L <- lipdR::readLipd("https://lipdverse.org/data/7XNtsEx1afLUVUtm4zUC/1_0_8/CO00FERA.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_2
archiveType: Coral
originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/1861
lipdVersion: 1.3
dataContributor: JZ
author: list(name = "Felis, T., J. Patzold, Y. Loya, M. Fine, A.H. Nawar, and G. Wefer")
citeKey: felis2000a
journal: Paleoceanography
volume: 15
pages: -15
title: A coral oxygen isotope record from the northern Red Sea documenting NAO, ENSO, and North Pacific teleconnections on Middle East climate variability since the year 1750
doi: 10.1029/1999PA000477
author: list(name = "Tierney, Jessica E. , Abram, Nerilie J. , Anchukaitis, Kevin J. , Evans, Michael N. , Giry, Cyril , Kilbourne, K. Halimeda , Saenger, Casey P. , Wu, Henry C. , Zinke, Jens")
citeKey: tierney2015tropical
title: Ocean2kHR-IndianRedSeaFelis2000
doi: 10.1002/2014PA002717
latitude: 27.85
longitude: 34.32
elevation: -6
siteName: Ras Umm Sidd, Red Sea
pages2kRegion: Ocean
TSid: LPD38217f22
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: Ocean2kHR_019_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
direction: decrease
interpDirection: decrease
scope: climate
seasonality: subannual
variable: temperature
variableDetail: sea@surface
variableDetailOriginal: sea_surface
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T
variableOriginal: temperature
scope: climate
scope: climate
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 12-Jun
integrationTimeBasis: The coral chronology is constructed by setting the maximum d18O value in a given year equal to mid-February (consistent with the climatological minimum in sea surface temperature) and assuming a constant coral growth rate between February of every year. Therefore we interpolated linearly between these fixed points for further age assignments. The resulting values were interpolated linearly to six equally spaced values per year, providing a bimonthly resolution.
integrationTimeUncertainty: 3 year in total
integrationTimeUncertaintyType: chronology
integrationTimeUnits: year
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: subannual
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
basis: SSS linked to rainfall
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 6/12
integrationTimeBasis: "The coral chronology is constructed by setting the maximum d18O value in a given year equal to mid-February (consistent with the climatological minimum in sea surface temperature) and assuming a constant coral growth rate between February of every year. Therefore we interpolated linearly between these fixed points for further age assignments. The resulting values were interpolated linearly to six equally spaced values per year, providing a bimonthly resolution."
integrationTimeUncertainty: 3 year in total
integrationTimeUncertaintyType: chronology
integrationTimeUnits: year
mathematicalRelation: linear
rank: 2
scope: isotope
variable: seawaterIsotope
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: d18O_seawater
coefficient: NA
fraction: NA
rank: NA
scope: isotope
root
pub
pub1
pub2
geo
PaleoData columns
year (yr AD)
interpretation
1
2
3
4
5
d18O (permil)
interpretation
1
2
3
4
5
6