Clumped-isotope evidence for the formation of nonplanar dolomite textures at near-surface temperatures—Reply

Clumped-isotope evidence for the formation of nonplanar dolomite textures at near-surface temperatures

A tropically hot mid-Cretaceous North American Western Interior Seaway

Looking upstream with clumped and triple oxygen isotopes of estuarine oyster shells in the early Eocene of California, USA

Subannual stable isotope records reveal climate warming and seasonal anoxia associated with two extinction intervals across the Cretaceous-Paleogene boundary on Seymour Island, Antarctica

Isotope sclerochronology indicates enhanced seasonal precipitation in northern South America (Colombia) during the Mid-Miocene Climatic Optimum

Calcium isotope evidence for environmental variability before and across the Cretaceous-Paleogene mass extinction

Temperature and salinity of the Late Cretaceous Western Interior Seaway