SP10WINZ - v1.0.6

Dataset Id: lY1tFahUrvVpsY4Ws5D7

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R code to load dataset:

L <- lipdR::readLipd("https://lipdverse.org/data/lY1tFahUrvVpsY4Ws5D7/1_0_6/SP10WINZ.lpd")

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In compilations: (only most recent versions are shown)

iso2k-1_1_2

root

archiveType: Speleothem

originalDataUrl: https://www.ncdc.noaa.gov/paleo/study/9792

lipdVersion: 1.3

pub
pub1

author: list(name = "Williams, PW")

doi: 10.5038/1827-806X.39.2.5

pub2

author: list(name = "Williams, P.W. , King, D.N.T., Zhao, J.-X., Collerson, K.D.")

doi: 10.1016/j.epsl.2004.10.024

geo

latitude: -42

longitude: 172

siteName: South Island Composite Record, New Zealand

PaleoData columns
year (yr AD)

TSid: MAT2a587a2727_iso2k

variableName: year

units: yr AD

description: Year AD

d18O (permil)

TSid: SP10WINZ01A_d18O_corr_iso2k

variableName: d18O

units: permil

description: carbonate

interpretation
1

scope: climate

variable: precipitation

variableDetail: Monsoon strength

variableGroup: P

variableOriginal: Precipitation_amount

2

scope: climate

3

scope: climate

4

coefficient: NA

direction: positive

equilibriumEvidence: Samples pass the Hendy test

fraction: 0.97

inferredMaterial: groundwater d18O

integrationTime: average 41

integrationTimeUncertainty: not said, but ages were determined by TIMS or alpha-counting (info from Williams et al., 2005)

integrationTimeUnits: years

rank: NA

scope: isotope

seasonality: Annual

variable: precipitationIsotope

variableGroup: P_isotope

variableGroupDirection: positive

5

coefficient: NA

equilibriumEvidence: Samples pass the Hendy test

fraction: NA

inferredMaterial: groundwater d18O

integrationTime: average 41

integrationTimeUncertainty: not said, but ages were determined by TIMS or alpha-counting (info from Williams et al., 2005)

integrationTimeUnits: years

rank: 2

scope: isotope

seasonality: Annual

seasonalityOriginal: Annual

6

coefficient: NA

fraction: NA

rank: NA

scope: isotope

d13C (permil)

TSid: SP10WINZ01A_d13C_iso2k

variableName: d13C

units: permil

description: carbonate

interpretation
1

scope: climate

2

scope: climate

3

scope: climate

4

coefficient: NA

fraction: NA

rank: NA

scope: isotope

variable: C3C4Ratio

variableGroup: composition C3-C4 plants

5

coefficient: NA

fraction: NA

rank: NA

scope: isotope

6

coefficient: NA

fraction: NA

rank: NA

scope: isotope

d18O (permil)

TSid: SP10WINZ01A_iso2k

variableName: d18O

units: permil

description: carbonate

interpretation
1

basis: Evident relationship of speleothem ?18O and temperature, which is generally positive (Williams et al. 2004, 2005, Whittaker 2008). It is probable that significant changes to d18Op would have resulted from perturbations in oceanic and atmospheric circulation patterns that altered the relative mix of vapour from subtropical and sub-Antarctic sources

interpDirection: positive

scope: climate

seasonality: Annual

seasonalityOriginal: Annual

variable: temperature

variableDetail: Changes in annual temperature modulated by oceanic circulation and gradients

variableGroup: Temperature

variableGroupDirection: negative

variableGroupOriginal: T

variableOriginal: Temperature

2

scope: climate

3

scope: climate

4

basis: There is a presend-day positive relationship between ?18O of precipitation and temperature of +0.35? / i¿½C.,Calculations with dripwater d18O values and calcite d18O values,,1 to 10,lamina counting, high resolution sampling to 100 microns,temperature,,year,,,,,,rainfall amount and source,,,,,,,,,,,,,https://docs.google.com/spreadsheets/d/1WNzh05-BveXAV0WvY6duO7iRR_drkRSgmosDu0BBmyU

coefficient: NA

direction: positive

equilibriumEvidence: Samples pass the Hendy test

fraction: NA

inferredMaterial: groundwater d18O

integrationTime: average 41

integrationTimeUncertainty: not said, but ages were determined by TIMS or alpha-counting (info from Williams et al., 2005)

integrationTimeUnits: years

rank: NA

scope: isotope

variable: precipitationIsotope

variableGroup: P_isotope

variableGroupDirection: positive

5

coefficient: NA

direction: negative

equilibriumEvidence: Samples pass the Hendy test

fraction: NA

inferredMaterial: groundwater d18O

integrationTime: average 41

integrationTimeUncertainty: not said, but ages were determined by TIMS or alpha-counting (info from Williams et al., 2005)

integrationTimeUnits: years

rank: NA

scope: isotope

variable: temperature

variableGroup: Temperature

variableGroupDirection: negative

variableGroupOriginal: Temperature_air

6

coefficient: NA

fraction: NA

rank: NA

scope: isotope