NA; paleoData_isPrimary has been standardized
NA; paleoData_summaryStatistic has been standardized
"Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane d2H values "; paleoData_summaryStatistic has been standardized
hus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaíba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values
NA; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized; paleoData_proxyGeneral has been standardized
originalDataUrl: '' has been replaced by 'https://doi.org/10.1594/PANGAEA.921255'
pub1_doi: '' has been replaced by '10.1029/2020PA003936'
Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_notes: '((( ((( "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane ��2H values "; paleoData_variableName updated; paleoData_summaryStatistic has been standardized ))) "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized /// "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized ))) "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane d2H values "; paleoData_summaryStatistic has been standardized /// "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized' has been replaced by '"Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane d2H values "; paleoData_summaryStatistic has been standardized'
Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_notes: '"Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized' has been replaced by '((( ((( "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane ��2H values "; paleoData_variableName updated; paleoData_summaryStatistic has been standardized ))) "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized /// "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized ))) "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane d2H values "; paleoData_summaryStatistic has been standardized /// "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized'
Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_QCCertification: '' has been replaced by 'CR'
Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_notes: '((( "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane ��2H values "; paleoData_variableName updated; paleoData_summaryStatistic has been standardized ))) "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized /// "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized' has been replaced by '"Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized'
Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_proxyGeneral: 'element' has been replaced by 'elemental'
organicCarbon (WEB-1b2bb-d42d-477f-b35d-3d7bc): paleoData_variableName: 'TOC' has been replaced by 'organicCarbon'
Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_notes: '"Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized' has been replaced by '((( "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane ��2H values "; paleoData_variableName updated; paleoData_summaryStatistic has been standardized ))) "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized /// "Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized'
Updated lipdverse database entry with a changed file.
Ti (WEB-15b43-29b6-4954-b979-bd3cc): paleoData_units: 'cts' has been replaced by 'count'
TOC (WEB-1b2bb-d42d-477f-b35d-3d7bc): paleoData_units: '%' has been replaced by 'percent'
depth (WEB-1f85e-f123-4563-bc58-d0e1f): paleoData_variableName: 'Depth' has been replaced by 'depth'
totalNitrogen (WEB-28e52-2862-4f52-9936-3a287): paleoData_units: '%' has been replaced by 'percent'
totalNitrogen (WEB-28e52-2862-4f52-9936-3a287): paleoData_variableName: 'TN' has been replaced by 'totalNitrogen'
Fe (WEB-297de-ae48-41da-99bb-d427e): paleoData_units: 'cts' has been replaced by 'count'
CaCO3 (WEB-64793-2fa7-488c-8153-4a5a8): paleoData_units: '%' has been replaced by 'percent'
Fe/Ca (WEB-84482-33c8-4bfd-843c-ed119): paleoData_notes: '' has been replaced by 'NA; paleoData_summaryStatistic has been standardized'
Fe/Ca (WEB-84482-33c8-4bfd-843c-ed119): paleoData_variableName: 'ln(Fe/Ca)' has been replaced by 'Fe/Ca'
Fe/Ca (WEB-84482-33c8-4bfd-843c-ed119): paleoData_summaryStatistic: '' has been replaced by 'ln'
Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_notes: '"Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "' has been replaced by '"Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "; paleoData_summaryStatistic has been standardized'
Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_variableName: 'ln(Ti/Ca)' has been replaced by 'Ti/Ca'
Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_summaryStatistic: '' has been replaced by 'ln'
d2H (WEB-a2486-c44a-4c63-af96-f33b3): paleoData_notes: '' has been replaced by 'NA; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized; paleoData_proxyGeneral has been standardized'
d2H (WEB-a2486-c44a-4c63-af96-f33b3): paleoData_proxyGeneral: '' has been replaced by 'isotopic'
d2H (WEB-a2486-c44a-4c63-af96-f33b3): paleoData_units: '‰ SMOW' has been replaced by 'permil'
d2H (WEB-a2486-c44a-4c63-af96-f33b3): paleoData_variableName: 'C29 dD' has been replaced by 'd2H'
d2H (WEB-a2486-c44a-4c63-af96-f33b3): paleoData_datum: '' has been replaced by 'SMOW'
d2H (WEB-a2486-c44a-4c63-af96-f33b3): paleoData_measurementMaterial: '' has been replaced by 'C29'
Ca (WEB-cc290-b0d2-4c75-87a0-f2e95): paleoData_units: 'cts' has been replaced by 'count'
age (WEB-e16ae-9cff-449b-bfd3-1c4b8): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
age (WEB-e16ae-9cff-449b-bfd3-1c4b8): paleoData_units: 'cal year BP' has been replaced by 'yr BP'
age (WEB-e16ae-9cff-449b-bfd3-1c4b8): paleoData_isPrimary: '' has been replaced by 'TRUE'
Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): interpretation1_variable: 'P' has been replaced by 'precipitation'
ln(Ti/Ca) (WEB-84c26-cf61-4730-a2fb-5101f): interpretation1_seasonality: 'Annual' has been replaced by '1,2,3,4,5,6,7,8,9,10,11,12'
pub1_doi: '10.1029/2020PA003936' has been replaced by ''
geo_elevation: '-1211' has been replaced by ''
geo_gcmdLocation: '' has been replaced by 'Atlantic Ocean>South Atlantic Ocean'
ln(Ti/Ca) (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_proxy: 'ln(Ti/Ca)' has been replaced by 'Ti/Ca'
ln(Ti/Ca) (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_notes: '' has been replaced by '"Thus, by exclusion, we interpret the general decrease in our ln(Fe/Ca) and ln(Ti/Ca) values (Figures 2e, 2f, and 3c) to represent a decrease in the input of continental siliciclastic material to the western equatorial Atlantic related to a decrease in fluvial input from northern NE Brazil and, more specifically, from the Parnaiba River drainage basin (Figure 1). This interpretation is corroborated by the decrease in MARsil (Figure 2a) and is supported by the C29 long-chain n-alkane δ2H values "'
ln(Ti/Ca) (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_proxyDetail: '' has been replaced by 'ratio'
ln(Ti/Ca) (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_proxyGeneral: '' has been replaced by 'element'
ln(Ti/Ca) (WEB-84c26-cf61-4730-a2fb-5101f): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
pub1_author: 'list(list(name = "C. M. Chiessi"), list(name = "S. Mulitza"), list(name = "N. K. Taniguchi"), list(name = ""), list(name = "M. Prange"), list(name = "M. C. Campos"), list(name = "C. Häggi"), list(name = "E. Schefuß"), list(name = "T. M. L. Pinho"), list(name = "T. Frederichs"), list(name = "R. C. Portilho-Ramos"), list(name = "S. H. M. Sousa"), list(name = "S. Crivellari"), list(name = ". W. Cruz"))' has been replaced by 'C. M. Chiessi'
Ti (WEB-15b43-29b6-4954-b979-bd3cc): interpretation1_scope: '' has been replaced by 'climate'
TOC (WEB-1b2bb-d42d-477f-b35d-3d7bc): interpretation1_scope: '' has been replaced by 'climate'
TN (WEB-28e52-2862-4f52-9936-3a287): interpretation1_scope: '' has been replaced by 'climate'
Fe (WEB-297de-ae48-41da-99bb-d427e): interpretation1_scope: '' has been replaced by 'climate'
CaCO3 (WEB-64793-2fa7-488c-8153-4a5a8): interpretation1_scope: '' has been replaced by 'climate'
ln(Fe/Ca) (WEB-84482-33c8-4bfd-843c-ed119): interpretation1_scope: '' has been replaced by 'climate'
C29 dD (WEB-a2486-c44a-4c63-af96-f33b3): interpretation1_scope: '' has been replaced by 'climate'
Ca (WEB-cc290-b0d2-4c75-87a0-f2e95): interpretation1_scope: '' has been replaced by 'climate'
Mid- to Late Holocene Contraction of the Intertropical Convergence Zone Over Northeastern South America