The clumped isotopic composition of carbonate‐derived CO2 (denoted Δ47) is a function of
carbonate formation temperature and in natural samples can act as a recorder of …

Carbonate clumped isotope thermometry is based on the temperature-dependent formation
of 13 C 18 O 16 O 2 2− ion groups within the lattice of solid carbonate minerals. At low …

Natural dolomites exhibit a wide range of compositional and structural characteristics with
respect to the amount and positions of calcium and magnesium cations within the crystal …

Various geochemical proxies are used to constrain the diagenetic origin and evolution of
ancient dolomites. Dolomite stoichiometry (mole% MgCO3) and cation ordering, two …

Carbonate clumped isotopes offer a potentially transformational tool to interpret Earth's
history, but the proxy is still limited by poor interlaboratory reproducibility. Here, we focus on …

Dolomite is a very common carbonate mineral in ancient sediments, but is rarely found in
modern environments. Because of the difficulties in precipitating dolomite in the laboratory at …

This work focuses on an exceptionally complex natural laboratory, the Triassic Latemar
isolated platform in the Dolomite Mountains of northern Italy. It explores spatial and temporal …

Much debate exists on the extent to which early dolomites recrystallize and preserve the
signature of their primary diagenetic setting. Here, we combine clumped isotopes …

The application of clumped isotopes (Δ 47) in carbonate minerals as a sensitive temperature
proxy in paleo-environments depends on a well-constrained clumped isotope fractionation …

The topographic history of mountain belts reflects changes in lithospheric structure and
rheology and exerts an influence on climate. Although substantial progress has been made …