L <- lipdR::readLipd("https://lipdverse.org/data/hoNIMzXkyb2OxhlM7tD3/1_0_6/CO06DATZ.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/10808
lipdVersion: 1.3
dataContributor: JZ
author: list(name = "Damassa, T.D.")
citeKey: damassa2006enhanced
journal: Paleoceanography
volume: 21
pages: n/a-n/a
title: Enhanced multidecadal climate variability in the seventeenth century from coral isotope records in the western Indian Ocean
doi: 10.1029/2005PA001217
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-IndianMafiaDamassa2006
doi: 10.1002/2014PA002717
latitude: -8.0167
longitude: 39.5
elevation: -6
siteName: Mafia Archipelago, Tanzania
pages2kRegion: Ocean
TSid: MATab972076e1
variableName: year
units: yr AD
description: Year AD
fraction: NA
rank: NA
scope: climate
fraction: NA
rank: NA
scope: climate
rank: NA
scope: climate
fraction: NA
rank: NA
scope: climate
rank: NA
scope: climate
TSid: Ocean2kHR_007_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: The coral captures approximately 60% of the full range of annual SST (4i¿½C = 0.88%).
coefficient: NA
direction: negative
fraction: 0.6
inferredMaterial: seawater
integrationTime: 1 to 2
integrationTimeBasis: chronology constructed using seasonal cycles in d18O as well as density couplets in xrays. "we assigned the most enriched value of d18O in each cycle to consecutive Augusts (the average coldest month) down core. We inter- polated linearly between age-assigned d18O data points (sequential Augusts) to assign intra-annual ages, using programs in the ARAND software package (available at http://www.ncdc.noaa.gov/paleo/softlib/arand/arand.html) (P. Howell, personal communication, 1998). "
integrationTimeUncertainty: 1 yr
integrationTimeUncertaintyType: chronological
integrationTimeUnits: months
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: subannual
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 1 to 2
integrationTimeBasis: chronology constructed using seasonal cycles in d18O as well as density couplets in xrays. "we assigned the most enriched value of d18O in each cycle to consecutive Augusts (the average coldest month) down core. We inter- polated linearly between age-assigned d18O data points (sequential Augusts) to assign intra-annual ages, using programs in the ARAND software package (available at http://www.ncdc.noaa.gov/paleo/softlib/arand/arand.html) (P. Howell, personal communication, 1998). "
integrationTimeUncertainty: 1 yr
integrationTimeUncertaintyType: chronological
integrationTimeUnits: months
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