Current understanding of the long-term carbon cycle posits that Earth's climate is stabilized
by a negative feedback involving CO 2 consumption by chemical weathering of silicate …

Flood basalts were Earth's largest volcanic episodes that, along with related intrusions, were
often emplaced rapidly and coincided with environmental disruption: oceanic anoxic events …

The existence of stabilizing feedbacks within Earth's climate system is generally thought to
be necessary for the persistence of liquid water and life. Over the course of Earth's history …

Despite recent advances, the link between the evolution of atmospheric CO2 and climate
during the Eocene greenhouse remains uncertain. In particular, modelling studies suggest …

Massive carbon dioxide (CO2) emissions are widely assumed to be the driver of the end-
Permian mass extinction (EPME). However, the rate of and total CO2 released, and whether …

Abstract The Middle Eocene Climatic Optimum (MECO) was a gradual warming event and
carbon cycle perturbation that occurred between 40.5 and 40.1 Ma. A number of …

Current climate change may induce positive carbon cycle feedbacks that amplify
anthropogenic warming on time scales of centuries to millennia. Similar feedbacks might …

In the wake of rapid CO2 release tied to the emplacement of the Siberian Traps, elevated
temperatures were maintained for over five million years during the end-Permian biotic …

The response of the Earth system to greenhouse-gas-driven warming is of critical
importance for the future trajectory of our planetary environment. Hyperthermal events–past …

Abstract The Palaeocene-Eocene Thermal Maximum (ca. 56 million years ago) offers a
primary analogue for future global warming and carbon cycle recovery. Yet, where and how …