Version history for 3sneXJXGkJAe6jcXbR0e -
MacalChasm.Akers.2016
Version: 1.0.18
- lastVersion: 1.0.17
- curator: nicholas
- timestamp: 2025-06-25 22:46:26.289069 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR9DSUVgi2FG): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LR9DSUVgi2FG): paleoData_QCCertification: ‘((( null ))) CH
/// CH, CR’ has been replaced by ‘CH, CR’
- d13C (S2LRE5ZXEOA0gV): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d13C (S2LRE5ZXEOA0gV): paleoData_QCCertification: ‘((( null ))) CH
/// CH, CR’ has been replaced by ‘CH, CR’
- Paleo Interpretation metadata:
- d18O (S2LR9DSUVgi2FG): interpretation1_variable: ‘((( null ))) P ///
precipitation’ has been replaced by ‘precipitation’
- d13C (S2LRE5ZXEOA0gV): interpretation1_variable: ‘((( null ))) P-E
/// effectivePrecipitation’ has been replaced by
‘effectivePrecipitation’
Version: 1.0.17
- lastVersion: 1.0.16
- curator: nicholas
- timestamp: 2025-06-25 21:22:08.462984 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR9DSUVgi2FG): paleoData_notes: ‘“The d18O variation of
rainfall in many tropical locations like the Vaca Plateau is largely
controlled by the amount effect, where increased amounts of rainfall are
correlated with lower d18O values” (Akers et al., 2016)’ has been
replaced by ‘((( null ))) “The δ18O variation of rainfall in many
tropical locations like the Vaca Plateau is largely controlled by the
amount effect, where increased amounts of rainfall are correlated with
lower δ18O values” (Akers et al., 2016) /// “The d18O variation of
rainfall in many tropical locations like the Vaca Plateau is largely
controlled by the amount effect, where increased amounts of rainfall are
correlated with lower d18O values” (Akers et al., 2016)’
- d18O (S2LR9DSUVgi2FG): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LR9DSUVgi2FG): paleoData_QCCertification: ‘CH, CR’ has been
replaced by ‘((( null ))) CH /// CH, CR’
- d18O (S2LR9DSUVgi2FG): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d18O (S2LR9DSUVgi2FG): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- d13C (S2LRE5ZXEOA0gV): paleoData_notes: ‘“Since vegetative
productivity is sensitive to water-stress in the karstic Vaca Plateau,
drier conditions reduce the amount of biogenic carbon (although
potentially with a tem- poral lag), and thus drier conditions would be
expected to produce higher d13C values of water in the epikarst” (Akers
et al., 2016)’ has been replaced by ‘((( null ))) “Since vegetative
productivity is sensitive to water-stress in the karstic Vaca Plateau,
drier conditions re- duce the amount of biogenic carbon (although
potentially with a tem- poral lag), and thus drier conditions would be
expected to produce higher δ13C values of water in the epikarst” (Akers
et al., 2016) /// “Since vegetative productivity is sensitive to
water-stress in the karstic Vaca Plateau, drier conditions reduce the
amount of biogenic carbon (although potentially with a tem- poral lag),
and thus drier conditions would be expected to produce higher d13C
values of water in the epikarst” (Akers et al., 2016)’
- d13C (S2LRE5ZXEOA0gV): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d13C (S2LRE5ZXEOA0gV): paleoData_QCCertification: ‘CH, CR’ has been
replaced by ‘((( null ))) CH /// CH, CR’
- d13C (S2LRE5ZXEOA0gV): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d13C (S2LRE5ZXEOA0gV): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- Paleo Interpretation metadata:
- d18O (S2LR9DSUVgi2FG): interpretation1_variable: ‘precipitation’ has
been replaced by ‘((( null ))) P /// precipitation’
- d13C (S2LRE5ZXEOA0gV): interpretation1_variable:
‘effectivePrecipitation’ has been replaced by ‘((( null ))) P-E ///
effectivePrecipitation’
Version: 1.0.16
- lastVersion: 1.0.15
- curator: nicholas
- timestamp: 2024-09-05 21:24:33.299788 UTC
- changes:
- Paleo Interpretation metadata:
- uncertainty (S2LR1EJaw1fqZ9): interpretation2_scope: NULL has been
replaced by ‘climate’
- uncertainty (S2LR1EJaw1fqZ9): interpretation3_scope: NULL has been
replaced by ‘climate’
- uncertainty (S2LR1EJaw1fqZ9): interpretation4_scope: NULL has been
replaced by ‘isotope’
- uncertainty (S2LR1EJaw1fqZ9): interpretation5_scope: NULL has been
replaced by ‘isotope’
- uncertainty (S2LR1EJaw1fqZ9): interpretation6_scope: NULL has been
replaced by ‘isotope’
- d18O (S2LR9DSUVgi2FG): interpretation2_scope: NULL has been replaced
by ‘climate’
- d18O (S2LR9DSUVgi2FG): interpretation3_scope: NULL has been replaced
by ‘climate’
- d18O (S2LR9DSUVgi2FG): interpretation4_scope: NULL has been replaced
by ‘isotope’
- d18O (S2LR9DSUVgi2FG): interpretation5_scope: NULL has been replaced
by ‘isotope’
- d18O (S2LR9DSUVgi2FG): interpretation6_scope: NULL has been replaced
by ‘isotope’
- sampleID (S2LRAZhf4859ko): interpretation2_scope: NULL has been
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- sampleID (S2LRAZhf4859ko): interpretation6_scope: NULL has been
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- d13C (S2LRE5ZXEOA0gV): interpretation2_scope: NULL has been replaced
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- d13C (S2LRE5ZXEOA0gV): interpretation3_scope: NULL has been replaced
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- d13C (S2LRE5ZXEOA0gV): interpretation4_scope: NULL has been replaced
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- d13C (S2LRE5ZXEOA0gV): interpretation5_scope: NULL has been replaced
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- uncertaintyLow (S2LRNXIANjxG6j): interpretation2_scope: NULL has
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- uncertaintyLow (S2LRgK1TKE7twV): interpretation2_scope: NULL has
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- thickness (S2LRmoKawXbvpm): interpretation2_scope: NULL has been
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- uncertaintyHigh (S2LRo5y4V8WLt3): interpretation2_scope: NULL has
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- uncertaintyHigh (S2LRo5y4V8WLt3): interpretation3_scope: NULL has
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- uncertaintyHigh (S2LRo5y4V8WLt3): interpretation4_scope: NULL has
been replaced by ‘isotope’
- uncertaintyHigh (S2LRo5y4V8WLt3): interpretation5_scope: NULL has
been replaced by ‘isotope’
- uncertaintyHigh (S2LRo5y4V8WLt3): interpretation6_scope: NULL has
been replaced by ‘isotope’
- mineralogy (S2LRpLFGK9HqWh): interpretation2_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRpLFGK9HqWh): interpretation3_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRpLFGK9HqWh): interpretation4_scope: NULL has been
replaced by ‘isotope’
- mineralogy (S2LRpLFGK9HqWh): interpretation5_scope: NULL has been
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replaced by ‘isotope’
- uncertaintyHigh (S2LRrupH1S23Sm): interpretation2_scope: NULL has
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- uncertaintyHigh (S2LRrupH1S23Sm): interpretation3_scope: NULL has
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- uncertaintyHigh (S2LRrupH1S23Sm): interpretation4_scope: NULL has
been replaced by ‘isotope’
- uncertaintyHigh (S2LRrupH1S23Sm): interpretation5_scope: NULL has
been replaced by ‘isotope’
- uncertaintyHigh (S2LRrupH1S23Sm): interpretation6_scope: NULL has
been replaced by ‘isotope’
- correction (S2LRx5OBxKN1aB): interpretation2_scope: NULL has been
replaced by ‘climate’
- correction (S2LRx5OBxKN1aB): interpretation3_scope: NULL has been
replaced by ‘climate’
- correction (S2LRx5OBxKN1aB): interpretation4_scope: NULL has been
replaced by ‘isotope’
- correction (S2LRx5OBxKN1aB): interpretation5_scope: NULL has been
replaced by ‘isotope’
- correction (S2LRx5OBxKN1aB): interpretation6_scope: NULL has been
replaced by ‘isotope’
Version: 1.0.15
- lastVersion: 1.0.14
- curator: nicholas
- timestamp: 2023-08-10 23:05:19 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_author: NULL has been replaced by ‘Pete D. Akers and George A.
Brook and L. Bruce Railsback and Fuyuan Liang and Gyles Iannone and
James W. Webster and Philip P. Reeder and Hai Cheng and R. Lawrence
Edwards’
- pub1_journal: NULL has been replaced by ‘Palaeogeography,
Palaeoclimatology, Palaeoecology’
- pub1_pages: NULL has been replaced by ‘268–288’
- pub1_title: NULL has been replaced by ‘An extended and
higher-resolution record of climate and land use from stalagmite {MC}01
from Macal Chasm, Belize, revealing connections between major dry
events, overall climate variability, and Maya sociopolitical
changes’
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2023-05-31 20:39:36 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR9DSUVgi2FG): paleoData_notes: ‘((( ((( “The ��18O
variation of rainfall in many tropical locations like the Vaca Plateau
is largely controlled by the amount effect, where increased amounts of
rainfall are correlated with lower ��18O values” (Akers et al., 2016)
))) “The δ18O variation of rainfall in many tropical locations like the
Vaca Plateau is largely controlled by the amount effect, where increased
amounts of rainfall are correlated with lower δ18O values” (Akers et
al., 2016) /// “The δ18O variation of rainfall in many tropical
locations like the Vaca Plateau is largely controlled by the amount
effect, where increased amounts of rainfall are correlated with lower
δ18O values” (Akers et al., 2016) ))) “The d18O variation of rainfall in
many tropical locations like the Vaca Plateau is largely controlled by
the amount effect, where increased amounts of rainfall are correlated
with lower d18O values” (Akers et al., 2016) /// “The δ18O variation of
rainfall in many tropical locations like the Vaca Plateau is largely
controlled by the amount effect, where increased amounts of rainfall are
correlated with lower δ18O values” (Akers et al., 2016)’ has been
replaced by ‘“The d18O variation of rainfall in many tropical locations
like the Vaca Plateau is largely controlled by the amount effect, where
increased amounts of rainfall are correlated with lower d18O values”
(Akers et al., 2016)’
- d13C (S2LRE5ZXEOA0gV): paleoData_notes: ‘((( ((( “Since vegetative
productivity is sensitive to water-stress in the karstic Vaca Plateau,
drier conditions re- duce the amount of biogenic carbon (although
potentially with a tem- poral lag), and thus drier conditions would be
expected to produce higher ��13C values of water in the epikarst” (Akers
et al., 2016) ))) “Since vegetative productivity is sensitive to
water-stress in the karstic Vaca Plateau, drier conditions re- duce the
amount of biogenic carbon (although potentially with a tem- poral lag),
and thus drier conditions would be expected to produce higher δ13C
values of water in the epikarst” (Akers et al., 2016) /// “Since
vegetative productivity is sensitive to water-stress in the karstic Vaca
Plateau, drier conditions re- duce the amount of biogenic carbon
(although potentially with a tem- poral lag), and thus drier conditions
would be expected to produce higher δ13C values of water in the
epikarst” (Akers et al., 2016) ))) “Since vegetative productivity is
sensitive to water-stress in the karstic Vaca Plateau, drier conditions
re- duce the amount of biogenic carbon (although potentially with a tem-
poral lag), and thus drier conditions would be expected to produce
higher d13C values of water in the epikarst” (Akers et al., 2016) ///
“Since vegetative productivity is sensitive to water-stress in the
karstic Vaca Plateau, drier conditions re- duce the amount of biogenic
carbon (although potentially with a tem- poral lag), and thus drier
conditions would be expected to produce higher δ13C values of water in
the epikarst” (Akers et al., 2016)’ has been replaced by ‘“Since
vegetative productivity is sensitive to water-stress in the karstic Vaca
Plateau, drier conditions reduce the amount of biogenic carbon (although
potentially with a tem- poral lag), and thus drier conditions would be
expected to produce higher d13C values of water in the epikarst” (Akers
et al., 2016)’
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2023-05-30 15:49:49 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR9DSUVgi2FG): paleoData_notes: ‘“The δ18O variation of
rainfall in many tropical locations like the Vaca Plateau is largely
controlled by the amount effect, where increased amounts of rainfall are
correlated with lower δ18O values” (Akers et al., 2016)’ has been
replaced by ‘((( ((( “The ��18O variation of rainfall in many tropical
locations like the Vaca Plateau is largely controlled by the amount
effect, where increased amounts of rainfall are correlated with lower
��18O values” (Akers et al., 2016) ))) “The δ18O variation of rainfall
in many tropical locations like the Vaca Plateau is largely controlled
by the amount effect, where increased amounts of rainfall are correlated
with lower δ18O values” (Akers et al., 2016) /// “The δ18O variation of
rainfall in many tropical locations like the Vaca Plateau is largely
controlled by the amount effect, where increased amounts of rainfall are
correlated with lower δ18O values” (Akers et al., 2016) ))) “The d18O
variation of rainfall in many tropical locations like the Vaca Plateau
is largely controlled by the amount effect, where increased amounts of
rainfall are correlated with lower d18O values” (Akers et al., 2016) ///
“The δ18O variation of rainfall in many tropical locations like the Vaca
Plateau is largely controlled by the amount effect, where increased
amounts of rainfall are correlated with lower δ18O values” (Akers et
al., 2016)’
- d18O (S2LR9DSUVgi2FG): paleoData_QCCertification: ‘CH’ has been
replaced by ‘CH, CR’
- d13C (S2LRE5ZXEOA0gV): paleoData_notes: ‘“Since vegetative
productivity is sensitive to water-stress in the karstic Vaca Plateau,
drier conditions re- duce the amount of biogenic carbon (although
potentially with a tem- poral lag), and thus drier conditions would be
expected to produce higher δ13C values of water in the epikarst” (Akers
et al., 2016)’ has been replaced by ‘((( ((( “Since vegetative
productivity is sensitive to water-stress in the karstic Vaca Plateau,
drier conditions re- duce the amount of biogenic carbon (although
potentially with a tem- poral lag), and thus drier conditions would be
expected to produce higher ��13C values of water in the epikarst” (Akers
et al., 2016) ))) “Since vegetative productivity is sensitive to
water-stress in the karstic Vaca Plateau, drier conditions re- duce the
amount of biogenic carbon (although potentially with a tem- poral lag),
and thus drier conditions would be expected to produce higher δ13C
values of water in the epikarst” (Akers et al., 2016) /// “Since
vegetative productivity is sensitive to water-stress in the karstic Vaca
Plateau, drier conditions re- duce the amount of biogenic carbon
(although potentially with a tem- poral lag), and thus drier conditions
would be expected to produce higher δ13C values of water in the
epikarst” (Akers et al., 2016) ))) “Since vegetative productivity is
sensitive to water-stress in the karstic Vaca Plateau, drier conditions
re- duce the amount of biogenic carbon (although potentially with a tem-
poral lag), and thus drier conditions would be expected to produce
higher d13C values of water in the epikarst” (Akers et al., 2016) ///
“Since vegetative productivity is sensitive to water-stress in the
karstic Vaca Plateau, drier conditions re- duce the amount of biogenic
carbon (although potentially with a tem- poral lag), and thus drier
conditions would be expected to produce higher δ13C values of water in
the epikarst” (Akers et al., 2016)’
- d13C (S2LRE5ZXEOA0gV): paleoData_QCCertification: ‘CH’ has been
replaced by ‘CH, CR’
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-03-29 19:56:23 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR9DSUVgi2FG): paleoData_notes: ‘((( “The ��18O variation of
rainfall in many tropical locations like the Vaca Plateau is largely
controlled by the amount effect, where increased amounts of rainfall are
correlated with lower ��18O values” (Akers et al., 2016) ))) “The δ18O
variation of rainfall in many tropical locations like the Vaca Plateau
is largely controlled by the amount effect, where increased amounts of
rainfall are correlated with lower δ18O values” (Akers et al., 2016) ///
“The δ18O variation of rainfall in many tropical locations like the Vaca
Plateau is largely controlled by the amount effect, where increased
amounts of rainfall are correlated with lower δ18O values” (Akers et
al., 2016)’ has been replaced by ‘“The δ18O variation of rainfall in
many tropical locations like the Vaca Plateau is largely controlled by
the amount effect, where increased amounts of rainfall are correlated
with lower δ18O values” (Akers et al., 2016)’
- d13C (S2LRE5ZXEOA0gV): paleoData_notes: ‘((( “Since vegetative
productivity is sensitive to water-stress in the karstic Vaca Plateau,
drier conditions re- duce the amount of biogenic carbon (although
potentially with a tem- poral lag), and thus drier conditions would be
expected to produce higher ��13C values of water in the epikarst” (Akers
et al., 2016) ))) “Since vegetative productivity is sensitive to
water-stress in the karstic Vaca Plateau, drier conditions re- duce the
amount of biogenic carbon (although potentially with a tem- poral lag),
and thus drier conditions would be expected to produce higher δ13C
values of water in the epikarst” (Akers et al., 2016) /// “Since
vegetative productivity is sensitive to water-stress in the karstic Vaca
Plateau, drier conditions re- duce the amount of biogenic carbon
(although potentially with a tem- poral lag), and thus drier conditions
would be expected to produce higher δ13C values of water in the
epikarst” (Akers et al., 2016)’ has been replaced by ‘“Since vegetative
productivity is sensitive to water-stress in the karstic Vaca Plateau,
drier conditions re- duce the amount of biogenic carbon (although
potentially with a tem- poral lag), and thus drier conditions would be
expected to produce higher δ13C values of water in the epikarst” (Akers
et al., 2016)’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-03-24 22:25:38 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR9DSUVgi2FG): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d13C (S2LRE5ZXEOA0gV): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- Paleo Interpretation metadata:
- d13C (S2LRE5ZXEOA0gV): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-02-13 23:50:56 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR9DSUVgi2FG): paleoData_notes: ‘“The δ18O variation of
rainfall in many tropical locations like the Vaca Plateau is largely
controlled by the amount effect, where increased amounts of rainfall are
correlated with lower δ18O values” (Akers et al., 2016)’ has been
replaced by ‘((( “The ��18O variation of rainfall in many tropical
locations like the Vaca Plateau is largely controlled by the amount
effect, where increased amounts of rainfall are correlated with lower
��18O values” (Akers et al., 2016) ))) “The δ18O variation of rainfall
in many tropical locations like the Vaca Plateau is largely controlled
by the amount effect, where increased amounts of rainfall are correlated
with lower δ18O values” (Akers et al., 2016) /// “The δ18O variation of
rainfall in many tropical locations like the Vaca Plateau is largely
controlled by the amount effect, where increased amounts of rainfall are
correlated with lower δ18O values” (Akers et al., 2016)’
- d13C (S2LRE5ZXEOA0gV): paleoData_notes: ‘“Since vegetative
productivity is sensitive to water-stress in the karstic Vaca Plateau,
drier conditions re- duce the amount of biogenic carbon (although
potentially with a tem- poral lag), and thus drier conditions would be
expected to produce higher δ13C values of water in the epikarst” (Akers
et al., 2016)’ has been replaced by ‘((( “Since vegetative productivity
is sensitive to water-stress in the karstic Vaca Plateau, drier
conditions re- duce the amount of biogenic carbon (although potentially
with a tem- poral lag), and thus drier conditions would be expected to
produce higher ��13C values of water in the epikarst” (Akers et al.,
2016) ))) “Since vegetative productivity is sensitive to water-stress in
the karstic Vaca Plateau, drier conditions re- duce the amount of
biogenic carbon (although potentially with a tem- poral lag), and thus
drier conditions would be expected to produce higher δ13C values of
water in the epikarst” (Akers et al., 2016) /// “Since vegetative
productivity is sensitive to water-stress in the karstic Vaca Plateau,
drier conditions re- duce the amount of biogenic carbon (although
potentially with a tem- poral lag), and thus drier conditions would be
expected to produce higher δ13C values of water in the epikarst” (Akers
et al., 2016)’
Version: 1.0.9
- lastVersion: 1.0.8
- curator: nicholas
- timestamp: 2023-02-10 14:34:13 UTC
- changes:
- Paleo Interpretation metadata:
- uncertaintyLow (S2LReVbTDNXVO3): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRgK1TKE7twV): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRmz3bfJ9Ryv): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRNXIANjxG6j): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRo5y4V8WLt3): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRrupH1S23Sm): interpretation1_scope: NULL has
been replaced by ‘climate’
Version: 1.0.8
- lastVersion: 1.0.7
- curator: nicholas
- timestamp: 2023-02-09 15:59:07 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Geographic metadata:
- geo_elevation: NULL has been replaced by ‘530’
- Paleo Column metadata:
- uncertainty (S2LR1EJaw1fqZ9): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_measurementMaterial has been standardized;
paleoData_method has been standardized’
- uncertainty (S2LR1EJaw1fqZ9): paleoData_variableName: ‘d18OStandard’
has been replaced by ‘uncertainty’
- uncertainty (S2LR1EJaw1fqZ9): paleoData_measurementMaterial: NULL
has been replaced by ‘d18O carbonate’
- uncertainty (S2LR1EJaw1fqZ9): paleoData_method: NULL has been
replaced by ‘standard’
- age (S2LR8jtbWV1Y2A): paleoData_notes: NULL has been replaced by
‘NA; paleoData_method has been standardized; paleoData_isPrimary has
been standardized; paleoData_datum has been standardized’
- age (S2LR8jtbWV1Y2A): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LR8jtbWV1Y2A): paleoData_variableName: ‘agecopRa’ has been
replaced by ‘age’
- age (S2LR8jtbWV1Y2A): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LR8jtbWV1Y2A): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- age (S2LR8jtbWV1Y2A): paleoData_method: NULL has been replaced by
‘copRa’
- age (S2LR98NJRr1Jy5): paleoData_notes: NULL has been replaced by
‘NA; paleoData_method has been standardized; paleoData_isPrimary has
been standardized; paleoData_datum has been standardized’
- age (S2LR98NJRr1Jy5): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LR98NJRr1Jy5): paleoData_variableName: ‘ageBchron’ has been
replaced by ‘age’
- age (S2LR98NJRr1Jy5): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LR98NJRr1Jy5): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- age (S2LR98NJRr1Jy5): paleoData_method: NULL has been replaced by
‘Bchron’
- depth (S2LRaekMKaZQxo): paleoData_notes: NULL has been replaced by
‘NA; paleoData_isPrimary has been standardized’
- depth (S2LRaekMKaZQxo): paleoData_units: ‘depth_sample’ has been
replaced by ‘mm’
- depth (S2LRaekMKaZQxo): paleoData_isPrimary: NULL has been replaced
by ‘TRUE’
- uncertainty (S2LRaZEDsWzhgR): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_measurementMaterial has been standardized;
paleoData_method has been standardized’
- uncertainty (S2LRaZEDsWzhgR): paleoData_variableName: ‘d13CStandard’
has been replaced by ‘uncertainty’
- uncertainty (S2LRaZEDsWzhgR): paleoData_measurementMaterial: NULL
has been replaced by ‘d13C’
- uncertainty (S2LRaZEDsWzhgR): paleoData_method: NULL has been
replaced by ‘standard’
- sampleID (S2LRAZhf4859ko): paleoData_variableName: ‘sisalSampleID’
has been replaced by ‘sampleID’
- age (S2LRbDf26igq0I): paleoData_notes: NULL has been replaced by
‘NA; paleoData_method has been standardized; paleoData_isPrimary has
been standardized; paleoData_datum has been standardized’
- age (S2LRbDf26igq0I): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRbDf26igq0I): paleoData_variableName: ‘agelinInterp’ has
been replaced by ‘age’
- age (S2LRbDf26igq0I): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRbDf26igq0I): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- age (S2LRbDf26igq0I): paleoData_method: NULL has been replaced by
‘linInterp’
- uncertaintyLow (S2LReVbTDNXVO3): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyLow (S2LReVbTDNXVO3): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LReVbTDNXVO3): paleoData_variableName:
‘ageBchronUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LReVbTDNXVO3): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LReVbTDNXVO3): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyLow (S2LReVbTDNXVO3): paleoData_method: NULL has been
replaced by ‘Bchron’
- uncertaintyLow (S2LRgK1TKE7twV): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyLow (S2LRgK1TKE7twV): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LRgK1TKE7twV): paleoData_variableName:
‘agecopRaUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LRgK1TKE7twV): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LRgK1TKE7twV): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyLow (S2LRgK1TKE7twV): paleoData_method: NULL has been
replaced by ‘copRa’
- uncertainty (S2LRLp2doS8RlW): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_measurementMaterial has been standardized;
paleoData_method has been standardized’
- uncertainty (S2LRLp2doS8RlW): paleoData_variableName:
‘d18OPrecision’ has been replaced by ‘uncertainty’
- uncertainty (S2LRLp2doS8RlW): paleoData_measurementMaterial: NULL
has been replaced by ‘d18O carbonate’
- uncertainty (S2LRLp2doS8RlW): paleoData_method: NULL has been
replaced by ‘precision’
- uncertaintyHigh (S2LRmz3bfJ9Ryv): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyHigh (S2LRmz3bfJ9Ryv): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyHigh (S2LRmz3bfJ9Ryv): paleoData_variableName:
‘agecopRaUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
- uncertaintyHigh (S2LRmz3bfJ9Ryv): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh (S2LRmz3bfJ9Ryv): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyHigh (S2LRmz3bfJ9Ryv): paleoData_method: NULL has been
replaced by ‘copRa’
- uncertaintyLow (S2LRNXIANjxG6j): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyLow (S2LRNXIANjxG6j): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LRNXIANjxG6j): paleoData_variableName:
‘agelinInterpUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LRNXIANjxG6j): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LRNXIANjxG6j): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyLow (S2LRNXIANjxG6j): paleoData_method: NULL has been
replaced by ‘linInterp’
- uncertaintyHigh (S2LRo5y4V8WLt3): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyHigh (S2LRo5y4V8WLt3): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyHigh (S2LRo5y4V8WLt3): paleoData_variableName:
‘ageBchronUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
- uncertaintyHigh (S2LRo5y4V8WLt3): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh (S2LRo5y4V8WLt3): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyHigh (S2LRo5y4V8WLt3): paleoData_method: NULL has been
replaced by ‘Bchron’
- uncertaintyHigh (S2LRrupH1S23Sm): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyHigh (S2LRrupH1S23Sm): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyHigh (S2LRrupH1S23Sm): paleoData_variableName:
‘agelinInterpUncertaintyHigh’ has been replaced by
‘uncertaintyHigh’
- uncertaintyHigh (S2LRrupH1S23Sm): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh (S2LRrupH1S23Sm): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyHigh (S2LRrupH1S23Sm): paleoData_method: NULL has been
replaced by ‘linInterp’
- correction (S2LRx5OBxKN1aB): paleoData_notes: NULL has been replaced
by ‘NA; paleoData_method has been standardized’
- correction (S2LRx5OBxKN1aB): paleoData_variableName:
‘hasAragoniteCorrection’ has been replaced by ‘correction’
- correction (S2LRx5OBxKN1aB): paleoData_method: NULL has been
replaced by ‘aragonite correction’
- uncertainty (S2LRYvhu4IB1a0): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_measurementMaterial has been standardized;
paleoData_method has been standardized’
- uncertainty (S2LRYvhu4IB1a0): paleoData_variableName:
‘d13CPrecision’ has been replaced by ‘uncertainty’
- uncertainty (S2LRYvhu4IB1a0): paleoData_measurementMaterial: NULL
has been replaced by ‘d13C’
- uncertainty (S2LRYvhu4IB1a0): paleoData_method: NULL has been
replaced by ‘precision’
- age (S2LRyW6OF9xwWN): paleoData_notes: NULL has been replaced by
‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been
standardized’
- age (S2LRyW6OF9xwWN): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRyW6OF9xwWN): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRyW6OF9xwWN): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- Paleo Interpretation metadata:
- d18O (S2LR9DSUVgi2FG): interpretation1_seasonality:
‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘Annual’
- d18O (S2LR9DSUVgi2FG): interpretation1_variable: ‘P’ has been
replaced by ‘precipitation’
- d13C (S2LRE5ZXEOA0gV): interpretation1_seasonality:
‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘Annual’
Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2022-07-28 17:36:54 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘530’ has been replaced by NULL
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2022-07-15 23:06:12 UTC
- changes:
- Paleo Interpretation metadata:
- d18OStandard (S2LR1EJaw1fqZ9): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRaZEDsWzhgR): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRAZhf4859ko): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRLp2doS8RlW): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRmoKawXbvpm): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRpLFGK9HqWh): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRx5OBxKN1aB): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CPrecision (S2LRYvhu4IB1a0): interpretation1_scope: NULL has been
replaced by ‘climate’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2022-05-18 00:27:52 UTC
- changes:
- Paleo Interpretation metadata:
- d18OStandard (S2LR1EJaw1fqZ9): interpretation1_scope: ‘climate’ has
been replaced by NULL
- d18O (S2LR9DSUVgi2FG): interpretation1_variableGroup: NULL has been
replaced by ‘P’
- d13CStandard (S2LRaZEDsWzhgR): interpretation1_scope: ‘climate’ has
been replaced by NULL
- sisalSampleID (S2LRAZhf4859ko): interpretation1_scope: ‘climate’ has
been replaced by NULL
- d13C (S2LRE5ZXEOA0gV): interpretation1_variableGroup: NULL has been
replaced by ‘P-E’
- d18OPrecision (S2LRLp2doS8RlW): interpretation1_scope: ‘climate’ has
been replaced by NULL
- thickness (S2LRmoKawXbvpm): interpretation1_scope: ‘climate’ has
been replaced by NULL
- mineralogy (S2LRpLFGK9HqWh): interpretation1_scope: ‘climate’ has
been replaced by NULL
- hasAragoniteCorrection (S2LRx5OBxKN1aB): interpretation1_scope:
‘climate’ has been replaced by NULL
- d13CPrecision (S2LRYvhu4IB1a0): interpretation1_scope: ‘climate’ has
been replaced by NULL
- Paleo Column metadata:
- agecopRa (S2LR8jtbWV1Y2A): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- agecopRa (S2LR8jtbWV1Y2A): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- ageBchron (S2LR98NJRr1Jy5): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- ageBchron (S2LR98NJRr1Jy5): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- d18O (S2LR9DSUVgi2FG): paleoData_proxyLumps: NULL has been replaced
by ‘isotope’
- d18O (S2LR9DSUVgi2FG): paleoData_proxyLumpsOriginal: NULL has been
replaced by ‘d18O’
- agelinInterp (S2LRbDf26igq0I): paleoData_units: ‘yr BP’ has been
replaced by ‘BP’
- agelinInterp (S2LRbDf26igq0I): paleoData_unitsOriginal: NULL has
been replaced by ‘yr BP’
- d13C (S2LRE5ZXEOA0gV): paleoData_proxyLumps: NULL has been replaced
by ‘isotope’
- d13C (S2LRE5ZXEOA0gV): paleoData_proxyLumpsOriginal: NULL has been
replaced by ‘d13C’
- ageBchronUncertaintyLow (S2LReVbTDNXVO3): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageBchronUncertaintyLow (S2LReVbTDNXVO3): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- agecopRaUncertaintyLow (S2LRgK1TKE7twV): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- agecopRaUncertaintyLow (S2LRgK1TKE7twV): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- agecopRaUncertaintyHigh (S2LRmz3bfJ9Ryv): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- agecopRaUncertaintyHigh (S2LRmz3bfJ9Ryv): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- agelinInterpUncertaintyLow (S2LRNXIANjxG6j): paleoData_units: ‘yr
BP’ has been replaced by ‘BP’
- agelinInterpUncertaintyLow (S2LRNXIANjxG6j):
paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
- ageBchronUncertaintyHigh (S2LRo5y4V8WLt3): paleoData_units: ‘yr BP’
has been replaced by ‘BP’
- ageBchronUncertaintyHigh (S2LRo5y4V8WLt3): paleoData_unitsOriginal:
NULL has been replaced by ‘yr BP’
- agelinInterpUncertaintyHigh (S2LRrupH1S23Sm): paleoData_units: ‘yr
BP’ has been replaced by ‘BP’
- agelinInterpUncertaintyHigh (S2LRrupH1S23Sm):
paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
- age (S2LRyW6OF9xwWN): paleoData_units: ‘yr BP’ has been replaced by
‘BP’
- age (S2LRyW6OF9xwWN): paleoData_unitsOriginal: NULL has been
replaced by ‘yr BP’
- Chron Column metadata:
- age_type (S2LcR8h1p8UpYRM): chronData_variableName: ‘ageType’ has
been replaced by ‘age_type’
- age_type (S2LcR8h1p8UpYRM): chronData_variableNameOriginal: NULL has
been replaced by ‘ageType’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2021-10-05 21:41:08 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: NULL has been replaced by ‘North
America>Central America>Belize’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nick
- timestamp: 2021-04-13 02:34:25 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (S2LR9DSUVgi2FG): interpretation1_seasonality:
‘1,2,3,4,5,6,7,8,9,10,11,270’ has been replaced by
‘1,2,3,4,5,6,7,8,9,10,11,12’
- d13C (S2LRE5ZXEOA0gV): interpretation1_seasonality:
‘1,2,3,4,5,6,7,8,9,10,11,271’ has been replaced by
‘1,2,3,4,5,6,7,8,9,10,11,12’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nick
- timestamp: 2021-03-17 01:55:10 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Interpretation metadata:
- d18O (S2LR9DSUVgi2FG): interpretation1_seasonality: NULL has been
replaced by ‘1,2,3,4,5,6,7,8,9,10,11,270’
- d13C (S2LRE5ZXEOA0gV): interpretation1_seasonality: NULL has been
replaced by ‘1,2,3,4,5,6,7,8,9,10,11,271’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:29:20 UTC
- changes:
- Paleo Interpretation metadata:
- d18OStandard (S2LR1EJaw1fqZ9): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LR9DSUVgi2FG): interpretation1_direction: NULL has been
replaced by ‘negative’
- d18O (S2LR9DSUVgi2FG): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LR9DSUVgi2FG): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Annual’
- d18O (S2LR9DSUVgi2FG): interpretation1_variable: NULL has been
replaced by ‘P’
- d18O (S2LR9DSUVgi2FG): interpretation1_variableDetail: NULL has been
replaced by ‘amount@surface’
- d13CStandard (S2LRaZEDsWzhgR): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRAZhf4859ko): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRE5ZXEOA0gV): interpretation1_direction: NULL has been
replaced by ‘negative’
- d13C (S2LRE5ZXEOA0gV): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13C (S2LRE5ZXEOA0gV): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Annual’
- d13C (S2LRE5ZXEOA0gV): interpretation1_variable: NULL has been
replaced by ‘P-E’
- d13C (S2LRE5ZXEOA0gV): interpretation1_variableDetail: NULL has been
replaced by ‘@surface’
- d18OPrecision (S2LRLp2doS8RlW): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRmoKawXbvpm): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRpLFGK9HqWh): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRx5OBxKN1aB): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CPrecision (S2LRYvhu4IB1a0): interpretation1_scope: NULL has been
replaced by ‘climate’
- Paleo Column metadata:
- d18O (S2LR9DSUVgi2FG): paleoData_notes: NULL has been replaced by
‘“The δ18O variation of rainfall in many tropical locations like the
Vaca Plateau is largely controlled by the amount effect, where increased
amounts of rainfall are correlated with lower δ18O values” (Akers et
al., 2016)’
- d18O (S2LR9DSUVgi2FG): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LR9DSUVgi2FG): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LR9DSUVgi2FG): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LR9DSUVgi2FG): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d13C (S2LRE5ZXEOA0gV): paleoData_notes: NULL has been replaced by
‘“Since vegetative productivity is sensitive to water-stress in the
karstic Vaca Plateau, drier conditions re- duce the amount of biogenic
carbon (although potentially with a tem- poral lag), and thus drier
conditions would be expected to produce higher δ13C values of water in
the epikarst” (Akers et al., 2016)’
- d13C (S2LRE5ZXEOA0gV): paleoData_proxy: NULL has been replaced by
‘d13C’
- d13C (S2LRE5ZXEOA0gV): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d13C (S2LRE5ZXEOA0gV): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d13C (S2LRE5ZXEOA0gV): paleoData_QCCertification: NULL has been
replaced by ‘CH’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:25:28 UTC
- notes: Created from SISALv2