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L <- lipdR::readLipd("https://lipdverse.org/data/JYZp8fpNdD5plMRDVcyk/1_0_10/TR18GRPM.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_2
archiveType: Wood
originalDataUrl: this compilation
lipdVersion: 1.3
author: list(list(name = "GrieSSinger, Jussi"), list(name = "Langhamer, Lukas"), list(name = "Schneider, Christoph"), list(name = "SaSS, Bjoern-Lukas"), list(name = "Steger, David"), list(name = "Skvarca, Pedro"), list(name = "Braun, Matthias H."), list(name = "Meier, Wolfgang J.-H."), list(name = "Srur, Ana M."), list(name = "Hochreuther, Philipp"))
journal: Frontiers in Earth Science
volume: 6
pages: 1-17
title: Imprints of Climate Signals in a 204 Year δ18O Tree-Ring Record of Nothofagus pumilio From Perito Moreno Glacier, Southern Patagonia (50°S)
doi: 10.3389/feart.2018.00027
latitude: -50.5167
longitude: -70.1167
elevation: 540
siteName: Perito Moreno
TSid: WEB9c5ce25c
variableName: year
units: yr AD
description: year ad
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: WEBcdcf63cd
variableName: d18O
units: permil
description: cellulose
direction: positive
scope: climate
seasonality: Summer
variable: precipitationIsotope
variableDetail: Souther Annular Mode (SAM)
variableGroup: d18O
scope: climate
scope: climate
basis: Temperature (positive) and precipitation amount (negative) have a significant influence on the isotopic composition of precipitation, which influences the isotopic composition of cellulose. The southern annular mode is correlated with both climate variables.
direction: positive
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Oct-Jan
seasonalityOriginal: Oct-Jan
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
variableGroupOriginal: T_air
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