The Paleocene–Eocene Thermal Maximum (PETM, approx. 56 Ma) provides a test case for
investigating how the Earth system responds to rapid greenhouse gas-driven warming …

On geological time-scales, the production and degree of recycling of biogenic carbon in the
marine realm and ultimately its removal to sediments, exerts a dominant control on …

Carbon release rates from anthropogenic sources reached a record high of∼ 10 Pg C yr− 1
in 2014. Geologic analogues from past transient climate changes could provide invaluable …

As an episode of rapid global warming associated with the release of massive quantities of
carbon to the atmosphere and oceans, the Paleocene–Eocene Thermal Maximum (PETM,∼ …

Abstract Knowledge of the onset duration of the Paleocene-Eocene Thermal Maximum—the
largest known greenhouse-gas-driven global warming event of the Cenozoic—is central to …

The links between the Siberian Traps and the end-Permian mass extinction, and between
the North Atlantic igneous province (NAIP) and the Paleocene–Eocene thermal maximum …

The composition and distribution of deep-sea sediments is the result of a multitude of
climatic, biotic and oceanic conditions relating to biogeochemical cycles and environmental …

A transect of paleoshelf cores from Maryland and New Jersey contains an~ 0.19‐to 1.61‐m‐
thick interval with reduced percentages of carbonate during the onset of the Paleocene …

Since preindustrial times, as atmospheric CO2 concentration increases, the ocean
continuously absorbs anthropogenic CO2, reducing seawater pH and [CO 3 2−], which is …

Geological heritage is an important resource for socio-economic development of Egypt, and,
thus, it requires careful exploration. Potentially unique geological features available in Luxor …