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 potential for carbonate clumped isotope thermometry to independently constrain both the
formation temperature of carbonate minerals and fluid oxygen isotope composition allows …

The clumped isotopic composition of carbonate‐derived CO 2 (denoted Δ 47 ) is a function
of carbonate formation temperature and in natural samples can act as a recorder of …

Carbonate clumped isotope (Δ 47 ) thermometry has been applied to a wide range of
problems in earth, ocean and biological sciences over the last decade, but is still plagued by …

We describe an approach to estimating the crystallization temperatures of diagenetic
calcites using clumped-isotope thermometry, a paleothermometer based on the 13 C– 18 O-bond …

Rationale The clumped isotope composition of CO 2 (Δ 47 ) derived from carbonate is widely
used as a paleotemperature proxy with broad applications in geoscience. Its accuracy is, …

Quantifying the timing and temperature of soil carbonate formation is important for interpreting
isotopic records of Earth-surface temperature and soil water composition from paleosols. …

Reconstructing the thermal history of minerals and fluids in continental environments is a
cornerstone of tectonics research. Paleotemperature constraints from carbonate clumped …

Studies of active mountain ranges suggest that atmospheric and geodynamic processes
may be strongly coupled through erosion — a hypothesis that has led to a debate over the …

Global data suggest that erosion rates variously scale with steepness or climate forcing (precipitation
or glacial excavation), but the relative influence of these factors has proven difficult …