Version history for bEkuKbhwOQtm1hxK6gUc - NamCo. Kasper.2015
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-08-10 23:08:20 UTC
- changes:
- Publication metadata:
- pub1_journal: ‘Journal of Quaternary Science’ has been replaced by
‘Quaternary Science Reviews’
- pub1_pages: ‘70–78’ has been replaced by ‘73–85’
- pub1_title: ‘Hydrological variations on the Central Tibetan Plateau
since the Last Glacial Maximum and their teleconnection to
inter-regional and hemispheric climate variations’ has been replaced by
‘Indian Ocean Summer Monsoon ({IOSM})-dynamics within the past 4~ka
recorded in the sediments of Lake Nam Co, central Tibetan Plateau
(China)’
- pub1_year: ‘2015’ has been replaced by ‘2012’
- pub1_author: NULL has been replaced by ‘Thomas Kasper and Torsten
Haberzettl and Stefan Doberschütz and Gerhard Daut and Junbo Wang and
Liping Zhu and Norbert Nowaczyk and Roland M√§usbacher’
- Paleo Column metadata:
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxy: ‘((( PCA )))
deleteMe /// multiproxy’ has been replaced by ‘multiproxy’
- Ca (WEB-c116b-dc14-4936-87dc-ee868): paleoData_variableName: ‘((( Ca
peak area ))) Ca /// Ca’ has been replaced by ‘Ca’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-07-05 00:52:10 UTC
- changes:
- Publication metadata:
- pub1_doi: NULL has been replaced by
‘10.1016/j.quascirev.2012.02.011’
- Paleo Column metadata:
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxy: ‘multiproxy’
has been replaced by ‘((( PCA ))) deleteMe /// multiproxy’
- ((( Ca peak area ))) Ca /// Ca (WEB-c116b-dc14-4936-87dc-ee868):
paleoData_variableName: ‘Ca’ has been replaced by ‘((( Ca peak area )))
Ca /// Ca’
Version: 1.0.9
- lastVersion: 1.0.8
- curator: nicholas
- timestamp: 2023-05-31 20:39:48 UTC
- changes:
- Paleo Column metadata:
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_notes: ‘((( ((( “PC1
is suggested to reflect the balance of minerogenic input and
autochthonous carbonate precipitation in the large Nam Co lake
system….Therefore, PC1 is interpreted as an inflow���evaporation index
(IEI). For a significantly smaller lake system with lower lake levels
the coupling of PC1 (IEI) to precipitation is weakened. Here PC1
indicates solely the minerogenic influx due to the short distance
between the coring position and the shore.”; paleoData_method has been
standardized; paleoData_proxy updated ))) “PC1 is suggested to reflect
the balance of minerogenic input and autochthonous carbonate
precipitation in the large Nam Co lake system….Therefore, PC1 is
interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized /// “PC1 is suggested to
reflect the balance of minerogenic input and autochthonous carbonate
precipitation in the large Nam Co lake system….Therefore, PC1 is
interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized ))) “PC1 is suggested to
reflect the balance of minerogenic input and autochthonous carbonate
precipitation in the large Nam Co lake system….Therefore, PC1 is
interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized /// “PC1 is suggested to
reflect the balance of minerogenic input and autochthonous carbonate
precipitation in the large Nam Co lake system….Therefore, PC1 is
interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized’ has been replaced by
‘“PC1 is suggested to reflect the balance of minerogenic input and
autochthonous carbonate precipitation in the large Nam Co lake
system….Therefore, PC1 is interpreted as an inflow–evaporation index
(IEI). For a significantly smaller lake system with lower lake levels
the coupling of PC1 (IEI) to precipitation is weakened. Here PC1
indicates solely the minerogenic influx due to the short distance
between the coring position and the shore.”; paleoData_method has been
standardized’
Version: 1.0.8
- lastVersion: 1.0.7
- curator: nicholas
- timestamp: 2023-05-30 15:50:01 UTC
- changes:
- Paleo Column metadata:
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_notes: ‘“PC1 is
suggested to reflect the balance of minerogenic input and autochthonous
carbonate precipitation in the large Nam Co lake system….Therefore, PC1
is interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized’ has been replaced by
‘((( ((( “PC1 is suggested to reflect the balance of minerogenic input
and autochthonous carbonate precipitation in the large Nam Co lake
system….Therefore, PC1 is interpreted as an inflow���evaporation index
(IEI). For a significantly smaller lake system with lower lake levels
the coupling of PC1 (IEI) to precipitation is weakened. Here PC1
indicates solely the minerogenic influx due to the short distance
between the coring position and the shore.”; paleoData_method has been
standardized; paleoData_proxy updated ))) “PC1 is suggested to reflect
the balance of minerogenic input and autochthonous carbonate
precipitation in the large Nam Co lake system….Therefore, PC1 is
interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized /// “PC1 is suggested to
reflect the balance of minerogenic input and autochthonous carbonate
precipitation in the large Nam Co lake system….Therefore, PC1 is
interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized ))) “PC1 is suggested to
reflect the balance of minerogenic input and autochthonous carbonate
precipitation in the large Nam Co lake system….Therefore, PC1 is
interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized /// “PC1 is suggested to
reflect the balance of minerogenic input and autochthonous carbonate
precipitation in the large Nam Co lake system….Therefore, PC1 is
interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized’
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxyGeneral:
‘biophysical’ has been replaced by ‘elemental’
Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2023-05-12 22:05:57 UTC
- changes:
- Paleo Column metadata:
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_notes: ‘((( “PC1 is
suggested to reflect the balance of minerogenic input and autochthonous
carbonate precipitation in the large Nam Co lake system….Therefore, PC1
is interpreted as an inflow���evaporation index (IEI). For a
significantly smaller lake system with lower lake levels the coupling of
PC1 (IEI) to precipitation is weakened. Here PC1 indicates solely the
minerogenic influx due to the short distance between the coring position
and the shore.”; paleoData_method has been standardized; paleoData_proxy
updated ))) “PC1 is suggested to reflect the balance of minerogenic
input and autochthonous carbonate precipitation in the large Nam Co lake
system….Therefore, PC1 is interpreted as an inflow–evaporation index
(IEI). For a significantly smaller lake system with lower lake levels
the coupling of PC1 (IEI) to precipitation is weakened. Here PC1
indicates solely the minerogenic influx due to the short distance
between the coring position and the shore.”; paleoData_method has been
standardized /// “PC1 is suggested to reflect the balance of minerogenic
input and autochthonous carbonate precipitation in the large Nam Co lake
system….Therefore, PC1 is interpreted as an inflow–evaporation index
(IEI). For a significantly smaller lake system with lower lake levels
the coupling of PC1 (IEI) to precipitation is weakened. Here PC1
indicates solely the minerogenic influx due to the short distance
between the coring position and the shore.”; paleoData_method has been
standardized’ has been replaced by ‘“PC1 is suggested to reflect the
balance of minerogenic input and autochthonous carbonate precipitation
in the large Nam Co lake system….Therefore, PC1 is interpreted as an
inflow–evaporation index (IEI). For a significantly smaller lake system
with lower lake levels the coupling of PC1 (IEI) to precipitation is
weakened. Here PC1 indicates solely the minerogenic influx due to the
short distance between the coring position and the shore.”;
paleoData_method has been standardized’
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2023-03-24 22:25:50 UTC
- changes:
- Paleo Column metadata:
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxy: NULL has been
replaced by ‘multiproxy’
- Paleo Interpretation metadata:
- PC1 (WEB-747c6-735e-4b08-a565-465fb): interpretation1_variable:
‘P-E’ has been replaced by ‘effectivePrecipitation’
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2023-02-16 23:26:00 UTC
- changes:
- Paleo Column metadata:
- organicCarbon (WEB-fa835-5619-44ed-b38c-5d029):
paleoData_variableName: ‘TOC’ has been replaced by ‘organicCarbon’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2023-02-13 23:53:00 UTC
- changes:
- Paleo Column metadata:
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_notes: ‘“PC1 is
suggested to reflect the balance of minerogenic input and autochthonous
carbonate precipitation in the large Nam Co lake system….Therefore, PC1
is interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized’ has been replaced by
‘((( “PC1 is suggested to reflect the balance of minerogenic input and
autochthonous carbonate precipitation in the large Nam Co lake
system….Therefore, PC1 is interpreted as an inflow���evaporation index
(IEI). For a significantly smaller lake system with lower lake levels
the coupling of PC1 (IEI) to precipitation is weakened. Here PC1
indicates solely the minerogenic influx due to the short distance
between the coring position and the shore.”; paleoData_method has been
standardized; paleoData_proxy updated ))) “PC1 is suggested to reflect
the balance of minerogenic input and autochthonous carbonate
precipitation in the large Nam Co lake system….Therefore, PC1 is
interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized /// “PC1 is suggested to
reflect the balance of minerogenic input and autochthonous carbonate
precipitation in the large Nam Co lake system….Therefore, PC1 is
interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”; paleoData_method has been standardized’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2023-02-09 16:05:43 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Geographic metadata:
- geo_elevation: NULL has been replaced by ‘4718’
- Paleo Column metadata:
- grainSize (WEB-1a4b1-7ce3-4e10-9927-ce204): paleoData_notes: NULL
has been replaced by ‘NA; paleoData_datum has been standardized’
- grainSize (WEB-1a4b1-7ce3-4e10-9927-ce204): paleoData_units: ‘%’ has
been replaced by ‘percent’
- grainSize (WEB-1a4b1-7ce3-4e10-9927-ce204): paleoData_variableName:
‘<2 um’ has been replaced by ‘grainSize’
- grainSize (WEB-1a4b1-7ce3-4e10-9927-ce204): paleoData_datum: NULL
has been replaced by ‘<2 um’
- Si (WEB-1d341-d989-4093-bfa4-58e46): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_method has been standardized’
- Si (WEB-1d341-d989-4093-bfa4-58e46): paleoData_units: ‘pa/kcps’ has
been replaced by ‘peak area’
- Si (WEB-1d341-d989-4093-bfa4-58e46): paleoData_variableName: ‘Si
peak area’ has been replaced by ‘Si’
- Si (WEB-1d341-d989-4093-bfa4-58e46): paleoData_method: NULL has been
replaced by ‘peak area’
- Fe (WEB-2447e-a89e-42fd-92e5-8a2e5): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_summaryStatistic has been standardized;
paleoData_method has been standardized’
- Fe (WEB-2447e-a89e-42fd-92e5-8a2e5): paleoData_units: ‘pa/kcps’ has
been replaced by ‘peak area’
- Fe (WEB-2447e-a89e-42fd-92e5-8a2e5): paleoData_variableName: ‘Fe
peak area’ has been replaced by ‘Fe’
- Fe (WEB-2447e-a89e-42fd-92e5-8a2e5): paleoData_method: NULL has been
replaced by ‘peak area’
- Fe (WEB-2447e-a89e-42fd-92e5-8a2e5): paleoData_summaryStatistic:
NULL has been replaced by ‘area’
- sand (WEB-36161-63b4-4a14-b08e-89235): paleoData_units: ‘%’ has been
replaced by ‘percent’
- sand (WEB-36161-63b4-4a14-b08e-89235): paleoData_variableName:
‘Sand’ has been replaced by ‘sand’
- grainSize (WEB-440ea-0750-4721-b01c-ea1bd): paleoData_notes: NULL
has been replaced by ‘NA; paleoData_summaryStatistic has been
standardized’
- grainSize (WEB-440ea-0750-4721-b01c-ea1bd): paleoData_variableName:
‘Grain size mean’ has been replaced by ‘grainSize’
- grainSize (WEB-440ea-0750-4721-b01c-ea1bd):
paleoData_summaryStatistic: NULL has been replaced by ‘mean’
- potassium (WEB-5111e-2b32-4823-9828-0593f): paleoData_notes: NULL
has been replaced by ‘NA; paleoData_method has been standardized’
- potassium (WEB-5111e-2b32-4823-9828-0593f): paleoData_units:
‘pa/kcps’ has been replaced by ‘peak area’
- potassium (WEB-5111e-2b32-4823-9828-0593f): paleoData_variableName:
‘K peak area’ has been replaced by ‘potassium’
- potassium (WEB-5111e-2b32-4823-9828-0593f): paleoData_method: NULL
has been replaced by ‘peak area’
- depth (WEB-5f4be-9507-4e94-b5e0-3d246): paleoData_variableName:
‘Depth’ has been replaced by ‘depth’
- age (WEB-675d7-ee3e-4d36-8461-a483e): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_isPrimary has been standardized’
- age (WEB-675d7-ee3e-4d36-8461-a483e): paleoData_units: ‘cal year BP’
has been replaced by ‘yr BP’
- age (WEB-675d7-ee3e-4d36-8461-a483e): paleoData_isPrimary: NULL has
been replaced by ‘TRUE’
- totalNitrogen (WEB-6ab51-dfe9-46cf-9c83-a2625): paleoData_units: ‘%’
has been replaced by ‘percent’
- totalNitrogen (WEB-6ab51-dfe9-46cf-9c83-a2625):
paleoData_variableName: ‘TN’ has been replaced by ‘totalNitrogen’
- TIC (WEB-6b7fb-2366-40af-94e7-7986e): paleoData_units: ‘%’ has been
replaced by ‘percent’
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_notes: ‘“PC1 is
suggested to reflect the balance of minerogenic input and autochthonous
carbonate precipitation in the large Nam Co lake system….Therefore, PC1
is interpreted as an inflow–evaporation index (IEI). For a significantly
smaller lake system with lower lake levels the coupling of PC1 (IEI) to
precipitation is weakened. Here PC1 indicates solely the minerogenic
influx due to the short distance between the coring position and the
shore.”’ has been replaced by ‘“PC1 is suggested to reflect the balance
of minerogenic input and autochthonous carbonate precipitation in the
large Nam Co lake system….Therefore, PC1 is interpreted as an
inflow–evaporation index (IEI). For a significantly smaller lake system
with lower lake levels the coupling of PC1 (IEI) to precipitation is
weakened. Here PC1 indicates solely the minerogenic influx due to the
short distance between the coring position and the shore.”;
paleoData_method has been standardized’
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxy: ‘PCA’ has
been replaced by NULL
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_method: NULL has
been replaced by ‘principal components’
- TOC/TN (WEB-91189-4901-4dd9-8908-5a9c9): paleoData_units: ‘%’ has
been replaced by ‘percent’
- Ba (WEB-918cc-0dbc-4269-94d8-d6f4d): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_method has been standardized’
- Ba (WEB-918cc-0dbc-4269-94d8-d6f4d): paleoData_units: ‘pa/kcps’ has
been replaced by ‘peak area’
- Ba (WEB-918cc-0dbc-4269-94d8-d6f4d): paleoData_variableName: ‘Ba
peak area’ has been replaced by ‘Ba’
- Ba (WEB-918cc-0dbc-4269-94d8-d6f4d): paleoData_method: NULL has been
replaced by ‘peak area’
- sedimentationRate (WEB-91b4c-dcba-4928-a3f1-3c8e5): paleoData_units:
‘cm/a’ has been replaced by ‘cm/yr’
- sedimentationRate (WEB-91b4c-dcba-4928-a3f1-3c8e5):
paleoData_variableName: ‘Sedim rate’ has been replaced by
‘sedimentationRate’
- sedimentationRate (WEB-989d3-c8d2-4972-8922-d0285): paleoData_units:
‘cm/a’ has been replaced by ‘cm/yr’
- sedimentationRate (WEB-989d3-c8d2-4972-8922-d0285):
paleoData_variableName: ‘Mean Sedim rate’ has been replaced by
‘sedimentationRate’
- Ti (WEB-a0a8c-89d4-4883-ba22-c77d0): paleoData_units: ‘pa/kcps’ has
been replaced by ‘peak area’
- Ti (WEB-a0a8c-89d4-4883-ba22-c77d0): paleoData_variableName: ‘Ti
peak area’ has been replaced by ‘Ti’
- Rb (WEB-aefd4-7d29-4318-a5e0-d0d86): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_method has been standardized’
- Rb (WEB-aefd4-7d29-4318-a5e0-d0d86): paleoData_units: ‘pa/kcps’ has
been replaced by ‘peak area’
- Rb (WEB-aefd4-7d29-4318-a5e0-d0d86): paleoData_variableName: ‘Rb
peak area’ has been replaced by ‘Rb’
- Rb (WEB-aefd4-7d29-4318-a5e0-d0d86): paleoData_method: NULL has been
replaced by ‘peak area’
- silt (WEB-b5ec1-d06b-488c-805c-d065b): paleoData_units: ‘%’ has been
replaced by ‘percent’
- silt (WEB-b5ec1-d06b-488c-805c-d065b): paleoData_variableName:
‘Silt’ has been replaced by ‘silt’
- needsToBeChanged (WEB-ba688-529f-42a6-898a-d3048): paleoData_units:
‘%’ has been replaced by ‘percent’
- needsToBeChanged (WEB-ba688-529f-42a6-898a-d3048):
paleoData_variableName: ‘TS’ has been replaced by
‘needsToBeChanged’
- Ca (WEB-c116b-dc14-4936-87dc-ee868): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_method has been standardized’
- Ca (WEB-c116b-dc14-4936-87dc-ee868): paleoData_units: ‘pa/kcps’ has
been replaced by ‘peak area’
- Ca (WEB-c116b-dc14-4936-87dc-ee868): paleoData_variableName: ‘Ca
peak area’ has been replaced by ‘Ca’
- Ca (WEB-c116b-dc14-4936-87dc-ee868): paleoData_method: NULL has been
replaced by ‘peak area’
- Sr (WEB-c217c-4ad7-45b8-b19f-af038): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_method has been standardized’
- Sr (WEB-c217c-4ad7-45b8-b19f-af038): paleoData_units: ‘pa/kcps’ has
been replaced by ‘peak area’
- Sr (WEB-c217c-4ad7-45b8-b19f-af038): paleoData_variableName: ‘Sr
peak area’ has been replaced by ‘Sr’
- Sr (WEB-c217c-4ad7-45b8-b19f-af038): paleoData_method: NULL has been
replaced by ‘peak area’
- depth (WEB-c3a95-bb07-4f2a-86a3-ffd8f): paleoData_variableName:
‘Depth’ has been replaced by ‘depth’
- Al (WEB-dd04a-340e-4371-bcd9-24c63): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_method has been standardized’
- Al (WEB-dd04a-340e-4371-bcd9-24c63): paleoData_units: ‘pa/kcps’ has
been replaced by ‘peak area’
- Al (WEB-dd04a-340e-4371-bcd9-24c63): paleoData_variableName: ‘Al
peak area’ has been replaced by ‘Al’
- Al (WEB-dd04a-340e-4371-bcd9-24c63): paleoData_method: NULL has been
replaced by ‘peak area’
- age (WEB-f89e6-6a01-4391-adcc-b1e5f): paleoData_notes: NULL has been
replaced by ‘NA; paleoData_isPrimary has been standardized’
- age (WEB-f89e6-6a01-4391-adcc-b1e5f): paleoData_units: ‘cal year BP’
has been replaced by ‘yr BP’
- age (WEB-f89e6-6a01-4391-adcc-b1e5f): paleoData_isPrimary: NULL has
been replaced by ‘TRUE’
- TOC (WEB-fa835-5619-44ed-b38c-5d029): paleoData_units: ‘%’ has been
replaced by ‘percent’
- Paleo Interpretation metadata:
- PC1 (WEB-747c6-735e-4b08-a565-465fb): interpretation1_seasonality:
‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘Annual’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2023-01-27 00:05:41 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_doi: ‘10.1002/jqs.2759’ has been replaced by NULL
- Geographic metadata:
- geo_elevation: ‘4718’ has been replaced by NULL
- geo_gcmdLocation: NULL has been replaced by ‘Asia>Eastern
Asia>China’
- Paleo Column metadata:
- <2 um (WEB-1a4b1-7ce3-4e10-9927-ce204): paleoData_variableName:
‘<2 µm’ has been replaced by ‘<2 um’
- Grain size mean (WEB-440ea-0750-4721-b01c-ea1bd): paleoData_units:
‘µm’ has been replaced by ‘um’
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_variableName: ‘PC1
loading’ has been replaced by ‘PC1’
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_notes: NULL has been
replaced by ‘“PC1 is suggested to reflect the balance of minerogenic
input and autochthonous carbonate precipitation in the large Nam Co lake
system….Therefore, PC1 is interpreted as an inflow–evaporation index
(IEI). For a significantly smaller lake system with lower lake levels
the coupling of PC1 (IEI) to precipitation is weakened. Here PC1
indicates solely the minerogenic influx due to the short distance
between the coring position and the shore.”’
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxyDetail: NULL
has been replaced by ‘XRF core scan data (element abundance)’
- PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxyGeneral: NULL
has been replaced by ‘biophysical’
- Paleo Interpretation metadata:
- <2 um (WEB-1a4b1-7ce3-4e10-9927-ce204): interpretation1_scope:
NULL has been replaced by ‘climate’
- Si peak area (WEB-1d341-d989-4093-bfa4-58e46):
interpretation1_scope: NULL has been replaced by ‘climate’
- Fe peak area (WEB-2447e-a89e-42fd-92e5-8a2e5):
interpretation1_scope: NULL has been replaced by ‘climate’
- Sand (WEB-36161-63b4-4a14-b08e-89235): interpretation1_scope: NULL
has been replaced by ‘climate’
- Grain size mean (WEB-440ea-0750-4721-b01c-ea1bd):
interpretation1_scope: NULL has been replaced by ‘climate’
- K peak area (WEB-5111e-2b32-4823-9828-0593f): interpretation1_scope:
NULL has been replaced by ‘climate’
- TN (WEB-6ab51-dfe9-46cf-9c83-a2625): interpretation1_scope: NULL has
been replaced by ‘climate’
- TIC (WEB-6b7fb-2366-40af-94e7-7986e): interpretation1_scope: NULL
has been replaced by ‘climate’
- PC1 (WEB-747c6-735e-4b08-a565-465fb): interpretation1_seasonality:
‘Annual’ has been replaced by ‘1,2,3,4,5,6,7,8,9,10,11,12’
- PC1 (WEB-747c6-735e-4b08-a565-465fb):
interpretation1_variableDetail: ‘shoreline@surface’ has been replaced by ‘@surface’
- PC1 (WEB-747c6-735e-4b08-a565-465fb):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- TOC/TN (WEB-91189-4901-4dd9-8908-5a9c9): interpretation1_scope: NULL
has been replaced by ‘climate’
- Ba peak area (WEB-918cc-0dbc-4269-94d8-d6f4d):
interpretation1_scope: NULL has been replaced by ‘climate’
- Sedim rate (WEB-91b4c-dcba-4928-a3f1-3c8e5): interpretation1_scope:
NULL has been replaced by ‘climate’
- Mean Sedim rate (WEB-989d3-c8d2-4972-8922-d0285):
interpretation1_scope: NULL has been replaced by ‘climate’
- Ti peak area (WEB-a0a8c-89d4-4883-ba22-c77d0):
interpretation1_scope: NULL has been replaced by ‘climate’
- Rb peak area (WEB-aefd4-7d29-4318-a5e0-d0d86):
interpretation1_scope: NULL has been replaced by ‘climate’
- Silt (WEB-b5ec1-d06b-488c-805c-d065b): interpretation1_scope: NULL
has been replaced by ‘climate’
- TS (WEB-ba688-529f-42a6-898a-d3048): interpretation1_scope: NULL has
been replaced by ‘climate’
- Ca peak area (WEB-c116b-dc14-4936-87dc-ee868):
interpretation1_scope: NULL has been replaced by ‘climate’
- Sr peak area (WEB-c217c-4ad7-45b8-b19f-af038):
interpretation1_scope: NULL has been replaced by ‘climate’
- Al peak area (WEB-dd04a-340e-4371-bcd9-24c63):
interpretation1_scope: NULL has been replaced by ‘climate’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2023-01-26 23:08:33 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Base metadata:
- Geographic metadata:
- geo_elevation: NULL has been replaced by ‘4718’
- geo_gcmdLocation: ‘Asia>Eastern Asia>China’ has been replaced
by NULL
- Publication metadata:
- pub1_doi: NULL has been replaced by ‘10.1002/jqs.2759’
- Paleo Column metadata:
- <2 µm (WEB-1a4b1-7ce3-4e10-9927-ce204): paleoData_variableName:
‘<2 um’ has been replaced by ‘<2 µm’
- Grain size mean (WEB-440ea-0750-4721-b01c-ea1bd): paleoData_units:
‘um’ has been replaced by ‘µm’
- PC1 loading (WEB-747c6-735e-4b08-a565-465fb): paleoData_notes: ‘“PC1
is suggested to reflect the balance of minerogenic input and
autochthonous carbonate precipitation in the large Nam Co lake
system….Therefore, PC1 is interpreted as an inflow–evaporation index
(IEI). For a significantly smaller lake system with lower lake levels
the coupling of PC1 (IEI) to precipitation is weakened. Here PC1
indicates solely the minerogenic influx due to the short distance
between the coring position and the shore.”’ has been replaced by
NULL
- PC1 loading (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxyDetail:
‘XRF core scan data (element abundance)’ has been replaced by NULL
- PC1 loading (WEB-747c6-735e-4b08-a565-465fb):
paleoData_proxyGeneral: ‘biophysical’ has been replaced by NULL
- PC1 loading (WEB-747c6-735e-4b08-a565-465fb):
paleoData_variableName: ‘PC1’ has been replaced by ‘PC1 loading’
- Paleo Interpretation metadata:
- <2 µm (WEB-1a4b1-7ce3-4e10-9927-ce204): interpretation1_scope:
‘climate’ has been replaced by NULL
- Si peak area (WEB-1d341-d989-4093-bfa4-58e46):
interpretation1_scope: ‘climate’ has been replaced by NULL
- Fe peak area (WEB-2447e-a89e-42fd-92e5-8a2e5):
interpretation1_scope: ‘climate’ has been replaced by NULL
- Sand (WEB-36161-63b4-4a14-b08e-89235): interpretation1_scope:
‘climate’ has been replaced by NULL
- Grain size mean (WEB-440ea-0750-4721-b01c-ea1bd):
interpretation1_scope: ‘climate’ has been replaced by NULL
- K peak area (WEB-5111e-2b32-4823-9828-0593f): interpretation1_scope:
‘climate’ has been replaced by NULL
- TN (WEB-6ab51-dfe9-46cf-9c83-a2625): interpretation1_scope:
‘climate’ has been replaced by NULL
- TIC (WEB-6b7fb-2366-40af-94e7-7986e): interpretation1_scope:
‘climate’ has been replaced by NULL
- PC1 loading (WEB-747c6-735e-4b08-a565-465fb):
interpretation1_seasonality: ‘1,2,3,4,5,6,7,8,9,10,11,12’ has been
replaced by ‘Annual’
- PC1 loading (WEB-747c6-735e-4b08-a565-465fb):
interpretation1_seasonalityGeneral: ‘Annual’ has been replaced by
NULL
- PC1 loading (WEB-747c6-735e-4b08-a565-465fb):
interpretation1_variableDetail: ‘@surface’
has been replaced by ‘shoreline@surface’
- TOC/TN (WEB-91189-4901-4dd9-8908-5a9c9): interpretation1_scope:
‘climate’ has been replaced by NULL
- Ba peak area (WEB-918cc-0dbc-4269-94d8-d6f4d):
interpretation1_scope: ‘climate’ has been replaced by NULL
- Sedim rate (WEB-91b4c-dcba-4928-a3f1-3c8e5): interpretation1_scope:
‘climate’ has been replaced by NULL
- Mean Sedim rate (WEB-989d3-c8d2-4972-8922-d0285):
interpretation1_scope: ‘climate’ has been replaced by NULL
- Ti peak area (WEB-a0a8c-89d4-4883-ba22-c77d0):
interpretation1_scope: ‘climate’ has been replaced by NULL
- Rb peak area (WEB-aefd4-7d29-4318-a5e0-d0d86):
interpretation1_scope: ‘climate’ has been replaced by NULL
- Silt (WEB-b5ec1-d06b-488c-805c-d065b): interpretation1_scope:
‘climate’ has been replaced by NULL
- TS (WEB-ba688-529f-42a6-898a-d3048): interpretation1_scope:
‘climate’ has been replaced by NULL
- Ca peak area (WEB-c116b-dc14-4936-87dc-ee868):
interpretation1_scope: ‘climate’ has been replaced by NULL
- Sr peak area (WEB-c217c-4ad7-45b8-b19f-af038):
interpretation1_scope: ‘climate’ has been replaced by NULL
- Al peak area (WEB-dd04a-340e-4371-bcd9-24c63):
interpretation1_scope: ‘climate’ has been replaced by NULL
Version: 1.0.0
- curator: Cody
- timestamp: 2023-01-26 22:34:37 UTC
- notes: Starting the change log with import for Monsoon
21k