Download LiPD file without ensemble tables
Download LiPD file as JSON-LD (no ensemble data)
Download LiPD file with ensemble data
L <- lipdR::readLipd("https://lipdverse.org/data/v949j4zAPMiid0ZfKCP8/1_0_7/CO17MUMA.lpd")Report an issue (include datasetId and version)
In compilations: (only most recent versions are shown)
iso2k-1_1_0
archiveType: Coral
originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/24630
lipdVersion: 1.3
journal: Geophysical Research Letters
volume: 44
pages: 11,967-11,975
title: Climatic Influences on Southern Makassar Strait Salinity Over the Past Century
doi: 10.1002/2017GL075504
agency: National Research Foundation Singapore
grant: NRFF-2012-03
country: Singapore
agency: National Oceanic and Atmospheric Administration, Division of Climate Observations, U.S. Department of Commerce
grant: UCAR-Z15-17551
country: USA
latitude: -5.382
longitude: 117.914
elevation: -5
siteName: Doangdoangan Besar
country: Indonesia
TSid: WEBe4f13d8f
variableName: year
units: yr AD
rank: NA
scope: climate
rank: NA
scope: climate
TSid: WEB4d49a073
variableName: d18O
units: permil
description: carbonate
scope: climate
scope: climate
scope: climate
basis: Authors calculated the contribution of SST to the δ18Ocoral signal, using a δ18O-SST slope of 0.18‰/°C (Gagan et al., 1998) and a range of published δ18O-SSS slopes (Moore, 1995; Fairbanks et al., 1997; Gorman et al., 2012; Morimoto et al., 2002; Conroy et al., 2017; Table S1 and supporting information text). They estimate that SST has a 29–39% influence on the δ18Ocoral, supporting that SSS drives the δ18Ocoral signal. Authors therefore used seasonal SSS tie points to develop the age model.
direction: positive
scope: isotope
seasonality: subannual
variable: seawaterIsotope
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: d18O_seawater
direction: negative
scope: isotope
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
scope: isotope
TSid: WEBd1b38fb7
variableName: year
units: yr AD
rank: NA
scope: climate
rank: NA
scope: climate
TSid: WEB1a9fc096
variableName: d18O
units: permil
description: carbonate
scope: climate
scope: climate
scope: climate
basis: Authors calculated the contribution of SST to the δ18Ocoral signal, using a δ18O-SST slope of 0.18‰/°C (Gagan et al., 1998) and a range of published δ18O-SSS slopes (Moore, 1995; Fairbanks et al., 1997; Gorman et al., 2012; Morimoto et al., 2002; Conroy et al., 2017; Table S1 and supporting information text). They estimate that SST has a 29–39% influence on the δ18Ocoral, supporting that SSS drives the δ18Ocoral signal. Authors therefore used seasonal SSS tie points to develop the age model.
direction: positive
rank: 1
scope: isotope
seasonality: subannual
variable: seawaterIsotope
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: d18O_seawater
direction: negative
rank: 2
scope: isotope
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
scope: isotope
root
pub
pub1
funding
funding1
funding2
geo
PaleoData columns
year (yr AD) [1-1]
interpretation
1
2
d18O (permil) [1-1]
interpretation
1
2
3
4
5
6
year (yr AD) [1-2]
interpretation
1
2
d18O (permil) [1-2]
interpretation
1
2
3
4
5
6