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L <- lipdR::readLipd("https://lipdverse.org/data/jQ1ihXRcRqOKG2L207SA/1_0_10/TR08HORA.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/asia/russia/
lipdVersion: 1.3
author: list(name = "Holzkoemper S.")
doi: 10.2478/v10003-008-0025-6
latitude: 68.1
longitude: 60
elevation: 40
siteName: Northwestern Russian Tundra
TSid: MAT187cea98d6
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: TR08HORA01
variableName: d18O
units: permil
description: cellulose
direction: negative
interpDirection: negative
scope: climate
seasonality: Nov-Feb
variable: precipitation
variableDetail: Seasonal, annual
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_amount
scope: climate
scope: climate
basis: After evaluating the relationship between d18O and observed temperature and precipitation it can be concluded that there is some correlation of oxygen isotope values with late winter to early summer temperatures and a clear negative correlation with winter precipitation (November-February).
direction: positive
inferredMaterial: precipitation
integrationTime: 1
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Nov-Feb
seasonalityOriginal: November, December, January, February
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
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