Version history for P7Z1kYeBvksrJvhw45Qb - GeoB16204-2.Chiessi.2022

Version: 1.0.11

  • lastVersion: 1.0.10
  • curator: nicholas
  • timestamp: 2023-07-05 00:40:05 UTC
  • changes:

Version: 1.0.10

  • lastVersion: 1.0.9
  • curator: nicholas
  • timestamp: 2023-05-31 20:38:30 UTC
  • changes:
    • Paleo Column metadata:
      • 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’

Version: 1.0.9

  • lastVersion: 1.0.8
  • curator: nicholas
  • timestamp: 2023-05-30 15:48:40 UTC
  • changes:
    • Paleo Column metadata:
      • 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: NULL has been replaced by ‘CR’

Version: 1.0.8

  • lastVersion: 1.0.7
  • curator: nicholas
  • timestamp: 2023-05-12 21:54:55 UTC
  • changes:
    • Paleo Column metadata:
      • 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’

Version: 1.0.7

  • lastVersion: 1.0.6
  • curator: nicholas
  • timestamp: 2023-03-24 22:24:21 UTC
  • changes:
    • Paleo Column metadata:
      • Ti/Ca (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_proxyGeneral: ‘element’ has been replaced by ‘elemental’

Version: 1.0.6

  • lastVersion: 1.0.5
  • curator: nicholas
  • timestamp: 2023-02-16 23:24:58 UTC
  • changes:
    • Paleo Column metadata:
      • organicCarbon (WEB-1b2bb-d42d-477f-b35d-3d7bc): paleoData_variableName: ‘TOC’ has been replaced by ‘organicCarbon’

Version: 1.0.5

  • lastVersion: 1.0.4
  • curator: nicholas
  • timestamp: 2023-02-13 23:42:40 UTC
  • changes:
    • Paleo Column metadata:
      • 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’

Version: 1.0.4

  • lastVersion: 1.0.3
  • curator: nicholas
  • timestamp: 2023-02-09 15:42:07 UTC
  • notes: Updated lipdverse database entry with a changed file.
  • changes:
    • Paleo Column metadata:
      • 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: NULL 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: NULL 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: NULL has been replaced by ‘ln’
      • d2H (WEB-a2486-c44a-4c63-af96-f33b3): paleoData_notes: NULL 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: NULL 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: NULL has been replaced by ‘SMOW’
      • d2H (WEB-a2486-c44a-4c63-af96-f33b3): paleoData_measurementMaterial: NULL 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: NULL 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: NULL has been replaced by ‘TRUE’
    • Paleo Interpretation metadata:
      • 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’

Version: 1.0.3

  • lastVersion: 1.0.2
  • curator: nicholas
  • timestamp: 2022-09-09 02:06:13 UTC
  • changes:
    • Paleo Interpretation metadata:
      • 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’

Version: 1.0.2

  • lastVersion: 1.0.1
  • curator: nicholas
  • timestamp: 2022-07-28 17:31:25 UTC
  • changes:
    • Publication metadata:
      • pub1_doi: ‘10.1029/2020PA003936’ has been replaced by NULL
    • Geographic metadata:
      • geo_elevation: ‘-1211’ has been replaced by NULL
      • geo_gcmdLocation: NULL has been replaced by ‘Atlantic Ocean>South Atlantic Ocean’
    • Paleo Column metadata:
      • 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: NULL 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: NULL has been replaced by ‘ratio’
      • ln(Ti/Ca) (WEB-84c26-cf61-4730-a2fb-5101f): paleoData_proxyGeneral: NULL has been replaced by ‘element’
    • Paleo Interpretation metadata:
      • ln(Ti/Ca) (WEB-84c26-cf61-4730-a2fb-5101f): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’

Version: 1.0.1

  • lastVersion: 1.0.0
  • curator: nicholas
  • timestamp: 2022-07-15 23:01:19 UTC
  • changes:
    • Publication metadata:
      • 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’
    • Paleo Interpretation metadata:
      • Ti (WEB-15b43-29b6-4954-b979-bd3cc): interpretation1_scope: NULL has been replaced by ‘climate’
      • TOC (WEB-1b2bb-d42d-477f-b35d-3d7bc): interpretation1_scope: NULL has been replaced by ‘climate’
      • TN (WEB-28e52-2862-4f52-9936-3a287): interpretation1_scope: NULL has been replaced by ‘climate’
      • Fe (WEB-297de-ae48-41da-99bb-d427e): interpretation1_scope: NULL has been replaced by ‘climate’
      • CaCO3 (WEB-64793-2fa7-488c-8153-4a5a8): interpretation1_scope: NULL has been replaced by ‘climate’
      • ln(Fe/Ca) (WEB-84482-33c8-4bfd-843c-ed119): interpretation1_scope: NULL has been replaced by ‘climate’
      • C29 dD (WEB-a2486-c44a-4c63-af96-f33b3): interpretation1_scope: NULL has been replaced by ‘climate’
      • Ca (WEB-cc290-b0d2-4c75-87a0-f2e95): interpretation1_scope: NULL has been replaced by ‘climate’

Version: 1.0.0

  • curator: nicholas
  • timestamp: 2022-07-12 17:10:35 UTC
  • notes: Added to lipdverse database.