Non-Linear Clumped Isotopes from DIC Endmember Mixing and Kinetic Isotope Fractionation in High pH Anthropogenic Tufa
Clumped isotope values (Δ47) of carbonates forming in high pH conditions do not correspond to mineral precipitation temperatures due to...
Effects of brine chemistry and polymorphism on clumped isotopes revealed by laboratory precipitation of mono-and multiphase calcium carbonates
Carbonate clumped isotopes are applied to an increasing number of geological archives to address a wide range of Earth science...
Tropical temperature in the Maastrichtian Danish Basin: Data from coccolith Δ47 and δ18O
The Cretaceous Earth, with its greenhouse climate and absence of major ice caps in the polar regions, represents an extreme...
Laboratory calibration of the calcium carbonate clumped isotope thermometer in the 25–250 C temperature range
Many fields of Earth sciences benefit from the knowledge of mineral formation temperatures. For example, carbonates are extensively used for...
InterCarb: A community effort to improve interlaboratory standardization of the carbonate clumped isotope thermometer using carbonate standards
Increased use and improved methodology of carbonate clumped isotope thermometry has greatly enhanced our ability to interrogate a suite of...
Exploring the geological features and processes that control the shape and internal fabrics of late diagenetic dolomite bodies (Lower Khuff equivalent–Central Oman Mountains)
The Lower Permian carbonate rock succession of the Oman Mountains represents a stratigraphical surface analogue for Middle Eastern Lower Khuff...
Impact of dynamic sedimentation on facies heterogeneities in Lower Cretaceous peritidal deposits of central east Oman
This study, based in the Haushi‐Huqf area of central east Oman, aims to characterize the controls on facies distribution and...
Reducing contamination parameters for clumped isotope analysis: The effect of lowering Porapak™ Q trap temperature to below–50 C
Carbonate clumped isotope thermometry examines the thermodynamic preference of 13C–18O bonds to form within the carbonate crystal lattice. The 13C18O16O...
Changing surface ocean circulation caused the local demise of echinoid Scaphechinus mirabilis in Taiwan during the Pleistocene–Holocene transition
Abundant fossil specimens of Scaphechinus mirabilis, now occurring mostly in temperate waters, have been found in the Toukoshan Formation (Pleistocene)...
Chemostratigraphy in Miocene heterozoan carbonate settings: applications, limitations and perspectives
The temporal variability of geochemical proxies can be used in time intervals characterized by global changes in marine chemistry to...