Version history for Qg48HDODkKXCqocWQBVm -
Xiaobailongcave.Cai.2015
Version: 1.0.17
- lastVersion: 1.0.16
- curator: nicholas
- timestamp: 2023-08-10 23:23:07 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_author: NULL has been replaced by ‘Yanjun Cai and Inez Y. Fung
and R. Lawrence Edwards and Zhisheng An and Hai Cheng and Jung-Eun Lee
and Liangcheng Tan and Chuan-Chou Shen and Xianfeng Wang and Jesse A.
Day and Weijian Zhou and Megan J. Kelly and John C. H. Chiang’
- pub1_journal: NULL has been replaced by ‘Proceedings of the National
Academy of Sciences’
- pub1_pages: NULL has been replaced by ‘2954–2959’
- pub1_title: NULL has been replaced by ‘Variability of
stalagmite-inferred Indian monsoon precipitation over the past 252,000
y’
Version: 1.0.16
- lastVersion: 1.0.15
- curator: nicholas
- timestamp: 2023-05-31 20:40:44 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR3sFUdg8g4z): paleoData_notes: ‘((( ((( ((( “We therefore
conclude that XBL ��18Oc serves as a proxy of Indian Monsoon strength,
defined as the intensity of rainfall over both the Bay of Bengal and the
Monsoon Zone…A Speleothem ��18O record from Xiaobailong cave in
southwest China characterizes changes in summer monsoon precipitation”
(Cai et al., 2015) ))) Amount effect: “We therefore conclude that XBL
��18Oc serves as a proxy of Indian Monsoon strength, defined as the
intensity of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem ��18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015) /// Amount effect: “We therefore conclude that XBL ��18Oc serves
as a proxy of Indian Monsoon strength, defined as the intensity of
rainfall over both the Bay of Bengal and the Monsoon Zone…A Speleothem
��18O record from Xiaobailong cave in southwest China characterizes
changes in summer monsoon precipitation” (Cai et al., 2015);
paleoData_variableName updated ))) ((( “We therefore conclude that XBL
δ18Oc serves as a proxy of Indian Monsoon strength, defined as the
intensity of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015) ))) Amount effect: “We therefore conclude that XBL δ18Oc serves as
a proxy of Indian Monsoon strength, defined as the intensity of rainfall
over both the Bay of Bengal and the Monsoon Zone…A Speleothem δ18O
record from Xiaobailong cave in southwest China characterizes changes in
summer monsoon precipitation” (Cai et al., 2015) /// Amount effect: “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015) /// ((( “We therefore conclude that
XBL δ18Oc serves as a proxy of Indian Monsoon strength, defined as the
intensity of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015) ))) Amount effect: “We therefore conclude that XBL δ18Oc serves as
a proxy of Indian Monsoon strength, defined as the intensity of rainfall
over both the Bay of Bengal and the Monsoon Zone…A Speleothem δ18O
record from Xiaobailong cave in southwest China characterizes changes in
summer monsoon precipitation” (Cai et al., 2015) /// Amount effect: “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015) ))) Amount effect: “We therefore
conclude that XBL d18Oc serves as a proxy of Indian Monsoon strength,
defined as the intensity of rainfall over both the Bay of Bengal and the
Monsoon Zone…A Speleothem d18O record from Xiaobailong cave in southwest
China characterizes changes in summer monsoon precipitation” (Cai et
al., 2015) /// Amount effect: “We therefore conclude that XBL δ18Oc
serves as a proxy of Indian Monsoon strength, defined as the intensity
of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015)’ has been replaced by ‘Amount effect: “We therefore conclude that
XBL d18Oc serves as a proxy of Indian Monsoon strength, defined as the
intensity of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem d18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015)’
Version: 1.0.15
- lastVersion: 1.0.14
- curator: nicholas
- timestamp: 2023-05-30 15:50:57 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR3sFUdg8g4z): paleoData_notes: ‘Amount effect: “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015)’ has been replaced by ‘((( ((( ((( “We
therefore conclude that XBL ��18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem ��18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015) ))) Amount effect: “We therefore
conclude that XBL ��18Oc serves as a proxy of Indian Monsoon strength,
defined as the intensity of rainfall over both the Bay of Bengal and the
Monsoon Zone…A Speleothem ��18O record from Xiaobailong cave in
southwest China characterizes changes in summer monsoon precipitation”
(Cai et al., 2015) /// Amount effect: “We therefore conclude that XBL
��18Oc serves as a proxy of Indian Monsoon strength, defined as the
intensity of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem ��18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015); paleoData_variableName updated ))) ((( “We therefore conclude
that XBL δ18Oc serves as a proxy of Indian Monsoon strength, defined as
the intensity of rainfall over both the Bay of Bengal and the Monsoon
Zone…A Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015) ))) Amount effect: “We therefore conclude that XBL δ18Oc serves as
a proxy of Indian Monsoon strength, defined as the intensity of rainfall
over both the Bay of Bengal and the Monsoon Zone…A Speleothem δ18O
record from Xiaobailong cave in southwest China characterizes changes in
summer monsoon precipitation” (Cai et al., 2015) /// Amount effect: “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015) /// ((( “We therefore conclude that
XBL δ18Oc serves as a proxy of Indian Monsoon strength, defined as the
intensity of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015) ))) Amount effect: “We therefore conclude that XBL δ18Oc serves as
a proxy of Indian Monsoon strength, defined as the intensity of rainfall
over both the Bay of Bengal and the Monsoon Zone…A Speleothem δ18O
record from Xiaobailong cave in southwest China characterizes changes in
summer monsoon precipitation” (Cai et al., 2015) /// Amount effect: “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015) ))) Amount effect: “We therefore
conclude that XBL d18Oc serves as a proxy of Indian Monsoon strength,
defined as the intensity of rainfall over both the Bay of Bengal and the
Monsoon Zone…A Speleothem d18O record from Xiaobailong cave in southwest
China characterizes changes in summer monsoon precipitation” (Cai et
al., 2015) /// Amount effect: “We therefore conclude that XBL δ18Oc
serves as a proxy of Indian Monsoon strength, defined as the intensity
of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015)’
- d18O (S2LR3sFUdg8g4z): paleoData_QCCertification: ‘CH’ has been
replaced by ‘CH, CR’
- Paleo Interpretation metadata:
- d18O (S2LR3sFUdg8g4z): interpretation1_seasonalityGeneral:
‘summerOnly’ has been replaced by ‘Summer’
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2023-05-25 18:00:24 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Geographic metadata:
- geo_elevation: NULL has been replaced by ‘1500’
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2023-05-12 22:14:59 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR3sFUdg8g4z): paleoData_notes: ‘((( ((( “We therefore
conclude that XBL ��18Oc serves as a proxy of Indian Monsoon strength,
defined as the intensity of rainfall over both the Bay of Bengal and the
Monsoon Zone…A Speleothem ��18O record from Xiaobailong cave in
southwest China characterizes changes in summer monsoon precipitation”
(Cai et al., 2015) ))) Amount effect: “We therefore conclude that XBL
��18Oc serves as a proxy of Indian Monsoon strength, defined as the
intensity of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem ��18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015) /// Amount effect: “We therefore conclude that XBL ��18Oc serves
as a proxy of Indian Monsoon strength, defined as the intensity of
rainfall over both the Bay of Bengal and the Monsoon Zone…A Speleothem
��18O record from Xiaobailong cave in southwest China characterizes
changes in summer monsoon precipitation” (Cai et al., 2015);
paleoData_variableName updated ))) ((( “We therefore conclude that XBL
δ18Oc serves as a proxy of Indian Monsoon strength, defined as the
intensity of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015) ))) Amount effect: “We therefore conclude that XBL δ18Oc serves as
a proxy of Indian Monsoon strength, defined as the intensity of rainfall
over both the Bay of Bengal and the Monsoon Zone…A Speleothem δ18O
record from Xiaobailong cave in southwest China characterizes changes in
summer monsoon precipitation” (Cai et al., 2015) /// Amount effect: “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015) /// ((( “We therefore conclude that
XBL δ18Oc serves as a proxy of Indian Monsoon strength, defined as the
intensity of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015) ))) Amount effect: “We therefore conclude that XBL δ18Oc serves as
a proxy of Indian Monsoon strength, defined as the intensity of rainfall
over both the Bay of Bengal and the Monsoon Zone…A Speleothem δ18O
record from Xiaobailong cave in southwest China characterizes changes in
summer monsoon precipitation” (Cai et al., 2015) /// Amount effect: “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015)’ has been replaced by ‘Amount effect:
“We therefore conclude that XBL δ18Oc serves as a proxy of Indian
Monsoon strength, defined as the intensity of rainfall over both the Bay
of Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015)’
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-03-24 22:26:50 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR3sFUdg8g4z): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-02-14 00:00:02 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR3sFUdg8g4z): paleoData_notes: ‘((( “We therefore conclude
that XBL δ18Oc serves as a proxy of Indian Monsoon strength, defined as
the intensity of rainfall over both the Bay of Bengal and the Monsoon
Zone…A Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015) ))) Amount effect: “We therefore conclude that XBL δ18Oc serves as
a proxy of Indian Monsoon strength, defined as the intensity of rainfall
over both the Bay of Bengal and the Monsoon Zone…A Speleothem δ18O
record from Xiaobailong cave in southwest China characterizes changes in
summer monsoon precipitation” (Cai et al., 2015) /// Amount effect: “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015)’ has been replaced by ‘((( ((( “We
therefore conclude that XBL ��18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem ��18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015) ))) Amount effect: “We therefore
conclude that XBL ��18Oc serves as a proxy of Indian Monsoon strength,
defined as the intensity of rainfall over both the Bay of Bengal and the
Monsoon Zone…A Speleothem ��18O record from Xiaobailong cave in
southwest China characterizes changes in summer monsoon precipitation”
(Cai et al., 2015) /// Amount effect: “We therefore conclude that XBL
��18Oc serves as a proxy of Indian Monsoon strength, defined as the
intensity of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem ��18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015); paleoData_variableName updated ))) ((( “We therefore conclude
that XBL δ18Oc serves as a proxy of Indian Monsoon strength, defined as
the intensity of rainfall over both the Bay of Bengal and the Monsoon
Zone…A Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015) ))) Amount effect: “We therefore conclude that XBL δ18Oc serves as
a proxy of Indian Monsoon strength, defined as the intensity of rainfall
over both the Bay of Bengal and the Monsoon Zone…A Speleothem δ18O
record from Xiaobailong cave in southwest China characterizes changes in
summer monsoon precipitation” (Cai et al., 2015) /// Amount effect: “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015) /// ((( “We therefore conclude that
XBL δ18Oc serves as a proxy of Indian Monsoon strength, defined as the
intensity of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015) ))) Amount effect: “We therefore conclude that XBL δ18Oc serves as
a proxy of Indian Monsoon strength, defined as the intensity of rainfall
over both the Bay of Bengal and the Monsoon Zone…A Speleothem δ18O
record from Xiaobailong cave in southwest China characterizes changes in
summer monsoon precipitation” (Cai et al., 2015) /// Amount effect: “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015)’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-02-10 14:35:02 UTC
- changes:
- Paleo Interpretation metadata:
- uncertaintyLow (S2LR0hUKAUJNxq): interpretation1_scope: NULL has
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Version: 1.0.8
- lastVersion: 1.0.7
- curator: nicholas
- timestamp: 2023-01-27 00:06:06 UTC
- changes:
- Paleo Column metadata:
- d18OComposite (S2LR3sFUdg8g4z): paleoData_notes: ‘Amount effect: “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015)’ has been replaced by ‘((( “We
therefore conclude that XBL δ18Oc serves as a proxy of Indian Monsoon
strength, defined as the intensity of rainfall over both the Bay of
Bengal and the Monsoon Zone…A Speleothem δ18O record from Xiaobailong
cave in southwest China characterizes changes in summer monsoon
precipitation” (Cai et al., 2015) ))) Amount effect: “We therefore
conclude that XBL δ18Oc serves as a proxy of Indian Monsoon strength,
defined as the intensity of rainfall over both the Bay of Bengal and the
Monsoon Zone…A Speleothem δ18O record from Xiaobailong cave in southwest
China characterizes changes in summer monsoon precipitation” (Cai et
al., 2015) /// Amount effect: “We therefore conclude that XBL δ18Oc
serves as a proxy of Indian Monsoon strength, defined as the intensity
of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015)’
Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2022-07-28 17:44:08 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘1500’ has been replaced by NULL
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2022-07-15 23:12:51 UTC
- changes:
- Paleo Interpretation metadata:
- hasAragoniteCorrectionComposite (S2LR2BkFBsjalB):
interpretation1_scope: NULL has been replaced by ‘climate’
- d18OStandard (S2LR2NV6siVvES): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LR2VjITyheAR): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LR3Cj1yBTFbt): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandardComposite (S2LR3Eu0RV0f6W): interpretation1_scope: NULL
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- d18OStandard (S2LR3sjjYISKly): interpretation1_scope: NULL has been
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- d18OPrecision (S2LR48DaxS7PLf): interpretation1_scope: NULL has been
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- sisalSampleID (S2LR8tUFfubEXJ): interpretation1_scope: NULL has been
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- d18O (S2LR9uWdelIiPr): interpretation1_scope: NULL has been replaced
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- hasHiatus (S2LRAEgQ3HLDMW): interpretation1_scope: NULL has been
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- mineralogy (S2LRagfY2ITXax): interpretation1_scope: NULL has been
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- d18OPrecision (S2LRAle4XojWsZ): interpretation1_scope: NULL has been
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- entityName (S2LRBk7KmNUz0Y): interpretation1_scope: NULL has been
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- d18OPrecision (S2LRcvp5a4WpAS): interpretation1_scope: NULL has been
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- d18OPrecision (S2LRe8ROE5xTeR): interpretation1_scope: NULL has been
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- d18O (S2LRF01poyDydo): interpretation1_scope: NULL has been replaced
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- sisalSampleID (S2LRf43Zl7rW8n): interpretation1_scope: NULL has been
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- d18OPrecision (S2LRfuCoEIy0TO): interpretation1_scope: NULL has been
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- mineralogy (S2LRg2pQF530jv): interpretation1_scope: NULL has been
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- d18OStandard (S2LRgHQFcYVCXB): interpretation1_scope: NULL has been
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- hasAragoniteCorrection (S2LRH8Wv71WXQ5): interpretation1_scope: NULL
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- d18O (S2LRHfD9B2cXNG): interpretation1_scope: NULL has been replaced
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- mineralogy (S2LRhm4gQNR9W7): interpretation1_scope: NULL has been
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- mineralogy (S2LRHxYTj81ozD): interpretation1_scope: NULL has been
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- d18O (S2LRhzvEeYh1JT): interpretation1_scope: NULL has been replaced
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- d18OPrecision (S2LRIIAn1ny8IP): interpretation1_scope: NULL has been
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- mineralogy (S2LRIkaheaDwoe): interpretation1_scope: NULL has been
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- sisalSampleID (S2LRKjj24nwmxO): interpretation1_scope: NULL has been
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- sisalSampleID (S2LRKXhqpu8xgi): interpretation1_scope: NULL has been
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- d18O (S2LRL9weutwCZH): interpretation1_scope: NULL has been replaced
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- d18OStandard (S2LRlg2u87nv8q): interpretation1_scope: NULL has been
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- d18OPrecision (S2LRLmmGhdReli): interpretation1_scope: NULL has been
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- hasAragoniteCorrection (S2LRMJSqNnzN0v): interpretation1_scope: NULL
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- sisalSampleID (S2LRnb5i6z0Sdm): interpretation1_scope: NULL has been
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- d18OPrecision (S2LRO5WfYstxEL): interpretation1_scope: NULL has been
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- hasAragoniteCorrection (S2LROGaCB3pRYV): interpretation1_scope: NULL
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- d18OStandard (S2LRP3MDqNx6Nf): interpretation1_scope: NULL has been
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- d18OStandard (S2LRpAUynzPDsV): interpretation1_scope: NULL has been
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- sisalSampleIDComposite (S2LRpFuWdbNb8L): interpretation1_scope: NULL
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- hasAragoniteCorrection (S2LRpJbVdWwhUj): interpretation1_scope: NULL
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- d18OStandard (S2LRPKnw54HlZJ): interpretation1_scope: NULL has been
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- hasAragoniteCorrection (S2LRqmOvgxHSYf): interpretation1_scope: NULL
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- sisalSampleID (S2LRqTaShhRslx): interpretation1_scope: NULL has been
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- d18OStandard (S2LRRmuZq7ZeWp): interpretation1_scope: NULL has been
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- hasAragoniteCorrection (S2LRTfVf0pqUMY): interpretation1_scope: NULL
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- hasAragoniteCorrection (S2LRTPpjcA9Eyu): interpretation1_scope: NULL
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- sisalSampleID (S2LRtPuvWHUufb): interpretation1_scope: NULL has been
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- hasAragoniteCorrection (S2LRtvcersD9j0): interpretation1_scope: NULL
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- d18O (S2LRuNIdWtcMd5): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LRX5UNL5MHWc): interpretation1_scope: NULL has been
replaced by ‘climate’
- depthComposite (S2LRx9tmNGlkzv): interpretation1_scope: NULL has
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- d18OPrecisionComposite (S2LRxR3IAFk3Ns): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18O (S2LRXxYbecdweG): interpretation1_scope: NULL has been replaced
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- mineralogy (S2LRyUuVM7nV5m): interpretation1_scope: NULL has been
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- sisalSampleID (S2LRZ7s2ebRzsd): interpretation1_scope: NULL has been
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- mineralogyComposite (S2LRZBLv7vtfeA): interpretation1_scope: NULL
has been replaced by ‘climate’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2021-11-17 02:10:59 UTC
- changes:
- Paleo Column metadata:
- d18OComposite (S2LR3sFUdg8g4z): paleoData_notes: ‘“We therefore
conclude that XBL δ18Oc serves as a proxy of Indian Monsoon strength,
defined as the intensity of rainfall over both the Bay of Bengal and the
Monsoon Zone…A Speleothem δ18O record from Xiaobailong cave in southwest
China characterizes changes in summer monsoon precipitation” (Cai et
al., 2015)’ has been replaced by ‘Amount effect: “We therefore conclude
that XBL δ18Oc serves as a proxy of Indian Monsoon strength, defined as
the intensity of rainfall over both the Bay of Bengal and the Monsoon
Zone…A Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015)’
- Paleo Interpretation metadata:
- d18OComposite (S2LR3sFUdg8g4z): interpretation1_variable: ‘M’ has
been replaced by ‘P’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2021-10-05 21:43:36 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 01:58:23 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Column metadata:
- d18OComposite (S2LR3sFUdg8g4z): paleoData_notes: ‘“We therefore
conclude that XBL δ18Oc serves as a proxy of Indian Monsoon strength,
defined as the intensity of rainfall over both the Bay of Bengal and the
Monsoon Zone…A speleothem δ18O record from Xiaobailong cave in southwest
China characterizes changes in summer monsoon precipitation” (Cai et
al., 2015)’ has been replaced by ‘“We therefore conclude that XBL δ18Oc
serves as a proxy of Indian Monsoon strength, defined as the intensity
of rainfall over both the Bay of Bengal and the Monsoon Zone…A
Speleothem δ18O record from Xiaobailong cave in southwest China
characterizes changes in summer monsoon precipitation” (Cai et al.,
2015)’
- Paleo Interpretation metadata:
- d18OComposite (S2LR3sFUdg8g4z): interpretation1_seasonalityGeneral:
‘Summer’ has been replaced by ‘summerOnly’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:29:59 UTC
- changes:
- Paleo Interpretation metadata:
- hasAragoniteCorrectionComposite (S2LR2BkFBsjalB):
interpretation1_scope: NULL has been replaced by ‘climate’
- d18OStandard (S2LR2NV6siVvES): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LR2VjITyheAR): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LR3Cj1yBTFbt): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandardComposite (S2LR3Eu0RV0f6W): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OComposite (S2LR3sFUdg8g4z): interpretation1_direction: NULL has
been replaced by ‘negative’
- d18OComposite (S2LR3sFUdg8g4z): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OComposite (S2LR3sFUdg8g4z): interpretation1_seasonality: NULL
has been replaced by ‘6,7,8’
- d18OComposite (S2LR3sFUdg8g4z): interpretation1_seasonalityGeneral:
NULL has been replaced by ‘Summer’
- d18OComposite (S2LR3sFUdg8g4z): interpretation1_variable: NULL has
been replaced by ‘M’
- d18OComposite (S2LR3sFUdg8g4z): interpretation1_variableDetail: NULL
has been replaced by ‘monsoon@surface’
- d18OStandard (S2LR3sjjYISKly): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LR48DaxS7PLf): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LR8tUFfubEXJ): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LR9uWdelIiPr): interpretation1_scope: NULL has been replaced
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- hasHiatus (S2LRAEgQ3HLDMW): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRagfY2ITXax): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRAle4XojWsZ): interpretation1_scope: NULL has been
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- entityName (S2LRBk7KmNUz0Y): interpretation1_scope: NULL has been
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- d18OPrecision (S2LRcvp5a4WpAS): interpretation1_scope: NULL has been
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- d18OPrecision (S2LRe8ROE5xTeR): interpretation1_scope: NULL has been
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- d18O (S2LRF01poyDydo): interpretation1_scope: NULL has been replaced
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- sisalSampleID (S2LRf43Zl7rW8n): interpretation1_scope: NULL has been
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- d18OPrecision (S2LRfuCoEIy0TO): interpretation1_scope: NULL has been
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- mineralogy (S2LRg2pQF530jv): interpretation1_scope: NULL has been
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- d18OStandard (S2LRgHQFcYVCXB): interpretation1_scope: NULL has been
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- hasAragoniteCorrection (S2LRH8Wv71WXQ5): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18O (S2LRHfD9B2cXNG): interpretation1_scope: NULL has been replaced
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- mineralogy (S2LRhm4gQNR9W7): interpretation1_scope: NULL has been
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- mineralogy (S2LRHxYTj81ozD): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRhzvEeYh1JT): interpretation1_scope: NULL has been replaced
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- d18OPrecision (S2LRIIAn1ny8IP): interpretation1_scope: NULL has been
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- mineralogy (S2LRIkaheaDwoe): interpretation1_scope: NULL has been
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- sisalSampleID (S2LRKjj24nwmxO): interpretation1_scope: NULL has been
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- sisalSampleID (S2LRKXhqpu8xgi): interpretation1_scope: NULL has been
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- d18O (S2LRL9weutwCZH): interpretation1_scope: NULL has been replaced
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- d18OStandard (S2LRlg2u87nv8q): interpretation1_scope: NULL has been
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- d18OPrecision (S2LRLmmGhdReli): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRMJSqNnzN0v): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRnb5i6z0Sdm): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRO5WfYstxEL): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LROGaCB3pRYV): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandard (S2LRP3MDqNx6Nf): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRpAUynzPDsV): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleIDComposite (S2LRpFuWdbNb8L): interpretation1_scope: NULL
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- hasAragoniteCorrection (S2LRpJbVdWwhUj): interpretation1_scope: NULL
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- d18OStandard (S2LRPKnw54HlZJ): interpretation1_scope: NULL has been
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- hasAragoniteCorrection (S2LRqmOvgxHSYf): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRqTaShhRslx): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRRmuZq7ZeWp): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRTfVf0pqUMY): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRTPpjcA9Eyu): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRtPuvWHUufb): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRtvcersD9j0): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18O (S2LRuNIdWtcMd5): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LRX5UNL5MHWc): interpretation1_scope: NULL has been
replaced by ‘climate’
- depthComposite (S2LRx9tmNGlkzv): interpretation1_scope: NULL has
been replaced by ‘climate’
- d18OPrecisionComposite (S2LRxR3IAFk3Ns): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18O (S2LRXxYbecdweG): interpretation1_scope: NULL has been replaced
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- mineralogy (S2LRyUuVM7nV5m): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRZ7s2ebRzsd): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogyComposite (S2LRZBLv7vtfeA): interpretation1_scope: NULL
has been replaced by ‘climate’
- Paleo Column metadata:
- d18O (S2LR3Cj1yBTFbt): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LR3Cj1yBTFbt): paleoData_QCnotes: NULL has been replaced by
‘This is the only holocene relevant record. However, can create author
composite by ““combined the different stalagmite records by
interpolating each to 10 yr resolution and averaging to produce the XBL
composite record” (Cai et al., 2015). Exact data unavailable.’
- d18OComposite (S2LR3sFUdg8g4z): paleoData_notes: NULL has been
replaced by ‘“We therefore conclude that XBL δ18Oc serves as a proxy of
Indian Monsoon strength, defined as the intensity of rainfall over both
the Bay of Bengal and the Monsoon Zone…A speleothem δ18O record from
Xiaobailong cave in southwest China characterizes changes in summer
monsoon precipitation” (Cai et al., 2015)’
- d18OComposite (S2LR3sFUdg8g4z): paleoData_proxy: NULL has been
replaced by ‘d18O’
- d18OComposite (S2LR3sFUdg8g4z): paleoData_proxyDetail: NULL has been
replaced by ‘calcite’
- d18OComposite (S2LR3sFUdg8g4z): paleoData_proxyGeneral: NULL has
been replaced by ‘isotope’
- d18OComposite (S2LR3sFUdg8g4z): paleoData_QCCertification: NULL has
been replaced by ‘CH’
- d18OComposite (S2LR3sFUdg8g4z): paleoData_QCnotes: NULL has been
replaced by ‘“We combined the different stalagmite records by
interpolating each to 10 yr resolution and averaging to produce the XBL
composite record” (Cai et al., 2015)’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:26:32 UTC
- notes: Created from SISALv2