Version history for j5rtTgIzQKqMnmSZEjPK - Heshangcave.C..2008
Version: 1.0.17
- lastVersion: 1.0.16
- curator: nicholas
- timestamp: 2025-06-25 22:46:12.250911 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR984dImqQzT): paleoData_proxy: ‘((( null ))) d13C /// d18O’
has been replaced by ‘d18O’
- d18O (S2LR984dImqQzT): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LR984dImqQzT): paleoData_QCCertification: ‘((( null ))) CH
/// CH, CR’ has been replaced by ‘CH, CR’
- Paleo Interpretation metadata:
- d18O (S2LR984dImqQzT): interpretation1_seasonality: ‘((( null )))
6,7,8 /// Jun-Aug’ has been replaced by ‘Jun-Aug’
- d18O (S2LR984dImqQzT): interpretation1_variable: ‘((( null ))) P ///
precipitation’ has been replaced by ‘precipitation’
Version: 1.0.16
- lastVersion: 1.0.15
- curator: nicholas
- timestamp: 2025-06-25 21:21:52.936675 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR984dImqQzT): paleoData_notes: ‘“The duration of the high
Mg/Ca values corresponds very closely to the high d18O values. Although
reflecting a local rainfall control, the Mg/Ca data is consistent with
the view that high d18O values reflect a regional decrease in rainfall
at this time, rather than only a decrease in temperature or change in
moisture source” (Liu et al., 2013) “therefore appears to be controlled
by the amount of rain falling between them…The calibrated delta d18O
record provides a quantitative history of rainfall in southwest
China…rainfall (and therefore stalagmite) d18O is dominated by the
summer monsoon.” (Hu et al., 2008)’ has been replaced by ‘((( null )))
“The duration of the high Mg/Ca values corresponds very closely to the
high δ18O values. Although reflecting a local rainfall control, the
Mg/Ca data is consistent with the view that high δ18O values reflect a
regional decrease in rainfall at this time, rather than only a decrease
in temperature or change in moisture source” (Liu et al., 2013)
“therefore appears to be controlled by the amount of rain falling
between them…The calibrated Δδ18O record provides a quantitative history
of rainfall in southwest China…rainfall (and therefore sta- lagmite)
δ18O is dominated by the summer monsoon.” (Hu et al., 2008) /// “The
duration of the high Mg/Ca values corresponds very closely to the high
d18O values. Although reflecting a local rainfall control, the Mg/Ca
data is consistent with the view that high d18O values reflect a
regional decrease in rainfall at this time, rather than only a decrease
in temperature or change in moisture source” (Liu et al., 2013)
“therefore appears to be controlled by the amount of rain falling
between them…The calibrated delta d18O record provides a quantitative
history of rainfall in southwest China…rainfall (and therefore
stalagmite) d18O is dominated by the summer monsoon.” (Hu et al.,
2008)’
- d18O (S2LR984dImqQzT): paleoData_proxy: ‘d18O’ has been replaced by
‘((( null ))) d13C /// d18O’
- d18O (S2LR984dImqQzT): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LR984dImqQzT): paleoData_QCCertification: ‘CH, CR’ has been
replaced by ‘((( null ))) CH /// CH, CR’
- d18O (S2LR984dImqQzT): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d18O (S2LR984dImqQzT): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- d18O (S2LRZLbkEc2Xd8): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d18O (S2LRZLbkEc2Xd8): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRfY9R6KETO2): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘FALSE’
- d18O (S2LRfY9R6KETO2): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- Paleo Interpretation metadata:
- d18O (S2LR984dImqQzT): interpretation1_seasonality: ‘Jun-Aug’ has
been replaced by ‘((( null ))) 6,7,8 /// Jun-Aug’
- d18O (S2LR984dImqQzT): interpretation1_variable: ‘precipitation’ has
been replaced by ‘((( null ))) P /// precipitation’
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2023-08-10 22:54:38 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_author: NULL has been replaced by ‘Chaoyong Hu and Gideon M.
Henderson and Junhua Huang and Shucheng Xie and Ying Sun and Kathleen R.
Johnson’
- pub1_journal: NULL has been replaced by ‘Earth and Planetary Science
Letters’
- pub1_pages: NULL has been replaced by ‘221–232’
- pub1_title: NULL has been replaced by ‘Quantification of Holocene
Asian monsoon rainfall from spatially separated cave records’
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2023-05-31 20:38:41 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR984dImqQzT): paleoData_notes: ‘((( ((( “The duration of
the high Mg/Ca values corresponds very closely to the high ��18O values.
Although reflecting a local rainfall control, the Mg/Ca data is
consistent with the view that high ��18O values reflect a regional
decrease in rainfall at this time, rather than only a decrease in
temperature or change in moisture source” (Liu et al., 2013) “therefore
appears to be controlled by the amount of rain falling between them…The
calibrated ����18O record provides a quantitative history of rainfall in
southwest China…rainfall (and therefore sta- lagmite) ��18O is dominated
by the summer monsoon.” (Hu et al., 2008); paleoData_variableName
updated ))) “The duration of the high Mg/Ca values corresponds very
closely to the high δ18O values. Although reflecting a local rainfall
control, the Mg/Ca data is consistent with the view that high δ18O
values reflect a regional decrease in rainfall at this time, rather than
only a decrease in temperature or change in moisture source” (Liu et
al., 2013) “therefore appears to be controlled by the amount of rain
falling between them…The calibrated Δδ18O record provides a quantitative
history of rainfall in southwest China…rainfall (and therefore sta-
lagmite) δ18O is dominated by the summer monsoon.” (Hu et al., 2008) ///
“The duration of the high Mg/Ca values corresponds very closely to the
high δ18O values. Although reflecting a local rainfall control, the
Mg/Ca data is consistent with the view that high δ18O values reflect a
regional decrease in rainfall at this time, rather than only a decrease
in temperature or change in moisture source” (Liu et al., 2013)
“therefore appears to be controlled by the amount of rain falling
between them…The calibrated Δδ18O record provides a quantitative history
of rainfall in southwest China…rainfall (and therefore sta- lagmite)
δ18O is dominated by the summer monsoon.” (Hu et al., 2008) ))) “The
duration of the high Mg/Ca values corresponds very closely to the high
d18O values. Although reflecting a local rainfall control, the Mg/Ca
data is consistent with the view that high d18O values reflect a
regional decrease in rainfall at this time, rather than only a decrease
in temperature or change in moisture source” (Liu et al., 2013)
“therefore appears to be controlled by the amount of rain falling
between them…The calibrated dd18O record provides a quantitative history
of rainfall in southwest China…rainfall (and therefore sta- lagmite)
d18O is dominated by the summer monsoon.” (Hu et al., 2008) /// “The
duration of the high Mg/Ca values corresponds very closely to the high
δ18O values. Although reflecting a local rainfall control, the Mg/Ca
data is consistent with the view that high δ18O values reflect a
regional decrease in rainfall at this time, rather than only a decrease
in temperature or change in moisture source” (Liu et al., 2013)
“therefore appears to be controlled by the amount of rain falling
between them…The calibrated Δδ18O record provides a quantitative history
of rainfall in southwest China…rainfall (and therefore sta- lagmite)
δ18O is dominated by the summer monsoon.” (Hu et al., 2008)’ has been
replaced by ‘“The duration of the high Mg/Ca values corresponds very
closely to the high d18O values. Although reflecting a local rainfall
control, the Mg/Ca data is consistent with the view that high d18O
values reflect a regional decrease in rainfall at this time, rather than
only a decrease in temperature or change in moisture source” (Liu et
al., 2013) “therefore appears to be controlled by the amount of rain
falling between them…The calibrated delta d18O record provides a
quantitative history of rainfall in southwest China…rainfall (and
therefore stalagmite) d18O is dominated by the summer monsoon.” (Hu et
al., 2008)’
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-05-30 15:48:52 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR984dImqQzT): paleoData_notes: ‘“The duration of the high
Mg/Ca values corresponds very closely to the high δ18O values. Although
reflecting a local rainfall control, the Mg/Ca data is consistent with
the view that high δ18O values reflect a regional decrease in rainfall
at this time, rather than only a decrease in temperature or change in
moisture source” (Liu et al., 2013) “therefore appears to be controlled
by the amount of rain falling between them…The calibrated Δδ18O record
provides a quantitative history of rainfall in southwest China…rainfall
(and therefore sta- lagmite) δ18O is dominated by the summer monsoon.”
(Hu et al., 2008)’ has been replaced by ‘((( ((( “The duration of the
high Mg/Ca values corresponds very closely to the high ��18O values.
Although reflecting a local rainfall control, the Mg/Ca data is
consistent with the view that high ��18O values reflect a regional
decrease in rainfall at this time, rather than only a decrease in
temperature or change in moisture source” (Liu et al., 2013) “therefore
appears to be controlled by the amount of rain falling between them…The
calibrated ����18O record provides a quantitative history of rainfall in
southwest China…rainfall (and therefore sta- lagmite) ��18O is dominated
by the summer monsoon.” (Hu et al., 2008); paleoData_variableName
updated ))) “The duration of the high Mg/Ca values corresponds very
closely to the high δ18O values. Although reflecting a local rainfall
control, the Mg/Ca data is consistent with the view that high δ18O
values reflect a regional decrease in rainfall at this time, rather than
only a decrease in temperature or change in moisture source” (Liu et
al., 2013) “therefore appears to be controlled by the amount of rain
falling between them…The calibrated Δδ18O record provides a quantitative
history of rainfall in southwest China…rainfall (and therefore sta-
lagmite) δ18O is dominated by the summer monsoon.” (Hu et al., 2008) ///
“The duration of the high Mg/Ca values corresponds very closely to the
high δ18O values. Although reflecting a local rainfall control, the
Mg/Ca data is consistent with the view that high δ18O values reflect a
regional decrease in rainfall at this time, rather than only a decrease
in temperature or change in moisture source” (Liu et al., 2013)
“therefore appears to be controlled by the amount of rain falling
between them…The calibrated Δδ18O record provides a quantitative history
of rainfall in southwest China…rainfall (and therefore sta- lagmite)
δ18O is dominated by the summer monsoon.” (Hu et al., 2008) ))) “The
duration of the high Mg/Ca values corresponds very closely to the high
d18O values. Although reflecting a local rainfall control, the Mg/Ca
data is consistent with the view that high d18O values reflect a
regional decrease in rainfall at this time, rather than only a decrease
in temperature or change in moisture source” (Liu et al., 2013)
“therefore appears to be controlled by the amount of rain falling
between them…The calibrated dd18O record provides a quantitative history
of rainfall in southwest China…rainfall (and therefore sta- lagmite)
d18O is dominated by the summer monsoon.” (Hu et al., 2008) /// “The
duration of the high Mg/Ca values corresponds very closely to the high
δ18O values. Although reflecting a local rainfall control, the Mg/Ca
data is consistent with the view that high δ18O values reflect a
regional decrease in rainfall at this time, rather than only a decrease
in temperature or change in moisture source” (Liu et al., 2013)
“therefore appears to be controlled by the amount of rain falling
between them…The calibrated Δδ18O record provides a quantitative history
of rainfall in southwest China…rainfall (and therefore sta- lagmite)
δ18O is dominated by the summer monsoon.” (Hu et al., 2008)’
- d18O (S2LR984dImqQzT): paleoData_proxy: ‘d13C’ has been replaced by
‘d18O’
- d18O (S2LR984dImqQzT): paleoData_QCCertification: ‘CH’ has been
replaced by ‘CH, CR’
- Paleo Interpretation metadata:
- d18O (S2LR984dImqQzT): interpretation1_seasonalityGeneral:
‘summerOnly’ has been replaced by ‘Summer’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-05-12 21:56:39 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR984dImqQzT): paleoData_notes: ‘((( “The duration of the
high Mg/Ca values corresponds very closely to the high ��18O values.
Although reflecting a local rainfall control, the Mg/Ca data is
consistent with the view that high ��18O values reflect a regional
decrease in rainfall at this time, rather than only a decrease in
temperature or change in moisture source” (Liu et al., 2013) “therefore
appears to be controlled by the amount of rain falling between them…The
calibrated ����18O record provides a quantitative history of rainfall in
southwest China…rainfall (and therefore sta- lagmite) ��18O is dominated
by the summer monsoon.” (Hu et al., 2008); paleoData_variableName
updated ))) “The duration of the high Mg/Ca values corresponds very
closely to the high δ18O values. Although reflecting a local rainfall
control, the Mg/Ca data is consistent with the view that high δ18O
values reflect a regional decrease in rainfall at this time, rather than
only a decrease in temperature or change in moisture source” (Liu et
al., 2013) “therefore appears to be controlled by the amount of rain
falling between them…The calibrated Δδ18O record provides a quantitative
history of rainfall in southwest China…rainfall (and therefore sta-
lagmite) δ18O is dominated by the summer monsoon.” (Hu et al., 2008) ///
“The duration of the high Mg/Ca values corresponds very closely to the
high δ18O values. Although reflecting a local rainfall control, the
Mg/Ca data is consistent with the view that high δ18O values reflect a
regional decrease in rainfall at this time, rather than only a decrease
in temperature or change in moisture source” (Liu et al., 2013)
“therefore appears to be controlled by the amount of rain falling
between them…The calibrated Δδ18O record provides a quantitative history
of rainfall in southwest China…rainfall (and therefore sta- lagmite)
δ18O is dominated by the summer monsoon.” (Hu et al., 2008)’ has been
replaced by ‘“The duration of the high Mg/Ca values corresponds very
closely to the high δ18O values. Although reflecting a local rainfall
control, the Mg/Ca data is consistent with the view that high δ18O
values reflect a regional decrease in rainfall at this time, rather than
only a decrease in temperature or change in moisture source” (Liu et
al., 2013) “therefore appears to be controlled by the amount of rain
falling between them…The calibrated Δδ18O record provides a quantitative
history of rainfall in southwest China…rainfall (and therefore sta-
lagmite) δ18O is dominated by the summer monsoon.” (Hu et al.,
2008)’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-03-24 22:24:34 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR984dImqQzT): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
Version: 1.0.9
- lastVersion: 1.0.8
- curator: nicholas
- timestamp: 2023-02-13 23:44:14 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR984dImqQzT): paleoData_notes: ‘“The duration of the high
Mg/Ca values corresponds very closely to the high δ18O values. Although
reflecting a local rainfall control, the Mg/Ca data is consistent with
the view that high δ18O values reflect a regional decrease in rainfall
at this time, rather than only a decrease in temperature or change in
moisture source” (Liu et al., 2013) “therefore appears to be controlled
by the amount of rain falling between them…The calibrated Δδ18O record
provides a quantitative history of rainfall in southwest China…rainfall
(and therefore sta- lagmite) δ18O is dominated by the summer monsoon.”
(Hu et al., 2008)’ has been replaced by ‘((( “The duration of the high
Mg/Ca values corresponds very closely to the high ��18O values. Although
reflecting a local rainfall control, the Mg/Ca data is consistent with
the view that high ��18O values reflect a regional decrease in rainfall
at this time, rather than only a decrease in temperature or change in
moisture source” (Liu et al., 2013) “therefore appears to be controlled
by the amount of rain falling between them…The calibrated ����18O record
provides a quantitative history of rainfall in southwest China…rainfall
(and therefore sta- lagmite) ��18O is dominated by the summer monsoon.”
(Hu et al., 2008); paleoData_variableName updated ))) “The duration of
the high Mg/Ca values corresponds very closely to the high δ18O values.
Although reflecting a local rainfall control, the Mg/Ca data is
consistent with the view that high δ18O values reflect a regional
decrease in rainfall at this time, rather than only a decrease in
temperature or change in moisture source” (Liu et al., 2013) “therefore
appears to be controlled by the amount of rain falling between them…The
calibrated Δδ18O record provides a quantitative history of rainfall in
southwest China…rainfall (and therefore sta- lagmite) δ18O is dominated
by the summer monsoon.” (Hu et al., 2008) /// “The duration of the high
Mg/Ca values corresponds very closely to the high δ18O values. Although
reflecting a local rainfall control, the Mg/Ca data is consistent with
the view that high δ18O values reflect a regional decrease in rainfall
at this time, rather than only a decrease in temperature or change in
moisture source” (Liu et al., 2013) “therefore appears to be controlled
by the amount of rain falling between them…The calibrated Δδ18O record
provides a quantitative history of rainfall in southwest China…rainfall
(and therefore sta- lagmite) δ18O is dominated by the summer monsoon.”
(Hu et al., 2008)’
Version: 1.0.8
- lastVersion: 1.0.7
- curator: nicholas
- timestamp: 2023-02-10 14:33:30 UTC
- changes:
- Paleo Interpretation metadata:
- uncertaintyLow (S2LRa2XG8bLDli): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRaqm4TrmTmp): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRPqZkuzvYC4): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LRyO93mEmF3K): interpretation1_scope: NULL has
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Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2022-07-28 17:32:31 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘294’ has been replaced by NULL
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2022-07-15 23:02:20 UTC
- changes:
- Paleo Interpretation metadata:
- hasAragoniteCorrection (S2LR3FLogXSuxH): interpretation1_scope: NULL
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- hasAragoniteCorrectionComposite (S2LR573TDxWOaZ):
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- d13CStandard (S2LR5cZ9i36T0q): interpretation1_scope: NULL has been
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- d13C (S2LR6BwDNc8xsC): interpretation1_scope: NULL has been replaced
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- mineralogyComposite (S2LR7W1xDfrC66): interpretation1_scope: NULL
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- mineralogy (S2LR98DNCBsqtH): interpretation1_scope: NULL has been
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- depthComposite (S2LRfQSED5niUJ): interpretation1_scope: NULL has
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- d18O (S2LRfY9R6KETO2): interpretation1_scope: NULL has been replaced
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- thickness (S2LRXhBTTCNWZ0): interpretation1_scope: NULL has been
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- d18O (S2LRZLbkEc2Xd8): interpretation1_scope: NULL has been replaced
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Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2021-10-05 21:39:52 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: NULL has been replaced by ‘Asia>Eastern
Asia>China’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nick
- timestamp: 2021-03-17 01:53:53 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Interpretation metadata:
- d18OComposite (S2LR984dImqQzT): interpretation1_seasonalityGeneral:
‘Summer’ has been replaced by ‘summerOnly’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:28:59 UTC
- changes:
- Paleo Interpretation metadata:
- hasAragoniteCorrection (S2LR3FLogXSuxH): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrectionComposite (S2LR573TDxWOaZ):
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- d13CStandard (S2LR5cZ9i36T0q): interpretation1_scope: NULL has been
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- d13C (S2LR6BwDNc8xsC): interpretation1_scope: NULL has been replaced
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- mineralogyComposite (S2LR7W1xDfrC66): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OComposite (S2LR984dImqQzT): interpretation1_direction: NULL has
been replaced by ‘negative’
- d18OComposite (S2LR984dImqQzT): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OComposite (S2LR984dImqQzT): interpretation1_seasonality: NULL
has been replaced by ‘6,7,8’
- d18OComposite (S2LR984dImqQzT): interpretation1_seasonalityGeneral:
NULL has been replaced by ‘Summer’
- d18OComposite (S2LR984dImqQzT): interpretation1_variable: NULL has
been replaced by ‘P’
- d18OComposite (S2LR984dImqQzT): interpretation1_variableDetail: NULL
has been replaced by ‘amount@surface’
- mineralogy (S2LR98DNCBsqtH): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRAjeYfU2bI4): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CComposite (S2LRbcIPbfbkeg): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandardComposite (S2LRc7ZN55Fi2y): interpretation1_scope: NULL
has been replaced by ‘climate’
- depthComposite (S2LRfQSED5niUJ): interpretation1_scope: NULL has
been replaced by ‘climate’
- d18O (S2LRfY9R6KETO2): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OPrecisionComposite (S2LRGb9d02JrGt): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleIDComposite (S2LRHKNDm7qyFS): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandard (S2LRhqhqloq3T2): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRIIunAKBwVd): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecisionComposite (S2LRIZT7IuAsIV): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OPrecision (S2LRkGbx6KeRL2): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRkPAiTdLLah): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRLCc6PglKzP): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRLvQ3Zmi3qE): interpretation1_scope: NULL has been replaced
by ‘climate’
- hasAragoniteCorrection (S2LRQ2VBe6hu4e): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CStandardComposite (S2LRqX8jU13fTa): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRTx6rEauxLX): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRvLgKIQb3ei): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRXhBTTCNWZ0): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRxzZLAw42KT): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRysheexn52X): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRZLbkEc2Xd8): interpretation1_scope: NULL has been replaced
by ‘climate’
- entityName (S2LRZut1uDfvZw): interpretation1_scope: NULL has been
replaced by ‘climate’
- Paleo Column metadata:
- d18OComposite (S2LR984dImqQzT): paleoData_notes: NULL has been
replaced by ‘“The duration of the high Mg/Ca values corresponds very
closely to the high δ18O values. Although reflecting a local rainfall
control, the Mg/Ca data is consistent with the view that high δ18O
values reflect a regional decrease in rainfall at this time, rather than
only a decrease in temperature or change in moisture source” (Liu et
al., 2013) “therefore appears to be controlled by the amount of rain
falling between them…The calibrated Δδ18O record provides a quantitative
history of rainfall in southwest China…rainfall (and therefore sta-
lagmite) δ18O is dominated by the summer monsoon.” (Hu et al.,
2008)’
- d18OComposite (S2LR984dImqQzT): paleoData_proxy: NULL has been
replaced by ‘d13C’
- d18OComposite (S2LR984dImqQzT): paleoData_proxyGeneral: NULL has
been replaced by ‘isotope’
- d18OComposite (S2LR984dImqQzT): paleoData_QCCertification: NULL has
been replaced by ‘CH’
- d18OComposite (S2LR984dImqQzT): paleoData_QCnotes: NULL has been
replaced by ‘High resolution sampling for 8.2 period. Both from same
stal. Could probably just use default lipd coposite’
- d18O (S2LRfY9R6KETO2): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRfY9R6KETO2): paleoData_QCnotes: NULL has been replaced by
‘“In this study, we describe a detailed investigation of this section of
HS4, focusing on a sub-sample measuring” (Liu et al, 2013)’
- thickness (S2LRXhBTTCNWZ0): paleoData_notes: NULL has been replaced
by ‘“At fast drip rates, such as those in Heshang, drip rate is not
normally the major control on growth rate so, although the thinner
layers are consistent with lower drip rates, the large change in
thickness during the event may also suggest a coeval cooling.” (Liu et
al., 2013)’
- d18O (S2LRZLbkEc2Xd8): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRZLbkEc2Xd8): paleoData_QCnotes: NULL has been replaced by
‘“Previous work on this sample has allowed construction of a
quantitative3 Holocene record of rainfall in Central China” (Liu et al,
2013)’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:26:23 UTC
- notes: Created from SISALv2