Version history for n44SNphWFj7Lb1m8FvSS -
LianhuacaveShanxi.Dong.2018
Version: 1.1.10
- lastVersion: 1.1.9
- curator: nicholas
- timestamp: 2023-08-10 23:03:29 UTC
- changes:
Version: 1.1.9
- lastVersion: 1.1.8
- curator: nicholas
- timestamp: 2023-06-02 19:02:17 UTC
- changes:
- Paleo Interpretation metadata:
- d18O (S2LRbRVYOu2hWu): interpretation1_seasonalityGeneral:
‘summerOnly’ has been replaced by ‘Summer’
Version: 1.1.8
- lastVersion: 1.1.7
- curator: nicholas
- timestamp: 2023-05-31 20:39:31 UTC
- changes:
- Publication metadata:
- pub1_author: ‘list(list(name = “Dong, Jinguo”), list(name = “Shen,
Chuan-Chou”), list(name = “Kong, Xinggong”), list(name = “Wu,
Chung-Che”), list(name = “Hu, Hsun-Ming”), list(name = “Ren, Haojia”),
list(name = “Wang, Yi”))’ has been replaced by ‘Dong, Jinguo’
Version: 1.1.7
- lastVersion: 1.1.6
- curator: ccr97
- timestamp: 2023-05-31 18:18:32.203531 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Publication metadata:
- pub1_author: ‘Dong, Jinguo’ has been replaced by ‘list(list(name =
“Dong, Jinguo”), list(name = “Shen, Chuan-Chou”), list(name = “Kong,
Xinggong”), list(name = “Wu, Chung-Che”), list(name = “Hu, Hsun-Ming”),
list(name = “Ren, Haojia”), list(name = “Wang, Yi”))’
- Geographic metadata:
- geo_elevation: ‘1200’ has been replaced by NULL
- Paleo Column metadata:
- d18O (S2LR0ph42Geqgi): paleoData_notes: ‘“d18O-inferred ASM var-
iations reflect a mean state of summer monsoon intensity or integrated
moisture transport rather than the amount of local precipitation. In
other words, a higher proportion of regional ASM rainfall and/or higher
spatially integrated monsoon rainfall between the tropical monsoon
sources and the cave site would result in more negative local stalagmite
d18O… we interpret Lianhua Cave stalagmite d18O records as qualitative
proxies for regional pre- cipitation and intensity of the EASM (at least
in northern China), with lower values expressing a stronger EASM, and
vice versa.” (Dong et al., 2018)’ has been replaced by ‘“δ18O-inferred
ASM var- iations reflect a mean state of summer monsoon intensity or
integrated moisture transport rather than the amount of local
precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LR8OHKKGfMcg): paleoData_notes: ‘“d18O-inferred ASM var-
iations reflect a mean state of summer monsoon intensity or integrated
moisture transport rather than the amount of local precipitation. In
other words, a higher proportion of regional ASM rainfall and/or higher
spatially integrated monsoon rainfall between the tropical monsoon
sources and the cave site would result in more negative local stalagmite
d18O… we interpret Lianhua Cave stalagmite d18O records as qualitative
proxies for regional pre- cipitation and intensity of the EASM (at least
in northern China), with lower values expressing a stronger EASM, and
vice versa.” (Dong et al., 2018)’ has been replaced by ‘“δ18O-inferred
ASM var- iations reflect a mean state of summer monsoon intensity or
integrated moisture transport rather than the amount of local
precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LRF81lufycSy): paleoData_notes: ‘“d18O-inferred ASM var-
iations reflect a mean state of summer monsoon intensity or integrated
moisture transport rather than the amount of local precipitation. In
other words, a higher proportion of regional ASM rainfall and/or higher
spatially integrated monsoon rainfall between the tropical monsoon
sources and the cave site would result in more negative local stalagmite
d18O… we interpret Lianhua Cave stalagmite d18O records as qualitative
proxies for regional pre- cipitation and intensity of the EASM (at least
in northern China), with lower values expressing a stronger EASM, and
vice versa.” (Dong et al., 2018)’ has been replaced by ‘“δ18O-inferred
ASM var- iations reflect a mean state of summer monsoon intensity or
integrated moisture transport rather than the amount of local
precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LRKp1XHISo1R): paleoData_notes: ‘“d18O-inferred ASM var-
iations reflect a mean state of summer monsoon intensity or integrated
moisture transport rather than the amount of local precipitation. In
other words, a higher proportion of regional ASM rainfall and/or higher
spatially integrated monsoon rainfall between the tropical monsoon
sources and the cave site would result in more negative local stalagmite
d18O… we interpret Lianhua Cave stalagmite d18O records as qualitative
proxies for regional pre- cipitation and intensity of the EASM (at least
in northern China), with lower values expressing a stronger EASM, and
vice versa.” (Dong et al., 2018)’ has been replaced by ‘“δ18O-inferred
ASM var- iations reflect a mean state of summer monsoon intensity or
integrated moisture transport rather than the amount of local
precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LRbRVYOu2hWu): paleoData_notes: ‘“d18O-inferred ASM var-
iations reflect a mean state of summer monsoon intensity or integrated
moisture transport rather than the amount of local precipitation. In
other words, a higher proportion of regional ASM rainfall and/or higher
spatially integrated monsoon rainfall between the tropical monsoon
sources and the cave site would result in more negative local stalagmite
d18O… we interpret Lianhua Cave stalagmite d18O records as qualitative
proxies for regional pre- cipitation and intensity of the EASM (at least
in northern China), with lower values expressing a stronger EASM, and
vice versa.” (Dong et al., 2018)’ has been replaced by ‘“δ18O-inferred
ASM var- iations reflect a mean state of summer monsoon intensity or
integrated moisture transport rather than the amount of local
precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LRbRVYOu2hWu): paleoData_QCnotes: ‘CR: I think the ages are
wrong on this one? CH: Author provides composite at: https://www.ncdc.noaa.gov/paleo-search/study/29190 “We
have added more 230Th dates and new d18O samples to improve the accuracy
and temporal resolution of the composite oxygen isotope records” (Dong
et al., 2018)’ has been replaced by ‘Author provides composite at: https://www.ncdc.noaa.gov/paleo-search/study/29190 “We
have added more 230Th dates and new δ18O samples to improve the accuracy
and temporal resolution of the composite oxygen isotope records” (Dong
et al., 2018)’
- d18O (S2LRqCzJUTvtCN): paleoData_notes: ‘“d18O-inferred ASM var-
iations reflect a mean state of summer monsoon intensity or integrated
moisture transport rather than the amount of local precipitation. In
other words, a higher proportion of regional ASM rainfall and/or higher
spatially integrated monsoon rainfall between the tropical monsoon
sources and the cave site would result in more negative local stalagmite
d18O… we interpret Lianhua Cave stalagmite d18O records as qualitative
proxies for regional pre- cipitation and intensity of the EASM (at least
in northern China), with lower values expressing a stronger EASM, and
vice versa.” (Dong et al., 2018)’ has been replaced by ‘“δ18O-inferred
ASM var- iations reflect a mean state of summer monsoon intensity or
integrated moisture transport rather than the amount of local
precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LRv6j1oBfGRN): paleoData_notes: ‘“d18O-inferred ASM var-
iations reflect a mean state of summer monsoon intensity or integrated
moisture transport rather than the amount of local precipitation. In
other words, a higher proportion of regional ASM rainfall and/or higher
spatially integrated monsoon rainfall between the tropical monsoon
sources and the cave site would result in more negative local stalagmite
d18O… we interpret Lianhua Cave stalagmite d18O records as qualitative
proxies for regional pre- cipitation and intensity of the EASM (at least
in northern China), with lower values expressing a stronger EASM, and
vice versa.” (Dong et al., 2018)’ has been replaced by ‘“δ18O-inferred
ASM var- iations reflect a mean state of summer monsoon intensity or
integrated moisture transport rather than the amount of local
precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- Paleo Interpretation metadata:
- d18O (S2LRbRVYOu2hWu): interpretation1_seasonalityGeneral: ‘Summer’
has been replaced by ‘summerOnly’
Version: 1.1.6
- lastVersion: 1.1.5
- curator: nicholas
- timestamp: 2023-03-24 22:25:32 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR0ph42Geqgi): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LR8OHKKGfMcg): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRF81lufycSy): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRKp1XHISo1R): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRbRVYOu2hWu): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRqCzJUTvtCN): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRv6j1oBfGRN): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
Version: 1.1.5
- lastVersion: 1.1.4
- curator: nicholas
- timestamp: 2023-02-10 14:34:09 UTC
- changes:
- Paleo Interpretation metadata:
- uncertaintyHigh (S2LR1DXU8KI5JQ): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LR4GHjC5a8qu): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LR52eMhr6xkQ): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR6TZAOcwyIS): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LR7D9NwwzvTk): interpretation1_scope: NULL has
been replaced by ‘climate’
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- uncertaintyLow (S2LRL7cAU3WleN): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRQNSTv03xAl): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRr96VPaSd0A): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRRJyyaBVD0R): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LRsDHBkMix82): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRtGJWBu2hEH): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRtoJGuF6ciY): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRUivRykoo8x): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LRUSd8EO0DnA): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LRVFE3gmAxrq): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRVp1uCnxQua): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LRW2RzwC9QZJ): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LRW49pOUzcsj): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LRWbyeZaKdd8): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRwHeYYSZv3X): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LRxARUJKlne3): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRxhmNDAxnEg): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRXkXvPRUhMY): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRXS7Z3nXmiy): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRyFuUnrAFOM): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRYkp7C7V7CN): interpretation1_scope: NULL has
been replaced by ‘climate’
Version: 1.1.3
- lastVersion: 1.1.2
- curator: nicholas
- timestamp: 2022-09-09 02:10:19 UTC
- changes:
- Paleo Interpretation metadata:
- d18OComposite (S2LRbRVYOu2hWu): interpretation1_seasonality: ‘JJAS’
has been replaced by ‘6,7,8,9’
Version: 1.1.2
- lastVersion: 1.1.1
- curator: nicholas
- timestamp: 2022-07-28 17:35:57 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘1200’ has been replaced by NULL
Version: 1.1.1
- lastVersion: 1.1.0
- curator: nicholas
- timestamp: 2022-07-15 23:05:24 UTC
- changes:
- Paleo Interpretation metadata:
- d18OStandard (S2LR02XzJ57F85): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LR0ph42Geqgi): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LR3amSIgAlSh): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LR5B1NkdXXRG): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LR8OHKKGfMcg): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OPrecision (S2LR9GsGUFTDJT): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LR9IhFpmb1Gm): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRa1EopBETO0): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRANXwlYqDH2): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LRC120XDdSNN): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRcA4kVo8BKo): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasHiatus (S2LRCubomy56Lq): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRDzWffkyZ51): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRE7W0jxkuTm): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LREX22GwQVyG): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRF81lufycSy): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OPrecision (S2LRG36wGF0BpB): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRGhB0uubxqp): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRiwhBc3B9LZ): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRjtjuhIPbMP): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18O (S2LRKp1XHISo1R): interpretation1_scope: NULL has been replaced
by ‘climate’
- hasAragoniteCorrection (S2LRm2WDy2WRNJ): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRmXW9cAQ9Na): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LRnmryPNH84g): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRnwGM2iQZQm): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRpIq3rtkWJy): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18O (S2LRqCzJUTvtCN): interpretation1_scope: NULL has been replaced
by ‘climate’
- sisalSampleID (S2LRs5DCghZsHh): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRsI5QNp4R2C): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRSI5TzrGJHS): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRTGhuFaFY4z): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRuyeF5M3MW7): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRv6j1oBfGRN): interpretation1_scope: NULL has been replaced
by ‘climate’
- sisalSampleID (S2LRwJ4F8JqZTR): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRwWHicCxhwX): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRy8oHyGLg91): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRYfV720UDV8): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRYh7HNQnMIB): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRZNaufoldj9): interpretation1_scope: NULL has been
replaced by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2021-10-05 21:40:48 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 01:54:48 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Interpretation metadata:
- d18OComposite (S2LRbRVYOu2hWu): interpretation1_seasonalityGeneral:
‘Summer’ has been replaced by ‘summerOnly’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:29:18 UTC
- changes:
- Paleo Interpretation metadata:
- d18OStandard (S2LR02XzJ57F85): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LR0ph42Geqgi): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LR3amSIgAlSh): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LR5B1NkdXXRG): interpretation1_scope: NULL has been
replaced by ‘climate’
- depthComposite (S2LR6nYsMI2cVC): interpretation1_scope: NULL has
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- d18O (S2LR8OHKKGfMcg): interpretation1_scope: NULL has been replaced
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- d18OPrecision (S2LR9GsGUFTDJT): interpretation1_scope: NULL has been
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- d18OPrecision (S2LR9IhFpmb1Gm): interpretation1_scope: NULL has been
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- d18OStandard (S2LRa1EopBETO0): interpretation1_scope: NULL has been
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- hasAragoniteCorrectionComposite (S2LRaDo8Ldae5n):
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- d18OPrecision (S2LRANXwlYqDH2): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OComposite (S2LRbRVYOu2hWu): interpretation1_direction: NULL has
been replaced by ‘negative’
- d18OComposite (S2LRbRVYOu2hWu): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OComposite (S2LRbRVYOu2hWu): interpretation1_seasonality: NULL
has been replaced by ‘6,7,8,9’
- d18OComposite (S2LRbRVYOu2hWu): interpretation1_seasonalityGeneral:
NULL has been replaced by ‘Summer’
- d18OComposite (S2LRbRVYOu2hWu): interpretation1_variable: NULL has
been replaced by ‘P’
- d18OComposite (S2LRbRVYOu2hWu): interpretation1_variableDetail: NULL
has been replaced by ‘@surface’
- hasHiatus (S2LRC120XDdSNN): interpretation1_scope: NULL has been
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- hasAragoniteCorrection (S2LRcA4kVo8BKo): interpretation1_scope: NULL
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- hasHiatus (S2LRCubomy56Lq): interpretation1_scope: NULL has been
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- d18O (S2LRF81lufycSy): interpretation1_scope: NULL has been replaced
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- d18OPrecision (S2LRG36wGF0BpB): interpretation1_scope: NULL has been
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- d18O (S2LRKp1XHISo1R): interpretation1_scope: NULL has been replaced
by ‘climate’
- hasAragoniteCorrection (S2LRm2WDy2WRNJ): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRmXW9cAQ9Na): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogyComposite (S2LRngKd4MkTQ8): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LRnmryPNH84g): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRnwGM2iQZQm): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRpIq3rtkWJy): interpretation1_scope: NULL
has been replaced by ‘climate’
- entityName (S2LRpqx5IrmFes): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRqCzJUTvtCN): interpretation1_scope: NULL has been replaced
by ‘climate’
- sisalSampleIDComposite (S2LRRaxln8aapV): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OPrecisionComposite (S2LRrayIxjPbCr): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRs5DCghZsHh): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRsI5QNp4R2C): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRSI5TzrGJHS): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRTGhuFaFY4z): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRuyeF5M3MW7): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRv6j1oBfGRN): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandardComposite (S2LRvZyYJuRdsB): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRwJ4F8JqZTR): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRwWHicCxhwX): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRy8oHyGLg91): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRYfV720UDV8): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRYh7HNQnMIB): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRZNaufoldj9): interpretation1_scope: NULL has been
replaced by ‘climate’
- Paleo Column metadata:
- d18O (S2LR0ph42Geqgi): paleoData_notes: NULL has been replaced by
‘“δ18O-inferred ASM var- iations reflect a mean state of summer monsoon
intensity or integrated moisture transport rather than the amount of
local precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LR0ph42Geqgi): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LR0ph42Geqgi): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LR0ph42Geqgi): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LR8OHKKGfMcg): paleoData_notes: NULL has been replaced by
‘“δ18O-inferred ASM var- iations reflect a mean state of summer monsoon
intensity or integrated moisture transport rather than the amount of
local precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LR8OHKKGfMcg): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LR8OHKKGfMcg): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LR8OHKKGfMcg): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18OComposite (S2LRbRVYOu2hWu): paleoData_notes: NULL has been
replaced by ‘“δ18O-inferred ASM var- iations reflect a mean state of
summer monsoon intensity or integrated moisture transport rather than
the amount of local precipitation. In other words, a higher proportion
of regional ASM rainfall and/or higher spatially integrated monsoon
rainfall between the tropical monsoon sources and the cave site would
result in more negative local stalagmite δ18O… we interpret Lianhua Cave
stalagmite δ18O records as qualitative proxies for regional pre-
cipitation and intensity of the EASM (at least in northern China), with
lower values expressing a stronger EASM, and vice versa.” (Dong et al.,
2018)’
- d18OComposite (S2LRbRVYOu2hWu): paleoData_proxy: NULL has been
replaced by ‘d18O’
- d18OComposite (S2LRbRVYOu2hWu): paleoData_proxyDetail: NULL has been
replaced by ‘calcite’
- d18OComposite (S2LRbRVYOu2hWu): paleoData_proxyGeneral: NULL has
been replaced by ‘isotope’
- d18OComposite (S2LRbRVYOu2hWu): paleoData_QCCertification: NULL has
been replaced by ‘CH’
- d18OComposite (S2LRbRVYOu2hWu): paleoData_QCnotes: NULL has been
replaced by ‘Author provides composite at: https://www.ncdc.noaa.gov/paleo-search/study/29190 “We
have added more 230Th dates and new δ18O samples to improve the accuracy
and temporal resolution of the composite oxygen isotope records” (Dong
et al., 2018)’
- d18O (S2LRF81lufycSy): paleoData_notes: NULL has been replaced by
‘“δ18O-inferred ASM var- iations reflect a mean state of summer monsoon
intensity or integrated moisture transport rather than the amount of
local precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LRF81lufycSy): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRF81lufycSy): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRF81lufycSy): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRKp1XHISo1R): paleoData_notes: NULL has been replaced by
‘“δ18O-inferred ASM var- iations reflect a mean state of summer monsoon
intensity or integrated moisture transport rather than the amount of
local precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LRKp1XHISo1R): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRKp1XHISo1R): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRKp1XHISo1R): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRqCzJUTvtCN): paleoData_notes: NULL has been replaced by
‘“δ18O-inferred ASM var- iations reflect a mean state of summer monsoon
intensity or integrated moisture transport rather than the amount of
local precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LRqCzJUTvtCN): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRqCzJUTvtCN): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRqCzJUTvtCN): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRv6j1oBfGRN): paleoData_notes: NULL has been replaced by
‘“δ18O-inferred ASM var- iations reflect a mean state of summer monsoon
intensity or integrated moisture transport rather than the amount of
local precipitation. In other words, a higher proportion of regional ASM
rainfall and/or higher spatially integrated monsoon rainfall between the
tropical monsoon sources and the cave site would result in more negative
local stalagmite δ18O… we interpret Lianhua Cave stalagmite δ18O records
as qualitative proxies for regional pre- cipitation and intensity of the
EASM (at least in northern China), with lower values expressing a
stronger EASM, and vice versa.” (Dong et al., 2018)’
- d18O (S2LRv6j1oBfGRN): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRv6j1oBfGRN): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRv6j1oBfGRN): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:29:09 UTC
- notes: Created from SISALv2