L <- lipdR::readLipd("https://lipdverse.org/data/4Zn8Y4l0vbrkiQiQJkeC/1_0_5/CO14ZIHO.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/16316
lipdVersion: 1.3
dataContributor: JZ
author: list(name = "Zinke, J. , Rountrey, A. , Feng, M. , Xie, S.-P. , Dissard, D. , Rankenburg, K. , Lough, J.M. , McCulloch, M.T.")
citeKey: zinke2014corals
journal: Nature Communications
volume: 5
title: Corals record long-term Leeuwin current variability including Ningaloo Ni�o/Ni�a since 1795
doi: 10.1038/ncomms4607
title: Ocean2kHR-IndianAbrolhosZinke2014HAB10A
latitude: -28.4589
longitude: 113.749
elevation: -8
siteName: Houtman Abrolhos
pages2kRegion: Ocean
TSid: MAT91c959899e
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
TSid: Ocean2kHR_026_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
direction: negative
interpDirection: negative
scope: climate
seasonality: Annual
seasonalityOriginal: Annual
variable: temperature
variableDetail: sea@surface
variableDetailOriginal: sea_surface
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T
scope: climate
scope: climate
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: We used the published bimonthly coral d18O record of Kuhnert et al.12 as our reference coral because the presence of seasonal cycles provided the best age control for all cores.The age model of the new corals was determined by assigning 1 year of growth to a couplet of high- and low-density banding in X-ray-positive prints cross-checked with luminescence banding. The high-density bands were equivalent to summer and low density to winter. The coral d18O record of Kuhnert et al. was averaged annually (January?December), and then each individual annually resolved coral proxy record was normalized to its variance relative to the 1900?1993 reference period. We used the COFECHA tool to aid in cross-dating the annual time series. We aligned the new annually resolved Sr/Ca and d18O records (normalized relative to the 1900?1993 reference period) with the Kuhnert et al. annual time series, and averaged all records to form a composite chronology that extends from 1795 to 2010.
integrationTimeUnits: year
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: Annual
seasonalityOriginal: Annual
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: Ocean2kHR_027_iso2k
variableName: Sr/Ca
units: mmol/mol
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
direction: decrease
interpDirection: decrease
scope: climate
seasonality: Annual
seasonalityOriginal: Annual
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)
interpretation
1
d18O (permil)
interpretation
1
2
3
4
5
6
Sr/Ca (mmol/mol)
interpretation
1
2
3
4
5
6