NA; paleoData_isPrimary has been standardized
NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
"The diatom evidence pre-sented below supports the argument that since the middle Holocene the lake has been relatively fresh and overflowing, thus near its present volume. The sta-ble isotopic evidence itself, specifically the low rate of d18O change (on order of 0.02‰ a–1), argues that the assumption of isotopic steady-state is also valid for our application."; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized
"cene). The diatom evidence pre-sented below supports the argument that since the middle Holocene the lake has been relatively fresh and overflowing, thus near its present volume. The sta-ble isotopic evidence itself, specifically the low rate of δ18O change (on order of 0.02‰ a–1), argues that the assumption of isotopic steady-state is also valid for our application."
NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized
"The diatom evidence pre-sented below supports the argument that since the middle Holocene the lake has been relatively fresh and overflowing, thus near its present volume. The sta-ble isotopic evidence itself, specifically the low rate of d18O change (on order of 0.02‰ a–1), argues that the assumption of isotopic steady-state is also valid for our application."
NA; paleoData_measurementMaterial has been standardized; paleoData_isPrimary has been standardized
originalDataUrl: 'https://www.ncei.noaa.gov/access/paleo-search/study/19160' has been replaced by 'https://doi.org/10.25921/nfts-ma14'
precipitation (WEB3a01bea5): interpretation1_variableDetail: 'precipitation@surface' has been replaced by 'amount@surface'
precipitation (WEB3a01bea5): paleoData_notes: '"The diatom evidence pre-sented below supports the argument that since the middle Holocene the lake has been relatively fresh and overflowing, thus near its present volume. The sta-ble isotopic evidence itself, specifically the low rate of δ18O change (on order of 0.02‰ a–1), argues that the assumption of isotopic steady-state is also valid for our application."' has been replaced by '"The diatom evidence pre-sented below supports the argument that since the middle Holocene the lake has been relatively fresh and overflowing, thus near its present volume. The sta-ble isotopic evidence itself, specifically the low rate of d18O change (on order of 0.02‰ a–1), argues that the assumption of isotopic steady-state is also valid for our application."'
precipitation (WEB3a01bea5): paleoData_QCCertification: '' has been replaced by 'CR'
d18O (WEBc42caceb): paleoData_notes: '"The diatom evidence pre-sented below supports the argument that since the middle Holocene the lake has been relatively fresh and overflowing, thus near its present volume. The sta-ble isotopic evidence itself, specifically the low rate of δ18O change (on order of 0.02‰ a–1), argues that the assumption of isotopic steady-state is also valid for our application."; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized' has been replaced by '"The diatom evidence pre-sented below supports the argument that since the middle Holocene the lake has been relatively fresh and overflowing, thus near its present volume. The sta-ble isotopic evidence itself, specifically the low rate of d18O change (on order of 0.02‰ a–1), argues that the assumption of isotopic steady-state is also valid for our application."; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized'
precipitation (WEB3a01bea5): paleoData_proxyGeneral: 'isotope' has been replaced by 'isotopic'
d18O (WEBc42caceb): paleoData_proxyGeneral: 'isotope' has been replaced by 'isotopic'
Updated lipdverse database entry with a changed file.
geo_elevation: '' has been replaced by '3880'
diatom (WEB1eb267a1): paleoData_notes: '' has been replaced by 'NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized'
diatom (WEB1eb267a1): paleoData_variableName: '%plank.dia' has been replaced by 'diatom'
diatom (WEB1eb267a1): paleoData_measurementMaterial: '' has been replaced by 'planktic diatom'
diatom (WEB1eb267a1): paleoData_summaryStatistic: '' has been replaced by 'percent'
age (WEB33d055e7): paleoData_datum: '' has been replaced by '1950'
age (WEB33d055e7): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (WEB33d055e7): paleoData_units: 'BP' has been replaced by 'yr BP'
age (WEB33d055e7): paleoData_isPrimary: '' has been replaced by 'TRUE'
depth (WEB38c9c2c2): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_isPrimary has been standardized'
depth (WEB38c9c2c2): paleoData_variableName: 'drive-depth' has been replaced by 'depth'
depth (WEB38c9c2c2): paleoData_isPrimary: '' has been replaced by 'FALSE'
depth (WEB38c9c2c2): paleoData_measurementMaterial: '' has been replaced by 'drive depth'
precipitation (WEB3a01bea5): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
depth (WEB4e384381): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
depth (WEB4e384381): paleoData_isPrimary: '' has been replaced by 'TRUE'
diatom (WEBa536a1ad): paleoData_notes: '' has been replaced by 'NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized'
diatom (WEBa536a1ad): paleoData_variableName: '%saline.dia' has been replaced by 'diatom'
diatom (WEBa536a1ad): paleoData_measurementMaterial: '' has been replaced by 'saline diatom'
diatom (WEBa536a1ad): paleoData_summaryStatistic: '' has been replaced by 'percent'
d18O (WEBc42caceb): paleoData_datum: '' has been replaced by 'PDB'
d18O (WEBc42caceb): paleoData_notes: '"The diatom evidence pre-sented below supports the argument that since the middle Holocene the lake has been relatively fresh and overflowing, thus near its present volume. The sta-ble isotopic evidence itself, specifically the low rate of δ18O change (on order of 0.02‰ a–1), argues that the assumption of isotopic steady-state is also valid for our application."' has been replaced by '"The diatom evidence pre-sented below supports the argument that since the middle Holocene the lake has been relatively fresh and overflowing, thus near its present volume. The sta-ble isotopic evidence itself, specifically the low rate of δ18O change (on order of 0.02‰ a–1), argues that the assumption of isotopic steady-state is also valid for our application."; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized'
d18O (WEBc42caceb): paleoData_units: 'permil (PBD)' has been replaced by 'permil'
d18O (WEBc42caceb): paleoData_variableName: 'd18Ocarb' has been replaced by 'd18O'
d18O (WEBc42caceb): paleoData_measurementMaterial: '' has been replaced by 'carbonate'
diatom (WEBe91ec12d): paleoData_notes: '' has been replaced by 'NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized'
diatom (WEBe91ec12d): paleoData_variableName: '%benth.dia' has been replaced by 'diatom'
diatom (WEBe91ec12d): paleoData_measurementMaterial: '' has been replaced by 'benthic diatom'
diatom (WEBe91ec12d): paleoData_summaryStatistic: '' has been replaced by 'percent'
precipitation (WEB3a01bea5): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
precipitation (WEB3a01bea5): interpretation1_variable: 'P' has been replaced by 'precipitation'
d18O (WEBc42caceb): interpretation1_seasonality: 'annual' has been replaced by 'Annual'
d18O (WEBc42caceb): interpretation1_variable: 'P' has been replaced by 'precipitation'
geo_elevation: '3880' has been replaced by ''
originalDataUrl: '' has been replaced by 'https://www.ncei.noaa.gov/access/paleo-search/study/19160'
%plank.dia (WEB1eb267a1): interpretation1_scope: '' has been replaced by 'climate'
drive-depth (WEB38c9c2c2): interpretation1_scope: '' has been replaced by 'climate'
%saline.dia (WEBa536a1ad): interpretation1_scope: '' has been replaced by 'climate'
%benth.dia (WEBe91ec12d): interpretation1_scope: '' has been replaced by 'climate'
%plank.dia (WEB1eb267a1): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
%plank.dia (WEB1eb267a1): paleoData_units: '%' has been replaced by 'percent'
%plank.dia (WEB1eb267a1): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
%plank.dia (WEB1eb267a1): paleoData_unitsOriginal: '' has been replaced by '%'
age (WEB33d055e7): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
age (WEB33d055e7): paleoData_units: 'yr BP' has been replaced by 'BP'
age (WEB33d055e7): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
age (WEB33d055e7): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
drive-depth (WEB38c9c2c2): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
drive-depth (WEB38c9c2c2): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
precipitation (WEB3a01bea5): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
precipitation (WEB3a01bea5): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
precipitation (WEB3a01bea5): paleoData_proxyLumps: '' has been replaced by 'isotope'
precipitation (WEB3a01bea5): paleoData_proxyLumpsOriginal: '' has been replaced by 'd18O'
depth (WEB4e384381): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
depth (WEB4e384381): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
%saline.dia (WEBa536a1ad): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
%saline.dia (WEBa536a1ad): paleoData_units: '%' has been replaced by 'percent'
%saline.dia (WEBa536a1ad): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
%saline.dia (WEBa536a1ad): paleoData_unitsOriginal: '' has been replaced by '%'
d18Ocarb (WEBc42caceb): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
d18Ocarb (WEBc42caceb): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
d18Ocarb (WEBc42caceb): paleoData_proxyLumps: '' has been replaced by 'isotope'
d18Ocarb (WEBc42caceb): paleoData_proxyLumpsOriginal: '' has been replaced by 'd18O'
%benth.dia (WEBe91ec12d): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
%benth.dia (WEBe91ec12d): paleoData_units: '%' has been replaced by 'percent'
%benth.dia (WEBe91ec12d): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
%benth.dia (WEBe91ec12d): paleoData_unitsOriginal: '' has been replaced by '%'
%plank.dia (WEB1eb267a1): interpretation1_scope: 'climate' has been replaced by ''
drive-depth (WEB38c9c2c2): interpretation1_scope: 'climate' has been replaced by ''
precipitation (WEB3a01bea5): interpretation1_variableGroup: '' has been replaced by 'P'
%saline.dia (WEBa536a1ad): interpretation1_scope: 'climate' has been replaced by ''
d18Ocarb (WEBc42caceb): interpretation1_seasonality: 'Annual' has been replaced by 'annual'
d18Ocarb (WEBc42caceb): interpretation1_seasonalityOriginal: '' has been replaced by 'Annual'
d18Ocarb (WEBc42caceb): interpretation1_variableGroup: '' has been replaced by 'P'
%benth.dia (WEBe91ec12d): interpretation1_scope: 'climate' has been replaced by ''
material (WEB5e003574): chronData_variableName: 'Material' has been replaced by 'material'
material (WEB5e003574): chronData_variableNameOriginal: '' has been replaced by 'Material'
precipitation (WEB3a01bea5): interpretation1_seasonality: 'Annual' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,12'
precipitation (WEB3a01bea5): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
geo_gcmdLocation: '' has been replaced by 'South America>Peru'
precipitation (WEB3a01bea5): paleoData_datum: '' has been replaced by 'abs'
precipitation (WEB3a01bea5): paleoData_notes: '' has been replaced by '"The diatom evidence pre-sented below supports the argument that since the middle Holocene the lake has been relatively fresh and overflowing, thus near its present volume. The sta-ble isotopic evidence itself, specifically the low rate of δ18O change (on order of 0.02‰ a–1), argues that the assumption of isotopic steady-state is also valid for our application."'
precipitation (WEB3a01bea5): paleoData_proxyGeneral: '' has been replaced by 'isotope'
d18Ocarb (WEBc42caceb): paleoData_notes: '' has been replaced by '"The diatom evidence pre-sented below supports the argument that since the middle Holocene the lake has been relatively fresh and overflowing, thus near its present volume. The sta-ble isotopic evidence itself, specifically the low rate of δ18O change (on order of 0.02‰ a–1), argues that the assumption of isotopic steady-state is also valid for our application."'
d18Ocarb (WEBc42caceb): paleoData_proxyGeneral: '' has been replaced by 'isotope'
d18Ocarb (WEBc42caceb): paleoData_QCnotes: '' has been replaced by 'Defer to calibrated reconstruction'
pub1_author: 'list(list(name = "Baker, Paul A."), list(name = "Fritz, Sherilyn C."), list(name = "Burns, Stephen J."), list(name = "Ekdahl, Erik"), list(name = "Rigsby, Catherine A."))' has been replaced by 'Baker, Paul A.'
The Nature and Origin of Decadal to Millennial Scale Climate Variability in the Southern Tropics of South America: The Holocene Record of Lago Umayo, Peru
Past Climate Variability in South America and Surrounding Regions