Version history for LIcGR4H0i9fYAWSm7zhN -
Chaaracave.AitBrahim.2018
Version: 1.0.19
- lastVersion: 1.0.18
- curator: nicholas
- timestamp: 2025-06-25 23:22:52.132309 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d18O (S2LR2w6LcELdJW): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
Version: 1.0.18
- lastVersion: 1.0.17
- curator: nicholas
- timestamp: 2025-06-25 23:19:07.077295 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d18O (S2LR2w6LcELdJW): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
Version: 1.0.17
- lastVersion: 1.0.16
- curator: nicholas
- timestamp: 2025-06-25 22:46:00.074061 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: ‘((( null ))) Morocco /// Africa>Northern
Africa>Morocco’ has been replaced by ‘Africa>Northern
Africa>Morocco’
- Paleo Column metadata:
- d18O (S2LR2w6LcELdJW): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LR2w6LcELdJW): paleoData_QCnotes: ‘((( null ))) Need to
modify composite or use rainfall index provided in ncdc “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) ///
Need to modify composite or use rainfall index provided in ncdc “The
Chaara cave record, described by a composite of the Cha1 and Cha2 d18O
records…a representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘Need to modify composite or use rainfall index
provided in ncdc “The Chaara cave record, described by a composite of
the Cha1 and Cha2 d18O records…a representative rainfall index of the
Western Mediterranean is constructed using the first axis of the PCA
(PC1) between the Chaara composite and Grotte de Piste record…Grotte de
Piste and Chaara Cave sites are only a few hundred meters apart” (Ait
Brahim et al., 2018)’
- d18O (S2LROeXqCyQIUp): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LROeXqCyQIUp): paleoData_QCCertification: ‘((( null ))) CH
/// CH, CR’ has been replaced by ‘CH, CR’
- d18O (S2LROeXqCyQIUp): paleoData_QCnotes: ‘((( null ))) CH1; “The
Chaara cave record, described by a composite of the Cha1 and Cha2 δ18O
records…a representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) ///
CH1; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 d18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018)’ has been replaced by ‘CH1; “The Chaara cave record,
described by a composite of the Cha1 and Cha2 d18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al.,
2018)’
- d18O (S2LRU6xGJ9gjMj): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LRU6xGJ9gjMj): paleoData_QCCertification: ‘((( null ))) CH
/// CH, CR’ has been replaced by ‘CH, CR’
- d18O (S2LRU6xGJ9gjMj): paleoData_QCnotes: ‘((( null ))) CH2; “The
Chaara cave record, described by a composite of the Cha1 and Cha2 δ18O
records…a representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) ///
CH2; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 d18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018)’ has been replaced by ‘CH2; “The Chaara cave record,
described by a composite of the Cha1 and Cha2 d18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al.,
2018)’
- d18O (S2LRzvlZ9Wrb8G): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LRzvlZ9Wrb8G): paleoData_QCnotes: ‘((( null ))) CH2 (common
era); “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018) /// CH2 (common era); “The Chaara cave record, described
by a composite of the Cha1 and Cha2 d18O records…a representative
rainfall index of the Western Mediterranean is constructed using the
first axis of the PCA (PC1) between the Chaara composite and Grotte de
Piste record…Grotte de Piste and Chaara Cave sites are only a few
hundred meters apart” (Ait Brahim et al., 2018)’ has been replaced by
‘CH2 (common era); “The Chaara cave record, described by a composite of
the Cha1 and Cha2 d18O records…a representative rainfall index of the
Western Mediterranean is constructed using the first axis of the PCA
(PC1) between the Chaara composite and Grotte de Piste record…Grotte de
Piste and Chaara Cave sites are only a few hundred meters apart” (Ait
Brahim et al., 2018)’
- Paleo Interpretation metadata:
- d18O (S2LR2w6LcELdJW): interpretation1_seasonality: ‘((( null )))
12,1,2,3 /// Dec-Mar’ has been replaced by ‘Dec-Mar’
- d18O (S2LROeXqCyQIUp): interpretation1_seasonality: ‘((( null )))
12,1,2,3 /// Dec-Mar’ has been replaced by ‘Dec-Mar’
- d18O (S2LROeXqCyQIUp): interpretation1_variable: ‘((( null ))) P-E
/// effectivePrecipitation’ has been replaced by
‘effectivePrecipitation’
- d18O (S2LRU6xGJ9gjMj): interpretation1_seasonality: ‘((( null )))
12,1,2,3 /// Dec-Mar’ has been replaced by ‘Dec-Mar’
- d18O (S2LRU6xGJ9gjMj): interpretation1_variable: ‘((( null ))) P-E
/// effectivePrecipitation’ has been replaced by
‘effectivePrecipitation’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_seasonality: ‘((( null )))
12,1,2,3 /// Dec-Mar’ has been replaced by ‘Dec-Mar’
Version: 1.0.16
- lastVersion: 1.0.15
- curator: nicholas
- timestamp: 2025-06-25 21:21:39.935482 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: ‘Africa>Northern Africa>Morocco’ has been
replaced by ‘((( null ))) Morocco /// Africa>Northern
Africa>Morocco’
- Paleo Column metadata:
- d18O (S2LR2w6LcELdJW): paleoData_notes: ‘“The GP5 and Cha2 d18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low d18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘((( null ))) “The GP5 and Cha2 δ18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) /// “The GP5 and Cha2 d18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low d18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019)’
- d18O (S2LR2w6LcELdJW): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LR2w6LcELdJW): paleoData_QCnotes: ‘Need to modify composite
or use rainfall index provided in ncdc “The Chaara cave record,
described by a composite of the Cha1 and Cha2 d18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘((( null ))) Need to modify composite or use
rainfall index provided in ncdc “The Chaara cave record, described by a
composite of the Cha1 and Cha2 δ18O records…a representative rainfall
index of the Western Mediterranean is constructed using the first axis
of the PCA (PC1) between the Chaara composite and Grotte de Piste
record…Grotte de Piste and Chaara Cave sites are only a few hundred
meters apart” (Ait Brahim et al., 2018) /// Need to modify composite or
use rainfall index provided in ncdc “The Chaara cave record, described
by a composite of the Cha1 and Cha2 d18O records…a representative
rainfall index of the Western Mediterranean is constructed using the
first axis of the PCA (PC1) between the Chaara composite and Grotte de
Piste record…Grotte de Piste and Chaara Cave sites are only a few
hundred meters apart” (Ait Brahim et al., 2018)’
- d18O (S2LR2w6LcELdJW): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d18O (S2LR2w6LcELdJW): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- d18O (S2LROeXqCyQIUp): paleoData_notes: ‘“The GP5 and Cha2 d18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low d18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘((( null ))) “The GP5 and Cha2 δ18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) /// “The GP5 and Cha2 d18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low d18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019)’
- d18O (S2LROeXqCyQIUp): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LROeXqCyQIUp): paleoData_QCCertification: ‘CH, CR’ has been
replaced by ‘((( null ))) CH /// CH, CR’
- d18O (S2LROeXqCyQIUp): paleoData_QCnotes: ‘CH1; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 d18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘((( null ))) CH1; “The Chaara cave record,
described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) ///
CH1; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 d18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018)’
- d18O (S2LROeXqCyQIUp): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d18O (S2LROeXqCyQIUp): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRU6xGJ9gjMj): paleoData_notes: ‘“The GP5 and Cha2 d18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low d18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘((( null ))) “The GP5 and Cha2 δ18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) /// “The GP5 and Cha2 d18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low d18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019)’
- d18O (S2LRU6xGJ9gjMj): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LRU6xGJ9gjMj): paleoData_QCCertification: ‘CH, CR’ has been
replaced by ‘((( null ))) CH /// CH, CR’
- d18O (S2LRU6xGJ9gjMj): paleoData_QCnotes: ‘CH2; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 d18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘((( null ))) CH2; “The Chaara cave record,
described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) ///
CH2; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 d18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018)’
- d18O (S2LRU6xGJ9gjMj): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d18O (S2LRU6xGJ9gjMj): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRzvlZ9Wrb8G): paleoData_notes: ‘“The GP5 and Cha2 d18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low d18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘((( null ))) “The GP5 and Cha2 δ18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) /// “The GP5 and Cha2 d18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low d18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019)’
- d18O (S2LRzvlZ9Wrb8G): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LRzvlZ9Wrb8G): paleoData_QCnotes: ‘CH2 (common era); “The
Chaara cave record, described by a composite of the Cha1 and Cha2 d18O
records…a representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘((( null ))) CH2 (common era); “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) ///
CH2 (common era); “The Chaara cave record, described by a composite of
the Cha1 and Cha2 d18O records…a representative rainfall index of the
Western Mediterranean is constructed using the first axis of the PCA
(PC1) between the Chaara composite and Grotte de Piste record…Grotte de
Piste and Chaara Cave sites are only a few hundred meters apart” (Ait
Brahim et al., 2018)’
- d18O (S2LRzvlZ9Wrb8G): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘FALSE’
- d18O (S2LRzvlZ9Wrb8G): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- Paleo Interpretation metadata:
- d18O (S2LR2w6LcELdJW): interpretation1_seasonality: ‘Dec-Mar’ has
been replaced by ‘((( null ))) 12,1,2,3 /// Dec-Mar’
- d18O (S2LR2w6LcELdJW): interpretation1_variable: NULL has been
replaced by ‘P-E’
- d18O (S2LROeXqCyQIUp): interpretation1_seasonality: ‘Dec-Mar’ has
been replaced by ‘((( null ))) 12,1,2,3 /// Dec-Mar’
- d18O (S2LROeXqCyQIUp): interpretation1_variable:
‘effectivePrecipitation’ has been replaced by ‘((( null ))) P-E ///
effectivePrecipitation’
- d18O (S2LRU6xGJ9gjMj): interpretation1_seasonality: ‘Dec-Mar’ has
been replaced by ‘((( null ))) 12,1,2,3 /// Dec-Mar’
- d18O (S2LRU6xGJ9gjMj): interpretation1_variable:
‘effectivePrecipitation’ has been replaced by ‘((( null ))) P-E ///
effectivePrecipitation’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_seasonality: ‘Dec-Mar’ has
been replaced by ‘((( null ))) 12,1,2,3 /// Dec-Mar’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_variable: NULL has been
replaced by ‘P-E’
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2023-08-10 22:45:21 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_author: NULL has been replaced by ‘Yassine Ait Brahim and
Jasper A. Wassenburg and Francisco W. Cruz and Abdelfettah Sifeddine and
Denis Scholz and Lhoussaine Bouchaou and Emilie P. Dassi{’{e}} and Klaus
P. Jochum and R. Lawrence Edwards and Hai Cheng’
- pub1_journal: NULL has been replaced by ‘Scientific Reports’
- pub1_title: NULL has been replaced by ‘Multi-decadal to centennial
hydro-climate variability and linkage to solar forcing in the Western
Mediterranean during the last 1000 years’
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2023-05-31 20:38:02 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LROeXqCyQIUp): paleoData_notes: ‘((( ((( “The GP5 and Cha2
��18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low ��18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) ))) “The GP5 and Cha2 δ18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low δ18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) ))) “The GP5 and Cha2 d18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low d18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘“The GP5 and Cha2 d18O records are
thus considered proxies for effective rainfall” (Ait Brahim et al. 2018)
“Cha1 and Cha2 records as proxy records of effective rainfall
variability during the Holocene, whereby low d18O values reflect humid
conditions and vice versa…The winter rainfall (December to March)
accounts for 80% of the annual rainfall amount…Grotte de Piste and
Chaara Cave sites are only a few hundred meters apart” (Ait Brahim et
al. 2019)’
- d18O (S2LROeXqCyQIUp): paleoData_QCnotes: ‘((( ((( CH1; “The Chaara
cave record, described by a composite of the Cha1 and Cha2 ��18O
records…a representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) )))
CH1; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018) /// CH1; “The Chaara cave record, described by a composite
of the Cha1 and Cha2 δ18O records…a representative rainfall index of the
Western Mediterranean is constructed using the first axis of the PCA
(PC1) between the Chaara composite and Grotte de Piste record…Grotte de
Piste and Chaara Cave sites are only a few hundred meters apart” (Ait
Brahim et al., 2018) ))) CH1; “The Chaara cave record, described by a
composite of the Cha1 and Cha2 d18O records…a representative rainfall
index of the Western Mediterranean is constructed using the first axis
of the PCA (PC1) between the Chaara composite and Grotte de Piste
record…Grotte de Piste and Chaara Cave sites are only a few hundred
meters apart” (Ait Brahim et al., 2018) /// CH1; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘CH1; “The Chaara cave record, described by a
composite of the Cha1 and Cha2 d18O records…a representative rainfall
index of the Western Mediterranean is constructed using the first axis
of the PCA (PC1) between the Chaara composite and Grotte de Piste
record…Grotte de Piste and Chaara Cave sites are only a few hundred
meters apart” (Ait Brahim et al., 2018)’
- d18O (S2LRU6xGJ9gjMj): paleoData_notes: ‘((( ((( “The GP5 and Cha2
��18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low ��18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) ))) “The GP5 and Cha2 δ18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low δ18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) ))) “The GP5 and Cha2 d18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low d18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘“The GP5 and Cha2 d18O records are
thus considered proxies for effective rainfall” (Ait Brahim et al. 2018)
“Cha1 and Cha2 records as proxy records of effective rainfall
variability during the Holocene, whereby low d18O values reflect humid
conditions and vice versa…The winter rainfall (December to March)
accounts for 80% of the annual rainfall amount…Grotte de Piste and
Chaara Cave sites are only a few hundred meters apart” (Ait Brahim et
al. 2019)’
- d18O (S2LRU6xGJ9gjMj): paleoData_QCnotes: ‘((( ((( CH2; “The Chaara
cave record, described by a composite of the Cha1 and Cha2 ��18O
records…a representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) )))
CH2; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018) /// CH2; “The Chaara cave record, described by a composite
of the Cha1 and Cha2 δ18O records…a representative rainfall index of the
Western Mediterranean is constructed using the first axis of the PCA
(PC1) between the Chaara composite and Grotte de Piste record…Grotte de
Piste and Chaara Cave sites are only a few hundred meters apart” (Ait
Brahim et al., 2018) ))) CH2; “The Chaara cave record, described by a
composite of the Cha1 and Cha2 d18O records…a representative rainfall
index of the Western Mediterranean is constructed using the first axis
of the PCA (PC1) between the Chaara composite and Grotte de Piste
record…Grotte de Piste and Chaara Cave sites are only a few hundred
meters apart” (Ait Brahim et al., 2018) /// CH2; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘CH2; “The Chaara cave record, described by a
composite of the Cha1 and Cha2 d18O records…a representative rainfall
index of the Western Mediterranean is constructed using the first axis
of the PCA (PC1) between the Chaara composite and Grotte de Piste
record…Grotte de Piste and Chaara Cave sites are only a few hundred
meters apart” (Ait Brahim et al., 2018)’
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-05-30 15:48:14 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR2w6LcELdJW): paleoData_notes: ‘“The GP5 and Cha2 δ18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘“The GP5 and Cha2 d18O records are
thus considered proxies for effective rainfall” (Ait Brahim et al. 2018)
“Cha1 and Cha2 records as proxy records of effective rainfall
variability during the Holocene, whereby low d18O values reflect humid
conditions and vice versa…The winter rainfall (December to March)
accounts for 80% of the annual rainfall amount…Grotte de Piste and
Chaara Cave sites are only a few hundred meters apart” (Ait Brahim et
al. 2019)’
- d18O (S2LR2w6LcELdJW): paleoData_QCnotes: ‘Need to modify composite
or use rainfall index provided in ncdc “The Chaara cave record,
described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘Need to modify composite or use rainfall index
provided in ncdc “The Chaara cave record, described by a composite of
the Cha1 and Cha2 d18O records…a representative rainfall index of the
Western Mediterranean is constructed using the first axis of the PCA
(PC1) between the Chaara composite and Grotte de Piste record…Grotte de
Piste and Chaara Cave sites are only a few hundred meters apart” (Ait
Brahim et al., 2018)’
- d18O (S2LROeXqCyQIUp): paleoData_notes: ‘“The GP5 and Cha2 δ18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘((( ((( “The GP5 and Cha2 ��18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low ��18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) ))) “The GP5 and Cha2 δ18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low δ18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) ))) “The GP5 and Cha2 d18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low d18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’
- d18O (S2LROeXqCyQIUp): paleoData_QCCertification: ‘CH’ has been
replaced by ‘CH, CR’
- d18O (S2LROeXqCyQIUp): paleoData_QCnotes: ‘CH1; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘((( ((( CH1; “The Chaara cave record, described by
a composite of the Cha1 and Cha2 ��18O records…a representative rainfall
index of the Western Mediterranean is constructed using the first axis
of the PCA (PC1) between the Chaara composite and Grotte de Piste
record…Grotte de Piste and Chaara Cave sites are only a few hundred
meters apart” (Ait Brahim et al., 2018) ))) CH1; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) ///
CH1; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018) ))) CH1; “The Chaara cave record, described by a composite
of the Cha1 and Cha2 d18O records…a representative rainfall index of the
Western Mediterranean is constructed using the first axis of the PCA
(PC1) between the Chaara composite and Grotte de Piste record…Grotte de
Piste and Chaara Cave sites are only a few hundred meters apart” (Ait
Brahim et al., 2018) /// CH1; “The Chaara cave record, described by a
composite of the Cha1 and Cha2 δ18O records…a representative rainfall
index of the Western Mediterranean is constructed using the first axis
of the PCA (PC1) between the Chaara composite and Grotte de Piste
record…Grotte de Piste and Chaara Cave sites are only a few hundred
meters apart” (Ait Brahim et al., 2018)’
- d18O (S2LRU6xGJ9gjMj): paleoData_notes: ‘“The GP5 and Cha2 δ18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘((( ((( “The GP5 and Cha2 ��18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low ��18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) ))) “The GP5 and Cha2 δ18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low δ18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) ))) “The GP5 and Cha2 d18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low d18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’
- d18O (S2LRU6xGJ9gjMj): paleoData_QCCertification: ‘CH’ has been
replaced by ‘CH, CR’
- d18O (S2LRU6xGJ9gjMj): paleoData_QCnotes: ‘CH2; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘((( ((( CH2; “The Chaara cave record, described by
a composite of the Cha1 and Cha2 ��18O records…a representative rainfall
index of the Western Mediterranean is constructed using the first axis
of the PCA (PC1) between the Chaara composite and Grotte de Piste
record…Grotte de Piste and Chaara Cave sites are only a few hundred
meters apart” (Ait Brahim et al., 2018) ))) CH2; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) ///
CH2; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018) ))) CH2; “The Chaara cave record, described by a composite
of the Cha1 and Cha2 d18O records…a representative rainfall index of the
Western Mediterranean is constructed using the first axis of the PCA
(PC1) between the Chaara composite and Grotte de Piste record…Grotte de
Piste and Chaara Cave sites are only a few hundred meters apart” (Ait
Brahim et al., 2018) /// CH2; “The Chaara cave record, described by a
composite of the Cha1 and Cha2 δ18O records…a representative rainfall
index of the Western Mediterranean is constructed using the first axis
of the PCA (PC1) between the Chaara composite and Grotte de Piste
record…Grotte de Piste and Chaara Cave sites are only a few hundred
meters apart” (Ait Brahim et al., 2018)’
- d18O (S2LRzvlZ9Wrb8G): paleoData_notes: ‘“The GP5 and Cha2 δ18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘“The GP5 and Cha2 d18O records are
thus considered proxies for effective rainfall” (Ait Brahim et al. 2018)
“Cha1 and Cha2 records as proxy records of effective rainfall
variability during the Holocene, whereby low d18O values reflect humid
conditions and vice versa…The winter rainfall (December to March)
accounts for 80% of the annual rainfall amount…Grotte de Piste and
Chaara Cave sites are only a few hundred meters apart” (Ait Brahim et
al. 2019)’
- d18O (S2LRzvlZ9Wrb8G): paleoData_QCnotes: ‘CH2 (common era); “The
Chaara cave record, described by a composite of the Cha1 and Cha2 δ18O
records…a representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘CH2 (common era); “The Chaara cave record,
described by a composite of the Cha1 and Cha2 d18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al.,
2018)’
- Paleo Interpretation metadata:
- d18O (S2LROeXqCyQIUp): interpretation1_seasonalityGeneral:
‘winterOnly’ has been replaced by ‘Winter’
- d18O (S2LRU6xGJ9gjMj): interpretation1_seasonalityGeneral:
‘winterOnly’ has been replaced by ‘Winter’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-05-12 21:51:15 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LROeXqCyQIUp): paleoData_notes: ‘((( “The GP5 and Cha2 ��18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low ��18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) ))) “The GP5 and Cha2 δ18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low δ18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘“The GP5 and Cha2 δ18O records are
thus considered proxies for effective rainfall” (Ait Brahim et al. 2018)
“Cha1 and Cha2 records as proxy records of effective rainfall
variability during the Holocene, whereby low δ18O values reflect humid
conditions and vice versa…The winter rainfall (December to March)
accounts for 80% of the annual rainfall amount…Grotte de Piste and
Chaara Cave sites are only a few hundred meters apart” (Ait Brahim et
al. 2019)’
- d18O (S2LROeXqCyQIUp): paleoData_QCnotes: ‘((( CH1; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 ��18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) )))
CH1; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018) /// CH1; “The Chaara cave record, described by a composite
of the Cha1 and Cha2 δ18O records…a representative rainfall index of the
Western Mediterranean is constructed using the first axis of the PCA
(PC1) between the Chaara composite and Grotte de Piste record…Grotte de
Piste and Chaara Cave sites are only a few hundred meters apart” (Ait
Brahim et al., 2018)’ has been replaced by ‘CH1; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al.,
2018)’
- d18O (S2LRU6xGJ9gjMj): paleoData_notes: ‘((( “The GP5 and Cha2 ��18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low ��18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019) ))) “The GP5 and Cha2 δ18O records are thus considered
proxies for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2
records as proxy records of effective rainfall variability during the
Holocene, whereby low δ18O values reflect humid conditions and vice
versa…The winter rainfall (December to March) accounts for 80% of the
annual rainfall amount…Grotte de Piste and Chaara Cave sites are only a
few hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘“The GP5 and Cha2 δ18O records are
thus considered proxies for effective rainfall” (Ait Brahim et al. 2018)
“Cha1 and Cha2 records as proxy records of effective rainfall
variability during the Holocene, whereby low δ18O values reflect humid
conditions and vice versa…The winter rainfall (December to March)
accounts for 80% of the annual rainfall amount…Grotte de Piste and
Chaara Cave sites are only a few hundred meters apart” (Ait Brahim et
al. 2019)’
- d18O (S2LRU6xGJ9gjMj): paleoData_QCnotes: ‘((( CH2; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 ��18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) )))
CH2; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018) /// CH2; “The Chaara cave record, described by a composite
of the Cha1 and Cha2 δ18O records…a representative rainfall index of the
Western Mediterranean is constructed using the first axis of the PCA
(PC1) between the Chaara composite and Grotte de Piste record…Grotte de
Piste and Chaara Cave sites are only a few hundred meters apart” (Ait
Brahim et al., 2018)’ has been replaced by ‘CH2; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al.,
2018)’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-03-24 22:23:52 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR2w6LcELdJW): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LROeXqCyQIUp): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRU6xGJ9gjMj): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRzvlZ9Wrb8G): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- Paleo Interpretation metadata:
- d18O (S2LROeXqCyQIUp): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
- d18O (S2LRU6xGJ9gjMj): interpretation1_variable: ‘P-E’ has been
replaced by ‘effectivePrecipitation’
Version: 1.0.9
- lastVersion: 1.0.8
- curator: nicholas
- timestamp: 2023-02-13 23:39:23 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LROeXqCyQIUp): paleoData_notes: ‘“The GP5 and Cha2 δ18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘((( “The GP5 and Cha2 ��18O records
are thus considered proxies for effective rainfall” (Ait Brahim et
al. 2018) “Cha1 and Cha2 records as proxy records of effective rainfall
variability during the Holocene, whereby low ��18O values reflect humid
conditions and vice versa…The winter rainfall (December to March)
accounts for 80% of the annual rainfall amount…Grotte de Piste and
Chaara Cave sites are only a few hundred meters apart” (Ait Brahim et
al. 2019) ))) “The GP5 and Cha2 δ18O records are thus considered proxies
for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2 records
as proxy records of effective rainfall variability during the Holocene,
whereby low δ18O values reflect humid conditions and vice versa…The
winter rainfall (December to March) accounts for 80% of the annual
rainfall amount…Grotte de Piste and Chaara Cave sites are only a few
hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’
- d18O (S2LROeXqCyQIUp): paleoData_QCnotes: ‘CH1; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘((( CH1; “The Chaara cave record, described by a
composite of the Cha1 and Cha2 ��18O records…a representative rainfall
index of the Western Mediterranean is constructed using the first axis
of the PCA (PC1) between the Chaara composite and Grotte de Piste
record…Grotte de Piste and Chaara Cave sites are only a few hundred
meters apart” (Ait Brahim et al., 2018) ))) CH1; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) ///
CH1; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018)’
- d18O (S2LRU6xGJ9gjMj): paleoData_notes: ‘“The GP5 and Cha2 δ18O
records are thus considered proxies for effective rainfall” (Ait Brahim
et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’ has been replaced by ‘((( “The GP5 and Cha2 ��18O records
are thus considered proxies for effective rainfall” (Ait Brahim et
al. 2018) “Cha1 and Cha2 records as proxy records of effective rainfall
variability during the Holocene, whereby low ��18O values reflect humid
conditions and vice versa…The winter rainfall (December to March)
accounts for 80% of the annual rainfall amount…Grotte de Piste and
Chaara Cave sites are only a few hundred meters apart” (Ait Brahim et
al. 2019) ))) “The GP5 and Cha2 δ18O records are thus considered proxies
for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2 records
as proxy records of effective rainfall variability during the Holocene,
whereby low δ18O values reflect humid conditions and vice versa…The
winter rainfall (December to March) accounts for 80% of the annual
rainfall amount…Grotte de Piste and Chaara Cave sites are only a few
hundred meters apart” (Ait Brahim et al. 2019) /// “The GP5 and Cha2
δ18O records are thus considered proxies for effective rainfall” (Ait
Brahim et al. 2018) “Cha1 and Cha2 records as proxy records of effective
rainfall variability during the Holocene, whereby low δ18O values
reflect humid conditions and vice versa…The winter rainfall (December to
March) accounts for 80% of the annual rainfall amount…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al. 2019)’
- d18O (S2LRU6xGJ9gjMj): paleoData_QCnotes: ‘CH2; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018)’
has been replaced by ‘((( CH2; “The Chaara cave record, described by a
composite of the Cha1 and Cha2 ��18O records…a representative rainfall
index of the Western Mediterranean is constructed using the first axis
of the PCA (PC1) between the Chaara composite and Grotte de Piste
record…Grotte de Piste and Chaara Cave sites are only a few hundred
meters apart” (Ait Brahim et al., 2018) ))) CH2; “The Chaara cave
record, described by a composite of the Cha1 and Cha2 δ18O records…a
representative rainfall index of the Western Mediterranean is
constructed using the first axis of the PCA (PC1) between the Chaara
composite and Grotte de Piste record…Grotte de Piste and Chaara Cave
sites are only a few hundred meters apart” (Ait Brahim et al., 2018) ///
CH2; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018)’
Version: 1.0.8
- lastVersion: 1.0.7
- curator: nicholas
- timestamp: 2023-02-10 14:33:00 UTC
- changes:
- Paleo Interpretation metadata:
- uncertaintyLow (S2LR0Ptx2Du5lj): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR4l8aZP5XuU): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR8h7LjALhNQ): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR8hf9NraLir): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LR9pC8UeIgoy): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRa5hXG8eKtT): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRAsnExPClc7): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRcMlhng1vIP): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRD4KKxhOmHY): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRDDFLSmk9Sa): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRDnuxNDC99k): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRFYgJvI9F62): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRJfRpMX4Guq): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRMOPw8px3NR): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRn72RNikWYm): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRqVU5k24DYI): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRuihZKyimgO): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRVJkzw5KXE2): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRZ9NRmCJNlv): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRzenqoH00XH): interpretation1_scope: NULL has
been replaced by ‘climate’
Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2023-02-09 15:34:34 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Geographic metadata:
- geo_elevation: NULL has been replaced by ‘1260’
- Paleo Column metadata:
- correction (S2LR0kFbQGcnlL): paleoData_notes: NULL has been replaced
by ‘NA; paleoData_method has been standardized’
- correction (S2LR0kFbQGcnlL): paleoData_variableName:
‘hasAragoniteCorrection’ has been replaced by ‘correction’
- correction (S2LR0kFbQGcnlL): paleoData_method: NULL has been
replaced by ‘aragonite correction’
- uncertaintyLow (S2LR0Ptx2Du5lj): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyLow (S2LR0Ptx2Du5lj): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LR0Ptx2Du5lj): paleoData_variableName:
‘ageBchronUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LR0Ptx2Du5lj): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LR0Ptx2Du5lj): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyLow (S2LR0Ptx2Du5lj): paleoData_method: NULL has been
replaced by ‘Bchron’
- d18O (S2LR2w6LcELdJW): paleoData_variableName: ‘d18OComposite’ has
been replaced by ‘d18O’
- age (S2LR3OZTiOGmy8): paleoData_notes: NULL has been replaced by
‘NA; paleoData_method has been standardized; paleoData_isPrimary has
been standardized; paleoData_datum has been standardized’
- age (S2LR3OZTiOGmy8): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LR3OZTiOGmy8): paleoData_variableName: ‘agecopRa’ has been
replaced by ‘age’
- age (S2LR3OZTiOGmy8): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LR3OZTiOGmy8): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- age (S2LR3OZTiOGmy8): paleoData_method: NULL has been replaced by
‘copRa’
- uncertaintyLow (S2LR4l8aZP5XuU): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyLow (S2LR4l8aZP5XuU): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LR4l8aZP5XuU): paleoData_variableName:
‘ageStalAgeUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LR4l8aZP5XuU): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LR4l8aZP5XuU): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyLow (S2LR4l8aZP5XuU): paleoData_method: NULL has been
replaced by ‘StalAge’
- correction (S2LR5XpVAMOYEh): paleoData_notes: NULL has been replaced
by ‘NA; paleoData_method has been standardized’
- correction (S2LR5XpVAMOYEh): paleoData_variableName:
‘hasAragoniteCorrection’ has been replaced by ‘correction’
- correction (S2LR5XpVAMOYEh): paleoData_method: NULL has been
replaced by ‘aragonite correction’
- sampleID (S2LR63y7rWLnCl): paleoData_variableName: ‘sisalSampleID’
has been replaced by ‘sampleID’
- age (S2LR7ZL5qqayck): paleoData_notes: NULL has been replaced by
‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been
standardized’
- age (S2LR7ZL5qqayck): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LR7ZL5qqayck): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LR7ZL5qqayck): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- uncertaintyLow (S2LR8h7LjALhNQ): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyLow (S2LR8h7LjALhNQ): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LR8h7LjALhNQ): paleoData_variableName:
‘ageStalAgeUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LR8h7LjALhNQ): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LR8h7LjALhNQ): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyLow (S2LR8h7LjALhNQ): paleoData_method: NULL has been
replaced by ‘StalAge’
- uncertaintyLow (S2LR8hf9NraLir): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyLow (S2LR8hf9NraLir): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LR8hf9NraLir): paleoData_variableName:
‘ageBchronUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LR8hf9NraLir): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LR8hf9NraLir): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyLow (S2LR8hf9NraLir): paleoData_method: NULL has been
replaced by ‘Bchron’
- uncertaintyHigh (S2LR9pC8UeIgoy): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyHigh (S2LR9pC8UeIgoy): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyHigh (S2LR9pC8UeIgoy): paleoData_variableName:
‘agelinInterpUncertaintyHigh’ has been replaced by
‘uncertaintyHigh’
- uncertaintyHigh (S2LR9pC8UeIgoy): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh (S2LR9pC8UeIgoy): paleoData_inferredMaterial: NULL
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- uncertaintyHigh (S2LR9pC8UeIgoy): paleoData_method: NULL has been
replaced by ‘linInterp’
- uncertaintyHigh (S2LRa5hXG8eKtT): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyHigh (S2LRa5hXG8eKtT): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyHigh (S2LRa5hXG8eKtT): paleoData_variableName:
‘ageBaconUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
- uncertaintyHigh (S2LRa5hXG8eKtT): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh (S2LRa5hXG8eKtT): paleoData_inferredMaterial: NULL
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- uncertaintyHigh (S2LRa5hXG8eKtT): paleoData_method: NULL has been
replaced by ‘Bacon’
- uncertainty (S2LRADXnWi6Nco): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_summaryStatistic has been standardized;
paleoData_measurementMaterial has been standardized; paleoData_method
has been standardized’
- uncertainty (S2LRADXnWi6Nco): paleoData_variableName:
‘d18OPrecisionComposite’ has been replaced by ‘uncertainty’
- uncertainty (S2LRADXnWi6Nco): paleoData_measurementMaterial: NULL
has been replaced by ‘d18O’
- uncertainty (S2LRADXnWi6Nco): paleoData_method: NULL has been
replaced by ‘precision’
- uncertainty (S2LRADXnWi6Nco): paleoData_summaryStatistic: NULL has
been replaced by ‘composite’
- uncertainty (S2LRApZte0Lybe): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_measurementMaterial has been standardized;
paleoData_method has been standardized’
- uncertainty (S2LRApZte0Lybe): paleoData_variableName: ‘d18OStandard’
has been replaced by ‘uncertainty’
- uncertainty (S2LRApZte0Lybe): paleoData_measurementMaterial: NULL
has been replaced by ‘d18O carbonate’
- uncertainty (S2LRApZte0Lybe): paleoData_method: NULL has been
replaced by ‘standard’
- uncertaintyLow (S2LRAsnExPClc7): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
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- uncertaintyLow (S2LRAsnExPClc7): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LRAsnExPClc7): paleoData_variableName:
‘agelinInterpUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LRAsnExPClc7): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LRAsnExPClc7): paleoData_inferredMaterial: NULL
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- uncertaintyLow (S2LRAsnExPClc7): paleoData_method: NULL has been
replaced by ‘linInterp’
- uncertaintyHigh (S2LRcMlhng1vIP): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyHigh (S2LRcMlhng1vIP): paleoData_units: ‘BP’ has been
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- uncertaintyHigh (S2LRcMlhng1vIP): paleoData_variableName:
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- uncertaintyHigh (S2LRcMlhng1vIP): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh (S2LRcMlhng1vIP): paleoData_inferredMaterial: NULL
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- uncertaintyHigh (S2LRcMlhng1vIP): paleoData_method: NULL has been
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- uncertaintyLow (S2LRD4KKxhOmHY): paleoData_notes: NULL has been
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paleoData_method has been standardized; paleoData_datum has been
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- uncertaintyLow (S2LRD4KKxhOmHY): paleoData_units: ‘BP’ has been
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- uncertaintyLow (S2LRD4KKxhOmHY): paleoData_variableName:
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- uncertaintyLow (S2LRD4KKxhOmHY): paleoData_datum: NULL has been
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- uncertaintyLow (S2LRD4KKxhOmHY): paleoData_inferredMaterial: NULL
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- uncertaintyLow (S2LRD4KKxhOmHY): paleoData_method: NULL has been
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- depth (S2LRDaqPOPyvMz): paleoData_notes: NULL has been replaced by
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- depth (S2LRDaqPOPyvMz): paleoData_units: ‘depth_sample’ has been
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- depth (S2LRDaqPOPyvMz): paleoData_isPrimary: NULL has been replaced
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- uncertaintyHigh (S2LRDDFLSmk9Sa): paleoData_notes: NULL has been
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- uncertaintyHigh (S2LRDDFLSmk9Sa): paleoData_units: ‘BP’ has been
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- uncertaintyHigh (S2LRDDFLSmk9Sa): paleoData_variableName:
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- uncertaintyHigh (S2LRDDFLSmk9Sa): paleoData_datum: NULL has been
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- uncertaintyHigh (S2LRDDFLSmk9Sa): paleoData_inferredMaterial: NULL
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- uncertaintyHigh (S2LRDDFLSmk9Sa): paleoData_method: NULL has been
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- uncertainty (S2LRDgqB0das2G): paleoData_notes: NULL has been
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- uncertainty (S2LRDgqB0das2G): paleoData_variableName:
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- uncertainty (S2LRDgqB0das2G): paleoData_measurementMaterial: NULL
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- uncertainty (S2LRDgqB0das2G): paleoData_method: NULL has been
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- uncertaintyHigh (S2LRDnuxNDC99k): paleoData_notes: NULL has been
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- uncertaintyHigh (S2LRDnuxNDC99k): paleoData_units: ‘BP’ has been
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- uncertaintyHigh (S2LRDnuxNDC99k): paleoData_variableName:
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- uncertaintyHigh (S2LRDnuxNDC99k): paleoData_datum: NULL has been
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- uncertaintyHigh (S2LRDnuxNDC99k): paleoData_inferredMaterial: NULL
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- uncertaintyHigh (S2LRDnuxNDC99k): paleoData_method: NULL has been
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- age (S2LREjmvqlTizA): paleoData_notes: NULL has been replaced by
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- age (S2LREjmvqlTizA): paleoData_units: ‘BP’ has been replaced by ‘yr
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- age (S2LREjmvqlTizA): paleoData_variableName: ‘ageStalAge’ has been
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- age (S2LREjmvqlTizA): paleoData_datum: NULL has been replaced by
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- age (S2LREjmvqlTizA): paleoData_isPrimary: NULL has been replaced by
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- age (S2LREjmvqlTizA): paleoData_method: NULL has been replaced by
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- depth (S2LRElWfovzfmJ): paleoData_notes: NULL has been replaced by
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- depth (S2LRElWfovzfmJ): paleoData_units: ‘depth_sample’ has been
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- depth (S2LRElWfovzfmJ): paleoData_isPrimary: NULL has been replaced
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- age (S2LRF4YWU4eth7): paleoData_notes: NULL has been replaced by
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- age (S2LRF4YWU4eth7): paleoData_units: ‘BP’ has been replaced by ‘yr
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- age (S2LRF4YWU4eth7): paleoData_variableName: ‘agecopRa’ has been
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- age (S2LRF4YWU4eth7): paleoData_datum: NULL has been replaced by
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- age (S2LRF4YWU4eth7): paleoData_isPrimary: NULL has been replaced by
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- age (S2LRF4YWU4eth7): paleoData_method: NULL has been replaced by
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- uncertainty (S2LRfq0QYOwHXQ): paleoData_notes: NULL has been
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- uncertainty (S2LRfq0QYOwHXQ): paleoData_variableName: ‘d18OStandard’
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- uncertainty (S2LRfq0QYOwHXQ): paleoData_measurementMaterial: NULL
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- uncertainty (S2LRfq0QYOwHXQ): paleoData_method: NULL has been
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- uncertaintyHigh (S2LRFYgJvI9F62): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyHigh (S2LRFYgJvI9F62): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyHigh (S2LRFYgJvI9F62): paleoData_variableName:
‘ageStalAgeUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
- uncertaintyHigh (S2LRFYgJvI9F62): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh (S2LRFYgJvI9F62): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyHigh (S2LRFYgJvI9F62): paleoData_method: NULL has been
replaced by ‘StalAge’
- sampleID (S2LRfyw3oaz017): paleoData_variableName: ‘sisalSampleID’
has been replaced by ‘sampleID’
- sampleID (S2LRiq7GTtjc8e): paleoData_variableName: ‘sisalSampleID’
has been replaced by ‘sampleID’
- uncertaintyHigh (S2LRJfRpMX4Guq): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyHigh (S2LRJfRpMX4Guq): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyHigh (S2LRJfRpMX4Guq): paleoData_variableName:
‘agelinInterpUncertaintyHigh’ has been replaced by
‘uncertaintyHigh’
- uncertaintyHigh (S2LRJfRpMX4Guq): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh (S2LRJfRpMX4Guq): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyHigh (S2LRJfRpMX4Guq): paleoData_method: NULL has been
replaced by ‘linInterp’
- uncertainty (S2LRjLcADWBvUK): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_measurementMaterial has been standardized;
paleoData_method has been standardized’
- uncertainty (S2LRjLcADWBvUK): paleoData_variableName:
‘d18OPrecision’ has been replaced by ‘uncertainty’
- uncertainty (S2LRjLcADWBvUK): paleoData_measurementMaterial: NULL
has been replaced by ‘d18O carbonate’
- uncertainty (S2LRjLcADWBvUK): paleoData_method: NULL has been
replaced by ‘precision’
- uncertainty (S2LRKN2CiuLelF): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_measurementMaterial has been standardized;
paleoData_method has been standardized’
- uncertainty (S2LRKN2CiuLelF): paleoData_variableName:
‘d18OPrecision’ has been replaced by ‘uncertainty’
- uncertainty (S2LRKN2CiuLelF): paleoData_measurementMaterial: NULL
has been replaced by ‘d18O carbonate’
- uncertainty (S2LRKN2CiuLelF): paleoData_method: NULL has been
replaced by ‘precision’
- age (S2LRKN9GsSVn6t): paleoData_notes: NULL has been replaced by
‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been
standardized’
- age (S2LRKN9GsSVn6t): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRKN9GsSVn6t): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRKN9GsSVn6t): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- hasHiatus (S2LRleUvbdSoBk): paleoData_notes: NULL has been replaced
by ‘NA; paleoData_summaryStatistic has been standardized’
- hasHiatus (S2LRleUvbdSoBk): paleoData_variableName:
‘hasHiatusComposite’ has been replaced by ‘hasHiatus’
- hasHiatus (S2LRleUvbdSoBk): paleoData_summaryStatistic: NULL has
been replaced by ‘composite’
- age (S2LRLmtgUOKmhG): paleoData_notes: NULL has been replaced by
‘NA; paleoData_method has been standardized; paleoData_isPrimary has
been standardized; paleoData_datum has been standardized’
- age (S2LRLmtgUOKmhG): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRLmtgUOKmhG): paleoData_variableName: ‘ageBchron’ has been
replaced by ‘age’
- age (S2LRLmtgUOKmhG): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRLmtgUOKmhG): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- age (S2LRLmtgUOKmhG): paleoData_method: NULL has been replaced by
‘Bchron’
- age (S2LRm2xHFW5mdU): paleoData_notes: NULL has been replaced by
‘NA; paleoData_method has been standardized; paleoData_isPrimary has
been standardized; paleoData_datum has been standardized’
- age (S2LRm2xHFW5mdU): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRm2xHFW5mdU): paleoData_variableName: ‘agelinInterp’ has
been replaced by ‘age’
- age (S2LRm2xHFW5mdU): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRm2xHFW5mdU): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- age (S2LRm2xHFW5mdU): paleoData_method: NULL has been replaced by
‘linInterp’
- age (S2LRM4TAhqTsM9): paleoData_notes: NULL has been replaced by
‘NA; paleoData_method has been standardized; paleoData_isPrimary has
been standardized; paleoData_datum has been standardized’
- age (S2LRM4TAhqTsM9): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRM4TAhqTsM9): paleoData_variableName: ‘ageBchron’ has been
replaced by ‘age’
- age (S2LRM4TAhqTsM9): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRM4TAhqTsM9): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- age (S2LRM4TAhqTsM9): paleoData_method: NULL has been replaced by
‘Bchron’
- correction (S2LRMbcmWThY66): paleoData_notes: NULL has been replaced
by ‘NA; paleoData_method has been standardized’
- correction (S2LRMbcmWThY66): paleoData_variableName:
‘hasAragoniteCorrection’ has been replaced by ‘correction’
- correction (S2LRMbcmWThY66): paleoData_method: NULL has been
replaced by ‘aragonite correction’
- uncertainty (S2LRmhTCW8knEI): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_summaryStatistic has been standardized;
paleoData_measurementMaterial has been standardized; paleoData_method
has been standardized’
- uncertainty (S2LRmhTCW8knEI): paleoData_variableName:
‘d18OStandardComposite’ has been replaced by ‘uncertainty’
- uncertainty (S2LRmhTCW8knEI): paleoData_measurementMaterial: NULL
has been replaced by ‘d18O’
- uncertainty (S2LRmhTCW8knEI): paleoData_method: NULL has been
replaced by ‘standard’
- uncertainty (S2LRmhTCW8knEI): paleoData_summaryStatistic: NULL has
been replaced by ‘composite’
- uncertaintyLow (S2LRMOPw8px3NR): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyLow (S2LRMOPw8px3NR): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LRMOPw8px3NR): paleoData_variableName:
‘agecopRaUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LRMOPw8px3NR): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LRMOPw8px3NR): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyLow (S2LRMOPw8px3NR): paleoData_method: NULL has been
replaced by ‘copRa’
- uncertaintyHigh (S2LRn72RNikWYm): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyHigh (S2LRn72RNikWYm): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyHigh (S2LRn72RNikWYm): paleoData_variableName:
‘agecopRaUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
- uncertaintyHigh (S2LRn72RNikWYm): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh (S2LRn72RNikWYm): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyHigh (S2LRn72RNikWYm): paleoData_method: NULL has been
replaced by ‘copRa’
- age (S2LRPi2y80Dsbz): paleoData_notes: NULL has been replaced by
‘NA; paleoData_method has been standardized; paleoData_isPrimary has
been standardized; paleoData_datum has been standardized’
- age (S2LRPi2y80Dsbz): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRPi2y80Dsbz): paleoData_variableName: ‘ageStalAge’ has been
replaced by ‘age’
- age (S2LRPi2y80Dsbz): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRPi2y80Dsbz): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- age (S2LRPi2y80Dsbz): paleoData_method: NULL has been replaced by
‘StalAge’
- notes (S2LRppiaoO76CN): paleoData_variableName: ‘entityName’ has
been replaced by ‘notes’
- correction (S2LRpSeAXmGD9B): paleoData_notes: NULL has been replaced
by ‘NA; paleoData_summaryStatistic has been standardized;
paleoData_method has been standardized’
- correction (S2LRpSeAXmGD9B): paleoData_variableName:
‘hasAragoniteCorrectionComposite’ has been replaced by ‘correction’
- correction (S2LRpSeAXmGD9B): paleoData_method: NULL has been
replaced by ‘aragonite correction’
- correction (S2LRpSeAXmGD9B): paleoData_summaryStatistic: NULL has
been replaced by ‘composite’
- uncertaintyHigh (S2LRqVU5k24DYI): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyHigh (S2LRqVU5k24DYI): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyHigh (S2LRqVU5k24DYI): paleoData_variableName:
‘ageBchronUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
- uncertaintyHigh (S2LRqVU5k24DYI): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh (S2LRqVU5k24DYI): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyHigh (S2LRqVU5k24DYI): paleoData_method: NULL has been
replaced by ‘Bchron’
- age (S2LRSJLOskmYJQ): paleoData_notes: NULL has been replaced by
‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been
standardized’
- age (S2LRSJLOskmYJQ): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRSJLOskmYJQ): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRSJLOskmYJQ): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- uncertaintyLow (S2LRuihZKyimgO): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyLow (S2LRuihZKyimgO): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LRuihZKyimgO): paleoData_variableName:
‘ageBaconUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LRuihZKyimgO): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LRuihZKyimgO): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyLow (S2LRuihZKyimgO): paleoData_method: NULL has been
replaced by ‘Bacon’
- uncertaintyHigh (S2LRVJkzw5KXE2): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyHigh (S2LRVJkzw5KXE2): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyHigh (S2LRVJkzw5KXE2): paleoData_variableName:
‘agecopRaUncertaintyHigh’ has been replaced by ‘uncertaintyHigh’
- uncertaintyHigh (S2LRVJkzw5KXE2): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyHigh (S2LRVJkzw5KXE2): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyHigh (S2LRVJkzw5KXE2): paleoData_method: NULL has been
replaced by ‘copRa’
- depth (S2LRvVcb3kQHsG): paleoData_notes: NULL has been replaced by
‘NA; paleoData_summaryStatistic has been standardized’
- depth (S2LRvVcb3kQHsG): paleoData_units: ‘depth_sample’ has been
replaced by ‘mm’
- depth (S2LRvVcb3kQHsG): paleoData_variableName: ‘depthComposite’ has
been replaced by ‘depth’
- depth (S2LRvVcb3kQHsG): paleoData_summaryStatistic: NULL has been
replaced by ‘composite’
- age (S2LRwXk26EZNC6): paleoData_notes: NULL has been replaced by
‘NA; paleoData_method has been standardized; paleoData_isPrimary has
been standardized; paleoData_datum has been standardized’
- age (S2LRwXk26EZNC6): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRwXk26EZNC6): paleoData_variableName: ‘agelinReg’ has been
replaced by ‘age’
- age (S2LRwXk26EZNC6): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRwXk26EZNC6): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- age (S2LRwXk26EZNC6): paleoData_method: NULL has been replaced by
‘linReg’
- age (S2LRXorvGf6Rds): paleoData_notes: NULL has been replaced by
‘NA; paleoData_method has been standardized; paleoData_isPrimary has
been standardized; paleoData_datum has been standardized’
- age (S2LRXorvGf6Rds): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRXorvGf6Rds): paleoData_variableName: ‘agelinInterp’ has
been replaced by ‘age’
- age (S2LRXorvGf6Rds): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRXorvGf6Rds): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- age (S2LRXorvGf6Rds): paleoData_method: NULL has been replaced by
‘linInterp’
- sampleID (S2LRxpK3zksIWV): paleoData_notes: NULL has been replaced
by ‘NA; paleoData_summaryStatistic has been standardized’
- sampleID (S2LRxpK3zksIWV): paleoData_variableName:
‘sisalSampleIDComposite’ has been replaced by ‘sampleID’
- sampleID (S2LRxpK3zksIWV): paleoData_summaryStatistic: NULL has been
replaced by ‘composite’
- mineralogy (S2LRxYxotB4AKS): paleoData_notes: NULL has been replaced
by ‘NA; paleoData_summaryStatistic has been standardized’
- mineralogy (S2LRxYxotB4AKS): paleoData_variableName:
‘mineralogyComposite’ has been replaced by ‘mineralogy’
- mineralogy (S2LRxYxotB4AKS): paleoData_summaryStatistic: NULL has
been replaced by ‘composite’
- depth (S2LRYjmFIkAeCA): paleoData_notes: NULL has been replaced by
‘NA; paleoData_isPrimary has been standardized’
- depth (S2LRYjmFIkAeCA): paleoData_units: ‘depth_sample’ has been
replaced by ‘mm’
- depth (S2LRYjmFIkAeCA): paleoData_isPrimary: NULL has been replaced
by ‘TRUE’
- uncertaintyLow (S2LRZ9NRmCJNlv): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyLow (S2LRZ9NRmCJNlv): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LRZ9NRmCJNlv): paleoData_variableName:
‘agecopRaUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LRZ9NRmCJNlv): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LRZ9NRmCJNlv): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyLow (S2LRZ9NRmCJNlv): paleoData_method: NULL has been
replaced by ‘copRa’
- uncertaintyLow (S2LRzenqoH00XH): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_inferredMaterial has been standardized;
paleoData_method has been standardized; paleoData_datum has been
standardized’
- uncertaintyLow (S2LRzenqoH00XH): paleoData_units: ‘BP’ has been
replaced by ‘yr BP’
- uncertaintyLow (S2LRzenqoH00XH): paleoData_variableName:
‘agelinRegUncertaintyLow’ has been replaced by ‘uncertaintyLow’
- uncertaintyLow (S2LRzenqoH00XH): paleoData_datum: NULL has been
replaced by ‘1950’
- uncertaintyLow (S2LRzenqoH00XH): paleoData_inferredMaterial: NULL
has been replaced by ‘age’
- uncertaintyLow (S2LRzenqoH00XH): paleoData_method: NULL has been
replaced by ‘linReg’
- age (S2LRZFcbWvB0YF): paleoData_notes: NULL has been replaced by
‘NA; paleoData_method has been standardized; paleoData_isPrimary has
been standardized; paleoData_datum has been standardized’
- age (S2LRZFcbWvB0YF): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRZFcbWvB0YF): paleoData_variableName: ‘ageBacon’ has been
replaced by ‘age’
- age (S2LRZFcbWvB0YF): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRZFcbWvB0YF): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- age (S2LRZFcbWvB0YF): paleoData_method: NULL has been replaced by
‘Bacon’
- age (S2LRZoncY3x1DM): paleoData_notes: NULL has been replaced by
‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been
standardized’
- age (S2LRZoncY3x1DM): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (S2LRZoncY3x1DM): paleoData_datum: NULL has been replaced by
‘1950’
- age (S2LRZoncY3x1DM): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- uncertainty (S2LRZOw9B7JpTj): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_measurementMaterial has been standardized;
paleoData_method has been standardized’
- uncertainty (S2LRZOw9B7JpTj): paleoData_variableName: ‘d18OStandard’
has been replaced by ‘uncertainty’
- uncertainty (S2LRZOw9B7JpTj): paleoData_measurementMaterial: NULL
has been replaced by ‘d18O carbonate’
- uncertainty (S2LRZOw9B7JpTj): paleoData_method: NULL has been
replaced by ‘standard’
- Paleo Interpretation metadata:
- d18O (S2LR2w6LcELdJW): interpretation1_seasonality: ‘12,1,2,3’ has
been replaced by ‘Dec-Mar’
- d18O (S2LROeXqCyQIUp): interpretation1_seasonality: ‘12,1,2,3’ has
been replaced by ‘Dec-Mar’
- d18O (S2LRU6xGJ9gjMj): interpretation1_seasonality: ‘12,1,2,3’ has
been replaced by ‘Dec-Mar’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_seasonality: ‘12,1,2,3’ has
been replaced by ‘Dec-Mar’
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2022-07-28 17:28:58 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘1260’ has been replaced by NULL
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2022-07-15 22:59:05 UTC
- changes:
- Paleo Interpretation metadata:
- hasAragoniteCorrection (S2LR0kFbQGcnlL): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasHiatus (S2LR1Qp1QdeRcN): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LR5XpVAMOYEh): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LR63y7rWLnCl): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecisionComposite (S2LRADXnWi6Nco): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LRAHXNhDGt9E): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRApZte0Lybe): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRDgqB0das2G): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRfq0QYOwHXQ): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRfyw3oaz017): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LRgUHQRxO1bI): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRiq7GTtjc8e): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRjLcADWBvUK): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRKN2CiuLelF): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRkNiU3Kl1n1): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatusComposite (S2LRleUvbdSoBk): interpretation1_scope: NULL has
been replaced by ‘climate’
- hasAragoniteCorrection (S2LRMbcmWThY66): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandardComposite (S2LRmhTCW8knEI): interpretation1_scope: NULL
has been replaced by ‘climate’
- entityName (S2LRppiaoO76CN): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrectionComposite (S2LRpSeAXmGD9B):
interpretation1_scope: NULL has been replaced by ‘climate’
- hasHiatus (S2LRPYCC3rsOWR): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRrrNRcVgucv): interpretation1_scope: NULL has been
replaced by ‘climate’
- depthComposite (S2LRvVcb3kQHsG): interpretation1_scope: NULL has
been replaced by ‘climate’
- sisalSampleIDComposite (S2LRxpK3zksIWV): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogyComposite (S2LRxYxotB4AKS): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandard (S2LRZOw9B7JpTj): interpretation1_scope: NULL has been
replaced by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2021-10-05 21:38:41 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: ‘Morocco’ has been replaced by ‘Africa>Northern
Africa>Morocco’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nick
- timestamp: 2021-03-17 01:52:12 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Interpretation metadata:
- d18O (S2LROeXqCyQIUp): interpretation1_seasonalityGeneral: ‘Winter’
has been replaced by ‘winterOnly’
- d18O (S2LRU6xGJ9gjMj): interpretation1_seasonalityGeneral: ‘Winter’
has been replaced by ‘winterOnly’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:28:37 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: NULL has been replaced by ‘Morocco’
- Paleo Interpretation metadata:
- hasAragoniteCorrection (S2LR0kFbQGcnlL): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasHiatus (S2LR1Qp1QdeRcN): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OComposite (S2LR2w6LcELdJW): interpretation1_direction: NULL has
been replaced by ‘negative’
- d18OComposite (S2LR2w6LcELdJW): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OComposite (S2LR2w6LcELdJW): interpretation1_seasonality: NULL
has been replaced by ‘12,1,2,3’
- d18OComposite (S2LR2w6LcELdJW): interpretation1_seasonalityGeneral:
NULL has been replaced by ‘Winter’
- d18OComposite (S2LR2w6LcELdJW): interpretation1_variable: NULL has
been replaced by ‘P-E’
- d18OComposite (S2LR2w6LcELdJW): interpretation1_variableDetail: NULL
has been replaced by ‘@surface’
- hasAragoniteCorrection (S2LR5XpVAMOYEh): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LR63y7rWLnCl): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecisionComposite (S2LRADXnWi6Nco): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LRAHXNhDGt9E): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRApZte0Lybe): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRDgqB0das2G): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRfq0QYOwHXQ): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRfyw3oaz017): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LRgUHQRxO1bI): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRiq7GTtjc8e): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRjLcADWBvUK): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRKN2CiuLelF): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRkNiU3Kl1n1): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatusComposite (S2LRleUvbdSoBk): interpretation1_scope: NULL has
been replaced by ‘climate’
- hasAragoniteCorrection (S2LRMbcmWThY66): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandardComposite (S2LRmhTCW8knEI): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18O (S2LROeXqCyQIUp): interpretation1_direction: NULL has been
replaced by ‘negative’
- d18O (S2LROeXqCyQIUp): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LROeXqCyQIUp): interpretation1_seasonality: NULL has been
replaced by ‘12,1,2,3’
- d18O (S2LROeXqCyQIUp): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Winter’
- d18O (S2LROeXqCyQIUp): interpretation1_variable: NULL has been
replaced by ‘P-E’
- d18O (S2LROeXqCyQIUp): interpretation1_variableDetail: NULL has been
replaced by ‘@surface’
- entityName (S2LRppiaoO76CN): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrectionComposite (S2LRpSeAXmGD9B):
interpretation1_scope: NULL has been replaced by ‘climate’
- hasHiatus (S2LRPYCC3rsOWR): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRrrNRcVgucv): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRU6xGJ9gjMj): interpretation1_direction: NULL has been
replaced by ‘negative’
- d18O (S2LRU6xGJ9gjMj): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRU6xGJ9gjMj): interpretation1_seasonality: NULL has been
replaced by ‘12,1,2,3’
- d18O (S2LRU6xGJ9gjMj): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Winter’
- d18O (S2LRU6xGJ9gjMj): interpretation1_variable: NULL has been
replaced by ‘P-E’
- d18O (S2LRU6xGJ9gjMj): interpretation1_variableDetail: NULL has been
replaced by ‘@surface’
- depthComposite (S2LRvVcb3kQHsG): interpretation1_scope: NULL has
been replaced by ‘climate’
- sisalSampleIDComposite (S2LRxpK3zksIWV): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogyComposite (S2LRxYxotB4AKS): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandard (S2LRZOw9B7JpTj): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_direction: NULL has been
replaced by ‘negative’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_seasonality: NULL has been
replaced by ‘12,1,2,3’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Winter’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_variable: NULL has been
replaced by ‘P-E’
- d18O (S2LRzvlZ9Wrb8G): interpretation1_variableDetail: NULL has been
replaced by ‘@surface’
- Paleo Column metadata:
- d18OComposite (S2LR2w6LcELdJW): paleoData_notes: NULL has been
replaced by ‘“The GP5 and Cha2 δ18O records are thus considered proxies
for effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2 records
as proxy records of effective rainfall variability during the Holocene,
whereby low δ18O values reflect humid conditions and vice versa…The
winter rainfall (December to March) accounts for 80% of the annual
rainfall amount…Grotte de Piste and Chaara Cave sites are only a few
hundred meters apart” (Ait Brahim et al. 2019)’
- d18OComposite (S2LR2w6LcELdJW): paleoData_proxy: NULL has been
replaced by ‘d18O’
- d18OComposite (S2LR2w6LcELdJW): paleoData_proxyDetail: NULL has been
replaced by ‘aragonite’
- d18OComposite (S2LR2w6LcELdJW): paleoData_proxyGeneral: NULL has
been replaced by ‘isotope’
- d18OComposite (S2LR2w6LcELdJW): paleoData_QCCertification: NULL has
been replaced by ‘CH’
- d18OComposite (S2LR2w6LcELdJW): paleoData_QCnotes: NULL has been
replaced by ‘Need to modify composite or use rainfall index provided in
ncdc “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018)’
- d18O (S2LROeXqCyQIUp): paleoData_notes: NULL has been replaced by
‘“The GP5 and Cha2 δ18O records are thus considered proxies for
effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2 records as
proxy records of effective rainfall variability during the Holocene,
whereby low δ18O values reflect humid conditions and vice versa…The
winter rainfall (December to March) accounts for 80% of the annual
rainfall amount…Grotte de Piste and Chaara Cave sites are only a few
hundred meters apart” (Ait Brahim et al. 2019)’
- d18O (S2LROeXqCyQIUp): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LROeXqCyQIUp): paleoData_proxyDetail: NULL has been replaced
by ‘aragonite’
- d18O (S2LROeXqCyQIUp): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LROeXqCyQIUp): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LROeXqCyQIUp): paleoData_QCnotes: NULL has been replaced by
‘CH1; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018)’
- d18O (S2LRU6xGJ9gjMj): paleoData_notes: NULL has been replaced by
‘“The GP5 and Cha2 δ18O records are thus considered proxies for
effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2 records as
proxy records of effective rainfall variability during the Holocene,
whereby low δ18O values reflect humid conditions and vice versa…The
winter rainfall (December to March) accounts for 80% of the annual
rainfall amount…Grotte de Piste and Chaara Cave sites are only a few
hundred meters apart” (Ait Brahim et al. 2019)’
- d18O (S2LRU6xGJ9gjMj): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRU6xGJ9gjMj): paleoData_proxyDetail: NULL has been replaced
by ‘aragonite’
- d18O (S2LRU6xGJ9gjMj): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRU6xGJ9gjMj): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRU6xGJ9gjMj): paleoData_QCnotes: NULL has been replaced by
‘CH2; “The Chaara cave record, described by a composite of the Cha1 and
Cha2 δ18O records…a representative rainfall index of the Western
Mediterranean is constructed using the first axis of the PCA (PC1)
between the Chaara composite and Grotte de Piste record…Grotte de Piste
and Chaara Cave sites are only a few hundred meters apart” (Ait Brahim
et al., 2018)’
- d18O (S2LRzvlZ9Wrb8G): paleoData_notes: NULL has been replaced by
‘“The GP5 and Cha2 δ18O records are thus considered proxies for
effective rainfall” (Ait Brahim et al. 2018) “Cha1 and Cha2 records as
proxy records of effective rainfall variability during the Holocene,
whereby low δ18O values reflect humid conditions and vice versa…The
winter rainfall (December to March) accounts for 80% of the annual
rainfall amount…Grotte de Piste and Chaara Cave sites are only a few
hundred meters apart” (Ait Brahim et al. 2019)’
- d18O (S2LRzvlZ9Wrb8G): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRzvlZ9Wrb8G): paleoData_proxyDetail: NULL has been replaced
by ‘aragonite’
- d18O (S2LRzvlZ9Wrb8G): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRzvlZ9Wrb8G): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRzvlZ9Wrb8G): paleoData_QCnotes: NULL has been replaced by
‘CH2 (common era); “The Chaara cave record, described by a composite of
the Cha1 and Cha2 δ18O records…a representative rainfall index of the
Western Mediterranean is constructed using the first axis of the PCA
(PC1) between the Chaara composite and Grotte de Piste record…Grotte de
Piste and Chaara Cave sites are only a few hundred meters apart” (Ait
Brahim et al., 2018)’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:28:39 UTC
- notes: Created from SISALv2