Large-scale magmatic events like the emplacement of the North Atlantic Igneous Province
(NAIP) are often coincident with periods of extreme climate change such as the Palaeocene …

Body size plays a critical role in mammalian ecology and physiology. Previous research has
shown that many mammals became smaller during the Paleocene-Eocene Thermal …

A hallmark of the rapid and massive release of carbon during the Palaeocene–Eocene
Thermal Maximum is the global negative carbon isotope excursion. The delayed recovery of …

Over the next few centuries, with unabated emissions of anthropogenic carbon dioxide
(CO2), a total of 5000 Pg C may enter the atmosphere, causing CO2 concentrations to rise to …

Abstract The Paleocene-Eocene Thermal Maximum (PETM) offers an excellent opportunity
to study the ecological and environmental responses to global warming. Discussing the so …

A perturbation of the carbon cycle and biosphere, linked to globally increased temperatures
about 55.9 million years ago, characterized the Palaeocene–Eocene Thermal Maximum. Its …

Geologically rapid global warming occurred during the Paleocene–Eocene Thermal
Maximum (PETM)~ 56Ma. Several studies have argued that important changes occurred in …

The Paleogene records the most prominent global climate change of the Cenozoic Era with
a shift from a greenhouse to an icehouse world. Several transient hyperthermal events …

Abstract Large Igneous Provinces (LIPs) are associated with the largest climate
perturbations in Earth's history. The North Atlantic Igneous Province (NAIP) and Paleocene …

• Premise of the study: The fossil record provides information about the long‐term response
of plants to CO2‐induced climate change. The Paleocene‐Eocene Thermal Maximum …