L <- lipdR::readLipd("https://lipdverse.org/data/4eKXrgFThelRgVWLxd0K/1_0_7/CO03CHBU.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/1903
lipdVersion: 1.3
dataContributor: KJA, JET
author: list(name = "Charles, C.D.; Cobb, K.M.; Moore, M.D.; Fairbanks, R.G.")
citeKey: charles2003monsoon
journal: Marine Geology
volume: 201
pages: -15
title: Monsoon?tropical ocean interaction in a network of coral records spanning the 20th century
doi: 10.1016/S0025-3227(03)00217-2
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-PacificBunakenCharles2003
doi: 10.1002/2014PA002717
latitude: -1.5
longitude: 124.833
elevation: -3
siteName: Bunaken Island
pages2kRegion: Ocean
TSid: MAT471a9a9675
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_171_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
basis: The annual variability of the Bunaken coral d18O refects the seasonal cycle of both salinity and temperature in the surrounding seawater
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 annual variability of the Bunaken coral d18O refects the seasonal cycle of both salinity and temperature in the surrounding seawater. The characteristics and correlations of the Bunaken Island coral d18O record strongly suggestthat it monitors the air-sea interaction associatedwith Southeast Asian summer monsoon.
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: anchoring seasonal maxima and minima of the d18O depth series to March and October of each year. Crosschecks on the age assignments were available through examination of the annual growth bands and the strong semi-annual carbon isotope signal
integrationTimeUncertainty: ~1/4
integrationTimeUncertaintyType: chronological
integrationTimeUnits: month
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: subannual
variable: seawaterIsotope
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: d18O_seawater
basis: The annual variability of the Bunaken coral d18O refects the seasonal cycle of both salinity and temperature in the surrounding seawater: "in the Indonesian coral records, coral d18O is more heavily infuenced by rainfall variability." The characteristics and correlations of the Bunaken Island coral d18O record strongly suggestthat it monitors the air-sea interaction associatedwith Southeast Asian summer monsoon.
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: anchoring seasonal maxima and minima of the d18O depth series to March and October of each year. Crosschecks on the age assignments were available through examination of the annual growth bands and the strong semi-annual carbon isotope signal
integrationTimeUncertainty: ~1/4
integrationTimeUncertaintyType: chronological
integrationTimeUnits: month
mathematicalRelation: linear
rank: 2
scope: isotope
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
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