Carbonate minerals contain stable isotopes of carbon and oxygen with different masses
whose abundances and bond arrangement are governed by thermodynamics. The clumped …

Soil carbonates are important paleoclimate archives, but interpretations of their isotopic
compositions (δ 18 O, δ 13 C, and Δ 47) are hampered by uncertainty in the annual timing of …

The geological record encodes the relationship between climate and atmospheric carbon
dioxide (CO2) over long and short timescales, as well as potential drivers of evolutionary …

Local meteoric water lines (LMWLs) represent the site‐specific long‐term covariation of
hydrogen and oxygen stable isotope ratios. LMWLs have practical utility as a hydrologic …

The stable isotopic composition of pedogenic carbonates is central to many studies of past
climate and topography, providing a basis for our understanding of Earth's terrestrial history …

Carbon sequestration with amendments in blue-green infrastructure soils could off-set
anthropogenic greenhouse gas emissions to alleviate climate change. In this 3-year study …

To assess how chemical weathering processes in large high-relief river systems respond to
climatic variability, we studied seasonal changes in radiogenic strontium (87 Sr/86 Sr) and …

In the arid landscape south of the Grand Canyon, natural springs and seeps are a critical
resource for endemic species and Native American tribes. Groundwater is potentially …

Carbon and oxygen isotope values of ancient pedogenic carbonates reflect the
paleoenvironmental conditions under which the carbonates formed. Carbon isotope values …

The pedogenic carbonates found in Pleistocene units of the coastal Brazilian Pampa,
informally designated as 'Caliche Cordão', include rhizocretions, soft masses and isolated or …