L <- lipdR::readLipd("https://lipdverse.org/data/ROQUBo8zC9rD7YtZWul9/1_0_7/CO05ASGU.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/1915
lipdVersion: 1.3
dataContributor: KJA, JET
author: list(name = "Asami, R.; Yamada, T.; Iryu, Y.; Quinn, T.M.; Meyer, C.P.; Paulay, G.")
citeKey: asami2005interannual
journal: J. Geophys. Res.
volume: 110
pages: -26
title: Interannual and decadal variability of the western Pacific sea surface condition for the years 1787?2000: Reconstruction based on stable isotope record from a Guam coral
doi: 10.1029/2004JC002555
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-PacificGuamAsami2005
doi: 10.1002/2014PA002717
latitude: 13.598
longitude: 144.836
elevation: -7.8
siteName: Guam Coral
pages2kRegion: Ocean
TSid: MAT12288777c6
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_166_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
basis: These results suggest that changes in Guam ?18Ocoral are mainly influenced by SST and SSS variations on seasonal and interannual timescales.
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 d18Ocoral anomaly is significantly correlated with SST anomaly (SSTA) (r = -0.69 and p < 0.01) and SSS anomaly (SSSA) (r = 0.49 and p < 0.01). These results suggest that changes in Guam d18Ocoral are mainly influenced by SST and SSS variations on seasonal and interannual timescales.
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 1-Jan
integrationTimeBasis: maximum and minimum ?18Ocoral values in a given year were assigned to February and August; linear interpolation between these fixed tie points
integrationTimeUnits: month
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: subannual
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
basis: The d18Ocoral anomaly is significantly correlated with SST anomaly (SSTA) (r = -0.69 and p < 0.01) and SSS anomaly (SSSA) (r = 0.49 and p < 0.01). These results suggest that changes in Guam d18Ocoral are mainly influenced by SST and SSS variations on seasonal and interannual timescales.
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 1-Jan
integrationTimeBasis: maximum and minimum ?18Ocoral values in a given year were assigned to February and August; linear interpolation between these fixed tie points
integrationTimeUnits: month
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
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geo
PaleoData columns
year (yr AD)
interpretation
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2
3
4
5
d18O (permil)
interpretation
1
2
3
4
5
6