Version history for j52KUHlfDnzjtukA5yhr -
Xianglongcave.Tan.2018
Version: 1.0.17
- lastVersion: 1.0.16
- curator: nicholas
- timestamp: 2025-06-25 22:46:47.048001 UTC
- changes:
- Paleo Column metadata:
- d13C (S2LRUt8Dp3CAkw): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d13C (S2LRUt8Dp3CAkw): paleoData_QCnotes: ‘((( null ))) “A spliced
XL δ18O record covering the middle-late Holocene is then constructed by
using XL16 and XL26 records, together with a previously published modern
sta- lagmite, XL21 record (Tan et al., 2015b). The composite XL δ18O
record includes original XL21 record from −59 to 38 year BP, orig- inal
XL16 record from 653 to 3331 yr BP, and the adjusted XL26 record (+0.5h)
from 3339 to 6651 yr BP ///”A spliced XL d18O record covering the
middle-late Holocene is then constructed by using XL16 and XL26 records,
together with a previously published modern sta- lagmite, XL21 record
(Tan et al., 2015b). The composite XL d18O record includes original XL21
record from −59 to 38 year BP, orig- inal XL16 record from 653 to 3331
yr BP, and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP’ has
been replaced by ‘“A spliced XL d18O record covering the middle-late
Holocene is then constructed by using XL16 and XL26 records, together
with a previously published modern sta- lagmite, XL21 record (Tan et
al., 2015b). The composite XL d18O record includes original XL21 record
from −59 to 38 year BP, orig- inal XL16 record from 653 to 3331 yr BP,
and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP’
- d18O (S2LRljclseoP6S): paleoData_proxyGeneral: ‘((( null ))) isotope
/// isotopic’ has been replaced by ‘isotopic’
- d18O (S2LRljclseoP6S): paleoData_QCCertification: ‘((( null ))) CH
/// CH, CR’ has been replaced by ‘CH, CR’
- d18O (S2LRljclseoP6S): paleoData_QCnotes: ‘((( null ))) “A spliced
XL δ18O record covering the middle-late Holocene is then constructed by
using XL16 and XL26 records, together with a previously published modern
sta- lagmite, XL21 record (Tan et al., 2015b). The composite XL δ18O
record includes original XL21 record from −59 to 38 year BP, orig- inal
XL16 record from 653 to 3331 yr BP, and the adjusted XL26 record (+0.5h)
from 3339 to 6651 yr BP ///”A spliced XL d18O record covering the
middle-late Holocene is then constructed by using XL16 and XL26 records,
together with a previously published modern sta- lagmite, XL21 record
(Tan et al., 2015b). The composite XL d18O record includes original XL21
record from -59 to 38 year BP, orig- inal XL16 record from 653 to 3331
yr BP, and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP’ has
been replaced by ‘“A spliced XL d18O record covering the middle-late
Holocene is then constructed by using XL16 and XL26 records, together
with a previously published modern sta- lagmite, XL21 record (Tan et
al., 2015b). The composite XL d18O record includes original XL21 record
from -59 to 38 year BP, orig- inal XL16 record from 653 to 3331 yr BP,
and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP’
- Paleo Interpretation metadata:
- d18O (S2LRljclseoP6S): interpretation1_seasonality: ‘((( null )))
6,7,8,9,10 /// Jun-Oct’ has been replaced by ‘Jun-Oct’
- d18O (S2LRljclseoP6S): interpretation1_variable: ‘((( null ))) P ///
precipitation’ has been replaced by ‘precipitation’
Version: 1.0.16
- lastVersion: 1.0.15
- curator: nicholas
- timestamp: 2025-06-25 21:22:30.045208 UTC
- changes:
- Paleo Column metadata:
- d13C (S2LRCbX62l4RNO): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘FALSE’
- d13C (S2LRCbX62l4RNO): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRQ7wYtgXH1C): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘FALSE’
- d18O (S2LRQ7wYtgXH1C): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d13C (S2LRUt8Dp3CAkw): paleoData_notes: ‘” Contrary to the
stalagmite d18O records, the d13C records does not show an increasing
trend since the mid- dle Holocene. However, there are significantly
positive correlation between the d13 C and the corresponding d18 O
records for XL2 (r =0.37, p <0.01), XL16 (r =0.26, p <0.01) and
XL26 (r =0.16, p < 0.01), indicating common influencing factors of
the two prox- ies on centennial- to decadal-timescales.. suggest- ing no
substantial climate induced changes of the C3/C4 plant- ratio on orbital
timescales in this region .” (Tan et al., 2018)’ has been replaced by
‘((( null ))) ” Contrary to the stalagmite δ18O records, the δ13C
records does not show an increasing trend since the mid- dle Holocene.
However, there are significantly positive correlation between the δ13 C
and the corresponding δ18 O records for XL2 (r =0.37, p <0.01), XL16
(r =0.26, p <0.01) and XL26 (r =0.16, p < 0.01), indicating common
influencing factors of the two prox- ies on centennial- to
decadal-timescales.. suggest- ing no substantial climate induced changes
of the C3/C4 plant- ratio on orbital timescales in this region .” (Tan
et al., 2018) /// ” Contrary to the stalagmite d18O records, the d13C
records does not show an increasing trend since the mid- dle Holocene.
However, there are significantly positive correlation between the d13 C
and the corresponding d18 O records for XL2 (r =0.37, p <0.01), XL16
(r =0.26, p <0.01) and XL26 (r =0.16, p < 0.01), indicating common
influencing factors of the two prox- ies on centennial- to
decadal-timescales.. suggest- ing no substantial climate induced changes
of the C3/C4 plant- ratio on orbital timescales in this region .” (Tan
et al., 2018)’
- d13C (S2LRUt8Dp3CAkw): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d13C (S2LRUt8Dp3CAkw): paleoData_QCnotes: ‘“A spliced XL d18O record
covering the middle-late Holocene is then constructed by using XL16 and
XL26 records, together with a previously published modern sta- lagmite,
XL21 record (Tan et al., 2015b). The composite XL d18O record includes
original XL21 record from −59 to 38 year BP, orig- inal XL16 record from
653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339 to
6651 yr BP’ has been replaced by ‘((( null ))) “A spliced XL δ18O record
covering the middle-late Holocene is then constructed by using XL16 and
XL26 records, together with a previously published modern sta- lagmite,
XL21 record (Tan et al., 2015b). The composite XL δ18O record includes
original XL21 record from −59 to 38 year BP, orig- inal XL16 record from
653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339 to
6651 yr BP ///”A spliced XL d18O record covering the middle-late
Holocene is then constructed by using XL16 and XL26 records, together
with a previously published modern sta- lagmite, XL21 record (Tan et
al., 2015b). The composite XL d18O record includes original XL21 record
from −59 to 38 year BP, orig- inal XL16 record from 653 to 3331 yr BP,
and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP’
- d13C (S2LRUt8Dp3CAkw): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d13C (S2LRUt8Dp3CAkw): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- d18O (S2LRdSFkWRklQZ): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘FALSE’
- d18O (S2LRdSFkWRklQZ): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRgFdZ9ES0fz): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘FALSE’
- d18O (S2LRgFdZ9ES0fz): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d13C (S2LRi0YQMT2gj6): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘FALSE’
- d13C (S2LRi0YQMT2gj6): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- d18O (S2LRljclseoP6S): paleoData_notes: ‘“we interpret our
stalagmite d18O record here as an indicator of EASM intensity on
orbital- to suborbital-timescales, but on centennial- to decadal-
timescales the monsoon precipitation amount in the upper Han- jiang
River region…The observed positive correlation between the stalagmite
d18O and d13C values confirm our interpretation of d18O as a rainfall
index in this region on short timescales.” (Tan et al., 2018)’ has been
replaced by ‘((( null ))) “we interpret our stalagmite δ18O record here
as an indicator of EASM intensity on orbital- to suborbital-timescales,
but on centennial- to decadal- timescales the monsoon precipitation
amount in the upper Han- jiang River region…The observed positive
correlation between the stalagmite δ18O and δ13C values confirm our
interpretation of δ18O as a rainfall index in this region on short
timescales.” (Tan et al., 2018) /// “we interpret our stalagmite d18O
record here as an indicator of EASM intensity on orbital- to
suborbital-timescales, but on centennial- to decadal- timescales the
monsoon precipitation amount in the upper Han- jiang River region…The
observed positive correlation between the stalagmite d18O and d13C
values confirm our interpretation of d18O as a rainfall index in this
region on short timescales.” (Tan et al., 2018)’
- d18O (S2LRljclseoP6S): paleoData_proxyGeneral: ‘isotopic’ has been
replaced by ‘((( null ))) isotope /// isotopic’
- d18O (S2LRljclseoP6S): paleoData_QCCertification: ‘CH, CR’ has been
replaced by ‘((( null ))) CH /// CH, CR’
- d18O (S2LRljclseoP6S): paleoData_QCnotes: ‘“A spliced XL d18O record
covering the middle-late Holocene is then constructed by using XL16 and
XL26 records, together with a previously published modern sta- lagmite,
XL21 record (Tan et al., 2015b). The composite XL d18O record includes
original XL21 record from -59 to 38 year BP, orig- inal XL16 record from
653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339 to
6651 yr BP’ has been replaced by ‘((( null ))) “A spliced XL δ18O record
covering the middle-late Holocene is then constructed by using XL16 and
XL26 records, together with a previously published modern sta- lagmite,
XL21 record (Tan et al., 2015b). The composite XL δ18O record includes
original XL21 record from −59 to 38 year BP, orig- inal XL16 record from
653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339 to
6651 yr BP ///”A spliced XL d18O record covering the middle-late
Holocene is then constructed by using XL16 and XL26 records, together
with a previously published modern sta- lagmite, XL21 record (Tan et
al., 2015b). The composite XL d18O record includes original XL21 record
from -59 to 38 year BP, orig- inal XL16 record from 653 to 3331 yr BP,
and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP’
- d18O (S2LRljclseoP6S): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘TRUE’
- d18O (S2LRljclseoP6S): paleoData_primaryTimeseries: NULL has been
replaced by ‘TRUE’
- d13C (S2LRrNXQsbjHkY): paleoData_meetsHoloceneHydroclimateCriteria:
NULL has been replaced by ‘FALSE’
- d13C (S2LRrNXQsbjHkY): paleoData_primaryTimeseries: NULL has been
replaced by ‘FALSE’
- Paleo Interpretation metadata:
- d18O (S2LRljclseoP6S): interpretation1_seasonality: ‘Jun-Oct’ has
been replaced by ‘((( null ))) 6,7,8,9,10 /// Jun-Oct’
- d18O (S2LRljclseoP6S): interpretation1_variable: ‘precipitation’ has
been replaced by ‘((( null ))) P /// precipitation’
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2023-08-10 23:23:01 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_author: NULL has been replaced by ‘Liangcheng Tan and Yanjun
Cai and Hai Cheng and Lawrence R. Edwards and Yongli Gao and Hai Xu and
Haiwei Zhang and Zhisheng An’
- pub1_journal: NULL has been replaced by ‘Earth and Planetary Science
Letters’
- pub1_pages: NULL has been replaced by ‘580–590’
- pub1_title: NULL has been replaced by ‘Centennial- to decadal-scale
monsoon precipitation variations in the upper Hanjiang River region,
China over the past 6650 years’
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2023-05-31 20:40:40 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRljclseoP6S): paleoData_QCnotes: ‘((( ((( “A spliced XL
��18O record covering the middle-late Holocene is then constructed by
using XL16 and XL26 records, together with a previously published modern
sta- lagmite, XL21 record (Tan et al., 2015b). The composite XL ��18O
record includes original XL21 record from ���59 to 38 year BP, orig-
inal XL16 record from 653 to 3331 yr BP, and the adjusted XL26 record
(+0.5h) from 3339 to 6651 yr BP )))”A spliced XL δ18O record covering
the middle-late Holocene is then constructed by using XL16 and XL26
records, together with a previously published modern sta- lagmite, XL21
record (Tan et al., 2015b). The composite XL δ18O record includes
original XL21 record from −59 to 38 year BP, orig- inal XL16 record from
653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339 to
6651 yr BP /// “A spliced XL δ18O record covering the middle-late
Holocene is then constructed by using XL16 and XL26 records, together
with a previously published modern sta- lagmite, XL21 record (Tan et
al., 2015b). The composite XL δ18O record includes original XL21 record
from −59 to 38 year BP, orig- inal XL16 record from 653 to 3331 yr BP,
and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP )))”A
spliced XL d18O record covering the middle-late Holocene is then
constructed by using XL16 and XL26 records, together with a previously
published modern sta- lagmite, XL21 record (Tan et al., 2015b). The
composite XL d18O record includes original XL21 record from −59 to 38
year BP, orig- inal XL16 record from 653 to 3331 yr BP, and the adjusted
XL26 record (+0.5h) from 3339 to 6651 yr BP /// “A spliced XL δ18O
record covering the middle-late Holocene is then constructed by using
XL16 and XL26 records, together with a previously published modern sta-
lagmite, XL21 record (Tan et al., 2015b). The composite XL δ18O record
includes original XL21 record from −59 to 38 year BP, orig- inal XL16
record from 653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from
3339 to 6651 yr BP’ has been replaced by ‘“A spliced XL d18O record
covering the middle-late Holocene is then constructed by using XL16 and
XL26 records, together with a previously published modern sta- lagmite,
XL21 record (Tan et al., 2015b). The composite XL d18O record includes
original XL21 record from -59 to 38 year BP, orig- inal XL16 record from
653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339 to
6651 yr BP’
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-05-30 15:50:53 UTC
- changes:
- Paleo Column metadata:
- d13C (S2LRUt8Dp3CAkw): paleoData_notes: ‘” Contrary to the
stalagmite δ18O records, the δ13C records does not show an increasing
trend since the mid- dle Holocene. However, there are significantly
positive correlation between the δ13 C and the corresponding δ18 O
records for XL2 (r =0.37, p <0.01), XL16 (r =0.26, p <0.01) and
XL26 (r =0.16, p < 0.01), indicating common influencing factors of
the two prox- ies on centennial- to decadal-timescales.. suggest- ing no
substantial climate induced changes of the C3/C4 plant- ratio on orbital
timescales in this region .” (Tan et al., 2018)’ has been replaced by ‘”
Contrary to the stalagmite d18O records, the d13C records does not show
an increasing trend since the mid- dle Holocene. However, there are
significantly positive correlation between the d13 C and the
corresponding d18 O records for XL2 (r =0.37, p <0.01), XL16 (r
=0.26, p <0.01) and XL26 (r =0.16, p < 0.01), indicating common
influencing factors of the two prox- ies on centennial- to
decadal-timescales.. suggest- ing no substantial climate induced changes
of the C3/C4 plant- ratio on orbital timescales in this region .” (Tan
et al., 2018)’
- d13C (S2LRUt8Dp3CAkw): paleoData_QCnotes: ‘“A spliced XL δ18O record
covering the middle-late Holocene is then constructed by using XL16 and
XL26 records, together with a previously published modern sta- lagmite,
XL21 record (Tan et al., 2015b). The composite XL δ18O record includes
original XL21 record from −59 to 38 year BP, orig- inal XL16 record from
653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339 to
6651 yr BP’ has been replaced by ‘“A spliced XL d18O record covering the
middle-late Holocene is then constructed by using XL16 and XL26 records,
together with a previously published modern sta- lagmite, XL21 record
(Tan et al., 2015b). The composite XL d18O record includes original XL21
record from −59 to 38 year BP, orig- inal XL16 record from 653 to 3331
yr BP, and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr
BP’
- d18O (S2LRljclseoP6S): paleoData_notes: ‘“we interpret our
stalagmite δ18O record here as an indicator of EASM intensity on
orbital- to suborbital-timescales, but on centennial- to decadal-
timescales the monsoon precipitation amount in the upper Han- jiang
River region…The observed positive correlation between the stalagmite
δ18O and δ13C values confirm our interpretation of δ18O as a rainfall
index in this region on short timescales.” (Tan et al., 2018)’ has been
replaced by ‘“we interpret our stalagmite d18O record here as an
indicator of EASM intensity on orbital- to suborbital-timescales, but on
centennial- to decadal- timescales the monsoon precipitation amount in
the upper Han- jiang River region…The observed positive correlation
between the stalagmite d18O and d13C values confirm our interpretation
of d18O as a rainfall index in this region on short timescales.” (Tan et
al., 2018)’
- d18O (S2LRljclseoP6S): paleoData_QCCertification: ‘CH’ has been
replaced by ‘CH, CR’
- d18O (S2LRljclseoP6S): paleoData_QCnotes: ‘“A spliced XL δ18O record
covering the middle-late Holocene is then constructed by using XL16 and
XL26 records, together with a previously published modern sta- lagmite,
XL21 record (Tan et al., 2015b). The composite XL δ18O record includes
original XL21 record from −59 to 38 year BP, orig- inal XL16 record from
653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339 to
6651 yr BP’ has been replaced by ‘((( ((( “A spliced XL ��18O record
covering the middle-late Holocene is then constructed by using XL16 and
XL26 records, together with a previously published modern sta- lagmite,
XL21 record (Tan et al., 2015b). The composite XL ��18O record includes
original XL21 record from ���59 to 38 year BP, orig- inal XL16 record
from 653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339
to 6651 yr BP )))”A spliced XL δ18O record covering the middle-late
Holocene is then constructed by using XL16 and XL26 records, together
with a previously published modern sta- lagmite, XL21 record (Tan et
al., 2015b). The composite XL δ18O record includes original XL21 record
from −59 to 38 year BP, orig- inal XL16 record from 653 to 3331 yr BP,
and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP /// “A
spliced XL δ18O record covering the middle-late Holocene is then
constructed by using XL16 and XL26 records, together with a previously
published modern sta- lagmite, XL21 record (Tan et al., 2015b). The
composite XL δ18O record includes original XL21 record from −59 to 38
year BP, orig- inal XL16 record from 653 to 3331 yr BP, and the adjusted
XL26 record (+0.5h) from 3339 to 6651 yr BP )))”A spliced XL d18O record
covering the middle-late Holocene is then constructed by using XL16 and
XL26 records, together with a previously published modern sta- lagmite,
XL21 record (Tan et al., 2015b). The composite XL d18O record includes
original XL21 record from −59 to 38 year BP, orig- inal XL16 record from
653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339 to
6651 yr BP /// “A spliced XL δ18O record covering the middle-late
Holocene is then constructed by using XL16 and XL26 records, together
with a previously published modern sta- lagmite, XL21 record (Tan et
al., 2015b). The composite XL δ18O record includes original XL21 record
from −59 to 38 year BP, orig- inal XL16 record from 653 to 3331 yr BP,
and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP’
- Paleo Interpretation metadata:
- d18O (S2LRljclseoP6S): interpretation1_seasonalityGeneral:
‘summerOnly’ has been replaced by ‘Summer’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-05-12 22:14:56 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRljclseoP6S): paleoData_QCnotes: ‘((( “A spliced XL ��18O
record covering the middle-late Holocene is then constructed by using
XL16 and XL26 records, together with a previously published modern sta-
lagmite, XL21 record (Tan et al., 2015b). The composite XL ��18O record
includes original XL21 record from ���59 to 38 year BP, orig- inal XL16
record from 653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from
3339 to 6651 yr BP )))”A spliced XL δ18O record covering the middle-late
Holocene is then constructed by using XL16 and XL26 records, together
with a previously published modern sta- lagmite, XL21 record (Tan et
al., 2015b). The composite XL δ18O record includes original XL21 record
from −59 to 38 year BP, orig- inal XL16 record from 653 to 3331 yr BP,
and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP /// “A
spliced XL δ18O record covering the middle-late Holocene is then
constructed by using XL16 and XL26 records, together with a previously
published modern sta- lagmite, XL21 record (Tan et al., 2015b). The
composite XL δ18O record includes original XL21 record from −59 to 38
year BP, orig- inal XL16 record from 653 to 3331 yr BP, and the adjusted
XL26 record (+0.5h) from 3339 to 6651 yr BP’ has been replaced by ‘“A
spliced XL δ18O record covering the middle-late Holocene is then
constructed by using XL16 and XL26 records, together with a previously
published modern sta- lagmite, XL21 record (Tan et al., 2015b). The
composite XL δ18O record includes original XL21 record from −59 to 38
year BP, orig- inal XL16 record from 653 to 3331 yr BP, and the adjusted
XL26 record (+0.5h) from 3339 to 6651 yr BP’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-03-24 22:26:46 UTC
- changes:
- Paleo Column metadata:
- d13C (S2LRUt8Dp3CAkw): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
- d18O (S2LRljclseoP6S): paleoData_proxyGeneral: ‘isotope’ has been
replaced by ‘isotopic’
Version: 1.0.9
- lastVersion: 1.0.8
- curator: nicholas
- timestamp: 2023-02-13 23:59:59 UTC
- changes:
- Paleo Column metadata:
- d18O (S2LRljclseoP6S): paleoData_QCnotes: ‘“A spliced XL δ18O record
covering the middle-late Holocene is then constructed by using XL16 and
XL26 records, together with a previously published modern sta- lagmite,
XL21 record (Tan et al., 2015b). The composite XL δ18O record includes
original XL21 record from −59 to 38 year BP, orig- inal XL16 record from
653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339 to
6651 yr BP’ has been replaced by ‘((( “A spliced XL ��18O record
covering the middle-late Holocene is then constructed by using XL16 and
XL26 records, together with a previously published modern sta- lagmite,
XL21 record (Tan et al., 2015b). The composite XL ��18O record includes
original XL21 record from ���59 to 38 year BP, orig- inal XL16 record
from 653 to 3331 yr BP, and the adjusted XL26 record (+0.5h) from 3339
to 6651 yr BP )))”A spliced XL δ18O record covering the middle-late
Holocene is then constructed by using XL16 and XL26 records, together
with a previously published modern sta- lagmite, XL21 record (Tan et
al., 2015b). The composite XL δ18O record includes original XL21 record
from −59 to 38 year BP, orig- inal XL16 record from 653 to 3331 yr BP,
and the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP /// “A
spliced XL δ18O record covering the middle-late Holocene is then
constructed by using XL16 and XL26 records, together with a previously
published modern sta- lagmite, XL21 record (Tan et al., 2015b). The
composite XL δ18O record includes original XL21 record from −59 to 38
year BP, orig- inal XL16 record from 653 to 3331 yr BP, and the adjusted
XL26 record (+0.5h) from 3339 to 6651 yr BP’
Version: 1.0.8
- lastVersion: 1.0.7
- curator: nicholas
- timestamp: 2023-02-10 14:34:59 UTC
- changes:
- Paleo Interpretation metadata:
- uncertaintyLow (S2LR0GOWiyWVJE): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR77ZhSPl7w0): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LR9ypKDevy4j): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRawbkku44yZ): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRbcdviJOuw7): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRd5SXaqGgp1): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LRDBPimUjPNI): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRdMudoBdZAU): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LREdP2bh1Kub): interpretation1_scope: NULL has
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- uncertaintyLow (S2LREkvOjuxgPH): interpretation1_scope: NULL has
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- uncertaintyLow (S2LREwI7dfFlYm): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRHBn3YarzZX): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRiuox3vQEzw): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LRJ0AFL50NIQ): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRj4zjLGPAvm): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRjOEIBh6j6w): interpretation1_scope: NULL has
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- uncertaintyLow (S2LRjuaA1qnTJw): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRMfCVuH9X4j): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRMG13AzOfXC): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRNgkdXuRY3e): interpretation1_scope: NULL has
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- uncertaintyHigh (S2LRNsBYuEFyDz): interpretation1_scope: NULL has
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- uncertaintyLow (S2LROdg0u9vif8): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRoJwxXj7ooA): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRPUmE5ze6y8): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRPY1orLnhro): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRqyyupql219): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRRb6RieTavl): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRrVdUT0FhsW): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRtNDLTrHfYQ): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRTQYcmrgWIL): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRtwlETZbeQ1): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRUdK8iNqmrI): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRv0FGllsBR4): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRWQISwysvyc): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRx2TCWYUOzN): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRxnvhjiCyQ9): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRXQ58GuhdHd): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRxuDiHuE1UJ): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRxwiIShzxvp): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyLow (S2LRZGW4udv32z): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRzLjCS9bzJq): interpretation1_scope: NULL has
been replaced by ‘climate’
- uncertaintyHigh (S2LRzRnw3a3yPW): interpretation1_scope: NULL has
been replaced by ‘climate’
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2022-07-28 17:44:07 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘940’ has been replaced by NULL
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2022-07-15 23:12:50 UTC
- changes:
- Paleo Interpretation metadata:
- sisalSampleIDComposite (S2LR3wujlJnQpR): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LR4dd85FRAxK): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LR5fY19YUuDc): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRbtG2iUHgP9): interpretation1_scope: NULL has been
replaced by ‘climate’
- depthComposite (S2LRCautiQpU3j): interpretation1_scope: NULL has
been replaced by ‘climate’
- d13C (S2LRCbX62l4RNO): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OPrecision (S2LRcr6Qm1vcvg): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRdBJPg5KhZn): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRdSFkWRklQZ): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogyComposite (S2LRekU3IGcYgF): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LRetTSP5ojpk): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRgFdZ9ES0fz): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OPrecisionComposite (S2LRhtQlQYjegR): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRHXjqBTDs5M): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRi0YQMT2gj6): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13CPrecision (S2LRj3I59FkSCM): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRjdzZSd6j6U): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrectionComposite (S2LRJytOPlBJ8X):
interpretation1_scope: NULL has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRmGkVRftILX): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRnnmYmKBc3U): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CPrecision (S2LRntZCJrDWPZ): interpretation1_scope: NULL has been
replaced by ‘climate’
- entityName (S2LROEOb5wVTaQ): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRPkuPxh5WEy): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRPv90TPyToR): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRQ7wYtgXH1C): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandardComposite (S2LRqMjNebXfG3): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13C (S2LRrNXQsbjHkY): interpretation1_scope: NULL has been replaced
by ‘climate’
- sisalSampleID (S2LRs2r3DDaJOI): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRS3vWNLDpGE): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRTXxVJmAOKt): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandardComposite (S2LRuQ4sp84LJY): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CComposite (S2LRUt8Dp3CAkw): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRV19vxOCy9u): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRVzmdYHT44b): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecisionComposite (S2LRYheTBGYPDs): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRYojFw5RY4s): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandard (S2LRzCJXFCFeEC): interpretation1_scope: NULL has been
replaced by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2021-10-05 21:43:35 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: NULL has been replaced by ‘Asia>Eastern
Asia>China’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nick
- timestamp: 2021-03-17 01:58:22 UTC
- changes:
- Base metadata:
- archiveType: ‘speleothem’ has been replaced by ‘Speleothem’
- Paleo Interpretation metadata:
- d18OComposite (S2LRljclseoP6S): interpretation1_seasonalityGeneral:
‘Summer’ has been replaced by ‘summerOnly’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:29:58 UTC
- changes:
- Paleo Interpretation metadata:
- sisalSampleIDComposite (S2LR3wujlJnQpR): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LR4dd85FRAxK): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LR5fY19YUuDc): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRbtG2iUHgP9): interpretation1_scope: NULL has been
replaced by ‘climate’
- depthComposite (S2LRCautiQpU3j): interpretation1_scope: NULL has
been replaced by ‘climate’
- d13C (S2LRCbX62l4RNO): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OPrecision (S2LRcr6Qm1vcvg): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRdBJPg5KhZn): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRdSFkWRklQZ): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogyComposite (S2LRekU3IGcYgF): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LRetTSP5ojpk): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRgFdZ9ES0fz): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OPrecisionComposite (S2LRhtQlQYjegR): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRHXjqBTDs5M): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRi0YQMT2gj6): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13CPrecision (S2LRj3I59FkSCM): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRjdzZSd6j6U): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrectionComposite (S2LRJytOPlBJ8X):
interpretation1_scope: NULL has been replaced by ‘climate’
- d18OComposite (S2LRljclseoP6S): interpretation1_direction: NULL has
been replaced by ‘negative’
- d18OComposite (S2LRljclseoP6S): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OComposite (S2LRljclseoP6S): interpretation1_seasonality: NULL
has been replaced by ‘6,7,8,9,10’
- d18OComposite (S2LRljclseoP6S): interpretation1_seasonalityGeneral:
NULL has been replaced by ‘Summer’
- d18OComposite (S2LRljclseoP6S): interpretation1_variable: NULL has
been replaced by ‘P’
- d18OComposite (S2LRljclseoP6S): interpretation1_variableDetail: NULL
has been replaced by ‘monsoon@surface’
- hasAragoniteCorrection (S2LRmGkVRftILX): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRnnmYmKBc3U): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CPrecision (S2LRntZCJrDWPZ): interpretation1_scope: NULL has been
replaced by ‘climate’
- entityName (S2LROEOb5wVTaQ): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRPkuPxh5WEy): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRPv90TPyToR): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRQ7wYtgXH1C): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandardComposite (S2LRqMjNebXfG3): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13C (S2LRrNXQsbjHkY): interpretation1_scope: NULL has been replaced
by ‘climate’
- sisalSampleID (S2LRs2r3DDaJOI): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRS3vWNLDpGE): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRTXxVJmAOKt): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandardComposite (S2LRuQ4sp84LJY): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CComposite (S2LRUt8Dp3CAkw): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRV19vxOCy9u): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRVzmdYHT44b): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecisionComposite (S2LRYheTBGYPDs): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRYojFw5RY4s): interpretation1_scope: NULL
has been replaced by ‘climate’
- d18OStandard (S2LRzCJXFCFeEC): interpretation1_scope: NULL has been
replaced by ‘climate’
- Paleo Column metadata:
- d13C (S2LRCbX62l4RNO): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRdSFkWRklQZ): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18O (S2LRgFdZ9ES0fz): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d13C (S2LRi0YQMT2gj6): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d18OComposite (S2LRljclseoP6S): paleoData_notes: NULL has been
replaced by ‘“we interpret our stalagmite δ18O record here as an
indicator of EASM intensity on orbital- to suborbital-timescales, but on
centennial- to decadal- timescales the monsoon precipitation amount in
the upper Han- jiang River region…The observed positive correlation
between the stalagmite δ18O and δ13C values confirm our interpretation
of δ18O as a rainfall index in this region on short timescales.” (Tan et
al., 2018)’
- d18OComposite (S2LRljclseoP6S): paleoData_proxy: NULL has been
replaced by ‘d18O’
- d18OComposite (S2LRljclseoP6S): paleoData_proxyDetail: NULL has been
replaced by ‘aragonite’
- d18OComposite (S2LRljclseoP6S): paleoData_proxyGeneral: NULL has
been replaced by ‘isotope’
- d18OComposite (S2LRljclseoP6S): paleoData_QCCertification: NULL has
been replaced by ‘CH’
- d18OComposite (S2LRljclseoP6S): paleoData_QCnotes: NULL has been
replaced by ‘“A spliced XL δ18O record covering the middle-late Holocene
is then constructed by using XL16 and XL26 records, together with a
previously published modern sta- lagmite, XL21 record (Tan et al.,
2015b). The composite XL δ18O record includes original XL21 record from
−59 to 38 year BP, orig- inal XL16 record from 653 to 3331 yr BP, and
the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP’
- d18O (S2LRQ7wYtgXH1C): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d13C (S2LRrNXQsbjHkY): paleoData_QCCertification: NULL has been
replaced by ‘CH’
- d13CComposite (S2LRUt8Dp3CAkw): paleoData_notes: NULL has been
replaced by ‘” Contrary to the stalagmite δ18O records, the δ13C records
does not show an increasing trend since the mid- dle Holocene. However,
there are significantly positive correlation between the δ13 C and the
corresponding δ18 O records for XL2 (r =0.37, p <0.01), XL16 (r
=0.26, p <0.01) and XL26 (r =0.16, p < 0.01), indicating common
influencing factors of the two prox- ies on centennial- to
decadal-timescales.. suggest- ing no substantial climate induced changes
of the C3/C4 plant- ratio on orbital timescales in this region .” (Tan
et al., 2018)’
- d13CComposite (S2LRUt8Dp3CAkw): paleoData_proxy: NULL has been
replaced by ‘d13C’
- d13CComposite (S2LRUt8Dp3CAkw): paleoData_proxyDetail: NULL has been
replaced by ‘aragonite’
- d13CComposite (S2LRUt8Dp3CAkw): paleoData_proxyGeneral: NULL has
been replaced by ‘isotope’
- d13CComposite (S2LRUt8Dp3CAkw): paleoData_QCCertification: NULL has
been replaced by ‘CH’
- d13CComposite (S2LRUt8Dp3CAkw): paleoData_QCnotes: NULL has been
replaced by ‘“A spliced XL δ18O record covering the middle-late Holocene
is then constructed by using XL16 and XL26 records, together with a
previously published modern sta- lagmite, XL21 record (Tan et al.,
2015b). The composite XL δ18O record includes original XL21 record from
−59 to 38 year BP, orig- inal XL16 record from 653 to 3331 yr BP, and
the adjusted XL26 record (+0.5h) from 3339 to 6651 yr BP’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:28:48 UTC
- notes: Created from SISALv2