To understand the climate dynamics of hypothesized past greenhouse intervals, it is
essential to constrain tropical sea‐surface temperatures (SST), yet existing proxy records …

This study examines the efficacy of published δ18O data from the calcite of Late Miocene
surface dwelling planktonic foraminifer shells, for sea surface temperature estimates for the …

The possibility exists that the magnitude of Glacial/Holocene δ18O change in the tropical
oceans was previously under‐estimated due to the dampening effect of bioturbation on bulk …

Much of our knowledge of past ocean temperatures comes from the foraminifera Mg/Ca
palaeothermometer. Several nonthermal controls on foraminifera Mg incorporation have …

Reconstruction of past sea surface temperatures (SST) is essential for understanding
processes that have controlled climate change throughout Earth's history. The amplitude of …

Abstract The Paleocene–Eocene Thermal Maximum (PETM), ca. 56 Ma, was a major global
environmental perturbation attributed to a rapid rise in the concentration of greenhouse …

We have used laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) to
measure elemental (Mg/Ca, Al/Ca, Mn/Ca, Zn/Ca, Sr/Ca, and Ba/Ca) ratios of 13 species of …

The Paleocene‐Eocene Boundary (PEB) was marked by an extraordinary climatic event,
hypothesized to originate from a large perturbation to the carbon cycle which fueled global …

The classic paleotemperature record based on δ18O data from pelagic foraminiferal calcite
suggests that equatorial sea-surface temperatures during the Maastrichtian (∼ 12–20° C) …

We have reconstructed mean annual coastal temperatures and seasonality during the
Eocene (Priabonian; 36.6–40 Ma) using oxygen isotope profiles of shallow marine …