L <- lipdR::readLipd("https://lipdverse.org/data/evWoABoM15RbQE7Ktza0/1_0_5/CO10HEIG.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/12893
lipdVersion: 1.3
dataContributor: KHK, CS
author: list(name = "Hetzinger, S. , M. Pfeiffer , W.-C. Dullo , D. Garbe-Schi¿½nberg , J. Halfar")
citeKey: hetzinger2010tropical
journal: Paleoceanography
volume: 30
pages: -26
title: Tropical sea surface temperatures for the past four centuries reconstructed from coral archives
doi: 10.1016/j.palaeo.2010.06.019
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-AtlanticGuadeloupeHetzinger2010
doi: 10.1002/2014PA002717
latitude: 16.2
longitude: -61.49
elevation: -1.7
siteName: Guadeloupe
pages2kRegion: Ocean
TSid: MATc41e7914fd
variableName: year
units: yr AD
description: Year AD
coefficient: NA
fraction: NA
rank: NA
scope: climate
TSid: Ocean2kHR_097_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
basis: Both geochemical proxies show a significant correlation with instrumental SST over a 41-year time period on both monthly and mean annual scales. We obtained proxy-SST calibrations that are consistent with previously published studies using other coral species from different regions. Hetzinger 2006 10.1029/2006GC001347
direction: decrease
interpDirection: decrease
scope: climate
seasonality: subannual
variable: temperature
variableDetail: sea surface
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T
variableOriginal: temperature
scope: climate
scope: climate
basis: Correlation and regression assesed with SODA SST, ERSST V2.0, and local air temperature for 1958-1999 for monthly values, extreme values only (max-min mehtod), and annual mean. ERSST extreme values had the correlation, this could be due to subannual dating uncertaincies and linear interpolation to monthly values. Calibration detailed in Hetzinger 2006, 10.1029/2006GC001347
coefficient: -0.209
direction: negative
fraction: 0.82
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: age model was established on the basis of the pronounced seasonal cycle in the Sr/Ca record. The maximum (minimum) Sr/Ca was tied to March (September), which is on average the coolest (warmest) month in the study area. The coral d18O and Sr/Ca time series were linearly interpolated between these anchor points using the Analyseries software [Paillard et al., 1996] to obtain monthly proxy time series.
integrationTimeUncertainty: ~1?2 months in any given year, no errors given for annual chronology
integrationTimeUncertaintyType: chronological
integrationTimeUnits: month
mathematicalRelation: linear
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: Ocean2kHR_098_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
seasonality: subannual
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