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L <- lipdR::readLipd("https://lipdverse.org/data/xMeZazGJKs6FzfXtgKcx/1_0_6/LS08STCR.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_2
archiveType: LakeSediment
originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/23081
lipdVersion: 1.3
journal: Quaternary International
volume: 188
pages: 139-148
title: Geochemical evidence for hydroclimatic variability over the last 2460 years from Crevice Lake in Yellowstone National Park, USA
doi: 10.1016/j.quaint.2007.11.012
latitude: 45
longitude: -110.5999
elevation: 1713
siteName: Crevice
TSid: MAT5074a6e772
variableName: year
units: yr AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: MAT865c27d65f
variableName: depth
units: cm
description: depth
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: LS08STCR
variableName: d18O
units: permil
description: carbonate
basis: The d18O record from the varved sediment from Crevice Lake is a proxy for hydroclimate, particularly discharge of the Yellowstone River, in Yellowstone National Park. Low d18O values are consistent with high flow of the Yellowstone River and, thus, wet winters with deep snow pack. They also correspond in general with tree-ring inferred estimates of increased precipitation in the YNP region. Prior to 2000 cal BP, decreasing d18O values suggest an increasingly wet climate or a gradual shift to winterdominated precipitation
direction: decrease
interpDirection: decrease
scope: climate
variable: streamflow
variableDetail: lake water
variableGroup: discharge
scope: climate
scope: climate
basis: Comparison of the oxygen-isotopic record with independent measures of climate suggests that the annual moisture balance is the primary isotopic control, with the seasonal timing of precipitation providing a possible secondary influence. High d18O values are associated with dry climate (e.g., evaporative enrichment of 18O) and/or wet summers relative to winters (higher d18O values of atmospheric precipitation).
direction: negative
inferredMaterial: lake water
integrationTime: 7
integrationTimeBasis: varve counts
integrationTimeUncertaintyType: sampling resolution
integrationTimeUnits: years
rank: 1
scope: isotope
variable: effectivePrecipitation
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: P_E
coefficient: NA
fraction: NA
basis: with the seasonal timing of precipitation providing a possible secondary influence. High d18O values are associated with dry climate (e.g., evaporative enrichment of 18O) and/or wet summers relative to winters (higher d18O values of atmospheric precipitation).
direction: negative
inferredMaterial: lake water
integrationTime: 7
integrationTimeBasis: varve counts
integrationTimeUncertaintyType: sampling resolution
integrationTimeUnits: years
rank: 2
scope: isotope
seasonality: Winter
variable: precipitationIsotope
variableGroup: P_isotope
variableGroupDirection: positive
coefficient: NA
fraction: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
TSid: WEBabc68a57
variableName: d13C
units: needsToBeChanged
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
scope: isotope
coefficient: NA
fraction: NA
rank: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
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: WEB919a4371
variableName: labID
units: NA
TSid: WEBc7c2bba9
variableName: MaterialDated
units: NA
TSid: WEB221d4bdf
variableName: age
units: yr BP
description: calibrated age of tephra
TSid: RIWgTe9ViJMpnH0kQ
variableName: SD-1
units: yr BP
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
d13C (needsToBeChanged)
interpretation
1
2
3
4
5
6
ChronData columns
depth (cm)
age14C (yr14C BP)
SD (yr14C BP)
labID (NA)
MaterialDated (NA)
age (yr BP)
SD-1 (yr BP)