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L <- lipdR::readLipd("https://lipdverse.org/data/LMifEVQKJJhSS4l0HHoc/1_0_10/TR11BAVO.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_2
archiveType: Wood
originalDataUrl: http://www1.ncdc.noaa.gov/pub/data/paleo/treering/isotope/southamerica/
lipdVersion: 1.3
author: list(name = "Ballantyne A.P.")
doi: 10.1175/2010EI277.1
latitude: -22
longitude: -66
elevation: 3500
siteName: Volcan Granada, Argentina
TSid: MAT6731b357bc
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: TR11BAVO02
variableName: d18O
units: permil
description: cellulose
basis: A 150-year record obtained from Polylepis spp. showed a significant negative relationship between d18O and March precipitation
direction: negative
interpDirection: negative
scope: climate
seasonality: Mar
seasonalityOriginal: March
variable: precipitation
variableDetail: Seasonal
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_amount
scope: climate
scope: climate
basis: Source water d18O is determined by P_isotopes, which is strongly influenced by precipitation amount.
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeUncertainty: 2
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Mar
seasonalityOriginal: March
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
variableGroupOriginal: precipitation amount
scope: isotope
scope: isotope
TSid: TR11BAVO01
variableName: d18O
units: permil
description: cellulose
basis: A 150-year record obtained from Polylepis spp. also showed a significant negative relationship between d18O and March precipitation
interpDirection: negative
scope: climate
seasonality: Mar
seasonalityOriginal: March
variable: precipitation
variableDetail: Precipitation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: Precipitation amount
scope: climate
scope: climate
basis: Source water d18O is determined by P_isotopes, which is strongly influenced by precipitation amount.
direction: positive
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Mar
seasonalityOriginal: March
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
variableGroupOriginal: precipitation amount
scope: isotope
scope: isotope
root
pub
pub1
geo
PaleoData columns
year (yr AD)
interpretation
1
2
3
d18O (permil)
interpretation
1
2
3
4
5
6
d18O (permil)
interpretation
1
2
3
4
5
6