d18O_c()
calculates the equilibrium d18O value of a carbonate grown
at a given temperature.
Arguments
- temp
Carbonate growth temperature (°C).
- d18O_H2O_VSMOW
Water d18O value expressed on the VSMOW scale (‰).
- min
Mineralogy. Options are as in
a18_c_H2O()
.- eq
Equation used for the calculations. Options depend on mineralogy and are listed in
a18_c_H2O()
.
Note
Use to_VSMOW()
and to_VPDB()
to convert
between the VSMOW and VPDB scales.
References
References are listed in the description of a18_c_H2O()
.
See also
d18O_H2O()
calculates the d18O value of the ambient water
from the d18O value of a carbonate and its growth temperature.
Examples
d18O_c(33.7, -13.54, min = "calcite", eq = "Coplen07")
#> [1] 14.57797
to_VPDB(d18O_c(temp = 12, d18O_H2O_VSMOW = -6.94,
min = "aragonite", eq = "GK86"))
#> [1] -5.212518