NA; paleoData_isPrimary has been standardized
"The association of sapropels with insolation‐driven monsoon intensifications is indicated by the close corre- lation with titanium‐to‐aluminum ratios (Ti/Al; Figure 2a). In this area, particles relatively high in Ti are mainly of aeolian origin, while Nile‐derived clay is relatively high in Al (Lourens et al., 2001). Hence, Ti/ Al values indicate dry/wet phases in North Africa, with the lower values associated with sapropels pointing to an increased monsoon intensity (Figure 2a; note that the Ti/Al y axis is descending)."
NA; paleoData_proxyGeneral has been standardized
Ba/Al (WEB-9e0dc-916a-4136-80ff-831ed): interpretation1_variable: 'null' has been replaced by 'deleteMe'
Mo (WEB-aa079-7429-4bdf-8921-419d3): interpretation1_variable: 'null' has been replaced by 'deleteMe'
Ba/Al (WEB-9e0dc-916a-4136-80ff-831ed): interpretation1_variable: '((( export-productivity ))) deleteMe /// null' has been replaced by 'null'
Mo (WEB-aa079-7429-4bdf-8921-419d3): interpretation1_variable: '((( anoxia ))) deleteMe /// null' has been replaced by 'null'
pub1_doi: '' has been replaced by '10.1029/2020GL089183'
Ba/Al (WEB-9e0dc-916a-4136-80ff-831ed): interpretation1_variable: '' has been replaced by '((( export-productivity ))) deleteMe /// null'
Mo (WEB-aa079-7429-4bdf-8921-419d3): interpretation1_variable: '' has been replaced by '((( anoxia ))) deleteMe /// null'
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): paleoData_proxyGeneral: 'biophysical' has been replaced by 'elemental'
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): paleoData_QCnotes: 'Pass age control' has been replaced by '*Pass age control'
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): paleoData_QCCertification: '' has been replaced by 'CR'
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): interpretation1_variable: 'P-E' has been replaced by 'effectivePrecipitation'
uranium (WEB-32551-3c2a-4d54-a7b4-48c2d): paleoData_notes: '' has been replaced by 'null'
Updated lipdverse database entry with a changed file.
depth (WEB-06983-b924-47d5-b303-42ceb): paleoData_variableName: 'Depth' has been replaced by 'depth'
uranium (WEB-32551-3c2a-4d54-a7b4-48c2d): paleoData_variableName: 'U' has been replaced by 'uranium'
age (WEB-657aa-0dc0-4c30-bc41-2d492): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
age (WEB-657aa-0dc0-4c30-bc41-2d492): paleoData_units: 'cal year BP' has been replaced by 'yr BP'
age (WEB-657aa-0dc0-4c30-bc41-2d492): paleoData_isPrimary: '' has been replaced by 'TRUE'
Ba/Al (WEB-9e0dc-916a-4136-80ff-831ed): paleoData_notes: '' has been replaced by 'NA; paleoData_proxyGeneral has been standardized'
Ba/Al (WEB-9e0dc-916a-4136-80ff-831ed): paleoData_proxyGeneral: '' has been replaced by 'elemental'
Ba/Al (WEB-9e0dc-916a-4136-80ff-831ed): paleoData_units: '(mg/kg)/(mg/kg)' has been replaced by 'ratio'
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): paleoData_units: '(mg/kg)/(mg/kg)' has been replaced by 'ratio'
uranium (WEB-32551-3c2a-4d54-a7b4-48c2d): interpretation1_variable: 'suboxia' has been replaced by 'dissolvedOxygen'
Ba/Al (WEB-9e0dc-916a-4136-80ff-831ed): interpretation1_variable: 'export-productivity' has been replaced by ''
Mo (WEB-aa079-7429-4bdf-8921-419d3): interpretation1_variable: 'anoxia' has been replaced by ''
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): 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.923197'
pub1_author: 'list(list(name = "Hennekam, Rick"), list(name = "Bolt, Bregje"), list(name = "Nes, Egbert H."), list(name = "Lange, Gert J."), list(name = "Scheffer, Marten"), list(name = "Reichart, Gert‐Jan"))' has been replaced by 'Hennekam, Rick'
pub1_doi: '10.1029/2020GL089183' has been replaced by ''
geo_elevation: '-1022' has been replaced by ''
geo_gcmdLocation: '' has been replaced by 'Atlantic Ocean>North Atlantic Ocean>Mediterranean Sea'
Ti (WEB-2e666-1a7d-45ce-822b-81b23): interpretation1_scope: '' has been replaced by 'climate'
Al (WEB-83bd8-e0df-46e2-94b3-5d222): interpretation1_scope: '' has been replaced by 'climate'
Ba (WEB-dfbba-a976-422d-8a78-e7ca4): interpretation1_scope: '' has been replaced by 'climate'
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): interpretation1_seasonality: 'Annual' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,12'
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): paleoData_notes: '' has been replaced by '"The association of sapropels with insolation‐driven monsoon intensifications is indicated by the close corre- lation with titanium‐to‐aluminum ratios (Ti/Al; Figure 2a). In this area, particles relatively high in Ti are mainly of aeolian origin, while Nile‐derived clay is relatively high in Al (Lourens et al., 2001). Hence, Ti/ Al values indicate dry/wet phases in North Africa, with the lower values associated with sapropels pointing to an increased monsoon intensity (Figure 2a; note that the Ti/Al y axis is descending)."'
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): paleoData_proxyGeneral: '' has been replaced by 'biophysical'
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): paleoData_QCnotes: '' has been replaced by 'Pass age control'
originalDataUrl: 'https://doi.org/10.1594/PANGAEA.923197' has been replaced by ''
pub1_author: 'Hennekam, Rick' has been replaced by 'list(list(name = "Hennekam, Rick"), list(name = "Bolt, Bregje"), list(name = "Nes, Egbert H."), list(name = "Lange, Gert J."), list(name = "Scheffer, Marten"), list(name = "Reichart, Gert‐Jan"))'
geo_elevation: '' has been replaced by '-1022'
geo_gcmdLocation: 'Atlantic Ocean>North Atlantic Ocean>Mediterranean Sea' has been replaced by ''
Ti (WEB-2e666-1a7d-45ce-822b-81b23): interpretation1_scope: 'climate' has been replaced by ''
Al (WEB-83bd8-e0df-46e2-94b3-5d222): interpretation1_scope: 'climate' has been replaced by ''
Ba (WEB-dfbba-a976-422d-8a78-e7ca4): interpretation1_scope: 'climate' has been replaced by ''
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): interpretation1_seasonalityGeneral: 'Annual' has been replaced by ''
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): paleoData_notes: '"The association of sapropels with insolation‐driven monsoon intensifications is indicated by the close corre- lation with titanium‐to‐aluminum ratios (Ti/Al; Figure 2a). In this area, particles relatively high in Ti are mainly of aeolian origin, while Nile‐derived clay is relatively high in Al (Lourens et al., 2001). Hence, Ti/ Al values indicate dry/wet phases in North Africa, with the lower values associated with sapropels pointing to an increased monsoon intensity (Figure 2a; note that the Ti/Al y axis is descending)."' has been replaced by ''
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): paleoData_proxyGeneral: 'biophysical' has been replaced by ''
Ti/Al (WEB-f9320-c765-469f-b4ee-6276b): paleoData_QCnotes: 'Pass age control' has been replaced by ''
Starting the change log with import for Monsoon 21k
Early‐Warning Signals for Marine Anoxic Events
Atlantic Ocean>North Atlantic Ocean>Mediterranean Sea