d18OcFromd18OwTemp: Equilibrium d18O of calcification from d18Ow and Temperature...

Description Usage Arguments Value References See Also Examples

View source: R/d18O-calibration.R

Description

The paleotemperature equation of O’Neil et al. (1969) and Shackleton (1974). The factor 0.27 was used to convert from water on the SMOW scale to calcite on the Peedee Belemnite (PDB) scale.

As described in Anand et al. 2003

Usage

1
d18OcFromd18OwTemp(d18Ow, Temp)

Arguments

d18Ow

d18O of seawater

Temp

Temperature in celcius

Value

d18O of calcite on PDB scale

References

O’Neil, J. R., R. N. Clayton, and T. K. Mayeda, Oxygen isotope fractionation in divalent metal carbonates, 51, 5547– 5558, 1969.

Shackleton, N. J., Attainment of isotopic equilibrium between ocean water and the benthonic foraminiferal genus Uvigerina: Isotopic changes in the ocean during the last glacial, Cent. Natl. Rech. Sci. Colloq. Int., 219, 203–209, 1974.

See Also

d18OwFromSalinity CalcifTemp

Examples

1
d18OcFromd18OwTemp(d18Ow = 0.6, 1:26)

EarthSystemDiagnostics/ecustools documentation built on Jan. 15, 2022, 5:22 p.m.