Version history for Rxl1e2BAfqTyeOzB9Jpd -
BucadellaRenella.Drysdale.2006
Version: 1.0.15
- lastVersion: 1.0.14
- curator: nicholas
- timestamp: 2025-06-25 22:45:56.637387 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (S2LRNh2zmbQt44): interpretation1_seasonality: ‘((( null )))
Summer /// Jun-Aug’ has been replaced by ‘Jun-Aug’
- d18O (S2LRNh2zmbQt44): interpretation1_seasonalityGeneral: ‘((( null
))) Summer /// summerOnly’ has been replaced by ‘summerOnly’
- d18O (S2LRNh2zmbQt44): interpretation1_variable: ‘((( null ))) P-E
/// effectivePrecipitation’ has been replaced by
‘effectivePrecipitation’
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2025-06-25 21:21:36.246758 UTC
- changes:
- Paleo Column metadata:
- d13C (S2LR19TvFEMe7E): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d13C (S2LR3yE4cc4jje): paleoData_notes: ‘“Interpretations of
Speleothem δ13C re- cords are more challenging because of the complex
reactions involving soil CO2, bedrock dissolution, and the reaction
kinetics in the CO2-H2O-CaCO3 system (e.g. Fairchild and Baker,
2012).”(Giovanni et al., 2016)’ has been replaced by ‘((( null )))
“Interpretations of speleothem δ13C re- cords are more challenging
because of the complex reactions involving soil CO2, bedrock
dissolution, and the reaction kinetics in the CO2-H2O-CaCO3 system
(e.g. Fairchild and Baker, 2012).”(Giovanni et al., 2016) ///
“Interpretations of Speleothem δ13C re- cords are more challenging
because of the complex reactions involving soil CO2, bedrock
dissolution, and the reaction kinetics in the CO2-H2O-CaCO3 system
(e.g. Fairchild and Baker, 2012).”(Giovanni et al., 2016)’
- d13C (S2LR3yE4cc4jje): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d13C (S2LR3yE4cc4jje): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- d18O (S2LR5Ue2SQ9Lrv): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRNYZQ63E2WT): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRNh2zmbQt44): paleoData_notes: ‘” Higher δ18O on the Apuan
Alps calcite Speleothem, in absence of large changes in the water
composition of the oceans, are inter- preted as due to decrease in
precipita- tion…Several lines of evidence suggest that this event could
be characterized by longer summer drought and possibly by little impact
on precipitation during winter…Longer summers (basically at the expense
of spring and autumn seasons) compared to winter, can affect the
isotopic budget of our caves, and can additionally help in explaining
our isotopic records.” (Giovanni et al., 2016)’ has been replaced by
‘((( null ))) ” Higher δ18O on the Apuan Alps calcite speleothem, in
absence of large changes in the water composition of the oceans, are
inter- preted as due to decrease in precipita- tion…Several lines of
evidence suggest that this event could be characterized by longer summer
drought and possibly by little impact on precipitation during
winter…Longer summers (basically at the expense of spring and autumn
seasons) compared to winter, can affect the isotopic budget of our
caves, and can additionally help in explaining our isotopic records.”
(Giovanni et al., 2016) /// ” Higher δ18O on the Apuan Alps calcite
Speleothem, in absence of large changes in the water composition of the
oceans, are inter- preted as due to decrease in precipita- tion…Several
lines of evidence suggest that this event could be characterized by
longer summer drought and possibly by little impact on precipitation
during winter…Longer summers (basically at the expense of spring and
autumn seasons) compared to winter, can affect the isotopic budget of
our caves, and can additionally help in explaining our isotopic
records.” (Giovanni et al., 2016)’
- d18O (S2LRNh2zmbQt44): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d18O (S2LRNh2zmbQt44): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- d13C (S2LRdb0jbhT7Ty): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d13C (S2LRnsPLb2GezB): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRvzAbTnzqS0): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- Paleo Interpretation metadata:
- d18O (S2LRNh2zmbQt44): interpretation1_seasonality: ‘Jun-Aug’ has
been replaced by ‘((( null ))) Summer /// Jun-Aug’
- d18O (S2LRNh2zmbQt44): interpretation1_seasonalityGeneral:
‘summerOnly’ has been replaced by ‘((( null ))) Summer ///
summerOnly’
- d18O (S2LRNh2zmbQt44): interpretation1_variable:
‘effectivePrecipitation’ has been replaced by ‘((( null ))) P-E ///
effectivePrecipitation’
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-08-10 22:44:22 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub2_doi: ‘http://amq.aiqua.it/index.php/issues-2012-2017/alpine-and-mediterranean-quaternary-29-1-2016/12-the-so-called-4-2-event-in-the-central-mediterranean-and-its-climatic-teleconnections’
has been replaced by ‘Zanchetta, G., Regattieri. E., Drysdale, R.N.,
Baneschi, I., & Hellstrom, J.C. .The so-called “4.2 Event” in the
central Mediterranean and its climate teleconnections (2015). Alpine and
Mediterranean Quaternary, 29(1), 5-17. https://amq.aiqua.it/index.php/amq/article/view/91’
- pub1_author: NULL has been replaced by ‘Russell Drysdale and
Giovanni Zanchetta and John Hellstrom and Roland Maas and Anthony
Fallick and Matthew Pickett and Ian Cartwright and Leonardo
Piccini’
- pub1_journal: NULL has been replaced by ‘Geology’
- pub1_pages: NULL has been replaced by ‘101’
- pub1_title: NULL has been replaced by ‘Late Holocene drought
responsible for the collapse of Old World civilizations is recorded in
an Italian cave flowstone’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-05-12 21:50:33 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRNh2zmbQt44): paleoData_notes: ‘((( ” Higher ��18O on the
Apuan Alps calcite Speleothem, in absence of large changes in the water
composition of the oceans, are inter- preted as due to decrease in
precipita- tion…Several lines of evidence suggest that this event could
be characterized by longer summer drought and possibly by little impact
on precipitation during winter…Longer summers (basically at the expense
of spring and autumn seasons) compared to winter, can affect the
isotopic budget of our caves, and can additionally help in explaining
our isotopic records.” (Giovanni et al., 2016) ))) ” Higher δ18O on the
Apuan Alps calcite Speleothem, in absence of large changes in the water
composition of the oceans, are inter- preted as due to decrease in
precipita- tion…Several lines of evidence suggest that this event could
be characterized by longer summer drought and possibly by little impact
on precipitation during winter…Longer summers (basically at the expense
of spring and autumn seasons) compared to winter, can affect the
isotopic budget of our caves, and can additionally help in explaining
our isotopic records.” (Giovanni et al., 2016) /// ” Higher δ18O on the
Apuan Alps calcite Speleothem, in absence of large changes in the water
composition of the oceans, are inter- preted as due to decrease in
precipita- tion…Several lines of evidence suggest that this event could
be characterized by longer summer drought and possibly by little impact
on precipitation during winter…Longer summers (basically at the expense
of spring and autumn seasons) compared to winter, can affect the
isotopic budget of our caves, and can additionally help in explaining
our isotopic records.” (Giovanni et al., 2016)’ has been replaced by ‘”
Higher δ18O on the Apuan Alps calcite Speleothem, in absence of large
changes in the water composition of the oceans, are inter- preted as due
to decrease in precipita- tion…Several lines of evidence suggest that
this event could be characterized by longer summer drought and possibly
by little impact on precipitation during winter…Longer summers
(basically at the expense of spring and autumn seasons) compared to
winter, can affect the isotopic budget of our caves, and can
additionally help in explaining our isotopic records.” (Giovanni et al.,
2016)’
- d18O (S2LRNh2zmbQt44): paleoData_QCnotes: ‘((( RL4_2018; SISAL Note:
“RL4_2006 (entity_id = 282), RL4_2016 (entity_id = 283) and RL4_2018
(entity_id = 381) share the same U-Th dates. Their”decay_constant=other”
because they were calculated using the following decay constants: 234U:
2.835���o10^(-6 )/yr and 230Th: 9.195 ���o 10^(-6)/yr. Duplicate isotope
samples of RL4_2006 (entity_id = 282) at depth_sample = 80.1, 78.63,
82.1mm with different interp_age and isotope values have been averaged.
RL4_2018 (entity_id = 381) supersedes RL4_2006 (entity_id = 282) and
RL4_2016 (entity_id = 283).” ))) RL4_2018; SISAL Note: “RL4_2006
(entity_id = 282), RL4_2016 (entity_id = 283) and RL4_2018 (entity_id =
381) share the same U-Th dates. Their”decay_constant=other” because they
were calculated using the following decay constants: 234U: 2.835√o10^(-6
)/yr and 230Th: 9.195 √o 10^(-6)/yr. Duplicate isotope samples of
RL4_2006 (entity_id = 282) at depth_sample = 80.1, 78.63, 82.1mm with
different interp_age and isotope values have been averaged. RL4_2018
(entity_id = 381) supersedes RL4_2006 (entity_id = 282) and RL4_2016
(entity_id = 283).” /// RL4_2018; SISAL Note: “RL4_2006 (entity_id =
282), RL4_2016 (entity_id = 283) and RL4_2018 (entity_id = 381) share
the same U-Th dates. Their”decay_constant=other” because they were
calculated using the following decay constants: 234U: 2.835√o10^(-6 )/yr
and 230Th: 9.195 √o 10^(-6)/yr. Duplicate isotope samples of RL4_2006
(entity_id = 282) at depth_sample = 80.1, 78.63, 82.1mm with different
interp_age and isotope values have been averaged. RL4_2018 (entity_id =
381) supersedes RL4_2006 (entity_id = 282) and RL4_2016 (entity_id =
283).”’ has been replaced by ‘RL4_2018; SISAL Note: “RL4_2006 (entity_id
= 282), RL4_2016 (entity_id = 283) and RL4_2018 (entity_id = 381) share
the same U-Th dates. Their”decay_constant=other” because they were
calculated using the following decay constants: 234U: 2.835√o10^(-6 )/yr
and 230Th: 9.195 √o 10^(-6)/yr. Duplicate isotope samples of RL4_2006
(entity_id = 282) at depth_sample = 80.1, 78.63, 82.1mm with different
interp_age and isotope values have been averaged. RL4_2018 (entity_id =
381) supersedes RL4_2006 (entity_id = 282) and RL4_2016 (entity_id =
283).”’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-03-29 19:42:54 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (S2LRNh2zmbQt44): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
Version: 1.0.9
- lastVersion: 1.0.8
- curator: nicholas
- timestamp: 2023-02-13 23:38:45 UTC
- changes:
- Paleo Interpretation metadata:
- uncertaintyLow (S2LR6cLXpb9s37): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LR6hjKGrOh7k): interpretation1_scope: NULL has
been replaced by ‘climate’
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- uncertaintyHigh (S2LRexkjxV6QPw): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRJT6isiz8Ei): interpretation1_scope: NULL has
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been replaced by ‘climate’
- uncertaintyLow (S2LRvnxNFlKiKq): interpretation1_scope: NULL has
been replaced by ‘climate’
- Paleo Column metadata:
- d18O (S2LRNh2zmbQt44): paleoData_notes: ‘” Higher δ18O on the Apuan
Alps calcite Speleothem, in absence of large changes in the water
composition of the oceans, are inter- preted as due to decrease in
precipita- tion…Several lines of evidence suggest that this event could
be characterized by longer summer drought and possibly by little impact
on precipitation during winter…Longer summers (basically at the expense
of spring and autumn seasons) compared to winter, can affect the
isotopic budget of our caves, and can additionally help in explaining
our isotopic records.” (Giovanni et al., 2016)’ has been replaced by
‘((( ” Higher ��18O on the Apuan Alps calcite Speleothem, in absence of
large changes in the water composition of the oceans, are inter- preted
as due to decrease in precipita- tion…Several lines of evidence suggest
that this event could be characterized by longer summer drought and
possibly by little impact on precipitation during winter…Longer summers
(basically at the expense of spring and autumn seasons) compared to
winter, can affect the isotopic budget of our caves, and can
additionally help in explaining our isotopic records.” (Giovanni et al.,
2016) ))) ” Higher δ18O on the Apuan Alps calcite Speleothem, in absence
of large changes in the water composition of the oceans, are inter-
preted as due to decrease in precipita- tion…Several lines of evidence
suggest that this event could be characterized by longer summer drought
and possibly by little impact on precipitation during winter…Longer
summers (basically at the expense of spring and autumn seasons) compared
to winter, can affect the isotopic budget of our caves, and can
additionally help in explaining our isotopic records.” (Giovanni et al.,
2016) /// ” Higher δ18O on the Apuan Alps calcite Speleothem, in absence
of large changes in the water composition of the oceans, are inter-
preted as due to decrease in precipita- tion…Several lines of evidence
suggest that this event could be characterized by longer summer drought
and possibly by little impact on precipitation during winter…Longer
summers (basically at the expense of spring and autumn seasons) compared
to winter, can affect the isotopic budget of our caves, and can
additionally help in explaining our isotopic records.” (Giovanni et al.,
2016)’
- d18O (S2LRNh2zmbQt44): paleoData_QCnotes: ‘RL4_2018; SISAL Note:
“RL4_2006 (entity_id = 282), RL4_2016 (entity_id = 283) and RL4_2018
(entity_id = 381) share the same U-Th dates. Their”decay_constant=other”
because they were calculated using the following decay constants: 234U:
2.835√o10^(-6 )/yr and 230Th: 9.195 √o 10^(-6)/yr. Duplicate isotope
samples of RL4_2006 (entity_id = 282) at depth_sample = 80.1, 78.63,
82.1mm with different interp_age and isotope values have been averaged.
RL4_2018 (entity_id = 381) supersedes RL4_2006 (entity_id = 282) and
RL4_2016 (entity_id = 283).”’ has been replaced by ‘((( RL4_2018; SISAL
Note: “RL4_2006 (entity_id = 282), RL4_2016 (entity_id = 283) and
RL4_2018 (entity_id = 381) share the same U-Th dates.
Their”decay_constant=other” because they were calculated using the
following decay constants: 234U: 2.835���o10^(-6 )/yr and 230Th: 9.195
���o 10^(-6)/yr. Duplicate isotope samples of RL4_2006 (entity_id = 282)
at depth_sample = 80.1, 78.63, 82.1mm with different interp_age and
isotope values have been averaged. RL4_2018 (entity_id = 381) supersedes
RL4_2006 (entity_id = 282) and RL4_2016 (entity_id = 283).” )))
RL4_2018; SISAL Note: “RL4_2006 (entity_id = 282), RL4_2016 (entity_id =
283) and RL4_2018 (entity_id = 381) share the same U-Th dates.
Their”decay_constant=other” because they were calculated using the
following decay constants: 234U: 2.835√o10^(-6 )/yr and 230Th: 9.195 √o
10^(-6)/yr. Duplicate isotope samples of RL4_2006 (entity_id = 282) at
depth_sample = 80.1, 78.63, 82.1mm with different interp_age and isotope
values have been averaged. RL4_2018 (entity_id = 381) supersedes
RL4_2006 (entity_id = 282) and RL4_2016 (entity_id = 283).” ///
RL4_2018; SISAL Note: “RL4_2006 (entity_id = 282), RL4_2016 (entity_id =
283) and RL4_2018 (entity_id = 381) share the same U-Th dates.
Their”decay_constant=other” because they were calculated using the
following decay constants: 234U: 2.835√o10^(-6 )/yr and 230Th: 9.195 √o
10^(-6)/yr. Duplicate isotope samples of RL4_2006 (entity_id = 282) at
depth_sample = 80.1, 78.63, 82.1mm with different interp_age and isotope
values have been averaged. RL4_2018 (entity_id = 381) supersedes
RL4_2006 (entity_id = 282) and RL4_2016 (entity_id = 283).”’
Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2022-07-28 17:28:30 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘300’ has been replaced by NULL
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2022-07-15 22:58:41 UTC
- changes:
- Paleo Interpretation metadata:
- d13CComposite (S2LR19TvFEMe7E): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LR3IE77TOiAB): interpretation1_scope: NULL has been
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Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2022-05-18 00:24:51 UTC
- changes:
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- sisalSampleID (S2LRvH1UzMlnhr): interpretation1_scope: ‘climate’ has
been replaced by NULL
- d18OComposite (S2LRvzAbTnzqS0): interpretation1_scope: ‘climate’ has
been replaced by NULL
- d13CPrecisionComposite (S2LRwth5kaN8Ly): interpretation1_scope:
‘climate’ has been replaced by NULL
- hasAragoniteCorrection (S2LRz4fo2Hbsmz): interpretation1_scope:
‘climate’ has been replaced by NULL
- sisalSampleID (S2LRzG3omgd7GG): interpretation1_scope: ‘climate’ has
been replaced by NULL
- sisalSampleIDComposite (S2LRzReS2ydm4h): interpretation1_scope:
‘climate’ has been replaced by NULL
- mineralogyComposite (S2LRZTc7E4wEKv): interpretation1_scope:
‘climate’ has been replaced by NULL
- Paleo Column metadata:
- ageBchronUncertaintyLow (S2LR6cLXpb9s37): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageBchronUncertaintyLow (S2LR6cLXpb9s37): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- agelinRegUncertaintyHigh (S2LR6hjKGrOh7k): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- agelinRegUncertaintyHigh (S2LR6hjKGrOh7k): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- agelinRegUncertaintyLow (S2LR8vpD7fkwrD): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- agelinRegUncertaintyLow (S2LR8vpD7fkwrD): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- ageBchronUncertaintyHigh (S2LR8XfswXk5sj): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageBchronUncertaintyHigh (S2LR8XfswXk5sj): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- agecopRaUncertaintyHigh (S2LRBa3GcWLupa): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- agecopRaUncertaintyHigh (S2LRBa3GcWLupa): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- ageBaconUncertaintyHigh (S2LRexkjxV6QPw): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageBaconUncertaintyHigh (S2LRexkjxV6QPw): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- ageBchron (S2LRfOs129tlt8): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- ageBchron (S2LRfOs129tlt8): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- ageBaconUncertaintyLow (S2LRJT6isiz8Ei): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageBaconUncertaintyLow (S2LRJT6isiz8Ei): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- ageStalAgeUncertaintyHigh (S2LRk0I2MqGRHM): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageStalAgeUncertaintyHigh (S2LRk0I2MqGRHM): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- agecopRaUncertaintyLow (S2LRlPsBgs9Ufa): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- agecopRaUncertaintyLow (S2LRlPsBgs9Ufa): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- age (S2LRMcgdvkQNLp): paleoData_units: ‘yr BP’ has been replaced by
‘BP’
- age (S2LRMcgdvkQNLp): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- agelinInterpUncertaintyHigh (S2LRMZmuYOHwy4): paleoData_units: ‘yr
BP’ has been replaced by ‘BP’
- agelinInterpUncertaintyHigh (S2LRMZmuYOHwy4):
paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
- ageBacon (S2LRn5sNTUnNun): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- ageBacon (S2LRn5sNTUnNun): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- d18O (S2LRNh2zmbQt44): paleoData_proxyLumps: NULL has been replaced
by ‘isotope’
- d18O (S2LRNh2zmbQt44): paleoData_proxyLumpsOriginal: NULL has been
replaced by ‘d18O’
- ageStalAge (S2LROBiwP2hhZC): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- ageStalAge (S2LROBiwP2hhZC): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- agelinInterp (S2LROpV8gKQ7FW): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- agelinInterp (S2LROpV8gKQ7FW): paleoData_unitsOriginal: NULL has
been replaced by ‘yr BP’
- age (S2LRpOZbwM2zji): paleoData_units: ‘yr BP’ has been replaced by
‘BP’
- age (S2LRpOZbwM2zji): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- ageStalAgeUncertaintyLow (S2LRQOYvvThDoP): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageStalAgeUncertaintyLow (S2LRQOYvvThDoP): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- age (S2LRrbarLxHI0e): paleoData_units: ‘yr BP’ has been replaced by
‘BP’
- age (S2LRrbarLxHI0e): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- agecopRa (S2LRrsuty2LrLk): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- agecopRa (S2LRrsuty2LrLk): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- agelinInterpUncertaintyLow (S2LRvnxNFlKiKq): paleoData_units: ‘yr
BP’ has been replaced by ‘BP’
- agelinInterpUncertaintyLow (S2LRvnxNFlKiKq):
paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
- age (S2LRxM7qWFbfyY): paleoData_units: ‘yr BP’ has been replaced by
‘BP’
- age (S2LRxM7qWFbfyY): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- agelinReg (S2LRZEcSZbZ4mP): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- agelinReg (S2LRZEcSZbZ4mP): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- Chron Column metadata:
- age_type (S2LcRbAgbL4s4Ne): chronData_variableName: ‘ageType’ has
been replaced by ‘age_type’
- age_type (S2LcRbAgbL4s4Ne): chronData_variableNameOriginal: NULL has
been replaced by ‘ageType’
- age_type (S2LcRgRNrksKYpD): chronData_variableName: ‘ageType’ has
been replaced by ‘age_type’
- age_type (S2LcRgRNrksKYpD): chronData_variableNameOriginal: NULL has
been replaced by ‘ageType’
- age_type (S2LcRIGdNZOtSJh): chronData_variableName: ‘ageType’ has
been replaced by ‘age_type’
- age_type (S2LcRIGdNZOtSJh): chronData_variableNameOriginal: NULL has
been replaced by ‘ageType’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2021-11-17 02:05:39 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (S2LRNh2zmbQt44): interpretation1_seasonality: ‘summer’ has
been replaced by ‘6,7,8’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2021-10-05 21:38:32 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: NULL has been replaced by ‘Europe>Southern
Europe>Italy’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nick
- timestamp: 2021-03-17 01:52:04 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Column metadata:
- d13C (S2LR3yE4cc4jje): paleoData_notes: ‘“Interpretations of
speleothem δ13C re- cords are more challenging because of the complex
reactions involving soil CO2, bedrock dissolution, and the reaction
kinetics in the CO2-H2O-CaCO3 system (e.g. Fairchild and Baker,
2012).”(Giovanni et al., 2016)’ has been replaced by ‘“Interpretations
of Speleothem δ13C re- cords are more challenging because of the complex
reactions involving soil CO2, bedrock dissolution, and the reaction
kinetics in the CO2-H2O-CaCO3 system (e.g. Fairchild and Baker,
2012).”(Giovanni et al., 2016)’
- d18O (S2LRNh2zmbQt44): paleoData_notes: ‘” Higher δ18O on the Apuan
Alps calcite speleothem, in absence of large changes in the water
composition of the oceans, are inter- preted as due to decrease in
precipita- tion…Several lines of evidence suggest that this event could
be characterized by longer summer drought and possibly by little impact
on precipitation during winter…Longer summers (basically at the expense
of spring and autumn seasons) compared to winter, can affect the
isotopic budget of our caves, and can additionally help in explaining
our isotopic records.” (Giovanni et al., 2016)’ has been replaced by ‘”
Higher δ18O on the Apuan Alps calcite Speleothem, in absence of large
changes in the water composition of the oceans, are inter- preted as due
to decrease in precipita- tion…Several lines of evidence suggest that
this event could be characterized by longer summer drought and possibly
by little impact on precipitation during winter…Longer summers
(basically at the expense of spring and autumn seasons) compared to
winter, can affect the isotopic budget of our caves, and can
additionally help in explaining our isotopic records.” (Giovanni et al.,
2016)’
- Paleo Interpretation metadata:
- d18O (S2LRNh2zmbQt44): interpretation1_seasonality: ‘Summer’ has
been replaced by ‘summer’
- d18O (S2LRNh2zmbQt44): interpretation1_seasonalityGeneral: ‘Summer’
has been replaced by ‘summerOnly’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:28:32 UTC
- changes:
- Paleo Interpretation metadata:
- d13CComposite (S2LR19TvFEMe7E): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LR3IE77TOiAB): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LR3yE4cc4jje): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LR5Ue2SQ9Lrv): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13CPrecision (S2LR84KmH5CK7c): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LR9g5Rdz5TH3): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRBCwVSuLDVD): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRbquS8pmgGS): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRdb0jbhT7Ty): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13CStandard (S2LRE0mu1vGIA8): interpretation1_scope: NULL has been
replaced by ‘climate’
- entityName (S2LRf3BaPDaAwk): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRFzHirDaxu8): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRgws7jEwyBV): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LRhGInhVVxLU): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRI8rpp9SfBK): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrectionComposite (S2LRIRO2L5E2gG):
interpretation1_scope: NULL has been replaced by ‘climate’
- d18OPrecision (S2LRIZrmvYTr1e): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandardComposite (S2LRjj0zzZMb76): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LRjRV6eFbULs): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRJtR6bra6ty): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandardComposite (S2LRluQlNGxv1h): interpretation1_scope: NULL
has been replaced by ‘climate’
- depthComposite (S2LRNDN4rL6pXr): interpretation1_scope: NULL has
been replaced by ‘climate’
- d18O (S2LRNh2zmbQt44): interpretation1_direction: NULL has been
replaced by ‘negative’
- d18O (S2LRNh2zmbQt44): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRNh2zmbQt44): interpretation1_seasonality: NULL has been
replaced by ‘Summer’
- d18O (S2LRNh2zmbQt44): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Summer’
- d18O (S2LRNh2zmbQt44): interpretation1_variable: NULL has been
replaced by ‘P-E’
- d18O (S2LRNh2zmbQt44): interpretation1_variableDetail: NULL has been
replaced by ‘@surface’
- d13C (S2LRnsPLb2GezB): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandard (S2LRnuV5oNLmzr): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRNYZQ63E2WT): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OPrecisionComposite (S2LRqZB7rn1uj3): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRr3VrANTCNh): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRsUrw25MaoB): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRSWiRx6UlNc): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRvdsAAUu1Qc): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRvH1UzMlnhr): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OComposite (S2LRvzAbTnzqS0): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecisionComposite (S2LRwth5kaN8Ly): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRz4fo2Hbsmz): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRzG3omgd7GG): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleIDComposite (S2LRzReS2ydm4h): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogyComposite (S2LRZTc7E4wEKv): interpretation1_scope: NULL
has been replaced by ‘climate’
- Paleo Column metadata:
- d13C (S2LR3yE4cc4jje): paleoData_notes: NULL has been replaced by
‘“Interpretations of speleothem δ13C re- cords are more challenging
because of the complex reactions involving soil CO2, bedrock
dissolution, and the reaction kinetics in the CO2-H2O-CaCO3 system
(e.g. Fairchild and Baker, 2012).”(Giovanni et al., 2016)’
- d13C (S2LR3yE4cc4jje): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d13C (S2LR3yE4cc4jje): paleoData_QCnotes: NULL has been replaced by
‘RL4_2018 ; SISAL Note: “RL4_2006 (entity_id = 282), RL4_2016 (entity_id
= 283) and RL4_2018 (entity_id = 381) share the same U-Th dates.
Their”decay_constant=other” because they were calculated using the
following decay constants: 234U: 2.835√o10^(-6 )/yr and 230Th: 9.195 √o
10^(-6)/yr. Duplicate isotope samples of RL4_2006 (entity_id = 282) at
depth_sample = 80.1, 78.63, 82.1mm with different interp_age and isotope
values have been averaged. RL4_2018 (entity_id = 381) supersedes
RL4_2006 (entity_id = 282) and RL4_2016 (entity_id = 283).”’
- d18O (S2LR5Ue2SQ9Lrv): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LR5Ue2SQ9Lrv): paleoData_QCnotes: NULL has been replaced by
‘RL4_2006; superseded by RL4_2018 (unpublished)’
- d13C (S2LRdb0jbhT7Ty): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d13C (S2LRdb0jbhT7Ty): paleoData_QCnotes: NULL has been replaced by
‘RL4_2016; superseded by RL4_2018 (unpublished)’
- d18O (S2LRNh2zmbQt44): paleoData_notes: NULL has been replaced by ‘”
Higher δ18O on the Apuan Alps calcite speleothem, in absence of large
changes in the water composition of the oceans, are inter- preted as due
to decrease in precipita- tion…Several lines of evidence suggest that
this event could be characterized by longer summer drought and possibly
by little impact on precipitation during winter…Longer summers
(basically at the expense of spring and autumn seasons) compared to
winter, can affect the isotopic budget of our caves, and can
additionally help in explaining our isotopic records.” (Giovanni et al.,
2016)’
- d18O (S2LRNh2zmbQt44): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRNh2zmbQt44): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRNh2zmbQt44): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRNh2zmbQt44): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRNh2zmbQt44): paleoData_QCnotes: NULL has been replaced by
‘RL4_2018; SISAL Note: “RL4_2006 (entity_id = 282), RL4_2016 (entity_id
= 283) and RL4_2018 (entity_id = 381) share the same U-Th dates.
Their”decay_constant=other” because they were calculated using the
following decay constants: 234U: 2.835√o10^(-6 )/yr and 230Th: 9.195 √o
10^(-6)/yr. Duplicate isotope samples of RL4_2006 (entity_id = 282) at
depth_sample = 80.1, 78.63, 82.1mm with different interp_age and isotope
values have been averaged. RL4_2018 (entity_id = 381) supersedes
RL4_2006 (entity_id = 282) and RL4_2016 (entity_id = 283).”’
- d13C (S2LRnsPLb2GezB): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d13C (S2LRnsPLb2GezB): paleoData_QCnotes: NULL has been replaced by
‘RL4_2006; superseded by RL4_2018 (unpublished)’
- d18O (S2LRNYZQ63E2WT): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRNYZQ63E2WT): paleoData_QCnotes: NULL has been replaced by
‘RL4_2016; superseded by RL4_2018 (unpublished)’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:26:43 UTC
- notes: Created from SISALv2