NA; paleoData_isPrimary has been standardized
NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
"The progressive increase of detrital input suggested by the Ti record, "
a closed basin system where kinetic frac-tionation due to evaporation is the most likely process for d18O enrichment We conclude that high (low) values of d18O reflect an increase (decrease) in the evaporation to precipitation ratio. We inferred that the variations in the Ca/Ti ratio react with authigenic precipitation of carbonates due to evaporative concentration.
originalDataUrl: 'https://www.ncdc.noaa.gov/paleo/study/29972' has been replaced by 'https://doi.org/10.25921/1ygr-v059'
Ca/Ti (WEB2b6a96dc): paleoData_proxyGeneral: '((( Element ))) element /// elemental' has been replaced by 'elemental'
Ti (WEBcdfe38ba): paleoData_proxyGeneral: '((( Element ))) element /// elemental' has been replaced by 'elemental'
Ti (WEBcdfe38ba): paleoData_units: '((( counts ))) count /// ln(cps)' has been replaced by 'ln(cps)'
originalDataUrl: 'https://www.ncei.noaa.gov/access/paleo-search/study/29972' has been replaced by 'https://www.ncdc.noaa.gov/paleo/study/29972'
Ca/Ti (WEB2b6a96dc): paleoData_proxyGeneral: 'elemental' has been replaced by '((( Element ))) element /// elemental'
Ti (WEBcdfe38ba): paleoData_proxyGeneral: 'elemental' has been replaced by '((( Element ))) element /// elemental'
Ti (WEBcdfe38ba): paleoData_units: 'ln(cps)' has been replaced by '((( counts ))) count /// ln(cps)'
Updated lipdverse database entry with a changed file.
Ca/Ti (WEB2b6a96dc): paleoData_notes: '"We inferred that the variations in the Ca/Ti ratio react with authigenic precipitation of carbonates due to evaporative concentration."' has been replaced by 'a closed basin system where kinetic frac-tionation due to evaporation is the most likely process for d18O enrichment We conclude that high (low) values of d18O reflect an increase (decrease) in the evaporation to precipitation ratio. We inferred that the variations in the Ca/Ti ratio react with authigenic precipitation of carbonates due to evaporative concentration.'
Ca/Ti (WEB2b6a96dc): paleoData_proxy: 'Ti/Ca' has been replaced by 'Ca/Ti'
Ca/Ti (WEB2b6a96dc): paleoData_QCCertification: 'CR' has been replaced by ''
Ca/Ti (WEB2b6a96dc): paleoData_QCnotes: 'CR: Age model constrained by 7 radiocarbon dates. Converted to natural log to match how the data are interpreted in Fig 6 of paper' has been replaced by ''
Ca/Ti (WEB2b6a96dc): paleoData_units: 'ratio' has been replaced by 'ln(ratio)'
Ti (WEBcdfe38ba): paleoData_QCCertification: 'CR' has been replaced by ''
Ti (WEBcdfe38ba): paleoData_QCnotes: 'CR: Age model constrained by 7 radiocarbon dates. Converted to natural log to match how the data are interpreted in Fig 6 of paper' has been replaced by ''
Ti (WEBcdfe38ba): paleoData_units: 'count' has been replaced by 'ln(cps)'
Ca/Ti (WEB2b6a96dc): interpretation1_variableDetail: '@surface' has been replaced by 'lake@surface'
Ca/Ti (WEB2b6a96dc): The size of the paleoData_values have changed, from 23083 to 23083 entries.
Ti (WEBcdfe38ba): The size of the paleoData_values have changed, from 23083 to 23083 entries.
age14C (WEB243e335c): chronData_units: 'yr BP' has been replaced by 'yr 14C BP'
uncertainty1s (WEB3d89b86a): chronData_proxyObservationType: 'error' has been replaced by 'uncertainty1s'
uncertainty1s (WEB3d89b86a): chronData_units: 'yr' has been replaced by 'year'
uncertainty1s (WEB3d89b86a): chronData_variableName: 'error' has been replaced by 'uncertainty1s'
Ti/Ca (WEB2b6a96dc): paleoData_proxyGeneral: 'Element' has been replaced by 'elemental'
Ti (WEBcdfe38ba): paleoData_proxyGeneral: 'Element' has been replaced by 'elemental'
Ti/Ca (WEB2b6a96dc): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'
geo_elevation: '' has been replaced by '1720'
Ti/Ca (WEB2b6a96dc): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
Ti (WEBcdfe38ba): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
Ti (WEBcdfe38ba): interpretation1_variable: 'P' has been replaced by 'precipitation'
depth (WEB9df8e731): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
depth (WEB9df8e731): paleoData_isPrimary: '' has been replaced by 'TRUE'
age (WEBa3c9945f): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (WEBa3c9945f): paleoData_datum: '' has been replaced by '1950'
age (WEBa3c9945f): paleoData_isPrimary: '' has been replaced by 'TRUE'
Ti (WEBcdfe38ba): paleoData_units: 'counts' has been replaced by 'count'
originalDataUrl: '' has been replaced by 'https://www.ncei.noaa.gov/access/paleo-search/study/29972'
pub1_author: 'list(list(name = "Wogau, Kurt H."), list(name = "Arz, Helge W"), list(name = "Böhnel, Harald N."), list(name = "Nowaczyk, Norbert R."), list(name = "Park, Jungjae"))' has been replaced by 'Wogau, Kurt H.'
geo_elevation: '1720' has been replaced by ''
geo_gcmdLocation: '' has been replaced by 'North America>Mexico'
Ti/Ca (WEB2b6a96dc): paleoData_proxy: '' has been replaced by 'Ti/Ca'
Ti/Ca (WEB2b6a96dc): paleoData_variableName: 'Ca/Ti' has been replaced by 'Ti/Ca'
Ti/Ca (WEB2b6a96dc): paleoData_notes: '' has been replaced by 'a closed basin system where kinetic frac-tionation due to evaporation is the most likely process for d18O enrichment We conclude that high (low) values of d18O reflect an increase (decrease) in the evaporation to precipitation ratio. We inferred that the variations in the Ca/Ti ratio react with authigenic precipitation of carbonates due to evaporative concentration.'
Ti/Ca (WEB2b6a96dc): paleoData_proxyGeneral: '' has been replaced by 'Element'
Ti (WEBcdfe38ba): paleoData_proxy: '' has been replaced by 'Ti'
Ti (WEBcdfe38ba): paleoData_notes: '' has been replaced by '"The progressive increase of detrital input suggested by the Ti record, "'
Ti (WEBcdfe38ba): paleoData_proxyGeneral: '' has been replaced by 'Element'
Ti/Ca (WEB2b6a96dc): interpretation1_seasonality: 'annual' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,12'
Ti/Ca (WEB2b6a96dc): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
Mn/Fe (WEBb81ba4a4): interpretation1_scope: '' has been replaced by 'climate'
Ti (WEBcdfe38ba): interpretation1_seasonality: 'annual' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,12'
Ti (WEBcdfe38ba): interpretation1_variableDetail: 'runoff' has been replaced by 'runoff@surface'
Ti (WEBcdfe38ba): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
originalDataUrl: 'https://www.ncei.noaa.gov/access/paleo-search/study/29972' has been replaced by ''
pub1_author: 'Wogau, Kurt H.' has been replaced by 'list(list(name = "Wogau, Kurt H."), list(name = "Arz, Helge W"), list(name = "Böhnel, Harald N."), list(name = "Nowaczyk, Norbert R."), list(name = "Park, Jungjae"))'
geo_gcmdLocation: 'North America>Mexico' has been replaced by ''
Ca/Ti (WEB2b6a96dc): paleoData_notes: 'a closed basin system where kinetic frac-tionation due to evaporation is the most likely process for d18O enrichment We conclude that high (low) values of d18O reflect an increase (decrease) in the evaporation to precipitation ratio. We inferred that the variations in the Ca/Ti ratio react with authigenic precipitation of carbonates due to evaporative concentration.' has been replaced by ''
Ca/Ti (WEB2b6a96dc): paleoData_proxy: 'Ti/Ca' has been replaced by ''
Ca/Ti (WEB2b6a96dc): paleoData_proxyGeneral: 'Element' has been replaced by ''
Ca/Ti (WEB2b6a96dc): paleoData_variableName: 'Ti/Ca' has been replaced by 'Ca/Ti'
Ti (WEBcdfe38ba): paleoData_notes: '"The progressive increase of detrital input suggested by the Ti record, "' has been replaced by ''
Ti (WEBcdfe38ba): paleoData_proxy: 'Ti' has been replaced by ''
Ti (WEBcdfe38ba): paleoData_proxyGeneral: 'Element' has been replaced by ''
Ca/Ti (WEB2b6a96dc): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'annual'
Ca/Ti (WEB2b6a96dc): interpretation1_seasonalityGeneral: 'Annual' has been replaced by ''
Mn/Fe (WEBb81ba4a4): interpretation1_scope: 'climate' has been replaced by ''
Ti (WEBcdfe38ba): interpretation1_seasonalityGeneral: 'Annual' has been replaced by ''
Ti (WEBcdfe38ba): interpretation1_variableDetail: 'runoff@surface' has been replaced by 'runoff'
Starting the change log with import for Monsoon 21k
High resolution paleoclimate and paleoenvironmental reconstruction in the Northern Mesoamerican Frontier for Prehistory to Historical times
Sedimentos de lago como registros paleoambientales