Juillet - Leclerc, A., and G. Schmidt, 2001: A calibration of the oxygen
isotope paleothermometer of coral aragonite from Porites.
Both events were accompanied by warming episodes the U-M-led team found by analyzing the chemical composition of fossil shells using a recently developed technique called the carbonate clumped
isotope paleothermometer.
Unlike previous methods, the clumped
isotope paleothermometer technique does not rely on assumptions about the isotopic composition of seawater.
Not exact matches
The group highlighted the added value of measuring paired coral strontium / calcium ratios (Sr / Ca) and oxygen
isotope ratios (δ18O), two key proxies for sea surface temperature that are often referred to as
paleothermometers (δ18O also reflects sea surface salinity).