D47()
calculates the equilibrium carbonate D47 value
for a given temperature.
Arguments
- temp
Carbonate growth temperature (°C).
- eq
Equation used for the calculation.
"Petersen19"
: the synthetic-only composite IUPAC-parameter calibration of Petersen et al. (2019)."Anderson21"
: the I-CDES90 calibration of Anderson et al. (2021)."Fiebig21"
: the CDES90 calibration of Fiebig et al. (2021).
Details
"Petersen19":
$$\Delta_{47, CDES90} = 0.0383 \times \frac{10^{6}}{T^{2}} + 0.170$$
"Anderson21":
$$\Delta_{47, I-CDES90} = 0.0391 \times \frac{10^{6}}{T^{2}} + 0.154$$
"Fiebig21":
$$\Delta_{47, CDES90} = 1.038 \times (-5.897 \times \frac{1}{T} - 3.521 \times \frac{10^{3}}{T^{2}} + 2.391 \times \frac{10^{7}}{T^{3}} - 3.541 \times \frac{10^{9}}{T^{4}}) + 0.1856$$
References
Petersen, S. V., Defliese, W. F., Saenger, C., Daëron, M., Huntington, K. W., John, C. M., et al. (2019). Effects of improved 17O correction on interlaboratory agreement in clumped isotope calibrations, estimates of mineral-specific offsets, and temperature dependence of acid digestion fractionation. Geochemistry, Geophysics, Geosystems, 20(7), 3495-3519. doi:10.1029/2018GC008127
Anderson, N. T., Kelson, J. R., Kele, S., Daëron, M., Bonifacie, M., Horita, J., et al. (2021). A unified clumped isotope thermometer calibration (0.5-1100°C) using carbonate-based standardization. Geophysical Research Letters, 48(7), e2020GL092069. doi:10.1029/2020gl092069
Fiebig, J., Daëron, M., Bernecker, M., Guo, W., Schneider, G., Boch, R., et al. (2021). Calibration of the dual clumped isotope thermometer for carbonates. Geochimica et Cosmochimica Acta. doi:10.1016/j.gca.2021.07.012
See also
temp_D47()
calculates growth temperature from a D47 value.