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L <- lipdR::readLipd("https://lipdverse.org/data/nEEoetHbXdBGm9w4AsoH/1_0_7/LS00WODE.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_2
archiveType: LakeSediment
originalDataUrl: this compilation
lipdVersion: 1.3
author: list(name = "Wolfe, B., Edwards, T., Aravena, R., Forman, S., Warner, B., Velichko, A., & MacDonald, G.")
journal: Quaternary Research
volume: 53
pages: 319-329
title: Holocene Paleohydrology and Paleoclimate at Treeline, North-Central Russia, Inferred from Oxygen Isotope Records in Lake Sediment Cellulose
doi: 10.1006/qres.2000.2124
latitude: 69.23
longitude: 86.57
elevation: 50
siteName: Dervanoi
TSid: MAT8292ebed05
variableName: year
units: yr AD
description: yr BP
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: MAT41df777573
variableName: depth
units: cm
description: depth
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: LS00WODE
variableName: d18O
units: permil
description: cellulose
basis: 18O of lake water largey controled by 18O of precip, which is attributed primarly to air temperature. The d18OP profiles have been reconstructed from a combination of: (1) estimated changes in MAT during the early to mid-Holocene assuming the modern relation 0.59? d18OP/i¿½C; (2) mid-Holocene paleo-d18OP inferred from peat porewater (described above); (3) minimum d18Olw values during the mid- to late Holocene at Middendorf and Dolgoe Lakes, which likely reflect values that have not been strongly influenced by evaporation; and (4) modern estimated d18OP for each site.
direction: positive
scope: climate
variable: temperature
variableDetail: air@surface
variableDetailOriginal: air
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T
variableOriginal: temperature
scope: climate
scope: climate
direction: positive
inferredMaterial: lake water
interpDirection: increase
rank: 1
scope: isotope
seasonality: Annual
seasonalityOriginal: Annual
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
coefficient: NA
fraction: NA
basis: Effects of evaporative related to circulation are secondary influence on hydrological balance
direction: negative
inferredMaterial: lake water
integrationTimeUncertaintyType: chronological
integrationTimeUnits: years
mathematicalRelation: linear
rank: 2
scope: isotope
variable: effectivePrecipitation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_E
coefficient: NA
fraction: NA
inferredMaterial: lake water & precipitation
integrationTimeUncertaintyType: chronological
integrationTimeUnits: years
scope: isotope
coefficient: NA
fraction: NA
rank: NA
TSid: chron1
variableName: depth
units: cm
description: midpoint depth
TSid: chron2
variableName: age14C
units: yr14C BP
description: 14C years before 1950
TSid: chron3
variableName: SD
units: yr14C BP
description: 14C years uncertainty
TSid: chron9
variableName: labID
units: unitless
description: laboratory ID from radiocarbon facility
TSid: chron10
variableName: materialDated
units: unitless
description: material analyzed
TSid: chron19
variableName: useInAgeModel
units: unitless
description: was this date used in the age modelpermil
TSid: RoyH8yDd1cg2twhqO
variableName: reject
root
pub
pub1
geo
PaleoData columns
year (yr AD)
interpretation
1
2
3
4
depth (cm)
interpretation
1
2
3
4
d18O (permil)
interpretation
1
2
3
4
5
6
ChronData columns
depth (cm)
age14C (yr14C BP)
SD (yr14C BP)
labID (unitless)
materialDated (unitless)
useInAgeModel (unitless)
reject ()