Regional-scale paleofluid system across the Tuscan Nappe–Umbria–Marche Apennine Ridge (northern Apennines) as revealed by mesostructural and isotopic analyses of stylolite–vein …
We report the results of a multiproxy study that combines structural analysis of a fracture–stylolite network and isotopic characterization of...
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...
Phosphogenesis and organic-carbon preservation in the Miocene Monterey Formation at Naples Beach, California—The Monterey hypothesis revisited
The middle part of the Miocene Monterey Formation at Naples Beach, west of Santa Barbara, California, is predominantly composed of...
The clumped (13C18O) isotope composition of echinoid calcite: Further evidence for “vital effects” in the clumped isotope proxy
Carbonate clumped isotope thermometry is based on the thermodynamically dependent relative abundance of 13Csingle bond18O bonds (quantified as Δ47) within...