analysis of d18O
values of precipitation from Darwin, Australia, the closest Global
Network of Isotopes in Precipitation station to either cave, are closely
tied to monthly precipitation amount” (Denniston et al., 2017)
“Stalagmite oxygen isotopic values track monsoon intensity via amount
effects in precipitation and reveal a dynamic Holocene IASM…interpreting
our stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)
/// “increased monsoon rainfall (lower d18O values) at KNI-51 coincides
with increased rainfall northward across the Indo-Pacific TRB”
(Denniston et al., 2016) “Oxygen isotopic values in stalagmites are a
commonly used proxy for tropical paleohydrology and are related to
amount effects in monsoon rainwater, the primary source of oxygen in
Speleothem carbonate. Analysis of d18O values of precipitation from
Darwin, Australia, the closest Global Network of Isotopes in
Precipitation station to either cave, are closely tied to monthly
precipitation amount” (Denniston et al., 2017) “Stalagmite oxygen
isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al.,
2013)’
- d18O (S2LRhTtQNZMrVu): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LRhTtQNZMrVu): paleoData_QCCertification: ‘CH, CR’ has been
replaced by ‘((( null ))) CH /// CH, CR’
- d18O (S2LRhTtQNZMrVu): paleoData_QCnotes: ‘Composite created from
all stals (as in Figure 4 of Denniston et al., 2013). KNI-51-10 values
adjusted by -1 (only in composite) to match analysis of original paper.
The adjustment was removed by SISAL to provide raw data. “For eight of
these 11 stalagmites, age models and oxygen isotopic ratios were
previously published (Denniston et al., 2013b); three KNI-51 stalagmite
records are newly reported here” (Denniston et al., 2017) (https://www.ncdc.noaa.gov/paleo-search/study/22990)
SISAL Note: “KNI-51-0 (entity_id = 331), KNI-51-3 (entity_id = 332),
KNI-51-4 (entity_id = 333), KNI-51-7 (entity_id = 334), KNI-51-10
(entity_id = 335), KNI-51-11 (entity_id = 336), KNI-51-A2-side1
(entity_id = 337), KNI-51-A2-side2 (entity_id = 338), KNI-51-C
(entity_id = 339), KNI-51-F (entity_id = 340), KNI-51-G (entity_id =
341), KNI-51-H (entity_id = 342), KNI-51-I (entity_id = 343), KNI-51-J
(entity_id = 344), KNI-51-N (entity_id = 345), KNI-51-O (entity_id =
346), KNI-51-A1 (entity_id = 418) and KNI-51-P (entity_id = 419): all
samples have been corrected by -1 permil to be a calcite equivalent. In
the original paper, entity KN51-10 was arbitrarily offset by -1 permil
to match other records; this offset has been removed. 234U/238U values
for KNI-51-1 (entity_id = 637) and KNI-51-8 (entity_id = 638) are
derived from d234U”’ has been replaced by ‘((( null ))) “For eight of
these 11 stalagmites, age models and oxygen isotopic ratios were
previously published (Denniston et al., 2013b); three KNI-51 stalagmite
records are newly reported here” (Denniston et al., 2017) (https://www.ncdc.noaa.gov/paleo-search/study/22990)
SISAL Note: “KNI-51-0 (entity_id = 331), KNI-51-3 (entity_id = 332),
KNI-51-4 (entity_id = 333), KNI-51-7 (entity_id = 334), KNI-51-10
(entity_id = 335), KNI-51-11 (entity_id = 336), KNI-51-A2-side1
(entity_id = 337), KNI-51-A2-side2 (entity_id = 338), KNI-51-C
(entity_id = 339), KNI-51-F (entity_id = 340), KNI-51-G (entity_id =
341), KNI-51-H (entity_id = 342), KNI-51-I (entity_id = 343), KNI-51-J
(entity_id = 344), KNI-51-N (entity_id = 345), KNI-51-O (entity_id =
346), KNI-51-A1 (entity_id = 418) and KNI-51-P (entity_id = 419): all
samples have been corrected by -1 permil to be a calcite equivalent. In
the original paper, entity KN51-10 was arbitrarily offset by -1 permil
to match other records; this offset has been removed. 234U/238U values
for KNI-51-1 (entity_id = 637) and KNI-51-8 (entity_id = 638) are
derived from d234U” /// Composite created from all stals (as in Figure 4
of Denniston et al., 2013). KNI-51-10 values adjusted by -1 (only in
composite) to match analysis of original paper. The adjustment was
removed by SISAL to provide raw data. “For eight of these 11
stalagmites, age models and oxygen isotopic ratios were previously
published (Denniston et al., 2013b); three KNI-51 stalagmite records are
newly reported here” (Denniston et al., 2017) (https://www.ncdc.noaa.gov/paleo-search/study/22990)
SISAL Note: “KNI-51-0 (entity_id = 331), KNI-51-3 (entity_id = 332),
KNI-51-4 (entity_id = 333), KNI-51-7 (entity_id = 334), KNI-51-10
(entity_id = 335), KNI-51-11 (entity_id = 336), KNI-51-A2-side1
(entity_id = 337), KNI-51-A2-side2 (entity_id = 338), KNI-51-C
(entity_id = 339), KNI-51-F (entity_id = 340), KNI-51-G (entity_id =
341), KNI-51-H (entity_id = 342), KNI-51-I (entity_id = 343), KNI-51-J
(entity_id = 344), KNI-51-N (entity_id = 345), KNI-51-O (entity_id =
346), KNI-51-A1 (entity_id = 418) and KNI-51-P (entity_id = 419): all
samples have been corrected by -1 permil to be a calcite equivalent. In
the original paper, entity KN51-10 was arbitrarily offset by -1 permil
to match other records; this offset has been removed. 234U/238U values
for KNI-51-1 (entity_id = 637) and KNI-51-8 (entity_id = 638) are
derived from d234U”’
- d18O (S2LRhTtQNZMrVu): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d18O (S2LRhTtQNZMrVu): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- Paleo Interpretation metadata:
- d18O (S2LRhTtQNZMrVu): interpretation1_variable: ‘precipitation’ has
been replaced by ‘((( null ))) M /// precipitation’
Version: 1.0.15
- lastVersion: 1.0.14
- curator: nicholas
- timestamp: 2023-08-10 22:58:41 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_author: NULL has been replaced by ‘Rhawn F. Denniston and
Karl-Heinz Wyrwoll and Victor J. Polyak and Josephine R. Brown and
Yemane Asmerom and Alan D. Wanamaker and Zachary LaPointe and Rebecca
Ellerbroek and Michael Barthelmes and Daniel Cleary and John Cugley and
David Woods and William F. Humphreys’
- pub1_journal: NULL has been replaced by ‘Quaternary Science
Reviews’
- pub1_pages: NULL has been replaced by ‘155–168’
- pub1_title: NULL has been replaced by ‘A Stalagmite record of
Holocene Indonesian{textendash}Australian summer monsoon variability
from the Australian tropics’
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2023-05-31 20:39:10 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRhTtQNZMrVu): paleoData_notes: ‘((( ((( “increased monsoon
rainfall (lower ��18O values) at KNI-51 coincides with increased
rainfall northward across the Indo-Pacific TRB” (Denniston et al., 2016)
“Oxygen isotopic values in stalagmites are a commonly used proxy for
tropical paleohydrology and are related to amount effects in monsoon
rainwater, the primary source of oxygen in Speleothem carbonate.
Analysis of d18O values of precipitation from Darwin, Australia, the
closest Global Network of Isotopes in Precipitation station to either
cave, are closely tied to monthly precipitation amount” (Denniston et
al., 2017) “Stalagmite oxygen isotopic values track monsoon intensity
via amount effects in precipitation and reveal a dynamic Holocene
IASM…interpreting our stalagmite d18O time series as reflecting changes
in rainwater d18O values which, in turn, track monsoon strength”
(Denniston et al., 2013); paleoData_variableName updated ))) “increased
monsoon rainfall (lower δ18O values) at KNI-51 coincides with increased
rainfall northward across the Indo-Pacific TRB” (Denniston et al., 2016)
“Oxygen isotopic values in stalagmites are a commonly used proxy for
tropical paleohydrology and are related to amount effects in monsoon
rainwater, the primary source of oxygen in Speleothem carbonate.
Analysis of d18O values of precipitation from Darwin, Australia, the
closest Global Network of Isotopes in Precipitation station to either
cave, are closely tied to monthly precipitation amount” (Denniston et
al., 2017) “Stalagmite oxygen isotopic values track monsoon intensity
via amount effects in precipitation and reveal a dynamic Holocene
IASM…interpreting our stalagmite d18O time series as reflecting changes
in rainwater d18O values which, in turn, track monsoon strength”
(Denniston et al., 2013) /// “increased monsoon rainfall (lower δ18O
values) at KNI-51 coincides with increased rainfall northward across the
Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen isotopic values in
stalagmites are a commonly used proxy for tropical paleohydrology and
are related to amount effects in monsoon rainwater, the primary source
of oxygen in Speleothem carbonate. Analysis of d18O values of
precipitation from Darwin, Australia, the closest Global Network of
Isotopes in Precipitation station to either cave, are closely tied to
monthly precipitation amount” (Denniston et al., 2017) “Stalagmite
oxygen isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)
))) “increased monsoon rainfall (lower d18O values) at KNI-51 coincides
with increased rainfall northward across the Indo-Pacific TRB”
(Denniston et al., 2016) “Oxygen isotopic values in stalagmites are a
commonly used proxy for tropical paleohydrology and are related to
amount effects in monsoon rainwater, the primary source of oxygen in
Speleothem carbonate. Analysis of d18O values of precipitation from
Darwin, Australia, the closest Global Network of Isotopes in
Precipitation station to either cave, are closely tied to monthly
precipitation amount” (Denniston et al., 2017) “Stalagmite oxygen
isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)
/// “increased monsoon rainfall (lower δ18O values) at KNI-51 coincides
with increased rainfall northward across the Indo-Pacific TRB”
(Denniston et al., 2016) “Oxygen isotopic values in stalagmites are a
commonly used proxy for tropical paleohydrology and are related to
amount effects in monsoon rainwater, the primary source of oxygen in
Speleothem carbonate. Analysis of d18O values of precipitation from
Darwin, Australia, the closest Global Network of Isotopes in
Precipitation station to either cave, are closely tied to monthly
precipitation amount” (Denniston et al., 2017) “Stalagmite oxygen
isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)’
has been replaced by ‘“increased monsoon rainfall (lower d18O values) at
KNI-51 coincides with increased rainfall northward across the
Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen isotopic values in
stalagmites are a commonly used proxy for tropical paleohydrology and
are related to amount effects in monsoon rainwater, the primary source
of oxygen in Speleothem carbonate. Analysis of d18O values of
precipitation from Darwin, Australia, the closest Global Network of
Isotopes in Precipitation station to either cave, are closely tied to
monthly precipitation amount” (Denniston et al., 2017) “Stalagmite
oxygen isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al.,
2013)’
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2023-05-30 15:49:21 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRhTtQNZMrVu): paleoData_notes: ‘“increased monsoon rainfall
(lower δ18O values) at KNI-51 coincides with increased rainfall
northward across the Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen
isotopic values in stalagmites are a commonly used proxy for tropical
paleohydrology and are related to amount effects in monsoon rainwater,
the primary source of oxygen in Speleothem carbonate. Analysis of d18O
values of precipitation from Darwin, Australia, the closest Global
Network of Isotopes in Precipitation station to either cave, are closely
tied to monthly precipitation amount” (Denniston et al., 2017)
“Stalagmite oxygen isotopic values track monsoon intensity via amount
effects in precipitation and reveal a dynamic Holocene IASM…interpreting
our stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)’
has been replaced by ‘((( ((( “increased monsoon rainfall (lower ��18O
values) at KNI-51 coincides with increased rainfall northward across the
Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen isotopic values in
stalagmites are a commonly used proxy for tropical paleohydrology and
are related to amount effects in monsoon rainwater, the primary source
of oxygen in Speleothem carbonate. Analysis of d18O values of
precipitation from Darwin, Australia, the closest Global Network of
Isotopes in Precipitation station to either cave, are closely tied to
monthly precipitation amount” (Denniston et al., 2017) “Stalagmite
oxygen isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013);
paleoData_variableName updated ))) “increased monsoon rainfall (lower
δ18O values) at KNI-51 coincides with increased rainfall northward
across the Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen isotopic
values in stalagmites are a commonly used proxy for tropical
paleohydrology and are related to amount effects in monsoon rainwater,
the primary source of oxygen in Speleothem carbonate. Analysis of d18O
values of precipitation from Darwin, Australia, the closest Global
Network of Isotopes in Precipitation station to either cave, are closely
tied to monthly precipitation amount” (Denniston et al., 2017)
“Stalagmite oxygen isotopic values track monsoon intensity via amount
effects in precipitation and reveal a dynamic Holocene IASM…interpreting
our stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)
/// “increased monsoon rainfall (lower δ18O values) at KNI-51 coincides
with increased rainfall northward across the Indo-Pacific TRB”
(Denniston et al., 2016) “Oxygen isotopic values in stalagmites are a
commonly used proxy for tropical paleohydrology and are related to
amount effects in monsoon rainwater, the primary source of oxygen in
Speleothem carbonate. Analysis of d18O values of precipitation from
Darwin, Australia, the closest Global Network of Isotopes in
Precipitation station to either cave, are closely tied to monthly
precipitation amount” (Denniston et al., 2017) “Stalagmite oxygen
isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)
))) “increased monsoon rainfall (lower d18O values) at KNI-51 coincides
with increased rainfall northward across the Indo-Pacific TRB”
(Denniston et al., 2016) “Oxygen isotopic values in stalagmites are a
commonly used proxy for tropical paleohydrology and are related to
amount effects in monsoon rainwater, the primary source of oxygen in
Speleothem carbonate. Analysis of d18O values of precipitation from
Darwin, Australia, the closest Global Network of Isotopes in
Precipitation station to either cave, are closely tied to monthly
precipitation amount” (Denniston et al., 2017) “Stalagmite oxygen
isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)
/// “increased monsoon rainfall (lower δ18O values) at KNI-51 coincides
with increased rainfall northward across the Indo-Pacific TRB”
(Denniston et al., 2016) “Oxygen isotopic values in stalagmites are a
commonly used proxy for tropical paleohydrology and are related to
amount effects in monsoon rainwater, the primary source of oxygen in
Speleothem carbonate. Analysis of d18O values of precipitation from
Darwin, Australia, the closest Global Network of Isotopes in
Precipitation station to either cave, are closely tied to monthly
precipitation amount” (Denniston et al., 2017) “Stalagmite oxygen
isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al.,
2013)’
- d18O (S2LRhTtQNZMrVu): paleoData_QCCertification: ‘CH’ has been
replaced by ‘CH, CR’
- Paleo Interpretation metadata:
- d18O (S2LRhTtQNZMrVu): interpretation1_seasonalityGeneral:
‘summerOnly’ has been replaced by ‘Summer’
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-05-12 21:59:17 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRhTtQNZMrVu): paleoData_notes: ‘((( “increased monsoon
rainfall (lower ��18O values) at KNI-51 coincides with increased
rainfall northward across the Indo-Pacific TRB” (Denniston et al., 2016)
“Oxygen isotopic values in stalagmites are a commonly used proxy for
tropical paleohydrology and are related to amount effects in monsoon
rainwater, the primary source of oxygen in Speleothem carbonate.
Analysis of d18O values of precipitation from Darwin, Australia, the
closest Global Network of Isotopes in Precipitation station to either
cave, are closely tied to monthly precipitation amount” (Denniston et
al., 2017) “Stalagmite oxygen isotopic values track monsoon intensity
via amount effects in precipitation and reveal a dynamic Holocene
IASM…interpreting our stalagmite d18O time series as reflecting changes
in rainwater d18O values which, in turn, track monsoon strength”
(Denniston et al., 2013); paleoData_variableName updated ))) “increased
monsoon rainfall (lower δ18O values) at KNI-51 coincides with increased
rainfall northward across the Indo-Pacific TRB” (Denniston et al., 2016)
“Oxygen isotopic values in stalagmites are a commonly used proxy for
tropical paleohydrology and are related to amount effects in monsoon
rainwater, the primary source of oxygen in Speleothem carbonate.
Analysis of d18O values of precipitation from Darwin, Australia, the
closest Global Network of Isotopes in Precipitation station to either
cave, are closely tied to monthly precipitation amount” (Denniston et
al., 2017) “Stalagmite oxygen isotopic values track monsoon intensity
via amount effects in precipitation and reveal a dynamic Holocene
IASM…interpreting our stalagmite d18O time series as reflecting changes
in rainwater d18O values which, in turn, track monsoon strength”
(Denniston et al., 2013) /// “increased monsoon rainfall (lower δ18O
values) at KNI-51 coincides with increased rainfall northward across the
Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen isotopic values in
stalagmites are a commonly used proxy for tropical paleohydrology and
are related to amount effects in monsoon rainwater, the primary source
of oxygen in Speleothem carbonate. Analysis of d18O values of
precipitation from Darwin, Australia, the closest Global Network of
Isotopes in Precipitation station to either cave, are closely tied to
monthly precipitation amount” (Denniston et al., 2017) “Stalagmite
oxygen isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)’
has been replaced by ‘“increased monsoon rainfall (lower δ18O values) at
KNI-51 coincides with increased rainfall northward across the
Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen isotopic values in
stalagmites are a commonly used proxy for tropical paleohydrology and
are related to amount effects in monsoon rainwater, the primary source
of oxygen in Speleothem carbonate. Analysis of d18O values of
precipitation from Darwin, Australia, the closest Global Network of
Isotopes in Precipitation station to either cave, are closely tied to
monthly precipitation amount” (Denniston et al., 2017) “Stalagmite
oxygen isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al.,
2013)’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-03-24 22:25:06 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRhTtQNZMrVu): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-02-13 23:46:37 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRhTtQNZMrVu): paleoData_notes: ‘“increased monsoon rainfall
(lower δ18O values) at KNI-51 coincides with increased rainfall
northward across the Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen
isotopic values in stalagmites are a commonly used proxy for tropical
paleohydrology and are related to amount effects in monsoon rainwater,
the primary source of oxygen in Speleothem carbonate. Analysis of d18O
values of precipitation from Darwin, Australia, the closest Global
Network of Isotopes in Precipitation station to either cave, are closely
tied to monthly precipitation amount” (Denniston et al., 2017)
“Stalagmite oxygen isotopic values track monsoon intensity via amount
effects in precipitation and reveal a dynamic Holocene IASM…interpreting
our stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)’
has been replaced by ‘((( “increased monsoon rainfall (lower ��18O
values) at KNI-51 coincides with increased rainfall northward across the
Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen isotopic values in
stalagmites are a commonly used proxy for tropical paleohydrology and
are related to amount effects in monsoon rainwater, the primary source
of oxygen in Speleothem carbonate. Analysis of d18O values of
precipitation from Darwin, Australia, the closest Global Network of
Isotopes in Precipitation station to either cave, are closely tied to
monthly precipitation amount” (Denniston et al., 2017) “Stalagmite
oxygen isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013);
paleoData_variableName updated ))) “increased monsoon rainfall (lower
δ18O values) at KNI-51 coincides with increased rainfall northward
across the Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen isotopic
values in stalagmites are a commonly used proxy for tropical
paleohydrology and are related to amount effects in monsoon rainwater,
the primary source of oxygen in Speleothem carbonate. Analysis of d18O
values of precipitation from Darwin, Australia, the closest Global
Network of Isotopes in Precipitation station to either cave, are closely
tied to monthly precipitation amount” (Denniston et al., 2017)
“Stalagmite oxygen isotopic values track monsoon intensity via amount
effects in precipitation and reveal a dynamic Holocene IASM…interpreting
our stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)
/// “increased monsoon rainfall (lower δ18O values) at KNI-51 coincides
with increased rainfall northward across the Indo-Pacific TRB”
(Denniston et al., 2016) “Oxygen isotopic values in stalagmites are a
commonly used proxy for tropical paleohydrology and are related to
amount effects in monsoon rainwater, the primary source of oxygen in
Speleothem carbonate. Analysis of d18O values of precipitation from
Darwin, Australia, the closest Global Network of Isotopes in
Precipitation station to either cave, are closely tied to monthly
precipitation amount” (Denniston et al., 2017) “Stalagmite oxygen
isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al.,
2013)’
Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2022-07-28 17:34:01 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘100’ has been replaced by NULL
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2021-11-17 02:07:36 UTC
- changes:
- Paleo Interpretation metadata:
- d18OComposite (S2LRhTtQNZMrVu): interpretation1_seasonality:
‘summer’ has been replaced by ‘12,1,2’
- d18OComposite (S2LRhTtQNZMrVu): interpretation1_variable: ‘M’ has
been replaced by ‘P’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2021-10-05 21:40:26 UTC
- changes:
- Geographic metadata:
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Zealand>Australia’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nick
- timestamp: 2021-03-17 01:54:24 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Column metadata:
- d18OComposite (S2LRhTtQNZMrVu): paleoData_notes: ‘“increased monsoon
rainfall (lower δ18O values) at KNI-51 coincides with increased rainfall
northward across the Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen
isotopic values in stalagmites are a commonly used proxy for tropical
paleohydrology and are related to amount effects in monsoon rainwater,
the primary source of oxygen in speleothem carbonate. Analysis of d18O
values of precipitation from Darwin, Australia, the closest Global
Network of Isotopes in Precipitation station to either cave, are closely
tied to monthly precipitation amount” (Denniston et al., 2017)
“Stalagmite oxygen isotopic values track monsoon intensity via amount
effects in precipitation and reveal a dynamic Holocene IASM…interpreting
our stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al., 2013)’
has been replaced by ‘“increased monsoon rainfall (lower δ18O values) at
KNI-51 coincides with increased rainfall northward across the
Indo-Pacific TRB” (Denniston et al., 2016) “Oxygen isotopic values in
stalagmites are a commonly used proxy for tropical paleohydrology and
are related to amount effects in monsoon rainwater, the primary source
of oxygen in Speleothem carbonate. Analysis of d18O values of
precipitation from Darwin, Australia, the closest Global Network of
Isotopes in Precipitation station to either cave, are closely tied to
monthly precipitation amount” (Denniston et al., 2017) “Stalagmite
oxygen isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al.,
2013)’
- Paleo Interpretation metadata:
- d18OComposite (S2LRhTtQNZMrVu): interpretation1_seasonalityGeneral:
‘Summer’ has been replaced by ‘summerOnly’
- d18OComposite (S2LRhTtQNZMrVu): interpretation1_seasonality: NULL
has been replaced by ‘summer’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:29:11 UTC
- changes:
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Darwin, Australia, the closest Global Network of Isotopes in
Precipitation station to either cave, are closely tied to monthly
precipitation amount” (Denniston et al., 2017) “Stalagmite oxygen
isotopic values track monsoon intensity via amount effects in
precipitation and reveal a dynamic Holocene IASM…interpreting our
stalagmite d18O time series as reflecting changes in rainwater d18O
values which, in turn, track monsoon strength” (Denniston et al.,
2013)’
- d18OComposite (S2LRhTtQNZMrVu): paleoData_proxy: NULL has been
replaced by ‘d18O’
- d18OComposite (S2LRhTtQNZMrVu): paleoData_proxyDetail: NULL has been
replaced by ‘calcite’
- d18OComposite (S2LRhTtQNZMrVu): paleoData_proxyGeneral: NULL has
been replaced by ‘isotope’
- d18OComposite (S2LRhTtQNZMrVu): paleoData_QCCertification: NULL has
been replaced by ‘CH’
- d18OComposite (S2LRhTtQNZMrVu): paleoData_QCnotes: NULL has been
replaced by ‘“For eight of these 11 stalagmites, age models and oxygen
isotopic ratios were previously published (Denniston et al., 2013b);
three KNI-51 stalagmite records are newly reported here” (Denniston et
al., 2017) (https://www.ncdc.noaa.gov/paleo-search/study/22990)
SISAL Note: “KNI-51-0 (entity_id = 331), KNI-51-3 (entity_id = 332),
KNI-51-4 (entity_id = 333), KNI-51-7 (entity_id = 334), KNI-51-10
(entity_id = 335), KNI-51-11 (entity_id = 336), KNI-51-A2-side1
(entity_id = 337), KNI-51-A2-side2 (entity_id = 338), KNI-51-C
(entity_id = 339), KNI-51-F (entity_id = 340), KNI-51-G (entity_id =
341), KNI-51-H (entity_id = 342), KNI-51-I (entity_id = 343), KNI-51-J
(entity_id = 344), KNI-51-N (entity_id = 345), KNI-51-O (entity_id =
346), KNI-51-A1 (entity_id = 418) and KNI-51-P (entity_id = 419): all
samples have been corrected by -1 permil to be a calcite equivalent. In
the original paper, entity KN51-10 was arbitrarily offset by -1 permil
to match other records; this offset has been removed. 234U/238U values
for KNI-51-1 (entity_id = 637) and KNI-51-8 (entity_id = 638) are
derived from d234U”’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:27:34 UTC
- notes: Created from SISALv2