L <- lipdR::readLipd("https://lipdverse.org/data/oIo107DJYmBL1asRONW1/1_0_7/CO03CHBA.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: JZ
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-IndianBaliCharles2003
doi: 10.1002/2014PA002717
latitude: -8.2573
longitude: 115.5757
elevation: -3
siteName: Lombok Strait, Bali, Indonesia
pages2kRegion: Ocean
TSid: MATa9d7e23e53
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_006_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
direction: decrease/increase
interpDirection: decrease/increase
scope: climate
seasonality: subannual
variable: temperature
variableDetail: sea surface
variableGroup: temperature and salinity
scope: climate
scope: climate
basis: in the Indonesian coral records, coral d18O is more heavily infuenced by rainfall variability
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: Chronological assignments for the record were generally straightforward, because of the clear seasonal cycle in d18O and the especially clear expression of annual growth bands. The seasonal extremes were an- chored to April and September of each year
integrationTimeUncertainty: ~1/5
integrationTimeUncertaintyType: chronological
integrationTimeUnits: month
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: subannual
variable: seawaterIsotope
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: d18O_seawater
basis: in the Indonesian coral records, coral d18O is more heavily infuenced by rainfall variability
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: Chronological assignments for the record were generally straightforward, because of the clear seasonal cycle in d18O and the especially clear expression of annual growth bands. The seasonal extremes were an- chored to April and September of each year
integrationTimeUncertainty: ~1/5
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