L <- lipdR::readLipd("https://lipdverse.org/data/gWwpc4lJjcaxkSJus9Ge/1_0_7/CO08ABSU.lpd")
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In compilations: (only most recent versions are shown)
iso2k-1_1_2
archiveType: Coral
originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/8607
lipdVersion: 1.3
dataContributor: NJA, Polovodova,Irina
author: list(name = "Abram, N.J., M.K. Gagan, J.E. Cole, W.S. Hantoro, and M. Mudelsee")
citeKey: abram2008recent
journal: Nature Geoscience
volume: 1
pages: -4
title: Recent intensification of tropical climate variability in the Indian Ocean
doi: 10.1038/ngeo357
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-IndianMentawaiAbram2008
doi: 10.1002/2014PA002717
latitude: -0.13
longitude: 98.52
elevation: -6
siteName: Mantawai Islands, West Sumatra, Indonesia
pages2kRegion: Ocean
TSid: MAT8333f8f3fc
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_010_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
basis: IOD upwelling cools the ambient SST and decreases rainfall, both of which increase coral d18O.
direction: decrease/increase
interpDirection: decrease/increase
scope: climate
seasonality: subannual
variable: temperature
variableDetail: sea surface
variableGroup: temperature and salinity
scope: climate
scope: climate
basis: IOD upwelling cools the ambient SST and decreases rainfall, both of which increase coral d18O.
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: annual cycles of d18O, verified using annual growth bands
integrationTimeUncertainty: 1/12-1/6
integrationTimeUncertaintyType: chronological
integrationTimeUnits: month
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: subannual
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
basis: IOD upwelling cools the ambient SST and decreases rainfall, both of which increase coral d18O.
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: annual cycles of d18O, verified using annual growth bands
integrationTimeUncertainty: 1/12-1/6
integrationTimeUncertaintyType: chronological
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
pub1
pub2
geo
PaleoData columns
year (yr AD)
interpretation
1
2
3
4
5
d18O (permil)
interpretation
1
2
3
4
5
6