Version history for nB7kY2gbX2GuZm8VCdiO - Dendi.Jaeschke.2020

Version: 1.0.11

lastVersion: 1.0.10
curator: nicholas
timestamp: 2023-06-02 19:01:03 UTC
changes:
- Paleo Column metadata:
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_notes: ‘((( ((( ((( We use ��Dwax to assess the regional precipitation history, and ��13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our ��D record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_variableName updated; paleoData_measurementMaterial has been standardized; paleoData_units updated; paleoData_datum has been standardized; paleoData_proxy updated ))) We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized /// We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized ))) “We use dDwax to assess the regional precipitation history, and d13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our dD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.” /// We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized ))) We use dDwax to assess the regional precipitation history, and d13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our dD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized /// We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized’ has been replaced by ‘We use dDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our dD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized’

Version: 1.0.10

lastVersion: 1.0.9
curator: nicholas
timestamp: 2023-05-31 20:38:16 UTC
changes:
- Paleo Column metadata:
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_notes: ‘We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized’ has been replaced by ‘((( ((( ((( We use ��Dwax to assess the regional precipitation history, and ��13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our ��D record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_variableName updated; paleoData_measurementMaterial has been standardized; paleoData_units updated; paleoData_datum has been standardized; paleoData_proxy updated ))) We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized /// We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized ))) “We use dDwax to assess the regional precipitation history, and d13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our dD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.” /// We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized ))) We use dDwax to assess the regional precipitation history, and d13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our dD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized /// We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized’

Version: 1.0.9

lastVersion: 1.0.8
curator: ccr97
timestamp: 2023-05-31 18:16:50.784101 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
- Dataset:
  - chronData has been added to this dataset
- Paleo Column metadata:
  - d13C (WEB-5f2db-4313-4adb-8a97-b13da): paleoData_proxyObservationType: ‘C29 d13C’ has been replaced by ‘d13C’
  - d2H (WEB-92c70-e9d3-404f-ac4b-fff82): paleoData_proxyObservationType: ‘C31 dD’ has been replaced by ‘d2H’
  - d13C (WEB-b38e4-c59c-48d4-8f47-7251d): paleoData_proxyObservationType: ‘C31 d13C’ has been replaced by ‘d13C’
  - uncertainty1s (WEB-b499b-1928-4524-99c7-e8c88): paleoData_proxyObservationType: ‘C31 d13C std dev’ has been replaced by ‘uncertainty1s’
  - uncertainty1s (WEB-d01cc-e624-47d0-858b-206bc): paleoData_proxyObservationType: ‘C29 d13C std dev’ has been replaced by ‘uncertainty1s’
  - uncertainty1s (WEB-dcf93-e2f9-4a82-8feb-b5a4f): paleoData_proxyObservationType: ‘C29 dD std dev’ has been replaced by ‘uncertainty1s’
  - depth (WEB-ded45-8bb9-403a-ad21-a3bba): paleoData_proxyObservationType: ‘Depth’ has been replaced by ‘depth’
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_notes: ‘((( ((( We use ��Dwax to assess the regional precipitation history, and ��13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our ��D record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_variableName updated; paleoData_measurementMaterial has been standardized; paleoData_units updated; paleoData_datum has been standardized; paleoData_proxy updated ))) We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized /// We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized ))) “We use dDwax to assess the regional precipitation history, and d13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our dD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.” /// We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized’ has been replaced by ‘We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized’
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_proxyObservationType: ‘C29 dD’ has been replaced by ‘d2H’
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_QCCertification: ‘CR’ has been replaced by NULL
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_QCnotes: ‘Multiple cores and correlation used for age model’ has been replaced by NULL
  - uncertainty1s (WEB-e3b96-1312-40ac-903d-3cd64): paleoData_proxyObservationType: ‘C31 dD std dev’ has been replaced by ‘uncertainty1s’
- ChronData table:
  - Column ‘WEB-013f1-ca29-478b-a847-70baf’, with variable name ‘reservoir’, was added to the dataset
  - Column ‘WEB-533b3-9050-4659-ba88-3ce18’, with variable name ‘age14C’, was added to the dataset
  - Column ‘WEB-5fc36-4609-4fdf-90a3-19a45’, with variable name ‘uncertainty2s’, was added to the dataset
  - Column ‘WEB-88bb2-2c6a-43f7-b941-d463c’, with variable name ‘depth’, was added to the dataset
  - Column ‘WEB-df9d7-4043-46c9-a191-f572d’, with variable name ‘core’, was added to the dataset
  - Column ‘WEB-f0413-0825-4627-9a07-f5057’, with variable name ‘depth’, was added to the dataset

Version: 1.0.8

lastVersion: 1.0.7
curator: nicholas
timestamp: 2023-05-12 21:52:53 UTC
changes:
- Paleo Column metadata:
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_notes: ‘((( We use ��Dwax to assess the regional precipitation history, and ��13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our ��D record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_variableName updated; paleoData_measurementMaterial has been standardized; paleoData_units updated; paleoData_datum has been standardized; paleoData_proxy updated ))) We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized /// We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized’ has been replaced by ‘We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized’

Version: 1.0.7

lastVersion: 1.0.6
curator: nicholas
timestamp: 2023-03-24 22:24:07 UTC
changes:
- Paleo Column metadata:
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_proxyGeneral: ‘isotope’ has been replaced by ‘isotopic’

Version: 1.0.6

lastVersion: 1.0.5
curator: nicholas
timestamp: 2023-03-23 23:03:12 UTC
changes:
- Geographic metadata:
  - geo_elevation: NULL has been replaced by ‘2836’

Version: 1.0.5

lastVersion: 1.0.4
curator: nicholas
timestamp: 2023-02-13 23:40:49 UTC
changes:
- Paleo Column metadata:
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_notes: ‘We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized’ has been replaced by ‘((( We use ��Dwax to assess the regional precipitation history, and ��13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our ��D record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_variableName updated; paleoData_measurementMaterial has been standardized; paleoData_units updated; paleoData_datum has been standardized; paleoData_proxy updated ))) We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized /// We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized’

Version: 1.0.4

lastVersion: 1.0.3
curator: nicholas
timestamp: 2023-02-09 15:37:56 UTC
notes: Updated lipdverse database entry with a changed file.
changes:
- Paleo Column metadata:
  - age (WEB-3bf07-09a0-4d77-83df-9992f): paleoData_notes: NULL has been replaced by ‘NA; paleoData_isPrimary has been standardized’
  - age (WEB-3bf07-09a0-4d77-83df-9992f): paleoData_units: ‘cal year BP’ has been replaced by ‘yr BP’
  - age (WEB-3bf07-09a0-4d77-83df-9992f): paleoData_isPrimary: NULL has been replaced by ‘TRUE’
  - d13C (WEB-5f2db-4313-4adb-8a97-b13da): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized; paleoData_proxyGeneral has been standardized’
  - d13C (WEB-5f2db-4313-4adb-8a97-b13da): paleoData_proxyGeneral: NULL has been replaced by ‘isotopic’
  - d13C (WEB-5f2db-4313-4adb-8a97-b13da): paleoData_units: ‘permil PDB’ has been replaced by ‘permil’
  - d13C (WEB-5f2db-4313-4adb-8a97-b13da): paleoData_variableName: ‘C29 d13C’ has been replaced by ‘d13C’
  - d13C (WEB-5f2db-4313-4adb-8a97-b13da): paleoData_datum: NULL has been replaced by ‘PDB’
  - d13C (WEB-5f2db-4313-4adb-8a97-b13da): paleoData_measurementMaterial: NULL has been replaced by ‘C29’
  - d2H (WEB-92c70-e9d3-404f-ac4b-fff82): paleoData_notes: NULL has been replaced by ‘NA; paleoData_datum has been standardized; paleoData_proxyGeneral has been standardized’
  - d2H (WEB-92c70-e9d3-404f-ac4b-fff82): paleoData_proxyGeneral: NULL has been replaced by ‘isotopic’
  - d2H (WEB-92c70-e9d3-404f-ac4b-fff82): paleoData_units: ‘permil SMOW’ has been replaced by ‘permil’
  - d2H (WEB-92c70-e9d3-404f-ac4b-fff82): paleoData_variableName: ‘C31 dD’ has been replaced by ‘d2H’
  - d2H (WEB-92c70-e9d3-404f-ac4b-fff82): paleoData_datum: NULL has been replaced by ‘SMOW’
  - d13C (WEB-b38e4-c59c-48d4-8f47-7251d): paleoData_notes: NULL has been replaced by ‘NA; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized; paleoData_proxyGeneral has been standardized’
  - d13C (WEB-b38e4-c59c-48d4-8f47-7251d): paleoData_proxyGeneral: NULL has been replaced by ‘isotopic’
  - d13C (WEB-b38e4-c59c-48d4-8f47-7251d): paleoData_units: ‘permil PDB’ has been replaced by ‘permil’
  - d13C (WEB-b38e4-c59c-48d4-8f47-7251d): paleoData_variableName: ‘C31 d13C’ has been replaced by ‘d13C’
  - d13C (WEB-b38e4-c59c-48d4-8f47-7251d): paleoData_datum: NULL has been replaced by ‘PDB’
  - d13C (WEB-b38e4-c59c-48d4-8f47-7251d): paleoData_measurementMaterial: NULL has been replaced by ‘C31’
  - uncertainty1s (WEB-b499b-1928-4524-99c7-e8c88): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized’
  - uncertainty1s (WEB-b499b-1928-4524-99c7-e8c88): paleoData_units: ‘+/- permil PDB’ has been replaced by ‘permil’
  - uncertainty1s (WEB-b499b-1928-4524-99c7-e8c88): paleoData_variableName: ‘C31 d13C std dev’ has been replaced by ‘uncertainty1s’
  - uncertainty1s (WEB-b499b-1928-4524-99c7-e8c88): paleoData_measurementMaterial: NULL has been replaced by ‘d13C C31’
  - uncertainty1s (WEB-b499b-1928-4524-99c7-e8c88): paleoData_summaryStatistic: NULL has been replaced by ‘1 sigma’
  - uncertainty1s (WEB-d01cc-e624-47d0-858b-206bc): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized’
  - uncertainty1s (WEB-d01cc-e624-47d0-858b-206bc): paleoData_units: ‘+/- permil PDB’ has been replaced by ‘permil’
  - uncertainty1s (WEB-d01cc-e624-47d0-858b-206bc): paleoData_variableName: ‘C29 d13C std dev’ has been replaced by ‘uncertainty1s’
  - uncertainty1s (WEB-d01cc-e624-47d0-858b-206bc): paleoData_measurementMaterial: NULL has been replaced by ‘d13C C29’
  - uncertainty1s (WEB-d01cc-e624-47d0-858b-206bc): paleoData_summaryStatistic: NULL has been replaced by ‘1 sigma’
  - uncertainty1s (WEB-dcf93-e2f9-4a82-8feb-b5a4f): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized’
  - uncertainty1s (WEB-dcf93-e2f9-4a82-8feb-b5a4f): paleoData_units: ‘+/- permil SMOW’ has been replaced by ‘permil’
  - uncertainty1s (WEB-dcf93-e2f9-4a82-8feb-b5a4f): paleoData_variableName: ‘C29 dD std dev’ has been replaced by ‘uncertainty1s’
  - uncertainty1s (WEB-dcf93-e2f9-4a82-8feb-b5a4f): paleoData_measurementMaterial: NULL has been replaced by ‘d2H C29’
  - uncertainty1s (WEB-dcf93-e2f9-4a82-8feb-b5a4f): paleoData_summaryStatistic: NULL has been replaced by ‘1 sigma’
  - depth (WEB-ded45-8bb9-403a-ad21-a3bba): paleoData_variableName: ‘Depth’ has been replaced by ‘depth’
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_notes: ‘We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.’ has been replaced by ‘We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.; paleoData_measurementMaterial has been standardized; paleoData_datum has been standardized’
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_proxy: ‘dDwax’ has been replaced by ‘dD’
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_units: ‘permil SMOW’ has been replaced by ‘permil’
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_variableName: ‘C29 dD’ has been replaced by ‘d2H’
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_datum: NULL has been replaced by ‘SMOW’
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): paleoData_measurementMaterial: NULL has been replaced by ‘C29’
  - uncertainty1s (WEB-e3b96-1312-40ac-903d-3cd64): paleoData_notes: NULL has been replaced by ‘NA; paleoData_summaryStatistic has been standardized; paleoData_measurementMaterial has been standardized’
  - uncertainty1s (WEB-e3b96-1312-40ac-903d-3cd64): paleoData_units: ‘+/- permil SMOW’ has been replaced by ‘permil’
  - uncertainty1s (WEB-e3b96-1312-40ac-903d-3cd64): paleoData_variableName: ‘C31 dD std dev’ has been replaced by ‘uncertainty1s’
  - uncertainty1s (WEB-e3b96-1312-40ac-903d-3cd64): paleoData_measurementMaterial: NULL has been replaced by ‘d2H C31’
  - uncertainty1s (WEB-e3b96-1312-40ac-903d-3cd64): paleoData_summaryStatistic: NULL has been replaced by ‘1 sigma’
- Paleo Interpretation metadata:
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): interpretation1_seasonality: ‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘Annual’
  - d2H (WEB-e04d6-7807-41df-9459-dafd8): interpretation1_variable: ‘P’ has been replaced by ‘precipitation’

Version: 1.0.3

lastVersion: 1.0.2
curator: nicholas
timestamp: 2022-09-09 02:04:58 UTC
changes:
- Paleo Interpretation metadata:
  - C29 dD (WEB-e04d6-7807-41df-9459-dafd8): 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 17:30:02 UTC
changes:
- Base metadata:
  - originalDataUrl: NULL has been replaced by ‘https://doi.org/10.1594/PANGAEA.923144’
- Geographic metadata:
  - geo_elevation: ‘2837’ has been replaced by NULL
  - geo_gcmdLocation: NULL has been replaced by ‘Africa>Eastern Africa>Ethiopia’
- Paleo Column metadata:
  - C29 dD (WEB-e04d6-7807-41df-9459-dafd8): paleoData_proxy: ‘dD’ has been replaced by ‘dDwax’
  - C29 dD (WEB-e04d6-7807-41df-9459-dafd8): paleoData_notes: NULL has been replaced by ‘We use δDwax to assess the regional precipitation history, and δ13Cwax to examine the distribution of C3 and C4 vegetation in the catchment…Our δD record indicates high precipitation during peak AHP (ca. 10 to 8 ka BP) followed by a gradual transition toward a drier late Holocene climate.’
  - C29 dD (WEB-e04d6-7807-41df-9459-dafd8): paleoData_proxyGeneral: NULL has been replaced by ‘isotope’
- Paleo Interpretation metadata:
  - C29 dD (WEB-e04d6-7807-41df-9459-dafd8): interpretation1_seasonalityGeneral: NULL has been replaced by ‘Annual’

Version: 1.0.1

lastVersion: 1.0.0
curator: nicholas
timestamp: 2022-07-15 23:00:05 UTC
changes:
- Publication metadata:
  - pub1_author: ‘list(list(name = “Jaeschke, Andrea”), list(name = “Thienemann, Matthias”), list(name = “Schefuß, Enno”), list(name = “Urban, Jonas”), list(name = “Schäbitz, Frank”), list(name = “Wagner, Bernd”), list(name = “Rethemeyer, Janet”))’ has been replaced by ‘Jaeschke, Andrea’
- Paleo Interpretation metadata:
  - C29 d13C (WEB-5f2db-4313-4adb-8a97-b13da): interpretation1_scope: NULL has been replaced by ‘climate’
  - C31 dD (WEB-92c70-e9d3-404f-ac4b-fff82): interpretation1_scope: NULL has been replaced by ‘climate’
  - C31 d13C (WEB-b38e4-c59c-48d4-8f47-7251d): interpretation1_scope: NULL has been replaced by ‘climate’
  - C31 d13C std dev (WEB-b499b-1928-4524-99c7-e8c88): interpretation1_scope: NULL has been replaced by ‘climate’
  - C29 d13C std dev (WEB-d01cc-e624-47d0-858b-206bc): interpretation1_scope: NULL has been replaced by ‘climate’
  - C29 dD std dev (WEB-dcf93-e2f9-4a82-8feb-b5a4f): interpretation1_scope: NULL has been replaced by ‘climate’
  - C31 dD std dev (WEB-e3b96-1312-40ac-903d-3cd64): interpretation1_scope: NULL has been replaced by ‘climate’

Version: 1.0.0

curator: nicholas
timestamp: 2022-07-12 17:10:34 UTC
notes: Added to lipdverse database.