L <- lipdR::readLipd("https://lipdverse.org/data/873EkNZdP2vfB7zEPWsW/1_0_5/CO05KUBE.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_2
archiveType: Coral
originalDataUrl: http://doi.pangaea.de/10.1594/PANGAEA.738188
lipdVersion: 1.3
dataContributor: KHK, CS
author: list(name = "Kuhnert, Henning , Cruger, Traute , Patzold, Jorgen")
citeKey: kuhnert2005nao
journal: Geochemistry, Geophysics, Geosystems
volume: 6
pages: n/a-n/a
title: NAO signature in a Bermuda coral Sr/Ca record
doi: 10.1029/2004GC000786
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-AtlanticBermudaKuhnert2005
doi: 10.1002/2014PA002717
latitude: 32.467
longitude: -64.7
elevation: -12
siteName: North East Breakers, Bermuda
pages2kRegion: Ocean
TSid: MAT7676220777
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
TSid: Ocean2kHR_105_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
direction: decrease
interpDirection: decrease
scope: climate
seasonality: subannual
variable: temperature
variableDetail: sea@surface
variableDetailOriginal: sea_surface
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T
variableOriginal: temperature
scope: climate
scope: climate
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: The age model for the record is based on the seasonal banding pattern, as seen in the X-radiographs, and the annual cycles in the skeletal geochemistry. To be consistent with earlier work [Kuhnert et al., 2002], we used the cyclicity in d18O (which is not further discussed) rather than that in Sr/Ca (the resulting age models are almost identical). The heaviest value in each annual cycle was assigned to March, which is the coldest month on average; i.e., the chronology uses one tie point per year. Ages for the other sampling points were interpolated according to their positions along the sampling profile. An equidistant (monthly) time series was interpolated from the original Sr/Ca data and was used as the base for further calculations.
integrationTimeUncertaintyType: chronological
integrationTimeUnits: month
rank: 1
scope: isotope
seasonality: subannual
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
TSid: MAT0ca9b639c7
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
TSid: Ocean2kHR_106_iso2k
variableName: Sr/Ca
units: mmol/mol
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
direction: decrease
interpDirection: decrease
scope: climate
seasonality: subannual
variable: temperature
variableDetail: sea@surface
variableDetailOriginal: sea_surface
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T
variableOriginal: temperature
scope: climate
scope: climate
coefficient: NA
fraction: NA
inferredMaterial: seawater
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
coefficient: NA
fraction: NA
rank: NA
scope: isotope
root
pub
pub1
pub2
geo
PaleoData columns
year (yr AD) [1-1]
interpretation
1
d18O (permil) [1-1]
interpretation
1
2
3
4
5
6
year (yr AD) [2-1]
interpretation
1
Sr/Ca (mmol/mol) [2-1]
interpretation
1
2
3
4
5
6