L <- lipdR::readLipd("https://lipdverse.org/data/XZ3JPyRLteBJERXWP3bW/1_0_5/LS14LASO.lpd")
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iso2k-1_1_1
archiveType: LakeSediment
originalDataUrl: https://doi.org/10.1594/PANGAEA.834963
lipdVersion: 1.3
citeKey: lauterbach2014climaticimprintofthemidla
journal: The Holocene
volume: 24
title: Climatic imprint of the mid-latitude Westerlies in the Central Tian Shan of Kyrgyzstan and teleconnections to North Atlantic climate variability during the last 6000 years
doi: 10.1177/0959683614534741
latitude: 41.7939
longitude: 75.1961
elevation: 3016
siteName: Sonk11D
TSid: WEBa86ea34e
variableName: year
units: yr AD
description: Year AD
TSid: WEB1a77aeb9
variableName: age
units: yr BP
description: Years before present (1950) BP
TSid: WEB48a85350
variableName: depth
units: cm
description: depth
TSid: LPD343ffe05_iso2k
variableName: d2H
units: permil
description: terrestrial biomarker
useInGlobalTemperatureAnalysis: TRUE
basis: previously published inferrences: fraction reflects evapotranspiration during the growing season
direction: negative
inferredMaterial: precipitation as modified by evapotranspiration
interpDirection: negative
rank: 1
scope: climate
seasonality: Summer
seasonalityOriginal: summer
variable: effectivePrecipitation
variableDetail: C-29
variableGroup: moisture (P-E)
scope: climate
scope: climate
basis: δDn-C29 record of the Son Kol sediments can be used to infer information about past summer moisture conditions.
direction: negative
scope: isotope
seasonality: Jun-Aug
variable: effectivePrecipitation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_E
scope: isotope
scope: isotope
TSid: LPDd7ba1947_iso2k
variableName: needsToBeChanged
units: unitless
useInGlobalTemperatureAnalysis: FALSE
scope: climate
scope: climate
scope: climate
scope: isotope
scope: isotope
scope: isotope
root
pub
pub1
geo
PaleoData columns
year (yr AD)
age (yr BP)
depth (cm)
d2H (permil)
interpretation
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2
3
4
5
6
needsToBeChanged (unitless)
interpretation
1
2
3
4
5
6