L <- lipdR::readLipd("https://lipdverse.org/data/h78xR5H5VN2axGBxxLTh/1_0_6/CO00COKY.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/1855
lipdVersion: 1.3
dataContributor: NJA, Ally May
author: list(name = "Cole, J.E.")
citeKey: cole2000tropical
journal: Science
volume: 287
pages: -2
title: Tropical Pacific Forcing of Decadal SST Variability in the Western Indian Ocean over the Past Two Centuries
doi: 10.1126/science.287.5453.617
author: list(name = "Auer, Gerald , Piller, Werner E. , Reuter, Markus , Harzhauser, Mathias")
citeKey: auer2015correlating
title: Ocean2kHR-IndianMalindiCole2000
doi: 10.1002/2014PA002716
latitude: -3.2556
longitude: 40.1433
elevation: -6
siteName: Malindi Marine Park
pages2kRegion: Ocean
TSid: MATac63aaf979
variableName: year
units: yr AD
description: Year AD
fraction: NA
rank: NA
scope: climate
fraction: NA
rank: NA
scope: climate
rank: NA
scope: climate
fraction: NA
rank: NA
scope: climate
rank: NA
scope: climate
TSid: Ocean2kHR_001_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
direction: decrease/increase
interpDirection: decrease/increase
scope: climate
variable: temperature
variableDetail: sea surface
variableGroup: temperature and salinity
scope: climate
scope: climate
basis: The coral 18O record from this site reflects primarily SST; a linear regression of coral 18O versus SST yields a slope of 0.24 per mil (a€°) 18O per 1A°C, explaining 47% of the SST variance (20).
coefficient: NA
direction: negative
fraction: 0.47
inferredMaterial: seawater
integrationTime: 1
integrationTimeUncertainty: .083 to 0.167 yrs
integrationTimeUncertaintyType: chronological
integrationTimeUnits: years
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Annual
seasonalityOriginal: Annual
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
basis: additional variability in coral 18O may arise from vari- ations in the 18O of seawater due to precip- itation, evaporation, or runoff, but at this site these changes are likely to be secondary be- cause local rainfall 18O is not strongly de- pleted from average seawater (21) and salin- ity gradients are small (22). Rainfall and SST influences are likely to be additive in terms of annual effect on coral 18O because warmer years tend to be wetter at this site.
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeUncertainty: .083 to 0.167 yrs
integrationTimeUncertaintyType: chronological
integrationTimeUnits: years
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