CO05BAFI - v1.0.7

Dataset Id: yaVdLbM5zu8od0n75N5P

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R code to load dataset:

L <- lipdR::readLipd("https://lipdverse.org/data/yaVdLbM5zu8od0n75N5P/1_0_7/CO05BAFI.lpd")

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Dataset changelog

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In compilations: (only most recent versions are shown)

iso2k-1_1_0

root

archiveType: Coral

originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/1916

lipdVersion: 1.3

dataContributor: KLD

pub
pub1

author: Bagnato, S., B.K. Linsley, S.S. Howe, G.M. Wellington, J. Salinger

citeKey: bagnato2005coral

journal: Geochemistry, Geophysics, Geosystems

volume: 6

pages: -26

title: Coral oxygen isotope records of interdecadal climate variations in the South Pacific Convergence Zone region

doi: 10.1029/2004GC000879

pub2

author: 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-PacificSuvaBagnato2005

doi: 10.1002/2014PA002717

geo

latitude: -16.8167

longitude: 179.2333

elevation: -2

siteName: Savusavu Bay, Fiji

pages2kRegion: Ocean

PaleoData columns
year (yr AD)

TSid: LPD17b939a5

variableName: year

units: yr AD

description: Year AD

interpretation
1

rank: NA

scope: climate

2

rank: NA

scope: climate

3

rank: NA

scope: climate

4

rank: NA

scope: climate

d18O (permil)

TSid: Ocean2kHR_142

variableName: d18O

units: permil

description: carbonate

useInGlobalTemperatureAnalysis: TRUE

interpretation
1

direction: decrease

interpDirection: decrease

scope: climate

seasonality: Annual

seasonalityOriginal: Annual

variable: temperature

variableDetail: sea@surface

variableDetailOriginal: sea_surface

variableGroup: Temperature

variableGroupDirection: negative

variableGroupOriginal: T

variableOriginal: temperature

2

scope: climate

3

scope: climate

4

direction: negative

inferredMaterial: seawater

integrationTime: 1

integrationTimeBasis: The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997

integrationTimeUnits: year

mathematicalRelation: linear

rank: 1

scope: isotope

seasonality: Annual

seasonalityOriginal: Annual

variable: temperature

variableGroup: Temperature

variableGroupDirection: negative

variableGroupOriginal: T_water

5

direction: positive

inferredMaterial: seawater

integrationTime: 1

integrationTimeBasis: "The d18O were tuned to the SST record by assigning the lowest (highest) d18O values of each year to the highest (lowest) SST. Age assignments were then linearly interpolated between these two annual anchor points using the Arand software package (P. Howell, personal commu- nication, 2002). A continuous monthly SST data set is available only as far back as 1970, so for age assignments before 1970 the lowest (highest) d18O and Sr/Ca values were assigned to March (August), March and August being the average times of highest and lowest SST, respectively, between 1970 and 1997"

integrationTimeUnits: year

mathematicalRelation: linear

rank: 2

scope: isotope

variable: seawaterIsotope

variableGroup: EffectiveMoisture

variableGroupDirection: negative

variableGroupOriginal: d18O_seawater

6

scope: isotope