L <- lipdR::readLipd("https://lipdverse.org/data/IhzvxKV8k4KmLBwQ6wW1/1_0_7/CO06MOTO.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/1924
lipdVersion: 1.3
dataContributor: KHK, Hong Yan
author: list(name = "Moses, C.S. , P.K. Swart")
citeKey: moses2006stable
journal: Proceedings of the 10th International Coral Reef Symposium (Okinawa)
pages: -7
title: Stable isotope and growth records in corals from the island of Tobago: Not simply a record of the Orinoco
doi: {moses2006stable}
author: list(name = "Moses, C.S.")
title: Ocean2kHR-AtlanticTobagoMoses2006Sidereastrea
latitude: 11.17
longitude: -60.85
elevation: -2
siteName: Buccoo Reef, Tobago
pages2kRegion: Ocean
TSid: MAT6eb9e56a45
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
TSid: Ocean2kHR_108_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
basis: The average interannual ?18O variability at Tobago represents a ?SST of ~1.0i¿½C from one year to the next, about 3.5 times the instrumental ?SST value. This disagreement implies that there are significant interannual changes in salinity responsible for the ?18O of the corals from Tobago.
direction: decrease/increase
interpDirection: decrease/increase
scope: climate
seasonality: Annual
seasonalityOriginal: Annual
variable: temperature
variableDetail: sea surface
variableGroup: temperature and salinity
scope: climate
scope: climate
basis: The average interannual ?18O variability at Tobago represents a ?SST of ~1.0i¿½C from one year to the next, about 3.5 times the instrumental ?SST value. This disagreement implies that there are significant interannual changes in salinity responsible for the ?18O of the corals from Tobago.
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: Annual extension rates based on sclerochronology were measured on X-radiograph positive prints from the beginning of one high-density band to the beginning of the next
integrationTimeUnits: year
mathematicalRelation: linear
rank: 2
scope: isotope
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
basis: The average interannual ?18O variability at Tobago represents a ?SST of ~1.0i¿½C from one year to the next, about 3.5 times the instrumental ?SST value. This disagreement implies that there are significant interannual changes in salinity responsible for the ?18O of the corals from Tobago.
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 1
integrationTimeBasis: Annual extension rates based on sclerochronology were measured on X-radiograph positive prints from the beginning of one high-density band to the beginning of the next
integrationTimeUnits: year
mathematicalRelation: linear
rank: 1
scope: isotope
variable: seawaterIsotope
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: d18O_seawater
coefficient: NA
fraction: NA
rank: NA
scope: isotope
TSid: Ocean2kHR_109_iso2k
variableName: d13C
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: FALSE
rank: NA
scope: climate
rank: NA
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
TSid: MATb8f69d72c7
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
TSid: Ocean2kHR_110_iso2k
variableName: d18O
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: TRUE
basis: The average interannual ?18O variability at Tobago represents a ?SST of ~1.0i¿½C from one year to the next, about 3.5 times the instrumental ?SST value. This disagreement implies that there are significant interannual changes in salinity responsible for the ?18O of the corals from Tobago.
direction: decrease/increase
interpDirection: decrease/increase
scope: climate
seasonality: Annual
seasonalityOriginal: Annual
variable: temperature
variableDetail: sea surface
variableGroup: temperature and salinity
scope: climate
scope: climate
basis: The average interannual d18O variability at Tobago represents a SST of ~1.0C from one year to the next, about 3.5 times the instrumental deltaSST value. This disagreement implies that there are significant interannual changes in salinity responsible for the d18O of the corals from Tobago.
coefficient: NA
direction: positive
fraction: NA
inferredMaterial: seawater
integrationTime: 2
integrationTimeBasis: Annual extension rates based on sclerochronology were measured on X-radiograph positive prints from the beginning of one high-density band to the beginning of the next
integrationTimeUnits: year
mathematicalRelation: linear
rank: 1
scope: isotope
seasonality: subannual
variable: seawaterIsotope
variableGroup: EffectiveMoisture
variableGroupDirection: negative
variableGroupOriginal: d18O_seawater
basis: The average interannual d18O variability at Tobago represents a SST of ~1.0C from one year to the next, about 3.5 times the instrumental deltaSST value. This disagreement implies that there are significant interannual changes in salinity responsible for the d18O of the corals from Tobago.
coefficient: NA
direction: negative
fraction: NA
inferredMaterial: seawater
integrationTime: 2
integrationTimeBasis: Annual extension rates based on sclerochronology were measured on X-radiograph positive prints from the beginning of one high-density band to the beginning of the next
integrationTimeUnits: year
mathematicalRelation: linear
rank: 2
scope: isotope
variable: temperature
variableGroup: Temperature
variableGroupDirection: negative
variableGroupOriginal: T_water
coefficient: NA
fraction: NA
rank: NA
scope: isotope
TSid: MAT72369a5b39
variableName: year
units: yr AD
description: Year AD
rank: NA
scope: climate
rank: NA
scope: climate
TSid: Ocean2kHR_111_iso2k
variableName: d13C
units: permil
description: carbonate
useInGlobalTemperatureAnalysis: FALSE
rank: NA
scope: climate
rank: NA
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
2
d18O (permil) [1-1]
interpretation
1
2
3
4
5
6
d13C (permil) [1-1]
interpretation
1
2
3
4
5
6
year (yr AD) [2-1]
interpretation
1
2
d18O (permil) [2-1]
interpretation
1
2
3
4
5
6
year (yr AD) [3-1]
interpretation
1
2
d13C (permil) [3-1]
interpretation
1
2
3
4
5
6