Version history for t67RkbCU37uSq4sPIV2w -
Paraisocave.Wang.2017
Version: 1.0.17
- lastVersion: 1.0.16
- curator: nicholas
- timestamp: 2025-06-25 22:46:31.578424 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR8WnuOSNjqX): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LREQSPY6CV9V): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LRKkd7T4UOdy): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LRKkd7T4UOdy): paleoData_QCCertification: ‘((( null ))) CH
/// CH, CR’ has been replaced by ‘CH, CR’
- d18O (S2LRLlCGJZFNdQ): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LRPhSwxRD3El): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LRW0ZCLC2qKn): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LRoU1k2s7EkD): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LRqtRt7IkALY): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- Paleo Interpretation metadata:
- d18O (S2LRKkd7T4UOdy): interpretation1_seasonality: ‘((( null )))
11,12,1,2,3,4,5,6 /// Nov-Jun’ has been replaced by ‘Nov-Jun’
- d18O (S2LRKkd7T4UOdy): interpretation1_variable: ‘((( null ))) P ///
precipitation’ has been replaced by ‘precipitation’
Version: 1.0.16
- lastVersion: 1.0.15
- curator: nicholas
- timestamp: 2025-06-25 21:22:14.125201 UTC
- changes:
- Paleo Column metadata:
- d13C (S2LR3UzRMfBxsw): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d13C (S2LR7LxzYebMoF): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LR8WnuOSNjqX): paleoData_notes: ‘“we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘((( null ))) “we infer that most of the δ18O variability in
our record results from changes in precipitation δ18O…changes in
rainfall δ18O therefore largely reflect a Rayleigh fractionation
process, by which water vapour enriched in 18O is progressively removed
from air masses.” (Wang et al., 2017) /// “we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’
- d18O (S2LR8WnuOSNjqX): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LR8WnuOSNjqX): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LREQSPY6CV9V): paleoData_notes: ‘“we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘((( null ))) “we infer that most of the δ18O variability in
our record results from changes in precipitation δ18O…changes in
rainfall δ18O therefore largely reflect a Rayleigh fractionation
process, by which water vapour enriched in 18O is progressively removed
from air masses.” (Wang et al., 2017) /// “we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’
- d18O (S2LREQSPY6CV9V): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LREQSPY6CV9V): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRKkd7T4UOdy): paleoData_notes: ‘“we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘((( null ))) “we infer that most of the δ18O variability in
our record results from changes in precipitation δ18O…changes in
rainfall δ18O therefore largely reflect a Rayleigh fractionation
process, by which water vapour enriched in 18O is progressively removed
from air masses.” (Wang et al., 2017) /// “we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’
- d18O (S2LRKkd7T4UOdy): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LRKkd7T4UOdy): paleoData_QCCertification: ‘CH, CR’ has been
replaced by ‘((( null ))) CH /// CH, CR’
- d18O (S2LRKkd7T4UOdy): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d18O (S2LRKkd7T4UOdy): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- d18O (S2LRLlCGJZFNdQ): paleoData_notes: ‘“we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘((( null ))) “we infer that most of the δ18O variability in
our record results from changes in precipitation δ18O…changes in
rainfall δ18O therefore largely reflect a Rayleigh fractionation
process, by which water vapour enriched in 18O is progressively removed
from air masses.” (Wang et al., 2017) /// “we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’
- d18O (S2LRLlCGJZFNdQ): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LRLlCGJZFNdQ): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d13C (S2LRPe6bPoY33R): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRPhSwxRD3El): paleoData_notes: ‘“we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘((( null ))) “we infer that most of the δ18O variability in
our record results from changes in precipitation δ18O…changes in
rainfall δ18O therefore largely reflect a Rayleigh fractionation
process, by which water vapour enriched in 18O is progressively removed
from air masses.” (Wang et al., 2017) /// “we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’
- d18O (S2LRPhSwxRD3El): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LRPhSwxRD3El): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRW0ZCLC2qKn): paleoData_notes: ‘“we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘((( null ))) “we infer that most of the δ18O variability in
our record results from changes in precipitation δ18O…changes in
rainfall δ18O therefore largely reflect a Rayleigh fractionation
process, by which water vapour enriched in 18O is progressively removed
from air masses.” (Wang et al., 2017) /// “we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’
- d18O (S2LRW0ZCLC2qKn): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LRW0ZCLC2qKn): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRbAyN26zkDN): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d13C (S2LRd4DgWbmKxm): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d13C (S2LReJe6OVBZmJ): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d13C (S2LRgvIJUcegl3): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d13C (S2LRmeZGYyl0If): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- d18O (S2LRoU1k2s7EkD): paleoData_notes: ‘“we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘((( null ))) “we infer that most of the δ18O variability in
our record results from changes in precipitation δ18O…changes in
rainfall δ18O therefore largely reflect a Rayleigh fractionation
process, by which water vapour enriched in 18O is progressively removed
from air masses.” (Wang et al., 2017) /// “we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’
- d18O (S2LRoU1k2s7EkD): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LRoU1k2s7EkD): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRqtRt7IkALY): paleoData_notes: ‘“we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘((( null ))) “we infer that most of the δ18O variability in
our record results from changes in precipitation δ18O…changes in
rainfall δ18O therefore largely reflect a Rayleigh fractionation
process, by which water vapour enriched in 18O is progressively removed
from air masses.” (Wang et al., 2017) /// “we infer that most of the
d18O variability in our record results from changes in precipitation
d18O…changes in rainfall d18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’
- d18O (S2LRqtRt7IkALY): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LRqtRt7IkALY): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d13C (S2LRtkvNyEToHp): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- Paleo Interpretation metadata:
- d18O (S2LRKkd7T4UOdy): interpretation1_seasonality: ‘Nov-Jun’ has
been replaced by ‘((( null ))) 11,12,1,2,3,4,5,6 /// Nov-Jun’
- d18O (S2LRKkd7T4UOdy): interpretation1_variable: ‘precipitation’ has
been replaced by ‘((( null ))) P /// precipitation’
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2023-08-10 23:10:45 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_author: NULL has been replaced by ‘Xianfeng Wang and R.
Lawrence Edwards and Augusto S. Auler and Hai Cheng and Xinggong Kong
and Yongjin Wang and Francisco W. Cruz and Jeffrey A. Dorale and
Hong-Wei Chiang’
- pub1_journal: NULL has been replaced by ‘Nature’
- pub1_pages: NULL has been replaced by ‘204–207’
- pub1_title: NULL has been replaced by ‘Hydroclimate changes across
the Amazon lowlands over the past 45,000 years’
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2023-05-31 20:39:57 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRKkd7T4UOdy): paleoData_notes: ‘((( ((( “we infer that most
of the ��18O variability in our record results from changes in
precipitation ��18O…changes in rainfall ��18O therefore largely reflect
a Rayleigh fractionation process, by which water vapour enriched in 18O
is progressively removed from air masses.” (Wang et al., 2017) ))) “we
infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al., 2017)
/// “we infer that most of the δ18O variability in our record results
from changes in precipitation δ18O…changes in rainfall δ18O therefore
largely reflect a Rayleigh fractionation process, by which water vapour
enriched in 18O is progressively removed from air masses.” (Wang et al.,
2017) ))) “we infer that most of the d18O variability in our record
results from changes in precipitation d18O…changes in rainfall d18O
therefore largely reflect a Rayleigh fractionation process, by which
water vapour enriched in 18O is progressively removed from air masses.”
(Wang et al., 2017) /// “we infer that most of the δ18O variability in
our record results from changes in precipitation δ18O…changes in
rainfall δ18O therefore largely reflect a Rayleigh fractionation
process, by which water vapour enriched in 18O is progressively removed
from air masses.” (Wang et al., 2017)’ has been replaced by ‘“we infer
that most of the d18O variability in our record results from changes in
precipitation d18O…changes in rainfall d18O therefore largely reflect a
Rayleigh fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-05-30 15:50:11 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR8WnuOSNjqX): paleoData_notes: ‘“we infer that most of the
δ18O variability in our record results from changes in precipitation
δ18O…changes in rainfall δ18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘“we infer that most of the d18O variability in our record
results from changes in precipitation d18O…changes in rainfall d18O
therefore largely reflect a Rayleigh fractionation process, by which
water vapour enriched in 18O is progressively removed from air masses.”
(Wang et al., 2017)’
- d18O (S2LREQSPY6CV9V): paleoData_notes: ‘“we infer that most of the
δ18O variability in our record results from changes in precipitation
δ18O…changes in rainfall δ18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘“we infer that most of the d18O variability in our record
results from changes in precipitation d18O…changes in rainfall d18O
therefore largely reflect a Rayleigh fractionation process, by which
water vapour enriched in 18O is progressively removed from air masses.”
(Wang et al., 2017)’
- d18O (S2LRKkd7T4UOdy): paleoData_notes: ‘“we infer that most of the
δ18O variability in our record results from changes in precipitation
δ18O…changes in rainfall δ18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘((( ((( “we infer that most of the ��18O variability in our
record results from changes in precipitation ��18O…changes in rainfall
��18O therefore largely reflect a Rayleigh fractionation process, by
which water vapour enriched in 18O is progressively removed from air
masses.” (Wang et al., 2017) ))) “we infer that most of the δ18O
variability in our record results from changes in precipitation
δ18O…changes in rainfall δ18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017) /// “we
infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al., 2017)
))) “we infer that most of the d18O variability in our record results
from changes in precipitation d18O…changes in rainfall d18O therefore
largely reflect a Rayleigh fractionation process, by which water vapour
enriched in 18O is progressively removed from air masses.” (Wang et al.,
2017) /// “we infer that most of the δ18O variability in our record
results from changes in precipitation δ18O…changes in rainfall δ18O
therefore largely reflect a Rayleigh fractionation process, by which
water vapour enriched in 18O is progressively removed from air masses.”
(Wang et al., 2017)’
- d18O (S2LRKkd7T4UOdy): paleoData_QCCertification: ‘CH’ has been
replaced by ‘CH, CR’
- d18O (S2LRLlCGJZFNdQ): paleoData_notes: ‘“we infer that most of the
δ18O variability in our record results from changes in precipitation
δ18O…changes in rainfall δ18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘“we infer that most of the d18O variability in our record
results from changes in precipitation d18O…changes in rainfall d18O
therefore largely reflect a Rayleigh fractionation process, by which
water vapour enriched in 18O is progressively removed from air masses.”
(Wang et al., 2017)’
- d18O (S2LRPhSwxRD3El): paleoData_notes: ‘“we infer that most of the
δ18O variability in our record results from changes in precipitation
δ18O…changes in rainfall δ18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘“we infer that most of the d18O variability in our record
results from changes in precipitation d18O…changes in rainfall d18O
therefore largely reflect a Rayleigh fractionation process, by which
water vapour enriched in 18O is progressively removed from air masses.”
(Wang et al., 2017)’
- d18O (S2LRW0ZCLC2qKn): paleoData_notes: ‘“we infer that most of the
δ18O variability in our record results from changes in precipitation
δ18O…changes in rainfall δ18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘“we infer that most of the d18O variability in our record
results from changes in precipitation d18O…changes in rainfall d18O
therefore largely reflect a Rayleigh fractionation process, by which
water vapour enriched in 18O is progressively removed from air masses.”
(Wang et al., 2017)’
- d18O (S2LRoU1k2s7EkD): paleoData_notes: ‘“we infer that most of the
δ18O variability in our record results from changes in precipitation
δ18O…changes in rainfall δ18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘“we infer that most of the d18O variability in our record
results from changes in precipitation d18O…changes in rainfall d18O
therefore largely reflect a Rayleigh fractionation process, by which
water vapour enriched in 18O is progressively removed from air masses.”
(Wang et al., 2017)’
- d18O (S2LRqtRt7IkALY): paleoData_notes: ‘“we infer that most of the
δ18O variability in our record results from changes in precipitation
δ18O…changes in rainfall δ18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘“we infer that most of the d18O variability in our record
results from changes in precipitation d18O…changes in rainfall d18O
therefore largely reflect a Rayleigh fractionation process, by which
water vapour enriched in 18O is progressively removed from air masses.”
(Wang et al., 2017)’
- Paleo Interpretation metadata:
- d18O (S2LRKkd7T4UOdy): interpretation1_seasonalityGeneral:
‘summerOnly’ has been replaced by ‘Summer’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-03-29 19:59:54 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRKkd7T4UOdy): paleoData_notes: ‘((( “we infer that most of
the ��18O variability in our record results from changes in
precipitation ��18O…changes in rainfall ��18O therefore largely reflect
a Rayleigh fractionation process, by which water vapour enriched in 18O
is progressively removed from air masses.” (Wang et al., 2017) ))) “we
infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al., 2017)
/// “we infer that most of the δ18O variability in our record results
from changes in precipitation δ18O…changes in rainfall δ18O therefore
largely reflect a Rayleigh fractionation process, by which water vapour
enriched in 18O is progressively removed from air masses.” (Wang et al.,
2017)’ has been replaced by ‘“we infer that most of the δ18O variability
in our record results from changes in precipitation δ18O…changes in
rainfall δ18O therefore largely reflect a Rayleigh fractionation
process, by which water vapour enriched in 18O is progressively removed
from air masses.” (Wang et al., 2017)’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-03-24 22:26:00 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LR8WnuOSNjqX): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LREQSPY6CV9V): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRKkd7T4UOdy): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRLlCGJZFNdQ): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRPhSwxRD3El): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRW0ZCLC2qKn): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRoU1k2s7EkD): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRqtRt7IkALY): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
Version: 1.0.9
- lastVersion: 1.0.8
- curator: nicholas
- timestamp: 2023-02-13 23:54:00 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRKkd7T4UOdy): paleoData_notes: ‘“we infer that most of the
δ18O variability in our record results from changes in precipitation
δ18O…changes in rainfall δ18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017)’ has been
replaced by ‘((( “we infer that most of the ��18O variability in our
record results from changes in precipitation ��18O…changes in rainfall
��18O therefore largely reflect a Rayleigh fractionation process, by
which water vapour enriched in 18O is progressively removed from air
masses.” (Wang et al., 2017) ))) “we infer that most of the δ18O
variability in our record results from changes in precipitation
δ18O…changes in rainfall δ18O therefore largely reflect a Rayleigh
fractionation process, by which water vapour enriched in 18O is
progressively removed from air masses.” (Wang et al., 2017) /// “we
infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al.,
2017)’
Version: 1.0.8
- lastVersion: 1.0.7
- curator: nicholas
- timestamp: 2023-02-10 14:34:29 UTC
- changes:
- Paleo Interpretation metadata:
- uncertaintyHigh (S2LR1hMXqCorIQ): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR2LaRsvuiFP): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LR45jbwDqXiy): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR4sz38EhTow): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LR5ctWdM0AiY): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR7syMVTXVaF): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR812X3IpXwj): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR8N0KsfWMxK): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR8ZF37MCFqq): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR9tAgVer7Fw): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRa4UXI8InLz): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRaAslOqMaur): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRajFn3SxuLq): interpretation1_scope: NULL has
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- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2022-07-28 17:39:12 UTC
- changes:
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Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2022-07-15 23:08:21 UTC
- changes:
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Version: 1.0.3
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- curator: nicholas
- timestamp: 2021-10-05 21:42:09 UTC
- changes:
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Version: 1.0.2
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- curator: nick
- timestamp: 2021-03-17 01:56:42 UTC
- changes:
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Version: 1.0.1
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- curator: nick
- timestamp: 2021-01-12 02:29:29 UTC
- changes:
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- sisalSampleID (S2LRQTves6EWEC): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRRkxleuJdp8): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LRrM2gsxGLwV): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRSpOw5MMozN): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandard (S2LRSQVX6aE3jH): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRsUtHu1cx0M): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRt6j8O0OXDH): interpretation1_scope: NULL has been
replaced by ‘climate’
- depthComposite (S2LRtgP8q1XDuc): interpretation1_scope: NULL has
been replaced by ‘climate’
- d13C (S2LRtkvNyEToHp): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandard (S2LRtYzvooQp2L): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRuuZa4bB8cO): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRV8wlgvphad): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRVbJg1xa3sb): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasGap (S2LRvlooOthtRw): interpretation1_scope: NULL has been
replaced by ‘climate’
- entityName (S2LRVS7MtKsZet): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRW0ZCLC2qKn): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OPrecision (S2LRWFLJ7TDQkL): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRxfWaZP8Tzh): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRXWPv0aP4yQ): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRYoPAIGK8Jq): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRZC65xe4cLh): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRzjd8GGht1U): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRzPHaVzSXBE): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRZvvGjbXdV8): interpretation1_scope: NULL has been
replaced by ‘climate’
- Paleo Column metadata:
- d18O (S2LR8WnuOSNjqX): paleoData_notes: NULL has been replaced by
‘“we infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al.,
2017)’
- d18O (S2LR8WnuOSNjqX): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LR8WnuOSNjqX): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LR8WnuOSNjqX): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LREQSPY6CV9V): paleoData_notes: NULL has been replaced by
‘“we infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al.,
2017)’
- d18O (S2LREQSPY6CV9V): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LREQSPY6CV9V): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LREQSPY6CV9V): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRKkd7T4UOdy): paleoData_notes: NULL has been replaced by
‘“we infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al.,
2017)’
- d18O (S2LRKkd7T4UOdy): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRKkd7T4UOdy): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRKkd7T4UOdy): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRKkd7T4UOdy): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRKkd7T4UOdy): paleoData_QCnotes: NULL has been replaced by
‘Author provided composite’
- d18O (S2LRLlCGJZFNdQ): paleoData_notes: NULL has been replaced by
‘“we infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al.,
2017)’
- d18O (S2LRLlCGJZFNdQ): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRLlCGJZFNdQ): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRLlCGJZFNdQ): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRoU1k2s7EkD): paleoData_notes: NULL has been replaced by
‘“we infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al.,
2017)’
- d18O (S2LRoU1k2s7EkD): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRoU1k2s7EkD): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRoU1k2s7EkD): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRPhSwxRD3El): paleoData_notes: NULL has been replaced by
‘“we infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al.,
2017)’
- d18O (S2LRPhSwxRD3El): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRPhSwxRD3El): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRPhSwxRD3El): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRqtRt7IkALY): paleoData_notes: NULL has been replaced by
‘“we infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al.,
2017)’
- d18O (S2LRqtRt7IkALY): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRqtRt7IkALY): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRqtRt7IkALY): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRW0ZCLC2qKn): paleoData_notes: NULL has been replaced by
‘“we infer that most of the δ18O variability in our record results from
changes in precipitation δ18O…changes in rainfall δ18O therefore largely
reflect a Rayleigh fractionation process, by which water vapour enriched
in 18O is progressively removed from air masses.” (Wang et al.,
2017)’
- d18O (S2LRW0ZCLC2qKn): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRW0ZCLC2qKn): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRW0ZCLC2qKn): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:23:28 UTC
- notes: Created from SISALv2