Carbonate minerals contain stable isotopes of carbon and oxygen with different masses
whose abundances and bond arrangement are governed by thermodynamics. The clumped …

Increased use and improved methodology of carbonate clumped isotope thermometry has
greatly enhanced our ability to interrogate a suite of Earth‐system processes. However …

The oxygen isotope compositions of carbonate and phosphatic fossils hold the key to
understanding Earth-system evolution during the last 500 million years. Unfortunately, the …

Carbon (13C) and oxygen (18O) isotopes in carbonates form clumped isotope species
inversely correlated with temperature, providing a valuable paleothermometer for …

The Δ 47 (paleo) thermometer has opened a new avenue to determine carbonate formation
temperatures independent of the oxygen isotopic composition of the fluid from which the …

Analyzing classic 18O/16O ratios in solids, liquids and gases has proven useful in almost
every branch of earth science. As reviewed in this book, additional 17O analysis generally …

Carbonate clumped isotope abundance is an important paleothermometer, but
measurement is difficult, slow, and subject to cardinal mass (m/z) interferences using isotope …

The application of carbonate clumped isotope (Δ 47) thermometry in deep-time is often
limited by modification of the original temperature signal by thermal resetting. New modeling …

The culmination of the glaciers in the European Alps during the Last Glacial Maximum
(LGM) is one of the most intensively studied paleoglaciological events, but its trigger and …

Reconstructing temperatures of ancient oceans is important for understanding Earth's
climate in deep time. Belemnites have been used widely to estimate Mesozoic seawater …