NA; paleoData_isPrimary has been standardized
NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
NA; paleoData_measurementMaterial has been standardized
NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized
NA; paleoData_method has been standardized
""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as dDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized
"We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "
originalDataUrl: 'https://www.ncei.noaa.gov/access/paleo-search/study/16399' has been replaced by 'https://doi.org/10.25921/nqe4-rv55'
PC1 (WEB88f459b8): paleoData_proxy: '((( PCA ))) deleteMe /// multiproxy' has been replaced by 'multiproxy'
PC1 (WEB88f459b8): paleoData_proxy: 'multiproxy' has been replaced by '((( PCA ))) deleteMe /// multiproxy'
PC1 (WEB88f459b8): interpretation1_variableDetail: 'lakelevel@surface' has been replaced by 'LakeLevel@surface'
PC1 (WEB88f459b8): paleoData_notes: '((( ((( ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as ��Dwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized; paleoData_proxy updated ))) ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized /// ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized ))) ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as dDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized /// ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized' has been replaced by '""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as dDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized'
PC1 (WEB88f459b8): paleoData_notes: '""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized' has been replaced by '((( ((( ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as ��Dwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized; paleoData_proxy updated ))) ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized /// ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized ))) ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as dDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized /// ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized'
PC1 (WEB88f459b8): paleoData_QCCertification: '' has been replaced by 'CR'
PC1 (WEB88f459b8): paleoData_notes: '((( ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as ��Dwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized; paleoData_proxy updated ))) ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized /// ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized' has been replaced by '""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized'
PC1 (WEB88f459b8): paleoData_proxyGeneral: 'hybrid' has been replaced by 'multiproxy'
PC1 (WEB88f459b8): paleoData_proxy: '' has been replaced by 'multiproxy'
PC1 (WEB88f459b8): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'
PC1 (WEB88f459b8): paleoData_notes: '""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized' has been replaced by '((( ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as ��Dwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized; paleoData_proxy updated ))) ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized /// ""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized'
Updated lipdverse database entry with a changed file.
geo_elevation: '' has been replaced by '4845'
lithics (WEB1e2bd571): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized'
lithics (WEB1e2bd571): paleoData_variableName: 'Lithics' has been replaced by 'lithics'
lithics (WEB1e2bd571): paleoData_measurementMaterial: '' has been replaced by 'lithics'
lithics (WEB39ef1ed2): paleoData_notes: '' has been replaced by 'NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized'
lithics (WEB39ef1ed2): paleoData_units: 'g/cm^2/y' has been replaced by 'g/cm2/yr'
lithics (WEB39ef1ed2): paleoData_variableName: 'Lithic Flux' has been replaced by 'lithics'
lithics (WEB39ef1ed2): paleoData_measurementMaterial: '' has been replaced by 'lithics'
lithics (WEB39ef1ed2): paleoData_summaryStatistic: '' has been replaced by 'flux'
BSi (WEB5b6c141d): paleoData_notes: '' has been replaced by 'NA; paleoData_method has been standardized'
BSi (WEB5b6c141d): paleoData_variableName: 'Inferred BSi' has been replaced by 'BSi'
BSi (WEB5b6c141d): paleoData_method: '' has been replaced by 'inferred'
PC1 (WEB88f459b8): paleoData_notes: '""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "' has been replaced by '""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "; paleoData_method has been standardized'
PC1 (WEB88f459b8): paleoData_proxy: 'PCA' has been replaced by ''
PC1 (WEB88f459b8): paleoData_method: '' has been replaced by 'principal components'
dryBulkDensity (WEB99c4425f): paleoData_units: 'g/cc' has been replaced by 'g/cm3'
dryBulkDensity (WEB99c4425f): paleoData_variableName: 'Dry Bulk Density' has been replaced by 'dryBulkDensity'
age (WEBe9bf2e19): paleoData_datum: '' has been replaced by '1950'
age (WEBe9bf2e19): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (WEBe9bf2e19): paleoData_units: 'BP' has been replaced by 'yr BP'
age (WEBe9bf2e19): paleoData_isPrimary: '' has been replaced by 'TRUE'
depth (WEBf197c5b3): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
depth (WEBf197c5b3): paleoData_isPrimary: '' has been replaced by 'TRUE'
organicMatter (WEBf6f06516): paleoData_variableName: 'OM' has been replaced by 'organicMatter'
PC1 (WEB88f459b8): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
geo_elevation: '4845' has been replaced by ''
originalDataUrl: '' has been replaced by 'https://www.ncei.noaa.gov/access/paleo-search/study/16399'
Lithics (WEB1e2bd571): interpretation1_scope: '' has been replaced by 'climate'
Lithic Flux (WEB39ef1ed2): interpretation1_scope: '' has been replaced by 'climate'
Inferred BSi (WEB5b6c141d): interpretation1_scope: '' has been replaced by 'climate'
Dry Bulk Density (WEB99c4425f): interpretation1_scope: '' has been replaced by 'climate'
PC2 (WEBf1800d04): interpretation1_scope: '' has been replaced by 'climate'
OM (WEBf6f06516): interpretation1_scope: '' has been replaced by 'climate'
archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
Lithics (WEB1e2bd571): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
Lithics (WEB1e2bd571): paleoData_units: '%' has been replaced by 'percent'
Lithics (WEB1e2bd571): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
Lithics (WEB1e2bd571): paleoData_unitsOriginal: '' has been replaced by '%'
Lithic Flux (WEB39ef1ed2): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
Lithic Flux (WEB39ef1ed2): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
Inferred BSi (WEB5b6c141d): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
Inferred BSi (WEB5b6c141d): paleoData_units: '%' has been replaced by 'percent'
Inferred BSi (WEB5b6c141d): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
Inferred BSi (WEB5b6c141d): paleoData_unitsOriginal: '' has been replaced by '%'
PC1 (WEB88f459b8): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
PC1 (WEB88f459b8): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
PC1 (WEB88f459b8): paleoData_proxyLumps: '' has been replaced by 'PCA'
Dry Bulk Density (WEB99c4425f): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
Dry Bulk Density (WEB99c4425f): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
age (WEBe9bf2e19): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
age (WEBe9bf2e19): paleoData_units: 'yr BP' has been replaced by 'BP'
age (WEBe9bf2e19): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
age (WEBe9bf2e19): paleoData_unitsOriginal: '' has been replaced by 'yr BP'
PC2 (WEBf1800d04): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
PC2 (WEBf1800d04): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
depth (WEBf197c5b3): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
depth (WEBf197c5b3): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
OM (WEBf6f06516): paleoData_archiveType: 'Lake Sediment' has been replaced by 'LakeSediment'
OM (WEBf6f06516): paleoData_units: '%' has been replaced by 'percent'
OM (WEBf6f06516): paleoData_archiveTypeOriginal: '' has been replaced by 'Lake Sediment'
OM (WEBf6f06516): paleoData_unitsOriginal: '' has been replaced by '%'
Lithics (WEB1e2bd571): interpretation1_scope: 'climate' has been replaced by ''
Lithic Flux (WEB39ef1ed2): interpretation1_scope: 'climate' has been replaced by ''
Inferred BSi (WEB5b6c141d): interpretation1_scope: 'climate' has been replaced by ''
PC1 (WEB88f459b8): interpretation1_variableGroup: '' has been replaced by 'P-E'
Dry Bulk Density (WEB99c4425f): interpretation1_scope: 'climate' has been replaced by ''
PC2 (WEBf1800d04): interpretation1_scope: 'climate' has been replaced by ''
OM (WEBf6f06516): interpretation1_scope: 'climate' has been replaced by ''
material (WEB8bfdbc85): chronData_variableName: 'Material' has been replaced by 'material'
material (WEB8bfdbc85): chronData_variableNameOriginal: '' has been replaced by 'Material'
PC1 (WEB88f459b8): interpretation1_seasonality: 'Annual' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,12'
PC1 (WEB88f459b8): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
geo_gcmdLocation: '' has been replaced by 'Asia>Eastern Asia>China'
PC1 (WEB88f459b8): paleoData_proxy: 'sediment' has been replaced by 'PCA'
PC1 (WEB88f459b8): paleoData_datum: '' has been replaced by 'anom'
PC1 (WEB88f459b8): paleoData_notes: '' has been replaced by '""We suggest that PC1 reflects oscillations between two end member depositional environments with fines indicative of deep lake conditions and coarser material reflective of shallower lake conditions (i.e., littoral zone sediments)...onsistent with the grain-size lake-level model, very fine to fine sand abundances increased during the middle Holocene as δDwax increased and PC1 and lithic flux decreased, suggesting diminished ISM rainfall reduced clastic (i.e., silt) deposition and lowered lake level "'
PC1 (WEB88f459b8): paleoData_proxyDetail: '' has been replaced by 'PCA'
PC1 (WEB88f459b8): paleoData_proxyGeneral: '' has been replaced by 'hybrid'
pub1_author: 'list(list(name = "Bird, Broxton W."), list(name = "Polisar, Pratigya J."), list(name = "Lei, Yanbin"), list(name = "Thompson, Lonnie G."), list(name = "Yao, Tandong"), list(name = "Finney, Bruce P."), list(name = "Bain, Daniel J."), list(name = "Pompeani, David P."), list(name = "Steinman, Byron A."))' has been replaced by 'Bird, Broxton W.'
A Tibetan lake sediment record of Holocene Indian summer monsoon variability