BACKGROUND Anthropogenic emissions are rapidly altering Earth's climate, pushing it toward a warmer state for which there is no historical precedent. Although no perfect analog …
It is unequivocal that the increases in atmospheric carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) since the pre-industrial period are caused by human activities. The …
The cause of the end-Cretaceous mass extinction is vigorously debated, owing to the occurrence of a very large bolide impact and flood basalt volcanism near the boundary …
The Paleocene–Eocene Thermal Maximum (PETM; 56 Ma) is one of our best geological analogs for understanding climate dynamics in a “greenhouse” world. However, proxy data …
Abstract The Palaeocene–Eocene Thermal Maximum,(PETM) was a global warming event that occurred about 56 million years ago, and is commonly thought to have been driven …
The early Earth's environment is controversial. Climatic estimates range from hot to glacial, and inferred marine pH spans strongly alkaline to acidic. Better understanding of early …
Ocean ecosystems have responded and will continue to respond to climate changes of different rates, magnitudes, and durations (virtually certain). Human societies depend on …
The Paleocene-Eocene Thermal Maximum (PETM;~ 55.9 Ma) was a geologically rapid warming period associated with carbon release, which caused a marked increase in the …
The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …