Version history for AHskGxbhSALGwiMPilqr -
LiangLuar.Griffiths.2016
Version: 1.0.16
- lastVersion: 1.0.15
- curator: nicholas
- timestamp: 2023-08-10 23:03:26 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_author: NULL has been replaced by ‘Michael L. Griffiths and
Alena K. Kimbrough and Michael K. Gagan and Russell N. Drysdale and
Julia E. Cole and Kathleen R. Johnson and Jian-Xin Zhao and Benjamin I.
Cook and John C. Hellstrom and Wahyoe S. Hantoro’
- pub1_journal: NULL has been replaced by ‘Nature Communications’
- pub1_title: NULL has been replaced by ‘Western Pacific hydroclimate
linked to global climate variability over the past two millennia’
Version: 1.0.15
- lastVersion: 1.0.14
- curator: nicholas
- timestamp: 2023-05-31 20:39:27 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRgwWVs7MIO3): paleoData_notes: ‘((( ((( “We interpret
millennial-scale changes in the stalagmite d18O records to primarily
reflect changes in the d18O of rainfall, and thus AISM intensity…This
large isotopic contrast means that changes in the amount of summer
rainfall, or the fraction of the year dominated by the northwest
monsoon, produce a significant shift in the d18O of Flores rainfall.”
(Ayliffe et al., 2013) “ased on observed and modelled precipitation d18O
systema- tics, we interpret variations in the Flores Speleothem d18O
records to primarily reflect regional rainfall amount…it is likely that
the d18O of the cave drip-water represents decadal (if not multi-year)
shifts in precipitation.” (Griffiths et al 2016) ))) Amount effect: “We
interpret millennial-scale changes in the stalagmite d18O records to
primarily reflect changes in the d18O of rainfall, and thus AISM
intensity…This large isotopic contrast means that changes in the amount
of summer rainfall, or the fraction of the year dominated by the
northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016) ///
Amount effect: “We interpret millennial-scale changes in the stalagmite
d18O records to primarily reflect changes in the d18O of rainfall, and
thus AISM intensity…This large isotopic contrast means that changes in
the amount of summer rainfall, or the fraction of the year dominated by
the northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016) )))
Amount effect: “We interpret millennial-scale changes in the stalagmite
d18O records to primarily reflect changes in the d18O of rainfall, and
thus AISM intensity…This large isotopic contrast means that changes in
the amount of summer rainfall, or the fraction of the year dominated by
the northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016) ///
Amount effect: “We interpret millennial-scale changes in the stalagmite
d18O records to primarily reflect changes in the d18O of rainfall, and
thus AISM intensity…This large isotopic contrast means that changes in
the amount of summer rainfall, or the fraction of the year dominated by
the northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016)’ has
been replaced by ‘Amount effect: “We interpret millennial-scale changes
in the stalagmite d18O records to primarily reflect changes in the d18O
of rainfall, and thus AISM intensity…This large isotopic contrast means
that changes in the amount of summer rainfall, or the fraction of the
year dominated by the northwest monsoon, produce a significant shift in
the d18O of Flores rainfall.” (Ayliffe et al., 2013) “ased on observed
and modelled precipitation d18O systema- tics, we interpret variations
in the Flores Speleothem d18O records to primarily reflect regional
rainfall amount…it is likely that the d18O of the cave drip-water
represents decadal (if not multi-year) shifts in precipitation.”
(Griffiths et al 2016)’
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2023-05-30 15:49:39 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRMbhiDpVPEM): paleoData_QCnotes: ‘LR07-A8. “We developed a
composite δ18Oc record comprising the data from all three stalagmites
(hereafter just referred to as “δ18Oc record”). We first
‘wiggle-matched’ the LR07-A9 to the LR07-A8 record” (because LR07-A8 had
a much better chronology for the period of overlap) and then converted
the higher resolution LR07-A8 record to the lower resolution LR07-A9
record. We then averaged the isotope values for the period of overlap
(~88–89 kyr)…the only portion of the LR07-E11 record that was included
in the composite was the youngest section following the hiatus between $
84 and $ 79 kyr. ” (Griffiths et al 2013),’ has been replaced by
‘LR07-A8. “We developed a composite d18Oc record comprising the data
from all three stalagmites (hereafter just referred to as “d18Oc
record”). We first ‘wiggle-matched’ the LR07-A9 to the LR07-A8 record”
(because LR07-A8 had a much better chronology for the period of overlap)
and then converted the higher resolution LR07-A8 record to the lower
resolution LR07-A9 record. We then averaged the isotope values for the
period of overlap (~88–89 kyr)…the only portion of the LR07-E11 record
that was included in the composite was the youngest section following
the hiatus between $ 84 and $ 79 kyr. ” (Griffiths et al 2013),’
- d18O (S2LRbkXUkEzZ3g): paleoData_QCnotes: ‘LR07-E11. “We developed a
composite δ18Oc record comprising the data from all three stalagmites
(hereafter just referred to as “δ18Oc record”). We first
‘wiggle-matched’ the LR07-A9 to the LR07-A8 record” (because LR07-A8 had
a much better chronology for the period of overlap) and then converted
the higher resolution LR07-A8 record to the lower resolution LR07-A9
record. We then averaged the isotope values for the period of overlap
(~88–89 kyr)…the only portion of the LR07-E11 record that was included
in the composite was the youngest section following the hiatus between $
84 and $ 79 kyr. ” (Griffiths et al 2013),’ has been replaced by
‘LR07-E11. “We developed a composite d18Oc record comprising the data
from all three stalagmites (hereafter just referred to as “d18Oc
record”). We first ‘wiggle-matched’ the LR07-A9 to the LR07-A8 record”
(because LR07-A8 had a much better chronology for the period of overlap)
and then converted the higher resolution LR07-A8 record to the lower
resolution LR07-A9 record. We then averaged the isotope values for the
period of overlap (~88–89 kyr)…the only portion of the LR07-E11 record
that was included in the composite was the youngest section following
the hiatus between $ 84 and $ 79 kyr. ” (Griffiths et al 2013),’
- d18O (S2LRgwWVs7MIO3): paleoData_notes: ‘Amount effect: “We
interpret millennial-scale changes in the stalagmite d18O records to
primarily reflect changes in the d18O of rainfall, and thus AISM
intensity…This large isotopic contrast means that changes in the amount
of summer rainfall, or the fraction of the year dominated by the
northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016)’ has
been replaced by ‘((( ((( “We interpret millennial-scale changes in the
stalagmite d18O records to primarily reflect changes in the d18O of
rainfall, and thus AISM intensity…This large isotopic contrast means
that changes in the amount of summer rainfall, or the fraction of the
year dominated by the northwest monsoon, produce a significant shift in
the d18O of Flores rainfall.” (Ayliffe et al., 2013) “ased on observed
and modelled precipitation d18O systema- tics, we interpret variations
in the Flores Speleothem d18O records to primarily reflect regional
rainfall amount…it is likely that the d18O of the cave drip-water
represents decadal (if not multi-year) shifts in precipitation.”
(Griffiths et al 2016) ))) Amount effect: “We interpret millennial-scale
changes in the stalagmite d18O records to primarily reflect changes in
the d18O of rainfall, and thus AISM intensity…This large isotopic
contrast means that changes in the amount of summer rainfall, or the
fraction of the year dominated by the northwest monsoon, produce a
significant shift in the d18O of Flores rainfall.” (Ayliffe et al.,
2013) “ased on observed and modelled precipitation d18O systema- tics,
we interpret variations in the Flores Speleothem d18O records to
primarily reflect regional rainfall amount…it is likely that the d18O of
the cave drip-water represents decadal (if not multi-year) shifts in
precipitation.” (Griffiths et al 2016) /// Amount effect: “We interpret
millennial-scale changes in the stalagmite d18O records to primarily
reflect changes in the d18O of rainfall, and thus AISM intensity…This
large isotopic contrast means that changes in the amount of summer
rainfall, or the fraction of the year dominated by the northwest
monsoon, produce a significant shift in the d18O of Flores rainfall.”
(Ayliffe et al., 2013) “ased on observed and modelled precipitation d18O
systema- tics, we interpret variations in the Flores Speleothem d18O
records to primarily reflect regional rainfall amount…it is likely that
the d18O of the cave drip-water represents decadal (if not multi-year)
shifts in precipitation.” (Griffiths et al 2016) ))) Amount effect: “We
interpret millennial-scale changes in the stalagmite d18O records to
primarily reflect changes in the d18O of rainfall, and thus AISM
intensity…This large isotopic contrast means that changes in the amount
of summer rainfall, or the fraction of the year dominated by the
northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016) ///
Amount effect: “We interpret millennial-scale changes in the stalagmite
d18O records to primarily reflect changes in the d18O of rainfall, and
thus AISM intensity…This large isotopic contrast means that changes in
the amount of summer rainfall, or the fraction of the year dominated by
the northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016)’
- d18O (S2LRgwWVs7MIO3): paleoData_QCCertification: ‘CH’ has been
replaced by ‘CH, CR’
- d18O (S2LRpuzm2bDIRS): paleoData_QCnotes: ‘LR07-A9. “We developed a
composite δ18Oc record comprising the data from all three stalagmites
(hereafter just referred to as “δ18Oc record”). We first
‘wiggle-matched’ the LR07-A9 to the LR07-A8 record” (because LR07-A8 had
a much better chronology for the period of overlap) and then converted
the higher resolution LR07-A8 record to the lower resolution LR07-A9
record. We then averaged the isotope values for the period of overlap
(~88–89 kyr)…the only portion of the LR07-E11 record that was included
in the composite was the youngest section following the hiatus between $
84 and $ 79 kyr. ” (Griffiths et al 2013),’ has been replaced by
‘LR07-A9. “We developed a composite d18Oc record comprising the data
from all three stalagmites (hereafter just referred to as “d18Oc
record”). We first ‘wiggle-matched’ the LR07-A9 to the LR07-A8 record”
(because LR07-A8 had a much better chronology for the period of overlap)
and then converted the higher resolution LR07-A8 record to the lower
resolution LR07-A9 record. We then averaged the isotope values for the
period of overlap (~88–89 kyr)…the only portion of the LR07-E11 record
that was included in the composite was the youngest section following
the hiatus between $ 84 and $ 79 kyr. ” (Griffiths et al 2013),’
- Paleo Interpretation metadata:
- d18O (S2LRgwWVs7MIO3): interpretation1_seasonalityGeneral:
‘summerOnly’ has been replaced by ‘Summer’
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2023-05-25 17:48:32 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Geographic metadata:
- geo_elevation: NULL has been replaced by ‘550’
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-05-12 22:02:24 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRgwWVs7MIO3): paleoData_notes: ‘((( “We interpret
millennial-scale changes in the stalagmite d18O records to primarily
reflect changes in the d18O of rainfall, and thus AISM intensity…This
large isotopic contrast means that changes in the amount of summer
rainfall, or the fraction of the year dominated by the northwest
monsoon, produce a significant shift in the d18O of Flores rainfall.”
(Ayliffe et al., 2013) “ased on observed and modelled precipitation d18O
systema- tics, we interpret variations in the Flores Speleothem d18O
records to primarily reflect regional rainfall amount…it is likely that
the d18O of the cave drip-water represents decadal (if not multi-year)
shifts in precipitation.” (Griffiths et al 2016) ))) Amount effect: “We
interpret millennial-scale changes in the stalagmite d18O records to
primarily reflect changes in the d18O of rainfall, and thus AISM
intensity…This large isotopic contrast means that changes in the amount
of summer rainfall, or the fraction of the year dominated by the
northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016) ///
Amount effect: “We interpret millennial-scale changes in the stalagmite
d18O records to primarily reflect changes in the d18O of rainfall, and
thus AISM intensity…This large isotopic contrast means that changes in
the amount of summer rainfall, or the fraction of the year dominated by
the northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016)’ has
been replaced by ‘Amount effect: “We interpret millennial-scale changes
in the stalagmite d18O records to primarily reflect changes in the d18O
of rainfall, and thus AISM intensity…This large isotopic contrast means
that changes in the amount of summer rainfall, or the fraction of the
year dominated by the northwest monsoon, produce a significant shift in
the d18O of Flores rainfall.” (Ayliffe et al., 2013) “ased on observed
and modelled precipitation d18O systema- tics, we interpret variations
in the Flores Speleothem d18O records to primarily reflect regional
rainfall amount…it is likely that the d18O of the cave drip-water
represents decadal (if not multi-year) shifts in precipitation.”
(Griffiths et al 2016)’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-03-24 22:25:28 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRgwWVs7MIO3): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-02-10 14:34:06 UTC
- changes:
- Paleo Interpretation metadata:
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Version: 1.0.8
- lastVersion: 1.0.7
- curator: nicholas
- timestamp: 2023-01-27 00:05:27 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRgwWVs7MIO3): paleoData_notes: ‘Amount effect: “We
interpret millennial-scale changes in the stalagmite d18O records to
primarily reflect changes in the d18O of rainfall, and thus AISM
intensity…This large isotopic contrast means that changes in the amount
of summer rainfall, or the fraction of the year dominated by the
northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016)’ has
been replaced by ‘((( “We interpret millennial-scale changes in the
stalagmite d18O records to primarily reflect changes in the d18O of
rainfall, and thus AISM intensity…This large isotopic contrast means
that changes in the amount of summer rainfall, or the fraction of the
year dominated by the northwest monsoon, produce a significant shift in
the d18O of Flores rainfall.” (Ayliffe et al., 2013) “ased on observed
and modelled precipitation d18O systema- tics, we interpret variations
in the Flores Speleothem d18O records to primarily reflect regional
rainfall amount…it is likely that the d18O of the cave drip-water
represents decadal (if not multi-year) shifts in precipitation.”
(Griffiths et al 2016) ))) Amount effect: “We interpret millennial-scale
changes in the stalagmite d18O records to primarily reflect changes in
the d18O of rainfall, and thus AISM intensity…This large isotopic
contrast means that changes in the amount of summer rainfall, or the
fraction of the year dominated by the northwest monsoon, produce a
significant shift in the d18O of Flores rainfall.” (Ayliffe et al.,
2013) “ased on observed and modelled precipitation d18O systema- tics,
we interpret variations in the Flores Speleothem d18O records to
primarily reflect regional rainfall amount…it is likely that the d18O of
the cave drip-water represents decadal (if not multi-year) shifts in
precipitation.” (Griffiths et al 2016) /// Amount effect: “We interpret
millennial-scale changes in the stalagmite d18O records to primarily
reflect changes in the d18O of rainfall, and thus AISM intensity…This
large isotopic contrast means that changes in the amount of summer
rainfall, or the fraction of the year dominated by the northwest
monsoon, produce a significant shift in the d18O of Flores rainfall.”
(Ayliffe et al., 2013) “ased on observed and modelled precipitation d18O
systema- tics, we interpret variations in the Flores Speleothem d18O
records to primarily reflect regional rainfall amount…it is likely that
the d18O of the cave drip-water represents decadal (if not multi-year)
shifts in precipitation.” (Griffiths et al 2016)’
Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2022-07-28 17:35:56 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘550’ has been replaced by NULL
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2021-11-17 02:07:59 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRgwWVs7MIO3): paleoData_notes: ‘“We interpret
millennial-scale changes in the stalagmite d18O records to primarily
reflect changes in the d18O of rainfall, and thus AISM intensity…This
large isotopic contrast means that changes in the amount of summer
rainfall, or the fraction of the year dominated by the northwest
monsoon, produce a significant shift in the d18O of Flores rainfall.”
(Ayliffe et al., 2013) “ased on observed and modelled precipitation d18O
systema- tics, we interpret variations in the Flores Speleothem d18O
records to primarily reflect regional rainfall amount…it is likely that
the d18O of the cave drip-water represents decadal (if not multi-year)
shifts in precipitation.” (Griffiths et al 2016)’ has been replaced by
‘Amount effect: “We interpret millennial-scale changes in the stalagmite
d18O records to primarily reflect changes in the d18O of rainfall, and
thus AISM intensity…This large isotopic contrast means that changes in
the amount of summer rainfall, or the fraction of the year dominated by
the northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016)’
- Paleo Interpretation metadata:
- d18O (S2LRgwWVs7MIO3): interpretation1_variable: ‘M’ has been
replaced by ‘P’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2021-10-05 21:40:47 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: NULL has been replaced by ‘Indian
Ocean>Indonesia’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nick
- timestamp: 2021-03-17 01:54:47 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Column metadata:
- d18O (S2LRgwWVs7MIO3): paleoData_notes: ‘“We interpret
millennial-scale changes in the stalagmite d18O records to primarily
reflect changes in the d18O of rainfall, and thus AISM intensity…This
large isotopic contrast means that changes in the amount of summer
rainfall, or the fraction of the year dominated by the northwest
monsoon, produce a significant shift in the d18O of Flores rainfall.”
(Ayliffe et al., 2013) “ased on observed and modelled precipitation d18O
systema- tics, we interpret variations in the Flores speleothem d18O
records to primarily reflect regional rainfall amount…it is likely that
the d18O of the cave drip-water represents decadal (if not multi-year)
shifts in precipitation.” (Griffiths et al 2016)’ has been replaced by
‘“We interpret millennial-scale changes in the stalagmite d18O records
to primarily reflect changes in the d18O of rainfall, and thus AISM
intensity…This large isotopic contrast means that changes in the amount
of summer rainfall, or the fraction of the year dominated by the
northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
Speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016)’
- Paleo Interpretation metadata:
- d18O (S2LRgwWVs7MIO3): interpretation1_seasonalityGeneral: ‘Summer’
has been replaced by ‘summerOnly’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:29:18 UTC
- changes:
- Paleo Interpretation metadata:
- thicknessComposite (S2LR0QfPy8vbKH): interpretation1_scope: NULL has
been replaced by ‘climate’
- d18O (S2LR1vtapiWULK): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OPrecision (S2LR21rhtdE0yp): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LR2C4KOXcHGR): interpretation1_scope: NULL
has been replaced by ‘climate’
- thickness (S2LR2K7X7jcr6M): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LR2kl7JuXob0): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LR2PdliHBPer): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LR2qn2dmgbz7): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LR3mHBGcsGZC): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LR3ywlrP1voq): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LR51P1J8SUp7): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LR5aAgDX5HFG): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LR5AyOuvbaSH): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LR5WanFIXfiI): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LR69fO3lV3MQ): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandard (S2LR6M49kCkRlK): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LR6TAGKAvwqp): interpretation1_scope: NULL has been replaced
by ‘climate’
- thickness (S2LR7dgu4bMqYu): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LR7XgiJCnkjj): interpretation1_scope: NULL has been replaced
by ‘climate’
- hasAragoniteCorrection (S2LR8sArKgPgFo): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LR8yOUiBuS88): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleIDComposite (S2LR9rf1erOpgP): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18O (S2LR9yt6seIaFh): interpretation1_scope: NULL has been replaced
by ‘climate’
- sisalSampleID (S2LRA8WkkyHLBX): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRAHvQuuxgnF): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRAMkQUvNxDx): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasHiatusComposite (S2LRb0dele0rhl): interpretation1_scope: NULL has
been replaced by ‘climate’
- d18OStandard (S2LRB1cnJijTUW): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRbkXUkEzZ3g): interpretation1_scope: NULL has been replaced
by ‘climate’
- sisalSampleID (S2LRblSg4rlqwf): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRBmvyIyHYEK): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRbpMhxUY5Q4): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRBQbtSy3aJK): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRBSiqMDWYC9): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LRc29CjbiLdp): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRC4fnGTTL1B): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRcNVgiGpWHU): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRCZ6QryJuEG): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRdoABKxGmFg): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRDpkw1CNI56): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRdYtPxPKdEj): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRE7451RwlQY): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRedbCIBVteP): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LREF1DOykGqz): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRElx3rYppOX): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LRfhQpcEbs0O): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRFPoxzQmxPG): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRfvbrEf5lvT): interpretation1_scope: NULL
has been replaced by ‘climate’
- thickness (S2LRGfNLIuJ7Qq): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRgicJu7zBMu): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandardComposite (S2LRGjse0lntgB): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OPrecision (S2LRGk8wYTBdjH): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRGpupyUvnIV): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRgwWVs7MIO3): interpretation1_direction: NULL has been
replaced by ‘negative’
- d18O (S2LRgwWVs7MIO3): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRgwWVs7MIO3): interpretation1_seasonality: NULL has been
replaced by ‘12,1,2,3’
- d18O (S2LRgwWVs7MIO3): interpretation1_seasonalityGeneral: NULL has
been replaced by ‘Summer’
- d18O (S2LRgwWVs7MIO3): interpretation1_variable: NULL has been
replaced by ‘M’
- d18O (S2LRgwWVs7MIO3): interpretation1_variableDetail: NULL has been
replaced by ‘monsoon@surface’
- d18OPrecision (S2LRGzd3qH4r1i): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRH3RPUO6klC): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRHe5QtpgFw4): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OComposite (S2LRHI9baIBtS0): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRHQuY2R5fhw): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRhSodHQIC4U): interpretation1_scope: NULL has been replaced
by ‘climate’
- hasAragoniteCorrection (S2LRHzV2Gix8Ky): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasHiatus (S2LRi30ME5DBVl): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LRI8xIxsMAqY): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRIEIDzL9j8I): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRIyCQzTHWMq): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRIzDTlgyNc6): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRiZZNzJ9Cg8): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRj9n1gyLX8V): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandard (S2LRjgutnhejdF): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRJS726pVfXR): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogyComposite (S2LRk26wZC5nfg): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OPrecision (S2LRk7jbOC9Yrx): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRko0FeXIYGA): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRkqklPKOYtm): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRLcddO7oTQP): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRljIXppwIHN): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRlLnl458UtH): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRm4m8Ti5w3B): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRMbhiDpVPEM): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRmlm7GzEccV): interpretation1_scope: NULL has been replaced
by ‘climate’
- sisalSampleID (S2LRMVxeMfSqW1): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRMywLymmaBJ): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRnaLwnPvghm): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRNDcoLlJZUn): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRNmUBqOKSUQ): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRNNaSMgQYgd): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRnNefTB4Gdc): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRNnHytSW8OR): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRNSHhzTC5Gz): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OPrecisionComposite (S2LRnTR3RIHcEI): interpretation1_scope: NULL
has been replaced by ‘climate’
- entityName (S2LRNwAlWnlDcR): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRoaK3dGNDl2): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LROX7sQhN9Xk): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13C (S2LROYBAl5rBox): interpretation1_scope: NULL has been replaced
by ‘climate’
- hasAragoniteCorrection (S2LRP4Gar6RHTp): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRpFyZ20MdVF): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18O (S2LRPQzwWynEX8): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRPRqqX3XxaY): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRpuzm2bDIRS): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRqaDcgBgtaH): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LRqFwMcGkdL5): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRqlu7hXaomj): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRQVuKkH7xYg): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRQxZY5IGBdQ): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRRG5bC4h0dM): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRrQJi1EelPj): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OPrecision (S2LRrsWmxrByT2): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRruOSxM2l8Q): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRseBbr2eoNL): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRSfV9MA69ek): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13CStandard (S2LRSHBIXc5Cag): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRTadjT8uVso): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRtvVYQiOBr6): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LRU2W5MS0mlF): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRuKW9YB0rFA): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRUPxsi1aPcr): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13CStandard (S2LRuw5e8QjTJy): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRv98BD5Et4A): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRvbjVC5lqkb): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRvNcjeih0Tv): interpretation1_scope: NULL has been replaced
by ‘climate’
- thickness (S2LRVt1PkCH6lA): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRvZsMLLjXHU): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrectionComposite (S2LRW0QdOBFyvD):
interpretation1_scope: NULL has been replaced by ‘climate’
- d18OStandard (S2LRw1iS7Fawvg): interpretation1_scope: NULL has been
replaced by ‘climate’
- depthComposite (S2LRW9SpSKlskD): interpretation1_scope: NULL has
been replaced by ‘climate’
- mineralogy (S2LRwasqOChbJi): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRWaz5E0cZlp): interpretation1_scope: NULL has been replaced
by ‘climate’
- sisalSampleID (S2LRWkoBQnf7mJ): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRwKQkx9zR3r): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRxfzoa6nohT): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRxjCPbSC48w): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRXn7OF0VICl): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRXQInTZBEq9): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LRy8rmm4naIv): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRZ0WE8SYDk9): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRZ249FOVFSt): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LRzk8IA39B7P): interpretation1_scope: NULL has been
replaced by ‘climate’
- Paleo Column metadata:
- d18O (S2LR1vtapiWULK): paleoData_QCnotes: NULL has been replaced by
‘LR06-C6’
- d18O (S2LR9yt6seIaFh): paleoData_QCnotes: NULL has been replaced by
‘LR06-B1_2016’
- d18O (S2LRbkXUkEzZ3g): paleoData_QCnotes: NULL has been replaced by
‘LR07-E11. “We developed a composite δ18Oc record comprising the data
from all three stalagmites (hereafter just referred to as “δ18Oc
record”). We first ‘wiggle-matched’ the LR07-A9 to the LR07-A8 record”
(because LR07-A8 had a much better chronology for the period of overlap)
and then converted the higher resolution LR07-A8 record to the lower
resolution LR07-A9 record. We then averaged the isotope values for the
period of overlap (~88–89 kyr)…the only portion of the LR07-E11 record
that was included in the composite was the youngest section following
the hiatus between $ 84 and $ 79 kyr. ” (Griffiths et al 2013),’
- d18O (S2LRElx3rYppOX): paleoData_QCnotes: NULL has been replaced by
‘LR06-C2’
- d18O (S2LRgwWVs7MIO3): paleoData_notes: NULL has been replaced by
‘“We interpret millennial-scale changes in the stalagmite d18O records
to primarily reflect changes in the d18O of rainfall, and thus AISM
intensity…This large isotopic contrast means that changes in the amount
of summer rainfall, or the fraction of the year dominated by the
northwest monsoon, produce a significant shift in the d18O of Flores
rainfall.” (Ayliffe et al., 2013) “ased on observed and modelled
precipitation d18O systema- tics, we interpret variations in the Flores
speleothem d18O records to primarily reflect regional rainfall amount…it
is likely that the d18O of the cave drip-water represents decadal (if
not multi-year) shifts in precipitation.” (Griffiths et al 2016)’
- d18O (S2LRgwWVs7MIO3): paleoData_proxy: NULL has been replaced by
‘d18O’
- d18O (S2LRgwWVs7MIO3): paleoData_proxyDetail: NULL has been replaced
by ‘calcite’
- d18O (S2LRgwWVs7MIO3): paleoData_proxyGeneral: NULL has been
replaced by ‘isotope’
- d18O (S2LRgwWVs7MIO3): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRgwWVs7MIO3): paleoData_QCnotes: NULL has been replaced by
‘LL_Comp_2013. “The d18O time-series for each Liang Luar stalagmite was
resampled at 100-year resolution to produce a composite d18O record for
Flores. d18O values for replicate analysis of samples for stalagmites
LR06-B3 and LR06-C6 were averaged for inclusion in the d18O time-
series….The final d18O time-series were averaged to produce the
composite d18O record (with 95% confidence limits across intervals of
overlap)” (Ayliffe et al 2013). Later published results only for last
2ky (Griffiths et al 2016). LR06-C5 has mixed mineralogy. Rest are
calcite’
- d18OComposite (S2LRHI9baIBtS0): paleoData_QCnotes: NULL has been
replaced by ‘Seperate holocene and 80-90ka compilations published, but
only Holocene is in sisal. “LR06-B1_2016 (entity_id = 226) and
LR06-B3_2016 (entity_id = 227) are high resolution resamplings of the
top 2000 years of LR06-B1_2009 (entity_id = 204) and LR06-B3_2009
(entity_id = 205), respectively. New ages recalculated with Cheng et
al., 2013 and updated detrital thorium correction are used.//
LR06-B3_2013 (entity_id = 367) supersedes original record of
LR06-B3_2009 (entity_id = 205) and extends beyond hiatus.// The d18O
time-series for each Liang Luar stalagmite was resampled at 100-year
resolution and then averaged to produce a composite d18O record for
Flores (LL_Comp_2013; entity_id = 372).// Entity LR06-C6 (entity_id =
371) had two samples at depth_sample = 722.1mm, these were
averaged.”’
- d18O (S2LRHQuY2R5fhw): paleoData_QCnotes: NULL has been replaced by
‘LR06-B3_2013’
- d18O (S2LRhSodHQIC4U): paleoData_QCnotes: NULL has been replaced by
‘LR06-C3_2013’
- d18O (S2LRMbhiDpVPEM): paleoData_QCnotes: NULL has been replaced by
‘LR07-A8. “We developed a composite δ18Oc record comprising the data
from all three stalagmites (hereafter just referred to as “δ18Oc
record”). We first ‘wiggle-matched’ the LR07-A9 to the LR07-A8 record”
(because LR07-A8 had a much better chronology for the period of overlap)
and then converted the higher resolution LR07-A8 record to the lower
resolution LR07-A9 record. We then averaged the isotope values for the
period of overlap (~88–89 kyr)…the only portion of the LR07-E11 record
that was included in the composite was the youngest section following
the hiatus between $ 84 and $ 79 kyr. ” (Griffiths et al 2013),’
- d18O (S2LRmlm7GzEccV): paleoData_QCnotes: NULL has been replaced by
‘LR07-E1-D’
- d18O (S2LRPQzwWynEX8): paleoData_QCnotes: NULL has been replaced by
‘LR06-C3_2011’
- d18O (S2LRPRqqX3XxaY): paleoData_QCnotes: NULL has been replaced by
‘LR06-B3_2016’
- d18O (S2LRpuzm2bDIRS): paleoData_QCnotes: NULL has been replaced by
‘LR07-A9. “We developed a composite δ18Oc record comprising the data
from all three stalagmites (hereafter just referred to as “δ18Oc
record”). We first ‘wiggle-matched’ the LR07-A9 to the LR07-A8 record”
(because LR07-A8 had a much better chronology for the period of overlap)
and then converted the higher resolution LR07-A8 record to the lower
resolution LR07-A9 record. We then averaged the isotope values for the
period of overlap (~88–89 kyr)…the only portion of the LR07-E11 record
that was included in the composite was the youngest section following
the hiatus between $ 84 and $ 79 kyr. ” (Griffiths et al 2013),’
- d18O (S2LRqaDcgBgtaH): paleoData_QCnotes: NULL has been replaced by
‘LR07-E1’
- d18O (S2LRSfV9MA69ek): paleoData_QCnotes: NULL has been replaced by
‘LR06-B1_2009’
- d18O (S2LRUPxsi1aPcr): paleoData_QCnotes: NULL has been replaced by
‘LR06-C5’
- d18O (S2LRWaz5E0cZlp): paleoData_QCnotes: NULL has been replaced by
‘LR06-B3_2009’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:25:52 UTC
- notes: Created from SISALv2