Milankovitch cycles are quasi-periodic fluctuations in insolation forced by the variation in
Earth's astronomical parameters. The astronomically induced climate change affected the …

Astronomical insolation forcing is well established as the underlying metronome of
Quaternary ice ages and Cenozoic climate changes. Yet its effects on earlier eras …

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 …

Power plant flue gas and industrial waste gas are produced in large quantities. Using these
as feedstocks for CO2 electroreduction has important practical significance for the treatment …

Understanding the long-term effects of ongoing global environmental change on marine
ecosystems requires a cross-disciplinary approach. Deep-time and recent fossil records can …

Potential temporal and causal connections among various geologic events have long been
discussed in the geological literature. More recently, signs of common periodicities in these …

Abstract The Permian–Triassic mass extinction is characterized by a massive injection of
carbon dioxide associated with Siberian Traps volcanism, pronounced global warming and …

Rapid extensive magmatism may have a profound effect on global climate by liberating and
releasing greenhouse gases to the atmosphere through contact metamorphism of …

Earth is the only planet known to be habitable, and is also unique with its liquid water, and
the operation of plate tectonics. The geological record shows that the habitability of our …

Abstract The Permian-Triassic Mass Extinction (PTME) is the greatest biotic crisis of the
Phanerozoic. In terrestrial settings, the PTME appears to have been diachronous and it has …