NA; paleoData_isPrimary has been standardized
NA; paleoData_method has been standardized
NA; paleoData_summaryStatistic has been standardized; 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."
NA; paleoData_datum has been standardized
NA; paleoData_summaryStatistic has been standardized
pub1_journal: 'Journal of Quaternary Science' has been replaced by 'Quaternary Science Reviews'
pub1_pages: '70–78' has been replaced by '73--85'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since the Last Glacial Maximum and their teleconnection to inter-regional and hemispheric climate variations' has been replaced by 'Indian Ocean Summer Monsoon ({IOSM})-dynamics within the past 4~ka recorded in the sediments of Lake Nam Co, central Tibetan Plateau (China)'
pub1_year: '2015' has been replaced by '2012'
pub1_author: '' has been replaced by 'Thomas Kasper and Torsten Haberzettl and Stefan Dobersch√ºtz and Gerhard Daut and Junbo Wang and Liping Zhu and Norbert Nowaczyk and Roland M√§usbacher'
PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxy: '((( PCA ))) deleteMe /// multiproxy' has been replaced by 'multiproxy'
Ca (WEB-c116b-dc14-4936-87dc-ee868): paleoData_variableName: '((( Ca peak area ))) Ca /// Ca' has been replaced by 'Ca'
pub1_doi: '' has been replaced by '10.1016/j.quascirev.2012.02.011'
PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxy: 'multiproxy' has been replaced by '((( PCA ))) deleteMe /// multiproxy'
((( Ca peak area ))) Ca /// Ca (WEB-c116b-dc14-4936-87dc-ee868): paleoData_variableName: 'Ca' has been replaced by '((( Ca peak area ))) Ca /// Ca'
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'
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'
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'
PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxy: '' has been replaced by 'multiproxy'
PC1 (WEB-747c6-735e-4b08-a565-465fb): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'
organicCarbon (WEB-fa835-5619-44ed-b38c-5d029): paleoData_variableName: 'TOC' has been replaced by 'organicCarbon'
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'
Updated lipdverse database entry with a changed file.
geo_elevation: '' has been replaced by '4718'
grainSize (WEB-1a4b1-7ce3-4e10-9927-ce204): paleoData_notes: '' 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: '' has been replaced by '<2 um'
Si (WEB-1d341-d989-4093-bfa4-58e46): paleoData_notes: '' 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: '' has been replaced by 'peak area'
Fe (WEB-2447e-a89e-42fd-92e5-8a2e5): paleoData_notes: '' 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: '' has been replaced by 'peak area'
Fe (WEB-2447e-a89e-42fd-92e5-8a2e5): paleoData_summaryStatistic: '' 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: '' 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: '' has been replaced by 'mean'
potassium (WEB-5111e-2b32-4823-9828-0593f): paleoData_notes: '' 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: '' 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: '' 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: '' 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 ''
PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_method: '' 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: '' 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: '' 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: '' 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: '' 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: '' 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: '' has been replaced by 'peak area'
Sr (WEB-c217c-4ad7-45b8-b19f-af038): paleoData_notes: '' 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: '' 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: '' 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: '' has been replaced by 'peak area'
age (WEB-f89e6-6a01-4391-adcc-b1e5f): paleoData_notes: '' 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: '' has been replaced by 'TRUE'
TOC (WEB-fa835-5619-44ed-b38c-5d029): paleoData_units: '%' has been replaced by 'percent'
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'
originalDataUrl: '' has been replaced by 'https://doi.org/10.1594/PANGAEA.779261'
pub1_doi: '10.1002/jqs.2759' has been replaced by ''
geo_elevation: '4718' has been replaced by ''
geo_gcmdLocation: '' has been replaced by 'Asia>Eastern Asia>China'
<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: '' 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: '' has been replaced by 'XRF core scan data (element abundance)'
PC1 (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxyGeneral: '' has been replaced by 'biophysical'
<2 um (WEB-1a4b1-7ce3-4e10-9927-ce204): interpretation1_scope: '' has been replaced by 'climate'
Si peak area (WEB-1d341-d989-4093-bfa4-58e46): interpretation1_scope: '' has been replaced by 'climate'
Fe peak area (WEB-2447e-a89e-42fd-92e5-8a2e5): interpretation1_scope: '' has been replaced by 'climate'
Sand (WEB-36161-63b4-4a14-b08e-89235): interpretation1_scope: '' has been replaced by 'climate'
Grain size mean (WEB-440ea-0750-4721-b01c-ea1bd): interpretation1_scope: '' has been replaced by 'climate'
K peak area (WEB-5111e-2b32-4823-9828-0593f): interpretation1_scope: '' has been replaced by 'climate'
TN (WEB-6ab51-dfe9-46cf-9c83-a2625): interpretation1_scope: '' has been replaced by 'climate'
TIC (WEB-6b7fb-2366-40af-94e7-7986e): interpretation1_scope: '' 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: '' has been replaced by 'Annual'
TOC/TN (WEB-91189-4901-4dd9-8908-5a9c9): interpretation1_scope: '' has been replaced by 'climate'
Ba peak area (WEB-918cc-0dbc-4269-94d8-d6f4d): interpretation1_scope: '' has been replaced by 'climate'
Sedim rate (WEB-91b4c-dcba-4928-a3f1-3c8e5): interpretation1_scope: '' has been replaced by 'climate'
Mean Sedim rate (WEB-989d3-c8d2-4972-8922-d0285): interpretation1_scope: '' has been replaced by 'climate'
Ti peak area (WEB-a0a8c-89d4-4883-ba22-c77d0): interpretation1_scope: '' has been replaced by 'climate'
Rb peak area (WEB-aefd4-7d29-4318-a5e0-d0d86): interpretation1_scope: '' has been replaced by 'climate'
Silt (WEB-b5ec1-d06b-488c-805c-d065b): interpretation1_scope: '' has been replaced by 'climate'
TS (WEB-ba688-529f-42a6-898a-d3048): interpretation1_scope: '' has been replaced by 'climate'
Ca peak area (WEB-c116b-dc14-4936-87dc-ee868): interpretation1_scope: '' has been replaced by 'climate'
Sr peak area (WEB-c217c-4ad7-45b8-b19f-af038): interpretation1_scope: '' has been replaced by 'climate'
Al peak area (WEB-dd04a-340e-4371-bcd9-24c63): interpretation1_scope: '' has been replaced by 'climate'
originalDataUrl: 'https://doi.org/10.1594/PANGAEA.779261' has been replaced by ''
geo_gcmdLocation: 'Asia>Eastern Asia>China' has been replaced by ''
pub1_doi: '' has been replaced by '10.1002/jqs.2759'
<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 ''
PC1 loading (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxyDetail: 'XRF core scan data (element abundance)' has been replaced by ''
PC1 loading (WEB-747c6-735e-4b08-a565-465fb): paleoData_proxyGeneral: 'biophysical' has been replaced by ''
PC1 loading (WEB-747c6-735e-4b08-a565-465fb): paleoData_variableName: 'PC1' has been replaced by 'PC1 loading'
<2 µm (WEB-1a4b1-7ce3-4e10-9927-ce204): interpretation1_scope: 'climate' has been replaced by ''
Si peak area (WEB-1d341-d989-4093-bfa4-58e46): interpretation1_scope: 'climate' has been replaced by ''
Fe peak area (WEB-2447e-a89e-42fd-92e5-8a2e5): interpretation1_scope: 'climate' has been replaced by ''
Sand (WEB-36161-63b4-4a14-b08e-89235): interpretation1_scope: 'climate' has been replaced by ''
Grain size mean (WEB-440ea-0750-4721-b01c-ea1bd): interpretation1_scope: 'climate' has been replaced by ''
K peak area (WEB-5111e-2b32-4823-9828-0593f): interpretation1_scope: 'climate' has been replaced by ''
TN (WEB-6ab51-dfe9-46cf-9c83-a2625): interpretation1_scope: 'climate' has been replaced by ''
TIC (WEB-6b7fb-2366-40af-94e7-7986e): interpretation1_scope: 'climate' has been replaced by ''
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 ''
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 ''
Ba peak area (WEB-918cc-0dbc-4269-94d8-d6f4d): interpretation1_scope: 'climate' has been replaced by ''
Sedim rate (WEB-91b4c-dcba-4928-a3f1-3c8e5): interpretation1_scope: 'climate' has been replaced by ''
Mean Sedim rate (WEB-989d3-c8d2-4972-8922-d0285): interpretation1_scope: 'climate' has been replaced by ''
Ti peak area (WEB-a0a8c-89d4-4883-ba22-c77d0): interpretation1_scope: 'climate' has been replaced by ''
Rb peak area (WEB-aefd4-7d29-4318-a5e0-d0d86): interpretation1_scope: 'climate' has been replaced by ''
Silt (WEB-b5ec1-d06b-488c-805c-d065b): interpretation1_scope: 'climate' has been replaced by ''
TS (WEB-ba688-529f-42a6-898a-d3048): interpretation1_scope: 'climate' has been replaced by ''
Ca peak area (WEB-c116b-dc14-4936-87dc-ee868): interpretation1_scope: 'climate' has been replaced by ''
Sr peak area (WEB-c217c-4ad7-45b8-b19f-af038): interpretation1_scope: 'climate' has been replaced by ''
Al peak area (WEB-dd04a-340e-4371-bcd9-24c63): interpretation1_scope: 'climate' has been replaced by ''
Starting the change log with import for Monsoon 21k
Thomas Kasper and Torsten Haberzettl and Stefan Dobersch√ºtz and Gerhard Daut and Junbo Wang and Liping Zhu and Norbert Nowaczyk and Roland M√§usbacher
Indian Ocean Summer Monsoon ({IOSM})-dynamics within the past 4~ka recorded in the sediments of Lake Nam Co, central Tibetan Plateau (China)