L <- lipdR::readLipd("https://lipdverse.org/data/H6w2icNZMsy6whGbYlUh/1_0_7/CO98BOFP.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/1876
lipdVersion: 1.3
dataContributor: KLD, Wu
author: list(name = "Boiseau")
citeKey: boiseau1998atmospheric
journal: Paleoceanography
volume: 13
pages: -14
title: Atmospheric and oceanic evidences of El Nino-Southern Oscillation events in the south central Pacific Ocean from coral stable isotopic records over the last 137 years
doi: 10.1029/98PA02502,10.1029/1999GL900595
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-PacificMooreaBoiseau2003
doi: 10.1029/1999GL900595
latitude: -17.5
longitude: -149.8333
elevation: -5
siteName: Moorea, French Polynesia
pages2kRegion: Ocean
TSid: MAT8707df8c02
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_132_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
direction: decrease/increase
interpDirection: decrease/increase
scope: climate
seasonality: subannual
variable: temperature
variableDetail: sea surface
variableGroup: temperature and salinity
scope: climate
scope: climate
basis: The relative distributionof rainfall and SST versus time (Figure4) compared with d18O versus core depth over the 1979-1990 period emphasizes a strong similarity between SST and d18O
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 2
integrationTimeBasis: The chronology is then established by associating each maximum and minimum in d18O with each minimum (August) maximum (March) in the SST record (Figure2), assuming a constant linear extension rate between these 2 months
integrationTimeUnits: months
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: subannual
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 2
integrationTimeBasis: The chronology is then established by associating each maximum and minimum in d18O with each minimum (August) maximum (March) in the SST record (Figure2), assuming a constant linear extension rate between these 2 months
integrationTimeUnits: months
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
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geo
PaleoData columns
year (yr AD)
interpretation
1
2
3
4
5
d18O (permil)
interpretation
1
2
3
4
5
6