Version history for d0XeA7lYFUx6ttuPQpvA -
Haozhucave.Zhang.2016
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-06-25 22:46:11.857197 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (S2LRCbiTKqyT4F): interpretation1_seasonality: ‘((( null )))
6,7,8,9 /// Jun-Sep’ has been replaced by ‘Jun-Sep’
- d18O (S2LRCbiTKqyT4F): interpretation1_variable: ‘((( null ))) P ///
precipitation’ has been replaced by ‘precipitation’
- d18O (S2LRmuTd4DkrsZ): interpretation1_seasonality: ‘((( null )))
6,7,8,9 /// Jun-Sep’ has been replaced by ‘Jun-Sep’
- d18O (S2LRmuTd4DkrsZ): interpretation1_variable: ‘((( null ))) P ///
precipitation’ has been replaced by ‘precipitation’
- d18O (S2LRxiKWn6JEMw): interpretation1_seasonality: ‘((( null )))
6,7,8,9 /// Jun-Sep’ has been replaced by ‘Jun-Sep’
- d18O (S2LRxiKWn6JEMw): interpretation1_variable: ‘((( null ))) P ///
precipitation’ has been replaced by ‘precipitation’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:28:58 UTC
- changes:
- Paleo Interpretation metadata:
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- d18O (S2LRCbiTKqyT4F): interpretation1_direction: NULL has been
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- d18O (S2LRCbiTKqyT4F): interpretation1_scope: NULL has been replaced
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- d18O (S2LRCbiTKqyT4F): interpretation1_seasonality: NULL has been
replaced by ‘6,7,8,9’
- d18O (S2LRCbiTKqyT4F): interpretation1_seasonalityGeneral: NULL has
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- d18O (S2LRCbiTKqyT4F): interpretation1_variable: NULL has been
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- entityName (S2LRDbx7spXqSr): interpretation1_scope: NULL has been
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- hasAragoniteCorrectionComposite (S2LRHzTMTqUE7T):
interpretation1_scope: NULL has been replaced by ‘climate’
- mineralogyComposite (S2LRjULv3X7enS): interpretation1_scope: NULL
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- d18OPrecision (S2LRkLl3mZQxoH): interpretation1_scope: NULL has been
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- sisalSampleID (S2LRKozWDACPJH): interpretation1_scope: NULL has been
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- depthComposite (S2LRKsXomJ1nKk): interpretation1_scope: NULL has
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- d18O (S2LRmuTd4DkrsZ): interpretation1_direction: NULL has been
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- d18O (S2LRmuTd4DkrsZ): interpretation1_seasonality: NULL has been
replaced by ‘6,7,8,9’
- d18O (S2LRmuTd4DkrsZ): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Summer’
- d18O (S2LRmuTd4DkrsZ): interpretation1_variable: NULL has been
replaced by ‘P’
- d18O (S2LRmuTd4DkrsZ): interpretation1_variableDetail: NULL has been
replaced by ‘amount@surface’
- d18OStandard (S2LRnbOo9tKaLq): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LROLzv2Lsbbc): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleIDComposite (S2LRPy0O0UVrHv): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OPrecision (S2LRQ1uXW4CoYg): interpretation1_scope: NULL has been
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- hasAragoniteCorrection (S2LRQVD11rJ3NM): interpretation1_scope: NULL
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- d18OComposite (S2LRxiKWn6JEMw): interpretation1_variable: NULL has
been replaced by ‘P’
- d18OComposite (S2LRxiKWn6JEMw): interpretation1_variableDetail: NULL
has been replaced by ‘amount@surface’
- mineralogy (S2LRZY7HTlGSdf): interpretation1_scope: NULL has been
replaced by ‘climate’
- Paleo Column metadata:
- d18O (S2LRCbiTKqyT4F): paleoData_notes: NULL has been replaced by
‘“we thus interpret the δ18O changes observed in stalagmites HZZ11 and
HZZ27 to reflect regional monsoon intensity and the subsequent effects
on upstream isotope depletion…Orbital to millennial scale variations in
speleothem δ18O from the Asian monsoon region have traditionally been
interpreted to reflect changes in local/regional rainfall amount… the
ratio of sum- mer to annual rainfall expressed as monsoon intensity”
(Zhang et al., 2016)’
- d18O (S2LRCbiTKqyT4F): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRCbiTKqyT4F): paleoData_proxyDetail: NULL has been replaced
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replaced by ‘CH’
- d18O (S2LRCbiTKqyT4F): paleoData_QCnotes: NULL has been replaced by
‘HZZ11. “If two or more δ18O time series replicate well, it can be as-
sumed that both δ18O profiles primarily reflect real climate sig- nals,
and kinetic fractionation is thus likely absent or insignif- icant…The
HZZ11 and HZZ27 δ 18 O records agree well with each other (Fig. 3A), and
are consistent with the results from Hulu” (Zhang et al., 2016)’
- d18O (S2LRmuTd4DkrsZ): paleoData_notes: NULL has been replaced by
‘“we thus interpret the δ18O changes observed in stalagmites HZZ11 and
HZZ27 to reflect regional monsoon intensity and the subsequent effects
on upstream isotope depletion…Orbital to millennial scale variations in
speleothem δ18O from the Asian monsoon region have traditionally been
interpreted to reflect changes in local/regional rainfall amount… the
ratio of sum- mer to annual rainfall expressed as monsoon intensity”
(Zhang et al., 2016)’
- d18O (S2LRmuTd4DkrsZ): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRmuTd4DkrsZ): paleoData_proxyDetail: NULL has been replaced
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- d18O (S2LRmuTd4DkrsZ): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRmuTd4DkrsZ): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRmuTd4DkrsZ): paleoData_QCnotes: NULL has been replaced by
‘HZZ 27 “If two or more δ18O time series replicate well, it can be as-
sumed that both δ18O profiles primarily reflect real climate sig- nals,
and kinetic fractionation is thus likely absent or insignif- icant…The
HZZ11 and HZZ27 δ 18 O records agree well with each other (Fig. 3A), and
are consistent with the results from Hulu” (Zhang et al., 2016)’
- d18OComposite (S2LRxiKWn6JEMw): paleoData_notes: NULL has been
replaced by ‘“we thus interpret the δ18O changes observed in stalagmites
HZZ11 and HZZ27 to reflect regional monsoon intensity and the subsequent
effects on upstream isotope depletion…Orbital to millennial scale
variations in speleothem δ18O from the Asian monsoon region have
traditionally been interpreted to reflect changes in local/regional
rainfall amount… the ratio of sum- mer to annual rainfall expressed as
monsoon intensity” (Zhang et al., 2016)’
- d18OComposite (S2LRxiKWn6JEMw): paleoData_proxy: NULL has been
replaced by ‘d18O’
- d18OComposite (S2LRxiKWn6JEMw): paleoData_proxyDetail: NULL has been
replaced by ‘calcite’
- d18OComposite (S2LRxiKWn6JEMw): paleoData_proxyGeneral: NULL has
been replaced by ‘isotope’
- d18OComposite (S2LRxiKWn6JEMw): paleoData_QCCertification: NULL has
been replaced by ‘CH’
- d18OComposite (S2LRxiKWn6JEMw): paleoData_QCnotes: NULL has been
replaced by ‘“If two or more δ18O time series replicate well, it can be
as- sumed that both δ18O profiles primarily reflect real climate sig-
nals, and kinetic fractionation is thus likely absent or insignif-
icant…The HZZ11 and HZZ27 δ 18 O records agree well with each other
(Fig. 3A), and are consistent with the results from Hulu” (Zhang et al.,
2016)’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:29:05 UTC
- notes: Created from SISALv2