L <- lipdR::readLipd("https://lipdverse.org/data/mMVze2VpD6ysrjTCryjP/1_0_7/CO93COTW.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/1845
lipdVersion: 1.3
dataContributor: KJA, Rogers
author: list(name = "Cole, J.E., R.G. Fairbanks, and G.T. Shen.")
citeKey: cole1990the
journal: Paleoceanography
volume: 5
pages: -14
title: The Southern Oscillation recorded in the d18O of corals from Tarawa Atoll
doi: 10.1126/science.260.5115.1790
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-PacificTarawaCole1990
doi: 10.1002/2014PA002717
latitude: 1.4167
longitude: 173.0333
elevation: -3
siteName: Tarawa Atoll, Republic of Kiribati
pages2kRegion: Ocean
TSid: MATdc4c3d9750
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
rank: NA
scope: climate
TSid: Ocean2kHR_178_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: At Tarawa, results from an ongoing monitoring program confirm that intenst rainfall alters the d18O and salinity of the surface mixed layer. Shallow-growing corals incorporate this isotopic shift in the d18O of their aragonite skeletons.
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: Ages were determined independently for the two cores on the basis of seasonal d13C variability, which is supported by radiometric and density-banding observations of young Tarawa corals. We normalized the records, spliced them together using diagnostic density and isotopic patterns, and interpolated them to monthly resolution for statistical analysis
integrationTimeUnits: month
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: subannual
variable: seawaterIsotope
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: d18O_seawater
basis: Correlation of Tarawa d18O record with local SST on monthly (0.62), seasonal (0.67) and annual (0.78) timescales compared to local rainfall on monthly (0.39 or 0.59), seasonal (0.47 or 0.66), and annual (0.59 or 0.80) timescales.
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: Ages were determined independently for the two cores on the basis of seasonal d13C variability, which is supported by radiometric and density-banding observations of young Tarawa corals. We normalized the records, spliced them together using diagnostic density and isotopic patterns, and interpolated them to monthly resolution for statistical analysis
integrationTimeUnits: month
mathematicalRelation: linear
rank: NA
scope: isotope
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
coefficient: NA
fraction: NA
rank: NA
scope: isotope
root
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PaleoData columns
year (yr AD)
interpretation
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2
3
4
d18O (permil)
interpretation
1
2
3
4
5
6