L <- lipdR::readLipd("https://lipdverse.org/data/MNN1hLqGHovxO9RxzqWP/1_0_5/CO06QUNG.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/6116
lipdVersion: 1.3
dataContributor: MNE
author: list(name = "Quinn, Terrence M. , Taylor, Frederick W. , Crowley, Thomas J.")
citeKey: quinn2006coral
journal: J. Geophys. Res.
volume: 111
title: Coral-based climate variability in the Western Pacific Warm Pool since 1867
doi: 10.1029/2005JC003243
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-PacificQuinn2008Rabaul
doi: 10.1002/2014PA002717
latitude: -4.1916
longitude: 151.9772
elevation: -8
siteName: Rabaul
pages2kRegion: Ocean
TSid: MAT85ba7be434
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
TSid: Ocean2kHR_144_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
basis: Coral d18O variations at Rabaul are likely driven by the combined variations in SST and seawater d18O (and hence SSS) given the general climatology of the WPWP
direction: decrease/increase
interpDirection: decrease/increase
scope: climate
seasonality: subannual
variable: temperature
variableDetail: sea surface
variableGroup: temperature and salinity
scope: climate
scope: climate
basis: Coral d18O variations are modestly correlated with SST variations over their common period of overlap (1970? 1993), both in terms of the monthly and monthly anomaly time series
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: Age models were constructed using the AnalySeries program [Paillard et al., 1996]. We used tie points to connect the lowest (highest) d18O values to the warmest (coolest) temperatures in the instrumental SST record to establish each year.The use of coral Sr/Ca values instead of coral d18O values to construct the age model results produces a similar chronology. The geochemical data were then interpolated to give monthly d18O values. The geochemically based age models were confirmed via comparison with ages determined by counting of skeletal density-band couplets in the X-ray images of the coral slab.
integrationTimeUnits: month
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: subannual
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
basis: The monthly coral d18O anomaly time series at Rabaul yields no significant correlation with the instrumental SSS record, despite the fact that similar coral records from Fiji [Le Bec et al., 2000] and Vanuatu [Kilbourne et al., 2004] have been demonstrated to reflect SSS variations. It is possible that the monthly coral d18O anomaly record does reflect local SSS variability at Rabaul and the observed low correlation between these two variables results from differences between the ship-track SSS record and the actual SSS variability at Rabaul
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: Age models were constructed using the AnalySeries program [Paillard et al., 1996]. We used tie points to connect the lowest (highest) d18O values to the warmest (coolest) temperatures in the instrumental SST record to establish each year.The use of coral Sr/Ca values instead of coral d18O values to construct the age model results produces a similar chronology. The geochemical data were then interpolated to give monthly d18O values. The geochemically based age models were confirmed via comparison with ages determined by counting of skeletal density-band couplets in the X-ray images of the coral slab.
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
TSid: Ocean2kHR_145_iso2k
variableName: Sr/Ca
units: mmol/mol
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
rank: NA
scope: climate
scope: climate
coefficient: NA
fraction: NA
inferredMaterial: seawater
rank: NA
scope: isotope
seasonality: subannual
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
TSid: Ocean2kHR_146_iso2k
variableName: d13C
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: FALSE
rank: NA
scope: climate
rank: NA
scope: climate
scope: climate
coefficient: NA
fraction: NA
inferredMaterial: seawater
rank: NA
scope: isotope
seasonality: subannual
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
root
pub
pub1
pub2
geo
PaleoData columns
year (yr AD)
interpretation
1
2
d18O (permil)
interpretation
1
2
3
4
5
6
Sr/Ca (mmol/mol)
interpretation
1
2
3
4
5
6
d13C (permil)
interpretation
1
2
3
4
5
6