Version history for b80Gp0jHNJdqglhwtnn4 - Baikal.Swann.2018

Version: 1.0.10

Version: 1.0.9

  • lastVersion: 1.0.8
  • curator: nicholas
  • timestamp: 2023-07-05 00:33:12 UTC
  • changes:
    • Publication metadata:
      • pub1_doi: ‘10..1016/j.quascirev.2018.04.013’ has been replaced by ‘10.1016/j.quascirev.2018.04.013’
    • Paleo Interpretation metadata:
      • precipitation (WEB2b09ab9c): interpretation1_variableDetail: ‘’ has been replaced by ‘
      • d18O (WEBd1125bee): interpretation1_seasonality: NULL has been replaced by ‘((( ))) Annual /// null’
      • d18O (WEBd1125bee): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’
      • d18O (WEBd1125bee): interpretation1_variableDetail: ‘Annual’ has been replaced by ‘

Version: 1.0.8

  • lastVersion: 1.0.7
  • curator: nicholas
  • timestamp: 2023-05-12 21:49:00 UTC
  • changes:
    • Paleo Column metadata:
      • precipitation (WEB2b09ab9c): paleoData_notes: ‘((( “Using the relationship betweend18Odiatomand precipitation from c.2010-1900 (Fig. 6c) we quantify decadal changes in annual pre-cipitation for Central Asia from our composite south basind18Odia-tomrecord, which extends back to c.1850 AD”; paleoData_units updated ))) “Using the relationship betweend18Odiatomand precipitation from c.2010-1900 (Fig. 6c) we quantify decadal changes in annual pre-cipitation for Central Asia from our composite south basind18Odia-tomrecord, which extends back to c.1850 AD” /// “Using the relationship betweend18Odiatomand precipitation from c.2010-1900 (Fig. 6c) we quantify decadal changes in annual pre-cipitation for Central Asia from our composite south basind18Odia-tomrecord, which extends back to c.1850 AD”’ has been replaced by ‘“Using the relationship betweend18Odiatomand precipitation from c.2010-1900 (Fig. 6c) we quantify decadal changes in annual pre-cipitation for Central Asia from our composite south basind18Odia-tomrecord, which extends back to c.1850 AD”’
      • d18O (WEBd1125bee): paleoData_notes: ‘((( “As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation”; paleoData_units updated; paleoData_datum has been standardized ))) “As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation”; paleoData_datum has been standardized /// “As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation”; paleoData_datum has been standardized’ has been replaced by ‘“As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation”; paleoData_datum has been standardized’

Version: 1.0.7

  • lastVersion: 1.0.6
  • curator: nicholas
  • timestamp: 2023-02-13 23:37:20 UTC
  • changes:
    • Paleo Column metadata:
      • precipitation (WEB2b09ab9c): paleoData_notes: ‘“Using the relationship betweend18Odiatomand precipitation from c.2010-1900 (Fig. 6c) we quantify decadal changes in annual pre-cipitation for Central Asia from our composite south basind18Odia-tomrecord, which extends back to c.1850 AD”’ has been replaced by ‘((( “Using the relationship betweend18Odiatomand precipitation from c.2010-1900 (Fig. 6c) we quantify decadal changes in annual pre-cipitation for Central Asia from our composite south basind18Odia-tomrecord, which extends back to c.1850 AD”; paleoData_units updated ))) “Using the relationship betweend18Odiatomand precipitation from c.2010-1900 (Fig. 6c) we quantify decadal changes in annual pre-cipitation for Central Asia from our composite south basind18Odia-tomrecord, which extends back to c.1850 AD” /// “Using the relationship betweend18Odiatomand precipitation from c.2010-1900 (Fig. 6c) we quantify decadal changes in annual pre-cipitation for Central Asia from our composite south basind18Odia-tomrecord, which extends back to c.1850 AD”’
      • d18O (WEBd1125bee): paleoData_notes: ‘“As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation”; paleoData_datum has been standardized’ has been replaced by ‘((( “As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation”; paleoData_units updated; paleoData_datum has been standardized ))) “As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation”; paleoData_datum has been standardized /// “As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation”; paleoData_datum has been standardized’

Version: 1.0.6

  • lastVersion: 1.0.5
  • curator: nicholas
  • timestamp: 2023-02-09 15:29:00 UTC
  • notes: Updated lipdverse database entry with a changed file.
  • changes:
    • Paleo Column metadata:
      • precipitation (WEB2b09ab9c): paleoData_units: ‘mm/a’ has been replaced by ‘mm/yr’
      • d18O (WEBd1125bee): paleoData_datum: NULL has been replaced by ‘VSMOW’
      • d18O (WEBd1125bee): paleoData_notes: ‘“As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation”’ has been replaced by ‘“As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation”; paleoData_datum has been standardized’
      • d18O (WEBd1125bee): paleoData_units: ‘permil (VSMOW)’ has been replaced by ‘permil’
      • age (WEBe0a0dc53): paleoData_datum: NULL has been replaced by ‘1950’
      • age (WEBe0a0dc53): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized’
      • age (WEBe0a0dc53): paleoData_units: ‘BP’ has been replaced by ‘yr BP’
      • age (WEBe0a0dc53): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
    • Paleo Interpretation metadata:
      • precipitation (WEB2b09ab9c): interpretation1_seasonality: ‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘Annual’
      • precipitation (WEB2b09ab9c): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’
      • d18O (WEBd1125bee): interpretation1_seasonality: ‘’ has been replaced by NULL
      • d18O (WEBd1125bee): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’

Version: 1.0.5

Version: 1.0.4

  • lastVersion: 1.0.3
  • curator: nicholas
  • timestamp: 2022-05-18 00:24:34 UTC
  • changes:
    • Paleo Column metadata:
      • precipitation (WEB2b09ab9c): paleoData_archiveType: ‘Lake Sediment’ has been replaced by ‘LakeSediment’
      • precipitation (WEB2b09ab9c): paleoData_variableName: ‘Precipitation’ has been replaced by ‘precipitation’
      • precipitation (WEB2b09ab9c): paleoData_archiveTypeOriginal: NULL has been replaced by ‘Lake Sediment’
      • precipitation (WEB2b09ab9c): paleoData_proxyLumps: NULL has been replaced by ‘isotope’
      • precipitation (WEB2b09ab9c): paleoData_proxyLumpsOriginal: NULL has been replaced by ‘d18O’
      • precipitation (WEB2b09ab9c): paleoData_variableNameOriginal: NULL has been replaced by ‘Precipitation’
      • d18O (WEBd1125bee): paleoData_archiveType: ‘Lake Sediment’ has been replaced by ‘LakeSediment’
      • d18O (WEBd1125bee): paleoData_archiveTypeOriginal: NULL has been replaced by ‘Lake Sediment’
      • d18O (WEBd1125bee): paleoData_proxyLumps: NULL has been replaced by ‘isotope’
      • d18O (WEBd1125bee): paleoData_proxyLumpsOriginal: NULL has been replaced by ‘d18O’
      • age (WEBe0a0dc53): paleoData_units: ‘yr BP’ has been replaced by ‘BP’
      • age (WEBe0a0dc53): paleoData_unitsOriginal: NULL has been replaced by ‘yr BP’
    • Paleo Interpretation metadata:
      • precipitation (WEB2b09ab9c): interpretation1_variableGroup: NULL has been replaced by ‘P’
      • d18O (WEBd1125bee): interpretation1_variableGroup: NULL has been replaced by ‘P’

Version: 1.0.3

  • lastVersion: 1.0.2
  • curator: nicholas
  • timestamp: 2021-11-19 21:06:13 UTC
  • changes:
    • Paleo Interpretation metadata:
      • Precipitation (WEB2b09ab9c): interpretation1_seasonality: ‘Annual’ has been replaced by ‘1,2,3,4,5,6,7,8,9,10,11,12’
      • Precipitation (WEB2b09ab9c): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’

Version: 1.0.2

  • lastVersion: 1.0.1
  • curator: nicholas
  • timestamp: 2021-11-17 02:05:24 UTC
  • changes:
    • Base metadata:
    • Geographic metadata:
      • geo_gcmdLocation: NULL has been replaced by ‘Europe>Eastern Europe>Russian Federation’
    • Paleo Interpretation metadata:
    • Paleo Column metadata:
      • Precipitation (WEB2b09ab9c): paleoData_datum: NULL has been replaced by ‘abs’
      • Precipitation (WEB2b09ab9c): paleoData_notes: NULL has been replaced by ‘“Using the relationship betweend18Odiatomand precipitation from c.2010-1900 (Fig. 6c) we quantify decadal changes in annual pre-cipitation for Central Asia from our composite south basind18Odia-tomrecord, which extends back to c.1850 AD”’
      • Precipitation (WEB2b09ab9c): paleoData_proxyDetail: NULL has been replaced by ‘diatom’
      • Precipitation (WEB2b09ab9c): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
      • d18O (WEBd1125bee): paleoData_notes: NULL has been replaced by ‘“As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation”’
      • d18O (WEBd1125bee): paleoData_proxyDetail: NULL has been replaced by ‘diatom’
      • d18O (WEBd1125bee): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
      • d18O (WEBd1125bee): paleoData_QCnotes: NULL has been replaced by ‘Defer to calibrated timeseries’
    • Paleo Calibration metadata:
      • Precipitation (WEB2b09ab9c): calibration_method: NULL has been replaced by ‘TRUE’

Version: 1.0.1

  • lastVersion: 1.0.0
  • curator: nicholas
  • timestamp: 2021-10-05 21:38:17 UTC
  • changes:
    • Publication metadata:
      • pub1_author: ‘list(list(name = “Swann, George E.A.”), list(name = “Mackay, Anson W.”), list(name = “Vologina, Elena”), list(name = “Jones, Matthew D.”), list(name = “Panizzo, Virginia N.”), list(name = “Leng, Melanie J.”), list(name = “Sloane, Hilary J.”), list(name = “Snelling, Andrea M.”), list(name = “Sturm, Michael”))’ has been replaced by ‘Swann, George E.A.’

Version: 1.0.0

  • curator: nick
  • timestamp: 2021-06-08 03:08:17 UTC
  • notes: Added to lipdverse database.