Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …

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 …

Carbonate mud represents one of the most important geochemical archives for
reconstructing ancient climatic, environmental, and evolutionary change from the rock …

Characterizing past climate states is crucial for understanding the future consequences of
ongoing greenhouse gas emissions. Here, we revisit the benchmark time series for deep …

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 …

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

Marine sedimentary ikaite is the parent mineral to glendonite, stellate pseudomorphs found
throughout the geological record which are most usually composed of calcite. Ikaite is …

Least-squares regression methods are mathematically powerful, conceptually and
computationally simple, and widely used in many fields. However, none of the commonly …

In parallel with pronounced cooling in the oceans, vast areas of the continents experienced
enhanced aridification and restructuring of vegetation and animal communities during the …